Rock Canyon is located in the Wasatch Mountains, in east Provo, Utah, United States. [1] [Note 1] It is popular with rock climbers and hikers (and a number of other outdoor enthusiasts of all types) due to its unique and rugged geology as well as its proximity to Brigham Young University. The mouth of the canyon is located just behind the Provo Utah Temple.
Recorded history of the canyon begins with the conflicts between Mormon settlers based at Fort Utah and the indigenous Timpanogos tribe living in Utah Valley in 1850. A contingent of Timpanogos, under the direction of Big Elk, fled to Rock Canyon following a battle with the Mormon militia. Squaw Peak is the name the settlers gave to the peak north of Rock Canyon, after Big Elk's wife who died in the canyon in the conflict. Some pictographs still exist from early Indian writings. There are large mineral deposits in the canyon and many shafts and tunnels still exist which may be explored. [2] Various rock climbing routes also exist throughout the canyon. [3]
Rock Canyon is home to a number of large game animals and it is common for visitors to observe deer, bighorn sheep, or other species. [4]
Rock Canyon shows excellent outcrops of dominantly Paleozoic age rocks, with Precambrian Tillite at the mouth of the canyon, and Quaternary colluvium and glacial deposits in the canyon. Rock Canyon preserves a record of multiple phases of the area, including: [5]
Folding in the canyon has mad may of the beds perpendicular to the trail. As you walk up the canyon you are walking up the depositional sequence. Rock units seen in outcrop in the canyon from mouth of the canyon (oldest) to back of the canyon (youngest) are as follows:
The Wasatch Range or Wasatch Mountains is a mountain range in the western United States that runs about 160 miles (260 km) from the Utah-Idaho border south to central Utah. It is the western edge of the greater Rocky Mountains, and the eastern edge of the Great Basin region. The northern extension of the Wasatch Range, the Bear River Mountains, extends just into Idaho, constituting all of the Wasatch Range in that state.
The geology of the Zion and Kolob canyons area includes nine known exposed formations, all visible in Zion National Park in the U.S. state of Utah. Together, these formations represent about 150 million years of mostly Mesozoic-aged sedimentation in that part of North America. Part of a super-sequence of rock units called the Grand Staircase, the formations exposed in the Zion and Kolob area were deposited in several different environments that range from the warm shallow seas of the Kaibab and Moenkopi formations, streams and lakes of the Chinle, Moenave, and Kayenta formations to the large deserts of the Navajo and Temple Cap formations and dry near shore environments of the Carmel Formation.
The exposed geology of the Bryce Canyon area in Utah shows a record of deposition that covers the last part of the Cretaceous Period and the first half of the Cenozoic era in that part of North America. The ancient depositional environment of the region around what is now Bryce Canyon National Park varied from the warm shallow sea in which the Dakota Sandstone and the Tropic Shale were deposited to the cool streams and lakes that contributed sediment to the colorful Claron Formation that dominates the park's amphitheaters.
The Uinta Mountains are an east-west trending chain of mountains in northeastern Utah extending a short distance into northwest Colorado and slightly into southwestern Wyoming in the United States. As a subrange of the Rocky Mountains, they are unusual for being the highest range in the contiguous United States running east to west, and lie approximately 100 miles (160 km) east of Salt Lake City. The range has peaks ranging from 11,000 to 13,528 feet, with the highest point being Kings Peak, also the highest point in Utah. The Mirror Lake Highway crosses the western half of the Uintas on its way to Wyoming. Utah State Route 44 crosses the east end of the Uintas between Vernal and Manila.
Mount Timpanogos, often referred to as Timp, is the second-highest mountain in Utah's Wasatch Range. Timpanogos rises to an elevation of 11,752 ft (3,582 m) above sea level in the Uinta-Wasatch-Cache National Forest. With 5,270 ft (1,610 m) of topographic prominence, Timpanogos is the 47th-most prominent mountain in the contiguous United States.
Timpanogos Cave National Monument is a United States National Monument protecting the Timpanogos Cave Historic District and a cave system on Mount Timpanogos in American Fork Canyon in the Wasatch Range, near Highland, Utah, in the United States. The site is managed by the National Park Service. The 1.5-mile (2.4 km) long trail to the cave entrance gains 1,092 feet (333 m) height, but it is paved and fairly wide making it accessible for most people. The three caves of the system, one of which is specifically called Timpanogos Cave, are only viewable on guided tours when the monument is open, usually from May through September depending on snow conditions and funding. There is the standard tour going through the cave system, and an Introduction to Caving tour which teaches Leave No Trace caving and goes further into Hansen Cave.
Little Cottonwood Canyon lies within the Wasatch-Cache National Forest along the eastern side of the Salt Lake Valley, roughly 15 miles from Salt Lake City, Utah. The canyon is part of Granite, a CDP and "Community Council" designated by Salt Lake County. The canyon is a glacial trough, carved by an alpine glacier during the last ice age, 15,000 to 25,000 years ago. A number of rare and endemic plant species are found in the canyon's Albion Basin. Introduced Mountain goats inhabit the surrounding mountains.
