On the Old Road Volume Ii Part 18

1. Simple aggregation, having no periodical or otherwise defined limit, and subject only to laws of cohesion and crystallization, as in inorganic matter.

2. Addition of similar parts to each other, under some law fixing their limits and securing their unity.

3. Enlargement, or systematic change in arrangement, of a typical form, as in the growth of the members of an animal.

285. The growth of trees came under the second of these heads. A tree did not increase in stem or boughs as the wrist and hand of a child increased to the wrist and hand of a man; but it was built up by additions of similar parts, as a city is increased by the building of new rows of houses.

Any annual shoot was most conveniently to be considered as a single rod, which would always grow vertically if possible.

Every such rod or pillar was, in common timber trees, typically either polygonal in section, or rectangular.

If polygonal, the leaves were arranged on it in a spiral order, as in the elm or oak.

If rectangular, the leaves were arranged on it in pairs, set alternately at right angles to each other.

Intermediate forms connected each of these types with those of monocotyledonous trees. The structure of the _arbor vitae_ might be considered as typically representing the link between the rectangular structure and that of monocotyledons; and that of the pine between the polygonal structure and that of monocotyledons.

Every leaf during its vitality secreting carbon from the atmosphere, with the elements of water, formed a certain quant.i.ty of woody tissue, which extended down the outside of the tree to the ground, and farther to the extremities of the roots. The mode in which this descending masonry was added appeared to depend on the peculiar functions of cambium, and (the speaker believed) was as yet unexplained by botanists.

286. Every leaf, besides forming this masonry all down the tree, protected a bud at the base of its own stalk. From this bud, unless rendered abortive, a new shoot would spring next year. Now, supposing that out of the leaf-buds on each shoot of a pentagonal tree, only five at its extremity or on its side were permitted to develop themselves, even under this limitation the number of shoots developed from a single one in the seventh year would be 78,125. The external form of a healthily grown tree at any period of its development was therefore composed of a ma.s.s of sprays, whose vitality was approximately distributed over the _surface_ of the tree to an equal depth. The branches beneath at once supported, and were fed by, this...o...b..cular field, or animated external garment of vegetation, from every several leaf of which, as from an innumerable mult.i.tude of small green fountains, the streams of woody fiber descended, met, and united as rivers do, and gathered their full flood into the strength of the stem.

287. The princ.i.p.al errors which had been committed by artists in drawing trees had arisen from their regarding the bough as ramifying irregularly, and somewhat losing in energy towards the extremity; whereas the real boughs threw their whole energy, and multiplied their substance, towards the extremities, ranking themselves in more or less cup-shaped tiers round the trunk, and forming a compact united surface at the exterior of the tree.

288. In the course of arrival at this form, the bough, throughout its whole length, showed itself to be influenced by a force like that of an animal's instinct. Its minor curves and angles were all subjected to one strong ruling tendency and law of advance, dependent partly on the aim of every shoot to raise itself upright, partly on the necessity which each was under to yield due place to the neighboring leaves, and obtain for itself as much light and air as possible. It had indeed been ascertained that vegetable tissue was liable to contractions and expansion (under fixed mechanical conditions) by light, heat, moisture, etc. But vegetable tissue in the living branch did not contract nor expand under external influence alone. The principle of life manifested itself either by contention with, or felicitous recognition of, external force. It accepted with a visible, active, and apparently joyful concurrence, the influences which led the bough towards its due place in the economy of the tree; and it obeyed reluctantly, partially, and with distorted curvatures, those which forced it to violate the typical organic form. The attention of painters of foliage had seldom been drawn with sufficient accuracy to the lines either of branch curvature, or leaf contour, as expressing these subtle laws of incipient volition; but the relative merit of the great schools of figure design might, in absence of all other evidence, be determined, almost without error, by observing the precision of their treatment of leaf curvature. The leaf-painting round the head of Arios...o...b.. t.i.tian, in the National Gallery, might be instanced.

289. The leaf thus differed from the flower in forming and protecting behind it, not only the bud in which was the form of a new shoot like itself, but a piece of permanent work, and produced substance, by which every following shoot could be placed under different circ.u.mstances from its predecessor. Every leaf labored to solidify this substance during its own life; but the seed left by the flower matured only as the flower perished.

This difference in the action and endurance of the flower and leaf had been applied by nearly all great nations as a type of the variously active and productive states of life among individuals or commonwealths.

