The Student's Handbook of Physical Geology

Cover The Student's Handbook of Physical Geology
The Student's Handbook of Physical Geology
A J Alfred John Jukes Browne
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p. 423. The successive depths at which turf beds occurred were 95, 155, 275, and 410 feet.
198 PROCESSES OF BECON8TBUCTION. [SEC. II.
way, all other parts within some miles of the shore having a> sandy bottom.
In the English channel there is nothing to be found but sand, often mixed with stones or gravel ; but opposite the mouth of the Bristol Channel there is a large, irregular patch of mud, stretching between the Scilly Islands and the coast of Wexford. This is at the bottom of water- varying
... from 40 to 60 fathoms in depth, and it is entirely surrounded by rather shallower water, the bottom of which is marked as sand. Another larger area of mud com* mences farther west, where the depth increases to 60 or 70 fathoms, and this leads out by a narrow lane of 80 fathoms towards the oozy bottom of the deep Atlantic.
In the Irish Sea, half-way between the coasts of Wexford and Cardigan, there is a considerable area of mud in water of 50 to 60 fathoms' depth, and another small one between Bray Head and Holyh^ui, in a hollow varying from 60 to 86 fathoms, surrounded by sandy ground of 20 to 30 fathoms only.


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