The New Encyclopaedia Britannica, Volume 16Encyclopaedia Britannica, 1974 - Encyclopedias and dictionaries |
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Page 199
... Range ( G.D.O'B . ) The Salt Range is a range of hills and low mountains between the valleys of the Indus and Jhelum rivers in the northern part of the Punjab region of Pakistan . It de- rives its name from extensive deposits of rock ...
... Range ( G.D.O'B . ) The Salt Range is a range of hills and low mountains between the valleys of the Indus and Jhelum rivers in the northern part of the Punjab region of Pakistan . It de- rives its name from extensive deposits of rock ...
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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