Timpanogos Glacier
Encyclopedia
Timpanogos Glacier is located in the Wasatch Range
Wasatch Range
The Wasatch Range is a mountain range that stretches approximately from the Utah-Idaho border, south through central Utah in the western United States. It is generally considered the western edge of the greater Rocky Mountains, and the eastern edge of the Great Basin region...

, Wasatch-Cache National Forest
Wasatch-Cache National Forest
Uinta-Wasatch-Cache National Forest is a United States National Forest located primarily in northern Utah , with smaller parts extending into southeastern Idaho and southwestern Wyoming . The name is from the Ute word Wasatch for a low place in high mountains, and the French word Cache meaning to...

, and is the only glacier in the U.S. state
U.S. state
A U.S. state is any one of the 50 federated states of the United States of America that share sovereignty with the federal government. Because of this shared sovereignty, an American is a citizen both of the federal entity and of his or her state of domicile. Four states use the official title of...

 of Utah
Utah
Utah is a state in the Western United States. It was the 45th state to join the Union, on January 4, 1896. Approximately 80% of Utah's 2,763,885 people live along the Wasatch Front, centering on Salt Lake City. This leaves vast expanses of the state nearly uninhabited, making the population the...

. The glacier is situated on the east slope of Mount Timpanogos
Mount Timpanogos
Mount Timpanogos, sometimes informally referred to as Timp, is the second highest mountain in Utah's Wasatch Range. Timpanogos rises to an elevation of 11,749 feet above sea level in the Uinta National Forest...

 (11749 feet (3,581.1 m)). Since at least the 1990s, Timpanogos Glacier has essentially disappeared, and by 2003 all visible surface ice had vanished. The glacier is now considered to be a rock glacier
Rock glacier
Rock glaciers are distinctive geomorphological landforms of angular rock debris frozen in interstitial ice which may extend outward and downslope from talus cones, glaciers or terminal moraines of glaciers. There are two types of rock glaciers: periglacial glaciers, or talus-derived glaciers, and...

, since some of the ice may now be buried in the talus.
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