... limestone districts, but without a trace of stalagmite or fossil of any kind. The 32 feet next below were occupied with similar materials, with the addition of a considerable quantity of tough, dark, unctuous clay. Between this mass and the outer... Geological Magazine - Página 399editado por - 1877Vista completa - Acerca de este libro
| Henry Woodward - 1877 - 642 páginas
...limestone districts, but without a trace of stalagmite or fossil of any kind. The 32 feet next below were occupied with similar materials, with the addition...mentioned. The bones the caverns yielded were all found within these 32 feet ; and were met with equally in the loose and the coherent breccia, as well... | |
| British Association for the Advancement of Science. Meeting - 1878 - 766 páginas
...limestone districts, but without a trace of stalagmite or fossil of any kind. The 32 feet next below were occupied with similar materials, with the addition...stalagmite, usually about 2 feet thick, and containing, at \>y no means wide intervals, firmly cemented masses of breccia identical in composition with the adjacent... | |
| British Association for the Advancement of Science. Meeting - 1878 - 722 páginas
...limestone districts, but without a trace of stalagmite or fossil of any kind. The 32 feet next below were occupied with similar materials, with the addition...plate of stalagmite, usually about 2 feet thick, and containiug, at by no means wide intervals, firmly cemented masses of breccia identical in composition... | |
| Sir Norman Lockyer - 1877 - 598 páginas
...limestone districts, but without a trace of stalagmite or fossil of any kind. The 32 feet next below were occupied with similar materials, with the addition...with the adjacent bed just mentioned. The bones the cavern yielded were all found within these 32 feet ; and were met with equally in the loose and the... | |
| 1877 - 1060 páginas
...districts, but without a trace of stalagmite or fossil of any kind. The thirty-two feet next below were occupied with similar materials, with the addition...nearly vertical plate of stalagmite, usually about two feet thick, and containing, at by no means wide intervals, firmly cemented masses of breccia identical... | |
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