ae nent ee eS i ot Se PRINTED AT THE HERALD OFFICE, NORTH GATE, BATH. mee ae ad HEE CAD ntiog.” en MELE F1i40 UT OA ae PALM Wat rR, cheery PROCEEDINGS OF THE BATH NATURAL HISTORY AND ANTIQUARIAN FIELD CLUB. BATH : PRINTED (FOR THE CLUB) AT THE HERALD OFFICE, NORTH GATE. 1889, wrist TABLE OF CONTENTS. Vou. VI, No. 1. 1.—CONTINUATION OF THE FUNGI oF Batu, By C. E. Broome, F.LS. _... vit ats ae we 2.—On AN ABNORMAL FLOWER OF A PENSTEMON, BY C. E. Brooms, F.L.S. ee ae ois 2 3.—NoTES ON RoMAN PAVING FOUND IN BRIDEWELL LANE, BY T. BROWNE 4,—THr BouRNEMOUTH Firs ; CONSIDERED AS THE REMAINS OF AN ANCIENT Forest. WAS THERE EVER A ForEST OF FIRS ON THE HILLS AROUND Bato? By tHe Rev. LeEoNARD BLOMEFIELD, M.A., F.LS., F.G.8., &. ... 5.—THE ALG OF THE BATH THERMAL WATERS, BY G. Norman, M.B. ... ve 6.—THE Earuiest Map oF Batu, BY EMANUEL GREEN, F.S.A. 7.—On RECENT DISCOVERIES MADE IN UNCOVERING THE ROMAN BATHS AT BATH, BY THE ReEv. Pres. ScARTH, M.A. 8.—UPON SOME SCULPTURE RECENTLY DISCOVERED AT THE Cross BATH, BY THE Rey. H. H. Winwvop, M.A., F.G.S, sie ie vi 25 bye Pace. 35 37 39 53 58 79 U2. CONTENTS. PAGE. 9,—Nores ON THE OCCURRENCE OF SALT SPRINGS IN HE CoAL MEASURES AT RADSTOCK, BY J. McMvrrtnie, F.G.S. ‘os ae fs ot ee 10.—List or Fosst, MAMMALIA FOUND NEAR BATH, BY rue Rev. H. H. Winwoop, M.A., F.GS. cae ee 11.—SUMMARY OF PROCEEDINGS FOR THE YEAR 1885-86, By THE SECRETARY... aie ee aoe ca’ Gen No. 2. 1.—Nores oN THE GEOLOGY OF BRENT KNOLL, BY Horace B. Woopwarp, F.G:S. ... ii ree 9.—PitAce NAMES DERIVED FRoM PLANTS (IN THE NEIGHBOURHOOD OF BATH), BY THE Rev. CANON ELLACOMBE ... dee me sy. ii ao ee 3.—ADDRESS TO THE MEMBERS OF THE BatH FIELD CLUB IN REFERENCE TO THE DEATH OF C. E. BROOME, F.LS., BY THE Rev. L. BLOMEFIELD, ‘M.A, F.LS., F.G.S., &c. ... is tds vee 4,—TRACES OF THE SAXON PERIOD IN BATH AND THE NEIGHBOURHOOD, BY THE REY. PREB. EARLE ... 153 5,—Lerrers ILLUSTRATING THE BATTLES OF CLAVERTON AND LANSDOWN, BY H. D. Sxrine, M.A. ae 6.—FurRTHER NoTES ON THE CLAVERTON SKIRMISH, BY H. D. Sxrine, M.A. 453 MG dis + ee 7—Norrs oN THE HAM HILL STONE, BY Hx.B, WoopwarbD, F,G.S. oF Rr and an Oe CONTENTS. _8.—FurtTHEr RESULTS OF METEOROLOGICAL OBSERVA- TIONS MADE AT THE BATH ROYAL LITERARY AND SCIENTIFIC INSTITUTION, BY THE REV. LEONARD BLoMEFIELD, M.A, F.L.S., F.G.S., &, . 9.—SUMMARY OF PROCEEDINGS FOR THE YEAR 1886-87, BY THE SECRETARY... ad fe Han My No. 3. 1.—ON SOME OSTRACODA FROM THE FULLERS - EARTH OoLITE AND BRADFORD CLAY, BY PROFESSOR T. RuPert JONES, F.R.S., F.G.S., anp C. DAvits SHERBORN, F.G.S. ... 2.—LANDSLIPS AND SUBSIDENCES, BY W. PUMPHREY ... 3.—THE DESTRUCTION OF THE Two CHURCHES OF ST. Mary In Batu, By Austin J. Kine 4.—A Barn Pott Tax 2 RicHarp II., py EMANUEL GREEN, F.S.A. ae a site ka eee 5.—REMARKS ON SOME HEMIPTERA-HETEROPTERA TAKEN IN THE NEIGHBOURHOOD OF BATH, BY LIEUT.- Cot. BLATHWAYT, F.L.S. F.Ent.S. a ane 6.—RECENT “ FINDS” IN THE VICTORIA GRAVEL PIT, BY THE Rev. H. H. Winwoop, M.A., F.G.S. a 7.—NoTE ON WEBBINA IRPEGULARIS (D’ORB.) FROM THE Oxrorp CLAY AT WrYMOUTH, BY C. DAvIES SHERBORN, F.G.S. ... Ba oe age ie 8.--SUMMARY OF PROCEEDINGS FOR THE YEAR 1887-88, BY THE SECRETARY Se LA: wae PHS 196 vu. CONTEN'S. No. 4. PAGE. 1.—On CuurcH Doorways, BY THE REV. REGINALD A; Gayiuy; McA. .«.. se ite aa .. 363 2.—BatH Lay Supsipies, Henry IV. to Henry VIII, BY EMANUEL GREEN, F.S.A. me ~ ase de 3.—Tue Divinine Rop, py THomas ForpER PLowMAN 411 4,—ListT OF TERRESTRIAL HEMIPTERA - HETEROPTERA TAKEN IN THE NEIGHBOURHOOD OF BATH, BY Lizut.-Con. Buatawayt, F.L.S., F.Ent.S. «s ) 432 5.—SUMMARY OF PROCEEDINGS FOR THE YEAR 1888-89, BY THE SECRETARY we i des .. 435 ~ In SA \ ¥ 8 JUN. 92 “OR OCT 13888. . : ‘ a PROCEEDINGS BATH NATURAL HISTORY ANTIQUARIAN FIELD CLUB NO. I. VOL, VI ‘PRICE . HALF-A-CROWN. ee SX BATH: ; ieee THE HERALD OFFICE, NORTH. GATE. | J. DAVIES, GRAND PUMP ROOM LIBRARY. 1886, 0 Continuation of the Fungi of Bath, By C. E. Brooms, F.LS. (Read March 18th, 1885.) Continuing our Notices of the Fungi of the Bath District from . a Paper read in March, 1883, before the Bath Field Club, we commence with the 26th Order of Mr. Berkeley’s arrangement in the Outlines of British Fungology, Spheriacei. The Order is characterized by producing its fruit, called sporidia, in little sacs, or asci, which grow in closed vesicles, perithecia, opening by a round or elongate mouth. This is perhaps one of the most interesting Orders of the Family Ascomycetes, especially to Microscopists, owing to the great variety it presents, both in the outward form and arrangement of the perithecia, and in the nature of the sporidia which, in this section, often afford good specific characters, either in their mode of division, coloration, or in the number contained in each ascus. Spherie are to be found in all parts of the world. They are most abundant in temperate climates ; but they are by no means rare in the tropics, especially insect-spherie, and such forms as approximate to Xylaria Hypoxylon, the finer states of which occur in the warmer climates; and it is probable that if tropical countries were thoroughly investigated, a great number of undescribed species would be the result. Ceylon has furnished us with conclusive evidence on this point, thanks to the exertions of my late friend, Mr. Thwaites, whose contributions to the mycology of that island have been recorded in the Linnean Journal (Vols. XI., p. 494 and ‘XIV., p. 29). The old unwieldy genus Spheria, of which Fries described, in his Systema Mycologicum, upwards of 1,000 species has, since that time, been divided into numerous genera and ‘subgenera by almost every author who has written on the subject. “Many of these divisions are, however, of doubtful value; we ‘shall, therefore, confine ourselves in the present enumeration to ‘such as appear to be of most value, and are more generally Vou. 6, No. 1. 2 recognized, Fries divided them in the Systema according to their simple, or compound habits. Those in the simple section are either innate in the bark of trees or plants, or at length emergent by a longer or shorter neck, with round or elongate mouths, or quite superficial on the surface of wood or sticks, and these are glabrous, or hairy, or tomentose, and sometimes seated on a shaggy subiculum. In the compound section the perithecia are aggregated together in the substance of wood, or leaves, or in the stems of herbaceous plants, assuming, at times, a circinate or quincuncial arrangement, or occupying carbonaceous receptacles which are immersed in the wood. Some- times they are located in a flat, or globose, stroma, which, in the more perfect species, assumes a simple or branched, erect form. To begin, however, with the more simple forms. We have in them instances of species without any true perithecia as in the genus Dothidea, where, however, that want is fully compen- sated by the various forms of fruit which have been traced to it in its early stages; thus in Dothidea melanops 7'ul. there are macrostylospores and microstylospores, as well as ascigerous fruit. Again in Diatrype stigma Fr. Stictosphzria Noffmanni Tul, we have conidia lining the interior of irregular cavities of the wood, or bark, on which it grows; and, on the same stroma, ascigerous conceptacles containing sporidia of a form very similar to the conidia. In Cucurbitaria macrospora Tul. the three forms of fruit are again to be seen, occupying one stroma. In Melanconis macrosperma the conidia are shown, in Tulasne’s figure, growing intermixed with macrostylospores. The conidiiferous tufts of Stigmatea frag- rariz also present us with a beautiful microscopic object; this species grows on living strawberry leaves. I cannot pass over without notice a minute plant, the structure of which is very curious. It grows on the leaves of Aira czspitosa, a coarse grass known to the Wiltshire farmers as Bull-polls, it has been described, as a new 3 genus, under the name of Oomyces, on account of its egg-shape. Madame Libert published it in her exsiccata, as Spheria carneo- alba Libert. It is about a line high, bluntly conical, and of a pinkish-yellow colour ; there is an outer, leathery receptacle, trun-. -eate at top, around the centre of which are four to seven dark dots ; a cross section shows that these are the mouths of as many delicate, membranous perithecia which are closely packed in the outer conceptacle. The perithecia contain a number of elongate, cylindrical, asci, filled with very long, flexuous sporidia. It has been placed in a new genus on account of its compound character ; the outer conceptacle containing free, ascigerous perithecia. In Pleospora herbarum Pers. and P. polytricha Wallroth., belonging to the section Denudatz of the genus Spheria, the early states were considered autonomous plants; but it has been demonstrated that the canidia of the first constitute the genus Mystrosporium of Desmaziere, which again appears to give origin to Cladosporium herbarum Link., a common pest in greenhouses, covering the plants with a sooty stratum. The conidia of the latter, Pleospora polytricha Wall., being stipitate, and septate, present an elegant appearance under the microscope, and probably belong to Acrothecium simplex B.and Br. Nectria cinnabarina Fr. the conidiiferous state of which is known as Tubercularia vulgaris Tode., is interesting, from its common occurrence on dead sticks, covering them with bright, scarlet spots. Another of the same genus Nectria inaurata B. and Br. has two forms of ascigerous fruit, a very unusual occurrence ; it grows on dead twigs of holly. Capnodium and its allies, as Fumago and others, belong to the Spheriacei since they produce their more perfect form of fruit in asci, their perithecia being furnished with a round mouth. To the unassisted eye these plants appear as a mere sooty stain on the leaves of trees and shrubs, thus spoiling their appearance. We may mention in this place that the conidiiferous state of Hypoxylon coccineum Bull. was described by Persoon as a mould under the name of Isaria farinosa Pers. ; but it has been since traced.to the Hypoxylon, it is 4 common on decaying Beech. The genus Hypocrea is intermediate between Nectria and Cordyceps, it is generally effused, and horizontal in habit, and more remarkable from the moulds which constitute its early state, or are associated with it, than in its per- fect form. These moulds were considered autonomous species till Tulasne traced them to their true position ; they constitute the genera Botrytis, Verticillium, and others. Hypocrea inclusa B. and Br. is curious from its place of growth. It is parasitic in the flesh of a small truffle, Tuber puberulum £.; its presence may be detected by a minute, rusty spot not larger than the head of the smallest pin, visible on making a section of the Truffle. Another species, nearly related, is not uncommon on grasses; it surrounds the stalk with a bandlike, yellow stroma, crowded with perithecia. Tulasne has given it the generic name of Epichloe ; it differs from Hypocrea in the sporidia being linear and continuous. In habit it resembles the latter. The genus ‘Hypomyces differs from Hypocrea in fruit, and in being generally parasitic on other fungi. In a Monograph of the genus, Mr. Plowright observes that Hypomyces luteo-virens attacks the Agaric on which it is parasitic, at a very early period before it ‘appears above ground, and so distorts it that it is impossible to say to what species it belongs: most commonly the Hypomyces do not attack other fungi till they are in a state of decay. Another species, he says, grows, not on the Agaric itself, but on the ground under, or near, the spot where it has decayed, the decay being the result of the growth of an earlier stage of the Hypomyces; in other words, the Hypomyces, in its conidial state, first attacks the Host-Fungus, and, by causing its decay, ‘generates the pabulum necessary for the nourishment and perfec- tion of the higher form of fructification. The genus Hypomyces is interesting from the various phases ‘through which many of its members pass. As a rule, the ascigerous, or perfect form is more rare,—the conidiiferous state the more common. Hypomyces aureo-nitens Tul. was of striking 5 beauty, as it occurred on a damp morning in North Wales, each of the conidia growing on a branched mucedinous mycelium, was surmounted by a minute drop of dew, glittering in the sun’s rays like a diamond. Hypomyces cervinus Tul. is another pretty microscopic object, its macroconidia, or second form of fruit, are globose and echinulate ; they may be seen everywhere on decaying Boleti in autumn, converting them into a mass of yellow powder. The genus Xylaria has a branched, erect, clavate stroma, the early state of which, particularly in Xylaria Hypoxylon, often puzzles beginners ; the tips of the branches are then covered with a white powder, consisting of conidia, which fall off on being touched, leading the student to consider the specimen as belonging to such of the Hymenomycetes as Clavaria; but later on the branches swell out at the tips, and numerous perithecia are. developed in their substance, containing asci and ovate, coloured sporidia, thus showing the true position of the specimen in the series. I shall just allude here to a curious fungus belonging to this section, although # is not British. It occurred on rotting Bamboo in Ceylon, It has been named Astrocystis, on account of its starlike habit; in form it resembles a Geaster, having a double perithecium, the outer coat splitting into several rays, which become recurved, as in that genus; the inner coat opens by a more or less, regular mouth, to allow the escape of the sporidia, which are those of an Hypoxylon. The similarity of habit may be regarded as an instance of—what is now much discussed—mimicry in nature ; the structure and true affinities are here far apart. The genus Cordyceps, or Torrubia of Tulasne, is one of the most interesting of the Spheriacei, both from the variety of its habitats, or places of growth, and from the medicinal properties of one of the species. I allude to the Ergot of grasses. In a paper on this plant, published in the Journal of the Agricultural Society of England (Vol. x., 8-8, part II.), Mr. Carruthers says, 6 “The full grown Ergot is often overlooked in the barn, among the corn, owing to its fesemblance to the dung of mice ; but it is worth especial pains in examining the seed to secure immunity from this parasite”—“ Ergot might supply an interesting text from which to exhibit the worthlessness of speculation, as opposed to observation and experiment in dealing with natural science. Replacing, as it does, the seed of different grasses, and always attaining, when full grown, a greater size than the normal seed, it was, at first, thought merely to indicate an extra quantity of life and vigour in the particular seeds, which exhausted themselves in the production of the anomalous, horned grain; no special qualities being then associated with these abnormal productions. All along, however, the Ergot has been exerting its baneful in- fluence on men and animals, without being suspected. Through its agency the inhabitants of whole districts in France had been visited with intermittent attacks of gangrenous diseases. England also has records of similar, although not so extensive calamities. In the same Journal it is stated that the loss to one breeder of cattle alone, in Shropshire, was £1,200 in three years owing to this cause. It has been determined that the power of Ergot in causing muscular contraction extends to all unstriped, or involuntary muscular fibre, and it has therefore been applied in treating certain maladies connected with the intestinal canal, and the arteries, because these organs are chiefly composed of this kind of muscular tissue. The comparative immunity of England from disease arising from Ergot is probably owing to the less quantity of rye grown for seed, and used in bread, than is the case in France. But its frequent occurrence on our grasses as on the Bromi, Alopecuri and Festuz, expose our cattle to very serious losses. Ergot from the seed of Dactylis glomerata was sown, when gathered in autumn and kept under a bell glass through the winter ; in the following spring a large crop of Cordyceps purpurea was produced. Ergot of rye bought at a chemist’s, although then quite dry, and sown as 7 above, germinated after a like lapse of time producing the same species, It is fortunate for us that this pest is much less frequent on wheat and barley than on rye. Some species of Cordyceps, or Torrubia, attack wasps nee other insects, and have given origin to what are known as “ vegetable wasps,” the insects flying about with the fungus attached. Cordyceps alutacea F7, may be alluded to as showing some of the difficulties attending the study of this group of Fungi. Fries regarded it as a Cordyceps from its form and habit; Tulasne, guided by its fruit, placed it in the genus Hypocrea, considering it parasitic on Clavaria ligula, clothing that species with a thin stroma in which the perithecia are immersed ; but it may be said against that view, that Clavaria ligula has not occurred in England unaccompanied by its presumed parasite; and as Cor- dyceps alutacea is not uncommon in our fir plantations, it is scarcely possible that such would be the case were the Clavaria equally common. We may therefore fairly conclude that Fries was right in placing our plant in the genus Cordyceps, and that it is not merely a parasite on a Clavaria, but an autonomous species. Cordyceps entomorrhiza is parasitic on the larve of insects, Mr. Berkeley supposes that the sporidia fall on the caterpillars before they bury themselves to undergo their pupa change, or if at a later period they may be washed down through the soil so as to attain their proper habitat, as is now said to be the case with the Peronospora of the potato. At all events this must be the case where such species as Cordyceps capitata Fr. take possession of Elaphomyces, a subterranean fungus which is buried, sometimes deep in the ground. When the sporidia reach their proper habitat they germinate and pierce the skin of the insect, or the rind of the fungus, and occupy the whole of its body with an intricate mass of threads. They then throw out branching roots into the surrounding soil ; from these roots an erect, club-shaped stroma arises, in which, at length, the perithecia are formed. Tulasne says that a second form of fruit, conidia, occurs at the 8 base of the stroma of Cordyceps capitata and C. entomorrhiza, Cordyceps, Robertsii, a’ New Zealand species, parasitic on the larva of Hepialus virescens, is one of the finest species belonging to this genus. | _ In the Order Perisporiacei the sporidia are set free by the decay of the perithecia, the species not being furnished with a mouth. Some of the plants belonging to the Order are beautiful objects for the microscope, but very prejudicial to our crops. Thus Spherotheca pannosa Lév. covers the leaves and shoots of roses with a clothlike felt, thus preventing respiration, and causing the destruction of leaves and flowers. Spherotheca Castagnii Lédv. is equally destructive of our hop crops. Phyllactinia guttata Fr. is common on the leaves of various trees. Erysiphe Martii Lk, attacks our late crops of peas, often destroying them utterly in dry seasons. These plants are supported on the leaves by very elegant supports, or fulera, There remains only the Physcmycetes and Mucorini to be considered. The first Order is intermediate between Ascomycetes and Hyphomycetes, agreeing with the former in the free formation of its sporidia within a, generally globose, closed sac ; with the latter in its free, fertile, threads which are never compacted into an hymenium. The species belonging to these Orders, like the greater part of moulds, grow on decaying substances, and frequently on such as are used for food. In some instances, perhaps, the germination of the sporidia induces decay, and certainly accelerates it. Certain species of Mucor promote fermentation in fluids, like the true moulds, as Penicillium. In the genus Syzygites common on decaying Agarics in woods, the fertile threads throw out little tubercles from their forked branches—the tubercles soon touch each other and coalesce; a dissepiment is formed on either side, the two intermediate membranes are absorbed, and, finally, the united cells swell and form an irregular sac, which soon produces an abundance of sporidia ; thus resembling the connecting tubes of Zygnema 9 among Alge. In the genus Acrostalagmus the sporidia grow from the apex of the peduncle which protrudes into the cyst, 80 that that genus varies somewhat from the character of the Order, in the absence of free formation of the fruit inacyst. Something similar occurs in Ascotricha. Enough has, perhaps, been said to show that these low types of fungi possess some interest, and exhibit the wonderful variety of form and structure made use of by nature in her work, affording an inexhaustible field of research to the Botanist and Microscopist. We will now proceed with a list of the species belonging to the Orders at present treated of, which have occurred in our District, and which carries us through its mycology according to the arrangement adopted by Fries. ORDER 26. SPHARIACEI. Perithecia carbonaceous or membranaceous, sometimes confluent with the stroma, pierced at the apex, and mostly papillate. Hymenium diffiuent. GENUS 288. CorDyceEps.* Stroma vertical, fleshy. Fructifying head distinct, hyaline or coloured. Sporidia repeatedly divided, submoniliform. Cordyceps ophioglossoides Fr. Spye Park, September, 1843, parasitic on Elaphomyces muricatus. C—— entomorrhiza Fr. Hartham Park, April, 1843, on some caterpillar buried in the ground in fir plantations, C——— nmuilitaris Fr. Hanham Woods, October, 1853. C—— myrmecophila Cesati. Leigh Woods, Bristol, March, 1879. ; C———— microcephala Tul. Leigh Wood, July, 1878. C. Bucknall. C———— purpurea Fr. Raised from Ergot on _ grasses. Batheaston, June, 1854. * Cordyceps, from Kordule, a club, and cephalos, a head 10 C————-pistillarizformis B. and Br, Annals of Natural History. No. 969, t. 16, fig 22, on dead sticks still attached to a bush. Batheaston, March, 1860. C————-alutacea Fr. Lucknam Grove, in fir plantations, October, 1859. GENUS 289. HYPOCREA.* 7. Stroma horizontal. Perithecia tender, hyaline or coloured. Hypocrea gelatinosa Fr. Langridge, March, 1875. H rufa Fr, Batheaston, November, 1859. H vitalbe B. and Br. Batheaston, February, 1859. Annals of Natural History, No. 829, t. 9, fig 8, on Clematis vitalba. H delicatula Zulasne. Lucknam Grove, April, 1866; Ann. des Sciences Nat., Ser. iv., vol. xiii., p. 18. H farinosa B. and Br. December, 1863. Ann. of Nat. Hist., No. 592. H inclusa B. and Br. Hanham and Leigh Wood ; parasitic in the flesh of Tuber pubcrulum B. ; November, 1869. Ann. of Nat. Hist., No. 970, t. 17, fig 23. H. lenta Fr. St, Catherine’s, November, 1866, on wood. GENUS 290. HYPOMYCES.¢ Tul. Parasitic on fungi; mycelium byssoid; perithecia globose, papillate; asci 8-spored (rarely 2 or 4), without paraphyses ; sporidia lanceolate or elliptic, rarely obtuse, uniseptate, ejected in tendrils. Hypomyces ochraceus Tul. Langridge, April, 1874. H asterophorus Jul. Leigh Wood (Macroconidia), C. Bucknall. H aurantius Tul. Batheaston, March, 1871, Langridge. * From upo, beneath, and kreas, flesh. + From upo, beneath, and muke, a fungus. 11 H torminosus Tul. Leigh Wood, October, 1879. C. Bucknall. ~ H. luteo-virens Tul. Ashton Court, Bristol, April, 1845 ; Bathford, December, 1864. H lateritius Tul. Leigh Woods, September, 1844. H aureo-nitens Tul. Lucknam Grove, December, 1864. H Broomeianus Jul. Batheaston, November, 1877. H——— candicans Plowright. Bathford, October, 1880. Grevillea xi., 50. GENUS 291. EPICHLOE.* J*7. Parasitic on grass, coloured ; perithecia fleshy, immersed in a mycelioid stroma ; sporidia linear. Epichloe typhina Berk. on stalks of grass. Bathford, &c., July, i877. GENUS 292. XYLARIAT Fr. Vertical, more or less stipitate. Stroma between fleshy and corky, covered with a black or rufous bark. Xylaria digitata Grev. Stapleton, June,1879. C. Bucknall. D.