Coast

For other uses, see Coast (disambiguation). "Shore", "Shoreline", and "Seacoast" redirect here. For other uses, see Shore (disambiguation). For the specific area, see Seacoast Region (New Hampshire).

Sunrise on the Jersey Shore coastline at Spring Lake, New Jersey, U.S.

Rugged coastline of the West Coast Region of New Zealand

Southeast coast of Greenland

Escorca coast, Serra de Tramuntana (Balearic Islands)

Coastline in Otranto, Salento, Apulia, Italy

A coast – also called the coastline, shoreline, or seashore – is the land next to the sea or the line that forms the boundary between the land and the ocean or a lake.^[1][2] Coasts are influenced by the topography of the surrounding landscape, as well as by water induced erosion, such as waves. The geological composition of rock and soil dictates the type of shore that is created. Earth contains roughly 620,000 km (390,000 mi) of coastline.

Coasts are important zones in natural ecosystems, often home to a wide range of biodiversity. On land, they harbor important ecosystems such as freshwater or estuarine wetlands, which are important for bird populations and other terrestrial animals. In wave-protected areas, they harbor salt marshes, mangroves or seagrasses, all of which can provide nursery habitat for finfish, shellfish, and other aquatic animals.^[3][4] Rocky shores are usually found along exposed coasts and provide habitat for a wide range of sessile animals (e.g. mussels, starfish, barnacles) and various kinds of seaweeds.

In physical oceanography, a shore is the wider fringe that is geologically modified by the action of the body of water past and present, while the beach is at the edge of the shore, representing the intertidal zone where there is one.^[5] Along tropical coasts with clear, nutrient-poor water, coral reefs can often be found between depths of 1–50 m (3.3–164.0 ft).

According to an atlas prepared by the United Nations, about 44% of the human population lives within 150 km (93 mi) of the sea as of 2013^[update].^[6] 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 port cities. Coastal fisheries (commercial, recreational, and subsistence) and aquaculture are major economic activities and create jobs, livelihoods, and protein for the majority of coastal human populations. Other coastal spaces like beaches and seaside resorts generate large revenues through tourism.

Marine coastal ecosystems can also provide protection against sea level rise and tsunamis. In many countries, mangroves are the primary source of wood for fuel (e.g. charcoal) and building material. Coastal ecosystems like mangroves and seagrasses 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 extreme weather and sea level rise, as well as related issues like coastal erosion, saltwater intrusion, and coastal flooding.^[7] Other coastal issues, such as marine pollution, marine debris, coastal development, and marine ecosystem destruction, further complicate the human uses of the coast and threaten coastal ecosystems.^[7]

The interactive effects of climate change, habitat destruction, overfishing, and water pollution (especially eutrophication) have led to the demise of coastal ecosystem around the globe. This has resulted in population collapse of fisheries stocks, loss of biodiversity, increased invasion of alien species, 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.^[8] Likewise, the United Nations has declared 2021–2030 the UN Decade on Ecosystem Restoration, but restoration of coastal ecosystems has received insufficient attention.^[9]

Since coasts are constantly changing, a coastline's exact perimeter 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.^[10] 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 United States.) Coasts with a narrow continental shelf that are close to the open ocean are called pelagic coast, while other coasts are more sheltered coast in a gulf or bay. A shore, 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

Somalia has the longest coastline in Africa.^[11]

The Earth has approximately 620,000 kilometres (390,000 mi) of coastline. Coastal habitats, which extend to the margins of the continental shelves, make up about 7 percent of the Earth's oceans,^[12] but at least 85% of commercially harvested fish depend on coastal environments during at least part of their life cycle.^[13] As of October 2010,^[update] about 2.86% of exclusive economic zones were part of marine protected areas.^[14]

The definition of coasts varies. Marine scientists think of the "wet" (aquatic or intertidal) 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 jurisdiction.^{[citation needed][15]} Government authorities in various countries may define coast differently for economic and social policy reasons.

