«%Kc Dp itt::iitii.,...^ ,, Soiitb :3liWi llssdclaiion fo. tbc ;.•,>, .:V., •.•;:'., Advancement . :•;':'•'.■,* Vr;*;^-Vs;V' . ,. ■ ' "■ .'^'•V/•^^''^^v.',•'.^v.«.'!,',>■,•,v.^'•V••■ •■■•'■ I' .■ Wi:>>^^t' ..;Mvr;:'^^^'n'^^ : '^v 'i v:;; ^:v v?v V ''^{fMii^MW: ■)^y\Qj^}^}is':. REPORT OF THE SIXTEENTH ANNUAL MEETING OF THE South African Association FOR THE ADVANCEiMEMT OF SCIENCE. JOHANNESBURG, 1918. JULY 8-13- CAPE TOWN : PUBLISHED BY THK ASSOCIATION. 1919. ' ■ IBR ARY ■ CONTENTS.-\ '*'•'*' /O PAG*. Officers, anh Cooncil i Tables : Past Annual MfefeTiNos ; — Places and Dates, Presidents. \ ice-Presidents, and Local Secretaries ii Sectional Presidents and Secretaries iV Evening Discourses viii JOHANNESBURG MEETING, 1918:— General Meetings ix Officers of Local and Sectional Committees x Proceedings of Sixteenth Annual General Meeting of Members xiv Report of Council, 1917-18 xviii General Treasurer's Account. 191 7- 18 xxiii Eleventh Award of the South Africa ^fedal (Plate i) xxVii Association Library xxx Address by the President hf the Association: Dr. C. F. Juritz, ' M.A., F.LC I Address by the President of Section A : Prof. J. T. Morrison, - M..A., B.Sc. F.R.S.E 31 Address by the President of Section B : P. .A. Wagner, B.Sc, Ing.D , ... 45 Address by the President of Section C: C. E. Lecat, B.Sc. ... 70 Address by the President of Section D : Prof. E. T. Goddard, B.A., D.Sc ... ... lOb .\ddress by the President of Section E : Rev. W. A. Norton, B.A.. B.Litt 107 Address by the President of Section F. : Prof. T. M. Forsyth. M.A., D.Phil 121 List of papers read at the Sectional Meetings .... ... ... 135 The desiccation of Africa : the cause and the remedy : Prof. F. IL L. ScHWARz, A.R.C.S.. F.G S 130 Uses of Mirahilis jalapa 190 Roval Society of South Africa 190 The medicine man in Natal and Zululand : Hon. Mr. Justice C. G. Jackson ... ... ... i0i Safety in winding operations : J. A. VaUghan, M-LCE., M.l.Mech.E. 265 .\tmospheric nitrogen 216 The world's wheat crops 216 Research grants 216 The medicinal springs of South Africa : supplement T : Prof. M. M. RiNDL, Ing.D 217 Solar bombs 225 A note on the flora of the Great Winterhoek Range: E. P. Phillips. M.A., D.Sc, F.L.S 226 The natives of Natal in relation to the land : M. S. Evans, C.M.G.. F.Z.S 235 Stellar distances and magnitudes 246 Some results of ostrich investigations: Prof. J. E. Duerden. M.Sc. Ph.D., A.R.C.S. (Plates 2-5 and four text figures') 247 The electro-magnetic theorv of light 285 Evolution and mankind: Prof. H. B. Fantham. M.A., D.Sc ... 287 The Zulu witch doctor and medicine-man : J. B. McCord, M.R.C.S.. L.R.C.P 306 Botanical survey • 3i| Electrical conductivity of milk 3i8 Suggestions towards a better provision for. the medical needs of the natives : C. T. Loram, M.A.. LL.B.. Ph.D 3I§ Epidemic catarrhal fever .• ... 3*4 32476 IV CONTENTS. PAGF.. On the persistence of arsenite of soda in tlie ?oil : C. W. Mau.v. M.Sc, F.L.S., F.E.S. ... ,_,„. 3^5 Mova Aquilce 329 The ethical principle of equity: Rev. S. R. Wfxch, B.A„ D.D.. Ph.P. 33^> CheraicaJ warfare service 23A Leucocytogregarines. and their occurrence in South Africa: A.vnie Porter, D.Sc, F.L.S. i Abstract ) ... ... 335 Stellar catastrophes ...... ... 336 Soxne parasitic protozoa found in South .Vfricah fishes and aniplri- • bians: Prof. H. B. F.s vth.\m. M.A., i.XSc. F.Z.S. {Abstracl) ... 33; South .\frican Coccida- s^'f'. Does it pay to educate the native?: Rev. A. E. Le Rov, B..\., P>.1). 330 The determination of phosphoric oxide, particularly in fertilisers. soil extracts, and the like: B. dk C. M.vkch.nnd, B.A., D.Sc... 3^7 Alligators as food 363 The diagnostic characters of some superlicial tunyi : lvrTii;.i M. DoiDGE, M.A.. D.Sc. F.L.S 364 Vaccine prophylaxis in intluenza .36S Behaviour of bacteria towards arsenic: H. H. Green. D.Sc., and N. H. Kestfili.. B.A 369 Paper from Megass 374 .Some South African snails and the cercariie which attack tlieni : F. G. C.vwsTo.v. B.A., M.D,. B.C.. M.R.C.S.. L.R.C.P 37.S "J'he traditional historj- and customs of tlie Alakaranga (Varozwe) : E. G. HowM.A X 383 Solar physics 393 Ostriches in Arizona 393 The killing of the Divine King in South .Africa : Rev. S. S. Dok.v \y. M.A., F.G.S. 394 The collapse of kelp potash .Wi Health problems in countrv districts, Transvaal and (grange P'ree State: J.^xe B. H. 'Ruthveik. M.D., [..R.C.P., L.R.C.S.E., L.R.F.P.'S.. F.R.S.A 400 The origin of novae 406 Walnut bacteriosis : Bacterium iuglandis. Pierce- Kthe!. M. DoinoE. M.A., D.Sc. F.L.S 407 Paraffin paper dressings in surgery 412 Radioactive colouring of minerals 412 Note on the persistence of the right posterior cardinal vein in Xciio- .^pus Uevis. and its significance: R. J. ORTi.Eri\ M.A. (with one text figure) 413 The pandemic in the United States 415 Some engravi'd stones of the Lydcnburg district and North-East Transvaal : the occurrence of cup-and-ring markings in South Africa: Dr. C. Pyper (Pis. 6-1 1) 416 The British Association 417 Religious beliefs and supersf ition'i of the Xosas : a study in philology • J. McL.xrex, M.A '.■. , 418 Radiotelephony 424 Cattle as a factor in the economic development of South Africa: Rev. J. R. L. Kingon, M.A.. F.R.S.E.. F.L.S 425 Calcium clouds in stellar space 440 Arts and crafts of the Xosas: a study based on philologv : T. McLaren. . M.A ... . ' ... 44J Salt water as a preventive of epidemic influenza 449 Some notes on a collecting trip to French Hoek: E. P. Pjiillips, M.A., D.Sc, F.L.S 450 Some early geographers and explorers of .Africa: Rev. W. A. Norton, B.A., B.Litt. ; 479 Purpose in Education : H. C. Reeve, ^LA 483 Who buih the Rhodesian ruins? W. H. Tooke 492 CONTENTS. V PAGE. Atomic weight of nebulium. . . ... ... ... 499 A' note on the pollination oi Cyamlla cupensis Linn. : E. P. Phillips, M.A., D.Sc, F.L.S. ... soo The bacterial blight of beans: Bacterium phaseoli Erw. Sm. : Ethel M. DoiDGE. M.A., D.Sc, F.L.S'. 50J Alcohol from Seaweed ... 305 L^nrealised Factors in Native economic development : Rev. ]. R. L. KiNGON. M.A.. F.R.S.E., F.L.S. ... ... ... 506 The pepper tree (Schiuits iiiolli') in its relation to epidemic hav fever : Prof. G. Potts, M.Sc, Ph.D 52*5 The engraved stone of Loe, Hechuanaland Protectorate : Mi§,s M. WiLMAN (Plates 12-15) 531 Radium production 534 Ageing of chemical elements _. ... 534 The pure-line hvpothes's and the inheritance of small variations : Prof. E. Wakren, D.Sc. (Plate 16) 535 Note on the Equatorial Sundial at the Castle, Capetown : J. Lunt. D.Sc. F.I.C. (Plate 17) 568 A Jovian prominence 5^9 Liquid hydrocyanic acid for fumigation 560 Additions and corrections to the recorded flora of the Transvaal and Swaziland : J. Burtt-Davv, F.L.S.. F.R.G.S 570 SIR WILLIAM CROOKES 572 Some experiments used in the rudimentary teaching of botany: Rev. F. C. KoLBfE. D.D.. D.Litt 575 Economic natural historv. and whv it should be taught in schools : F. W. FiTzSiMONs.'F.Z.S., F.R.M.S. ... 580 Problems of degeneration as represented by the ostrich : Prof. J. E. DuEFDEN. M.Sc. Ph.D.. A.R.C.S. (Title only) 587 The pineal bcdv in the ostrich : Prof. T. E. Duerden, M.Sc, Ph.D., A.R.C.S. (Title only) _ ... 587 Charts, photographs, and reports of the Rand Mines Sanitation Department: A. J. Orenstein, M.D.. ALR.C.S., L.R.C.P. (Title only) 58I7 Intoxication by gastrophilous larvae: G. van de Wall dei Kock, M.R.C.V.S. (TW^ only) 587 On the eradication of venereal diseases : R. T. A. Innes, F.R.A.S., F.R.S.E. (Title only) 587 Some features of the South African Odonata as a fauna: S. G. Rich, M.A., B.Sc 588 Crossing the North African and South African ostrich: Prof. J. E. DuERUEN. M.Sc. Ph.D., A.R.C.S. (Title only) 589 The natives in the larger towns : J. S. Marwick 590 Paper yarns 610 Are the Odonata of economic value? S. G. Rich, M.A., B.Sc. ... 611 Drug treatment in Nuttalliosis of equines : G. van de Wall de KocK. M.R.C.V.S. (Title only) 612 Bovine contagious abortion in South Africa: E. M. Robinson, M.R.C.V.S. (Title only) ... 612 On certain changes in the external sex-characters of ostriches, occurring after removal of the reproductive glands: Sir A. Theiler, K.C.M.G., D.Sc, and D. Kehoe, M.R.C.V.S. (Title only) 612 Spectrography of seaweed ashes 612 A preliminarv investi.eation into a disease attacking young Cupressus plants: Miss A. M. Bottomley, B.A. (Plates 18-21) 613 Are the Orthoptera and Neuroptera actual orders or conglomera- tions? S. G. Rich, M.A., B Sc 618 Rhodesian minerals 621 Epie poetry in French literature : Prof. R. D. Nauta 622 Suggestion for the education of public opinion on Native affairs : M. S. Evans, C.M.G., F.Z.S. ( Title only) 637 Social conditions of Natives on the Rand : Rev. W. F. Hill, M.A., (Title only) 637 vi CONTENTS. PAGK Place-names of Africa, No. II: Rev. W. A. Nokton, B.A.. B.Litt. (Title only) , 637 Note on the occurrence of a peculiar phosphate of aluminiam in a deposit of Bat guano : B. de C Marchand, B.A., D.Sc 63S More Sesuto etymologies: Rev. W. A. Norton, B.A.. B.Litt. (Title only) 639 Reconstitution of the Union Senate: R. T. A. Inne-s, F.R.A.S.. F.R.S.E. (Title only) 639 Decimal coinage: Prof W. A. Macfadyen, M.A., LL.D. (Title only) 639 Vicarious parenthood: a war suggestion: Mrs. F. McLaren (Title onlv) 639 War and the value of money: Prof. R. Leslie, M.A., F.S.S. (Title only) ...... ... 639 Some experiments on the fate of arsenic in the animal body: H. H. Green. D.Sc, and C. D. Dyk.man, M.A 64O National Chemical Service 651 Some preliminary observations on unseasonable veld-burning; and its possible relation to some stock diseases : A. (). D. Mogg, B.A. (Abstract) 653 The philologv of the Native languages ( Zulu and Xosa) : Rev. S. G. G.'AiTCHisoN, M.A., D.D. (Title only) 653 Wasted South African resources ; coal and its bye-products : A. Kloot, B.A., A.LC. (Abstract) ... 654 The evolution of a Native administration: Rev. T. R. L. Kingon, ^]. A.. F.R.S.E.. F.L.S. (Title only) " 655 Notes on the morphology and life history of Uromyces Aloes Cooke : V. A. PuTTERiLL, B.A. (Plates 22, 23, and six text Agures) ... 656 Scientific labour union 662 The Kap-tent wagon : J. Y. Gibson (Plate 24) 663 The geophone 669 Notes on the genus Balansia: Miss A. M. King, B.A. (Plate 25 and four text figures) 670 Paper from sugar cane leaves 67s Smoke screens ... ... ... ... ... ... ... • • • • • • 073 Native child life: Rev. S. G. G. Aitchison, M.A., D.D 674 Concrete sleepers 679 Discontinuous distribution in a few mammalian groups: T. F. Dreyer, B.A., Ph.D 680 Central African Folk-lore tales: Rev J. R. L. Kingon, M.A., F.R.S.E., F.L.S. (Title only) 689 A new type of accurate sundial or solar clock: J. Moir, M.A., D.Sc, F.LC. (Plate 26.) ... 690 Some photographic illustrations of South African vegetation: LB. Pole- Evans, M.A., D.Sc, F.L.S. (Title only) 693 Synthesis of sugars 693 Native customs in relation to small-pox amongst the Ba-Ronga : Rev. H. A. JuNOD 694 Infantile paralysis ... , 702 Nitrogenous products . . . 702 A philological method of exhibiting classical declensions and conju- gations: Rev. W. A- Norton. P. A.. I' 703 On the heterocerous fauna of Southern Rhodesia : A. J. T. Janse, FES 708 Bacteriological production of acetone 711 .\ survey of aboriginal place-names: Rev. J. R. L. Kingon, M.A.. F.R.S.E., F.L.S 712 Helium foi dirigibles ... 779 A rapid approximate method of calculating the occultation of stars bv the moon (for the Central Transvaal) : J. Moir, M.A., D.Sc, F.I.C 780 Officers and Council, 1918-19 i List of Members Hi Index xxxvii CONTENTS. Vll Plat No. I. 2. 3. 4- 5- 6. 7- 8. 9- 10. II. 12. 13- 14. 15. 16. 17- 18. 19. 20. 21. 22. ^3- 24. :25. 26. JST L)F PLATES. The South Africa Medal Some results of ostrich investigations Some results of ostrich investigations Some results of ostrich investigations Some results of ostrich investigations Engraved stones of the Lydenburg District Engraved stones of the Li'denburg District Engraved stones of the Lydenburg District Engraved stones of the Lydenburg District Engraved stones of the Lydenburg District Engraved stones of the Lydenburg District The engraved rock of Loe The engraved rock of Loe The engraved rock of Loe The engraved rock of Loe The pure line hypothesis An equatorial sundial A disease of young Cuprcssits plants A disease of young Cuj^ressiis plants A disease of young Cii/''i'i'ssits plants A disease of j'ouiig Cithrrssiis |)lants Lh'omyces Aloes t^ooke Vromyces Aloes Cooke The Kap-tent wagon The genus Balansia A new type of sundial To face Page xxvii 247 246 270 271 416 416 416 416 416 417 531 532 563 568 6x2 613 614 616 658 660 663 670 69O ERRATA. Page 191, Pag-e 192, Page 193, Page 194, Pai^c 202. 1 J 'age J03. 1 Page 322, Page 376, line line last line line line iiK- line ine iiie line line line line line line line 10. — For " heart "' read " art." 30. — For " therefore '' read " therefor." line. — For " practice " read " practise." 23.— For " practice " read " practise" 1.— Delete " it." 29. — For '■ practice " read " practise." 28. — For " Aiiiakiihiilo " read " Ainakubalo." 35.— For 41. — For 5. — For J 1 . — For 24. — For 44. — F'or .~l liii.ii\ IK ' II ic ituu ^ 1 limn iiuiiiL' . fsiiuliycndiya " read " Isindiyandiya.'' sparkling " read " .sprinkling." liabiyc " read " habuja." aiiiasttiut " read " aiiiasimu." ■ particuar " read " particular." 44. — ±ui poisonus " read " poisonous." 9 from bottom. — After "unless this" insert "is prevented b}- law." 3^ — For " Schistosome becattse of " read " Schis- losoiHiiin b\. ' 22. — For ■■ cercaria attacks " read " cercaria- •attack." 2 from bottom. — For " mixacidiitm " read " inira- cidiuni." VllI -ERRATA. Page 413, line x8 of text. — For '* precaval " read "postcaval." Page 414. line i. — For " Postcardial " read " Postcardinal.'" Page 414. text-tigure. — For " Sel." read " Scl." Page 415, line 19. — For " aiiiphibious " read "amphibians." Page 426, line 8 from bottom.— .\fter " of " delete " the." Page 428, line 4. — For " 1485 '" read " i486." Page 431, line 24. — For "east" read "last." Page 433, line 5. — For " counsellors " read " councillors." line 19. — After " contact and " insert " conflict." Page 437, line 28. — For "Machiavellian" read "gigantic." Page 438, line 25. — For " ignominous " read " ignominious." Page 43Q. line ti. — Before "the mainspring" insert "it will be seen that." Page n/o. line 6. — For ■" addition " read " additions." line 15.— For " Staff " read " Stapf." line 32— For " Staff " read " Stapf." line 34. — Insert full sto]) after '' Dur." line 35. — For " Staff " read " Stapf." line s^. — For " Cragrostis " read " Eragkostis," and for " Staff " read " Stapf." line 38. — Fur " lickloiis" read " EckJoiiis." Page 571, line i. — For " .hincics uxycarpns" read " JuNCUs OXYCARPUS." line 4. — For " Hook-fil." read ' Hook, fil." line 6.— For " 17 " read " 17384." line 9. — Delete full stop after " Zeyh." line 12- — For '' scuber" read " scaber." line 24.— Delete full stops after " FIelichrysum ' and " cephalojdeum/' and for " Dc ' read " n.c." line ^ti. — Insert full stop after " Port." line 2 from bottom. — For " Galp'mu" read " Galpinii last line. — For " naflensis '\ read " nataiensis." OFFICERS AND COUNCIL, 1917-1918. HONORARY PRESIDENT. HIS MAJESTY THE KING. PRESIDENT. C. F. JURITZ, M.A., D.Sc, F.I.C. EX-PRESIDENT. Professor J. ORR, B.Sc, M.I.C.E., M.I.Mech.E. VICE-PRESIDENTS. W. Ingham, M.I.C.E., M.I.M.E. i Prof. \V. N. Roseveahe. M.A. A. H. Reid, F.R.I.B.A., F.R.San.I. II. E. Wood, M.Sc, F.R.Mct.S. HON. GENERAL SECRETARIES, Rev. W. Flint, D.D., Library of Par- liament, Capetown. J. A. FooTE, F.G.S., F.E.I.S., Commer- cial High School, Plein Street, Jo- hannesburg. HON. GENERAL TREASURER. A. Walsh, P.O. Box 39, Cape Town. ASSISTANT GENERAL SECRETARY. H. Tucker, Cape of Good Hope Savings Bank Buildings, St. George's Street, Cap« Town. P.O. Box 1497. (Telegraphic Address: " Scientific.") ORDINARY MEMBERS OF COUNCIL. I. CAPE PROVINCE. Cape Peninsula. Prof. A. Brown, M.A., B.Sc, F.R.S.E. M.D., M.R.C.S., Prof. L. Crawford, M.A., D.Sc, F.R.S.E. Prof. R. Leslie. K.A.. F.S.S. C. W. Mally, M.Sc, F.E.S., F.L.S. R. W. Menmuir, A.M.I.C.E. Kimberlcy. Miss ^T. Wilman. Kingwilliamstozvn. 3. Leighton, F.R.n.S. Middelburg. A. Stead, B.Sc, F.C.S. Port Elisabeth. Rev. T. R. L. Kingon, M.A., F.R.S E., F.L.S. Stellenbosch. Prof. J. T. Morrison, M.A., B.Sc, F.R.S.E. Prof. B. de St. J. van der Riet, M.A., Ph.D. II. TRANSVAAL. Witwatersrand. I. Burtt-Davy, F.L.S., F.R.G.S. W. A. Caldecott, B.A., D.Sc, F.C.S. P. Cazalet. Lt.-Col. J. H. DoBSON, D.S.O., M.Sc, M.I.Mech.E., M.l'.E.E., A.M.I.C.E. Prof. H. B. Fantham, M.A., D.Sc, A.R.C.S., F.Z.S. F. Flowers. C.E., F.R.G.S., F.R.A.S. Jas. Gray, F.I.C. R. T. A. Innes, F.R.A.S., F.R.S.E. J. W. Kirkland, M.Am.I.E.E. J. Mitchell. Prof. C. E. IMoss, M.A., D.Sc, F.L.S., F.R.G.S. A. T. Orenstein, L.R.C.P, Prof. G. H. Stanley, A.R.S.M., M.I.M.E., M.I.M.M., F.I.C. H. A. Trubshaw. J. van Niekerk. alb., cm. W. Watkins - Pitchford, M.D., F.R.C.S., D.P.H. Prof. J. A. Wilkinson, M.A., F.C.S. Pretoria. 1. B. Pole Evans. M.A., B.Sc, F.L.S. Prof. W. A. Macfadyen, M.A., LL.D. Prof. D. F. DU Toit Malherbe, M.A.. Ph.D. Prof. H. A. Wager, A.R.C.S. Pctchefstrooin. E. Holmes Smith, B.Sc. III. ORANGE FREE STATE. Bloemfontein. T. F. Dreyer. B.A., Ph.D. Prof. M. I\r. Rindl, Ing.D. I\'. NATAL. Durban. M. S. EvAKS, C.M.G., F.Z.S. C. T. LoRAM, M.A., LL.B., Ph.D. M aritsburg. J. S. Henkel. Prof. E. Warren, D.Sc. V. RHODESIA. Bulawayo. Rev. S. S. DoRNAN, M.A. F.G.S. M. MOZAMBIQUE. S. Seruya. Endowment Fund. I W. Jagger, F.S.S. , M.L.A. W. RuNciMAN, M.L.A. Principal J. C. Beattie, F.R.S.E. TRUSTEES. S.A. Medal Fund. W. E. Gurney. C. Murray, M.A. D Sc W Thomson, M.A., B.Sc, F.R.S.E. LL.D., 11 PLACES AND DATES OF PAST MEETINGS, ETC. S <^ "S3 *** an s o IS -** -to V ■ii <3 S S O ^ 'i^ ■■3i Co ^ 2 "13 "« D^ l:^^ JS Pu ^ ci CO Vi UJ Q ^ < * <■ a: ^ o UJ " CO .2 -1 < o o 5 . -I C/3 f^,4 ■ fC CO H Z UJ Q CO UJ K Ol . § 111 "=* Q Ul M oc »* Q. HH Ul ii > < U - Ho U • c . o t: Vji/If-iO r< M o •J ,, •-i£ i-i < > <; Q 'Ft V c 3 w " ■ t/5 -d ^^ . • <: - "" ■"i -rn E «J c •- 1, .= C 3 l-H O PQ J; < O H W f< JU :w :« •fa «c/[ -d - c . . — « i-^cnt-C U l-H o § M ^ ocT W (N U tS 3 HH 60 S 3 < H O Pi « 2; D oa :d Is w z « < X w o P2| 1— . o o o w u <■ t/i u pi > : :Sw : r-^. : I'^Pi : : rfe • -a - . . "^ en ^ S °-- - Co ■— ■ r-" , ' 3m.. 23 Ul— . v: B ° < l-H ►J 1-1 fa w z Q BS U N c V fa bs 3 O c fa ' • nifefa' rOQ to d , -i-H r r c/i^^^ C/J c - -r-'c ? 3 ^2. d^ OS fa & 1-3 C/3 f OT n H d E fa ^ Sen : sd ; fa;OT . u_, ,_: **H iJ o^ o c Qs gd^ ?IU oca n « o fa<; ::< u Ui V)0 PLACES AND DATES OF PAST MEETINGS, ETC. Ill U (0 1— 1 UJ i^ l£ . o P-icO^< CO ! '■< fa -.^.^ U oU ., ^"d CO 'd pi o rt u o ^"^ fadco-ii Q o ^ • •Kp3 tT ? O O u Pih-PUCO CO d fa CO dco dw" p^ ' K >*-• -^ o en 1- z UJ o m Ul tc 0. CO pi fa" d d p^" W CO CO < c a M '-' 2 pP3 < co . °; U W n h-lW Q ^4 O PS < CO fa CO CO H Pi W pq O p; fi gco 09. Bloemfontein 1910- Cape Town$ 191 1. Bulawayo igi2. Port Elizabeth 19 1 3. LourenQO Marques 1914. Kimberley 1915. Pretoria 1916. Maritzburg . . 1917. Stellenbosch . . 1918. Johannesburg Prof. W. A. D. Rudge, M.A. Prof. J. C. Beattie, D.Sc, F.R.S.E. Rev. E. Goetz, S.J., M.A., F.R.A.S. H. J. Holder, M.I.E.E. J. H. von Hafe. Prof. A. Ogg, M.A., B.Sc, Ph.D. F. E. Kanthack, M.I.C.E., M.I.M.E. Prof. J. Orr, B.Sc. M.I.C.E. Prof. W. N. Roseveare. M.A. Prof. J. T. Morrison, M.A., B.Sc, F.R.S.E. H. B. Austin, F. Masey. A. H. Reid, F. Flowers. A. H. Reid, Rev. S. S. Dor- nan. A. H. Reid. Prof. J. Orr, J. Vaz Gomes. Prof. A. Brown. A. E. H. Din- ham-Peren. Prof. A. Brown, J. L. Sout- ter. Prof. A. Brown, P. Mesham. Prof. A. Brown, L. Simons. Prof. A. Brown, Prof. J. P. Dalton. SECTION B— ANTHROPOLOGY, ETHNOLOGY, BACTERIOLOGY, BOTANY, GEOGRAPHY, GEOLOGY, MINERALOGY AND ZOOLOGY. 1903. Cape Town . 1904. Johannesburg 1906. Kimberley R. Marloth, M.A., Ph.D. Prof. A. Dendy. G. S. Corstorphinc B.Sc, Dr. W. C. C. Pakes, W. H., Ph.D., F.G.S. Thos. Quentrall, M.I.Mech.E., F.G.S. Jollyman. C. E. Addams, H. Simpson. * Metallurgy added in 1904. t Geography and Geodesy transferred to Section A and Chemistry and Metallurgy to Section B, in 1907. t Irrigation added in 1910 and Geography transferred to Section B. PRESIDENTS AND SECRETARIES OF THE SECTIONS. Date and Place- Presidents. Secretaries. CHEMISTRY, METALLURGY, MLNERALOGY, ENGINEERING, MINING AND ARCHITECTURE. 1907. Natal 1908. Grahamstown C. W. Methven. M.I.C.E., F.R.S.E., F.R.I.B.A. Prof. E. H. L. Schwarz, A.R.C.S., F.G.S. R. G. Kirkby, W. Paton. Prof. G. E. Cory, R. W. Newman, J. Muller. CHEMISTRY. BACTERIOLOGY, GEOLOGY, BOTANY, MINERALOGY, ZOOLOGY, AGRICULTURE, FORESTRY, SANITARY SCIENCE. 1909. Bloemfontein C. F. Juritz, M.A., D.Sc, , Dr. G. Potts, A. Stead. I F.I.C. CHEMISTRY, GEOLOGY, METALLURGY, MINERALOGY AND 1910. Cape Town . . 191 1. Bulawayo 1912. Port Elizabeth 1913. Lourenqo Marques 1914. Kimberley 1915. Pretoria 1916. Maritzburg. . . 1917. Stellenbosch . . 1918. Johannesburg GEOGRAPHY. A. W. Rogers, M.A., Sc.D., F.G.S. A. J. C. Molyneux, F.G.S., F.R.G.S. Prof. B. de St. J. van der Riet, M.A., PhD. Prof. R. B. Young, M.A., D.Sc, F.R.S.E., F.G.S. Prof. G. H. Stanley, A.R.S.M., M.I.M.E., M.I.M.M., F.I.C. H. Kynaston, M.A., F C S Prof", j'. A. Wilkinson, M.A. F.C.S. Prof. M.'m. Rindl, Ing.D. P. A. Wagner. Ing.D.. B.Sc. J. G. Rose, G. F. Ayers. J. G. Rose, G. N. Blackshaw. J. G. Rose, J. E. Devlin. Prof. G. H. Stanley, Capt. A. Graqa. J. G. Rose, J. Parry. Dr. H. C. J. Tietz, Prof. D. F. du Toit Malherbe. Dr. H.C.J. Tietz, Prof. J. W. Bews. Dr. H. C. J. Tietz, Prof. B. de St. J. van der Riet. Dr. H. C. J. Tietz, Dr. J. Moir. SECTION C— AGRICULTURE, ARCHITECTURE, ENGINEERING, GEODESY, SURVEYING, AND SANITARY SCIENCE. 1903. Cape Town . . Sir Chas. Metcalfe, Bart., A. H. Reid. M.I.C.E. 1904- Johannesburg * , Lieut.-Colonel Sir Percy G. S. Burt Andrews, E. J. Girouard, K.C.M.G., Laschinger. D.S.O. 1906. Kimberley S. J. Jennings. C.E., D. W. Greatbatch, W. New- M.Amer.I.M.E., M.I.M.E. 1 digate. * Forestry added in 1904. VI PRESIDENTS AND SECRETARIES OF THE SECTIONS. BACTERIOLOGY, BOTANY, ZOOLOGY, FORESTRY, PHYSIOLOGY, 1907- Natal 1908- Grahamstown 1910. Cape Town * 1911. Bulawayo 1912. Port Elizabeth 1913. LouretiQO Marques 1914. Kimberley 1915. Pretoria 1916. Maritzburg. . . 1917. Stellenbosch . . Lieut.-Colonel H. Watkins Pitchford, F.R.C.V.S. Prof. S. Schonland, M.A., Ph.D., F.L.S., C.M.Z.S. Prof. H. H. W. Pearson, M.A., Sc.D., F.L.S. F. Eyles, F.L.S., M.L.C. F. W. FitzSimons. F.Z.S., F.R.M.S. A. L. M. Bonn, C.E. Prof. G. Potts, M.Sc, Ph.D. C. P. Lounsbury, B.Sc, F.E.S. I. b'. Pole-Evans, M.A., B.Sc, F.L.S. J. Burtt-Davy, F.L.S., F.R.G.S. AGRICULTURE AND HYGIENE. W. A. Squire, A. M. Neilson, Dr. J. E. Duerden. Dr. J. Bruce Bays, W. Robertson, C. W. Mally, Dr. L. H. Gough. W. D. Severn, Dr. J. W. B. Gunning. W. T. Saxton, H. G. Mundy. W. T. Saxton, I. L. Drege. F. Flowers, Lieut. J. B. Botelho. C. W. Mally. W. J. Calder. C. VV. Mally, A. K. Haagner. C W. Mally, Prof. E. Warren. C. W. Mally, C. S. Grobbelaar. BOTANY, BACTERIOLOGY. AGRICULTURE, AND FORESTRY. 1918. Johannesburg C. E. Legat, B.Sc. Dr. E. P. Phillips. J. Burtt- Davv. SECTION D.— ZOOLOGY, PHYSIOLOGY, HYGIENE, AND - SANITARY SCIENCE. 1918. Johannesburg ! Prof. E. J. Goddard, B.A., 1 C. W. Mally. R. T. Ortlepp. D.Sc. ' SECTION E.— ANTHROPOLOGY, ETHNOLOGY. ECONOMICS. SOCIOLOGY, AND STATISTICS. 1908. Grahamstown W. Hammond Tooke. I Prof. A. S. Kidd. ANTHROPOLOGY, ETHNOLOGY, NATIVE EDUCATION, PHILOLOGY, AND NATIVE SOCIOLOGY. 1917. Stellenbosch . . Rev. N. Roberts. 1918. Johannesburg ' Rev. W. A. Norton, B.A. B.Litt. * Sanitary Science added in 1910. Rev. E. W. H. Musselwhite. Prof. J. J. Smith. Rev. E. W. H. Musselwhite. Rev. G. Evans. PRESIDENTS AXD SECRETARIES OF THE SECTIONS. Vll Date and Place. Presidents. Secretaries. SECTION F.— ARCHEOLOGY, EDUCATION, MENTAL SCIENCE, PHILOLOGY, POLITICAL ECONOMY, SOCIOLOGY AND STATISTICS- 1903. Cape Town . 1904. Johannesburg 1906. Kimberley Thos. Muir, C.M.G., M.A., i Prof. H. E. S. Fremantle. LL.D., F.R.S., F.R.S.E. (Sir Percy Fitzpatrick, | Howard Pim, J. Robinson. M.L.A.), E. B. Sargant, | M.A. (Acting). A. H. Watkins, M.D., M.R.C.S. E. C. Lardner-Burke, E. W. Mowbray. ANTHROPOLOGY, ARCHEOLOGY, ECONOMICS. EDUCATION ETHNOLOGY. HISTORY, PSYCHOLOGY, PHILOLOGY, SOCIOLOGY, AND STATISTICS. 1907. Natal R. D. Clark, M.A. R. A. Gowthorpe, A. S. Langley, E. A. Belcher, ARCHEOLOGY. EDUCATION, HISTORY, PSYCHOLOGY. AND PHILOLOGY. 1908- Grahamstown E. G. Gane, M.A. I Prof. W. A. Macfadyen, W. I D. Neilson. ANTHROPOLOGY, ETHNOLOGY, EDUCATION, HISTORY, MENTAL SCIENCE, PHILOLOGY^ POLITICAL ECONOMY, SOCIOLOGY AND STATISTICS. 1909. Bloenifontein I Hugh Gunn, M.A. 1910. Cape Town .. 1 Rev. W. Flint, D.D. 191 1. Bulawayo .. ; G. Duthie, M.A., F.R.S.E 1912. Port Elizabeth | W. A.^Way, MA 1913. LourenQO ' ' — '- - Marques 1914. Kimberley 1915. Pretoria 1916. Marilzburg J. A. Foote, F.G.S. Prof. W. Ritchie, M.A. J. E. Adamson, M.A. M.S. Evans, C.M.G.,F.Z.S. C. G. Grant, Rev. W. A. Norton. G. B. Kipps, W. E. C. Clarke- G. B. Kipps, W. J. Shepherd G. B. KioDs, E. G. Brvant. H. Pim.'j. Elvas. Prof. R. D. Nauta, A. H. J. Bourne. Prof. R. D. Nauta, R. G. L. Austin. Prof.^ R. D. Nauta, Prof. O. Waterhouse. EDUCATION. HISTORY, MENTAL SCIENCE, POLITICAL ECO- NOMY. GENERAL SOCIOLOGY, AND STATISTICS. 1917. Stellenbosch . 1918. Johannesburg Rev. B. P. J. Marchand. B.A. Prof. T. M. Forsvth, M.A. D.Phil. Prof. R. D. Nauta, Dr. Bertha Stoneman. Prof. R. D. Nauta, J. Mitchell Vlll EVENING DISCOURSES. Date and Place- Lecturer. Subject of Discourse- 1903. Cape Town . 1904- Johannesburg 1906. Kimberley 1907. Maritzburg . Durban. 1908. Grahamstown 1909. Bloemfontein Maseru 1910. Cape Town 1911- Bulawayo 1912. Port Elizabeth 1913. LourenQO Marques 1914. Kimberley 1915. Pretoria 1916. Alaritzburg . Durban . . . . 1917. Stellenbosch . . 1918. Johannesburg Prof. W. S. Logeman, B.A., L.H.C. H. S. Hele-Shaw, LL.D., F.R.S., M.I.C.E. Prof. R. A. Lehfeldt, B.A., D.Sc. W. C. C. Pakes, L.R.C.P., M.R.C.S., D.P.H., F.I.C. R. T. A. Innes, F.R.A.S., F.R.S.E. Prof. R. B. Young, M.A., B.Sc, F.R.S.E.. F.G.S. Prof. G. E. Cory, M.A. A Theiler, C.M.G. C. F. Juritz, M.A., D.Sc, F.I.C. W. Cullen. R. T. A. Innes, F.R.A.S., F R S F Prof. H. Bohle, M.LE.E. J. Brown, M.D., CM., F.R.C.S., L.R.C.S.E. W. H. Logeman, M.A. A. W. Roberts, D.Sc, F.R.A.S., F.R.S.E. Prof. E. J. Goddard, B.A.. D.Sc S. Seruya. Prof. E. H. L. Schwarz, A.R.C.S., F.G.S. E. T. Mellor, D.Sc, F.G.S., M.I.M.M. C. W. Mally, M.Sc, F.E.S., F.L.S. C. P. Lounsburj', B.Sc, FES R. f. A.' Innes, F.R.A.S., F.R.S.E. H. E. Wood, M.Sc. F.R.Met.S. Prof. J. D. F. Gilchrist, M.A.. D.Sc. Ph.D., F.L.S.. C.M.Z.S. Prof. H. B. Fantham, M.A., D.Sc. A.R.C.S.. F.Z.S. Prof. J. E. Duerden, M.Sc. Ph.D.. A.R.C.S. The Ruins of Persepolis and how the Inscriptions were read. Road Locomotion — Present and Future. The Electrical Aspect of Chemistry. The Immunisation against Disease of Micro- organic Origin. Some Recent Problems in Astronomy The Heroic Age of South African Geology. The History of the Eastern Province. Tropical and .Sub-tropical Diseases of South Africa : their Causes and Propaga- tion. Celestial Chemistry. Explosives: their Manufac- ture and' Use. Astronomy. The Conquest of the Air. Electoral Reform — Propor- tional Representation. The Gyroscope. Imperial Astronomy. Antarctica. The history of Portuguese conquest and discovery. The Kimberley Mines, their discovery, and their rela- tion to other volcanic vents in South Africa. The gold bearing conglomer- ates of the Witwatersrand. The House fly under South African conditions. Scale Insects and their travels. Astronomy. Some imsolved problems of Astronomy. Some marine animals of South Africa. Evolution and Mankind. Ostriches. GENERAL MEETINGS AT JOHANNESBURG. On Monday, July ^, at 2.30 p.m., the Association was offi- cially welcomed by His Worship the Mayor of Johannesburg (Councillor T. F. Allen) in the Assembly Hall of the South African School of Mines and Technology. At 3.30 p.m.. Members of the Association proceeded on a motor drive round Johannesburg and suburbs. At 8.15 p.m.. in the Selborne Hall. Dr. C. F. Juritz, M.A., D.Sc, F.LC., took the chair as President, and delivered an address, for which see page i. The President subsequentlv presented the South Africa Medal to Mr. R. T. A. Innes, F.R.S.E., F.R.A.S. For the pro- ceedings see page xxvii. On Tuesday, July 9, at 2 p.m., Members of the Association visited the Crown Mines, and the Johannesburg Municipal Under- takings, Power Station and Abattoirs. At 8.15 p.m., in the Assembly Hall of the South African School of Mines and Technology, Prof. H. B. Fantham, M.A., D.Sc, A.R.C.S., F.Z.S., delivered a discourse on " Evolution and Mankind," the President of the Association presiding. On Wednesday, July 10. at 2 p.m., ^Members of the Asso- ciation visited the New Modderfontein Gold Mine and Dunswart Iron and Steel Works. At 2.30 p.m., Members visited the Johannesburg Trades School and the South African Institute of Medical Research. At 8.15 p.m., Members attended a reception held by His Worship the Mayor of Johannesburg, in the Town Hall. On Thursday, July 11, at 11.30 a.m., the Sixteenth Annual General Meeting was held in the Assembly Hall of the South African School of Mines and Technology, for Minutes of which see page xiv. At 2 p.m., Members of the Association visited the New Transvaal Chemical Works, Delmorc, and the Rosherville Power Station of the Victoria Falls and Transvaal Power Co., Ltd. At 8.15 p.m., Members attended a reception held by the Local and Reception Committees at the Union Observatory. On Friday, July 12, at 8 a.m., Members of the Association proceeded on an excursion to Vereeninging, and there visited the Union Steel Corporation Works, the Vereeniging Power Station of the Victoria Falls and Transvaal Power Co., and the site of the Rand Water Board Barrage on the Vaal River. At 8.15 p.m., in the Assembly Hall of the South African School of Mines and Technology, Prof. J. E. Duerden, M.Sc, Ph.D., A.R.C.S., delivered a discourse on " Ostriches," the Presi. dent of the Association presiding. On the morning of Saturday, July 13, members of the Asso- ciation inspected the underground working's of the Crown Mines. X OFFICERS OF LOCAL AND SECTIONAL COMMITTEES, JOHANNESBURG, 1918. LOCAL COMMITTEE. Chairman, H. E. Wood, M.Sc. F.R.Met.S. ; J. Burtt-Davy. F.L.S., F.R.G.S., W. A. Caldecott. B.A.. D.Sc, F.C.S., P. Oazalet, Lieutenant-Colonel J. H. Dobson. D.S.O., M.Sc, M.I.Medi.E.. M.I.E.E., A.M.I.C.E., Prof. H. B. Fantlham, M.A., D.Sc, A.R.C.S., F.Z.S., F. Flowers, C.E., F.R.A.S., F.R.G.S., J. Gray, F,I.C.. W. Ing-ham, M.I.C.E.. M.I.M.E., R. T. A. Innes. F.R.A.S.. F.R.S.E.. J. W. Kirkland, M.Am.F.E.E., T- Mitchell, Prof. C. E. Moss, M.A., D.Sc, F.L.S.. F.R.G.S., A. T- Orenstein. M.D.. M.R.C.S., L.R.C.P., Prof. [. Orr, B.Sc. M.I.C.E., M.I.Mech.E., Prof. (i. H. Stanley, A.R.S.M.. M.I.M.E., M.I.M.M., F.I.C., H. A. Trubshaw, J. Van Niekerk, M.B., CM.. W. Watkins-Pitchford, M.D., F.R.C.S., D.P.H., and Prof. J. A. Wilkinson, M.A., F.C.S. Local Sccrciar\\ ]. A. Foote, F.G.S., F.E.I.S. RECEPTION COMMITTEE. Chairman, His Worsihip itihe Mayor of Johannesburg (T. F. Allen) ; Vice-Chairman, the Deputy AJiayor of Johannesburg (D. Anderson) ; Chairman and Members of tthe Local Com- mittee: Councillors B. Alexander, G. B. Steer, M.P.C., J. A. Moffat, S. Scott, M.P.C., S. A. Smit, and C. V. Becker;' His Worship tllie Mayor of Benoni (I. Kuper). His Worship the ]\Iayor of Boksburg (A. Ruffels), His Worship the Mayor of Germdston (Dr. R. Straohan). His Worship the Mayor of Krugersdorp (J. Hoatson), His Worship the Mayor of Roode- poort (G. W. Arthur). His Worship the Mayor of Springs (E. Stanton Corke). President, Chamber of Mines (E. A. W^allers), President, Chamber of Commerce (F. C. Sturrock), President, Association of Mine Managers ( E. H. Bulmain), President. S.A. Institution of Engineers (C. D. Leslie). President, S.xA. Institute of Electrical Engineers (Prof. J. H. Dobson, D.S.O.), President, Chemical, Metallurgical and Mining Society of S.A. (H. A. W'hite, Vice-President), President, S.A. Society of Civil En- gineers (Mansergh Robinson). President, S.A. Society of Analy- tical Chemists (Prof. J. A. Wilkinson. Vice-Pres.) President. Geological Society of S.xA. (Dr. E. T. Mellor, Past President). President, Association of Ceritificated Engineers (H. Newbery), President, Association of Architect's of the Transvaal (■\1. J. Harris), President. Transvaal Insititute of Architects (D. M. Burton), President (London Society of Architects, S.A. Branch (D. M. Sinclair), President, Transvaal Society of Accountants (J. T. Goldsbury), President, Society of Incorporated Account- ant's (H. J. Macrae), President, S.A. Geographical Society OFFICERS OF SECTIONAL COMMITTEES. XI (J. H. Hutcheon, M.A.), President, Instkute of Land Surveyors (W. M. Harries), President, Britisih Medical Associiation, Wit- watersrand Branch (Dr. E. P. Baumann), President, Transvaal Medical Council (Dr. J. Van Niekerk), Presidenit, Transvaal Pharmacy Board (B. Owen Jones), President, Pharmaceutical Society of the Transvaal (J. Colebank), President, Incorporated Law Society of tlhe Transvaal (E. J. Van Gorkom), Chairman of Council, Soultlh African School of Mines and Technology (S. Evans). Principal, South African School of Mines and Technology (Dr. George S. Coirstorphine), President, Transvaal Teachers' Asisociait'ion (J. Mitchell), President, Johannesburg and Rand Teachers' Association (I. Abra- hams), Chairman, WitwE^tersrand Council of Education (Colonel W. Dalrymple, Deputy Chairman), Chairman, Witwaitersrand Central Sdhool Board (Howard Pim), Director, South African Institute of Meidical Researdh (Dr. W. Watkins-Pitchford), Chairman, Rand Water Board (T. A. R. Purohas). Chairman, Joh'annesburg Stock Exchange (D. C. Greig), President, Witwatersrand Commercial Exchange (A. Y. Niven), President, Witwatersrand Agricultural Society (John Roy), Chairman, South African National Union (J. Waldie Pierson), President, Transvaal Automobile Club (J. Davidson), Chairman, Rand Club (J. M. Buckland), Chairman, New Club (J. Hopkins), Chairman, Country Club (C. A. Wenitzel), Chair- man, Union Club (J. A. W. Kerr), Chairman, Unionisit Party Club (J. E. Jones), Chairman, South African Party Club (J. A. Coetzee), C. Aburrow, Alex. Aiken, Sir George Albu, Bart., P. M. Anderson, G. S. Burt Andrews, Norman Anstev, Sir Abe Bailey, K.C.M.G., A. J. Beaton. L. Blackwell, M.L.A., Major Blaney, D.S.O., W. R. Boustred, H. C. Boyd, J. Frank Brown, C.M.G., H. O. Buckle, Sir William St. J. Carr, E. Chappell. D. Ohristopherson, G. H. Clififoird, C. Chu'dieigh, L. Colquhoun, Lt.-Col. F. H. P. Cresswell, M.L.A., L. Clarence, Col. Cresswell Clark, C.M.G., Sir Thomas Cullinan, Richard Currie, J. P., D. Dingwall, M.E.C., Patrick Duncan, C.M.G., M.L.A., W. Easton, J. Emrys Evans, C.M.G., L. Edwards, S. E. T. Ewing, E. Farrar, P. Ross Frames, A. French, Sir Kendal Franks, M.D., L. Geldenhuys, M.L.A., Richard Goldman, W. T. Graham, H. Graumann, M.L.A., G. Hartog, M.E.C., R. H. Henderson, C.M.G., H. J. Hofmeyr, W. Hosken, A. C. Holtby, Sir William Hoy, Sir Wm. Van Hulsteyn, E. G. Izod, R. Ward Jackson, Julius Jeppe, J. L. Johnson, C. E. Knecht, Dr. F. E. T. Krause, J. Dale Lace, C. D. Leslie. J. Langley Levy, H. T. Lewis, Isaac Lewis, F. R. Lynch, H. McAlister, M.L.A., T. G. Macfie, W. B. Madeley,' M.L.A., Senator the Hon. Sam Marks, W. A. Alartin, H. Stuart Martin, J. B. MacKinlay, Dr. G. A. E. Murray, John Munro, Lt.-Col. Temple-Mursell, Dr. F. Napier, Emile Nathan, M.L.A., Dr. Manfred Nathan, M.P.C., James Neilson, H. Newhouse, Henry Nourse, J. W. O'Hara, J.P., W. J. Parrack, M.L.A., Bernard Xll OFFICERS OF SECTIONAL COMMITTEES. Price. H. P. Papenfus, K.C.. M.L.A., D. B. Pattison, E. J. Renaud. Theo. Reunert, F. Peabody Rice, J. B. Robinson, M.L.A.. F. G. A. Roberts, W. Rockey, M.L.A., W. Ross, H. W. Sampson, M.L.A., Sir H. Ross Skinner. H. Warrington Smj^th, A. Sutherland, W. H. Stucke, M.P.C., James Thompson, Senator the Hon. W. K. Tucker, C.M.G., A. M. Tippet, Walter Webber, W. L. White, D. Wilkinson, E. J. Way, Hon. Justice Ward, Senator the Hon. J. J. Ware, Senator the Hon. P. White- side. Hon. H. A. Wyndham, M.L.A. Hgvi. Secretary: H. A. Trubshaw. SECTIONAL COMMITTEES. Section A.— ASTRONOMY, MATHEMATICS. PHYSICS, METEOROLOGY, GEODESY, SURVEYING, ENGIN- EERING, ARCHITECTURE, AND IRRIGATION. President, Prof. J. T. Morrison, M.A., B.Sc, F.R.S.E. ; Vice- Presidents, W. Ingham, M.I.C.E., M.I.M.E., and H. E. Wood, M.Sc, F.R.Met.S. ; Members, C. J. Gyde, A.M.I.C.E.,A.Hammar, R. T. A. Innes, F.R.A.S., F.R.S.E., F. E. Kanthack, C.M.G., M.I.C.E., M.I.M.E., T. J. Niven, M.I.C.E., Prof. J. Orr, B.Sc, M.I.C.E., :\I.I.Mech.E., and Prof. W. N. Roseveare, M.A. ; Hon. Secretaries, Prof. A. Brown, M.A., B.Sc. (Recorder), and Prof. T. P. Dalton. M.A.. D.Sc. Section B.— CHEMISTRY, GEOLOGY, METALLURGY, MINERALOGY AND GEOGRAPHY. President, P. A. Wagner, B.Sc, Ing.D. ; Vice-Presidents, H. H. Green, D.Sc, F.C.S., and H. A. White. Members, ]. Hutcheon, M.A., F.R.S.G.S., Prof. D. F. du T. Malherbe, M.A., Ph.D., Prof. M. M. Rindl, Ing.D., Prof. E. H. L. Schwarz. A.R.C.S., F.G.S., Prof. G. H. Stanley, A.R.S.M., M.I.M.E., M.I.M.M., F.I.C., Prof. B. de St. J. van der Riet, M.A., Ph.D., Prof. T. A. Wilkinson, M.A.. F.C.S., and Prof. R. B. Young, M.A.. b.Sc, F.R.S.E., F.G.S.; Hon. Secretaries, H. C. T- Tietz. M.A., Ph.D. {Recorder), and J. Moir, M.A., D.Sc. Section C— BOTANY, BACTERIOLOGY, AGRICULTURE AND FORESTRY. President, C. E. Legat, B.Sc. ; Vice'Presidents, Ethel M. Doidge, A'l.A., D.Sc, F.L.S., and Prof. C. E. Moss, M.A., D.Sc. F.L.S., F.R.G.S. ; Members, Prof. J. W. Bews, M.A., D.Sc. I. B. Pole Evans, M.A., B.Sc, F.L.S., Prof. A. I. Perold, B.A., Ph.D.. Prof. G. Potts, M.Sc, Ph.D., T. R. Sim, E. Holmes-Smith, B.Sc, and Prof. H. A. Wager, A.R.C.S. ; Hon. Secretaries, E. P. Phillips. M.A.. D.Sc, F.L.S. {Recorder), and T- Burtt-Davy, F.L.S., F.R.G.S. OFFICERS OF SECTIONAL COMMITTEES. xiii Section D.— ZOOLOGY, PHYSIOLOGY, HYGIENE AND SANITARY SCIENCE. President, Prof. E. J. Goddard, B.A., D.Sc. ; Vice-Presidents Prof. H. B. Fantham, M.A., D.Sc, A.R.C.S., F.Z.S., and A. j! .Anderson, M.A., M.B., M.R.C.S., D.P.H. ; Members, C. G. S. de VilHers, M.A.. T. F. Dreyer, ©.A., Ph.D., Prof. J. E. Duerden, M.Sc, Ph.D.. A.R.C.S., Prof. J. D. F. Gilchrist, M.A., D.Sc, Ph.D., F.L.S., C.M.Z.S., Prof. W. A. Jolly, M.B., Ch.B., D.Sc, D. F. S. Lister, C. P. Lounsbury, B.Sc, F.E.S., D. T. Mitchell. M.R.C.V.S., G. A. E. Murray. M.D.. F.R.C.S., L.R.C.P., A. J. Orenstein, M.D.. M.R.C.S., L.R.C.P., Annie Porter, D.Sc, F.L.S., Prof. E. Warren, D.Sc. and W. Watkins- Pitchford, M.D., F.R.C.S., D.P.H. ; Hon. Secretaries. C. W. Mally, M.Sc, F.E.S., F.L.S. (Recorder), and R. J. Ortlepp, M.A. Section E.— ANTHROPOLOGY, ETHNOLOGY, NATIVE EDUCATION, PHILOLOGY, AND NATIVE SOCI- OLOGY. President, Rev. W. A. Norton, B.A., B.Litt. ; Vice- Presidents, Rev. S. S. Dornaoi, M.A.,F.G.S., and Rev. J. R. L, Kington, M.A., F.R.S.E., F.L.S. ; Members. Rev. S. " G. G. Aitchison, M.A., D.D., M. S. Evans, G.M.G., F.Z.S.. Hon. Justice C. G. Jackson, C. T. Loram, M.A., LL.B., Ph.D., J. McLaren, M.A., and S. Seruya ; Hon. Secretaries, Rev. E. W. H, Musselwhite, B.A. (Recorder), and Rev. G. Evans. Section F.— EDUCATION, HISTORY, MENTAL SCIENCE, POLITICAL ECONOMY, GENERAL SOCIOLOGY, AND STATISTICS. President, Prof. T. M. Forsvth, M.A., D.Phil.; Vice-^ Presidents, Prof. R. A. Lehfeldt, M.A., D.Sc, and Prof. W. A, Macfadyen, M.A., LL.D. ; Members, A. Aiken, Prof. F. Clarke, M.A., Prof. J. Finlay, C. W. F. Harrison, F.R.G.S., F.R.S.S.. Prof. R. Leslie, M.A., F.S.S., Prof. W. M. Macmillan, B.A., and Prof. O. Waterhouse, M.A. ; Hon. Secretaries, Prof. R. D. Nauta, (Recorder), and J. Mitchell. XIV PROCEEDINGS OF THE SIXTEENTH ANNUAL GENERAL MEETING OF MEMBERS. (Held in the S 021th African Schc^ol of Mines and Technology, Johannesburg, on Thursday, July 11, 1918.) Present: Dr. C. F. Juritz, M.A., D.Sc, F.I.C. (President), in the chair; C. Aburrow, Miss A. M. B'ottomley, P. Cazalet, Miss R. Clapton, W. P. Cohen. C. Constaneon, W. S. Cordiner, Prof. G. E. Cory, Prof. L. Crawford, Prof. J. P. Dalton, J. Daniel, Miss F. C. de Wet, Lieut.-Col. J. H. Dobson, Dr. Ethel M. Doidge, Prof. T- E. Duerden, Dr. A. L. du Toit, Rev. G. Evans, I. B. Pole Evans, Prof. H. B. Fantham, Mrs. H. Fitz- Simons, Prof. T. M. Forsyth, Prof. Elinor W. Gardner, F. Gimkewitz, Prof. E. J. Goddard, J. Gray, Dr. H. H. Green, Prof. J. H. Hofmeyr, J. Hntcheon, W. Ingham, R. T. A. Innes, Hon. Justice C. G. Jackson, A. J. T. Janse, A. E. Jensen, L. D. Jones, Rev. H. A Junod, F. E. Kanthack, Miss A. M. King, Rev. J. R. L. Kingon, Rev. Dr. F. C. Kolbe, C. E. Legat, Prof. R. A. Lehfeldt. Dr. C. T. Loram, W. M. McDavid, Prof. W. A. Mac- fadyen, Mrs. H. M. McKay, Mrs. F. V. McLaren. J. McLaren, Dr. B. de C. Marchand, J. Mitchell, A. O. D. Mogg, R. E. Mont- gomery, Prof .J. T. Morrison, H. K. Munro. Rev. W. A. Norton. Prof. J. Orr, R. J. Ortlepp, Dr. E. P. Phillips, Dr. C. Pijper, Dr. Annie Porter. V. A. Putterill, H. C. Reeve, S. G. Rich, Prof. M. M. Rindl. Prof. W. N. Roseveare, Prof. S. Schonland, Prof, E. H. L. Schwarz, S. Seruya, R. Shanks, G. A. Smith, Miss E. L. Teasdale, H. A. Trubshaw, Dr. P. A. Wagner, Hon. Sena- tor J. J. Ware, Prof. E. Warren, Prof. O. Waterhouse, W. C. Watson, Prof. J. A. Wilkinson, Miss M. Wilman, and H. E. Wood; Rev. Dr. W. Flint and J. A. Foote (General Secretaries), and H. Tucker (Assistant General Secretary). Minutes. — The Minutes of the Fifteenth Annual General Meeting, held at Stellenbosch, on 5th July, 1917, and printed on pp. xxiii to xxvii of the Report of the Stellenbosch Session, were confirmed. Annual Report of Council. — The Annual Report of the Council for 1917-18 having been suspended in the Vestibule since Qth July, was taken as read and adopted, on the motion of Mr. W. Ingham. (See p. xviii.) Report of General Treasurer and Statement of Ac- counts FOR 1917-18. — The General Treasurer's Report and the audited Financial Statements for the year ended 31st May, 1918, having been suspended in the Vestibule since 8th July, were taken as read and adopted, on the motion of Prof. Wiikinson. (See p. xxiii.) Alterations in Constitution. — i. Goold-Adams Medal Rules. — The question of either amending Rule (a), in view of the abolition of the University of the Cape of Good Hope re- ferred to therein, or discontinuing the award of the Goold-Adams PROCEEDINGS OF ANNUAL MEETING. XV Medals, and consequently abolishing all the rules relating thereto, was discussed. A letter having been read from Hrof. G. Potts, urging that the award of tlhe Medals should not be discontinued, as they were a great stimulus to students, the General Secretary, Capetown, explained that the founder of the Medals, in providing a die, had supplied no funds for expenses, so that the Associa- tion had to pay annually for the cost of striking and engraving the Medals. It was then moved by Prof. Rindl that the award should be discontinued for the present. Prof. Schonland moved an amendment to the effect that the question should be referred to a sub-committee for consideration and report to the incoming Council. The amendment being put to the vote, was rejected by 27 votes to 25 ; and Prof. Rindl's motion being put, was carried by 2;^ votes to 11. (2) Headquarters of Association. — Prof. Orr moved, in accordance with notice : — That "Johannesburg" be substituted for "Capetown" in Rule VIII of the Constitution. This was seconded by Dr. Annie Porter, and supported by Mr. Innes. Prof. Dalton moved as an amendment that the con- sideration of the change of Headquarters should be deferred until the next Annual Meeting. This was seconded by Mr. Kanthack, and the discussion was continued by Professors Rindl. Crawford and Morrison. The motion and amendment were then withdrawn by the movers. Reports of Sectional Committees. — The following reso- lutions, adopted by Section D Committee and recommended to the General Meeting, were read and adopted : — (a) By Prof. Goddard: This Committee, realizing the immediate necessity for the institution of a zoological survey of South Africa, strongly urges the Government to forthwith appoint a Scientific Committee to draft a practical scheme for its accomplishment. {b) By Mr. R. T. A. Innes: (i) That the Government be requested to introduce legislation restricting the sale of quack medicines, especially those professing to cure venereal diseases. (2) That information regarding the prophylaxis of venereal diseases should be published. (3) That the danger of venereal diseases and the necessity for early treatment be urged. A recommendation by Section E Committee that the Com- mittee should nominate officers for the section for the next An- nual Session was referred to the incoming Council, with power to act as might be found expedient. A resolution, adopted by Section F Committee, was read, viz. : — That four propositions relating to the Reconstitution of the Union Senate, submitted by Mr Innes, be sent forward to the Annual Meeting for discussion, to give Mr. Innes the opportunity of bringing the matter before the whole of the Associatio \ XVI PROCEEDINGS OF ANNUAL MEETING. It was resolved that as time did not allow of the discussion of the subject, it should be referred to the incoming Council. Election of Officers for 1918-19. — The following Officers were elected for 191^8-19: — President, Rev. W. Flint, D.D. ; Vice-Presidents, P. Cazalet, Prof. J. E. Duerden, M.Sc, Ph.D., A.R.C.S., W, Ing- ham, M.I.C.E., M.I.M.E.. and Prof. E. Warren, D.Sc. ; General Secretaries, C. F. Juritz, M.A., D.Sc, F.I.C., and J. A. Foote, F.G.S., F.E.I.S. ; General Treasurer, Prof. A. Brown, M.A., B.Sc, F.R.S.E. ; Editor of Publications, C. F. Juritz, M.A., D.Sc, F.I.C. Election of Council Members for 1918-19. — The follow- ing were elected members of Council for 1918-19 (the retiring President, Dr. C. F. Juritz, being also ex-officio a member of Council for the year) : — I. Cape Province. — (i) Cape Peninsula'. Prof. L. Craw- ford. M.A., D.Sc, F.R.S.E., Prof. R. Leslie, M.A., F.S.S.. C. W. Mally, M.Sc, F.L.S.. F.E.S.. Sir A. Theiler, K.C.M.G., D.Sc, and A. Walsh. (2) Kiniherley: Miss M. Wilman. (3) King William's Town: J. Leighton, F.R.H.S. (4) Middelburg: W. J. Lamont. (5) Port Elisabeth: Rev. J. R. L. Kingon, M.A.. F.R.S.E., F.L.S. (6) Stcllenbosch : Prof. E. J. Goddard, B.A.. D.Sc, and Prof. B. de St. J. van der Riet, M.A., Ph.D. II. Transvaal. — (i) IVitzmtersrand: C. Aburrow. M.I.C.E., M.S.A., J. Burtt-Davy. F.L.S., F.R.G.S., Lieut.-Col. J. H. Dobson, D.S.O., M.Sc, M.I.Mech.E., M.I.E.E., A.M.I.C.E., Prof. H. B. Fantham, M.A., D.Sc, A.R.C.S., F.Z.S., J. Grav, F.I.C, R. T. A. Innes, F.R.A.S., F.R.S.E.. J. W. Kirkland, M.Am.I.C.E., Dr. E. T. Mellor, MT.M.M.. F.G.S., Prof. C. E. Moss, M.A., D.Sc, F.L.S.. F.R.G.S., Prof. J. Orr, B.Sc, M.I.C.E., M.I.Mech.E., Ven. Archdeacon F. A. Rogers. H. A. Trubshaw, Prof. J. A. Wilkin.son. M.A., F.C.S., and H. E. Wood, M.Sc, F.R.Met.S. (2) Pretoria: I.'h. i^ole Evans, M.A., B.Sc, F.L.S., H. H. Green, D.Sc, F.C.S. A. [. T. Janse, :^.E.S., and R. E. Montgomery, M.R.C.V.S. (^) Potchef- stroom: E. Holmes Smith, B.Sc. III. Orange Free State (including Basutoland). — T. F. Dreyer, 'B.A., PhD., and Prof. M. M. Rindl, Ing.D. IV. Natal.— (i) Durban: Hon. Senator F. F. Churchill, and M. S. Evans, C.M.G., F.Z.S. (2) Maritsburg: Prof. J. W. Bews, M.A., D.Sc, and Prof. E. Warren. D.Sc V. Rhodesia. — Bulawayo: Rev. S. S.Dornan, M.A., F.G.S., VI. Mozambique. — Loureugo Marques: S. Seruya. In this connection a representation by the Rev. J. R. L. Kingon, that the present system of requiring a local Council Member representing a single-member centre to conduct the election of a representative for that centre for the following year placed such Council Member in an embarrassing position, was referred to the incoming Council for consideration. PROCEEDINGS OF ANNUAL MEETING. XVll Annual Session, 1919. — The acceptance by the Council of an invitation by the Mayors of Kino^ WilHam's Town and East London, for the Association to hold its next Annual Session at those towns, giving- three days to each, was confirmed. President for 1919-20 and Place of Meeting, 1920. — The provisional selection of these was discussed, and an invitation from the Alayor of Durban for the Association to hold its 1920 Session at that place was read ; but it was decided, on the motion of Prof. Orr, to leave the matter for the incoming Council to deal with. Exhibition of Apparatus. — A motion by Prof. Rindl to the following effect : — That at future meetings arrangements be made to have lantern slides, etc., illustrative of papers, and other interesting exhibits (original appa- ratus and specimens) on view at one of the evening functions. was referred to the incoming Council for consideration. Votes of Thanks. — On the motion of Prof. Duerden, it was unanimously resolved that the hearty thanks of the Associa- tion should be accorded to the following: — (i) To His Worship the Alayor and the Councillors of Johannesburg, for the cordial welcome extended to the Association, and for the Reception given to the Members at the Town Hall. (2) To the Local and Reception Committees for the excellent arrangements made for the accommodation, com- fort and entertainment of the visitors, and for the Reception given to the Members at the Union Observatory. (3) To the Council of the South African School of Mines and Technology, for their kindness in placing the School buildings at the disposal of the Association as the Headquarters for the Session, and for the use of the hostel " Sunnyside " as residential quarters. (4) To the ladies of the Home Industries Depot, for kindly taking charge of the arrangements for morning tea, and to the ladies assisting them. (5) To tihose in control who have afforded facilities for the inspection of the following: — Johannesburg Municipal Undertakings. Crown Mines. New Modderfontein Gold Mines. Dunswart Iron and Steel Works. South African Institute of Medical Research. Johannesburg Trades School. New Transvaal Chemical Works, Delmore. Power Stations of the Victoria Falls and Transvaal Power Company, at Rosherville and Vereeniging. Union Observatory. Union Steel Corporation Works, Vereeniging. Rand Water Board Barrage, on Vaal River. B XVm PROCEEDINGS OF ANNUAL MEETING. (6) To the following Clubs for admitting' Members as Honorary Members during the period of the meeting: — Rand Club. New Club. Automobile Club. Country Club. Union Club. Unionist Party Club. South African Party Club. (7) To those gentlemen who kindly provided motor cars for the motor drive round Johannesburg and Suburbs, and other excursions. (8) To the local Press for its appreciative references to the proceedings of the Session. Prof. Orr moved a vote of thanks to Dr. C. F. Juritz, the retiring President, for his services during his year of office ; and Rev. Dr. Flint moved a further vote of thanks to the retiring General Treasurer, Mr. A. Walsh, for his valuable services for many years. Both these votes of thanks were unanimously and heartilv accorded. REPORT OF THE COUNCIL FOR THE YEAR ENDED 30TH June, 1918. I. Obituary : Your Council desires to place on record its sense of the loss it has sustained during the year in the death of two of its former Presidents — Col. J. H. Hyslop, D.S.O., who was President at the Natal Meeting in 1907, and Prof. P. D. Hahn, M.A., Ph.D., who held the same office at Bulawayo in 191 1. Other losses are indicated by the names of General P. L. de Ij. da Silva, Prof. J. P. du Buisson, Rev. B. P. J. Marchaiid, Messrs. D. Cullen, C. L. Fischer (on active service), D. J. Haarlmft, A. GK>rdon Howitt (on active service), G. Rouliot, and W. W. Thompson. 2. Memuership: Notwithstanding the removal of 42 names from the register by resignation or resolution of the Council, in addition to the 11 removed by death, it is gratifying to report an increase from 712 to 774 members, no less than 115 new names having been added : The following is a comparative table showing the localities^ from which the members are drawn : — REPORT OF COUNCIL. XIX 1917. 1918. Cape Province . . . • . • ... 203 ... 215 Transvaal ... ... 337 ... 390 Orange Free State ... ... 7>7 ... 41 Natal ... ... 83 ... 82 Rhodesia . • • ... 18 19 Basutoland . ■ • . • • I Mozambique . . • ... 13 9 Swaziland ... ... I South-West Africa Protectorate 2 I Abroad • • ■ • • • 17 14 Unknown I 2 y 712 ... 774 The present number of Life Members is 84, one having died during the year, and five having been added. 3. Report of the Maritzburg Meeting, 1916: This, the thirteenth annual volume of the Transactions of the Association, has been completed and bound in uniformity with the previous issues of the series. It comprises 57 papers printed in full, and 23 by title only, making a volume of 714 pages. 4. Report of the Stellenbosch Meeting, 1917: The issue of this is well advanced in the Journal form, and the complete volume should be available at a much earlier date than last year. 5. Journal Expenditure: This has engaged the serious attention of the Council at several meetings during the year. Owing to the fact of the late publication of some of the numbers of the Journal containing the papers read at the Maritzburg meeting, the balance-sheet presented at the last Annual General Meeting did not reflect the true position of the Association, as was pointed out by the Treasurer. A Sub-committee was appointed early in the year, consisting of two sections representa- tive of Capetown and Johannesburg, to consider and report upon the financial situation, and a deputation waited upon the Minister of Education with a view of obtaining a Government Grant towards the expense of publishing the Transactions of the Asso- ciation. It was hoped that a sum of £250 might be obtained, and in due course the sum of £150 was voted by Parliament, and has been received. Without this sum the Council would have been unable to fulfil its obligations. The Council desires to place on record its thanks to the Minister of Education for his interest in the work of the Association. Ir must also he noted that by resolu- tion of the Council the sum of £150, together with £19 6s. 9d. in interest, was withdrawn from the bank, where it had been deposited in more favourable years, and was placed in the general fund. A special effort in Johannesburg to obtain subscriptions has added to the funds of the Association the sum of £150, and the thanks of the Council are due to the Sub-committee. The XX REPORT OF COUNCIL. Sub-committee has made certain suggestions with a view to cur- taiHng expenditure on the Journal, and it is hoped that these may not be without effect, although at the same time it must be borne in mind that, owing to the war, the cost of pubHcation will be considerably enhanced during the coming year if the same number of pages be printed. 6. South Africa Medal and Grant, 1918: The South Africa Medal Committee, comprising Dr. C. F. Juritz (Chair- man, Mr. J. Burtt-Davy. Dr. W. A. Caldecott," Prof. J. E. Duerden. Prof. H. B. Fantham, Prof. C. E. Moss, Sir Thos. Muir. Prof. J. Orr. Prof. M. M. Rindl, Dr. A. W. Roberts, Sir A. Theiler, and Prof. E. Warren, recommended Mr. R. T. A. Innes, F.R.A.S., F.R.S.E, Union Astronomer, Johannesburg, tor the eleventh award of the South Africa Medal, together with the grant of £50, which has invariably been presented with the Medal. This recommendation has been confirmed by the Council. 7. Goold Adams Medals, 1918: The eighth series of awards of the Goold-Adams Medals was made in connection with the Matriculation and Senior Certificate Examinations of the Uni- versity of the Cape of Good Hope, held in December last. The names of the recipients were as follows : — MatheiJiatics: Max Cohen, South African College Hi"f-^h School, Capetown. Physics: John Alexander Gilmore, South African College High School, Capetown, Chemistry : Bernard Gluck, Grey College School, Bloemfon- tein. Physical Science : Daphne Olive Tipper, Gill College High School, Somerset East. Botany : Edith Kathleen Tredgold, Girls' High School, Wyn- berg. The abolition of the University of the Cape of Good Hope will necessitate the amendment of the Medal Rules ; and the question of altering the rules or discontinuing the award of these medals is being referred by the Council to the Annual General Meeting for decision. 8. Research Grant Committee, 1918: Your Council has appointed Prof. H. B. Fantham, Rev. Dr. W. Flint, Dr. C. F. Juritz, and Mr. A. H. Reid as its representatives on the 1918 General Committee for Research Grants administered by the Council of the Royal Society of South Africa. The grants have not yet been awarded. 9. Metric Conference: In connection with the recom- mendations of this Conference for stimulating public interest in the adoption of the Metric System, the Witwatersrand Council Members were appointed a sub-committee to consider and report upon the steps necessary to give effect to the resolutions. 10. Memorial to Sir David Gill : The question of a Memo- rial to the late Sir David Gill, the first President of the Associa- REPORT OF COUNCIL. XXI tion, was considered, and several suggestions were made in regard thereto. It was resolved that a Sir David Gill Memorial Fund be instituted and allowed to accumulate for a number of years, until an amount is raised adequate for some purpose to be decided on later, and that the offer of Mr. R. T. A. Innes to act as Secretary and Treasurer of the Fund be accepted. 11. Standing Committee on Meteorological and Geo- physical Research : The recommendation of Section A at the last Annual Meeting, that a Standing Committee on Meteoro- logical and Geophysical Research should be appointed was approved by the Council, and the following Committee appointed : Principal J. C. Beattie, Prof. A. Brown, Prof. J. P. Dalton, Messrs. E. J. Hamlin, J. Hutcheon, S. S. Hough, R. T. A. Innes, and F. E. Kanthack ; Professors W. H. Logeman. f. T. Morrison and A. Ogg; Dr. A. W. Roberts, Mr. H. Pealing. Prof. W. N. Roseveare, Dr. E. T. Stegmann, Messrs. J. S. van der Lingen, and H. E. Wood; and also (subject to their joining the Associa- tion) Messrs. C. Stewart, T. Stewart, Dr. J. R. Sutton, and Prof. A. Young; Prof. Morrison to be Chairman, and Messrs. Hamlin and Wood to be joint Secretaries. 12. Subdivision of Section C: The recommendation of the Committee of Section C that the Section should be divided has been considered by the Council. Various proposals for carrying this into effect were brought under review, but as these diverged too widely to admit of reconciliation, it was resolved to accept the original proposal of Section C Committee for adoption at the Annual Session, viz. : ( i ) Botany, Bacteriology, Agriculture, and Forestry; (2) Zoology. Physiology, Hygiene, and Sanitary Science, the Committee appointed for that Session to be asked to report thereat whether any modifications appear desirable. 13. Central Committee of Industrial Research: Pro- fessor J. Orr and Messrs .J. Burtt-Davy and R. T. A. Innes were re-elected representatives of the Association on this Committee. 14. Endowment Fund Trustees: Mr. A. D. R. Tugwell, one of the trustees of the Endowment Fund, having died during the year, the vacancy was filled by the appointment of Principal J. C. Beattie, D.Sc, who has accepted the office. 15. Loan of Publications in the Library to Members: Requests having been received for the loan of publications in the Library to members, the Council resolved to approve the principle, and the following regulations regarding the same were adopted : ( i) A Member desirous of borrowing" books or journals shall forward a deposit of £1. (2) The borrower shall paj- postage both ways, and in the case of the loss of books or journals shall refund the value of the same. (3) Not more than three issues shall be held at one and the same time (4) Books and journals may not be kept longer than one month, but this period may be extended to two months if the application is renewed at the end of the first month. XXn REPORT OF COUNCIL. (5) An extension of the period shall not be granted 'f another application has been made for the same work during the first month. (6) In the case of specially valuable works, the Librarian shall have discretionary power as to the issue of the same. 16. The New Council: On the basis of membership pro- vided for in the Constitution of the Association. Section VI (d), the number of Members of Council assigned for the representa- tion of each centre during the ensuing twelve months should be distributed as follows: Cape Provhice : Cape Peninsula 5 Kimberley i Kingwilliamstown i Middelburg i Port Elizabeth i Stellenbosch 2 Transvaal : Witwatersrand 14 Pretoria 4 Potchefstroom i Orange Free State {with Basut eland) : Bloemfontein 2 Natal : Maritzburg 2 Durban 2 Rhodesia : Bulawayo i Mozambique : Lourengo Marques ... i 38 XXlll REPORT OF THE HONORARY TREASURER FOR THE YEAR ENDED MAY 31st, 1918. In handing you the audited financial statements for the year 1917-18, I regret to have to draw your attention to the fact that, notwithstanding the special grants amounting to i200, and al- though the ordinary revenue has been higher than last year by £74 i8s. id. (made up of the following: increases, subscriptions, £56 2s. 8d. : interest. £8 15s. 5d. ; Hfe fees, iio), the revenue has fallen short of the expenditure by no less than £122 12s. 46. On the expenditure side, printing and stationery is higher by £5 IIS. 5d., due to the general higher costs. Grants under Rule 9 are smaller than they otherwise would have been, owing to an amount of £3 17s. 6d. having been returned by the Maritz- burg centre. The expenses of the Annual Meeting include the amount of £10 los. granted to the Assistant General Secretary; other items are as usual. The expenses of the Journal are shown in the balance- sheet, and are sufficiently explanatory. The monthly issues have been brought closed to proper date, only April and May numbers not having been paid for at the end of May. The accounts for these have since come in, amounting together to £65 is. iid., so that the cash balance at the end of June of £92 los. 3d. may be considered as reduced by that amount, leaving £27 8s. 4d. to start the new year clear with. As I understand that the Council will frame some new regu- lations re expenditure, I would say that, excluding extraneous donations, the income for the year 1918-19 may be estimated at £725, and the balance as above added makes available for ex- penditure the sum of £752, against which the average ordinary expenses amount to approximately £270, leaving a balance of £482 for Journal expenditure and carrying forward. The Endowment Fund now amounts to £1,548, a sum of £60 having been added, and £10 withdrawn. The Medal Fund amounts to £1,445 13s. ,8d.. invested at 4 per cent. The annual requirements amount to £53, which would be yielded by £1,325. I would suggest that some of the surplus money might with advantage be used for grants in aid of scientific research, as that side of the Society's original pro- gramme has not been given effect to for many years, and our ordinary income does not allow of anything being done in that direction. All investments are taken at face value. A Walsh, Hon. Treasurer. June 20th, 19 1 8. XXIV GENERAL TREASURERS ACCOUNT. H W w u < > < W H Cii O fc 2; O < U o m CO < < u < ^-, o 00 w o> u 1— 1 y, .. w > t-H < U CO S fc Q W Q J3 < w o H o u (J < w H t— I Q w X w Q < w :d :^ w > w H* 0\ O CO o o OOOO o o o •r o 00 o o o o o 1^ > 0\ c o 5 0\ t/) On a . o t- in (« U r- r\ r: tn a; ni 3 >- fflco< 23 - ' • +j ^ ■•3 "* . !- ~ c 1/2 O 0; -a • I— J2 c o tn O c o o o o vo o o too 00 u-.vO t ■1-^ O 0\ t 00 *- t^ o OC o •-H O 00 IN 0\ O . en £ J2 ?? C>__ -" ^ ou- ...'TJ.a^iw.n:: 3-- o 3 w CS O a ■ n c o a) ;5w o o V (U S D C "O c o HH Ufe _: O\co O O O („• tN. <~o o o o 25; (/3 u H n < • OJ • ■< E.£- ^^ --g ° ^ s o "re . o o Q < Q W < I— I < H O CO ^ s; D O U U < w H Q 25 (d Ph X w < Ui > Pi •a -t li-. CO 1^ ON — u _: o ■^ .^ Q 00 '30 ir, -1" 'O ~1 O >0 CO -4-' ^ i:: fO:: o rt c U- o X ^. 1— 1 ^ — ON o t: " o , "tr f^ 03 03 ^ c f^ CTj kr- c/} r^ -«— ' _ u, C/J 'or. re C£ O . c ;= ,^ c ;*, So; XXVI GENERAL TREASURER S ACCOUNT. ^ o o o CO ° 2 ° H^ 0000 o c o o H w o Q 00 0\ V o • en ■ ^ ■ w • -M oc o c o o ooo - Tl- o r— — m ct o c <5 3 ^1=; -4-' rt^ S a P = <^ r o en 5! U c Oj oj CS rt m O , H ■ " o o o o ■13 tn C ^ I) a> 1 = ll O li ->-• u •ti o 5 rt o t» aj J-i > o cc; (L) en C >> i> Vh JS O ^c ^ n > o C8 O. o £"0 iwr; tn •"•O o c n o 03 jO o' ?^ ;n 'I' > U (/I •sec I- O O >^ en o U3 CS O u "^ tn "" I-. ^ l; Mineralogi, och Geologi. Geological Society of South Africa : Transactions. Geological Society of Tokyo: Journal. Geological Survey of New South Wales : Reports. Memoirs. Alineral Resources. Geological Institution of the University of Upsala : Bulletins. Geological Society, London : Abstracts of Proceedings. Bulletins of the Wyoming State Geologist. United States Geological Survey: Annual Reports. Mineral Resources. Bulletins. Monographs. Professional Papers. Florida State Geological Survey : Annual Reports. Union of South Africa Mines Department : Annual Reports. Canada Department of Mines: Museum Bulletins. Memoirs of the Geological Survey. Reports. Egyptian Ministry of Finance : Geological Reports. Geological Survey of Western Australia: Annual Progress Reports. Bulletins. Journal of Industrial and Engineering Chemistry. Journal of Chemical Technology. The Chemical News. ASS(K"1ATI()\ LIBRARY. XXXlll The Mineralogical Magazine. South African Association of Analytical Chemists: Proceedings. Meteorology. Royal Meteorological Society : Quarterly Journal. Mount Weather Observatory : Bulletins. Observatorio Campos Rodrigues : Relatorio. Resumo mensal. Egyptian Ministry of Finance: Meteorological Reports. Agriculture. Regia Scuola superiore agricoltura di Portici : Annali. International Institute of Agriculture, Rome. International Crop Report and Agricultural Statistics. International Review of the Sciemce and Practice of Agriculture. Documentary Leaflets. Statistical Notes on the Cereals. Massachusetts Agricultural h^xperiment Station : Annual Reports. Bulletins. Maine Agricultural Experiment Station : Annual Reports. Agricultural Gazette of New South Wales. Department of Agriculture, New South Wales, Science Bulletins. United States Department of Agriculture : Experiment Station Record. Year Book. Journal of Agricultural Research. Rhodesia Agricultural Journal. Biology and Physiology. Bulletin de la Societe Imperiale des naturalistes de Moscou. Kungl. Svenska Vetenskapsakademien : Arkiv for Botanik. Arkiv for Zoologi. Journal of the Linnean Society, Botany. Bulletin of the Wisconsin Natural History Society. The Medical Journal of South Africa. University of California: Publications in Botany. Linnean Society of New South Wales : Proceedings. Missouri Botanical Garden. Annual Reports. Annals. Bolus Herbarium : Annals. Smithsonian Institution (United States National Museum) : Contributions from the United States National Herbarium. XXXIV ASSOCIATION LIBRARY. Royal Botanic Gardens, Kew : Bulletins. Union of South Africa: Reports of the Director of Veterinary Research. The Australian Zoologist. Lloyd Library : Bibliographical contributions. Mycological Notes. Abstracts of Bacteriology. Entomology. Bulletin of Entomological Research. Review of Applied Entomology. Astronomy, Mathematics and Physics. Royal Astronomical Society: Memoirs. Monthly Notices. Journal of the Royal Astronomical Society of Canada. Harvard College Astronomical Observatory : Circulars. Annals. Annual Reports. Union Observatory Circulars. Observatoire Royal de Belgique; annuaire astronomique. KJiedivial Observatory, Helwan, Egypt : Bulletins. Kodaikanal Observatory Bulletins. Kodaikanal and Madras Observatories : Annual Reports. British Astronomical Association, Journal. Memoirs. Lick Observatory : Bulletins. Nizamiah Observatory : Reports. Astronomical Society of India; Journal. Monthly Notices. United States Naval Observatory Publications. American Ephemeris and Nautical Almanac. Western Australian Astronomical Society : Proceedings. Kungl. Svenska Vetenskapsakademien : Arkiv for Matematik, Astronomi och Fysik. Loaidon Mathematical Society : Proceedings. Tohoku Mathematical Journal. National Physical Laboratory, Middlesex: Collected Researches. Reports. Universidad Nacional de la Plata; Contribucion al estudio de las Ciencias fisicas y matematicas. F)iysiical Society of Londo-n : Proceedings. association library. xxxv Education, Political Economy and Sociology. United Empire. South Africa. Ohio State University Bulletin. International Institute of Agriculture, Rome: International Review of Agricultural Economics. Royal Dublin Society : Economic Proceedings. Athenaeum subject index to Periodicals. Geography, Oceanography and Hydrography. Societa Italiana per il progresso delle Scienze : Comitate talassografico : Bolletinos. Memorias. The Geographical Journal. The Geographical Review. United States Geological Survey; Water Supply Papers. Egyptian Ministry of Finance: Survey Department Papers. Istituto di geografia fisica e vulcanologica della R. Universita di Catania : pubblicazioni. United States Department of Commerce, Coast and Geodetic Survey : Special Publications. Annual Reports. Engineering. Proceedings of the American Institute of Electrical Engineers. Journal of the South African Institution of Engineers. Transactions of the South African Institute of Electrical Engineers. South African Society of Civil Engineers : Proceedings. South African Engineering. Technology. Patents for Inventions : Abridgments of Specifications. The Illustrated Official Patents Journal. Souitih African Journal of Industries. Anthropology and Ethnology. Journal of the African Society. x^rch.eology. Bulletins of the Archseological Survey of Nubia. PRESIDENT'S ADDRESS. ADDRESS BY CHARLES FREDERICK JURITZ, M.A., D.Sc, F.I.C. PRESIDENT. Since last we met in annual session we have had to mourn the loss of several of our members. Some of these have yielded up their lives in the service of their country — yes, and in a larger sphere of service, the service of humanity — on the field of battle ; others, who had, in another sense, spent their lives for South Africa, passed away in the quiet of their own homes. Amongst the latter I pause for a moment on the names of three who had held high offices during some of our past annual gather- ings : two had been Presidents of the Association, and the third was a sectional president. Paul Daniel Hahn, a man of con- spicuous personality and strength of character, who thoroughly appreciated the inestimable value of science as a factor in national prosperity, achieved an immense work for this land in fostering 2 PRESIDENT S ADDRESS. the scientific spirit during a period exceeding an entire generation, not only amongst the youth of the country generally, but more particularly amongst the agriculturists. James Hyslop, perhaps better known in the Province of Natal than in the rest of the Union, coupled military instincts with a keen desire to alleviate mental ailments among his fellow-beings. Modest and unobstru- sive, he accomplished the bulk of his valuable labours sa silently that the great world around was almost unaware of them, but those who came from other parts and saw, returned deeply im- pressed with admiration for the man and for what he had done. Then there was Bernard Alarchand, keen as an educationist, and, if that were possible, keener still to uplift sunken and degenerate countrymen, alive to every opportunity of fashioning such into thrifty and useful members of society. Each of those three worked for South Africa in the manner that best became him. In aims and methods they differed considerably, but all were alike practical, and their aggregate achievements covered a field so extensive that few, if indeed any, of us adequately realise its proportions. We are now meeting in annual session for the fourth time since the war began, a war which has made some of us wonder whether an association for the advancement of science is after all an institution beneficial or prejudicial to the best interests of the human race, for it is undoubtedly science — organised, calcu- lating, deliberately applied science — that has made this un- paralleled conflict — a conflict of arms, yes, but more of intellects — possible. But the suggestion is fallacious : fire and water are ills only when they are allowed unbridled scope and become mas- ters ; under control they serve us excellently. The world had got into the way of luxuriating in all the unprecedented benefits that new forms of applied science had conferred on human- kind during the first decade of this century, when the second decade let loose on an unprepared world all the evils, all the passions, all the debasing influences that misapplied and mis- directed science could call into being. I doubt whether humanity at large has even now learnt the lesson which this colossal disaster should teach it ; that principle and loftiness of purpose are more to be desired than knowledge, and that mere science, uncontrolled by man's higher aspirations and nobler feelings, may involve the human race in an inconceiv- ably stupendous catastrophe. We are fortunate indeed that we do not yet possess the highly dangerous power to unchain the interatomic energy now happily latent in our stabler chemical elements. Is science, then, to be blamed for that which the world now suffers? Is it not rather the circumscription of science that is the cause of it all? Inasmuch as science is knowledge, our science of necessity remains imperfect as long as we know only in part ; and if a so-called science levels in the dust all the highest moral and spiritual principles in man, if it outrages liberty, flaunts truth, tramples sanctity underfoot, casts chivalry to the winds, and acclaims as its god all that is vile and loathsome and devilish, it {'RKSIDKKT S ADDRESS. 3 remains a stunted travesty of the full-orbed science that seeks the highest ideals of knowled_2^c in every realm. And so Principal Beattie was unquestionably right some months ago when he said that the present world contest is a struggle not between nations, but between ideals. Admittedly neither ideal is perfect, but the ideal that is low and grovelling and sordid and selfish is obviously the ideal of a mind that has no vision for anything loftier. If science is to confer the highes^t benefits on mankind, its outlook must be ever broadening, and to a truly scientific people there should be nothing tending to prejudice or dogmatism resulting from a circumscribed range of A-ision. In one of his " short stories," H. G. Wells describes con- ditions amongst a race of degenerated human beings, who vege- tated in a mysteriously isolated and forgotten valley amongst the mountains — a valley that had in it all that the heart of man could desire — sweet water, verdant pastures, glorious climate — -but a valley cut off from the outside world, less bv reason of the ice- capped clifTs of rock that walled it in than because of the fact that 15 generations ago a strange disease had seized upon the dwellers in that valley, and had left to them total blindness as an inheritance. The walls of ice that isolated them geographically they could have surmounted, as man's ingenuity often scales the highest of material difficulties, btit the sightlessness which hemmed them in mentally cut them ofif efifectually from the world of men. The most serious obstacles to the advancement of a country are not geographical. When a great movement is in progress one sometimes finds that those who should be in the van fail to lead because they lack discernment. It was not Nelson who was blind at Copenhagen, but the amiable and kindly Sir Hyde Parker, who seldom ventured to take responsibility, while Nelson, when he put the telescope to his blind eye, had really the clearer vision of the two. Now South Africa had been geographically cut of¥ from the centres o'f scientific activity in the Northern Hemisphere for generations, but to-day all the important hap- penings of Europe are flashed across 6,000 miles of ocean in a few hours. The opening decades of last century brought no less sensation in the way of scientific discovery to our forefathers than the discoveries of the last 18 years have brought to us, and one of the chief contributors to the new light that dawned on men a century ago was Prof. Hans Christian Oersted, of Copenhagen, who laid the foundations of electro-magnetism by his discovery that the electrical current of a galvanic battery, when passed through a platinum wire, acted on a compass needle placed below the wire. Every naval man at the beginning of last century was not as clear-sighted as Nelson, and illustrations may be quoted of some of very different type who, it is much to be feared, still have representatives amongst us in this rapidly closing second decade of the twentieth century, as they had amongst our ancestors in the second decade of the nineteenth. 