Glamorganshire
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In our eReader you can find the full English version of the book. Read Glamorganshire 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 Glamorganshire
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As one travels westward the thickness of the Lias in- creases. The total depth in the district round Newport is only about 30 feet, at Penarth and Lavernock the deposits attain a thickness of about 130 feet, but in the neighbour- hood of Aberthaw they reach several hundred feet.
Section of the Lower Lias at Lavernock GEOLOGY AND SOIL 27 Generally speaking, the deposits consist of layers of blue or blue-grey argillaceous limestone alternating with blue, white, or yellowish shales and clays, the ...blue shales often containing notable quantities of iron pyrites. In the east the clays and shales predominate and the deposits attain their most aluminous character ; westward they become more siliceous and also more calcareous, the beds of stone greatly predominating.
Surface deposits of alluvial matter occur at the estuaries of all the rivers and along the valleys of the Nedd and Tawe. Extensive tracts of marshy land have been formed between the mouth of the Rhymney and Penarth Head, and at the foot of the hills in the neighbourhood of Aberavon.
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You can find similar books in the "Read Also" column, or choose other free books by Joseph Henry Wade to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
As one travels westward the thickness of the Lias in- creases. The total depth in the district round Newport is only about 30 feet, at Penarth and Lavernock the deposits attain a thickness of about 130 feet, but in the neighbour- hood of Aberthaw they reach several hundred feet.
Section of the Lower Lias at Lavernock GEOLOGY AND SOIL 27 Generally speaking, the deposits consist of layers of blue or blue-grey argillaceous limestone alternating with blue, white, or yellowish shales and clays, the ...blue shales often containing notable quantities of iron pyrites. In the east the clays and shales predominate and the deposits attain their most aluminous character ; westward they become more siliceous and also more calcareous, the beds of stone greatly predominating.
Surface deposits of alluvial matter occur at the estuaries of all the rivers and along the valleys of the Nedd and Tawe. Extensive tracts of marshy land have been formed between the mouth of the Rhymney and Penarth Head, and at the foot of the hills in the neighbourhood of Aberavon.
What to read after Glamorganshire?
You can find similar books in the "Read Also" column, or choose other free books by Joseph Henry Wade to read onlineMoreLess
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