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A coast ( coastline, shoreline, seashore) is the next to the or the line that forms the boundary between the land and the or a . Coasts are influenced by the of the surrounding landscape and by aquatic , such as that caused by . The composition of rock and dictates the type of shore that is created. has about of coastline.

Coasts are important zones in natural , often home to a wide range of . On land, they harbor ecosystems, such as or , that are important for birds and other terrestrial animals. In wave-protected areas, coasts harbor , , and , all of which can provide for fin, , and other .

(2025). 9789048124053, Springer Netherlands. .
are usually found along exposed coasts and provide habitat for a wide range of sessile animals (e.g. , , ) and various kinds of .

In physical oceanography, a shore is the wider fringe that is geologically modified by the action of the body of water past and present, and the is at the edge of the shore, including the where there is one.

(1990). 075062759X, . 075062759X
Along coasts with clear, nutrient-poor water, can often be found at depths of .

According to an atlas prepared by the , about 44% of the lives within of the sea . Due to its importance in society and its high population concentrations, the coast is important for major parts of the global food and economic system, and they provide many ecosystem services to humankind. For example, important human activities happen in cities. Coastal (commercial, recreational, and subsistence) and are major economic activities and create jobs, livelihoods, and for the majority of coastal human populations. Other coastal spaces like and generate large revenues through .

Marine coastal ecosystems can also provide protection against sea level rise and . In many countries, are the primary source of wood for fuel (e.g. ) and building material. Coastal ecosystems like mangroves and have a much higher capacity for carbon sequestration than many terrestrial ecosystems, and as such can play a critical role in the near-future to help mitigate climate change effects by uptake of atmospheric anthropogenic carbon dioxide.

However, the economic importance of coasts makes many of these communities vulnerable to climate change, which causes increases in and sea level rise, as well as related issues like , saltwater intrusion, and . Other coastal issues, such as , , coastal development, and destruction, further complicate the human uses of the coast and threaten coastal ecosystems.

The interactive effects of climate change, habitat destruction, , and (especially ) have led to the demise of coastal ecosystem around the globe. This has resulted in population collapse of fisheries stocks, loss of biodiversity, increased , and loss of healthy habitats. International attention to these issues has been captured in Sustainable Development Goal 14 "Life Below Water", which sets goals for international policy focused on preserving marine coastal ecosystems and supporting more sustainable economic practices for coastal communities.United Nations (2017) Resolution adopted by the General Assembly on 6 July 2017, ( A/RES/71/313) Likewise, the United Nations has declared 2021–2030 the UN Decade on Ecosystem Restoration, but restoration of coastal ecosystems has received insufficient attention.

Since coasts are constantly changing, a coastline's exact cannot be determined; this measurement challenge is called the coastline paradox. The term coastal zone is used to refer to a region where interactions of sea and land processes occur. Both the terms coast and coastal are often used to describe a geographic location or region located on a coastline (e.g., New Zealand's West Coast, or the East, West, and Gulf Coast of the .) Coasts with a narrow continental shelf that are close to the open ocean are called coast, while other coasts are more sheltered coast in a or . A , on the other hand, may refer to parts of land adjoining any large body of water, including oceans (sea shore) and lakes (lake shore).


Size
The has approximately of coastline. Coastal habitats, which extend to the margins of the continental shelves, make up about 7 percent of the Earth's oceans, but at least 85% of commercially harvested fish depend on coastal environments during at least part of their life cycle. about 2.86% of exclusive economic zones were part of marine protected areas.

The definition of coasts varies. Marine scientists think of the "wet" (aquatic or ) vegetated habitats as being coastal ecosystems (including seagrass, salt marsh etc.) whilst some terrestrial scientists might only think of coastal ecosystems as purely terrestrial plants that live close to the seashore (see also estuaries and coastal ecosystems).

While there is general agreement in the scientific community regarding the definition of coast, in the political sphere, the delineation of the extents of a coast differ according to . Government authorities in various countries may define coast differently for economic and social policy reasons.


Challenges of precisely measuring the coastline

Formation
often determine the range over which is deposited or eroded. Areas with high tidal ranges allow waves to reach farther up the shore, and areas with lower tidal ranges produce deposition at a smaller elevation interval. The tidal range is influenced by the size and shape of the coastline. Tides do not typically cause erosion by themselves; however, can erode as the waves surge up the river from the ocean.
(2025). 9780130183729, Prentice Hall.