4 PRESIDENTS ADDRESS. For some time before Oersted's clear reasoning- led him to the precise point at which his discovery was made, Ronalds, of Hammersmith, had been busy devising an electric telegraph, and succeeded in working it on a small scale between two stations 525 feet apart. When the possibilities latent herein were com- municated to the Admiralty, the reply was received that " tele- graphs of any kind were wholly unnecessary, and no other than the one in use would be adopted." The British Admiralty's stolid refusal to see any better way of doing things than that of the time-worn groove was emulated by a large proportion of the British nation when war was declared four years ago, and the silly formula, " Business as usual," was flaunted about. The dis- illusionment soon came, for the voice of Science began to assert itself, and demanded audience, until the stolidity that was pro- verbial began to melt, and the need of organising the stud\- and application of science was realised simultaneously with the dawn- ing of an unpleasant feeling that the enemy had been beforehand in this matter. Then it was that the leaders of science laid the responsibility for the lethargic condition of the nation at the door of the Gov- ernment, and charges of administrative inertia with respect to the support of science as a national duty were heard. The reply of the British Admiralty to Ronalds, of Hammer- smith, is an instance by no means unique of ci>rjx)rate self-com- placency in regard to science : an entire nation exhibited a similar mental twist when that brilliant chemist, Lavoisier, was executed by the French Republic in 1794. After his sentence he had pleaded for a fortnight's reprieve in order that certain experi- ments on which he had been engaged might be completed, but the reply was. " The Republic does not need such," and so the guillo- tine terminated Lavoisier's researches. We speak of Liebig as the father of modern agricultural chemistry, and justly so, but the extent to which Liebig might have been forestalled had not the blundering short-sightedness of the French Revolution sheared Lavoisier's life away nine years before Liebig was born we shall never know. " Wholly unnecessary !" " We do not need such !" The ejaculations, we say, of a purblind administration — of an ob- sessed nation! And yet. to-day, 120 years after Lavoisier's death, even to-day, after four years of intense warfare, it is surprising how much we are still inclined to echo the stupid cry of the Republic, " We do not need such !" What foundation is there for such an assertion ? What w'arrant has one for diagnosing national lethargy and adminis- trative inertia? Listen to some evidence. Many of us in South Africa have most perverted notions of what the national attitude with regard to the study and encouragement of science should be. In the United Kingdom, they probably imagine, that attitude is all that could be desired, and here, most likely, it is just what it is there. Both assumptions are incorrect, but as I do not wish you to accept such a statement on my bare assertion, I ask pardon for introducing several quotations. Much strong language has PRESIDENTS ADDRESS. 3 been uttered on this subject since the war began, but Httle of it has been stronger than that of the eminent bacteriologist. Sir Ronald Ross, in Nature of January 13th, 1916 — 17 months after the declaration of war : — Tt is idle to disguise the fact [said he] that recent events have filled most educated persons with a sense of extreme resentment against the administration of this country. . . . It is felt by many (and I am one of them) that we live under the rule of the invertebrates. The people who administer the country are not the best, the most vigorous, and the most sagacious of men. They are too often the time-servers and the mediocrities. The maladministration of scientific afifairs is only one of the many forms of maladministration ; but, on the whole, I think it is perhaps the most important form, because it gives to the mind of the whole nation a lower, a meaner, and a thoroughly sentimental and unpractical turn. Scarcely less trenchant in parts is an editorial in Nature of March 29th, 1917 — 31 months after war was declared. There we are told that such matters have been too much in the control of the clerical establish- ments> who are ignorant of the significance of chemistry, and its vital importance to the interests of the country. Even if one had no other evidence, the obvious consensus of opinion on the part of scientific men throughout the length and breadth of the British Dominions should suffice to convict the nation of criminal neglect of science in general, and of chem- istry in particular. Witness against this neglect has. I say. been borne in every part of the Empire. In England, Sir William Crookes suggested as a remedy a Ministry of Science, and repre- sentation of Science on the Privy Council. In the Nova Scotian Institute of Science, Professor Eraser Harris put forth a power- ful plea for the institution of a Department of Science, presided over by a Cabinet Minister. The comfortable mental inertia of the British race he deemed to be such that " nothing less than this irruption of Teutonic brutality " could have shaken it, and so he urged that the official interests and the economic aspects of science should be presided over by someone who knows some- thing about them.* Not mere lapse of time — not six score years of unparalleled scientific progress since the day when Erance rewarded the dis- coverer of oxygen with the guillotine — sufficed to break down the impenetrable crystalline structure of the British mind. Natura non agit nisi fluida, and so a stupendous war had to intervene and melt this conl}X)site solidity before anything like chemical action could be brought about. The war has been called a chem- ists' war. It has been described over and over again as a war between the engineers and chemists of the belligerent countries, with chemistry in the front ranks. Within limits the statement is true, and certainly it is far nearer the truth than many admin- istrative authorities realise. Bearing that in mind, hear the testimony of two chemists of note, one from the British and one from the American side of the Atlantic. * Nature (1917), 99, 237. D PRESIDENT S ADDRESS. Prof. G. G. Henderson, of the Royal Technical College, Glasgow, addressing the British Association as President of Section B. animadverted strongly on British failure to keep pace with other countries in industrial chemistry. This he ascribed to the general ignorance of and indifference to the methods and results of scientific work which characterise the people of Great Britain. For many years past [he said] our leaders in science have done all that lay in their power to awaken the country to the inevitable and deplor- able results of this form of " sleeping sickness," but hitherto tlieir recep- tion has been much the same as that accorded to the hero of " The Pilgrim's Progress : " they lookt upon him, and began to reply in this sort : Simple said, / see no danger; Sloth said. Yet a little more sleep; and Presumption said, Every vat must stand upon his ozvn bottom. And they lay down to sleep again, and Christian went on his way."* Similar in its kernel was an utterance by G. W. Thompson in the course of an address to the American Institute of Chemical Engineers last year.f Germany has made great advances in chemistry. Some think that this is due to her system of education, and probably this is partly true. Some think that it is due to the far-sighted wisdom of public men. This. too, is probably partly true, but the real success of chemistry in Ger- many in my own opinion has been due to its greater popular appreciation. . . . Progress ultimately is in the people of a nation, their developing thoughts, their appreciation of the world that is about them. One is astounded to find that a blundering nation may receive a staggering shock as a result of its blundering course and yet persist in the selfsame course. One expects a civilised nation to show more common-sense than a flock of sheep dashed into by a railway train. Britain was staggered when she discovered, at the outbreak of war, her extreme poverty in three departments of chemical manufacture — synthetic dyes, synthetic organic prin- ciples, synthetic drugs. One tnight imagine that this would have taught her wisdom, and that she would forthwith have begini employing her chemists to best advantage ; but no, it was not until the introduction of asphyxiating gases by the Germans that it begati to dawn on Britain that she was acting unwisely in making musket-bearers of her chemists. It was then, as Nature points out.t that the War Office called for volunteers with training in chemistry, and formed a new fighting force, " selecting the officers from chemists already holding commis- sions, and transferred non-commissioned officers and men with scientific qualifications from other units." But the awakening came far too late to be of the service that it might have been. Let me quote to you some forcible sentences by Dr. Geoffrey Martin, a graduate of the Universities of London, Bristol, and Rostock, a lecturer on technical chemistry in one of London's University colleges, one of the most lucid writers of the day on both theoretical and applied chemistry, and the author of numerous works both in English and in German. He says : — * Rept. Brit. Ass. for Adv. of Sc. (1916). Newcastle-on-Tyne. 369. ■f Jotirn. Ind. and Eng. Chemistry (1917). 9 [2], 182. X March 29, 1917, p. 85. PRESIDENT S ADDRESS. 7 British chemists believe that if their Government had h'stened to them years ago the Germans would have been beaten in the early stages of the great war, and that thousands of lives would have been saved, [and that] in the autumn of 1914 Germany was saved from a crushing defeat because she possessed the sense to encourage her chemists. We may. however, candidly admit that the Anglo-Saxon pub- lic has gone some distance in the direction of learning wisdom during these four years. An American chemist was delivering a presidential address to an academy of science on the evening of the day on which President Wilson .signed the Declaration of War, and he said that probably the greatest contribution to science of the present war is the awakening of the average mind to the power and value to mankind of that group of phenomena which we study as chemistry. This is probably because we most easily grasp and appreciate applications rather than generalisations, and the use of chemistry in war has been a revelation to the general puljlic. My predecessor of three years ago, in a paper read by him at our Stellenbosch meeting last year, urged that " each State must be organised for efficiency." If that be aimed at, then the principle " Every man in the post that fits him best " will have to become one of the guiding principles of organisation, as it has done in the United States. The Western Allies were slow to realise the need of applying this principle, at all events as far as scientific qualifications were concerned, but they have begun to see it now. In the " Report on the War Service for Chemists " to the Council of National Defence of the United States, it was stated that Eingland, France, and Italy found it necessary to recall all chemists from the ranks ; Canada does not allow chemists to enlist ; chemists have saved Germany up to the present time. Prof. Camille Matignon, writing in the Revue Gencrale dcs Sciences in January, 191 7, explains how this salvation was brought to pass. Germany would surely have been faced with disaster at the commencement of the present war had she not devised means of providing herself with a sufficiency of nitrates. These were absolutely essential for the production of explosives, and the outside supply being cut off, Germany could only be saved if the problem of converting ammonium sulphate into nitrates on a large scale could be solved. How this was done is too long a story to tell here ; suffice it to say that by encouraging people to use gas and coke instead of coal a large annual output of ammonium sulphate was secured, and by the end of 191 5 the Anhaltische Maschinenbau Gesellschaft of Berlin had established 30 installations for the conversion of this into nitric acid at the rate of 100,000 tons per month by means of a process newly worked out by Frank and Caro. A factory employing Pauling's process for the preparation of nitric acid from atmospheric nitro- gen was established in Saxony, and a third method — the direct synthesis of ammonia — was subsidised by the German Govern- ment after the Battle of the Marne, so as to increase its annual production to 300,000 tons of ammonium sulphate. 8 president's address. Contrast with this the official attitude in Great Britain when the war began. " The need for fit men was the first considera- tion," says the Editor of Nahit-e* and the need for chemists, as such, in other spheres directly connected with war was not at first recognised. OfiFers to the War Office of scientific assistance emanating from organised bodies and from individuals were politely acknowledged, and pigeon-holed for future reference in case of necessity. The British Admiralty and Ronalds over again ! It is true things are somewhat different to-day in the Old World: to quote a recent address by Prof. W. J. Pope, F.R.S.. of Cambridge, President of the Chemical Society if The general public, the public authorities, and our governing bodies now regard as vital to the interests of the country a science which they previously left unconsidered as being of purely academic interest. The error has been fully and frankly admitted. As the editor of the American Journal of Industrial and Engineering Chemistry wrote a few months ago,f France and England fully acknowledge that they greatly decreased their efficiency by sending their scientific men to the trenches. Although they have since withdrawn most of those still alive, § and are now using them in special service, the dearth of technically-trained men has been and is severelv felt. As I make this quotation I think in particular of such a man as the late H. G. J. Moseley, whom I had the privilege of meeting in Australia four years ago, and whose work in England as a scientific investigator was incomparably greater than the brief service which -he rendered in the fighting-line before his brilliantly begun career was cut short — a man of whom the Chairman of the Chemistry Committee of the United States National Research Council said that he was allowed to go to the front when he should have been retained at home at all costs. When America first entered the war there was for a brief period the danger that she, too, would follow the mistaken lead of England and France, and so Dr. W. H. Nichols, Chairman of the Committee on Chemicals of the United States Council of National Defence, felt impelled to say : Already serious trouble has come to many of our chemical plants, and plants employing chemists, as a result of the draft, and unless wise pro- vision be soon made we can foresee a condition which it will cost months to rectify. Lieut. Engel, of the French Commission, drove home these remarks : I desire first to emphasise [said he] the mistake it is to take chemists from where they are most needed, and to place them in the trenches, as we did ourselves, and have lost them where they were most needed — in the laboratories and the industries. We made this great mistake at the beginning of the war. We took all chemists available and sent them into * March 29, 1917. t Chem. News (1917), 116, 199. t (1917), 9 [11], 1002. § To the number of 128,000, it is said. — Journ. Ind. and Eng. Chem. (.1917), 9 fii], 1009. PRESIDENT S ADDRESS. 9 ' the regiments, mostly the infantry. Perhaps we lost 60 per cent, of the mobilised chemists below the age of 40. . . . At the National School. in the scientific department, there was a loss of about 52 per cent, in the first ten months of the war. I cannot tell you emphatically enough that we must in all of our allied nations do our best to keep scientific men where they are most needed, not only for war problems, but for the future upbuilding of these nations.* Such quotations as the above afford an informative pano- rama to the average South African, who has, I fear, but Httle conception of the manner in which the position is regarded by scientific inen overseas ; they give us, moreover, some inkling of where Germany's power and our own weakness He. If we wish to probe a Httle further into ulterior causes, we may find some- thing of what we seek in Sir Ronald Ross's remark that for more than half a century before the war England has ceased to be an intellectual nation ; the public at large has remained indifferent to science, art, literature, invention, and all the great intellectual pursuits, and has given itself up to game-playing, party-politics, faddism, and a debased drama. We are now paying the penalty, and, if I do not mistake, will have to pay a heavier one before the end. How is it that we do not realise that they do these things differently in Germany? Mr. A. G. Thacker, writing in Science Progress i8 months agof on the recent advances in anthropology, had occasion to refer incidentally to German science, and used these words : Even now the people of this country do not properly appreciate the fact that the remarkable strength displayed by the German nation during the last thirty months has been very largely the power of German science. Eailing a much more adequate cultivation of science, there will be no great future for Great Britain. Now why has German science such a power? The answer is : Because of the wise policy pursued in connection therewith. Let me offer you an illustration. Prof. J. Stieglitz, of the Uni- versity of Chicago, President of the American Chemical Society, a few months ago said with special emphasis that, in his opinion, the most important single factor which would lead to a tremen- dous increase in power in the industrial development of the United States is not immediately a question of scientific achieve- ment, but a factor found in a simple psychological analysis of the country's industrial situation. J Let our manufacturers but awaken [said he] to the full meaning of the simple old behest that the labourer is worthy of his hire, and they will be astounded at the results. He went on to relate how the chief chemist in one of the largest manufacturing concerns in the country perfected a device that saved the corporation perhaps 80,000 dollars a year: his reward was a princely increase of 200 or 300 dollars a year in salary. " Let me say," he continued, " that I promptly took him away from this corporation — we cannot afford to waste good men in such places." American tendency, he said, is to exploit *Jour. Ind. and Eng. Chem. (1917), 9 [10], 925-926. t January, 1917, p. 477- t Science (1917), 46, 324, 325. lO PRESIDENT S ADDRESS. the chemist as an employee, instead of treating him as a partner, and by way of contrast he mentioned the Badische Anilin-Fabrik, where, from the lowest workman up to the highest chemist, every individual is by contract guaranteed a royalty, a definite share in the money earned or saved by any suggestion or discovery on the part of the individual. Britain. I need not say, approxi- mates in this respect more to American than to German practice, and to say what some of Britain's colonies do is quite superfluous. Often we find that private manufacturing firms, who ought to be employing whole-time chemists of their own, seek to make amends for the lack by periodical interviews with Government chemists. On the other hand, it is a significant comment on the rate of remuneration in Government scientific departments that one of the must important laboratories in this country should have lost five members of its stafi:' within the last six months because considerably better financial prospects were offered by a private firm and by an adjacent administration — this at a time when the Government was already achertising for three chemists to fill other vacancies caused by the war. American scientific journals have reiterated that chemists have become scientific hacks solely because they have not made their voices heard. They are, 1 know, proverbially a ])atient class, and have e\'er been so. As long as 200 years ago Pope spoke of The starving chemist, in his golden views Supremely blest. But there are limits. Let me revert to the comparison between British and Ger- man methods in regard to chemists. In a supplement to the Manchester Guardian of June 30th, 1917, Prof. A. G. Green attributes the decadence of the dyestuff industry in Britain, and its prosperous career in Germany, to the fact that though in both ■countries the managing firms were originally chemists, those in England gradually passed into the hands of purely commercial men. Some of you may recollect that, in my presidential address given in this city three years ago to the South African Association of Analytical Chemists, I referred to the British efforts to regain the lost industry, and quoted the late Prof . Meldola as saying that the supposition that this could be done by staring a company whose directorate is to consist solely of business men is simply ludicrous. What do we hear on the subject to-day? This: The Government meant well, the husiness men meant well, but after three years the hard facts can no longer l)e denied. The protests of British scientific opinion, ignored at the time, are in the event justified beyond all measure. The fact is, it is not enough to mean well ; it is knowledge that is wanting, not good will. That is the state of affairs in Britain : how far is South Africa behind Britain? South Africa is a new country, and her future — she imagines — lies all before her : shall we be right in adapting Mr. Thacker's remark that, failing an adequate cultivation of science, she will have no future at all? On the other hand, one does not wish PRESIDENTS ADDRESS. II these reflections to be misunderstood. A mere cultivation of science is hopeless.ly inadequate to ensure the best results. If we never realised this before, we should certainly be positive of it now. South Africa, I trust, will have something more than mere organised science. G. K. Chesterton has said that the weakness of Prussian organisation is that it is destitute of all that is or- ganic. An organ is not at best, he says, when it is a barrel organ. Precisely what makes the difference between the mechanical and the organic is the presence throughout the system of that invisible vital principle which we call in the lower organisms " life," and in the higher organisms " soul." I have spoken about the symptoms of inertia: to a certain extent it has been generally admitted that the diagnosis is correct, and efforts are being made to apply remedies, but it is to be feared that in some cases, even where the heart has been put right, the head is still woefully wrong. Prof. W. J. Pope has wisely insisted that public opinion should be educated to realise that concentration upon scientific progress, urgent in time of war, is also vital in time of peace*. If such be not done, legislators and administrative bodies will be in danger of flying off at a tangent when a crisis occurs, and when a nation thus loses its head, panic legislation sometimes results : measures are adopted which effect more harm than good. We. I trust, are not in such a condition now. Nationally, our heads may be cool enough, but the dawning sensation that our nurture of science has been de- fective and is in urgent need of buttressing has roused in us a zeal which, at times, I fear, is not altogether according to know- ledge, and that blessed word " research " is again brought for- ward, dazzling the uninitiated with the fancy that it is a kind of Kut-el-amara, by the taking of which we may expect to gain control of all Mesopotamia. Is it consistent — not to say dignified — on the part of a nation and its rulers to treat science with apathy, and starve scientific investigators in days of ease and plenty, and then to turn to them with wringing hands when smitten by panic? Some years after I was first appointed to a position under the Government of the Cape Colony, a far-seeing permanent head of the Minis- terial Department to which I then belonged, said to me, " If I could have had my way, twelve chemists would have been ap- pointed instead of one." If nothing more than the mere training of men for such posts had then been begun, and appointments made five or six years later, a vast amount of useful work accomplished would now stand to the country's credit. Now turn to another picture. When the South-West African Cam- paign was undertaken, and there were fears of the water supplies being poisoned, and there was a dearth of chemists, a score of men were sent helter-skelter into my laboratory one day, and I gave them an hour's experimental lecture on testing for poisons, after which they were attached to various units, provided with the requisite appliances, and despatched to different parts of the * Chetn. News (1917), 202. D 12 PRESIDENTS ADDRESS. invaded territory, in order to apply their hastily-acquired skill. Most of them had never before had so much as an hour's lecture on chemistry in their lives. Panic research will undoubtedly lead to effects analogous lo those resulting from panic legislation. In neither case can the procedure be sane, well-considered, evenly-balanced. In the United States Experiment Station Record last October it was said that The lesson has been taught that research cannot be carried on spas- modically under stress of temporary emergency, but must go forward continuously, year in and year out, from generation to generation. And it must be surrounded by conditions in which it will best thrive, without the handicap of being expected to produce something every day of imme- diate market value or application. Now in many respects our mode of action in the past has been the exact antithesis of this. Let me given you one example from a printed report of my own, dated 13 years ago. Discussing ihe investigation of our poisonous plants. I remarked: This most important branch of the laboratory's work is perhaps the most unsatisfactorily performed. It is carried on at present in a most casual way, instead of being earnestly and systematically undertaken. Whenever a poisoning or suspected poisoning case occurs, problems have to be grappled at short notice, and in a hurried and therefore often per- functory manner, which should have been carefully investigated at leisure months beforehand. In eleven successive annual reports I continued making allusions to this matter, and in a report four years later than that just quoted from I said : The complaint that I have to make is that the casual and incidental character that these investigations are compelled to assume greatly militates against results of enduring usefulness being arrived at. Matters of this kind should be dealt with because of their intrinsic value and not, as they at present are, merely as side-issues to the legal proceedings against some " Kaffir doctor." In scientific research, as in so many other phases of activity, it is " slow and steady that wins the race ": ad hoc measures only court failure; and carrying this principle to its logical conclusion means that research in pure science has the strongest claim on State aid and encouragement. Prof. A. W. Crossley, in an address on " Science and industrial problems," delivered before the Royal Institution about three years ago, aptly quoted a remark made, some two months before the war broke out, by one of the world's most prominent industrial chemists — " Pure scientific research work, carried out in the laboratory, is the soul of industrial prosperity " ; and, as Sir J. J. Thomson has said, applied science ma)^ lead to reforms, while research in pure science leads to revolutions, a remark which may be supplemented by one of Prof. W. J. Pope, that " practically every useful chemical development of a technical kind has arisen as the result of some [)urely scientific investigation."* But this is not the class of research that appeals to Govern- ments : the research that they want and are willing to encourage * Chcni. News (1917), 116, 200. PRESIDENTS ADDRESS. I3 15 of the ad hoc type — perfectly utilitarian. Read what an edi- torial in Nature of June 2131.1917, says in this connection: Though we are assured that " after the war " scientific research is to receive substantial aid from the State, there is reason to fear that this aid will be given with qualifications. In other words, the promise is extended only to investigations calculated to further the ends of commerce. Students of what is commonly known as " pure science" will not only not participate in the grants that are to be made, but they may be called upon to subsist upon even smaller doles than were allotted to them in the pre-war days. Our administrators seem incapable of appreciating the fact that "applied science" has its roots in "pure science," so that if these be starved the tree will of necessity be stunted. B'ut surely, some may say. during a period of great national emergency, at all events, we cannot alTord to spend on pure scientific research time and money which should be devoted to the objects of the immediate and critical present. Admitting that there may be validity in such an argument, and that those researches which concern the manufacture of arms and ammu- nition are vital, yet an adequate supply of foodstuffs is equally essential even for the waging of war, and that supply depends upon the nation's agricultural prosperity, which is in turn de- pendent upon the farmer's ability to maintain his soil at its normal productivity, and. if possible, to increase the latter. More- over, it remains for the close of the war to reveal how much pure scientific research has been able to achieve in the years through which we are now struggling; and let us never forget that excessive devotion to the merely practical may hinder rather than help the attainment of even the most " practical " discoveries. To quote some lines from an address on " Industrial re- search and the colleges " given last October by Dr. A. E. Ken- nelly before the American Institute of Electrical Engineers : While under extraordinary circumstances, such as those due to the present World-German war, the pure science departments may advan- tageously take up industrial research, yet, as a general rule, the best con- tribution of those departments to industry is by restricting their attention to pure science. Sir A. G. Bourne, F.R.S.. in his presidential address to the Indian Science Congress at Bangalore, in January, 1917, said: Who can say how many profound truths await discovery because some utilitarian who happened upon a glimmering of them did not think it worth while to pause and investigate the apparently irrelevant? . . . How much patient work and loving care have been bestowed upon inves- tigations seemingly impossible of application to any of the specific problems of the day? Upon research of this kind no utilitarian would have been at all likely to embark, yet, sooner or later, such research has either proved capable of direct application, or — and this has more often been the case — has unexpectedly formed a corner-stone, or occupied a more humble, but still useful position, in building up some far-reaching generalisation capable of being seized upon at once bv the worker in applied science, thus in turn perhaps stimulating further scientific research. Such remarks as the above, many times repeated in varying keys and modes, are slowly educating administrators and the public, and one is not without hope that at some not very distant date the value of true research in pure science may be far more 14 PRESIDENT S ADDRESS. generally realised that it now is. Meanwhile one may rejoice that even applied science has received an amount of recognition formerly denied to it, or at best grudgingly conceded. In this connection a most unfortunate fact is that almost everyone who has had a general education imagines himself in the possession of sufficient knowledge of scientic subjects to be able to decide what kind of research should be undertaken in each branch. Here such a science as astronomy has an advantage : the average educated man is so ignorant of astronomy that the astronomer is usually left to pursue his investigations unmolested, and it is only when persons who themselves carry on these pursuits prostitute science to personal ends that the astronomer finds him- self obstructed by lay intervention. An instance of this kind seems to have occurred when Sir David Gill had served the Admiralty for as long a period as 15 years. In a letter to Prof. Kapteyn. Sir David wrote : A deliberate attempt was made to hand over the Observatory to the Cape Government — which would have been equivalent ro its extinction — and the appointment of a successor to George Maclear (one of my assist- ants) was refused — in consequence of statements made to the Treasury that I had been neglecting my proper duties and been observing mmor planets and other pursuits on my own account. Fortunately Newcomb wrote me a letter, acknowledging in strong terms the value of the Cape work to the American Ephemeris, which gave the lie direct to my false accusers, and ended in my getting a warm official letter of thanks from the Admiralty for these very services.* Another instance of workers in science endeavouring to thwart research may be quoted from the same book (p. 175) : It would be laughable [says Prof. Forbes], if it were not almost tragic. to record the fact that Gill's work was opposed because, at a Royal Society Conversazione in 1886, his photographs, showing so few stars, were placed beside the long-exposure photographs of the Milky Way. showing thou- sands of stars. Gill wrote to Newcomb: "I told them that I had heard of babies crying for the moon, but I had never dreamt of anything so funny as a row of Fellows of the Royal Society insisting on having more g^ magnitude stars in the heavens, else they would stop supplies." Unfortunately astronomy is not the only branch of science in regard to which such episodes as the above have occurred, but there is surely nothing more reprehensible in the history of scientific investigation than opposition to the inception or con- tinuance of necessary work, engineered by those who should be aware of the value of that work, but who labour to oppose it in order to serve personal ends. Proceedings like these would be less likely to occur if there were a Department of Science as suggested by Sir William Crookes and Prof. Fraser Harris, for such a Department would be less liable to be misled by the un- scrupulous, and better able to gauge the capabilities of its workers and the value of their work. After four years of war we are looking forward to a time when accounts shall be ruled off, and a balance-sheet drawn up. Each country, each State, will be estimating its assets and Ha- * George Forbes, F.R.S., "David Gill: Man and Astronomer.'' pp. .V)0-I. president's address. 15 bilities, and unquestionably such a process will go on in this Union amongst the rest. We are continually hearing a great deal about our assets : last year at Stellenbosch the Rev. Noel Roberts reiterated the view that the native population is one of South Africa's greatest assets ;* we need not be told to regard the country's enormous mineral wealth as one of its chief assets ; and the economic potentialities of our almost boundless floral riches constitute another, while the many still untapped resources of agriculture form an asset that is almost without rival in variety and importance. If the end of the war is to find the country a going concern — to adopt commercial parlance — we should not risk the need of having to put up our shutters for stock-taking when peace comes : we should reckon out and invest our assets without delay, so that the proclamation of peace may find them at least on the high road to the production o^f substantial interest. We are, I know, working in that direction, but is there that whole-hearted co-operation that is so highly essential if a commu- nity means to succeed in a task that calls for grit and strenuous action ? As we wax hot in faction, In battle we wax cold. We have at times considered the subject of a national bo- tanical survey, but for some unexplained reason this matter, economically so important, hangs fire. South Africa had, a cen- tury ago, acquired a world-wide reputation as a field for botanical students, and. in addition to botanists from other continents, is now building up botanical schools of her own. The worth of a botanical survey is everywhere admitted, and even the type of person who shrugs his shoulders at observations of minor planets has no botanical counterpart. Yet the survey lags, and not alone South Africa, but the world, remains the poorer on that account. One hesitates to surmise reasons for the delay, but so much is certain, the vastness of the undertaking makes it imperative that the co-operation of every possible worker shall be enlisted, and the American principle, " Every man in the post that fits him best,'" would no doubt find loyal acceptance with all. The need of an agricultural survey o'f the country's soils I have discussed on several previous occasions, t Such a survey, if it is to be thoroughly carried out, should include a study not only of the inherent character and properties of the soils them- selves, but also of the soil in relation to its environment; that *Rept. S.A.A.A.S., Stellenbosch (1917), 88. t See inter alia — Senior Analyst's Report, Cape of Good Hope (1892), 6. "Need for organised research in Cape Colony": Addresses and Papers. Brit, and S.A. Assocs. for Adv. of Sc. (1905), 1, 221. '' Fertility of some Colonial soils as influenced by geological con- ditions "' : Trans. S.A. Phil. Sac. (1907), 18, 13. Presidential address, Sect. B, Rept. S.A. Assoc, for Ad7\ of Sc, Bloemfontein (1909), 33. "The study of the soil": Agricultural S. Africa (1910), I9- "Soil Surveys": Proc. Jsi Ann. Transvaal Dry Farming Congress (1910), 25, 30. 1 6 president's address. is to say, the soil must be studied both absolutely and relatively. Regarding the soil itself, we have to study its chemistry, its physics, and its biology, the last including the indigenous vege- tation on the surface as well as the micro-biology beneath the surface. In respect of the soil's external relations, we have to learn all that we can about the orography, the geology, and the meteorology of the tract of country surveyed. Hence the soil may be studied, as to its inherent qualities, in the soil laboratory (though only after having been properly sampled) ; but as to its external relationships co-operation with the surveyor, the geologist and the meteorologist is needed. The whole subject of soil chemistry in relation to crop pro- duction is comparatively little understood, not only in South Africa, but all the world over. How little we know of it we realise but too keenly when the world is faced with a wheat shortage. All things are in a state of flux,* said Heraclitus, the Greek sage, and he doubtless had a prevision of twentieth- century science. It is little more than half a century ago that the doctrine began to be preached that the crop-producing power of a soil can be determined by a mere chemical analysis. There- after arose a school that ridiculed such teaching, and upheld practical plot experiments. To-day we find men like Patten declaring that the manner of conducting fertiliser tests by measuring the crop produced has failed to materially increase our knowledge of soil conditions, and it is now quite generally recognised that it is unsafe to draw general con- clusions from results based upon such experiments. + All this shows the need of agricultural chemical research, for which South Africa affords a peculiarly well-adapted field. To come closer to particulars : the world has been threat- ened with a wheat famine, and, second only to the problem of munitions, there has come the wheat problem. On the day that I left Australia — two months after the declaration of war — the Commonwealth newspapers announced that the Government had authorised the immediate conversion of large extents of forest into wheat lands, and had set great bodies of men to work at felling the trees. Of late we, too, have begun to show some concern about our wheat crops, and the two problems that faced us were how to make existing lands yield larger crops, and how to extend the present wheat area. These problems have been rendered none the easier by the extreme scarcity of fertilisers, and with us, as, indeed, all over the world, the scarcity has brought to the fore another problem — how to turn potential into available supplies. These are all-important matters for research, even in war-time ; in fact, all the more important because it is war-time. Under war conditions, then, the cultivation of cereal lands must of necessity be, as far as possible, intensive, and so we need fertilisers containing not merely phosphates and nitrogen, * TIdvra pet- t Mich. Acad, of Science, T3th Report, (igii), 44. PRESIDENTS ADDRESS. \J but containing them in a state as readily available as possible for the cereals to absorb. How to get our raw materials into this readily available state is precisely the problem on which all our chemical energies should have been concentrated for some time past. Regarding the utilisation of our phosphate deposits there is much work to be done, both on the field and in the laboratory. The Saldanha Bay deposits were first investigated in the Cape laboratories about nine years ago,* but until the war quickened the pulse, very little was done in the direction of ascertaining the best way of converting these aluminium-iron phosphates into a form available to plants, and of their value in the unconverted form we know scarcely anything more from field experiments than we knew nine years ago. With regard to nitrogen, we scarcely realise that we live at the bottom of an atmospheric ocean of which the bulk consists of free nitrogen — free, not only in the chemical sense, but likewise so free that no war can cut us off from it as the present war has cut us off from the essen- tially German potash ; and not alone free, but abundant, for there is a weight of seven tons of this nitrogen above every square yard of the earth's surface. Now there are two nitrogen cycles in constant operation, and in each cycle the animal kingdom has a definite part to perform. There is a cycle of free nitrogen, and there is a cycle of com- bined nitrogen. The former is relatively simple, the latter more complex. We breathe in the free nitrogen of the atmosphere' and exhale it again, thus restoring it to the air unchanged, and as free as it was before. The. combined nitrogen taken by animals as a constituent of their food undergoes a change within the animal body, is returned to the soil as new nitrogenous com- pounds in the form of manure, and becomes converted by the soil bacteria into nitrates, which are capable of being absorbed by the vegetation. Animals feed on and assimilate this vegetable ifoodstufif. and so the cycle begins anew. The two nitrogen cycles — ^^the.breathinw cycle and the feeding cycle — move in per- fect independence of each other, and the problem of the chemist — a problem that has been largely solved within little more than the last dozen years — has been to bring free nitrogen within the sphere of operation of the cycle of combined nitrogen. I say this problem has been to a great extent solved. Chemistry has discovered two methods which are commercially practicable whereby the nitrogen of the air can be "' fixed," as it is called. One is the manufacture of cyanamide, which can then be used directlv as a fertiliser. For this manufacture two things are essential — almost pure nitrogen and electrical energy as a source of heat. The nitrogen is obtained by liquefying air. and allow- ing the liquid air to evaporate, when the nitrogen boils away first and is collected. This " fractional distillation " of the liquid air is generally carried out in a Linde or Claude apparatus. * C. F. Juritz : Report of Senior Anal.vst, Cape of Good Hope (1909), 159. 1 8 president's address. The electrical energ^^ is obtained from water-power. It is re- markable that in the United States, where there is much water- power available, there was not a single factory of the above type when America entered the war. South Africa has many rivers furnishing waterfalls of no mean size, but none of these has hitherto been utilised in this direction. The other commercial method for the fixation of nitrogen is also dei)sndent upon electrical action. Water is decom43osed into its constituent elements by electrolysis, and under great pressure at high temperature the hydrogen is made to combine, in the presence of a catalyst, with nitrogen produced by the frac- tional distillation of liquid air, and thus forms ammonia. To the practical operation of this process is largely due the fact that Germany has still the means of manufacturing explosives. The ammonia produced as above is converted into nitric acid, also by catalytic agency in the presence of atmospheric air, and nitric acid is the chemical basis of all explosives. Before the introduction of these methods the far greater power-consuming process of Birkeland and Eyde, first commer- cially practised in the neighbourhood of the Niagara Falls, and subsequently developed in Scandinavia, played a great part in bringing within Germany's reach the potentiality of producing enormous quantities of nitric acid, and it was to the perception of this potentiality by Germany that the present war was due, for then began to be Jaid the foundations of the scheme of munition production which in turn made it possible for Ger- many to embark on a definite war policy. That this was actually the position is now thoroughly well recognised amongst chemists all the world over. The President of the Ohio Academy of Science put the facts in a nutshell at the Columbus meeting- a year ago, when he said, in the course of an address on " The relation of war to chemistry," that, with British control of the seas, German armies with all their num- bers, thorough equipment, and solendid military power, would have been impotent in a few weeks or months without the chem- ical ability to get nitric acid from atmospheric nitrogen instead of from Chilean nitrate, for without nitric acid high explosives, and even smokeless powder, are impossible.* The class of investigation that finds most favour amongst Governments and populace in Britain and her dependencies to- day is that which is commonly known by the name of " Indus- trial Research." The reason of this is of course quite plain : both officials and public are capable of grasping the direct benefits of applied science and technologv. and hence technological inves- tigation is frequently favoured in quarters where pure scientific research is despised. Obviously we cannot make any real advance in scientific investigation or research unless we have adequate facilities, qualified workers, well-equipped laboratories. Naturally all this * Ohio Joiinil. of Science. (igiS). 18 [3], 70. PRESIDENTS ADDRESS. IQ means a financial backing, l)ut we shall never reap the bounteous fruits that science is able to afford until we cease to look upon money devoted to such objects as expenditure, and dubious ex- penditure at that, and begin to believe in it as direct investment. As long as we hold the former view, scanty returns \v\\\ be deservedly proportionate to our niggardly treatment of science. And the treatment has in the past been niggardly because — to quote the editorial in A'atitrc (March 29th. 1917) again — such matters have been too much in the control of the clerical estaMish- ments, who are ignorant of the significance of chemistry, and its vital importance to the interests of the country. Prof. Pope, alluding, in an address given by him in the Regent Street Polytechnic last October, to the establishment of the Department of Scientific and Industrial Research with an endowment of £1.000.000. asked why that experiment was not made 20 years ago. at a time when it would undoubtedly have prevented the horrors of the last three years. We have suffered [he said] in the past from the exclusively British method of making the specialist entirely subservient to the administrator, the administrator being generally chosen because he is available, because he is politically acceptable, and because he knows nothing whatever about the subject which is to be administered, and is therefore not likely to be prejudiced by any previous convictions. That process of appointing some- one who knows nothing to supervise the work of someone who does know how to do the job seems to have been at the bottom of a great many of our misfortunes in the past. There was a time — now, fortunately, long past — when I used to be asked to submit an annual requisition for the " drugs " which I would require in the course of my chemical work, and the request used to be accompanied by an instruction to call for tenders for the supply of these " drugs " from the various pharmacists in the city. It was with the utmost difificulty that I managed to persuade the authorities that the laboratory under my charge needed not drugs but chemicals, and that the disciples of Galen and .^sculapius were quite unable to supply those needs ; the chemist, whose concern during war-time is largely with explosives, gases, foodstuffs, follows a calling totally dis- tinct from that of the druggist, who concerns himself solely with pills, potions and plasters ; but this is a distinction wholly beyond the ken of those pilloried by the editor of Nature. Those day.s — when one used to be called a Trades Unionist for suggesting that when a Government Analyst was wanted it was scarcely appropriate to appoint a physician to the post — have happily passed away, even in South Africa, which gener- ally lags behind in such matters, and thanks to such books as Sir William Tilden's " Chemical Invention and Discovery in the Twentieth Century." the general reader is at last beginning to arrive at clear notions regarding the chemist and his work ; not a moment too soon, for, as a contributor to the Manchester Guardian remarked a few months ago.* * January. 9, 1918. 20 PRESIDENT S ADDRESS. it is high time that the public began to distinguish between the druggist or pharmacist, who sells toilet articles and medicine, and the chemist, whose prime business is chemistry and its application to production. The popular confusion that formerly existed in the British mind between the chemist and the apothecary is largely respon- sible for the false perspective of chemical matters that the whole iBritish nation has had. In Germany such a Hogarth's picture of the chemist and his functions never prevailed. It is unfortunately true that, however inadequate the value placed upon chemical attainments and qualifications in England, the position is distinctly worse in South Africa. Two years ago the South African Association of Analytical Chemists appointed a Sub-Committee to report upon the duties and responsibilities of Government Analysts. The resulting report — a very exhaus- tive one — was subsequently printed in that Association's Pro- ceedings,''' and it proclaims with emphasis that with the emolu- ments obtained by analysts in the Imperial Government Labora- tory the conditions of the South African service compare most unfavourably, a condition of afifairs which it attributes to " the lack of scientific training extant among ministers and responsible officials." The Government Laboratories [the report continues] could be more fully utilised in investigating the industrial resources of the country. The crying need of this countr}' is research, and the Government should provide the necessary staff and laboratories for investigational work ; at present, the time of the officials is largely taken up by work of a routine character. In another part of the report occurs this paragraph : This failure to realise the importance and necessity of the cliemist is found among the general public as well as among Government officials, and it will be necessary, in order to effect an improvement and secure proper recognition of the value of the chemist, to continually emphasise his importance to the welfare of the State. Many, no doubt, do not comprehend what functions the re- search chemist can exercise in South Africa, and what scope the country can offer for his labours. Following the United States' principle of the best men in the best posts, where, they ask, can we place him so that the country may, through his instrumen- tality, reap the greatest advantage? To answer such questions one needs, first of all, to consider how scientific research — and therefore inferentially chemical research — may be distributed. As a matter of convenience, a threefold grouping is adopted — imiversity research, industrial research, and national research. Adapting the definitions given by Mr. C. E. Skinner a few month> ago at a meeting of the American Institute of Electrical Engineers, we may say that university research includes the pure scientific research, which naturally finds its home in the univer- sity and all other research done there for the purpose of training- men. Industrial research comprises all that done by or for industrial concerns with the purpose of advancing industry. * Proc. S.A. Assoc. Anal. Chemists (1916-17), 32-51. PRESIDENT S ADDRESS. 21 National research is that carried on by the Government for the purpose of benefitting the people as a whole. Now it is plain that between these three types of research there can be no sharp lines of demarcation, but university research is often the step- ping-stone to industrial advancement, while national research is repeatedly industrial in its objects. Mr. Skinner rightly holds that the primary function of the university in research should be the training of research men, and that universities should be equipped to turn out research men just as they are now equipped to turn out men with academic and engineering degrees. Prof. G. G. Henderson, in the address from which I have already quoted, laid down that the training of the chemist, so far as that training can be given in a teaching institution, must be regarded as incomplete unless it includes some research work.* The demand for research in almost every field is growing with a rapidity wholly unprecedented, and to the universities alone can we look for men able and ready to take their places in the strenuous efifort that is bound to be put forth on all hands. We have just inaugurated a triple university system: Prof. Craw- ford, in his presidential address to this Association at Maritz- burg, asked and sought to answer what South Africa expects from its universities, and referred, in particular, to the need of encouraging the study of science and of furthering research. In developing this theme he asked us to remember that the highest form of research is not made to order, and that there is more in genius than industry and opportunity. It would benefit us to bear this in mind, and in juxtaposition with Prof. Crawford's words, to place a sentence from Mr. Skinner's address : If it takes a genius to recognise a genius yet undeveloped, and properly to stimulate and direct that geniusj liow necessary it is that we place men of genius at the head of the research departments of our universities. It comes to this, then : that we should see to it that our universities are well equipped with scientific research workers, and it is pre-eminently desirable that a system of research pro- fessorships should be instituted, the chairs to be occupied by men of enthusiasm — men who will inspire a like zeal and devotion amongst those of the younger generation whom they gather around them, men of personality and character, who will kindle in the breasts of the research students feelings of admiration and respect for them and their work. " In training research men," says Mr. Skinner again, " the university will naturally become the custodian and the promoter of pure scientific research." Here is the fountain-head whence , we shall ultimately draw our men for industrial research, and for national research ; how important, then, that the source of all our supplies be of crystal purity! Whatever more utilitarian * Kept. Brit. Assoc, for Adv. of Science. Xe\vcastlc-on-'l"ync (i<)i6), 374- 22 PRESIDENT S ADDRESS. form of research one may subsequently take up, research in pure science is invaluable in the earlier part of the research student's career, for it will give him a zest and a stimulus that will remain with him throughout, enrich his scientific imagina- tion, and adorn all his subsequent work. At the same time uniyersity research may lead to the most utilitarian results : some of the most important dyes, artificial alizarin, the phthaleins. indigo, and such drugs as phenacetin, antipyrin, and aspirin, were all discovered in university chemical laboratories. Now. why have we so few persons doing research work in South Africa? Is it in part because no research geniuses are born, or is it that we failed to recognise them, and neglected to pro- vide them with the essential facihties? — youths, maybe, on whose humble birth fair science frowned not, flowers " born to blush unseen and waste their sweetness on the desert air," mute in- glorious Miltons, whose genius remained latent because we took no trouble to draw it out? Science to their eyes her ample page. Rich with the spoils of time, did ne'er unroll. Dr. P. G. Nutting about a year ago said that some writers have spoken of the investigator as a rare individual, to be sifted out from educational institutions with great care for a particular line of work. My personal opinion is that a large percentage of the men students are fitted for research work if properly started along the right line. What we in South Africa lack — next to the facilities for research — is not so much the research students as the men to start them on right lines. I think that Principal Beattie, at the inauguration of the University of Capetown three months ago, sounded the correct note in observing that the youth of South Africa did not lack enthusiasm or ability for research, but they lacked opportunity, and, he added, much depended on the men they had as professors. That is the secret of it all. In this dread war South Africans have more than once exhibited a phy- sical courage and a pertinacity equal to anything that Australia or New Zealand could show ; why should not South Africa, then, produce a Bragg or a Rutherford as well as Australia and New Zealand, seeing that intellectul courage and pertinacity are two indispensable qualities in a successful research worker? The position is analogous to that which war has developed in Europe and America : there the opportunity has made the man. An American chemist already quoted said that the German General Staff has learned, if others have not, that German chemical achievement, which is great indeed, is no sign that equal ability does not exist elsewhere. The Allies and America improvised a muni- tions industry in two years to match their machine of forty years' pre- paration. And then he went on to make a remark which we may well take to heart : PRESIDENT S ADDRESS. 23 War could force us to do nothing we did not possess capacity for before. " The potential research worker," says the editor of the United States Experiment Station Record, " is probably less born than made," and Dr. Nutting thus clothes the same thought in different language : Fertility of mind is not so m,uch an inborn quality of the mind itself as of the training and association which that mind has had.* Hence it is our solemn duty as a young nation to provide abundant facilities at each of our three universities for the making of our future research workers. We pass on to speak of industrial research, which always has some utilitarian end in view, whereas the purpose of pure scientific research is more exclusively philosophic — the discovery of truth. The investigator in pure science has been likened to the explorer who discovers new continents, or islands, or lands before unknown; the investigator in industrial research to the pioneer who surveys the newly-discovered land in order to locate its mineral resources, to determine its forest areas, and ascer- tain the position of its arable land.f I quote these remarks with all circumspection, for after all there are no sharp boundaries between research in pure science and in applied or industrial science, and Huxley was right when he wrote that " what people call ' applied science ' is nothing but the application of pure science to particular problems." The fact is that applied science is impossible until a foundation of pure science has been laid to build it on. You cannot apply a science which is not there to apply, and, as Sir William Tinney has said, until men began to interrogate nature for the sake of learning her ways, and without concentrating their attention on the expectation of useful applications of such knowledge, little or no progress was made. Industrial chemistry has been defined as that branch of chemical science which uses all the rest of chemistry, and much' engineering, for the furtherance of production of chemical sub- stances, or the use of chemical means or methods for manufac- turing any material of commerce ; and hence industrial research for the most part differs widely from university research. True„ there are instances to the contrary : thus Michigan University has at Ann Arbor a tank for testing ship resistance,' and Illinois University has a laboratory for investigations on a full-size loco- motive engine, but industrial research is for the most part im- practicable for universities, and as often as not needs to be carried out under large-scale conditions, as it were in situ, and by persons already possessing practical experience in the various phases of the problem under investigation. At the same time * Nature (1917), 100, 157. t Col. J. J. Carty: Presidential address: Proc. Amer. Inst. Elec. Engi- neers (1916), 35, [10], 1415. 24 PRESIDENT S ADDRESS. there should be much closer co-operation between the university and industrial research. Industry should recognise that it must depend primarily upon the universities for its trained research men, and co-operate to the fullest possible extent to the end that properly trained men be turned out. Do you realise what this last sentence involves — you who are connected with the big industries? It involves that industry should recognise that, from a purely selfish motive if from no other, its interest lies in endowing research chairs at the univer- sities, and in seeing that they are occupied by men of genius. The very nature of industrial research implies that there must be a constant accession to the ranks of its workers of persons trained in pure scientific research. If such accession be inter- m.itted. or if the increase of knowledge by means o'f pure scienti- fic research be hampered, industrial research will inevitably be limited in corresponding degree. The Government has acted wisely and well in endeavouring to establish a system of industries in this country : do we want these industries to fizzle out, or to go through years of laborious struggling? If we wish to minimise preventable disadvantages of that kind, let us do without delay whatever we can to foster research, so that the men to conduct it become available as soon as they are needed. National research approaches more nearly to the industrial than to the university type. It is often undertaken for the advantage of industry in general, but its outlook is considerably broader than that above embraced within the scope of industrial research, restricted, as the latter is, to the requirements of indi- vidual industries. In South Africa the cry for industrial re- search has become more imperative of late, and the Industries Advisory Board, as well as the Scientific and Technical Com- mittee appointed on the initiative of the Minister of Mines and Industries, have gone some distance, both in educating the public to the need of this type of research and in giving an impetus in the required direction. Mainly, however, the agencies used were of two classes : the laboratories of the University Colleges and those of certain Government Departments, together with the respective officers of those institutions. There are two fundamental principles on which I must now lay stress : they are expressed in the words " co-operation " and " co-ordination " — co-operation between workers in different branches of science, co-ordination amongst those who work in the same branch, in order that the maximum of benefit may be attained. So interdependent, in fact, so interlaced, are the three types of research to which I have briefly alluded, that it should be patent as the sun at noon that the closest co-operation between them all is essential. It is to be feared that this is not yet as clearly realised as it should be. The waste of time and energy that has arisen from overlappping, which in turn has resulted from lack of collaboration, is incredibly great. It has stifled work of value in the past to an extent that is certainly not president's address. 2^ realised ; it has thrown back for many years branches of investi- gation in which ere now incalculable progress might have been made, and untold pecuniary advantages reaped. Would that the dire necessity of this searching^ war could stir up the South African nation to a correct appreciation of the facts! About a year ago the President of the Society of Chemical Industry, in his address at Birmingham, insisted on the absolute necessity for the engineer and the chemist to " get into double harness as quickly as possible," and work sympathetically to- gether for the progress of chemical industry. In South Africa, too, this necessity has been manifested, but I am glad to say that we have had more than manifestation: we have had realisation, and we have had operation. For example, when, some months ago, the fertiliser scarcity arose. I was deputed to investigate the potentialities of unutilised raw materials in the Union, and found, amongst other things, that there were several thousand tons of good material going to waste in various places in connec- tion with such institutions as slaughter-houses and crayfish can- neries for lack of by-products plant to deal with it. When I had completed my tour of inspection and furnished my report, the engineers were charged to follow on, and set to work to make good the deficiency in plant, with the result that a respect- able quantity of fertilisers will now be produced from the refuse that hitherto has been going to waste. May I just here repeat^because they are still applicable to- day— a few remarks which I made in my presidential address to the Cape Chemical Society six years ago: As an industrial science, chemistry never operates in isolation. When we concern onrselves with the chemistry of the country's vegetable products, it is the science of botany that has to afford additional aid; if it is general agriculture that we arc dealing with, the chemist may also have to work in co-operation with the zoologist, entomologist, or mycolo- gist. Often, in connection with the investigation of the country's mineral products, and of its agricultural soils, consultation with the geologist is required. In any case, there is tliis one outstanding fact : that these various scientific offices need to be in closest touch with each other in order to promote the smoothest working of the entire machine of investi- gation as an organised whole. This close contact between science and science is of great importance, but it is still more important that contact between the various workers in one and tJ:c same science should be as intimate as proper co-ordination and organisation can make it. During its annual convention towards the close of iQiOj the American Society of Agronomy was very largely occupied with the standardising of methods for conducting experiments. It was then shown, again and apain, that a large amount of experimental work, done in the United States, has led to results which could not be compared with each other, were difficult to interpret in a reliable way, and were liable to lead to wrong conclusions, because there had been no agreement as to method amongst the various institutions involved in the work. We do not wish to have these mistakes repeated in South Africa; our desire is rather to profit by the experience of other lands ; but unless we look well to our steps we stand to repeat some of those very mistakes in an aggravated form. Therefore, lest we should go on a wrong track with regard to this matter of investigation and research, two principles should remain deeply graven on 'nir minds : these are co-ordination of effort and unity of plan. 26 president's address. Some of us have read what H. G. Wells describes as ideal in his " Modern Utopia " : In Utopia a great multitude of selected men, chosen volunteers, will be collaborating on this new step in man's struggle with the elements. . . . . Ever}- university in the world will be urgently working for priority in this aspect of the problem or that. Reports of experiments, as full and as prompt as the telegraphic reports of cricket in our more sportive atmosphere, will go about the world. Clearly co-operation and co-ordination cannot become effec- tive without efficient organisation. We were afforded a splendid illustration of what may thus be eft'ected in the case of a private corporation on the occasion of the Stellenbosch meeting, a year ago, when we visited the dynamite factory at Somerset West. and listened to the historical account given by the general manager. Established at the beginning of the present century for the purpose of supplying dynamite to the Kimberley Mines, the sphere of operations had so extended that during the twelve months immediately preceding our visit the works had exported to the Commonwealth of Australia over £100,000 worth of explo- sives manufactured in South Africa, in addition to supplying our own needs. From that manufacture other industries developed, one by one, and the works now include plant for the manufacture of sulphuric, hydrochloric, and nitric acids, and of copper sulphate and the nitrates of barium and lead, while others are under consideration. Farmers have been supplied with the sulphur which they need for sheep-dipping and vine-spraying, while 20.000 gallons monthly of a lime-sulphur solution for sheep- dipping have been turned out. The works bid fair to develop into a general chemical factory after the war. Thus far the private concern; what we need in the 'way of a Government establishment is an institute for research in pure and applied chemistry — such a National Chemical Laboratory as Prof. Hen- derson has been longing to see established in England, but Eng- land is not yet sufficiently responsive. " We don't conduct research." says H. G. Wells. " we simply let it happen." Ah. that is where England dift"ers from South Africa — we don't let it happen : sometimes we make ourselves believe that we do, and then we let other things happen to interfere with it. Why, I have been pleading these twenty- four years in this agricultural country for a properly organised system of chemical, physical, biological research with respect to our agricultural soils, and it has not come yet. The way in which a nation can organise itself and its re- sources for war has impressed a world. Other nations are talking about organising themselves for the commercial struggle that will ensue upon the present strife, but mere talking about reconstruction will not enable us to face the future serenely. " We all talk about the weather," said Mark Twain, " but nothing is done!" Why is it that England, France, Australia. New Zealand, Canada, are mobilising their scientific men for research? Dr. G. E. Hale. Chairman of the Department of PRESIDENT S ADDRESS. 2/ Science and Research of the United States Council of National Defence, says that it is because, looking ahead, it was seen that the conchision of peace would be followed by a trade war witli German}', in which no industry not perfected by scientific research could hope to succeed. Can this country compete industrially with a country that has shown me what organisation can achieve if we starve the very soul of industrial prosperity — pure and applied scientific research carried out in the laboratory ? Mr. W. C. Dampier Whetham, F.R.S., in his recently pub- lished book on " The War and the Nation," devoted a section to '■' The organisation of iBxitish industry and commerce," in regard to which a reviewer says that three years of war have done more than a century of peace to impress upon the public mind the indispensability of scientific research to national prosperity. The result has been that the Imperial Government has called into being a Department for the express purpose of organising and directing research, and has placed considerable sums of money at this Department's disposal. But perhaps the most important outcome is that « the leaders of British industries have licgun to acquire the hal^it of working together in order to conduct associated researches.* Now let me emphasise the point that there is not one of these industries for which the chemist is not essential at one stage or another. An interesting address given some months ago by the President of the American Cyanamide Companyt shows how universal the need of the chemist is. Two thousand grades of glassware are required for a vast variety of purposes ; for this the skilled glass-maker must work under chemical con- trol. The iron and steel of oin* cutlery, the extraction of silver, gold, and, in fact, of all metals from the ores, need the chemist at every step ; the clothing we wear, the dyes that colour it, and more particularly synthetic dyes, 'the host of other uses to which cotton is put, the use of cellulose in the form of artificial silk as a new textile material, all are interwoven with the resources of the chemist. The preparation and preservation of our foods, and the securing of their purity, both depend on chemical con- trol. The manufacture of synthetic drugs, such as antipyrin, phenacetin, sulphonal. veronal, novacain, aspirin, and salvar- san ; the introduction of synthetic perfumes like heliotropin, of synthetic flavours like vanillin, of synthetic rubber and synthetic camphor ; the quality of the fuel we use, the efficiency of the fertilisers we put into the soil, the extraction and utilisation of the various animal and vegetable oils, and the conversion of some of them into solid fats by catalytic agency, and so into soaps or candles, with glycerine- as a by-product ; the production of liquid * Journ. Roy. Soc. of Arts (iyi7), 65, 755. fChem. Nezi's (1917), 116, 157-159. 28 president's address. fuels — every one of these would be impossible without chemical aid. There are a few facts regarding the chemist which I want every South African, and particularly those in high positions, to realise. First of all, get rid of the idea that he is a druggist or pharmacist, any more than he is a baker of plumber, or belongs to any other avocation in which chemistry takes a share. And then, grasp the fact that there is scarcely an avocation on the face of this earth intO' which chemi.stry does not enter, or wherein the chemist would not be of some use. One does not need to tell Johannesburg that it has to thank the chemist for its pros- perity, for without him many of the mines would long have ceased to work. The other great industry of South Africa, agriculture, is at the mercy of the chemist in respect of the manu- facture of fertilisers, and many agricultural products owe to him the processes employed in their preparati(m ; chemical operations are fundamental to every branch of the dairy industry, the making of jam, the drying of fruit; the tinned vessels in which many of these articles are preserved are all subservient to the chemist. Without him the economical production of metals of any kind could not take place, there would be no locomotive engines, no assurance that the water which these engines need w\\\ not corrode their boiler tubes, no testing of the coal which converts that water into steam, no orovision of steel rails to run the locomotives on, or. to go further, no steel armour for our battleships and no alloys for shrapnel, aeroplanes, or submarines. It is also the chemist's work to control the driving power of ships of war and merchandise alike, whether that driving power be coal, oil, or electricity, for the materials employed by the elec- trician must all in the first place be scrutinised by the chemist. All explosives are essentially chemical in their make-up, and, in fact, the whole army, as well as the navy, is dependent on the chemist all along the line, inasmuch as he has to vouch for the purity of all their supplies of food and drink, even well- water ; and not only their natural purity, but also their freedom from fraudulent adulteration or deliberate poison- ing. The various gases so much used in the present war are all the productions of the chemist, and so are the means adopted to secure immunity from those gases. It is the chemist who controls the army's drugs, disinfectants and anaesthetics. The colouring of the material used for clothing not only the military and naval services, but the whole civil population as well, is subject to the careful scrutiny of the chemist. His functions also include the manufacture of the leather which provides an army with boots : without him that leather cannot be tanned, as the entire wattle and other tanning industries are conducted under his advice. The finished leather, too, is investigated by him, lest fraudulent practices should have participated in its manufacture Without the chemist there could be no books, for chemical processes are fundamental to the PRESIDENTS ADDRESS. 