The Columbia River flood basalt province: Stratigraphy, areal extent, volume, and physical volcanology
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Published:August 01, 2013
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CiteCitation
Stephen P. Reidel, Victor E. Camp, Terry L. Tolan, Barton S. Martin, 2013. "The Columbia River flood basalt province: Stratigraphy, areal extent, volume, and physical volcanology", The Columbia River Flood Basalt Province, Stephen P. Reidel, Victor E. Camp, Martin E. Ross, John A. Wolff, Barton S. Martin, Terry L. Tolan, Ray E. Wells
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The middle Miocene Columbia River Basalt Group is the youngest and smallest continental flood basalt province on Earth, covering over 210,000 km2 of mainly Oregon, Washington, and Idaho, with an estimated basalt volume of ~210,000 km3. A well-established regional stratigraphic framework built upon six formations contains numerous flows and groups of flows that can be readily distinguished by their physical and compositional characteristics, thus producing mappable units, the areal extent and volume of which can be calculated and correlated with their respective feeder dikes. The distinct physical features that help to define these units originated during their...
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Contents
The Columbia River Flood Basalt Province

GeoRef
- basalt flows
- basalts
- Cenozoic
- chemical composition
- Columbia River Basalt Group
- contraction
- cooling
- degassing
- dikes
- emplacement
- flood basalts
- geometry
- Grande Ronde Basalt
- Idaho
- igneous rocks
- intrusions
- Miocene
- Neogene
- nomenclature
- Oregon
- paleomagnetism
- Picture Gorge Basalt
- Saddle Mountains Basalt
- Tertiary
- United States
- volcanic rocks
- volume
- Wanapum Basalt
- Washington
- Imnaha Basalt
- Steens Basalt
- Prineville Basalt