Yellowstone National Park
-
What is Yellowstone National Park?
Yellowstone National Park, established on March 1, 1872, is the United States' oldest national park and is renowned for its extensive hydrothermal features, including geysers and hot springs. Situated primarily in Wyoming, with parts extending into Montana and Idaho, the park covers 3,472 square miles.
The park's landscape is shaped by volcanic activity, ice, and water, featuring broad plateaus, mountain ranges, and scenic lakes like Yellowstone Lake, North America's highest mountain lake of its size. Yellowstone is home to a diverse array of wildlife, boasting the most significant collection of mammals in the United States outside of Alaska, including bison, elk, bears, and wolves. It was designated a UNESCO biosphere reserve in 1976 and a World Heritage site in 1978.
4 Britannica SourcesCreated from Britannica articles using AI. AI can make mistakes, so verify using Britannica articles. -
Where is Yellowstone National Park located?
Yellowstone National Park is primarily located in northwestern Wyoming, with portions extending into southern Montana and eastern Idaho. This vast park, established in 1872, is renowned for its extensive hydrothermal features and is considered the United States' oldest national park. The park covers an area of 3,472 square miles and is surrounded by several national forests. Access to Yellowstone is available through entrances in the north, northeast, east, south, and west.
3 Britannica SourcesCreated from Britannica articles using AI. AI can make mistakes, so verify using Britannica articles. -
Why is Yellowstone famous for geysers and hot springs?
Yellowstone National Park is renowned for its geysers and hot springs due to its location over a volcanic hotspot. This geological activity causes groundwater to interact with magma or hot igneous rocks, leading to the formation of these hydrothermal features. The park contains approximately half of the world's known hydrothermal features, including over 300 geysers.
The unique conditions within Yellowstone's caldera allow for the dramatic eruptions of geysers like Old Faithful, where superheated water flashes into steam, forcing columns of water and steam into the air. The mineral-rich water also creates colorful hot pools and terraces, contributing to the park's spectacular and unusual geological landscape.
3 Britannica SourcesCreated from Britannica articles using AI. AI can make mistakes, so verify using Britannica articles. -
What kinds of animals live in Yellowstone National Park?
Yellowstone National Park is home to a diverse array of wildlife, boasting the most extensive collection of mammals in the United States outside of Alaska. Large mammals frequently observed include bison, elk, mule deer, black bears, foxes, and coyotes. Smaller populations of grizzly bears, bighorn sheep, pronghorns, mountain goats, and moose also inhabit the park. Reintroduced wolves are now found throughout much of Yellowstone, and beavers have made a significant comeback along its waterways.
The park also supports over 300 bird species, including permanent residents like jays, chickadees, and ravens, as well as waterfowl such as trumpeter swans and Canada geese. Summer breeders of note include sandhill cranes and American white pelicans. Yellowstone's lakes and streams are home to various fish, though native cutthroat trout are threatened by introduced predators. Fewer than a dozen reptile and amphibian species are present, including prairie rattlesnakes and boreal chorus frogs.
2 Britannica SourcesCreated from Britannica articles using AI. AI can make mistakes, so verify using Britannica articles. -
How was Yellowstone National Park formed?
Yellowstone National Park was formed by a series of massive volcanic eruptions. The most significant event occurred approximately 640,000 years ago, creating the vast Yellowstone Caldera, which measures about 30 by 45 miles. This caldera is the youngest and largest of three that have formed in the region due to volcanic activity over millions of years. The park sits atop a supervolcano, and the heat from its volcanic past is responsible for the area's famous hydrothermal features like geysers and hot springs.
3 Britannica SourcesCreated from Britannica articles using AI. AI can make mistakes, so verify using Britannica articles. -
Why is Yellowstone considered important for conservation and history?
