Bridgland, D. R. (2001). The Pleistocene evolution and Palaeolithic occupation of the Solent River. In: n.e. Palaeolithic archaeology of the Solent River:. 38--56 Orsman Road: Lithic Studies Society. pp. 15-25.
Title The title of the publication or report |
The Pleistocene evolution and Palaeolithic occupation of the Solent River | |||||||
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Issue The name of the volume or issue |
Palaeolithic archaeology of the Solent River: | |||||||
Series The series the publication or report is included in |
Lithic Studies Society Occasional Papers | |||||||
Volume Volume number and part |
7 | |||||||
Page Start/End The start and end page numbers. |
15 - 25 | |||||||
Biblio Note This is a Bibliographic record only. |
Please note that this is a bibliographic record only, as originally entered into the BIAB database. The ADS have no files for download, and unfortunately cannot advise further on where to access hard copy or digital versions. | |||||||
Publication Type The type of publication - report, monograph, journal article or chapter from a book |
MonographSeriesChapter | |||||||
Abstract The abstract describing the content of the publication or report |
the author describes the Solent system of Middle Pleistocene river terraces which now form the hinterland to the south coast, many of which contain Lower Palaeolithic artefacts, although these are absent from the older terraces pre-dating human occupation, and from the lowest terraces and valley-floor gravels contemporaneous with the disappearance of humans from Britain prior to the last interglacial. Only the last two interglacials are directly represented within the sedimentological sequences of the Solent and its tributaries, and the author proposes the use of other evidence to assess the ages of the higher terraces, including age indications provided by Palaeolithic archaeology. The paper explains that the first appearance of artefacts is thought likely to be around 600,000 years ago; then twisted ovates are prevalent in assemblages from OIS 11, suggesting that the Old Milton Gravel incorporates material of that age; and finally Levallois technique appears in the Taddiford Farm Gravel, thought by analogy with the Thames to date from around the OIS 9/8 transition. The Solent has more Middle Pleistocene terraces than other UK rivers, perhaps because rejuvenation has taken place twice during each climatic cycle. The author argues that the age indications from the archaeological data enable some attempt at modelling the formation of the terraces in response to both climate change and background uplift, although the results remain speculative | |||||||
Year of Publication The year the book, article or report was published |
2001 | |||||||
Locations Any locations covered by the publication or report. This is not the place the book or report was published. |
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Source Where the record has come from or which dataset it was orginally included in. |
BIAB
(The British & Irish Archaeological Bibliography (BIAB))
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Created Date The date the record of the pubication was first entered |
28 Jun 2006 |