Challenges of precisely measuring the coastline

This section is an excerpt from Coastline paradox.[edit]

The coastline paradox is the counterintuitive observation that the coastline of a landmass does not have a well-defined length. This results from the fractal curve-like properties of coastlines; i.e., the fact that a coastline typically has a fractal dimension. Although the "paradox of length" was previously noted by Hugo Steinhaus,^[16] the first systematic study of this phenomenon was by Lewis Fry Richardson,^[17][18] and it was expanded upon by Benoit Mandelbrot.^[19][20]

The measured length of the coastline depends on the method used to measure it and the degree of cartographic generalization. Since a landmass has features at all scales, from hundreds of kilometers in size to tiny fractions of a millimeter and below, there is no obvious size of the smallest feature that should be taken into consideration when measuring, and hence no single well-defined perimeter to the landmass. Various approximations exist when specific assumptions are made about minimum feature size.

Formation

Atlantic rocky coastline, showing a surf area. Porto Covo, west coast of Portugal

Seaside in Budelli, Italy. Budelli beach is famous for the color of its sand, which is pink due to the presence of fragments of a microorganism called Miniacina miniacea.^[21]

Tides often determine the range over which sediment 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, tidal bores can erode as the waves surge up the river estuaries from the ocean.^[22]: 421

Geologists classify coasts on the basis of tidal range into macrotidal coasts with a tidal range greater than 4 m (13 ft); mesotidal coasts with a tidal range of 2 to 4 m (6.6 to 13 ft); and microtidal coasts with a tidal range of less than 2 m (7 ft). The distinction between macrotidal and mesotidal coasts is more important. Macrotidal coasts lack barrier islands and lagoons, and are characterized by funnel-shaped estuaries containing sand ridges aligned with tidal currents. Wave action is much more important for determining bedforms of sediments deposited along mesotidal and microtidal coasts than in macrotidal coasts.^[23]

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 abrasion or cliffed coast.

Sediment deposited by rivers is the dominant influence on the amount of sediment located in the case of coastlines that have estuaries.^[24] 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.^[25]

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

Importance for humans and ecosystems

Human settlements

Further information: Port, island nation, Coastal management, and Coastal development hazards

The Coastal Hazard Wheel system published by UNEP for global coastal management

More and more of the world's people live in coastal regions.^[26] According to a United Nations atlas, 44% of all people live within 150 km (93 mi) of the sea.^[6] Many major cities are on or near good harbors and have port facilities. Some landlocked places have achieved port status by building canals.

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 navy and some form of coast guard.

• 
  Paddy fields by the coast of Fengbin, Hualien
• 
  Coastline of Barcelona as viewed from Port Fòrum, with Montjuïc and Port Vell can also be seen.

Tourism

Coasts, especially those with beaches and warm water, attract tourists often leading to the development of seaside resort communities. In many island nations such as those of the Mediterranean, South Pacific Ocean and Caribbean, tourism is central to the economy. Coasts offer recreational activities such as swimming, fishing, surfing, boating, and sunbathing.

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 coastal erosion 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, managed retreat to remove communities from the coast.

• 
  A passenger car ferry arrives at the coast of Mariehamn, Åland.
• 
  Amalfi Coast, Italy, attracts international tourists of all classes annually^[27] and is listed as a UNESCO World Heritage Site.^[28]

Ecosystem services

See also: Marine coastal ecosystem

This section is an excerpt from Ecosystem service § Estuarine and coastal ecosystem services.[edit]

Estuarine and marine coastal ecosystems are both marine ecosystems. Together, these ecosystems perform the four categories of ecosystem services in a variety of ways: The provisioning services include forest products, marine products, fresh water, raw materials, biochemical and genetic resources. Regulating services include carbon sequestration (contributing to climate change mitigation) as well as waste treatment and disease regulation and buffer zones. Supporting services of coastal ecosystems include nutrient cycling, biologically mediated habitats and primary production. Cultural services of coastal ecosystems include inspirational aspects, recreation and tourism, science and education.

Coasts and their adjacent areas on and offshore are an important part of a local ecosystem. The mixture of fresh water and salt water (brackish water) in estuaries provides many nutrients for marine life. Salt marshes, mangroves and beaches also support a diversity of plants, animals and insects crucial to the food chain. The high level of biodiversity creates a high level of biological activity, which has attracted human activity for thousands of years. Coasts also create essential material for organisms to live by, including estuaries, wetland, seagrass, coral reefs, and mangroves. Coasts provide habitats for migratory birds, sea turtles, marine mammals, and coral reefs.^[29]

Types

Emergent coastline

Further information: Emergent coastline and Submergent 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 landforms, which are above the high tide mark, such as raised beaches. In contrast, a submergent coastline is one where the sea level has risen, due to a global sea-level change, local subsidence, or isostatic rebound. Submergent coastlines are identifiable by their submerged, or "drowned" landforms, such as rias (drowned valleys) and fjords

Concordant coastline

Further information: Concordant coastline and Discordant 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 eroded by the ocean waves. The less resistant rocks erode faster, creating inlets or bay; the more resistant rocks erode more slowly, remaining as headlands or outcroppings.

