Junction Butte

Last updated
Junction Butte
Junction Butte from Grand View Point.jpg
North aspect from Grand View Point
Highest point
Elevation 6,400 ft (2,000 m) [1]
Prominence 1,720 ft (520 m) [1]
Parent peak Elaterite Butte (6,552 ft) [1]
Isolation 10.16 mi (16.35 km) [2]
Coordinates 38°17′11″N109°52′23″W / 38.286513°N 109.873045°W / 38.286513; -109.873045 Coordinates: 38°17′11″N109°52′23″W / 38.286513°N 109.873045°W / 38.286513; -109.873045 [1]
Geography
USA Utah location map.svg
Red triangle with thick white border.svg
Junction Butte
Location of Junction Butte in Utah
Usa edcp relief location map.png
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Junction Butte
Junction Butte (the United States)
Location Canyonlands National Park
San Juan County, Utah, U.S.
Parent range Colorado Plateau
Topo map USGS Monument Basin
Geology
Age of rock Late Triassic
Type of rock Wingate Sandstone
Climbing
Easiest route class 5.2 climbing [2]

Junction Butte is a 6,400-foot (2,000-meter) elevation summit located in the Island in the Sky District of Canyonlands National Park, in San Juan County, Utah. [3] It is set about one mile south of the southern tip of Island in the Sky. A short hike to Grand View Point provides a view of Junction Butte. Access to this butte is via the four-wheel drive White Rim Road, which is another option to view Junction Butte. Topographic relief is significant as the top of this geological formation rises 1,400 feet above the road in less than one mile. Precipitation runoff from Junction Butte drains east into the nearby Colorado River, and west into nearby Green River. Junction Butte is situated north of the junction of these two major rivers.

Contents

Geology

This feature is composed of hard, fine-grained Wingate Sandstone, which is the remains of wind-borne sand dunes deposited approximately 200 million years ago in the Late Triassic. This Wingate sandstone, capped by Kayenta Formation, forms steep cliffs as it overlays softer layers of the Chinle Formation. [4]

East aspect, from White Rim Road White Rim Road (Island in the Sky).jpg
East aspect, from White Rim Road

Climate

Spring and fall are the most favorable seasons to visit Junction Butte. 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 −0 °C (32 °F) and at least 50% of the total annual precipitation being received during the spring and summer. This desert climate receives less than 10 inches (250 millimeters) of annual rainfall, and snowfall is generally light during the winter.

Climate data for Island in the Sky Visitor Center, elevation 5,666 ft (1,727 m), 1981-2010 normals, extremes 1981-2019
MonthJanFebMarAprMayJunJulAugSepOctNovDecYear
Record high °F (°C)58.6
(14.8)
69.0
(20.6)
79.8
(26.6)
86.1
(30.1)
98.5
(36.9)
103.9
(39.9)
106.4
(41.3)
101.1
(38.4)
97.9
(36.6)
86.9
(30.5)
71.0
(21.7)
59.2
(15.1)
106.4
(41.3)
Average high °F (°C)38.1
(3.4)
44.1
(6.7)
54.9
(12.7)
63.5
(17.5)
74.2
(23.4)
85.4
(29.7)
91.7
(33.2)
88.7
(31.5)
79.5
(26.4)
65.8
(18.8)
49.7
(9.8)
38.1
(3.4)
64.6
(18.1)
Average low °F (°C)20.8
(−6.2)
25.8
(−3.4)
33.3
(0.7)
40.0
(4.4)
49.5
(9.7)
59.8
(15.4)
66.0
(18.9)
63.9
(17.7)
54.9
(12.7)
42.5
(5.8)
31.1
(−0.5)
21.3
(−5.9)
42.5
(5.8)
Record low °F (°C)−8.0
(−22.2)
−12.4
(−24.7)
10.4
(−12.0)
16.3
(−8.7)
26.0
(−3.3)
28.7
(−1.8)
46.0
(7.8)
50.2
(10.1)
27.6
(−2.4)
9.2
(−12.7)
6.2
(−14.3)
−9.4
(−23.0)
−12.4
(−24.7)
Average precipitation inches (mm)0.53
(13)
0.50
(13)
0.76
(19)
0.72
(18)
0.70
(18)
0.45
(11)
0.93
(24)
1.04
(26)
1.06
(27)
1.30
(33)
0.70
(18)
0.58
(15)
9.27
(235)
Average dew point °F (°C)18.6
(−7.4)
21.8
(−5.7)
23.3
(−4.8)
25.7
(−3.5)
29.5
(−1.4)
32.7
(0.4)
41.2
(5.1)
45.1
(7.3)
37.6
(3.1)
29.5
(−1.4)
23.2
(−4.9)
17.9
(−7.8)
28.9
(−1.7)
Source: PRISM [5]