Chaucer's poem of the "Flower and Leaf" is the most definite expression of the mediaeval feeling in this respect, while the fables of the rape of Proserpine and of Apollo and Daphne embody that of the Greeks. There is no Greek G.o.ddess corresponding to the Flora of the Romans. Their Flora is Persephone, "the bringer of death." She plays for a little while in the Sicilian fields, gathering flowers, then s.n.a.t.c.hed away by Pluto, receives her chief power as she vanishes from our sight, and is crowned in the grave. Daphne, on the other hand, is the daughter of one of the great Arcadian river G.o.ds, and of the earth; she is the type of the river mist filling the rocky vales of Arcadia; the sun, pursuing this mist from dell to dell, is Apollo pursuing Daphne; where the mist is protected from his rays by the rock shadows, the laurel and other richest vegetation spring by the river-sides, so that the laurel-leaf becomes the type, in the Greek mind, of the beneficent ministry and vitality of the rivers and the earth, under the beams of sunshine; and therefore it is chosen to form the signet-crown of highest honor for G.o.ds or men, honor for work born of the strength and dew of the earth and informed by the central light of heaven; work living, perennial, and beneficent.

J. R.

FOOTNOTES:

[Footnote 34: Read by Mr. Ruskin at the weekly evening meeting of the Royal Inst.i.tution (see _Proceedings_, vol. iii., pp. 358-60), April 19, 1861.--ED.]

ON THE FORMS OF THE STRATIFIED ALPS OF SAVOY.[35]

290. The purpose of the discourse was to trace some of the influences which have produced the present external forms of the stratified mountains of Savoy, and the probable extent and results of the future operation of such influences.

The subject was arranged under three heads:--

I. The Materials of the Savoy Alps.

II. The Mode of their Formation.

III. The Mode of their subsequent Sculpture.

291. I. _Their Materials._--The investigation was limited to those Alps which consist, in whole or in part, either of Jura limestone, of Neocomian beds, or of the Hippurite limestone, and include no important ma.s.ses of other formations. All these rocks are marine deposits; and the first question to be considered with respect to the development of mountains out of them is the kind of change they must undergo in being dried. Whether prolonged through vast periods of time, or hastened by heat and pressure, the drying and solidification of such rocks involved their contraction, and usually, in consequence, their being traversed throughout by minute fissures. Under certain conditions of pressure, these fissures take the aspect of slaty cleavage; under others, they become irregular cracks, dividing all the substance of the stone. If these are not filled, the rock would become a mere heap of debris, and be incapable of establishing itself in any bold form. This is provided against by a metamorphic action, which either arranges the particles of the rock, throughout, in new and more crystalline conditions, or else causes some of them to separate from the rest, to traverse the body of the rock, and arrange themselves in its fissures; thus forming a cement, usually of finer and purer substance than the rest of the stone. In either case the action tends continually to the purification and segregation of the elements of the stone. The energy of such action depends on accidental circ.u.mstances: first, on the attractions of the component elements among themselves; secondly, on every change of external temperature and relation. So that mountains are at different periods in different stages of health (so to call it) or disease. We have mountains of a languid temperament, mountains with checked circulations, mountains in nervous fevers, mountains in atrophy and decline.

292. This change in the structure of existing rocks is traceable through continuous gradations, so that a black mud or calcareous slime is imperceptibly modified into a magnificently hard and crystalline substance, inclosing nests of beryl, topaz, and sapphire, and veined with gold. But it cannot be determined how far, or in what localities, these changes are yet arrested; in the plurality of instances they are evidently yet in progress. It appears rational to suppose that as each rock approaches to its perfect type the change becomes slower; its perfection being continually neared, but never reached; its change being liable also to interruption or reversal by new geological phenomena. In the process of this change, rocks expand or contract; and, in portions, their mult.i.tudinous fissures give them a ductility or viscosity like that of glacier-ice on a larger scale. So that many formations are best to be conceived as glaciers, or frozen fields of crag, whose depth is to be measured in miles instead of fathoms, whose creva.s.ses are filled with solvent flame, with vapor, with gelatinous flint, or with crystallizing elements of mingled natures; the whole ma.s.s changing its dimensions and flowing into new channels, though by gradations which cannot be measured, and in periods of time of which human life forms no appreciable unit.

