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Mountain in Alberta and British Columbia, Canada
Scarp Mountain is located on the border of Alberta and British Columbia, at the southern end of Mount Robson Provincial Park. It was named in 1922 by Arthur
Scarp_Mountain
Steep slope or cliff separating two relatively level regions
the term scarp to be incorrectly used interchangeably with escarpment, which refers to the margin between two landforms as opposed to scarp, which refers
Escarpment
Scarp east of Perth, Western Australia
The Darling Scarp (Nyungar: Katta Moorda), also referred to as the Darling Range or Darling Ranges, is a low escarpment running north–south to the east
Darling_Scarp
Feature of the Pacific Ocean floor
Rise The Wishbone scarp is a Pacific Ocean floor feature in the oceanic crust, that if were on land would be similar to a mountain range fault system
Wishbone_scarp
Mountain range in south-central Tanzania
are protected by the Udzungwa Mountains National Park and the Udzungwa Scarp Nature Forest Reserve. The Udzungwa Mountains are covered with lowland rainforest
Udzungwa_Mountains
Strzelecki Ranges Victorian Alps Carnarvon Range(s) Chichester Range Darling Scarp Hamersley Range Musgrave Ranges Napier Range Ophthalmia Range Oscar Range
Mountain_ranges_of_Australia
National park in the eastern Sanaag region of Somaliland
steeply from the coastal plain to the top of the scarp of the limestone mountains. On the summit of the scarp, average annual rainfall is about 650 mm. Daallo
Daallo_Mountain
Mountain in Ross Dependency, Antarctica
78.100°S 161.450°E / -78.100; 161.450. A pointed, mostly ice-covered mountain, 2,450 metres (8,040 ft) high, located 4 nautical miles (7.4 km; 4.6 mi)
Colwell_Massif
Features of the moon of Jupiter
Ionian mountains have been summarized. Basal scarps: basal scarps always appear as an abrupt boundary of Ionian mountains that separate mountains from volcanic
Mountains_of_Io
list of the tallest mountains in the Solar System. This list includes peaks on all celestial bodies where significant mountains have been detected. For
List of tallest mountains in the Solar System
List_of_tallest_mountains_in_the_Solar_System
Scarp retreat is a geological process through which the location of an escarpment changes over time. Typically the cliff is undermined, rocks fall and
Scarp_retreat
Martian volcano, highest point on Mars
University Press. p. 132. ISBN 978-0-521-80393-9. "HiRISE | Layers in a Scarp on Olympus Mons (PSP_001432_2015)". hirise.lpl.arizona.edu. Retrieved 2025-05-17
Olympus_Mons
Large blocks of rock created by tectonic and localized stresses in Earth's crust
and that of Mesta. Tilted type block mountains have one gently sloping side and one steep side with an exposed scarp, and are common in the Basin and Range
Fault_block
on scarp slopes where, although the height difference is not so great, they tend to have a larger catchment area than mountain streams. Mountain streams
Mountain_stream
Mountain range, west of Brecon Beacons, Wales
are to be found beneath the spectacular north and east facing sandstone scarps in the north-east of the range, especially below Fan Hir. There are smaller
Black_Mountain_(range)
Steeply sloping triangular landform
Talus flatirons lie within the scarp slope – and pediment flatirons occur within the transition zone between scarp and foreland. Pediment flatirons
Flatiron_(geomorphology)
Hill or ridge with a gentle slope on one side and a steep slope on the other
wine-growing regions of Côte d'Or. Cuestas are very widespread in the Caucasus Mountains' northern part, with each progressive ridge from north to south being
Cuesta
Mountain range in Central Europe
The Ore Mountains are a Hercynian block tilted so as to present a steep scarp face towards Bohemia and a gentle slope on the German side. They were formed
Ore_Mountains
Escarpment in Canada and the United States
the Genesee River flows through the city in three waterfalls over the scarp face. The escarpment thence runs westward to the Niagara River, forming
Niagara_Escarpment
Place in Azerbaijan