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.^[30] 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.^[31]

High energy coasts are exposed to the direct impact of waves and storms, and are generally erosional environments.^[31] 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.^[32]

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.^[33] 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 plunging 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.^[34] Low waves that are further apart and break by spilling, 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.^[34]

Rivieras

The Cinque Terre, along the Italian Riviera

Riviera is an Italian word for "shoreline",^[35][36][37] ultimately derived from Latin ripa ("riverbank"). It came to be applied as a proper name to the coast of the Ligurian Sea, in the form riviera ligure, then shortened to riviera. Historically, the Ligurian Riviera extended from Capo Corvo (Punta Bianca) south of Genoa, north and west into what is now French territory past Monaco and sometimes as far as Marseille.^[35][38][39] Today, this coast is divided into the Italian Riviera and the French Riviera, although the French use the term "Riviera" to refer to the Italian Riviera and call the French portion the "Côte d'Azur".^[36]

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.^[35] Such places using the term include the Australian Riviera in Queensland and the Turkish Riviera along the Aegean Sea.^[36]

Other coastal categories

• A cliffed coast or abrasion coast is one where marine action has produced steep declivities known as cliffs.
• A flat coast is one where the land gradually descends into the sea.
• A graded shoreline is one where wind and water action has produced a flat and straight coastline.
• A primary coast isone which is mainly undergoing early stage development by major long-term processes such as tectonism and climate change A secondary coast is one where the primary processes have mostly stabilised, and more localised processes have become prominent.^[31]
• An erosional coast is on average undergoing erosion, while a depositional coast is accumulating material.^[31]
• An active coast is on the edge of a tectonic plate, while a passive coast is usually on a substantial continental shelf or away from a plate edge.^[31]

Landforms

The following articles describe some coastal landforms:

Coastal landforms. The feature shown here as a bay would, in certain (mainly southern) parts of Britain, be called a cove. That between the cuspate foreland and the tombolo is a British bay.

• Barrier island
• Bay
• Cove
• Headland
• Peninsula

Cliff erosion

• Much of the sediment deposited along a coast is the result of erosion of a surrounding cliff, or bluff. Sea cliffs 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.^[24]
• A natural arch is formed when a headland is eroded through by waves.
• Sea caves 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.^{[24][clarification needed]}

Coastal features formed by sediment

• Beach
• Beach cusps
• Cuspate foreland
• Dune system
• Mudflat
• Raised beach
• Ria
• Shoal
• Spit
• Strand plain
• Surge channel
• Tombolo

Coastal features formed by another feature

• Estuary
• Lagoon
• Salt marsh
• Mangrove forests
• Kelp forests
• Coral reefs
• Oyster reefs

Other features on the coast

• Concordant coastline
• Discordant coastline
• Fjord
• Island
• Island arc
• Machair

Coastal waters

See also: Eutrophication § Coastal waters

Overview of different zones of coastal waters: Input, production, transport and storage pathway of carbon in marine waters, including movement across maritime zones of national jurisdiction: territorial sea, Exclusive Economic Zone (EEZ), continental shelf, high seas (international waters), and deep seabed.

"Coastal waters" (or "coastal seas") is a rather general term used differently in different contexts, ranging geographically from the waters within a few kilometers of the coast, through to the entire continental shelf which may stretch for more than a hundred kilometers from land.^[40] Thus the term coastal waters is used in a slightly different way in discussions of legal and economic boundaries^[41] (see territorial waters and international waters) or when considering the geography of coastal landforms or the ecological systems operating through the continental shelf (marine coastal ecosystems). The research on coastal waters often divides into these separate areas too.

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.^[42] The term "coastal waters" has been used in a wide variety of different ways in different contexts. In European Union environmental management it extends from the coast to just a few nautical miles^[43] while in the United States the US EPA considers this region to extend much further offshore.^[44][45]

"Coastal waters" has specific meanings in the context of commercial coastal shipping, and somewhat different meanings in the context of naval littoral warfare.^{[citation needed]} Oceanographers and marine biologists have yet other takes. Coastal waters have a wide range of marine habitats from enclosed estuaries to the open waters of the continental shelf.

