IMAGE EVALUATION TEST TARGET (MT-3) 1.0 !.l 11.25 Ifl^ HIM '" i^ III 2 2 ;ij u" 0° III 2.0 M IIIIII.6 V] <^ /; "c-l c*: ^ ^ <^ '% V CIHM/ICMH Microfiche Series. CIHIVI/iCMH Collection de microfiches. Canadian Institute for Historical Microreproductions Institut Canadian de microreproductions historiques 1980 Technical and Bibliographic Notes/Notes techniques et bibliographiques The Institute has attempted to obtain the best original copy available for filming. Features of this copy which may be bibliographically unique, which may alter any of the imagM in the repi oduction. or which may significantly change the usual method of filming, are checked below. V D Coloured covers/ Couverture de couleur I I Covers damaged/ Couverture endommag^e Covers restored and/or laminated/ Couverture restaur6e et/ou pellicul6e r~| Cover title missing/ The to tl L'Institut a microfilm* le meilleur exemplaire qu'il lui a 6t6 possible de se procurer. Les details de cet exemplaire qui sont peut-Atro uniques du point de vue bibliographique, qui peuvent modifier une image reproduite, ou qui |«tiuvent exiger une modification dans la mithode normale de filmage sont indiquis ci-dessous. □ Coloured pages/ Pages de couleur □ Pages domaged/ Pages endommagies □ Pages restored and/or laminated/ Pages restaurdes et/ou peilicuides Le titre de couverture manque The post of tl film Orig begi the sion othi first sion or 11 Pages discoloured, stained or foxed/ Pages ddcoiordes, tachetdes ou piqu^es □ Coloured maps/ Cartes g^ographiques en couleur □ D D Coloured ink (i.e. other than blue or black)/ Encre de couleur (i.e. autre que bieue ou noire) □ Coloured plates and/or illustrations/ Planches et/ou illustrations en couleur □ Bound with other material/ Reli6 avec d'autres documents Tight binding may cause shadows or distortion along interior margin/ La reliure serr6e peut causer de I'ombre ou de la distortion le long de la marge intdrieure Blank leaves added during restoration may appear within the text. Whenever possible, these have been omitted from filming/ II se peut que certaines pages blanches ajout^es lors d'une restauration apparaissent dans le texte, mais, lorsque cela 6ta\t possible, ces pages n'ont pas 6t6 filmdes. □ Pages detached/ Pages ddtachdes □ Showthrough/ Transparence □ Quality of print varies/ Quality in6gale de I'impression I I Includes supplementary material/ D Comprend du materiel suppl^mentaire Only edition available/ Seuie Mition disponible The shal TIN whi Mar diff< enti beg righ reqi met Pages wholly or partially obscured by errata slips, tissues, etc., have been refilmed to ensure the best possible image/ Les pages totalement ou partiellement obscurcies par un feuillet d'errata, une pelure, etc., ont 6t6 filmdes d nouveau de fapon k obtenir la meilleure image possible. D Additional comments:/ Commentaires suppl6mentaires: This item is filmed at the reduction ratio checked below/ Ce document est film6 au taux de rMuction indiqui ci-dessous. iQX 14X 18X 22X 26X 30X J 12X 16X 20X 24X 28X 32X ills Ju difier ine age The copy filmed here hes been reproduced thanks to the generosity off: Library of the Pubiic Archives of Canada The images appearing here are the best quality possible considering the condition and legibility of the original copy and in keeping with the filming contract specifications. L'exemplaire film* fut reproduit grAce A la gAn6rosit6 de: La bibiiothdque des Archives publiques du Canada Les images sulvantes ont M reproduites avec le plus grand soin, compte tenu de la condition et de la netteti de l'exemplaire film6, et en conformity avec les conditions du contrat de filmage. Original copies in printed paper covers are ffllmed beginning with the ffront cover and ending on the last page with a printed or illustrated impres- sion, or the back cover when appropriate. All other original copies are filmed beginning on the first page with a printed or illustrated impres- sion, and ending on the last page with a printed or illustrated impression. The last recorded frame on each microfiche shall contain the symbol ^»> (meaning "CON- TINUED"), or the symbol y (meaning "END"), whichever applies. Les exemplaires originaux dont la couverture en papier est imprimie sont film6s en commen9ant par le premier plat et en terminant soit par la derniire page qui comporte une empreinte d'impression ou d'illustration, soit par le second plat, selon le cas. Tous les autres exemplaires originaux sont fllmte en commenpant par la premidre page qui comporte une empreinte d'impression ou d'illustratior et en terminant par la dernlAre page qui comporte une telle empreinte. Un des symboles suivants apparaTtra sur la derniire image de cheque microfiche, selon le cas: le symbols -^- signifie "A SUIVRE", le symbole y signifie "FIN". Maps, plates, charts, etc.. may be filmed at different reduction ratios. Those too large to be entirely included in one exposure are filmed beginning in the upper left hand corner, left to right and top to bottom, as many frames as required. The following diagrams illustrate the method: Les cartes, planches, tableaux, etc., peuvent dtre fiimds d des taux de reduction diffdrents. Lorsque le document est trop grand pour dtre reproduit en un seul clichd, il est IWrni A partir de Tangle sup6rieur gauche, de gauche i droite, et de haut en has, en prenant le nombre d'images nicessaire. Les diagrammes suivants illustrent la mithode. rata > elure. 3 32X 1 2 3 1 2 3 4 9 6 ^T" '/' THl '\k , f m'f'mm •'<.' mmm ^ •-.; .-> F /^ 4t>99^ THE FORESTS OF CANADA AND THEIR DISTRIBUTION, WITH NOTES ON THE MORE INTERESTING SPECIES. JOHN MACOUN, M.A., F.L.S. "^ t^ '\«^'^^n.l •"4 »»■■" »,5 •V4,, t ' . T» "S *.(• "■5^ '/.^•v -*^X ^f*V, ■f <-.,-t ■'-- #1!:, r <• » ^ -i y '* ..I \,w ■ \% .//If .:■■;,. •- f it- '" f -•: >:i ^ T.^ - f N. m 1 ,'. *' r — ' •.•'■}■•■ ; ^•:: A,- ,■-■'' 1 ''. ■' m '~^-. Oeoloqical Survey op Canada, George AT. Dawson, CM.G., LL.D., F.R.S.. OtPOTV HEAD AND DIRECTOR, Maa.™ AND OnpiOB, 3um,x &rR.„, Ottawa. ^^4-. /t^... /CP^^ ^ ^ ^^,^y^ /^f^^^t~zi^ ^^^-^\.^ 4%^<^,...r ,^;.^r- I i^^^ l^lC^1/l ■■■l.