1943
DOI: 10.2307/2256783
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Studies on the Biology of the Bristol Channel: XI. The Physical Environment and Intertidal Fauna of the Southern Shores of the Bristol Channel and Severn Estuary

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Cited by 51 publications
(23 citation statements)
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“…At neap-tides the amount of water entering is less, and so the amount of water forced into the lagoon at springs can run out and so produce lower levels, reaching a minimum a day or so after the smallest neap-tide. A similar phenomenon has been recorded by Bassindale (1943) as occurring in the narrower reaches of the Severn estuary.…”
Section: Downloaded By [Monash University Library] At 23:08 02 Februasupporting
confidence: 83%
“…At neap-tides the amount of water entering is less, and so the amount of water forced into the lagoon at springs can run out and so produce lower levels, reaching a minimum a day or so after the smallest neap-tide. A similar phenomenon has been recorded by Bassindale (1943) as occurring in the narrower reaches of the Severn estuary.…”
Section: Downloaded By [Monash University Library] At 23:08 02 Februasupporting
confidence: 83%
“…Mr G. I. Crawford has sent me material from the British Museum, including samples collected by himself after leaving Plymouth; his earlier collections (see Crawford, 1936Crawford, , 1937 were available for examination at the Plymouth Laboratory. Mr R. Bassindale's interesting series of samples from the Severn Estuary has already been recorded and commented on in the ' Studies on the Biologyof the Bristol Channel' publications (Bassindale,1941(Bassindale, , 1942a(Bassindale, , 1942b(Bassindale, ,1943.Prof. Hobson's material included collections from the Inner Hebrides, from streams flowing on to the shore, of which an account is published by Beadle & Cragg (1940).…”
Section: Speciesmentioning
confidence: 99%
“…1). Sand dunes on this part of the Severn coast are limited to a five and a Bassindale, 1943) showing the location of the transect site marked by an: X half mile stretch facing west between Burnham-on-Sea and Brean down. The Berrow dunes are located at the southern end of this dune coast line, and here they are most extensively developed, forming parallel ridges of up to half a mile in width (HopeSimpson & Willis, 1955).…”
Section: Description Of Sitementioning
confidence: 99%