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Bald Knoll volcano

cinder cones 2135 m / 7,005 ft
Utah, Canada and USA (mainland), 37.33°N / -112.41°W
Current status: normal or dormant (1 out of 5) | Reports
Bald Knoll volcano books
Typical eruption style: strombolian
Bald Knoll volcano eruptions: several hundreds to a few thousands of years ago
TimeMag. / DepthDistanceLocation
Thu, 22 Oct 2020 (UTC)
Thu, 22 Oct 13:31 UTCM 1.8 / 10.2 km9 km9 Km ESE of Alton, Utah, USA
Mon, 3 Aug 2020 (UTC)
Mon, 3 Aug 18:54 UTCM 1.2 / 14.9 km18 km17 km E of Alton, Utah (USA)
Wed, 10 Jun 2020 (UTC)
Wed, 10 Jun 18:07 UTCM 0.9 / 13 km24 km16 km SE of Hatch, Utah (USA)
Bald Knoll is the youngest of a group of basaltic cinder cones on the SW part of the Paunsaugunt Plateau in southern Utah, between the southern end of Bryce Canyon National Park and the western margin of Grand Staircase-Escalante National Monument.
The Bald Knoll cinder cone probably erupted only a few thousands years ago. It has an intact crater, which has produced a massive youthful-looking lava flow that traveled about 12 km to the SSE.
Buck Knoll and Black Knoll are 2 other cinder cones to the west, located on the western side of Kanab Creek.

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