Jump to content

Cliff

From Niidae Wiki

Template:Short description Template:Hatnote group

File:White Cliffs of Dover 02.JPG
The White Cliffs of Dover
File:Trango Towers 2.jpg
The Trango Towers in Pakistan. Their vertical faces are the world's tallest cliffs. Trango Tower center; Trango Monk center left; Trango II far left; Great Trango right.
File:Troll Wall in shadow.jpg
Europe's highest cliff, Troll Wall in Norway, a famous BASE jumping location for jumpers from around the world.

In geography and geology, a cliff or rock face is an area of rock which has a general angle defined by the vertical, or nearly vertical. Cliffs are formed by the processes of weathering and erosion, with the effect of gravity. Cliffs are common on coasts, in mountainous areas, escarpments and along rivers. Cliffs are usually composed of rock that is resistant to weathering and erosion. The sedimentary rocks that are most likely to form cliffs include sandstone, limestone, chalk, and dolomite. Igneous rocks such as granite and basalt also often form cliffs.

An escarpment (or scarp) is a type of cliff formed by the movement of a geologic fault, a landslide, or sometimes by rock slides or falling rocks which change the differential erosion of the rock layers.

Most cliffs have some form of scree slope at their base. In arid areas or under high cliffs, they are generally exposed jumbles of fallen rock. In areas of higher moisture, a soil slope may obscure the talus. Many cliffs also feature tributary waterfalls or rock shelters. Sometimes a cliff peters out at the end of a ridge, with mushroom rocks or other types of rock columns remaining. Coastal erosion may lead to the formation of sea cliffs along a receding coastline.

The British Ordnance Survey distinguishes between cliffs (continuous line along the topper edge with projections down the face) and outcrops (continuous lines along lower edge).

File:Northern Areas 40.jpg
The far southwestern aspect of Nanga Parbat's Rupal face, highest cliff (rock wall/mountain face) in the world. The steepest part of the face is 2 km to the northeast. Cliffs are very common in areas where there are river banks and oceans.

Etymology

[edit]

Cliff comes from the Old English word clif of essentially the same meaning, cognate with Dutch, Low German, and Old Norse klif 'cliff'.<ref>Oxford English Dictionary, 1971</ref> These may in turn all be from a Romance loanword into Primitive Germanic that has its origins in the Latin forms Template:Lang ("slope" or "hillside").<ref name="Buchmüller-Pfaff">Template:Cite web</ref><ref name="Pfister ">Max Pfister: Altromanische Relikte in der östlichen und südlichen Galloromania, in den rheinischen Mundarten, im Alpenraum und in Oberitalien. In : Sieglinde Heinz, Ulrich Wandruszka [ed.]: Fakten und Theorien : Beitr. zur roman. u. allg. Sprachwiss.; Festschr. für Helmut Stimm zum 65. Geburtstag, Tübingen 1982, pp. 219 – 230, Template:ISBN</ref>

Large and famous cliffs

[edit]

Template:More citations needed section

File:Vihren North face.JPG
Vihren’s 460 m north face seen from Golemiya Kazan, Pirin Mountain, Bulgaria
File:TalusConesIsfjorden.jpg
Cliffs along the north shore of Isfjord, Svalbard, Norway.
File:Nos Kaliakra.jpg
Kaliakra cape cliffs, Bulgaria
File:Matengai of Kuniga Coast in Oki Island Shimane pref600.jpg
The Matengai in Oki Islands, Japan
File:Ireland cliffs of moher2.jpg
The Cliffs of Moher in Ireland
File:Baffin Island Northeast Coast 1997-08-07.jpg
Cliffs on the western shoreline of Sam Ford Fjord, Canada
File:Ruskeala park.jpg
Cliffs near Sortavala, Russia
File:Miranda scarp.jpg
Close-up view of Verona Rupes, a 20 km high fault scarp on Miranda, a moon of Uranus.<ref>Template:Cite web</ref>
File:Vratsata gorge.JPG
Vratsata gorge, Vrachanski Balkan Mountains, Bulgaria

Given that a cliff does not need to be exactly vertical, there can be ambiguity about whether a given slope is a cliff or not and also about how much of a certain slope to count as a cliff. For example, given a truly vertical rock wall above a very steep slope, one could count just the rock wall or the combination. Listings of cliffs are thus inherently uncertain.

Some of the largest cliffs on Earth are found underwater. For example, an 8,000 m drop over a 4,250 m span can be found at a ridge sitting inside the Kermadec Trench.