^ m '% n ■\ ' i. ;^.. ■T. Vi "W-^^'f '"'v^ ' >^»' iteltol- »v.,-. -£.^*^«A.*.ii,V. ' '!l Obolooical Survey of Canada, George M. Dazvson, CAf.C, LL.D., I-./i.S., DEPUTY HEAD AND DIRECTOR, Muaiou AND OmoM, Susau Strir. Ottawa. ^ /. S- ^^^--^ /y^.^^^ y /^ .^^^47 .2^^. ^ ;^;-,^ ^.^ ^,^ /^ /^'^Z' ^xr T^ ^C%-?-K,2*=^--j ^'c^a/lli? /< -7/ ^ * . (j X,*-^ /r^'-t^^n c^^ 1^^; -^1 ^F.- \t*r gg^_ ■(; * -^-3 tti..' •^i ,1 Kjii ^ H|l P Bp'*^it >,*' l&t^** « ) !^Sf '-.^ u H^n^^^v^ » »-'^ Ib^> ^'•i HEHga^ ^ U^' ■ 1 Ib(^ ^ ^ K^' - n^" ' 1 ^ '^ J %- ^ -.; > , :t ' ^ Vv .. -^ r ■fe*^' ,1.M HnkJ)!.. .. ■k ^^'^ B 7^ ': N. .'' •,' .N V I . ■-, N . ■ > -••«*'>. :.v;t,?s:"~:r"-f5r^ Skction IV., 1894. Tbans. Uoy. 800. Canada. I. — 77i»' Foi'i'sfn of (lainiilii mill Ihf'ir PlHtrUni/iini, nut/i N'otiM on tlir iiiorr /iifirrHl!itif Snri'liH. Hv .loiiN Macoiin, M. a. ; V. L. S. (Kciid.Mu) 21', IMM.) The foivrtts of the Dominion ot'Ouiindu uri* one of its oliiof nsst't« anil ntu' tliiit it sccins tlic aim of j^overniruMitu and iudividualn to anniliihite as tjuifkly as possildf, Insti-ad of atteinptH being made to conserve the»o nut^ural coverings of the land, means, liotli legitimate and illegal, have heeii taken to destroy them. In all the older provinces this has been done to such an extent that in many sections that were covered with nnhroken forest tifty years ago there is to-day scarcely a tree to he seen. The great fertility of the land in former times is spoken of as if it pertained to the forest when in reality it was due to other causes. On the sea coivst, cutting away the forests has let in the sea air, and to-day the soil of Prince Kdward Island and parts of Nova Scotia is wetter than wlu'U the timber was tirst cut off. As a proof of this, tamarack is now growing in [)astures and meadows wlurc hardwood once covered the land, and under-drainage has become an absolute necessity. On the other hand the deforesting of Ontario has dried up springs, lessened the How of rivers, caused sudden and early thaws in winter, and in summer droughts over large areas, and as a result lessened the [troilucts of the soil at least onc-haU". Year by year this state of things is becoming more intensified, yet the supineness of the authorities i.- so great that no sensible attempt is made to remedy this state of things. The forests of northern Ontario an- being cut down to supph' the increasing dennvnd for pine and other wootls, and in the wake of the cutting follows the ainiual fires which, besides burning over the districts from which the timber has been cut, extend in many instances through the untoucheil forests and destroy more timber than the woodman with his axe. Year after year this goes on, and now when a hundred miles or more intervenes between the settlements and the lumber camps, little attention is paid to tlie subject, but when the public awakes to the truth it will be appalled at the enormous waste and loss that has been going on for more than a generation. Some years since a large area was set apart in northern Ontario as a park for the pre- servation of game and of the mitural forest, but more especially as a covering to the soil at the sources of a number of streams falling into the Trent and Ottawa rivers. The pub- lic was not informed of one important fact, however, which was that the lumbermen had rights there that a venal government was going to uphold, and at present much of the park has been cut over, and in a few short years will be a blackened wilderness of naked rocks and dead trees. Twenty-five years ago the Algonm district, over 1,000 miles from east to west and we may say 200 miles from north to south, was a solid coniferous forest. To-day most of it ■s>«5 -';- JOHN i" ACOl'N ON !h ho complt'tcly (UmhuIimI of trooH tliat cvi'ii tlic doiul iiiiil whitoiiod trinikH of hoiuc lociiHticB liavc ri'pIiMH'd by rivurn of mud, trecn and rockH. Tlu'inoiiiituiiiH will bu diHtigurod,uii(l tmvi-lliiig in Hiring will lK>buth micvrtitin uiid r<)UH, ' Kui'b Hucci'i'dinj^ Hiinimor on Vuncoiivor IhIhiiiI tlu> Humo rli'r*t ruction got's on. A great (b'lil of tin' interior Iuvk Ikhmi biirnt'd ovor rt'|u'iitt'(lly, and owinj? to tlu' long nununor droughts and tho lack of brUMh ainongt»t tho tall trcon the inoHw and l<»g»« bcconu' dry «nineness of governments and people are resj)onsible for this state of things which will continue until the trees are nearly all dead and the destruction of our noble forests all but completed ; then when the end has como party parliamentarians will rise in their jilaces and denounce all but themselves for having permitted such senseless and culpable destruction. Sub-arctic Forest Belt. Lying south of the watershed in Labrador and south of a line drawn northwesterly from Fort Churchill to near the mouth of the .Nfackciizie River in tlie Northwest Territories is a belt of forest that is continuous except where the surface becomes a [>eat bog too wet to sup[iort trees or the depressions are deeper and become lakes. This extensive belt at the base of the Rocky Mountains extends from lat. 63 to 07 in the valley of the Macken?ne. Tt trends to the south as it goes easterly so that in the meritlian of Lake Winnipeg its limits are between ftO and r>S ; passing still eastward it gets narrower, so tluit when it reaches the Atlantic coast it is a mere fraction of wliat it was. In round numbers this immense region contains about 1,500,000 square miles, and its forest is made up of very few species of trees, the principal ones being pine, spruce, tanuirack and aspen poplar. Indeed eight species of trees may be said to constitute the whole arborescent flora of the region in question. The ' Wliat is here foretold actually happened a few days after this paper was read. # JOHN MAfOUN ON species are : — Piiins Banksiana, Lain., Picea alh.i, Link., Plrea nu/ra, Link., Lorir Americana, Miehx., Popalus treniuloides, Michx., Populus h'lhauiifera, Linn., Bdida papyri/era, Miehx., and in less abundance and of more circumscribed range Abies balsamea, Marsb. Oil tbe soutbeastern margin Thuya occideiitalis, Liini., and Dctiila lutea, Mx., are