The West Mageik Lake Sill Complex as an analogue for magma transport during the 1912 Eruption at the Valley of Ten Thousand Smokes, Alaska
- 1 August 1991
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 18 (8) , 1569-1572
- https://doi.org/10.1029/91gl01082
Abstract
No abstract availableThis publication has 12 references indexed in Scilit:
- The plinian eruptions of 1912 at Novarupta, Katmai National Park, AlaskaBulletin of Volcanology, 1992
- Petrogenesis of high-silica rhyolite on the Alaska PeninsulaGeophysical Research Letters, 1991
- New perspectives on the eruption of 1912 in the valley of ten thousand smokes, Katmai National Park, AlaskaBulletin of Volcanology, 1987
- Field relations between dikes and joints: Emplacement processes and paleostress analysisJournal of Geophysical Research, 1986
- Research drilling at Katmai, AlaskaEos, 1986
- The compositionally zoned eruption of 1912 in the Valley of Ten Thousand Smokes, Katmai National Park, AlaskaJournal of Volcanology and Geothermal Research, 1983
- The Stratigraphy of the Ejecta from the 1912 Eruption of Mount Katmai and Novarupta, AlaskaPublished by Geological Society of America ,1968
- GEOLOGY OF THE ALASKA PENINSULA_ ISLAND ARC AND CONTINENTAL MARGIN (PART 1)Published by Geological Society of America ,1965
- MECHANICAL ANALYSIS OF THE DIKE PATTERN OF THE SPANISH PEAKS AREA, COLORADOGSA Bulletin, 1957
- The Katmai Region, Alaska, and the Great Eruption of 1912The Journal of Geology, 1920