Temple Butte
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Temple Butte, in the
Grand Canyon The Grand Canyon is a steep-sided canyon carved by the Colorado River in Arizona, United States. The Grand Canyon is long, up to wide and attains a depth of over a mile (). The canyon and adjacent rim are contained within Grand Canyon Nati ...
,
Arizona Arizona is a U.S. state, state in the Southwestern United States, Southwestern region of the United States, sharing the Four Corners region of the western United States with Colorado, New Mexico, and Utah. It also borders Nevada to the nort ...
, US is a prominence below the East Rim. The butte lies on the west bank of the south-flowing
Colorado River The Colorado River () is one of the principal rivers (along with the Rio Grande) in the Southwestern United States and in northern Mexico. The river, the List of longest rivers of the United States (by main stem), 5th longest in the United St ...
. The outfall from the
Little Colorado River The Little Colorado River () is a tributary of the Colorado River in the U.S. state of Arizona, providing the principal drainage from the Painted Desert region. Together with its major tributary, the Puerco River, it drains an area of about in ...
, draining from the Painted Desert to the east and southeast, is about two miles upstream. Temple Butte is in elevation. It is the historical site of some wreckage of the
1956 Grand Canyon mid-air collision The Grand Canyon mid-air collision occurred in the Western United States, western United States on June 30, 1956, when a United Air Lines Douglas DC-7 struck a Trans World Airlines Lockheed L-1049 Super Constellation over Grand Canyon Nationa ...
. It was first thought that smoke from Temple Butte, was due to a lightning strike fire, but later was found to be the result of the mid-air collision. A closer view of Chuar and Temple Buttes.


Trails

The
Tanner Trail The Tanner Trail is a hiking trail located on the South Rim of the Grand Canyon National Park, located in the U.S. state of Arizona. The trailhead is located at Lipan Point, a prominent lookout located to the east of the Grand Canyon Village, a ...
from Desert View, Arizona down to the Colorado River, follows the west ridgeline of Tanner Canyon, and has numerous views looking due-north to Temple Butte. The trail ends at a viewpoint on the upper surfaces of a
Redwall Limestone The Redwall Limestone is an erosion-resistant, Mississippian age, cliff-former, cliff-forming geological formation that forms prominent, red-stained cliffs in the Grand Canyon. these cliffs range in height from to . It is one of the most fossili ...
ridge. The Redwall Limestone is seen prominently below the East Rim, and is the cliff-forming shelf upon which the redbeds of the Supai Group accumulate.


Geology

The prominence of Temple Butte is composed of the upper unit of the Supai Group, ("redbeds"), the
cliff-former A cliff-former is a geological unit of bedrock that is more resistant to erosion than overlying or underlying strata and consequently produces outcrops with high slope angles. It is more or less equivalent to ''ridge-former'', and may be contrast ...
,
Esplanade Sandstone The Lower Permian Esplanade Sandstone is a cliff-forming, resistant sandstone, dark red, geologic unit found in the Grand Canyon. The rock unit forms a resistant shelf in the west Grand Canyon, south side of the Colorado River, at the east of th ...
. The entire prominence is a much eroded, cliff remainder of the Esplanade, but the four units of the Supai Group, are compact, in an approximate north-south direction, with a large-
pyramid A pyramid () is a structure whose visible surfaces are triangular in broad outline and converge toward the top, making the appearance roughly a pyramid in the geometric sense. The base of a pyramid can be of any polygon shape, such as trian ...
-shape at the north, a pointed-pyramid at the south, and an eroded saddle in between. The Supai Group sits on the platform, upper surface of the
Redwall Limestone The Redwall Limestone is an erosion-resistant, Mississippian age, cliff-former, cliff-forming geological formation that forms prominent, red-stained cliffs in the Grand Canyon. these cliffs range in height from to . It is one of the most fossili ...
, on
Cambrian The Cambrian ( ) is the first geological period of the Paleozoic Era, and the Phanerozoic Eon. The Cambrian lasted 51.95 million years from the end of the preceding Ediacaran period 538.8 Ma (million years ago) to the beginning of the Ordov ...
rock units below. Another upper platform of the cliff-forming
Muav Limestone The Muav Limestone is a Cambrian geologic formation within the 5-member Tonto Group. It is a thin-bedded, gray, medium to fine-grained, mottled dolomite; coarse- to medium-grained, grayish-white, sandy dolomite and grayish-white, mottled, fine-g ...
, underlies the Redwall. (It is a double-platform rock unit.) The
slopes In mathematics, the slope or gradient of a Line (mathematics), line is a number that describes the direction (geometry), direction of the line on a plane (geometry), plane. Often denoted by the letter ''m'', slope is calculated as the ratio of t ...
of colorful
Bright Angel Shale The Bright Angel Shale is one of five geological formations that comprise the Cambrian Tonto Group. It and the other formations of the Tonto Group outcrop in the Grand Canyon, Arizona, and parts of northern Arizona, central Arizona, southeast Cali ...
are below. And below that are the short cliffs of
Tapeats Sandstone Except where underlain by the Sixtymile Formation, the Tapeats Sandstone is the Cambrian geologic formation that is the basal geologic unit of the Tonto Group. Typically, it is also the basal geologic formation of the Phanerozoic strata exposed ...
, (typically bordering gorges and the Colorado River), famous for making the
Tonto Platform Tonto is a fictional character; he is the Native American (either Tonto Apache, Comanche, or Potawatomi) companion of the Lone Ranger, a popular American Western character created by George W. Trendle and Fran Striker. Tonto has appeared in ...
, above the 1,000-million year old
Great Unconformity The term Great Unconformity is frequently applied to the unconformity observed by John Wesley Powell in the Grand Canyon in 1869. It is an exceptional example of relatively young sedimentary rock strata overlying much older sedimentary or crysta ...
of lost time, and eroded rock units. The east strike (section) of the Butte Fault is on the west side of Temple Butte. The west section of the Butte Fault is the East Kaibab Monocline. The Butte Fault sections are north-south trending, and are part of the uplift of the
Kaibab Plateau The Kaibab Plateau is a plateau almost entirely in Coconino County, Arizona (but extending slightly north into Kane County, Utah) in the Southwestern United States. The high plain is also known as the Buckskin Mountain, Buckskin Plateau, and Ka ...
.


