Morphodynamic evolution in recent deglaciated high mountain areas: The case of the Veleta Cirque, Sierra Nevada. Consequence of climate change?
Dead ice and alpine permafrost in the Veleta cirque are remnants of the environmental conditions during the Little Ice Age (15th to 19th century). Topographic control and thermal monitoring of the Veleta cirque rock glacier indicate the degradation of dead ice and discontinuous permafrost since 2001...
Main Authors: | , , , , , |
---|---|
Format: | Article in Journal/Newspaper |
Language: | Spanish |
Published: |
Universitat de Barcelona
2008
|
Subjects: | |
Online Access: | https://redib.org/Record/oai_articulo1412870-evolución-morfodinámica-de-un-enclave-montañoso-recién-deglaciado-el-caso-del-corral-del-veleta-sierra-nevada-¿consecuencia-del-cambio-climático |