from the crater of every active volcano to a great depth below, perhaps several miles or leagues, and the effects which are produced deep in the bowels of the earth may, or rather must, be distinct; so that volcanic and plutonic rocks, each different... The Student's Elements of Geology - Seite 547von Sir Charles Lyell - 1878 - 672 SeitenVollansicht - Über dieses Buch
| Sir Charles Lyell - 1838 - 582 Seiten
...volcanic. The beginner will easily conceive that the influence of subterranean heat may extend downwards from the crater of every active volcano to a great depth below, perhaps several miles or leagues (see Frontispiece), and the effects which are produced deep in the bowels of the earth may, or rather... | |
| Sir Charles Lyell - 1838 - 606 Seiten
...volcanic. The beginner will easily conceive that the influence of subterranean heat may extend downwards from the crater of every active volcano to a great depth below, perhaps several miles or leagues (see Frontispiece), and the effects which are produced deep in the bowels of the earth may, or rather... | |
| Sir Charles Lyell - 1839 - 330 Seiten
...beginner will easily conceive that the influence of subterranean heat may extend downwards from the erater of every active volcano to a great depth below, perhaps several miles or leagues (see Frontispiece,) and the effects which are produced deep in the bowels of the earth may, or rather... | |
| Sir Charles Lyell - 1841 - 946 Seiten
...rocks." The beginner will easily conceive that the influence of subterranean heat may extend downwards from the crater of every active volcano to a great depth below, perhaps several miles or leagues (see Frontispiece), and the effects which are produced deep in the bowels of the earth may, or rather... | |
| Sir Charles Lyell - 1845 - 338 Seiten
...volcanic. The beginner will easily conceive that the influence of subterranean heat may extend downwards from the crater of every active volcano to a great depth below, perhaps several miles or leagues (see Frontispiece,) and the effects which are produced deep in the bowels of the earth may, or rather... | |
| Sir Charles Lyell - 1846 - 358 Seiten
...volcanic. The beginner will easily conceive that the influence of subterranean heat mi^ extend downwards from the crater of every active volcano to a great depth below, perhaps several miles or leagues (see Frontispiece,) and the effects which are produced deep in the bowels of the earth may, or rather... | |
| Sir Charles Lyell - 1851 - 602 Seiten
...rocks." The beginner will easily conceive that the influence of subterranean heat may extend downwards from the crater of every active volcano to a great...even in composition, may originate simultaneously, the one at the surface, the other far beneath it. By some writers, all the rocks now under consideration... | |
| Sir Charles Lyell - 1851 - 540 Seiten
...downwards from the crater of every active rolcano to a great depth below, perhaps several miles or league*, and the effects which are produced deep in the bowels of the earth may, or rather most be, distinct; so that volcanic and pltttonic rock*, each different in texture, and sometimes even... | |
| Sir Charles Lyell - 1852 - 578 Seiten
...rocks." The beginner will easily conceive that the influence of subterranean heat may extend downwards from the crater of every active volcano to a great...even in composition, may originate simultaneously, the one at the surface, the other far beneath it. By some writers, all the rocks now under consideration... | |
| Sir Charles Lyell - 1853 - 548 Seiten
...rocks." The beginner will easily conceive that the influence of subterranean heat may extend downwards from the crater of every active volcano to a great...or rather must be, distinct ; so that volcanic and plutonio rocks, each different in texture, and sometimes even in composition, may originate simultaneously,... | |
| |