The Rift Valleys Geology of Eastern Sinai
The Rift Valleys Geology of Eastern Sinai
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As though the difficulties connected with the superficial deposits were not sufficient, there occur in the lower part of Wadi Nasb, and especially close to its junction with Wadi Abuksheib, certain terraces resting on Nubian sand- stone and granite, containing boulders of syenite, biotite- gneiss, felsite, and red granite (often over one metre in diameter), cemented together by crystalline calcite in the form of well-developed scalenohedral crystals. The question of the source of the calcite wh...ich has acted as the cementing substance rises. In connection with other beds which appear in most unexpected places, viz. : \e. TRAVERTINE AND CONGLOMERATE CEMENTED BY TRAVERTINE.
The igneous hills are probably the last place in which one would expect to find deposits of the above character, but, subsequent to the first discovery by Mr. Skill of typical calcareous travertine of spongy texture lining the walls of a granite gully, or couloir, we frequently met with it in out-of-the-way valleys, either in similar positions or at the foot of precipitous steps, which would be waterfalls in time of rain.
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You can find similar books in the "Read Also" column, or choose other free books by W F William Fraser Hume to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
As though the difficulties connected with the superficial deposits were not sufficient, there occur in the lower part of Wadi Nasb, and especially close to its junction with Wadi Abuksheib, certain terraces resting on Nubian sand- stone and granite, containing boulders of syenite, biotite- gneiss, felsite, and red granite (often over one metre in diameter), cemented together by crystalline calcite in the form of well-developed scalenohedral crystals. The question of the source of the calcite wh...ich has acted as the cementing substance rises. In connection with other beds which appear in most unexpected places, viz. : \e. TRAVERTINE AND CONGLOMERATE CEMENTED BY TRAVERTINE.
The igneous hills are probably the last place in which one would expect to find deposits of the above character, but, subsequent to the first discovery by Mr. Skill of typical calcareous travertine of spongy texture lining the walls of a granite gully, or couloir, we frequently met with it in out-of-the-way valleys, either in similar positions or at the foot of precipitous steps, which would be waterfalls in time of rain.
What to read after The Rift Valleys Geology of Eastern Sinai?
You can find similar books in the "Read Also" column, or choose other free books by W F William Fraser Hume to read onlineMoreLess
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