Tiki Tower | |
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Tiki Tower to right, north aspect | |
Highest point | |
Elevation | 5,500 ft (1,700 m) [1] |
Prominence | 160 ft (49 m) [1] |
Parent peak | Point 5601 [1] |
Isolation | 0.09 mi (0.14 km) [1] |
Coordinates | 38°23′54″N109°48′54″W / 38.3984°N 109.8149°W Coordinates: 38°23′54″N109°48′54″W / 38.3984°N 109.8149°W [1] |
Geography | |
Location | Canyonlands National Park San Juan County, Utah, U.S. |
Parent range | Colorado Plateau |
Topo map | USGS Musselman Arch |
Geology | |
Age of rock | Late Triassic |
Type of rock | Wingate Sandstone |
Climbing | |
First ascent | 1991 |
Easiest route | class 5.9 A1 Climbing [1] |
Tiki Tower is a thin 300-foot (91-meter) tall sandstone pinnacle located in the Airport Tower/Monster Tower/Washer Woman area of the Island in the Sky District of Canyonlands National Park, in San Juan County, Utah. [2] It is situated one-half mile northwest of Airport Tower, and is composed of Wingate Sandstone, which is the remains of wind-borne sand dunes deposited approximately 200 million years ago in the Late Triassic. Access to this tower is via the four-wheel-drive White Rim Road. The top of this spire rises 1,100 feet above the road in a little more than one mile. Precipitation runoff from Tiki Tower drains southeast into the nearby Colorado River via Buck and Lathrop Canyons. The first ascent of Tiki Tower was made in November 1991 by Jeff Widen and Mitch Allen, via Brave Little Toaster (5.11, 3 pitches), with Fred Lifton and Paul Frank working the first pitch. [3] [4]
Spring and fall are the most favorable seasons to visit Tiki Tower. 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. [5] This desert climate receives less than 10 inches (250 millimeters) of annual rainfall, and snowfall is generally light during the winter.
Mount Spry is a small 5,720-ft elevation mountain summit made of Navajo Sandstone located in Zion National Park, in Washington County of southwest Utah, United States. Officially named in 1934, it honors William Spry (1864-1929), the third governor of Utah. The nearest higher peak is The East Temple, 0.34 miles (0.55 km) to the east. Precipitation runoff from the mountain drains into tributaries of the North Fork Virgin River.
The East Temple is a prominent 7,709 feet (2,350 m) summit composed of Navajo Sandstone in Zion National Park, in Washington County of southwest Utah, United States. It is one of the notable landmarks in the park. The nearest neighbor is Twin Brothers, one-half mile to the north, and the nearest higher peak is The West Temple, 3.85 miles (6.20 km) to the west-southwest. The mountain is situated 1.8 miles northeast of the park headquarters, at the confluence of Pine Creek and the North Fork Virgin River. This feature's name was applied by John Wesley Powell during his explorations in 1872, and was officially adopted in 1934 by the U.S. Board on Geographic Names. The first ascent was made in 1937 by Glen Dawson, Dick Jones, Homer Fuller, Wayland Gilbert, and Jo Momyer.
Merrimac Butte is a 5,627-foot (1,715-metre) sandstone summit located in Grand County of Utah, United States. Merrimac Butte is situated 12 miles northwest of the town of Moab. Merrimac Butte is a thin 200-600 feet wide, and 1,600 feet long east-to-west butte with 200 ft vertical Entrada Sandstone walls overlaying a Carmel Formation base. Monitor Butte is situated immediately east of Merrimac Butte. These two buttes were named after The Monitor and The Merrimack, two American Civil War steamships. They can be seen from Highway 313 after it climbs out of Sevenmile Canyon en route to the Island in the Sky section of Canyonlands National Park or Dead Horse Point State Park.
Druid Arch is a 150-ft tall Cedar Mesa Sandstone arch located within the Needles District of Canyonlands National Park, in San Juan County, Utah. It is situated at the head of Elephant Canyon, and precipitation runoff from Druid Arch drains north into the nearby Colorado River via Elephant Canyon. Druid Arch is one of the most popular hiking destinations in the Needles district. A 5.4 mile hike to Druid Arch starts at the Elephant Hill Trailhead, and the final quarter-mile is steep with some scrambling and one ladder. The name comes from its resemblance to the Stonehenge monument in England, which is believed to be a Druid temple. This feature's name was officially adopted in 1963 by the U.S. Board on Geographic Names.
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. This feature's name was officially adopted in 1963 by the U.S. Board on Geographic Names. The first ascent was made in June 1993, by John Markel and Kevin Chase.
Monster Tower is a 600-foot (180-meter) tall sandstone tower located in the Island in the Sky District of Canyonlands National Park, in San Juan County, Utah. It is situated 300 feet southeast of Washer Woman, which is a towering arch nearly as high. Washer Woman is so named because the feature gives the appearance of a woman bent over a washtub. Monster and Washer Woman are an eroded fin 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 Aztec Butte, 2 mi (3.2 km) to the west-northwest, Airport Tower is set 1.6 mi (2.6 km) to the east, and Mesa Arch is situated 1.5 mi (2.4 km) to the west. A short hike to Mesa Arch provides the easiest view of Monster Tower. Access to the tower is via the four-wheel drive White Rim Road, which is the other way to see Monster. The top of this geological formation rises 1,400 feet above the road in approximately one mile. Precipitation runoff from Monster Tower drains southeast into the nearby Colorado River via Buck Canyon.
