Articles | Volume 16, issue 8
https://doi.org/10.5194/nhess-16-1881-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/nhess-16-1881-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
15 Aug 2016
Research article |
| 15 Aug 2016
Factors controlling erosion/deposition phenomena related to lahars at Volcán de Colima, Mexico
Rosario Vázquez
CORRESPONDING AUTHOR
Centro de Geociencias, UNAM-Campus Juriquilla, Querétaro, C.P., 76046,
Mexico
Lucia Capra
Centro de Geociencias, UNAM-Campus Juriquilla, Querétaro, C.P., 76046,
Mexico
Velio Coviello
Centro de Geociencias, UNAM-Campus Juriquilla, Querétaro, C.P., 76046,
Mexico
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Cited
13 citations as recorded by crossref.
- Localized and distributed erosion triggered by the 2015 Hurricane Patricia investigated by repeated drone surveys and time lapse cameras at Volcán de Colima, Mexico T. Walter et al. 10.1016/j.geomorph.2018.07.020
- Factors controlling volcanic debris flows two decades after the 1990–1995 eruption at Mount Unzen in Japan J. Park et al. 10.1016/j.geomorph.2024.109119
- Flow connectivity in active volcanic areas: Use of index of connectivity in the assessment of lateral flow contribution to main streams A. Ortíz-Rodríguez et al. 10.1016/j.catena.2017.05.009
- UAV-Based Quantification of Dynamic Lahar Channel Morphology at Volcán de Fuego, Guatemala J. Mock et al. 10.3390/rs15153713
- Seismic characterization of hyperconcentrated flows in a volcanic environment V. Coviello et al. 10.1002/esp.4387
- Twenty-Five Years of Geomorphological Evolution in the Gokurakudani Gully (Unzen Volcano): Topography, Subsurface Geophysics and Sediment Analysis C. Gomez et al. 10.3390/geosciences11110457
- Emplacement temperature estimation of the 2015 dome collapse of Volcán de Colima as key proxy for flow dynamics of confined and unconfined pyroclastic density currents A. Pensa et al. 10.1016/j.jvolgeores.2018.05.010
- Hydrological control of large hurricane-induced lahars: evidence from rainfall-runoff modeling, seismic and video monitoring L. Capra et al. 10.5194/nhess-18-781-2018
- Runoff‐generated debris flows: Observation of initiation conditions and erosion–deposition dynamics along the channel at Cancia (eastern Italian Alps) A. Simoni et al. 10.1002/esp.4981
- Debris-flow monitoring and warning: Review and examples M. Hürlimann et al. 10.1016/j.earscirev.2019.102981
- Debris flow amplification in a moraine terrace and related engineering measures in the Zongzhai Valley, Southeastern Tibetan Plateau M. Deng et al. 10.1080/19475705.2018.1508507
- Research Progress of Initial Mechanism on Debris Flow and Related Discrimination Methods: A Review J. Du et al. 10.3389/feart.2021.629567
- Reconstruction of gully erosion based on exposed tree roots in a recent landform of Paricutin Volcano, Mexico O. Franco‐Ramos et al. 10.1002/esp.5269
13 citations as recorded by crossref.
- Localized and distributed erosion triggered by the 2015 Hurricane Patricia investigated by repeated drone surveys and time lapse cameras at Volcán de Colima, Mexico T. Walter et al. 10.1016/j.geomorph.2018.07.020
- Factors controlling volcanic debris flows two decades after the 1990–1995 eruption at Mount Unzen in Japan J. Park et al. 10.1016/j.geomorph.2024.109119
- Flow connectivity in active volcanic areas: Use of index of connectivity in the assessment of lateral flow contribution to main streams A. Ortíz-Rodríguez et al. 10.1016/j.catena.2017.05.009
- UAV-Based Quantification of Dynamic Lahar Channel Morphology at Volcán de Fuego, Guatemala J. Mock et al. 10.3390/rs15153713
- Seismic characterization of hyperconcentrated flows in a volcanic environment V. Coviello et al. 10.1002/esp.4387
- Twenty-Five Years of Geomorphological Evolution in the Gokurakudani Gully (Unzen Volcano): Topography, Subsurface Geophysics and Sediment Analysis C. Gomez et al. 10.3390/geosciences11110457
- Emplacement temperature estimation of the 2015 dome collapse of Volcán de Colima as key proxy for flow dynamics of confined and unconfined pyroclastic density currents A. Pensa et al. 10.1016/j.jvolgeores.2018.05.010
- Hydrological control of large hurricane-induced lahars: evidence from rainfall-runoff modeling, seismic and video monitoring L. Capra et al. 10.5194/nhess-18-781-2018
- Runoff‐generated debris flows: Observation of initiation conditions and erosion–deposition dynamics along the channel at Cancia (eastern Italian Alps) A. Simoni et al. 10.1002/esp.4981
- Debris-flow monitoring and warning: Review and examples M. Hürlimann et al. 10.1016/j.earscirev.2019.102981
- Debris flow amplification in a moraine terrace and related engineering measures in the Zongzhai Valley, Southeastern Tibetan Plateau M. Deng et al. 10.1080/19475705.2018.1508507
- Research Progress of Initial Mechanism on Debris Flow and Related Discrimination Methods: A Review J. Du et al. 10.3389/feart.2021.629567
- Reconstruction of gully erosion based on exposed tree roots in a recent landform of Paricutin Volcano, Mexico O. Franco‐Ramos et al. 10.1002/esp.5269
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Latest update: 04 Nov 2024
Short summary
We present the morphological changes experienced by Montegrande ravine (Volcán de Colima, Mexico) during the 2013, 2014 and 2015 rainy seasons. A total of 11 lahars occurred during this period of time, and their erosion/deposition effects were quantified by means of cross sections and rainfall analysis. The major factors controlling the E/D rates are the channel-bed slope, the cross-section width, the flow depth and the joint effect of sediment availability and accumulated rainfall.
We present the morphological changes experienced by Montegrande ravine (Volcán de Colima,...
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