Yellowstone National Park holds immense importance for conservation and history. Established on March 1, 1872, it was the world's first national park, setting a precedent for conservation efforts globally. This designation aimed to protect its unparalleled hydrothermal features, the largest concentration worldwide, including geysers like Old Faithful, hot pools, and terraces.
Historically, the region shows evidence of human presence for over 11,000 years, with various Indigenous peoples inhabiting or visiting the area. The park's creation was influenced by explorers like John Colter and Ferdinand Vandiveer Hayden, and advocacy from figures like Jay Cooke, who recognized its recreational and tourism potential. Yellowstone's designation marked a pivotal moment in preserving natural wonders for future generations and understanding human history within these landscapes.
2 Britannica SourcesCreated from Britannica articles using AI. AI can make mistakes, so verify using Britannica articles.
News •
Yellowstone National Park, the oldest, one of the largest, and probably the best-known national park in the United States. It is situated principally in northwestern Wyoming and partly in southern Montana and eastern Idaho and includes the greatest concentration of hydrothermal features in the world. The park was established by the U.S. Congress on March 1, 1872, as the countryās first national park. It is also generally considered to have been the first national park in the world, though some naturalists and others have argued that there is evidence that indicates that the creation of Yellowstone was predated by the creation of Bogd Khan Mountain National Park in Mongolia, which may date from as early as 1778. Yellowstone was designated a UNESCO biosphere reserve in 1976 and a World Heritage site in 1978. The park, which forms a squarelike rectangle with an irregular eastern side, is 63 miles (101 km) from north to south and 54 miles (87 km) from east to west at its widest point and covers an area of 3,472 square miles (8,992 square km). The John D. Rockefeller, Jr., Memorial Parkway, an 80-mile (130-km) scenic roadway that was established in 1972, connects Yellowstone with Grand Teton National Park to the south. In addition, Yellowstone is surrounded by Gallatin (northwest and north), Custer (northeast), Shoshone (northeast and east), Bridger-Teton (southeast and south), and Caribou-Targhee (southwest) national forests. Headquarters are at Mammoth Hot Springs near the northern entrance to the park.
Natural environment
Geology
Yellowstone is situated in a region that has been volcanically and seismically active for tens of millions of years. Tectonic movement of the North American Plate has thinned Earthās crust in the area, forming a hotspot (a place where a dome of magma, or molten rock, comes close to the surface). About 2.1 million years ago a subsurface magma dome that had been building up in the Yellowstone area blew up in one of the worldās most cataclysmic volcanic eruptions. Some 600 cubic miles (2,500 cubic km) of rock and ash were ejected, equivalent to about 6,000 times the amount of volcanic material that was released during the eruption of Mount Saint Helens in 1980. (Observations made in the early 21st century indicated that this single eruption actually consisted of two events about 6,000 years apart: one very large and a second much smaller one.) Subsequent massive eruptions occurred about 1,300,000 and 640,000 years agoāthe last event (consisting in large part of lava flows) producing about two-fifths as much material as the first one.
Each of those eruptions caused the magma dome that had built up to collapse as its contents were released, leaving an enormous caldera. The present-day Yellowstone Caldera, the product of the third eruption, is a roughly oval-shaped basin some 30 by 45 miles (50 by 70 km) that occupies the west-central portion of the national park and includes the northern two-thirds of Yellowstone Lake. Two resurgent magma domesāone just north of and the other just west of Yellowstone Lakeāhave been forming in the caldera, and the western dome underlie many of the parkās best-known hydrothermal features.
The Yellowstone region is also extremely active seismically. A network of faults associated with the regionās volcanic history underlies the parkās surface, and the region experiences hundreds of small earthquakes each year. The great majority of those quakes are of magnitude 2.0 or less and are not felt by people in the area, but occasionally a more powerful temblor will strike in the region and have effects in the park. One such event, a deadly quake that struck in 1959 in southern Montana just outside the northwestern corner of the park, affected a number of hydrothermal features in Yellowstone, including its iconic geyser, Old Faithful.