2g making of paper, of printing and writing ink. not to mention again the materials wherewith bool^s are bound and the colouring of the binding. The production of illustrations in those books, by whatever means, and also the whole art of photography, must Stand or fall with the ability of chemistry to assist them. And then, as I have already said, there is the increasingly large sub- ject of fine and synthetic chemicals, beginning with manufactures like those of starch, glucose, and dextrine, the synthetic dyes which surpass natural products in brilliance and permanence, the synthetic perfumes which far transcend natural odours in potency, the synthetic drugs which have done much to afford relief to the suffering ; artificial products — I do not say imita- tions, for they are often better suited to their applications than the natural products which they replace — artificial products in substitution of rubies, of bone, horn, and ivory, of resins, and of leather, are all the result of chemical research. Again and again the chemist has shown us how to produce the most valu- able commodities out of waste and refuse. The refuse of the Bessemer steel works gave rise to one of our most efficient fer- tilisers ; the refuse of the gas works provided the world with dyes, drugs, and a marvellously long list of other useful articles ; the waste of wool-washeries furnishes us with lanoline. Waste wood, if destructively distilled, and. amongst others, waste wattle wood, of which large quantities are annually available in Natal, is capable of producing acetone, whereof enormous quantities are now being used for the manufacture of propellants. And so we may rightly claim that the present age is the age of the chemist. The chemist has never before had such oppor- tunities for the application of his knowledge to the betterment of material conditions upon earth, and never has he more effec- tively applied it to the attainment of this aim. It is also sadly true that never before has he applied his knowledge with such damaging eft'ect as during the present w^ar ; but when the war shall have run its course, all the chemist's resourcefulness, all his energy, all his persistence will be needed to repair the damage done, and to start exhausted nations upon new lines of industry. On the chemist, more than on anyone else, will this task devolve, and in South Africa in particular he will find abundant work awaiting him. Is he to be there to respond to the call? Then it is for us to educate and train him to the necessary standard ; it is for us to provide the means whereby his purpose may be accom- plished ; it is 'for us to accord him sympathetic treatment. Do not let us regard him as useful only as long as he is bound down to routine work, and as academic when he is occupied with in- vestigations beyond our limited capacity to understand. We have heard much during the past four years of the diffi- culties under which the chemist has been labouring in Britain and America — of the apathetic attitude adopted towards him by Governments, public institutions, and industrial concerns, of the sparing hand wherewith the essentials for the pursuit of his 30 PRESIDENT S ADDRESS. investigations have been doled out to him. I have deemed it very desirable to place before you this evening some of the opinions which have been expressed on these topics north of the equator, because I am convinced that many of our administra- tors, politicians, educationists, and commercial men are wholly unaware of the strong remonstrances which have grown to quite a literature during these four years, and are probably under the illusion that in South Africa the chemist has now the oppor- tunity, if he cares to make use of it, to help the Union, with eclat to himself, safely through some of the difificulties resulting ifrom the war. I have, in fact, heard such a view seriously ex- pressed. The idea is, of course, perfectly absurd. At the same time it falls to the chemist in particular to do all that in him lies to aid production during this time of crisis, and to assist those directly engaged in the work of production, whether it be the manufactures or agriculttire. And those who have it in their power to strengthen the chemist's hands in such a work will themselves not only be aiding the State, but will be assisting to bear up the lofty principles for the maintenance of which amongst men Britain and her Allies are contending. Thoughts somewhat akin to these were well developed by the American chemist, James R. Withrow, President of the Ohio Academy of Science, whom I have more than once quoted in the course of these remarks, and now I close by commending to your attention the concluding paragraph of his able and thought- ful address : It has become so evident in this war that the intelligent and scientific criminal is a terrible menace, and dislodging him at times such a weary and fatal task, that we must find some way of preventing our leaders and groups or classes, whether governmental or industrial, from becoming this kind of danger. Have we not reached the time when we are willing to turn to the One Who ordained civil government for our good, acknow- ledge that He ordained it and not we ourselves, and make our leaders or rulers " whom God and this people shall choose " — " men fearing God and hating covetousness "? Section A.— ASTRONOMY, MATHEMATICS, PHYSICS, METEOROLOGY, GEODESY, SURVEYING, EN- GINEERING, ARCHITECTURE, AND IRRIGATION. President of the Section : — Professor J. T. Morrison, M. A., B.Sc, F.R.S.E. MONDAY. JULY 8. The President delivered the following address : — ON THE INTERNAL STRUCTURE OF THE EARTH. Some fourteen years ago, Parsons, of steam-turbine fame, when President of the Engineering Section of the British Asso- ciation, devoted a considerable part of his presidential address to the question of the feasibility of the sinking of a mine-shaft to the enormous depth of 12 miles. He went in some detail into the methods of construction and probable cost of such a shaft, basing his proposals largely on the experience gained in deep mining on the Rand. His suggestions gave rise to a considerable amount of discussion, which was directed more particularly to the question whether the rocks surrounding such a shaft would not flow like plastic solids at the pressures and temperatures which must occur at so great a depth ; but at that time there v/ere few accurate experimental data on which to base a well- considered judgment on this question. Since the date of Parsons' address, a great deal of research has been directed towards the elucidation of the conditions that obtain at various depths in the earth's interior, and as much of this research is geophysical rather than geological in character, it has occurred to me that the subject of the internal structure of the earth in its broad aspects would be a suitable one for the presidential address to Section A of this Association, more espec- ially at a town such as Johannesburg, whose material welfare is so largely dependent on mining operations. The problem of the structure of the earth is one that pos- sesses many elements of fascination and attractiveness. It has important bearings on almost all the sciences. For the astrono- mer, the earth sei'ves as the short and incessantly moving base from which all astronomical positions and distances must be measured, as well as the planet whose life-history is most likely to throw light on the course of cosmical development. To the physicist and physical chemist it has the interest that it must contain materials under conditions of temperature and pressure, such that their faint imitation calls for the highest resources of experimental skill, and that their effect on the physical behaviour of the materials will always present a wide field for the specula- tive tendencies of molecular philosophers. For the geologist, the knowledge of the internal structure of the earth is the only 32 PRESIDENTIAL ADDRESS — SECTION A. key to the mystery of those incessant rises and falls, those thrusts and bucklings and occasional tearingfs of the apparently rigid crust, of which the surface rocks are so plain a record. For the evolutionist student of the biological sciences and of the history of man, the question is wrapped up with such important matters as the area and extent and connections of old land surfaces, their possible climates as affected by changes in alti- tude and other terrestrial and astronomical conditions, the per- manence and physical state of the oceans, and the like. Finally, the subject has presented tO' the mathematician problems at once of the greatest interest and of the greatest difficulty, problems that test in the 'highest degree his resources of imagination and his clarity of thinking. I shall discuss the question chiefly from the side of geo- physics, partly because it is on this side that my own ignorance of the subject is perhaps less complete than on others, and partly because the methods of geophysics, because of their quantitative character and comparative simplicity, are those which have of late years been the most fruitful in trustworthy results. I say this with no want of respect for the large body of exact know- ledge accumulated by the researches of geologists. But it appears to me that to a considerable extent the work of the geophysicist begins where that of the geologist ends, and that it lies with the former__to discover, as far as may be, the exact processes by which those incessant movements have been maintained to which the geological record is so indubitable though perplexing a witness. The methods that have been of greatest service in geo- physical research are the following: — (i) Exact geodetic surveys, accompanied by astronomical observations of latitude, longitude, and meridian. Such surveys have not only given the size and shape of the earth so far as these can be determined from land observations, but have also in recent years thrown a considerable amount of light on the probable density and strength of the earth's crust and the layers lying immediately thereunder. (2) Determinations of the total mass of the earth and of the densities of the chief rocks. (3) Exact determinations of the intensity of gravity at points kno'wn in geodetic height and position. (4) Determinations of temperature, heat conduction and radium content in surface rocks. (5) Laboratory determinations of the elastic constants of rocks, and of their greatest stress-bearing power at the ordinary and higher temperatures. (6) Investigations into the small deformations of the earth that occur under the tidal forces of the moon and sun. (7) And perhaps the most fruitful of all, investigation by seismometers of the rates of propagation of earth- PRESIDENTIAL ADDRESS SECTION A. 33 quake waves in various directions round and through the earth. I should like to add that in my opinion the recent pro- foundly important discoveries of the arrangement of the mole- cules in crystals is likely to lead at an early date to our being able to calculate the elastic constants and strength of solids even at the enormous pressures and high temperatures that must exist in the interior of the earth. If such be the case, the whole of our knowledge of the interior of the earth will attain an exactitude quite unexpected only a few years ago. This summary of methods will show how impossible it is for anyone to attempt anything but the shortest outline of some of the more certain results that have been yielded by them, or to make more than passing reference to the need there is in many cases simply to suspend judgment. The size and shape of the earth have been measured with something like accuracy, only by geodetic surveys made on con- tinental areas. Such measurements vary slightly, but the general result is that the land surfaces, when reduced to a mean level, are very approximately those of a flattened ball or spheroid such as would be produced by spinning an ellipse round its shorter axis, the equatorial radius or semi-axis being 6,378.2 km. very nearly, or 3,963.3 miles, and the solar radius being 1/298 part shorter. It is worth pointing out that the radius of curva- ture of the oceans has not been directly determined. It is known from dynamical theory that if the earth consisted of a series of concentric shells, each of uniform density, the free surface would be a flattened spheroid such as has been described. But a direct determination of the curvature of the ocean by a goedetic chain of triangles extending over some of the Pacific Islands would, if feasible, yield information of great interest. The method of such geodetic surveys is, of course, a well- known one, but as it has an intimate bearing on some questions dealing with the strength and movements of the earth's crust that will come up for our consideration later on, I may be par- doned if I refer to it briefly. A level base line several miles long is carefully measured, and from its ends the angular posi- tions of two marks set up on neighbouring hilltops are accurately determined by a theodolite. The base line is thus the base of two triangles that have the hilltop marks as vertices. The line joining these serves as a new base from which one or two other points are determined. So the process of triangulation goes on, the triangles spreading over the country, and the individual sides being ultimately usually about 30 miles long. The vertices of the triangles are almost invariably beacons set up on promi- nent mountain peaks. I need hardly say that the highly accur- ate and extensive geodetic sun'ey of South Africa which we owe to the energy and skill of the late Sir David Gill and of Colonel Sir Richard Morris is one of the finest examples ever effected. To find the shape of the earth we must also by star observations 34 PRESIDENTIAL ADDRESS SEt TION A. determine very accurately at as many vertices as possible pre- cisely how a plumbline would hang with reference to the sides of the triangles that meet at the vertex. One may imagine the whole network as a system of triangles whose sides are made of long, straight wires with plumblines hanging from as many of the vertices as possible. Now the problem of the geodesist is to find what shape of flattened spheroid will pass as nearly as pos- sible at right angles to these various plumblines, and will start from the mean sea-level at some chosen point of the coast. This shape gives the figure of the earth as calculated from that par- ticular survey. When the average figure lias been calculated that will most nearly cut the plumblines perpendicularly, it is invariably found that practically all the plumblines show minute deviations from perpendicularity. These deviations, usually called residual deflec- tions, are. of course, related to local irregularities of surface or of density. They throw a clear light on the density of the crust underlying the surface to depths far beyond those we can reach by boring, and we shall return to their consideration towards the close of this address. It is well to remember how enormous the dimensions of the earth are, when compared with the thickness of the surface rocks with which we are directly acquainted. On a model of the earth of a diameter of six feet, the ten miles' vertical interval which separates the highest mountain-top from the greatest ocean depths would be represented by a thickness of only i/ii of an inch, and the elevation of a sea-coast through a mile, with its consequent profound change of climate and its exposure of the surface to agencies of new character and intensity would be represented by a movement of the model surface through merely the thickness of thick paper. These comparisons will help us to realize how gentle a tilting of the earth's crust would cause surface changes of the greatest biological and geological importance. The density of the earth, as determined by recent accurate comparisons of its gravitational attraction with the gravitationr^l attraction exerted by a small body of known shape and mass, is very nearly five and a half times as great as that of water. The mean density of the chief rocks of the crust being only about two and three-quarter times that of water, it is obvious that the parts towards the centre must have a density so far exceeding the average as to make up for the deficient density of the crust. It may therefore be regarded as very probable that the central parts contain predominant quantities of iron and other heavy metals, though it is to be noted that the pressures that obtain in the interior are so enormous that they must compress all ma- terials considerably and cause their densities to rise proportion- ately. As we do not know how the different layers increase in density, we cannot calculate these pressures exactly, but it is easy to give rough approximations. At a depth of 40 miles, i.e., only one hundredth part of the earth's radius, the pressure must be about 250,000 lbs., or (say) no tons to the square PKESIIM", N'TIAL ADDRESS SliCTlON A. 33 inch, while at 2,000 miles, or half-way to the centre, a probable estimate is 8.000 tons to the square inch. It will help to gave some idea of the effects of such pressures if we recollect that a block of good granite, if unsupported laterally, will generally begin to crush under a pressure of about 11 tons to the square inch, so that a column of granite four miles high will, if devoid of lateral support, begin to crumple at the base under its own weight. We shall see. however, later that strength to resist crushing is immensely increased if the column be given lateral support. To complete a first rough picture of the earth's structure, we must turn now to the question of the temperature of the interior and of its physical state. As all w^ho have to do with mining are well aware, after a borehole passes through the first few feet, the temperature always gets higher the deeper we go. The rises observed in dif- ferent boreholes and tunnels have varied considerably, but we shall not be far wrong in taking a rise of about one Centrigrade degree for every 100 feet, or, say. 50 degrees per mile as an average. If this rate were maintained for even a few miles in the crust, we see that at a depth of only 40 miles the temperature would be about 2,000° C, a temperature well above the melting- point of all known rocks, when these rocks are subjected to ordinary pressures. The deduction made by most geologists and many physicists till well on in the nineteenth century was that a part of the interior of the earth must be liquid, and the innermost part even a highly compressed gas. There are, however, many facts which militate very strongly against the soundness of such conclusions. In the first place, it is, as we shall see, very doubtful whether the surface gradient is maintained. Again, direct experiments on substances in the laboratory show that increase of pressure raises the melting-points of almost all substances, including rocks, and also increases enormously their stiffness or rigidity when below the melting-point. Finally, the evidence of observations on earth- tides practically precludes the possibility of the existence of a continuous shell of liquid or gas anywhere, and this is confirmed strongly by the evidence of the propagation of earthquake waves as observed by the seismometers now installed at numerous places. On the other hand, these is strong evidence of the existence of a layer beginning at some depth between 20 and 100 miles beneath the surface, and probably extending considerably down- wards, wdiich is relatively less rigid than the rest, and which intermittently, perhaps, or like a plastic solid, adjusts itself to the constantly varying burden which the surface agencies lay upon it when they corrode and denude the continental areas, and deposit the products along the oceanic borders. We shall shortly consider these points in turn. 36 PRESIDENTIAL ADDRESS SECTION A. Lord Kelvin showed many years ago. that if we can regard the earth as cooHng in the manner of a small ball of uniform conductivity and uniform initial temperature, and if we know that initial temperature and the surface gradient, we can specify the temperature at any depth, and can also tell the duration of cooling. The diagram ( Fig. i ) illustrates Kelvin's result, and one striking point about it is the slight extent to^ which the tempera- ture of the innermost parts elf the earth would be affected by con- duction even after the lapse of many millions of years. Thus if the earth had been initially at 4,000° C. throughout, and its surface had at once been reduced to our ordinary temperature, its fall of temperature after 1,000,000 years, at a depth of 7.6 miles, would have been about 630 Centigrade degrees, at 15.2 miles only 17 degrees, and at 22.8 miles barely one-tenth of a degree; while after the lapse of 100.000,000 years these falls of temperature would have penetrated only ten times as far, that is, the fall at the comparatively small depth of 228 miles would have been less than one-tenth of a degree, while the remaining 3,700 miles of the radius would have been still more minutely affected by the surface cooling. Kelvin used his calculations to determine the so-called age of the earth, that is, the limits of time Vv-ithin which the conditions oi the earth's surface were likely to have been such as to make life possible thereon. Several things go to invalidate the sound- ness of his ?ireument. but two facts are made clear by his reason- ing which will always have an important bearing on our subject. The first is that owing to the enormous distances and to the poor conducting powers of rocks, the various layers of the earth are much isolated from each other as far as the distribution of heat is concerned. The second is that a wave of cooling progresses slowly from the .surface inwards, so that while at first the free surface itself cools most quickly, thereafter the layers that cool most cjuickly are to be found always deeper and deeper as time goes on. This is independent of any maintenance of temperature that may arise from the presence of radium, but is slightly af- fected by the heating that is generated by shrinkage. The dia- gram (Fig. i) shows the curves of Kelvin's imaginary earth after periods of cooling of 25,000.000 aufl 50,000.000 years re- spectively, and it will be seen by the third curve, which repre- sents the fall of temperature in the intervals, that a layer 30 miles deep had cooled most during the second 25,000,000 years. It is ea.sy to calculate what layer is cooling most rapidly after any given lapse of time on Kelvin's data. For instance, if apart from radio-active action a fairly uniform temperature had pre- vailed in the surface layers 100,000,000 years ago, the layer that would now be cooling most rapidly would be only 54 miles deep, and this is not unlikely to be something like the actual fact. Further, if the initial temperature had been 3.700° C, as Kelvin assumed, the rate of cooling of this layer would at present be one Centigrade degree in loo.oco years. The shrinkage pro- duced in this layer by its more rapid cooling would have tended PRESIDENTIAL ADDRESS — SECTION A. 37 to relieve the pressure on it, have produced in it a tendency to plasticity, and would have caused intense horizontal thrusts in the more superficial crustal layers — all of which are phenomena the occurrence of which must be regarded as extremely probable from other lines of evidence. There is now a general consensus of opinion that we must probably look to two sources for the origin of supply of the earth's internal heat. The first, and in some ways, the more important, is that which has arisen from the almost certain fall- ing together of the earth's materials from a much more widely disseminated state ; the second, the discovery and further in- vestigation of which we owe chiefly to the researches of Strutt and Joly, arises from the presence of uranium and its child radium in the rocks of the earth's crust, and perhaps to some slight extent in the interior of the earth. Temp. tuoo 3T0- ^ 'B ^ 5000 / / / 1 1 i J00 SECTIOX I!. sistent ; the quantity of ore available — in comj)arison with the reserves in the Pretoria beds — being small. The ore is thinl}- laminated and ranges in character from soft brown limonite, through compact red haniiatie to dense, hard fine-grained magnetite, the last being a product of the metamor])hisn] of beds of limonite and haematite by sheets of dolerite intrusive in the coal measures. The ore to be smelted at Vereeniging is of this type, occurring almost immediately below a sheet of dolerite. It is the purest iron-ore yet discovered in Soutli Africa, assaying from 66 to 69 per cent, of iron and from .5 to 1.5 per cent, of silica. Suljjhur and phosphorus are low, and it is quite free from titanium. The tonnage in sight, however, is not very great. A third Transvaal company, proposing to undertake the production of iron and steel, is the Locale and Industrielle Maatschappij of Pretoria, who have leased a large area of the Pretoria town lands adjoining the lease of the Pretoria Iron Mines, Ltd. The other blast-furnaces referred to are in Natal, one at Wentw^orth, a suburb of Durban, and the other at Sweetwaters; near Maritzburg. The former is being erected by the Iron. Concrete, and Asbestos Company, of Durban, and the latter was put up many years ago by Mr. S. L. Green. A preliminary attempt, recently made, to utilise this furnace failed, but I understand that after certain alterations have been carried out a further attem])t is to be made. In both instances sedimentary iron-ores from the Ecca beds of the Karroo system are to be smelted. That for the Wentw^orth furnace is being quarried at Elvarston, while at Sweetwaters it is proposed to use a mixture of local ore and Ermelo magnetite. The progress of these smelting ventures, at least two of which are merely the forerunners of far more ambitious projects, will be watched with the greatest interest, as it is generally recognised that an established iron and steel industry would be of the utmost benefit to the whole of South Africa. Prospects are very hopeful, as the South African demand for iron and steel is well over 50.000 tons i)cr annum, and is almost certain to increase.* The dimensions to which the industry will ultimately attain depend largely upon the success of the eftorts that are to be made as soon as practicable at Pretoria, to smelt the rich titaniferous magnetites of the Bushveld complex. The available reserves of these ores are practically inexhaustible — I estimate them at least at 2.000,000,000 tons — and if they could, as suggested 'by Stanley,! be smelted on a large scale in admixture with the siliceous ore * Cf. Stanley, G. H. : S.A. Journ. Industries. December, 1917. t Cf. Journ. Cheiii. Met. and Min. Soc. S.A.. November, 1909, and May, X910. PRESIDENTIAL ADDRESS SECTION ]!. 6l of the Pretoria series — of which I estimate that there are some 1,000,000,000 tons available — using cheap non-caking Transvaal coal as fuel. South Africa should be able to export iron and steel in competition with the great iron-producing countries of the world. Iron Pyrite. Owing to the increasing difificulty of obtaining adequate supplies of sulphur fron] Sicily and the United States, a consider- able proportion of the sulphuric acid requirements of the large explosive companies and other indnstrial concern'^ is now manu- factured from pyrite mined, or obtained as a by-product of gold- mining, in the Transvaal. The available reserves of the mineral are considerable, and, as the acid can be made more cheaply from local pyrite than from imported sulphur, there is every prosj^ect of pyrite-mining becoming one of the permanent industries of the country. Kaolin. Since the closing-down of the pottery at Olifantsfontein, between Germiston and Pretoria, the only use to which kaolin has been put in South Africa is the manufacture of whiting, distempers, and wall paints, " Blanco," and the like. The prin- cipal producers are the Sienna Paint Company, of Durban, who obtain their kaolin from a deposit near Padleys Station, on the Durban-Maritzburg railway. Lead. Small pockets and veins of galena occur and have been worked at many localities in the Dolomite of the Transvaal system in the Transvaal and on the Kaap Plateau. The mineral is also found in fissure veins in the Pretoria series and in the Waterberg sandstone formation, of which several are being exploited. At the present time the lead output of the Union is derived mainly from a vein in Waterberg sandstone, in the Blaauwberg Range, in the northern part of the Zoutpansberg district of the Transvaal, and from occurrences in the Dolomite. There is little prospect of any considerable increase in production. A plant for the production of white lead from cerussite has been erected at the Edendale lead mine, to the north of Hatherly. Zinc. There is no production of zinc or zinc ores in the Union at present. The only important deposits hitherto discovered are in the Malmani division of the Transvaal, near Ottoshoop, where lead and zinc ores occur partly in the form of pipes and partly in the form of disseminations in the Dolomite of the Transvaal system. In 191 4 a concentrating plant was erected at the Blane- Witkop Mine, jjnd was worked for a short time, but it was found 62 PRESIDENTIAL ADDRESS SECTION V.. impossible to dispose of the concentrate at a remunerative price owing to the fact that, at that time, smelters in the United Kingdom and the United States, had more ore than they could deal with. x\bout 200 tons of concentrate, averaging 50 per cent, of zinc, were produced. Arsenic. Within the past six months a promising start has been made to produce white arsenic locally, this material being extensively used in the manufacture of arsenite of soda for sheep and cattle dips, insecticides, and the like. The output for the first four months of 1918, amounting to 6.185 tons, valued at £619, came from the Stavoren Tin Mine, where massive arsenopyrite occurs, together with cassiterite, scheelite, copper pyrite, and other minerals. A plant for the production of white arsenic is also being erected at the Consort Mine in the Barberton district. Here arsenopyrite is associated with gold. As some £80,000 worth of arsenite of soda is annually con- sumed in the Union, the prospects of the industry appear very hopeful. Magnesite. The Union has considerable resources of magnesite, but owing to the low price of the mineral it is at present only being worked at Budd's Mine, near Malelane, in the Barberton district. The output of the mine amounted in 1917 to 781 short tons, valued at £2,050. The production of magnesite may be expected to increase with the expansion of the local steel industry, but there is little prospect of estabHshing an export trade in it.* Manganese. The manganese output, recorded in the table for 191 7, came ];art]y ifrom a vein deposit in the Magaliesberg quartzite, near Derdepoort. and partly from an occurrence which is being ex- ploited on the farni Daniels Rust, 12 miles north of Krugersdorp. Here the manganese occurs as nodules, up to 12 inches in diameter, composed of a mixture of pyrolusite and psilomelane. These are scattered indiscriminately through residual clay, resulting from the weathering of the dolomite of the Transvaal system. The nodules average about 47 per cent, of metallic manganese. The deposits appear to be of considerable extent, and can be cheaply worked. A somewhat similar occurrence is being opened up at Rand Gate, near Randfontein. At this locality, however, the man- ganese content of the nodules is lower than on Daniels Rust. Within the last week a promising deposit of this nature has * Cf. Wagner, P. A.: S.A. Joiirii. [)idusfries. March. 1918. PRESIDENTIAL ADDRESS — SECTION B. 63 also been discovered on the property of the Randfontein Central Gold Mining Company. Mica. The pegmatites of the so-called Mica Belt, in theLeydsdorp division of the Transvaal, yield muscoviate mica of excellent quality, of which there is a small but steady production. Efforts are being made to establish an export trade in the mineral, which is in great demand at the present time for aeroplanes and the condensers of wireless stations. Limited quantities are used in South Africa for electrical purposes, and there is a small mica factory in Johannesburg, where mica lamp-chimneys, stove-fronts, and micanite sheets are made.* Soda. The soda production of the Union, amounting m 1917 to 5,674.75 tons, value at £29,192 is derived from the remarkable salt-panf on the farm Zoutpan, 25 miles north-west of Pretoria. Hitherto operations have practically been confined to thin layers of nearly pure trona, but enormous quantities of soda are also available in the mud underlying and interbedded with the trona layers. This has been proved to a depth of over 200 feet, and averages about 15 per cent, of NaoCog. A plant for the preparation of pure soda from the mud is at present being erected, and if it proves successful the future of the industry will be assured for many years to come. Talc. Almost the whole of the talc production of the Union comes from the Verdite Mine, near Noordkaap Station, in the Barberton district of the Transvaal, "in the neighbourhood of which there are other considerable deposits. There is also a small production in the Krugersdorp district of the Transvaal, and in Zululand. The talc of the Barberton district deposits has been proved to be well adapted to the manufacture of paper and rubber. As it can be cheaply mined, and the railage to Delagoa Bay is only 3s. 6d. per ton, it is confidently anticipated that a large export trade in it will be established after the war.* Tungsten. The small output of tungsten recorded in the table of mineral production comes from the Stavoren Tin Mine, in the Olifants River tin-fields. Several tons of scheelite were also recovered in 1917 from a deposit in the neighbourhood of Leydsdorp, but this is not being worked at the present time. * Cf. Wagner, P. A. : S.A. Journ. Industries, April, 1918. t For a description and plan of the Salt Pan see Wagner, P. A. : Proc. Geol. Soc. S.A. (1917), 30-38. t S.A. Journ. Industries, June, 19 18. 64 PRESIDENTIAL ADDRESS SECTION B. No workable occurrence of wolframite has been found in the Union, though the mineral occurs in association with cassi- terite in certain of the mines of the Waterberg tin-fields, and in the quartz-lodes on the farm Annexe Langverwacht, near Capetown. Lime. A recent survey* has shown that the Union has very considerable resources of limestone, though the largest deposits unfortunately are rather unfavourably situated with regard to the principal industrial centres. The most important occurrence being worked at the present time is that near Taungs, which is estimated to contain 7,000,000 tons of high-grade limestone. There is also a considerable deposit near Potgietersrust, in which the limestone has resulted from the de-dolomitisation of the normal dolomite of the Trans- vaal system. f Pure cave limestone occurs in the Dolomite at many localities. Until recently deposits of this type supplied the greater part of the pure lime used in the cyanide works on the Witwatersrand, and they still make an important contribution to the total output. Fairly considerable quantities of " blue " lime obtained from "burning" ordinary dolomite, are produced at Irene, Olifants- fontein, andjDther localities. It is used principally for building purposes. Arenaceous surface-limestone is very largely employed for the manufacture of cement. Rock Phosphate. There has now for nearly two years been a steady output of crushed rock phosphate from the deposits at Saldanha Bay. These are of great extent, $ readily accessible, and capable of being cheaply worked ; and are without doubt destined to afford the basis of a very important industry. The phosphate, an intimate mixture of aluminium and iron phosphates, has been formed mainly by the phosphatisation of granite and quartz porphyry detritus, and to a less extent by the phosphatisation of these rocks in situ. Though almost completely insoluble in ammonium citrate, it has practically demonstrated that the phosphate, if finely ground, has a very beneficial effect when applied together with finely-ground lime to soils poor in phosphorus, and to sour soils; the phosphorus being doubtless rendered assimilable by the agency of soil bacteria. It was early realised, however, that its efficiency as a fertiliser could be greatly increased by rendering the phos- phoric acid more soluble and several processes to effect this have * Cf. Wybergh, W., and Du Toit, A. L. : The Limestone Resources of the Union, Geological Survey Memoir, No. 11, Union of South Africa. t Cf. Young, R. B., Trans. Geol. Soc. S.A.. 1916. p. 57. + Cf. Du Toit, A. L. : Report on the Phosphates of Saldanha Bay. Memoir No. 10, Geological Survey, Union of South Africa. PRESIDENTIAL ADDRESS — SECTION B. 65 been devised. When one or the other of the processes has been successfully applied, there should be a big increase in the output. There is also a small deposit of the more valuable calcium phosphate or phosphorite in the neighbourhood of Saldanha Bay on the Hoetjes Bay Peninsula, and this encourages the belief that further deposits of phosphorite remain to be discovered in this locality or along some other section of the littoral. As the soils of the Union are, generally speaking, very deficient in phos- phorus, any discovery of this nature would be of the utmost importance. Another source of rock phosphate investigated by Du Toit* are the phosphatic nodules occurring in the Upper Ecca shales in the Weenen area and other localities in Natal. These contain from 20 to 30 per cent, of phosphoric acid, and have been proved experimentally to have considerable fertilising value when finely ground. ( )wing to their irregular and sparing distribution through the shale, operations will perforce have to be confined to the mere collecting of the nodules set free by weathering or still partially imbedded in the matrix. Du Toit is of opinion that there is enough of this material scattered over the Weenen area to enable a mill to operate with a small output for some time. With the experience gained it is suggested that other localities, such as the neighbourhood of Tadysmith, might with advantage be investi- gated. Chert. Chert, suitable for lining tube-mills, has a wide distribution in the Dolomite formation, and is won in the neighbourhood of Frederikstad. in the Potchefstroom district of the Transvaal. Owing to the introduction pf steel and composite liners, the demand has fallen considerably, the output for 191 7 having amounted tO' only 180 tons against 604 tons in 1913. Gypsum. This mineral is principally used in South Africa in the manu- facture of Portland cement, in which it acts as a retarder. There are important deposits at Ngbevu, in the Tugela Valley, in Natal, on the farm Vrede, in the Boshof district of the Orange Free State, and on the farm Bestpan, near Kimberley. The demand for gypsum is limited, and there is no likelihood of any great increase in production in the near future. Kieselguhr. Kieselguhr occurs as an earthy deposit in the beds of certain pans in the Amsterdam district of the Transvaal ; also near Krugersdorp, and in Griqualand West. * Cf. Du Toit, A. L. : The Ecca Prosphates of Natal. S.A. Journ. Industries, January, 1918. 66 PRESIDENTIAL ADDRESS SECTION li. It is used in admixture with asbestos for covering boilers and steam pipes, and for preparing brass and metal polish. There was a small production of the mineral in 191 3, but, so far as I am aware, none of the deposits are being worked at present. Salt. The salt industry of the Union continues to make steady progress, though very little is heard of it, and information regarding recent progress is difficult to obtain. The whole of the output, amounting at the present time to nearly 60,000 tons per annum, is derived from salt-pans, most of which are located on the Dwyka tillite or shales. The supply of salt, which owes its origin to a process of natural concentration, is constantly replenished, and the pans, as pointed out by Rogers and Du Toit,* are undoubtedly among the most valuable assets of the country. For the actual production and refining of the salt, solar evaporation in shallow pans is generally relied upon. This system, while very economical, has the disadvantage that the output is dependent on weather conditions, being greatly diminished during the winter months, when very little evaporation takes place. To remedy this, some of the salt companies have of recent years supplemented their evaporating ponds by furnace-heated pans, which enable a fairly steady output to be maintained all the year round. Cement, Clay Products, and Siructukal Material. The value of the output of the industries under this heading amounted in 1917 to £877,934, an increase of £255,941, compared with 191 3. This is due largely to the great expansion of the local cement industry, which is now supplying the whole of the rapidly- increasing South African requirements. The Union has three large cement factoreis, and the erection of two others is con- templated. The clay and pottery industries have also made very satis- factory progress, the cutting-ofT of oversea supplies having given a great impetus to the production of roofing tiles, stoneware, and fireclay goods. There is also a magnificent opening for the local manufacture of electrical insulators, sanitary ware, and crockery, and the ceramic industry appears altogether to be capable of very considerable expansion. The great shortages of bottles has led to the establishment of a bottle factory at Dundee, in Natal. The glass is obtained by melting broken bottles. The actual manufacture of glass is, however, also to be undertaken shortly, sand for this purpose being available at several localities. It is to be hoped that this and other industries that have come into existence as a result of the existing conditions, will be * Cf. The Geology of the Cape Colony, p. 478. PRESIDENTIAL ADDRESS SIXTION H. 6/ adequately protected after the war, when it is probable that dumping on a colossal scale will be attempted. Future Discoveries. The future of the mineral industry of South Africa, in so far as it is dependent on deposits actually known or worked at the present time, has already been discussed at some length in the foregoing review. It remains to consider what prospects the country offers in the matter of fresh discoveries. In dealing with this interesting subject, it will be useful to divide the Union into a number of mineral provinces — ^^that is, natural divisions, which by virtue of the geological or physiographical conditions prevailing within them yield, or may be expected to yield, certain minerals. Those having even a passing acquaintance of the geological features of the Union will realise that this scheme, if rigorously carried out, would involve the discrimination of a large number of areas, many of which, in addition to being ([uite unimportant, could, owing to their small size, not be shown on the accompanying map. For this and other reasons it is proposed to adopt the following nine-fold division, though it in nearly every instance involves the inclusion in the individual provinces of rocks of different geological age or of widely separated areas of the same formation : — ( I ) The Witwatersrand-Ventersdorp Province. ( 2 ) The Karroo Province. (3) The Transvaal Sj^stem Provinces. (4) The Bushveld Province. (5) The Old Granite-Swaziland System Provinces. (6) The Copper Region of Little Namaqualand. (7) The West Coast Province. (8) The Cape System Province. (9) The Kalahari Region. The boundaries of the provinces, except where actually determined by geological boundary lines, are largely arbitrary. The Witwatersrand-V'hnti'ksdokp Province. The Witwatersrand-Ventersdorj) Province embraces a con- siderable extent of country in the Southern Transvaal and adjacent territories occupied or underlain at comparatively shallow depth by the rocks of the Witwatersrand and Ventersdorp systems, which for the purposes of the present address have been grouped together. It includes a fairly considerable area of Karroo rocks to the east and south-east of Boksburg, narrovN strips of dolomite to the west of Randfontein and to the south- east of Klerksdorp. and has also for convenience been made to embrace the area of older granite to the north of Johannesburg, 68 PRESIDENTIAL ADDRESS SECTION B. and several areas of older granite and Karroo rocks in the South- western Transvaal. Including as it does the greatest gold-field and the two greatest alluvial diamond fields in the world, this is easily the most important of the nine divisions, contributing about 80 per cent, by value of the total mineral output of the Union. In addition to gold and diamonds, it yields silver, coal, asbestos, building-stone, quartz, talc, and a considerable variety of clays. As regards future discoveries, the possibility of locating further outcrops of the Main Reef, or areas underlain by it, will doubtless continue to act as a powerful incentive to prospecting and boring within the tract of country over which the Witwaters- rand beds are known to extend.* On the whole it does not appear likely that the productive area of the Rand gold-field will be very materially added to, either to towards the east, south-east, or west. It is possible, however, that some of the work now being carried out in the Heidelberg area may bear fruit, and that the faulted continuation of the Main Reef zone will eventually be located beneath the Dolomite to the south-west of the Randfontein group of mines. There is also a remote possibility that a " Farther "' East Rand may await discovery below the coal-measures of the Bethal and Middelburg districts, but this systematic deep-boring alone can decide. In regard to the Venterskroon and Klerksdorp gold-fields, the outlook is not very hopeful. The prospecting and boring operations carried out in the former area some years ago, under the direction of Dr. Corstorphine, render it practically certain that the Main Reef zone does not exist in the Witwatersrand beds as developed within it. In so far as the Klerksdorp district is concerned, it still remains to be proved whether or not the Main Reef zone is represented, and, until the complex geological structure of the area has been more completely unravelled, it will hardly be possible to do this. Some geologists have identified Buffeldoorn Reef, until recently worked by the Quest Gold Mining ( onipany, with the Main Reef, but the correlation rests on rather a slender basis. In any case, the disappointing results obtained from the exploitation of this ' reef " indicate that, if it is the Main Reef, the latter is verv th'n and patchy in the Klerksdorp district. Coal. — Fairly considerable quantities of coal are produced from the coal-measures overlying the Witwatersrand beds and * The most easterly exposure of undoubted Main Reef zone hitherto located is on, or more correctly speaking, beneath the farm Droogefontein- No. 447, on the Far East Rand ; the most westerly, in the south-western corner of the claim-holaing of the South Randfontein Deep, on the Wefet Rand; and the most southerly, on the farm Platkopje, No. 63, 16 miles south-west of Heidelberg. PRESIDENTIAL ADDRESS — SECTION B. 69 Dolomite on the Far East Rand, but the generally superior quality of the coal found farther east, combined with the improved railway facilities, have tended of recent years to diminish the amount of coal mined in the area There is little probability of any important coal-bearing areas, other than those known at present, being located within the province. Diamonds. — The whole of the Witwatersrand-Ventersdorp Province falls within the Diamond Belt previously defined, and it is not unlikely, therefore, that important pipes and dykes of diamondiferous kimberlite await discovery within it. The Karroo Province. The Karroo Province, occupied by the sedimentary and igneous rocks of the Karroo system and dykes, sills, and laccolites of dolerite intrusive in them.* is by far the most extensive of the mineral provinces, embracing over one-half of the area of the Union. In the value of its mineral production it is second only to the Wtiwatersrand Province, the supremacy of which it will doubtless eventually rival. It is not only the great repository of the fuel-wealth of the country, but includes the most productive section of the Diamond Belt. Apart from coal and diamonds, its mineral products include salt, iron-ore, rock-phosphates, fireclay, and other clays, gannister, building-stone and gypsum. Gold has also been found. f Potential sources of mmeral wealth are natural gas, oil and alum shale, and the magnetic copper-nickel deposits of Griqualand East. The Copper-Nickel Deposits of lusisiva, Tahankuln, and l^onki, in Griqualand East. — These deposits are similar in many respects to those of Sudbury in Canada, at the present time the principal source of the world's supply of nickel. The ore-bodies occur J at the lower contacts of great cakes or basin-shaped masses of gabbro-norite, merging downward into picrite§, which have been shown by Du Toit to be the remnants of a vast sill intrusive in the lower division of the Beaufort series. The lower surface of this sill appears to have undulated considerably. The existing gabbro masses represent the parts filling the hollows, the inter- vening dome-like connections having been removed by denudation. The principal ore-minerals are pyrrhotite chalcopyrite and pent- landite, with smaller amounts of bornite and niccolite. Platinum * It has also been made to embrace the broad belt of Cretaceous and Tertiary rocks along the coast of Zulnland, and several inliers of Older Granite and rocks belonging to the Transvaal and Waterbera; systems to the south and south-west of Prieska. t At Cekkers Kloof, near Cradock, where the gold occurs in asso- ciation with prehnite. t Cf. Du Toit, A. L. : The Geology of the Transkei. an Explanation of Sheet 27 (Cape). Geological Survey, Union of South Africa (1917) , 18-27. § These rocks represent a special phase of the widespread Karroo dolerite. 70 PRESIDENTIAL ADDRESS — SECTION li. is also present. Assays of several ounces to the ton have been recorded, but the average platinum content of the ore appears to be between ^ dwt. to i dwt. per ton. The ore clearly owes its origin to a process of gravitative differentiation, and it is believed that ore bodies very much larger than any hitherto exposed await discovery on the concealed floors of the basins or cakes. Thus, the mineralised zone, on which most exploratory work has been done at Insiswa, is in all prob- ability only the eastern edge of a great lens-shaped mass of ore underlying the Insiswa Mountain. The same applies to the Tonti and Tabankulu occurrences, and as the massifs are of very great size — ^that forming the Insiswa Mountain is ten miles in diameter — it will be seen that the area offers enormous possibilities. Some, indeed, see in it a second Sudbury. Apart from the value of its metallic contents, the ore is of value as a potential source of sulphur. Petroleum. — The Karroo Province contains the only area in the Union — namely, the so-called Folded Belt, along its southern margin — within which some, at any rate, of the requisite conditions for the formation and concentration of petroleum in commercial quantities are satisfied. The prospects of finding oil in the Folded Belt are, as has been pointed out elsewhere,* not very hopeful, because, if present, it is probably so deeply buried as to be beyond com- mercial accessibility, but the possibility of its being struck none the less exists. Oil-Shale. — There are extensive deposits of oil-shale in the Ermelo and Wakkerstroom districts of the Transvaal, and in the Utrecht and Impendhle divisions of Natal, and equally extensive deposits are said to exist in the north-eastern portion of the Orange Free State. . The deposits are likely sooner or later to form the basis of an important industry. Natural Gas. — Natural gas has so far only been struck in considerable quantity on the farm Gruisfontein, in the Heidelberg district of the Transvaal, f where it was encountered at a depth of 540 feet, beneath a dolerite sill, which acted as an impervious cover. Cunningham Craig| is of opinion that there may be other isolated and irregular reservoirs of gas in the area, and also considers that the Fauresmith district of the Orange Free State and the Folded Belt of the Karroo system offer favourable con- ditions for the occurrence of gas. Diamonds. — The discovery of further workable occurrences of Kimberlite within the Karroo Province may be predicted with confidence, the neighbourhood of Kimberley and the north- * C/. S.A. Journal of Ivdustries, October, 1917. t Dr. Du Toit inforrhs me that an important strike of natural gas was made some months ago near Dannhauser, in Natal. X Report on the Petroleum Prospects in the Union of South Africa. Pretoria, 1914, P- T9. PRESIDENTIAL ADDRESS — SECTION Jl. /I eastern portion of the Boshof district of the Orange Free State holding out the greatest promise.* The Bushveld Province. This region coextensive with the Bushveld igneous complexf yields a great variety of useful and valuable minerals, all derived by differentiation or other processes of natural concentration from the Bushveld granite and allied rocks. The following metals and minerals have been or are being worked: Tin, copper, arsenic, bismuth, tungstem, lead, J^old, silver, molybdenite, and trona. Of the important mineral deposits within the area, that have not as yet been worked, but are receiving attention at the present time, mention may be made of the occurrence of high- grade haematite on the farm Kromdraai, south-east of Settlers — a replacement deposit along a zone of fracture in felsite; the chromite deposits on the farm Jachtlust No. 333, 50 miles south- south-east of Pietersburg ; and the copper-nickel deposits on the ifarm Vlakfontein. No. 902, west-south-west of the Pilandsberg, in the Rustenburg district. The Vlakfontein deposits are in the form of irregular masses of nickeliferous pyrrhotite containing varying amounts of copper, developed along fairly well-defined parallel zones of fissure in pyroxenite belonging to the marginal phase of the Bushveld Igneous Complex. The zones have been followed over a con- siderable distance, and are being opened up by means of shafts and tunnels. The Vlakfontein ores contain small amounts of platinum, and it is of interest to recall that platinum is also present in the remarkable stratiform segregations of chromite occurring at much the same horizon in the basic margin of the Bushveld laccolite. Thus a series of samples of chromite taken by me to the south-east and south-west of Turfgrond Station, in the Rusten- burg district, assayed up to 1.5 dwts. of platinum and .15 dwt. of osmium and iridium per ton. Here, as in certain other areas where the chromite has been tested, the platinum metals, unfor- tunately, are not uniformly distributed through it, and the average values obtained by sampling were not sufficiently high to warrant the exploitation of deposits, either as a source of platinum or chromite. Having regard to the enormous extent of the deposits — they crop out intermittently over a distance of fully 400 miles — it is quite possible, however, that some sections of the chromite " layers ' will be found to contain platinum in profitable quantities. The chromite itself, as previously intimated, is being opened uj) on the farm JachtkiPt, situated 50 miles south-south-east of * Cf. The Diamond Fields of Southern Africa, p. 4. t For convenience it has also been made to include the VVaterberg Plateau, and the igneous and sedimentary rocks of Karroo age underlying the Springbok Flats. ~2 I^KESIUENTIAL ADDRESS SECTION H., Pietersburg, where there are two distinct layers of the mineral, averaging six feet and 12 inches in thickness respectively. The main layer averages 39 per cent, of chromic oxide, and it is believed that this can easily be brought up to 42 per cent, by hand-picking. The principal mineral product of the Bushveld Province is tin. which, as already stated, has a very wide distribution. Con- ditions known to be favourable to the occurrence of the metal, moreover, exist over extensive areas, as yet but imperfectly pros- pected, and it may safely be predicted, therefore, that many important cassiterite deposits will, in the course of time, be discovered within it. The same applies to most of the other metals previously mentioned, and the Bushveld Province appears altogether ^ be an area of exceptional promise from the point of view of future discoveries. The Transvaal .Snstem Provinces. These are t\vo in number. The more important, marked A on the accompanying map, takes in a large tract of country in the Central and Southern Transvaal ; and the other, marked B, the greater part of Griqualand West. They are occupied mainly by the rocks of the Transvaal system, but for convenience both have been made to include fairly considerable areas of sedimentary and igneous rocks belonging to the Waterberg system, the Transvaal region in the Pretoria and Middelburg districts, and the Griqualand West region along its western margin. The Transvaal region of the Transvaal .System Province ranks third in point of output among the various provinces. It includes the Premier Diamond Mine,* the Pilgrim's Rest and Ottoshoop goldhelds, the gold mines on the Black Reef, in the Southern and South -Western Transvaal, the asbestos occur- rences of the Lydenburg district, and the extensive deposits of iron-ore in the Pretoria series, and is clearly destined for many years to be an important source of mineral wealth. It also produces lead, pyrite, manganese, blue lime, fluorspar, and slate, and contains the only economically-important deposits of zinc hitherto discovered in the Union. Silver, copper, and cobalt have been worked, and potassium nitrate, cinnabar, f and lead vanadate fQiind within it. The great variety of its mineral products, the fact that these occur at such widely-separated localities, and the uniformity of the geological conditions prevailing over great areas render the prospects of future discoveries within the province distinctly bright. * The Premier Mine, tliough almost completely surrounded by felsite, belonging to the Bushveld complex, lies well within the limits of the area occupied by the Pretoria series. + Tn the Malmani district at Ottoshoop. PRESIDENTIAL ADDRESS SECTION B. 73 It is a practical certainty, for example, that further workable deposits of gold and asbestos remain to be found in the Ly den- burg district, and that many occurrences of lead and zinc await discovery in the Western Transvaal, while the possibilities of gold mining in that region cannot by any means be said to have been exhausted. In so far as the Central Transvaal is concerned, most of the epigenetic mineral deposits occurring in the Transvaal system appear to be related genetically to the Bushveld granite and allied rocks, and it is the portion of the province falling within the sphere of influence of the intrusive activity of the Bushveld complex that thus holds out the greatest promise. As the province includes a considerable part of the Diamond Belt, there is also a possibility of further discoveries of Kim- berlite pipes and dykes within it. II. — The Griqualand West region, as already indicated, is far less important. Its mineral products include asbestos, lime- stone, lead, and alluvial diamonds. It also contains enormous deposits of iron-ore that may some day be of great importance. Potassium nitrate, which occurs as thin veins in and as an encrus- tation on the shales and slates of the Pretoria series, and also in angular fragments as a scree deposit, has a wide distribution to the north and north-east of Prieska. The mineral is believed to have been derived by a process of nitrification from the excreta of rock-rabbits, bats, and the like. Up to the present efforts to work the deposits have not met with success. Some very promising occurrences are said, however, to have been discovered recently, and a company has been formed in Johannesburg to exploit them. The results of its activities will be awaited with interest. Further discoveries of lead, zinc, and asbestos may be expected within the province. The Old Granite, Swaziland System Provinces. Under this heading are included four large disconnected areas occupied by the rocks of the Swaziland system, or their supposed equivalents, and old granite and gneiss intrusive in them. The areas are numbered I, II, III, and I\' on the accompanying map. I. — Embraces the whole of the Northern, North- western, and B>astern Transvaal, Swaziland, and portion of Northern Natal. II. — Includes portions of Griqqualand West, and of the Ma f eking division of the Cape Province. III. — Includes an elongated tract of country in Natal and Zululand, occupied partly by the granite and rocks belonging to the Swaziland system, and partly by Table Mountain sandstone, which it was found more convenient to group with these rocks than with the Karroo beds. 74 PRESIDENTIAL ADDRESS SECTION li. IV. — Takes in almost the whole of the Calviiiia and Kenhardt divisions of the Cape Province, the southern and western portions respectively of the (jordonia and Prieska districts, and a portion of little Namaqualand. Of the afore-mentioned, 1, which includes considerable areas of Waterberg sandstone and a small patch of Karroo rocks, is by far the most important. It is a region that stands unrivalled in the variety of mineral resources. These include gold, copper, silver, antimony, tin. lead, corundum, graphite, magnesite, talc, timgsten. arsenic, pyrite. mercury, mica, ornamental stones, salt, and limestone. By virtue of the geological conditions prevailing t)ver large areas, prospects of future discoveries — particularly of gold and copper — are very hopeful, and as regards latent potentialities, it is probably the most promising of the various provinces. Further discoveries of gold may be expected in the Rarberton district, where, according to Hall,* the contact belts of the De Kaap and Crocodile Poort granite massifs merit particular atten- tion; also the Murchison Range and surrounding area. As regards copper, the neighbourhood of the Messina Mine appears to ofier the greatest possibilities, though deposits of the metal have been found at a number of widely separated points in the North-Eastern Transvaal. The north-western and extreme eastern portions of the area, which are virtually unprosjiected. will also doubtless be the scene of many future discoveries. II. — This area, occupied for the most part by granite and gneiss, includes three belts of ancient schistose and sedimentary rocks, belonging to the Kraaipan series, which have many features in common with the rocks of the Swaziland system. A number of auriferous veins were opened up in the Kraaipan series at Madibi and Kraaipan some years ago, but proved disappointing. No other mineral deposits have hitherto been found. In view, however, of the similarity in geolgical conditions to those pre- vailing in the goldfields of Southern Rhodesia and in the Barberton district, and of the fact that the greater part of the area has not been prospected, it can hardly be doubted that further gold occurrences remain to l)e discovered. III. — Gold has been mined at a number of localities in this province. Asbestos and talc are being quarried on a small scale, and tin. copper, graphite, and mica have alsc^ been worked. Results on the whole have been disappointing, but the area is generally regarded as offering considerable possibilities in the matter of future discoveries. According to Hatch, t there are large areas within it that should be the home of many deposits * Memoir No. 9, Geological Sunry. Union of South Africa, pp. 322, 329- t Cf. Report on the Mines and Mineral Resources of Natal, p. 15. PRESIDENTIAL ADDRESS SECTION H. 75 of metals, such as ,^old, iron, and copper, while the pegmatites that vein the schists of the Swaziland system, near the margins of the granite intrusions, are favourable to the occurrence of tin, molybdenite, and mica. IV. — This area is occupied by granite and gneiss, except along its eastern margin, where there is a broad belt of metamor- phosed sedimentary and igneous rocks, belonging to the Kheis esries — correlated tentatively with the Swaziland system. The only important mineral deposits hitherto discovered are the lenses of pyrite, in part cupriferous, that are being opened up at the Areacheap Mine, tojhe north-west of Upington. Copper-bearing quartz veins occur in gneiss in the neigh- bourhood of Pella on the Orange River, and copper in the form of malachite, chrysocalla and copper glance is also found in quartz veins on the farm Toekomst West, on the Molopo. about five miles south of the Keetmanshoop railway. These occurrences, while not workable, serve to indicate that copper is widely distributed. The greater part of the region is still a terra incognita in so far as the prospector is concerned, and certainly seems to merit more attention than it has hitherto received. The Copper Province of Little Namaqualand. This province, occupying a fairly considerable extent of country in the north-western corner of the Cape Province, embraces two distinct mineral areas,* namely, ( i ) a northern region characterised by veins containing native copper and copper sulphides in a gangue of quartz, carbonates, felspar, and chlorite. None of these are being worked at the present time. The Kodas and Numees Mines, situated in the mountainous country near the Orange River, yielded considerable quantities of high-grade ore in the seventies of last century. Transport, however, offered insurmountable difficulties, and they were closed down after a time. Both mines are said to contain considerable reserves of ore, which will doubtless be exploited as soon as the area is rendered more accessible by the constrijction of roads and railways, when other workable deposits will also doubtless be discovered. (2) A southern region, embracing about 2,000 square miles in the middle of the Namaqualand division, characterised by the presence of dykes and irregular intrusions of a genetically con- nected series of igneous rocks — ranging from mica-diorite at Ookiep, through norite at Tweefontein, to hypersthenite at Naba- beep — which contain as primary constituents varying amounts of copper sulphides ; the country rock being gneiss. No fewer than 344 distinct intrusions have hitherto been located and mapped, and others in all probability await discovery. * Rogers, A. W. : The Copper Deposits of Little Namaqualand, Proc. Geol. Soc. S.A., 1916, pp. xxi-xxxiv. 76 PRESIDENTIAL ADDRESS — SECTION B. To date over £22,500,000 worth of copper has been produced in this region. This area also yields corundum and merchantable mica, and columbite, beryl, and spodumene occur in the pegmatites of the Steinkopf district. It is thus evidently highly mineralised, but is unfortunately handicapped by its inaccessibility, its arid character, and the lack of transport facilities. The West Coast Region of the Capf. Province. This includes a strip of country running along the west coast of the Cape Province from Cape Point to the mouth of the Orange River. It is occupied by rocks belonging to the Nama system, granite, and porphyries intrusive in them, recent calcareous deposits and sands, and for convenience has been made to embrace several areas of Table Mountain sandstone. Its mineral products include tin, rock-phosphate, building- stone, clays, limestone, and niineral-water. Among other economic minerals that occur, but have not hitherto been discovered in workable quantities, mention may be made of wolframite, arsenopyrite, molybdenite, and gypsum. In the matter of future discoveries, rock-phosphates and tin appear to hold out the greatest promise. Du Toit's investigations of the phosphate deposits of Saldanha Bay render it highly prob- able thatsimJar occurrences, not onlyof aluminous rock-phosphate, but of phosphorite, are to be found along the coast, and the whole of the littoral between Table Bay and the Orange River mouth appears to be worthy of careful investigation. As regards tin, it would be remarkable indeed if further workable deposits of that metal do not await discovery around the margins of the great intrusions of granite in the Western Province, while the newer granites of the Van Rhyn's Dorp district and Tittle Nama- qualand offer possibilities in the same direction. The Cape System Province. The Cape System Province embraces practically the whole extent of country in the southern and south-western districts of the Cape Province occupied tjy the rocks of the Cape and Creta- ceaus systems, and the important inliers of the Nama system in these. The area is singularly deficient in metallic mineral wealth, which is probably due to the almost complete absence of igneous rocks within it. The only important occurrences of metallic minerals hitherto discovered are the veins and deposits of manganese ore in the Table Mountain sandstone series in the Western Province, the alluvial gold deposits of the Millwood fields, in the Knysna PRESIDENTIAL ADDRESS — SECTION B. "JJ district, and the deposits of argentiferous galena found many years ago at the Maitland Mine, to the west of Port Elizabeth. Of the manganese deposits, only three, according to Welsh,*, are of any extent, and of these only one is really considerable, containing possibly about 500,000 tons of ore. The exploitation of this particular deposit, however, would hardly be feasible, because it happens to be the site of the Caledon hot springs and sanatorium. In the Milhvood goldfield, situated in the Outeniqua Moun- tains, steeply folded shales and sandstones, believed to belong to the Table Mountain sandstone series, are traversed by auriferous quartz-veins, carrying pyrite, blende, galena, and sometimes siderite. The occurrences are not worthy of exploitation, the small quantities of gold won on these fields being all alluvial. Natural gas and petroleum may exist beneath the anticlines into which the fossiliferous Bokkeveld beds have been thrown between Touws River and Montagu, but it is a remote possibility. The most promising potential sources of mineral wealth in the area are the occurrences of limestone, belonging to the Nama system, that occur in the inliers already referred to. A deposit of this nature is to form the basis of a large cement and lime- works at Robertson, and the possibilities of another inlier between Hankey and Port Elizabeth are being investigated with a view to establishing cement works in that neighbourhood. The dolomite limestone of the Cango area will also, no doubt, eventually become of importance as a source of " blue " lime. The clays and shales of the Cretaceous Uitenhage series are made into good tiles, pipes, and bricks at several localities. The formation also contains beds of lignite of inferior quality, but efforts to utilise this material have not so far proved suc- cessful. Certain sections of the southern coast of Cape Province, included in the area, appear to be worth prospecting for rock phosphate. The Kalahari Region. The Kalahari Region embraces the portion of the Kalahari falling within the Union. No important mineral deposits have been discovered within it, which is hardly a matter of surprise, seeing that, in addition to being practically waterless, the greater part of the area is covered with a deep mantle of sand and surface limestone that completely obscure the underlying rocks. The only economic minerals hitherto discovered in the Kalahari region are potassium nitrate and kieselguhr. The former occurs in the Matsap salt-pan, but apparently not in payable quantities. Kieselguhr is found in the Witkop pan in * Cf. Welsh, A. B. : Report on Manganese in the South-West Districts of the Cape Proz'ince. Dept. of Mines and Industries, Union of South Africa, 1917. 78 PRESIDENTIAL ADDRESS SECTION B. Gordonia, and also in some of the pans on the Grlqiialand West side of the Kalahari. Great stores of mineral wealth may be locked up in this tract of country, but there is little probability of any important discoveries in the near future. Conclusion. In concluding this brief and necessarily imperfact survey of the potential mineral resources of the Union, I would remind you that Africa has ever been a land of surprises. All things considered, it is improbable that any discovery rivalling in importance that of the Kimberley diamond mines or of the Witwatersrand goldfield remains to be made, but there is no knowing what may be in store ; and when it is remembered that the past decade has witnessed the discovery of the asbestos and corundum deposits of the Northern Transvaal, the phosphate occurrences of Saldanha Bay, two small diamond mines and a number of promising deposits of tin and other metals, and that vast tracts endowed by nature with geological conditions favour- able to the development of mineral wealth are as yet virtually unattacked by the pick of the prospector, you will, I think, agree with me that there is every warrant for the most sanguine expectations in regard to the future. Section C— BOTANY, BACTERIOLOGY, AGRICULTURE, AND FORESTRY. President of the Section : C. E. Legat, B.Sc. WEDNESDAY. JULY lo. . The President delivered the following address : — TIMBER SUPPLIES AND FORESTRY IN THE UNION. The Union is almost entirely dependent for its timber sup- plies on importations from abroad. In this respect its position is similar to that of Great Britain. Both countries are very poorly wooded. A recent return shows that the area of wood- land per head of population in the United Kingdom is 0.067 o^ an acre. If the native population is included, the figure is prac- tically the same here, viz.,- 0.07. Calculated on the basis of the white population alone, the South African figure is more favour- able, viz., 0.32 acre. But there is an important difference be- tween the position in Great Britain and here. The woodlands of the United Kingdom are cultivated forests, and as such more productive, and they are comparatively accessible to roads and railways. In South Africa, on the other hand, the forests are wild, and considerable areas are far removed from roads and rail, so that the present direct utility of much of them is very small. For the past thirty years or more there has been a growing public opinion in Great Britain that something should be done to place that country in a more independent position in regard to its timber supply. For the five years previous to the outbreak of war the country's timber bill had been on the average about £37,000,000 per annum, and the local production insignificant. Commissions and committees were appointed at intervals to go into the matter, and they made recommendations, but nothing very concrete resulted. Now the war has brought home to the Government and the country most forcibly the unsoundness of the national position in regard to this question. At a time when shipping was most urgently required for other purposes there was no alternative but to earmark a large amount to transport this essential war material, even though it involved reduced rations for the people. During the years 1915 and 1916 the imports of timber absorbed 7.000,000 nett tons of shipping, and cost £74,000,000, or £37,000,000 in excess of the pre-war value. The Prime Minister, in his speech of February, 191 7, on the submarine menace, emphasised that the saving of this tonnage was a vital necessity, and that to effect it, it would be necessary to fall back on the country's own timber resources and to arrange with the French Government for some of their forests to be placed at Great Britain's disposal. In view of this state of affairs the appointment of a Forestry Sub-Committee of the Reconstruction Committee " to consider and report upon the best means of conserving and developing the woodland and forestry resources of the United Kingdom D 8o PRESIDENTIAL ADDRESS SECTION C. having regard to the experience gained during the war "' was not surprising. This Sub-Committee has now reported. One of the con- clusions arrived at was that " the war has disclosed no demand which could ncit have been satisfied by timber grown in this country." In other words, Britain's neglect of forestry cost the country £37,000,000, and seriously impaired her war efficiency. Another conclusion was : " Forests are a national necessity ; the country must have them, even though (they yield less than the current rate of interest on the capital invested. The whole sum involved is less than half the direct loss incurred during the years 1915-1916 through dependence on imported timber." I have thus referred to the position in Great Britain for the lesson seems wholesome, and one which this country, being in much the same position as Great Britain, can assimilate with advantage, especially when it is remembered that our timber has to come a distance of 6,000 miles, whereas Great Britain ha.