The South Kaibab Trail is a hiking trail in Grand Canyon National Park, located in the U.S. state of Arizona. Unlike the Bright Angel Trail which also begins at the south rim of the Grand Canyon and leads to the Colorado River, the South Kaibab Trail follows a ridge out to Skeleton Point allowing for 360-degree views of the canyon.
The North Kaibab Trail is a hiking trail in the North Rim side of the Grand Canyon, in Grand Canyon National Park, located in the U.S. state of Arizona.
The Tonto Trail is a hiking trail on the South Rim of the Grand Canyon in Grand Canyon National Park, located in the U.S. state of Arizona.
The Boucher Trail is a hiking trail of the South Rim in Grand Canyon National Park, located in the U.S. state of Arizona.
The Clear Creek Trail is a hiking trail below the North Rim, from lower Bright Angel Canyon into lower Clear Creek Canyon of the Grand Canyon National Park, located in the U.S. state of Arizona.
The New Hance Trail is a hiking trail on the South Rim of the Grand Canyon National Park, located in the U.S. state of Arizona. It is one of the "unmaintained" trails and, along with the similar Tanner Trail, is considered one of the most difficult trails on the South Rim. Unlike the Tanner Trail, there is no parking available at the trailhead, which is located about a 5-minute walk north of the South Rim main road. The trail ends at the Hance Rapids on the Colorado River. It is approximately 6.5 hiking miles and a 4400' descent from the South Rim main road at ~7040' to the Colorado River at ~2600' elevation.
Newton Butte, in the Grand Canyon, Arizona, United States is a prominence below the South Rim, northwest of Grandview Point, and north on a ridgeline from Shoshone Point which is one mile east of Yaki Point, East Rim Drive. Shoshone Point and Yaki are both on access roads from East Rim Drive, with Yaki being the more advantageous to different viewing directions.
The Tonto Group is a name for an assemblage of related sedimentary strata, collectively known by geologists as a Group, that comprises the basal sequence Paleozoic strata exposed in the sides of the Grand Canyon. As currently defined, the Tonto groups consists of the Sixtymile Formation, Tapeats Sandstone, Bright Angel Shale, Muav Limestone, and Frenchman Mountain Dolostone. Historically, it included only the Tapeats Sandstone, Bright Angel Shale, and Muav Limestone. Because these units are defined by lithology and three of them interfinger and intergrade laterally, they lack the simple layer cake geology as they are typically portrayed as having and geological mapping of them is complicated.
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-grained limestone. It also contains beds of shale and intraformational conglomerate. The beds of the Muav Limestone are either structureless or exhibit horizontally laminations and cross-stratification. The Muav Limestone forms cliffs or small ledges that weather a dark gray or rusty-orange color. These cliffs or small ledges directly overlie the sloping surfaces of the Bright Angel Shale. The thickness of this formation decreases eastward from 250 feet (76 m) in the western Grand Canyon to 45 feet (14 m) in the eastern Grand Canyon. To the west in southern Nevada, its thickness increases to 830 feet (250 m) in the Frenchman Mountain region.
Temple Butte, in the Grand Canyon, Arizona, US is a prominence below the East Rim. The butte lies on the west bank of the south-flowing Colorado River. The outfall from the Little Colorado River, draining from the Painted Desert to the east and southeast, is about two miles upstream.
Isis Temple is a prominence in the Grand Canyon, Arizona, Southwestern United States. It is located below the North Rim and adjacent to the Granite Gorge along the Colorado River. The Trinity Creek and canyon flow due south at its west border; its north, and northeast border/flank is formed by Phantom Creek and canyon, a west tributary of Bright Angel Creek; the creeks intersect about 3 mi (4.8 km) southeast, and 1.0 mi (1.6 km) north of Granite Gorge. The Isis Temple prominence, is only about 202 ft (62 m) lower than Grand Canyon Village, the main public center on Grand Canyon’s South Rim.