occasiomdly met witb but may be cxcIucUhI wIjcu speaking generally. Willows of many species are found tbrougbout tbe wbole region but seldom become trees. Altbougb tbe above trees occupy the area under discussion it must not be understood tbat tbey grow indiscriminately over tbe wbole surface. Tbe tamarack or larcb, as witb us in tbe east, is still inclined to occupy tbe wet ground around muskegs, but as it nears its nortbern limit it leaves tbcir vicinity and grows wbere the soil is drier and more heated in summer. Tbe black spruce in tbe east prefers tbe boggy ground, but as it approaches its northern limit it too seems to enjoy the drier ground and vieswitli tbe white spruce, in occupying tbe last oases before tbe forest ceases altogether and the continuous barren grounds commence. Wherever tbe ground is sandy or rocky, or both, tbe Banksian pine flourishes, and as it passes from east to west it loses its low and scrubby character as is tbe case along the St. Lawrence and Lake Suiterior, though it is a nuich tincr tree in tbe latter district, and becomes a handsome tree west of Lake Winnipeg. On tbe Beaver, the English, the Athabasca and the C'learwater rivers, Itetween lat. 53 ' and 58 , it attains its greatest dimensions, and is there a stately tree over 100 feet high and having a diameter from 12 to 20 inches. Tbe four trees mentioned above are tbe conifers of the nortbern forest and may be classed as forming the suh-arctic forest proper. Tbey keep tiicir tree form to their utmost limit, not dwindling to mere shrubs as tbey do on moimtain summits but forming outliers, iti the barren grounds, of fairly developed trees even at tbcir extreme limit. This being tbe case some other cuise than the absence of beat must be given to account fortius. From tbe statements of Mr. J. B. Tyrrell, who traversed tbe barren grounds last season, I am led to believe that the true reason fur this barrenness is too nnicb humidity in tbe air, and conse- quently a wet cold soil thai scarcely rises a few degrees above freezing under tlie very best conditions, and in which trees could not exist, much less grow. The poplars and birch grow under altogether diffeient conditions from tbe conifers. The aspen in the east seems to bo a poor sickly tree, very seldom having a thrifty look and preferring gravelly hillsides and borders of swamps. Its habit and aj)pearance change wonderfully as we come upon it on the Canadian Pac^ific railway after passing out of the spruce and tamarack before reaching the jirairie on our way to Winnipeg. Lying between the tamarack and siiruce, and tbe prairie is the belt of aspen which is only a few miles wide along tbe railway but which extends from the intennitional boundai'j' in lat. 49"^ all around tbe prairie regions, and may be said to constitute nearly tbe whole forest growth of the prairies outside of the river valleys. North of the prairie it penetrates the coniferous forest wherever there is good dry soil, and is the bulk of the forest in the Peace River country and on tbe plains lying along tbe Liard and the Mackenzie. It nniy be said witb truth tbat aspen forest means agricultural land wherever found, and as it is in southern Manitoba so is it on ihe Peace River plains and farther north. In tbe Riding and Porcupine Mountains and westward through the forests to Prince Albert and Edmonton, a distance of 800 miles, this species is found to be a fine tall tree. In many cases tbe bark is (pute white and the round smooth trunk, rising from fifty to one hundred feet, with a diameter ranging from six to THE FORESTS OF CANADA. 7 eighteen inches, is a remarkable object when seen in company with t'le brown barked gloomy looking wprnce. The aspen in it northwestern home keeps out of the flood jiluin of the river valleys and never apjjcars on islands or indeed on alluvium at any time. On the other hand, balsam p()l)lar makes its homo there and is seldom found anywhere else. On the Saskatchewan and all its branclu's this tree grows to a large size, but these are but pigmies compared with those on the Peace, Athabasca, Liard, Slave and Mackenzie rivers. On the islands in these rivers it grows to an immense size and it f Fnndy, the coast apecie.s are chiefly spruces and firs ; but a few hundred feet of elevation aliove the river valleys bring us into a hardwood forest composed of maple, l)eech, ash and birch, with a sprinkling of spruce and pine, except in the western parts where spruce, fir and tamarack are the prevailing trees ; in general terms this may I)e also said of Quebec, as the forests of northern New Brunswick are almost identical with those of that province. The American elm is, as usual, found most highly developed in the river valleys, birch and red maide growing with it here as elsewhere in the eastern provinces. A .study of the itonditions under which the forests of Xova Scotia grow and occujiv the ground shows that the sea air is not congenial to the native hardwood trees except tiie birch. An examimition of the trees ot the inner slope of North Mountain near Annai)olis shows that the conditions necessary for the growth cf hardwood trees are those required Kn- the full development of the apple, and it would be well for fruit growers to preserve with care the forests on the Bay of Fundy side of the beautiful Annaiiolis valley. Since the forests were cut away in the neighbourhood of Kentville, Wolfville and Grand Pre, the soil has become much wetter and in many places where formerly the soil did not require drainage it is now necessary. The cutting away of the forests and letting in of the sea air has allowed tannirack to grow where formerly beech and maple occupied the soil. The tendency in Nova Scotia and New Brunswick is for the i'orest to rc-clotlic tin- soil, but when the hardwood trees of the original forests disappear, spruce, balsam, birch antl tamarack take their place and everything shows that in that region the cutting away of the forests does not lessen the rainfall, but rather increases the deposition or brings the general air nearer to the point of saturation. The change in