The Kaibab Limestone is a resistant cliff-forming, Permian geologic formation that crops out across the U.S. states of northern Arizona, southern Utah, east central Nevada and southeast California. It is also known as the Kaibab Formation in Arizona, Nevada, and Utah. The Kaibab Limestone forms the rim of the Grand Canyon. In the Big Maria Mountains, California, the Kaibab Limestone is highly metamorphosed and known as the Kaibab Marble.
The Traverse Mountains, or sometimes Traverse Range, are an anomalous, geologically complex, east-trending range that separates Salt Lake Valley and Utah Valley in Salt Lake and Utah counties in the U.S. State of Utah.
The Provo City School District is a school district in Provo, Utah, United States, which has boundaries that almost entirely coincide with those of the city, except for one small portion.
Provo Canyon is located in unincorporated Utah County and Wasatch County, Utah. Provo Canyon runs between Mount Timpanogos on the north and Mount Cascade on the south. The canyon extends from Orem on the west end to Heber City on the east. Provo Canyon is situated to the east of Utah Valley and grants access to the valleys and Uinta Basin regions that lie beyond the Wasatch front.
Mount Timpanogos Wilderness is a 10,518-acre (42.56 km2) wilderness area protecting Mount Timpanogos and the surrounding area. It is located in the front range of the Wasatch Mountain Range, between American Fork Canyon on the north and Provo Canyon on the south, within the Uinta-Wasatch-Cache National Forest on the north eastern edge of Utah County, Utah, United States. The wilderness area receives fairly heavy use due to its proximity to the heavily populated cities of Provo and Salt Lake City. It is bordered on the north by the Lone Peak Wilderness.
The Bonneville flood was a catastrophic flooding event in the last ice age, which involved massive amounts of water inundating parts of southern Idaho and eastern Washington along the course of the Snake River. Unlike the Missoula Floods, which also occurred during the same period in the Pacific Northwest, the Bonneville flood happened only once. It is believed to be the second-largest flood in known geologic history.
The Mineral Fork Formation is a mapped Proterozoic bedrock unit in Utah.
The Bass Formation, also known as the Bass Limestone, is a Mesoproterozoic rock formation that outcrops in the eastern Grand Canyon, Coconino County, Arizona. The Bass Formation erodes as either cliffs or stair-stepped cliffs. In the case of the stair-stepped topography, resistant dolomite layers form risers and argillite layers form steep treads. In general, the Bass Formation in the Grand Canyon region and associated strata of the Unkar Group-rocks dip northeast (10°–30°) toward normal faults that dip 60+° toward the southwest. This can be seen at the Palisades fault in the eastern part of the main Unkar Group outcrop area. In addition, thick, prominent, and dark-colored basaltic sills intrude across the Bass Formation.
The Dox Formation, also known as the Dox Sandstone, is a Mesoproterozoic rock formation that outcrops in the eastern Grand Canyon, Coconino County, Arizona. The strata of the Dox Formation, except for some more resistant sandstone beds, are relatively susceptible to erosion and weathering. The lower member of the Dox Formation consists of silty-sandstone and sandstone, and some interbedded argillaceous beds, that form stair-stepped, cliff-slope topography. The bulk of the Dox Formation typically forms rounded and sloping hill topography that occupies an unusually broad section of the canyon.
The Battle at Fort Utah was a violent attack in 1850 in which 90 Mormon militiamen surrounded an encampment of Timpanogos families on the Provo River one winter morning, and laid siege for two days, eventually shooting between 40 and 100 Native American men and one woman with guns and a cannon during the attack as well as during the pursuit and capture of the two groups that fled the last night. One militiaman died from return fire during the siege. Of the Timpanogos people who fled in the night, one group escaped southward, and the other ran east to Rock Canyon. Both groups were captured, however, and the men were executed. Over 40 Timpanogos children, women, and a few men were taken as prisoners to nearby Fort Utah. They were later taken northward to the Salt Lake Valley and sold as slaves to church members there. The bodies of up to 50 Timpanogos men were beheaded by some of the settlers and their heads put on display at the fort as a warning to the mostly women and children prisoners inside.
Cascade Mountain is located in central Utah. With an elevation of 10,908 feet (3,325 m), it is not as high as its neighbors, to the north Mount Timpanogos and Provo Peak to the south, but it is one of the major peaks of the Wasatch Range.
The geology of Utah, in the western United States, includes rocks formed at the edge of the proto-North American continent during the Precambrian. A shallow marine sedimentary environment covered the region for much of the Paleozoic and Mesozoic, followed by dryland conditions, volcanism, and the formation of the basin and range terrain in the Cenozoic.
Kyhv Peak is a peak in the Wasatch Mountain range. It was once known as "Squaw Peak" and was officially renamed in 2022 as part of a federal order to remove the ethnic slur "squaw" from federally owned places in the United States.
