GLACIATION LINKS

Updated June 2005


To have a glacial advance requires a change in the global temperature so as to lower the values over the majority of the Earth's surface (or at least one hemisphere). Milankovitch suggested a way in which the earth's orbit might change to bring this about.

Animations of the changes can also be seen at the SCOTESE site, which is Recommended. It also features (for example) the very useful diagram reproduced below which shows the fluctuations in the Earth's climate over the last hundreds of thousands of years which have swung between periods of warm and cold weather. Students have to get to grips with diagrams such as this, to appreciate that the weather conditions we are used to are not the 'norm'. We live in interesting times....

Image from http://www.scotese.com - click to enlarge

The Pleistocene Ice Age, the Ice and its Impact

Glaciers: their types, movements and economies

The Anatomy of a Valley Glacier

Glacial Erosion

Glacial Deposition and Depositional Landforms

Fluvioglacial Deposition

Human Activity and Glacial Movements

RETURN TO A2 COLD ENVIRONMENTS