Geologists classify coasts on the basis of into macrotidal coasts with a tidal range greater than ; mesotidal coasts with a tidal range of ; and microtidal coasts with a tidal range of less than . The distinction between macrotidal and mesotidal coasts is more important. Macrotidal coasts lack and , and are characterized by funnel-shaped estuaries containing sand ridges aligned with tidal currents. Wave action is much more important for determining of sediments deposited along mesotidal and microtidal coasts than in macrotidal coasts.

(1980). 9780136427100, Prentice-Hall.

Waves erode coastline as they break on shore releasing their energy; the larger the wave the more energy it releases and the more sediment it moves. Coastlines with longer shores have more room for the waves to disperse their energy, while coasts with cliffs and short shore faces give little room for the wave energy to be dispersed. In these areas, the wave energy breaking against the cliffs is higher, and air and water are compressed into cracks in the rock, forcing the rock apart, breaking it down. Sediment deposited by waves comes from eroded cliff faces and is moved along the coastline by the waves. This forms an or .

Sediment deposited by rivers is the dominant influence on the amount of sediment located in the case of coastlines that have estuaries.

(1999). 9780138609580, Prentice Hall.
Today, riverine deposition at the coast is often blocked by dams and other human regulatory devices, which remove the sediment from the stream by causing it to be deposited inland. Coral reefs are a provider of sediment for coastlines of tropical islands.

Like the ocean which shapes them, coasts are a dynamic environment with constant change. The 's natural processes, particularly sea level rises, waves and various phenomena, have resulted in the , accretion and reshaping of coasts as well as flooding and creation of continental shelves and drowned river valleys ().


Importance for humans and ecosystems

Human settlements
More and more of the world's people live in coastal regions. According to a atlas, 44% of all people live within 150 km (93 mi) of the sea. Many major cities are on or near good and have facilities. Some places have achieved port status by building .

Nations defend their coasts against military invaders, smugglers and illegal migrants. Fixed coastal defenses have long been erected in many nations, and coastal countries typically have a and some form of . File:花蓮新社梯田.jpg| by the coast of Fengbin, Hualien File:170209 219 R.jpg|Coastline of as viewed from Port Fòrum, with Montjuïc and can also be seen.


Tourism
Coasts, especially those with beaches and warm water, attract tourists often leading to the development of communities. In many such as those of the , South Pacific Ocean and , . Coasts offer recreational activities such as swimming, fishing, surfing, boating, and .

Growth management and coastal management can be a challenge for coastal local authorities who often struggle to provide the infrastructure required by new residents, and poor management practices of construction often leave these communities and infrastructure vulnerable to processes like and sea level rise. In many of these communities, management practices such as beach nourishment or when the coastal infrastructure is no longer financially sustainable, to remove communities from the coast. File:Maarianhamina SNV10312 -2B.jpg| A passenger car ferry arrives at the coast of , Åland. File:Amalfi Coast (Italy, October 2020) - 75 (50558355441).jpg|, Italy, attracts international tourists of all classes annually and is listed as a World Heritage Site.


Ecosystem services

Types

Emergent coastline
According to one principle of classification, an emergent coastline is a coastline that has experienced a fall in sea level, because of either a global sea-level change, or local uplift. Emergent coastlines are identifiable by the coastal , which are above the high tide mark, such as . In contrast, a submergent coastline is one where the sea level has risen, due to a global sea-level change, local , or isostatic rebound. Submergent coastlines are identifiable by their submerged, or "drowned" landforms, such as (drowned valleys) and


Concordant coastline
According to the second principle of classification, a concordant coastline is a coastline where bands of different rock types run parallel to the shore. These rock types are usually of varying resistance, so the coastline forms distinctive landforms, such as coves. Discordant coastlines feature distinctive landforms because the rocks are by the ocean . The less resistant rocks erode faster, creating or ; the more resistant rocks erode more slowly, remaining as or .