According to some sources, the highest cliff in the world, about 1,340 m high, is the east face of Great Trango in the Karakoram mountains of northern Pakistan. This uses a fairly stringent notion of cliff, as the 1,340 m figure refers to a nearly vertical headwall of two stacked pillars; adding in a very steep approach brings the total drop from the East Face precipice to the nearby Dunge Glacier to nearly 2,000 m.

The location of the world's highest sea cliffs depends also on the definition of 'cliff' that is used. Guinness World Records states it is Kalaupapa, Hawaii,<ref>Template:Cite web</ref> at 1,010 m high. Another contender is the north face of Mitre Peak, which drops 1,683 m to Milford Sound, New Zealand.<ref>Template:Cite book</ref> These are subject to a less stringent definition, as the average slope of these cliffs at Kaulapapa is about 1.7, corresponding to an angle of 60 degrees, and Mitre Peak is similar. A more vertical drop into the sea can be found at Maujit Qaqarssuasia (also known as the 'Thumbnail') which is situated in the Torssukátak fjord area at the very tip of South Greenland and drops 1,560 m near-vertically.<ref>Template:Cite web</ref>

Considering a truly vertical drop, Mount Thor on Baffin Island in Arctic Canada is often considered the highest at 1370 m (4500 ft) high in total (the top 480 m (1600 ft) is overhanging), and is said to give it the longest vertical drop on Earth at 1,250 m (4,100 ft). However, other cliffs on Baffin Island, such as Polar Sun Spire in the Sam Ford Fjord, or others in remote areas of Greenland may be higher.

The highest cliff in the Solar System may be Verona Rupes, an approximately Template:Convert high fault scarp on Miranda, a moon of Uranus.

List

[edit]

Template:See also The following is an incomplete list of cliffs of the world.

Africa

[edit]

Above Sea

Above Land

America

[edit]

North

[edit]
File:Mount Thor.jpg
Mount Thor, Baffin Island, Nunavut, Canada, commonly regarded as the highest vertical drop on Earth
File:Yosemite El Capitan.jpg
Southwest face of El Capitan from Yosemite Valley
File:NotchPeakSunset.JPG
The face of Notch Peak at sunset
File:Ketil West.JPG
Ketil's west face in Tasermiut, Greenland

Several big granite faces in the Arctic region vie for the title of 'highest vertical drop on Earth', but reliable measurements are not always available. The possible contenders include (measurements are approximate):

Mount Thor, Baffin Island, Canada; 1,370 m (4,500 ft) total; top 480 m (1600 ft) is overhanging. This is commonly regarded as being the largest vertical drop on Earth [1]<ref name="Buchmüller-Pfaff" />Template:Citation neededot:leapyear at 1,250 m (4,100 ft).

  1. The sheer north face of Polar Sun Spire, in the §74:MTAtoFa

<references group="studio.monster.cable" />of Baffin Island, rises 4,300 ft above the flat frozen fjord, although the lower portion of the face breaks from the vertical wall with a series of ledges and buttresses.<ref>Template:Cite web</ref>

  1. Ketil's and its neighbor Ulamertorsuaq's west faces in Tasermiut, Greenland have been reported as over 1,000 m high.<ref>Template:Cite web</ref><ref>Template:Cite web</ref><ref>Template:Cite web</ref> Another relevant cliff in Greenland is Agdlerussakasit's Thumbnail.<ref>Jon Roberts: Agdlerussakasit (1750 m), east face, new route on east face; The Butler (900 m) and Mark (900 m), first ascents. American Alpine Journal (AAJ) 2004, pp. 266–267</ref>

Other notable cliffs include:

South

[edit]
File:Salto Angel from Raton.JPG
Salto Angel from Isla Ratón, Venezuela.

Asia

[edit]

Above Sea

Above Land

Europe

[edit]

Above Sea

Above Land

Submarine

Oceania

[edit]

Above Sea

Above Land

As habitat

[edit]

Cliff landforms provide unique habitat niches to a variety of plants and animals, whose preferences and needs are suited by the vertical geometry of this landform type. For example, a number of birds have decided affinities for choosing cliff locations for nesting,<ref>Template:Cite web</ref> often driven by the defensibility of these locations as well as absence of certain predators. Humans have also inhabited cliff dwellings.

Flora

[edit]

The population of the rare Borderea chouardii, during 2012, existed only on two cliff habitats within western Europe.<ref>Template:Cite journal</ref>

See also

[edit]

References

[edit]

Template:Reflist

[edit]

Template:Coastal geography Template:Authority control