dinuite is causing a decline in grain- •".ising and increasing the area of drained soil devoted to fruit-growing ami stock-farming. In southern New Bnmswick, Jiiglmts cinerea, Tilia Americana and Quernis marrorarpa are found in some abundance, but they cannot be said to be common anywhere and they indicate a higher temperature as we pass from the conditions peculiar to the coast. Quebec. The forests of Quebec are still very valuable and very extensive and aitproach those of northern and central Ontario in the number and distribution of species. The conditions Sec. IV , isot. 2. fe^ MWiMi to JOHN MArOUN ON found on tlie New Brunswick border extend into Quebec and south of the St. Lawrence to ^[outreiii. The same conditiourt obtain in the vuHey of tlie St. Jolm Rivei' and up the Ottawa to itrt source. Except in the more southern districts, the elms, inapk>s anil beeches occupy restricted areas as they do further east, but the general distribution is the same and the trees of Quebec with few exceptions are the trees of the maritime provinces. The fol- lowing additional species enter (iuebec but only along the Ottawa and St. Lawrence valleys. Acer tlasycarjium, Ehrli. (Broad-fruited maple). Cratirgtu coccinea, Linn. ( [ted-frnited tliorn). Ulmui (vim, Michx. (Slippery elm). " racemom, Thomas. (Bock elm). CelluoccidenlalU, Linn. (Nettle tree). Caryaamara, Nutt (Bitternut). Cnrya albn, Nutt. (Shell-bark hickory). Carpimu CaroUniana, Walt. (R ue beech)- Q"ercus alba, Linn. (White oak). Populw mnnUifera, Ait. (Cotton-wood). Janiperua Virginiana, Linn. (Red cedar) None of the above trees are very abundant and the elms and bitternut are the only species that could le called common anywhere in (iuebec. The hickory and nettle-tree cling to the St. Lawrence and are seldom seen elsewhere in the province. The northern forests of (iuobec are a part of the sub-arctic forests and are composed of only a few species of trees. The more valuable woods of commerce are found south of tlio watershed of the luirthern tributaries of the St. Lawrence and the Ottawa, and these con- stitute the present lumber regions of the province. Still further south on both sides of the St. Lawrence and the lower Ottawa lie the fertile lands of the province that in the [last had a mixed forest of hardwood trees where the ash, mtiple, birch, beech and elm gave t'baracter to the landscajie and natural beauty to river, lake and shore. Many areas of mixed forest remain almost tmtouchcd in (iucbec, and when these forests are cleared away hundreds of smiling farms will take their place. The two most important areas are the Lake St. John district, north of Quebec, and the very valuable and large tract of country towards the sources of the Ottawa. Ontario. Owing to the position and extent of Ontario its forests are not all of the same character and while in the north and northwest the species are identical with th(.)se tbunil in (Jucbec, those in the south and southwestern peninsula are (piite distinct and may be said to be a rei)roduction of the northern Ohio and IVmisylvai.ia forests. A few words will suffice for the north and northwest. Wiiat was said of (Juebcc north and south of the St. Lawreiu-e waterslu'd is applicable here. Oidy the species of the sub-avctic forest find a congenial honu> in this region and at the head of the streams flowing southward into the Ottawa and the great lakes are to be found the remnants of the noble forests that supplied material for the deviistation of the last half century. It is truly appalling when the magnitude of the natioinil interests at stake are considered, to view the spoliation which has been carrieil on quite recklessly under the protection of permits and licenses. AVhen one is soberly told that this destruction was necessary in the interests of trade and for the developnuMit of the country, one is forced to deny the truth of such statements and to enter a protest against the fallacy concealed in them. It there bad been any just or proiiortionatc return to the tisc from such oji-'rations tlu' objections might have less force, but when it is realized that for this splendid heritage the people of Canada have directly received only a nominal return in dues and bonuses, the rcs^.onsibility for such a waste of resources, which should be guarded TUB FORESTS OF CANADA. 11 for the present ttiul future generations of Canadians, is imlood grave. It is linrdly a forcible argument to advance, that the money placed in circulation as wages to labourers employed in lumbering and the eonse([uent local stinuilatiou to trade or the enormous increase of private capital are a sufficient indirect gain. The cash paid as wages for such labour, labour which should have been used in the protection and development of these very forests, could never represent if multiplied numy hundred times, the loss which has occurred owing to its mis- direction ; and the capital represents only a fraction of the use and value of the forests which should have been guarded for the public benefit. It is not yet too late to formulate a policy which will pnjteet the sparse rcnniins of this once dense forest ami control them for the best interests of the whole country ; it is a policy which the present generation demands and the neglect of such a plain duty on the oart of our legislators will only lie an evidence of short- sighteilness, of the triumph of party over patriotism, for which they will be visited with the just reprobation of those who will have to suffer from the present ill-considered action. That part of the southwestern penins\ila of Ontario which lies west of Toronto has a flora quite distinct in nmny resi)ects from any other part of Canada. Its position between Lakes Ontario and ?]rie and along the latter lake accounts for this, and to this also is due its value as a fruit garden. The trees peculiar to this district are : Aalmina triloba, Daval, (Cucumber-tree). Linodendron Tulipifera, Linn. (Tulip-tree). Qymnocladui tjanadensi»,haxa. (Kentucky coffee-troe)i Cercit Canadensis, Linn. (Judaa-tree). Oledil'chia tricanthos, Linn. (Honey