heights of up to 3 metres (9.8 ft) at the base of a 10-metre-wide (33 ft) scarp below a hillside, although other sources cite varying figures. Yanar Dagh
Yanar_Dagh
Mountain range in Riverside County, in southern California
fault on the west and the San Andreas fault system on the east. The fault scarp on the northern and eastern side is one of the most abrupt in North America
San_Jacinto_Mountains
Paleozoic fold and thrust belt in South Africa
Cape Fold Belt (CFB) is a 1,300 kilometres (810 mi) long fold-and-thrust mountain belt along the western and southern coastlines of Western Cape, South Africa
Cape_Fold_Belt
Rounded hills of bare granite formed by exfoliation
well as the maintenance of scarps of essentially constant inclination and morphology during backwearing. Sugarloaf Mountain in Rio de Janeiro, Brazil Liberty
Granite_dome
Mountain in Western Australia
Australia town of Jarrahdale, is one of the highest points on the Darling Scarp, at 582 metres (1,909 ft). It was named after William Ernest Cooke, Western
Mount_Cooke
Tall, near vertical rock face
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
Cliff
Major feature group in the Transantarctic Mountains
from the shelf ice, stand great tabular mountain masses, 13,000 feet high, having a sharply defined fault-line scarp on the northern side. The northern foothills
Queen_Maud_Mountains
Long, narrow, elevated landform
side of a strike ridge is relatively short, steep or cliff-like slope (scarp slope) that cuts across the tilted layers of rocks. In foldbelts such as
Ridge
Raised landform with a flat top
Watson-Morris, M.J.; Wigginton, S.S. (2016). "Observations on normal-fault scarp morphology and fault system evolution of the Bishop Tuff in the Volcanic
Tableland
Volcano in Hawaii
topography as essentially a flat crater floor surrounded by cones and fault scarps, the main caldera is affected relatively little by erosion from water. Most
Kohala_(mountain)
Volcano in the Azores, Portugal
Eastern Fissural zone, that includes many of the volcanic alignments and scarps. The second fault zone, running NNW-SSE, are markedly less in number and
Mount_Pico
Mountain in Western Australia
the first European explorer to venture into the Darling Scarp. Western Australia portal Mountains portal Mount Cooke Mount Gunjin "The Sketcher". Western
Mount_Dale
Mountain range in Southern Greece
of the dip, causing earthquakes. Single earthquakes result in 1–12 m of scarp. The Sparta fault is zig-zag in strike, varying between N 170° E and N 140°
Taygetus
Ridge of erosion-resistant rock in South Africa
less commonly, the Reef) is a 56-kilometre-long (35 mi), north-facing scarp in South Africa. It consists of a hard, erosion-resistant quartzite metamorphic
Witwatersrand
Fault line in North America
right-lateral event in 1972 and a relatively young (Holocene) 14 km (8.7 mi) scarp with a maximum offset of 2.5 m (8 ft 2 in). A 2025 study suggests that stress
Tintina_Fault
Branch of geomorphology
can cause fault scarps to appear either individually or as multiple subparallel scarps. Valleys are the low areas lying between mountains or hills in which
Morphotectonics
Area of East Riding of Yorkshire, England
Chalk formations form the lower parts of the west and north facing Wolds scarp but it is the overlying Welton Chalk Formation which forms the greater part
Yorkshire_Wolds
Most of Alberta's mountains are found on the western edge of the province of Alberta, consisting of the eastern slopes of the Canadian Rockies, which
List_of_mountains_of_Alberta
Draw – Long area of downward-sloping low ground Escarpment, also known as scarp – Steep slope or cliff separating two relatively level regions Fall line –
Glossary_of_landforms
River in Greece
that develops at the foot of the scarp and crosses under Route 48 just below the pass east of Arachova, a mountain city. The upper Pleistos and its valley
Pleistos
Range of hills in east central Scotland
It is the Portpatrick Formation which forms the main northwest facing scarp. There are also small fault-related intercalations of the Moffat Shales
Moorfoot_Hills
Mountain range
The Songwe Scarp terminates the Rukwa Trough at its southeast end and forms the northwestern side of the Mbeya Range. The Poroto Mountains and Mount Rungwe
