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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: 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, 6 Dec
Thu, 6 Dec 13:29 UTCM 2.0 / 21 km34 km- Utah
Tue, 27 Nov
Tue, 27 Nov 12:05 UTCM 1.6 / 1.8 km13 km- 37km SSW of Panguitch, Utah
Tue, 20 Nov
Tue, 20 Nov 14:32 UTCM 1.8 / 11.4 km37 km- Utah
Tue, 20 Nov 10:26 UTCM 1.9 / 13.7 km38 km- Utah
Mon, 19 Nov
Mon, 19 Nov 16:07 UTCM 1.7 / 3.6 km17 km- 26km S of Panguitch, Utah
View all recent quakes
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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