Geomorphology of Las Derrumbadas dome complex, Puebla Mexico
This paper comprises a geomorphologic map of the Las Derrumbadas (LDR) volcanic complex in Mexico. The complex stretches over more than 285 km2, the stratigraphic column encompasses a range age from Cretacious to Quaternary. The methodology used involved the analysis of digital morphometric models,...
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Online Access: | http://dx.doi.org/10.1080/17445647.2019.1650839 |
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doaj-c39751ea14e04a57a2053ee3c1713d412020-11-25T04:03:49ZengTaylor & Francis GroupJournal of Maps1744-56472019-07-0115260161010.1080/17445647.2019.16508391650839Geomorphology of Las Derrumbadas dome complex, Puebla MexicoJ. A. Muñiz-Jáuregui0C. S. Guzmán-Cervantes1V. H. Garduño-Monroy2A. Jiménez-Haro3P. Layer4Cátedras CONACYT, Instituto de Investigaciones en Ciencias de la Tierra, Universidad Michoacana de San Nicolás de HidalgoCentro Mexicano de Innovación en Energía Geotérmica, Proyecto 17 (CeMIE Geo P17), Universidad Michoacana de San Nicolás de HidalgoCentro Mexicano de Innovación en Energía Geotérmica, Proyecto 17 (CeMIE Geo P17), Universidad Michoacana de San Nicolás de HidalgoCentro Mexicano de Innovación en Energía Geotérmica, Proyecto 17 (CeMIE Geo P17), Universidad Michoacana de San Nicolás de HidalgoDepartment of Geology and Geophysics, University of Alaska FairbanksThis paper comprises a geomorphologic map of the Las Derrumbadas (LDR) volcanic complex in Mexico. The complex stretches over more than 285 km2, the stratigraphic column encompasses a range age from Cretacious to Quaternary. The methodology used involved the analysis of digital morphometric models, satellite imagery and absolute datings. The result is a 1:40,000 scale map, which is divided into two large geomorphologic groups in terms of the dominant processes: exogenic and endogenic This, in turn, are divided into various subgroups representing the morphological complexity of the study area, principally related to volcanic processes and their coherence with slope processes.http://dx.doi.org/10.1080/17445647.2019.1650839collapseavalanchedomeslas derrumbadas volcanic area |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
J. A. Muñiz-Jáuregui C. S. Guzmán-Cervantes V. H. Garduño-Monroy A. Jiménez-Haro P. Layer |
spellingShingle |
J. A. Muñiz-Jáuregui C. S. Guzmán-Cervantes V. H. Garduño-Monroy A. Jiménez-Haro P. Layer Geomorphology of Las Derrumbadas dome complex, Puebla Mexico Journal of Maps collapse avalanche domes las derrumbadas volcanic area |
author_facet |
J. A. Muñiz-Jáuregui C. S. Guzmán-Cervantes V. H. Garduño-Monroy A. Jiménez-Haro P. Layer |
author_sort |
J. A. Muñiz-Jáuregui |
title |
Geomorphology of Las Derrumbadas dome complex, Puebla Mexico |
title_short |
Geomorphology of Las Derrumbadas dome complex, Puebla Mexico |
title_full |
Geomorphology of Las Derrumbadas dome complex, Puebla Mexico |
title_fullStr |
Geomorphology of Las Derrumbadas dome complex, Puebla Mexico |
title_full_unstemmed |
Geomorphology of Las Derrumbadas dome complex, Puebla Mexico |
title_sort |
geomorphology of las derrumbadas dome complex, puebla mexico |
publisher |
Taylor & Francis Group |
series |
Journal of Maps |
issn |
1744-5647 |
publishDate |
2019-07-01 |
description |
This paper comprises a geomorphologic map of the Las Derrumbadas (LDR) volcanic complex in Mexico. The complex stretches over more than 285 km2, the stratigraphic column encompasses a range age from Cretacious to Quaternary. The methodology used involved the analysis of digital morphometric models, satellite imagery and absolute datings. The result is a 1:40,000 scale map, which is divided into two large geomorphologic groups in terms of the dominant processes: exogenic and endogenic This, in turn, are divided into various subgroups representing the morphological complexity of the study area, principally related to volcanic processes and their coherence with slope processes. |
topic |
collapse avalanche domes las derrumbadas volcanic area |
url |
http://dx.doi.org/10.1080/17445647.2019.1650839 |
work_keys_str_mv |
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1724439129834389504 |