¢ polymorpha Grev. Rudlow, March, 1843. X—— hypoxylon Grev. Lucknam, &c., October, 1854. D4 carpophila Fr. Spye Park, October, 1843. X——— vaporaria Berk, Clitfe Pypard, November, 1863 ; on cow dung laid in a heap, proceeding from a sclerotioid body. pedunculata Fr. Wraxall, near Bristol, March, 1845 ; Bathford Hill, November, 1863. X——— bulbosa P. Lucknam, October, 1859; Bathford Hill, in plantations. Xx * Epichloe, from epi, upon, and chloe, green grass. + Xylaria, from Xulon, wood. 12 GENUS 293. PORONIA.* Fr. Between fleshy and corky. Fructifying surface margined, orbicular. Perithecia immersed, vertical. Poronia punctata Fr. Batheaston, April, 1871; Hanham. GENUS 294. HYPOXYLON.¢ Bull. Stroma, corky or brittle, convex or plane, immarginate, at first clothed with a floccose veil, then with a black crust, distinct from the matrix. Perithecia vertical or divergent. Hypoxylon ustulatum Bul/. Batheaston, on old stumps. H — nummularium Bull. Stapleton, near Bristol, October, 1853 ; Leigh Wood, September. H————- luteum Fr. St. Catherine’s, April, 1867 ; Warleigh February, 1862. — gastrinum Fr. Batheaston, December, 1862 ; Rudlow, February, 1843. H-~————- concentricum Grey. Batheaston; common on ash timber. H———— coccineum Bull. Batheaston, on beech timber. H H— multiforme Fr. Batheaston, November, 1875. H— argillaceum fr. Batheaston, winter, common on ash sticks. H—-——- fuscum fr. Very common on sticks. H————- rubiginosum Fr. On bare trunks, &c. H———— serpens Fr, Common on dead wood. H-————— coprophilum Fr. Batheaston, October, 1864; on cow dung. H —udum Fr. Leigh Wood, April, 1877. OC. Bucknall. H————- atro-purpureum Fr. Leigh Wood, April, 1877. C. Bucknall. * Poronia, from poros, a pore. + Hypoxylon, from upo, beneath, and xulon, wood. 13 GENUS 295. DIATRYPE.* ’ Stroma partly formed from the matrix, and not distinct from it ; perithecia sunk, elongated above into a distinct neck; and frequently rostrate. Dyatrype pantherina (B.) Leigh Wood, April, 1879. C. Bucknall. D———— scobina, Nike. Brockley Coombe, May, 1879. C. Bucknall. D—— bullata Fr. Batheaston ; common. D———- undulata Fr. Rudlow, April, 1865 ; on dead sticks. D————- stigma Fr. Rudlow, January, 1843 ; very common. D—_— disciformis Fr. Rudlow, January, 1843; very common. D———— favacea Fr. Spye Park, March, 1859. D—— verruceformis. Batheaston, March, 1872. D——- scabrosa Fr. Near Bristol, March, 1872. D — sordida Fr. Spye Park, February, 1851. D quercina Fr. Batheaston ; winter. D——- ferruginea Fr. Shockerwick, March, 1854. D——— ceratosperma Fr. Swainswick, March, 1856. D strumella Fr. Batheaston, April, 1852. D— corniculata B. and Br. Lucknam, March, 1853. D——— podoides Fr. Leigh Wood, February, 1877. C. Bucknall. D———— aspera Fr. Shirehampton, January, 1878. C. Bucknall. . D———- angulata Fr. Shirehampton, March, 1880. C. Bucknall. . D — ilicina Che. (Diaporthe). Durdham Down, May, 1878. C. Bucknall. -D———— lirella Mont. (Diaporthe). Boiling Wells, Bristol, June, 1881. C. Bucknall. i a nS ee ee * Diatrype, from dia, through, and trupe, a hole. . 14 D——— Laschii Nike. (Diaporthe). Leigh Wood, May, 1883. C. Bucknall. D—— euphorbie Che. (Diaporthe). Leigh Wood, May, 1883. C. Bucknall. GENUS 296. VALSA.* Fry. Perithecia carbonaceous, perfect, circinating, elongated into con- verging necks ; ostiola erumpent, joined together, or ending in a common disc. Valsa prunastri Fr. Rudlow, January, 1843 ; on sloe. V stellulata Fr. Batheaston, March, 1859. V. syngenesia Fr. Batheaston, March, 1870. V. detrusa Fr. Wraxall, January, 1845. V— fibrosa Fr. Rudlow, May, 1843. V nivea Fr, Bathampton, March, 1864. V. leucostoma Fr. Batheaston, February, 1851. V controversa Fr, Leigh Wood, January, 1880. C. Bucknall. V—— taleola Fr. Shirehampton. C. Bucknall. V. circumscripta Mont, Near the Avon, March, 1880. C. Bucknall. Vv pini Fr, Leigh Wood, December, 1866, V. profusa Fr. St. Catherine’s, April, 1852. V—— coronata Fr. Spye Park, February, 1851. V chrysostroma Fr. February, 1850; on hornbeam. V—— suffusa Fr. Spye Park, August, 1859. V—— leiphemia Fr. Rudlow, May, 1843. V. salicina Fr. Swainswick, January, 1852. V—— ambiens Fr. Rudlow. V—— stilbostoma Fr. Rudlow; var. platanoides. V— — tetratrupha B. and Br. Spye Park, March, 1859 ; on alder. ¥: fenestrata B. and Br. Spye Park, March, 1859. * Valsa, a word used by Adanson, derivation uncertain. 15 V—— tetraploa B, and Curt. Batheaston, February, 1850. V. rhodophila B. and Br. Leigh Wood, C. Bucknall V—— pulchella Fr. Brockley Coombe, January, 1845. V. quaternata Fr, Near Chippenham, February, 1850 ; on beech. V. hypodermea Fr. Batheaston, December, 1851. V. hapalocystis B. and Br. Batheaston, ‘April, 1850, on plane. V— bitorulosa B. and Br. Batheaston, December, 1851. V—tilie Tul. Leigh Wood, May, 1881. C. Bucknall, V. gastrinoides (Anthostoma) P. and Wr., Grevillea X. 71. Leigh Wood ; Bristol Fungi, pl. IL, fig. 11. ©. Bucknall. V—— pustula Desm. Leigh Wood, June, 1882. C. Bucknall ; Bristol Fungi, fig 9. V—— conjuncta (Nees) Fr. On Rubus idzus; Batheaston, February, 1850. GENUS 297. MELOGRAMMA.* Fr. Perithecia confluent with the stroma, more or less free above, destitute of any neck; contents oozing out, and often forming eirrhi. GENUS 298. DOTHIDEA.t Jr. Perithecia none. Nucleus contained in globose cavities, immersed in the stroma, with a decided neck and papilleform ostiolum. Dothidea ribesia P. Langridge, April, 1872; on currant. D rose Fr. Batheaston, &c. ; common on roses. D filicina Fr. Leigh Wood, May, 1878. C. Bucknall. D striefornis Fr. Batheaston, January, 1857. D rubra P. Rudlow, September, 1843. 2s I 2 AIR ih pa ee me * Melogramma from Melas, black, and gramma, a letter or mark, + Dothidea, from dothien a tumour, and, eidos, a resemblance. 16 D——— ulmi /r. Rudlow, November, 1841. D——— trifolii Fr. Westbury, Bristol, April. C. Bucknall. D——— Johnstoni B. and Br. Sandy Lane, May. C. Bucknall. D chetomium Fr. Batheaston, February, 1851. D——— graminis Fr. Derry Hill, winter. D——— brassice Desm. Batheaston, &c. GENUS 299. ISOTHEA.* 7, Nucleus without any perithecium, coloured or black, covered by ‘the transformed substance of the matrix, or immersed in it. Isothea pustula Berk. Batheaston, winter ; on oak leaves, GENUS 300. HYPOSPILA.t 7. Perithecia globose, black, mouthless; altogether innate, concealed by the blackened substance of the leaves, and when that falls away, splitting across. GENUS 301. STIGMATEAL Fr. Parasitic. Perithecia globose, black, innate, slightly prominent. ‘Nucleus firm, at first mouthless, then bursting with a roundish aperture. Stigmatea geranii Fr. Batheaston ; on various Geraniums. S——_—— robertiani Fr. On Geranium robertianum. GENUS 302. oomMyces§ JB. and Br. Perithecia erect, contained in a polished, coloured sac, which is free above. Ostiola punctiform, apical. Oomyces carneo-albus. B. and Br. Spheria Libert. On leaves of Aira cespitosa. Batheaston and Bowood, autumn and spring. Ann. of Nat. Hist., No. 590. Libert excicc, No. 241. * Jsothea, beautiful. + Hypospila, from upo, beneath, and spilon, a stain, { Stigmatea, from stigma, a spot or mark, § Oomyces, from Oon, an egg, and muke, a fungus. 17 GENUS 302. Necrria.* . Fr. Stroma none; or, if present, bearing the coloured, naked perithecia on its surface. Nectria cinnabarina Fr. Batheaston, common. N——— coccinea Fr. Batheaston, common. N——— ccucurbitula Fr. Batheaston, winter. N——— sinopica Fr. Batheaston, January, 1856, on ivy. N——— aquifolia Berk. Ashwick, April, 1854, on holly. N——— inaurata B. and Br. Ashwick, April, 1854, on holly. Ann. of Nat. Hist., No. 781. N. citrino-aurantia Lacroiz. Decem., 1873, on willow twigs. N——— ochracea Fr. Batheaston, Langridge, January, 1872. N——— aurantia Fr. Batheaston, winter, 1869. N——— Albertini B. and Br. Bathford, April, 1865. N—— flavida Fr. Batheaston, March, 1877. N——— furfurella B. and Br. Batheaston, February, 1869, on old cabbage stalks. Annals of Nat. Hist., No. 1,331. N. Peziza Fr. Rudlow, August, 1842, common. N— sanguinea Fr. Rudlow, February, common. N. epispheria Fr. Batheaston, winter, on old, decaying hypoxyla. N— Rousselliana Mont. Batheaston, March, 1859, on box leaves. N——— graminicola B. and Br. Batheaston, April, 1854. Annals of Nat. Hist., No. 897, fig. helminthicola B. and Br. Bathford, January, 1859. Annals of Nat. Hist., No. 896, on Helminthssporia, N——— ochraceo-pallida B. and Br. Batheaston, February, 1877. Annals of Nat. Hist., No. 607, on dead elm. erubescens Desm., on holly leaves. Clifton, Oct., 1879. C. Bucknall; with a figure. Fungi of the Bristol District. N— N. * Nectria, from necto, to join together, the perithecia of some of the species being united by a definite stroma. B 18 N. muscivora B. and Br., on mosses. Bristol. Annals of Nat. Hist., No. 608. N. mammoidea P. and Ph. Walton Hill, July, 1881. C. Bucknall. N— dacrymycella Nyl. Blaize Castle, May, 1882. C. Bucknall. N arenula B.and Br. Batheaston, February, 1851, on Aira cespitosa. Annals of Nat. Hist., No. 622, with a figure. GENUS 303. SPH#&RIA.* Hall. Perithecia black, pierced at the apex, mostly papillate, superficial or erumpent, without any stroma. Series J. SUPERFICIALES. Byssisede, Spheria thelena Fr. Box quarries on timber underground. April, 1872. William Broome. aquila Jr. Batheaston, common on sticks. April. tristis ode, Batheaston, common on sticks. March, 1861. S——— pheostroma Mont. Batheaston, January, 1859. S————. racodium P. Spye Park, February, 1851. S S S vervecina Desm. Rudlow, Dec., 1842, on the ground in woods. S Epochnii B. and Br. Warleigh. Annals of Nat. Hist., No. 1,177, with a figure, t. 5, fig 36. Villosz. S_———. ovina P. Batheaston, March, 1869, on rotten wood. g——. brassicee KJ, Batheaston, April, 1869, on cabbage stalks. ee i ee * Spheeria, from sphaira, a sphere. 19 canescens P. Lucknam Grove, April, 1866, on rotten S wood. Ss hirsuta Fr. Batheaston, January, 1869, on wood. Ss macrotricha B. and Br. Bathampton, February, 1851. Annals of Nat. Hist., No. 619, with a figure. S—_—. Chetomium Fda. Batheaston, winter, on Carex pendula. SS) eres B. and Br. Spye Park, February, 1850, on dead carices. Annals of Nat. Hist., No. 621, with a figure. S exilis_4. and 8. Lucknam Grove, March, 1859, on pine. S pilosa P. Bathford, December, 1875, on decayed wood. 8 hispida Tode. St. Catherine’s, January, 1852, on decayed wood. S membranacea B. and Br. Langridge, April, 1874, on wood. Annals of Nat. Hist., No. 1493. S———-_ barbula B. and Br. Belmont, near Bristol, March, 1859, on pine. Annals of Nat. Hist., No. 870, t. 10, f. 20. exosporioides Desm. Batheaston, March, 1859, on dead leaves of Carex pendula. S——— felina Feks. Batheaston, March, 1869, on dead stalks of Rubus. Ss Ss — cupulifera B. and Br. Langridge, April, 1869, on decayed elm stumps. Annals of Nat. Hist., No. 1,333, witha figure. Ss pellita Fr. Leigh Wood, April. C. Bucknall. S——— capillifera Currey. Leigh Wood, autumn. C, Bucknall, Denudate. S—— bombarda Batsch. Rudlow, October, 1843, on wood. S—— spermoides Hoffin. St. Catherine’s, 1869, on wood. S- papaverea B. and Br. Batheaston, October, 1869, on an elm stump. Annals of Nat. Hist., No. 612, with a figure 20 S——— moriformis Tode. Rudlow, February, 1843, on wood. S innumera B. and Br. St. Catherine’s, March, 1871, on wood, Annals of Nat. Hist., No. 2,578. Tulasne Carpologia IL. p, 253, t xxxlii—f. 7 to 9. (Cheetospheria). S- stercoraria Sow. Batheaston, January, 1867, on horse dung. s- pomiformis Pers. Rudlow, November, 1841, on old apple trees. Annals of Nat. Hist., Series iv., Vol. 7, pl. xxi., _ fig. 28, conidia. S——-— obducens Fr. Batheaston, January 7, 1852, on wood. S——— pulvis-pyrius P. Batheaston, October, 1860, on wood. S——— rhytidodes B. and Br, St. Catherine’s, January, 1852. Annals of Nat. Hist., No. 873, with a figure. On ash pollards. S——— perexigua Lév. Leigh Wood, April, 1877. C. Bucknall. Ss pulveracea Ehr. Batheaston, February, 1859. NS) myriocarpa Fr. St. Catherine’s, May, 1864, S vesticola B. and Br. Batheaston, December, 1858, on old cloth. Annals of Nat. Hist., No. 874. S——— rubicola Currey, M.SS. Batheaston, March, 1869 ; Lin. Trans. 319. S—— caudata Currey. L.c., with a figure. S——— ostioloidea Che. on Hymenochete. Leigh Wood, January, 1878. C. Bucknall; Greville iv., 113. S———- Stevensoni B. and Br. Stapleton, June, 1882. C. Bucknall, Annals of Nat. Hist., No. 1,926. Fungi of the Bristol districts, No, 1,016. S——— platyspora (Sordaria) Ph. and P. Leigh Down, May, 1879. C. Bucknall. equorum (Sordaria) Winter in Hedwigia, 1871. Leigh Down, May, 1878, OC. Bucknall. S——— merdaria (Sordaria) Fr. Leigh Down, May, 1878. C. Bucknall, s 21 S minuta (Sordaria) Winter, 1.c., var. tetraspora. Leigh Down, January, 1881. C. Bucknall; with a figure, pl. 4, fig. 6. S curvula De By. (Sordaria) Hedwigia, 1871. Stapleton, February, 1881. C. Bucknall, 8 pleiospora Winter, Grev. x., 72. Leigh Down, January. C. Bucknall ; with a figure. S——— Winteri Ph. and P. (Sordaria). Leigh Down, January, 1881. C. Bucknall. bisporula Hans. (Sordaria). Leigh Down, March. C. Bucknall. S——— sparganicola PI. in littera (Sordaria). Yatton, July, 1881. C. Bucknall; on Sparganium ramosum. S——— microspora Ph. and Pl. (Sordaria). C. Bucknall. Leigh Down, with a figure, December, 1881. Grevillea x., 73. Ss) 8 polyspora Ph. and Pl, (Sordaria), Grevillea x.,73. Leigh Down, December, 1881. C. Bucknall, s intermedia Awd. (Sporormia). Leigh Down, April, 1879. C. Bucknall. Pertuse. S——— pertusa Fr. St. Catherine’s, February, 1852. S——— brachythele B. and Br. Batheaston, February, 1859, of dead elder. Annals of Nat. Hist., No. 877, with a figure. S——— mastoidea Fr. Batheaston, January, 1857. S——— vilis Fr. Batheaston, January, 1757. 8 pedida B. and Br. Langridge, April, 1859, on beech wood. Annals of Nat. Hist., No. 1,396, with a figure, pl. x., fig. 13. Series I]. ERUMPENTES. Ceespitose. $————- cupularis P. Batheaston, January, 1869. S Saubinetii Mont. Batheaston, April, 1859, on elm sticks. 22 naucosa Fy. Batheaston, January, 1860. nigerrima Blox. St. Catherine’s, April, 1867. Parasitic on various Diatrypes. This seems to be the same thing as Dothidea Jerdoni. Obturate. S——— obliterans B. and Br. Batheaston, on bare fir poles. Annals of Nat. Hist., No, 890, with a figure. Ss eulmifraga Fr. Rudlow, winter, 1851. Lophiostome. S macrostoma Fr. Spye Park, April, 1859, on holly. NS caulium Fr. Batheaston, December, 1858. S Arundinis Fr. Batheaston, March, 1854. S——— angustilabra B. and Br. Annals of Nat. Hist., No. 881, with a figure. Leigh Wood, April, 1852. C. Bucknall. S——— bicuspidata Che. Bristol, near the Avon. C. Bucknall. Ceratostome. S rostrata Fr. Batheaston, December, 1866. 8 lampadophora B. and Rr. Combe Hay, May, 1859, on elm stumps. Annals of Nat. Hist., No. 882, with a figure, Batheaston, on white thorn. S——— ligneola B. and Br. Batheaston, on decayed oak. Annals of Nat. Hist., No. 883, with a figure. 8 ampullacea Che, Leigh Wood, February, 1877. C. Bucknall, Series III. sSUBTECTA. Immerse. S——— hypotephra B. and Br. Batheaston, January, 1861, on oak palings. Annals of Nat. Hist., No. 624, with a figure. Ss - velata P. Leigh Wood, April, 1882. C. Bucknall. S——— verecunda Currey. Near the Avon, April, 1878. C. Bucknall. 23 Endophlez. S—— decedens F7. Batheaston, on hazel. S——— apiculata Currey. Batheaston, on bramble. S——— fraxinicola Currey. Brockley Coombe, May, 1869. C. Bucknall. S rubelloides Plowright. Cheddar, June, 1882. S——— melanotes B. and Br. Leigh Wood, December, 1841. Annals of Nat. Hist., No. 623, with a figure. Endocaule. S——— inquilina Fr. Langridge, March, 1853. S——— phomatospora B. and Br. Batheaston, Nov., 1850, on potato haulm, Annals of Nat. Hist., No. 647, with a figure. S———._ spiculosa P. Batheaston, January, 1860, on goose- berries. Obtectee RAMEALES. Ss siparia B. and Br. Spye Park, February, 1850, on birch twigs. Annals of Nat. Hist., No. 625, with a figure. S —— = unicaudata B. and Br. Batheaston, February, 1859, on Clematis Vitalba. Annals of Nat. Hist., No. 885, with a figure S——— ssalicella Fr. Near Chippenham, March, 1859, on willow. g——— Argus B. and Br. Spye Park, on birch wood, Feb., 1850. Annals of Nat. Hist., No. 626, with a figure. S-_—. aucta B. and Br. Spye Park, April, 1852, on alder. Annals of Nat. Hist., No. 625, with a figure. gigaspora Desm. Batheaston, February, 1860, on maple. conformis B. and Br. Spye Park, March, 1850, on alder. Annals of Nat. Hist., No, 635, with a figure. . g__-—._ trivialis B. & Br. Batheaston, March, 1854, on hazel. Annals of Nat. Hist., No. 632, with a figure. Ss S 24 S——— peristens B. and Br. Batheaston, March, 1850, on Rosa canina. Annals of Nat. Hist., No. 637, with a figure. S——— futilis B. and Br. Batheaston, March, 1857. Annals of Nat. Hist., No. 638, with a figure. S———__ oblitescens B. and Br. Spye Park, January, 1851, on Cornus. Annals of Nat. Hist., No. 887, with a figure. melina B. and Br, Batheaston, March, 1850, on ash wood. Annals of Nat. Hist., No. 888, with a figure. S——— clypeata Nees. Batheaston, Leigh Wood, February, 1845, on Rubus. S S——— appendiculosa B. and Br. Batheaston, March, 1850. Annals of Nat. Hist., No. 613, with a figure, on Rubus fruticosus, S——— rusci Wail. Batheaston, winter, on Ruscus aculeatus. S——— obtecta Currey. Batheaston, November, 1878, on alder. Annals of Nat. Hist., No. 979, with a figure (=S. celata Currey-Cke). S hemitapha B. and Br. Batheaston, Feb., 1852, on oak. Annals of Nat, Hist., No. 885, with a figure. S thodobapha B. and Br. Batheaston, April, 1869, on dead branches. Annals of Nat. Hist., No. 1,334, with a figure. S——— quadrinucleata Currey. The Gully, Bristol. C. Bucknall. S8——— deflectens Karst (Teichospora) Myc. Fennicx, Staple- ton. December, 1878. C. Bucknall. Grevillea x., 73, with a figure. Herbicolz. S tomicum Lév. Batheaston, January, 1850, on Aira czespitosa. S acus Blox. Batheaston, Jan., 1859, on stems of dock. | Ss clivensis B. and Br. Bristol, near the Avon, April, 1878. C. Bucknall. Annals of Nat. Hist., No. 643, with a figure. . 25 Caulicole. S——— _ acuta Moug. Batheaston, on nettle stems. S——— doliolum P. Batheaston, on herbaceous stems. S———._ complanata Tode. Rudlow, on herbaceous stems, winter, 1842, S——— hematites Roberge. Batheaston, March, 1854, on Clematis vitalba. S. acuminata Sow. Rudlow, May, 1843, on thistles. S——— Thwaitesii B. and Br. Batheaston, January and March, 1864, Annals of Nat. Hist., No. 646, with a figure. S———-tenebrosa B. and Br. Batheaston, on Arctium lappa, April, 1859. Annals of Nat. Hist., No. 649, with a figure. parsnip. Annals of Nat. Hist., No. 643, with a figure. S——— nigrans Rob. and Desm. Batheaston, June, 1847, on Dactylis glomerata. S——— tosta B. and Br. Rudlow, February, 1843, on Epilobicem. _ Annals of Nat. Hist., No. 648, with a figure. cariceti B. and Br. Batheaston, December, 1858, on Aira exspitosa. Annals of Nat. Hist., No. 983, with a figure. S——— planiuscula B. and Br. Batheaston, June, 1857, on Umbellifere. Annals of Nat. Hist., No. 891, with a figure. S—— rubella P. Clifton, April, 1878. C. Bucknall. S——— superflua Awd. Durdham Down, May, 1878. C. Bucknall. S——— ulnaspora Che. West Town. C. Bucknall. S——— agnita Desm. Bristol, near the Avon, May, 1880. C. Bucknall. | S——— infectoria Fekl. Bristol, near the Avon, May, 1880. C. Bucknall. S——— endopteris, Plowright (in littera). Leigh Down, April, 1882 ; Bristol district, Fungi of, on Pteris aquilina, with a figure. C. Bucknall. Ss 26 Ss— Ogilviensis B. and Br. Leigh Wood, June, on Senecio jacobea, Annals of Nat. Hist., No. 642, with a figure. C. Bucknall. % S——— herbarum P. Batheaston, on various plants, S——— typhecola Che. Grevillea v., 21.; Pill, April, 1882. C. Bucknall. Foliicole. Rostellate. S——— setacea P. Rudlow, February, 1843, on oak leaves. s— tubeformis Tode. Batheaston, March, 1843, Spye Park. S——— gnomon 7ode. Batheaston, March, 1852. Ss— avellanee Schmidt. Batheaston, January, 1867. Ss— ostruthii Fr. St. Catherine’s, December, 1850. Spherostome. S——— pheosticta B. Batheaston, January, 1850, on Carex pendula. Annals of Nat. Hist., No. 651, with a figure. S——— anarithma B. and Br. Batheaston, June, 1867. Annals of Nat. Hist., No. 893, with a figure. sS—— caine B. and Br. Batheaston, January, 1850, on Carex paniculata. Annals of Nat. Hist., No. 654, with a figure. S eucrypta B. and Br. Batheaston, January, 1850, on Carex pendula, Annals of Nat. Hist., No. 652, with a figure. S——— rumicis Desm. Batheaston, December, 1851, on dock. 8 helicospora B. and Br. Spye Park, Batheaston, June, 1867, on Carices. Annals of Nat. Hist., No. 653, with a figure. 8 brassicecola B. and Br. Batheaston, on cabbage leaves (Asteroma brassice Chev). Annals of Nat. Hist., No. 656, with a figure, S——— punctiformis Fr. Batheaston, on dead leaves ; winter. NS) alliarie 4wd. Stoke, near Bristol, April. C. Bucknall. S——— italica Sace. Clevedon, Mr. Green (Sace, sylloge, No. 1,107, anthostoma), 27 GENUS 304, SPHARELLA.* De Not. Perithecia membranaceous, immersed or semi-immersed, scarcely papillate, sporidia elliptical or oblong, two or more celled, rarely simple, hyaline, pale or colourless. Spherella maculzformis (P.) Che. Batheaston, on dead leaves. S — errabunda (Desm.) Awd. Batheaston, May, 1871, on beech leaves. s—— carpinea Fr. Batheaston, on hornbeam, Annals of Nat. Hist., No. 655, with a figure. S—— _ hedereecola Fr. Batheaston, May, 1851 (Depazea). S———— dianthi Desm. Batheaston, March, 1851, on carnations. S———— inequalis Che. Durdham Down, March, 1879. C. Bucknall. S————- taxi Che. Leigh Wood, February, 1878. C. Bueknall. 8 — oblivia Cke. Brockley Coombe, May, 1879. C, Bucknall. S———— latebrosa Che. Leigh Wood, May, 1879. C. Bucknall. GENUS 305. MASSARIA.t De Not. Perithecium subcarbonaceous, Ostiolum papilleform, Sporidia septate or simple, oozing out and staining the matrix. Massaria inquinaus Fr. Batheaston, on elm branches. M fedans Fr, Batheaston, with conidia, February, 1852. (Sph. amblyospora B. and Br.) M——— macrospora Desm. Box, March, 1843, on beech. M eburnea Zul. Batheaston, December, 1858, with conidia (Septoria princeps B. and Br.) Annals of Nat. Hist., No. 940, with a figure. M fimeti Fr. Bathford Hill, on rabbits’ dung. M holoschista (B. and Br.) On alder, Spye Park. Annals of Nat. Hist., No. 977, with a figure. * Spherella, a diminutive of Sphzria. + Massaria, so named in honour of Dr. Massare, a botanist, 28 GENUS 306. HYPOCREOPSIS.* Winter, Hedwigia, 1875. Compound ; perithecia immersed in a fleshy red stroma, covered on the surface by a reddish down; ostiola erumpent, darker ; asci oblongo-ventricose, subsessile, 4 to 8 spored ; sporidia elliptic, simple, hyaline. Hedwigia Vol. 5, p. 123. Hypocreopsis pulchra, Winter. On sheeps’ dung, Bathford Hill, October, 1874. GENUS 307. HERCOSPORA.t F*r. Perithecium subcarbonaceous, cup-shaped, open above, covered by the bark, and differently coloured ; papilla heterogeneous, erumpent, GENUS 308. PYRENOPHORA.S JF’. Nucleus slowly formed, immersed in a sclerotioid mass which performs the office of a perithecium, Ostiolum at length slightly’ prominent, Sporidia mulsetiptate. Pyrenophora pheocomes Fr. Radlow, June, 1843, on Alisma plantago. GENUS 309. GIBBERA§ Fr. Perithecium between waxy and horny, at length free, radiato— rimose from the centre, always closed. Gibbera pulicaris /r. On various branches, common. G——— Saubinetii Mont. Batheaston, on twigs of elm, &e. GENUS 310. DICHANA|| 7. Perithecia subcarbonaceous, elliptic, closed, bursting by a longi tudinal fissure. Nucleus and asci diffluent, innato-erumpent. Dichena rugosa /r. On living barks of oak and beech. * Hypocreopsis, from its resemblance to Hypocrea. + Hercospora, from erkos, an inclosed space and sporos a seed. + Pyrenophora, from puren, a core or kernel, and phoreo, to bear. § Gibbera, from gibber, hunch-backed. || Dichzena, from dis, twice, and chaino, to crack or gape. 29 GENUS 311. cAPNopIUM.