Bald Knoll Vulkan, Utah (Canada and USA (mainland))

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Bald Knoll Vulkan

cinder cones 2135 m / 7,005 ft
Utah, USA (mainland exept Alaska), 37.33°N / -112.41°W
Aktueller Status: nicht aktiv (1 von 5)

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Typische Aktivität: strombolianische
Ausbrüche des Bald Knoll: several hundreds to a few thousands of years ago
Letzte Erdbeben in der Nähe:

Zeit	Mag. / Tiefe	Distance	Ort
Mon, 10 Jun
Mon, 10 Jun 00:55 UTC	M 1.3 / 26 km	40 km	19km ENE of Fredonia, Arizona
Tue, 14 May
Tue, 14 May 09:09 UTC	M 1.1 / 20.9 km	34 km	34km E of Kanab, Utah
Tue, 14 May 09:00 UTC	M 1.7 / 19.6 km	34 km	34km E of Kanab, Utah
Tue, 14 May 08:15 UTC	M 1.8 / 20 km	33 km	33km ENE of Kanab, Utah
Tue, 14 May 07:49 UTC	M 2.5 / 15.3 km	37 km	36km E 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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