Geology of Clydesdale And Arran Embracing Also the Marine Zoology And the Flor
Geology of Clydesdale And Arran Embracing Also the Marine Zoology And the Flor
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In our eReader you can find the full English version of the book. Read Geology of Clydesdale And Arran Embracing Also the Marine Zoology And the Flor 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 Geology of Clydesdale And Arran Embracing Also the Marine Zoology And the Flor
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To quickly assess the difficulty of the text, read a short excerpt:
f The sandstone is so much altered by the dikes which here traverse it that the species cannot be exactly determined.
132 masses of sandstone. These fell about 100 years ago with a loud noise heard in Bute and Argyll. The debacle is more extensive than that of the Fallen Rocks, but inferior in grandeur. It was produced by a landslip of the mountain side, the traces of which yet remain in a long deep rent near the summit. Scrambling for a long way among the fallen masses, we reach an open shingl...y beach, along which the line of the old slate advancing from the interior, striken the shore, and cuts off the red sandstone ; but the nature of the ground does not permit the junction to be seen. The slate here dips about S. E, at 40. The change takes place near a glen, with a burn, called Alt-Mhor (large burn. ) The variety called chlorite slate occurs here, and quartz abounds in veins and beds in the slate.
91. A short distance forward, at Newton point, where the coast bends round into Loch Ranza, and a small stream, called Alt-Beith (birch burn)> enters the sea, there occurs one of the most instruc- tive sections to be seen in Arran.
What to read after Geology of Clydesdale And Arran Embracing Also the Marine Zoology And the Flor?
You can find similar books in the "Read Also" column, or choose other free books by James Bryce Bryce to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
f The sandstone is so much altered by the dikes which here traverse it that the species cannot be exactly determined.
132 masses of sandstone. These fell about 100 years ago with a loud noise heard in Bute and Argyll. The debacle is more extensive than that of the Fallen Rocks, but inferior in grandeur. It was produced by a landslip of the mountain side, the traces of which yet remain in a long deep rent near the summit. Scrambling for a long way among the fallen masses, we reach an open shingl...y beach, along which the line of the old slate advancing from the interior, striken the shore, and cuts off the red sandstone ; but the nature of the ground does not permit the junction to be seen. The slate here dips about S. E, at 40. The change takes place near a glen, with a burn, called Alt-Mhor (large burn. ) The variety called chlorite slate occurs here, and quartz abounds in veins and beds in the slate.
91. A short distance forward, at Newton point, where the coast bends round into Loch Ranza, and a small stream, called Alt-Beith (birch burn)> enters the sea, there occurs one of the most instruc- tive sections to be seen in Arran.
What to read after Geology of Clydesdale And Arran Embracing Also the Marine Zoology And the Flor?
You can find similar books in the "Read Also" column, or choose other free books by James Bryce Bryce to read onlineMoreLess
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