* ont. ' Parasitic, Mycelium ereeping, black, consisting of branched, articulated, even or monliform threads, Perithecia elongated, frequently branched, composed of confluent threads, the tips of which are often free. Capnodium elongatum 2. and Desm. On pear leaves, common. C—— sphericum Oke. Leigh Wood, February, 1878. C. Bucknall. ORDER 27. PERISPORIACEI. Perithecia subglobose, always closed, except in decay, mostly membranaceous. Nucleus never diffluent. GENUS 312. PERISPORIUM.t 7%. _ Peridium subglobose, without any manifest thallus or append- ages. Asci clavate. Spores indefinite. Perisporium vulgare Cda. Batheaston, on old rope, November, 1864. GENUS 313. LASIonoTRYS.{ Kye. Erumpent. Central peridium between fleshy and horny, pro- liferous, collapsing above, attached to radiating fibres. Secondary peridia ascigerous. Asci cylindrical. GENUS 314. SPHZROTHECA.$ Lév. Mycelium arachnoid. Perithecia globose, containing a single globose ascus. Appendages numerous, floccose. Sphzrotheca pannosa Lévy. On the leaves and shoots of roses, very common. S$ —————— castagnei Lév. On hops. * Capnodium, from capnédes, smoky. + Perisporium, from peri, around, and sporos, a seed, t Lasiobotrys, from lasios, hairy, and botrus, a bunch of grapes. §Spherotheca, fromsphaira, a globe, and theke, a receptacle. 30 GENUS 315. PHYLLACTINIA.* Lév. Parasitic. Perithecia hemispherical, at length depressed, seated on a persistent or evanescent membranaceo—granular receptacle. Appendages straight, rigid, acicular, at length bent back. Phyllactinia guttata 77. On various leaves, Batheaston, common. GENUS 316, UNCINULA.t Lév. Mycelium floccose. Perithecia globose, Appendages rigid, simple, bifid or dichotomous, uncinate, at length bent upwards. Uncinula adunca Lév. On poplar and other leaves, common. U bicornis Lév. On maple leaves and other leaves, common. GENUS 317. MiIcROSPH@RA.{ Lév. Mycelium arachnoid. Appendages straight, dichotomous. Branchlets swelling at the tip, or filiform. Microsphera penicillata Lév. Bathford, September, on hazel. GENUS 318. ERYSIPHE$ edu. Mycelium arachnoid. Appendages floccose, simple, or irregularly branched. Erysiphe tortilis Zév. Rudlow, September, common. E communis Schlecht, on various leaves. E— macularis Fr, Batheaston, July, on hops. GENUS 319. CEPHALOTHECA,|| ekl. Symb. Mycol. der-theinischen Pilze. Perithecia simple, free, carbonaceous, very fragile, composed of * Phyllactinia, from phullon, a leaf, and aktin, a ray or spoke of a wheel. + Uncinula, from uncinus, a hook. t Microsphera, from micros, small, and sphaira, a sphere. § Erysiphe, from Erysibe, mildew. || Cephalotheca, from cephalos, a head, and theke, a receptacle. 31 _ small pentagonal or hexagonal, radiato-striate cells, globose, and at first clothed on all sides with villose hairs, then glabrous, brown or black at the apex; asci at first seated on the tips of branched threads forming globose clusters, afterwards free, 8-spored. Sporidia heaped together, then free, simple, ovate or subfusiform ek. I find globose asei seated laterally on irregular hyphe, filled with globose sporidia. Cephalotheca sulfurea /kl., on the underside of damp boards in Mr. Percival’s grapery at Henbury, near Bristol. The ville are bright, sulphur-coloured, the threads and sporidia pale. sulphur. Annals of Nat. Hist., No. 1,729, with a figure. GENUS 320. CH#ZTOMIUM.* Kze. Perithecium thin, brittle, mouthless. Asci linear, containing dark, lemon-shaped sporidia. Chetomium elatum Kze and Schmidt. Leigh Wood, Bristol, Oct., 1859, on an old, cast-off dress. C————. graminis Rabenh, Rudlow, November, 1842. C rufulum £. and Rr. Batheaston, May, 1871, on an old paper box under a bell glass. Annals of Nat. Hist., No. 1,397, with a figure. C— chartarum Ehb. Batheaston, April, 1862, on damp paper in a tin box. GENUS 321. ASCOTRICHA.t Berk. Perithecium thin, free, mouthless, seated on loose, branched, conidiiferous threads. Asci linear, containing dark, elliptic, sporidia. Annals of Nat. Hist., No. 116. Ascotricha chartarum Berk. Batheaston, June, 1874. The conidia are at first developed in a mucous (hollow 1) globose: mass, which at length disappears, on damp paper. * Chetomium, from chaite, a hair. + Ascotricha, from ascos, a sac, and thrix, a hair. 32 GENUS 322. EuROTIUM.* Lk. Perithecia reticulated, vesicular, coloured, attached to mucedinous threads, asci delicate. ; Eurotium herbariorum Zk. Batheaston, on plants in herbaria. This is considered merely an ascigerous state of Aspergillus. St. Catherine’s on damp sticks and leaves in the woods. ORDER 28. ONYGENEI. Peridium formed of loosely interwoven threads. Sporidia at length forming a compact, dusty mass. GENUS 323. ONYGENAS P. Parasitic on animal substances. Peridium stipitate or sessile, paper like, at length splitting. Asci delicate. Sporidia at length forming a dusty mass. Onygena apus B. and Br. Hanham, on bones buried in the soil in woods. FAMILY VI. PHYSOMYCETES.{ Threads free, or only slightly felted, bearing vesicles which contain indefinite sporidia, ORDER 29. ANTENNARIEIL. Threads black, more or less felted, moniliform and equal in the same felt, bearing here and there irregular sporangia. * Eurctium, from euros, mouldiness, + Onygena, frem onux, a hoof, and ginomai, to spring from. + Physomycetes, from phusa, a bladder, and muke, a fungus, 33 GENUS 324. ANTENNARIA.*~ Lh. Threads felted, black, articulated, often moniliform. Walls of sporangia mostly cellular. Spores chained together, immersed in gelatinous pulp. Antennaria semiovata B. and Br. Hanham, on fronds of Filix mas, September, 1853. Annals of Nat. Hist., No. 784, with a figure, _ GENUS 325. ZASMIDIUM.+ Fr. - Sporangium thin, carbonaceous but brittle, growing on a septate, byssoid, equal mycelium. Mouth subumbilicate. Spores simple. Zasmidium cellare. Common in wine cellars, forming brown, byssoid tufts, rarely forming any fruit. ORDER 30. MUCORINI. Threads free, bearing terminal or lateral appendages. GENUS 326. ascopHoRA.t Tode. Sporangia collapsing, and at length hanging down over the fructifying apices like a hood. Fruit sometimes of two kinds. Ascophora mucedo Tode. On bread, common. GENUS 327. MucoR.§ Mich. Threads free, Sporangia at length bursting, but not dependent. Mucor amethystiuus Berk. Rudlow, October, 1847, on rotting pears. M ramosus Bull. Box, October, 1863, on rotten wood. M mucedo LZ, - On paste, very common. M fusiger Lk. Rudlow, October, 1843, on rotten Agarics, * Antennaria, from antenna, a sailyard. + Zasmidium, perhaps from zosma, a kind of seaweed. { Ascophora, from ascos, a vessel, and phero, to bear. § Mucor, mould. Cc 34 GENUS 328. HYDROPHORA.* Tode. Threads erect, tubular, sparingly articulate, equal above, ter- minated by a vesicle which is at first watery and crystalline, then turbid, and at length indurated and persistent from the conglo- meration of the spores. Hydrophora stercorea Tode. On dung, common, GENLS 329. ENDODROMIA.| Berk Vesicle very delicate, perforated by the stem, filled with delicate, branched, radiating threads, and globose spores, with a nucleus endowed with active motion. Endodromia vitrea Berk. Hook, f. 1., 1841, iii, t. 1, fig. C.; has not occurred in the district. GENUS 330. SPORODINIA.{ Lk. Stem dichotomously branched. Vesicles solitary, terminal, at length splitting horizontally. Columella large. Spores simple, growing on the columella. This genus has not occurred in our district. GENUS 331. ACROSTALAGMUS§$ Cda. Flocci branched. Branches verticillate. Vesicles terminal, pierced by the threads, from the tips of which the spores are produced within the cells. * Hydrophora, from udor, water, and phero, to bear. + Endodromia, from endos, within, and dromos, a running about. t{Sporodinia, from sporos, a seed, and dineuo, to whirl about or move. Link remarks “continuatio Wild,c. I. p. 94, ‘ Ehrenberg vidit massam sporulosam e floccis in sporangium moveri. § Acrostalagmus, from akros, pointed, and stalagmos, a drop, or a state of dropping. 35 Acrostalagmus cinnabarinus Cda. Batheaston, on decaying plants, Verticillium lateritium. One of the Mucedines is found to be a form of this species, with naked spores. See Corda Icones c, ii, 15, t. 10, fig 66. GENUS 332. syzyGiTEs* Jhb. Threads branched above. Vesicles of separate branches con- jugating, and forming a distinct sporangium. Syzygites megalocarpus Ehb. Has not occurred in our district, at least in its perfect state. GENUS 333. ENDOGONE.Tt Lk. Hypogeous. Flocci collected into a globose, spongy mass. Vesicles globose, solitary, or collected in little fascicles at the ends of the branches. Endogone pisiformis Zi, Near Bristol, in woods, autumn. . Onan abnormal Flower of a Penstemon, By C, E. Broome, F.L.S. (Read March 18th, 1885.) A flower of a Penstemon, communicated to me by C. Timmins, Esq., in May, 1884, presented the following peculiarities :— The calyx was leafy, the calyx leaves nearly those peculiar to the species, the corolla was situated closely above the calyx and was composed of segments partly green and partly blue, one stamen with its filament was normal; the other four stamens were converted into distorted green, leafy appendages; the style * Syzygites, from sun, together, and zugon, a yoke. + Endogone, from endon, within, and gone, seed. 36 ‘was prolonged into a green stalk about one inch in length, which was furnished with two leaves of the normal form. About two- thirds up there was a flower bud, above which the stem was again continued for about a quarter of an inch, and surmounted by a whorl of four leaves with an axillary flower bud as before. The above were the features presented by the specimen sent me, and they would seem to come under Dr. Master’s case of prolification of the flower mentioned in page 115 of his Teratclogy. Where the centre of the flower is occupied by a bud or branch, the growing point, or termination of the axis, which ordinarily ceases to grow after the formation of the carpels, has here taken on new growth. The mixed colours of the corolla, in the present instance partly green and partly blue, were of interest as tending to show the true nature of the floral leaves, viz., that they are merely the ordinary leaves of the plant converted into petaloid leaves, I do not find the genus Penstemon among those in which such reversion has been recorded, it has been observed, however, in other genera belonging to the order Scrophulariaceew, as Verbascum. Similar transfor- mations are not uncommon in other orders. Dr. Masters gives a remarkable instance in a flower of a cherry in which there was‘a gradual change from the floral to the foliar condition ; there were five distinct lanceolate sepals, the arrange- ment of whose veins betokened that they were leaf-sheaths rather than perfect leaves, ten petals partly foliaceous and sheath- like as to their venation, one of them funnel-shaped. The stamens were ten in number, their connectives prolonged into foliaceous appendages so that the filament represented the stalk of the leaf. The pistil was entirely absent, and its place was supplied by a branch with numerous perfectly formed stipulate leaves. The genus Plantago presents numerous instances of this kind of transformation, its monstrosities are not uncommon in our gardens, and that of P. major is frequent in our fields, it is also common in cultivated roses. 37 It seems probable that the prolification of the parts of flowers arises from over luxuriance of growth, since a check given to vegetative development, as by root pruning, &c., tends to the production of flowers and fruit, as is well known to gardeners, and the converse doubtless holds true, and plants which increase freely by scions, &c., are less free to blossom and produce seed. Notes on Roman Paving Found in Bridewell Lane. By T. BROWNE, Esq. (Read March 18th, 1885.) At the request of our Secretary, I have brought together a few notes on the fragments of tesselated Roman Pavement that were found in August, 1884, in digging the foundations for a new building in connection with the Mineral Water Hospital. The largest piece was found near the south-west corner, and under the old front wall of what had been a public-house known as the “Sedan Chair,” at a depth of about 7ft. Qin. below the pavement of the lane. The Paving was an irregular fragment that would be included in a measurement of 6ft. each way. A careful exploration was made for some distance all round, in hopes of finding more; but nothing further was discovered. The original Paving seems to have been largely destroyed in the making of a drain from the old public-house to the sewer, no doubt many years ago. A small fragment was also found at about the same depth near the north-west corner of the building, and} almost in a line with the other, and at about the same level. On comparing the depth at which the Paving was found with that which was discovered in 1859, when the Blue Coat School and Mineral Water Hospital were built, it appears that these fragments are about 3 ft. below the level of the old Roman 38 Paving which was then found, and is still preserved in sifu in the basement of the Hospital. The annexed photograph of the large fragment will give some idea of the patterns of the work. It will be seen that this was very richly designed, with a series of large octagons measuring 2ft. 8in, across, and containing in the interior of each a series of circles in small stones, and between the circles and the margins were foliated patterns worked in coloured stones. Apparently there must have been considerable variety of design in the whole of the original Paving, for we have here only one complete octagon, and fragments of two others, and the patterns are different in each. The small squares and triangles filling in the spaces between the several octagons and the outer borders are filled in with rows of tesserae with reversed squares of colour. On the outer border there is a line of dark tiles, and beyond this again we found a margin of tiles laid herring-bone fashion and of which three rows could be traced. This was no doubt intended to fill up the space between the ornamental centre and the walls of the room ; but no trace of the walls could be found. The Paving was bedded upon fine red concrete made from pounded bricks and lime—at least six inches thick, and resting upon the earth. The Pavement has been carefully lifted up in pieces, and secured to a fresh base of cement; and it was found to be in such a loose, rotten state, and the surface so damaged that it was most difficult to lift up anything but small portions at a time. A few of the tesserae have thus got slightly misplaced ; but as a whole the patterns are nearly as perfect as when first discovered. A portion has been brought here for the inspection of the members. The small fragment of Paving found at the north-west corner is of a much plainer character, and consists of a series of squares with dividing lines and border, and was probably from a room not considered worthy of a more ornamental Paving. 39 The tesserae in both cases appear to consist of pieces of white and blue lias, red brick or tile, and a purply red sandstone, all of which were probably obtained not far from Bath. Many of the stones are decayed and rotten, and would scarcely bear handling when once uncovered, no doubt from the effect of wet and corrosion in the ground, and subsequent drying in the air. Of course the question naturally arises whether these fragments have any connection with those found some 25 years ago at the adjoining Hospital and Blue Coat School, and I think there can be very little doubt that they all belong to the remains of a Roman building of some importance, but of which no sufficient remains are left to enable us to form any definite idea of its extent or plan. A great many irregular masses of concrete were found on the site (apart from these fragments) at different points, but they had been so broken and disturbed that no theory or idea of any regular plan could be derived from them, although they all appeared to be similar in character arid. of the well-known Roman composition. ecg? The governors of the Hospital have taken great interest in the discovery of these fragments of Paving, and have had them permanently preserved in their new building. The Bournemouth Firs; considered as the Remains of an Ancient Forest. Was there ever a Forest of Firs on the Hills around ‘Bath? By the Rev. LEONARD BLOMEFIELD, V.A., F.LS., F.GS., &c., President. (Read December 9th, 1885.) No one who has been at Bournemouth, and noticed the fir trees that give so peculiar a character to that place—if he take any interest in the suhject,—can fail to desire some information as to their origin and history. Yet he would find it difficult to get his curiosity satisfied, and be obliged, in great measure, to work out 40 the question for himself as he could. During a visit paid to Bournemouth this last summer (1885) I was surprised to find how few persons seemed to know much about these firs or cared to consider the matter. The usual guide books scarce afford any help, except on one point, to which I shall revert hereafter. They speak of the firs as having been always there and forming part of the place, and they go no further. Persons, however, who say this do not consider of what modern growth the whole place and its surroundings are, whether as a place of sea-side resort for the public, or for permanent residence on the part of the large numbers who have made it their home; nor set themselves to inquire what was the state of things previously, As the place appears now, broad roads, equal to any in England, are seen branching off in various directions with elegant houses or villas on either side, at intervals, each having its own grounds and garden; the firs that have been left simply growing by the sides of the roads, or along the sides of the gardens, where they often form a boundary, as it were, between two contiguous properties. These roads and houses are mostly on the cliffs, or they run back more or less away from the sea; the town— properly so called—being at the bottom, nearly at sea-level, and, much like the towns in other watering places, calling for no particular remark. What now was the character of the place before all these roads and buildings came into existence? I was informed by a lady living in the neighbourhood, that an aged acquaintance of hers had known the locality ever since the early part of this century, when hardly a single building had been erected, or the first step taken towards bringing it into its present condition. It was in its wild primitive state—an enormous forest of Scotch Firs, with scarce any break, reaching for miles away from the sea into the surrounding country. Who, now, planted all these firs, supposing them for a moment to have been planted? Not one man, nor many men. Is it likely either that the several owners of the 4] different properties, over which the forest must have extended in those days, would have all come to one agreement in this matter ? Let us bear in mind the contiguity of this forest of firs to the New Forest in Hampshire. The latter was formerly much more extensive than it is at the present day. “ By some it is thought probable that William, instead of actually creating the forest, simply added to the extent of a vast tract of woodland which previously existed there.”* Wise, too, states that the forest “ occupied nearly the entire §.W. angle of Hampshire:’+ if so it must have been conterminous with the Bournemouth forest, or mixed up with it. And though the New Forest is more distinguished at the present day for its oaks, beeches, and birches, &c. than for its conifere, it must surely have had formerly a large growth of firs in addition to the trees above mentioned, or at least in certain parts of the forest. - Lymington Heath is spoken of in the “New Forest Guide Book,” as “a vast stretch of heather and gorse extending down to the “Beaulieu estate, broken here and there by a few barrows and a « solitary fir tree, presenting a wild, inhospitable and dreary scene.” To my thinking, these solitary fir trees here and there are the sole survivors of a much larger number formerly growing in that part of the forest. According to a statement in the Times newspaper, “ there are hundreds of thousands of Scotch Firs in the New Forest at the present time.”{ Probably a large number of these have been planted, but the circumstance shows how con- genial the soil and other conditions of the forest are to the habits of the fir. As for the firs in the original Bournemouth forest, they must have been practically innumerable. It is said that even at the present day, notwithstanding the clearances that have been made, peng ARE AREF SS * New Forest Hand Book, 2nd Ed., p. 8. See also Leland, Itineraries, 2nd Ed.,, vol. vi., p. 88. + History of the New Forest, p. 20. { Times, September 19, 1885. 42 ‘upwards of three million pine trees remain in the different districts of Bournemouth and its immediate surroundings.”* The gravels and sands, which cover so large a portion of the Bournemouth district, seem naturally favourable for the growth of the Scotch fir, and seedling plants abound everywhere, which if left to themselves would soon grow up into a thick plantation. There are a few groups of firs lying some way east or north east of the pier—one group especially, at the termination of the cliff road, and just within the one-mile radius, of a somewhat rectangular form, and reaching quite to the cliffs edge—which distinctly give the idea of having been self-originated and undisturbed by man. In this last group, away from all buildings, the trees present a very uniform appearance. They are near together, and of a fair height; but from never having been thinned out, are drawn up into mere poles, with a considerable brush of foliage at top, the ground underneath being quite bare of grass or any other herbage. There are, again, a few trees very much larger than any of the above; one especially, known to the inhabitants of the neighbourhood by the name of “The Four Evangelists,” from its spreading out, a few feet from the ground, into four large branches. This tree, thought by a friend resident in Bournemouth to be the largest in the district, stands in the angle formed by Grove Lane and the road leading from Christchurch to Herne Court. I measured it with the help of another party, and found it to be 13 feet and a half in girth, at about three and a half feet from the ground.t It is between three and four miles from Bournemouth, and had probably grown up, in times far back, near the border of an old forest, or in some open space, where with more light and air, it had room for expansion. * Fortnightly Review, Sept., 1885, p. 386. + Loudon mentions firs in the Scotch forests 18 and 20 feet in girth, but does not say at what height from the ground, Arboretwm Britannt- cum. vol. iv. p. 2169. 43 There are other trees under conditions very different from those of the trees last mentioned ; trees on the edge of the cliff, exposed to the full force of winter storms, dwarfed, bent and distorted in various ways; others, below the cliffs, struggling, as it were, for life amid the shelving sand heaps threatening, to all appearance, to drag them gradually down into the sea. I have entered into the above details, as affording strong ground, in my opinion, for believing that the Bournemouth firs are true natives of that part of the country,—in opposition to those who assert that the Scotch fir, though indigenous in Scotland is not indigenous in England. Let us now go into this argument which dates back to the well known statement in Cesar’s Commentaries that there was the same timber in Britain as in Gaul, except the fir and the beech— “ preter fagum atque abietem.” This remark of Czsar’s, however, is of little worth. First, he could have seen scarce anything of Britain except Kent and the Thames district ;* secondly, in addition to the fir, he mentions the beech as not found in Britain, where he is certainly wrong, as witnessed by Windsor, Epping, Savernake, and many other native woods and forests; thirdly, firwood is recorded “to have been found under the foundation of some Roman roads.”