See also

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Monster Tower

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Candlestick Tower

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Washer Woman

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Chimney Rock (Utah)

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Airport Tower (Canyonlands)

Airport Tower is a 700-foot (210-meter) tall sandstone butte located in the Island in the Sky District of Canyonlands National Park, in San Juan County, Utah. It is situated 1.64 mile east of Washer Woman, which is a towering arch similar in height. Each are composed of Wingate Sandstone, which is the remains of wind-borne sand dunes deposited approximately 200 million years ago in the Late Triassic. The nearest higher neighbor is Monster Tower, 1.6 mi (2.6 km) to the west, and Mesa Arch is situated 3.2 mi (5.1 km) to the west. A short hike to Mesa Arch provides the easiest view of Airport Tower. Access to this tower is via the four-wheel drive White Rim Road, which is another option to see Airport Tower. The top of this geological formation rises 1,400 feet above the road in less than one mile. Precipitation runoff from Airport Tower drains southeast into the nearby Colorado River via Buck and Lathrop Canyons. This geographical feature's name was officially adopted in 1986 by the U.S. Board on Geographic Names. It was so named because the rock formation resembles the appearance of an airport control tower.

Zeus and Moses

Zeus and Moses, variant Moses and Zeus, is a 500-foot (150-meter) tall sandstone formation located in the Island in the Sky District of Canyonlands National Park, in San Juan County, Utah. These rock towers' names refer to Zeus, god of Roman mythology, and Moses, an important prophet of several religions. Zeus and Moses is composed of Wingate Sandstone, which is the remains of wind-borne sand dunes deposited approximately 200 million years ago in the Late Triassic. This formation is situated in Taylor Canyon, 3 mi (4.8 km) north-northeast of Upheaval Dome. Access to the towers is via the four-wheel drive White Rim Road, and a spur road into Taylor Canyon. The top of this geological formation rises 900 feet above the canyon floor at road's end, approximately one-half mile away. Precipitation runoff from Zeus and Moses drains into the nearby Green River via Taylor Canyon.

Aztec Butte

Aztec Butte is a 6,312-foot (1,924-meter) elevation sandstone summit located in the Island in the Sky District of Canyonlands National Park, in San Juan County, Utah. Aztec Butte is composed of white cross-bedded Navajo Sandstone, which is the remains of wind-borne sand dunes deposited approximately 170 million years ago during the Jurassic Period. It resembles the Pyramid of the Sun in Mexico, which was built by the Aztecs. Ancestral Puebloans traveled to the Island in the Sky area to hunt and gather seeds, then stored their food in stone granaries near the top of Aztec Butte. These well-preserved granaries date to AD 1200–1300. A half-mile hiking trail through flat grassland, followed by a quarter-mile scramble with 200-feet gain, leads to the top of the butte and the granaries. The trailhead is located alongside the road to Upheaval Dome. In addition to Upheaval Dome, other nearby attractions include Mesa Arch which is situated less than 1 mi (1.6 km) to the southeast, Muffin Butte to the south, Green River Overlook to the southwest, and Trail Canyon to the north. Precipitation runoff from Aztec Butte drains to the Green River.

Eph Hanks Tower

Eph Hanks Tower is a 6,540-foot (1,990-meter) elevation summit located in Capitol Reef National Park, in Wayne County of Utah, United States. This landmark is situated 8 mi (13 km) southeast of the park's visitor center, 3.5 mi (5.6 km) south-southeast of Ferns Nipple, and 1.4 mi (2.3 km) south-southwest of Golden Throne, at the mouth of Capitol Gorge where the Capitol Reef Scenic Drive road ends. It towers 900 feet above the picnic area below its north aspect. Precipitation runoff from this feature is drained by Capitol Wash and Pleasant Creek, a tributary of the Fremont River, which in turn is within the Colorado River drainage basin. This geological feature is named after Ephraim Knowlton Hanks (1826–1896), a Mormon pioneer and first permanent settler in the Capitol Reef area, who with his family homesteaded in the Pleasant Creek area of Capitol Reef in 1881. Ephraim Hank's Floral Ranch on Pleasant Creek supposedly offered a safe retreat for polygamists along the Mormon underground railroad.

