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Cape (geography) Cascadia Channel; Channel (geography) Chenier; Chevron (land form) Cliff; Cliff-top dune; Cliffed coast; Coast; Coastal plain; Coastal waterfall; Cold seep; Continental shelf; Continental shelf of Chile; Coral reef; Cowaramup Bombora; Cuspate foreland; Cyclic steps
Collapsed Ordovician limestone bank showing coastal erosion. NW Osmussaar, Estonia. Coastal geography is the study of the constantly changing region between the ocean and the land, incorporating both the physical geography (i.e. coastal geomorphology, climatology and oceanography) and the human geography (sociology and history) of the coast.
The shelf usually ends at a point of increasing slope [3] (called the shelf break).The sea floor below the break is the continental slope. [4] Below the slope is the continental rise, which finally merges into the deep ocean floor, the abyssal plain. [5]
In the adjacent diagram, the two waves cancel each other out, creating a flat surface. However, this is a highly simplified version of events. The incoming wave has the same wave period as the edge wave, so the incoming wave changes from a peak to a trough over the same period as it takes the standing wave to change so they keep the same pattern.
A continental margin is the outer edge of continental crust abutting oceanic crust under coastal waters. It is one of the three major zones of the ocean floor, the other two being deep-ocean basins and mid-ocean ridges. The continental margin consists of three different features: the continental rise, the continental slope, and the continental ...
[1] In the case of a cuspate foreland that has formed close to an island, it is possible for it to extend right up to the island, forming a tombolo. [1] Depending on the physical conditions such as storms, the feature can alternate between a cuspate foreland and a tombolo. [1] Gabo Island in South Australia is an example of where this occurs. [1]
The methodology used to estimate length is based on the following: 1) A country's coastline is made up of individual lines, and an individual line has two or more vertices and/or nodes. 2) The length between two vertices is calculated on the surface of a sphere.
The oceanic zone is typically defined as the area of the ocean lying beyond the continental shelf (e.g. the neritic zone), but operationally is often referred to as beginning where the water depths drop to below 200 metres (660 ft), seaward from the coast into the open ocean with its pelagic zone.
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related to: geography coastal landforms diagram printable chart 1 200This site is a teacher's paradise! - The Bender Bunch