+ In truth, firwood is abundant in many of the ancient mosses in England, and old roots of the Scotch Fir are found in the bogs of Ireland. In an Article on the Conifere in the Edinburgh Review it is stated that “remains of the Scotch Fir “are plentifully distributed in the northern peat bogs ; and that “the tree appears to have covered large districts, and to have “flourished continuously on the same spot for long periods of “time , .. . It has maintained its place, not by the long * “Cresar’s account (of Britain) is necessarily confined to Kent, the district known to him.” Scarth’s Roman Britain, p. 5. + Notes and Queries, vol. i. (Sixth Ser.), p. 78. t Withering, British Plants, and other Authors. 44 “endurance of individual trees, but by successive propagation. It “was the prevailing tree not only in England and Scotland, but “over much of the north of Europe.” In the sunken forest at Cromer, in Norfolk, in a deposit of a period immediately preced- ing the glacial, even the spruce fir is found as well as the Scotch. This was proved by the cones being submitted to the scrutiny of the celebrated Robert Brown, the first botanist of his age, who pronounced them to be those of the spruce.* The Spruce, however, did not survive the glacial period, and is consequently, in this country, extinct ; but the Scotch Fir continues on to the present day, its range being now confined mainly to the Scotch mountains, though formerly extending to several of the northern counties of England. Gerard, in his “ Herball,”t speaking of the ‘‘firre tree,” says—I have seen these trees “ growing in Cheshire, Staffordshire and Lancashire, where they “grew in great plenty, as is reported, before Noah’s Flood ; but “then being overturned and being overwhelmed, have lien since in “the mosses and watery moorish grounds, very fresh and sound *See an Article on the Conifere, Edin. Rev., Oct., 1864, p. 347; also a Lecture by the late Professor Rolleston, on “The modifications of the externa] aspects of Organic Nature produced by man’s In- terference,” 1880, p. 13. See, further, Winch’s ‘‘Essay on the geographical distribution of Plants through the counties of North- umberland, Cumberland and Durham, 8vo., 1825.” In this essay are some remarks of much interest on the subject in question. The author says—“ On some of the elevated moors of this district the “roots and trunks of very large pines (P. Sylvestris) are seen protruding from the black peat moss, being exposed to view by the ‘‘water of these bogs having drained off and left the peat bare, but “this tree is no longer indigenous with us.” He then adds—“It is “worthy of remark, that the Scotch Fir does not at this day attain “the size of these ancient pines, though planted in similar moorland “situations, even though the young trees be protected, and the “plantations situated at a lower level.” + Ed. 2, by Johnson, 1636, p, 1364. 45 “ until this day.” We may smile at a part of this statement, but what Gerard had seen himself is a direct proof of the matter in question ; and there are other statements that bear evidence the same way. Merrett, in his ‘Pinax Rerum Naturalium Britannicarum,” published in 1666,* under the head of Abies, the Fir tree, writes—“in Alpibus Scoticis, et quondam in plurimis Angliz locis Borealibus.”—Ray, in his ‘Synopsis Stirpium Britannicarum,” first published in 1696, nearly repeats the same words. Wordsworth, the poet, in a private letter, gave it as his opinion that the “ Westmoreland mountains were formerly “covered in some places to their very summits by pines (the “ Highland Pine).” He speaks of many that had survived, and were living when he was a boy.t Selby, in his “British Forest Trees,” considers that formerly the Scotch Fir ‘“ occupied most ‘of the elevated tracts of the kingdom, though the natural “forests now remaining are confined to the mountainous districts “ of Scotland.”{ Hooker, in his “* Student’s Flora of the British Islands, ”§ says of the Pinus sylvestris, “ Highlands, ascends to 2,200 feet, rare in a native state ; formerly native over many parts of Britain.” Coming down now to the southern counties of England, we have important testimony in two local Floras. of comparatively recent date, ‘‘Mansel-Pleydell’s Flora of Dorset,” published in 1874, and Townsend’s “ Flora of Hampshire,” published in 1883. It is on the confines of these two counties that Bournemouth is situated, and in consequence each author has something to say on the subject of the fir trees. Mansel-Pleydell speaks of the Scotch Fir as common on heathy places, but_ considers it a doubtful native of Dorset. Neverthe- less he states it is to be found in all the four adjacent counties of Devon, Hants, Somerset and Wilts.|| ill eS as, aa *P.1, + Notes and Queries, vol. 3 (2nd Ser.), p. 445. {P. 399. § 2nd Ed., 1878, p. 368. | Flora of Dorsetshire, p. 232. 46 Townsend, though he too calls the Scotch Fir “a doubtful native,” speaks of it as ‘‘common on the heaths around Bourne- mouth,” and shortly afterwards says “there are abundant evidences that the pine formerly grew wild throughout the county.” In another place he says—“ it seems to me possible that living pine trees in some parts of the county may be descendants from the wild plant.”+ Such is the testimony afforded by botanists, in favour of the Scotch Fir being indigenous in England as well as Scotland. Other testimony is afforded to the same effect by local names. ‘Taylor, in his “ Words and Places,” thinking to confirm Czsar’s statement above alluded to, ventured the assertion that—“‘In no single instance throughout the Anglo-Saxon charters do we meet with a name implying the existence of any kind of pine or fir, a circum- stance which curiously corroborates the assertion of Cesar, that there was no fir found in Britain.”{ I have the high authority of Mr. Earle, the Professor of Anglo-Saxon, for saying that here “Taylor is wrong ;” and Mr. Earle has kindly looked out for me several names of places all of which he considers as undoubtedly derived from the fir: such are Firbank in Westmoreland,—Fur- becke (or Firbeck) in West Riding, and Firbie (or Firby) and Furgarth in East Riding, Yorkshire,— Furbie (or Firby or Firsby) in Lincolnshire,—Furcombe, in the parish of Farnborough, Berks, —Furlé (or Furleigh) in Sussex, Pevensy Rape. In addition to the above local names, I mentioned to Mr. Earle two others in the south of England,—Furland, a tithing of Crew- kerne in Somerset, and Furland Hill, one of arange of hills between Brixham and Dartmouth : both of which he had no doubt, were also named after the fir tree. But I come now to a still more important fact, in especial con- nection with the fir trees at Bournemouth. It is the circumstance * Flora of Hampshire, pp. 321-2. + Words and Places, Ed. vi., p. 249: 47 I alluded to in the beginning of this paper as mentioned in the Bournemouth guide books. We read that “the remains of a “submerged forest may, under certain conditions of the beach, “be seen at the mouth of the valley, on the western side of the © “pier, This was especially the case in the early months of the year 1871, when some four or five of the remains of the trees, “tof which near thirty were at one time exposed, were removed ‘‘ for examination, and were proved to be the Pinus Sylvestris or “common fir of the district, with an occasional alder, The “condition and position of these remains prove that at some “ comparatively remote period the valley extended a considerable * Jistance beyond its present sea board, and was covered with trees *‘ of a similar character to those now common to the locality.”* Of this submerged forest a detailed account has been given by the late Sir Charles Lyell, in his “Principles of Geology.”+ The forest is said, by him, to have been laid open during a low spring tide in 1831. ‘It is situated between the beach and a “bar of sand about 200 yards off, and extends 50 yards along the “shore, cropping out from beneath a bed of sand and shingle. “Tt also lies in the direct line of the Bournemouth valley, from ‘the termination of which it is separated by 200 yards of shingle “and drift sand. Down the valley flows a large brook traversing “near its mouth a considerable tract of rough, boggy, and heathy “round, producing a few birch trees and a great abundance of “the Bog Myrtle (Myrica gale). In that part of the submerged “peat, which was exposed at low water, were seen twenty or “more large stumps of fir, from one to two feet in height, the roots “and bases of which still retain their bark. The sap wood of “these is soft and spongy, but perfectly white, and exhibiting its ‘‘ original character; the heartwood is exceedingly hard and tough.” After some other details he goes on to observe that “as the sea * Sydenham’s Guide to Bournemouth, 15th Ed., p. 76. + 12th Ed., vol. iL, p. 536. 48 is encroaching on this shore we may suppose that at some former “period the Bournemouth valley extended further, and that its “extremity consisted, as at present, of rough and boggy ground, “ partly clothed with fir trees.” His conclusion seems to be that the whole “had been sunk and submerged in modern times by the undermining of the sandy strata on which the peat and «trees rested, and did not imply a general subsidence or change of “level in that part of the coast.” Another submerged forest, of the same character as that of Bournemouth, and due to the same causes, is said by Sir Charles Lyell to occur on the north side of Poole Harbour. In truth, as stated by Geikie and others, submerged forests occur in places all round our coasts, testifying to what an extent living forests must have formerly prevailed in this island. Speaking of the Scotch Fir in particular, Geikie says—‘“ In ancient times it must have grown indiscriminately throughout the length and breadth of Britain, since we meet with it in the English mosses, as well those of southern as of northern districts.”* There were, according to Hutchins, some very large forests in Dorset formerly—one forest is said to have “extended over the whole island of Purbeck ”+—and we cannot but suppose fir trees to have abounded there as in the adjoining county of Hants. Taking all the above facts together, in connection with what was stated in the earlier part of this paper respecting the number and condition of the firs still growing at Bournemouth, we can hardly doubt the existence of an immense forest of firs on this part of the south coast of England, reaching over long distances east and west, in prehistoric times ; and which, continuing on by spontaneous propagation, has remained in great part to the present day. But there is another part of this enquiry yet to be considered. * Great Ice Age, p. 307. + History of Dorsetshire, vol. i., p. 171. 49 How far north did this forest extend? As the fir abounds to this day in the Highlands of Scotland, of course it was not climate that determined its northern limit. Its advances in that direction could only have been checked by the progress of civilisation and agriculture. It is hardly possible to fix the boundary line exactly ; but as a rude approximation towards it, I interested myself in tracing on the return journey from Bournemouth to Bath, for what distance on either side of the line, the firs might still be noticed. The speed of railway travelling forbids any accurate observations of this nature; and possibly I may have been mis- taken in some instances. But certainly the firs were distinctly seen, though in gradually diminishing numbers, for a very considerable distance. They were in abundance—large patches of them here and there—as far as Wimborne; afterwards (but the patches fewer in number, or the firs only standing here and there in rows), they were noticed up to Blandford. There is a manifest reason, however, for their falling off here. The sands and gravels of the Bournemouth tertiary beds are exchanged, after a while, for the underlying chalk which is far more profitable for agricultural purposes, and which must have long since led to a clearance,of the firs on that account, if on no other. I have just said that some of the trees may be seen standing in rows, and it looks as if they had been purposely left so, when the clearance was made, to serve as a border line between two contiguous fields or holdings. One can hardly imagine them to have been planted for such a purpose, as farmers in general (certainly in the eastern counties) consider low hedges, and not a row of trees, essential for good corn crops, allowing a free circulation of air overhead, and thereby in great measure prevent- ing mildew. Passing Blandford there was a decided falling off in the number of the firs for the rest of the journey ; only a few observed here and there at rare intervals. I am almost sure I saw some at Templecombe and Wincanton, and others in the vicinity of one D 50 or two stations nearer Bath. Some of these last might certainly have been planted ; but taking them in connection with the large numbers that we had passed on different parts of the line since leaving Bournemouth, it seemed to myself as if there must have been originally one continuous growth of firs the whole way ; and the question occurred to me—Did the firs ever reach to Bath itself? And then I remembered a few old scattered, scraggy, forlorn-looking firs growing on Combe Down when I first came into this neighbourhood five and thirty years ago. These firs had always been a puzzle to me. Who planted them there? supposing them to have been planted. Who cared to set them on a sort of no man’s land, or if not so, strictly speaking— on an open down, where persons wander at will, and the trees are subjected to the rough usage of every passer by? No doubt the trees had a history once, but they looked, when I last saw them, as if awaiting extinction,—life’s day all but run out. May there not have been more firs once, and in full vigour? And is it not possible they may have had some connection, I do not say with the Bournemouth firs, but with a large growth of firs existing ages back over all the downs by which Bath is surrounded, and as truly plentiful and indigenous in those days as in Bourne- mouth itself, or any other part of Great Britain? The Combe Down trees, in that case, must have had a long ancestry, and they alone survive to tell the tale of the past, reminding one of the solitary firs on Lymington Heath above spoken of. There is something of sadness felt on hearing of things in which we take an interest being found or seen for the last time. The botanist mourns for the loss of some rare plant no longer to be met with in spots where he used to gather it. And the tree as well as the flower may evoke a feeling of this kind; or steps may be taken, as they have been taken in some cases, to preserve a few individuals still remaining. The rare and beautiful Ladies’ Slipper Orchis, formerly met with in many places in the north, is now, I believe, 51 restricted to one wood in Yorkshire, where (I have heard) the owner of the ground watches over and strictly preserves the few plants growing there still. More to our present purpose, however, is a record of the last Scotch Fir seen in Ireland. It is said that “in ancient times all Ireland was full of woods on every side;”* and there is no question but there were formerly forests of firs there, as well as in England. More+ gives a few localities in which till lately they were still found ; adding— “There is one large and old fir tree, supposed to be a last relic of the ancient forests, still growing on an open bog . . in Mayo, and which was lately fenced in and carefully ssolannca by the Earl of Arran, who is the owner of the land.” I do not propose any such close imprisonment for the few remaining firs on Combe Down. But I think they should be looked after, and some record kept as to their existence before they quite disappear. Babington makes no allusion whatever to these Scotch Firs in his “ Flora of Bath.” Should not the matter be taken up by our Club, expressly instituted for the investigation of the Natural History and Antiquities of the neighbourhood of Bath? There may be antiquity in trees as well as in stones. My own botanising excursions have necessarily for many years been discontinued ; and I was about to ask if some other of our members would not make it an object of one or more of their weekly walks to take a general survey of the downs, and to note what trees they might still find there and the condition they were in. I have, however, been anticipated in this matter. One of our mem- bers, Mr. Frederick Inman, on hearing of what I wanted, forthwith kindly volunteered his services; rambled over all the downs in turn, and sent me in a statement of what he had found. He has got together a good many details of much interest, and such * See “TIreland’s Natural History” by Boate (1652), p. 119 + “Cybele Hibernica,” -p. 276. 52 as would furnish matter for a separate paper which I hope he may be induced to give the Club at some future time. I will only here give a short summary of what he has ascertained. Setting aside fir trees growing in the proximity of houses, or in adjacent woods containing other trees besides firs, where it would be difficult to distinguish between such as were wild and such as had been planted ; he finds, on the open ground, scattered trees upon Kingsdown, Banner Down and Lansdown. I have already — spoken of the Combe Down Firs, and Mr. Broome informs me that he had seen formerly a few old trees, some merely stumps, in the vicinity of Sham Castle. On Hampton Down, on the edge of the hill near the Rifle Butts, where Mr. Inman remembers to have seen formerly about a dozen trees, only three stumps of trees are now left. This looks as if the race of old original firs was dying out. There are several trees scattered about the top of Banner Down in one place, where the ground looks more “ as if it had been covered with these trees at one time than any other place at the top ofthe hill.” There are no firs on Solsbury Hill. This may, perhaps, be well explained by Solsbury having been in aneient times, according to Mr. Earle, ‘‘the site of a well-inhabited and populous British city,’* which circumstance would necessarily have led to an early clearance of any natural forest that grew on its summit and slopes. Taking Mr. Inman’s notes as a whole, I consider there is evidence to show that these trees once existed in much larger numbers; and, in connection with all that I have said in the early part of this paper, sufficient to warrant the question— “Was there not formerly, in prehistoric times, if not later, a forest of Scotch firs covering all the hills by which Bath is surrounded ?” I cannot but think the answer to this question, if answer be possible, would be in the affirmative. * Bath Ancient and Modern, p. 9. 53 The Alge of the Bath Thermal Waters. By G. NoRMAN, Esq., M.B. (Read December 9th, 1385. ) The interest attaching to the occurrence of Fresh Water Alge in thermal waters is due, not so much to the discovery of numerous fresh species, as to the mere fact of the existence of Alge under such exceptional circumstances, and of their being able to grow and flourish at a temperature that would be fatal to members of the same genus or even species taken from a normal habitat. For instance, if a portion of Oscillaria were taken from the canal or river in our neighbourhood and subjected to a temperature of 150 degrees it would undoubtedly be killed outright, whilst at the thermal springs of Karlsbad, Oscillaria grows freely in water of the temperature of 160°. Algz have been found in many of the thermal springs of Europe ; but the most important one both on account of the heat of the water, and of the variety of genera to be found in it, is that of Karlsbad, already mentioned. Here the calcareous and silicious deposits surrounding the spring are covered with Algz which also line the troughs conveying away the water into the river. In these various situations a large number of genera and species of Algz including diatoms are to be found, and some of the species of Oscillaria and Mastigocladus are peculiar to this water. At another very hot spring, the Herculesbad of Mehadia in Austria, no less than nineteen species of Alge have been found, including five species of Oscillaria. These waters are saline- sulphurous in character and vary in temperature from 80° to 180°. In the spring itself only a few forms exist, amongst them the Oscillaria—the others are found in the outflow only. Closely allied with this is the organic matter found in the sul- phurous thermal waters of the Pyrenees called “ Sulfuraire de Fontan” or “Baregine” which has been lately shewn to consist almost entirely of felted masses of Oscillatoria ; this is especially seen at Cauterets, where the temperature is as high as 140°. Numerous Alge have also been observed in and around the 54 margins of the hot springs of Iceland, fully exposed to the influence of steam and boiling water—they consisted principally of Oscillatoria and species of Conferve. Dr. Hooker in his Himalayan Journal describes Conferve as present in the hot springs of Belcuppee. He says—‘Conferve abound in the warm stream from the springs and two species, one ochreous brown and the other green, occur on the various margins of the tanks themselves and in the hottest water; the brown is the best Salamander and forms a belt in deeper water than the green; both appear in broad luxuriant strata, whenever the temperature is cooled down to 168° and as low as 90°.” On the same expedition Dr. Thomson and Captain Strachey found Alge in the springs of Pugha in Tibet, which attain a temperature of 174°, and at the hot springs of Mormay, with a temperature of 110°. The Rev. J. M. Berkeley, who examined these specimens, says of them :—‘The vegetation in the three sets of springs was very different. As regards the Conferve, taking the word in its older sense, the species in the three are quite different, and even in respect of genera there is little identity ; but amongst the Diatomacez there is no striking difference except in those of the Behar springs, where three out of the four did not occur elsewhere. In the Pugha and Mormay springs the species were either identical with or nearly allied to those found in neighbouring localities, where the water did not exceed the ordinary temperature . . . . . The species are less numerous . . . . . than might be supposed from the vegetation of those European hot springs which have been most investigated.” In America, Horatio Wood describes two new species of Alge, Nostoc calidarium, and Chroococcus thermophilus, found in the hot springs of Benton, California, the temperature of which is 160°; and in the Yeliowstone River district are some remarkable boiling mud springs which are coloured bright green by the mul- titude of Algz contained in them—this observation was made by 55 Professor Ramsay of University College, Bristol, during the Canadian meeting of the British Association, and mentioned by him at a meeting of the Bristol Naturalists’ Saciety. Lastly, Professor Moseley, whilst naturalist to the Challenger expedition, obtained Fresh Water Algz from the boiling springs of Furnas, at 8. Michael’s in the Azores. He describes the Algz as growing on the sides of clefts in the ground, about a foot wide from which, sulphuretted hydrogen, steam, and water so hot as to scald the hands, are discharged in jerks and splashes. Close to these were shallow pools of hot water, in the bottom of which were hollow channels from which hot gases and water were discharged ; the edges of these were green with deposits of Algz, which, however, were difficult to get on account of the heat of the water, In another place were swamps of hot mud, with pools of hot water, too hot to bear the finger in, constantly discharging gases and surrounded with crystals of sulphur, and here also Alge were found. He estimates the heat of the water in the hottest parts to be as high as 194°, and in others from 176°—149° ; but no accurate observations were made there. About thirty species of Algz were found, including some new ones; it was doubtful whether any Oscillaria was amongst the collection. As regards the Bath Thermal Waters, although they have been fully and frequently dealt with from historical and medical points of view, I am not aware of any recorded observations con- cerning their natural history, with, however, this exception, that both Harvey and Hassall in their respective manuals of the ‘British Fresh Water Algee” mention one species of Oscillaria as peculiar to the Bath Waters, viz., O. tenuissima, which is described as occurring in irregular, broad, velvet-like patches of a dark green colour. The irregularity of its appearance arises from the filaments being collected together into little ascending tufts, apparently rooted in the muddy deposit of the water. Each tuft proves on examination to consist of simple, uniform, even filaments, crowded together and quite pellucid, and equally 56 destitute of joints and branches ; their diameter is not more than the eight or ten thousandth part of an inch. In various parts of the baths I have found an Alga corresponding very much to this description, although Cooke, in his recently published manual of the “ British Fresh Water Algz,” discards this species with many others, remarking that “the species of Oscillaria are at present distinguished by very artificial characters, which are by no means permanent, in which respect the genus is not in a much better condition than it was forty years ago.” The observations I have up to the present been able to make may be classed under three heads, according to locality, viz. :— 1. The Algze of the Roman Bath. 2. The Algz of the King’s Bath. 3. ‘The vegetation of the Central Well. 1. The Roman Bath.