locust). Pints coronaria, Linn. (Crab apple). Oratiegus Cru^-nalli, Linn. (Uoclc-.spur thorn). " tomentoin, Linn. (Downy-leave J thorn). Amelanchier Canadensis, T. & G. (June-berry). Corniu florida, Linn. (Flowering dogwooil). Ni/ssa mulUHora, Wang. (Sour gum). Fraxinus (jvadrangulala, Michx. (Blue ash). In the above list there are 23 species which represent a flora that has its affinities in the south and gives an entirely different asjiect to the forests of the western peninsula when com- pared with those of the east. One leading feature is the almost total absence of coniferous trees and the great development of the hickories, the oaks, the button-wood, the chestnut and the tulip-tree. The shrubs and herbaceous plants change with the forests, and scores of species not found in other parts of Canada grow here in profusion. The cucumber-tree was once common around Niagara and Queenston, now it is so rare that only the older people can tell one of its existence. In June, 1892, I searched for days l)i'fore 1 found a clump fit to photograph. These were on the Niagara esiurpment near .\[erritton. I have also found it fruiting at Leamington, in Essex Co. Although the sassafras is scattered through the old forest and is quite a large tree, it is liccoming scarce around clearings, and is seldom planted. There are man}' fine specimens about two or three miles from Niagara Falls on the high road to Merritton and St. Catharines. The Kentucky coffee-tree, honey locust and Judas-tree are confined to Pelee Island and were not observed on any part of the main- land except when cultivated, yet the two former are (piite hardy at Ottawa, and two tine specimens of the first species are now growing in front of Riocau hall. Another peculiarity of the peninsula is that species which in other parts of the province are only large shrubs or very small trees are here well developed, and have become fair-sized Sassafras officinale, Nees. (Sassafras). Pialanus occidentalis, Linn. (Button-wood). Carya porcina, Nutt. (Hog-nut hickory). " tomentosa, Nutt (White-heart hickory). " micromr/ia, Nutt. (Small-fruited hiol«ory). Juglans nigra, Linn. (Black walnut). Caslanea saliva. Mill, var. Americani. GrAy. (Chestnut). Qmjcus bicolor, Willd. (Swamp white oak). " coccinea, Willd. (Scarlet oak). " paluslris, Du Roi. (Swamp oak). „ linctor'ut, Bart. (Black oak). 12 JOHN MACOUN ON trees. IiK'liulctl in tliis groiij) are four species of CraMgus and t\w J nnchcrry {A mddnchier), wliii'li ill the vicinity of Niugara-ou-tlio-Lake are very iioticcal)le. Even the wild grape, Vilis cestinalis, Inis often a stem over four inches in diameter, and Conius alternijloni, Samhucus raccmosa and ViliKnnim LeuUtgo become trees, and in fence corners make a tine slnide for cattle and sheep. Were my jMiper intended to illustrate climatic conditions or tlie many lessons to be learned from the natural distribution of the forest, I might show from the wild grape, the plum, the wild apple and tlie wild cherry tlie economic importance of tliis district as a fruit producer. Only a few years since our own people believed that peaches and certain varieties of the grape could be grown only in favoured localities, yet the forest growth if read aright would have told them that with jiroper local shelter all the tiner fruits of tem- perate elinuites were suited to the district under consideration, and not alone to this district but to the whole of Ontario along the St. Lawrence and Lake Ontario. With the exception of the peach, every other species can be profitably raised as far east as Ottawa, if proper shelter be forthcoming, for it is not a low temperature so much as unsuitable conditions that prevents the successful culture of fruits in Ontario. A lesson hard to lear;i is that shelter from nipping winds is just as necessary for vegetation as it is for the shorn lamb, and when horticulturists and others realize this to its full extent there will be fewer failures in fruit growing. Lying between the west end of Lake Superior and the Lake of the "Woods on the aouth and Hudson's Bay on the north is a tract of country that is indeed a province in itself It is a land of lakes and rivers which discharge their waters to the north, and although its trees are tliose of the sub-arctic forest, they are as a rule well developed and indicate a clinuite well suited for the growth of vegetables and the coarser grains at least, and there is no climatic reason why the greater \M\Yt of this region should not produce wheat. I wish, however, to draw attention to the forests. Mr. A. V. Low's rejiort on his exploration of a part of this region in 1886 sliows that both soil and climate are good, and that black and wliite spruce, and unpen, and balsam poplar grow to a large size and will produce in the future much merchantable timber. I am speaking more particuhirly of tlie country near Trout Lake, but the district along the upper Severn River is of the same character. A railway from Rat I'ortage by way of Lake Seul to penetrate tliis re^^ion can be built at small cost and would open it up for settlement and brhig its timber within reach. Manitoba and the Northwest Territories. The trees of the forests of this immense region are few in number and nearly all be- long to the sub-arctic forest, and as a whole have been treated under that head. Two trees which we have had with us from Nova Scotia appear in Manitoba, but they are never found in much al)nndance and seldom out of the river valleys. These are the elm and the balsam poplar. The green ash (Froxiiuts rlridls) and red ash (Fra.riniis nu'eniosus) are found in the valleys of the Red, Assinaboine and Souris rivers but do not leave their valleys. On the otlier hand the over-cup oak (Qiicrcus macrncurpa) forms thickets aiul open forests in many parts of Manitoba, becoming a line tree at times, but dies out west of the Assiniboine above Fort Ellice. The elm disajipears on the Red Deer River — not far west of Liike Winnipegoosis, and at its extreme limit is still a well-developed and large tree. The last THE FORESTS OF CANADA. 