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Encyclopedia > Ipswichian interglacial

The Ipswichian interglacial is a name for an interglacial period which occurred between 150,000 and 115,000 years ago. The name is used by British geologists and archaeologists who named it after the town of Ipswich in the English county of Suffolk where some of the deposits it created were first found.


It is a Pleistocene stage of the Quaternary period and is analogous to the Sangamon interglacial in North America, the Eemain interglacial in northern Europe and the Riss-Würm interglacial in the Alps. It was a warm period and its deposits directly overlie material from the preceding wolstonian glaciation and lie beneath those from the following Devensian glaciation


Mousterian flint tools have been found in Ipswichian deposits. .


  Results from FactBites:
 
Eemian interglacial - Encyclopedia, History, Geography and Biography (581 words)
The Eemian interglacial era (known as the Sangamon interglacial in North America, the Ipswichian interglacial in the UK, and the Riss-Würm interglacial in the Alps) is the second-to-latest interglacial era of the Ice Age.
Changes in orbital parameters from today (greater obliquity and eccentricity, and perihelion), known as the Milankovitch cycle, probably led to greater seasonal temperature variations in the Northern Hemisphere, although global annual means temperatures were probably similar to those of the Holocene.
Eemian interglacial, Sea level, Ipswichian interglacial, See also, References, Glaciology, History of climate and Periods and stages in archaeology.
Quaternary Palaeoenvironments Group (QPG) » Controls on interglacial sedimentation (2435 words)
Interglacial fluvial sediment sequences are common in lowland Britain where their palaeontology has been considerably studied but their sedimentology is poorly known.
The utility of using Holocene sequences as analogues for previous interglacial sedimentation is discussed and an attempt is made to explain the proposed four-phase pattern in terms of predictable fluvial responses to an interglacial climate cycle.
Although interglacial fluvial sediments have been studied in detail, in particular to understand their stratigraphical significance for subdivision of fluvial and related sequences in general, most of the research has been undertaken by palaeontologists.
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