—The conditions under which Alge grow here are very favourable; the temperature of the water which is just tepid, and the sheltered position, with exposure to the sunlight, encourage luxuriance of growth to the utmost. The consequence is that one species of Cladophora, viz., C. insignis, has almost monopolised the bath, to the exclusion of many other species. Professor Nordstedt, to whom a specimen was sent, says that it is the finest species of Cladophora he has seen, and rivals the typical specimens in his collection. Growing upon the Cladophora are numerous diatoms, the principal of which is Amphiprora paladosa. This is so abundant as to produce the appearance of a white fringe on the Algze when seen in bright sunlight. Mr. Grove says it is a remarkably fine specimen, as large as his typical specimens from the shores of the Tay, and the frustules look healthy and full of endochrome. Besides this are found Surirella ovalis, Synedra tenera, Nitzschia amphioxys and linearis, and a few other minute forms. The only other Alga I have been able to find has occurred in small, darkish green patches around the margins of the bath, and may possibly represent the Oscillaria tenuissima already described. 2. The King’s Bath.—This, I believe, would prove a very 57 productive field for the smaller filamentous and unicellular Algze ; but owing to the zeal of the caretakers of the bath to prevent the floor and walls becoming slimy and slippery, by means of weekly scrubbings and occasional lime washings, the algal vegetation is very scarce. However, by scraping the sediment from the floor of the bath when the water has been let out, I have been able to find portions of several species of Alge ; and the fact of their being able to grow in spite of the warfare carried on against them, justifies, I think, the opinion I have expressed as to the habitat being a favourable one. The principal genus is a Phormidium, or Lyngbya, as it is now termed by Cooke, of which there are two species, a larger and a smaller, probably P. corium and inundatum, also a few filaments of Nostoc and some unicellular Alge, principally Glzocystis. On the under sides of the wooden seats in the bath is a plentiful supply of the fungus Merulius lacrymans, common dry rot. 3. The Central Well.—tThis is the centre of highest temperature in the baths, the water being generally about 118°, flowing up directly from the source to fill the King’s Bath. The whole of the inside wall of the well presents a curious appearance, being lined thronghout by a thick coating of the fungus Merulius lacrymans, which itself is stained by the iron deposited by the mineral water, and pierced by numberless filaments exceedingly fine in character, of the small Phormidium before mentioned. Under the microscope this arrangement may be well seen; but the Alga is so small that it is with difficulty detected by the naked eye. There are various patches of Algz around the mouth and outer walls of the well; but none different, as far as I at present know, from those found in the King’s Bath. I regret that, owing to the late period of the year at which I took up this subject, and to the pressure of other duties, I have been unable to do as much justice to my subject as I should have wished ; but I propose to continue my observations, and to supplement this paper on another occasion. 58 The Earliest Map of Bath. By EMANUEL GREEN, F.S.A. (Read 13th January, 1886.) In the British Museum there is a manuscript, a quarto volume, entitled: The Particular Description of England, with the Portratures of Certaine of the Chieffest Citties and Townes. Having been given by Sir Paul Methuen to Sir Hans Sloane, it now reposes in the Sloane Collection, being numbered 2,596. The author of the book was one William Smith, who, after being at Oxford, studied heraldry and antiquities, became Rouge Dragon, and died in 1618. He seems in his wanderings to have copied the plans of different citics when he found them already done, and when not so, to have drawn them for himself. The plans given are all coloured. Bristol, placed with the county of Gloucester, is labelled :—Measured and laid in Platforme by me, Wm. Smith, at my being at Bristow, the 30th and 31st July, Ano. Dom, 1568. Canterbury is dated 1588 ; and as the title page is dated 1588, it may be fairly assumed that the work was then finished. It may be mentioned that the volume has been privately printed ; but so privately and so small an impression that the fact is barely known. Bath, described as but a “little Cittie, yet one of ye most auncientest in England,” is here reproduced. Taking it in hand as a novelty, as if the sight were quite new, it is seen to be a walled city. Then comes the desire to know all about those walls. The Domesday survey does not mention it, as it does a few other places, as being a walled city. Two years later, in 1088, our histories mention, as Florence of Worcester and other Chroniclers record, the coming of a party from Bristol in rebellion against William Rufus, when Bath was burned, plundered and devastated : William of Malmesbury says, depopulated and the spoils treasured up at Bristol. These are very strong words. There is again no intimation in these accounts that it was a walled city, or that it offered resistance as if it were so. Passing 59 now over some seventy years, we come to a Chronicle of extreme interest, the Gesta Stephani,* hitherto altogether over- looked. Covering the time of Stephen, a terrible time, imperfectly known through our present histories, this Chronicle is of particular interest, as, contrary to those more known, it is in Stephen’s favour. Unlike the others too, which treat more of northern affairs, the western events being but shortly mentioned and from general rather than personal knowledge, this one treats the western events fully, the author writing as having been an eye witness of what he records. Who the author was is unknown; but he was clearly cotemporary—probably a Norman—and connected either with the Court or the King. After describing Bristol and the Castle, and telling us that the latter, “‘ vast and fearful” to beholders, was made terrible to the district by a garrison of freebooters and robbers, he adds :— “There is a city six miles [error for twelve] from Bristol where the hot springs circulating in channels beneath the surface are -conducted in channels artificially constructed and are collected into an arched reservoir, to supply the warm baths which stand in the middle of the place—most delightful to see and beneficial for health. The city is called Batta, the name being derived from a word in the English tongue which signifies Bath, because infirm people resort to it from all parts of England for the purpose of washing themselves in these salubrious waters, and persons in health also assemble there to see the curious bubbling up of the warm springs and to use the baths.” The date of this charmingly pretty account is 1138, and it is the earliest mention of the scene. By a little imagination we can see Bath, “The” bath back to the Conquest, and had the writer added that in a gallery hard by minstrels minstreled, we should have before us almost as perfect a picture as through any much later description. * By Sewell. 60 Bath being held for Stephen, the Bristol. men in rebellion wished to get it, the more especially as it could be easily fortified (co quod facilis esset ad muniendum) A party therefore marched out stealthily in the dusk of early morning, carrying ladders and other implements for scaling the wall (scalis que secum et aliis machinulis ad murum conscendendum convectis), and took post under cover of a hollow, while scouts reconnoitred to choose the most advisable point for attack. Geoffrey Talbot, and Gilbert de Lacy, his cousin, were selected as scouts, and went out hoping to do their work unobserved; but the guards within espying them they sallied out upon them, and after a struggle secured Geoffrey as their prisoner—took him and put him in fetters and threw him into their deepest dungeon; Gilbert, stronger and more wary, escaped and returned to tell of the mischance. A curious picture this, these resolute citizens struggling with the two knights, who were, presumably, in the chain armour of the time. Then one would like to know where this dungeon was. Determined to liberate Geoffrey, the Bristolians approached Bath and summoned the Bishop (Robert) to come out and treat with them, promising him safe conduct and safe return. The Bishop “dwelling in his house with simplicity,” giving credit to their words, went out accordingly, when he was quickly seized and held a prisoner. He was then covered with abuse, and threatened with hanging unless he released Geoffrey. As soon as it was known within that the Bishop was captured, the citizens closed the gates and manned the walls (conclusis portis wd muros defendendos concurrerant) ; no assistance or succour consequently could be sent out and the Bishop was obliged to order that Geoffrey should be set at liberty. The Chronicler endeavours to excuse this, first, as being a clemency more becoming a bishop, and also because reason did not require him either to expose himself to insult, or to sacrifice his life. For Geoffrey, however, he had no biessing, but duly doomed him to the usual torment. The Bishop, being free, became emboldened, and charged his 61 captors with violation of their pledge, threatening them with discomfiture in all future enterprises. To all this they answered with jeers, and reminded him of his simplicity in supposing they were pledged ; then throwing back perhaps a little of the Bishop’s own teaching, they argued that, being already a perjured lot, their pledges went for nothing. The robberies and cruelties of the Bristol garrison becoming too notorious, King Stephen determined to reduce it. Setting out hurriedly, he unexpectedly arrived at Bath. The Bishop on his approach went out to meet the royal cavalcade ; and at once had to soften the King’s anger against himself, for having let Geoffrey go. After telling his story, how grossly insulted he had been and well nigh hanged, he was restored to favour, and the King accompanied him into the city. Stephen examined the entire circuit of the walls, commanded them to be raised higher and outworks to be constructed, and marked a special spot very capable of defence which would defy assault (ideoque muros altius sustolli, propugnacula in devectum surrigi). Then, says the Chronicle, he marched to Bristol—‘ the seat of fraud.” The Bath men, meanwhile, gallantly and vigorously maintained themselves, using every means to make the walls and ramparts impregnable (muros et aggeres omni resistendi artificio inexpugnabiliter firmare.) Keeping the walls always manned, they sometimes sallied out at night, placing parties in ambush, whilst by day the country folk and the men at arms overran the Bristol lands, sometimes appearing in force even at the gates, or setting fire to churches or houses, or whatever would burn. Bristol, however, was not taken, and the King marched on to other work. Our own records are few for this date. Passing, then, some seventy years, we come to the reign of King John. The custom of the Kings to journey with their Courts from place to place prompts a search for the movements of John, as, after the year 1200, documents may possibly be found. In 1206 some arrange- 62 ments apparently were in progress for a western journey, as the King sent to the Bishop of Bath and Wells twenty-four palfreys and twelve stable boys, and also a servant with one horse and one stable boy. Twelve palfreys and four stable boys were ordered to be removed from Taunton to Wells; five others and two stable boys were moved from Winchester to Glastonbury, and ten others with three stable boys were to be placed at Bath ; also six mares were paid for three tonells of wine sent from Bristol to Bath, with nine shillings for carriage.* There is no record, however, of a visit in this year. In 1207, the Bailiff of Bath was directed to see if the king had two dolia of wine at Bath; and presumably he had not as the Constable of Bristol was ordered to send that quantity to Bath, and place it in the house, which was the Bishop’s house.t There seems again to be no record remaining of a royal visit in this year. In 1209, however, John was at Bath for two days, May 13th and 14th; but no account of his stay can be found. In 1212, John paid another visit, being in the city on the 17th October ; and for this time there happens to be an account of the petty or smaller expenses. Besides a hundred and fourteen warreners, of whom two had three farthings per day, there were twenty-five dogs in the care of a huntsman, costing for two days, fifteenpence; then there was the huntsman himself at sevenpence halfpence per day ; and twenty-four keepers who, for the two days’ stay at Bath, had four shillings ; the total being 16s. 10d. There was also charged for hire of a cart with two horses, bringing fruit from Gillingham to Bath, from Bath to Bristol, and from Bristol to Lacock, three days, two shillings. To Odo who stayed a night at Bath with the wardrobe and the “harness” of the wardrobe, and one night at Bristol, eightpence. To five carriers of the wardrobe, five shillings, and to nine others, nine shillings. There * Close Rolls, 7 John, m. 1. + Close, 9 John, m. 15, m. 12. + Itinerary. 63 was also a payment to Agnes, the laundress, of twelvepence ; and there was an outlay of sevenpence, pro tribus wrinalibus for the use of the king ; there is another entry, pro wrinalibus et chassiis ad urinalia imponendi. An entry a little later, not specially relating to Bath, but giving an idea of what must have been the case, accounts for fifty-five stable boys who had between them six shillings and fourpence per day, and sixty-two horses costing for forage, hay, corn, and shoeing for the night, sixteen shillings and fourpence halfpenny. Six carters divided twelvepence per day, and fifteen ‘horses consumed sixteen bushels of oats; the charge for a night’s livery, hay, oats, forage, lights and litter, being three shillings and twopence. In 1213, March 13th, John was again at Bath, but the expen- diture is only briefly recorded. Five shillings were paid for fowl for the falcons, and five pounds were given between the head falconer and his associates. A day or two later the falconers were paid ten mares for flying their birds. Eighty tonells of wine were obtained from Bristol, thirty-seven at 26/-, and forty-three at 24/-* This roll is unique, and of extreme interest ; no other record affords such minute information, even down to the loss of five shillings when the king played at ‘Tables.” To dwell too long on it would be out of place, yet, besides the insight into prices, the picture is ever curious, with the cavalcade, the incessant move- ment, usually twenty or thirty miles a day; the hounds and huntsmen ; the falconers and falcons ; then the preparation in advance, and the hubbub and arrival of the party in the little— very little city. In 1216, John was again at Bath, and for the last time. Going. from Bristol to Hinton, then to Sherbourn, he was at Wells, 27th August; Bath, 28th; Bradford, 29th; and Chippenham, 1st September.t There is no record of the expenditure. In 1223, Henry III. apparently had an intention to visit the west, * Rotulus Mise, 14 John. + Close, 18 John. 64 as he ordered the Prior of Bath to repair his houses there, at a cost of sixty shillings, and to account for the same to the exchequer.* He appears to have been there, however, in 1235, as a patent was dated therefrom in that year.t There seems no other record of the visit, except an entry on the Pipe Roll of the following year be taken as a result of personal inspection. By this the Prior of Bath rendered his account for £13 11s.—a considerable sum at that time,—spent by order of the king in repairing the king’s houses and the wall around the King’s bath (in domibus Regis in villa Bathonie que reparatione indigent, et muro circa balneum Regis ibidem reparandis.{ This is so far the first known mention of the King’s bath under that name, and it shows the origin of the name as being not from usage as generally supposed, but from owner- ship, distinguishing it from the Prior's bath so named from the same cause. Henry III. died abroad, having been absent from England for some years. Edward I. on succeeding, in 1273 made inquiry in every Hundred concerning the rights or dues of the Crown, and to discover the neglect in payment or performance during the late king’s absence. Relating to Bath there are three returns; two for the city and one for the Hundred “Forinsecum” or outside the city. The last is sometimes written as the Hundred Forinsecum de Berton Bathonie ; or, the Hundred Forinsecum Bathonie de la Berton. In some documents it is noticed as the Barton Regis extra civitate. By adopting the early mode of contracting, and taking the first and last syllables of “Forinsecum” we get Forum; and thus Bath Forum is simply Bath outside the city and has nothing to do with a forum, as has been stated. As to Bath City, the juries found that King John had given the city and the Hundred “ Forinseewm” to the Prior of Bath ; and then we get a return well showing the utter neglect into * Close, 7 H.IIL,m.5. 7+ Pat. Roll, 19 H., ITI, m. 5. t Pipe Roll, 20 H. III., dors. 65 which everything had fallen, and showing clearly how reasonable the enquiry was. It was found that Henry de Courteney had built a noble chamber on the city wall, for which he had taken the stone from the wall. That the miller of the Prior took stone from the wall for repairing the pool of his mill. That the Prior took stone for building an almshouse. That he, as also had other Priors before him, made lime from the walls at the Southgate ; and other Priors had made lime at the Westgate for eight perches towards Monksmill; and that the defunct Prior had carried stones to the Priory, to the damage of the whole city. That the Master of the Hospital of St. John took stone for his house ; that Thomas Wlbeyn, William le Commandur, Roger Budde, William Faber, John Koker and William Cocer carried away stone from the walls to construct or repair their houses. That Peter Forester took stone for the pool of his mill, and Thomas Sweyn took stone to build the house in which Thomas Sweyn his son lived, and that Gunilla le Marescal’ held a house built of the stone from the wall: all being declared to the damage of the city and of the King. It was also found that the King’s own houses within the gates of the Abbey were deteriorated and destroyed, and to repair them to their pristine state would cost ten mares beyond the cost already expended on two houses within the metes of the Priory. It was also found that Robert Cherin had a tenement within the city and a meadow without, for which he kept the gate on the bridge in time of war.* This is an early mention of such a bridge. No order for repairs seems to have followed these enquiries, and so the picture here drawn must have been seen by the King himself when he came to Bath three years later, on the 15th September, 1276. He stayed the 16th, and then went on to Keynsham the 17th, and then to Bristol. He was in Somerset again in 1278, but did not visit Bath. In 1285, coming now from Bristol, Edward was in * Hundred Rolls. 66 Bath for four days, the 3rd, 4th, 5th and 6th January, and then went onto Marlborough.* There seem to be no accounts existing relating to these visits. Passing on to another reign, in 1369, 43 Edward III., there was a prospect of a war with France, and the king was asked to set his house in order. A petition presented to Parliament, prayed that all fortresses, cities and towns should be hastily surveyed and put in “ sauve garde ;” and that a command should be given to all Mayors and Bailiffs to have their walls, ditches and gates duly furnished.t This was done accordingly, and a letter was ordered, 4th June, to be sent to the Mayor of Bath concerning enclosing the city.t Then came the letter or patent on 8th July, directed to Nicholas de Berkeleye, chiv., and the Mayor and Bailiff of Bath, and Henry de Forde. That whereas the walls and towers of the city are in divers places destroyed and broken, the walls being threatened with imminent ruin ; and whereas the ditches around the walls are obstructed by trees and herbs growing in them, and are used for dungheaps and ordure (fimos et fimare), and other sordid filthy things thrown therein ; unless a quick remedy be applied, as well by us as by the said city and parts adjacent, heavy dangers and damages are likely to happen immediately or at any moment. Being willing to remove these damages and dangers, as has been requested, We assign you to survey the walls and towers and ditches aforesaid, and to repair and mend the defects existing in the same ; and to clear the said ditches from the trees and herbs growing in the same ; and to cut and clear out all sordid matter and filth. And, with power to compel and distrain ; to cause all those who have land, tenements and rents in the city or suburbs, or those who are resi- dent, or carry on business therein and gain by reason of their stay, to contribute to the said reparation and clearing,—viz., each one * Itinerary. + Rolls of Parliament, vol. ii., p. 300, t Pat. 43 Ed. IIL, pt. 1, m. 23. 67 according to his status or ability as reasonably as may be, so that none have consideration. And to you and each of you we command that you set about the work with all diligence. We give orders also to all and singular the men of the city, by tenor of these presents, that they appear and attend to assist us or our deputy in making and executing the said work, as by you or others for us on our part shall be required.