The Pleistocene Moraine Stages of West-Central Peru

Abstract Detailed field mapping in three massifs of the central Andes of Peru indicates that there are four glacial moraine stages. Historical evidence and correlation with Patagonia and South Georgia suggest that the three youngest stages relate to Neoglacial re-advances which culminated before 400...

Full description

Bibliographic Details
Published in:Journal of Glaciology
Main Author: Clapperton, Chalmers M.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1972
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000022243
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000022243
id crcambridgeupr:10.1017/s0022143000022243
record_format openpolar
spelling crcambridgeupr:10.1017/s0022143000022243 2024-03-03T08:46:07+00:00 The Pleistocene Moraine Stages of West-Central Peru Clapperton, Chalmers M. 1972 http://dx.doi.org/10.1017/s0022143000022243 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000022243 en eng Cambridge University Press (CUP) Journal of Glaciology volume 11, issue 62, page 255-263 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1972 crcambridgeupr https://doi.org/10.1017/s0022143000022243 2024-02-08T08:32:56Z Abstract Detailed field mapping in three massifs of the central Andes of Peru indicates that there are four glacial moraine stages. Historical evidence and correlation with Patagonia and South Georgia suggest that the three youngest stages relate to Neoglacial re-advances which culminated before 4000 b.p., between a.d. 1750 and 1800 and during the late nineteenth century. The oldest moraine stage may be of late Wisconsin/Weichselian age. The absence of older moraines suggests that the Peruvian Andes were not high enough earlier in the Pleistocene to support larger glaciers. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Patagonia Journal of Glaciology 11 62 255 263
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Clapperton, Chalmers M.
The Pleistocene Moraine Stages of West-Central Peru
topic_facet Earth-Surface Processes
description Abstract Detailed field mapping in three massifs of the central Andes of Peru indicates that there are four glacial moraine stages. Historical evidence and correlation with Patagonia and South Georgia suggest that the three youngest stages relate to Neoglacial re-advances which culminated before 4000 b.p., between a.d. 1750 and 1800 and during the late nineteenth century. The oldest moraine stage may be of late Wisconsin/Weichselian age. The absence of older moraines suggests that the Peruvian Andes were not high enough earlier in the Pleistocene to support larger glaciers.
format Article in Journal/Newspaper
author Clapperton, Chalmers M.
author_facet Clapperton, Chalmers M.
author_sort Clapperton, Chalmers M.
title The Pleistocene Moraine Stages of West-Central Peru
title_short The Pleistocene Moraine Stages of West-Central Peru
title_full The Pleistocene Moraine Stages of West-Central Peru
title_fullStr The Pleistocene Moraine Stages of West-Central Peru
title_full_unstemmed The Pleistocene Moraine Stages of West-Central Peru
title_sort pleistocene moraine stages of west-central peru
publisher Cambridge University Press (CUP)
publishDate 1972
url http://dx.doi.org/10.1017/s0022143000022243
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000022243
geographic Patagonia
geographic_facet Patagonia
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 11, issue 62, page 255-263
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000022243
container_title Journal of Glaciology
container_volume 11
container_issue 62
container_start_page 255
op_container_end_page 263
_version_ 1792502028654608384