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Books Bücher 1 - 4 von 4 in In a previous report f the writer grouped the Carboniferous and Devonian beds of...
" In a previous report f the writer grouped the Carboniferous and Devonian beds of the upper White and Tanana rivers together under the name Nutzotin series. This Nutzotin series would in a measure correspond to the subdivision called Upper Paleozoic on... "
United States Geological Survey Professional Paper - Seite 27
1902
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Bulletin of the Geological Society of America, Band 13

1902
...the south, where the Canadians have done some more or less detailed mapping. In a previous report f the writer grouped the Carboniferous and Devonian...called Upper Paleozoic on the accompanying map, but will probably also embrace a part, at least, of the argillites which lie adjacent to the Coast range....
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Professional Paper - United States Geological Survey

Geological Survey (U.S.) - 1902
...shown on the map. The more recent volcanic phenomena, so far as known, are limited to Mount Kdgecumbe, a volcano on Kruzof Island, just west of Sitka. CORRELATION....Coast Range. In the report cited the limestones of (Jlacier Bay were all put in the Nutzotin, as they were then believed to be Carboniferous. In the same...
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Bulletin of the Geological Society of America, Band 13

1902
...the south, where the Canadians have done some more or less detailed mapping. In a previous report f the writer grouped the Carboniferous and Devonian...called Upper Paleozoic on the accompanying map, but will probably also embrace a part, at least, of the argillites which lie adjacent to the Coast range....
Vollansicht - Über dieses Buch

Bulletin of the Geological Society of America, Band 13

Geological Society of America - 1902
...the south, where the Canadians have done some more or less detailed mapping. In a previous report f the writer grouped the Carboniferous and Devonian...called Upper Paleozoic on the accompanying map, but will probably also embrace a part, at least, of the argillites which lie adjacent to the Coast range....
Vollansicht - Über dieses Buch




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