The New Encyclopaedia Britannica, Part 3, Volume 16Encyclopaedia Britannica, 1980 - Encyclopedias and dictionaries |
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Page 199
... Range ( G.D.O'B . ) slopes , is the lower . In the west and east , the Range divides into separate mountain masses , or massifs . West of Sakesar the course of the Range swings to the northwest , with low , longitudinal ranges . The ...
... Range ( G.D.O'B . ) slopes , is the lower . In the west and east , the Range divides into separate mountain masses , or massifs . West of Sakesar the course of the Range swings to the northwest , with low , longitudinal ranges . The ...
Page 200
... range , red laterites ( porous , claylike , iron - rich rocks ) are characteristic for the Upper Triassic deposits . Limestone layers in the eastern parts of the range contain more clay , and the overall thickness of the Triassic in ...
... range , red laterites ( porous , claylike , iron - rich rocks ) are characteristic for the Upper Triassic deposits . Limestone layers in the eastern parts of the range contain more clay , and the overall thickness of the Triassic in ...
Page 472
... range is extremely low , particularly among sediments that are silty and clayey only ; ( 3 ) radiolarian and ribbon cherts and siliceous shales are present ; ( 4 ) turbidites ( graded sediments ) , graded bedding , chaotic , and other ...
... range is extremely low , particularly among sediments that are silty and clayey only ; ( 3 ) radiolarian and ribbon cherts and siliceous shales are present ; ( 4 ) turbidites ( graded sediments ) , graded bedding , chaotic , and other ...
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