Mbeya_Range
Mountain in Italy
activity is showed by structures like the Cordone del Vettore, a fault scarp that reactivated after the 2016–17 Central Italy earthquakes. The southwestern
Monte_Vettore
Mountains in Morogoro Region, Tanzania
rare tree Dombeya amaniensis is also found in this region. The Mahenge Scarp Catchment Forest Reserve, established in 1954, is 3.87 km2 in area and begins
Mahenge_Mountains
Geology of Mercury, Venus, Earth, Mars and Ceres
by basin-facing scarps. Lineated terrain extends for about 1,000 kilometres (621 mi) out from the foot of a weak discontinuous scarp on the outer edge
Geology of solar terrestrial planets
Geology_of_solar_terrestrial_planets
Earthquake sequence in Nevada
eleven hours after the M 6.8. Rupture was to the south of the Rainbow Mountain Fault scarp from the mainshock and had a larger strike slip component. It was
1954_Nevada_earthquakes
Mountain in Oregon
mountain is basalt. The mountain has a west-facing fault scarp with a steep cliff face overlooking the Goose Lake Valley. The mountain's fault-block displacement
Crane_Mountain
Mountain in Western Australia
Mountain in Western Australia
Mount Gunjin (Western Australia)
Mount_Gunjin_(Western_Australia)
Mountain in southeast Wales
Lord Hereford's Knob is a mountain in south-east Wales, forming a part of the great northwest scarp of the Black Mountains. It lies 1.86 miles (3 km)
Twmpa
(BCGNO). "Scarp Mountain". BC Geographical Names. Government of British Columbia – B.C. Geographical Names Office (BCGNO). "Mastdon Mountain". BC Geographical
List of peaks on the Alberta–British Columbia border
List_of_peaks_on_the_Alberta–British_Columbia_border
Intersection of a geological fault with the Earth's surface
known as a fault scarp. As mentioned above, a scarp is a formation caused by vertical offset between two fault blocks. Fault scarps can be seen as meter
Fault_trace
Lake in south Wales
It is those rocks which form vertical crags along the top edge of the scarp. The northern face of Waun Lefrith was home to a glacier during the ice
Llyn_y_Fan_Fach
Region of south central Oregon
landscapes, creating into towering scarp- mountains that are gently sloped on one side and terminate into a sharp scarp face on the other. The east portion
Fremont_National_Forest
Flat expanse in western North America
dissected than the rest, and falls off to the south in a frayed-out fault scarp. This scarp overlooks the coastal plain of the Rio Grande embayment. The central
Great_Plains
Mountain range in the US state of Idaho
and the Lost River Range rose, leaving a fault scarp of up to 14 ft (4.3 m) along the base of the mountains. The range then rises into its high central section
Lost_River_Range
Mountain rising from the ocean seafloor that does not reach the water's surface
the northern edge of Vlinder Seamount resulted in a pronounced headwall scarp and a field of debris up to 6 km (4 mi) away. A catastrophic collapse at
Seamount
Topics referred to by the same term
Navy patrol vessel of World War I Scarpe, in heraldry, a type of ordinary Scarp (disambiguation) This disambiguation page lists articles associated with
Scarpe
Volcano on the island of Kyushu, Japan
is a sea scarp which is 7.8 km wide and 9.3 km long, the shape is similar to a horseshoe in the seabed at the southern foot of the mountain. There is
Mount_Kaimon
Wilderness area in Virginia, United States
(951+ meters). The wilderness area is characterized by a steep south-facing scarp that provides an outstanding view from an elevation of 3,060 feet at the
Stone_Mountain_Wilderness
Mountain in Bangor, Wales
Bangor Mountain (Welsh: Mynydd Bangor) is a scarp face of a hill below which the city of Bangor in Gwynedd, Wales, sits. Though not a mountain in the
Bangor_Mountain
Cliff in Lake County, Oregon, United States
longest exposed fault scarp in North America. Bighorn sheep were transplanted to the rim in 1975 and 1977 from nearby Hart Mountain, and are often spotted
Abert_Rim
Mountain in the Adirondack range of U.S. state of New York
the slopes rise steeply from the pass to the granite cliffs, their main scarp face 600 feet (180 m) high and a mile wide, that bracket the summit and
