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BRACKLESHAM BEDS
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Source
Encyclopaedia Britannica (1911) / britannica_1911
License
public_domain
Chunk ID
1911:bracklesham beds:542ed6813b89
Section
Hash Algorithm
sha256
Stored Hash
15c7de7551680763a77ac094d2bb651de9fc4d4743220527726daf459864855e
Computed Hash
15c7de7551680763a77ac094d2bb651de9fc4d4743220527726daf459864855e
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ggnorm 1.0
Observed
2026-02-08 18:42:39
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Verified Text
bracklesham beds, in geology, a series of clays and marls, with sandy and lignitic beds, in the middle eocene of the hampshire basin, england. they are well developed in the isle of wight and on the mainland opposite; and receive their name from their occurrence at bracklesham in sussex. the thickness of the deposit is from 100 to 400 ft. fossil mollusca are abundant, and fossil fish are to be found, as well as the _palaeophis_, a sea-snake. nummulites and other foraminifera also occur. the bracklesham beds lie between the barton clay above and the bournemouth beds, lower bagshot, below. in the london basin these beds are represented only by thin sandy clays in the middle bagshot group. in the paris basin the "calcaire grossier" lies upon the same geological horizon. see f. dixon, _geology of sussex_ (new ed., 1878); f.e. edwards and s.v. wood, "monograph of eocene mollusca," _palaeontographical soc._ vol. i. (1847-1877); "geology of the isle of wight," _mem. geol. survey_ (2nd ed., 1889); c. reid, "the geology of the country around southampton," _mem. geol. survey_ (1902).