Abstract
The Nevado del Ruiz eruption of November 13 provided an opportunity for investigating the dynamic response of a well-developed volcanic hydrothermal system to a major plinian eruption. This study summarizes changes that have been observed in the chemical and isotopic compositions of acid-sulfate-chloride thermal waters at Nevado del Ruiz in the 37 months following the November 13, 1985 eruption, and discusses possible relations of these changes to the behavior of the volcano.
| Original language | English (US) |
|---|---|
| Pages (from-to) | 203-210 |
| Number of pages | 8 |
| Journal | Journal of Volcanology and Geothermal Research |
| Volume | 42 |
| Issue number | 1-2 |
| DOIs | |
| State | Published - Jul 30 1990 |
ASJC Scopus subject areas
- Geophysics
- Geochemistry and Petrology
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