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It can be transcluded on pages by placing {{Coastal geography}} below the standard article appendices. Initial visibility This template's initial visibility currently defaults to autocollapse , meaning that if there is another collapsible item on the page (a navbox, sidebar , or table with the collapsible attribute ), it is hidden apart from ...
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.
Print/export Download as PDF ... Coastal landforms and Physical oceanography topographic landforms ... Sound (geography) Spit (landform) Stack (geology) Steep coast ...
This work has been released into the public domain by its author, Feydey.This applies worldwide. In some countries this may not be legally possible; if so: Feydey grants anyone the right to use this work for any purpose, without any conditions, unless such conditions are required by law.
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.
This list catalogues about 400 of the coastal landforms of the island including bays, estuaries, harbours, headlands, and many others. [3] [4] [5] Most offshore features such as islands, stags , and rocks are omitted but are presented at List of islands of Ireland. A list of beaches is available at List of beaches in Ireland.
A stack or sea stack is a geological landform consisting of a steep and often vertical column or columns of rock in the sea near a coast, formed by wave erosion. [1] Stacks are formed over time by wind and water, processes of coastal geomorphology. [2]
The intertidal zone or foreshore is the area above water level at low tide and underwater at high tide; in other words, it is the part of the littoral zone within the tidal range.
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