* The way in which cities were taxed in early times is of interest; but unfortunately no special plan was ordered or granted by this patent, and the plan adopted is therefore unknown. Patents for murage, pavage and pontage are found for several other cities, but not one for Bath. Sometimes such aid was got by taxing all articles brought through the gates ; thus a cart paid sixpence ; skins, 1d.; skins of lamb, hare, &c., td. ; salmon, congers and eels, 4d. One city, 6 Richard II., was granted the privilege of not sending a burgess to Parliament for five years, the cost saved to go towards building the walls.+ The payment to a burgess ranged apparently from two shillings to four shillings per day ; the sheriffs getting eight shillings.t In 1377, 1 Richard II., the Commons again prayed, as a necessary preparation for war, that cities having walls should repair and make them defensible ; all who had property in them, Religious houses as well as others, and merchants for their merchandize, to be reasonably taxed, following the usual custom, “come y ad estee usee devant cest heure.” This was ordered accordingly, and a writ issued to the Mayor and Bailiff of Bath to survey and repair; but coming so soon after the more imperative order of 1369, it must have been unnecessary, except perhaps as reviving dormant energy. A patent issued in 1417 raised hopes that some good account of the city would be found. It was for repairs of walls, ditches, ER ES ER te eR Tia RTIG a TOT * Pat, 43 Ed. IIL, Pt. ii, m. 39. + Colchester, Pat. Pt. ii, m. 26. + Rolls of Parliament, 68 gutters, water courses, and stone bridges between the city of Bath and the town of Bristol, which by constant flux and reflux of the sea, and inundations and encroachments of the water, and neglect of reparation were greatly damaged and broken.* Beyond the above facts there is, however, no further special allusion to Bath. These notes clear the way for understanding the early maps. With a little imagination, a little filling-in of domestic habits and domestic events, a fairly clear image of the city is seen, including “The” bath, for the first time back to the Conquest. Whatever the condition in which the walls and the city were left after the damage of 1088, both were perfect in 1138, in the time of Stephen. After this there seems to have been a general easy neglect, until during the absence of Henry III., say after 1235, heavy damage was actually done, as declared in 1273, when the walls appeared waste and the stones the common property of any who chose to take them. So all remained yet another ninety odd years, until 1369, when the great reparation was ordered and the ditches cleared. To this date, 1369, we may feel inclined to assign the using up of the Roman stones, recorded by Leland some 250 years later, as seen by him in the walls; and, after another repairing, these would be the walls seen by ‘“‘The Most Illustrious Lord the Lord Richard ” when he was in Bath in July, 1658. Thus the medizval period passes, and we come to a time with which we are more in touch, a time more readily under- standed of all men, the time of the view or plan now to be considered. Giving this plan a glance, it is seen not to be exact, as it shows the Abbey church without the Abbey or Priory house. The grounds around the church are represented as all grass, unfor- tunately so, as Leland writing some thirty-five years earlier, records that “a great square tower with other ruins” of the once * Pat. 5 Henry V., m. 34, dors, The Kings Bath) RB The Grofs Bath Thetomon Balk. |] dhe mucll Bu th yemor Het Place. SLOANE MSS. Wo. 2596. 69 existing bishop’s palace on the south-west of the monastery were then to be seen. Had Smith marked these, supposing they were there in his time, we should know the exact site of the palace, the “bishop’s house” of King John’s time. Possibly they were removed under the Act of 1540, 32 Hen. VIII, cap. 18, for re-edifying townes, which declared that in Bath, as well as other cities named, houses had fallen down decayed and so “doo “lye as desolate and vacante groundis, many replennyshed “withe unclennes and filthe.” After proclamation made they were to be re-edified or repaired within three years; but here re-building would not be likely, and the greater improvement would be to remove altogether. On a further examination of the plan it is seen that although the bridge is shown, the gate is omitted—the great gate with a stone arch at the centre of the bridge ; recorded in 1273 as being kept as a service for certain land and a tenement. Another peculiarity must be noticed, as this Smith’s map attempts to show the suburb southward over the bridge, this being the more remarkable as not only does he so but he marks a church just at the foot of Holloway, at the corner on the left turning towards Widcombe. What does this mean? Was there ever a church here? Going first to the dissolution documents and the accounts of particulars for grants or for leases, there is found full notice relating to the “ cathedral” and the site of the Priory, and the Grange, and le Hayes, and le Ham and pasture for three hundred and twenty-two sheep called the hogflock. Then there were pastures in Walcot and Barton; and a pasture on Launce- down with all commons; and pasture for a flock of three hundred and sixty ewes called the eweflock of Barton.* Selecting Wid- combe more especially, there was the farm of the manor of Widcombe and Lyncombe with the lands and feed called Bewchen- clyff, or Beauchyncliff, or Bychincliff, or Beachynclyffe, with Prior * Particulars for Leases, Ed. VI., sec. i. 70 park and other meads and pastures.* Going still backwards, the Valor mentions Stalls with the chapel of Widcombe annexed ; and earlier still, in the Wells registers the same thing is found. In 1322, Bishop Drokensford’s register mentions the admission of the Vicar of Stalls with the chapel of Widcombe, with all the tithes of Widcombe and Lyncombe. So is it in other registers. There is no record of a church or chapel on the site here marked by Smith. Smith’s plan may be considered perhaps, not as a map plotted exactly as a survey, but rather asa view—a bird’s-eye view—“ a - portrature” as if taken from Beechen cliff. This church may then be accounted for, the intention being, not to mark exactly a site, but, after the manner of early maps, to mark that here in this suburb was another parish ; and this would then be the parish church of Widcombe. In this case too, as it happens, this was, ecclesiastically, really a part of Bath. It is not forgotten that there was the chapel for lepers, the chapel of St. Mary Magdalen in Holloway. This is found noticed in 1256 as the chapel of St. Mary “extra civitate Bathonie,” thus perhaps marking it as the otherwise unrecognised church of St. Mary extra muros, often mentioned in the local records.* But it need not be confounded with the site or suggested site of the church now considered. One note must be made, as from the above documents we get the origin of the name Beachen cliff—this being Beau Chine cliff, chine meaning one side of a gorge such as this is; and so from Beauchine we drop to Beechen or Beachen, as from Beauchamp we get to Beecham ; without any origin from the beech tree, as many suppose. The intention in these notes is not to examine minutely any differences in the early maps, as that may be better done by one more capable and with more minute local knowledge ; but there is yet one point which must be attentively considered, and here too must be quoted for once, one local author, but quoted only to * Particulars for Grants, Hen. VIII. + Pat. 40, H. iii, m. 7. 71 criticise. John Wood in his description of Bath, on page 84, vol. i. of 2nd edition, has given an engraving of what he calls :—“A “copy of Doctor Jones’s view of the city of Bath, as it was ‘* published in the year MDLXXII.” He gives it boldly as being a view taken in the reign of Queen Elizabeth to illustrate Jones’s book, “The Bathes of Bathes Ayde ;” and considering it suitable for illustrating his own text, he adds—(p. 84) “I have therefore copied it.” First, here the title to this map is Wood’s own ; with attentive reading that is clear, and so it must not be confounded or taken as being the copy of an original, as a hasty general reader may readily do. On pp. 85-86, Wood has described this map by the usual method of using capital letters ; and then he has marked by the use of other small letters or figures of his own, certain localities which, as he says, are ‘“‘neither named nor referred to by Dr. Jones.” Thus alluding to a certain house, he writes, ‘‘it stood by the fig. 5 in Dr. Jones’s view ”—adding—“‘some of the parts of which view he (Jones) thus described.” Then he refers to the capital letters as being Jones’s. Now all this is false. Dr. Jones’s book does not name or refer to the city, nor does he by means of letters or figures refer to any ° spot or locality in it. There are no such letters in the book, nor is there any description of or allusion to any such subject as a map. The treatise is entirely on the baths, as the heading of the four chapters or books given in the dedication clearly show. The first book treats of the descent of Bladud, and of the sicknesses the baths help ; the second book shows the divers opinions concerning the cause of the waters ; the third expresses things natural and non-natural, and the signs of the sick for the better consultation whether the baths will help them or not; and the fourth book declareth aphorisms and rules how the baths shall be used. Again in vol. ii., p. 305, Wood says when speaking of Bellot’s hospital, “it was built on the ground marked “k” in Jones’s view,” thus conveying two entirely erroneous impressions ; first, that the “k” on the map is Dr. Jones’s own letter, and also that Bellot’s hospital 72 must have been founded before 1572, the date given for the map, whereas Bellot’s hospital was not founded until 1609. Again, writing here in vol. ii. he has forgotten that in vol. i., p. 86, in the description there, whilst “i” marks the site of Counter’s tower, and “1” the site of St. Catherine’s hospital, the “k,” which should come between these letters and mark Bellot’s hospital, is omitted from the letterpress, although it appears on the engraved map. An excellent example this of how a thing may be conspicuous by its absence, as had the ““k” been in its place it must at once have attracted attention; Bellot’s hospital, as already noticed, not being in existence. This little fact seems to show that Wood knew what he was doing; that this omission was deliberately made. Comparing now this Jones’s map with two other early ones, Speed’s and Johnson’s, any little differences will be seen. Speed’s—entitled, ‘‘ The plott of the famous and most wholsom waters and citie of the Bathe,” was published in a corner of the map of Somerset as issued in his volume, entitled, ‘“‘ The kingdom of England described.” Some of his maps are dated 1605, some 1608, some 1610, others are undated. Somerset is undated, but usually the year 1610 is assigned for it ; yet when the date is used it should be stated as being only approximate, or else the figures should be put in brackets to convey that correct impression. To print such date on the map and so imply no doubt, is to falsify it, and convey an impression which may be erroneous. Johnson’s was published in 1634 in his Therme Bathonicz,—an extremely rare little book which treats not only of the baths, but, De urbe et Thermis,—and is the first map published in book form, Wood inlettering his Joneshas shifted two or three letters slightly at the beginning, but it may be noted that the letter “x” marks the site of the Leper’s bath, and ‘‘y” the Hot bath, whilst in Speed these letters are reversed, “y” marking the Leper’s bath and “x” the Hot bath. Johnson follows Speed exactly except in these two letters, and just as Wood’s Jones differs here in these two letters from Speed, so does he differ, to correspond with Johnson. Further, 73 Speed shows the ferry outside the North gate complete, the uprights being seen on either shore, with the ferry on the river. Johnson shows only the uprights on the shore, without the ferry, and so does Wood’s Jones. Here again Johnson differs slightly from Speed, the difference exactly occurring in Wood’s Jones. Another peculiarity is that in the Timber green near Gascoigne’s tower ; the timber lying about as shown in Speed’s, has not been moved in Johnson, the seven logs shown in the one are still seven logs in the other, lying too in exactly the same positions. As Johnson is exactly like Speed, so again is Wood’s Jones exactly like Johnson. Speed, too, marks some trees such as by Monk’s mill, with two small houses; Johnson marks the houses, but not the trees. Here again, as Johnson differs from Speed, so does Wood’s Jones agree with Johnson. This so called Jones’s map has been misnamed and misdated ; it is simply Johnson’s of 1634. ‘There is not, and there never was a Jones’s map of Bath. Besides a personal knowledge of several copies of Jones’s book—a scarce work notwithstanding—the above argument is founded on or taken from Wood’s 2nd edition, this being the one usually quoted or referred to, the complete edition in four parts. The earlier edition or Part i, issued in 1742, it not often seen, and as being only a part would not be bought or sought by a general reader. For this reason it has been overlooked that the 2nd edition is the first in which the so called Jones’s map appears, for, on referring to the 1st edition of 1742, Parti, p. 83, the map there given, is given honestly as Johnson’s. The paragraph describing it actually begins :—‘‘In “the year 1634, Dr. Thos. Johnson wrote a description of Bath and “therein inserted a draught of the same, a copy of which I have “caused to be engraven.” The map is then given as in Johnson without any heading or name. It is the same map as given in the 2nd edition, but there called Jones’s. The small letters on it mark the same spots, not only without any reference to Jones or 74 his pretended omissions, but actually with direct allusion to Dr. Johnson. The letter “‘k” noticed for its absence from the letter- press in the 2nd edition in the description of the so called Jones’s, duly and properly appears here in its place in the letterpress as well as on the map, and marking Bellot’s hospital ; fair evidence that it was purposely omitted in the 2nd edition. That the two maps are the same may be seen from the fact that both have two “ w’s”; one near the Guildhall having no reference, the other marking the Cross bath. The difference in them is that Wood has added small figures in the 2nd edition in extending his references, and also the line on the margin naming it Jones's, for which, as can be seen by the pressure indent, the plate just allowed sufficient space. Wood gives no reason for this alteration, attempts no explana- tion whatever. Thus he leaves the conclusion open that he was not misled, but that he supposed the change would not be noticed. Further, it must be clear, that he either never saw Jones’s book, or that if he did so, he has wilfully practised a fraud. Smith’s view now brought to notice, for it is rather a view, a “portrature,” than a map, is, clearly, independently made. The walls are shown more bastioned than in the other maps, and the timber green, although green, is without timber. Whether it were “measured and laid in platform” like Bristol and at the same time as Bristol, viz., 1568, cannot be stated. No exact date can be given for it. If not done in 1568, it may be taken as not done after 1588. Asit is the earliest known thing of the kind, there seems no great reason why the Bristol date of 1568 should not be given to it, as no change took place in the form of the city during the twenty years named. If it cannot be accepted as quite exact, yet better than any other map since, it conveys a very exact idea hardly realized by us to-day, of what must have been the original appearance of this very ancient and pretty, but yet very little, city of The Bath. “a (te ee 75 On Recent discoveries made in Uncovering the Roman Baths at Bath. By the Rev. Preb. ScARTH, M.A. (Communicated 13th January, 1886.) In the proceedings of the Bath Field Club, Vol. iv., no. 4, p. 357, will be found an account of the excavations made at the baths, by Major Davis, who gave some very interesting details to the Club. This was in 1881, and as further important discoveries have been made since that date, it is well that an account of them should find a place in the records of the Field Club. The Roman sewer had then been fully examined and utilized for conveying away the waste water from the thermal spring, and this led to the discovery of the Roman tank for receiving the hot springs, as described by Major Davis ; but since then the large Rectangular Bath has been exposed to view, together with the Ambulatory (or Scholz) which surrounds it, and the three recesses on the north and south sides of the Ambulatory. The whole seems to have formed a vast Hall for bathing,—111ft. 4in. long by 68ft. Gin. wide, and about 6ft. 8in. deep. The bottom of the bath, like that of the tank or reservoir which received the hot springs, is covered with sheet lead, and is 73ft. 2in. by 29ft. Gin. The sheets of lead covering it are about 10ft. by 5ft., and are supposed to have been laid rather to keep the hot water which rises through the earth from entering the bath, than to make the bath water-tight. Six steps lead down into the bath, but do not appear to have been covered with lead. At the bottom step in in the N.E. corner, was a bronze sluice, with an opening 13in. by 12in., which may now be seen in the Pump Room; an overflow was provided also. The extreme surface of the water, according to Major Davis’s measurement, was 83ft. 8in. by 40ft. 2in., and formed a parallelo- gram, except that the N.W. angle was cut off by the steps being carried obliquely in three tiers for a length of 7ft. Some of the 76 stones of the bath are 10ft. long,—square sockets appear cut in some of the steps, as if to support a baluster to a handrail.* At present the offices of the Poor Law Board stand above rather more than one-third of this bath ; but it is hoped that before long this building may be purchased, and the offices removed elsewhere, so as to allow the whole area to be laid open. Six piers of wrought stone stand on each side of the bath, the width of the platform surrounding the bath is 14ft. This has been arched, as the remains of the roofing have been found in large fragments, composed of hollow tiles, wedge shaped. It is probable that the whole was orginally covered—the roof of the central bath being higher than that of the platform surrounding it. The present piers remain only to the height of 6 or 7ft., and appear to have been strengthened by additions. Fragments of the capitals of the pilastres have been found from which the arches took their spring, and some portious of a frieze, also the figure of a lion, which seems to have served as an antefix. Since the large bath above described was exposed to view, further discoveries have been made at the western end, near to the large tank or reservoir below the King’s Bath. These consist of a Hall, 55ft. long by 36ft. wide, in the centre of which is a circular bath with steps leading into it ; the depth is the same as the great bath. To the south of this are vaulted chambers, as may be seen in the plan given in the guide to the Roman Baths, drawn by Major Davis, to whom very much is due for the spirit and energy he has shewn in elucidating these remains. The steps which surround the circular bath and form seats, are quite perfect, and the bath is now filled with water. To the south of this a drain has been found by which the over- flow from the baths was carried off. This circular bath has been connected with the large Roman reservoir, which also supplied * See Paper by Major Davis in Trans. of Bristol and Gloucester Arch, Soe., vol. viii., pt. i, p. 89 and following. 17 the large Rectangular Bath. The short columns supporting the roof of the Ambulatory which surrounded this circular bath, are found perfect in one or two instances ; but the arched roof that ‘must have rested on them has been removed. This circular bath occupies the western end of the large Rectan- gular Swimming Bath, as the Rectangular Bath, found in the last century, formed the eastern end. The workmanship of the circular bath does not seem so massive or well put together as that of the large bath. They may perhaps eventually be found to be of different dates, though both are undoubtedly Roman, and form portions of a grand arrangement for bathing. A circular bath is not common in Roman bathing establish- ments, but semi-circular baths are very common ; and circular chambers of very large proportions were attached to baths as Sudatories and halls. This may be seen at Rome in the Pantheon, which was a circular hall, with chambers attached, for the purposes of the Sudatorium, or Vapour Bath ; also the same may be seen at the baths of Dioclesian, where one or more have been turned to the purpose of a Circular Church. Contiguous to the Circular Bath, and beyond the Ambulatory surrounding it, a chamber has been opened, which seems to have been used for heating purposes. The remains of a Hypocaust have also been found. It is probable that this Circular Bath (as well as the Rectangular one) was supplied with cold water from a spring, not mineral, but which could be used for ordinary washing or other purposes. Much, however, remains yet to be discovered, and more must be laid open before the exact purposes and arrangement of these baths can be accurately ascertained. The lead coating of the Circular Bath, which probably also covered the steps or seats that surround it, had been removed in past times. Major Davis, in his paper recently read to the Bath Literary and Philosophical Society, supposes that the entire establishment of 78 the Roman Baths was contained in a parallelogram of 440ft., or 460ft. from east to west, with a width of from 140ft. to 160ft. from north to south, and the total area would then be nearly 6,500 sq. ft.; but this would not include the outer Courts or Gardens, and the whole probably covered two acres. It has also been stated that the area marked by the Medizval Walls—helieved to stand on the foundation of the ancient Roman—is too small for a Roman town, and comprehended the baths only ; but as their circuit is nearly a mile in extent, there was ample space not only for the forum, baths, and other edifices, but for a population of considerable extent, knowing how closely they were packed in ancient times. The area allowed for the baths seems to be a fair allowance of space, though considerably less than was assigned to their area in a paper read last year to the Literary and Philosophical Society, which supposed the area of the Roman Baths to have extended over the whole space of the enclosure within the walls, from E. to W. The Roman Baths only occupied the southern front of the forum which is now represented by the Abbey Church Yard; but the space occupied by the ancient forum is much encroached upon by modern buildings. If the medizeval walls followed the line of the Roman, they enclosed an area of 224 acres; and if the Roman Baths extended over 2} acres, their remain 20 acres for the forum, streets, temples and other buildings of the ancient town. We cannot but hope that the investigation of these baths will be continued, and that their remains may be carefully preserved, The coins and vessels hitherto found have been few, considering the extent of the area now laid open; but such discoveries are always uncertain, as the baths were probably in use for a limited time after the Roman domination had ceased, and were well ransacked for articles in later times, before they became permanent ruins. The inscribed Metal Plate, of much interest, found in the he 79 bath, is not yet admitted to be satisfactorily explained. If access to this plate could be allowed to certain competent scholars, something more might be known as to the correctness of the reading. Upon some Sculpture recently discovered at the Cross Bath. By Ruv. H. H. WInwoop. (Read January 13th, 1886.) In the Bath Herald, of September 12th, 1885, was a letter upon “ Preshr discoveries at the Baths,” describing the recent “ find” of a stone with carving on three sides. “At a depth (the writer says) “ of very nearly 20ft. in the excavations at the Cross Bath, was dug “up on Tuesday, 8th inst., a stone, 30in. high by about 17in. wide “and 10in. in thickness,with carving on three sides. The carving on “the first side is little more than incisive work, the second side is “sculptured in high relief, the third side is fractured—showing it was “ attached to other masonry, and the back is a carving in low relief, «‘ having no connection as to scale with the principal work. The “incisive carving (No. 1)is a tree with spreading roots and branches, “the trunk being entwined by aserpent. Two figures occupy the “front of the stone ; they are headless and almost armless. The _ “figure of a man partially covered below the waist by some drapery “is on the right reclining on a bank beneath atree. The figure on “the left is that of a woman (nude), and is erect reaching something “from the tree, but the other arm has perished. Between the « fioures is a vase or wallet. On the back of the stone is a large “ dog (?) somewhat like the Danish boar hound, except that it has “a tail like a collie turned up over its back (some architectural “foliage and that may be another tail), the Sculpture (and now “ comes the startling theory), I believe to represent the temptation “and fallof Adam. It is possible that it may be Hercules and the « Hesperides ; but the male figure is by no means Herculean, The 80 “discovery is the first found in Bath that may be said to be of “Christian or rather Biblical character, and certainly the only “important one of similar character found in Britain.” So far for the letter with its ingenious conclusion. This brought forth one or two other letters from another antiquary, written from a distance, in which an equally hasty suggestion was made that the stone described was probably the portion (lower shaft) of a Saxon cross of which two other portions were in the Museum of the Institution. Having inspected the carved stone myself several times and looked at the pieces of Sculpture in the Museum, I could not possibly reconcile either of the above statements with the actual facts of the case. Not deeming myself sufficiently competent to controvert the views set forth by two such authorities, a lucky chance presented itself, or rather a Deus ex Machina appeared in the person of Professor Sayce, who accompanied me to the Roman Bath where this interesting stone is fast being injured (if not destroyed) by exposure to the action of the weather, stated his impressions as to the Sculpture at the time and has since written to me on the subject.