The Grand Canyon Supergroup is a Mesoproterozoic to a Neoproterozoic sequence of sedimentary strata, partially exposed in the eastern Grand Canyon of Arizona. This group comprises the Unkar Group, Nankoweap Formation, Chuar Group and the Sixtymile Formation, which overlie Vishnu Basement Rocks. Several notable landmarks of the Grand Canyon, such as the Isis Temple and Cheops Pyramid, and the Apollo Temple, are surface manifestations of the Grand Canyon Supergroup.
The Surprise Canyon Formation is a geologic formation that consists of clastic and calcareous sedimentary rocks that fill paleovalleys and paleokarst of Late Mississippian (Serpukhovian) age in Grand Canyon. These strata outcrop as isolated, lens-shaped exposures of rocks that fill erosional valleys and locally karsted topography and caves developed in the top of the Redwall Limestone. The Surprise Canyon Formation and associated unconformities represent a significant period of geologic time between the deposition of the Redwall Limestone and the overlying Supai Group.
Vishnu Temple is a 7,533-foot-elevation (2,296-meter) summit located in the Grand Canyon, in Coconino County of Arizona, US.
Angels Gate is a 6,761-foot (2,061 m)-elevation summit located in the Grand Canyon, in Coconino County of Arizona, United States. It is situated seven miles (11 km) due north of the Grandview Point overlook on the canyon's South Rim, three miles (4.8 km) west of Vishnu Temple, and three point five miles (5.6 km) southeast of Zoroaster Temple. Topographic relief is significant as it rises over 4,200 feet (1,300 m) above the Colorado River in three miles. Angels Gate is the place in Paiute mythology where the gods would return to Earth by descending from the shadow world above.
Horseshoe Mesa is a 5,246-foot-elevation mesa-summit located in the eastern Grand Canyon, in Coconino County of northern Arizona, US. It is located 1.5 mi south of the Colorado River and Granite Gorge; also 4 mi due-south of the Cape Royal overlook, and ~2.0 mi northwest from Grandview Point, of the East South Rim, Grand Canyon. The Grandview Trail descends to Horseshoe Mesa, then drops down to meet the, the Tonto Trail.
Sinking Ship is a 7,344-foot (2,238 m) elevation summit located in the Grand Canyon, in Coconino County of northern Arizona, United States. This butte is situated 1.7 miles (2.7 km) southeast of the Grandview Point overlook on the canyon's South Rim, and 1.25 miles (2.01 km) southwest of Coronado Butte. Topographic relief is significant as it rises 4,800 feet (1,500 m) above the Colorado River in 4 miles (6.4 km). According to the Köppen climate classification system, Sinking Ship is located in a cold semi-arid climate zone.
Topaz Canyon is a linear, narrow canyon in the western Grand Canyon, below the South Rim. It lies in a region of four canyons, and a fifth smaller canyon, all trending mostly northeasterly towards the west-flowing Colorado River, in western Grand Canyon National Park. The name of Topaz Canyon was named by the Board of Geographical Names for precious stones of the region. Topaz Canyon is the southeast border of the linear, and major, forested-landform, Diana Temple; .
The northeast terminus of Topaz Canyon intersects with the outfall of Boucher Canyon and the tract of the Tonto Trail. The Boucher Trail starting in Hermit Canyon,, ends at the termini of both Topaz and Boucher Canyons.
Mescalero Point is a 6,627 foot (2,020 m)-cliff-elevation point located in the central,, Grand Canyon, Coconino County of northern Arizona, United States. Mescalero Point is 3.6 miles from its closest highest scenic viewpoint, Yuma Point (6,654 ft), located east at Eremita Mesa, at the northeast, overlooking Central Hermit Canyon.
Mescalero Point is in a region of points, at the headwaters of canyons, and landforms below the South Rim. Jicarilla Point lies ~1.0 mile west-northwest, and Mimbreno Point lies ~0.7 miles southeast.
Mescalero Point is distinctive because it has separated from the water divide between two canyons, by flat and forested, Diana Temple, which is narrow and linear, about a mile long. A saddle, about 0.1 mi long separates Mescalero Point from Diana Temple. Mescalero Point is at the headwaters of Slate Canyon, northwest, and Topaz Canyon, southeast.
