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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)
Bald Knoll volcano books
Typical eruption style: strombolian
Bald Knoll volcano eruptions: several hundreds to a few thousands of years ago
TimeMag. / DepthDistanceLocation
Mon, 11 Dec
Mon, 11 Dec 06:03 UTCM 1.9 / 14.8 km26 km- 37km NNW of Kanab, Utah
Mon, 11 Dec 06:03 UTCM 1.9 / 14.8 km26 km- 37km NNW of Kanab, Utah
Sun, 26 Nov
Sun, 26 Nov 21:48 UTCM 2.8 / 9.5 km17 km- 27km SE of Cedar City, Utah
Thu, 16 Nov
Thu, 16 Nov 09:26 UTCM 2.1 / 17 km14 km- 27km SE of Cedar City, Utah
Thu, 26 Oct
Thu, 26 Oct 16:56 UTCM 1.4 / 14.5 km27 km- 36km NNW of Kanab, Utah
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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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