13 sugar maiilo was left at MeKiiy's Mountain near Lako Siiiicrior, and the red or swamp inajile disapjieared at Rainy Lake, but a tew hasswood inanajre to reaeh nearly as tar west us Brandon in tlio Assinihoine valley, and from tlienee westward all trees, apart from tlie species belonging to the sub-arctie forest, are of western origin, except Popalus mun'difeva (cotton-wood) and Neijundo anemiiks (ash-leaved maple). These trees extend, in the river valleys, far out towards the Rocky Afountains, but do not reach them. In the (lypress Hills west of long. 110 west, at an elevation of over 3,000 feet, the Rocky Mountain scrub pine (Piims Murrdi/'iHa) is found in ai)undance, and from this tree the hills take their name, the scrub pine of the east (Pin us Bankshom) being the cypres of the French voyageurs. In tlie valleys of the rivers fornnng the South Saskatchewan two species of poplar (Popultis miijitnlifulAa and P. Irichocdrjui) are found. Tliese are a part of the more southern forest and are not known north of Medicine Hat. Rocky Mountains and British Columbia. The trees of tlie Rocky Mountains may with few exceptions be classed with the western flora, and those that have not that origin belong to the sub-arctic forest, and have descended from the north along the mountains. The following list'includes all the trees of the Rocky Mountains, a few of them occurring only on the western slopes facing the valley of the Columbia River. Rocky Mountains. Popidtu tremulmdes, Michx. { Agpen). " bahamifera, Linn. (Balsam poplar). Picea alba, Link. (Wliite spruce). " Engelmanni, Engelni. (Engelmann's spruee). Albies xubalpina, Engelni. (Mountain balsam). PieiuioUiuga Douglam, t'arr. (Douglas fir). PinwflexiUs, .Tames, (Rocky mountain pine). " Murrayava, Balfour. (Black pine). " albkavlit, Engelm. (VVhite-barke 1 pine). Lar'tx Lyallii, Pari. (Mountain larch) Other species in the Columbia Valley and Selkirk Mountains. Popuius trichocarpa, Torr & Gr.iy. Pimu pondcrosa var. scopvloorum, Engelm. (Yellow pine) Juniperus Virgiinana, Linn. (Red cedar). Tsuga Puttoniana, Engelm. (Mountain hemlock). T/mi/a ffij^oiiica, Nutt (Western white cedar). " Merte7idana,Ca.Tr. (Western hemlock). Pinuiimniiticola,Uoug\. (Western white pine). Larix occidmlatis, Xutt. (Western larch). Additional Pacific Coast Species. Acer cireinatwn, Pursli. (Vine maple). " macrophyltum, Pursh. (Broad-Ieavdd maple). PhamnuK Piirthvina, DC. ("Barberry "|. Prunus cinargiimlK, Walp. (Western bird cherry). Pirunrivtilarin, Dougl. (Western crab apple). Cornut Nuttallii, And. (Western flowering dogwood) ArbuluK Mevzietdi, Pursh. (Madrona). Salix Scotdeiiana, Barratt. ( Western willow). Thuya excelm, Bong. (Yellow cypress). Tax-un brenfolia, Nutt. (Western yew). Pinns contnrla, Dougl. (Western scrub pine). Pimi Silchenm, Carr. (Menziea spruce). Ahiim gmndin, Lindley. (Mountain fir). " amaWiii, Forbes. (White fir). The bulk of the forest in the Rocky Mountains south of lat. 53 ' is made up of white spruce, Engelmann's siiruce, black pine, Douglas tir and balsam fir. These five species include at least 90 per cent of the forest growth, the remaining 10 per cent being made up of the other five species. Otthoac Pi mis Jie.ci Us is found only on the margins of the rivers issuing from the mountains, and the poplars in the valleys and open spaces where the original forest ha« been burnt oft". On the other hand /'//*//.s albicmdis and L«rix Lyollii form a zone 14 JOHN MACOUN ON more or U'bh pronounced at the extrenie limit of treen, nhmit 7,000 to 7,500 fwt iiltittiiJo, and in Septond)er tlie latter tree Htandn out very diHtinetly owing to the changing of its leaven from green to yellow. All the valleyH are filled with white npruce, and the mountain slopcH, where gravel or sand predominatert, are covered with pine. Ah we ascend aliove 5,000 feet, the pines are left behind and spruce anil fir with Douglan fir take their place. Descending from the Rocky mountain summit by the Kicking Horse Pass, we meet the western cedar as a mere shrub, but in the Columbia Valley it becomes a gigantic tree, often having a diameter often feet, in the valley of Beaver Creek. Ascending the slope on the west side of the valley we come at once into a belt of the western hemlock and white pine, wbich is characteristic of all the mountains from here to the Coast Range. Above these trees, but often intermixed with them, as at the Glacier hotel, Selkirk Mountains, Patton's hemlock is found capping the mountains oc forming the last groves on their sides. On the Coast Range a change takes place, and the upper slopes are clothed with this tree and the white fir {Ahies amahilis). Fine groves of this shapely tree are to be seen here, and the difference between it and the Rocky mountain species {Abies siibali>iiia) is very apparent, as the former has green cones and the latter bright purple ones. Descending the Columbia River, groves of the western larch are seen below the Upper Arrow Lake, and this fine tree is not uncommon on the lower slopes of the mountains on both the east and west sides of the Gold Rnnge. Generally speaking, all the valleys throughout both the Gold and Selkirk ranges are filled with cedar and spruce, and the mountain slopes are covered with Douglas fir and hemlock. The trees are in all cases well-developed, and from their size are suited for any purpose. This is the character of all the timber from the Columbia valley to the western slopes of the Gold Range. The valleys of the streams discharging westward from the latter range into the Eagle and Spullamacheen rivers and Shuswap Lake are also filled with fine timber of the same species. Passing westward from these mountains we come gradually into a drier region, and the country becomes open, with only scattered groves or single trees on the lower slopes and plateaus, and the yellow pine {Fiinia iHDiilerosa) so characteristic of the dry interior of British Columbia is the chief feature in the landscape. The light rainfall east of the Coast Range in British Columbia prevents the growth of a continuous forest oiitside the flood-plains of the