Roderick Impey Murchison

../../ (1862)

Summary

Roderick Impey Murchison,  ../../ (1862)

“ In speaking of the structure of Russia, I thus wrote:—"The Carboniferous system is surmounted to the east of the Volga by a vast series of beds of marls, schists, limestones, sandstones, and conglomerates, to which I propose to give the name of 'Permian System,' because, although this series represents as a whole the Lower New Red Sandstone (Rothe-todte-liegende) and the Magnesian Limestone or Zechstein, yet it cannot be classed exactly, whether by the succession of the strata or their contents, with either of the German or British subdivisions of this age." ”
Source: Wikisource

Roderick Impey Murchison,  ../../ (1862)

“ Quite irrespective, however, of the question of whether there are or are not localities in Germany where the Zechstein passes upwards into a red rock, which forms no true part of the Bunter Saudstein of the Trias, we have only to look to the environs of Dresden, on the one hand, and to Lower Silesia on the other, to see the inapplicability of the word "Dyas" to this group. ”
Source: Wikisource

Roderick Impey Murchison,  ../../ (1862)

“ Geinitz has seized upon one illustration in my work 'Siluria' which shows that in certain tracts, where the Zechstein or Magnesian Limestone is subordinate to an enveloping series of sandstones, the Permian of my classification is there as much a tripartite Palæozoic group as the Trias of Central Grermany is a triple formation of Mesozoic age. ”
Source: Wikisource

Get perspective with Kwize: daily news enlightened by great literature