> practically at its doors in Norway, Sweden, and France large supplies to draw on. The lack of an adequate timber supply has not been felt as acutely in the Union as in Great Britain, but there can be no doubt that the industrial expansion and general development of the country has been seriously handicapped by it. Before the outbreak of war the following were the prices of pine timber per cubic foot ; Deals, 2s. 3d.; flooring, lis.; ceiling, los. 6d. To-day they are: Deals, 9s. yd.; flooring, 24s. yd.; ceiling, 27s. Under the circumstances, it is not to be wondered that no building is being done which can possibly be avoided. The popu- lation is, however, increasing, and consequently the demand for houses is increasing. Rents have risen accordingly, and thus timber shortage has had a considerable influence on the increased cost of living. To take other examples: In 1914 sleepers for railway pur- poses cost 6s. 2d. each. To-day the Administration has to pay 9s. to los. Wood is required for the marketing and distribution of many articles produced m the country, such as fruit, cheese, jams, soap, candles, boots, dynamite, etc. The cost of the wood is reflected in the price of the articles, and so all through the community has to pay higher prices owing to the absence of an adequate South African timber supply. The Union is only on the threshold of its agricultural and industrial development, and in proportion as that expands so will the need for timber expand, for experience shows that increased consumption of timber goes hand in hand with the progress of a country. In 1910 Germany had over 54,000 square miles of forest, and yet imported 27 per cent, of her consumption ; France had 37,000 square miles, and imported 6 per cent. The shortage oif timber is felt now, but under similar circumstances in 50 or 100 years' time it would be felt still more. Though one sincerely hopes that war will not again recur, it is a possibility ; and, as the countries on which we now depend for wood may be involved^ PRESIDENTIAL ADDRESS SECTION C. 8 1 supplies may be entirely cut off, thus leading to complete or par- tial dislocation of industrial life. Apart from that aspect of the matter, there is the considera- tion that the world's consumption of timber is rapidly increasing, and prices have risen considerably in recent years. Between 1895 ^^<^ 1913 ^^6 increase in Great Britain amounted to 33 per cent. It would therefore seem only prudent that this country .should take steps to see that its future is provided for in this respect, and I think it may be of interest to this Association if the position of the Union in regard to forestry and timber supply is placed before it. During 191 3 — the last normal year— the Union imported over 15^ million cubic feet (15,617,000) of unmanufactured timber, valued at just short of one million pounds sterling £980,000). Over and above that £252,000 worth of manufactured timber was brought into the country, of which the cubic contents are not known, but which, at a conserv^ative estimate, may be placed at about two million feet. Thus the total timber .importa- tion in 1913, exclusive of furniture and one or two other items, was about 17 J^ million cubic feet, worth rather less than 1% million pounds sterling (£1,232.000). Of this amount nearly 90 per cent, was coniferous timber, that is to say, the soft timber derived from the class of trees known as pines, spruces, and firs. It may be of interest to note that Sweden furnished practi- cally half our requirements, Norway about i/5th, while the United States, Canada, and Russia were mainly responsible for the balance, in the order they are mentioned. I do not suppose the most pessimistic person would question that agricultural and industrial expansion during the next fifty years will be on such a scale that the timber requirements of the Union will be at least double what they are now. The estimate is certainly conservative, and a timber consumption of 35 million cubic feet per annum, of which 30.000.000 cubic feet will be pine timber, is a safe assumption. Now, what is the Union's present equipment to meet this probable demand? If reference is made to the last report of the Forest Depart- ment it will be seen that the total area of forest reserves on the 31st Alarch, 1917, was rather over 1.000,000 morgen, of which 747,000 morgen were classed as demarcated and 252,000 as un- demarcated. It might be as well to explain what is implied by the terms ' demarcated " and " undemarcated." " Demarcated forest " is any area, not necessarily wooded, of which the boun- daries have been defined, and which, after certain preliminaries into which it is unnecessary to enter now, has been declared by the Minister in the Gazette to be demarcated. Forest land once demarcated cannot be alienated without the consent of both Houses of Parliament, and the penalties for offences on such land are more drastic than in the case of undemarcated forests. All forest areas imder more intensive management, or which it is desirable to safeguard from alienations are, as far as possible, 82 PRESIDENTIAL ADDRESS- -SECTION C. demarcated. Demarcation is a useful weapon for the Depart- ment because it is not unusual for forest reserves to be " Naboth's vineyards " to the general public, and even to other Departments. " Undemarcated forest " embraces Crown land set aside as a forest reserve with the approval of the Minster of Lands, and, to quote the Forest Act in so far as the protection and utilisation of forest produce is concerned, includes — (I ) Outspans and commonages situate on Crown land, e.g., Burnshill Commonage, Frankfort Commonage ;. (2) Crown land on which forest produce exists, e.g., wooded Government farms in the Waterberg district ; (3) any other land of which the Crown retains a right to the trees, timber, and other forest produce. The Department's control over such undemarcated areas is much less complete than in the case of demarcated forests, and therefore when circumstances allow, and it is otherwise desirable, demarcation is efifected. One million morgen is a very large area, and certainly if it were all under forest the country would be in a sound position. Unfortunately, that is far from being the case. Large tracts consist of steep, rocky, mountainous country carrying few, if any, trees, and quite unsuitable for planting, either because the climatic conditions are unfavourable or because the country is too remote, inaccessible or broken. Examples of such reserves are the areas on the Zwartberg Mountain range in the Laings- burg, Prince Albert and Oudtshoorn districts, stretching from the BufTels River to the Willowmore and Uniondale boundaries, having an area of 109,497 morgen. It may be asked how these areas fall to be administered by the Forest Department. The answer is simple. The Irrigation Department for the past ten years has recommended that the Government should retain control of the mountain tops and sides in the catchment areas of the rivers of the country in the hope that ultimately it may be possible to check veld burning and maintain and encourage the growth of the natural vegetation, thus assisting to prevent erosion and flooding, and to conserve the flow of rivers and streams on which the country depends for irrigation. It was felt that if sold such mountain lands would fetch the most paltry sums, and later on, in the national interest, it might be necessary to acquire them again. The Forest Department had convenient machinery for locking uj) these lands by demarcation, and they were accordingly handed over to it. I am sorry to say circumstances have not, so far, allowed of much being done to realise the objects for which the reserv^es w^ere made, but when normal times return greater pro- gress may be possible. Coastal reserves and drift sands form a considerable percen- tage of the forest reserves (80,000 morgen) as the prevention, reclamation, and control of drift sands fall within the scope of the Forest Department's duties. Only in exceptional cases do these reserves carry a crop of wood, and when they do poles and PRESIDENTIAL ADDRESS — SECTION C. 83 firewood for local consumption are the principal products. Much of the reserves is grass veld, and all that is required is the regu- lation of grazing to maintain the surface cover and to avoid the exposure of the sand surface to the wind. In other cases, e.g., at Port Elizabeth, Bellville, Rerste River and Strandfontein, costly works have had to be undertaken to fix the sands. The reclamation work at Port Elizabeth took 20 years to carry out, and cost i6o,ooo. Another large tract of forest land, aggregating 100,000 morgen (83,000 morgen demarcated, 17,000 undeniarcated) is the Cedarberg, on which are found the Cedar forests. These forests hardly fill the popular conception of what a forest should be, for the trees composing them are sparsely scattered among the boulders of the precipitous mountain sides, and their flat, spreading tops do not meet and form canopy, so that heaths and other sour veld vegetation are free to flourish between them. In form the old Cedars, botanically known as Callitris arboreci, look exactly like the Cedars of North Africa (Ccdrus atlantica). which grow in a similar rocky country and within the snow belt. These Cedar forests have been carefully conserved and fire-protected 'for the past 25 years, and there is abundant natural regeneration. The trees grow to 60 feet in height and 5 feet in diameter. Un- fortunately, even old trees are very susceptible to damage from fire, and all over the mountains may be seen specimens from which the bark has been burnt long ago, but which, on account of the great durability of the wood, remain otherwise almost intact. The occurrence of this tree is interesting. It is only found on the Cedarberg, between 3.400 and 4,800 feet above the snow line, and is absent from the Winterhoek, where similar climatic conditions exist. Lister is inclined to believe that the difference in the geological formation between the two localities sufficientlv explains the distribution, but the general appearance of the sur- face soil in the two places is much the same. The timber which has a strong cedar odour is not of general economic importance, and is used locally principally for fence posts. In the past it was used for planking, and is still to a small extent, though the sale of timber is now entirely confined to dead trees. The out- put of this vast area during the year 1916-1917 was only 1,151 cubic feet. These reserves, extensive though they are. will never appreciably afi'ect the timber position in this country, though, if fire protection continues to be successful, they will greatly increase in value. C)wing, however, to the occurrence of Buchu on them, their conservation is meantime carried out with financial profit to the country. Thus a big percentage of the forest reserves consist of waste lands, most of which will never be of any value for afiforestation. What proportion is plantable is not known, for no close investi- gation or survey to ascertain this has vet been made. The matter, however, is not one of urgency, as there is at present sufficient accessible ground to occupy the attention of the Department. Of the large total of forest reserves, the area of dense indi- 84 PRESIDENTIAL ADDRESS —Sl'XTION C. genoits forest belonging to Government is only about 200,000 morgen, and besides that there are 35,000 morgen under planta- tions. There is probably 25,000-50,000 morgen of private forest. If the indigenous forest were as productive as a plantation, were accessible, and produced timber of a kind that could be generally used like imported pine, that area would suffice to meet our pre- sent needs as well as our requirements during the next fifty years, but that is far from being the case. The indigenous forests are found along the south and south- east coastal belt, and on the slopes of the mountain ranges falling within 100-150 miles of the sea, though in the Transvaal and in parts of Natal they penetrate further inland. They generally have a south or south-eastern aspect. In the Western Province, where there is a purely winter rainfall, the forests are small and detached, being mostly confined to sheltered kloofs, but as one travels east the forests become more frequent, and between George and Humansdorp the largest continuous stretch of forest in the Union is 'found. There the rain falls all through the year. In the Eastern Province, the Transkei, Natal and the Trans- vaal the rainfall is entirely a summer one, yet in general character the forest differs little from that found in the west. Some new species come in, and the percentage of each species present differs somewhat, but the variation is hardly so marked as might be expected, considering the forests range from 34° S. Latitude to the Tropics in 23° S. Latitude. The indigenous forest is essentially a mixed forest, that is to say, it consists of a large number of species growing together, the composition oi the mixture varying according to the district, elevation, soil and climate. Some species seem to appear in the forests almost wherever forests occur ; such are Beukenhout {Rapanca melanophelos) and Vlier {Nuxia florihunda). Others, again, are less accommodating. Keur {Virgilia capensis) con- fines itself to the coastal area from the Cape to Port Elizabeth, and seems to avoid the summer rainfall zone. Kamassi (Gonioma kamassi) is abundant in the Knysna forests, and is found occa- sionally along the coast as far as East London. It does not. however, occur in the Transkei, Natal, nor, I believe, in the Transvaal. It is reported, however, to occur in Rhodesia. The true South African Box (Buxus macozmni) is absent from the Knysna forests, but is fairly abundant at Alexandria and near East London, and in one or two Transkeian forests. Else- where it is missing. Stinkwood (Ocofea bullata) occurs in the Cape Peninsula. Knysna, Transkeian, Natal and Transvaal forests, but seems most vigorous in Knysna. In the Eastern Province it is practically missing from the forests, though when the Pirie forests were recently worked an isolated group of fine Stinkwood was discovered. Though Stinkwood and Sneezewood (Ptaeroxylon utile) refuse to meet at Knysna, and hardly know one another in the Eastern Province, they grow to great perfec- tion side by side in the Transkeian forests along with Yellows- wood. The Yellowwoods {Podooarpus thunhcrgii and P. elun- gata) are foimd to a greater or less extent in the larger proper- PRESIDENTIAL ADDRESS — SECTION C. 85 tion of the dense forests, but the Falcate Yellow wood (P. falcata) is peculiar to Pondoland and Natal. The distribution and occurrence of our forest trees is a most interesting study, and one which has been little touched on as yet. The field is a wide one, and should afiford plenty of scope for investigation to members of the increasing band of botanists now in the Union. The forests are managed under what is known as the " Selec- tion System." Generally in this country one notices pine and gum plantations are clean felled, and are either regenerated by planting or from seed on the ground or from coppice shoots. In the indigenous forests under Government control, on the other hand, clean felling is avoided and only the mature, over- mature and depreciating trees, or trees which for sylvicultural reasons should be felled are removed, and their place is taken in time either by self-sown seedlings or coppice growth. A forest worked under this method looks to a layman viewing it from outside as if it had not been worked. Trees of all ages, from one year old to the oldest, are constantly represented over the whole area and, theoretically, the work of selecting trees for cutting extends at all times over the whole forest. In practice, however, the forest is divided into series, and further into sec- tions, which are gone over in turn, so that cutting returns to the same section after 40 years. Systematic management was introduced into the Cape forests in 1883 by a French forester, the Comte de Vasselot de Regne, whose services were obtained for that purpose by the Govern- ment. The broad principles he laid down were sound, but his ideals have scarcely been attained for various reasons. The data on which he worked were necessarily of the sketchiest nature, the forests were in a highly abnormal condition, and trees, which in the interest of the forests should have been removed, were unsaleable, and left to encumber the ground and prevent the re- growth of a better crop. It will take a very long time before the forests reach a nor- mal state, and, meantime, the urgent need is a careful study of the sylvicultural requirements of the different species compris- ing the forest, for without more knowledge than is at present available, progress in forest management is not hkely to be rapid or sure. In Natal till Union there was never a settled forest policy, and the forests were worked spasmodically without much system. In the Transvaal before the Boer War there was little attempt at control or conservation, and most accessible forests were worked out. Since then most of the forests have been closed. Of all the species of trees in the indigenous forest the only ones that produce timber that can be regarded as a substitute for imported pine time are the Yellowwoods. The Yellowwoods attain large dimensions, the largest of any trees in the forest. There are three kinds — the Real, the Bastard, and the Falcate. The Real Yellowwood grows 80 to 100 feet in height, and occasionally to 7 feet in diameter. The 86 PRESIDENTIAL ADDRESS SECTION C. Bastard grows even larger. It will reach ,80 to 120 feet in height and a diameter of 9 feet, with a clear trunk of 40 to 80 feet ; but more usually the diameter does not exceed 3 to 4 feet. Yellowwood timber is rather harder and heavier than Pine, but is much stronger and greatly superior in appearance, and is comparatively free of the heavy knots found in most imported wood. Apart from that it is excellent for beams, rafters, tiooring, and ceiling. The beams, floors, ceilings, and doors of many of the old homesteads at the Cape are of Yelloww^ood. Yellowwood creosotes well, and it has been largely used on the South African Railways for sleepers, close on 3,000,000 having been supplied from Knysna during the past 30 years. Generally speaking, the other kinds of timber are only suitable for special purposes, such as furniture-making and wagon-building. Some, such as Stink- wood, White Els, Red Els. and Beukenhout, are of great beauty. Stinkwood is well-known throughout the country as a furniture wood, and it is also valued for wagon construction. Though it has been used for planks and beams it is too valuable and scarce for such work. It is fortunately one of the quicker-growing species, and the re-growth in the Knysna forests is good. Sound trees are, however, rare. It will grow 3 to 5 feet in diameter, and 60 to 90 feet high. Assegai, White Pear, and Ironwood are greatly sought after by wheelwrights, and of late years Iron- wood has found a ready market on the Rand for stamp blocks. Sneezewood is very hard, heavy, strong and durable. It is much appreciated by engineers for bridge-building, but large- sized timber is now scarce. It grows 50 feet in height and 2 in diameter. It is chiefly used as a fence pole, and the tree is split or sawn up into suitable dimensions for the purpose. But all these trees have limited use compared with Yellow- wood, and, as I said before, that is the only kind which can be used in place of imported deals. In most of the forests in which it occurs Yellowwood preponderates, and is readily pur- chased where facilities for cutting and marketing exist. .\t Knysna during 1916-1917 52 per cent, by volume and 30 per cent. of the total output of 336.000 cubic feet was Yellowwood, and during the same period, when the total output of all the Govern- ment indigenous forests was approximately one and a half million cubic feet, over 600,000 cubic feet was Yellowwood. In the Eastern Province, the Transkei. and Natal 40 to 75 per cent. of the exploitable unworked forest is of this species. As the result of the roughest of calculations — data on which to base a reliable estimate being absent — I should say that possibly all the forests of the Union — demarcated and undemar- cated and private — together contain about 75,000,000 cubic feet of Yellowwood of exploitable size, or ju.st about five times as much as the annual importation of softwood in 1913. The esti- mate, I believe, to be a liberal one, but it serves to show how restricted the timber resources of the Union are. Under present conditions it would not be a ct>mmercial proposition to place one- third of that timber on the markets of the Union, even if from a sylvicultural point of view it were permissible ; for many of the PRESIDENTIAL ADDRESS SFATION C. 87 forests are far removed from road and rail or carry but a few- trees to the acre, or for social reasons it is inexpedient to accelerate their exploitation. As the country opens up, more forests will be tapped, but at present many are of purely local value. To meet the existing shortage of wood the Department has placed more than the normal supply of Yellowwood on the market, and, should circumstances warrant, still more will be done in that direction. The stock of timber referred to is the accumulation of centuries, and if it could be removed it would take genera- tions to replace. In considering how far the indigenous forests can go towards meeting our timber requirements when once they are in a normal condition, it is important to arrive at ?;ome idea of the rate at which the forests produce Yellowwood timber. I regret to have to admit our information on this point is scanty, for investigations on this and kindred matters have received very little attention. However, McNaughton. who for many years was Conser- vator at Knysna, made some careful computations during the course of preparing a working plan for the Sourflats forests. He arrived at the conclusion that on an acre of forest of first-class quality the annual increment of all s]>ecies amounted to approxi- mately 31 cubic feet. Of this 31 cubic feet 21 cubic feet were made up of valuable species, mainly the two Yellowwoods, Stinkwood, Assegai, White Pear, Iron wood, Kamassi, and a few others of less importance, and the balance of 10 cubic feet, of inferior species, unsaleable for industrial purposes, and useful only for fuel. The two Yellowwoods contributed .3 of the increment of the valuable species, or 6.3 cubic feet per acre per annum. These figures are probably not very wide of the mark. Now. adopting that figure it will be seen that, if all the forests of the Union were of equally good quality as the Sour- flats forest, and every year only the amount of timber were felled that was produced, the annual out-turn of Yellowwood would reach 6.3 X 400.000=2,520,000 per annum. It must, however, be remembered that a certain projxvrtion of the dense forests of the Union are devoid of Yellowwood, are inaccessible, and that much Yellowwood forest is inferior to Sourflats. Under those circumstances it is probably not safe to assume that a greater output than one and a quarter of a million cubic feet of Yellowwood per annum could be looked for, when once the forests have been brought into a normal condition, a process which will take a very long time. No doubt as further experience is gained of the native forests and more intensive management becomes feasible, the total annual increment might be consider- ably enhanced ; so that a somewhat greater supply of Yellowwood would be forthcoming, especially if steps were taken to foster the better species. But even under the most favourable circum- stances, it is quite clear that the outptit of the indigenous forests of the Union are entirely inadequate to provide much more than 5 per cent, of the probable future requirements of the country for- softwood timber, and softwood timber, as I pointed out before, comprises 90 per cent, of the timber consumption ob PRESIDENTIAL ADDRESS SECTION C. of the Union. If the Union is not to continue importing timber for ever, and to remain dependent on other countries for its sup- plies, it must form adequate artificial forests. There is no other remedy. The Forest Department has realised this position for many years, and the matter was prominently brought to the public notice by Hutchins when he was Conserv^ator at the Cape between 1896 and 1906. The subject was then regarded as the meritorious fad of a few enthusiasts, but of late years the pro- paganda work of the Comte \'asselot de Regne. Lister, Hutchins. McNaughton, and other pioneers has begun to bear fruit, and is reflected in the better provision made by Parliament nowadays for afiforestation. It will no doubt be suggested by some that, as South Africa is so poorly wooded naturally, it would seem risky, to say the least of it, to embark on afforestation. If the country were adapted for the growth the trees would have been there. Luckily it is jx>ssible to meet this theory with facts. Exotic trees producing softwood of the kind this country requires are, and have been, grown in plantation form to maturity or to com- mercial size under varying conditions. Why it is that large tracts which are capable of aft'orestation with exotic trees are devoid of natural forest is a matter for speculation, and one for which it is difficult to find a satisfactory solution. I know of many places in the Cape Province where the Cluster pine, as long as fires are excluded, spreads itself vigorously and matures, yet on the same ground there is no vestige of a native forest ex- cept in the deep kloofs, nor has there ever been any since the first Dutch settlers arrived in the country. These are places. tot>, where there is a heavy regular seasonal rainfall. I have in mind the valley of the Berg River, Genadentlal and the Cape Peninsula. Other people maintain that if plantations are required they should be composed of native trees, as native trees having grown for centuries in South Africa must be better suited to its climatic conditions. This attitude seems entirely reasonable, but what I have just stated rather disposes of it. Native trees, at least nf the more valuable kinds, such as Yellowwood. seem to require a certain degree of shade and shelter, at any rate in early youth, to establish themselves, and as this is generally almo.st entirely absent on the class of land that has to be planted, they cannot well be used for afforestation. Planted on bare hillsides exposed to the full effect of sun and wind they would, if they lived, make such slow progress that the cost of cleaning and cultivation would remove any prospect of them proving a profitable crop. In selected sheltered bottom lands it is no doubt possible to raise small groves successfully, but for general commercial afforesta- tion native trees must be ruled out. It being admitted that it is possible to grow in this country a large proportion of the timber now imported or of timber to replace it. it remains to inquire what area should be afforested to carry this object into effect, and what has so far been done in that direction in the past, and what it is planned lo do in the future. I'RKSIDKNJ lAI. ADDRESS SECTION C. St) Before going further it might be as well to explain that cer- tain classes of timber will always have to be imported, for they cannot be grown in South Africa. Such kinds are Teak, Mahogany. Ash, Hickory, and Walnut. Pitch Pine may also have to come from abroad, though experimental plantings of this species seem to indicate that it may be possible to cultivate it in some parts of the Union with success. These kinds, however, form only a small percentage of the total imports, and do not materially aifect the general question of growing our own tim1)er su])plies. I previously estimated that the annual consumption of timber in the Union in 50 years' time will be 35,000,000 feet. Now, an acre of pine plantation can be expected to produce 100 cubic feet of timber per annum. Measurements taken in this country show that that amount is often exceeded, e.g., the yearly increment of a stand of P'mus itisignis 29 years old at Tokai was 275 cubic feet, and of a 30 year old stand of Cluster Pine also at Tokai was 157 cubic feet, but to be on the safe side, and taking good and bad stands together, 100 cubic feet per acre seems to be a safe figure to adopt. If it is assumed that five out of the 35,000.000 feet of timber is made up of hardwoods and other kinds that cannot be grown in South Africa, it will be necessary to plant about 300,000 acres to produce the balance. Up to the present the total area afiforested by Government is, in round numbers, 70,000 acres, of which 21,000 belong to the Railway Administration. Of the 70.000 acres a considerable proportion cannot be regarded as of a nature that will serve to meet the general timber requirements of the country. For in- stance, the bulk of the plantations in the Transkei, amounting to over 7,000 acres, consist mainly of Wattles and Eucalypts grown especially to meet native wants, and to relieve the strain on the indigenous forests. Again, the jjlantations in connection with the drift sands at Port Elizabeth, aggregating 5,000 acres, are only useful as fuel reserves. Other plantations, such as some of those in the Transvaal and the Free State, will serve to pro- vide only local needs for fuel, poles, and rough farm material for which, owing to the treeless character of the country, a good demand exists. A considerable area of plantations in all the Provinces has been experimental, and there have naturally been failures, and the result.s, as far as timber production is concerned, can be disregarded. If due allowance is made for all these circumstances, and deducting the land under hardwood plantations, the area r- tance of a softwood timber su])ply, it should not be overlooked that the consumption of hardwoods is hkely to reach considerable proportions. Hardwoods are used largely in railway work, especially for sleepers. The length of railway now open is 90 PRESIDENTIAL ADDRESS SECTION C. 9.500 miles. That will probably be doubled in 50 years, so that if there is a sleeper to every yard, a mile of track will contain 4,400 cubic feet; and the railway system of 19,000 miles, 19,00 X 4400 = 83,600,000 cubic feet If the sleepers were all hardwood, and renewed every 15 years, the annual consumption of timber per niile would be 293 cubic feet, and for the whole system 5,567.000 cubic feet. Assum- ing that a Eucalypt plantation yields 200 cubic feet per acre per annum (and measurements show that this is a reasonable figure) the Railway Administration would require 27,834 acres of plan- tation to meet their requirements for sleepers alone. Hardwoods are used for many other purposes besides sleepers, and therefore their cultivation should not be neglected. Probably the Union will be able to absorb in 50 years' time the product of 50,000 acres. The Cape Province was the pioneer in plantation work in South Africa. The first Government plantation was started by Lister at Worcester in 1876, and consisted of Blue Gum (Eucalyptus globulus). The plantation, 72 acres in extent, was grown under irrigation, and it was formed with the idea of pro- viding fuel for locomotives. It was. however, sold in 1892-1895 to De Beers for mine timber, and yielded a profit of £4,338 (ex- clusive of interest charges). The re-growth was sold during 1916 and 1917, and the plantation finally disposed oif to the Municipality, the second rotation having yielded a nett return of £2 I OS. per acre per annum. Encouraged by the success at Worcester, plantations on a larger scale were started in 1883 ^^ Concordia, Knysna, in 1884 at Tokai and Kluitjes Kraal, and in 1889 at Fort Cunynghame in ihe Eastern Province. Different kinds of trees from all over the world were tested at these cen- tres, as well as difl:"erent methods of sylviculture. Little was known then of many of the trees experimented with, and infor- mation on the subject in the absence of adequate literature was difficult to procure. Sylvicultural practice which had proved to be successful in other countries was found by bitter experience to fail here, e.g. in 1884 it was considered unnecessary to kill ofif the natural veld as a preparation for planting. The conse- quence was the young trees died wholesale, and it was only when the approved European method was jettisoned that success re- sulted. Planting espacements were often wide, 20 feet apart each way, but there is evidence in the shape of underplantings in some of the old stands of trees that the foresters of those days early realised their mistake. Among the trees planted was Pinus insignis. There was a specimen of it growing in the Gardens at Cape Town, and the Conservator (Lister), attracted by its appearance, thought he would test it on the slopes of Tokai. He did so, and the trees then planted succeeded so well that it was possible recently to arrange for their sale. Many of the trees are now over 100 feet in height and 2 feet 6 inches in diameter. South Africa owes a great debt of gratitude to these pioneers of forestry — Harison. Comte Vasselot de Regne. Hutchins, Lister. PRESIDENTIAL ADDRESS SECTION C. 9^ and Heywood — who, in spite of lack of funds, of adverse criti- cism, failures and want of encouragement, quietly and unobtru- sively added an acre here and an acre there, and paved the way for forest extension on a large scale. The Stone and Cluster Pines had been naturalised in the Western I-'rovince before the Government plantations were started, but those valuable species the Canary Island and Ingisnis Pines were practically tmknown. Many different kinds of Eucalypts were experimented with, and as experience was gained it became possible to discard some and fit others into the zones best suited to their requirements. Eucalyptus corynocalyx, the Sugar Gum. R. diver skolor, the Karri, and E. rostrata, the Red Gum. were useful introductions of that period. E. marginata, the Jarrah, was also tested, but the results have no't proved sufficiently satisfactory to warrant ex- tended cultivation. Prior to the Forest Department taking up the trial of the then unfamiliar species the Blue Gum was prac- tically the only Eucalypt cultivated in the Union, and many fine specimens can be seen at homesteads all through the country, its popularity being greatly enhanced by its rapid growth and general hardiness. The work of the past 40 years has made it possible to decide at least for the winter and all-the-year-round rainfall areas of the Cape Province, which species of trees, particularly conifers, are mo.st suitable to grow, and to allocate to such species within certain limits the conditions needed for their best development. A great deal has still to be learned about these exotics, but enough is kno\\'n about their requirements to justify them being planted on a large scale in the areas referred to. In the summer rainfall areas of the Eastern Province and the Transkei the situation is not so clearly defined, and there is some element of risk in extension which is absent in the west. Greater care is called for in choice of species and of sites for planting, and until some of the plantations reach maturity this will remain the position. On the other hand, planting is mainly confined to the natural forest zone, where conditions can be expected to to be favourable, and results so far attained indicate that certain species can be counted on to reach a commercial size, if not large dimensions. The Cluster Pine and Insignis Pine, which are so at home in the winter and all-the-year-round rainfall zones, though they do well in favoured spots, are prone to disease, and their place in the Eastern Province mountains would seem to be taken by the Chir Pine {Piniis longifolia) from India, and perhaps by the Canary Island Pine. Some Mexican species are now under trial, but are too young to give any reliable indication of their possible future value. The Portuguese Cypress and, in parts, the Deodar, flourish on the mountains, and in the kloofs the common Oalc and the White Poplar grow remarkably. Certain Eucalypts appear much at home, and magnificent groves of Blue Gum of 120 feet in height serve to show what may be expected of younger plantations. 92 PRESIDENTIAL ADDRESS SECTION C. In the Cape Province commercial afforestation propositions are confined to the coast and coastal mountains in the natural forest zone, though trees and small plantations to provide for local needs can be grown in selected places in all but the most arid parts. In Natal forestry under Government auspices has had a chequered career. A most excellent forest policy was laid down in 1889 by H. G. Fourcade in a careful report, but unfortunate! after a feeble attempt to put it into practice under a German forest officer it was abandoned. After the Boer War the sub- ject was again taken up, and steps taken to conserve what was left of the indigenous forests ; further, plantations were started at Cedara, Empangeni, and on a smaller scale at other centres. During the period of retrenchment in 1907 the young Depart- ment which had sprung up was seriously affected, and till Union and some time after progress was slow. Even now the total area of Government plantation in Natal and Zululand is only a little over 2,500 acres, but this is being regularly added to. As is well known, there is no Province in the Union where more tree planting has been done by private enterprise than in Natal, and this probably explains why so little has been accomplished in this direction by past Governments. There are about 250,000 acres of wattle plantation in Natal, and on many farms are to be seen fine plantations and collection of exotic trees. The planting of hardwoods has been and is most in favour, and the Rand has reason to be thankful that so much was done in this way in former years, for Natal has been a fruitful source of supply for the timber it requires. Pines, generally speaking, have given disappointing results. Possibly this is due to wrong kinds having been planted. The species most favoured have been Pinus insignis and P. pinaster, but it is doubtful if these are climatically suited to Natal condi- tions any more than they are to the summer rainfall areas of the Eastern Province and the Transvaal. It is likely more satis- factory results will be obtained from other kinds, such as Pinus longifolia, the Chir Pine, on the hills av/ay froiii the coast, and from species such as P. mistralis, P. tacda, and P. mitls, both on the coast and the hills. Specimens of some of these pines are thriving in Natal, but records of trials that may have failed are unfortunately lacking. Natal is likely to become highly industriahsed in time, and the need for softwood timber will be strongly felt, and this pK)int must be kept in view in determining the future policy of the Department, and an effort made to extend the planting of Conifers. Before the Boer War Government afforestation in the Transvaal was confined to one Eucalypt plantation near Pretoria, which was planted by contract in 1896. After the war Govern- ment plantations ancl nurseries were started in various parts of the Province, and since the capabilities of the country for affores- tation were so little known much work of an experimental nature PRESIDENTIAL ADDRESS — SECTION C. 93 was undertaken. In 1903 the Government of the day secured the services of D. E. Hutchins to report on forestry in the Trans- vaal. Hutchins found the mistake made in the Eastern Province and Natal being- repeated, and that in spite of the difference in climatic conditions the same trees were being planted in the Transvaal as in the Cape. He recommended a radical change in policy, and urged, among other things, that the Transvaal should draw on the rich forest flora of Mexico for its trees, as Mexico, of all countries in the world, most resembled the Transvaal in climate. This policy was adopted, but great difficulty has all along been experienced in obtaining the required seeds on account of the chronically disturbed state of Mexico and subse- qently the war. The first importations were made in 1907. To obtain these seeds it was necessary to send a collector specially from the United States. The expedition was satisfactory, and led to the introduction into the Union of two Pines from Northern Mexico — Pinits arizonica and P. cngelmanni or. as it is perhaps more correctly named, P. macrophylla. The results have so far amply justified Hutchin's predictions. These species are being tested often imder very adverse conditions alongside the species that have hitherto been grown in the country, and in every case are more reliable in growth and hardiness. It may be of interest to give here some particulars of their growth under plantation conditions. Locality. Espace- ment in Feet. Age in Years Height in Feet. Diameter Breast Height in Inches. Pinus arizonica. Belfast Arboretum... 4x4 9 17 5-4 Jessievale ,, 4x4 10 20 43 Ermelo ,, 4x4 10 20 4-8 Pinus engehnanni (syn. macrophylla). Belfast Arboretum.., 4x4 9 15 4.4 Jessievale ,, 4x4 10 15 40 Ermelo ,, 4x4 10 16 4-3 About the same time some Pinus montezitmce transplants were raised, and a year later some P. leiophylla. Then followed some P. montezumcc var. hartzvegli, P. montezunKe var. lindleyi, P. patula, P. teocote, P. lumholtsii, P. hnvsoni, P. oocarpa var. 94 PRESIDENTIAL ADDRESS SECTION C. microphylla, P. chihuahuana, P. pseudostrobus van tenui'foHa Siud pseudostrobus. To give an idea of the growth of some of these have made I give a ifew further figures. Locality. Espace- ment in Feet. Age in Years. Height in Feet. Diameter Breast Height in Inches. Pinus leiophylla. Belfast Arboretum... 4x4 9 24 6-3 Jessievale „ 4x4 8 22 4-8 Woodbush ,, ? 8 23 45 Pinus iHontezumce. Belfast Arboretum... 4x4 6^ 16 40 Jessievale „ 4x4 8 22 49 Woodbush ,, ? 10 20 50 Pinus pntula. Belfast Arboretum .. 4x4 5i 16 3-3 Jessievale ,, 4x4 6 14 4-0 Woodbush ,, ? 4 16 2-5 Some of the Mexican Cypresses, such as Cupressus benthami and C. lindleyi, were also obtained, and two kinds of Oak (one Quercus reticulata, the other unnamed), and Juglans rupestris, a Walnut. Hutchins also advocated the cuhivation of some Indian species, particularly Deodars and Pinus longifolh, and, as far as circumstances have permitted, these have been given trial. From what I have said it will be gathered that afiforestation in the Transvaal is not, and cannot in the nature of things be, in such an advanced state as in the oldest Province of the Union, and that it will take years before it will be possible to assign with certainty to each of the various types of country the tree or trees best suited to it. I would lay stress on this point for many strenuous advocates of afforestation lose sight of it and think that planting can proceed on a wholesale scale without risk of failure, which is far from being the case. If it were not for the fortunate circumstance that timber even of comparatively small dimensions is saleable for mining and otlier purposes it PRESIDENTIAL ADDRESS SECTION C. 95 would be a question whether an even more cautious poHcy than is now in vogue should no't be adopted. Hutchins's recommendations, however, have been amply justi- fied as far as it is possible to judge at present, and if it were feasible to obtain seed of the kinds that have done best, the Department, through its nurseries, would encourage their culti- vation. Till the war is over nothing can be done in this direc- tion, and even then much will depend on how Mexico settles down. Even in the ten years the Department has been dealing with these species a a good deal has been learnt about their sylvi- cal characters, and in the next twenty it should be possible to use them with considerable assurance. -By that time it should be possible to get seed locally, and thus the progress of afforestation in the Northern portion of the Union would receive an impetus such as is at present impossible. Just as in the Cape Province the Cluster and Insignis Pines have acclimatised themselves, so in due course I anticipate that some of the Mexican Pines, such as Pinus arisonica,, P. montesmncc, and P. nvacrophylla, together with P. longifoUa from India will take hold in the Transvaal. In the Transvaal, as in Natal, the cultivation of hardwoods is more advanced than that of Conifers. Certain areas of the Transvaal, such as the warm, moist Eastern slopes of the Drakensberg, grow Eucalypts of the best timber-producing varie- ties excellently, and in most parts a Eucalypt of some kind or other can be, cultivated for mining purposes. But the coal fields of the Transvaal cannot be divorced from industries and, indus- tries require coniferous timber, and, as in Natal, the Department has to keep this point in view in shaping its policy. The Trans- vaal is an inland country, and therefore its need for a local timber supply is more important even than it is for the coastal Pro- vinces. The extent of Government plantations in the Transvaal is 7,600 acres. In the Free State 'before the Boer War there was no organ- ized forest work. Shortly after the Government test plantations and nurseries were opened at various central places. Generally speaking, the conditions in the Free State for afforestation are unfavourable, but good work was done by Carlson, the Cape Forest Officer appointed to take charge of afforestation, in spite of many difficulties and much discourage- ment in ascertaining the most suitable species to plant under different circumstances and the best methods to employ. The success of some of the plantations, particularly the one at Har- rismith, has been remarkable, and the object lesson afforded by Government plantations has undoubtedly led to increased plant- ing by the general public, which is one of the principal objects the Department has in view, especially in that Province, for other portions of the Union are more favourably situated for afforesta- tion on commercial lines. Millions of young trees have been distributed from the Government nurseries in the Free State (and for that matter in the Transvaal) during the past 15 years, and anyone familiar with these Provinces after the Boer War 96 PRESIDENTIAL ADDRESS — SECTION C. and now must remark the advance that has been made. Some of the species now under trial in the Transvaal are also being tested in the Free State, and it is possible some of them will ultimately turn out to be valuable introductions. As the farms in the Free State become reduced in size, tree- planting will become more general, and the movement that has been taking place in the past 15 years may be expected to become intensified. Now as to 'the steps which are being taken to provide for the future timber requirements of the Union: during 1915-16 and 191 6- 1 7 the areas afforested were 2,384 and 2,655 acres, respectively. At that rate of progress it would take more than 100 years before the acreage which I have estimated would be required to replace our present importations would be planted. The Government, appreciating the position, decided during last Session of Parliament to provide money on the loan estimates (^50.000) to permit of a programme of extension being em- barked on. This has now been initiated. In deciding on the localities at which to commence operations the factors taken into consideration have been suitability of soil and climate for the species to be grown and reasonable accessibility to rail or port. The places at which Government has sanctioned operations being started are : — Name of Area. District. Area available for Afforestation. Acres. Funds to be expended during 1918-19. £ Tollberg and 1 Geelhoutboomberg ) George ... 6,000 3,000 Groenkop ,, ... 10,000 3,000 Buffels Nek Knysna ... 8,000 3,500 Farleigh )) • • • 2,000 3,500 Witte Els Bosch ... Humansdorp 12,000 7,000 Hankey >) 24,000 7,000 Isidenge Stutterheim Total 2,000 3,000 64,000 In addition to these, schemes for Natal and the Transvaal ■are still under consideration. PRESIDENTIAL ADDRESS — SECTION C. 97 It may be thought that it would be advisable to push on with one or two schemes and finish them rather than scatter opera- tions over several centres, but there would be obvious difficulties in concentrating all the labour required at one or two centres and in arranging for ploughing by contract and departmentally. It will be noted that all the schemes now sanctioned except one are in districts bordering the South Coast, where rain falls all the year round. The plantation sites are on the southern slopes of the mountain ranges. The labour employed on the work will be mainly white. The principal species to be grown in the plantations will be Piiins iiisiguis. P. pinaster and P. canariensis. Pliu's insigfiis^ the Insignis Pine, is a rapid grower, and produces a greater volume of wood per acre per annum than any other pine. From 12 to 15 years it is large enough to yield boxwood, and at 30 years it reaches a height of 100 feet with a diameter of from 18 to 24 inches. The total yield of two stands of 29 years of age at Tokai were 7,972 and 7,721 cubic feet per acre, which shows a mean annual increment per acre of 275 and 266 cubic feet. The gross money yields were in 19s. 7d. and £10 9s. lod. per acre per annum, respectively, the timber being sold standing. The costs of formation and tending are not known, but even granting these amounted to a high figure, such as £20. and reckoning compound interest at 4 per cent., a rough calculation will show the credit balance is still large. The sales, of course, took place under war conditions, but, even allowing for that, a good margin of profit could be counted on, especially as nowadays planting is not likely to^ exceed £io-£i2 per acre, and more satisfactory crops could be obtained. At 40 years of age a fully-stocked wood of Insignis Pine on good soil should yield 10.000-12,000 cubic feet of timber per acre. The wood of Phius insignis is not strong or durable in con- tact with the ground. It is practically free from resin, and being tough, is useful for fruit-boxes. It is also' a good wood for match-boarding, ceilings, joinery, packing-cases, and generally for any purposes where strength and durability are not required. Pin us pinaster, the Cluster Pine, is a hardy species. Its timber is useful for flooring, rafters, joists and general car- pentry. It is rather resinous for fruit-boxes, but is excellent for packing-cases. When creosoted it makes a good sleeper. Pinus canariensis, the Canary Island Pine, produces a hard and durable pine timber. It grows faster than Cluster Pine, but slower than P. insignis. The wood works well and has a nice grain. It is a good timber for building and constructional pur- poses generally. To break up the masses of Pines into sub-compartments and protect the boundaries against fire, deciduous trees like Oaks and Poplars, as well as Blackwoods and some Eucalypts will be planted according to the nature of the soil. At Isidenge. Canary Island Pine and Chir Pine will be the 98 PRESIDENTIAL ADDRESS SECTION C. species mainly used. The kloofs will be planted with Oak and Poplars. Tollberg and Groenkop are within ten miles of the George- Mossel Bay Railway. Buffels Nek is five miles from the term- inus of the South- Western Railway leading^ to the port of Knysna, from which it will be possible to distribute wood to Durban. East London, Port Elizabeth and Capetown, should the railway at George not be extended to Knysna in 50 years' time, which however, is unthinkable. Farleigh lies about 12 miles by road from Knysna, but the extension of the railway to Knysna would reduce road transport by about two-thirds. Witte Els Bosch is at present 18 miles >from the railway at Assegai Bosch, from which extension can in due course be expected. The afforesta- tion contemplated there, if persevered with, would of itself largely justify construction. The Hankey area is served by the narrow gauge railway running from Port Elizabeth to Loerie River. Isidenge is about 14 miles from the main Eastern line, but the road communica- tions are good, and bearing in mind the prospect of the develop- ment of mechanical transport, it is not thought the distance is excessive. From Revenue funds two other large schemes have been inaugurated during the last two years, both in connection with the employment of poor whites. One is at French Hoek, in the valley of the Berg River, and the other at Jonkersberg, on the southern slopes of the Outeniquas. The latter adjoins on its eastern boundary Tollberg and Geelhoutboomberg, so that when the two schemes are complete there will be a continuous stretch of artificial forest on the southern slopes of the Outeniquas, from Brak River in the west, to Montague Pass in the east, a di.stance of at least 20 miles. The scheme of afiforestation here and at F'rench Hoek will be on the same lines as those already men- tioned, the same species of trees being employed. The area of plantable ground at French Hoek has not yet been accurately determined, but is likely to amount to 5,000 acres. When in addition to the work now being done all these schemes are fairly launched, it should be possible to advance at the rate of 8,000-10,000 acres per annum as long as funds are forthcoming. In the course of this address I have endeavoured to place before you the salient features of the position in regard to timber supplies and forestry in the Union. The position is one that calls for earnest consideration by all who take an interest in the welfare of this country. While the forest reserves in the Union amount to a respectable total, the actual area of forest capable of producing timber suitable for general use is very restricted, and the best possible annual output that can be looked for is almost negligble in comparison with the country's needs. Unless, therefore afforestation is seriously tackled, this country, like Great Britain, will always have to depend on the favour of other countries for its timber supplies. Apart from PRESIDENTIAL ADDRESS SECTION C. 99 the ({uestion of (ler..;ice, that is a state of affairs which is aUo- gether unsound and to be avoided. In spite of the more exten- sive use of iron, steel and concrete in recent years, the amount of timber used throughout the world is rapidly increasing without any corresponding increase in the forest area. South Africa, unless it augments its own timber resources — and that it can and should do^ — will have to look forward to competing with countries more favourably situated geographi- cally for some of the world's surplus timber, and will be forced to buy, whatever the price, or else helplessly have to see its industries strangled or paralyzed for lack of an adequate local supply of this prime essential of industry. In this connection it is interesting to recall, especially in this golden city, what Evelyn. the famous English forester, wrote more than 250 years ago. Referring, of course, to England, he said: *' Since it is certain and demonstrable that all arts and artisans whatsoever must fail and cease if there were no timber and wood in a nation (for he that shall take his pen and begin to set down what art. mystery or trade belonging any way to human life could be maintained and exercised without wood will quickly find I speak no paradox), I say when this shall be well considered, it will appear that we had better be without gold than without timber." Bearing in mind what the position is in regard to this vital question, it is a matter for satisfaction that a strong forward move has now been initiated in aft'orestation. The country, if it is wise, will see that the move is continued. Section D.— ZOOLOGY, PHYSIOLOGY, HYGIENE, AND SANITARY SCIENCE. President of the Section: Prof. E. J. Goddakd, B.A., D.Sc. THURSDAY, JULY ii. The President delivered the following address : — To decide on a special topic for a IVesidential Address, which, despite its specialised character, would appeal to all is a difficult matter, and in attempting to discover such a topic I was led to see that this occasion demanded really a survey of the status of Zoology and the means obtaining in this country for the development of the various branches of zoological research. The fact that the Zoological Section makes its debut at this meeting of the Association has guided me in this direction, particularly so since the conditions obtaining in the world at the present day have stimulated interest in researches whose economic value and importance is patent to all, and even in such as in many cases were hardly appreciated in pre-war days. This sudden realisation, or rather appreciation, of the fact that there is a direct relationship between Pure and Applied Science, may, in its embryonic phase and its youthful lack of perspective, lose sight of the fact that this apparent discovery is just what the pure scientist has been attempting for years to unravel before the eyes of the modern world, hungering for that appreciation which was his due, and for that encouragement which our Governments have been loath to give. Already we find a Technical and Scien- tific Connnission in existence in this country, and we should seize the occasion to point out that such a Commission (which is cog- nisant of the value of scientific research in general), while bound to suggest and open lines of research which will lead to greater production within this country, is equally strongly bound to encourage scientific research even where the object in view may be of so abstract a nature that the mind of the modern commer- cialist can perceive no direct economic return therefrom. For, after all, the value of the work of any such Commission will be measured, not by this generation alone, and not by the actual number of lines of research which it has opened, but rather by the extent to which it has itself encouraged and led our governing bodies to develop the spirit of research — be it concerned with afifairs patently of economic importance or apparently abstract or abstruse. The extent to which they succeed in this will be a true measure of their work, for it will be a measure of the ability of the country in future to deal with fosterings not yet patent to us, but which must continually arise de novo. It seems to me that this is the outstanding defect throughout the British Empire, namely, that we have continually dififerentiated between so-called Pure and Applied Pesearch. and have given a half-hearted PRESIDENTIAL ADDRESS SECTION D. 101 support to the latter division, almost entirely refusing support to the former. Such a policy has been almost fatal to research, for, despite the attitude of governing bodies, the scientist con- cerned in research which has a patently economic value will admit that it is impossible to draw a line of division, and further, that so-called Applied ^Science is directly dependent on Pure Science. Consequently, the progress made is comparatively small. The present world-confiict has demonstrated to us all that in such matters Germany was leading the way. The organisation charac- teristic of that country appreciated the way in which the whole was constituted, and realised the value of each unit. There we find a whole-hearted Government support given to all that may be called scientific research, and accompanying this policy a rapid progress. In ever}- branch of Science — Pure and Applied — we must admit thoroughness and minuteness. It is only by adopting such a scheme that we can hope to advance, missing nothing by the way. This amounts to the encoiu-agernent of the spirit of research. Cultivate such, and then the rest is assured. Lhnit the lines of research — for arbitrary choice of certain branches for encouragement spells limitation — and then vv-e are lost. " Orga- nisation and Thoroughness " should be our motto. l^erhaps the subject of Zoology is that, or one of those, development of whose research is most likely to be overlooked. There are a few divisions of the subject which have a patent economic importance, and these are just those which receive some attention at the hands of Government experts. Such divisions are Entomology. Protozoology, etc. Yet these are not supported as they should be, if the work is to be done thoroughly and scien- tifically, and, further, tiiat work is far too localised. VVe have in this country a number of universities, museums, and Government departments, the stafifs of which are actively engaged in zoological work. Progress is made under extreme difficulties, and although much has been accomplished, can we say that it approaches what might be expected from such a number? Routine work inten- sified by understaffing, and lack of literature, combine to militate against research work. More important still, there is very little attempt towards co-ordination. It is time that we made up our minds to attack seriously and scientifically the zoological problems in this coimtry, and further to encourage South Africans to take their share in that work. In glancing over the spheres of work in which research is being attempted in this country, it is noteworthy that nearly all the main divisions of the animal kingdom are receiving some attention. It is, indeed, most fortunate that there is little over- lapping. Protozoa, Ccelenterata, Phatyhelmintlies, Polychseta, Oligochieta, Hirudinea, Nematoda, Crustacea, Myriapoda, Insecta, Arachnida, Pisces, Amphibia, and Reptilia are all being investi- gated. Much of this work is purely systematic, but it is the first and essential step towards a deeper knowledge of the zoological problems of this country. I am sure that workers in all these I02 PRESIDENTIAL ADDRESS SECTION D. groups will agree with me that there should be much greater co-ordination. We require to know, not merely the various species represented in this country, but the distribution in detail of each species. To no worker should this appeal more than to the parasitologist and veterinary. Anyone interested in zoological problems will realise that systematic zoology must play a very important and basal part, and that broad generalisations will lack support unless they have been built up in full cognisance of the systematics of the group or groups concerned. The mere description of new species or genera at the present day fails to attract many zoologists, but all will recognise the necessity for the description of all existing forms. Many no doubt will see in such descriptions the corroboration of morpho- logical generalisations, interesting information bearing on prob- lems in heredity, genesis of species, distribution, palseogeography, phylogeny, or possibly the key to a classification not before possible owing to our ignorance of the existence of intermediate forms. To all zoologists the completion of a census of the fauna of South Africa will appeal as a necessary and ideal task, for the reasons above mentioned. The carrying out of such, however, will demand the labours of more zoologists than are at present available in our universities, museums, and Government depart- ments, and thus directly and indirectly demands greater financial assistance. In inaking any such request I think we, will all feel that it devolves on us to demonstrate that, beyond the great necessity for such a zoological survey in elucidating the fauna (jf South Africa, there is a direct economic side, and again to indicate the means by which such a survey can be carried out. Perhaps no country in the world possesses more interest for the parasitologist than Southern and Equatorial Africa. The pro- tozoologist has here a life work, and continues to discover new forms and find the clue to life-history cycles. He soon realises that what is known of South African parasitic Protozoa repre- sents but a small part of what remains to be known, and that patient work, with encouragement, will lead to results that may yet be appreciated from the direct,ly economic standpoint. The protozoologist is concerned not merely with the morphological characters of his protozoon, but also with its life-history, and this demands a specific census of a great number of other grou|)s. Hence from this standpoint alone we can furnish a very strong case for a complete zoological survey. It will, I think, a])peal to all that this knowledge merely will not furnish us with a scienti- fically complete record. We need really a detailed distribution list of each particular species, both of host and parasite. It is only by possessing such information that we can set to work to encounter scientifically any trouble due to parasitic iforms that may arise at any time. This concerns not only parasites which are endemic, but also specific hosts which may act as intermediaries for exotic forms which may arrive. Further, much interesting work of a PRESIDENTIAL ADDRESS SECTlUN D. IO3 Statistical nature has been initiated in connection with such para- sites as the germ of malaria, and such is dependent to a large extent on our knowledge of the distribution of anopheles. A detailed knowledge of the latter form, tor example, may be needed ere long, as there is every possibility that malaria will atlect much wider areas than m pre-war days. Quite recently Bilharzia has made its appearance in many areas within the Union, and unless the greatest precaution is exercised, will spread throughout this territory, ihis state of altairs, when we realise at the same time our comparative ignor- ance of the specific nature of tlic numerous riatyhelminthes in this country, and needless to say, their life-history, necessitates a detailed census of the Mollusca, both from the specific and dis- tributional standpoints. We have several workers in this group, but they have not the time nor opportunity under present condi- tions of even attempting any such serious task. Such workers need an army of trained collectors. To quote one outstanding example, it may be pointed out that we are ignorant of the life- history of the tapeworm affecting the ostrich. Such work neces- sitates much patient labour, and can be carried out only with relief from an excess of routine work and Government assistance. Under any circumstances it will occupy many years, but a start must be made, and 1 feel strongly tliat we should now plead for the initiation of such. What has been said in reference to the Trematoda and Cestoda applies equally well in the case of the Nematoda. Great attention to these parasites is encouraged by European, American, and Australian Governments, and tnere is equal need in South Africa. We want to know much more of the structure and life-history of South African forms, and especially of their life-history. This is necessary if we are to attempt a scientific control over parasites affecting stock. The important part played by insects and ticks as intermediate hosts in tiiis country is known to all, and I think it unnecessary to ask for support in suggesting the urgency of a census of these forms. I have mentioned a few groups, the economic significance of which will no doubt appeal to all. But we must bear in mind that other groups have an equally strong claim, and some may yet claim greater attention, such as Myriapoda, UligochcCta, Hiru- dinea, etc. In fact, it becomes at once dogmatic and unscientific to attempt to differentiate, although it must be granted in the present state of our knowledge that certain groups have the stronger claim. It would be better, however, to work towards the ideal, and follow the scientific path by instituting a complete zoological survey. A recently-published bulletin of the United States Depart- ment of Agriculture presents the results of the second annual bird count in the United States, carried out in 1915. It is based on 315 reports, from every State in the Union except Utah and Nevada, and shows a gratifying agreement with the results obtained in the I04 PRESIDENTIAI, ADDRESS SECTION D. previous year. " When an enumeration of birds was suggested,'", says the author, " the project was the subject of much good- natured banter and some criticism from those who declared the scheme utterly visionary," but these animadversions were based upon the misunderstanding of methods to be employed and the objects in view. The average bird population of that part of the North-Eastern United States devoted to agriculture has been determined with sufficient accuracy to furnish data having various practical and scientific applications, and some useful general information has been obtained in reference to the rest of the counti"y. The average in the North-Eastern States is about 800 pairs of birds to the square mile. It is not yet possible to estimate the population of each species, except for a few of the com- monest and most widely distributed, such as the English sparrow and the robin, for which the reports are sufficiently numerous to permit an approximate estimate. The most elaborate report received in 1915 was that of the Campus of Cornell University. Its 256 acres were divided into six blocks, and the survey of each was made by a different person, the whole being in charge of Professor Allen. The densest bird poi^ulation was found on a small private estate near Washington, D.C.,with 135 pairs nesting on five acres, and the most varied population in the bird sanctuary and park, known as Woollen's (iarden, near Indianapolis, wuth 62 species on 44 acres." I quote this as illustrating the efiforts of the American Government. In that country a great deal of attention is now being given to the study of Animal (Ecology and animal communities. This most important study is necessary if we are to attempt to comprehend the significance of " Balance in Nature." The ruthless destruction of certain types of animals, notably birds, the importation of an exotic pest, have many times demonstrated the existence of such a " balance." This is very patent in the case of insect pests. Our experiences in this country with the Australian wax scale is a case in point. An understanding of this balance necessitates a knowledge of Animal Oncology, the prelude* to which must be a more or less complete census of our species, and their distributions. Other countries have realised this, and South Africa should fall into line. But independent of the directly economic aspect, such a survey would enable us to deal more effectively with the origin and distribution of our fauna. Botanists have realised that the .scientific basis from which we must orientate in grappling with the problem of distribution is oecological, and a great amount of research is accomplished already in that direction. The claim is equally strong to the zoologist. There are portions of our fauna — particularly terrestrial invertebrata — which are practically unknown. The same state of affairs exists in regard to the distri- bution of our littoral shallow-water and deep-water marine forms. As we are living to-day in a time when the generalisations in any one science are so markedly overlapping those of other sciences, the necessity for a deeper knowledge of faunal distri- PRESIDENTIAL ADDRESS SECTION D. IO5 butioiis in this country — terrestrial and marine— should ai)peal strongly. For South Africa possesses great interest to the zoo- geographer. The history of our fauna cannot be elucidated, nor the true relationship to other parts of the world indicated satisfac- torily until such data as a survey would supply are accessible. Many of the generalisations accepted at the present day are based on meagre information, and will no doubt be revised. Localised surveys of certain groups which appear to possess some special interest to zoogeogra])hers have been attempted, but naturally are far from having any character of completeness. The fauna of the Bokkeveld beds, and the fauna and flora of the beds of the Karroo Basin, suggest close relationships in Devonian, and in late Palaeozoic and earlv Mesozoic times with South Africa and India, and possibly even more directly with the Antarctic Continent. There is much evidence supporting the idea of a late Palaeozoic and earlv Mesozoic Gondwanaland, but this evidence can by no means be regarded as conclusive. The existence of such a land mass is of great importance to the geolo- gist working in the Southern Hemisphere ; and the acceptance of such must fundamentally affect the problems of dvnamical geologv in this hemisphere. The student of zoogeography must also take into consideration the significance of such a land mass in attempting to elucidate the meaning of the present faunal distribution. Further, if such be the case, we might exr)ect that a deeper knowledge of present faunal distributions in this country might be reflected on the problem of Gondwanaland. We might reasonably hope for the discovery of forms i^reserved on our mountains, and descendants of a stock derived from Gondwana- land. So far the little survey work attempted has been successful in finding generic representatives of Phreodrilid Oligochfetes, and the peculiar Crustacean — Phreatoicus. The former grotip occupies an important intermediate position between Microdrilid and Megadrilid Oligochceta, and enjoys a circumpolar distribu- tion, being found in South America, South Africa, Australia. Tas- mania, and New Zealand. The peculiar habitat — the forms occurring on mountains or adopting a semi-parasitic habit on hosts endemic to the particular area — strongly support the idea that they are the remains of an archaic stock which probably once occurred throughout Gondwanaland. Phreatoicus enjoys a cir- cumpolar distribution, and is highly sjiecialised. Further search may yet unearth such archaic forms as Anaspides. which so far has been found only in the mountains of Tasmania. From these remarks I think it should be clear that a detailed zoological survey will furnish not only information of direct economic value and data of interest to zoological research, but will help materially towards developing a positive position on the part of zoologists ir rep-ard to the generalisations accepted by many geologists, which are of the greatest importance to geological research in general. 106 PRESIDENTIAL ADDRESS — -SECTION D. We have now to consider the means by which a survey can be carried out. It is quite clear that the present staff of zoologists available within the Union cannot undertake such a survey with the hope of completing it. Systematic collections must be made by trained zoologists, and the work of the various zoologists co-ordinated. 1 have already stated that there is a most fortunate distribution of the various groups among the workers in this country, and assisted by systematic collectors and other workers a great deal can be accomplished. In addition to university, museum, and Government departmental zoologists, there are a number of private investigators engaged in research, and the services of the latter could be relied on for investigation and collation of data in connection with their special groups. With the appointment of a number of young trained zoologists, the country could be mapped out into areas, and each of these systematically investigated. This will offer special opportunities for South Africans anxious to assist in elucidating the fauna of their own country. At the present time we lijid that Zoology, as a subject, has not the same attraction for the bulk of our Science students at the Universities, except in the case of medical and agricultural students, as have those sciences which will assist them in the teaching profession. In this way there can be little doubt that many who would show aptitude for zoological work are lost. A limited number of scholarships are offered by the Government for students anxious to undertake Entomology and Veterinary Science. In this connection I would suggest that scholarships should be made available for those anxious to prosecute zoo- logical work, and that the services of such candidates be enlisted in connection with the proposed survey. The details of any such scheme as suggested must await the acce]:)tance of such a pro- posal. I trust that 1 have in this address the support of the Zoological Section, and that they feel with me the importance of a Zoological Survey of South Africa. Section E.