Termination (geomorphology)
id:
termination-geomorphology-268-10710040
title:
Termination (geomorphology)
text:
Termination, as used by Quaternary geologists, oceanographers, and paleoclimatologists is the period of time during a glacial cycle when there is a relatively rapid transition from full glacial climates to full interglacial climates. For the Quaternary period, terminations are numbered using Roman numerals from the most recent termination as “I” and with increasing value, e.g. “II”, “III”, and so forth, into the past. Termination I, also known as the Last Glacial Termination, is the end of Marin
brand slug:
wiki
category slug:
encyclopedia
description:
Transition period from full glacial to full interglacial climates in the glacial cycle
original url:
https://en.wikipedia.org/wiki/Termination_(geomorphology)
date created:
date modified:
2023-10-01T12:07:18Z
main entity:
{"identifier":"Q23582432","url":"https://www.wikidata.org/entity/Q23582432"}
image:
fields total:
13
integrity:
14