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JOURNAL ARTICLE
Did Plinian eruptions in California lead to debris flows in Nevada? An intriguing stratigraphic connection
John W. Bell
John W. Bell
1
Nevada Bureau of Mines and Geology, University of Nevada, Reno, Nevada 89557, USA
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P. Kyle House
P. Kyle House
1
Nevada Bureau of Mines and Geology, University of Nevada, Reno, Nevada 89557, USA
Search for other works by this author on:
Geology (2007) 35 (3): 219-222.
Published:
March 01, 2007
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John W. Bell, P. Kyle House; Did Plinian eruptions in California lead to debris flows in Nevada? An intriguing stratigraphic connection. Geology ; 35 (3): 219–222. doi: https://doi.org/10.1130/G23330A.1
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Index Terms/Descriptors
- absolute age
- ash falls
- burial
- C-14
- California
- carbon
- Cenozoic
- Churchill County Nevada
- Copper Canyon
- cores
- correlation
- dates
- debris flows
- Holocene
- igneous rocks
- Inyo Domes
- isotopes
- mass movements
- Mineral County Nevada
- Mono County California
- Mono Craters
- Nevada
- plinian-type eruptions
- pyroclastics
- Quaternary
- radioactive isotopes
- storm environment
- tephrochronology
- United States
- upper Holocene
- volcanic ash
- volcanic rocks
- volcanism
- Walker Lake
Latitude & Longitude
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