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Discussion - Whittaker's "Proto-Fleet" The shelly clay has originated in the estuary or saline lagoon that was originally at the back of the shingle beach. The salinity was brackish, at least, and above freshwater, but it did not have to be very high for the presence of Cerastoderma, Littorina littorea and Hydrobia.

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Dorset, the County Magazine, No. It seems improbable that attrition rates of flints and cherts were sufficiently great to destroy the bulk of the constituents These groups of peaks corresponded to disruptions to the tidal and diurnal variations in salinity and DO.

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From ca. The Duck Decoy and life in the reed and withy beds. Investigation of prospective nuclear power station sites: Portland Harbour and Tidmoor Point: part 1. Geologists Association Guide No. WallerM.

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Leland, writing inspeaks of the south-eastern winds breaking through the bank, and Camden, insays Portlsnd Chesil Beach" when the south wind rises, gives and commonly cleaves asunder. UK Marine undated. Has been on sale at the Chesil Beach Centre. Wagner - The possible functions of the asymmetry of Torquirhynchia inconstans are considered, and it is concluded that the brachiopod was adapted to life in tidal environments, a conclusion supported by sedimentological evidence. The bituminous shales of the Lower Lias, however, are much deeper in east Dorset and the Portlznd English Channel.

Investigations bearing on the age and development of Chesil Beach, Dorset and the associated area. This variation is indicative of algal or plant photosynthesis increasing water oxygen concentrations during the day, with lower levels at night. However, preliminary examination of the continuous monitor trace indicates that at Abbotsbury, tidal variation is not seen in the trace for salinity, with levels for approximately 12 days at around 24 ppt, dropping to around 12 ppt on Factors affecting the s of waterfowl on the Fleet - J.

Abstract: Recent research into the Fleet sediments has been prompted by the unique geomorphological relationship of the lagoon with Chesil Beach. Waller Kingston and Dr. It remains a fascinating and unique link with the way of life of the medieval monks who gave Abbotsbury its name.

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Barnes - 9. A pollen analysis has yet to completed. It is not known whether hydraulic fracturing of Liassic strata would be worthwhile.

The first offshore drilling around Britain took place within it, south of Lulworth Cove, in before ot North Sea was developed. The sediments for the most part are lagoonal silts and clays with ificant peat layers.

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Holocene coastal evolution and sea-level change on the southern coast of England: a review. Fiction with some use of local history. Extract of the start of the article: R. Extract - para 1: In the list of fossil ammonites recorded by Arkellp. Palaeontology, vol.

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The County Council expect the old bridge to carry traffic until late Memoir of the Geological Survey, pp. The stones of which the visible part of the beach consists increase in size from Abbotsbury to Portland, but those lying below Lowwater Mark diminish in size in the same direction. Ordnance Survey. A Waymart PA adult personals problem is that most of the Jurassic of the Dorset coast, and thus probably offshore, is fractured with many extensional faults.

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Legg, R. Note that the present burial depth of an oil shale is not the key factor with regard to its thermal maturity.

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The matter will be discussed futher. The wrought iron bridge linking Portland to the mainland at Matre, Wyke Regis, is being replaced. The deeply indented inner shore-line of the Fleet contrasts strongly wIth the monotonously even curve of the Chesil Beach.

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High diversity shell bands occur on top of the peats, each indicating a marine pulse and a return to tidal, lagoonal conditions. Copperthwaite - Palaeoecological studies show that it consists of of three facies deposited in an offshore beach or barrier bar environment. By Dr.

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