Three Penguins | |
---|---|
Highest point | |
Elevation | 4,488 ft (1,368 m) [1] |
Prominence | 120 ft (37 m) [2] |
Isolation | 0.65 mi (1.05 km) [2] |
Coordinates | 38°37′09″N109°37′05″W / 38.6192228°N 109.6179263°W [1] |
Geography | |
Country | United States |
State | Utah |
County | Grand |
Protected area | Arches National Park |
Parent range | Colorado Plateau [3] |
Topo map | USGS Moab |
Geology | |
Rock age | Jurassic |
Rock type | Entrada Sandstone [4] |
Climbing | |
First ascent | 1976 |
Easiest route | class 5.10a climbing [2] |
Three Penguins is a 4,488-foot-elevation (1,368-meter) summit in Grand County, Utah, United States.
Three Penguins is located within Arches National Park and it is the first notable rock feature to greet visitors as they enter the park on the main road. [5] Like many of the rock formations in the park, it is composed of Entrada Sandstone, specifically the Slick Rock Member overlaying the Dewey Bridge Member. [4] [6] The tower is 140 feet tall, [7] and topographic relief is significant as the summit rises 350 feet (107 meters) above Moab Canyon in 0.15 miles (0.24 km). Precipitation runoff from Three Penguins drains to the nearby Colorado River via Moab Canyon. This landform's descriptive toponym has been officially adopted by the United States Board on Geographic Names. [1]
The first ascent of the summit was made in November 1976 by Larry Bruce, Molly Higgins, and Michael Kennedy via the class 5.10 Center Chimney. [8] [9]
Other rock-climbing routes on Three Penguins:
The Right Chimney is considered one of the best rock-climbing routes in the park. [7]
According to the Köppen climate classification system, Three Penguins is located in a cold semi-arid climate zone with cold winters and hot summers. [13] Spring and fall are the most favorable seasons to experience Arches National Park, when highs average 60 to 80 °F (15 to 25 °C) and lows average 30 to 50 °F (0 to 10 °C). Summer temperatures often exceed 100 °F (40 °C). Winters are cold, with highs averaging 30 to 50 °F (0 to 10 °C), and lows averaging 0 to 20 °F (−20 to −5 °C). As part of a high desert region, it can experience wide daily temperature fluctuations. The park receives an average of less than 10 inches (25 cm) of rain annually.
Arches National Park is a national park of the United States in eastern Utah. The park is adjacent to the Colorado River, 4 mi (6 km) north of Moab, Utah. The park contains more than 2,000 natural sandstone arches, including the well-known Delicate Arch, which constitute the highest density of natural arches in the world. It also contains a variety of other unique geological resources and formations. The national park lies above an underground evaporite layer or salt bed, which is the main cause of the formation of the arches, spires, balanced rocks, sandstone fins, and eroded monoliths in the area.
The Titan is a 6,112-foot-elevation (1,863-meter) pillar in Grand County, Utah, United States.
Mount Tukuhnikivatz is a 12,482-foot elevation summit located in San Juan County of Utah, United States. Mount Tukuhnikivatz is the third-highest peak of the La Sal Mountains, and is the premier ski mountaineering destination in the La Sals. It is situated in a dry, rugged, sparsely settled region, and set on land administered by Manti-La Sal National Forest. Precipitation runoff from this mountain drains into tributaries of the Colorado River. The nearest town is Moab, 19 mi (31 km) to the northwest, and the nearest higher neighbor is Mount Peale, 1.7 mi (2.7 km) to the east. The mountain's name is a Native American word that translates as "Where the sun sets last." Locals call it Mount Tuk for short. This mountain has a subsidiary peak unofficially called Little Tuk, approximately one-half mile to the north-northwest.
