Supervolcano 30 Times Larger Than Yellowstone Discovered in Utah [Wah Wah Springs] ... 12-13 eruption. The magma was calc-alkaline, dacitic (68 wt.

The Wah Wah Springs tuff is home to a group of 17 ancient volcanoes so big they are classified as “supervolcanoes.”


The scientists found that the Wah Wah Springs eruption buried a vast region extending from central Utah to central Nevada and from Fillmore on the north to Cedar City on the south. Wah Wah Springs Eruption in Utah und Nevada vor etwa 30 Millionen Jahren, 5500 km³ La-Garita-Caldera Eruption in Colorado, vor etwa 28 bis 26 Millionen Jahren, 5000 km³ Huckleberry Ridge Eruption, Yellowstone (Vulkan) vor 2,1 Millionen Jahren, mit 2500 km³ Tephra [5] They found that the Wah Wah Springs eruption buried a vast region extending from central Utah to central Nevada and from Fillmore on the north to Cedar City on the south.

Compared to more recent volcanic events, it …

It formed 30 Ma when an estimated 5,900 km 3 of crystal-rich dacitic magma erupted to form the Wah Wah Springs tuff. I also remember reading they said the magma chamber was recharging itself in the 2-3 weeks after the eruption, so maybe its full with 80 million cubic meters again. The "Wah Wah" name comes from Wah Wah Springs, on the eastern slope of the mountain range. .

. 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. Video courtesy of BYU News.

This time period is known for explosive silicic activity due to the subduction of the Farallon Plate along North America’s western edge. Upon its detection in 2013, scientists claimed that its last eruption was so devastating that it would have been “catastrophic” to all living things within hundreds of kilometres. The Indian Peak caldera is the largest in the complex; the topographic margin extends ~40 km north-south and, after correction for post-eruption east-west extension, the area of the structural caldera is about 1,000 km 2.

- /? The Wah Wah Springs Tuff (30.0 Ma) is one of several very large volume ash-flow tuffs (>3200 km³ of erupted magma) that were emplaced near the peak of the flare-up of activity in the Great Basin ignimbrite province of western North America. The 29.5 Ma Wah Wah Springs Formation which erupted from the Indian Peak Caldera has an estimated volume of > 3900 km 3 making it one of the largest ignimbrites on earth. These supervolcanoes aren’t active today, but 30 million years ago more than 5,500 cubic kilometers of magma erupted during a one-week period near a place called Wah Wah Springs.

The Indian Peak caldera is the largest in the complex; the topographic margin extends ~40 km north-south and, after correction for post-eruption east-west extension, the area of the structural caldera is about 1,000 km 2. Upon its detection in 2013, scientists claimed that its last eruption was so devastating that it would have been “catastrophic” to all living things within hundreds of kilometres. Eruptions at Toba (74,000 years ago), Yellowstone (640,000 years ago), and Lake Taupo (26,500 years ago) are three of the 47 VEI 8 sites that have been identified. Wah Wah Springs: 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 lava flows more than 4,000 metres (13,000 ft) thick 30,600,000 5,500–5,900 km 3: La Garita Caldera: San Juan volcanic field: Colorado, United States It’s the volcanic particles that … It formed 30 Ma when an estimated 5,900 km 3 of crystal-rich dacitic magma erupted to form the Wah Wah Springs tuff.
. Back then a weeklong eruption near what is now Wah Wah Springs, Utah produced over 13 hundred cubic miles of magma.

Wah Wah Springs is located on the border of Utah and Nevada in the US, but is difficult to detect due to erosion, researchers say. "Wah Wah" is reported to mean "good clear water". They found that the Wah Wah Springs eruption buried a vast region extending from central Utah to central Nevada and from Fillmore on the north to Cedar City on the south. The Wah Wah Springs Tuff and the Wah Wah Springs Intrusive Granodiorite are both part of the Indian Peak caldera complex in southwest Utah, an area of intense volcanic activity 30 million years ago. Wah Wah Springs: 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 lava flows more than 4,000 metres (13,000 ft) thick 30,600,000 5,500–5,900 km 3: La Garita Caldera: San Juan volcanic field: Colorado, United States . Geological Survey and Department of Geology, Brigham Young University, Provo, Utah 84602 ... the outflow member of the Wah Wah Springs Formation is about 1,500 km3 if an east-west - .. . Number 5.


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