Poke-O-Moonshine_Mountain
Karst trench in Kazakhstan
funnels and caves that eventually collapsed. Today the trench features many scarps and offsets and generates long rain clouds caused by the air rising above
Karagiye
of mountains often have steep scarps along one or more margins. Only a handful of mountains on Io appear to have a volcanic origin. These mountains resemble
List_of_mountains_on_Io
Mountain in British Columbia, Canada
highest on the east flank of the Fraser Canyon and enjoys views over the Scarped Range and Thompson Plateau to the east and southeast, across the Thompson
Botanie_Mountain
Mountain in the Pyrenees
plateau summit of Puigmal d'Err is split for several hundred metres by a bold scarp, in places over 20 metres high, with the eastern half having slipped bodily
Puigmal
Topics referred to by the same term
condiment brand Wishbone scarp, a Pacific Ocean floor feature in the oceanic crust Wishbone Ridge, a ridge associated with the Wishbone scarp or a ridge in the
Wishbone
Forest in South Africa
Hlathikulu Forest is a coastal scarp forest in the Lebombo Mountains of South Africa, between Ingwavuma and the Pongola Gorge. The forest is also known
Hlathikhulu_Forest_Reserve
Mountain in Chile
River. The eastern slope of the mountain is a sharp fault scarp as is part of its western slope. The name of the mountain is Mapuche based on llecu, meaning
Llecué
Mountain in Chile
and Panguipulli lakes. Part of the southeastern slope of the mountain range is a fault scarp. There are historical placer-type gold mines in the Troltrolhue
Troltrolhue
Suburb of Perth, Western Australia
in the Shire of Mundaring, Western Australia, on the edge of the Darling Scarp. It is a vital point in the transport routes from the Swan Coastal Plain
Greenmount,_Western_Australia
Forest vegetation type in South Africa
bamboo (Flagellaria guineensis) and flame lily (Gloriosa superba). Coastal scarp and mistbelt forests were the main source of timber in South Africa before
Forests_of_KwaZulu-Natal
Province of the larger Canadian Shield physiographic division
the appearance of mountains 500–800 meters high; looking across the plateau, the relief is more moderate and subdued. These scarps mark the dramatic southern
Laurentian_Upland
Swamp in South Carolina, United States
the Mount Pleasant Scarp and the north by the Awendaw Scarp. The Little Wambaw Swamp drains north through a gap in the Awendaw Scarp into the Wambaw Swamp
Wambaw_Swamp
Mountain of the Transverse Ranges in California, United States
Pinos and the mountains immediately to the north. The trace extends all the way to Soda Lake in the Carrizo Plain along the Elkhorn Scarp. The lights of
Mount_Pinos
Mountain range in Njombe Region, Tanzania
edge of the range, and abuts Kitulo National Park on the south. Chimala Scarp Forest Reserve, on the northern escarpment of the range overlooking the
Kipengere_Range
Landscape in Switzerland, Bavaria and Baden-Württemberg
present scarp landscape was formed during the Mesozoic era. About 350 million years ago a large basin emerged which was surrounded by mountain ranges and
South_German_Scarplands
Mountain pass in South India
(Madagascar) and Western Ghats (India) - Implications for Understanding Scarp Evolution at Passive Margins". Geological Society of India. 71 (6): 763–779
Palakkad_Gap
Long, narrow ridge
stratum called a dip slope. The other side (its escarpment, frontslope or "scarp slope") is an erosion face that cuts through the dipping strata that comprises
Hogback_(geology)
National park in Western Australia
John Forrest National Park is a national park in the Darling Scarp, 24 km (15 mi) east of Perth, Western Australia. Proclaimed as a national park in November
John_Forrest_National_Park
Active volcano in Hawaii
sandwiched beneath an ash layer on a fault scarp known as Hilina Pali; however, samples dated from higher up the scarp indicate ash deposition at an average
Kīlauea
Volcano in Guatemala
complex is known as La Horqueta. Between Fuego and Acatenango is La Meseta, a scarp marking the remains of an older volcano that collapsed around 8,500 years