* The following communication clears up the whole matter and brings conviction to every reasonable mind :— “‘Thave not had time before to write down for you my notions about the curious altar-like stone found last summer in the Cross Bath, which we examined together a few weeks ago. I believe it must have come from a chapel dedicated to Aisculapius, a deity very likely to be worshipped in the neighbourhood of the hot springs. The serpent entwined around a staff, which is engraved on one of the faces of the stone, is his well-known symbol. The dog repre- sented on another face was also associated with Aisculapius. * It is but fair to add that on January 8th a note from the writer of the first letter states that “he has altogether changed his views as to this Sculpture.” : 81 According to Festus, dogs were employed in the temples of that god because he had been “suckled” by one of them, and the monuments of Epidauros, and of the Asklépion at Athens, as well as the coins of the Magnetes show us the dog in combination with the serpent. Inscriptions recently discovered at Epidauros prove that dogs acted there as the ministers of Asklépios. The piece of Sculpture on the third face of the stone seems to me to represent Apollo and Kéronis the mother of Asklépios. It may be compared with a bas-relief, once built into the walls of Bath, and figured by Guidott who makes out that it depicts a shepherd and his mistress! On the newly found stone the male figure seems evidently intended to represent Apollo. Can any traces of a crow be detected among the branches of the tree above the head of the reclining female figure ?” The Rev. Preb. Scarth, having examined the Sculpture and formed an independent opinion thereon before hearing Professor Sayce’s interpretation, read the following notes at the Anniversary dinner of the Club February 18th. “The statement of Solinus respecting the “Calidi Fontes” in Britain, “Opiparo exculti apparatu,” has received singular con- firmation, after an interval of 1,500 years, by the discovery of an interesting Sculpture in the form of an Altar, but not quite so massive as Roman Altars of the same dimensions usually are. “This stone has two Sculptures on opposite sides, front and back, and one on the side,—the other side seems to have been fixed into masonry. “The Sculptures are much defaced, but shew signs of early, Roman art, being executed with much spirit. The stone has a plinth which projects, and the subjects are on panels, the figures being in relief. “The whole surface of the front face is occupied by two Se the one standing and the other reclining. “The standing figure is that of a man extending the right arm, and. holding what on minute examination is found to be a lamb, % F 82 above the head of the reclining figure. The reclining figure rests on one elbow (the left) and extends the right arm, while the head is turned away, as if to reject the offering. This is a female figure ; the lower portion of the body is draped, one leg being extended the other bent, “Tn the space between these figures is a large bowl, on one side of which appears to be a serpent. “On the side of the stone, reaching from the base to the upper portion, is a tree, around which is coiled a serpent, with the head downward. “On the opposite side of the stone, in the upper portion, is a wide panel, extending over half the surface. On this is a dog with a bushy tail, in the act of walking; at the back of the dog is a tree. “Below this Sculpture in relief, the surface is quite plain, apparently without any lettering, though, unfortunately, like the rest of the stone, much injured. The top portion of the stone projects considerably over the panel. “In a letter to the Bath Herald (September 12th, 1885) this Sculpture was considered to be a representation of the fall of our first parents! but a careful study of the stone at once shews it to be connected with the Heathen Mythology. “This was discovered at once by Professor Sayce, es on examining it, made the suggestion to the Secretary of the Field Club, in a letter addressed to him, that it was a representation of Apollo and the nymph Kéronis. Before seeing his communication, or knowing the explanation he had given, I had on two examinations of the stone come to the conclusion that it must be Aésculapius (the Greek Asklepios) offering a lamb to the goddess Hegiéa. The serpent feeding out of the crater, or large cup, and the serpent entwined round the tree, are emblems of Aisculapius, and the dog also is connected with the worship of that god. Hegiéa was worshipped in the Temple of Adsculapius at Argos, where these two divinities had a sanctuary ; also at Athens and a 83 at Corinth ; also the Goddess Hegiéa is usually represented as feeding a serpent froma bowl or cup. The bowl, or large cup, upon the Sculpture may also indicate the healing waters of the Bath Thermal Spring. The dog also is not only a symbol of Aisculapius, the god of healing, but represents also the Dog Star, (xuwv) adopted by the Romans from the Greeks, and indicating the passage of the sun into the constellation Leo. The season known as the ‘Dies Caniculares.” The dog may therefore here be an emblem of the heat of the thermal springs. It is not unworthy of remark how the “serpent” enters con- tinually into the ancient Sculptures found in Bath. The drawings of the Sculptures given by Guidott in his work, formerly to be seen in the city walls, contain two representations of figures, one of which, apparently a female, carries two serpents ; this figure is nude, the other, apparently a male figure, is clothed and carries one serpent. Two heads are represented as covered with hair formed of serpents, and serpents are sculptured in the hair and beard of the head of Medusa, which formed the centre of the pediment of the temple,—the remains of which are now in the portico of the Literary and Scientific Institution. All these seem to be emblematic of the healing properties of the thermal springs, which have been for so many hundred years celebrated, and granted, as Solinus expresses it, ‘ad usus mortalium.” The chief Altars found in Bath are dedicated to the goddess Sul, or Sul-Minerva. The British goddess being associated with the Roman. But the Roman Minerva was the same as the Greek Athena, and Athena was the goddess of health as well as of the arts and sciences. According to Proclus, a late Roman writer, H A@HNA NIKH gpocayopeverar cat YIIEIA. Athena or Minerva is called victory and health, and this leads me to the conclusion that the Sculpture represents Alsculapius making an offer to Hegiea, the goddess of health, and that she is the presiding goddess of the thermal springs. 84 These remarks are only offered until some more satisfactory explanation can be found for the meaning of a Sculpture which appears to me to be of no common interest, and which should be carefully preserved among the other interesting lapidary records of Roman Bath. Notes on the occurrence of Salt Springs in the Coal Measures at Radstock. By J. McMurtrig, F.G.S. (Read 10th February, 1886 ). While engaged during the past year in carrying out a deep sinking in the Coal Measures at Radstock, the writer encountered certain Salt Springs not previously met with in the parish, and believing it to be a comparatively rare occurrence in the Carboni- ferous series, he has thought it of sufficient importance to bring it under the notice of the Bath Field Club. Had these springs been met with in working coal near or under the sea, as in the Whitchaven, Newcastle and other coal fields, their presence would not have occasioned any surprise ; but their occurrence in an inland coal field, twenty-one miles from the nearest sea board, is very remarkable, and it has given rise to much speculative inquiry as to their probable source. In order to explain the position in which these Springs were met with, it is necessary to point out the geological features of the locality in which they occur, which are probably familiar to some who have turned their attention to the subject, but may not be so to others. Although Radstock is known chiefly in connection with coal, a geological stranger visiting the place would be surprised to find that, after examining every hill and valley within the parish he had entirely failed to discover any trace of Coal Measures, except- ing those unsightly shale tips which now disfigure what was once a picturesque rural parish. The explanation of all this is that the ———— 85 Carboniferous rocks, having undergone many changes and much denudation, were in later but still very remote geological times overlaid by newer formations which now cover the entire surface of the parish, capping the higher ground with Inferior Oolite and Lias, while the lower slopes and the bottoms of the valleys are occupied by the Rheetic beds and Keuper Marls. The Middle Pit, in which the sinking operations referred to have been carried on, is situated about 100 yards on the North side of the Radstock Market Place, and is easily recognised by its tall, circular stone chimney, which visitors may have noticed on their right in driving into Radstock from Bath. The shaft, being situated in the bottom of the valley, did not meet with the Lias and Rheetic beds, but passed at once into the Keuper Marls, which are here 89 feet in thickness, and rest on a bed of Conglomerate immediately overlying the Coal Measures. These Marls, fed by the rain and streams from above, and resting on a water-tight bed beneath, yield a large quantity of water ; but it is ordinary spring water, without any special mineral ingredient. It is hardly necessary to state that it is these same Marls which, in the Midland Counties, yield almost all the Rock Salt and Brine Springs which we possess in England. Although only about 17G feet in thickness in the Radstock area, the New Red Sandstone of Cheshire attains a thickness of 1,700 feet; and it is the upper 700 feet of this formation which contains the Salt Mines and Brine Springs which, in Worcestershire and Cheshire, yield annually from 160,000 to 170,000 tons of prepared Salt. But although geologically identical, no trace of either Rock Salt or Salt Springs has ever, so far as the writer is aware, been met with in the Keuper Marls of Radstock. Immediately under the New Red Sandstone, but not at all conformable with it, lies the upper or Radstock group of the Somersetshire Coal Measures, to win which the Middle Pit was originally sunk, and which has here been worked successfully for 86 many years. The strata comprised in this series yield very little water, the Conglomerate at the base of the New Red Sandstone serving as a nearly water-tight covering, through which only a very moderate quantity of water ever passes. The only feeder worth naming occurs in a thick bed of Sandstone overlying the Middle Vein ; but the water produced here and elsewhere in the series is entirely free from Salt, of which the writer has never discovered any trace. The Middle Pit was originally sunk to the lowest seam of the Radstock group, which was here met with at a depth of 875 feet, and beneath which there lay an unknown country. The sinking operations carried on under the direction of the writer began at that point on the 8th of May, 1884, and having been carried down through the second or Farrington group of the Somersetshire Coal Measures, reached a depth of 1791 feet from the surface on the 25th of January last; the ground below this point having since been proved by a boring to a total depth of 1846 feet. It is not the object of the present paper to describe the geological features met with in this exploration, nor to record in any detail the strata passed through ; but it may be noted that the thickness of barren ground, intervening between the lowest vein of the Radstock series and the first workable vein of the Farrington group, was here found to be 628 feet, and that it contained the well known beds of Red Shale which invariably lie between the two groups. It may also be stated in passing, that the result of this sinking has entirely falsified the expectations of some who had turned their attention to the subject. It had long been held in certain quarters that wherever the Farrington veins have been worked beneath the Radstock series, the former have been thin and inferior ; and that the Farrington veins are only valuable in the margin outside the outcrop of the Radstock group. The writer could never see any good ground for this contention, believing that the range and thickness of the seams composing the Farrington group could not be affected by strata by which they were not overlaid for nan nna =i == -=-=-------=--=-- RADSTOCK SERIES, ------—---~-----> € ---=-—----------------' FARRINGTON SERIES. SECTION OF MIDDLE PIT, RADSTOCK. ScALe 280FT TO AN INCH. Pre [ee] | |New Repo SANDSTONE =| CONGLOMERATE =| GREAT VEIN Top LitTLe VEIN Mippte VEIN _|Styvinc VEIN Bottom LitTLe VEIN Butt VEIN DHjOverae Faurt Styvinc VEIN, Bottom LitTLe VEIN But Vein Nine IncH VEIN Rep SHALES 177 0 ;|}0 ee SALT SPRING 225 |.3 | 0 a. 2ND SALT SPRING 230 | 5 | 0 \ | | “H3ro SALT SPRING 282 1 i) | Bottom oF Pit 298 Std. iS Bottom oF Bore Hote || 307 4} 10 | 87 long ages afterwards. He considered the contention in question especially valueless, because in all probability the entire area now occupied by the Farrington group was originally covered by the Radstock series ; and the fact of one part having been denuded while another area had escaped denudation, could not in his judgment affect the thickness of the seams lying beneath. And without expressing any sanguine opinion as to the com- mercial value of the undertaking, which a little time will probably establish, the writer can only say that the result of this sinking, carried out in the very centre of the Radstock basin, has entirely disproved the evil predictions referred to; the thickness of coal proved being fully equal to what has been met with in other parts of the district. To return however to the subject of the paper, the strata immediately under the Radstock series yielded little or no water, and what little there was appeared to be quite fresh. The Red Shales already referred to were cut at a depth of 190 feet below the 9 inch vein, and were found to be 170 feet in thickness, presenting no feature of special importance. The first indica- tion of Salt water was in a bed of Sandstone met with at a total depth of 1353 feet, and it yielded 90 gallons an hour. Ata depth however of 1385 feet from the surface, and in a bed of Grey Sandstone, 21 feet in thickness, a much more considerable spring of water was met with which was found to be highly impregnated with Salt. In approaching this bed the miners were first warned of the presence of these Springs, by the water issuing with consider- able force from the bore holes made for blasting purposes, in some instances spouting up to a height of several feet, and evidently indicating considerable pressure. On reaching the rock from which the water came, it was found to be full of joints and fissures from which the water issued on all sides in considerable quantity, amounting at first to 1,000 gallons per hour; but gradually decreasing until it did not much exceed 400, Although the water was excessively salt, as members will find who taste the 88 sample produced, an examination of the rock from which it issued shewed that it contained no trace whatever of Rock Salt. An attempt was made to stop back the water, which was found both expensive and troublesome in sinking, and for that purpose the shaft was lined for 30 feet with iron casting, technically called ‘“tubbing,” the operation being attended with some degree of success. In thus damming back the water, it was necessary to carry a small vent pipe from the casting, as high up the shaft as the water would rise, in order to carry off any pent-up gasses; and it was found that the water rose up the pipe to a height of 102 feet. The pressure under this head of water was so considerable, that the water forced its way through joints and fissures in the strata, and did not rise any higher ; but it is probable that the natural level of the water may have been much higher than was indicated by the height of the water in this pipe. Through the kindness of Mr. Coomber, principal of the Merchant Venturers’ School in Bristol, whose valuable assistance the writer is glad to have this opportunity of acknowledging, he is enabled to supply the following analysis of the water. Writing on the 5th February, Mr. Coomber states as follows :— ‘“‘T have made a qualitative analysis of your sample. “There is almost as much matter dissolved in the sample as in sea water. “Next to the Chloride of Sodium present (Sea Salt), Lime Salts occur in greatest quantity. There is a considerable quantity of Carbonate of Lime held in solution by Carbonic Acid. ‘Potassium Salts also occur in quantity, Alkaline Carhonate is present, and perhaps both Potash and Soda are present in this form. “There are also present in small quantity Iron, Alumina, Magnesia, Lithia, Sulphuric Acid and a trace of Phosphoric Acid.” 89 And Mr. Coomber has supplemented this by the following more exact analysis received to-day :— “T regret to say that I have been unable to get an exhaustive quantitative analysis of your sample of water completed in time for your paper upon it, but its qualitative examination is complete, and almost all the weighings made that have any teaching regarding the sample. ‘The principal constituent of the water is Chloride of Sodium. Other constituents present in quantity are Lime, occurring both as Calcium Chloride and as Carbonate of Lime held in solution by Carbonic Acid. “Potassium Chloride is also present in appreciable quantity as well as Silica. “Lithium and Iron occur in very small quantity, and there are also present exceedingly small traces of Magnesium and of Sulphates and Phosphates. _ “Jodides, Bromides, and Nitrates are entirely absent. . “The specific gravity of the sample is 1:02899. “The total weight of the solids dissolved (dried at 180c°), is 1292-34 grains per gallon. “The weighings that have been made are the following :— «“ Calcium Chloride ait ... 149-27 grains per gal. “Carbonate of Lime... me 11:99 i amount of Potassium, Chloride and Silica ” “Sodium Chloride, with a small broore 1252-75 re _ The writer does not possess sufficient chemical knowledge to discuss as fully as he could wish the chemical aspect of the question; and the analysis having only come to hand this morning, there has not been sufficient time to give it adequate consideration; but the following remarks may serve to direct attention to one or two points in the analysis. 90 The specific gravity may be compared as follows :— Pure Water being ... ae Me 1-000. Sea Water is ae aud is 1:027. Bath Mineral Water is... ... 