Candlestick Tower is a 450-foot (140-meter) tall sandstone butte located in the Island in the Sky District of Canyonlands National Park, in San Juan County, Utah. Its descriptive name is from its resemblance to a candlestick. Candlestick Tower is 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 Shaft Benchmark, 2 mi (3.2 km) to the east, Upheaval Dome is set 3 mi (4.8 km) to the north, and the Green River Overlook is situated 2.5 mi (4.0 km) to the east. Access to the tower is via the four-wheel drive White Rim Road. Candlestick is situated north of Soda Springs Basin and south of Holeman Spring Basin, and the top of this geological formation rises 1,400 feet above the White Rim Road in approximately one mile. Precipitation runoff from Candlestick Tower drains into the nearby Green River via these two basins.
Washer Woman is a 500-foot (150-meter) tall sandstone arch and tower located in the Island in the Sky District of Canyonlands National Park, in San Juan County, Utah. It is situated 300 feet northwest of the slightly higher Monster Tower. Washer Woman is so named because the feature gives the appearance of a washerwoman bent over a washtub. This geographical feature's name was officially adopted in 1986 by the U.S. Board on Geographic Names after previously having similar names such as Washer-Woman Arch and The Washer Woman. Washer Woman and Monster Tower are an eroded fin composed of Wingate Sandstone, which is the remains of wind-borne sand dunes deposited approximately 200 million years ago in the Late Triassic. Airport Tower is set 1.6 mi (2.6 km) to the east, and Mesa Arch is situated 1.5 mi (2.4 km) to the west. A short hike to Mesa Arch provides the easiest view of Washer Woman. Access to this formation is via the four-wheel drive White Rim Road, which is the other option to see it. The top of this geological formation rises 1,300 feet above the road in approximately one mile. Precipitation runoff from Washer Woman drains southeast into the nearby Colorado River via Buck Canyon.
The Witch Head is a 7,340-foot (2,237-meter) elevation white Navajo Sandstone summit located in Zion National Park, in Washington County of southwest Utah, United States. The Witch Head is situated in the "Towers of the Virgin", 2.5 mi (4.0 km) west of Zion's park headquarters, towering 3,300-feet above the floor of Zion Canyon and the Virgin River which drains precipitation runoff from this mountain. Its neighbors include The West Temple, The Sundial, Altar of Sacrifice, Meridian Tower, Bee Hive, and Three Marys. The first ascent of this feature was made in early March 1997 by Dan Stih and Ron Raimonde via the west face, which they rated a class 5.10 climb.
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, Tiki Tower is one-half mile northwest, 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, 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.
Crazy Quilt Mesa is a 6,760 ft (2,060 m) elevation white Navajo Sandstone summit located in Zion National Park, in Kane County of southwest Utah, United States. Crazy Quilt Mesa is situated southwest of the park's east entrance, towering 1,000-feet above the Zion – Mount Carmel Highway. Its nearest neighbor is Checkerboard Mesa, one-half mile immediately east, and separated by Checkerboard Mesa Canyon. This canyon holds pools of rainwater which provide a vital source of water for resident bighorn sheep. Other nearby peaks include Nippletop to the west, and Ant Hill to the northwest. Precipitation runoff from this mountain drains into tributaries of the Virgin River.
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.
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. 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.
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 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 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.
The Sixshooter Peaks are two iconic sandstone summits located in Bears Ears National Monument, in San Juan County of Utah, United States. The larger and higher North Sixshooter Peak rises to an elevation of 6,379 feet, whereas South Sixshooter Peak rises to 6,154 feet, with approximately 1.5 mile separation between the two. These buttes tower nearly 1,400 feet above the surrounding terrain, and are historic landmarks visible from State Route 211 between Newspaper Rock and the Needles District of Canyonlands National Park. They are situated 1.5 mile outside the boundary of the park, and four miles northwest of Bridger Jack Butte. Variant names for the peaks include "North Six-Shooter Peak", "South Six-shooter Peak", "Six Shooter Peaks", and "Six-shooter Peak". They are so named because of their resemblance to a pair of revolvers pointing skyward.
The Bridger Jack Butte is a sandstone summit located in Bears Ears National Monument, in San Juan County of Utah, United States. This butte, which is set at the northern tip of namesake Bridger Jack Mesa, and above the confluence of Indian and Lavender Creeks, rises to an elevation of 5,890 feet, and towers over 700 feet above the surrounding terrain and floor of Lavender Canyon to its west. This landmark is situated four miles southeast of Sixshooter Peaks, and is visible from State Route 211 between Newspaper Rock and the Needles District of Canyonlands National Park. "Bridger Jack" was a Paiute medicine man.
Window Blind Peak is a 7,030-foot elevation summit located in the San Rafael Swell of Emery County, Utah, U.S.. Towering 1,800 feet above its surrounding terrain, it is the highest point of the Mexican Mountain Wilderness Study Area. Ownership is administered by the Bureau of Land Management. It is situated 2.1 miles (3.4 km) southeast of Bottleneck Peak, and the nearest higher neighbor is Cedar Mountain, 8.95 miles (14.40 km) to the north-northeast. 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.