High and low energy coasts
Parts of a coastline can be categorised as high energy coast or low energy coast. The distinguishing characteristics of a high energy coast are that the average wave energy is relatively high so that erosion of small grained material tends to exceed deposition, and consequently landforms like cliffs, headlands and wave-cut terraces develop. Low energy coasts are generally sheltered from waves, or in regions where the average wind wave and swell conditions are relatively mild. Low energy coasts typically change slowly, and tend to be depositional environments.

High energy coasts are exposed to the direct impact of waves and storms, and are generally erosional environments. High energy storm events can make large changes to a coastline, and can move significant amounts of sediment over a short period, sometimes changing a shoreline configuration.


Destructive and constructive waves
Swash is the shoreward flow after the break, backwash is the water flow back down the beach. The relative strength of flow in the swash and backwash determines what size grains are deposited or eroded. This is dependent on how the wave breaks and the slope of the shore. Depending on the form of the breaking wave, its energy can carry granular material up the beach and deposit it, or erode it by carrying more material down the slope than up it. Steep waves that are close together and break with the surf down onto the shore slope expend much of their energy lifting the sediment. The weak swash does not carry it far up the slope, and the strong backwash carries it further down the slope, where it either settles in deeper water or is carried along the shore by a longshore current induced by an angled approach of the wave-front to the shore. These waves which erode the beach are called destructive waves. Low waves that are further apart and break by , expend more of their energy in the swash which carries particles up the beach, leaving less energy for the backwash to transport them downslope, with a net constrictive influence on the beach.


Rivieras
Riviera is an Italian word for "shoreline",
(2025). 9781442643291, University of Toronto Press.
The more common ones are puntellare and litorale. ultimately derived from Latin ripa ("riverbank"). It came to be applied as a proper name to the coast of the , in the form riviera ligure, then shortened to riviera. Historically, the Ligurian Riviera extended from Capo Corvo (Punta Bianca) south of , north and west into what is now territory past and sometimes as far as . Today, this coast is divided into the and the , although the French use the term "Riviera" to refer to the Italian Riviera and call the French portion the "Côte d'Azur".

As a result of the fame of the Ligurian rivieras, the term came into English to refer to any shoreline, especially one that is sunny, topographically diverse and popular with tourists. Such places using the term include the Australian Riviera in and the along the .


Other coastal categories
  • A or abrasion coast is one where marine action has produced steep declivities known as .
  • A is one where the land gradually descends into the sea.
  • A is one where wind and water action has produced a flat and straight coastline.
  • A isone which is mainly undergoing early stage development by major long-term processes such as tectonism and climate change A is one where the primary processes have mostly stabilised, and more localised processes have become prominent.
  • An is on average undergoing erosion, while a depositional coast is accumulating material.
  • An is on the edge of a tectonic plate, while a is usually on a substantial continental shelf or away from a plate edge.


Landforms
The following articles describe some coastal landforms:


Cliff erosion
  • Much of the sediment deposited along a coast is the result of erosion of a surrounding , or bluff. retreat landward because of the constant undercutting of slopes by waves. If the slope/cliff being undercut is made of unconsolidated sediment it will erode at a much faster rate than a cliff made of bedrock.
  • A is formed when a headland is eroded through by waves.
  • are made when certain rock beds are more susceptible to erosion than the surrounding rock beds because of different areas of weakness. These areas are eroded at a faster pace creating a hole or crevice that, through time, by means of wave action and erosion, becomes a cave.
  • A stack is formed when a headland is eroded away by wave and wind action or an arch collapses leaving an offshore remnant.
  • A stump is a shortened sea stack that has been eroded away or fallen because of instability.
  • Wave-cut notches are caused by the undercutting of overhanging slopes which leads to increased stress on cliff material and a greater probability that the slope material will fall. The fallen debris accumulates at the bottom of the cliff and is eventually removed by waves.
  • A wave-cut platform forms after erosion and retreat of a sea cliff has been occurring for a long time. Gently sloping wave-cut platforms develop early on in the first stages of cliff retreat. Later, the length of the platform decreases because the waves lose their energy as they break further offshore.