293. II. _Formation._--Mountains are to be arranged, with respect to their structure, under two great cla.s.ses--those which are cut out of the beds of which they are composed, and those which are formed by the convolution or contortion of the beds themselves. The Savoy mountains are chiefly of this latter cla.s.s. When stratified formations are contorted, it is usually either by pressure from below, which raises one part of the formation above the rest, or by lateral pressure, which reduces the whole formation into a series of waves. The ascending pressure may be limited in its sphere of operation; the lateral one necessarily affects extensive tracts of country, and the eminences it produces vanish only by degrees, like the waves left in the wake of a ship. The Savoy mountains have undergone both these kinds of violence in very complex modes and at different periods, so that it becomes almost impossible to trace separately and completely the operation of any given force at a given point.

294. The speaker's intention was to have a.n.a.lyzed, as far as possible, the action of the forming forces in one wave of simple elevation, the Mont Saleve, and in another of lateral compression, the Mont Brezon: but the investigation of the Mont Saleve had presented unexpected difficulty. Its facade had been always considered to be formed by vertical beds, raised into that position during the tertiary periods; the speaker's investigations had, on the contrary, led him to conclude that the appearance of vertical beds was owing to a peculiarly sharp and distinct cleavage, at right angles with the beds, but nearly parallel to their strike, elsewhere similarly manifested in the Jura.s.sic series of Savoy, and showing itself on the fronts of most of the precipices formed of that rock. The attention of geologists was invited to the determination of this question.

The compressed wave of the Brezon, more complex in arrangement, was more clearly defined. A section of it was given, showing the reversed position of the Hippurite limestone in the summit and lower precipices.

This limestone wave was shown to be one of a great series, running parallel with the Alps, and const.i.tuting an undulatory district, chiefly composed of chalk beds, separated from the higher limestone district of the Jura and Lias by a long trench or moat, filled with members of the tertiary series--chiefly nummulite limestones and flysch.

This trench might be followed from Faverges, at the head of the lake of Annecy, across Savoy. It separated Mont Vergi from the Mont Dorons, and the Dent d'Oche from the Dent du Midi; then entered Switzerland, separating the Moleson from the Diablerets; pa.s.sed on through the districts of Thun and Brientz, and, dividing itself into two, caused the zigzagged form of the lake of Lucerne. The princ.i.p.al branch then pa.s.sed between the high Sentis and the Glarnisch, and broke into confusion in the Tyrol. On the north side of this trench the chalk beds were often vertical, or cast into repeated folds, of which the escarpments were mostly turned away from the Alps; but on the south side of the trench, the Jura.s.sic, Tria.s.sic, and Carboniferous beds, though much distorted, showed a prevailing tendency to lean towards the Alps, and turn their escarpments to the central chain.

295. Both these systems of mountains are intersected by transverse valleys, owing their origin, in the first instance, to a series of transverse curvilinear fractures, which affect the forms even of every minor ridge, and produce its princ.i.p.al ravines and boldest rocks, even where no distinctly excavated valleys exist. Thus, the Mont Vergi and the Aiguilles of Salouvre are only fragmentary remains of a range of horizontal beds, once continuous, but broken by this transverse system of curvilinear cleavage, and worn or weathered into separate summits.

The means of this ultimate sculpture or weathering were lastly to be considered.

296. III. _Sculpture._--The final reductions of mountainform are owing either to disintegration, or to the action of water, in the condition of rain, rivers, or ice, aided by frost and other circ.u.mstances of temperature and atmosphere.

All important existing forms are owing to disintegration, or the action of water. That of ice had been curiously over-rated. As an instrument of sculpture, ice is much less powerful than water; the apparently energetic effects of it being merely the exponents of disintegration. A glacier did not produce its moraine, but sustained and exposed the fragments which fell on its surface, pulverizing these by keeping them in motion, but producing very unimportant effects on the rock below; the roundings and striation produced by ice were superficial; while a torrent penetrated into every angle and cranny, undermining and wearing continually, and carrying stones, at the lowest estimate, six hundred thousand times as fast as the glacier. Had the quant.i.ty of rain which has fallen on Mont Blanc in the form of snow (and descended in the ravines as ice) fallen as rain, and descended in torrents, the ravines would have been much deeper than they are now, and the glacier may so far be considered as exercising a protective influence. But its power of carriage is unlimited, and when ma.s.ses of earth or rock are once loosened, the glacier carries them away, and exposes fresh surfaces.