Access

Desert View is the closest paved route site to Temple Butte viewpoints. It is located on the East Rim, and is about east of
Grand Canyon Village Grand Canyon Village is a census-designated place (CDP) located on the South Rim of the Grand Canyon, in Coconino County, Arizona, United States. Its population was 2,004 at the 2010 Census. Located in Grand Canyon National Park, it is wholly ...
, on the East Rim Road, (
Arizona State Route 64 State Route 64 (SR 64) is a State highway (US), state highway in Northern Arizona, the northern part of the US state of Arizona. It travels from its western terminus in Williams, Arizona, Williams to its intersection with U.S. Route 8 ...
). Desert View is also west of U.S. 89, by way of Arizona 64.


Observation viewpoints

Temple Butte can be viewed from the south at East Rim, Grand Canyon viewpoints in the vicinity of Desert View, Arizona. Lipan Point, Desert View Point, and to the south Hollenback Point have views due-north into the Grand Canyon. About north of Desert View Point by unimproved road, or hiking is Comanche Point, a distance of 5-mi south-southeast of Temple Butte. An unimproved route, going north from Desert View, about 12 to 14 mi long ends at Cape Solitude; the point is adjacent the south canyon outfall of the
Little Colorado River The Little Colorado River () is a tributary of the Colorado River in the U.S. state of Arizona, providing the principal drainage from the Painted Desert region. Together with its major tributary, the Puerco River, it drains an area of about in ...
and canyon, with the Colorado River. Temple Butte is west.Arizona DeLorme Atlas & Gazetteer, p. 32.


Gallery

File:Grand Canyon - panoramio (48).jpg, Cape Solitude,
Chuar Lava Hill,
Temple Butte &
Chuar Butte Chuar Butte is a prominent summit located in the Grand Canyon, in Coconino County of northern Arizona, US. It is situated 1.5 miles northwest of Cape Solitude on the canyon's East Rim, three miles southeast of Gunther Castle, and immediately ...
prominence File:Temple Butte, aerial from north.jpg, (aerial view)-Chuar Lava Hill,
Temple Butte,
Chuar Butte File:Chuar and Temple buttes.jpg, Chuar and
Temple Buttes File:Temple Butte, north aspect, Chuar Butte, East Flank - stratigraphy.png, Temple Butte,
(north aspect) and
(east aspect)
Chuar Butte (east aspect) File:Chuar and Temple buttes.jpg, A partial west
aspect of Temple
Butte.
shows Redwall on short
Muav Limestone cliff,
on Bright Angel Shale,
on Tapeats Sandstone
lining on the gorge edges


References

* Arizona Road & Recreation Atlas, Benchmark Maps, 2nd Edition, c. 1998, 112 pages, pp. 28–29, 62–63. * Arizona DeLorme Atlas & Gazetteer, 5th Edition, c. 2002, 76 pages, pp. 32, 24.


External links


Temple Butte, Eastern Grand Canyon, at Little Colorado River, (lat-long.com), coordinates, Coconino County, AZ
{{Geology of the Grand Canyon area Grand Canyon Landforms of Coconino County, Arizona Mountains of Arizona Mountains of Coconino County, Arizona