— ANTHROPOLOGY, ETHNOLOGY, NATIVE EDUCATION. PHILOLOGY, AND NATIVE SOCIO- LOGY. President of the Section : — Rev. W. A. Norton, B.A., B.Litt. FRIDAY, JULY 12. The President delivered the followinsf address : AN OUTLINE SKETCH OF RESEARCH INTO THINGS NATIVE, WITH SPECIAL REFERENCE TO THE BANTU AND THE WORK OF THIS ASSOCIATION. It seems natural that a presidential address from time to time should summarise the progress made hitherto, and I therefore propose, after sketching very lightly the field of this section and the workers in that field of the past, to treat in more detail of those subjects which have occupied the meetings of the section since its separation from Section D, and former papers which would have been contributed to Section E. had that section then existed. Finally, to draw attention to subjects crying for solu- tion, and the possible bearing of that solution on the whole of our field. Section E is intended to be the native section (not that the members of it are native, except in so far as a large and in- creasing number of us are African-born), but in the sense that it has, with becoming modesty, taken all the Sciences for its province which have to do, specially or immediately, with natives. According to the programme of the last two annual meet- ings, the subjects of Section E are Anthropology, Ethnology, Native Education, Philology, and Native Sociology. It is true that the Philology is not specifically Bantu, or even African, but I notice that philological papers like that of Professor Nauta on French literature were wont to be taken with the educational subjects, which now, we are glad to see, have a section to them- selves. For two years now, Section E has been in the same condi- tion, the subjects of which tended before unduly to crowd with papers Section D — our parent section — which has now, therefore, the time to discuss that useful bird, the ostrich, and other matters. I called my paper " A Sketch of the Field and of the Workers contributing directly or indirectly to the subjects of our section.," This will, I hope, make it clear that my treatment will be neces- sarily rapid. I shall skip over regions and centuries like a hart upon the hills ; but I would ask you at the end to draw with me a definite conclusion. Obviously all African explorers would be alone too large a scope to treat of, or even to I'ist, in a paper of this sort, so I will I08 PRESIDENTIAL ADDRESS — SECTION E. confine myself mainly to modern South African workers, or workers in the Southern half of Africa. II. I have no intention of treating in detail the various English and other travellers who made the civilized world acquainted with the different lands of Africa, or even those of the present Union. We will not linger over the Portuguese writers, their brave missionaries and warriors, who have been so exhaustively treated of by Dr. Theal, except to mention, from the side of philology, the work of Dias, the Jesuit, on Angola, and of Brusciotto on Congo, published in the seventeenth century at Lisbon and Rome respectively. Purchas, in the early seventeenth century, touches lightly on South Africa: Peter Kolbern made known the un- pleasant manners of the Hottentots in German, Dutch and Eng- lish in the early eighteenth century. We had a train of visitors — Sparrman, Paterson, Thunberg, Stavorinus, and Le Vaillant, who, himself romantic, reminds us of his ingenious parodist, the greater romancer, Damberger, with his extraordinary fiction of a journey from the Cape, through the Kaffirs, to Timbuctoo. Percival and Barrow arrived at the be- ginning of the eighteenth century. Burchell, Campbell, Lichten- stein, Latrobe the Moravian in the 'teens ; Thompson in the twenties, Owen, Arbousset, Casalis in the thirties, Methuen in the forties, Smith in 1850, left us accounts of their pilgrimage. Bor- cherd had begun his by 1801, but did not publish till '61. Time would fail me to tell the tithe of those who since have followed in their train — of the lands and tribes they visited — of the observations they made — of the sciences and nationalities they represented. They are a great cloud of witnesses, many of them worthy to rank with the pioneer ex])lorers of West an'l Central Africa, with Park, Barth, and others in the former, with Bruce, Burton, Speke, Grant, Stanley, the unfortunate Tinne ladies, Petherick, the Bakers, Sweinfurth, in the Nile basin; and in East Africa, with Rebmann, Krapf, and a host of others ; ad- ministrators like Gordon, hunters like Oswell, and the late heroic Selous ; explorers and scientists like Holub and Miss Mary Kings- ley ; missionaries like Du Plessis in recent times, and earlier Dr. Moffat, whose son, Mr. John Moffat, is still happily with us — a fount of information about the Bechuana and the days of Loben- gula. These, in North and South, helped, in one way or another, in less or greater degree, to open up the mighty continent which we inhabit. One name, of course, stands out above them all for universal travel, many-sided interest, and appeal to the native 'mind, for his magnificent character, his imperial determination, his grit and patience — the immortal name of Dr. David Living- stone. In spite of the intelligible but regrettable opposition of the London Missionary Society, which would have chained the Pro- PRESIDENTIAL ADDRESS — SECTION E. IO9 metheus of Central African discovery to the mission station of Kuruman or Mabotsa (over there among the Bakgatla, vi^hom I also, a few years ago, was teaching) , he braved alone the perils of river, swamp, and forest, of slave-trader and barbarous chief, and came safely through, where Stanley, with an army, found op- iposition at every turn. He became the typical opener up of Africa, whom his mission would have used to teach a few Bech- uana. When will missions and when will governments learn to know and use their men ? Further than the crying and historic case of Livingstone, I cannot venture to speak of other denominations than my own; but of that I am bold to say — for truth is better than dear friends — the failure of thoise responsible for the training and equipping of the minds of our missionaries for their task, linguistically and ethnologically — the failure to use them when they have equipped theniselves, fills me oftentimes with grief, despair and shame. You may think that this is too strong language, and more- over not a concern of this Association, nor of any but the mis- sionary societies. This I deny. The missionaries, as a class, are in closer touch than any other European, with the native, i.e., with the bulk of the population of this country ; and I consider that their effectual training and the moral (I do not say religious) training of the native which depends upon it, is a very serious matter for the community in general. In Nigeria I was told by an administrator that missionaries who are not ethnologists are not encouraged by the Government for fear of complication with the Mohammedans. No one desires such an attitude here, but the fact is very significant. Nor can our governments escape blame for the lack of training of Admin- istrators. If I may quote Mr. A. E. Griffiths in a recent paper on the South African Undergraduate : — " The part our undergraduate has to play in the administra- tion of native affairs has received no consideration from our University or Ministerial Authorities. The fact that South Africa looks among the rising generation for the future rulers of her native races is not yet understood. There exists, apparently, no correlation between University work and preparation for na- tive administration ; at least, we have no specific University course — no professorial chair of native languages." (And that is still true in spite of one advertised last year.) " No national school of administration. . . . Are we surprised that our undergraduate has given this — the first of South African fields — no serious attention?" in. Mommsen has said of Scipio Africanus that in his quiet chamber he no less died for Rome than if he had fallen beneath the walls of Carthage. Thus (may we not say?) the scholar Lepsiiis, for example, in addition to his labours for European scholarship, did more for African missions by his phonetic no PRESIDENTIAL ADDRESS SECTION E. system than many missionaries have done. The figure of Livingstone kneeling dead by his camp bed in Ujiji — dead for Africa and its tribes, for the removal of the plague spot of the world, the slave trade — touches the mind with its peculiar pathos ; but there is another name I would mention, who gave his life for Africa, though, like Scipio, he died at home; who gave it in studies of portentous magnitude and effect. The mind reels at 'the thought of the 80 note-books of Bushman lore, still (alas) in manuscript only, with which Dr. Bleek's indus- try has endowed the South African library. What African philology owes to this scholar and his family passes telling; one of that family survives, as, I believe I am right in saying, the only Bushman scholar in the world. Bushman paintings and engravings are a special care to a learned lady of this Associa- tion, but firsthand knowledge of their language depends upon a single life; and again we must lament the lack of interest which South Africa has taken in things Bushman, her unique contribu- tion to philology, and the history of primitive art. I cannot conclude this part of my subject without a reference to that veteran historian of equal industry, Dr. Theal, whose contribution to South African literature it would be presump- tuous of me to praise, especially as he too, thank God, still sur- vives. One is thankful that here the succession is not entirely broken, as younger historians are present to carry on the torch. It is, strangely enough, upon a Rhodes chemistry chair that Elijah's mantle seems to have fallen. Other sections may consider it unsuitable and even im- proper to carry introspection to such an extent as to make past contributions to itself the subject of a presidential paper. But Section E, at least, need feel no squeamishness in this regard, and for this reason — ^that (though the papers of all the sections doubtless contains original research into branches of science which have been worked for decades, if not for generations) some of the founders of ethnology are still with us, and the scientific study of the natives of this country and their language is still very much in its infancy, or (shall we say?) in its embryo stage ; and this Association, especially in Sections D and E, may venture justly to say Pars magna fui. This is my apology for proceeding to mention some of the contributions which it has made to the scientific study of South Africa on the native side. IV. Mr. Hammond Tooke. as early as 1905, directed the atten- tion of the Association (soon after her birth) to the subject of uncivilised man south of the Zambesi, which in 1820 he divided into five groups, viz., the Zulu-Xosa, Gvvamba. who tekesa (as the Zulus say) in their speech, the Kalanga, Chwana, and Herero — which last were identified as possibly the Mazimba of early Portuguese writers. Mr. Tooke followed up this essay PRESIDENTIAL ADDRESS SECTION E. Ill outside the pages of our journal with notes on the Bantu of the loth century as described in extracts from the " Golden Meadows of Mas'udy," and these were published by the African Monthly in 1907. I had originally intended to discuss the early geographers and explorers of Africa in connection with this paper, but to avoid undue length, have already read those pages as a separate paper before my section. In them I drew attention to the fact of the great importance of philology in regard to all research into the testimony of the early and present writers about our country. I cannot doubt (and in this I find I have the agree- ment of Dr. Theal), that much material still remains to be dis- interred : not only from the libraries and other hiding places of the West, but also from Oriental sources ; and, for the interpre- tation and use of such authorities, philology will be indispensable — not only knowledge, and in so wide a field, necessarily com- parative knowledge, of Semitic and other groups made use of in ancient geography and kindred subjects, but also comparative knowledge of the dialects of Africa, which will certainly throw much light upon the records of the past, as can be seen, for example, in the case of Mas'udy, whom I treated in my ex- cerpted pages, alluded to above ; but to this point I will again return. I have, in the other paper, used Mr. Tooke's work on the Arab geographer as a starting point for a resume of the earlier writers on Africa. I may now use his paper before your Asso- ciation in 1905 as a starting-point for the later and contemporary work with which I am in the briefest outline to deal. It is, of course, as I said before, impossible to attempt to mention, not to say appraise (even if the present speaker were worthy to do so), all the recent work upon native Africa or South Africa. I can but endeavour to say a few words about our debt to some of those writers who have come in any way before our Associa- tion. V. Let me begin by paying a tribute to the industry and effec- tiveness with which our President in this section last year — Mr. Roberts — largely in conjunction with Mr. C. A. T. Winter, has set before us the results of their research into the tribes of the Northern Transvaal. Would that he were here to-day to assist our deliberations, though we must not grudge his services at the seat of war. We will hope that his presence in Europe may procure the publication of his papers in a more permanent form than the present, and we shall look forward, please God, to a speedy return of him and all our heroes. I need not specify his manifold work here, nor that of Mr. J. A. Winter. The latter contributed in 191 2 the " History of Sekwati," the " Tradi- tions of Ralolo." the "Praises of the Chiefs," and "Circum- cision among Sekukuni's Folk," followed in 1914 by his " Men- tal and Moral Capabilities of the Natives." Mr. Junod, to travel F 112 PRESIDENTIAL ADDRESS — SECTION E. further East, contributed in the same year an arresting paper on the " S.E. Natives in the i6th Century, and has since produced a most valuable contribution to the ethnology of the same field in his two volumes upon the " Thonga." Mr. Garbutt has written of Rhodesia, and compared the custom of Egypt and the South ; Mr. Dornan not only writes on native poisons (a subject which the President of Section B last year has also made his own), but has further had the courage to enter the lists, and that from the side of native tradition, in that delicate question which, from time to time, shakes Africa — I mean the Zimbabwe origins, which have been discussed in our Transactions, in the past, by no less an authority than Mr. Hall. While very willing to join with the Oxford Professor in claiming more culture for past generations of natives than we in this sub-continent are always ready to grant, I feel that so weighty a question may not, till the end of the chapter, be settled ; but the very fact that claims and counterclaims of date range over some two millenia, not only in the case of African Zimbabwe, but even in that of British Stonehenge, shows how very little way we have gone in settling the sciences of anthropology and ethnology, and how very little encouragement is at present given, either by government or the public. But there are economic sciences considerably more inti- mate and pressing, not always, perhaps, to my own, but to the public mind, to which are made the masterly contributions of my other Vice-President, Mr. Kingon, especially within his own sphere, the Transkei. I note that he apparently sides with the presidential address of my predecessor in doubting of the weighty warnings, which a veteran authority on the Eastern lands, like Mr. Maurice Evans, gave us, as regards the likelihood of real competition between white and native workers, in case of a labour-market free from the present artificial restraints of law and custom ; a subject of peculiar interest at the present juncture. I note another difi^erence of opinion between one of the writers last mentioned and Dr. Loram in his book, so full of valuable statistics, on the education of the native, and ask, " Is it, or is it not, the fact that they, at the age of puberty, become, any more than whites, mind atrophied ? VI. There are grave questions, and evidently at preseiU it is hopeless to expect anything but disagreement among the doctors. If we turn to the missionaries we find the same disagreement, but here the shocking neglect of professional training on the physchological side for dealing with foreign nations oft'ers very largely the explanation. Let me give an example of a moot point among us; the majorities in our missionary synods and conferences have legislated against the traditional manner of native customs like circumcision, with a minority protest, to which I confess that, after study, I incline. What has struck me is the very little vahd evidence that most missionaries have PRESIDENTIAL ADDRESS — SECTION E. II3 to offer of the essential character and moral effect (in the wider sense) of the rites, and how very little dispassionate study is given to the matter. (My own discoveries I ventured to sub- mit to you some years ago, as did Mr. Roberts for the Trans- vaal recently). Early missionaries had to make a decision before the birth of ethnology, and that they did fearlessly, according to their light, however much their own immediate success was hindered. It may be that then was the time for trenchant severance from an evil inevitable legacy of past abuse. But now, I cannot help feeling, the native suffers grievous loss of very much needed discipline, through the uprooting of the landmarks of immemorial sanction, and I hope it may not be too late to save some part of the structure of what is now recog- nised, among serious students, as a highly respectable ethnic sys- tem, in the face of the obvious failure of the effect to Euro- peanise. Pray do not think me a Julian endeavouring to galvanise a twice-dead heathenism ; it is just because I believe that true re- ligion should find room, in most cases, for the pre-Christian Ethic, and build upon it, that I regret the complete (and, I fear, largely needless) ruin of the sanctions of the Bantu past. The fact, which I emphasize again and again, is that we have too little study of that past and its meaning, on the part of those who have to guide policy, both in Church and State ; and even the academic world is not allowed to contribute as it should to the solution of the native problem. Academics themselves are now awake to the need, but only partially, even they. I shall not for- get the surprise of a Professor of a South African University College, who was very deeply interested in totemism, when he discovered from me, for the first time, that the totemists were at his gate, as I called a native lad to him and asked him what he danced — that is to say, his seboko. or " totem." I am only say- ing in much oif this what Mr. Roberts said last year at greater length and with greater effectiveness : " The work of the Chris- tian missionary requires very special training, and, until this fact is recognised by the churches, the results of their work among the Bantu are bound to be disappointing and more or less of a failure. The fault lies with those in authority. The training should include the study of comparative ethnology." Note the " comparative !" No true philology or ethnology can be other. This is a practical matter, not an academic. If we break an arm we choose a first-aider to help us, rather than one who says he has the love of heaven or of mankind, if it has not led him to learn duly the science of giving first aid, by studying bones and muscles : a study which seems to the layman academic. So must we study native cult and custom if we would best commend our own. Dale, of Zanzibar, was able to tell some Moslem teachers that the text they were quoting was not in the Koran but in a 114 PRESIDENTIAL ADDRESS SECTION E. commentary upon it ; they marvelled that he knew their own books better than they did themselves. We want more men trained thus fully for their special work ; then should we find no lack of trained administrators and missionaries as experienced contributors to ethnology, far better than the scientific visitor who has not the confidence oi the particular tribe. If we were thus learners as well as teachers, how many solecisms in translation, how many mistakes in policy we might avoid, which alike proclaim our systems alien (externally, though not fundamentally). We have no difficulty in realising the point with our fellow white-men. We know that we must enter into their lives, and the more thoroughly, that is, the more scientifi- cally, the better. We do not need to live all their lives, as we need not, nor are able, to live a native's, but we need to study the lives scientifically, alongside of the language, and until we do so we deserve to be ousted by others who will. One day I happened to mention the names of some of his ancestors to the son of a chief of the Batlokoa who was visiting. In a few weeks three pages of foolscap arrived filled with a neat though elaborate genealogy which I could largely verify, and which went back nearly 30 generations (probably something over 600 years). There was confidence established, and the native shyness broken down by an interest shown in their his- tory. As a high government official points out in Mr. Hollis's excellent book on the Masai, a genuine interest in the native mind and language is one of the most hopeful ways of avoiding even punitive expeditions. If all that I have said is true of the missionary, surely it is true also, if not more true, of the administrator and his assis- tants. How true also it has been in this war that often all has depended on such intelligence and staff work, and indeed the principle has long been recognised in the navy, so far as the encouragement of language study is concerned ; yet a recent num- ber of the English Rczneiv gives a case of a loss at sea costing the country £3,000,000, due to ignorance on the part of an officer of the distinction in sound between German and Nor- wegian. I could give many examples of similar mistakes in native tongues, often laughable enough, but too frequent to be amusing, seeing the estrangement which their cause in the long run brings between ruled and ruler, teacher and taught. VII. This is the case with us English in the matter especially of philology, in spite of the fact that the science deals with speech, the prerogative of man alone, the chief interpreter of the mind, and therefore the chief interpreter of man to man. Yet this is the science which we carefully avoid. Though near a century and a half has gone by since the derided discovery of Sanscrit as the key to European tongues, instead of Hebrew or what not. philology is still commonly considered a mark of the faddist, or PKE'^IDENTIAL ADDRESS SECTION E. II5 the wide-sundered metiers of the philologist, necessarily compara- tive, and the linguist, whether polyglot or idiomatist, are con- fused. It is not realised that the philologist does not claim to be an expert on every tongue as spoken, which indeed were quite impossible, 'but can yet throw light, as perhaps no one else can, on the meaning of the idioms within the family he studies, and often far beyond ; for, once again, let us recall it, speech is the key to the main gate of psychology. I may illustrate this failure to realise the position of the philologist by the si;rprise and sometimes indignation I have met with from the speaker of a dialect, whether European or native, when one presumes to suggest a derivation for a personal or place name. The non-philologist bystander, even of intelligence, is apt to endorse the unfavourable verdict; but a concrete illustration from an English place-name will shew the unreasonableness of this attitude. I spent some years upon the Trent bank in the combined parish of Kelham and Averham (pronounced A'erum), near Newark. The spelling of both names suggested a home originally; but of what? The Domesday " Calune " was rejected as the mishearing of a Norman scribe, but a chronological listing of the forms, in which the names occurred, revealed the fact that 'the spelhng was a fallacy of association in both cases, and phonetic script made plain that the local pronounciation preserved the Anglo-Saxon locative phrase, all but exactly, which describes the place as "set cellum and atherum " (gen plur : forms), i..e., " at the springs and watercourses." The native Notts villager had preserved the sotmd all those generations, but all his re])eti- tions could not have guided him to the meaning of the name without philology. As an Englishman born and bred, with no trace, so far as I know, of foreign blood in me, I deeply regret that this simple bit of English philology was due to a German scholar, who very probably spoke bad English, and might rouse our indignation or amusement at his temerity, if we did not understand the use and purpose of the philologist, his distinc- tion from the linguist, and his practical value, nevertheless, to the same. Why need we be so behind in matters of such sim- plicity? It reminds me of a certain front of a war where inter- cepted enemy wireless messages were being passed to head- quarters and uselessly filed, while the freely offered services of an experienced decipherer were refused. May I venture to suggest that we see this same weakness reflected in our own association, and even in Section E. Many useful papers appear dealing with the customs of different tribes or with their dialects, but how little comparative work is done on the one or the other over any wide field. It may be thought that this is due to the time not having yet arrived — but this is not so, for the Berlin Orientalisches Seminar, and the Hamburg Kolonial Institut (only recently at last followed by our London school of Oriental languages), have long been working under the guidance of ?\Ieinhof on the comparative study of Bantu, Il6 PRESIDENT] AI, ADDRESS SECTION E. and have produced results which stand the test of practical application to individual dialects, as I myself have often proved. (I beg to refer to my paper on South African language study in 1914.) It is just that co-operation which we need in the future between the idiomatist, who knows something of comparative philology, the philologist, who knows some- thing of the idioms, and the ethnologist, who knows, as too often he does not, something considerable of both. Our present enemies have taken the forehand and advantage of us by securing this co-operation in the past. They do this by Government endowment and publication of re- search, instead of waiting, as we too often do, till we have broken the heart of the researcher by leaving him to the tender mercies of the publisher, who at his peril rises above the demands of the inanes voces populi. Of university presses, it is true, we reap better things ; would that somebody would endow in this way our new universities here. Again, to illustrate from Meinhof 's work : Endemann in Sesuto ; Hahn, Brincker, Kolbe, and \^iehe in Herero, etc., are all laid under contribution by him for comparative purposes, and are themselves often highly alive to the need and importance of comparative work, and hence of a sound phonetic, in which again, doubtless owing to the abominations of our English spelling, we are ourselves but beginners. Steere, however, was in East Africa an exception; in Swahili, Yao, Nyamwezi, Shaimbala and Konde, he is acknowledged by the Germans as a match, and has a digne successor in the truly venerable Archdeacon Woodward, of Zanzibar, who has, if 1 remember aright, recently brought out his sixth African grammar. To the scholarship of Mr. Madan. senior student of Christ Church, was due a Swahili dictionary and Testament. Would that the tradition of learned students after the pattern of Bishops Colenso and Callaway, for example, had been better kept amongst our missionaries here in South Africa, or adminis- trators found with interest in their people equal to the production of books upon them, such as those of Sir H. Johnston, the Lugards, Routledge, and Mollis of the Masai. Let me pay a tribute to those who have (paved the path for the comparative work of which I speak ; to the collections of Fr. lorrend ; and, among idiomatic work, Kay's researches in Kaff- raria ; Holden, on the Xosas in the 6o's (of whom and others I am reminded by my kind friend the Parliamentary Librarian) ; the Zulu labours of Fr. Bryant, those in Suto of the Paris Mis- sion ; the magnificent and growing treasures of Kropif and his continuators ; the Kaffir Bibles of Appleyard and others ; and (last but not least) the many useful works of Mr. McLaren, Mr. Scully, etc. ; and I beg to congratulate Miss A. Werner, more especially, the Reader in Swahili at the London Language School, on her persistent and increasingly successful efforts to make the PRESIDENTIAL ADDRESS — SECTION E. II7 soundest comparative work known to the English public, not to speak of her own labours in many spheres of research. [To those beginning their study of the subject I can recommend no better book than her " Language Families in Africa," published by the S.P.C.K., and her translation of Meinhof's lectures, pub- lished by Dent.] I have omitted the work of Tindall, Shaw, and some Ger- mans, in Hottentot, as lying somewhat beside my main subject, though extremely interesting philologically, and continuing the treatment of one of the earlier South African problems attacked by Peter Kolben and other officials of the Dutch Colony, who took an interest in these neighbour tribes, worthy of more imita- tion by modern administrators. I must not forget in this para- graph to mention the great work done on the aboriginals, ethonolo" gically, by the distinguished Director of the Cape Town Museum. VIII. For the future, it remains to get an adequate phonetic script used in every language, including, let us hope, our own, even if not adopted for ordinary publication in each : too often their orthography has been inadequately, misleadingly, and contradic- torily settled, even in allied tongues, and it is already too late to expect a reformation ; witness the case of Sesuto and the Sech- wana dialects, where the sounds and forms are almost identical, though, of course, peculiar words occur in each special vocabu- lary. The new literary languages, however, as published, are trenchantly separated into Sesuto, Serolong, and Setlaping, this being largely due to the dialects met with by each group of missionaries, when they reached the publishing stage, being stereotyped as standard, within their various fields. Had the science of phonetics, through more adequate training, then im- possible, reached the missionaries earlier, one consistent ortho- graphy might doubtless have been adopted, followed by translations containing the most expressive words and idioms of every dialect, and giving (like our Authorised Version) a rich, permanent, common standard of vocabulary and diction through- out the whole of Central South Africa. In case some of my hearers may be expert in Sechwana dialects, I may explain that I found this statement on experience in a Native Training College, containing representatives of some score of tribes, who were asked to write, each in his own home- speech, the simple sentences: — " The chief has made a good law." " He has not yet done it." The experiment proved, as was expected, that the rea.1 vernaculars, unstandardized artificially by missionary translation, faded into one another, like the colours of the spectrum, and of the twenty versions of these short phrases scarcely two agreed. Another desirable move is the introduction of comparative grammars for European students of Bantu, like those of Latin Il8 PRESIDENTIAL ADDRESS SECTION E. and Greek now used in schools, having similar forms under like- numbered paragraphs — an arrangement lending itself admirably to Bantu, the dialects of which are so extraordinarily consistent. This plan had been adopted, both in German and in English, by Meinhof, for grammars, before the war. The grouping of these dialects is a problem scarcely touched, which would be greatly helped by such comparative methods ; the relation of Bantu to Hamitic and to the Soudanese group might then approach solution, and the place be found of the sundry Pygmy dialects as well as of the remnants of Bushman. All kinds of subjects standing between philology and anthropology would thus more easily be attacked. Personally, I hope wide-reaching re- sults from the study of those branches in which I am specially interested, and have had the privilege of speaking about them before you in the past, viz., native music and poetry, fauna and flora names, star-names and place-naimes — these, having reference to objective facts, observed by all the tribes, must certainly throw new light, if widely enough studied, on the wanderings of the peoples and on cultural borrowing. In this connection we welcome the large increase of know- ledge of native praise-songs and similar traditions, which this section owes to Mr. Stuart, of Natal, and others. Again, wide research into chief's genealogies would not be difficult to record and compare, and would lead, as in my own experience, to much access of knowledge about tribal history, and so contribute to- that of Africa in general. The South African Historical Society, now, I fear, suspended for the time, show^ed this in the care Prof. Cory and others took to collect in- formation, both from natives and Europeans. An admirable illustration of the use of such work is pro- vided by M. Ellenberger's book (and that of his translator. Mr. McGregor) on the Basuto tribes, upon which French and Swiss missionaries, both Catholic and Protestant, have settled with so great effect for more than interpret reality in the most concise and comprehensive terms, science advances to ever-wider generalizations of experience and the statement of laws of co-exis- tence and sequence in more and more general formulae, until the symbols it uses seem far away from, and to have little reference to, the experiences from which they took their rise. By means of such symbols or conceptual constructions it is able to form a working thought-model of the universe by which to express, as simply and completely as possible, the conditions of experience. But its concepts remain descriptive formulae for phenomenal occurrences or changes, i.e., ifor the order and connexion of our sense-perceptions. Accordingly, the road of advance — the way to union of the philosophical and the scientific standpoints — lies in the further analysis of sense-impressions, or, more generally, further elucida- tion of the nature of immediate experience, and the more precise and systematic derivation from these of the conceptions by which it is sought to explain experience. The realization of this is to- day common standing-ground to the experiential philosophers and the philosophical scientists. It is the explicit attitude of the philosophers whose conception of philosophical method I have cited ; and it finds equal expression in the insistence on the part of scientists when they incjuire into the foundations of science, of the need of justifying scientific concepts by derivation from sense-impression, and in their tentative suggestions in this direc- tion. The chief example is Mach's Analysis of the Seusatwns, with its concluding chapter on the influence of this investiga- tion on the mode of conceiving physics. But there are also sug- gestions in Poincare's Science and Hypothesis, in Ostwald's Natural Philosophy, and in Bertrand Russell's Our Khok:- ledge of the External World. Russell shows how some of the main conceptions of science, such as the indestructibility of matter or things, and a single time and space, might be stated in terms of sense-data. He defines a thing as a certain series of aspects or sensible appearances related to one another by continuity and ^^ Science of Mechanics, pp. 84-5. I30 ]'KESlDliNTlAL ADDRKSS SECTION F. causal connexion, which is ])recisely the sort of definition which modern philosophy in general tends to give, and he indicates how points and instants may be defined in a similar way." What this implies is that there is no inconsistency but rather reciprocity between the philosophical or psychological account of the actual nature of sense-experience, so long as it is not combined with uncritical assumptions, and the mathematical treatment of the very same experience in terms of particles, points, and instants, in spite of the non-existence of such entities; and that their definition in terms of actual experience, i.e., as logical functions of sense-data, is what is required to ])r()ve their applicability to reality as a thorough-going exi^eriential i)hilosophy must con- ceive it. Tn a similar strain Russell's collaborator, Whitehead, in bis little " Introduction to Mathematics," seeks to relate the funda- mental ideas of mathematics to individual sense-experience. For example, wdien dealing with co-ordinate geometry and speaking of the origin O and the two axes OX, OY. he says : " From an abstract mathematical point of view the idea of an arbitrary origin may appear artificial and clumsy, and similarly for the arbitrarily drawn axes. But in relation to the application of matbematics to the events of the universe we are here symbolizing with direct simplicity the most fundamental fact respecting the outlook on the world afl^orded to us b}- our senses. We each of us refer our sen>ible ])erce])tions of things to an origin which we call " here "" : our location in a particular part of .space round which we group the whole universe is the essential fact of our ])odily existence. We can imagine beings who observe all phenomena in all space with an e(jual eye, unbiassed in favour of any part. With us it is otherwise, a cat at our feet claims more attention than an earthquake at Cape Horn, or than the destruction of a world in the Milky Way. It is true that in making a common stock of our knowledge with our fellowmen, we have to waive something of the strict egoism of our own individual ' here.' We substitute ' nearly here ' for ' here " ; thus we measure miles from the town hall o:f the nearest town, or from the capital of the country. In measuring the earth, men of science will put the origin at the earth's centre; astrono- mers even rise to the extreme altruism of putting their origin inside the sun. But, far as this last origin may be, and even if we go further to some convenient point amid the nearer fixed stars, yet, compared to the immeasurable infinities of space, it remains true that our first i)rocedure in ex])loring the universe is to fix upon an origin ' nearly here." "''' " O/' cif., lect. iv; cf. Poincare, pp. S5-7. "A. X. Whitehead: " Iiitrodvctiuii to Matliciihitu\< ft-. ^^5-6. Com- pare with this the reflexion characteristic of the ideas advanced hj' Clerk Maxwell, which have hecomc familiar ones today, viz., that "a line is not originally a mark on the hlackboard, whicli can equally he called BA as AB, hut is the locus of a motion from A to B." Quoted from lloffding, Modern Philosophers, p. iti. i'KIiSIDliNTlAl. ADDKIuSS SECTION V. l^l The significance of this conception is that "point" funda- mentally means " here " ; " line " means '* from here " ; " instant '' means " now " ; " unit/' " particle," or " thing " means " this " — all of which imply the standpoint of the individual percipient with his actual j^resent experience. Science is all derivative from this, instead of this heing in any ultimate view an accident or incident in the real world. Absolute or conceptual space and time are constructions from the relative spaces and times oif individual perceptual experience, i.e., fundamentally from visual, tactual, and muscular sensations. Similarly, the i)rinciple of continuity is formed from the experiential fact of differences in the degree of dixersit}' Avith increase or decrease in the num- ber of terms in a series of perceptible things or phenomenal changes, the idea of absolute continuity being reached by regard- ing the number of terms as inhnite. The principle of relativity — that all phenomena are relative to the percipient or observer — is a general and far-reaching expression of this same i)oint. In general, science treats of ideal cases which are constructed by abstraction from actual experience. To the laws of such ideal cases experience approximates in proportion as it is less complex and varied. But it is immediate concrete experience that gives us direct apprehension of reality, our particular and individual apprehensions of which it is the function of the indirect or scientific conception to unify or correlate. Philosophy expresses this fundamental truth in such principles as : " A thing is an ex- perience that has been repeated." " A unit is an act of discrimi- nation." " The root-idea of distance is fatigue." " The first psychological meaning of object is oibstacle." All of these have the same general import, namely, that things are fundamentally inter])retable only in terms of actual individual experience. The position, then, is this. The entities of scientific thought are not reality. They are constructions devised to give a con- ceptual representation of reality. Their purpose is to tran- scribe perceptual experience in such a way as to enable us to know as fully, exactly, and rajjidly as possible what to expect under determinate conditions, "J'he criterion of this jjrocedurc ■ — the test of scientific constructions — is. on the one hand, their own self-consistency, and, on the other hand, their applicability. It is only by keeping to experiential terms or logical and veri- fiable derivatives from these that science is able confidently and successfully to anticipate or predict experiences. Scientific con- cepts, therefore, are valid or have objective truth, not through being direct statements of the nature of reality, but through systematizing the facts of actual experience and j^redicting resvdts that are afterwards verified by experience. It is in this sense that science is able to " exi)lain " experience, namely, by relating sense-im])ressions or other experiences to their conditions in the common or objective world. That it accomplishes this shows that its symbols or counters are trustworthy indices of reality, that they " correspond " to realit\-. though they cannot claim definitively to express reality. 1^2 PRESIDENTIAL ADbRESS^SECTION F. Now philosophy has Hkewise no just claim to any full or final expression of the nature of things. It is as worthless apart from the detailed inquiries of science as science is apart from the efifort of philosophy to unify — or (in Plato's phrase) to " see things together " as one whole. But what it insists upon is that, since immediate experience is our point of contact with reality, the suggestions that arise from it are, equally with the construc- tions of science, indispensable clues to the nature of things. That interpretative concepts originate, and must he logically derived, 'from immediate experience implies that any actuality so reached must still be of the same general nature as this. But this is just what philosophy says when it contends that reality must be continuous with our experience. Whatever its ultimate character or content, i.e., whatever it would be to experience ultimate reality, it cannot be of a nature wholly different from conscious experience— ^of which consciousness is only the aware- ness. It is actualized for us only in our experience, and any further actualization of it can only consist in further modes of experience. Matter is a limiting conception. It represents the material or stuff or substance or, better still, the nature of reality, and therefore the unknown as conditioning our experience. But the reality, though unknown in its character and content, must be thought of as realizable in further or fuller experience. Thus conceptual constructions as symbols of reality have a meaning only as instruments — somewhat analogous in this respect to such instruments as the telescope and microscope — which make pos- sible the realization or the development of further modes of immediate experience.^" In other words, reality is actually realised for us only in experience, and can therefore be finally interpreted only in terms of experience and as being continuous with experience. Philosophy expresses this by saying that all reality must be somehow akin to what we know as consciousness. Philosophy, then, is not being false to the experiential method, l)ut only Ijeing radical or thorough-going in the concep- tion and use of this method, when it suggests that not only can reality be known only by way of experience, but it can ultimately consist in nothing but ex])erience. This ]>rinciple signifies that reality or existence is meaningless apart from some kind or degree of consciousness as its correlate, just as consciousness is meaningless apart from something or another of which it is the awareness. It implies, further, that the real meaning of the economy of knowledge is that the function of knowledge, as the guide of action, is to lead through action to further experience, or that knowledge and action upon it — knowledge as enlightening " Compare on this point Clifford's allegorically-expressed speculation to the effect that " as the ph3sical senses have heen gradually developed out of confused and uncertain impressions, so a set of intellectual senses or iiisi^i^ltts are still in course of development, the operation of which may ultimately be expected to be as certain and immediate as our ordinary sense-perceptions.'' — Quoted from Sir F. Pollock's liiographical sketch prefixed to the Lectures and Essays, where the allegory is instanced. TKESIDKNTIAL ADDRICSS SKCTIOX V. 1 33 action and action as applying knowledge — are the inseparable factors in the development of concrete experience itself. Lastly, this principle means that the ultimate nature or reality of what we are wont to call things must be analogous to what we know in ourselves as experience. ]^Jore generally, everything that is real must have some kind of inner hfe of its own. I shall con- clude with a word or two on this last point. If it is asked what there is in our actual experience to sug- gest this conception, the answer is that, in a true analysis of experience, things are known to us not merely as facts of which we may l)ecome aware, but as entities of which we have to take account in our practical life, and therefore as related to our efforts and purposes. When we regard things in this way, we find it impossible to think of them only as objects of know- ledge, and not in some degree as subjects or centres of experience. Things respond in different ways to different modes of treat- ment on our part, and they exhihit differences oif quality through adaptation or facilitation. They have their own ways and habits and tendencies, their own attitude or point of view, their owai conatus in suo esse perseverarc, as Spinoza put it. There is a passage in F. C. S. Schiller's " Studies in Humanism "' ^' that ex- presses this point in a quaint but suggestive way : " A stone, no doubt, does not apprehend us as spiritual beings, and to preach to it would be as fruitless (though not as dangerous) as preach- ing to deaf ears. But does this amount to saying that it does not apprehend us at all, anfl takes no note whatever of our existence ? Not at all ; it is aware of us and affected by us on the plane on which its own existence is passed, and quite capable of making us effectively aware of its existence in our transactions with it. The " common world " shared by us and the stone is not, perhaps, on the level o:f ultimate reality. It is only a phy- sical world of " bodies," and " awareness " in it can apparently be shown only by being hard and hea\y and coloured and space- filling, and so forth. And all these things the stone is, and recognises in other " bodies." It faithfully exercises all the physical functions, and influences us by sO' doing. It gravitates and resists pressure, and obstructs ether vibrations, etc., and makes itself respected as such a body. And it treats us as of a like nature with itself, on the level of its understanding, i.e., as bodies, to which it is attracted inversely as the square of the distance, moderately hard, and capable of being hit. That we may also be hurt it does not know or care. But in the kind of cognitive operation Avhich interests it, viz., that which issues in a physical manipulation of the stone, e.g., its use in house- building, it ])lays its part and responds according to the measure of its capacity." Philosophy stands, therefore, for the recognition of the suggestions or indications as to the nature of things which spring from immediate experience — not only (from sense-impressions, "P. 442 ~~ " 134 PRESIDENTIAL ADDRl'.SS SiaXloN F. but from feelings, impulses, aspirations, instinctive or intuitive awarenesses of any kind. A cautious philosophy, like a cautious science, will not make confident assertions that go beyond the limits of probable knowledge. 'But philosophy cannot admit that the unknown reality must remain unknown. And the function and justification of philosophy lie in the fact that without its speculative ventures into the unknown, which are of the very same nature as scientific hypotheses, although vaster and further- reaching, knowledge could not advance for lack of inspiration and impetus. It is in this spirit that a genuine philosophy of experience suggests — as a hypothesis that arises from reflection on the nature of our experience and from the inspirations of life itself — that matter may, after all, be only mind in disguise, or that what we call things must have an inner nature or being- for-self which is not wholly different from our own. It is t'he same feeling of our oneness with nature that leads science to seek to reduce mind to terms of matter and philosophy to reduce matter to terms of mind. It is only the double tendency, and the gradual approach of the two through open-minded sugges- tion and verification, that can lead to further truth. " We shall then discover," says Mach, " that our hunger is not so essentially different from the tendency of sulphuric acid for zinc, and our will not so greatly different from the pressure of a stone, as now appears " ;^* or as philosophy puts it from the other side, that "if ' atoms ' and ' electrons ' are more than counters of phy- sical calculation, they, too, know us, after their fashion. Not as human beings, o!f course, but as whirling mazes of atoms and electrons like themselves, which somehow preserve the same general patterns of their dance, influencing them and reciprocally influenced."'^-' Such conceptions, in ovu* present state of know- ledge, seem unreal. But they are finger-posts on the way to truth. At all events, they are better than the attitude expressed (whichever way we take it) in the old saw: " What is mind ? No matter. What is matter? Never mind." ^^ Science of Media iiics. p. 464. "• .Schiller. /(;<•. cit. LIST OF PAPERS READ AT THE SECTIONAL MEETINGS. Section A. — Astronomy, Mathematics, Physics, Meteor- ology, Geodesy, Surveying, Engineering, Architec- ture, AND Irrigation. MONDAY, JULY 8. 1. Address by Prof. J. T. Mokkison, M.A., B.Sc, F.R.S.E., President of tlie Section. WEDNESDAY, JULY la 2. Safety in winding operations : J. A. Vaughan, M.I.C.E., M.I.Mech.E. 3. A new type of accurate sundial or solar clock : J. Moik, M.A., D.Sc, F.I.C. 4. A rapid approximate method of calculating the occultation of stars by the moon (for the Central Transvaal) : J. MoiR, M.A., D.Sc, F.I.C. THURSDAY. JULY n. 5. The desiccation of Africa : the cause and the remedy : Prof. E. H. L. ScHWARz, A.R.C.S., F.G.S. Section B. — Chemistry, Geology, Metallurgy, Mineralogy, AND Geography. TUESDAY, JULY 9. 1. Address by P. A. Wagner, Ing.D., B.Sc, President of the Section. 2. The medicinal springs of South Africa — Supplement I : Prof. M. M. RiNDL, Ing. D. 3. On the persistence of arsenite of soda in the soil : C. W. Mally, M.Sc, F.L.S.. F.E.S. WEDNESDAY, JULY 10. 4. Note on the occurrence of a peculiar phosphate of aluminium in a deposit of bat guano : B. de C. Maechand, B.A., D.Sc. 5. The determination of phosphoric oxide ; particularly in fertilisers, soil extracts, and the like : B. ue C. Marchand, B.A., D.Sc. 6. Wasted South African resources : coal and its by-products : A. Kloot, B.Sc. A.I.C. THURSDAY, JULY 11. 7. Some experiments on the fate of arsenic in the animal body: H. H. Green, D.Sc, F.C.S., and C. D. Dykman, M.A. 8. The behaviour of bacteria towards arsenic: H. H. Green, D.Sc, F.C.S., and N. H. Kestell, B.A. Section C. — Botany, Bacteriology, Agriculture, and Fores- Try TUESDAY, JULY 9. 1. Some experiments in the rudimentary teaching of Botany: Rev. F. C. KoLBE, B.A., D,D. 2. Some notes on a collecting trip to French Hoek: E. P. Phillips, M.A., D.Sc. F.L.S. 136 LIST OF PAPERS READ AT SECTIONAL MEETINGS. 3. A note on the flora of the Great Winterhoek Range : E. P. Phillips, M.A., D.Sc, F.L.S. 4. A note on the pollination of Cyanella capensis, L. : E. P. Phillips, M.A., D.Sc, F.L.S. WEDNESDAY, JULY 10. 5. Address by C. E. Legat, B.Sc, President of the Section. 6. Some photographic illustrations of South African vegetation : I. B. Pole Evans, M.A., D.Sc, F.L.S. 7. The diagnostic characters of some superficial fungi : Miss E. M. Doiuci:, M.A.. D.Sc, F.L.S. 8. Notes on the genus Balansia: Miss A. M. King, B.A. 9. Additions and corrections to the recorded flora of the Transvaal and Swaziland. II: J. Burtt-Davy, F.L.S., F.R.G.S. 10. Walnut bacteriosis : Bacterium Juglandis Pierce : Miss E. M. Doidge, M.A., D.Sc. F.L.S. 11. The bacterial blight of beans: Bacterium phaseoU Erw. Sm. : Miss E. M. Doidge. M.A., D.Sc, F.L.S. 12. A preliminary investigation into a disease attacking young Cupressus plants : Miss A. M. Bottomley, B.A. 13. Notes on the morphology and life history of Uromyces Aloes Cooke: V. A. Putterill, B.A. 14. Some preliminary observations on unseasonable veld-burning; and its possible relation to some stock diseases : A. O. D. Mogg, B.A. 15. The pepper-tree (Schinus molle) in its relation to epidemic hay fever: Prof. G. Potts, M.Sc, Ph.D. Section D. — Zoology, Physiology, Hygiene, and Sanitary Science. TUESDAY, JULY 9. 1. Problems of degeneration as represented by the ostrich : Prof. J. E. DuERUEN. M.Sc, Ph.D., A.R.C.S. 2. The pure-line hypothesis and the inheritance of small variations : Prof. E. Warren, D.Sc. WEDNESDAY, JULY 10. 3. The pineal body in the ostrich: Prof. J. E. Duerden, M.Sc, Ph.D., A.R.C.S. 4. Charts, photographs, and reports of the Rand Mines Sanitation Department: A. J. Orensiein, M.D., M.R.C.S., L.R.C.P. 5. The moth fauna of Southern Rhodesia: A. J. T. Janse, F.E.S. 6. Note on the persistence of the right posterior cardinal vein in Xenopus lecvis and its significance : R. J. Ortlepp, M.A. 7. Leucocytogregarines, and their occurrence in South Africa. Annie Porter, D.Sc, F.L.S. 8. Some parasitic protozoa found in South African fishes and amphibians : Prof. H. B. Fantham, M.A., D.Sc, F.Z.S. 9. Intoxication by gastrophilous larvae: G. de Kock, M.R.C.V.S. 10. Some South African snails and the Cercarise which attack them : F. G. Cawston, B.A.. M.D., B.C., M.R.C.S., L.R.C.P. 11. Arc the Orthoptera and Neuroptera actual orders or conglomerations? S. G. Rich, M.A., B.Sc 12. Are the Odonata of economic value? S. G. Rich, M.A., B.Sc. ^ 13. On the eradication of venereal diseases : R. T. A. Innes, F.R.S.E., F.R.A.S. 14. Some features of the South African Odonata as a fauna: S. G. Rich. M.A., B.Sc tlSV OF PAPERS READ AT SECTIONAL MEETINGS. I37 THURSDAY. JULY II. ■ ..^^ 55. Address bj' Prof. E. J. Goddard, B.A., D.Sc, President of the Section. FRIDAY. JULY 12. 36. Crossing the North African and South African ostrich: Prof. J. E. DuERDEN, M.Sc, Ph.D., A.R.C.S. 17. Drug treatment in Nuttalliosis of equines : G. de Kock, M.R.C.V.S. 38. Bovine contagious abortion in South Africa : E. M. RoBINso^f, M.R.C.V.S. iy. On certain changes in the external sex-characters of ostriches, occur- ring: after removal of the reproductive glands; Sir A. Theiler, K.C.M.G., D.Sc.. and D. Kehoe. M.R.C.V.S. 20. Discontinuous distribution in a few mammalian groups : T. F. Dreyer, B.A., Ph.D, \ Section E. — Anthropology, Ethnology, Native Education, Philology, and Native Sociology. TUESDAY, JULY 9. 1. The Natives of Natal in relation to the land: M. S. Evaxs, C.M.G., F.Z.S. 2. Native customs in relation to small-pox among the Ba-Ronga ; Rev-. H, A. JuNoo. 3. The medicine-man in Natal and Zululand : Hon. Justice C. G. Jackson : 4. The Zulu witch-doctor and medicine-man: J. B. McCord, M.R.C.S., L.R.C.P. 5. Suggestions towards a better provision for the medical needs of the Natives: C. T. Loram, M.A., LL.B., Ph.D. 6. Suggestion for the education of public opinion on native affairs : M. S. Evans, CM.G., F.Z.S. WEDNESDAY, JULY 10. 7. The engraved rock of Loe, Bechuanaland Protectorate: Miss M. WiLMAN. 8. Religious beliefs and superstitions of the Xosas : a study in philologv ; J. McLaren, M.A. 9. Arts and crafts of the Xosas : a study based on philology : J. Mc- Laren, M.A. 10. Some early geographers and explorers of Africa : Rev. W. A. Norton, B.A., B.Litt. 11. Some unrealised factors in Native economic development: Rev. J. R. L. KiNGON, M.A., F.R.S.E., F.L.S. 12. Does it pay to educate the Native? Rev. A. E. Le Roy. 13. Social conditions of Natives on the Rand : Rev. W. F. Hiix, M.A. THURSDAY JULY 11. i-|. The killing of the Divine King in South Africa: Rev. S. S. Durnan. M.A.. F.G.S. 15. The traditional history and customs' of the Makaranga (Varozwe) : E. G. How man. 16. Who built the Rhodesian ruins? W. H. Tooke. 17. Cattle as a factor in South African race relationships: Rev. J. R. L. KiNGON, M.A., F.R.S.E., F.L.S. 18. The philology of the Native Language (Zulu and Xosa) : Rev. S. G. G. AiTCHisoN, M.A., D.D. ig. Place names of Africa, No. II : Rev. W. A. NokxoN. B.A., B.Litt. 20. The evolution of a Native administration ; Rev. J. R. L. Kingon. M.A., F.R.S.E., F.L.S. 1^8 LIS'T OF PAPERS READ aT SEXTIO^AL MEETIN'GS. " 21. Central African folk-lore tales. Second Series : Rev. J. R. L. KiNGOif^ M.A., F.R.S.E., F.L.S. 22. Classification of Bantu place names: Rev. J. R. L. Kingon, M.A.. F.R.S.E., F.L.S. 23. More Sesuto etymologies : Rev. W. A. Norton, B.A., B.Litt. FRIDAY. JULY 12. 24. Address by Rev. W. A. Norton, B.A., B.Litt., President of the Section, 25. The Natives in the larger towns : J. S. Marwick. 26. Some engraved stones of the Lydenburg District (North-East Trans- vaal) : the occurrence of cup-and-ring markings in South Africa: Dr. C. Pyper. 27. Native child-life: Rev. S. G. G. Aitchison, M.A., D.D. Section F. — Education^ History, Mental Science, Political Economy, General Sociology, and Statistics. TUESDAY, JULY 9. t. Reconstitution of the Union Senate : R. T. A. Innes, F.R.S.E.,. F.R.A.S. 2. Decimal coinage: Prof. W. A. Macfadyen, M.A., LL.D. 3. Epic poetry in French literature : Prof. R. D. Nauta. WEDNESDAY, JULY 10. 4. Economic Natural History, and why it should be taught in schools ; F. W. FiTzSiMONS, F.Z.S., F.R.M.S. 5. Purpose in education: H. C. Reeve, M.A. 6. The ethical principle of equity : Rev. S. R. Welch, B.A., D.D., Ph.D. FRIDAY. JULY 12. 7. Address by Prof. T. M. Forsyth, M.A., D.Phil., President of the Section. 8. Health problems in country districts, Transvaal and Orange Free State: Jane B. H. Ruthven, M.D.. L.R.C.P., L.R.C.S.E., L.R.F.P.S., F.R.S.A. 0. Vicarious parenthood: a war suggestion: Mrs. F. McLaren. 10. Philological method of teaching classical declensions and conjuga- tions : Rev. W. A. Norton, B.A., B.Litt. SATURDAY, JULY 13. 11. War and the value of money: Prof. R. Leslie, M.A., F.S,S, 12. The kap-tent wagon : J. Y. Gibson, 139 THE PROGRESSIVE DESICCATION OF AFRICA THE CAUSE AND THE REMEDY. By E. H. L. SCHWARZ, A.R.C.S., F.G.S. (With eight text figures.) That Africa is drying up is a fact that is as apparent in the north as in the south of the continent. In the north within the historic period there was a vast population living where now the desert sand drives over the land. In the south the forefathers of the present generation have left records of forests, lakes and running rivers where to-day there are practically desert — or at least Karroo — conditions. The two great central reservoirs, Lake Chad for North Africa and Lake Ngami for South Africa, are the insignificant remnants of vast sheets of water, the old terraces of which are still to be seen like those of Lakes Lahontan and Bonneville, in North America. Even within the short period during which these regions have been visited by white men they have shrunk very considerably. This drying up is due to the fact that Africa stands at a great height above sea-level as a plateau, with an elevated edge bordering the sea; this edge I shall call the Coastal Rampart.* Inland, great rivers once traversed the continent, yielding fertility to all the lands adjoining, but the short coast streams, rising in the mountains along the edge, having precipitous courses to the sea and consequently great tearing or erosive power, have cut back into the inland basin and have drawn off the waters. Then the rain falling in the area of the inland plateau, instead of collecting in rivers which flowed placidly through the continent amid plains covered with luxuriant vegetation, was drawn off in the rocky channels of the coast streams and was hurried to the sea. This process is still going on and every year more territory is gained by the coast streams at the expense of the inland system. The study of the cause of the progressive desiccation of Africa resolves itself, therefore, into a study of the river svstem, which, as I shall show, consisted origfinally of four main streams, three flowing from the centre northwards * Livingstone, in his "' Missionary Travels." p. 474, describes how on visiting Lake Dilolo on his return from St. Paul de Loando, he came to regard Central Africa as an elevated trough, with a border of mountain ranges. He was led awav from discovering the true cause for the rivers being drawn away from this trough by a state- ment bv Sir Roderick Murrhison. that the rents by which the rivers escape have been suddenlv formed by volcanic upheavals. — President's address, Royal Geographical Society, 1852, -I40 THE DESICCATION OF AFRICA. and one from the centre southwards; these I have called the PROTO-Niger, the PROTO-Congo and the ProtO-Nile for the northern tract, and the ProtO-ORANGE for the southern. The remedy for this distressing state of affairs is the revival of the great inland sources of supply for the rainfall of the interior, the re-flooding of Lakes Chad and Ngami. While the scheme for Lake Chad involves too much expense for it to be advocated at the present time, the case of Lake Ngami is quite different. The rivers supplying Lake Ngami are actually now being stolen by the head-streams of the coastal rivers, and a quite moderate weir across the Cunene River would turn the whole Fig. I. — Map of Africa. tSiiowiNG THE Original C'orR,SF:s of the Prixoipal Uivers. THE DESICCATION OF AFRICA. 141 of the water coming down from the Angola highlands in a southern direction into Lake Ngami, instead of rushing uselessly to the sea. A second barrage at the outlet of the Ngami depression, where the Chobe River filters into the Zambesi River, would prevent the waters escaping and would fiood thousands of square miles in the Ngami and Makarikari depressions. From the evaporation from these vast expanses of water the air throughout South Africa would receive a most notable increase in moisture and the humidity of the continent would be permanently increased. The surface of water exposed when these depressions were filled was greater than that of Lakes Victoria and Tanganyika; one can judge, therefore, what an immense loss to the humidity of the continent has ensued since these have been drained. According to Chapman, the Makarikari dried up about 1820, leaving vast quantities of hippopotami, crocodiles and fish which lived in the lake, to perish, when they were devoured by vultures. Even in Chapman's time (1852-4) the Chobe occasionally flowed towards Ngami. The proposed weir at Ngoma on the Chobe would have to be, according to data hitherto published, which, however, are very uncertain, not more than 10-12 feet high. That is, taking Ngami to be 3,117 feet above sea-level and Kasungula at the Chobe-Zambesi confluence 3,084 feet ; between Ngoma and Kasungula there are the Sebuba Rapids formed by a bar of hard rock which crosses both the Chobe and the Zambesi. THE AFRICAN RIVER SYSTEM. If one glances at the map of Africa, one is at once struck by the extraordinary courses of the rivers. The Niger rises m the coastal mountains of the south-western corner of North Africa, goes north-east to Timbuktoo as if about to run through the desert, then turns right round and enters the sea on the very coast on which it commenced its course. The Congo, likewise, begins by running northwards, then turns a complete semi-circle and pierces the rampart of mountains on the west coast, instead of following the low ground up towards Lake Chad. The Nile is again peculiar in its course, and the Zambesi and Orange alone seem to run straight from source to mouth like normal rivers of the Amazon or Mississippi type^ but these appearances are, as we shall see, deceptive. The second noticeable feature in the African map is the prevalance of deserts like the Sahara and the Kalahari. There is a very widespread misconception of the nature of deserts; the Sahara, for instance, is not a waste of drifting sand as is often imagined, but has an Alpine range of mountains, the Tibesti Highlands, in the centre, and on either side are tracts 142 THE DESICCATION OF AFRICA. which may be covered with drifting sand, the " Ergs," or they may be just bare stony ground, the " Hammada," or, again, they may be covered with pebbles, when they are called " Serirs." The deserts are in actual fact seamed by great water-courses or wadys; some of these, like the Igharghar, north of Tasili, can be traced as gorges through the hills and as deep river-beds in the flats, though no water now flows down their channels, and in places sand dunes entirely obliterate all traces of them. Prehistoric stone implements for the grinding of corn are found all over the western Sahara, and the ruins of cities of stone-built houses occur, as at Taodeni, north of Timbuktoo, where settled life is no longer possible. River fish of the barbel family are found in pools in the Tasili plateau, far from any river now flowing. All these facts go to prove that the deserts are of recent origin and were at no very distant date fair portions of the earth's surface inhabited by man. Paradoxically enough, the very fact that the desert is over large tracts covered with drifting sand is proof, according to Captain Courbis, of underground moisture, which, by capillary attraction, rises through the sand and binds the grains together; were there no ground moisture the sand would all blow away as in the stony deserts or hammada. For the same reasons Foureau considered the Ergs, or areas of drifting sand, to be the broad basins of a former river system. The deserts and the peculiar courses of the rivers are causally related, and we shall see evidence in the sequel to show that the great African rivers originally ran through the deserts, giving them the requisite moisture to make them normal fertile regions, but that, owing to the diversion of these rivers by others working backwards from the coast and capturing the waters of the inland system, a large portion of the continent has been bereft of its natural supply. Before we begin the detailed evidence of the capture of the several great rivers, there are a few fundamental facts to be mentioned with regard to the topography of Africa, which perhaps are not generally recognised, but which will help us considerably in understanding this question of desiccation. In the first place, Africa is divided into two halves, the line of division being a great volcanic fissure commencing in the Gulf of Guinea by the string of islands, Anobon, St. Thomas, Price's Island and Fernando Po. Then inland, there are the volcanic peaks of the Cameroons, Mt. Atlantica, south of Yola, the Marra Hills in Darfur, and the volcanoes in the Bayuda bend of the Nile, between Dongala and Khartoum. The half of Africa north of this line lies for the most part below 1,500 feet above sea-level and that south of this line above 1,500 feet. THE DESICCATION OF AFRICA. 1 43 On the east, from the Zambesi to Abyssinia, there is a great stretch of very high ground traversed by rift-faults of such recent date that they cut across and interrupt the rivers, the courses of which had already been laid down. Here there is a portion of the country to which the ordinary laws of erosion and river development cannot be applied, and we must leave this area out of consideration. Many of the lakes m this area, indeed, have no outlet and all the drainage from the country adjoining is absorbed in the basins lying in the rift valleys. Lakes Tanganyika and Kivu have been tapped by the Congo and Victoria, Albert, and Albert Edward Nyanzas by the Nile. Lakes Rudolf and Stephanie are drainless, and in the south. Lake Nyasa is drained by the Shire. In Cape Colony, the volcanic lavas of the Drakensberg have been thrown across the drainage from the main watershed of the country and the upper courses have been turned and the waters forced across this watershed as the Orange River. The original lower courses of these rivers, the Bashee, Umzimvubu, Umzimkulu and so on, run impetuously down the steep slopes of the Drakensberg and straight to the sea. So great is the velocity of the water flowing on such a steep and so short an incline, that the erosion is very intense, and these rivers on the coast side of the Drakensberg are eating back into the mountains and are in reality trying to restore the original water-parting. In Abyssina similar features are exhibited ; the short coastal rivers are pitted against the inland system, which, whether flowing into the Nile or Congo, have to traverse the whole length and breadth of the continent, or whether draining into basins without outlet, have far less precipitous courses and consequently erode or wear down their beds far less rapidly. In far future ages the original water- parting will be restored, but the faulted mass is so broad that at present we cannot recognise the plan as we can in the Drakensberg. Africa is a great fault-block which has risen recently, speaking in a geological sense, from the sea, much as an iceberg rises when the top burden melts. The continent of Africa is different entirely from the other continents, which have as predominant features folded mountains. The folds, contemporary with the African faults, form, as it were, two concentric ripples round the fault block of Africa, the nearest ripple being the Alps-Himalayan chain of folds of Europe and Asia and the further ripple being the Aleutian Islands- Rocky. Mountains-Andean chain of America. All the waters, then, run from high tablelands, which, owing to the limited time of exposure to the effects of river erosion, have not been carved into the hills and valleys of the more familiar scenery of Europe; the topography is said to be immature. The rivers run in deep gorges separated by wide tablelands, and they flow rapidly to the sea with water- falls or cataracts in 144 THE DESICCATION OF AFRICA. at least some parts of their courses. This vigorous energy of their flow has as a result an intense destructive influence on the beds of the rivers, and erosion is more marked as a trenching or downward cutting effect than as a lateral one, such as we see in Europe, where alluvial valleys are the more characteristic. The amount of sand and gravel carried by a river depends on the energy of the stream, which is measured by its velocity; the sand and gravel dragged along by the river acts as a rasp that wears away the rocks, and hence the greater the velocity the greater is the erosion. The greatest velocity, and consequently the greatest amount of sand and boulders borne by the streams is at the sources of the streams where they commence in the hills. This portion of the rivers is, then, enabled to arode its bed more rapidly than the lower ones, and its action is called Headstream erosion. Headstream erosion is the means by which the short, rapid coast streams eat back through the heart of the coastal mountains and tap the waters of the inland system, whose waters are more sluggish. Headstream erosion has tapped the Niger and the Congo, diverting their waters from the Sahara and leaving it dry. Headstream erosion, again, has tapped the Zambesi basin from the east and has diverted its waters, which once flowed south-west through the Kalahari, and has turned it into a desert. Africa is such a homogeneous mass; its features are so distinctive, different from those of other lands, yet the same in character throughout the length and breadth of its enormous extent, that an illustration taken from one part is an explana- tion for any other area. The nature and effect of headstream erosion, then, may be illustrated by a perfect small example in Cape Colony and can be apphed to the elucidation of problems in central and northern Africa. This example occurs in the hills south of Grahamstown. A ridge of Carboniferous sandstone forms the edge of a great tableland, 2,500 feet above sea-level; to the south, the coast-shelf is a thousand feet lower, and the ridge forms, as it were, the hardened edge of a step in a gigantic staircase. On the north, a river scoured a valley in which Grahamstown lies; it flowed east by south and eventually entered the Great Fish River. The rivers on the south of the ridge, heading in the thousand-feet cliffs of a former sea-coast, have been working vigorously to breach this rampart, and three gaps have been made in it. The flrst two near Grahamstown, Howieson's Poort and Woest Hill, have simply excavated large basins in the hills and are every year stealing a little more from the northern drainage-area, with its rivers running in beds with only moderate falls. The third poort, however, is the Blaauw Krans, where the river has actually pierced the ridge and captured all the eastward- flowing water. The continuation eastwards is the Cap River, THE DESICCATION OF AFRICA. U5 Fig. 2. — Capture of the Cap River by the Blue Krantz (Blaauw Krans). 146 THE DESICCA-TION OF AFRICA. which is now beheaded, and its natural head-waters find an outlet through the Blaauw Krans gorge. The deviation is the effect of headstream erosion; the fact that a stream flowing eastwards in a natural valley made for it should turn abruptly at right angles and pierce a high range of quartzite hills, can have no other explanation, unless we have recourse to faults, of which there is no evidence. The coastal rampart of hills on the east coast, or on the Gold Coast, is similar to that of the Grahamstown mountain ridge, or Zuurberg. Substitute for the three streams, the Kariega, the Kowie and the Blaauw Krans, the Sanaga (Cameroons), the Ogowe and the Congo, or the Bandama, the Volta and the Niger, and we see on a large scale what has happened on a small scale near Grahamstown ; this fact, the capture of the inland water-system by the smaller, but more vigorously-flowing coast streams, is the great fundamental fact which explains the alterations gomg on in the physical conditions all over Africa. I have referred to the phenomenon of headstream erosion in the Grahamstown hills because I happen to live m that town, and the example is compact and complete, but quite as good examples occur in the western mountains, especially north of Ceres and generally throughout Cape Colony. In Oudtshoorn there is a further example of two parallel rivers, the Olifants, running in soft Cretaceous rocks, and the Kammanassie, running in comparatively hard Devonian slates. Here we have the conditions represented by the Niger, which flows in Cretaceous strata above the Bussa Falls, and its tributary, the Kaduna, which, originally probably of equal* extent to the Niger itself, having to erode its bed m hard granite, progressed but feebly, while the Niger spread back and absorbed the whole of the drainage behind the coastal rampart. The Olifants River has similarly spread back and worn for itself a great alluvial plain, while the Kammanassie has lost much of its original drainage area and lies in a narrow valley. The topography of Europe, Asia and Africa was laid down in the Eocene epoch. At the end of the Cretaceous period" enormous changes took place ; the whole fauna of the world was wiped out and new forms took their places. Among vertebrates, for instance, the predominant type in the Cretace- ous period was that of the reptiles, and in the Eocene the modem mammalian types were introduced. Africa, which up till then formed one continent with India, was riven by gigantic faults, and the trough of the Indian Ocean was produced. Round this fault-block the continents of Europe and Asia became ranged, with the Alps-Himalayan chains as the backbone. The destruction of life was related to these THE DESICCATION OF AFRICA. 