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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
Fri, 22 Feb 2019
Fri, 22 Feb 00:40 UTCM 1.8 / 1.5 km68 kmExplosion - 6km W of Prineville, Oregon (USA)
Wed, 20 Feb 2019
Wed, 20 Feb 00:38 UTCM 1.7 / 1.5 km66 kmExplosion - Oregon (USA)
Tue, 19 Feb 2019
Tue, 19 Feb 19:55 UTCM 1.4 / 0.3 km83 km20km ESE of Yoncalla, Oregon (USA)
Sun, 17 Feb 2019
Sun, 17 Feb 07:37 UTCM 1.0 / 1.4 km3 km30km S of Diamond Lake, Oregon (USA)
Thu, 14 Feb 2019
Thu, 14 Feb 01:33 UTCM 2.0 / 1.5 km67 kmExplosion - 6km W 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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