Buttes of the Cross

Buttes of the Cross is two sandstone summits located in the northern reach of Glen Canyon National Recreation Area, in Wayne County of Utah, United States. The larger and higher south butte reaches an elevation of 5,642 feet, whereas the north butte rises to 5,569 feet, with approximately 0.6 mile separation between them. When viewed from the north-northeast near Labyrinth Canyon, they align to form the shape of a cross, creating the appearance of a single butte. The name "Butte of the Cross" was first applied by John Wesley Powell during the Powell Geographic Expedition of 1869. A few miles further down the Green River, Powell finds that this geographical feature is two buttes when viewed from the east, so it was renamed Buttes of the Cross. Buttes of the Cross towers over 1,400 feet above its surrounding terrain. It is situated 6.8 miles west of Candlestick Tower, and one-half mile outside the boundary of Canyonlands National Park.

Ekker Butte

Ekker Butte is a 6,260-foot (1,910-meter) elevation summit located in the northern reach of Glen Canyon National Recreation Area, in Wayne County of Utah, United States. It is situated seven miles southeast of Buttes of the Cross, six miles northeast of Elaterite Butte, and less than two miles outside the boundary of Canyonlands National Park, where it towers over 1,400 feet above the surrounding terrain. Distant views of this remote butte can be seen from the Grand View Point and Green River Overlooks at Island in the Sky of Canyonlands National Park. This geological landmark is named for the pioneering Art Ekker family which operated the nearby Robbers Roost Ranch and grazed cattle on land adjacent to the nearby Maze. Arthur Benjamin Ekker (1911–1978) took Robert Redford on a tour of nearby Robbers Roost, the hideout of outlaw Butch Cassidy and the Wild Bunch.

Elaterite Butte

Elaterite Butte is a 6,552-foot (1,997-meter) elevation summit located in The Maze District of Canyonlands National Park, in Wayne County, Utah. Elaterite Butte is situated 6 mi (9.7 km) southwest of Ekker Butte, and the Maze Overlook is situated 2.5 mi (4.0 km) to the northeast. Elaterite Butte is composed of hard, fine-grained Wingate Sandstone, which is the remains of wind-borne sand dunes deposited approximately 200 million years ago in the Late Triassic. This Wingate sandstone overlays a 432-foot thick layer of the softer Chinle Formation. The top of this geological formation rises over 1,400 feet above Elaterite Basin. The butte and basin are named for elaterite, which is a dark brown, tar-like, elastic mineral resin that seeps from parts of the nearby White Rim Sandstone. Access to the remote butte is via a four-wheel drive road in Elaterite Basin. Precipitation runoff from Elaterite Butte drains into the nearby Green River, which in turn is within the Colorado River drainage basin.

Chip and Dale Towers

Chip and Dale Towers are two 300-foot (91-meter) tall sandstone towers located in the Island in the Sky District of Canyonlands National Park, in San Juan County, Utah. Dale Tower rises to an elevation of 5,620 feet, whereas the lower Chip Tower is 5,420-feet. Airport Tower is set 2.5 mi (4.0 km) to the southwest, and Dead Horse Point State Park overlook is situated 4.5 mi (7.2 km) to the north-northeast. Chip and Dale Towers are an eroded fin composed of hard, fine-grained Wingate Sandstone, which is the remains of wind-borne sand dunes deposited approximately 200 million years ago in the Late Triassic. This Wingate Sandstone overlays a softer layer of the Chinle Formation. Access to the towers is via the four-wheel drive White Rim Road, and a scramble to reach the base. The top of the towers rise over 1,000 feet above the road in approximately one-half mile. Precipitation runoff from Chip and Dale Towers drains east to the nearby Colorado River.

References

  1. 1 2 3 4 "Junction Butte, Utah". Peakbagger.com. Retrieved 2020-11-01.
  2. 1 2 "Junction Butte - 6,400' UT". listsofjohn.com. Retrieved 2020-11-01.
  3. "Junction Butte". Geographic Names Information System . United States Geological Survey . Retrieved 2020-11-01.
  4. S.W. Lohman, The Geologic Story of Canyonlands National Park, US Government Printing Office, 1974, page 25.
  5. "PRISM Climate Group, Oregon State University". Archived from the original on August 25, 2019. Retrieved February 19, 2019.