Geology and hydrothermal alteration, Glass Buttes, Southeast Oregon
The Glass Buttes volcanic complex consists of many domes and individual vents that erupted both rhyolitic and basaltic lavas during the late Miocene to early Pliocene. The east half of the complex, in the vicinity of Little Glass Butte, contains interfingering, finely flow-banded rhyolite and black...
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ndltd-pdx.edu-oai-pdxscholar.library.pdx.edu-open_access_etds-41642019-10-20T04:29:49Z Geology and hydrothermal alteration, Glass Buttes, Southeast Oregon Berri, Dulcy Annette The Glass Buttes volcanic complex consists of many domes and individual vents that erupted both rhyolitic and basaltic lavas during the late Miocene to early Pliocene. The east half of the complex, in the vicinity of Little Glass Butte, contains interfingering, finely flow-banded rhyolite and black obsidian flows. The youngest unit, an obsidian, has been dated at 4.9 m.y. East of Little Glass Butte lie two northwest-trending ridges, Antelope and Cascade Ridges, composed of two or more overlapping exogenous domes that formed along northwest-trending faults. 1982-01-01T08:00:00Z text application/pdf https://pdxscholar.library.pdx.edu/open_access_etds/3158 https://pdxscholar.library.pdx.edu/cgi/viewcontent.cgi?article=4164&context=open_access_etds Dissertations and Theses PDXScholar Areal Geology Volcanology Oregon Hydrothermal Alteration Geology Volcanology |
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Areal Geology Volcanology Oregon Hydrothermal Alteration Geology Volcanology |
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Areal Geology Volcanology Oregon Hydrothermal Alteration Geology Volcanology Berri, Dulcy Annette Geology and hydrothermal alteration, Glass Buttes, Southeast Oregon |
description |
The Glass Buttes volcanic complex consists of many domes and individual vents that erupted both rhyolitic and basaltic lavas during the late Miocene to early Pliocene. The east half of the complex, in the vicinity of Little Glass Butte, contains interfingering, finely flow-banded rhyolite and black obsidian flows. The youngest unit, an obsidian, has been dated at 4.9 m.y. East of Little Glass Butte lie two northwest-trending ridges, Antelope and Cascade Ridges, composed of two or more overlapping exogenous domes that formed along northwest-trending faults. |
author |
Berri, Dulcy Annette |
author_facet |
Berri, Dulcy Annette |
author_sort |
Berri, Dulcy Annette |
title |
Geology and hydrothermal alteration, Glass Buttes, Southeast Oregon |
title_short |
Geology and hydrothermal alteration, Glass Buttes, Southeast Oregon |
title_full |
Geology and hydrothermal alteration, Glass Buttes, Southeast Oregon |
title_fullStr |
Geology and hydrothermal alteration, Glass Buttes, Southeast Oregon |
title_full_unstemmed |
Geology and hydrothermal alteration, Glass Buttes, Southeast Oregon |
title_sort |
geology and hydrothermal alteration, glass buttes, southeast oregon |
publisher |
PDXScholar |
publishDate |
1982 |
url |
https://pdxscholar.library.pdx.edu/open_access_etds/3158 https://pdxscholar.library.pdx.edu/cgi/viewcontent.cgi?article=4164&context=open_access_etds |
work_keys_str_mv |
AT berridulcyannette geologyandhydrothermalalterationglassbuttessoutheastoregon |
_version_ |
1719271041174339584 |