In marine geology, a guyot, also known as a tablemount, is an isolated underwater volcanic mountain (seamount) with a flat top more than 200 m (660 ft) below the surface of the sea. The diameters of these flat summits can exceed 10 km (6.2 mi). Guyots are most commonly found in the Pacific Ocean, but they have been identified in all the oceans except the Arctic Ocean.
South Twin Mountain is a mountain located in Grafton County, New Hampshire. The mountain is part of the Twin Range of the White Mountains. South Twin forms the high point of a north-south ridge, with North Twin Mountain lying approximately one mile to the north and Mount Guyot two miles (3 km) to the southeast. Galehead Mountain, a lower spur of South Twin, is to the west.
Guyot Glacier is a 34-mile (55 km) long and 8-mile (13 km) wide glacier located in the east end of the Robinson Mountains in the U.S. state of Alaska. It begins 5.6 mi (9.0 km) north of Yaga Peak and heads east-southeast to Icy Bay, south of the Guyot Hills and 73 miles (117 km) northwest of Yakutat. It borders Yahtse Glacier on the northeast. The glacier was named by the New York Times expedition of 1886 for Arnold Henry Guyot.
Hills and mountains named Guyot, after geologist Arnold Guyot (1807–1884):
Mount Bond is a mountain located in Grafton County, New Hampshire, United States. The mountain is named after Professor George P. Bond (1825–1865) of Harvard University, and is the southernmost extension of the Twin Range of the White Mountains. Mount Bond is flanked to the north by Mount Guyot.
Mount Guyot is a mountain located in Grafton County, New Hampshire. The mountain is named after Professor Arnold H. Guyot (1807–1884) of Princeton University, and is part of the Twin Range of the White Mountains. Mount Guyot is flanked to the northwest by South Twin Mountain, to the northeast by Mount Zealand, and to the south by Mount Bond. Guyot is on the northern boundary of the Pemigewasset Wilderness. The immediate area around the summit consists of high-altitude spruce-fir forest or krummholz.
Silers Bald is a mountain in the western Great Smoky Mountains, located in the Southeastern United States. Its proximity to Clingmans Dome and its location along the Appalachian Trail make it a popular hiking destination.
Mount Kephart is a mountain in the central Great Smoky Mountains, located in the Southeastern United States. The Appalachian Trail crosses the mountain's south slope, making it a destination for thru-hikers. The Jumpoff, a 1,000-foot (300 m) cliff on the northeast side of the mountain, has views of the central and eastern Smokies. A stand of Southern Appalachian spruce-fir forest coats the mountain's upper elevations.
Old Black is a mountain in the Great Smoky Mountains, located in the Southeastern United States. While often overshadowed by Mount Guyot, its higher neighbor to the south, Old Black is the 5th-highest mountain in Tennessee and the 7th-highest in the Great Smoky Mountains National Park. The Appalachian Trail crosses its western slope, connecting the Cosby-area trail system with the heart of the Eastern Smokies.
Mount Guyot is a mountain in the eastern Great Smoky Mountains, located in the southeastern United States. At 6,621 feet (2,018 m) in elevation, Guyot is the fourth-highest summit in the Eastern U.S., and the second-highest in the Great Smoky Mountains National Park. While the mountain is remote, the Appalachian Trail crosses its south slope, passing to within 1,000 feet (300 m) of the summit.
Mount Sequoyah is a mountain in the Great Smoky Mountains, located in the Southeastern United States. It has an elevation of 6,003 feet above sea level. While the Appalachian Trail crosses its summit, Sequoyah is an 11.5-mile (18.5 km) hike from the nearest parking lot, making it one of the most remote places in the Great Smoky Mountains National Park.
Mount Collins is a mountain in the Great Smoky Mountains, located in the Southeastern United States. It has an elevation of 6,188 feet (1,886 m) above sea level. Located along the Appalachian Trail between Clingmans Dome and Newfound Gap, the mountain is a popular destination for thru-hikers. A backcountry shelter and a major trail junction are located along the mountain's northeastern slope. The mountain's summit is located amidst the Southern Appalachian spruce-fir forest that covers much of the upper elevations in the central Smokies.
Mount Chapman is a mountain in the Great Smoky Mountains, located in the Southeastern United States. It has an elevation of 6,417 feet above sea level. While the mountain is located deep within the Great Smokies, the Appalachian Trail crosses its eastern slope, coming to within 200 feet (61 m) of the summit. Mount Chapman is among the 10 highest mountains in the Appalachian range, if subpeaks are not included.
Bonticou Crag is a mountain in the Shawangunk Mountains, located in the Catskill Mountains of New York south of High Falls. Formally Known as Bunticoo Point and Bontecou Crag. Guyot Hill is located west-southwest of Bonticou Crag.
Mount Guyot is a high mountain summit in the Front Range of the Rocky Mountains of North America. The 13,376-foot (4,077 m) thirteener is located 6.3 miles (10.2 km) east-southeast of the Town of Breckenridge, Colorado, United States, on the Continental Divide separating Pike National Forest and Park County from Arapaho National Forest and Summit County. The mountain was named in honor of Arnold Henry Guyot, a Swiss-American geologist.
The Mid-Pacific Mountains (MPM) is a large oceanic plateau located in the central North Pacific Ocean or south of the Hawaiian–Emperor seamount chain. Of volcanic origin and Mesozoic in age, it is located on the oldest part of the Pacific Plate and rises up to 2 km (1.2 mi) above the surrounding ocean floor and is covered with several layers of thick sedimentary sequences that differ from those of other plateaux in the North Pacific. About 50 seamounts are distributed over the MPM. Some of the highest points in the range are above sea level which include Wake Island and Marcus Island.
Resolution Guyot is a guyot (tablemount) in the underwater Mid-Pacific Mountains in the Pacific Ocean. It is a circular flat mountain, rising 500 metres (1,600 ft) above the seafloor to a depth of about 1,320 metres (4,330 ft), with a 35 kilometres (22 mi) wide summit platform. The Mid-Pacific Mountains lie west of Hawaii and northeast of the Marshall Islands, but at the time of its formation the guyot was located in the Southern Hemisphere.
Allison Guyot is a tablemount (guyot) in the underwater Mid-Pacific Mountains of the Pacific Ocean. It is a trapezoidal flat mountain rising 1,500 metres above the seafloor to a depth of less than 1,500 m, with a summit platform 35 by 70 kilometres wide. The Mid-Pacific Mountains lie west of Hawaii and northeast of the Marshall Islands, but at the time of their formation were located in the Southern Hemisphere.
Cape Johnson Guyot is a guyot in the Pacific Ocean, more precisely in the Mid-Pacific Mountains, and the type locality of guyots. It is of middle Cretaceous age and a number of fossils have been dredged from it.
