ON THE SUPPOSED FORMER INTENSITY OF THE IGNEOUS FORCES.
Volcanic action at successive geological periods--Plutonic rocks of different ages--Gradual development of subterranean movements--Faults--Doctrine of the sudden upheaval of parallel mountain-chains--Objections to the proof of the suddenness of the upheaval, and the contemporaneousness of parallel chains--Trains of active volcanoes not parallel--As large tracts of land are rising or sinking slowly, so narrow zones of land may be pushed up gradually to great heights--Bending of strata by lateral pressure--Adequacy of the volcanic power to effect this without paroxysmal convulsions.
When reasoning on the intensity of volcanic action at former periods, as well as on the power of moving water, already treated of, geologists have been ever prone to represent Nature as having been prodigal of violence and parsimonious of time. Now, although it is less easy to determine the relative ages of the volcanic than of the fossiliferous formations, it is undeniable that igneous rocks have been produced at all geological periods, or as often as we find distinct deposits marked by peculiar animal and vegetable remains. It can be shown that rocks commonly called trappean have been injected into fissures, and ejected at the surface, both before and during the deposition of the Carboniferous series, and at the time when the Magnesian Limestone, and when the Upper New Red Sandstone were formed, or when the Lias, Oolite, Green Sand, Chalk, and the several tertiary groups newer than the chalk, originated in succession. Nor is this all: distinct volcanic products may be referred to the subordinate divisions of each period, such as the Carboniferous, as in the county of Fife, in Scotland, where certain masses of contemporaneous trap are associated with the Lower, others with the Upper Coal measures. And if one of these masses is more minutely examined, we find it to consist of the products of a great many successive outbursts, by which scoriæ and lava were again and again emitted, and afterwards consolidated, then fissured, and finally traversed by melted matter, constituting what are called dikes.[239] As we enlarge, therefore, our knowledge of the ancient rocks formed by subterranean heat, we find ourselves compelled to regard them as the aggregate effects of innumerable eruptions, each of which may have been comparable in violence to those now experienced in volcanic regions.