147 convulsions in the earth's crust, and we can reconstruct from geological evidence a picture of what then went on. The earth's crust was disturbed, was broken and crumpled, as if a blow had been given it and the material were plastic like modelling clay. The convulsions were not confined to a single short period, but were spread over what would be regarded historically as an immense stretch of time, and at the end the world-segments, the continents and oceans, emerged more or less in the broad outlines in which we now see them. The movements continued during the Eocene period and altered somewhat the original plan, but we can regard these as supplementary. As a matter of fact, the barriers raised by these later movements are definitely athwart an earlier topography, and the rivers with which we are chiefly concerned are busy removing them and restoring the earlier features. It is on this assumption that the reasoning in the following pages is based, but it would take us- too far from the subject in hand to develop it fully. To put it concisely, the features of the earth's surface, its topography, its rivers, hills, coast-lines, etc., date from the dawn of the modern period, the Eocene; these were on a different plan and had no relationship to the topography of the earth's surface in earlier periods. That, in the widest sense, is a sort of master-key to the understanding of the present condition of affairs, and the changes that are now going on are alterations of that original Eocene plan. Individual terrains, when examined in detail, confuse this prime conception, because we may find that the original topographical features were laid down later than the Eocene, or, may be, earlier, as in Cape Colony, and it would be more strictly accurate to leave the period in which the stamp was set indefinite : that a stamp was set and that its recognition explains why the conditions in various countries are changing, we shall see ample evidence in the sequel. THE NIGER. The Niger rises m the granite hills of Tembi Kundu, 2,764 feet above sea-level. These hills form part of the coastal rampart which guards access to the interior from the sea on the Gold Coast and which, indeed, is a characteristic feature on the whole west coast as far as Cape Colony. It is deeply canyoned on the sea-ward side towards Sierra Leone and Liberia and the main watershed has retreated inland under the action of headstream erosion by the short, rapid rivers of the coast. Some of the heights of the original crest, like Mt. Drouple, 9,750 feet, are left isolated and far south of the watershed- On the north, the Tankisso River, flowing from the sand- s,tone hills of Futa Jallon, joins the Niger at Siguiri, which is 148 THE DESICCATION OF AFRICA. 1,100 feet above sea-level; thus the Niger has a fall of 1,664 feet in 260 miles and the rest of the course of this great river, which amounts to 2,340 miles, has to be accomplished with a fall of a little over two feet to the mile. Further down, the Sankarain River joins the Niger from the south, rising in Mt. Kon, 4,550 feet, part of the Mt. Drouple group. Finally, the two rivers, the Baoule and the Bagoe, a little further east, rise in the same way, but unite as the Bani River ; the latter, after following a course parallel to the main river for some distance, falls into the Debo Swamp. This is the first stage in the capture of the tributaries ; the Baoule and the Bagoe are hesitating in their courses, and loose themselves in a level swamp, ready to be deflected. The next river to the east, which rises in the same way from the coastal rampart, is the Black Volta; this flows northwards as the others do, but a coastal stream still further east has eaten back through the rampart, stolen the waters of the northwards-flowing stream, and this in turn has captured the waters of the Black Volta, uniting, thus, three original rivers in one great stream. A small tributary from the north, flowing into the Volta at the bend, marks the former course of the stream into the Niger.* This precisely is the history of the Niger itself, carried out on a smaller scale. The other branch of the Volta, the White Volta, does not show this diversion so clearly; its headstreams penetrate nearly to the Hombori Mountains in the bend of the Niger, and a string of lakes on the north of the mountains lie in depressions which probably mark the course of the river before its waters were captured and brought south. All the tributaries east of the Bagoe have been reft from the Niger, and a very little further erosion by the Bandama River will bring the waters of the Bagoe southwards ; then the Baoule will form a bend similar to that of the Black Volta. Its waters will flow southwards along the drained channel of the Bagoe, and will reach the sea at Grand Lahou by the Bandama River- The Bani, now forming the common conduit for the Baoule and the Bagoe, will then gradually silt up and all connection with the Niger will be lost. We shall see later, in connection with the Benue and Cunene Rivers, that some African rivers are just in this stage when the waters are hesitating as to which way they shall run, and the river with the shorter course always wins in the end, draining the area and leaving the bigger river without its natural tributaries. Not only has the Niger lost the waters of the White and Black Voltas, but, nearer its source, the Senegal River has * Attention was first drawn to this capture by R. de Lamothe, in> "Contribution a I'etude geologique des territoires du Haut Senegal - Niger." Bull. Soc. geol. Fr. (4), IX., 1Q09, p. 528. THE DESICCATION OF AFRICA. 149 invaded the drainage area of the river, and in the tributaries, the Bafing, the Bakoy and another river of the name Baoule, we see clearly by their courses that they once belonged to the larger river. The Senegal River originally began m the Tamboura Mountains, near Bafoulabe, but the short, straight course, combined with the easily-weathered, horizontal sand- stones of this area, allowed it to eat into and rob the Niger of a considerable portion of its waters. As it is, the Senegal River is steadily gaining ground in the natural basin of the Tankisso, and at some future date this great tributary of the Niger will be lost to it. The floods of the Niger extended more than a hundred miles north of Timbuktoo within the memory of man, but these inundations are far more restricted nowadays; this is usually ascribed to the drying up of the continent, but it is far more probably due to the fact that every year sees many square miles of country which formerly contributed its waters to the Niger, drained by the encroaching coastal rivers. The Senegal is the chief thief on the west, and on the south there are the Liberian rivers, the Sassandra, the Bandama and the Comoe. Thus, waters which originally went to fertilise the inland districts are now drained rapidly to the sea, and their beneficial effects are lost. Some 300 miles above Timbuktoo the Niger enters a great level plain which is liable to inundations, the waters at such times forming a lake i/o miles long and 80 miles broad. At ordinary times the waters are restricted to a reticulating system of channels and one more or less permanent lake, Lake Debo. A further system of shallow depressions extends northwards, west of Timbuktoo, the largest being Lake Faguibine and Lake Horo. All the wells dug north of Timbuktoo as far as Arouan, 200 miles north of the Niger, are in fiuviatile deposits, full of shells of Melania, Physis and Planorbis, showing the former extension of the flood-lake system. A vast region like this, with practically no fall, indicates a temporary phase in the evolution of a river system; the Niger below the Debo Swamp has not cleared its course sufficiently to accommodate itself to the new conditions. At one time it was thought that round about Timbuktoo there had been an inland sea like the Black Sea, which communicated with the Atlantic through a channel in the Adrar Highlands ; Chudeau even designated this channel as the depression El Khat (lat., 19° N.). According to Lemoine, however, all the evidence for such a sea lies solely in the presence of countless shells of Margmella, which are found strewn about in the soil round Timbuktoo. These sea-shells were at one time used as money and were probably the "cowries " which poor Mungo Park was presented with by the 1 50 THE DESICCATION OF AFRICA. Sultan of Segu ; Park estimated his present of 5,000 as being worth about twenty shillings. The cheapness and profusion of these shells would lead to the improvident natives dropping quantities of them, and hence their presence round the city can be explained. The great salt desert of El Juf, with the salt mines at Taodeni on the eastern margin, is the relic of a dried-up lake, rather than that of a sea, and further, the levels of Timbuktoo (787 feet) and Taodeni (722 feet) rule out this theory, unless we bring in movements of the earth's crust, which can only be purely speculative. To the north of El Juf there are the Ergs, regions of shifting sand-dunes, which are, according to Foureau, the broad basins of a quaternary river system. It has now vanished, but it once led north into the great Igharghar and thence to the sea by the shotts, or lagoons, of Algeria. Just south of Taodeni, Lenz marks a depression only 400-500 feet (120-150 m.) above sea-level, inviting the waters of the Niger to flow into it and to form a great central Saharan lake.* Further north, there are the oases of Twat, Gourara and Ouargla in the course of such a supposed river. Comparatively high ground lies between Gourara and Ouargla, but the whole of this area is covered with enormous thicknesses of recent debris, washed down from the Atlas Mountains; this would obscure any pre-existing river valley and would also have aided in the obstruction and final diversion of the stream. There is another possible outlet for this river system, namely, through the Adrar Highlands, bordering the west coast. At Cape Blanco there is a great estuary, between four and five miles broad, now filled in with light, friable, sandstones, that could have been the mouth of this river. This, however, would not have given the requisite moisture to the Ahaggar Mountains and allowed them to pour plentiful rivulets out into the present deserts, which, joined together, scoured the great river beds we find m these regions; the larger ones, such as the Tanegrouf, In Azoua and Tafassasset, are now, indeed, dry, but at one time they were filled with water and communicated with the sea. In the heart of the Ahaggar, in the pools, there still live the river fish, Barbus deserti and B. biscarensis, which must have originally swum up a river that flowed far from their present haunts. These central Saharan highlands are so hemmed in on all sides by vast plains, separating them from the coastal regions, that no climatic changes would suffice to bring rain-laden clouds in such quantities as to allow of their giving rise to great rivers that could flow the 1,200-1,500 miles to the coast, unless the * See Lieut. Cortier's " Route March from Timbucktoo to Taodini." La Geographie, 1906, pp. 317-341. THE DESICCATION OF AFRICA. 151 plains around them were moist with an irrigation brought there from more favoured regions. On the north of the Ahaggar massif, which is of granite (Mt. Hamane, 7,150 feet), the great Igharghar waddy cuts first a deep canyon through the Tasili, or plateau, of the Azdjer, consisting of Devonian and Carboniferous rocks, and then becomes lost under the great Erg, or region of shifting dunes. On the north of the Erg, the wady reappears and its course is marked by wells and irrigation works, showing the presence of abundant underground water. It seemed possible at one time, that the Lake Chad might have discharged its waters northwards and, through a rift in the Ahaggar high- lands, have led down into the Igharghar, but the documents of the Foureau-Lamy mission are so definite as to the great escarpment facing south and barring all drainage from south to north, that one had to abandon the idea. To come back to the Niger, the river, after leaving the neighbourhood of Timbuktoo, enters the Burrum Gorge, flowing in it due east for 250 miles in a trench scarcely 300 feet wide. Thence it follows along the junction of granite on the south-west and soft Cretaceous and Eocene rocks on the north-east, until it reaches the Falls of Bussa, where Mungo Park perished. Here the granite stretches across the river in a comparativeh' narrow bar and. forms, on the east, the continuation of the coastal rampart, which rises near Bauchi to 6,400 feet. The Niger in this region consists of two branches, the Niger proper and the Kaduna River- Both originally rose in the coastal rampart. The Kaduna has eaten back by headstream erosion, but, its upper tributaries draining a compact granite area and having only hard rock to work on, has not progressed far into the interior; the Niger, on the other hand, having only a narrow bar of hard rock to eat back through, and, behind that, the soft rocks of the Cretaceous and Eocene formations, has tapped the whole of the drainage area behind the coastal rampart. The course of the Niger between Timbuktoo and the Bussa Falls, was once a river rising on the north of the coastal rampart and flowing north-east. The region of dead water in the Debo Swamp indicates where the two northwards-flowing rivers originally met. The stages in the erosion of the rivers of the Gold Coast are so complete in their varying degree of reaching the coastal rampart, and the action is so similar, on a large scale, to what is found going on in so many of the rivers of Africa, like in the Kowie, that one is justified in drawing the conclusion that the Niger once flowed into the Sahara and made it a habitable region. The fact that has enabled the Niger to work this act of spoliation is the sudden thinning 152 THE DESICCATION OF AFRICA. of the bar of hard rock at Bussa, which elsewhere guards the drainage of the interior, and the presence, behind it, of soft uncompacted strata. The future development of the Niger region is full of disaster for North Africa. The Volta has completed its spoliation; the Bandama is busy stealing the Bagoe and Baoule tributaries; the vigorous headstreams in Sierra Leone and Liberia are eating into the area of the upper Niger, and some time in the future this will drain to the sea by the St. Paul or the Moa River; the Senegal River is stealing into the basin of the Tankisso River. Thus, the ultimate evolution of the south-western Sahara will result in an absolutely waterless desert. Not one of its present streams, whose waters reach the sea by such a long route, can compete with the boring headstreams of the coast rivers. The only thing that would prevent the fulfilment of this would be a bodily tilting of the whole continent, and such readjustments, due to the lightening of the earth's crust by the mass of rock weathered away and carried to the sea by the rivers, and also by the absence of millions of tons of ground-water that now permeate the soil, have taken place in the past, and may do so again in the future- For the geology of this portion of Africa I have used the work of P. Lemoine in Steinmann and Wilken's " Handbuch der Regionalen Geologie," and for the. topography, geology and archiology of the central Sahara the two volumes of the "Mission Foureau-Lamy," Paris, 1905. THE BENUE. This great tributary of the Niger is, at its confluence, a larger river than the mam stream; it comes fresh from the Adamawa Highlands and the coastal rampart hills, whereas the waters of the Niger have come a very long way, and have visited the outskirts of the Sahara. The Benue, in the original plan, began in the coastal rampart, or escarpment, through which it has now cut back. The physiography of the country immediately adjoining the stream is very characteristic. Above Yola, where it occupies a river-bed in which the waters formerly flowed towards Lake Chad, instead of away from it, there is the same deep, narrow channel that we saw in the Niger, below Timbuktoo, and which we shall see again below Stanley Pool, on the Congo, and m the Kebrabasa Falls, on the Zambesi. Below Yola, where head- stream erosion has been in play, the coastal rampart appears as two great ranges bounding the valley, at some places approaching, at others retiring some distance from the river. It is very instructive to compare this river gorge with that THE DESICCATION OF AFRICA. I 53 in which the Congo flows below Stanley Pool; here the Congo flows ni a steeply inclined river-bed, interrupted by continual rapids; whereas the Benue, breaching the same rampart, is navigable throughout, with a fall of only one foot in the mile. In other words, the cutting of the breach, in the case of the Congo is of much more recent date than in the case of the Benue- This leads one to the question of what happened to the waters of the Congo before the breach was made? The answer is that it flowed north to Lake Chad, but I shall develop the evidence for this later. The Benue has had, however, long ages of thieving to its credit, and its tributaries are everywhere stealing into the basin of Lake Chad. Captain Lenfant, starting from Garua, on the Benue, ascended the river in a small boat, the Benoit -Gamier, drawing two feet of water; by following the Moakebi River he actually reached the Tuburi Swamps, and thence, descending the Logone River, he reached Lake Chad. At Bmdere-Moundang he had to take the boat to pieces and carry it for twenty miles before reaching the Tuburi Swamps. The whole of this Tuburi region is one of hesitating flow, like round the Etosha Pan, that is still connected with the Cunene River in flood time; a deserted river-bed to the south of the present one connects the Kebi River with the Tuburi Swamp. To the north and south of the upper Benue tributaries can be seen on the map interdigitatmg with the Chad affluents; it is only a question of time before the whole system of rivers flowing into Lake Chad will be captured by the Benue and diverted to the Atlantic. The robbery is actually proceeding under the eyes of living men; Lake Chad is yearly becoming less extensive and the desert sands are filling it up. We can, then, compare the Logone and Shari Rivers, which are in the course of being diverted to the Benue, to (say) the Kasai and the upper Congo, which have actually been diverted to the Atlantic. The direction these rivers take is the same: a direct northerly run, then west, and then south. The whole of the Congo drainage, the whole of the Lake Chad drainage, once poured north into the Sahara ; first the Congo portion was filched, and next the Chad portion is going. THE CONGO. The plan of the Congo River as it exists at present is surely the most puzzling of any river system in the world. There are three sections. The first is the section from the Kwango River to the Sankuru River, where some twenty great rivers flow from the highlands of north Angola, in almost straight courses, due north, and then are collected by a river flowing due west. Two of the northwards-flowing 154 THE DESICCATION OF AFRICA. rivers, the Lomami and the Lualaba, further east, have not been tapped by the westwards-flowing river, but continue their northward course for another three hundred miles, till the Aruwimi River, flowing west, cuts them off; this is the second section. The third section is the Ubangui-Welle River, which flows west from the mountains about Albert Nyanza, and then turns south. All the water poured forth by these great rivers ponds up against the coastal rampart and forms the Stanley Pool, from which it flows over a series of cateracts to the sea. On the northern bank of the Ubangui River rise the tributaries flowing into Lake Chad; the Gribingi and Fufa Rivers actually rise some seventy miles north of the Ubangui. The watershed between the Gribingi and the Ubangui is about 400 feet high above the Ubangui stream- level. Just at the bend of the Ubangui the Tomi River has a course similar to that of the Black Volta; it rises in the hills, about fifty miles north of the Ubangui, flows north towards Lake Chad, and then makes a complete semicircle and flows south into the Ubangui. This shows that the rivers are more vigorous on the south of the divide than on the north. The opening of the poort through the coastal rampart, to let through the waters of the Congo, is fairly recent, but it has allowed the rivers to scour their valleys very considerably, and a scour of 400 feet is not a very large one to assume. In Cape Colon}', in the Eastern Province and the Transkei we see valleys which have cut deep, narrow canyons four times as deep. Raise the level of the rock barrier at Stanley Pool and the whole water-system behind will be checked ; if the elevation be sufficient the whole drainage of the Congo would pour into Lake Chad- The following are the heights above sea-level: — In the bend of the Ubangui, Zongo In the bend of the Ubangui, Banzyville... Mean-mouth of Tomi River (about) Highest point in the Ubangui-Gribingi divide Stanley Pool In other words, it requires an elevation of 485 feet at the mouth of the Tomi River to empty the Ubangui River into Lake Chad, and an elevation of 897 feet at Stanley Pool to empty the whole of the Congo waters into Lake Chad. There is a poort in the Zwartberg Mountains, in Cape Colony, called Meiring's Poort, in which the mountains rise to 7,000 feet above sea-level, while the level of the river is 1,000-1,200 feet, giving a depth of a river-cut gorge of 5,800-6,000 feet. Throughout the coastal mountains of Cape Colony there are similar poorts cut by the rivers since the Cretaceous period, Difference Feet. Feet. 1,287 1,384 1,335 ... 1,820 ... 485 ■ 923 ... 897 THE DESICCATION OF AFRICA. 155 and there is nothing, therefore, to stop one assuming that a river of the vokime of the Congo in flood may have cut down some 900 feet in comparatively recent times. The whole plan of the river system on the inside of the coastal rampart shows that the barrier existed quite recently, and that the rivers have not yet had time to adjust their beds to the changed direction of flow. The Kwango River and all the northwards-flowing rivers, as far as the Sankuru River, now deliver their waters to the Congo by the Kwa River, but the first ten or a dozen apparently gathered together and ran north through the Leopold II. Lake and Lake Tumba, from here, northwards, along the valley of the Ubangui River and thence down the Gribingi River to the Shari River and so to Lake Chad. The next eight or so of the northwards-flowing rivers originally took a similar course, but all trace of them has been lost in the great plain in the embrace of the horseshoe of the Congo; this area is now drained by rivers flowing west and which rise quite abnormally close to the left bank of the Lomami River. The next two rivers, the Lomami and the Lualaba, maintain a northernly course for a greater distance before being deflected westwards ; their original courses were, probably, across the flat divide, between the Congo and the Ubangui River, which is some 120 feet above the level of the main stream, and found an outlet into the Ubangui River some- where near where the Welle River now enters that river. The progressive stages of the deflection of the northwards-flowing rivers, as one passes eastwards, is very instructive ; near the breach in the coastal rampart, the rivers have been drawn closely in, and as one goes further away, the westerly drag becomes less and less felt. The whole horseshoe of the Congo, from Stanley Falls (1,391 feet) to Stanley Pool (923 feet) has a fall of 478 feet; as the distance is quite 1,000 miles, this gives an average fall of less than half a foot in the mile. Lake Chad is 81 feet lower than Stanley Pool, but from Stanley Falls it is 200 miles further, so there is a nice balance between the two outlets. To appreciate this, one must obliterate all valleys as they now exist and think of the country as an inclined, featureless plain ; we then see that the rivers, were they free to flow without their present confining banks, would have very little choice between Stanley Pool and Lake Chad ; in practice, however, the more vigorous coastal streams always prevail over the more encumbered ones of the interior. Stanley Pool has absorbed the Congo drainage for a very long time, but the sluggishness of the river above the Pool shows that the capture has not been so very remote. The horseshoe of the Congo represents the bend of the Niger 156 THE DESICCATION OF AFRICA. above the Bussa Falls, but the original outlet to the north is not so clearly marked in the case of the Congo as it is in the case of the Niger, at Timbuktoo. The crest of the coastal rampart is a range of hills„ nearly half-way between Stanley Pool and the head of the estuary, at Matadi, culminating in Mt. Ulia, 3,430 feet. From this ridge the Congo originally flowed west to the sea, like the rivers to the north, the Chiloango, the Nairi Quilo, the Nyanga and others. The next great river to the norths however, the Ogowe, has eaten back through the coastal rampart and is making a bid for the inner drainage of the continent. With two rivers equally vigorous, tapping the same source, the river traversing the softer rocks wins. The escarpment rises to 4,500 feet at Mt. Otombi, where the Ogowe traverses it and generally, with this coastal rampart, it may be taken that the higher the peaks, the more massive and more resistant to the agencies of weathering they are. There is an interesting example of complicated river capture in the Dscha tributary of the Sanga, a large river that enters the Congo, just below the Ubangui confluence. It rises in the south of the Cameroons and flows westwards, as if to join a coast stream, the Nyong River, which is just south of the Sanaga River. This Nyong River pierced the coastal rampart and was stealing the waters of the interior, when the great thief, the Congo, seized the prize, and the Dscha now turns round in a semi-circle and flows eastwards. Tributaries of the two rivers, the Sso of the Nyong River and the Lobo of the Dscha, come very close to one another. The struggle for territory is very keen in this area. The affluents of Lake Chad, the original owners, are steadily retreating northwards, as the Sanaga and other coast streams invade their basins. The Congo, in turn, through its western affluents, bringing every year more force to the head streams as the lower river becomes cleared, is steadily filching from the Lake Chad area and the conquered territory of the coast streams. LAKE CHAD. Lake Chad lies 842 feet above sea-level. It is a sheet of water that is rapidly diminishing from the filching away of areas originally draining into it, by more vigorous streams from the west and south. It is not a lake in the ordinary sense of the word, with well-defined basin, but falls into the category in which are Lake Ngami, the Etosha Pan, Lake Leopold II., Lakes Debo and Faguibine on the Niger and the Bahr-el-Ghazal on the Nile. That is to say, Lake Chad is part of a river system that has been blocked up and is evidence THE DESICCATION OF AFRICA. 157 of the diversion of the general drainage of the country, which is in the act of being consummated. On the west, the natural boundaries of the Lake Chad drainage area is the coastal rampart in the Cameroons and Fig. 3. — iST Stage. — The Nyong and the Dscha Rise in the CoasTAl Rampart. Fig. 4. — 2ND Stage. — The Nyong eats back through the Coastal Rampart and captures the Inland Drainage. Fig. 5. — 3RD Stage (Present Time).^-The Dscha has Re-captured Two of its Head-streams. Q C < • P CAMEROONS \y LOKUN •7 The Struggle for Drainage Area in the Cameroons. 158 THE DESICCATION OF AFRICA. Nigeria ; this is continued into the Sahara, through the high- lands of Air, or Asben, up to the Tasili, or Plateau, of Azdjer. From this side only two affluents now reach the lake, the Kamerduga Yobe, from the direction of Kano and the Jedseram, to the south. The Benue thrusts itself boldly into the south-western drainage area, and on the north-west the Saharan highlands have now no moisture to contribute to waters of the lake. There is, however, an oasis in the desert, east of Air, called Agram, which owes its existence to under- ground moisture. These oases, as one learns from the Igharghar, are on the courses of dried-up streams, and the underground rivers are relics of former streams that flowed above ground. On the south, the Lagone affluent is being filched by the Benue, through the Tuburi Swamps, and there remains only the Shari River, with its many tributaries, as a constant and settled contributor. On the east, there is the Bahr-el-Ghazal, which has nothing to do with the Nilotic river of that name. The eastern boundary of the Chad basin is formed by the Tibesti High- lands and the Ennedi Hills; one would expect these to drain towards the lake. One finds, however, that at the foot of the Tibesti Highlands there are places, visited by Nachtigal, which are 350 feet below the level of Lake Chad. This is evidence that the waters of Lake Chad are held up by silt and sand above the normal height, and explains the expansion of the river into a lake; it also shows that this river system once flowed from the lake towards the Tibesti Highlands in an easterly direction. The whole system of wadys on the western side of the Tibesti Highlands is collected by larger wadys directed towards the south-east ; that is to say, when there was sufficient water to fill these wadys, it did not flow towards Lake Chad, but turned round southwards and made for a gap in the Ennedi Hills. The inclination of the Bahr-el- Ghazal is in the same sense eastwards. The Bodele and the Djourab are districts lying under the Ennedi Hills, at the eastern end of the Bahr-el-Ghazal, with a general level of some 200 to 300 feet below that of Lake Chad. According to the geological map of this region, by Captain Arnaud, the depres- sion of the Bahr-el-Ghazal lies within a semi-circle of high granite hills, Tibesti on the north and a series of heights to the south, about Wadai ; these connect with the granite of the coastal rampart. The Shari and Logone Rivers pass through a gap in the granite hills. Between the Tibesti massif and the southern one, there is the gap of the Ennedi Hills, which are composed of horizontal sandstones, such as Foureau has made us familiar with in the Tasili, or Plateau, of Azdjer, which lies to the north-west. Foureau found this latter breached by a vast canyon, in which the Igharghar once flowed from the THE DESICCATION OF AFRICA. ISO C/circbceotui I Jci£e^c Fig 6. — Lake Chad. watershed on the south. The expedition of Captain Arnaud visited the southern end of the Ennedi Hills and no outlet was observed through the escarpment. Such an outlet may exist, although it may not be visible from a distance. Many of the deepest poorts cutting the coastal mountains of Cape Colony, like Meiring's Poort, cannot be identified from a distance, nor l6o THE DESICCATION OF AFRICA. would a way through the mountains be suspected by anyone approaching to within even a few miles of the poorts. It is the general rule among geographers to make the Tasili-Tibesti-Marra Hills line a great water divide for this part of Africa, but there is no real reason for maintaining this. I would rather divide North Africa into three partitions, served by three northwards-flowing rivers, the Proto-Niger, the Proto- Congo and the Proto-Nile. Besides the fact that the gradient of the rivers is inclined from Lake Chad towards the Ennedi Hills, which is similar to the case of Lake Faguibine on the Niger, with the depression near Taodeni, 300 feet below the level of the lake, there is a further parallel between the Niger and the Chad systems. At Taodeni, there are vast deposits of rock-salt, filling in synclines of the older rocks and often outcropping on the surface. To the east of the Djourab depression, on the other, that is, the east side of the Ennedi Hills, there are the salt mines of Domi. In the case of Taodeni, we ascribed the salt deposits to the drying up of an inland lake, like the Great Salt Lake of Utah; the same applies to the salt deposits of Domi. The water to fill such a lake must have come from the Lake Chad direction, for the Tibesti Highlands could never of themselves have aff^orded sufficient moisture to fill it, seeing that they are entirely isolated by immense stretches of desert. Further, we find east and north of Tibesti the great depression of the Libyan Desert, filled with shifting sand-dunes; there is still abundant underground moisture, however, which comes to the surface in the Kufra Oases and, further north, in the Oasis of Augila. The Tibesti Highlands culminate in the volcanic peak of Tusidde (7,800 feet). Nachtigal found the valleys on both sides of the range, with flowing water and with apes, gazelles and birds to enliven the scenery. The moisture to maintain this state of affairs is drawn from the depressions of the Djourab, Bodele and Chad, and is precipitated by the cold surface of the high peaks of the Tibesti range. The rivers now disappear in the sand at the foot of the hills, and what we now see in the shape of animal and plant life is a relic of a time when the whole district was not only much more moist, but was connected by fertile plains with the rest of the habit- able parts of Africa. Until an actual outlet to the east has been found for the Bahr-el-Ghazal, our arguments cannot amount to more than a surmise, but the evidence seems sufficiently strong to indicate that the Congo once flowed north along the Gribingi and Shari Rivers to Lake Chad. If that was so, then there must have been an outlet through the gap, we suppose exists, between the high granite hills to the east, a gap which apparently is barred THE DESICCATION OF AFRICA. l6l by the horizontal sandstones of the Ennedi Hills. Once through the gap, the course of the Proto-Congo would lie past the oases of Kufra, which cover 7,000 square miles of fertile ground in the centre of the Libyan Desert; thence to Augila and so out to sea in the Gulf of the Great Syrtis. On the west of Augila, there is a valley, between the Tasili and the Azdjer, on the south, and the Black Hills on the north, in which lies the great oasis of the Fezzan. It is a very large, fertile district, with vast, dry river courses directed towards our supposed former river, as if to join it as tributaries. Here, again, we have evidence of a former, much more plentiful rainfall. At Augila, there is a great wady, the Bessame-Schecherre, which is in the form of a horseshoe, with the rounded end point- ing south. This rounded end would have received our sup- posed Proto-Congo ; the eastern portion was connected with the Nile through the Oasis of Siwa and the Bahr-bila-ma, while the western branch led to the sea. At one time it was thought that the Augila Oasis, together with the depressions to the east, formed an arm of the Mediterranean; this theory was due to a wrong estimation of the height of Augila above sea-level. Rolfs first put this height as 100 feet below, but later measure- ments have fixed it at 130 feet above the Mediterranean level. From this supposed inland sea, the great fertility of the Fezzan, in early historic times, was thought to be due ; this, however, would be far more naturally explained by the fact of the Congo waters flowing through the desert and fertilising the neighbouring lands, as one river, the Nile, still fortunately does. On the coast, north of Augila, is the Barka Plateau, where about 600 B.C. flourished five cities of the most astonish- ing luxuriance, Gyrene, Apollonia, Arsinoe, Berenice and Barke (Ptelomais), constituting the Pentapolis of Cyrenaica. One can picture the condition of things in those times. The great river passing the Tibesti Highlands, which, precipitating the moisture drawn from the fertile valleys at their base, sent many tributaries to join it ; from there to the sea, a well-watered land, with pastures stretching eastwards till they united with those along the Nile and, on the west, the whole of the Fezzan a continuous tract of luxuriant vegetation. All the wealth of this back country reached the cities of Cyrenaica, which attained an opulence quite unexplainable on other grounds. Then the coastal river, far to the south, eating back through the coastal rampart, tapped the headstreams and, century by century, captured more waters, till the whole of the Congo drainage was diverted ; the head of the river system then began where the Gribingi now does. Then the Benue, eating inland, captured a great part of the effective drainage area still left. The river flood was no longer able to surmount the barrier of i62 THE DESICCATION OF AFRICA. the Ennedi Hills and the fair country along the river, of which a sample can still be seen in the Oases of Kufra, became " A region of emptiness, howling and drear, Which man hath abandoned, from famine and fear." The filching of drainage areas by the Benue is still going on and is reacting on the Libyan Desert to its disadvantage by lessening the flow of underground water. How recent these changes are can be realised by the fact that when Rolfs in 1874 set out from Dakhel Oasis in Egypt to cross the desert" to Kufra, by a track that had been in use from time immemorial, he found that dunes had risen across the route to such an extent that it was no longer a practicable course. THE NILE. Of the three great rivers which flowed north and fertilised North Africa in ancient times, only one remains, the Nile. Owing to recent volcanic eruptions north of Lake Kivu, the drainage area of Tanganyika and Kivu has been cut off from the Nile, but before this happened the northerly course of the Nile was as long as that of the Proto-Congo, from the Congo- Zambesi divide to the Great Syrtis Gulf. Curiously enough, Livingstone, when exploring Lake Nyasa, was told by a native that Tanganyika was of the same shape as that of Lake Nyasa, but that the outlet was on the north of the lake, instead of, as in Lake Nyasa, on the south ; as the native had not seen this himself, Livingstone dismisses the statement as a piece of Arab geography, but the fact remains, that the M'fumbiro volcanoes, north of Lake Kivu, have only recently been thrown up; it may well be that the Arab slave-hunters, not long before Living- stone's time, did actually see Tanganyika discharging north- wards, into the Nile. The Nile, however, is by no means a simple river, and there is abundant evidence that important changes have taken place in fairly recent times. The most striking feature is the S-shaped bend in the Nubian region, stretching across the southern bend from some distance above Khartoum to Ambukol, where the river runs south-west, and then resumes its northerly course, there is a deep channel, the Wady Mokattem. It is now dry, but it once was the main stream of the Nile, making a straight course for the Blue Nile, from the Ethiopian uplands, in a north-westerly direction. There is no question here of headstream erosion, or river capture, for the volcanoes in the Bayuda bend of the Nile, Magaga, Ghilif and Ghekdul, are the cause of the deflection, that is to say, the accumulations of lavas and ash piled up to such an extent that they turned aside the river. The Blue Nile, then, ran north- west, down the Wady Mokattem to Ambukol, thence along the THE DESICCATION OF AFRICA. 1 63 bed of the Nile to Amara and then out into the desert, past the oases of Charga, Dakhel and Farafra. The Atbara, also, flows north-west from the same high- lands as the Blue Nile ; it joins the Nile above Berber and flows m a straight course to Abu Hamed and then turns south- west. Again, a deep wady continues the straight course of the original Atbara, cutting across the bend and joining the present Nile at Asaki, above Assuan ; this is the Wady Galgabba, with its northern continuation, the Bahr-bila-ma, " the river without water " (not the river of the same name we mentioned in connection with the Siwa Oasis). The Nile, then, originally w'as two rivers running parallel. Owing to the failing of the Proto-Congo and the conversion of the open country into a desert and consequent filling of the river-bed with sand and, also, probably, owing to the lowering of the bar of syenite at Assuan by the erosion of the river, giving the more easterly stream a more drawing power than its western neighbour; the former worked back by a side-stream across the divide and tapped the western stream. The lakes of Charga then dried up. In Upper Egypt, the Libyan Desert commences at the foot of the escarpment of Lower Eocene rocks, that form a plateau between it and ttie Nile. Underground water is plentiful, as the oases indicate, and underground water is everywhere asso- ciated with former streams above ground. We have reason, therefore, to continue the western Nile on the desert side of the escarpment, to Siwa, where there is the Temple of Jupiter Ammon. Here was once a populous Roman city with every evidence of abounding fertility in the country around it. There is the other " river without water," the Bahr-bila-ma, here, which is connected with the present Nile through the Fayum. The Fayum is a depression into which a western branch of the Nile, the Bahr-el-Yussuf, discharges, and there is still a lake, the Birket-el-Qurun, in the depression, that serves as an illus- tration of what existed in most of the oases in bye-gone times. The Bahr-el-Yussuf leaves the Nile a little below Assuan and flows parallel to it for 120 miles; in the same way the original western Nile, leaving its present course at Amara, flowed on the western side of the Libyan Desert escarpment and discharged into the Charga Oasis. There are two areas of lake-deposits here, with salt-pans, indicating the connec- tion of the oasis with running water m former times. From Charga the escarpment runs westwards; following the foot of the hills, one comes to the oasis of Dakhel (Dakla), which is of a similar nature. Thence the plateau trends north-west to Farafra. Siwa and Jarabub Oases lie at the foot of a table- land composed of sandy Mid-Tertiary deposits, that separates the Lib}'an Desert from the sea and the escarpment runs, ]G4 THE DESICCATION OF AFRICA. somewhat irregularly, east and west. These places were ■ connected at one time with the present Nile by the Bahr- bila-ma, but if the western Nile did flow on the desert side of the plateau escarpment, as there is reason to believe it did, then, at an earlier stage it must have penetrated here also. There are a number of salt-marshes, or sebkhas, between Siwa and Jarabub, that are fed by underground water; they form a series of depressions connecting Jarabub with Augila. Rolfs conceived the project of transforming this chain of oases into an inland gulf by admitting the Mediterranean waters through a cutting to the Wady Fareg or the Bir Rassam. A waterway, he thought, might thus be opened far into the arid Libyan Desert, the climate improved and Cyrenaica converted into an island in the middle of the Mediterranean- Rolfs himself, however, gave up the idea after his expedition into the Libyan Desert, when it was found that Siwa alone with its eastern extensions fell below the level of the Mediterranean (Siwa -98, Sittra -80, and the Birket-el-Ourun - 141 feet). Augila and Jalo were, on the contrary, found to stand 130 and 296 feet respectively above sea-level, so that the marine inlet cannot have pene- trated very far in recent geological times. Rudaire had a similar project in connection with the shotts of Algeria. Beyond these marginal floodings, no engineering feat can bring the Mediterranean into the Sahara, because it stands much above sea-level. In 1877 Donald Makenzie proposed a plan for opening Central Africa by flooding the Sahara; he published a book, "The Flooding of the Sahara," which was widely read, and is the reason that the idea is so prevalent. There are no facts to support Makenzie. As bearing on the question of the Proto-Congo, we find a very large western tributary of the Nile coming from the volcanic region of Darfur ; this is the Wady Malik, that joins the Nile at Old Dongola. Nowadays the Marra Hills have no moisture to spare for the plains and the fact that a very large river once took its rise in these hills, shows that the climatic conditions were very much more favourable at one time. According to our arguments, the Marra Hills lay in the bend of. the Proto-Congo and its once copious rainfall is readily explained by this fact. In the Sudan, the Nile has a swampy region, like Lake Chad, called the Bahr-el-Ghazal. There is a more or less well- defined river-bed which bears this name, but it has practically no fall. On the east, the Sobat enters the Bahr-el-Ghazal on the same course, but flowing in the opposite direction, and if both rivers are in flood at the same time there is a great congestion of water at the confluence. It is an axiom that when a river system contains such a region of dead water, THE DESICCATION OF AFRICA. 165 or when two rivers meet in such an unnatural manner, that changes have taken place recently, and that the river has not yet adapted itself to the new conditions. Here, however, we come up against the Rift-system of East Africa, which is a region of block uplift as well as of trough faults, and the whole original plan of drainage is obscured. One is tempted to suggest that the original river-bed extended from the Marra Hills as the Bahr-el-Arab, then down the Bahr-el-Ghazal, down the Sobat and out to sea by the Juba River; that the mountains of block uplift rose across this and turned the Sobat from a south-easterly flowing river to a north-westerly one. Given sufficient time and no further shifting of the earth's crust, the Juba River will eat back through the high- lands of Abyssinia, tap the Sobat and actually cause such a river to come into existence. At the time when such a condition of things obtained, the Rift Valleys of the Red Sea and Gulf of Aden had not yet been formed, and Arabia was joined on to the continent of Africa. Africa then was a symmetrical block, with a central extension north and south, together with a northern cross-piece, the West African shoulder being balanced by the Arabian shoulder on the east. The central portion was drained and fertilised by the Proto-Congo, flowing from the Congo- Zambesi divide to the Great Syrtis Gulf. On the west the Niger and the Igharghar drained the country from south to north and on the east; the Arabian shoulder was drained by the twin Niles. The whole of the continent was then as well watered as the North American Continent. With the Rift system we cannot deal here, but for the rest, the drying up of North Africa is due to the capture and diversion of its natural river system whereby the waters which once tra- versed the continent are now hurried in short, precipitous courses to the sea- SOUTH AFRICA. In South Africa we have the central depression of the Kalahari, surrounded on all sides by high ground. In the centre lies Lake Ngami, corresponding, in many respects, with Lake Chad. East of Lake Ngami there is another great depression, occupied by the Soa Salt Pan and the Ntwetwe Pan, and constituting the Makarikari depression. The Soa Pan. covers an area of about 2,000 square miles and is 56 miles from north to south; the Ntwetwe Pan is 86 miles long, by 5-8 miles broad. If the whole of the Makarikari depres- sion, which lies some 150 feet below the level of Lake Ngami, were to be filled by the overflow from that lake through the Botletle River, a lake of 15,000 square miles in area would 1 66 THE DESICCATION OF AFRICA. be created, a sheet of water about double the size of Tangan- yika and more than half the size of Victoria Nyanza. The Soa and the Ngami Lake are connected by the Botletle River and the relationship between the two is the same as that between the Bodele and Lake Chad, the Botletle River representing the Bahr-el-Ghazal. To the south-west of the Soa Pan there is another pan, Andersson's Vley, con- nected by a dry river-bed, or "omuramba," with the Soa system, and from here to the Molopo River there are the sand hills of the Kalahari; these are what the French call " Ergs morts," that is, dunes that have been anchored by vegetation. The sand belt occupies the centre of the course of the original great river of South Africa, which T am going to call the Proto- Orange, in accordance with the nomenclature adopted in the case of the North African rivers. This river failed owing to the capture of its head waters- The original central South African river, this Proto- Orange, rose in the highlands about Tanganyika and is now called the Loangwe River. This flows south-west and joins the Zambesi near Zomba; thence it originally flowed up the channel of the Zambesi to Wankie, where it met the Batoka basalts, and then followed a course parallel to the Deka fault, in a valley, the Gwai Poort, still open to it, to the Soa Pan. From the Soa Pan it flowed to Andersson's Vley and the Molopo River at Mokopon, and so out to sea by the lower Molopo and the Orange River. Livingstone, in his " Mission- ary Travels," 1857, p. 477, alludes to the ancient river which once flowed from the Linyanti (Chobe) basin to the Orange River, so I am stating no new idea of my own, but rather developing the facts recognised by actual travellers. The original coastal rampart, on the east, was the Kirk range, that skirts the western shore of Lake Nyasa and is continued on the south, as the Melsetter Range; this latter forms the boundary between Southern Rhodesia and Mozam- bique. The original Zambesi rose in these hills and flowed south-east to the sea. On the inland side the river ran in its present channel, but north-westwards and then west- wards, to join the Loangwe River. The original rampart is now much degraded by weathering and erosion where the Zambesi traverses it; at one time it was, judging from some of the peaks left standing, like Mt. Dombo, 6,240 feet, at a general average height of 6,000 feet, which is a constant level for all the coastal ranges of South Africa- From this range the Zambesi had a run of 350 miles to the sea, or a fall of 17 feet to the mile. On the inland side the river had a course of between 2,500 and 3,000 miles, or about two feet to the mile; in other words, the erosive power of the coast THE DESICCATION OF AFRICA.- 167 stream was eight and a half times greater than that of the inland one. The place where the Zambesi originally rose is now occu- pied by the Kebrabasa Cateracts, which, have a fall of i6d feet. On the right bank stands the mountain Zakavuma and on the left, Morumba, some 3,000 feet high. The river is jammed between these two mountains in a channel with per- pendicular sides and less than 50 yards wide; the rocks are water-worn and smooth, with huge pot-holes even 100 feet above low-water. We can at once recognise the relationship of this gorge to that below Stanley Pool on the Congo, and the Falls of Bussa on the Niger. The swell of the land in which the Victoria Falls are situated runs in a north-north- westerly direction and is a secondary water-parting; at one time the Zambesi cut back to as far as the Batoka Gorge and all the water above the Falls was restrained within the. Ngami depression, with an outlet to the Makarikari, and so through the Kalahari to the Orange River. This was actually the arrangement of the water system that the Portuguese imagined to exist, before Livingstone ascended the Zambesi from the mouth of the Falls in i860; it is only a coincidence, based on faulty information, since even the early missionaries at Zomba could scarcely have been there before the Zambesi breached the ramparts of the Batoka basalts. The Makarikari depression to the east of Lake Ngami is a vast plain with the sides rising gradually or in terraces, like in the old Lake Bonneville in Utah. In this plain the salt pans lie sunk a few feet beneath the general surface and are occasionally filled with water. Formerly there was a lake, Kumado, in the southern corner, corresponding to the present Ngami in the bed of its former extension; in Chapman's time (1852) it was still a marsh, in the centre of which the Chief Chapo had his town- The fact that in both depressions the water accumulated in the southern ends leads me to think that the natural outlet was formerly here, and not in the north or east. The Gwai Poort, "the land of a thousand vleys." forms a long bay in the high walls that separate the depression from the Zambesi valley, but it is now partially choked up with sand. On the south-west the valley of the Gwai Poort is continued by the Omuramba Epukira. These omirimba are shallow, grass-covered valleys, practically with- out gradient; they were once river-beds but they have become choked by silting or the' accumulation of wind-borne sand and after rain, instead of being filled with running water they become a series of vleys. A still further desiccation and all connection with a river system becomes lost and the depres- sions become isolated pans. The physiographical features of this part of the country render it probable that the Gwai 1 68 THE DESICCATION OF AFRICA. Fig 7. Map of the Makarikari Depressions Passarge and Percy C. Reid. .—After Dr. S. THE DESICCATION OF AFRICA. 169 Poort was the continuation of the Loangwe River before the Zambesi cut across it. On the Kalahari side we are fortunate in having a com- plete description of the river-system by Livingstone, J. Chapman, Galton Andersson, P. C. Reid, A. Schulz, and by Passarge, in his work on the Kalahari- The Etosha Pan forms practically a drainless area just inside the coastal rampart- From the north the Cunene River drains the high- lands of Angola, and formerly it poured its ample waters mto the Etosha Pan; the vigorous head-stream erosion of the coastal river, however, has cut back through the coastal rampart and has now drained off most of this water. The capture is actually in progress at the present time. Although now when in flood, some of the water may overflow into the Etosha Pan, m ordinary times the drainage from the Angola highlands goes straight to the sea. Above Kinga the Cunene River flows through an extensive plain with practically no fall, and the river lies in a broad, marshy valley, with very low banks. When in flood the river overflows its southern bank, and the flood water finds its way, to the east of Humba and above Kinga, into two large omirimba, the Oware and the Kwamatua, which lead into the Etosha Pan. One large river from the Angola highlands still, however, flows directly to the pan, and in a few years this will be the only source of supply. WAL V I S H 8 ^ Y 'a.noersso,*>s VUEY V Fig. 8. I70 THE DESICCATION OF AFRICA. Below Kinga the Cunene enters the rocky defile through the coastal rampart and flows down a series of cateracts and waterfalls, one of which is 330 feet high; there is no doubt that the vigorous erosion going on here will shortly deprive the inland system of all drainage from the Angola plateau. The waters that once went to fertilise many thousands of square miles m the Kalahari will all be diverted and hurried uselessly to the sea. It is not practical politics to advocate the building of a 900 feet dam across the Congo at Stanley Pool to turn the whole of the Congo waters northwards into the Sahara, but it is worth while pointing out that a weir built across the Cunene River below Kinga, of very moderate dimensions, would re-divert all the western waters of the Kalahari into their original channels and make of that desert a fertile, habitable region. At the present time the flood waters of the Cunene River, after filling the Etosha Pan, work their way up the Ovambo, and eventually by the Omatako reach the Okavango River. The latter river has in flood discharged into the Omatako during recent .years, but in the floods of 1908-1909 the Omatako became a raging torrent pouring into the Okavango- As far as I can find them, the levels are: Kinga 3,501 feet, Etosha Pan 3,447 feet, and where the Omatako flows into the Oka- vango, 3,510 feet. A weir of 30 feet will give an elevation of 21 feet above the Omatako confluence, and the depth of water in the Etosha Pan 73 feet. These levels will have to be adjusted by actual survey. The Okavango River has its source m the highlands of Angola, not far from that of the Cunene; between Cuangar and Andara, the Libebe of Livingstone, it flows in a broad, open valley, and the reed-bordered stream winds through extensive flood-plains that are under water for a considerable part of the year. It is a deep, clear river, having an average width of about 100 yards, and is navigable for light craft throughout this portion of its course. The river is m many places bordered by aUuvial terraces of mud and sand, no gravel being present, and on these forests of luxuriant growth flourish. Just below Andara the river broadens out, with sandy wooded islands in mid-stream, and then encounters a bar of reddish quartzite striking north and south across the stream. Over this the river, which is here 700-800 yards wide, falls vertically some twenty feet. The river then enters a sort of estuary, between the high walls of the Mabula and Koka Plateaux, _where it divides into many inter- communicating branches. This estuary lies in the floor of the old Ngami Lake, now dried up all but a few swamps, of which the present Lake Ngami is one. The original lake now appears as a depression, like a shallow rift-valley, directed >^ THE DESICCATION OF AFRICA. 17 1 north-east south-west. On the other side of this there are the Madenassa, Haina and Chansi Plateaux, separatmg the Ngami from the Makarikari. The two great hollows are connected by the Botletle River and to the south by, the Omuramba Epurika. Lake Ngami is an expansion in the system of inter- communicating canals of the Okavango Delta and lies under the eastern bank of its former basin. Livingstone, who dis- covered the lake on August 1st, 1849, described it as being 60 miles wide, and from the writings of Livingstone, Chap- man, Baines and other travellers of that time, the general impression has arisen that Lake Ngami is a respectable sheet of water. In 1897 Passarge found that the water had entirely disappeared and its place taken by a brown expanse of reeds, between the roots of which the traveller sinks into treacherous mud. This was the condition of Lake Kumado in the south of the Makarikari depression in 'Chapman's time, 1852, and here the lake has entirely disappeared, a? Ngami will shortly if nothing is done to prevent it. Livingstone recognised that Ngami land was once the sight of a vast lake; he came to this conclusion from the prevalence of fresh-water shells in the limestone layers that appear underneafh the sand. He it was, too, who first explained the climatic changes in South Africa as due to the draining of this lake by the Zambesi. Livingstone called it "a breaking through " of the Zambesi, but I have ascribed it to the head-stream erosion of the river. The limits of the two great Kalahari Lakes are shown in the map which I have drawn from that by C. Jurisch, which accompanies Passarge's work on the Kalahari. The limits of the Makarikari are indefinite on the north, for here we have the Gwai Poort, which is the old valley of the Loangwe, before the Zambesi trenched across it. There has been doubt expressed as to whether, if the Makarikari were to be filled up again, the water would not escape by the Gwai Poort, but Chapman is positive that there is a distinct water-shed, separating the two areas. The Kwando, Linyanti, or Chobe River, like the Okavango, enters the Ngami depression by a sort of delta, receiving an important tributary from the Okavango which is short-circuiting the water past Lake Ngami and then expands into a vast swamp, through which the water filters into the Zambesi. Livingstone happened to be on the borders of this swamp in i860 and describes how, after a period of drought, the natives were burning the reeds in order to drive out the elephants that fed in the swamps. The chief, Makompa, with his men lying in wait, had killed five elephants and three buffaloes with their spears, as well as 172 THE DESICCATION OF AFRICA. wounding several others which escaped. With man helping to clear away the obstructions, the draining of Ngami by the Zambesi became accelerated. Hundreds of similar examples might be quoted from Cape Colony, many of which I have seen myself; a swamp, either of reeds or palmiet, is burnt in the dry season and in a very few years there is produced a dry valley, down which the flood waters rush during the rains, leaving no portion held in reserve in the swamp, that, like a sponge, had previously retained it. The Chobe Swamp has been driven away from the eastern side of the Ngami depression here, but a portion of the Chobe water, together with some from the Okavango, reaches the far side to form the Mababe Swamp. The north-eastern continuation of this is the Komane River, which apparently no longer connects with the Zambesi, if it exists at all at the present day as a river bed. It was crossed by Chapman in 1852 and has not been seen since. The Zambesi enters the Ngami depression by the Mpandwe Falls and leaves it at Kasungula, where the Chobe joins the Zambesi, some 50 miles above the Victoria Falls. Between these two points the river follows the north-eastern border of the depression. When the lip of the Victoria Falls was a few feet higher, the whole of the Ngami depression was a vast lake, 300 miles long, from south-west to north- east, and 100 miles broad, having the appearance of a rift-valley lake, like Nyaso and Tanganyika, which are 350 and 235 miles long respectively. At a still earlier stage, the Victoria Falls formed an unsurmountable barrier for the Zambesi and its waters went into and filled up the entire Ngami depression. This lake was tapped by the Zambesi below the Falls, eating back by head-stream erosion, just as Tanganyika has been tapped by the Lukuga in quite recent times; in a few centuries Tanganyika will be drained dry by the Lukuga and its basin will present the same appearance as the Ngami depression now does. Livingstone's description of the country is as follows t" Missionary Travels," p. 527): — The level of the lower portion of the Lekone is about 200 feet above the Zambesi at the Falls and considerably more than the altitude of Linyanti ; consequently, when the river flowed along this ancient bed, instead of through the rent, the whole country between this and the ridge, beyond Andara westwards. Lake Ngami and the Zouga (Botletle) southwards, and eastwards beyond Nchokotsa, was one large fresh water lake. The whole of this space is paved with a bed of tufa, more or less soft according as it is covered with soil or left exposed to atmospheric influences. Whenever ant-eaters make deep holes in this THE DESICCATION OF AFRICA. I -JZ ancient bottom, fresh-water shells are thrown out, identical with those now existing in Lake Ngami and the Zambesi. The whole of these lakes was let out by means of cracks or fissures made in the subtending sides by the upheaval of the country. The fissure made at the Victoria Falls let out the water of this great valley and left a small patch in what was probably its deepest portion and is now called Ngami. The Congo, also, finds its way to the sea through a narrow channel. The greater Ngami found an outlet southwards down the Botletle, to the Makarikari, the two sheets of water being thus connected, like Albert and Albert Edward Nyanzas by the Semliki River. Livingstone, who approached the Makarikari in 1849, by way of the Makoko River, states ("Missionary Travels," p. 61) that the Makoko below Lotlakani spreads out into a very large lake, of which Ngami formed a very small part. According to Chapman, who crossed the Ntwetwe Pan several times, and who was on the eastern side of the depres- sion in 1854, the banks on the east are abrupt and steep. The older Bushmen told him that some thirty or forty years ago the lake never dried up and abounded with hippopotamus, crocodiles and fish. Suddenly, they said, the waters from Lake Ngami ceased to flow, the lake dried up and the dead fish and animals were devoured by the vultures. In Chap- man's time the vast expanse of the Soa Pan was nothing but a barren plain, level as a plank floor and covered with a white, saline incrustation. This level plain became inundated during some months of the year, assuming then a very grand appear- ance, though only twelve to eighteen inches deep.* Aurel Schulz (1897) states that the natural outlet for the Makarikari is through the Macloutsie Poort, down the Shashi River and so to the Limpopo, but Chapman (loc. cit., p. 257), who was in this angle of the depression, states that there is a range of hills shutting in the view and directed S.W.-N.E. In the same way other travellers maintain that the Gwai Poort is the natural outlet, and that if the depression were to be filled up, the water would flow down the Gwai River, and so into the Zambesi below the Falls. Chapman discovered the Gwai River, and he distinctly states that there is a big rise from the Makarikari to the water-shed, and the fact that the Makarikari was a lake at one time, rather discounts this view ; besides the whole drainage on the east of the depression is towards the pans, as shown by the Shua or Nata River. Livingstone recog- nised that the original outlet was on the south, and he calls it the old river that flowed through the Kalahari and joined the Orange River. People who have been over this ground recently *J. Chapman, " Travels," London, 1868, vol. I., p. 242. J74 THE DESICCATION OF AFRICA. tell me that there are still great forest trees standing along the course of this river, though they look as if they had been dead for centuries, and at one place there is a great debris heap of boulders, sand and trunks of trees in the bed of this old river, which may have been the prime cause of its diversion. Before the Zambesi drained the Ngami basin, the Kafue was not diverted into its present course, but made straight for the Ngami depression, instead of, as at present, turning abruptly at right angles and joining the Zambesi below the Falls. The wear and tear of the rock-lip of the Victoria Falls is so tremendous that every year the level is sinking and more water is being drawn from the Chobe-Okavango system. Livingstone noticed evident deepening of the river bed above Sesheke ("Missionary Travels," p. 216). The Chobe Swamp will soon be drained, though at the present moment (May, 191 8) owing to unprecedented rains it is a vast inland sea, the old channels to the Ngami are sanded up and the water cannot escape fast enough over the Falls. What is to be feared is that, after such a flood as has occurred this year, the water from the Okavango will find a straight course by the Selinda branch to the Zambesi and the Ngami Lake will disappear as completely as the Kumado Lake in the Makarikari. To complete the preservation of what is left of the river system of the Kalahari and to prevent desert conditions from spreading beyond the Kalahari, as they obviously are at the present day, it will be necessary to weir up the Chobe River, between the swamps and its confluence with the Zambesi, to prevent the water that is turned into the system by the pro- posed weir on the Cunene River from escaping down the Zambesi, and increasing, perhaps, the beauty of Mosioatunya, as the natives call the Victoria Falls, but doing no good to the country. The site for this weir is about thirty miles from the junction of the Chobe with the Zambesi, three miles east of the village of Ngoma; here there is high ground on both sides of the river. Lower down, at the Sebuba Rapids, seven miles from the confluence, there is a bar of hard rock crossing the river, but there is only high ground on the south; on the north there is a dead level plain, flooded by the Zambesi. The same bar of rock crosses the Zambesi, and forms the Alambova Rapids. The idea of the weir is not to form an absolute bar- rier to the outflow of the waters, but to provide an impediment, which will make the water pound up against it, and allow the water from the Okavango, coming straight to the Ngami, to clear the old channels of the sand which now blocks their beds. The weir, in such tremendous floods as have occurred this year, would be entirely submerged, but gradually, as the old chan- nels are scoured out, the water would flow into the Makarikari, THE DESICCATION OF AFRICA. 175 and the weir would become more of the nature of an unsub- merged wall. To recreate the greater Ngami in its entirety would mean the building of a barrage across the Zambesi, which is too big a scheme to advocate just at present; there are, also, too many interests involved, not the least of which are those of the natives who live in the Ngami depression; if the whole depres- sion were to be flooded, these natives would be drowned out. As the Makarikari depression is 150 feet below the level of Lake Ngami, the proposed Chabe weir would cause a consider- able expansion of the area of Lake Ngami, would turn the Mababe, Mashabe and Chobe Swamps into large lakes, and the overflow would go down the Botletle River and All up the Makarikari basin. A sheet of water of this size, some 15,000 square miles in area, in the middle of the Kalahari, would turn this great thirst land from being the source whence all the drought-producing hot winds originate, into an evaporating dish, supplying rain clouds for the whole of South Africa; for moisture in the centre of a continent is not dissipated as on the sea-board, by winds that may blow the rain-laden clouds out to sea, but, as it transpired by the leaves of the forest trees and the grass of the meadows, or evaporated from the surfaces of lakes, it ascends into the air and is precipitated as rain over the adjoining country, and the process is repeated in ever- widening circles. The converse is also true; a desert keeps the air hot and dry, devastating hot winds blow from these regions and scorch up the adjoining lands. In South Africa, whether in the Karroo or the coastal plains on the west, one sees after rain the original vegetation spring up, green and tender, among the hardy, permanent bushes; this " opslag," as the Boers call it, is very short-lived, for in a few days the hot winds come and wither it up. It is a fact, too, that many of the severest droughts in South Africa are not due to deficiency of rainfall, but occur because between the falls of rain the desert winds come and wring out of the soil every drop of moisture. As a case in point, I may mention the drought in the Eastern Province in 191 3- 191 7. With quite a fair average rainfall, the hot winds had so dried the soil that the run-off, after rain, was reduced to 4 per cent, 96 per cent, being absorbed in the ground which had become as dry as ashes; in the latter half of 191 7 the drought broke and a succession of rains fell without the intervening periods of hot winds and, the run-off rose to 80 per cent., only 20 per cent, being required by the soil. To revive the whole of the Proto-Orange system is no longer possible ; it is more impossible than to revive the Proto- Congo system. South Africa stands at such an elevation above the sea, that the rivers quickly cut for themselves deep canyons. 176 THE DESICCATION OF AFRICA. The Loangwe River, for instance, which was once on the Ngami level, now enters the Zambesi below the Victoria Falls, at an elevation of 774 feet, whereas Lake Ngami is 3,117 feet and the Soa Pan 2,954 feet above sea-level. Kasungula, at the confluence of the Chobe and Zambesi, is about 30 feet below Ngami ; the site I have indicated as suitable for a weir cannot be much more than 10 feet below Ngami; in fact, Chapman found the Chobe flowing up the Talmalukan towards Ngami in 1853.* As we have taken the Soa Pan to have been on the course of the Central South African river, the Proto-Orange, the Zambesi must have cut downwards 2,161 feet since it cap- tured the Loangwe. This seems a vast amount, but when one regards the gorges of double and treble the depth, cut by our small rivers in Cape Colony, through the coastal rampart, it docs not seem so great after all. South of Andersson's Vley, all trace of a river system becomes lost, and what rain does fall collects in isolated, shallow pans. We And, however, on the south-east the Kaap Plateau draining into the Kalahari, by stream-beds of con- siderable size, though now dry. All these are directed to the north-west and some of them connect with the central portion of the Molopo River. The present commencement of the Molopo near Mafeking is a stream that often flows, but the water does not get many miles west of the town; the river, after proceeding in a westerly course, turns north-west, then due west, and then due south. At this last bend, marked Mokopon, I have placed the junction of the Proto-Orange with the present bend of the Molopo, as the most probable place, making, thus, the Molopo a tributary of this river above the bend ; below this, the Molopo would be the bed of the original principal stream. According to the relief map in L. Schultze's book on Namaland and the Kalahari (1907), the main river may have joined the Nosob first, the Molopo entering it lower down. At any rate, the natural inclination of the land would lead the water in the direction I have stated, and the Makari- kari Lake, if refilled, would not flow north or east through the Kwai or Macloutsie Poorts. The Kalahari sand has obliterated the more northerly portion, between Mokopon and the Makari- kari, just as the Saharan sand has obliterated the middle portion of the Igharghar. On the west of the Kalahari, we have the highlands of the coastal rampart, and these drain by several very large, dry rivers into a central channel, the Molopo; they all run in a south-easterly direction, and the chief one is the Nosob. ^Between the site of the weir and Kasungala there are the Sebuba. rapids (Chapman's "Travels," 1868, vol. I., p. 184). THE DESICCATION OF AFRICA. 