Similarly, the term littoral zone has no single definition. It is the part of a sea, lake, or river that is close to the shore.^[46] In coastal environments, the littoral zone extends from the high water mark, which is rarely inundated, to shoreline areas that are permanently submerged.

Coastal waters can be threatened by coastal eutrophication and harmful algal blooms.^[47][48][49]

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 (paleogeography). 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.^[50]

Sediments deposited in the shoreface are preserved as lenses of sandstone in which the upper part of the sandstone is coarser than the lower part (a coarsening upwards sequence). Geologists refer to these are parasequences. 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.^[50]

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 late Cretaceous Period (about 100 to 66 million years ago). These are beautifully exposed along the Book Cliffs of Utah and Colorado.^[51]

Geologic processes

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

• Attrition
• Currents
• Denudation
• Deposition
• Erosion
• Flooding
• Longshore drift
• Marine sediments
• Saltation
• Sea level change
  • eustatic
  • isostatic
• Sedimentation
• Coastal sediment supply
  • sediment transport
  • solution
  • subaerial processes
  • suspension
• Tides
• Water waves
  • diffraction
  • refraction
  • wave breaking
  • wave shoaling
• Weathering

Wildlife

See also: Coastal ecology and Marine coastal ecosystem

Animals

See also: Seashore wildlife

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

There are many kinds of seabirds on various coasts. These include pelicans and cormorants, who join up with terns and oystercatchers to forage for fish and shellfish. There are sea lions on the coast of Wales and other countries.

Coastal fish

This section is an excerpt from Coastal fish.[edit]

Schooling threadfin, a coastal species

Coastal fish, also called inshore fish or neritic fish, inhabit the sea between the shoreline and the edge of the continental shelf. Since the continental shelf is usually less than 200 metres (660 ft) deep, it follows that pelagic coastal fish are generally epipelagic fish, inhabiting the sunlit epipelagic zone.^[52] Coastal fish can be contrasted with oceanic fish or offshore fish, which inhabit the deep seas beyond the continental shelves.

Coastal fish are the most abundant in the world.^[53] They can be found in tidal pools, fjords and estuaries, near sandy shores and rocky coastlines, around coral reefs and on or above the continental shelf. Coastal fish include forage fish and the predator fish that feed on them. Forage fish thrive in inshore waters where high productivity results from upwelling and shoreline run off of nutrients. Some are partial residents that spawn in streams, estuaries and bays, but most complete their life cycles in the zone.^[53]

Plants

Many coastal areas are famous for their kelp beds. Kelp is a fast-growing seaweed that can grow up to half a meter a day in ideal conditions. Mangroves, seagrasses, macroalgal beds, and salt marsh are important coastal vegetation types in tropical and temperate environments respectively.^[3][4] Restinga is another type of coastal vegetation.

Threats

See also: Coastal development hazards and marine coastal ecosystem

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 water pollution, nutrient pollution (leading to coastal eutrophication and harmful algal blooms), oil spills or marine debris that is contaminating coasts with plastic and other trash.
• Sea level rise, and associated issues like coastal erosion and saltwater intrusion.

Pollution

See also: Human impact on marine life

A settled coastline in Marblehead, Massachusetts. Once a fishing port, the harbor is now dedicated to tourism and pleasure boating. Observe that the sand and rocks have been darkened by oil slick up to the high-water line.

This stretch of coast in Tanzania's capital Dar es Salaam serves as a public waste dump.

Dead zones occur when phosphorus and nitrogen from fertilizers cause excessive growth of microorganisms, which depletes oxygen and kills fauna.

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

Marine pollution

This section is an excerpt from Marine pollution.[edit]

Marine pollution occurs when substances used or spread by humans, such as industrial, agricultural and residential waste, particles, noise, excess carbon dioxide or invasive organisms enter the ocean and cause harmful effects there. The majority of this waste (80%) comes from land-based activity, although marine transportation significantly contributes as well.^[54] It is a combination of chemicals and trash, most of which comes from land sources and is washed or blown into the ocean. This pollution results in damage to the environment, to the health of all organisms, and to economic structures worldwide.^[55] Since most inputs come from land, either via the rivers, sewage or the atmosphere, it means that continental shelves are more vulnerable to pollution. Air pollution is also a contributing factor by carrying off iron, carbonic acid, nitrogen, silicon, sulfur, pesticides or dust particles into the ocean.^[56] The pollution often comes from nonpoint sources such as agricultural runoff, wind-blown debris, and dust. These nonpoint sources are largely due to runoff that enters the ocean through rivers, but wind-blown debris and dust can also play a role, as these pollutants can settle into waterways and oceans.^[57] Pathways of pollution include direct discharge, land runoff, ship pollution, bilge pollution, atmospheric pollution and, potentially, deep sea mining.

