Window Blind Peak | |
---|---|
Highest point | |
Elevation | 7,030 ft (2,143 m) [1] |
Prominence | 1,410 ft (430 m) [1] |
Parent peak | Cedar Mountain (7,665 ft) [1] |
Isolation | 8.99 mi (14.47 km) [1] |
Coordinates | 39°02′41″N110°39′23″W / 39.0447°N 110.6563°W [1] |
Geography | |
Country | United States |
State | Utah |
County | Emery |
Protected area | Mexican Mountain Wilderness |
Parent range | San Rafael Swell Colorado Plateau |
Topo map | USGS Bottleneck Peak |
Geology | |
Rock age | Late Triassic to Jurassic |
Rock type | sandstone, siltstone, shale |
Climbing | |
First ascent | 1973 |
Easiest route | class 5.7 climbing [1] |
Window Blind Peak is a 7,030-foot-elevation (2,143-meter) summit located in the San Rafael Swell of Emery County, Utah, U.S. [2] [3] Towering 1,800 feet above its surrounding terrain, it is the highest point of the Mexican Mountain Wilderness Study Area. [1] Ownership is administered by the Bureau of Land Management. It is situated 2.1 miles (3.4 km) southeast of Bottleneck Peak, 1.52 miles (2.45 km) south of Assembly Hall Peak, and the nearest higher neighbor is Cedar Mountain, 8.95 miles (14.40 km) to the north-northeast. [3] Precipitation runoff from this feature drains north into the nearby San Rafael River. The first ascent of this peak was made September 23, 1973, by Jim Langdon, Dale Black, and Dave Palmer via the West Face. [4]
This major erosional remnant along the San Rafael River is composed of Wingate Sandstone, which is the remains of wind-borne sand dunes deposited approximately 200 million years ago in the Late Triassic, overlain by Kayenta Formation, and capped by Jurassic Navajo Sandstone. [5] Lightly-colored slopes of Chinle Formation are exposed in places around the base of the mountain.
Spring and fall are the most favorable seasons to visit Window Blind Peak. According to the Köppen climate classification system, it is located in a Cold semi-arid climate zone, which is defined by the coldest month having an average mean temperature below 32 °F (0 °C), and at least 50% of the total annual precipitation being received during the spring and summer. [6] This desert climate receives less than 10 inches (250 millimeters) of annual rainfall, and snowfall is generally light during the winter.
Bottleneck Peak is a natural monolith located on the eastern side of Sids Mountain in the Utah San Rafael Swell wilderness area. It is situated 2.1 miles (3.4 km) northwest of Window Blind Peak. Precipitation runoff from this feature drains north into the San Rafael River.
The Titan is a 6,112-foot-elevation (1,863-meter) pillar in Grand County, Utah, United States.
Angel Arch is the largest natural arch located within Canyonlands National Park, in San Juan County, Utah. Some consider it the most beautiful and spectacular arch in the park, if not the entire canyon country. It is situated in a side canyon of Salt Creek Canyon, in the Needles District of the park. Precipitation runoff from Angel Arch drains north into the nearby Colorado River via Salt Creek. A 29-mile round-trip hike to Angel Arch leads to a viewpoint, and an additional 0.75-mile trail scrambles up into the arch opening. The arch's descriptive name comes from its resemblance to an angel with wings folded, and standing with its back to the arch opening. Before this feature's name was officially adopted in 1963 by the U.S. Board on Geographic Names, it was called Pegasus Arch. The first ascent was made in June 1993, by John Markel and Kevin Chase.
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Family Butte is a 7,405-foot-elevation (2,257-meter) summit in Emery County, Utah, United States.
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