177 The Molopo River enters the Orange River below the great bar of granite at the Aughrabies Falls. The whole of the area under discussion, that is to say, the drainage area of the Proto-Orange, is a plateau inclined to the south-west, and we have assigned to it its natural outlet. This Proto-Orangc has been beheaded ; its head streams have been diverted by the Zambesi, and the central portion has been bereft of its natural aliment and has become a desert. Luckih', its southern affluents, the present Orange and Vaal Rivers, still have water in them, but the same process is going on all round the basins of their head streams, the coastal streams are eating back through the girdle of the coastal rampart, and every year more and more water is being hurried precipitously to the sea, instead ©f going the long journey across the continent, where it can do some good. In Cape Colony, the rampart of dolerite-capped hills of the Karroo guard the inland waters, what little is left of them, the tough nature of the rock yielding very gradually to the agencies of Weathering and erosion, but still the Great Fish River has eaten a great bite out of the inner drainage area. The dolerite-capped escarpment of the Karroo is a secondary water-shed and stands in the same relationship to the coast ranges, as the Batoka basalts of the Victoria Falls stand tb Kirk and Melsetter Ranges. In the Transvaal, we see the Komati River stealing into the territory of the Vaal River; the Olifants River draining inland as far as Pretoria, and the Limpopo River reaching back even to the outskirts of the Kalahari. Further north, the Sabi River has pierced the Melsetter barrier range and drains the whole country from Bulawayo to Salisbury ; finally the Zambesi sends back its tentacles almost to the West Coast. Every one of these rivers started originally at the coastal rampart and has eaten back by headstream erosion. The waters inside the barrier-ranges once flowed towards Central South Africa and made the central depression a land of running rivers and of great fertility. We cannot hope to bring all or any of these rivers back to their original courses, and to w^eir up the inland streams is simply to check their flow and to give a further advantage to the vigorous coastal streams. We can, however, stop the further desiccation of the central portions of South Africa by building two weirs, one across the Cunene River, below Kinga, and the other across the Selinda River, or, better still, across the Chobe River, between the swamps and the Zambesi. The study of any good map of South Africa will show one how the steep, coastal rivers are stealing inland and draining the waters that flow towards the centre, so that the waters that once went to fertilise the plains are turned back and hurried 178 THE DESICCATION OF AFRICA. uselessly to the sea. Not only are the courses of the rivers steeper on the seaward side of the mountain rampart, but owing to the fact that this intercepts the moisture-laden sea- breezes, there is more precipitation on the seaward side. If we could give more rain to the inland area, we should equalise matters more nearly and delay the invasion of the coastal streams indefinitely. The scheme outlined here is a practicable one to give South Africa a greater general humidity, and is not an exces- sively expensive one. The two weirs across the Cunene and Chobe Rivers will cause the Etosha Pan to fill up and Lake Ngami to cover much of its former area, making one great lake out of the present separated tracts of Ngami, the Mababe and Chobe Swamps; the overflow would fill the Makarikari depression, which, with the Gwai and Macloutsie extensions, covers an area of 15,000 square miles, There would be, thus, created a source of supply for rain-clouds, that would refresh the Kalahari and clothe its sand-hills with permanent pasture. The water transpired by the vegetation covering this great tract would ascend and be precipitated throughout the area within the girdle of the coastal rampart; the condition of South Africa would be restored to that of some two or three hundred 'years back, when the Karroo was a flower garden, supporting vast herds of game and the present dry rivers ran throughout the year. Unless this is done, the central supply for our rain will dry up entirely ; desert conditions will spread until South Africa will become a waste land like North Africa, and the fate of Capetown and Pretoria will be that of Berenice and Taodeni. Such a future will not be fulfilled in our lifetime, nor in a century, but we can go back in this descent several hundred years in one step, by stopping up the leak while it is still mendable ; we can preserve South Africa from the fate of North Africa, where the leak has become a tear, beyond our present skill in engineering of repair. DISCUSSION. Mr. F. E. Kanthack, C.M.G., M.I.C.E., Director of Irriga- tion, after moving a cordial vote of thanks to Professor Schwarz for his interesting and courageous paper, went on to deplore the fact that such a very inadequate amount of time had been allowed for this paper and its discussion, in view of the extreme importance of the matter, and, more especially of the remedies proposed by Professor Schwarz, and of the far- reaching beneficial results which, he claimed, would result therefrom. The fact that Professor Schwarz had, some months ago, brought his ideas before the public through the medium of the Press, and that his ideas had stimulated very consider- able interest, not only amongst the public at large, but also in THE DESICCATION OF AFRICA. I79 the Senate, where the matter was debated, and in the course of which debate it was pointed out that the scientific aspects oi Professor Schwarz's proposals were to be discussed by members of this Society, made it most desirable, therefore, that a full discussion on the subject should be allowed. In view of the very short time at his disposal, however. Air. Kanthack said that he must confine his remarks to only a few aspects of the case, and as these remarks dealt to a large extent with meteorological, geological and botanical aspects, sciences which were represented at the meeting by recognised authorities, he would endeavour to raise points Which would stimulate definite criticism on the part of these authorities. Professor Schwarz's paper he considered could be roughly divided into four sections : Firstly, there was what could be described as the Paleo- graphical Section, in which Professor Schwarz attempted to reconstruct the ancient drainage system of the African Con- tinent as deduced from general geological and present-day topographical conditions. Regarding the views put forward by Professor Schwarz under this heading, he did not feel competent to express any opinion, but presumed that his geological friends would do so. The second section of the paper dealt with more modern drainage conditions, both hydrographic and topographical, and dealt mainly with the vast area included within the drainage area of what Professor Schwarz describes as the Proto-Orange River system. In this section Mr. Kanthack ix>inted out that, from personal knowledge, he could not agree with some of the statements made in the paper, amongst them the statement that the Omatako River, in the South-West Protectorate, was an un- defined drainage line, as described in the paper. He had, during 191 5, explored this river for about 150 miles, from its head waters downwards, and was of opinion that the Omatako was a most pronounced drainage line arising on the high watershed of the Northern Protectorate, and embracing such very prominent features as the Omatako Mountain and the Waterberg Range, from which there was a most decided gradient draining in an easterly direction. The assertion made that this channel, or Omuramba, as it is called locally, was capable of conveying water alternately westward or eastward was, in his opinion, impossible ; it would imply in the case of the westward flow, a most pronounced flow up-hill. Then, again, in the case of the Ovambo River, which was also well known to him, and which was a pronounced drainage channel running from east to west, Mr. Kanthack took exception to the statement that the flow of water in this river could be reversed so as to convey water from the Etosha Pan into the Okovango River system. With regard to general statements made in the paper relating to the relative levels of the Kunene, Okovango, Chobe and Zambesi Rivers, in relation to the N'Gami and Makarikari Lakes, he had to point out that these were based entirely upon aneroid t8o the desiccation of AFRICA. observations, and, as everyone knew who had had experience with observations made with such instruments, no matter what precautions were taken, such levels were liable to very great errors, and, in vievv' of the very small difference in altitude, on which Professor Schwarz based his scheme, extreme caution was necessary in accepting such data. The third section of the paper dealt with the partial restoration of Professor Schwarz's Proto-Orange River drainage system., and this was, to a large extent, an engineering question. The entire absence of reliable levels had already been referred to and it is impossible to criticise many of the far-rea6hing engineering proposals made without having essential data of this kind. It has already been stated that, in so far as the proposal to divert the Kunene into the Okavango system is concerned, the proposals appear to be impracticable, and this raises many misgivings regarding the practicability, ifrom an engineering point of view, of the proposals concerning the Zambesi River and its tributaries. Another matter which is oil 'thei utmost limportance in connection with the proposals is the availability of sufficient volumes of water to be derived from the Kunene, Okovango and other drainage areas, which would be required for the purpose, firstly of creating an enormously enlarged Etosha Lake, which, according to Proifessor Schwarz, would attain a depth of over 70 feet, and, secondly, of recreating the Makarikari Lake, the superficial area of which he estimates at 15,000 square miles. The extensive knowledge which we have now in our possession relating to the percentage of rainfall which runs from a given area in the form of stream flow, clearly demonstrates that the enormous volumes of water required to give practical effect to this sdheme would rarely or even never be forthcoming, and, in this case, far from achieving the objects desired, the proposed works would merely lead to the creation of vast salt deserts and swamps. To engineering and technical difficulties, such as referred to above, must, of course, be added very great politico-economic difficulties, and also what Professor Schwarz, in his resume, euphemistically described as sentimental difficul- ties. Supposing, however, for the moment, that it were possible to carry out the sc'heme, and that the vast inland seas in the northern South-West Protectorate and in the Kalahari or the Bechuanaland Protectorate came into existence, we then come to the most important section of the paper, namely, the advantages which would be derived from the scheme. It is clear that, in plac- ing such an enormous scheme before the people of the Union of South Africa, which, it must be said, would certainly cost a vastly greater amount of money than Professor Schwarz appears to imagine, assured benefits of a far-reaching and very sub- stantial character would be demanded. The main results claimed for the scheme by Professor Schwarz are the pronounced amelioration of climatic conditions in the arid parts of the Union, more especially the Karroo, and, % THE DESICCATION OF AFRICA. l8l whilst it is not so definitely stated in the paper before us, it is clear from Professor Schwarz's prelim,inary remarks in the newspapers that he claims that in the Karroo, within historic times — that is, within the period of the last few generations — climatic agricultural conditions were vastly more favourable in the past than they are now, and he claims that his scheme will restore to the Karroo those favour- able conditions, and it is mainly on the question of the beneficial results to be derived from the scheme that the greatest exception was taken to Professor Schwarz's proposal. It is, in the first place, denied that, within what could possibly be described as recent times, the Karroo, or any other portion of arid South Africa south of the Molopo, was anything but a pronouncedly arid stretch oi country. The very name " Karroo " is, it is understood, the Bushman or Hottentot word implying aridity. It is true that, during the past few generations, the Karroo, to a large extent, has suffered greatly as a result of erosion, which is due entirely to artificial causes ; but, wliilst this erosion or slooting has been responsible for the most widespread drying up of vleis, etc., and whilst the destruction of mountain vegetation by fires and overgrazing has given rise to destructive floods, which 'have eroded large areas of land, and rendered other large areas useless by covering them with sand, boulders and detritus, and in many cases the rate of run-off of the rainfall has been increased to an extent wholly prejudicial to the country, there is no evidence whatever, during the whole of this period, that the rainfall over the Union or its intensity has been decreased, or that meteorological conditions, in general, have altered to a greater extent than is shown by possible periodic variations due to causes at present impenfectly understood, and which cannot be properly analysed with the comparatively short record at our disposal. All the evidence at our disposal goes to show that arid South Africa has been arid for ages which can only be measured in geological time. Taking, in the first place, the botanical evidence, we have, in arid South Africa, what I believe to be an unique flora composed largely of succulent and other species which have been adapted by nature to be extremely drought-resisting. It is well known to any observer of such things that this peculiar vegeta- tion, which may be called Karroo vegetation, is unable to exist under more humid climatic conditions. Along the edges of the arid belt, where the rainfall begins to be more regular and greater in amount, but where these better conditions are not fully established, the Karoo vegetation has to put up a very severe struggle for existence, and two or three favourable rainfall years are sufficient to drive it out altogether. If Karroo veld is irrigated, the Karoo vegetation is almost immediately killed, and, if such irrigation is stopped, the re- establishment of Karroo vegetation takes place very slowly from the margin. It is obvious that a vegetation so unique in the world and with such pronounced characteristics, has not come l82 THE DESICCATION OF AFRICA. into existence within a few generations, but must have required an enormously long period of time for its evolution. The (further development of this line of argument must be left to botanical authorities, such as Dr. Pole Evans and others, who, it is hoped, will take part in this discussion. Secondly, from the geological and physiographical point of view, evidence most strongly supports the theory of the extreme age of the present arid conditions. The great vleis in the Karroo, which, in the past, were such a feature in the landscape, but w'hich are now unfortunately, to a large extent, arid and eroded flats, due to causes already mentioned, have obviously come into existence only throughout a long period of arid conditions. In this connection, Mr. Kanthack cited examples of the nature and formation of such vleis as derived from experi- ences in building dams in the Karroo, more especially the valuable evidence obtained in the building of the great dam on the Smartt Syndicate Estate in the Britstown district. He further drew comparison between the conditions under which these vleis had been formed and the formation oif the great Loess plains and steppes of South-East Europe. He also drew attention to the interesting discovery of a fossil skeleton of a large saurian in the Henkries Valley in Northern Namaqualand, which was recently discovered by Dr. Rogers, and which was embedded in, and entirely covered by, deposits of material derived from erosion under extreme arid conditions, which pointed to the extreme length of time throughout which desert conditions had obtained in that part of Namaqualand. Thirdly, he pointed out that agricultural evidence indicated clearly in the Cape Province that, with soils derived from identical geological formations, the degree of fertility was, more or less, in inverse proportion to the rainfall. Thus the alluvial soils of the most arid parts of the Karroo were vastly more fertile than the soils derived from almost exactly the same geological formations situated further east in regions of much greater rainfall. Fourthly, there is the historic evidence contained in old accounts of travels of high ofificials, etc., which are to be found in the Cape Archives, in which frequent reference is made to the most severe droughts. All the above, and much more evidence of a varied character, goes to show that the present arid conditions of the Karroo are of enormously longer standing, and that if, as is asserted, any great changes took place in the northern parts of Bechuanaland such as the sudden drying up of the N'Gami and Makarikari Lakes, these catastrophes made no impression upon the climatic conditions of the Karroo, either for the worse or for the better. , ., It remains to deal with the problem from the meteorological point of view, which, in many respects, is the most important aspect of the case. This was, however, a matter which Mr. Kanthack stated he preferred to leave in the hands of authorities THE DESICCATION OF AFRICA. 183 on -meteorology, such as Mr. Charles Stewart, Chief Meteoro- logist for the Union. Dr. I. B. Pole Evans. M.A., F.L.S., Chief of the Division of Botany, Union Department of Agriculture, said that he was much in the same position as the previous speaker (Mr. Kanthack) ; in that he had not yet had an opportunity of reading through Professor Schvvarz's interesting paper; he could there- fore, in the short time at his disposal, only touch upon a few of the points which had occurred to him whilst listening to Pro- fessor Schwarz. The first point was that with regard to Professor Schwarz's suggestion that at one time in the history of Africa some of the great rivers instead of flowing directly into the oceans first ran inland. If such had been the case one would naturally expect to find evidence of the peculiar coast-belt flora in the interior along the courses of these rivers. As far as he was aware, there was at present no evidence of a botanical nature to support this view. The second point was with regard to Professor Schwarz's idea that the desert conditions of the KarroO' were of com- paratively recent origin. The botanical evidence certainly did not bear this out, for the Karroo flora was of a very highly specialised type. All the organs, such as the leaves, stems, and roots, were constructed either for the purposes of storing water or for preventing the evaporation of water. Such a high degree of specialisation could not possibly have been brought about in even a comparatively short geological period of time. Furthermore, it was common knowledge that the Karroo xerophytes were the most difficult of all plants to grow out of their natural habitat, and could not be easily acclimatised by man like many of our other plants. By creating such a huge mass oif water as Professor Schwarz proposed in the interior of the continent, it must be borne in mind that we would be disturbing the balance ui nature, and it would be very difficult to predict, without considering the matter in all its aspects from a biological standpoint, whether the presence of such a lake would be to the benefit of the country or otherwise. _ Mr. C. M. Stewart, B.Sc, Chief Meteorologist of the Union, said that before proceeding to make any comments, he must express his admiration for the originality and boldness of the ideas contained in Professor Schwarz's paper. Apart from the geological aspect of the probable cause of aridity, the most important because the most practical considera- tion in connection with this proposed scheme is the probable effect of such a body of water on the climate of South Africa. There are certain results which would naturally ensue from the damming up of a body of water 15,000 square miles in area. Among these may be mentioned, first, a modification of the local atmospheric circulation similar to the land and sea breezes of the coastal districts. Owing to its great specific heat, the water would 184 THE DESICCATION OF AFRICA. become heated much more slowly than the land during the day, and would part with its heat equally slowly during the night, so that as a general rule the water would be colder than the adjoining land by day and warmer during the night. As a result there would be on-shore breezes during the day, and on-lake breezes at night, or, at least, a modification of the general cir- culation due to the pressure distribution, in consequence of the tendency to the production of such winds. A second result would be an increase in the humidity of the atmosphere due to the evaporation from this large water-surface. A third effect would be a tendency to the reduction of the extremes of daily temperature, tlie maximum being slightly lowered, the minima being raised more particularly, owing to hot winds being cooled and cold winds warmed in their passage over the water. These last two effects would be more apparent on the leeward than on the windward side. A somewhat similar result would be locally apparent in the seasonal variation. A similar effect is met with along the eastern shore of Lake Michigan (20,000 square miles in area), where the amelioration of the climate due to the presence oif tthis large body of water is such that peaches, grapes, etc., can be grown in a narrow strip known as the " Fruit Belt." Whilst there can be but little doubt that the impounding of a large sheet of water such as this would produce the modifications of local climate just mentioned, it is a very different matter when we come to consider the modifica- tions of actual precipitation that are likely to ensue. It then becomes necessary to ask the questions. Is the proposed scheme capable of producing the effects claimed for it? And if so, is it likely that the results claimed for the scheme would be actually produced? The mere proximity of extensive sheets of water is of itself insufficient to^ ensure any area having a large or even moderate rainfall, otherwise there would not be such a state of affairs as prevails at Walvisch Bay, on the West Coast, where precipitation amounts tO' something like one-third of an inch in the year. If for the sake oif argument it be allowed that a rain- fall of 20 inches per annum is the minimum on which agricultural operations can be carried on without artificial watering {i.e., without the assistance of irrigation), it is found that in the Union of South Africa alone there are approximately 240,000 square miles having less than this amoimt.* Of these, something like 128,000 square miles have less than 10 inches; so that, on a rough estimate, an additional amount of 9 inches per annum would on the average require to be dis- tributed over these 240,000 square miles to bring the annual rainfall up to the minimum assumed necessary for agricultural purposes. Even granting that the evaporation from this water- surface amounts to 100 inches per annum, and further assuming that the whole of this amount were transported and distributed *Schunke Hollway states that the desert region of South Africa measures 700,000 square miles. THE DESICCATION OF AFRICA. 185 over the Union in proportion to the requirements df each locality, a simple calculation shows that it would add an additional 6 inches to the rainfall, bringing the average up to 17 inches, thus leaving an additional 3 inches to be met from artificial watering. It is of course not only possible, but very probable, that a certain proportion would be re-e\aporated from the ground and re-precipitated, but this would take place in decreasing amount as the distance from the source of supply increased, and with each recurrence of precipitation and subse- quent evaporation. In order to produce the desired result it is not sufficient merely to get the moisture into the air, but the mechanism must also be available, not only to transport the moist air to the desired area, but also to re-precipitate it over that region. The main cause of aridity in any part of the world is not that there is not sufficient moisture in the air, but that nature has withheld the means of cooling the atmosphere sufficiently over sudh regions to cause condensation. It is evident that in order that this scheme should benefit the arid and semi-arid portions of the Union, there ought to be a fairly persistent northerly to north-easterly wind to transport the moisture ; whilst over these dry regions the means of dynamically cooling the air to such an extent as to produce precipitation must be at hand to take advantage of the presence of the moist currents. This might take the form of a denser stratum of air, which, by under-running the warm, moist layer, would cause it to rise and so cool by expansion to such an extent as to cause it to part with its moisture ; or the atmosphere over t'he dry regions must be so warmed as to cause convectional (vertical) ascent, resulting in thunderstorms, etc. As the attitude of the proposed scheme is approximately 3,500 feet, and as the dry areas of the Union vary from 1,500 to 4,500 feet (mostly about 4,000 feet) it is evident that but little rain could be expected from orographic causes, that is produced by cooling due to forced ascent over mountains or other high ground. Athough nothing is known of the meteorological conditions prevailing over the site of this proposed scheme, it may be per- missible to examine the weather conditions at Bulawayo as published by the Rev. Father Goetz in his papers on " Some Meteorological Features of Southern Rhodesia " and " The Rainfall of Rhodesia." Bulawayo (20°9' South Lat.) is in practically the same latitude as, but a little further east than, the Alakarikari, and so lies well within the Tropics. It is not, therefore, surprising to learn that Father Goetz asserts that a rainfall not accompanied by electrical phenomena is an exception from October to April. An examination of the tables of hourly distribution of rainfall shows that 75 per cent, of the total occurs between i p.m. and midnig'ht, the largest portion (42 per cent.) falling between i and 6 p.m. It would therefore appear that thunderstorms are the most l86 THE DESICCATION OF AFRICA. effective agents in producing rainfall over this area. The direction and rate at which they travel will be dependent on the currents some distance up : of these we know very little, except that " cirrus " clouds travel from a little north of west. Now the frequent occurrence of afternoon thunderstorms presupposes an almost stagnant atmosphere, so tliat one is prepared for the statement that the winds at Bulawayo are mostly light (forces 3 to 4 on the Beaufort Scale being considered strong for Bulawayo) . The prevalent direction is very nearly E.S.E. Although Father Goetz states that " it is not easy to decide whether there are any w^inds especially associated with a fall of rain, he finds, on correlating the self-recording anemometer and rain gauge records, that 55 per cent of the total that fell between 24th January, 1904, and ist May, 1908, occurred with winds between E. and S., leaving 45 per cent, distributed among the remaining five points and calms. If one may be allow^ed to apply these results to the Makari- kari region, it seems reasonable to believe that the result of the conversion of these marshes into a lake would be an increase in the humidity of the air, particularly on the west side ; an increased rainfall in the immediate vicinity of the lake ; and a much smaller increase at a greater distance, noticeable all round — possibly to a distance of two hundred miles — but more par- ticularly on the north and west sides. In order to benefit the dry regions of the Union, a radical readjustment of the distribution of pressure over South Africa and the surrounding seas would be necessary, including the obliteration oif the permanent anti-cyclone off the West Coast, one of the most effective factors in causing the rainfall to be low over the western half of this country. Such an alteration is certainly far beyond what could be effected by Professor Schwarz's scheme,, large though one may consider it. For these reasons I am afraid that tlie climatic results that would ensue from the carrying out of this scheme would fall far short of those depicted ; our arid regions would remain arid, and the Karroo continue to be merely " Karroo."* * As mention has been made of Lake Michigan in the above remarks, the subjoined extract from the letterpress of the U.S. Weather Bureau publication, "' Meteorological Chart of the Great Lakes/' by Alfred J. Henry and Norman B. Conger (1907), ought to prove of some interest. These five Great Lakes together cover an area of about 93,000 square miles, and lie directly in one of the main storm tracks of the North American Continent, consequently the atmospheric circulation is mainly horizontal. The prevailing winds are from north-west to south-west, so that the effects of evaporation from the Lakes ought to be most apparent to eastward. On the subject of "The Lake Influence," the authors remark as follows : — " It is a rather common belief that the Great Lakes, by reason of the enormous possibilities of evaporation they possess, are an effective THE DESICCATION OF AFRICA. 187 Dr. p. A. Wagner, B.Sc. : The thanks of the Association are due to the author for having brought this very important matter before us. We, the colleagues of Professor Schwarz, do not always see eye to eye with him in geological matters, but we know that he can be relied upon to present his view^s in a most interesting manner, and you will, I think, agree with me that on the present occasion he has excelled himselif. Many of the questions raised in the paper have already been fully discussed. I shall therefore confine myself, as far as possible, to points not hitherto dealt with. In the first place, I should like to offer a word of criticism in regard to the author's conception of the Proto-Orange. Professor Schwarz joins up to Loangwe River with the lower course of the Molopo, and thus conjures up the vision of a mighty stream traversing what is at present the Kalahari. Now there can be no question that the Molopo at soine former period must — at times, at any rate — ^have been a swiftly-flowing stream, for, during a recent visit to the Southern Kalahari, I found on a small island in the middle of the present dry channel, about six miles south of the Upington-Keetmanshoop railway, an extensive terrace of coarse river wash, 15 feet in thickness, with well- rounded boulders up to 18 inches in diameter. lu regard to the age df the deposit, the top of which is about 35 feet above the river-bed, there is no evidence. It may, however, be, and in all probability is, very ancient. The Molopo Valley itself is without doubt of great antiquity, and, like some of the old valleys leading down to the Orange River from the south, was probably in existence in Cretaceous times. The Loangwe, on the other hand, flows in a rift-valley of comparatively recent origin. Indeed the faulting to which the valley owes its origin is still cause of precipitation, and that because of their presence the precipitation of the Lake country is greater than it would be were they absent. " The increase in precipitation due to the presence of the Great Lakes is believed to be small, probably not more than two or three inches annu- ally. This conclusion is reached by considering the precipitation of the lake region in its relation to that of the remainder of the country east of the Mississippi. The heaviest precipitation of the Mississippi occurs in the Southern and South-Eastern States, and the amount diminishes both in a northerly direction toward the interior of the continent and in a westerly direction toward the sub-arid region of the far West. The rate of decrease of precipitation, considering the region of 50 inches as a reference point, is quite sharp in a westerly direction, being as much as 30 inches in 450 miles, or an inch in 15 miles. In a northerly direction the decrease is much less ; in 300 miles it is at the rate of i inch in .30 miles ; for the next step northward, which includes the lake region, it is only an inch in 50 miles. In other words, the rate of diminution between the isohyetal of 50 inches and the isohyetal of 40 inches, if projected northward, would cause the isnhvetal of 30 inches in the lake region to pass about 200 miles southward of its present position. This displace- ment would mean an average loss of two or three inches of precipitation over the greater portion of the lake region. Considering also the distribu- tion of precipitation on both sides of the lake region, it would appear that the foregoing estimate is a fair allowance for the increase of precipi- tation which might reasonably be attrilnited to the effect of the Lakes themselves." l88 THE DESICCATION OF AFRICA, in procuress, as is evidenced by the frefjuent earthquakes emanating from that quarter. To join up these valleys, which are separated by a distance of over 800 miles, and reconstruct in the imagination the channel of a hypothetical Proto-Orange is thus, to say the least of it. not justifiable. Taking the present physiography of South-Central Africa as a basis, it appears more probable to me that the waters of the Okavango and Kwando, and also possibly of the Upper Zambesi, at one time flowed into the Indian Ocean z'ia the Makarikari depression and the Limpopo Valley, and that they were diverted to the courses they now take either by a regional uplift or north- ward tilting of the Central Kalahari, or, as suggested by Pro- fessor Schwarz, by the headstream erosion of what is now the Lower Zambesi. In the absence of an accurate topographical map oif the Makarikari Basin and the area to the east of it, I hesitate, however, definitely to put forward the theory. Turning to Professor Schwarz's project for the re-flooding of Lake Ngami, I agree with the author that the waters of the Kunene could be turned into the Etosha Pan by building a weir across the river above Kinga. His statement that the flood waters of the Kunene. after filling the Eto'sha Pan, " work their way up the Omuramba Ovambo, and eventually by the Omatako reach the Okavango River," however, is not only incorrect but misleading, inasmuch as the Omuramba Ovambo is a very clearly defined watercourse with a pronounced fall towards the west, which is separated from the Omuramba Omatako by a tract of elevated sand-veld. The Onuiramba Omatako became a raging torrent during the rainy season, 1908-1909 — the statement, by the way, is taken from my memoir on " The Geology and Mineral Industry of South-West Africa " — not because of the flooding oif the Etosha Pan by the Kunene, but because of the abnormal rains that fell in the Grootfontein and Waterberg districts in that season. Speaking from personal knowledge O'f the area, I can assure Professor Schwarz that the flooding of the Etosha Pan, to a depth sufficient to make the Kunene flow 7'ia the Omuramba Omatako into the Okavango, would require far more water than the Kunene is capable of supplying, quite apart from the fact that ic would result in the submergence of the whole of Ovamboland and considerable portions of the fertile Grootfontein and Out jo districts. This part of the project is therefore, in my opinion, not worthy of serious consideration. In regard to the diversion of the waters of the Okavango and Kwando Rivers intO' the N'Gami depression by erecting a barrage across the Chobe, about 30 miles from its confluence with the Zambesi, it appears to me, having regard to the fact that these rivers, on entering the N'Gami region, flow in broad marshy valleys with low banks bordered by very flat country, that, instead of creating a greater Lake N'Gami, the efifect of raising the level of the Chobe. in the manner suggested, would THE DESICCATFON OF AFRICA. 189 be indefinitely to enlarge the vast Okavango-Kwando swamp- land : a region of almost indescribable dismalness, absolutely useless for any purpose, and \ery unhealthy. Now there appears to be considerable misapprehension in regard to the Northern Kalahari. Much the greater part of this alleged desert is well timbered and grassed, and is, in the opinion of competent judges, admirabl}- adapted to cattle-ranching. The only obstacles to the settlement of t'he area, apart from its inaccessibility, are the lack of surface water during the greater part of the year and its iinhealthy character in the rainy season. In regard to the first oif these obstacles, I am convinced that water could be obtained by putting down boreholes through the thick mantle of sand with which the whole region is covered, seeing that the average annual rainfall over the area probably exceeds 20 inches, while tlie run-off is nil. It is also relevant to observe that excellent supplies of artesian water have been struck in the eastern part oi the Southern Kalahari in the Protectorate of South-West Africa. In regard to the second obstacle, t^e climate of the Northern Kalahari, except in the neighbourhood of the Okavango swampland, is probably not more unhealthy than that of other malarial regions in Southern and South-Western Africa wbich have been successfully colonised. Professor Schwarz's barrage, in addition to permanently destroying enormous areas of this potentially valuable ranching country would render equally large areas so unhealthy as to be uninhabitable by Europeans, and as the benefits to be derived, judging by wdiat we have heard from Messrs. Kanthack and Stewart, are very problematical, it appears to me that this boldly conceived scheme, though appealing powenfully to the imagina- tion, is in fact quite impracticable. Dr. A. L. Du ToiT, B.A., F.G.S., Government Geologist, said that the course of the Proto-Orange across the Kalahari, as advocated by Professor Schwarz, receives considerable geological support, and there are also indications that the damming back oif the drainage over the N'Gami region may have been brought about by gentle unwarping along an east-west line through the Central Kalahari, this action provoking the capture of the waters of the S3^stem by the more active young Zambesi on the east. Such a tilting movement might not yet have ceased, and its continuance might be an important influence in diverting the waters of the depression towards the north even at the present day. Presuming that there was originally a great body of water in this hollow, it does not necessarily follow that the area was any more fertile in the past than to-day. for it is important to observe that in almost all the continental masses there are, on their western shores or just within their western interiors at about t'he Tropics, extensive areas over which desert or semi-arid conditions prevail. A most important point is the magnitude of the evaporative losses from such a large body of water. Taking evaporation at about 8 feet per annum, the loss would be equivalent to about 190 THE DESICCATION OF AFRICA. 7,000 cubic feet per second for each thousand square miles of surface. The gaug-in^s of the Zambesi above the Falls are given in a very recent Rhodesian Report as 11,750 cubic ieet per second for the seven winter months of 1905, and although the summer flow would be enormous, yet these figures should prevent one ifrom too readily assuming that a basin of the size advocated could be kept filled during normal years. Moreover, such a body would bring abotit the extension of the present fever-stricken swamps, and would, through periodical floodings, give rise to marginal barren salt-flats, while the effects upon the climate of any re-condensation of the moisture evaporated, upon which the success O'f the whole scheme depends, would be more or less problematical. Uses of Mirabilis JalAPA.— F. Mancada Guignones gives an account in La Rivista Agricola'^' of a long study of the plant commonly known as Marvel of Peru (Mirabilis jalapa). When grown in gardens it flowers abundantly, but jjroduces small seeds. Imt if grown under arid conditions, and i)articularly if fertilised with ashes, it flowers less, but produces seeds which are much larger and richer in starch. This starch is of very good quality, and produces an excellent floitr capable of being used for bread, biscuits, etc. The seeds also contain a sugar, and can be subjected to alcoholic fermentation. The stamens, jjistils and perianth (which dries up without separating from the seed) yield a fast purple, which can be used for dyeing silk. The flowers open towards evening (hence another common name for the plant in SoiUh Africa is " Vier-uur bloem " or " Four o'clock ") and exhale a strong odour during the night which is said to stupify or drive away mosquitoes. In such a case it might be advantageously cultivated in malarious areas. It grows in a semi-wild condition in several parts of South Africa — for instance, near Idutywa in the Transkei, and on the Rhodesian veld. RoYAii Society of South Africa.— At the annual meeting of the Royal Society of South Africa, held on the 25th September. 1918, the following were elected Fellows of the Societv: Prof. A. Brown, M.A., B.Sc. F.R.S.E. ; Miss E. M. Doidge. M.A., D.Sc, F.L.S. ; S. H. Haughton, B.A. F.G.S. ; Prof. H. B. Fantham, M.A., D.Sc, A.R.C.S., F.Z.S. : and Prof. A. Yoimg, M.A.. D.Sc, F.G.S., F.G.S. '-• 14 ( igi8), 142, 143. TllF MF.DICINE ^^lAN IN NATAL AND ZULULAND. By the Hon'ble Mr. Justice Cecil Gower Jacksox. The medicine man or herbahst plays an important i)art among all the Bantu tribes of South Africa. For good or ill he plies his trade, secure in the conviction that his office is an indispensable one, and content to follow the primitive methods which his forbears for generations past have practised in the treatment of disease. Little is known generally by Europeans of these methods: little is known of the man himself; yet the lives of many are in his keeping. By some he is credited with having gradually acquired a considerable degree of cleverness in his heart, and a close knowledge of many indigenous plants of high medicinal value, an analysis and study of which would repay otu- own doctors and chemists. On the other hand, there are many who hold that he is an evil in the land ; that his treat- ment for the most part is entirely experimental, and carried out by methods which in themselves are sufficient to jeopardise the recovery of any but the most obstinate patients. The subject is not one which has been widely discussed ; probably even those who have expressed divergent views as with authority would not not claim to have made a deep study of the matter, but base their opinions on facts which have come to their knowledge in a general way. Statistics, naturally, are not available; accurate information as to the number of patients which an average prac- titioner may attend in the course of a year, and the result of his ministrations, would be difficult if not impossible to obtain. If such a return, even approximately correct could be compiled, it may well be that the figures would be startling. Anyone even moderately familiar with Native life and customs may soon glean enotigh to satisfy himself that the cult of the medicine man is one which gives unrestricted scope to experiments in the medical and surgical treatment of disease and wounds, as well as in midwifery, and constitutes a problem which calls for investi- .gation. The urgency of the problem might be well exemplified by a reference to concrete cases, both civil and criminal, v.'hich have come before the Courts, and which alone would furnish sufficient data of a reliable and convincing nature to illustrate its impor- tance. A study of these judicial records would be instructive ; a comprehensive gamut of human nature, from comedy to tragedy, would fall within its purview, and could not fail to reveal much of interest from a material and psychological standpoint. Limi- tations of time and space, however, preclude an attempt to deal with this phase of the subject in a hasty sketch which does not aim at being other than a superficial review of the medicine man, his legal status, his position in the economic life of the Native. and his general method of procedure. In this connection a popular fallacy that the issue of a licence to a Native doctor A Hj2 THE MEDICINE MAN IN NATAL AND ZULULAND. is a guarantee of efficiency, and secures him a certain measure (-'f immunity when a charge of culpable homicide is laid against him, may be contradicted. The mere fact that a man has taken out a herbalist's licence is no protection in such cases, which are, t)f course, governed by the ordinary principles of law appli- cable tb.ereto : but it is often a matter of great difficulty for the Crown to prove the case. There have, however, been a number of convictions for culpable homicide where death has resulted from the improper or careless administration of Native medi- cines : and even where a prosecution may fail, a good result has been obtained in teaching these men to desist from the use of certain drugs or plants, of the properties of which they know little or nothing. The medicine man is common to all parts of South Africa, but reference to him will he confined to Natal and Zululand, where his office is to some extent regulated by special legislation. In the other Provinces he is, I understand, untrammelled by official recognition, unless he trespasses within the prohibited regions of witchcralft. The Natal Native Code of 1891 deals with medicine men and herbalists, who are known respectively as izinyanga zokum Lapa— those skilled in healing — and i:;inyanga ze mlti — herbal- ists. The office may be held by both men and women, but it is seldom that the latter make any attempt to follow the profession except as midwives. Women diviners are common, notwith- standing the stringent penalties attaching to the practice of this art, and some of them claim to heal by divination or otherwise — 'but the ordinary lady doctor is scarcely known. In revising and amplifying the old Native Code of 1878, and substituting therefore the Code of 1891, it was considered desirable to place restrictions on the indiscriminate practice of medicine by Natives in Natal, and with this object it was declared illegal for any man or woman to practise his or her calling for hire unless duly licensed by the Magistrate. Women, however, who act as mid- wives only are not required to be so licensed. Before obtaining a licence, the applicant must be recommended by his chief, or the chief of the tribe in which he seeks to practice, and no other formality is necessary. The Magistrate may, of course, (for sufficient reasons, refuse to grant the licence, and this has been held to be an administrative act not subject to a judicial appeal. It is infrequent that any applicant is refused a licence, but the Magistrate would exercise his discretion in the case of a man whom he has occasion to believe is undesirable, whether by reason of a reputation for being a witch-doctor, or Ifor any other sufficient reason. No form of qualification is required ; no inquiry is made as to any previously acquired knowledge of herbs or the treatment of disease ; the law is complied with if the approval of the chief is given, and there is no obligation on the latter to satisfy himself as to the applicant's competency. The amount of the licence is £3, and it must be renewed annually by a like payment. The holder may thereafter practice in any THE MEDICINE MAN IX XATAL AND ZULULAXD. I93 part of Natal — as distinct from Zululand. He is permitted to charge a preliminary or retaining- fee {iilitg.va), which must not exceed ten shilhngs ; further payments depend on the wise principle of " no cure, no pay." The patient is further protected by the right to claim civil damages ifor blunders or negligence, entailing bad results, independent of any criminal charge which may be preferred. It may be remarked that if the number of such civil claims bears any relation to the number of failures, the Native doctor must be a singularly proficient man, for it is seldom that recourse is had to law to obtain compensation for the consequences of improper treatment. One such case may be mentioned — a claim against a doctor for eleven head of cattle, representing the loholo, or marriage consideration, which would have been received for a girl if she had not unfortunately met her death at the hands of her medical attendant before the mar- riage took place. It is not suggested that failures are few ; under their own customs this class of litigation would not generally be invoked, Ifor it may be a dangerous thing to make an enemy of the medicine man ; and the fact that European-made law afifords this sanction is perhaps not widely known. Those who have suffered at the hands of the physician are no doubt content to know that he at least can claim no payment for his pains. To practice without a licence is to incur the penalty of the law, and carries with it the further disability that no claim for fees will be entertained. A sharp distinction is drawn between the offices of the medicine man and the diviner. The sale of love philtres and charms is prohibited, and any medicine man resorting to such means of gain will have his licence can- celled, his stock-in-trade confiscated, and himself imprisoned or fined. The rain doctor, the lightning doctor, the witch-doctor are not countenanced, and any Native who thus dabbles in the occult is severely punished if he is found out — ^which, in most instances, he is not. The heavy hand of the law is not confined to the diviner, but falls also on his client, for it is an offence to consult or employ, either personally or by agent or messenger, a witch-doctor in any of his varied capacities ; and to round up the circle the luckless agent or messenger is also caught in the net. To profess for gain any knowledge of witchcraft, or the use of spells or charms, or to give advice with the object of be- witching or injuring any person or property, or to supply any pretended means of witchcraft is to court disaster. Disaster is nevertheless courted very freely and widely, and the eleventh commandment — not to be found out — is successlf'ully observed in the majority of cases. Thus far the law in Natal, as set forth in the Native Code of 1891. In Zululand. to which most of the Natal laws apply, this Code is not in force, but speciil regulations, issued under Pro- clamation, follow much the san.e lines. Offences arising out of witchcraft are dealt with under Proclamation 2 of 1887, and to accuse another of witchcraft is an offence. No such cases can be tried by the chiefs (who have far wider criminal powers 194 THE MEDICINE MAN IN NATAL AND ZULULAND. than in Xatal), but it must be heard by a Magistrate. Native medicine men and herbalists receive attention under Zululand Proclamation No. 7 of 1895. The annual licence there, how- ever, is only ii. An alien doctor, from outside the territory of Zululand, is required to take out a monthly licence at the rate of 2s. 6d. 'for each patient he attends. No goats or beasts can be demanded to be killed, nor can the medicine man require that the meat of any goat or beast be supplied for the purjx)se of better effecting a cure. The reason for this is presumably two- fold— to 4)revent the doctor from increasing his preliminary fee by the acquisition of meat, and to dispel the idea that portions of these animals are a necessary requisite in the cure. It is safe to say that this prohibition is not taken very seriously. The earnings of midwives, both in Natal and Zululand, are not to be regarded as a personal perquisite, but belong to their special house : they, like all Native women, are minors in law, and act merely as agents. The fees due to them, and the debts contracted b} them in the course of their profession, can only be recovered or discharged by their principals — the husband, father, or guardian. It is the opinion of many that the licensing of Native d(Ktors is a mistake, and should no longer be permitted. By others it is contended that the legal restrictions which encircle them serve a useful purpose, and give some mea.sure o»f protection to their clients, who might otherwise be preyed U[>on to a greater extent if these restrictions were withdrawn. Not a few, notably cer- tain missionaries, think that the office should be abolished alto- gether, and that it should be made illegal for any Native to practice as a medicine man. There is one direct evil which should be remedied — the sale of so-called medicines by licensed doctors. This is especially the case in towns where, under cover of this licence, the vending of atrocities which are called medicines has become an established practice in the streets, and at recognized depots. These wares are not confined to roots and herbs, but include a variety of other products of high medicinal value, such as snake flesh and skin, powdered bones, portions of the dried flesh of wild animals, the fat of birds and beasts, mysterious powders, and the many other substances known to the Native pharmacopoeia. It may be of interest to give some idea as to the number of natives who have been granted licences as medicine men. In 1909 the numbers were : 754 in Natal, and 683 in Zululand. The total population is then shown as 1,039,269. of whicii 245,335 were resident in Zululand, and the remainder in Natal. (Fifty years before, the Native population in Natal was computed at 150,000.) According to the statistics of 1909 there was. roughly, one licensed doctor in Natal to every 1,050 Natives, and in Zululand one for every 360. In 1914 the number of practi- tioners for both territories is shown as 1,924. an increase of 487 in five years. To-day it is probably larger. There are many unlicensed men, especially in locations, who are content to save THE ^[F.nl(■I^^: max in natal and zululand. 195 their licence-money until >uch time as an evil chance may bring them to the notice of the authorities. There is no inspection of licenses, and if a doctor fall in arrear for two or three years he expects to have to make good the deficiency when at length seeking a renewal. There is a general tendency in speaking of medicine men to confuse them with witch-doctors and wizards, and to divide them into three classes — (i) witches and wizards, (2) the witch- doctor or smeller-out, (3) herbalists or medical practitioners. All Native tradition, however, points to the fact that the calling of the medicine man or herbalist is, anrl always has been, recog- nized as distinct from that of the witch-doctor, and still more from the dreaded wizard. It is true that a medicine man may deal in charms against witchcraft, and be ready to supply medica- ments for the frustration of the snares of the evil-doer ; and it is true, also, that the witch-doctor may combine the treatment Gif disease with his other functions ; but there is no connection between the training which a medicine man undergoes and the mysterious rites which the candidate for the office of a witch- doctor must oljserve in his novitiate. The medicine man, in the course of his experience, acquires a knowledge of certain reputed antidotes to witchcraft, and is often called upon to supply self- protective metlicines or charms to ward ofif the threatened evil, but he is not a smeller-out. The witch-doctor, in encroaching on the clinical preserves of the medicine man. does so by reason of his powers of divination. He traces the cause of the malady to rts tmdoubted source — the wizard — and prescribes the remedy. Nevertheless, there is a sharp distinction between the two pro- fessions— not arising out of legislative restrictions, but from ancient times 1)\ the Natives themselves. The witch or wizard ii far removed from both the witch-doctor and herbalist. He is the arch-fiend, the enemy of all, the source of every evil under the sun. His unlimited powers may certainly enable him to rival and excel the greatest accomplishments claimed by the others, but his works are the works of darkness, and he comes not to bless but to curse. Not even remotely would he be linked as an associate df those whose aim it is to defeat his machina- tions. It is quite conceivable, however, that if the medicine man and witch-doctor did not exist the wizard, too, might disappear. Of him. and of the witch-doctor, nothing further need be said; they make a fascinating study, but it is the medicine man proper and he onlv who is under present consideration. Although not capable of inspiring the feeling of dread which the mere mention of the Umtakati, or wizard, conjures up, or of commanding the same degree and respectful admiration accorded to the witch-doctor, the medicine man is yet a great power in the land. His orders are complied with, and his directions im- plicitly followed in a way which not every European doctor would be certain of; and his patients, if he be a man of repute, have faith in his ability and the efficacy of his treatment. This goes I(l6 THE MEDICINE MAN IN NATAL AND ZULULAND. ) far towards ensuring success ; at all events, in functional dis- orders. Suggestion has its psychological effect to perhaps a greater extent on the mind oif a primitive and illiterate people than on those of a higher standard of civilization. If the doctor says that a definite result will follow a definite course of treat- ment, that result is looked for with certainty. It is not intended to imply that the medicine man is a faith-healer, or that the suc- cess which often attends his efforts is simply the result of sug- gestion. The power of mind over matter is a recognised factor in disease, particularly those of a neurotic nature ; and the con- fidence which Natives have in their doctors is in itself a powerful aid to recovery. The medicinal qualities elf certain herbs and roots are well known to the Native practitioner, but he is seldom content to confine himself to these useful remedies, even in simple ailments. His knowledge of pathology is very limited — indeed from the standpoint of science it may be said to be non-existent ; his diagnosis is based on symptoms which, however misleading, he thinks he recognizes as requiring certain treatment, but of the cause, effect, and nature of the disease he troubles little. The cause is never looked for as a trespass against the laws of nature, but as supernatural, the w'ork of a secret enemy ; with the disease itself he has only such nodding ac(|uaintance as to seek to identify it, erroneously or otherwise, with i)revious cases within his experi- ence ; its effect comes not within the range of his study. Of therapeutics he has acquired some elementary knowledge, not based on scientific principles, but the outcome of a common sense observation of experimental treatment. He is not ignorant of the rudiments of pharmacy wMthin a strictly limited radius, and may occasionally be surprisingly accurate in his selection and prepara- tion of suitable remedies. His knowledge of animals, and the dissection of those killed for food or medicine, has given him some conception of anatomy and physiology, but he has never heard of the nervous system, and his ideas about the circulation of blood are vague; the aorta he associates with the seat of life, l)Ut since it is devoid of blood when examined he has no clear estimate of its functions. In dry- bone anatomy he might be able to make useful suggestions to a medical student who had just taken up that course, and he is well versed in many cif the organs of the body, and could give a super- ficial explanation of the purposes they serve. His experiments in surgery are crude, not to say barbaric : fortunately oi>erations of a serious nature are not readily agreed to by his patients. In mid- wifery it is seldom that the consequences to mother or child, or both, are otherwise 'than dire in abnormal cases, to which alone he is usually summoned. Instances to the contrary are alleged where the happy result has been achieved — or so it is claimed — by the administration of medicines only; but when the knife and other instruments are employed, injury is rarely averted. In attempting to arrive at a just estimate of the capabilities of. and degree of knowledge possessed by a body of men whose THE MEDICINE MAN IN NATAL AND /.ULULAND. ly/ numbers are considerable, it is impossible to do more than take the average as a basis upon which to work, and to seek to form an approximately correct conclusion upon that average. There is no school of medicine among the Natives by which their attainments may be judged; the apjiellation by which they are known is not communistic except as a title to distinguish them from other Natives; it is an individualistc community with a common object — 'the healing of disease — ^Ixit as to the methods employed, each man is more or less a law unto himself. While it is safe to assert that no single member of that community can be said to have even a moderate grasp of his profession as a science in the sense imder- stood by us, it would be incorrect to affirm that as a body they are so completely ignorant as to be incapaole of efifecting simple cures. Among them, as in every community, are to be found men of much greater skill than the average, who have some right to the reputation accorded to them; but if their standard were the aver- age it would still be so low as to bear no comparison with the lowest qualifications in therapeutics and pharmacy in any estab- lishment where these subjects are scientifically taught. To say that there is no school of medicine among the Natives is not to imply that there is no common use of the same in- gredients for the same purposes. There is little or no interchange of ideas between medicine men ; but the properties of certain herbs, roots, plants and bark which are widely used is common knowledge among them. So, also, in speaking of the medicine man as representati\'e df his class, it is asstimed that he has undergone, to some extent at least, the preliminary training which is expected of him. To-day there is probably an in- creasing number who seek to earn an easy if precarious livelihood by entering the " profession " without such training, and, whether licensed or not, pass themselves oft' as doctors. The medicine man proper serves his apprenticeship as a medicine carrier (Impakata or Uhlaka) or assistant to some one actually in ])ractice, and his novitiate may extend over a number of years. He is not at first permitted to do more than watch his master, and pick up what fragments of knowledge he may ; but in time he is allowed to help in the preparation of the various decoctions which form the materia inedica of the trade, and to administer them under super\ision. Later on he may be dispatched to visit a patient by himself to carry out some minor details of the course of treatment, and report progress. All this stands him in good stead ; he becomes well known and makes the most of the authority committed to him. Thus, eventually, when he breaks away from his instructor, and starts a practice of his own, he feels that he has graduated with honour and that his credentials are secure. He has probably paid a premium — ^perhaps a beast or two — for his tuition, and given his services free, and ma}' reasonably expect to reap his reward in due time. Not many, however, are now content to undergo a lengthy training. The demand for labour lias tatight them the value oif their ser\ices lo8 THE MEDICINE MAN IN NATAL AND ZULULAND. in the open market, and time is of greater object than it was in the days of their fathers. This, it may be conjectured, must tend to lower the standard of efficiency, and the average medicine man to-day may know less, for good or evil, than his predecessors. This possibly would not have ec[ual application where a son succeeds his father. The office is hereditary, and is not lightly permitted to die out in a family which for many generations has numbered one of its members in the profession, the stock-in-trade and goodwill passing from father to son. There are. of course, yearly accretions to the ranks by those who have no claim to the prestige which heredity affords. The Zulu medicine man is easily recognizable, with his strips of skin, tails, small baskets, horn, bottles and haversack. He is wiry and alert, for the ambulatory nature of his practice gives him exercise in plenty; and he carries himself with dignity. On reaching the kraal to which he has been summoned he is not forgetful to secure his iihigxa, or ])reliminary fee, before com- mencing his treatment. It may be that there has already been a death in the family, and that others are down with the same complaint. A goat must be killed, not only as a sacrifice to the ancestral spirits, but because its blood, and certain tendons and muscles, and other parts of the carcase, are required in the treat- ment. Incidentally, too, it is convenient to be assured of a supply of meat "during his residence at the kraal — which may extend over several weeks, for the treatment must not be hurried. If there have been unusual or mysterious occurrences connected with his patients, it is first necessary to safeguard them by a dose of insizi composed of many ingredients, such as burnt portions of flesh or skin and herbs made into a black powder, the effect of which must be heightened by certain restrictions or ukusila. These may take the form of abstinence from particular fcK)ds, or the avoidance of some customary usage. The evil having been thus countered, the potent eft'ects of the treatment itself must be corrected by a purification process known as ukupotida. The body must be washed or anointed with certain medicaments. followed by a dose olfi what is known as white medicine to dis- tmguish it from iiisisi, or black medicine, which it cleanses away. To further protect the kraal or the hut of the patient from the spells of a secret enemy, a preparation of the leaves of certain trees or herbs, usually found in secluded places, is compounded, and is kno'wn as Intclesi. This is used to sprinkle or cela around and within the hut by means of wild broom or small branches. As a still further precaution the ])atient may be given a charm or inifijigo to render harmless the intrigues of the evil one. Having thus secured him immunity from the sinister influences which are lield accountable for all untoward events, the doctor is tree to attend to the main purpose of his visit — the curing of the disease. Almost certainly an emetic will be given, made up possibly from a i^lant known as Matunga (Cyrtaniliiis obliguus) or any other plant cr root know'n to be efficacious. This may be followed by THF. MEDICINE MAN IN NATAL AND ZULULAND. I99 a clyster — (for both these forms of treatment are widely prac- tised, and are regarded as a specific for the removal of bile. If rightly prescribed, and medicines of a harmless nature used, they may form the most valuable part of the course ; hut several instances are on record where death has resulted both from the emetic and the clyster,* due to the inclusion of a poisonous ingretiient. If there is pain in any part of the body this must be removed by a counter-irritant. Cutaneous incisions are made over the afflicted spot, and a j^owdered substance is rubbed in. Mr. J. Y. Gibson, late Nati\e Commissioner for Zululand, informs me that he witnessed one of these operations at a Royal kraal, the peculiarity of which was that the assistant had a frog in readiness in a pail of water. After the powder had been rubbed in, the doctor took the frog and wiped off what remained with the mouth of the ifrog, passing it over the incised surface. Replacing it in the pail he then directed the assistant to take it back to the stream and let it go. The frog may in this case have been regarded as the scapegoat to take away and dissipate the evil which caused the pain. External. treatment is almost invariably complementary to the taking^ of drugs. (It is a disappointed native wdio comes away from a European doctor without a lotion which can make its presence felt on the skin.) In the preparation of prescriptions and the administration of the medicines, whether for internal or external use, there is much solemnity and ritual. The delibera- tion and care with which the ingredients — whether bone, quartz, (fat, snake-skin, dried flesh, bark, root, and the rest — are selected; the cutting oflt" of tiny fragments here and there, the roasting of some on the udcngesi, or potsherd, the pounding up of others ; the boiling of leaves and roots, the infusion of green herbs, the .scraping of tendons from the slaughtered animals, and the addi- tion df the requisite amount of blood — all this must in itself be an inspiration to the expectant patient and his friends. Elaborate instructions also are given for the taking of these nostrums. Interest may be further kept up by a little judicious cupping by means of a hollow horn. Possibly the condition of the patient requires something more drastic, and a pit or underground oven is prepared and heated, into which, when the fire is scraped away, he is placed. ( )r. instead of this form of Turkish bath — which is not popular — a shower bath may be prescribed. This is very reviving when the patient is in extremis, or thinks he is too ill to move. Herbs and medicines of the intelesi class are thrown into boiling water, and the patient is plenteously besprinkled over the body with a mixture hot enough to raise blisters. The idea that he is incapable of moving is thus effectively refuted. This is a u.seful remedy, irrespective of the nature of the disease — * The metliod of administering a clyster by means of a cow's horn is very arionrately described by Dr. Park Ross in his article "A fictitious Native di.sease — ifiifrrrbrdhln " iAinmlN of Tropical Medicine and Ftixis-ito- h^ny, 7, 371). 200 THE MEDICINE MAN IN NATAL AND ZULULAND. whether iniikiililaiie (a chest complaint, fevers, malaria, etc.) or any other. Not to unduly extend the somewhat comprehensive range of disorders which our modern ^sculapius is called upon to attend at the kraal to which he has been summoned, let it be supposed that one of the inmates is suffering from an attack of mumps. He cannot be expected to recover until he has supplemented his treatment by walking backward to an ant-bear hole into which he must shout " Zagiga, Zagiga. iigi yckc, ngi yekc!" (numips. numips leave me, leave me). His final cases mu.st be surgical. A collision with a kno'bkerrie has perhaps resulted in a fractured skull. The wound is well probed, and loose pieces of bone extracted. The aperture, by this time considerable, must be tilled up with a specially prepared suppository, and plastered over with cow dung. When septicaemia is well advanced the Euro- pean doctor will ])robably be sent for. No such necessity, how- ever, arises with the concluding operation — a dislocated ankle or knee. The injured limb is buried in the ground, and the earth made fast around it by ramming with a pole — then " a long, long pull and a strong strong pull "' by half a dozen stalwarts will soon give the required relief. It is not proposed to attempt to detail fully the course of treatment which a medicine man may follow in any particular malady, or to give an exhaustive account of the various methods that may be employed. The rough outline that has been attempted may serve to illustrate some of the ordinary ways of alleviating pain and suft'ering, without suggesting that they may not be varied according to circumstances, or necessarily be resorted to in every case. Imitation of the European doctor's methods is not un- common, and European medicines, especially powders, are a frequent addition to the dispensary of a native doctor, though he may know nothing of their properties and uses. In one instance arsenite of soda was administered in good Ifiaith, but with a tragic result. In another, a medicine man, who was impressed with the value of vaccination, inoculated a number of natives from the postules in a case of confluent smallpox. There were eight deaths, himself included, before the matter was reported to the authori- ties. Time is no object in the healing of disease — as distinguished from accidents which may obviously call for a less leisured attention, or snake-bite, where every moment is ])recious. The princi])le of " no cure, no pay " carries with it a hope for the best while life lasts, and ensures a long attendance in obstinate cases; not easily must the patient be surrendered — and if eventu- ally he recovers, whether as a triumph to nature in spite of the doctor, or to the doctor in spite of nature, the applause and reward (usually a beast) are claimed by the doctor. If the fates rule otherwise, the fault must he attributed, not to the medicine man. whose prestige may remain unassailed, but to a flank attack by the secret enemy, whose witchcralft has proved too strong. THE MEDICINE MAN IN NATAL AND ZULULAND. 20i In eitlier contingency the doctor is unruffled and philosophical, and may say with Milton I argue not Against Heaven's liaml or will, nor bate a jot Of heart and hope: l>nt still hear up and steer Right onward. He probably has several cases in hand at once, and conies out well enough on the average. His medicine is slow working; if a recovery ensues months after he last saw the jxitient, the credit is claimed by him — but he does not always get the cash. There are grades in the profession. Some medicine men never aspire to be anything more than herbalists jnire and simple — a sort of family doctor in ordinary ailments, and aliandoned for one of higher reputation when complications arise. Others, more ambitious, may be regarded as specialists, and will be sent for from long distances, or lengthy journeys undertaken to visit them. They are not averse to breaking fresh ground in new districts in the expectation that their presence will bring them further work to the discomfiture of the local practitioners. Some n/icn have secured fame in cases of snake bite. They have high confidence in their own abilities, and claim great achievements. One man, well accredited locally, informed me that he had never had a failure even with a black mamba { Dendraspis aiK/itsticcps) or puff adder (Bitis arietans) — a strong claim, and doubtful of credence. He gave me some of his isibiba, or snake cure, about the size of a ginger biscuit, not unlike cow dung in appearance, with an assurance that if it were dissolved in water and swallowed within a reasonable time^ — the sooner the better— the result was certain. Unfortunately no opportimity for testing it has presented itself. It is indeed difficult to test and authenticate a reputed cure. One case seemed hopeful. A girl was said to have been bitten by a black mamba, and the Chief's own special doctor, who happened to be within call, successfully admin- istered the antidote. I was satisfied that the girl had been bitten, and that there had been a swelling, and the evidence that it was a black mam'ba appeared irrefutable, as it had been killed and identified without question. Later on, I closely interrogated the girl, and she admitted that she had not actually seen the snake. as it was in the long grass, but that the next day a black mamba had been killed in tlie vicinit\ — the conclusion beino- certain that this was the reptile which had attacked her. More ])rabably the snake was one of less lethal ],i)\\er: the venom of a mamba acts with great rapidity and certaintx'. and half-an-hour's delay might place the victim l)e\i;n.d hope superstitious practices, and yet who still rank as medicine men and not as witch doctors, in that they prdfess no ]x>wers of divination. It has been made clear that stringent legislation has endeavoured to render it im]x)ssible for a medicine luan to resort to magic in any form in attending to hisi patients, but it is doubtful if there are any who do not transgress in some way or other. The description which has been attempted of the Native doctor and his methods is true enough to-day in spite of legisla- tion, useful though such legislation has been in checking illegal practices based on superstition and its ramifications. It has reference only to Natal and Zululand ; but, as a type, the sketch in its nnigh outline is perhaps sufficiently accurate to apph . luutotis iiiiifandis, to the Native doctor of all the Bantu tribes in South Africa. It is not sought to minimise in any degree the undoubted knowledge possessed by many of these men in regard to the useful qualities of certain plants as medicines — the male fern (Felix tnas) for tapeworm; the innondi (Chlorocodou- JJliitei) for indigestion and flatulence, and many others; but with this knowledge goes a profound ignorance o)f the dangerous and ix>isonus nature of other plants if recklessly used, not to mention the admixture of deleterious animal and mineral sub- stances with their prescriptions. When misadventure results and death ensues, it is often difficult for' the pathologist who may investigate the case to ascertain what poison has been introduced, the toxic f[ualities of many South African plants having yet to be determned by scientific research. In one such case, arising out of a charge of culpable homicide, it could only be said that 204 TIII^ MEDICINE MAN IN NATAL AND ZULULAND. possibly it was tlie uuihlonlilo {Euphorbia grandidens) which had been used, but no definite opinion could be given. What, then, is to be the future of the medicine man? For many centuries he has been an integral part in the life of the ])eople ; he has their confidence to a remarkable degree, although that confidence may l)e founded largely on superstition ; he is often the only available source from which they may seek to obtain assistance in time of need, and that assistance is sometimes attended with results which are unquestionably beneficial. On the other hand, he is responsible for many evils, his methods are crude and unscientific, often barbarous, and fraught with considerable danger to life; and he is an active factor in pro- moting and fostering a belief in witchcraft as the source of all evil. Should his office be prohibited by law? ought further re- strictions to be imposed? or should all legislation be withdrawn and he be regarded merely as a part of the domestic economy of the Native, without interference on the part of the governing powers? However variously these questions may 'be answered, it will have to be recognized that, whether by warrant of law, or w^ithout. the medicine man will long continue to exist in those districts which are not in close touch with civilization. The solution of the problem may lie in the gradual elimination of the medicine man by the substitution of educated natives who have received some degree of medical training. The evolution df a practical scheme, even if only experimental in its nature, should not present insuperable difficulties. As regards midwifery, something has already been done l)y a Natal doctor who has a large Native practice, and who has trained or is training Native women with encouraging results. Confidence in the European doctor is increasing, especially among Natives who have come under direct civilizing influences. Those who are more highly educated would seldom elect to con- sult a medicine man unless impelled to do so by their friends. Many raw Natives have learned to discriminate between skilled and unskilled treatment ; yet many a life is lost through the refusal of parents or friends to allow a child or relative to have proper medical or surgical attendance when such is proferred. Rather must the patient be taken back to the insanitary condition of kraal life, and the ministrations of a Native doctor. Especially have they a dread oi hospitals ; nor will they readily consent to an amputation even as the last means of saving life. The problem generally is one of much per])lexity, but in the interests of the Natives themseh es it should be faced. Postscript. — The Rev. A.T. Bryant has devoted much time to the study of Native Medicine. His interesting and able article " Zulu Medicine and Medicine Men " {Annals of the Natal Museum (1909) 2 [i] was not available for reference when this paper was written, nor was there opportunity to seek for further literature, if .such exists, on the subject. (Read, July gth, 1918.) SAFETY IN WINDING OPERATIONS. By J. A. Vaughan, M.I.C.E., MT.Mech.E. (Read July lo, 191 8.) The author has chosen a title which covers a very large field, but intends to confine his remarks in the main to the ques- tion of the safe handling of the winding-engine, having recently dealt with the subject of the winding-rope in the proceedings uf another institution. On the Witwatersrand, besides a large number (about i.oooj of small auxiliary hoists or winches of average horse power — t6 steam and 65 electric — there are installed main winding plants to the extent of 443 in number, of collective horse power totalling 173,038. These statistics refer to 31st December, 1916. and are the latest obtainable. The comparative figures subsequently tjuoted will therefore be taken for that date, although later figures are in these cases available. Of this total of 443 main winding plants, 262 are driven by steam and 181 by electric motor. The number out of use is not known, but the published return shows that 372 were licensed for the conveyance of persons, the maximum capacity of the con- veyance being rated for 10,790 persons. Taking 200,000 persons as the number employed under- ground on the Witwatersrand, it would need only 20 trips to lower and raise this complement in the 242 shafts. But the lowering and raising operations are not always simultaneous, the loading of the cages is not always up to full complement, and the trips at the beginning and end of the shifts are not nearly all the occasions on which persons are being transported. Instead of trying to estimate the number of hoists in which there is a human freight, it is better to regard the general wind- ing operation in trying to estimate the accident risk. It has also to be remembered that accidents such as overwinding cause annually great and expensive damage to plant, besides the personal casualties that will be treated later on. Let us suppose, what are very close to the facts, that 400 main winding i:)lants are regularly at work, and that an average of nine trips per hour are made ; a " trip " being the downward and upward journey of the conveyance, whether the companion drum is sinmltaneouslv in motion or not. The annual total will be just over 31.000,000. while the winding accidents such as we are considering amount to about 62. ecjuivalent to a rate of i in 500.000. This low accident rate could be regarded with complacency if it were felt certain that the mistake was in all cases inevitable and the resulting accident absolutely unpreventable. Regarded in another way, it may be assumed that 800 certificated engine- drivers are responsible for 50 accidents annually, so that if each driver was restricted to one accident he would have a chance of 2o6 SAFETY IN WINDING OPERATIONS. driving for i6 years. However, it is usual for a first offence to be dealt with by an official caution, subsequent offences by short ]ieriods of suspension, while it is extremely rare for a driver's certificate to be cancelled. It has never been proved that suspensions of certificates or ])rosecutions in the Criminal Courts have ever actually brought about a reduction in the number of winding accidents, but those who await the proof before believing, and who are unprepared to allow that any deterrent effect is produced in the delinquent, will still doubtless admit tlie possib)lit\ or even ])robabih'tv of " encouraging the others." It is fairly certain, however, that, if the supply of capable drivers is not maintained, the accident rate will increase. The training of winding-engine-drivers has been discussed off and on for the last 15 years, but no satisfactory scheme has been evolved. Since the year 1904 there has been a provision in Regulation 308 (5) for a sort of adult apprenticeship. This regulation allows of a person being accepted as a candidate U>r the vhia-vocc examination who, having had one year's charge of engines or boilers, including at least six months' charge of a reversing engine, has also served six months' ap])renticeship tmder a certificated driver in a main hauling engine-room. This plan has not been so successful, no more than ore candidate ]»er annum having been trained. The greater number of locally-trained winding-engine-drivers (jualify under Regulation 308 (4) for examination on small rock hoists and winches. This regulation states the condition. vi:~., " that he has had at least one v^ar's charge of an engine or engines used in the ordinary hoisting of minerals, unless he is the holder of an engine-driver's certificate, in which case a period of six months shall suffice." It has to be remembered that 21 is the mininumi age (jf applicants for winding-engine-drivers' certificates. To enable the youth of the country to qualifv in the best way. it remains to be decided what is the most suitable training between the ages of 16 and 21. The author feels disposed to commend a system proposed to him in 1916 by two eminent engineers who were then considering apprenticeship schemes for the various trades. The ]>roposal was that the engine-driver apprentice should after two years in the Trade School serve one and a half year? learning fitting and turning, one and a half years tending boilers and engines, and the remaining time (at least 12 months) imder a certificated driver in a main winding-engine-room. The number of candidates presenting themselves for exami- nation has been diminishing, the average number of certificates issued annually during the last five years being less than 50 cent, of the average ntunber issued during the |)receding similar period. The most recent figures available as to the number of certificated winding-engine-drivers in service on the mines of the Witwatersrand relate to the ist August. 