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A summer storm hits Wah Wah Valley and the Wah Wah Mountains, in May 2009. Wah Wah Springs Caldera is a supervolcanic eruption remnant discovered in 2013 in Utah.It released 5,500 to 5,900 cubic kilometres (1,300 to 1,400 cu mi) of tephra, as the Wah Wah Springs Tuff, about 30.06 million years ago in the early Oligocene.
The "Wah Wah" name comes from Wah Wah Springs, on the eastern slope of the mountain range. "Wah Wah" is reported to mean "good clear water". [3] The Bureau of Land Management, which administers most of the land within the Wah Wah Mountains, has designated two wilderness study areas, one in the north and one in the central portion of the range.
Wah Wah Springs Caldera: Indian Peak–Caliente Caldera Complex Utah, United States The largest of the Indian Peak-Caliente Caldera Complex eruptions, preserved as the Wah Wah Springs Tuff; includes pyroclastic flows more than 500 meters (1,600 ft) thick 30,600,000 5,500–5,900 km 3 [27] [28] La Garita Caldera: San Juan volcanic field
Many geological features in Western United States have a Northeastern orientation, the North American craton motion has the same orientation as well. [1] For example: the Trans-Challis fault zone, Idaho; the Snake River in Oregon; the Garlock Fault, California; the Colorado River in Utah; the Colorado Mineral Belt; Crater Flat-Reveille Range-Lunar Crater lineament, the Northwestern Nevada ...
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Volcanic calderas of Utah, United States. ... Wah Wah Springs Caldera This page was last edited on 17 May 2022, at 07:16 (UTC). Text ...
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Wah Wah Springs Tuff: 30.06 Indian Peak-Caliente Caldera Complex 5,500–5,900: The largest of the Indian Peak-Caliente Caldera Complex, and includes flows over 4,000 meters thick at the most. [18] [10] Caxias do Sul—Grootberg ~132 Paraná and Etendeka traps 5,650: The nature of eruption is disputed.