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Pyramidal peak. The Matterhorn, a classic example of a pyramidal peak. A pyramidal peak, sometimes called a glacial horn in extreme cases, is an angular, sharply pointed mountain peak which results from the cirque erosion due to multiple glaciers diverging from a central point. Pyramidal peaks are often examples of nunataks.
Arête. Striding Edge, an arête viewed from Helvellyn with the corrie Red Tarn to the left and Nethermost Cove to the right. An arête (/ əˈrɛt / ə-RET; French: [aʁɛt]) [1] is a narrow ridge of rock that separates two valleys. It is typically formed when two glaciers erode parallel U-shaped valleys. Arêtes can also form when two glacial ...
The Matterhorn (German: [ˈmatɐˌhɔʁn] ⓘ, Swiss Standard German: [ˈmatərˌhɔrn]; Italian: Cervino [tʃerˈviːno]; French: Cervin [sɛʁvɛ̃]; Romansh: Mont (e) Cervin (u)) [ note 3 ] is a mountain of the Alps, straddling the main watershed and border between Italy and Switzerland. It is a large, near-symmetric pyramidal peak in the ...
·dotted grey line: Snowdon Mountain Railway The ‘knife-edge’ arête of Crib Goch (foreground) and the pyramidal peak of Snowdon (background) are both the result of glaciation. The classic traverse of Crib Goch from East to West leads up from the Pyg track to a ‘bad step’, where hands and feet are both needed briefly.
A cirque (French: [siʁk]; from the Latin word circus) is an amphitheatre -like valley formed by glacial erosion. Alternative names for this landform are corrie (from Scottish Gaelic: coire, meaning a pot or cauldron) [1] and cwm (Welsh for 'valley'; pronounced [kʊm]). A cirque may also be a similarly shaped landform arising from fluvial erosion.
Alpspitze. The Alpspitze is a mountain, 2628 m, in Bavaria, Germany. Its pyramidal peak is the symbol of Garmisch-Partenkirchen and is one of the best known and most attractive mountains of the Northern Limestone Alps. It is made predominantly of Wetterstein limestone from the Upper Triassic.
The "knife-edge" arête of Crib Goch (foreground) and the pyramidal peak of Snowdon (background) are both the result of glaciation. A 1682 survey estimated that the summit of Snowdon was at an elevation of 3,720 feet (1,130 m); in 1773, Thomas Pennant quoted a later estimate of 3,568 ft (1,088 m) above sea level at Caernarfon.
Funeral Mountains. The Funeral Mountains is a short, arid mountain range in the United States along the California - Nevada border approximately 100 mi (160 km) west of Las Vegas. The mountains are considered a subrange of the Amargosa Range that form the eastern wall of Death Valley. The crest of the range is within Death Valley National Park.