Beestonian stage

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The Beestonian Stage is an early Pleistocene stage in the geological history of the British Isles. It is named after Beeston Cliffs near West Runton in Norfolk where deposits from this stage are preserved.

The Beestonian precedes the

Marine isotope stages 22 to (60?).[1][2][3] The Beestonian Stage and Marine Isotope Stage 22 ended about 866,000 years ago.[4][5]

The Beestonian corresponds temporally to the

Alpine region. Based on finding in the Low Countries, the corresponding stage in northern continental Europe is divided into four stages, the Bavelian, Menapian, Waalian, and Eburonian.[6]

The Beestonian had also been equated to the

Nebraskan glaciation in North America. However, the Nebraskan Stage, along with the Kansan and Aftonian Stages, have been abandoned by North American Quaternary geologists and merged into the Pre-Illinoian Stage.[7][8] At this time, the Beestonian stage is correlated with the period of time, which includes the Pre-Illinoian F, Pre-Illinoian G, and Pre-Illinoian H glaciations of North America.[2][8]

See also

Historical names of the "four major" glacials in four regions.
Region Glacial 1 Glacial 2 Glacial 3 Glacial 4
Alps
Günz
Mindel Riss Würm
North Europe Eburonian
Elsterian
Saalian
Weichselian
British Isles Beestonian
Anglian
Wolstonian
Devensian
Midwest U.S. Nebraskan Kansan Illinoian
Wisconsinan
Historical names of interglacials.
Region Interglacial 1 Interglacial 2 Interglacial 3
Alps Günz-Mindel Mindel-Riss
Riss-Würm
North Europe Waalian Holsteinian
Eemian
British Isles Cromerian Hoxnian
Ipswichian
Midwest U.S. Aftonian
Yarmouthian
Sangamonian

References

Further reading

External links