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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: dormant (1 out of 5)
Devis Lake volcano books
Typical eruption style: Explosive
Devis Lake volcano eruptions: 2790 BC (?) (radiocarbon dated)
TimeMag. / DepthDistanceLocation
Thu, 18 Jan
Thu, 18 Jan 23:57 UTCM 1.7 / 3.3 km12 km- 48km E of La Pine, Oregon
Wed, 17 Jan
Wed, 17 Jan 22:46 UTCM 2.2 / 1.7 km56 kmExplosion - 8km E of Terrebonne, Oregon
Fri, 5 Jan
Fri, 5 Jan 21:27 UTCM 1.0 / 0.9 km34 kmExplosion - 32km ESE of Sweet Home, Oregon
Sun, 31 Dec
Sun, 31 Dec 20:55 UTCM 0.1 / 0.8 km2 km- 23km ESE of Three Rivers, Oregon
Fri, 29 Dec
Fri, 29 Dec 00:38 UTCM 0.9 / 12.9 km79 km- 15km ENE of Coburg, 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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