Abstract
The Andes form one of the world's great mountain ranges, and the extreme altitudinal, latitudinal and climatic variability of the Chilean Andes provides the setting for a remarkable range of glacial environments. During the Quaternary, glacier advance and recession have reflected variations in important climatic systems such as the southern westerlies and South American Summer Monsoon. As a result, Chile has assumed considerable importance as a location where the patterns and timing of Southern Hemisphere climatic events can be reconstructed, and where models of global climate change can be tested.
| Original language | English |
|---|---|
| Pages (from-to) | 739-756 |
| Number of pages | 18 |
| Journal | Developments in Quaternary Science |
| Volume | 15 |
| DOIs | |
| Publication status | Published - 2011 |
Keywords
- Chile
- Glaciation
- Quaternary
- Southern Hemisphere