V.—Observations on the Sequence of the Glacial Beds
- 1 February 1870
- journal article
- research article
- Published by Cambridge University Press (CUP) in Geological Magazine
- Vol. 7 (68) , 61-68
- https://doi.org/10.1017/s0016756800209242
Abstract
Turning now to the physical evidence, it is well known that the Moel Tryfaen bed is 1390 feet above the sea-level; and a depression which would bring the sea up to that point would, unless we suppose a great change in the relative elevations, place the Chalk many hundreds of feet beneath the sea.Keywords
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