Bulletin of the New York State Museum, Vydania 308–313University of the State of New York, 1937 |
Vyhľadávanie v obsahu knihy
Výsledky 1 - 3 z 79.
Strana 88
... evidence for any of this was found , except that the mountain stands out rather prominently in the surrounding country . The second largest fault in the Thirteenth Lake quadrangle extends for about seven miles in a northeast direction ...
... evidence for any of this was found , except that the mountain stands out rather prominently in the surrounding country . The second largest fault in the Thirteenth Lake quadrangle extends for about seven miles in a northeast direction ...
Strana 72
... evidence indicates that fault movements occurred at least once in Precambrian time before the intrusion of diabase , and occurred at least once after Utica time . There is no evidence which determines whether there have been more than ...
... evidence indicates that fault movements occurred at least once in Precambrian time before the intrusion of diabase , and occurred at least once after Utica time . There is no evidence which determines whether there have been more than ...
Strana 75
... evidence for this fault is more clear - cut than the physiographic evidence . In this case the mere presence of a large rectilinear valley can not be considered evidence of faulting , as the valley is crudely parallel to the strike of ...
... evidence for this fault is more clear - cut than the physiographic evidence . In this case the mere presence of a large rectilinear valley can not be considered evidence of faulting , as the valley is crudely parallel to the strike of ...
Obsah
GEOLOGY OF THE THIRTEENTH LAKE | 5 |
Precambrian Rocks | 14 |
Precambrian Rocks | 15 |
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Iné vydania - Zobraziť všetky
Časté výrazy a frázy
Adirondacks Albany albite Allegany amphibolite anorthosite apatite augite Balk biotite border cent color County Creek diabase east evidence facies fault feet feldspar ferromagnesian minerals Figure folds foliation gabbro garnet garnet deposit garnet gneiss Geol Geologist Geology glacial gneiss gneissic structure Gore mountain grains granite gray band Grenville rocks Grenville sediments Group hornblende hypersthene igneous rocks inches Indian intrusion joints labradorite labradorite crystals lenses limestone linear structure Lyon Mountain mafic magma magnetite masses metagabbro microcline microperthite miles Miller N. Y. Specimens N. Y. State Mus northeast northwest occur origin outcrops Paleozoic parallel Park pegmatite Piseco Piseco Lake plagioclase pond Precambrian pyroxene quartz syenite quartzite recrystallized region relation rims river Santa Clara Complex Santa Clara quadrangle scientific sills slope St Regis granite surface syenite and granite syenite-granite syncline thin section Thirteenth Lake quadrangle tion titanite valley York State Museum zone