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Yellowstone Caldera, ... required a flow distance of at least 20 km ... exposed near the Grand Canyon of the Yellowstone and likely vented near Wapiti Lake. ...
The Grand Canyon of the Yellowstone is the first large canyon on the Yellowstone River downstream from Yellowstone Falls in Yellowstone National Park in Wyoming. The canyon is approximately 24 miles (39 km) long, between 800 and 1,200 ft (240 and 370 m) deep and from 0.25 to 0.75 mi (0.40 to 1.21 km) wide.
Yellowstone National Park spans an area of 3,468.4 sq mi (8,983 km 2), [3] with lakes, canyons, rivers, and mountain ranges. [11] Yellowstone Lake is one of the largest high-elevation lakes in North America and is centered over the Yellowstone Caldera, the largest super volcano on the continent.
Cascading from the 590,000 year old Canyon Rhyolite lava flow, Lower Falls of the Yellowstone River is the largest volume waterfall in the Rocky Mountains of the United States. [ citation needed ] These falls ( 44°43′05″N 110°29′46″W / 44.71806°N 110.49611°W / 44.71806; -110.49611 ) are 308 feet (94 m) high, or nearly ...
The Yellowstone Plateau Volcanic Field, also known as the Yellowstone Supervolcano or the Yellowstone Volcano, is a complex volcano, volcanic plateau and volcanic field located mostly in the western U.S. state of Wyoming, but it also stretches into Idaho and Montana. [4] [5] It is a popular site for tourists. [6] Map of Yellowstone Volcano ash beds
Mount Washburn, elevation 10,219 feet (3,115 m), is a prominent mountain peak in the Washburn Range in Yellowstone National Park, Wyoming, United States.The peak was named in 1870 to honor Henry D. Washburn, leader of the Washburn–Langford–Doane Expedition.
The 10,000 year old Grand Canyon of Yellowstone surrounds the mighty Yellowstone River. Gazing from the canyon rim into the 1,000-feet deep gorge should make even the most seasoned traveler feel ...
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 ...
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