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Devis Lake volcano

volcanic field 2163 m / 7,096 ft
Oregon, USA (mainland exept Alaska), 43.57°N / -121.82°W
Current status: normal or dormant (1 out of 5) | Reports
Devis Lake volcano books
Typical eruption style: Explosive
Devis Lake volcano eruptions: 2790 BC (?) (radiocarbon dated)
TimeMag. / DepthDistanceLocation
Thu, 6 Dec
Thu, 6 Dec 00:24 UTCM 2.1 / 1.4 km69 kmExplosion - Oregon
Wed, 5 Dec
Wed, 5 Dec 22:39 UTCM 1.7 / 1.7 km59 kmExplosion - Oregon
Wed, 5 Dec 00:38 UTCM 2.0 / 1.5 km75 kmExplosion - 3km N of Prineville, Oregon
Sun, 18 Nov
Sun, 18 Nov 16:46 UTCM 1.1 / 13.9 km73 km- 19km SSW of Sweet Home, Oregon
Wed, 14 Nov
Wed, 14 Nov 00:45 UTCM 1.7 / 1.6 km76 kmExplosion - 4km NNE of Prineville, Oregon
View all recent quakes
Davis Lake area in Oregon, USA, is a volcanic field with 3 cinder cones and lava flows of three cinder cones and associated lava flows.

Background:

The cinder cones of the Davis Lake field are on a N-S line at the feet of a group of older basaltic-andesite shield volcanoes east of the crest of the Cascade Range and south of the Mount Bachelor volcanic chain.
The northernmost lava flow built a natural barrier forming Davis Lake. It lies at the western base of the Pleistocene Davis Mountain shield volcano and at the SW end of the Wickiup Reservoir.
The two southern flows are located in a plain straddling Crescent Creek between Hamner and Odell Buttes.
The middle lava flow erupted from a small cinder cone on the lower southern flank of Hamner Butte and appears to be the youngest of the lava flows in the field.
The southernmost lava flow was erupted from a cone at the ENE base of Odell Butte.
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Source: GVP


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