Records of the Geological Survey of India
Records of the Geological Survey of India
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In our eReader you can find the full English version of the book. Read Records of the Geological Survey of India Online - link to read the book on full screen. Our eReader also allows you to upload and read Pdf, Txt, ePub and fb2 books. In the Mini eReder on the page below you can quickly view all pages of the book - Read Book Records of the Geological Survey of India
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As Rewil village is approached the valley becomes filled with stream deposits, and no more roches moulonneesare seen rising from it ; the northern side still rises steeply and the steep face shows, in places, signs of glaciation. These are seen conspicuously on the bridle-path which leads along the hillside between Kulan and Gagangir, and the trough shape of the lower part of the valley can be recognised as far as that village.
At Gagangir the slates give place to limestone, forming a narrow ba...nd, separated from the main mass of limestone to the north by a ridge composed of altered volcanic rocks, in the manner indicated in Mr. Lydekker's map. This ridge of volcanics forms a barrier across continuation of the Sind valley, which not only makes a bend in its general direction at this place, but also changes in form and char- acter. On the west side of the Song valley, joining the Sind just above Gagangir, the limestone ridge rises with a smooth and some- what rounded surface, which looks as if it might have been smoothed by a mighty glacier coming down the main valley.
What to read after Records of the Geological Survey of India?
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To quickly assess the difficulty of the text, read a short excerpt:
As Rewil village is approached the valley becomes filled with stream deposits, and no more roches moulonneesare seen rising from it ; the northern side still rises steeply and the steep face shows, in places, signs of glaciation. These are seen conspicuously on the bridle-path which leads along the hillside between Kulan and Gagangir, and the trough shape of the lower part of the valley can be recognised as far as that village.
At Gagangir the slates give place to limestone, forming a narrow ba...nd, separated from the main mass of limestone to the north by a ridge composed of altered volcanic rocks, in the manner indicated in Mr. Lydekker's map. This ridge of volcanics forms a barrier across continuation of the Sind valley, which not only makes a bend in its general direction at this place, but also changes in form and char- acter. On the west side of the Song valley, joining the Sind just above Gagangir, the limestone ridge rises with a smooth and some- what rounded surface, which looks as if it might have been smoothed by a mighty glacier coming down the main valley.
What to read after Records of the Geological Survey of India?
You can find similar books in the "Read Also" column, or choose other free books by Geological Survey of India to read onlineMoreLess
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