dating

Morphostratigraphy

This article is taken from: Davies, B.J., 2022. CRYOSPHERIC GEOMORPHOLOGY: Dating Glacial Landforms I: archival, incremental, relative dating techniques and age-equivalent stratigraphic markers. (link) Introduction to relative dating Relative dating techniques aim to order landscape features. It assumes that moraines closer to the ice limit are usually assumed to be younger, and those further are […]

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Lichenometry

This article is taken from: Davies, B.J., 2022. CRYOSPHERIC GEOMORPHOLOGY: Dating Glacial Landforms I: archival, incremental, relative dating techniques and age-equivalent stratigraphic markers. (link) Dating boulder exposure age with lichens Lichenometry, mostly using the species Rhizocarpon subgenus Rhizocarpon, has been widely used to date Late Holocene (last ~1000 years) glacial landforms, including the Northern Hemisphere

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Cryospheric Geomorphology: Dating Glacial Landforms

This section draws on two book chaper publications by Bethan Davies. Authors accepted versions can be viewed below, along with the link to the published chapters. Not all dating methods are covered here; please refer to the published book chapters for more information. Archival, incremental and relative dating techniques Davies, B.J., 2022. 4.12: Dating Glacial

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Case study: In situ 14C exposure age dating in Antarctica

This page was written by Dr Keir Nichols, who is using 14C exposure age dating to unravel the past behaviour of the West Antarctic Ice Sheet (WAIS). Given that the ice sheets in Antarctica and Greenland contain enough water to raise global sea level by about 65 metres, it is important to understand how ice

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Cosmic Rays

What are cosmic rays? | The cosmic ray cascade | The cosmic ray intensity flux | Formation of cosmogenic nuclides | Further reading | Glossary | References | Comments | What are cosmic rays? Cosmic rays are high energy particles that flow into our solar system from outer space. They are essential for the production

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Case study: Quantifying ice sheet thinning using cosmogenic nuclide ages

By Richard Selwyn Jones, from the Antarctic Research Centre at Victoria University of Wellington. In this article, Richard describes his research and how he uses cosmogenic nuclide ages to estimate rates of ice sheet thinning in Antarctica. All images are copyright Richard Selwyn Jones. An Antarctic expedition to estimate ice sheet thinning Antarctica might seem

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Dating glacial environments

This section of the website introduces some of the very many different ways in which we can date glacial environments. These techniques have evolved through time, and different techniques are applied in different circumstances. For example, where organics are available, sediments can be dating using radiocarbon dating. This may be applied in glacial environments by,

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