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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
Mon, 8 Oct
Mon, 8 Oct 17:43 UTCM 1.2 / 5.9 km76 km- 19km ENE of Springfield, Oregon
Fri, 28 Sep
Fri, 28 Sep 20:18 UTCM 1.0 / 0.9 km53 kmExplosion - 24km SE of Sweet Home, Oregon
Tue, 25 Sep
Tue, 25 Sep 19:29 UTCM 1.7 / 0.6 km70 kmExplosion - 24km NE of Glide, Oregon
Tue, 25 Sep 18:08 UTCM 1.8 / 0.6 km74 kmExplosion - 23km ESE of Canyonville, Oregon
Tue, 25 Sep 16:05 UTCM 1.4 / 0.6 km73 kmExplosion - 25km NNE of Glide, 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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