Generation of fine hydromagmatic ash by growth and disintegration of glassy rinds
January 1, 2007
The deposits of mafic hydromagmatic eruptions are more fine grained and variable in vesicularity than dry magmatic deposits. Blocky, equant shapes of many hydromagmatic clasts also contrast with droplet, thread, and bubble wall morphology of dry magmatic fragments. Small (
Citation Information
| Publication Year | 2007 |
|---|---|
| Title | Generation of fine hydromagmatic ash by growth and disintegration of glassy rinds |
| DOI | 10.1029/2005JB003883 |
| Authors | Larry G. Mastin |
| Publication Type | Article |
| Publication Subtype | Journal Article |
| Series Title | Journal of Geophysical Research B: Solid Earth |
| Index ID | 70033157 |
| Record Source | USGS Publications Warehouse |
| USGS Organization | Volcano Hazards Program |