rivers so that yellow pine and Douglas fir are scattered over the Okanagan and Kamloops country until we reach an altitude of about 3,600 feet. Above this is a belt of dense forest composed chiefly of spruce and black pine {Phuis Murrayana) with which is mixed, in places, a considerable quantity of Douglas fir. This forms a zone of from 2,000 to 3,000 feet above which the forest thins out and grassy meadows, with beautiful groves of fir, cap the mountains. The transition from the arid region of British Columbia to the humid coast district is a sudden one. As soon as the summit of the range is passed a change occurs, and descending by the valley of the Fraser, this is noted a few miles above Boston Bar where the mountain barrier closes the valley to the moisture-laden winds from the Pacific. Descending into the lower valley of the Fraser causes little change in the trees outside the flood-plains, but they at once increase in size and more than double their heiglit. It is in the lower Fraser valley that we first see the Pacific coast forest and are lost in wonder at the height of tlie Douglas fir, Menzies spruce and the western cedar. Trees of Douglas fir 300 feet high and ten or ^ TIIK FORRSTS OF CANADA. 15 hvclvc tV'ct in diiiniotcr were fninu>rly((inini()n,aiiil many fine HpociiiiciiH p>till ri'iiiaiii. A visit to Stanli'y jiark at N'aiuoiiviT will satiHty tluMiioHtHki'iiticai, aiiad-leavcd maple. The former with its large laurel-like ever- green leaves is a living proof of the mildness of the clinuite, and its red inner bark and green leaves as it is seen standing on a rocky j)oint or jutting rock along the coast relieves the stmihre aspect of the thick forests of Douglas tir. The dogwood may often be seen in company with it, its white invobu're, over three inches across, covering the tree with a man- tle of white, broken here and there by protruding leaves. le JOHN MACOUN ON CONCLUSION. The exnnuniition of the Caiiudiuii fon-Htrt brings out Honii' iiotowortliy points roliitivo to the distribution of species. Without referring to the origin of our flora, whieli it is not in- tended to discuss in this paper, it nmy be interesting to note tiie secpience of species in some genera na they [uiss from east to west. Piiiiis BnitLsidtxi, P. Miirriii/iiiifi and P. rontarht form a natural grouji of scrub pines that under one form or anotlier pass, witliout intermixing, from the Atlantic to tiie Pacific. The first extends without a break from tlic Atlantic coast of Nova Scotia to the Athabasca River at Fort Assiniboine. Hero at its western limit and as far east as J'rince Albert on the Saskatchewan it is u fine tree. Scarcely a day's journey west of Fort Assiniboine the writer found the second species in great i)rof'usion, but never more than three inches in diameter. Mr. McConnell found l)oth species on the Liard River, J'. Mnrnn/inni being near the mountains and P. BoHksiaim lower down the stream towards the Mackenzie. Tliroughout the Rocky Mountains 7*. Miirniyiiini is the principal tree, between 4,000 and r),000 feet, and in British Columbia on the plateau between lat. 51 ' and oo , at an altitude of from 2,000 to 4,000 feet. F'assing from the Coast Range to the valley of the Fraser the third species comes in, l>ut excejit on the coast it prefers 8wam[is to dry ground. Pireii (illm, P. E)i(j(:lniiH and /'. Silchensis form aiKjthcr natural group and are dis- tributed in nearly tiie same way. In this case, liowever, our knowledge is not so definite, and there may be four species instead of three. Picmalhu'iH found in abundance from Nova Scotia westward to the prairie region, and even there occasionally on river l)anks. It is plentiful, too, in the Cypress Hills. This species enters the Rocky Mountains, and is found in river valleys as far west as the valley of Kagle River, west of the Gold Range. In the higher mountain valleys Piccn Eiif/eliiKtnni takes its place, and is the spruce fouiul on nearly all mountains from the Rockies to the Coast Range. Crossing the Coast Range Picea Sil- chotsls comes in and is the only coast s[iecies. Tlie firs have the same distribution and pass from east to west in the same way, tiie Rocky Mountains and west coast having their own species, tiie se(pience being Abicn Ixilsamca, A. snbolphm and A. (jvdiidi.s. The habitat of Jiiniitenis Vinjiiiiaini i-hanges as it passes from east to west. In the east it grows on tht' rocky banks of streams or on shallow soil on limestone. In the west, on the other hand, it grows in peat bogs or by lake shores, and althougli so distinct in habit there seems to be no clear character by which it may be si'parated into two species. The only trees that pass from east to west without ai)parent changi^ are the asjjcn and the canoe birch. The latter, however, never becomes tlie tine tree on the west coast that it does in the east. On Vancouver Island there are two forms of the aspen, oneof whi(!h may be the European P. tremula. Both forms grow in clumps, but the leaves of the one supposed to be P. tremula were quite brown in character when I saw them in 1803, wliile those of the other form which grew near it were the usual light green colour. Tlie old leaves of the former were quite round and seldom pointed, the teeth were sinuate and appressed and not erect and regular as they arc in the common aspen. In conclusion I may say that including Vancouver Island a coniferous forest may he said to extend from the Pacific to the Atlantic, bounded on the north by the tundra of TIIK KOUKSTS OP CANADA. 