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  2. Yellowstone Caldera - Wikipedia

    en.wikipedia.org/wiki/Yellowstone_Caldera

    It was Yellowstone's third and most recent caldera-forming eruption. Geologists closely monitor the elevation of the Yellowstone Plateau, which has been rising as quickly as 150 millimetres (5.9 in) per year, as an indirect measurement of changes in magma chamber pressure. [41] [42] [43]

  3. Geothermal areas of Yellowstone - Wikipedia

    en.wikipedia.org/.../Geothermal_areas_of_Yellowstone

    This in turn released the enclosed magma as lava and caused the surface above the emptied magma chamber to collapse. [20] Water later filled the collapsed area of the caldera, forming an extension of Yellowstone Lake. This created the source of heat and water that feed the West Thumb Geyser Basin today. Geyser cone under water at West Thumb ...

  4. Yellowstone hotspot - Wikipedia

    en.wikipedia.org/wiki/Yellowstone_hotspot

    The Yellowstone hotspot is a volcanic hotspot in the United States ... Map of recent Yellowstone eruption ... (46,000 km3 magma reservoir below chamber) This ...

  5. Yellowstone National Park - Wikipedia

    en.wikipedia.org/wiki/Yellowstone_National_Park

    The magma chamber that lies under Yellowstone is estimated to be a single connected chamber, about 37 miles (60 km) long, 18 miles (29 km) wide, and 3 to 7 miles (4.8 to 11.3 km) deep. [85] The current caldera was created by a cataclysmic eruption that occurred 640,000 years ago, which released more than 240 cu mi (1,000 km 3 ) of ash, rock and ...

  6. List of Yellowstone geothermal features - Wikipedia

    en.wikipedia.org/wiki/List_of_Yellowstone...

    Map all coordinates using OpenStreetMap. Download coordinates as: KML; ... and other geothermal features in the geothermal areas of Yellowstone National Park.

  7. Lava Creek Tuff - Wikipedia

    en.wikipedia.org/wiki/Lava_Creek_Tuff

    The zircon and phenocrysts rims recorded that the magma of the Lava Creek Tuff was generated from a mix of mantle, Archean crust, and shallow hydrothermally altered intra-caldera rocks. Member A and B were sourced from separate magma reservoirs prior to eruption, [ 19 ] at a depth range of 3–6 km (1.9–3.7 mi) [ 20 ] and a temperature of 790 ...

  8. Category : Geothermal features of Yellowstone National Park

    en.wikipedia.org/wiki/Category:Geothermal...

    Geothermal features of Yellowstone National Park — features of volcanism, including geysers and hot springs. Pages in category "Geothermal features of Yellowstone National Park" The following 85 pages are in this category, out of 85 total.

  9. Caldera - Wikipedia

    en.wikipedia.org/wiki/Caldera

    If magma continues to be injected into the collapsed magma chamber, the center of the caldera may be uplifted in the form of a resurgent dome such as is seen at the Valles Caldera, Lake Toba, the San Juan volcanic field, [7] Cerro Galán, [26] Yellowstone, [27] and many other calderas. [7]