1916, at which date SAFET^ IiX WINDJ.NG OPERATIONS. 20/ there were 'j<<)'j driving-engines licensed for the conveyance of persons, 15 ch-ivin^ nnhcensed hoists, whilst 2}^ were otherwise employed. If 3 per cent, is a reasonable wastage to estimate, then at least 40 new drivers should be produced each year. The average number of certificates issued by the Johannesburg Board of Examiners for the past five years has been only 24, so that it appears (juite time that a satisfactory and popular system of apprenticeshi]) be put into operation if the mining industry is to continue (»n tlie same scale as at present. It would be very rash, however, to sui)pose that an assured satisfactory- supply of perfectly-trained winding-engine-drivers, even working shorter shifts and medically inspected periodically, as has l^een sometimes suggested, would entirely provide against " overwinding " and " runaway '' shaft accidents. By closely considering the nature of the winding-engine-driver's duties it mav be seen that some small proportion of errors should be regarded as inevitable. The right thing must always be done at exactly the right time, and a moment's lapse at the critical instant is very likely to lead to disaster. In endeavouring to prevent mishap following on the error or omission, it is therefore wise to employ all automatic safeguards that engineering ingenuity can devise, provided that no new elements of danger are introduced that are not of less possible consequence. Before considering the safety aj^pliances at present in use. tiieir more general application and the possibilities of the intro- duction of further preventive measures, attention may be directed to the classes of accident that now occur, and their frequency and imjjortance. compared with other shaft accidents. The accompanying table shows this comparison for a period of ten vears. From a study of the figures in the various columns it will l)e seen that, excejjt in the cases of the lirst and second columns, the percentage ligures for Class T ( " ( )verwinds and Runaways") and Class II ("Ropes, Chains, or Connections Breaking " ) are fairly low. The non-casualty accidents report- able under Regulation 274, outside the two classes just mentioned. ma\- obviously be expected to be of much rarer occurrence, and the liigher percentage ligures in Column 2 in these classes should not occasion any surprise. It may be of interest to i)oint out here that the classes of accident that ])roduce the great bulk of the casualties in shaft accidents are " Material ( stones, timber, tools, etc.) falling in shaft"; "While ascending or descending bv machinery — exclusive of accidents under Classes I and II " ; " Struck by cage or skip " ; and " Miscellaneous." Tlie meaning of the term " overwinding " is that the conveyance is either raised or lowered too far, but, in the case of a non-casualty accident it is not supposed that a failure exactly to meet the landing is reportable. In the crise of a " runaiway.'' it is meant 208 SAFKT\- IN WINDING OPRRATTONS. TABLE SHEWING FOR MINES OP TR.\NSVAAL(>NLY SHAFT ACCIDENTS FOR THE YEARS 19<)8-1917, WITH CLASSES 1 AND 11 OF SAME SET FORTH FOR COMPARISON WITH TOTALS. Ye a Total Number of Separate Accidents. Not causing persona injury. Under Reg. 274. Causing personal injury. Casualties Fatal Non- fatal. Deal lis. Wht. Clrd. Total Injuries Wht. Clrd. Total 190S 1909 1910 1911 1912 191.H 1914 1915 igiC) 1917 Averages . . Percentasres of Total Shalt Accidents. 37 78 53 80 75 74 58 53 52 60 62.0 14-3 Class !.— Oveuwi.nhs di; RqNA\v.>vs. 27 57 36 55 50 61 44 46 36 45 46.3 eo.6 0 11 4 10 11 (; , 18 7 10 9 10 8 5 9 2 5 12 4 II 4 9.C 0.1 5 8 3 2 17 3.4 14.1 6 r- — 17 IS 3 17 21) 2 ■29 32 3 '^1 31 5 21 22 f^ IS 21 7 2 2 3 12 29 10 ! 12 13 5 1 10.1 19 5 4.3 9.4 10 0 ss 5 14 13 25 20 H 14 2 15 10 12. 7.0 5 17 15 28 2') 13 21 5 25 15 16.9 7.3 Class II.— Ropes, Chaiks, or Conkecttons Brivakino. Exclx'sivk cf Breakages DUE TO OVKRWINDS OR Ru.VAWAVS. 1908 1909 1910 1911 1912 1913 1914 1915 1916 1917 Averages 17 14 14 15 11 17 £0 20 30 .30 19.4 Percentages of Total Shaft Accidents. 4.5 9 8 9 10 8 7 14 13 17 16 11. 5 4 ^ 4 1 9 5 4 9 7 5.2 1 14.5 3.1 1 — 1 2 7 1 3 1 4 . 7 1 1 - 3.1 08 5 11 8 1 11 7 5 10 6 8,1 9 5 10 8 1 13 8 6 16 7 8.9 1.6 3.3 i 4.7 4 0 — 6 — 3 — 1 1 2 4 1 8 4 9 — 3 _ 10 9. 7 0.8 5 16 2.9 6 3 1 3 4 9 13 3 10 9 6. 2.6 Total Shaft . \CCIDENTS. 1908 354 44 169 141 18 162 ISO 32 129 161 1909 481 113 206 162 24 201 224 47 148 195 1910 474 53 219 202 25 226 251 69 168 237 191 1 523 71 235 217 33 240 273 68 209 277 1912 547 81 196 270 23 215 238 53 274 327 1913 456 92 152 212 26 161 190 57 203 260 1914 407 80 126 201 19 139 158 54 195 249 1915 4fO 82 136 182 17 130 147 48 162 210 1916 362 74 118 170 35 125 160 47 189 236 1917 319 74 112 133 21 105 126 31 133 164 Averrges .. 432 3 76.4 166 9 189.0 1 24.1 170. e 191.7 tO.6 181.0 231.6 SAFETY IX WINDING OPERATIONS. 20g that the w inchiig-druiu has hecome uncontrolled, ht-ing in-hand neither hy the clutch nor hy the brake. Overwinds or runaways due to defective plant amount to about 14 per cent, of the total, that is to say. nine out of the average of 62 may be so classified. The two chief causes of this class of accident are: (i) Troubles with the reversing or control lever ; correct design and regular examination should provide against these. ( 2)F"ailure of the depth indicator to record j^roperlw Chain and sprocket drives have been mostly at fault. They should be watched and the chain not allowed to become too slack. In the one or twti instances where rod and pinion drives have failed, the keys <»f the wheels have been allowed to become slack and drop out. Here again watchful care should be exercised. It is reall}- doubtful in some of the cases just mentioned, and others in which the .locking devices of clutches or brakes have failed, whether the accident should not really have been attributed to the driver's deficiency in the matter of close insj^ection of the j)lant m his charge. There have been a few instances of the failin-e of friction clutches due to the iractru'e of some of the parts transnu'tting the l)ressure from the toggle to the eyes of the clutch bands. If the adjustment of the toggle is set incorrectly, so that the toggle lever approaches the vertical, these ])arts and the bands themselves may be stressed to the breaking point. The adjusting bolt at the fixed end of the bands also re(|uires some freedom of motion in its attachment to prevent the occurrence of dangerous repeated bending stresses. Occasional annealing of these parts is also desirable. Engineers who have to deal with this class of clutch are, however, generally aware of the necessity for these precau- tionary measures. In this connection the accident in 191.^ at the " Edgar's " shaft of the Mysore ( lold Mine may be mentioned, in which 42 persons were killed outright. Deducting from the total of 62 — 9 ^= 53, a small number of accidents due to miscellaneous causes, such as faulty signalling, physical incapacity, or distraction of attention of driver, etc., etc., it a])pears reasonable to regard 50 overwinds or runaways as being the average number that occur annually due to the faults or omissions of the winding-engine-drivers. These may be classified as follows :— 1. Starting to lower with the reversing lever in the position for raising. 2. Proceeding too far at the conclusion of the wind in either direction. 3. .Allowing a drum to run away through faulty application of clutch or brake. Dealing with Class i, it has to be noted that this fault has been somewhat checked dtu'ing recent years owing to the intro- duction of Philip's patent safety device. This invention links up the reversing lever, or some part of the gear, with the ])ointer of the depth indicator by means of an electric circuit, which remains 2jO safety in winding operations. open normally, but becomes closed if the reserving lever is not in the correct i)osition when the cage or skip enters the " danger zone." When the circuit is closed, an electric hooter or loud- sounding bell comes into operation close to the driver. The chief reason that Philip's safety device, although litted, has not prevented accidents in many cases, is that, as most of the licensed winding plants are used for ordinary rock hoisting as well as the conveyance of persons, the contact whicli closes the circuit has to he set for the tip. that is, unless there is a two-way switch in the circuit to be operated by the driver when the conditions of hoisting alter. If there is no such switch, and the driver does start to lower with lever in the wrong direc- tion, a certain amount of speed is acquired before the warning is given, and an accident is not averted. This also may occur if the device is set too "coarse," as it may be in some cases where a "fine" adjustment leads to a frequent blowing of the hooter, which irritates the driver. Incident- ally it may be remarked that optical warning signals, such as a red li.ght, have been found to be of little effect for the circumstance under consi- deration. The htting of the two-way switch is not itself sufficient for the change-over may be forgotten. It is really necessary to interlock this switch with another one in the bell circuit, so that reply, " three bells." signifying that persons may enter the cage, cannot be given by the driver unless he has set the Philip's device for the bank. Exact adjustment is not ahvaj's possible, owing to slack motion on the reversing and indicating gears, and, unless the warning is given directly the lever is out of the neutral, it is too late to be of service. Failures also have occurred through rope grease being thrown on to the contact plates, cither at the Iiack of the indicator dial or on the driver's platform. Class 2 must be sub-divided for full consideration. Sixteen years' experience guides the author to the following classifica- tion : — (f the blocks which accom- panies the [lerformance of this illegal act, are of no use after a certain speed of descent is attained. It n')w remains for consideration as to how far castialties to persons and damage to plant can be prevented by means of auto- matic contrivances in the event of the (Kctirrence of any of the lapses eiuimerated in Classes 2 and 3. Dealing with Class 2, it may at hrst be remarked that over- winds do not generally take place with the conveyance travelling at any great speed. In these cases, therefore, as also in those occurring under Class 1, a detaching hook is a very reliable safeguard. These hooks have in almost every instance been effec- tual unless the speed is too great, and many lives have been saved during recent years oh the W'itwatersrand through their instru- mentality. In one case, in 1916, a cage carrying 19 natives was safely held, but unfortunately the shock was so great that two were seriovisly injured, one of them subsequently dying. Again in 19 1 7, at the Simmer and Jack, when the morning trip was going down, a cage loaded with 24 natives was raised, instead of 2J2 SAFETY IN WINDING OPERATIONS. lowered. The detaching hook did its duty, the conveyance being safely, suspended, and the occupants sustaining no casualties. Detaching hooks are not fitted to cages or skips running in every vertical shaft, for various practical reasons. They are not considered suitable for use in incline shafts on the Rand, although in the case of another African gold field thev have been, and possibly still are, used as a safeguard against the vagaries of the native engine-drivers. In one " compound " shaft on the Rand the " Humble " hook has been successfully adopted, in this case necessarily fitted quite close up to bridle of the skip. There have been a few cases of detaching hooks failing during the process of the vertical hoist, the assignable causes being — {a) rocks falling and striking the wings of the internal plates; (b) brittleness of the hooked end of these plates, which might have been ])revented by more regular annealing. With respect to the process of annealing, the following table may be quoted containing the recommendations of the American Society for Testing Materials : — Range of Carbon Content, Range of Annealing per cent. Temperature, Degrees C. Less than 0.12 S75 to 925 From o. 12 to 0.29 840 to 870 0.30 to 0.49 815 to 840 0.50 to 0.90 790 to 815 From a pai)er recording the results of a series of experiments carried out in the U.S. Naval Yard, Boston, presented by Messrs. ^\'ebster and Patch, to the American Society of Mechanical Engineers, in December, 1916, it is noted that iron for annealing should l)e heated to about 950 degrees C, insead of 890 degrees, as was the j)revious practice. Heating to this temperature and cooling in air gives strong and better chain than heating to lower tem])eratures, and higher tem]>eratures give no imp'-ovement. The air should preferably be still, and there should be ])rotection from rain or snow. These chain cable results are quite applicable in tiie case of t-age or ski]) connection, whether safety-hook, draw-bar. bridle, or link. It has been noted that the detaching hook is of no avail in the case of an overwind at speed, and in this respect it is subject to the same limitations of successful employment as other safety devices which aim at avitomatically applying the brakes to the (^Irums when the conveyance reaches the " danger zone." The necessary safety arrangements are evidently: — (a) the requisite movements of the control or reversing levers so that speed mav be reduced before ( h) the automatic ajiplication of the brakes. It is now well known that compliance with (h) is ineffec- tual unless (a) is also com])lied with previously and adequately. Tliere is no difficulty in complying with ib). This is done SAFETY IX WINDIAC Ol'liKATIONS. _' 1 J automatically, with success, by such i^ears as the " Whitniore," the " \'isor," and others. There are ditiiculties in the \va}- of comijlying with (a), i'his operation must not be too gradual or winding speed is sacrificed. The only successful ai)paratus in use on the Rand for this purpose appears to be that htted to several of the \\'ard-Leonard sets. 'J he operating cams in these instances ar;.' readily adjustable to suit various conditions of winding, in tiie case of Ward- Leonard hoists, the speed that the conveyance travels, whether empty or full, downward or upward, is i)ractically fixed for any definite position of the control lever, and in api)roaching i or when at) the neutral, there is consideraljle braking effect, due to the regenerative action of the motors acting as generators. The three-phase winding-engine resemljles more the steam- winder, in that the s]:)eed for any position of the contrcr] lever depends on the load as well as on the extent to which resi>tance IS applied in the rotor circuit. The eddy-current brake, howeven if applied to either of them would, inde])endent of the 1; ad or direction of motion, so redtice the speed of the drum tiiat the mechanical brakes, if automatically applied, would effectively prevent an overwind. The E.C. l^rake should, of course, also be automatic in application, both for overspeeding and for o\er- winding. The automatic apparatus for either (a) or {b) has, except in the case of winding ])lant used solely for persons, to be set and reset, to provide for the journey to and at, either the collar of the shaft or the tip, and this setting should not be " permissive," but " compulsory " on the part of the engine-driver, or absolutely out of liis hands. There are two or three local inventions installed embodying this principle, or some approach to it. It is therefore very desirable that the working of these appliances be en(iuired into, and that those found to be really reliable should be brought into general use. Tt has been oljserved that the induction motor in regard to its suitability for speed control against overwinding is not so w cH fitted as the direct current winder, but attention may be directed to a description of three devices designed to eff'ect this pur])ose contained in an article entitled, " Electric \\Mnding for Mines," by W. I\. Evans, R.Sc. (Eng. ), ptiblished in the Mining MiU/a.cinc, London, September, 1917. It is to be ho])ed that the a])p1icability (if these inventions, under the conditions of winding on the Rand, will l)e seriously considered, and that a suitable apparatus ma\- be installed for trial before long. With regard to (7^) and (c) of Class 2, the author can only advertise the necessity for invention in respect of the ])revention of these contingencies, and regret that up to the ])resent nothing satisfactory has to his knowledge been suggested. The contingency referred to in (d) of Class 2 has l)een so ably dealt with by Mr. G. K. Chambers, in his paper on " The 2T4 SAFETY IN WINDING OPERATIONS. braking of high-speed winding-engines,"'* that it appears quite unnecessary to add anything further on the point, except to recall that Mr. Chambers was not in accord with the arrangement as installed on the winding plant which he was describing, whereby the failiu-e of current led to the automatic apjjlication of the inechanical brakes, the eddy-current brake being available for hand application by the driver, lie ])referred the reverse of this proceeding. Class 2 {e) deals with a class of accident which is fortunately very rare, and which no properly-trained driver is ever likely to cause. An automatically-operated overspeed device, bringing an eddy-current brake into action, would of course prevent harm resulting. With regard to Class 2 (/), a safety ])recaution might easily be applied to prevent the control or reversing lever being moved into the downward position when the opposite clutch is " out.'' This might possibly, under some circumstances, hamper the driver in his handling of the engine when just starting to lower. With further reference to Class 3, it remains to be stated that it is a growing practice to interlock the levers on the operating systems of the brake and clutch in a similar manner to that adopted on the railways to link up signals and ])oints. This is effected in many diti'erent ways, there being no standard method, each winding-engine receiving api)ropriate treatment. Where the clutches are operated by steam, it is better for the pin-pose of the lock to utilise the movement of the clutch itself, and not merely that of the slide valve of the clutch engine. Sluggish action of this engine is then provided against, and it becomes impossible to luiclutch a drum unless the corresponding brake is properly applied. A runaway drum, es])ecially if of the cast-iron variety, is a very dangerous hap])ening, similar to a flywheel explosion. The whole winding-rope is usualh- lost ; much damage may be caused to shaft, track, and timbering, and, if the drum fractures when the rope has run out to the end, there is great likelihood of tlie engine-room being comi)letely wrecked. The Eddy current brake j^rnvides an ideal method of safe- guarding unclutched drums. Mr. Chambers suggested that with steam-winders the existing current for the brakes could be conve- niently obtained from a small direct converted steam-driven generator, situated in the engine-room itself, but it has to be remembered that on several of the older mines, where steam winding prevails, direct-current clectricit\- is imiuediately avail- able. The Kddy current 1)rake does not actually stop all motion, but it brings down the speed to a low value, so that counter current or the mechanical brake can be used safely and success- fully to bring the drum or the hoist to rest. *Journ. S.A. Assoc, of Engineers. Nov. 1912. SAFETY IN WINDING OPERATIONS. 21 5 After preaching the gospel of tliis safety brake to a leading " safety-first " financier the other clay, the author was immediately asked the question, " What is it gouig to cost?" In looking into this important matter, it has to be acknowledged that the extra cost is serious, bringing up the price of an A.C hoist, fitted with E.C brake, to just about that of a Ward-Leonard set. Mr. Chambers stated that the cost of the E.C. brake for a five-ton hoist, with a rope speed of 3,500 per minute, was £2,000. Mr. J. H. Rider, at the Institution of Electrical Engineers, 1915, in his paper on " The Power Supply of the Central Mining Rand Mines Group," gave the cost (with the motor, generator, etc.) as nearly two-thirds that of the winding motor. He also stated that ail expenditure of energy at the rate of about 45 K.W. in the field magnet system of the E.C. brake obtained a result equal to a rate of about 1,600 K.W . in the case of counter current braking. This comparison invites the author to make a few closing remarks v/ith respect to electric winding. The A.C. hoist can j^robably be made as safe as the Ward- Leonard, and doubtless when normal times return further steps will be taken in this direction, 'ilie author was present at tUc tests varried out on the A.C winding hoist at the Village Deep, Ltd., when, witli an unl)alance(l load of y,ooo lbs., the speed was reduced from 3,000 to 250 feet ])er minute in a few seconds, one d(jzen being al)out the figm-e. \\'ith a \\'ard-Leonard set at the Consolidated J.anglaagte, he had the privilege to witness an important test, of which the following details give the description. The winding motor was accelerated as quickly as possible, until a normal rojje speed of 2,500 feet ])er minute was reached; the driver was then taken off the platform and the hoist allowed to com])lete the wind with only the safetv-gear controlling it. The cams l)rought the winding drmns to an almost imperceptible cree])ing speed, and when this speed had caused a sufiicient jiressm-e to bear on the brake trigger gear, the brakes were ap])lied, the current cut oft", and the lioist brought to rest. This test, the antlior is informecl, is ap])lied to the Ward-Leonard hoists of this ])articular group once a week. If a thi'ee-])hase hoist be installed where the winding c\cle IS sucli. in ordinary l)alance winding, that the upward load always overbalances the downward load, then if failure of current takes jflace, it is obvious that before the hoist could run awav the rope direction nnist be reversed, and the load which before the failure was l)eing wound ]n an ujnvard direction nmst change to a down- ward direction. ( )l)viously, then, at some moment the load will 1k' stationary, and therefore the automatic application of the I)rakfs will ])ull the hoist u]>, and no runaway will take place; whereas if the downward load overbalanced the ui)ward load, and a failure of power took place, the direction of hoisting will not be reversed, the speed will be accelerated, and the ai)plication of the brakes w ill l)e ineft'ectual. With the Ward-Leonard lun'st. although 2:6 SAFETY JX WINDING OPERATIONS. the failure of power has taken place, the regeneration control will not be absent, because the winding motor, acting as a generator, will raise the speed of the converter set, thus assisting the brakes to pull the hoist up. It appears, therefore, that in any winding proposition in which the downward load at any period of the cycle overl)alances the upward load, the \\ ard-Leonard type of hoist is preferable, but when the upward load predominates throughout the whole wind, the three-phase motor is the more suitable. The autliur, in conclusion, expresses the hope that the statis- tics, facts, and opinions cjntained in this short paper will tend to stimulate the " safety-first " movement, not only in tlie winding engine-room, but in the office of the consulting engineer. Atmospheric Nitrogen. — According to The Ameri- can Fertiliser * a very important syndicate has been formed in Great Britain in connection wth a large chemcal company which proposes to utilise the hydrogen — at present a waste product from the company's plant — for the fixation of atmospheric nitrogen, and also for the manufacture on a large scale of ammonia and nitrates. The company's waste hydrogen has been found to be of high purity and suitable for the manufacture of svnthetic ammonia. The WORLD'S Wheat Crops. — TheBulletin of Agri- eiillural and CoiiiDiereia! Statistics, pul^lishefl by the International Institute of Agriculture. Rome, states that Canada estimates its 191 8 wiieat cro]) to yield 70,045 ([uintals, about one-tenth more than in 1917, atid very nearly equal to the average yield during the five years from 1912 to 1916. In the United States a cro|) of 242,495 quintals is the estimate. The aggregate yield of the four countries, Canada, United States, British India, and Tunis, of which three arc quite the largest exjiorters of wheat at present, was 418.574 quintals in 1918. against .HS-'^SO in 191 7 and 387,905, the average from 1912 to 1016. As regards rye. the yield in the United .States will this year attain 20.'/2'j (iiu'ntals. Research Grants. — The Council of tlie Royal Society of .South Africa has recently awarded the following grants in aid of research : — Prof. M. M. Rindl. Ing.D., £40, for continua- tion of investigation of the active princii^les of toxic and medicinal indigenous plants. Mr. I. .'^. van der Lingen, R.A.,£too. for continu- ation of researches in radiology and cr) stallography. Mr.C. R.Har- denl)erg. M.A.. £40. for a study of the fann"lv Psvchida- ;md other I.epido|)tera. Mr. .S. H. Tlaughtou. P>.A.. £40. for investigation of the vertebrate and invertebrate fauna of the .'^t. »rmberg Reds, mainly in the north-eastern portion of the Ca|)e Colom . Mr. R. W. P. Tucker. R..A.. £40. for the stu(l\- and collection '>f the Arachnid fauna in tlie Pastern Transvaal. Pxdenburg I)istrict, Selati Region. *49 (tot8^ f.^1. 152. THE MKDICINAL SPRINGS OF SOUTH AFRICA SUPPLEMENT I. Rv Vroi. Max Morris Rindl, Ing-.D. The sympathetic reception which was accorded to my paper on tlie medicinal springs of South xAfrica, read at the Maritzburg meeting of the Sotith African Association for the Advancement of Science in 1916,* and the encouraging criticisms that ha\e come to my notice, have inchiced me to continue the work of collecting information on the subject. My hopes of being able to throw more light on the prol)lem from the therapeutic point of view have not been fulfilled, but I am in a position to add several new springs to those i)reviously recorded. Among these the springs cle fissure. The strata on both sides of the fissure show no signs of vertical displacement relati\e t(^ one another, so that, apparently, no faulting has taken place. The extent of the original fissure is indicated by a vein of quartzitic material of 15-25 metres breadth, which forms the continuation oif the springs' fissure. This vein has been traced to a distance of roughly 3.4 km., and runs in a more or less north-southerly direction. The brown and yellow colour is due to deposition of, and impregnation with, iron hyd.-ate. The nature of the quartzitic material (crystalline (|uartz and chalcedony), and its structure (variability in trans- parency and colour) characterize it as a deposit from aqueous solution. Orif/iit of fhc Sprhu/s. — 'I'he high temperatures show t!ie springs to be of deep-seated origin. There is ample geological evidence that the micaceous .schists extend to a very considerable deptli. so that the rate of increase of the temperature downwards is pr(.bal)ly uniform. Taking the average temperature of Gross- * Kept. S.A. Ass. for Adv. of .SV., Maritzburg (1910). 028-5.52. i From an iiii|iiilpli^lu'il lopnit on tlie Windluik niiiicnil sprin;,'^. by Di. Kroncnkcr. 2l8 THE MEDICINAL SPRINGS OF SOUTH AFRICA. Winclhuk (^19.2°) as being the temperature of the upper layers of the rock, and the maximum temperature of the water (77-5°) as that of the lower layers from which the water derives its heat, the average difference of 58.3° between the surface and lower layers at the " eye "of the springs, gives a depth df origin of at least 2,000 metres. The temperature gradient is taken as 33 met.cs per i°C.* No allowance is made for the cooling effect of the rocks before the water reaches the surface, nor for the possible infiltration of cooler surface-waters. Such corrections, if data were available, would give a higher figure than the one calculated above. Considerable discussion has centred round the question whether the water of the springs is of meteoric origin, (vadose Thermen), or whether the water is liberated from the magma as water vapour or even hydrogen under high pressure (juvenile Thermen). Although the question has not been solved definitely, the balance of evidence is in favour of the asstmiption that the springs are, at least in great part, of the latter origin, namely, the high and uniform temperature, the regularity of flow, the independence of the water supply elf seasonal variations in rain- fall, and the considerable amount of free carbon dioxide and carbonates dissolved in the water. Chemical Nature of the Water. — The composition of the residue from 100,000 c.c. of the water of the Pahlquelle, heated sufficiently high to decompose bicarbonates and hydrates, and to drive oft' water of crystallisation, is as follows* : — NaCl 10.7 grams. Na^SO^ 12.78 grams. Na^CO. 32.OT grams. K,SO^ 8.80 grams. MgSO^ 3.08 grams. CaCO;^ 8.93 grams. MgCO, 1.45 grams. ALO.^ 0-70 grams. SiO. 8.90 grams. The water contains appreciable amounts of free carbon dioxide, so that the carbonates of both the alkalis and alkaline earths should be calculated as bicarbonate ions. Lithium and other balneologically important constituents are present in small quantities, but the actual amounts have not been determined. In estimating the proximate composition of the mixture of saline constituents of a water the silicic acid is usually regarded as uncombined. Whilst this assumption, even ilf incorrect, in- troduces no appreciable error in the majority of cases, it is wholly unwarranted in the case of hot alkaline springs like those * In tlip discussion of the .paper it was suggested that this figure is too h>w. t Dr. K. Renz, " I l)er die Eignung der Windhuker heiasen Quellen zu Heilzwecken," from Der Weltkrieg, Windhuk. .Tune, 1917. THE MEDICINAL SPRINGS OF SOUTH AFRICA. 2I9 of Windhuk. In the table of ion equivalents the silicic acid has been calculated both as the ortho- and meta-acid. The values for the ion-equivalents are obtained as usual b}' dividing the weight of each ion (expressed in grams per 100,000) by its atomic weight (or the sum of the atomic weights), and multiplying by the valency in order to obtain monovalent ions. Table of Ion Equivalents. Cations. Anions. Ka 0.9669 X I = 0.9669 HCO. 0.40CS4 X I = 0.4084 K 0.10099 X I == 0.10099 SO^ 0.166 X 2 = 0.3320 Mg 0.04278 X 2 -- 0.08556 CI 0.1830 X T -- 0.1830 Ca 0.0892 X 2 = 0.T784 SiO, 0.1476 X 2 = 0.2952 Al 0.0137 X 3 =--^ 0.041 1 or(Sir)^ 0.1476 X 4 = C).5904) 1.3729 1. 2 186 or 1.5138 Dissolved Gases. — Apart from the carbon dioxide previously referred to, the water contains dissolved sulphuretted hydrogen in small quantity, which intermittently rises to the surface in bubbles. The radioactivity also fluctuates between the limits 3 and 10 Mache units. Classification. — The spring is described as a radioactive alkaline-muriatic-sullidic bitter water. In my previous paper I classified the springs only according to the principal divisions, there being hardly sufficient data to justify the introduction of additional mixed groups. In view of the ])redominance of sodium bicarbonate, and of the presence of appreciable quantities of the bicarbonates of calcium and magnesium, the inclusion of these springs in the group olf alkaline waters rather than in any other seems justified. Therapeutic Properties. — Medical men who have had ex- perience of the effect of these springs are agreed as to their efficacy, and the concensus of opinion is that their use is indicated in cases of digestive and metabolic disorders, of catarrhs of the respiratory organs, and female complaints. The other two springs have also been examined, and do not differ materially from the one described. Apart from geysers, the Windhuk springs belong to the hottest springs known. The well-known Karlsbad Springs are only a fraction of a degree hotter than the average temperature of the Pahlquelle (73.8" as compared to 73.5°). { /' ) (ikOSS-BAKMEN. The thermal spring on the farm Gross-Barmen (District Okahandja ) has a temperature of 64-65°, a feebly alkaline reaction, and smells and tastes strongly of suljihuretted hydrogen. 220 THE MEDICINAL SI'RTNflS OF SOUTH AFRICA. 'I'lie following analytical data will give an idea of its composi- tion.* Grams per 100,000. Total solids 113-94''^ Solid residue on heating to redness T02.465 SO, ' 37-382 CaO 5.307 ^IrO 0.437 cr 12.788 H.,S 0.425 K.'O 16.167 . Na/) : 17.823 NFI,/ trace Tai!li-: of I().\ Kouivalents. Cations. Ayiions. Na 0.575 X I -■= 0.575 ''^<^4 0-389 X 2 = 0.778 K 0-343 X I == 0.343 CI 0.3606 X r = 0.3606 Ca 0.0946 X 2 = 0.1892 . AFg 0.0109 X 2 = 0.0218 1. 1 38') 1 . 1 290 The figures for the pt>tassium contents are interesting in view oif the paucity of the South African springs in potash. Of the springs in the Union recorded in my previous paper, the one at Kouhad ( No. 14) contain less than one-third of the above amount. The (juantity of sulphuretted hydrogen in the spring is probably much higher, as the analysis was only carried out some time after collecting the water. The radioactivity is stated to be considerable. The spring might be provisionally classified as a sulphur-spring. The South-West Protect(>rate is comparatively poor in springs. But there is a zone running through the middle of the country from north to south, practically through its entire length. in which there are quite a large number of springs with an ample supply of water, and all of them of comparatively high tempera- ture.f Some of these are merlicinal. but only teni])erature measurements are recorded. Rehoboth 53°C Klein-Barmen (Otji Katiti ) 6i-62°C Omapiu 61° Oniburo, given variously as. . . . 61° and 77°C Warmbad and the other springs described in this paper lie in the zone, and a prolongation of the line strikes a number of the hot springs in the Cape Colony, namely, Clanwilliani * Dr. ('. Grimme: " Weideverhaltnisse in ryeutsch-Siiclwestafrika," 197 (1011). ^'l■l■;■)l^(■IltIi^thllnf^(■Il (ifi- Deutschen rjandwirtsdiafts-Gesell- ischaft. + (Ji-iiiniK'. I0C. cit. THE MEDICINAL Sl'KIN(;s OF SOUTH AFRICA. 221 ( 42-43' C). (iotulini (40'), Brandvlei (62°). and Caledon (49°). The majority of the remaining- hot springs in the Colony he on a hue running from Caledon more or less parallel to the coast as far as Port Elizabeth, namely, Montagu (45°). Barrvdale (no temperature recorded, but said to be un- comfortabh hot to the touch), Warmbad, Olifants River (45.6"), Tuoverwater Poort (49°), and Zwartkops (54.5°). It might l)e interesting to ascertain whether this regularity of grouping is not something more than mere accident. ((■) The Springs at W'ini'.urc. O.F.S. The water of the baths at Winburg. which were referred to under X >. 55 of my ])rcvious paper on the medicinal springs of South Africa, has been analysed, and in view of the preponder- ance of sodium chloride over all other constituents, the spring should be classified as a salt spring. The baths are situated on the farm De Villiersgunst, eight miles south-south-west from Winburg. A stone bath, approximately 8 'feet long by 5 feet wide, and closed in with corrugated iron, is built over the " eye " of the spring. This is described as the ladies' bath, and there is a similar structure for the use of men adjoining it, also fed by a spring. The water is described as being tepid and impregnated with sulphuretted hydrogen, and there is a continuous rush of l)ubb]es of gas through the water over the " eyes " of the springs. When the water reached the laboratory it contained no trace of either -ul])huretted hvdrogen or carbon dioxide. There are said to be indications of deposits of sulphur outside the bath build- ings, but none in the baths themselves. The only accommodation consists of a primiti\'e stone Iniilding of three rooms, and visitors must make their own arrangements for obtaining supplies. As is usual at springs of this kind, the majority camp in tents and wagons. The springs seem to enjoy a measure of reputation, having been patronised by some 150 people during the past 12 months. The water seems to be preferred for bathing rather than for internal use. and is reported to be efficacious in cases of chronic rheumatism, gout, sciatica and lumbago. As in the case of the majority of South African medicinal springs, only such unreliable and i)rejudiced iniformation about the therapeutic pro- perties is available as is supplied by enthusiastic patients. Density. — The density at 4° C (distilled water 4=^ C -= i ) = 1. 00 1 7. Total Solids. — 100 c.c. of water of 12°, evaporated and heated to 105''. gave 0.2204 of a gram of residue. 100,000 c.c. of water of 4' therefore contain 220.50 grams of dissolved solid constituents. Ih-icnuinat'uni of the A)iio)is. — Silica. I. 2 litres of 12.95° g^ve 0.0827 gram SiO. + BaSO^. Residne obtained on treatment with hydrofluoric acid, 0.0040 gram of BaSO^. 222 TlIF, MKUICINAL SPRINGS OF SOUTH AFRICA. II. 500 c.c. of water of 1 1 .6" j^^ave 0.0223 gram of SiO., -p BaSO,,. III. 2 litres of 12" gave 0.0753 gram of SiO. -|- BaSOj. 100,000 c.c. of water of 4° therefore contain 3.9273 grams of SiOg and 0.2000 gram of BaSO^, correspond- ing to 0.1 177 gram of barium. Chlorine. I. 25 c.c. of water of 10° require 29. i c.c. AgNO... of which ICC. corresponds to i mg CI. N II. 25 c.c. of 12° require 40.95 c.c. — AgNO:^. 100,000 c.c. of water of 4° therefore contain 116.33 grams of chlorine. Sulphuric Acid {50.^). — Two litres of water of {2.()^° give 0.0145 gram BaS04, corresponding to 0.2984 gram SO^ per 100,000 c.c. to which must be added 0.0823 gram from the BaSO.j precipitated with the SiOo, giving a total of 0.3807 gram of SO4 per 100,000 c.c. of water of 4°. AlkaJinit\. N 50 c.c. of water of 14.3° are neutralised In' 1.15 c.c. — r H^SO^ (four estimations). 100,000 c.c. of 4° therefore contain 2,8204 gi'anis HCO... Determination of the Cations. — Calcium. I. 500 c.c. of water give 0.0605 .^''am Ca( ). II. 1,000 c.c. of water give 0.1179 gram CaO. 100,000 c.c. of water therefore contain 11.945 grams CaO, corresponding to 8.5375 grams of calcium. Iron. Determined colorimetrically with thiocyanate solution (two determinations). 50 c.c. of water contain the same amount olf iron as 0.2 c.c. of a standard ferric chloride solution, of which i c.c. corresponds to o.i mg. Fe. 100,000 c.c. of water therefore contain 0.04 gram 1 if iron. Aluuiiu'uui. 2 litres oif 12° give 0.0099 Fe^Og -(- ALO... Subtracting the iron leaves 0.338 gram Al,( ),, per 100,000 c.c. of 12°, corresponding to 0.1793 gram oi alumin- ium in 100. oco c.c. of water of 4°. Auunouia. 298 c.c. oi water correspond to i c.c. NH^Cl solution con- taining 0.1 mg NH.. per c.c. (Nesslerised ; four esti- mations). THE MEDICINAL SPRINGS OF SOUTH AFRICA. 22^ 100,000 c.c. of water therefore contain 0.0336 gram of NH3, corresponding to 0.03559 gram NH^. Magnesium. 1 litre of water gives 0.0332 gram of ]\Ig.P._.07. 100,000 c.c. of water therefore contain 0.7253 gram of magnesium. Sodium. 2 Htres of water of 12.95° were evaporated to dryness and left, after removal of silicia, iron, aluminium, calcium and magnesium, 3.5350 grams NaCl. 100,000 c.c. of water of 4° therefore contains 69.580 grams of sodium. Tal!le of Ion Equivalents. Cations. Anions. 69.58 116.33 Na X I = 3025 CI. X I = 3.281 23 3546 8.5375 2.8204 €a X 2 = 0.426 HCO.; X I = 0.046 40.09 61.008 0.7253 0.3807 Mg X 2 = 0.060 SO^ X 2 = 0.008 24.32 96.07 0.1 177 Ba X 2 = 0.002 137-37 0.03559 NH4 X I == 0.002 18.042 0-1793 Al X 3 = 0.020 27.1 0.04 Fe • X 3 = 0.002 55-85 3-537 3-335 2.?4 THE MEDICINAL SPRINGS OF SOUTH AFRICA. SpECTRoscoric Examination of Solid Residue. Spark Spectrum ill Nature and Intensity of Lines. Element or Conipound Wave-lengths. Identified. 67_1 Well defined, bright Lithium 670-8 (->563 Well defined, but often faint Hydrogen(C) 656-3 (S51-637-5 Faint band, only in concen- CaCl., trated solution 627-616 Bright band, continues very CaCl., faint to D line 621 Well defined and fairly bright, ? but only in concentrated solution 618 • Intensity and definition as 621 ? 594 W^ell defined, but faint Nitrogen j^ggl 589-6 1 Very bright and sharply de- 589 j fined ' Sodium (D) 569 Bright and well defined Sodium 5688 5(.;j^.'> ■ J Sodium 5682 1 Nitrogen 668 Bright bands, but edges ill-de- \ 556 ;:>-552-5 I fined. Figures give approx- , 552 - 550 I imate positions of edges of j ^^^^'- bands ' 554 Bright and well defined Barium 553-7 519 Faint, but sharpiv defined ? =;w i\/r • 518-4) , oks .. ^^ ,, ^, Magnesium 517.3 [? \Lir •• '• " " Sodium c^jg !• 4985 „ „ „ „ Sodium 498-3 (Nitrogen 463-1 ""^' ^ " " " " (Lithium 460-2? 446 So faint that position only Calcium 445 5 approximately determined AA'i^ \ 442-2 So faint that position only Calcium 4x9. c ' approximately determined 423-3 Bright and well defined Calcium 422-7 The residue, after precipitating iron, calcium, magnesium, etc., was examined spectroscopically, and gave the follawing lines in addition to those underlined in the preceding table: Spectruni in Element. Wave-lengths. 615-5 Sodium 615-5 616 1 Hvdrogen (F) 486-2 4865 THE MEDICINAL SPRINGS OF SOUTH AFRICA. 22$ Of the definitely identitied lines due to metals only those of lithium and sodium were seen in this concentrated residue. No potassium, rubidium or caesium lines were found. The line 461.2 is i)robably not due to lithium, as the line 610.4 could not be found, and this line is of at least the same intensity as the line 460.2. As only the line 670.8 could be located, and that only with a strong discharge, it would seem as if only traces of lithium were present. The line 554 coincides with that of barium, but is probably not due to this meta], as it could be easily discerned in the con- centrated residue, which had been twice treated with precipitants of the heavy metals and alkaline earths. The absence of calcium lines gives evidence that this metal has been completely removed, so that the presence of any barium in this residue is most im- likely. In the above spectroscopic tables the figures in the third column are taken from a catalogue of spectra. Where no values are given i^c.g., calcium chloride), the identification was efifected by comparing a spectrum of the salt in the third column with that of the saline residue. I desire to place on record my indebtedness to Dr. K. Renz, of Windhuk, for placing analytical data and other information at my disposal, to Dr. H. H. Green, of Onderstepoort, for assisting me with relevant literature, to Major Haywood, S.A.P.. Bloem- fontein, for obtaining supplies of water from the Winburg Baths for me, and to my assistants, Messrs. V. A. Putterill, B.A., and C. Brink, B.A., for their assistance in carrying out the analyses of this water. {Read, July 9, 1918.) Solar Bombs. — An interesting phenomenon has lately been investigated at the Mount Wilson Observatory. Spectro- scopically it consists in the sudden appearance of a very brilliant narrow band, including the region of Ha. the latter meanwhile retaining its character of a dark line. As a rule this appearance was found to last between one and three minutes, seldom con- tinuing for as long as five to ten minutes. These " bombs " of solar hydrogen are said to follow one anotlier, at intervals from 10 to 20 minutes, like the balls of a Roman candle, and it is suggested that they are caused by explosions in which only- hydrogen is involved. As the dark hydrogen line Ha remains unaltered, the level at which the explosions occur evidently lies below the reversing layer, and it is thought that the eruptions take place round and among active sun-spot groups. A NOTE ON THE FLORA OF THE GREAT WINTER- HOEK RANGE.* By Edwin Percy Phillips. ATA., D.Sc, F.L.S. The area investigated botanically was the Sneeinvgat Valley, and the mountains and valleys surrounding" it, including the Great Win- terhoek itself. The Winterhoek Peak reaches an altitude of 6,8x8 feet ; on the Tulbagh side it is precipitous, but on the northern side the slopes fall gradually away. At the base of the Peak is the Sneeuwgat Valley, which is entered by a nek between the Little Winterhoek and the Witzenberg Range. The Sneeuwgat Valley has an average altitude of about 4,000 feet, is well watered, and has several kloofs entering it from the mountains on the north-east. As the valley a})proaches the W'itzenberg Range it gradually widens out and merges into the slopes of the Witzen- berg. This region was visited on two occasions, vi:::.. in A])ril and November, 1916, and consequently species were collected on the first visit which were not recorded in the second, and 7'icr versa. April appears to be near the end of the flowering season for most plants, except the heaths, which were more numerous than at the beginning of the season, in November. As the slopes of the Winterhoek are ascended frtjm Mr. Theron's farm at the head of the Tulbagh Valley, the change in the character of the vegetation is very marked. The streams at the foot of the mountain are lined with trees, while the o])en slopes carry fine specimens of the Waaboom {Proted grandiflora). Between 2.000 to 3,000 feet the trees diasppear and the slopes are covered with dense bush, such as Salvia africano, Psoralea pinnata, tall plants of Sutherlandla frufescens, Rhus spp., etc. Above the 3,000 feet level — more noticeable, however, between 3,500 and 4,000 feet — the vegetation again changes, and the t^U bush is replaced by small shrubs, grasses, and sedges. In some places large patches were covered with Borhart'ia robiista. Perhaps the largest bush present at this altitude was Barosma pnchella, two to three feet high, which is very common, and gives oiT a strong lemon-like odour. A few sttmted specimens of Podocarpns latifolius were seen growing quite isolated among some rocks, and were evidently outliers from the lower levels. The true tnountain flora starts from an altitude of 3,500 feet. A partial study of the flora of the Matroosberg, on the Ceres side (recently undertaken) leads me to suppose that a line indicating the lower- most limits of the mountain flora in the Western Province will not always be at the same altitude, but will rise and fall according to the locality in question, and that altitude alone is not the deciding factor. At present I am not in a position to discuss this fully, but from my observations on several mountain trips I am * The data for this paper were gathered when on a collecting expedi- tion for the South African Museum, Capetown. A NOTE ON THE FLORA OF WINTERHOEK RANGE. 22/ inclined to believe that it is the " exposure " which determines the altitude at which the mountain flora begins, and this may be as low as 3,000 feet or as high as 5,000 to 6,000 feet. On the French Hoek Mountains, for instance, the mountain type of vegetation may be found at 3,000 feet, while at Seven Weeks Poort, in the Zwartbergen, it does not appear until peaks over 5,000 feet are reached. To give any detailed account of the flowering period of the of the various species, continuous visits during the year must be made to the locality under observation ; this, unfortunately, I have not been able to do. One point, however, was noticed very markedly, vis., that at the higher altitudes the flowering period is much later — e.g., Microdon lucidus was freely flowering in November between 3,000 to 3,500 feet, but was still in bud at all altitudes above 4,000 feet, and finishes flowering at the higher altitudes in April. Ccelidium roscnm was collected at the base of the Great Winterhoek (4,300 feet) in fruit only, while on the Peak itself (6,000 feet) it was in full flower, and showed no signs of fruiting. The flowering period of most of the species at the same altitude is very short — e.g., Cyclopia bonneana was in full flower on November i/th, and a week later not a flower was to be found on any of the bushes. Aspalathiis triqitetra showed extremely young buds on November 17th, and was beginning to flower freely by November 28th ; how long the flowering period lasts I cannot say, but it is certainly over by April. Gladiolus' involntns in flower was very common on November 17th, but a few days later all the flowers had disappeared. Other examples could be cited, but the above will suffice to show the extraordi- narily short space of time in vvhich the species flower and fruit. The character of the vegetation covering the Sneeuwgat Valley, the mountains, and slopes is not homogeneous, and it can best be described by detailing the types which occur in the various localities. The upper reaches of the Sneeuwgat Valley, running south-east and north-west, have gentle J^opes with kopjes on the eastern side rising to 500 to 600 feet above the valley. In the valley itself are found chiefly grasses and .sedges, together with prostrate plants, such as Borbonia villusa. Argyro- lobimn lanceolatum, Indigofera fiilcrata, etc. Near the nek overlookingTulbagh Valley were numerous plants of Euryops abrotanifoliiis. The steeper slopes of the kopjes have a shrubby aspect, due to the numerous bushes of A. Comparing this list with that given by Bolus for the South- West Region generally, it is found that the first three orders, Compositae, Ericaccce, and Leguminosae, occupy the same relative positions in importance ; the grasses are better represented, while the Liliaceae are but poorly represented. Too much stress must not be laid on this comparison, as the area under consideration is but a small portion of that dealt with by Bolus. We will only be able to tell whether the mountain flora differs in com])Osition from the flora of lower levels when the highland and lowland floras of several localities have been thoroughly explored and worked up. The most important results obtained, ])erhaps, are those relating to the character of the vegetation existing under mountain conditions, and in this I have followed the classification of Raunkiaer, as outlined by Bews, in his paper on " The Vegeta- tion of Natal." The results are as follows : — Species. Per cent. Plemicryptophytes ... 86 35 • 10 Cham^ephytes 60 24.48 Nanophanerophytes . . ;i,^ I5- 10 Geophytes t,o 12 . 24 Therophytes. ...... 18 7 -M Helophytes 10 4-o8 Microphanerophytes . . 3 t . 22 A N(^TE ON THE FLORA OF WINTERHOEK RANGE. 23I These hgures prove quite conclusively that the habit of the species inhabiting this region is influenced by the rigorous condi- tions under which they live. Nearly 60 per cent, of the species are prostrate plants with winter buds below the surface of the soil, or a few inches above the ground-level (^Hemicryptophytes and Chanijephytes), while the "bushes" (Nanophanerophytes) only constitute 15. 10 per cent, of the flora. If the Geophytes and Therophytes, as a general class, are included witlj the Hemi- cryptophytes and Chamaephytes as representing a type adapted for tiding over adverse climatic conditions, we then find that 79.16 per cent, of the flora of the Winterhoek and environs is of this extremely xerophytic type. This, however, is not so important from the point of view in which these investigations are being pursued, as the predominance of the Hemicrypto- phytes and Chamaephytes in the flora. Wq know that the high mountains of South Africa carry a sub-alpine type of vegeta- tion, but I do not know of any systematic investigation on this point dealing with the Western Province flora. The results as given in this paper are not of much value in themselves ; many such mountain peaks must be worked on the same lines, the results obtained co-ordinated and compared with those of lower altitudes in the vincinity of the peaks explored. It is only then tliat any definite statements can be made regarding the mountain flora of South Africa. Reverting back to the type of plants, the small number (three) of Microphanerophytes is noticeable when com- pared with the list of small trees found at the foot of the moun- tain. Plants with woody stems, quite irrespective of their form, constitute 54.22 per cent, of the flora, while the herbs or herba- ceous plants make up the remaining 45.77 per cent. A stud}- of the leaf -characters of plants growing in areas under the same climatic conditions may lead to some general conclusions if several such floras are worked, and I have adopted here a similar scheme to that employed in my paper on the French lloek flora. The bulk of the species possesses sessile, alternate, entire, expanded, glabrous leaves. Linear leaves are fairly common, but deeply incised (or compound), cricoid, terete, revolute (or involute), leathery, or hairy leaves are less common. These facts are naturally corollated with the predominance of I lemicrypto- ])hytes and Chamaephytes present in the flora. The species in this region have not only to contend against a summer drought as the plants of the valleys, but have also to make provision against the cold of winter, when the ground is covered with snow for two or three months in the year, which kills the aerial vegetative shoots, but does not injure the dormant winter buds. In the period intervening between two winters, the plant produces a type of leaf best fitted for rapid transpiration, assimilation, and respiration, .so that it may build up in as short a time as possible reserve food for the following year's underground stem, and at the same time produce flowers and fruit before the 27,2 A NOTE ON THE FLORA OF WINTERIIOEK RANCE. advent of the second winter. It must not be inferred from this, however, that the chief type of leaf is mesophytic; the xerophytic type is predominant. Plants with cricoid, filiform, terete, involute, revolute, leathery, and hairy leaves, if taken collecti\'ely, outnumber the mesophytic type. The following list shows the various leaf-characters: — Sf'ccics. Per cent. of Whole. 68.42 ,V.5« 91 •♦^'S ^-97 Leaves sessile i-« Leaves petioled 66 Leaves alternate . . . 223 1 .eaves opi)osite . ... 22 1 .eaves sim])le and cntu'c 174 Leaves comi:)Ound, deejih' incistrd, or lobed. or leaflets with dentate or crenate maronis . . 26 Leaves filiform, terete or sennterete ]2 Leaves cricoid 39 /r.o -> 10. 6 T 4.^w LS-91 Leaves flat and ex- panded 84 34 • 28 Leaves invohue or re- volute 46 '^'^■77 Leaves leathery. ... 31 12.65 Leaves glabrous. ... 136 .^5 -51 Leaves hairy 66 -6.93 Leaves glandular ... 13 .^-.^f^' Leaves ]iungcnt or spiny 8 ?,-2^^ The type of inflorescence, size and colour of the flowers, and tyi)C of fruit have all been worked out in detail, and are embodied in the following lists: — LVFLORESCENCE. species. A capitulum 63 Flowers solitary 46 An umbel 31 A spike 2^ .\ raceme 21 A corymb 11 A i^anicle 3 (The Restiacene, Cy])erace ■ ■ ■ Flowers medium. ... 71 Flowers small 3^^ Per cent. 4; • -' .> 6 I 17 20 9 21 3 I 13 (Raunkiaer) ijr.f. If we take the biological spectrum of Natal as given by Bews as being typical of one of the larger general areas, with conditions varying from sub-tropical and mesophytic on the coast to alpine temperate on the Drakensbergen, the comparison table given above brings out certain interesting points. The taller trees belonging to the class M.M. (Mega and Mesophanerophytes) are totally unrepresented on the \\"interhoek. Of small trees on the Winterhoek the percentage is only 1.2, as against 14 in Natal. Chamsephytes and Hemicryptophytes show a large increase. Geophytes (bulbous plants), on the other hand, are not quite so numerous as in Natal, and certainly not nearly so numerous as in the grass-veld ])ortion of Natal. They may be looked upon as a type peculiarly adapted to steppe conditions, though they are fairly well represented in the moimtainous areas also. The pro- portion of marsh plants is slightly less, that of annuals ( Thero- phytes) slightly greater tlian in Natal. The annuals would, of course, be more abundant were the area under cultivation. The increase in the number of Hemicryptophytes, which is nearly double that of Natal, is to be explained by the lower winter temperature on the Winterhoek. It shows a nearer approach to temperate conditions as opposed to sub-tropical. It is 8 per cent, greater than Raunkiaer's normal for the whole world's flora, but is not quite so great as for most true temperate regions in the Northern Hemisphere.* As I pointed out previously, any facts given in this paper have been published in the hope that when other workers \.wx\\ their attention to investigations on similar lines, some use may be made of them. I hope to be able still to continue this work, and later on to make some general statements regarding the high mountain flora, based on a detailed study of each individual species. In conclusion, I am greatly indebted to Dr. J. \\^ . Bews for his kindly interest and f riendl}^ criticism. * See examples of biological spectra, Bews. loc. cif. THE NATIVES OF NATAL IN RELATION TO THE LAND. Bv Maurice Smethurst Evans, C.M.G., F.Z.S. To a greater extent than any of the other races inhabiting South Africa, the life of the Bantu people is boimd up with and directly dependent upon the occupation of the land. This is quite as true df Natal and Zuiuland as of any part of the Union. There are probably about a quarter of a million native families living in Natal, and out of this large number I do not suppose there are more than a few hundred who do not raise the greater part of their sustenance directly from the soil by the labour of their own hands. It is true that from every kraal one or more of its members go forth to work for the white man, but their earnings are not usually spent in food, which is drawn direct from Mother Earth by the labours of those who remain at home. In a sense it may be said that these also are working for the white man, for if the native had no such holding his present wages would hardly support his family and pay his taxes. His earnings may be said to be supplemental to his crops, or, if you prdfer it, his crops supplement his earnings. Viewed thus, the umfaan who herds the goats and the women and girls who hoe the gardens are also working for the benefit of the European. Since the Native Land Act of 1913 passed through Parlia- ment, the present position of the native on the land, and his future thereon, have been much discussed ; and much more so in Natal than elsewhere. It may therefore be of some value to give a brief description of the position of the native in relation to the land in that province, where his numbers, in proportion to Europeans, are so much greater than in any other Province of the Union. The past history and the present occupation of the land, both by Europeans and natives, in the old G)lony of Natal is ?ur may in truth he very dear ; intelligent, willing work has been proved all the world over to be really cheaper than un- intelligent, ignorant work, even if a much higher wage should be l^aid. The high wage paid to farm workers in Australia. New Zealand and America, and their higher standard of living, does not prevent these countries from sending their produce to Africa, ill the face of our low wages and mealie-pap-fed labourers. This elementarv. but important, fact must be learned by the land- owners of Natal, and when learnt, there will be hope for the native who works as farm servant, for he may then hope to advance his position and earn wages more commensurate with the more difficult and responsible work he is often called upon to nndt-rt'ike. in these days of more advanced agricultural practice. THE XATIVES OF NATAL IN' RELATION" TO THE LAND. 24 1 In past years considerable grants of land were vested by the Government in missionary bodies, and these grants are called in Natal, Mission Reserves. In all. these reserves amount to 313,867 acres, and are inhabited by 43.10) natives. There are resident European missionaries on most of them. The native people living on these reserves are not all Christians ; a number of uncon- verted natives have been allowed to reside on them. Formerly, in a few of these reserves, individual freehold title was given to a limited number of allotment holders, but the practice ceased many years ago, and the greater part of the native residents have no title to their holdings. On some reserves the missionaries have made an effort to encourage and teach better agricultural methods ; generally speaking, the natives on the reserves, who are under the ini|uence of the missionaries, have better homes and make ])etter use of the ground than any of those previously mentioned. There are a number of native freeholders in Natal who have purchased their farms, either as individuals or as members of a syndicate. Altogether there are 359,708 acres held by these native freeholders. The holdings are not usually df large size, but as they are often contiguous, a considerable continuous area may be owned and occupied by these native farmers. Unless one is acquainted with the details of one of these farm areas, it is (litBcult to estimate the cpality of the farming operations carried on by the actual owner, for they nearly all have copied the Euro- pean in taking on other natives as tenants, and the crops of these tenants are no better than those of the native tenants of unoccu- jtied European farms. It is generally understood that these native landlords charge high rents and deal promptly with defaulters through the agency of the law. Still, speaking generally, the native owner, when he does cultivate, makes better use of the ground than any of the classes we have mentioned hitherto ; there are not a few instances in which the advance is noteworthy and creditable. The maji who has had the thrift and foresight to buy a piece of land is, as a general rule, the man who makes the best use of it. Fundamentally, human nature is the same all the world over. There has been much anxiety evinced in some parts of the Union because of the alleged increasing desire, on the part of natives, to purchase land in the midst of white communities. To prevent this intermixture was one of the objects of the Natives Land Act of 1913. In Natal this fear is not generally entertained. The Europeans ha\e already acquired all the most desirable agricultural and pastoral land, and are being more and more firmly entrenched therein by the adoption of improved methods, which means higher prices for the land ■ and more capital and capacity to work it profitably. In many cases native purchasers ha\'e been unable to retain their land through lack of business ability, foresight, and thrift; and the instalments ]>aid. and the land itself has been lost to them. With Government aid I think it is possible for the native farmer to survive, if his operations are on a limited scale, but I do not 242 THE NATIVES OK XATAL IN RELATION TO THE LAND. think lie can compete successfully with Europeans in a European area, much less be a menace to European occupation on such areas. I speak, of course, of Natal only. I have now treated of the position oif the native on the various classes of land in Natal ; it remains to say a few words on his position in Zuiuland. The large num'bers of natives on private land in Natal are not found in Zuiuland. Prac- tically the whole native population lives either in the reserves or Crown lands demarcated by the Saunders Com- mission of 1902-04, so that the involved questions of tenancy, rent, and labour complications do not arise. A large number of male Zulus turn out to work, proceeding to Natal and the Transvaal, or getting work on the sugar estates of the Zuiuland coasts, and these bring the new and disturbing ideas, bred by contact with the white man's civilization, to the old environment; but on the whole, social liife and the use and occti])ation of the land is not much changed in Zuiuland among the natives. Except- ing in one or two areas in which the missionaries have encouraged better methods, the agriculture to-day is as in former days. But in proportion to the population land is more plentiful in Zulu- land than in Natal, and the evidence of worn-out fields is not present. In Northern Zuiuland the natives belong to the Tonga branch of the 'Bantu, and here the people grow a greater variety of cro])s than further south, and are, on the whole, better agri- culturists. But what was said of Natal applies to the whole of Zuiuland ; also there are no surplus crops grown by the people ; nothing is sent to market or exported from the land tilled by the natives of Zuiuland. I have now reviewed the present position of the native as occupant and cultivator of the soil, and the position cannot be considered satisfactory. It is over 60 years since Europeans first settled on the land of this Province. At first, and for some vears, their cultivation was not much in advance of the Bantu, but year by year they improved, until now the gap between the two races in this respect is enormous. Excepting in isolated cases, which certainly give ground for hope, the native has not advanced, and it is probable that on the whole he has retrograded. This is a question of serious national importance, for it means that millions of acres are not fully utilised, and human life is not sustained as it might be. I know that according to native ideas the locations are already full, and at many meetings of natives I have attended the cry went up that they were over- crowded, but there is no doubt that if properly organised, utilised, and cultivated, they would carry a much larger population. To ascertain the reasons for this backwardness among these people would be a most valuable and interesting subject for scientific enquiry. Meantime, pending such an enquiry, I will venture to give a few thoughts on the subject, tentative conclusions I have arrived at from my own observations and discussions with many who are familiar with native life. And first I would say that it is not lack of capacity, either physical or mental. It is true, as THIi NATIVES OF NATAL IN RELATION TO THE LAND. 243 I said beftjrc. that the average native could not successfully carry on farming on a large scale, involving knowledge of scientific method and modern business. But I believe many are quite capable of good and profitable cultivation of small farms. JKs before stated, many Euro[)ean farmers have natives who do excellent work, and who, learning the routine, may be trusted to continue without much supervision. In the Southern United States negro farmers have made extraordinary progress in late years, extending their holdings and im[)roving their methods to an extent comparing very favourably with their white neigh- bours. In i^arts of Africa, notably in Nigeria and Uganda, people akin to our Bantu are growing exportable crops of great value. It is not, then, lack of natural ability which is the cause of the backwardness of our natives. What is it, then? Many I have spoken to give but one reason — indolence. But under sufficient and appropriate stimulus, or when in the employ of European^ whom he trusts, in a situation he values, he certainly cannot be called indolent. What my friends call indolence, I think is rather an innate conservatism, coupled with the absence of the will to advance for the sake of advance. If this is so, there is hope, for, as I said before, human nature is fundamen- tally the same all the world over, and stimulus, encouragement, instruction, and supervision may work some of the marvels one see^ in some of the negro communities in the Southern States, i his conser\'atism gives play to a factor which certainly plays a part. In a tribal location all believe in witchcralft, and the witch-doctor openly or secretly carries on his calling. He is a great upholder of ancient custom, and any person departing therefrom, or introducing innovations, is likely to be suspected and at least ostracised. So the man who would like to plant wattles refrains from doing so lest he incur the dislike or hos- tility of his neighbours. Another factor is the gradual break- down of the old rigid social s\'stem. After ploughing, the culti- vation i^ the work of the women, and they can no longer be punished for failing to carr}- out their duties. Competent obser- vers also say that the old emulation between the women, and the pride they took in their respective gardens is no longer present ; they are now not ashamed of slovenly garden-plots. In old times, a beer-drink was a gathering of the men on some important occa- sion, anti women and youths were excluded. But now they are held whenever amabclc is procurable, and women and imma- ture young men attend, and character and industry suffer in con- sequence. Under communal tenure, whilst a kraal will not be evicted so long as it is occuj)ied. when the area becomes crowded, there are frequent garden disputes, and of course this system does not {)ro vide- the stimulus which is furnished by individual tenure, and there is no inducement to improve when a man is in doubt whether he will retain the fruits cif his labour or they will pass to another. Many in Natal are of the opinion that the custom o\ polygamy is the source and fount of all that is back- ward and barbarous in the life of the Zulu. It nuLst be admitted 244 THE NATIVES OF NATAL IN RELATION TO THE LAND. that it is a cement binding together many ancient customs which to-day are proving hindrances to advancement. In a mono- gamous society when a man has courted and married, his attention is devoted to earning his Hving, and, if possible, a better living, year by year, and so the State progresses. Among our Bantu, instead of working and earning, our married man goes philander- ing among the girls, and, from the standpoint we are now considering, he wastes the time of many others as well as himself. When he is sufficiently married the position is no better, for the man who should provide most of the brain and muscle, now reposes in the shade while his wives scratch the ground to grow their scanty crop. It wili be seen that I attribute the failure of the Bantu to advance largely to social customs. While many of the customs had a high value, when incorporated as part of a system they lose this value when the whole system is breaking down., The position is a most unfortunate one. By our contact and example we dis- integrate old social order but fail to put anything in its place. I made a comparison a little while back l)etween the agricultural progress made by the European and the Bantu in the last few decades. Such a comparison would be unfair if we did not remember that during the time many hundreds of thousands, if not millions, have been spent in Natal alone to help the European to better his position on the land, while not a ])enny has been given to the native from the public exchequer for the same purpose. We are constanjly preaching the doctrine of the dignity of labour to the native, but we do not see that he has in his labour that greatest incentive of all — hope. When the native sees that by energy and thrift he can acquire many desirable things, and the road is pointed out to him, hope will spring up and make all the difference in his life. But we must show him the road and we must encourage and support hini in it. He cannot achieve, un- aided, progress towards a better life in the native areas, and agri_ citltural development therein is a main road, but Government initiative and assistance will be needed. This work should form one of the chief duties of the non-political Native Affairs Council which I have so ciften recommended, and the idea of which was embodied in the Native Administration Bill of 1917. On general lines the development would follow what has been done in such large measures for the European farmers by the Agricultural Department — agricultural education, establishment of experi- mental plots, introduction of new crops, help in marketing and all the other plans now familiar to us. But the details would have to be altered and adjusted to suit the character and cai>acity of the |>eople with whom we are dealing. For a people like our Bantu who are either in, or just emerging from the patriarchal state, the personal element counts for much more than it does among a ];eople who are indi\idualistic like ourselves. Much will depend