 Taking the country examined from south to north, Loch Broom was first described. Here the author considered there was clear proof of dislocation. Between the Torridon and the Caledonian there were several subparallel faults, which increased in throw from...  Geological Magazine - Seite 273herausgegeben von - 1883Vollansicht - Über dieses Buch
 | 1883 - 528 Seiten
...considered there was clear proof of dislocation. Between the Torridon and the Caledonian there were several subparallel faults, which increased in throw...discussed. The author described several sections which ho considered to prove that this baud was the ordinary quartzite repeated east of a great fault which... | |
 | Sir Norman Lockyer - 1877 - 848 Seiten
...formations into a series of folds, thro vn over towards the west, so as to cause a general1 easterly dip. In Assynt > the "Upper Quartzite" was first discussed....sections which he considered to prove that this band was the ordinary quartzite repeated east of a great fault, which brought up the Hebridean; in one place,... | |
 | 1881 - 484 Seiten
...considered there was clear proof of dislocation. Between the Torridon and the Caledonian there were several subparallel faults, which increased in throw...sections which he considered to prove that this band was the ordinary quartzite repeated east of a great fault, which brought up the Hebridean ; in one... | |
 | Henry Woodward - 1883 - 636 Seiten
...considered there was clear proof of dislocation. Between the Torridon and the Caledonian there were several subparallel faults, which increased in throw...through the dolomite, while still further east the Hebrideau was thrown up, the Caledonian appearing east of the Hebridean. This Hebridean was the " porphyry... | |
 | Sir Norman Lockyer - 1883 - 680 Seiten
...formations into a series of folds, thro.vn over towards the west, so as to cause a general easterly dip. In Assynt the "Upper Quartzite" was first discussed....sections which he considered to prove that this band was the ordinary quartzite repeated east of a great fault, which brought up the Hebridean ; in one... | |
 | 1883 - 502 Seiten
...considered there was clear proof of dislocation. Between the Torridon and the Caledonian there were several subparallel faults, which increased in throw...sections which he considered to prove that this band was the ordinary quartzite repeated east of a great fault which brought up the Hebridian, in one place... | |
 | 1883 - 526 Seiten
...considered there was clear proof of dislocation. Between the Torridon and the Caledonian there were several subparallel faults, which increased in throw...several sections which he considered to prove that this baud was the ordinary quartzite repeated east of a great fault which brought up the Hebridian, in one... | |
 | Sir Norman Lockyer - 1883 - 724 Seiten
...formations into a series of folds, thro*n over towards the west, so as to cause a general easterly dip. In Assynt the "Upper Quartzite" was first discussed....sections which he considered to prove that this band was the ordinary quartzite repeated east of a great fault, which brought up the Hebridean ; in one... | |
 | Sir Norman Lockyer - 1883 - 892 Seiten
...formations into a series of folds, thro-vn over towards the west, so as to cause a general easterly dip. In Assynt the "Upper Quartzite" was first discussed....sections which he considered to prove that this band was the ordinary quartzite repeated east of a great fault, which brought up the Hebridean ; in one... | |
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