 | Geological Survey of Canada - 1857 - 520 páginas
...the gneiss, but it is scarcely possible to know, from mere local inspection, whether any mass of the limestone in one part is equivalent to a certain mass in another. They all resemble one another more or less lithologically, and although masses are met with running for considerable distances rudely... | |
 | Geological Survey of Canada - 1857 - 520 páginas
...the gneiss, but it is scarcely possible to know, from mere local inspection, whether any mass of the limestone in one part is equivalent to a certain mass in another. They all resemble one another more or less lithologically, and although masses are met with running for considerable distances rudely... | |
 | Samuel Almond Miller - 1889 - 732 páginas
...attending it arise from the absence of fossils to characterize its different members. Bands of the crystalline limestone are easily distinguished from...met with, running for considerable distances rudely parellel with one another, it is scarcely ever safe to take for granted that they are stratigraphically... | |
 | Geological Survey (U.S.) - 1892 - 1336 páginas
...characterize its different members. Bands of crystalline limestones are easily distinguished from the bauds of gneiss, but it is scarcely possible to know from local...one part is equivalent to a certain mass in another part. They all resemble one another lithologically. The dips avail but little in tracing out the structure,... | |
 | Geological Society of America - 1893 - 550 páginas
...limestone are easily distinguished from bands of gneiss, but it is scarcely possible to know, from mere local inspection, whether any mass of limestone in...certain mass in another. They all resemble one another more or less lithologi'-allv, and although masses are met with, running fur considerable distances... | |
 | Geological Society of America - 1893 - 512 páginas
...limestone are easily distinguished from bands of gneiss, but. it is scarcely possible to know, from mere local inspection, whether any mass of limestone in one part is equivalent to a certain ma.«s in another. They all resemble one another more or Irss lithologically, and although masses are... | |
 | Charles Richard Van Hise, Charles Kenneth Leith - 1909 - 956 páginas
...character1/(' its dirtVivnt members. Bands of crystalline limestones are easily distinguished from the bands of gneiss, but it is scarcely possible to know from local...one Part is equivalent to a certain mass in another part. They all resem™< one another lithologically. The dips avail but little in tracing out 'he structure,... | |
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Bands of crystalline limestone are easily distinguished from bands of gneiss, but it is scarcely possible to know, from mere local inspection, whether any mass of limestone in one part is equivalent to a certain mass in another. They all resemble one... 