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Headland

From Wikipedia, the free encyclopedia
For other uses, seeHeadland (disambiguation).
Landform extending into a body of water, often with significant height and drop
Land's End, England

Aheadland, also known as ahead, is acoastallandform, a point of land usually high and often with a sheer drop, that extends into abody of water. It is a type ofpromontory. A headland of considerable size often is called acape.[1] Headlands are characterised by high, breakingwaves,rocky shores, intenseerosion, and steepsea cliff.

Headlands andbays are often found on the same coastline. A bay is flanked by land on three sides, whereas a headland is flanked by water on three sides. Headlands and bays form on discordant coastlines, where bands of rock of alternating resistance run perpendicular to the coast. Bays form when weak (less resistant) rocks (such assands andclays) are eroded, leaving bands of stronger (more resistant) rocks (such aschalk,limestone, andgranite) forming a headland, orpeninsula. Through the deposition ofsediment within the bay and the erosion of the headlands, coastlines eventually straighten out, then start the same process all over again.

List of notable headlands

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Africa

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Cape Malabata, Morocco

Asia

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Europe

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Cliffs atBeachy Head, England

North America

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Point Reyes, California, USA

Canada

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Greenland

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Mexico

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United States

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Oceania

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Hanauma Bay andKoko Crater atKoko Head, O'ahu Island, Hawai'i, USA
Sydney Heads, New South Wales, Australia
South West Cape, Tasmania

Australia

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New Zealand

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United States (Hawaii)

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South America

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Cape Horn, Chile

See also

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References

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  1. ^Whittow, John (1984).Dictionary of Physical Geography. London: Penguin, 1984, pp. 80, 246.ISBN 0-14-051094-X.
Wikimedia Commons has media related toHeadlands.
Landforms
Coastal and oceanic landforms

Dois Irmãos - Fernando de Noronha
Beaches
River mouths
Processes
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