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Bald Knoll volcano

cinder cones 2135 m / 7,005 ft
Utah, USA (mainland exept Alaska), 37.33°N / -112.41°W
Current status: 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
Wed, 25 Jul
Wed, 25 Jul 11:42 UTCM 1.8 / 3.3 km14 km- 20km SSW of Panguitch, Utah
Fri, 20 Jul
Fri, 20 Jul 03:49 UTCM 1.3 / 21.7 km40 km- 5km ENE of Fredonia, Arizona
Tue, 17 Jul
Tue, 17 Jul 15:36 UTCM 2.0 / 20.4 km34 km- 12km ESE of Kanab, Utah
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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