| 词条 | Cerro Deslinde |
| 释义 |
Deslinde was glaciated during the Pleistocene, with moraines occurring at elevations of {{convert|4200|m}}.[2] South of Deslinde, a long glacier developed and spread westward.[4] References1. ^1 {{cite journal|last1=Kull|first1=Christoph|last2=Grosjean|first2=Martin|title=Late Pleistocene climate conditions in the north Chilean Andes drawn from a climate–glacier model|journal=Journal of Glaciology|date=2000|volume=46|issue=155|pages=622–632|doi=10.3189/172756500781832611|url=https://www.cambridge.org/core/journals/journal-of-glaciology/article/late-pleistocene-climate-conditions-in-the-north-chilean-andes-drawn-from-a-climateglacier-model/95B673B447E8158D9EE8144D3BCC95B1|ref=harv|issn=0022-1430}} [1][2]2. ^1 2 {{Cite journal|via=http://www.atmos.albany.edu/facstaff/mathias/pubs/Messerli_et_al_1992.pdf|last=Messerli|first=Bruno|last2=Grosjean|first2=Martin|last3=Graf|first3=Kurt|last4=Schotterer|first4=Ueli|last5=Schreier|first5=Hans|last6=Vuille|first6=Mathias|date=1992|title=Die Veränderungen von Klima und Umwelt in der Region Atacama (Nordchile) seit der Letzten Kaltzeit (Climate and Environmental Change in the Atacama Region (Northern Chile) since the Last Cold Maximum)|jstor=25646405|journal=Erdkunde|volume=46|issue=3/4|pages=257–272|doi=10.2307/25646405}} }}{{Volcanology-stub}}{{Chile-geo-stub}} 2 : Volcanoes of Chile|Mountains of Chile |
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