HEINE, K (1994) PRESENT AND PAST GEOCRYOGENIC PROCESSES IN MEXICO. PERMAFROST AND PERIGLACIAL PROCESSES, 5 (1). pp. 1-12. ISSN 1045-6740,
Full text not available from this repository.Abstract
Periglacial processes and landforms are described from the Cordillera Neovolcanica of central Mexico. Inactive rock glaciers are related to different late-glacial and Holocene phases of permafrost conditions. Active discontinuous permafrost occurs above c. 4600 m ASL and appears to be from the Little Ice Age. The lower limit of late-glacial rock glaciers is situated 500 and 600 m lower than during the Little Ice Age.
| Item Type: | Article |
|---|---|
| Uncontrolled Keywords: | ; PERIGLACIAL PHENOMENA; PERMAFROST; ROCK GLACIERS |
| Depositing User: | Dr. Gernot Deinzer |
| Last Modified: | 19 Oct 2022 08:40 |
| URI: | https://pred.uni-regensburg.de/id/eprint/53388 |
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