Late Pleistocene to Holocene glacial, periglacial, and paraglacial geomorphology of the upper Río Limarí basin (30–31° S) in the Andes of central Chile-Reference-Cited by-同舟云学术

Late Pleistocene to Holocene glacial, periglacial, and paraglacial geomorphology of the upper Río Limarí basin (30–31° S) in the Andes of central Chile

Published:2024-04-12 Issue:1 Volume:20 Page:
ISSN:1744-5647
Container-title:Journal of Maps
language:en
Short-container-title:Journal of Maps

Author:

Carraha Javiera¹²,García Juan-Luis¹²,Nussbaumer Samuel U.³,Fernández-Navarro Hans⁴,Gärtner-Roer Isabelle³

Affiliation:

1. Instituto de Geografía, Facultad de Historia, Geografía y Ciencia Política, Pontificia Universidad Católica de Chile, Santiago, Chile

2. Centro UC Desierto de Atacama, Pontificia Universidad Católica de Chile, Santiago, Chile

3. Department of Geography, University of Zurich, Zurich, Switzerland

4. Instituto de Ciencias Agroalimentarias, Animales y Ambientales (ICA3), Universidad de O'Higgins, San Fernando, Chile

Publisher

Informa UK Limited

Link

https://www.tandfonline.com/doi/pdf/10.1080/17445647.2024.2329179

Reference77 articles.

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2. The effects of interannual climate variability on the moraine record

3. Glaciation of alpine valleys: The glacier – debris-covered glacier – rock glacier continuum

4. Anderson, R. S., & Anderson, S. P. (2010). Geomorphology: The mechanics and chemistry of landscapes. Cambridge University Press.

5. Hydrological and geomorphological significance of rock glaciers in the dry Andes, Chile (27°-33°S)

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