Please use this identifier to cite or link to this item:
http://hdl.handle.net/2122/7222| Authors: | Russo, M.* Campostrini, I.* |
Title: | AMMINEITE, MATLOCKITE AND POST 1944 ERUPTION FUMAROLIC MINERALS AT VESUVIUS | Issue Date: | 19-Sep-2011 | Keywords: | AMMINEITE MATLOCKITE POST 1944 ERUPTION VESUVIUS |
Subject Classification: | 04. Solid Earth::04.04. Geology::04.04.99. General or miscellaneous 04. Solid Earth::04.04. Geology::04.04.05. Mineralogy and petrology |
Abstract: | The 1944 eruption of Vesuvius began on March 18th and ended on the 29th of the same month. It was the last eruption of Vesuvius and marked the transition from an open conduit to a closed conduit state. The eruption took place during wartime so that nobody was interested to sample fumarolic minerals before and after the eruption. The only mineralogical work was made by Parascandola (1951), but most interesting were his comments on the temperature of the fumaroles and his observations about fumarolic minerals in the period between 1947 and 1960. Parascandola indicated the presence of about ten mineral species found on the fumaroles.... |
| Appears in Collections: | Conference materials |
Files in This Item:
| File | Description | Size | Format | |
|---|---|---|---|---|
| Plinius - Ammineite.pdf | 1.37 MB | Adobe PDF | View/Open |
Page view(s) 50
237
checked on Apr 17, 2024
Download(s) 50
261
checked on Apr 17, 2024
