The Quaternary
The Quaternary is the most recent period of the geological record, and covers the last 2.6 million years. It is often thought of as the 'Ice Age', however, although it's most distinctive feature is the repeated oscillations between cold (glacial) and warm (interglacial) states. The Earth is presently in an interglacial called the Holocene, which has lasted for about 11,500 years.
In a glacial landscape
Bergen is located at the coast of Western Norway in a landscape formed by glacial activity. The fjords are some of the most spectacular landforms, and are in principle drowned glacial eroded valleys. In Sognefjorden north of Bergen the glacial erosion removed nearly 3 km of rock, during the Quaternary.
2.6 million years of dramatic changes
The Research Group in Quaternary and Paleoclimate studies the geological history and the climatic shifts that caused the dramatic variations during the Quaternary (last 2.6 million years). Knowledge of the environmental changes that affected the Earth in the recent geological past is fundamental to our understanding of the modern world and for making predictions of the future. Research and education is based on a combination of field work and laboratory analyses using a wide spectrum of techniques and proxy data.
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News
New PhD - Ronghua Wang
Friday 25. November 2011, Ronghua Wang defended her PhD-thesis at Department of Earth Science, University of Bergen
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News
New PhD - Herbjørn Presthus Heggen
Friday 28. October 2011 Herbjørn Presthus Heggen defended his PhD-thesis at Department of Earth Science, University of Bergen
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News
New PhD - Kristian Vasskog
Friday 21. October 2011 Kristian Vasskog defended his PhD-thesis at Department of Earth Science
News
- New PhD - Ronghua Wang (16.12.2011)
- New PhD - Herbjørn Presthus Heggen (01.11.2011)
- New PhD - Kristian Vasskog (25.10.2011)
- New PhD - Eivind N. W. Støren (31.05.2011)
- New PhD - Rannveig Øvrevik Skoglund (22.01.2010)