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  2. Glossary of landforms - Wikipedia

    en.wikipedia.org/wiki/Glossary_of_landforms

    Butte – Isolated hill with steep, often vertical sides and a small, relatively flat top; Canyon – Deep chasm between cliffs; Cliff – Tall, near vertical rock face; Col – Lowest point on a mountain ridge between two peaks; Cuesta – Hill or ridge with a gentle slope on one side and a steep slope on the other

  3. Butte - Wikipedia

    en.wikipedia.org/wiki/Butte

    The term butte is sometimes applied more broadly to isolated, steep-sided hills with pointed or craggy, rather than flat, tops. [1] Three notable formations that are either named butte or may be considered buttes even though they do not conform to the formal geographer's rule are Scotts Bluff in Nebraska which is a collection of five bluffs ...

  4. Hill - Wikipedia

    en.wikipedia.org/wiki/Hill

    Drumlin – an elongated whale-shaped hill formed by glacial action. Butte – an isolated hill with steep sides and a small flat top, formed by weathering. Kuppe – a rounded hill or low mountain, typical of Central Europe. Tor – a rock formation found on a hilltop; also used to refer to the hill, especially in South West England and the ...

  5. Drumlin - Wikipedia

    en.wikipedia.org/wiki/Drumlin

    Drumlins generally have a length to width ratio of between 1.7 and 4.1 [8] and it has been suggested that this ratio can indicate the velocity of the glacier. That is, since ice flows in laminar flow, the resistance to flow is frictional and depends on area of contact; thus, a more elongated drumlin would indicate a lower velocity and a shorter ...

  6. Saddle (landform) - Wikipedia

    en.wikipedia.org/wiki/Saddle_(landform)

    Cross-section diagram of three hills, with two saddles marked by X. • There are three peaks ( Schartenhöhe ) or prominences shown labeled 'A', 'B', & 'C' . • The diagram illustrates the topographic isolation (German: Dominanz )- the distance from a prominence which is also a minimum to the point of the same height .

  7. Homoclinal ridge - Wikipedia

    en.wikipedia.org/wiki/Homoclinal_ridge

    [1] [2] [4] [5] Because the slope of a homoclinal ridge dips in the same direction as the sedimentary strata underlying it, the dip angle of this bedding (Ө) can be calculated by v/h= tan(Ө) where v is equal to the vertical distance and h is equal to the horizontal distance perpendicular to the strike of the beds. [6]

  8. World's strangest: The road where cars roll uphill

    www.aol.com/news/2014-05-30-worlds-strangest-the...

    In this case, Chris was able to confirm that the apparent top of the hill is actually 292 feet above sea level, while the apparent bottom of the hill is 303 feet above sea level.

  9. Cuesta - Wikipedia

    en.wikipedia.org/wiki/Cuesta

    In general usage, a cuesta is a hill or ridge with a gentle slope (backslope) on one side, and a steep slope (frontslope) on the other. The word is from Spanish: "flank or slope of a hill; hill, mount, sloping ground". In geology and geomorphology, cuesta refers specifically to an asymmetric ridge with a long and gentle backslope called a dip ...

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