The Geology of the Country Around Oxford
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In our eReader you can find the full English version of the book. Read The Geology of the Country Around Oxford 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 The Geology of the Country Around Oxford
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Geol. Soc. , Ixiii. , 1907, p. 30, and Proc. Geol. Assoc. , xx. , 185.
2 These were identified in the Paleeontological Department of the Geological Survey.
CORALLIAN. AMPTHILL CLAY. 45 Portland outlier on Rids Hill, east of Brill. Applying these data to the west side, it is found that at about the same distance below the Portland Sands of Muswell Hill, there is a very marked feature where water oozes freely from the clay. There is evidently a water-bearing stratum, and though it may not be the ...cement-stone bed of Brill brick-pit, it is at nearly the same horizon. The foot of this slope has accordingly been taken as the boundary of the Ampthill and Kimeridge Clays. Further south the features become indistinct, and the thickness of the two clays, judging from their vertical and horizontal extent, is much reduced. This apparent irregularity may, however, be due to the greater inclination of the strata or to a small fault of which evidence could not be obtained. The physical features no longer serve as guide, owing probably to the inconstancy of the hard bands in the clay.
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You can find similar books in the "Read Also" column, or choose other free books by Theodore Innes Pocock to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
Geol. Soc. , Ixiii. , 1907, p. 30, and Proc. Geol. Assoc. , xx. , 185.
2 These were identified in the Paleeontological Department of the Geological Survey.
CORALLIAN. AMPTHILL CLAY. 45 Portland outlier on Rids Hill, east of Brill. Applying these data to the west side, it is found that at about the same distance below the Portland Sands of Muswell Hill, there is a very marked feature where water oozes freely from the clay. There is evidently a water-bearing stratum, and though it may not be the ...cement-stone bed of Brill brick-pit, it is at nearly the same horizon. The foot of this slope has accordingly been taken as the boundary of the Ampthill and Kimeridge Clays. Further south the features become indistinct, and the thickness of the two clays, judging from their vertical and horizontal extent, is much reduced. This apparent irregularity may, however, be due to the greater inclination of the strata or to a small fault of which evidence could not be obtained. The physical features no longer serve as guide, owing probably to the inconstancy of the hard bands in the clay.
What to read after The Geology of the Country Around Oxford?
You can find similar books in the "Read Also" column, or choose other free books by Theodore Innes Pocock to read onlineMoreLess
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