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- W2022376002 abstract "Holocene estuarine deposits up to 21 m. in thickness, which were encountered in boreholes and excavations at Fawley, partly fill the south-western side of the drowned valley of Southampton Water. Saltmarsh clays with peat lie above and below tidal-flat clays of Atlantic age. The mollusc, foraminifera and ostracod faunas and the coccolith and diatom floras of these Holocene deposits are discussed. Gravels of Calshot Spit are interbedded with these sediments to a depth which suggests the existence of the spit in Atlantic times or earlier. The spit has deflected the deep tidal channel eastwards and has protected the south-western borders of the estuary from erosion. In the northern part of Southampton Water, late Holocene estuarine beds transgress northward over Holocene freshwater sediments. Much of the thick estuarine sequence at Fawley corresponds in age to a thin freshwater succession in the north." @default.
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- W2022376002 date "1972-01-01" @default.
- W2022376002 modified "2023-09-26" @default.
- W2022376002 title "Holocene deposits of Fawley, Hampshire, and the Development of Southampton Water" @default.
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- W2022376002 doi "https://doi.org/10.1016/s0016-7878(72)80015-4" @default.
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