| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4729196 | Journal of African Earth Sciences | 2011 | 10 Pages |
Abstract
⺠Water-magma interaction drove the evolution of the eruption of Montaña Pelada. ⺠Proximal deposits suggest high W/M ratios at the beginning of the eruption. ⺠Turbulent pyroclastic surges indicate lower W/M ratios and higher effective fragmentation. ⺠The new hydrological conditions allowed the input of phreatic waters, increasing the W/M and reducing the fragmentation degree.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geology
Authors
J. Carmona, C. Romero, J. Dóniz, A. GarcÃa,