Skip to content
Norsk A A A

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.

 

Quaternary climate based on oxygen isotope stratigraphy

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.

 

profiltekstbilde
Prof. Atle Nesje teaching, 2009

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.

Read more

 

  • News
    ingressbilde

    New PhD - Ronghua Wang

    Friday 25. November 2011, Ronghua Wang defended her PhD-thesis at Department of Earth Science, University of Bergen

  • News
    ingressbilde

    New PhD - Herbjørn Presthus Heggen

    Friday 28. October 2011 Herbjørn Presthus Heggen defended his PhD-thesis at Department of Earth Science, University of Bergen

  • News
    ingressbilde

    New PhD - Kristian Vasskog

    Friday 21. October 2011 Kristian Vasskog defended his PhD-thesis at Department of Earth Science