Origin and stratigraphy of phreatomagmatic deposits at the Pleistocene Sinker Butte volcano, western Snake River Plain, Idaho

BD Brand, CM White - Journal of Volcanology and Geothermal Research, 2007 - Elsevier
Sinker Butte is the erosional remnant of a very large basaltic tuff cone of middle Pleistocene
age located at the southern edge of the western Snake River Plain. Phreatomagmatic …

[引用][C] Origin and stratigraphy of phreatomagmatic deposits at the Pleistocene Sinker Butte Volcano, Western Snake River Plain, Idaho

BD BRAND, CM WHITE - Journal of volcanology and …, 2007 - pascal-francis.inist.fr
Keyword (en) scours channels color debris flows lava flows geologic sections cones base
surges explosive eruptions exhibits troughs bedding palagonitization middle Pleistocene …

Origin and stratigraphy of phreatomagmatic deposits at the Pleistocene Sinker Butte Volcano, Western Snake River Plain, Idaho

BD Brand, CM White - Journal of Volcanology and Geothermal Research, 2007 - infona.pl
Sinker Butte is the erosional remnant of a very large basaltic tuff cone of middle Pleistocene
age located at the southern edge of the western Snake River Plain. Phreatomagmatic …

Origin and stratigraphy of phreatomagmatic deposits at the Pleistocene Sinker Butte Volcano, Western Snake River Plain, Idaho

BD Brand, CM White - Journal of Volcanology and …, 2007 - ui.adsabs.harvard.edu
Sinker Butte is the erosional remnant of a very large basaltic tuff cone of middle Pleistocene
age located at the southern edge of the western Snake River Plain. Phreatomagmatic …

[PDF][PDF] Origin and stratigraphy of phreatomagmatic deposits at the Pleistocene Sinker Butte Volcano, Western Snake River Plain, Idaho

BD Brand, CM White - Journal of Volcanology and Geothermal …, 2007 - academia.edu
Sinker Butte is the erosional remnant of a very large basaltic tuff cone of middle Pleistocene
age located at the southern edge of the western Snake River Plain. Phreatomagmatic …

Origin and stratigraphy of phreatomagmatic deposits at the Pleistocene Sinker Butte Volcano, Western Snake River Plain, Idaho

BD Brand, CM White - Journal of Volcanology and Geothermal Research, 2007 - infona.pl
Sinker Butte is the erosional remnant of a very large basaltic tuff cone of middle Pleistocene
age located at the southern edge of the western Snake River Plain. Phreatomagmatic …

[引用][C] Origin and stratigraphy of phreatomagmatic deposits at the Pleistocene Sinker Butte Volcano, Western Snake River Plain, Idaho

BD BRAND, CM WHITE - Journal of volcanology and geothermal research, 2007 - Elsevier