10025. And Radstock Salt Springs -- 102899: Then as to Solids,—the Bath Mineral Waters contain only 144:018 grains, according to Merck and Galloway, while other writers give even less; but the Radstock Salt Springs yield, according to Mr. Coomber’s analysis, 1292°34 grains per gallon. It may be further noted that nearly all the ingredients in the Bath Mineral Waters are present in these springs, although in very different proportions. Soon after this Spring was tapped, it was found, much to the annoyance of the Engineer in chage, that certain boilers which were partly fed by the water from tl.is mine had become encrusted with Salt. A specimen of this encrustation is now produced, and the quantity of Salt it contains is very remarkable— considering that the water before reaching the boilers was diluted with about twenty times its volume of fresh water from other sources. As the sinking proceeded, another Salt Spring was met with about 302 feet below the one I have already described, and at a total depth of 1,693 feet from the surface. In this instance also the Spring indicated very great pressure from beneath, for not only did the water rise some height out of the bore holes, but the beds of shale in the bottom of the shaft were heaved up bodily through its agency. No separate analysis of this Spring has been obtained ; but it was apparently similar in character to the one previously met with. Its yield was found to be 100 gallons per hour ; but a corresponding decrease seems to have taken place in the upper Spring, with which it may possibly be connected, as the total quantity continued as before at about 400 gallons per hour, and it has so remained down to the present time. Although new in Radstock, the occurrence of Salt Springs 91 seems to have been discovered in several previous sinkings to the same series in other parts of the district. The writer has not been able to obtain particulars of some of the earlier shafts, which were sunk many years ago; but he is indebted to the Managers of various neighbouring Collieries for the following information on the subject. At Braysdown Oolliery, where, about the year 1862, the shaft was sunk from the Radstock to the Farrington series, the Manager reports as follows :— “The water found in the sinking to the Farrington series was a little Salt before we came to the Red Shales; after passing through these it was and is at the present time intensely Salt ; it was very much like brine, from the Red Shales down to where we left off sinking. “The water is most destructive to iron and steel, destroying their properties by eating them away, exposing the grain of iron as if it was wood, and making it very hard and uncertain. It covers wood with a coat almost like sheet iron, and preserves it from decay. At the sides of the roads where it runs, it leaves a thick sediment very much the colour of blood, but perhaps a little darker. This I believe to be largely composed of iron, and it is very heavy indeed. “These Springs of water do not increase with us in any case, and if they decrease it is very little indeed, having remained much the same for the last twenty-four years.” At Foxcote Colliery, where the same ground was afterwards proved, a similar result was experienced. The then Manager informs me that “at a depth of 531 feet from the surface, and in avery hard bed of Grey Sandstone, 33 feet in thickness, he met with a Spring which yielded 700 gallons per hour. Also that 87ft. 9in. below this bed he had another Spring, which yielded 96 gallons per hour; and again, at a point 391 feet lower down, he cut a third Spring, yielding 80 gallons per hour, which so increased in going downwards that the sinking had to 92 be abandoned at a total depth of 1,212 feet from the surface. The water from all these Springs was extremely Salt. The Manager tested it on several occasions by boiling a gallon of it, and when the water was boiled away, he had a common tea cup full of Salt left on each occasion.” At the Old Mills Colliery, on the other hand, where two shafts have been sunk through exactly the same ground, although a good deal of water was met with, it was uniformly fresh ; and it remains so to this day. In this instance, however, the circumstances are somewhat different, the Secondary beds overlying the Coal Measures being very thin, and the shaft having passed direct from the New Red Sandstone into the Farrington Measures, without any of the Radstock series occurring between. It may be instructive to compare the depths at which these Brine Springs have been met with in the different localities to which I have referred, taking the sea level as the datum for comparison. Middle Pit. Foxcote. | Braysdown.| Old Mills. Depth in | Depth in | Depth in | Depth in Feet Below| Feet Below] Feet Below | Feet Below Sea Level. | Sea Level. | Sea Level. | Sea Level. To I. Spring. 1,110 176 708 242 Feet eA hee we 1,142 264 to (water pea Clear 1,450 655 1,241 fresh), As to the probable source.—The frequent occurrence of these Salt Springs in the Deeper Measures in and around Radstock, has naturally given rise to some speculation as to their probable source ; and whatever their origin may be, it seems tolerably 93 certain that they cannot derive their supply from the Keuper Marls above. In the memoirs of the Geological Survey mention is made of crystals of Rock Salt occurring in these Marls at Hallatrow, and at one or two other places, which, apart from other evidence, may be taken to indicate their identity with the same formation in Worcestershire and Cheshire, where it is so rich in Salt; but having examined the New Red Sandstone at many points in and around Radstock, the writer has never found ~ even an isolated crystal of Rock Salt ; and it may be stated with tolerable certainty that nothing in the nature of Salt Springs exists in the Keuper Marls of this neighbourhood. In proof of this it may be stated, that all the wells in the lower parts of Radstock and adjoining parishes have been sunk in these Marls, the water obtained being perfectly suitable for domestic purposes; and, as already stated, the shaft sinkings through the same ground shew a like result. It also seems clear that the source of supply cannot be in the upper or Radstock Coal Measures, which have been worked extensively for many years, without any trace of Salt Springs being met with. It also seems evident that these Springs cannot have their origin in the beds of Sandstone from which they flow, for the writer having observed them very closely has never found the slightest trace of Salt in those rocks, It also seems unlikely that these Springs can come from the Pennant rocks which lie at no great distance beneath, for it is well known that they contain no Rock Salt; and although they are commonly very heavily watered, they generally derive their supply from the rainfall near the outcrop; the water being so pure that the Bristol Water Company at one time proposed to acquire a celebrated Spring in an Iron Mine in the Pennant, at Frampton Cottrell, in order to augment the supply of Bristol. The more the facts are considered, the more difficult it seems to be to account for these Springs; the origin of which must 94 probably remain a matter of conjecture. Notwithstanding the distance from the nearest coast line, and the fact that the outcrop of the Farrington series is far inland, it is possible that the source may be the waters of the Bristol Channel, which may find their way along the lines of faults or other underground fissures to this inland district. The great difference of level, however, between these Springs at diffeaent Collieries hardly seems to favour this theory. But is it not also possible that we have in these Salt Springs, long hermetically sealed, a remnant of that ancient sea which swept away the upturned edges of the Coal Measures, before the New Red Standstone began to be deposited. In conclusion, the writer would only allude to one or two circumstances connected with these Springs, which may or may not have some bearing on their origin. Sir Charles Lyell, in his Elements of Geology, page 362, remarks that “As in various parts of the world red and mottled Clays and Sandstones, of several distinct geological epochs, are found associated with Salt, Gypsum, and Magnesian Limestone, or with one or all of these substances, there is in all likelihood a general cause for such coincidence. Nevertheless, we must not forget that there are dense masses of Red and Variegated Sandstones and Clays, thousands of feet in thickness, and of vast horizontal extent, wholly devoid of Saliferous or Gypseous matter. There are also deposits of Gypsum and of common Salt, as in the Blue Clay formation of Sicily, without any accompanying Red Sandstone or Red Clay.” Now it is a strange coincidence that the beds of Grey Sand- stone in which these Radstock Springs rise, occur near, and, for the most part, immediately under the Red and Mottled Shales which intervene between the Radstock and Farrington series; but this may be a coincidence only, and it may be questioned whether either of the theories indicated offers any adequate solution of the origin of these Springs, which will probably remain a matter of doubt and uncertainty. 95 By Rev. H. H. List of Fossil Mammalia Found near Bath. Wixwoop, F.G.S. Read 10th February, 1886. from alns d other rem ia an the drift deposits in the Bath basin,” was read before our Club the Paper, on “the Mammali Since by the late Charles Moore in 1869, some fresh sections have been 1 additions made to the list I have, therefore, thought it might be ,» and severa opened in the gravel beds of extinct animals. tabulated iscoveries in a useful to record the result of those d form for the sake of easy reference. *M01999[[09 S'M “H ‘H ‘uinasny, Weg ‘mIneSsN]L ywweq sow *[[098,"M"H’H ‘TUnesny, We ‘munesny WIV “we YS OW ‘TI8H UAL, "001909 100 8M ‘HH ‘mnesny Weg *201499[[09 8’ “H “H ‘unesny Weg ‘wnesny Weg *U01402T 709 8M “H "HE ‘wanesnyy yaeq 10g TUnesny, WIV “CHLIsodaa quagHM *J9911G 9789489 ‘1e[[90 OJ sumo1yBAvd “x9 "ployysory *|[eyyre'yT ‘uussnd ga ‘xog “ITH SIPPIAT ‘ornssy 9191[0O *ployysoay spoq joavry "xog ‘TH SIPPIIA “Seanssy 9141/00 *paoyyseig speq [eavsy _ S68 “WBysy OI Ieou ‘UOAW JOATI ou SUIYsy Ul pe]suvjue peo *paxoyqse. iy *prlojyysor iy ‘spoq [aav14y ‘od pig “Wey “TeyywyT “3014 -qnd ploygeroyy ‘pxrozyysor iy “TG Ae T ‘espliquie’y ‘yIeq qyeg "a0j10m 7,42 M [1837 qyosioq pues yasiau0g *SU14jNO pleyaroyy "pros “JIBS “90'T “JG WOFMON ‘Adojomen §=sqmMooplAy 2 oquiooud'T *pxrozyso. iy ‘TeGALeT spoq [aavsy “CNOO4 WHGHM *souImBy ‘som0q pur q}90} Le;OpT som0g 29 prox *eu0q dary O[BULT 29 OB UL —spvoy oM, "029 ‘44093 IB[Oul'e.1g9}19 A. "4390 xe[OW *sd@[OUL pue viqry‘sysny, “SHIOUdS *1'8OQ DIEM ‘snuaf nfouos sng *(SI[ISSOJ) ‘snyjnqny snnbq "snvndoungy Uosig "SniuabiWitdd SOT *199pUlIY ‘SNPUDADZ Snarsag ‘deeyqg ysuyl ‘snqnyosopy snquaoQ *so1200U 1qy pousoy omy ‘poarey Buoy ‘snu. -1.40Y 91] SOLBIOULY QT | snnbyup snydayq YROWUMD TT 10 snr UAB Uletd sNY MAT aNV SONaS eo 96 Summary of Proceedings for the Year 1885-86. Mr. PRESIDENT AND GENTLEMEN, In reviewing the events of the past year, the first fact to record is the absence again from the Anniversary programme of the evening’s social gathering. The Committee appointed to carry this out were unable to do so by difficulties which they found to be insurmountable ; with the exception of this incident, a subject of regret to many, the Proceedings of the year may be considered fairly successful. The Papers read at the afternoon meetings sustained their usual character, and the attendance was more encouraging ; though there is still room for improvement in this respect, as barely one-fourth of the whole number of members were present. Natural History has been well repre- sented, and it can not be deemed invidious to others if especial allusion be made to the admirable paper on the ‘‘ Bournemouth Firs” by our venerable President. The vigour of his mind and the lucidity of his pen seem not in the least abated ; and may he be long spared to us to enrich our ‘‘ Proceedings ” with the results of his keen observation, accuracy of statement and eloquent simplicity of language ! AFTERNOON MEETINGS. The afternoon of March 18th was given up to Mr. Broome who continued his account of the Fungi of Bath and its neighbourhood, and contributed another of those valuable papers on Mycology, the study of which has been his life-long pursuit, and has acquired for him well earned reputation (vide page 1). This was followed by a short description of an abnormal flower of Penstemon sent to him for examination by a member of the Club (vide page 35). Canon Ellacombe’s remarks on “ Study of Varieties with reference to Field Club work” was postponed till the Quarterly Meeting on 7th April, when Excusing himself for having but little to lay before them, and that 97 little not being new, he said, that clubs like the one he was addressing ought to be a clubof observers, and as their president had oftenimpressed upon them the duty of observing, he would venture to bring before them some examples of matters which required their observation. They need not go out of their way to do this, but everything they met with in their regular walks or excursions that was a deflection from a given type, anything abormal or eccentric ought to be at once catalogued ; by so doing local clubs would do much good. There were three or four objects he would specially call their attention to as worthy of this observation. First, Architecture ; It had long been laid down that an accurate date could be fixed for Norman, Early English, Decorated, and the Perpendicular styles ; but the conclusion he had at length arrived at was that though these dates were most valuable, yet they must be received with great modification. It was often thought that architects worked by a certain fixed law in Medieval times and never departed from this law and standard, but he thought architects then were much like architects now, and they went in for imitations of a past period. Then as now in their church restorations they were as reckless as the destroyers of our own day ; in fact, they had not any hard and fast rule. Though it was difficult to prove the cases in which architects previous to date had anticipated the style peculiar to that date, yet in some instances it could easily be traced, eg., Norman architects by the intersection of two round arches built pointed arches as much as those of a subsequent period. To come to latter instances ; why in Decorated architecture should there never he a vertical line as some suppose? Look at Gloucester Cathedral, there Perpendicular work was found at least 100 years before the accepted date of that style. Fan tracery, so distinguishing an English feature, was con- sidered not to have come in till temp. Henry VII., exceptin Gloucester Cathedral, where we find it in work of the 14th century (1360). Then again we have architects directly imitating work of an earlier period ; take for instance the so-called Norman work at Bradenstoke Priory, and the Norman work introduced into the Perpendicular wall at Kilmersdon. To come nearer home take the case of Bitton (his own church), originally an Ante-Norman building, where the Bishop Buttons of the 14th century literally smashed up the old Norman work, the 15th century architects destroyed the old chancel and west front, and G 98 those of a later period put a Norman corbel table into a Perpendicular wall. The churches at Dauntsey and Iron Acton contain likewise copies of older work, and this is very conspicuous in the buildings of Oxford. Hence the conclusion he wished to impress upon the members was that the date of a building could not be always determined by the style of its architecture. He ventured to think that the interest in the Somerset and Devonshire churches was much lessened by this fact of many of them being simply an imitation and reproduction of each other. Then there was another point worthy of observation, the stone which was found in the old buildings ; beneath the variety in the stone often lurked a great history, e.g., in one church granite was found mixed up with the stones peculiar to the neighbourhood. This led to the discovery that the original founder had property in Cornwall, whence, doubtless, this foreign material was derived, The mention of this led him on to the second subject, z.e. (2) Geology. Here every variety in the strata should be noted. Were the strata always uniform, one bed following another in regular succession, how little should we know about the study ; but the variation in their succession caused by the disturbances and topsy-turvy movements of some of the beds added go very much to the interest of the study ; the greater the variations the greater the interest, eg., the disturbances in our own Mendips, as at Vobster. Though not professing to be a geologist himself, yet when in the north of Ireland, between Port Rush and the Giant’s Causeway, he could not fail to be struck with the varieties in the colour of the rocks—white rocks stained by red streaks and capped by black. Then there were the varied movements of a river ; take, for instance, the Avon, which ought naturally to flow in a straight line, but witness itsmany windings, study the causes of these windings, follow the turns ; consider why the water retires here and encroaches there, and you will have a good key to the geology of the district between Bath and Bristol. Then again the gorge of the Avon, which drained off the ancient lake which must have existed there once; viewed from the Hogsback it looked a mere crack in the rocks, yet consider how this came about, and the vast alteration in the surrounding country were this gorge to be dammed up, as it might easily be by some Brunell of the period. Finally, the third subject he wished to notice was his favourite one (3) Botany. Of this 99 he certainly knew more than Geology. How full was the study of all sorts of deviations from the accepted forms of classification, both in the flowers, the leaves, and the roots, called “vegetable monstrosities,” until Darwin taught us that all these variations were but the gradual workings of nature pointing back to old forms once existent, or forward to some evolution about to come. Note every variety, whether of leaf or flower, accumulate facts, they will all fall into their right place at some time or other. This was the one of the chief lessons that great observer taught us, Carnivorous plants notice especially ; they not only killed but digested the insects. This food was necessary for their existence. The utricularia, with its fibrous roots and the little bladders at the end has recently been discovered to be a feeder on fish, these appendages being used for that purpose. Notice, too, all those plants that are visited by insects and find out the reason of these visits, The colours of plants should be observed; the two opinions about them are that they were originally (1) all green, (2) all yellow. Green, he thought, was the more ordinary colour, and that most of them arose from green originals ; the richer colours (the golden autumnal tints) arising from decay and death. All yellow flowers were entomophilous—fertilised by insects—all green, anemophilous—or fertilised by wind—according to Sir Joseph Hooker. The observations of Col. Jones of a few white spots on lady- ferns led to an important result as to fertilisation. In conclusion, he would impress upon local clubs the necessity also of noting the variation in language, local phrases, peculiarities and expressions, which were fast passing away. Mr. Browne agreed with Canon Ellacombe as to his remarks respecting the imitations in some of the churches mentioned, but the subject was too great a one to deal with on the spur of the moment. After some remarks from Mr. Broome, the warm thanks of those present were given to Mr. Ellacombe for his admirable address and hope expressed that they might see it in a more permanent form for their future instruction. The SECRETARY (Rev. H. H. Winwood) exhibited some fossils, which he found during a visit last autumn (1884), to the Rocky Mountains. Having briefly pointed out, on the maps recently 100 published by the Geological Survey of Canada, the geology of those regions, he said— The Canadian Pacific Railway, which would shortly connect the Atlantic Ocean on the east with the Pacific on the west, had lately opened out a tract of country in the heart of the Rockies hitherto but little known ; and it was his good fortune to accompany Professor Selwyn, Dr. Dawson, Professor Boyd Dawkins and other geologists in a geological ramble down the Kicking Horse Pass in search of some fossil evidence, which would help to determine the age of the beds. The Secondary and Tertiary strata, so horizontal in the Prairie country to the east, became much disturbed and folded at the “foot hills” of the Rockies, until on approaching the head of the Kicking Horse Pass, some 5,000 feet high, the older beds—which here come in and are sup- posed to be of Devonian age—became tilted up in some places quite vertical, if not reversed altogether. These beds, consisting of Quartzites and calcareous rocks, were diligently searched for fossils in vain ; but just after crossing the high trestle bridge over the Kicking Horse River, on the left of the track a micaceous slab of rock with apparently an easterly dip had been exposed, and certain markings thereon like worm tracks attracted his attention ; on examining these he found also the trace of something evidently organic, which after some time and trouble was chiselled out. The exact nature of the fossil he was unaware of at the time, but a short distance further west on the same side of the track he found a band of calcareous rock six inches thick, crammed full of portions of ¢rilobites. On returning home he shewed them to Dr. Hicks, well versed in the Archzan rocks of England, and was informed by him that the first specimen contained the tail of a Paradoxides upon it, and that the calcareous fossiliferous band was full of portions of the same genus, and of Conocoryphe and other allied forms, thus shewing that these rocks contained a Primordial fauna, and that they belonged to what Dr. Hicks calls the Menevian zone, so ably worked out by himself in Wales. He further stated that in his opinion these beds were not far distant from an Archean axis. This was a fortunate discovery, as it will enable future explorers to take these beds as a datum line, and it is expected that Dr. Dawson, who was then about to survey that portion of the track, will have by this time been enabled to define the position of the other beds both eastward and westward. Specimens of the fossils were exhibited. LLMs Oe eee 101 The first of the winter meetings took place on Wednesday afternoon, December 9th, when the President (the Rev. L. Blomefield) read a paper on the Bournemouth firs (vide page 40). Before beginning his subject he exhibited a nest of the water- ouzel presented to the institution by Mr. Bankart. This “dipper,” he said, allied to the thrush and the blackbird, is essentially a waterbird, whilst the latter are land birds. It may be seen by the sides of rapid streams, and diving into the water like a moor- hen. It endeavours to keep at the bottom of the water as much as possible in search of its food, consisting of water beetles and fresh water shells. Its nest is built in the rocky inequalities by the banks of streams, and is composed of a tangled mass of brown rootlets. The specimen in question was from the Yorkshire moors. The bird is a native of Somerset, and especially frequents the rocky streams on its borders near Devon. The President took the opportunity of expressing a wish that some one connected with the county would present a local specimen to the museum in Bath. The Rey. Canon ELLACoMBE, who had taken the chair, ex- pressed the pleasure it gave the Club, and especially himself, at hearing another of the President’s papers, so full of interest and originality. Though a labour of love to him yet they all felt that he must have taken no ordinary trouble in preparing it, and he was glad to see so large an audience on the occasion. He had never doubted that the Scotch fir was indigenous. The Pinus pinaster too, associated with the former at Bournemouth, had been admitted into the English flora. Mentioned in old writers as the pine apple tree, it had now lost this name when the present fruit was discovered in America. Owing to the rapid onward march of the Scotch fir it is a wonder that it has not spread even further. Kingsley alludes to the way which the pollen of this tree propagates itself in his charming essay “ My Winter Garden.” The growth of the Scotch fir on our neigh- bouring hills was alluded to by many of the members present, 102 and the President said the tracing of its former existence in the neighbourhood might well be one of the objects of the Club’s weekly walks. Mr. NorMAN then gave some notes on the Algz of thermal waters, with especial reference to those of Bath (vide page 53). In the discussion which followed, the PRESIDENT congratulated the writer on his researches into the natural history of our hot springs, and urged him to continue his observations therein, so that their natural history, both animal and vegetable, might in course of time be well known. Some remarks on the temperature of the water followed, and a wish was expressed that the scien- tific observations which it was believed were being systematically carried on should be made public, so that those locally interested in the question might be able to obtain some trustworthy data as to the variation, if any, in their volume and temperature. The third meeting took place on Wednesday, January 13th, Mr Skrine in the chair, when Mr. GREEN read a paper on “ The Earliest Map of Bath ”(vide page 58); another of those valuable historical leaflets with which Mr. Green has favoured the club from time to time. The orginal, he said, was to be found in the British Museum. No exact date could be given for it, but it was made about 1568 by one Wm. Smith, a herald and antiquary, who in his account calls Bath “A little cittie, yet one of ye most anncientest in England.”