Volcán_de_Fuego
Stream in Salt Lake City, Utah, United States
City Creek is a small but historically important mountain stream that flows from City Creek Canyon and across part of Salt Lake City, Utah, and into the
City Creek (Salt Lake County, Utah)
City_Creek_(Salt_Lake_County,_Utah)
Suburb of Perth, Western Australia
Darling Scarp, bisected by Nyaania Creek and north of the Helena River. About one kilometre to the west of Darlington and lower on the Darling Scarp lies
Darlington,_Western_Australia
Range of hills in Saskatchewan and Manitoba, Canada
Saskatchewan–Manitoba border. The eastern slopes of the range are considered to be a scarp. They were created by glacial scouring and formed the western shore of prehistoric
Manitoba_Escarpment
Physiographic region of the contiguous United States
on the other side in relief. Such scarps are known as fault-line scarps, in distinction from the original fault scarps. They are peculiar in having their
Intermontane_Plateaus
Mountain in Western Australia
when Australia broke away from the super continent, Gondwana. The Darling Scarp formed around 570 million years ago and is composed of 3700 million-year-old
Mount_Saddleback
Waterfall on the Zambezi River in Zambia and Zimbabwe
alluvium. A 15–45 m scarp bounds the river about 5–6 km from the main channel, and a series of river terraces are evident between the scarp and the channel
Victoria_Falls
Inlet on the eastern coast of the Antarctic Peninsula
Glacier, and Lammers Glacier. Other features include Werner Peak, Norwood Scarp, Mount Solus, Eisner Peak and Mount Blunt. Mobiloil Inlet was discovered
Mobiloil_Inlet
Largest impact crater on Venus
and its innermost concentric scarp is interpreted as the rim of the original crater cavity. No inner peak-ring of mountain massifs is observed on Mead
Mead_(crater)
Sacred site and oracle of Ancient Greece
northern slope of a pass between Mount Parnassus on the north and the mountains of the Desfina Peninsula on the south. The pass is of the river Pleistos
Delphi
Major earthquake in California
two parallel mountain ranges; the Sierra Nevada on the west and the Inyo Mountains on the east of the Owens Valley, and formed fault scarps from north of
1872_Owens_Valley_earthquake
Seismic faults in Washington State
involving the Saddle Mountain fault zone (discussed below) and associated faults. This is supported by geologically recent scarps and other signs of active
Puget_Sound_faults
Hill (677m) in Powys, Wales
ridge of the Black Mountain and the Hatterrall Ridge. A more gentle path to the summit follows the crest of the northwest-facing scarp, known as Ffynnon
Hay_Bluff
Geological fault in Oklahoma, United States
kilometers (14–16 mi) long conspicuous fault scarp but the fault extends beyond the ends of this scarp. The Meers fault is part of a group of faults
Meers_Fault
Innermost Galilean moon of Jupiter
of mountains often have steep scarps along one or more margins. Only a handful of mountains on Io appear to have a volcanic origin. These mountains resemble
Io_(moon)
German businessman and rocket engineer (1908–1985)
launching mail rockets. A film based on Zucker's attempts with mail rockets at Scarp was released in 2004, called The Rocket Post, starring Ulrich Thomsen as
Gerhard_Zucker
Range of hills in Scotland
to the Ochils Mountain Rescue Team (founded in 1971), a local division of the Mountain Rescue Committee of Scotland. The Ochils Mountain Rescue Team consists
Ochil_Hills
Flash flood disaster in Nepal and China
(08:37 NPT; 10:52 BJT) and was centred just north of Langtang Lirung, a mountain in Langtang National Park. The seismic event was initially believed to
2026_Nepal–Tibet_floods
1907–1934 state in South Arabia
strip of the Tihamah region and extending about 40 mi (64 km) inland to the scarp of highland Asir al-Sarah. Its capital was Sabya. It gained the support
Emirate_of_Asir
Mountain range in South Australia
disappearing under younger alluvium in the inner northern suburbs. The scarp which this fault has formed is covered with houses in the northern suburbs
Mount_Lofty_Ranges
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