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- W2612597966 abstract "This chapter looks at how a relatively rising, constant, or falling sea level threatens to destroy a prehistoric deposit, and under what immediately local conditions it is likely to survive in a way that preserves information, preferably in the context of its terrestrial landscape, which can be interpreted by archaeologists. It addresses the generic problem of how some prehistoric sites and remains on the sea floor are preserved through the vicissitudes of inundation by transgressing surf and subsequent submergence, and why others are destroyed. The chapter further considers the timescale which would embrace a stadial oscillation within a glacial cycle, a Dansgaard-Oeschger (D-O) event, or the deglaciation since the Last Glacial Maximum (LGM), in terms of how coastal and other marine processes might preserve or destroy anthropogenic material and terrestrial landscapes. It also considers to what extent these defensive barriers and protective shields can be destroyed on a longer timescale." @default.
- W2612597966 created "2017-05-19" @default.
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- W2612597966 date "2017-05-12" @default.
- W2612597966 modified "2023-09-26" @default.
- W2612597966 title "Non‐Cultural Processes of Site Formation, Preservation and Destruction" @default.
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- W2612597966 doi "https://doi.org/10.1002/9781118927823.ch3" @default.
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