Generally, the work of water and ice is in mountain surgery like that of lancet and sponge--one for incision, the other for ablution. No excavation by ice was possible on a large scale, any more than by a stream of honey; and its various actions, with their limitations, were only to be understood by keeping always clearly in view the great law of its motion as a viscous substance, determined by Professor James Forbes.

297. The existing forms of the Alps are, therefore, traceable chiefly to denudation as they rose from the sea, followed by more or less violent aqueous action, partly arrested during the glacial periods, while the produced diluvium was carried away into the valley of the Rhine or into the North Sea. One very important result of denudation had not yet been sufficiently regarded; namely, that when portions of a thick bed (as the Rudisten-kalk) had been entirely removed, the weight of the remaining ma.s.ses, pressing unequally on the inferior beds, would, when these were soft (as the Neocomian marls), press them up into arched conditions, like those of the floors of coal-mines in what the miners called "creeps." Many anomalous positions of the beds of Spatangenkalk in the district of the Lake of Annecy were in all probability owing to this cause: they might be studied advantageously in the sloping base of the great Rochers de Lanfon, which, disintegrating in curved, nearly vertical flakes, each a thousand feet in height, were nevertheless a mere outlying remnant of the great horizontal formation of the Parmelan, and formed, like it, of very thin horizontal beds of Rudisten-kalk, imposed on shaly ma.s.ses of Neocomian, modified by their pressure. More complex forms of harder rock were wrought by the streams and rains into fantastic outlines; and the transverse gorges were cut deep where they had been first traced by fault or distortion. The a.n.a.lysis of this aqueous action would alone require a series of discourses; but the sum of the facts was that the best and most interesting portions of the mountains were just those which were finally left, the centers and joints, as it were, of the Alpine anatomy. Immeasurable periods of time would be required to wear these away; and to all appearances, during the process of their destruction, others were rising to take their place, and forms of perhaps far more n.o.bly organized mountain would witness the collateral progress of humanity.

J. R.

FOOTNOTES:

[Footnote 35: Read by Mr. Ruskin at the weekly evening meeting of the Royal Inst.i.tution (see _Proceedings_, vol. iv., pp. 142-46), June 5, 1863.--ED.]

THE RANGE OF INTELLECTUAL CONCEPTION PROPORTIONED TO THE RANK IN ANIMATED LIFE.[36]

A THEOREM.

298. I suppose this theorem to be a truism; but I venture to state it, because it is surely desirable that it should be recognized as an axiom by metaphysicians, and practically does not seem to me yet to have been so. I say "animated life" because the word "life" by itself might have been taken to include that of vegetables; and I say "animated" instead of "spiritual" life because the Latin "anima," and pretty Italian corruption of it, "alma," involving the new idea of nourishment of the body as by the Aliment or Alms of G.o.d, seems to me to convey a better idea of the existence of conscious creatures than any derivative of "spiritus," "pneuma," or "psyche."

I attach, however, a somewhat lower sense to the word "conception" than is, I believe, usual with metaphysicians, for, as a painter, I belong to a lower rank of animated being than theirs, and can only mean by conception what I know of it. A painter never conceives anything absolutely, and is indeed incapable of conceiving anything at all, except as a phenomenon or sensation, or as the mode or locus of a phenomenon or sensation. That which is not an appearance, or a feeling, or a mode of one or the other, is to him nothing.

299. For instance, he would deny the definition of the phenomenon which he is himself first concerned in producing--a line--as "length without breadth." He would say, "That which has no breadth is nothing, and nothing cannot be long." He would define a line as a narrow and long phenomenon, and a mathematician's idea of it as an idea of the direction of such a phenomenon.

The act of conception or imagination with him, therefore, is merely the memory, simple or combined, of things that he has seen or felt. He has no ray, no incipience of faculty beyond this. No quant.i.ty of the sternest training in the school of Hegel, would ever enable him to think the Absolute. He would persist in an obstinate refusal to use the word "think" at all in a transitive sense. He would never, for instance, say, "I think the table," but "I think the table is turning," or is not, as the case might be. And if he were to be taught in any school whatever to conceive a table, his first demand would be that he should be shown one, or referred to other things that had the qualities of one in ill.u.s.trative degree.