Chimney Rock is a 6,420-foot (1,960 m) summit in Capitol Reef National Park in Wayne County, Utah, United States. This landmark is situated 2.5 mi (4.0 km) northwest of the park's visitor center, towering over 300 feet (91 m) above Utah State Route 24. Chimney Rock is also 2.5 mi (4.0 km) northwest of another of the park's landmarks, The Castle. Precipitation runoff from this feature ends up in the Colorado River drainage basin. The Chimney Rock Trail is a 3.5-mile loop trail that takes hikers to a view of Chimney Rock from above Mummy Cliffs.
The Three Gossips is a 4,700-foot-elevation (1,433-meter) sandstone pillar in Grand County, Utah, United States.
Kingfisher Tower is a 6,794-foot-elevation (2,071-meter) pillar in Grand County, Utah, United States.
Argon Tower is a 4,750-foot-elevation (1,448-meter) pillar in Grand County, Utah. It is located within Arches National Park and like many of the rock formations in the park, Argon Tower is composed of Entrada Sandstone. The tower is 260 feet tall, and topographic relief is significant as the summit rises 450 feet vertically above the Park Avenue Trail in 400 feet laterally. Precipitation runoff from Argon Tower drains to the nearby Colorado River via Courthouse Wash. This landform was shown briefly in the opening scene credits of the 1989 American action-adventure film Indiana Jones and the Last Crusade.
Tower of Babel is a 4,655-foot-elevation (1,419-meter) summit in Grand County, Utah. It is located within Arches National Park and like many of the rock formations in the park, it is composed of Entrada Sandstone. The tower is 500 feet tall, and topographic relief is significant as the summit rises 500 feet vertically above the main park road in approximately 200 feet laterally. Precipitation runoff from Tower of Babel drains to the nearby Colorado River via Courthouse Wash. This landform's descriptive toponym has been officially adopted by the United States Board on Geographic Names. This landform was shown briefly in the opening scene of the 1989 American action-adventure film Indiana Jones and the Last Crusade.
The Organ is a 4,735-foot-elevation (1,443-meter) pillar in Grand County, Utah, United States
Queen Nefertiti Rock is a 4,741-foot-elevation (1,445-meter) pillar in Grand County, Utah. The feature is located within Arches National Park and like many of the rock formations in the park, Queen Nefertiti Rock is composed of Entrada Sandstone. Topographic relief is significant as the summit rises 400 feet above the Park Avenue Trail in 0.1 mile. Precipitation runoff from Queen Nefertiti Rock drains to the nearby Colorado River via Courthouse Wash. This landform's descriptive toponym has been officially adopted by the United States Board on Geographic Names, and is so named because the feature resembles the head of Queen Nefertiti.
Cottontail Tower is a 5,980-foot-elevation (1,823-meter) pillar in Grand County, Utah, United States.
Ancient Art is a 5,420-foot-elevation (1,652-meter) pillar in Grand County, Utah, United States.
Echo Tower is a 5,784-foot-elevation (1,763-meter) pillar in Grand County, Utah, United States.
The Oracle is a 6,060-foot-elevation (1,847-meter) pillar in Grand County, Utah, United States.
Sheep Rock is a 4,564-foot-elevation (1,391-meter) pillar in Grand County, Utah. It is located within Arches National Park and like many of the rock formations in the park, it is composed of Entrada Sandstone, specifically the Slick Rock Member overlaying the Dewey Bridge Member. The tower is 440 feet tall, and is approximately 0.15 mile from the main park road. Sheep Rock is believed to be a remnant abutment of an ancient fallen arch. Precipitation runoff from Sheep Rock drains to the nearby Colorado River via Courthouse Wash. This landform's descriptive toponym has been officially adopted by the United States Board on Geographic Names.
Queen Victoria Rock is a 4,780-foot-elevation (1,457-meter) pillar in Grand County, Utah, United States.
Jello Tower is a 4,510-foot-elevation (1,375-meter) pillar in Grand County, Utah, United States.
The Candelabrum is a 4,700-foot-elevation (1,433-meter) pillar in Grand County, Utah, United States.
Mars Hotel is a 4,635-foot-elevation (1,413-meter) summit in Grand County, Utah, United States.
Marching Men is an area of pillars in Grand County, Utah, United States.