17 AliiHka mill tlic Hiiitimi Gronndu dftlu' Ddiiiiiiioii, niid Houtln-rly wifli ii viiryiiiff Ixji-dcr until it iiiwtH imd iiiti'rininf,'l('s with tin- poidur lorwtrt of tiio >f(irlli\vi'Ht Tcrritorii's. i'liKHiiij,' Htill imHtwunl tlic jiopliir inixoH with it to the Houth until aftvr imnHing Lak*- Su|it'nor it .Urai 111 ally nu'rj,'cs into tlio di'i^iduoUH foroHtH of Ontario, HoutluTU (iuoltw and tiio dovatiMl and interior rcfjion of New Urunnwick, Nova Scotia and I'rinco Kdward Inland. Afti'r all lian lifcn naid about our wanti' hoth by niysulf and otluTH it is ovidont that wt- havo woodland fnoufjh in tho north to supply ovcry di-nnnid that nuiy bo nnidc upon it for many goiu'rations, but liki; everything that is valuable, it is hard to get at. When it will he wanted none ('an say, but that it in therein incaleulableiiuantities is alisolutely certain. A belt 200 miles deep and 3,000 miles wide gives us an area of 000,000 sijuare miles, but we »rc quite safe in estimating it at 1,000,000. The [loplar forest and the mi.xed growth to the lortli of it extends from Kdmonto?i to Winnipeg, a distance of about 000 miles, and averages over 50 miles in width, wiiieh gives an area of 45,000 s(|uare miles of aspen forest for the use of the settlors wiio will by degrees occupy this region, for the aspen districts have, as a rule, good soil. rl Sec. IV., 1894. 3. It JOHN MACOUN ON List of Khrkht Tiikks ok tiik Dominion, Siiowinu tiikik Distuiiuition in tiik VaKIOHH I'ltoVlNt'KH. 5 (I 7 H II 1(1 II 12 13 V 15 l« 17 II- II! 211 21 22 •£i 24 25 2(1 27 2H 211 :«) :n :j2 :« •M :i6 37 us :)ii AHiiiiinik Irlloliii, Diiiiul. (.ViiiiM'Irnii |iB|inw) l.irJDil' Milriiii lulipiri'rii, Mill), ('fillip Irvi-) Tillii Aiiii'i'liaiiii, I. inn. (HnMNWoiHl) " pnlii'strii'H, All. (Iliiwny luHViul IuihhwoimI) niiiiniiiUH I'lii'xliliiniih, DC, (" Harlicrry") AriT l'('ini') '■ dimyrarpiini, Klirli. iSIImthi' wIiIIc innpU'l " niliniin, l.lnn. (Hod or soft iniiplc) .N'cKuniln accroldi"*, Minicli. (Box clili-r, " .Manitoba ninple"). HIiiiH typliina, l.lnn. iStaK horn snniai'li) (iyinniH'ladiis CanadciiHls, l.ani. (Kentiirky foffeo-tn-f) (ili'dltHclila triicanlliu", I. inn. iTIiri'c thoriicd aeacla) (VrclH CanadenNlM, Mini. (.liidaH tror) Pninns .VnifHcann, Marsli. iWild plum) I^'nn^ylvallil•a, l.lnn. lUird cherry) cni«r>i;lnat», Walp. (\V<'Sti!rn l)lrd chcrryi Vlivlniana, l.lnn. (Clioki' clicrry) " .s<'n)(lna, Ehrli. (Hlack cherry) PiriiN eoi'onarla, l.lnn. (Anierican erah-apple) " rivularlH, Donml. (\Ve»U'rn eraliapplei " .\inerleana, l)(". (.Monntalii aslo Cratte^iiH t'oceinea l.lnn. (Scarlet fruited llicirn) " toinentosa, l.lnn. (I)lack or pear tliorni •' sniivllloha, Sehrader. (Downy leaved thorn) " ('ruH ffalli, l.lnn. (I'ockspur thorn) Aniulancliier CanadviiMlH, Torr. & Gray. (June berry) HanianieliH VIrginlana, Linn. (Witch haxel) Corniisalternirolia, l.lnn. (Alternate-leaved cornel) " florida, l.lnn. (Flowering dogwood) " Nuttnllll, .\nd. (Western flowering dogwood) NysRa niiiltitlora, Wang. (Pepperidge, son"-niini tree) Vllinrnum I.enliigo, l.lnn. (Sheep berry) Sanibncus Canadensi.s ami pibeiiN In V. I ArlnitnH Menziesli, I'urMli. (Madrona) ftj |«5 1 I 1 & 8. W. IW 1 1 1 1 1 I 1 1 1 1 1 1 1 s. s. s. 1 1 if 'A K. K. 1 1 W. E. 1 1 1 1 1 1 1 1 W. W. W. 1 C. , 1 ,...1 1 C. 1 ■^ T 1 1 !•; F( »RKS'rs () I' ( A NA I » A. List or Fokkst Treeh of the Dominion — CiniUiuieil, •4 I I Id »5 aJ ft. N >5 41 42 4a 44 4» 4U 47 4« 4U no ni 52 nil fM ss 5fl 57 5H 51) (Ml 01 m M 05 00 07 08 01) 70 71 72 73 74I 75' 76| 77 I 78 79 80 Kraximm Aincricnim, Linn. (Wliltt- iinIi) " |iulH>M'i>nN, 1,11111. flU'il or rim unIi) ., " vlriilix, Miclix. (rn, Linn. (HihI mulberry) I'lnttiiiu.s iKi'ldcntiillH, Linn. (Hiittonwudil) Cnryti iillxi, \nt(. (Slicllhark hickory) " tonivntoHii, NiUt. (Wlilte heart hickory) .... " porclnii, Mutt. (I'lK-nut or hrooni hickory) . , . " uMiarii, Nutl. (Ilittorinit hickory) " niicrocarpH, Nutt. (Small fruited hickory). . . . Hetuin lentil, Llini. (t'hcrry or l)lm'k hircli) hiteft, Michx. f.( Yellow hirch) " pu|)ulifoliii, Alt. (American while birch) .. " piipyrifcrii, MnrNh. (I'liperor canoeJiiix-h) , AluuM rubra, Bonganl. (Ked alder) " rhombifolia, Nutl. (Mountain alder.) CarpinuH t'arollniana, Walter. (Hiue licech) Ostrya Vlr«inica, Willd. (Iron wood) Quercua alba, Linn. (White oak) " Garryana, Douglas. (Western white oak) . " obtusiloba, Mich.\. (I'oHt oak) " nincrocarpa, Mich.x. (Mos.sy-cup oak) bicolor, Willd. (Swamp White oak) " Prinus, Linn. (Rock Chestnut oak) " prinoldes, Willd. (Chestnut oak) " rubra, Linn. (Ke 81 Si a 84 8fi 8e 87 88 8U IK) 1)1 iy^ m IM 05 Wi 97 98 9!l IIKI 101 102 lOH m lO.-. IIH> 107 108 lOi) 110 111 112 li:i 114 115 110 117 118 US) 120 121 Solix niftra. Hook. (Bliitk willow) 1 1 1 1 1 1 PopuluH treinula I.iiiii. (Ruropear. aspen) 1 1 treniuluideH, Miuhx. (As|)en) 1 1 1 1 1 1 1 1 1 1 1 1 ' 1 1 1 I " giaiididentata, Miclix. (Large-toothed aNprii) " baKsaiiiirera, Linn. (Bai.saiii poplar) " anKUstifolla, .TainL'g. (Black cotton- wood) 1 I s.w. 1 1 1 1 " trichocarpa, Torr. & Gray 1 1 1 " monilifcra, Alton. (Cotton- wood) w. I 1 1 w. 1 ■Tuglans cinerea, Linn. (Butternut) I s. " -liKra, Linn. (Black walnut) — 1 — Thuya occidentali.s, Linn. (White cedar) 1 1 1 1 N. E. 1 " giganlea, Nutt. (Western white cedar) 1 1 1 1 1 1 1 " excclsa. Bong. (Yellow cypress) r .Tuniperus Virginiana, Linn. (Bed cedar) 1 1 1 1 C. Taxus '>revifolia, N'utt. (Western yew) Pinurt Strobus, Linn. (White pine) 1 1 1 1 1 E. " nionticola, Uuugl . (Western white pine) 1 1 1 " liexilis, .lanics. (Rocky mountain pine) W. " albicaulis, Kngelni. ( White-barked pine) 1 I " resinosa, Ait. (Red pine) " pondcrosa, var. scopulorum, Engelni. (Heavy pine) ...t 1 1 1 1 1 E. 1 .... " Banksiana, Lam. (Scrub pine) " Murrayana, Balfour. (Mountain or l)lack pine) 1 1 I 1 1 N. S. 1 1 c. 1 " rontorta, Uougl. (Western .scrub pine) " ri^ida, Miller. (Fitch pine) St L Picca ni^ia, Link. (Black spruce) 1 1 1 1 1 1 1 1 I 1 1 1 1 E. 1 N. N. N. •■••. " rubra, (Red spruce) " alba. Link. (W liite spruce) ' I 1 1 1 C. 1 " KuKclmanni, Kngelm. (Engel maims si)ruce) " Sitclieiisis, ("arr. (Mcnzies' spruce) Tsujia Cunailensis, Carr. (Hemlock) 1 1 1 1 1 " Mertenslana, Carr. (Western henilnck) 1 1 1 1 1 1 1 1 1 " Patloniaua, Kngi'Im. (Mountain hemlock) Pseudotsuga Douglasii, Carr. (Douglas (Ir) W. E. A'.iies balsamea. Miller. (Canada balsam llr) " subalpiiin, Eiigelm. (Mountain balsam) 1 1 1 1 1 1 1 C. 1 N. 1 1 1 1 " grandis, Liudley. ( We.stern balsam Hr) " amabilis, Korbes. (White tir) 1 N. Larix Americana, Miclix. (Tamarack, larch) " occidentalis, Nutt. (Western larch) 1 1 1 1 1 N. " Lyallii, Parlalore. (Mountain larch) 1 ■^