Fremont Canyon is a

stream A stream is a continuous body of water, body of surface water Current (stream), flowing within the stream bed, bed and bank (geography), banks of a channel (geography), channel. Depending on its location or certain characteristics, a stream ...

and a deep

valley A valley is an elongated low area often running between Hill, hills or Mountain, mountains, which will typically contain a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers ...

canyon A canyon (from ; archaic British English spelling: ''cañon''), or gorge, is a deep cleft between escarpments or cliffs resulting from weathering and the erosion, erosive activity of a river over geologic time scales. Rivers have a natural tenden ...

that runs from its mouth at its

confluence In geography, a confluence (also: ''conflux'') occurs where two or more flowing bodies of water join to form a single channel. A confluence can occur in several configurations: at the point where a tributary joins a larger river (main stem); o ...

with Coyote Creek at the head of

Fremont Wash Fremont Wash sometimes called Fremont Canyon in its upper reach, is a stream and a valley in the north end of Parowan Valley, in Iron County, Utah. Its mouth lies at its confluence with Little Salt Lake at an elevation of 5,686 feet / 1,733 meters. ...

in Iron County, Utah, eastward across the Tushar Mountains to its head at on the west side of Fremont Pass in Garfield County, Utah. The Canyon was named for

John C. Frémont John Charles Frémont or Fremont (January 21, 1813July 13, 1890) was an American explorer, military officer, and politician. He was a U.S. Senator from California and was the first Republican nominee for president of the United States in 1856 ...

References

Landforms of Iron County, Utah Canyons and gorges of Garfield County, Utah Canyons and gorges of Utah {{Utah-geo-stub