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Updated: June 20, 2025
The moment the Plutonic power is let loose, and the loveless Alberic comes into the field with his corrupting millions, the gods are face to face with destruction; since Alberic, able with invisible hunger-whip to force the labor of the dwarfs and to buy the services of the giants, can outshine all the temporal shows and splendors of the golden age, and make himself master of the world, unless the gods, with their bigger brains, can capture his gold.
So long as he is preoccupied with love of you, the gold, and all that it implies, will escape him: the golden age will endure. Not until he forswears love will he stretch out his hand to the gold, and found the Plutonic empire for himself. But the choice between love and gold may not rest altogether with him.
Those who believed the hypogene rocks to have originated antecedently to the creation of organic beings, imputed the absence of lime, so remarkable in metamorphic strata, to the non-existence of those mollusca and zoophytes by which shells and corals are secreted; but when we ascribe the crystalline formations to Plutonic action, it is natural to inquire whether this action itself may not tend to expel carbonic acid and lime from the materials which it reduces to fusion or semi-fusion.
So one glass of brandy I'm sorry to say, unmixed with water the handsome misanthropist sipped and sipped, to the last drop; and then sat down before his fire, and struck, and poked, and stabbed at it in a bitter, personal sort of way, until here and there some blazes leaped up, and gave his eyes a dreamy sort of occupation; and he sat back, with his hands in his pockets, and his feet on the fender, gazing among the Plutonic peaks and caverns between the bars.
In the second place, the perfect tranquillity, under which it is probable that the plutonic masses, buried at profound depths, have cooled, would, most likely, be highly unfavourable to the separation of their constituent minerals; for, if the attractive force, which during the progressive cooling draws together the molecules of the different minerals, has power sufficient to keep them together, the friction between such half-formed crystals or pasty globules would effectually prevent the heavier ones from sinking, or the lighter ones from rising.
Moreover, I believe that it is impossible to explain the structure of great mountain-chains, such as that of the Cordillera, were the strata, capping the injected axis of plutonic rock, have been thrown on their edges along several parallel and neighbouring lines of elevation, except on this view of the rock of the axis having been repeatedly injected, after intervals sufficiently long to allow the upper parts or wedges to cool and become solid; for if the strata had been thrown into their present highly inclined, vertical, and even inverted positions, by a single blow, the very bowels of the earth would have gushed out; and instead of beholding abrupt mountain-axes of rock solidified under great pressure, deluges of lava would have flowed out at innumerable points on every line of elevation.
For more than two hundred miles northward of Navidad, the coast consists of plutonic and metamorphic rocks, with the exception of some quite insignificant superficial beds of recent origin. At Tonguay, twenty-five miles south of Coquimbo, tertiary beds recommence.
I quite agree that areas undergoing opposite movements are somehow connected; but volcanic outbursts must, I think, be looked at as mere accidents in the swelling tip of a great dome or surface of plutonic rocks; and there seems no more reason to conclude that such swelling or elevation in mass is the cause of the subsidence than that the subsidence is the cause of the elevation; which latter view is indeed held by some geologists, I have regretted to find so little about the habits of the many animals which you have seen.
I shall merely observe in this place that had such junctions alone been visible, and had we not learnt, from other sections, how long a period elapsed between the consolidation of the gneiss and the injection of this granite, we might have suspected that the gneiss was scarcely solidified, or had not yet assumed its complete metamorphic character when invaded by the Plutonic rock.
Granite, indeed, and other Plutonic rocks, rarely make their appearance at the surface, notwithstanding the deep ravines which lay open to view the internal structure of these mountains.
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