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Encyclopedia > Flandrian

The Flandrian interglacial or stage is the name given by geologists and archaeologists in the British Isles to the first, and so far only, stage of the Holocene, covering the period from around 10,000 years ago when the last ice age ended to the present day. As such, it is in practice identical in span to the Holocene. A geologist is a contributor to the science of geology. ... Archaeology or sometimes in American English archeology (from the Greek words αρχαίος = ancient and λόγος = word/speech) is the study of human cultures through the recovery, documentation and analysis of material remains, including architecture, artefacts, biofacts, human remains, and landscapes. ... British Isles is also an old name for the Great Britain, Great Britain Ireland The Isle of Man The Isle of Wight The Northern Isles, including Orkney, Shetland and Fair Isle The Hebrides, including the Inner Hebrides, Outer Hebrides and Small Isles Rockall The islands of the lower Firth of... The Holocene Epoch is a geologic period that extends from the present back about 10,000 radiocarbon years. ... Variations in CO2, temperature and dust from the Vostok ice core over the last 400 000 years For the animated movie, see Ice Age (movie). ...


It follows the Devensian glaciation, the last stage of the Pleistocene and is traditionally seen as the latest warm interglacial in a series that has been occurring throughout the Quaternary system. The Devensian glaciation is a name for an ice age period which occurred between 120,000 and 10,000 years ago. ... The Pleistocene epoch is part of the geologic timescale, usually dated as 1. ... Glaciation, often called an ice age, is a geological phenomenon in which massive ice sheets form in the Arctic and Antarctic and advance toward the equator. ... This article is about the geologic period. ...


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NYC Regional Geology (2144 words)
The name "Flandrian" has been applied to the current sea level rise affecting the coastal regions around the globe which began approximately 18,000-19,000 years ago (Stage 1 - beginning in latest Pleistocene time and continuing progressively through Holocene to the present).
This rise in sea level is directly related to the melting of the Wisconsin (Stage 2) continental polar and mountain piedmont glaciers.
During the following Flandrian transgression, sea level rise was very rapid early in the Late Pleistocene, but the rate of sea level rise has slowed drastically during the progress of the Holocene.
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