Coastal features formed by sediment


Coastal features formed by another feature


Other features on the coast


Coastal waters
"Coastal waters" (or "coastal seas") is a term that carries different meanings depending upon the context, ranging from a geographic reference to the waters within a few kilometers of the coast, to describing the entire continental shelf that may stretch for more than a hundred kilometers from land.
(1991). 9780471926733, Wiley.
The term is used in a different manner when describing legal and economic boundaries, such as territorial waters
(2025). 9780314199492, West.
and international waters,
(2025). 9780314199492, West.
(defining "navigable sea")
or when describing the geography of coastal landforms or the ecological systems operating through the continental shelf (marine coastal ecosystems).

The dynamic fluid nature of the ocean means that all components of the whole ocean system are ultimately connected, although certain regional classifications are useful and relevant. The waters of the continental shelves represent such a region.

(2025). 9780521877626, Cambridge University Press. .
The term "coastal waters" has been used in a wide variety of different ways in different contexts. In environmental management it extends from the coast to just a few nautical miles while in the United States the US EPA considers this region to extend much further offshore.USEPA (2001) Nutrient Criteria Technical Guidance Manual, Estuarine and Coastal Marine Waters, U.S. Environmental Protection Agency

"Coastal waters" has specific meanings in the context of commercial coastal shipping, and somewhat different meanings in the context of naval . and have yet other takes. Coastal waters have a wide range of from enclosed to the of the continental shelf.

Similarly, the term has no single definition. It is the part of a , , or that is close to the . In coastal environments, the littoral zone extends from the high water mark, which is rarely inundated, to shoreline areas that are permanently .

Coastal waters can be threatened by coastal eutrophication and harmful algal blooms.


In geology
The identification of bodies of rock formed from sediments deposited in shoreline and nearshore environments (shoreline and nearshore facies) is extremely important to geologists. These provide vital clues for reconstructing the geography of ancient continents ( ). The locations of these beds show the extent of ancient seas at particular points in geological time, and provide clues to the magnitudes of tides in the distant past.
(2025). 9781405177832, Wiley-Blackwell.

Sediments deposited in the are preserved as lenses of in which the upper part of the sandstone is coarser than the lower part (a coarsening upwards sequence). Geologists refer to these are . Each records an episode of retreat of the ocean from the shoreline over a period of 10,000 to 1,000,000 years. These often show laminations reflecting various kinds of tidal cycles.

Some of the best-studied shoreline deposits in the world are found along the former western shore of the Western Interior Seaway, a shallow sea that flooded central North America during the Period (about 100 to 66 million years ago). These are beautifully exposed along the of and .


Geologic processes
The following articles describe the various geologic processes that affect a coastal zone:


Wildlife

Animals
Larger animals that live in coastal areas include , and rockhopper penguins, among many others. and various kinds of live on rocky coasts and scavenge on food deposited by the sea. Some coastal animals are used to humans in developed areas, such as and who eat food thrown for them by tourists. Since the coastal areas are all part of the , there is a profusion of marine life found just off-coast, including sessile animals such as , sponges, starfish, mussels, seaweeds, fishes, and .

There are many kinds of on various coasts. These include and , who join up with and to forage for fish and shellfish. There are on the coast of and other countries.


Coastal fish

Plants
Many coastal areas are famous for their beds. Kelp is a fast-growing that can grow up to half a meter a day in ideal conditions. , , macroalgal beds, and are important coastal vegetation types in tropical and temperate environments respectively. is another type of coastal vegetation.


Threats
Coasts also face many human-induced environmental impacts and coastal development hazards. The most important ones are:
  • Pollution which can be in the form of , nutrient pollution (leading to coastal eutrophication and harmful algal blooms), or that is contaminating coasts with plastic and other trash.
  • Sea level rise, and associated issues like and saltwater intrusion.


Pollution
The pollution of coastlines is connected to which can occur from a number of sources: (garbage and industrial debris); the transportation of petroleum in tankers, increasing the probability of large ; small oil spills created by large and small vessels, which flush water into the ocean.


Marine pollution

Marine debris

Microplastics

Sea level rise due to climate change

Global goals
International attention to address the threats of coasts has been captured in Sustainable Development Goal 14 "Life Below Water" which sets goals for international policy focused on preserving marine coastal ecosystems and supporting more sustainable economic practices for coastal communities. Likewise, the United Nations has declared 2021–2030 the UN Decade on Ecosystem Restoration, but restoration of coastal ecosystems has received insufficient attention.


See also


Further reading


External links

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