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 …
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 …
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 …
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