The types of marine pollution can be grouped as pollution from marine debris, plastic pollution, including microplastics, ocean acidification, nutrient pollution, toxins and underwater noise. Plastic pollution in the ocean is a type of marine pollution by plastics, ranging in size from large original material such as bottles and bags, down to microplastics formed from the fragmentation of plastic material. Marine debris is mainly discarded human rubbish which floats on, or is suspended in the ocean. Plastic pollution is harmful to marine life.

Marine debris

This section is an excerpt from Marine debris.[edit]

Marine debris, also known as marine litter, is human-created solid material that has deliberately or accidentally been released in seas or the ocean. Floating oceanic debris tends to accumulate at the center of gyres and on coastlines, frequently washing aground, when it is known as beach litter or tidewrack. Deliberate disposal of wastes at sea is called ocean dumping. Naturally occurring debris, such as driftwood and drift seeds, are also present. With the increasing use of plastic, human influence has become an issue as many types of (petrochemical) plastics do not biodegrade quickly, as would natural or organic materials.^[58] The largest single type of plastic pollution (~10%) and majority of large plastic in the oceans is discarded and lost nets from the fishing industry.^[59] Waterborne plastic poses a serious threat to fish, seabirds, marine reptiles, and marine mammals, as well as to boats and coasts.^[60]

Dumping, container spillages, litter washed into storm drains and waterways and wind-blown landfill waste all contribute to this problem. This increased water pollution has caused serious negative effects such as discarded fishing nets capturing animals, concentration of plastic debris in massive marine garbage patches, and increasing concentrations of contaminants in the food chain.

Microplastics

This section is an excerpt from Marine plastic pollution § Microplastics.[edit]

A growing concern regarding plastic pollution in the marine ecosystem is the use of microplastics. Microplastics are beads of plastic less than 5 millimeters wide,^[61] and they are commonly found in hand soaps, face cleansers, and other exfoliators. When these products are used, the microplastics go through the water filtration system and into the ocean, but because of their small size they are likely to escape capture by the preliminary treatment screens on wastewater plants.^[62] These beads are harmful to the organisms in the ocean, especially filter feeders, because they can easily ingest the plastic and become sick. The microplastics are such a concern because it is difficult to clean them up due to their size, so humans can try to avoid using these harmful plastics by purchasing products that use environmentally safe exfoliates.

Because plastic is so widely used across the planet, microplastics have become widespread in the marine environment. For example, microplastics can be found on sandy beaches^[63] and surface waters^[64] as well as in the water column and deep sea sediment. Microplastics are also found within the many other types of marine particles such as dead biological material (tissue and shells) and some soil particles (blown in by wind and carried to the ocean by rivers). Population density and proximity to urban centers have been considered the main factors that influence the abundance of microplastics in the environment.

Sea level rise due to climate change

This section is an excerpt from Sea level rise.[edit]

Between 1901 and 2018, the average sea level rose by 15–25 cm (6–10 in), with an increase of 2.3 mm (0.091 in) per year since the 1970s.^[65]: 1216 This was faster than the sea level had ever risen over at least the past 3,000 years.^[65]: 1216 The rate accelerated to 4.62 mm (0.182 in)/yr for the decade 2013–2022.^[66] Climate change due to human activities is the main cause.^{[67]: 5, 8} Between 1993 and 2018, melting ice sheets and glaciers accounted for 44% of sea level rise, with another 42% resulting from thermal expansion of water.^[68]: 1576

Sea level rise lags behind changes in the Earth's temperature by many decades, and sea level rise will therefore continue to accelerate between now and 2050 in response to warming that has already happened.^[69] What happens after that depends on human greenhouse gas emissions. If there are very deep cuts in emissions, sea level rise would slow between 2050 and 2100. It could then reach by 2100 slightly over 30 cm (1 ft) from now and approximately 60 cm (2 ft) from the 19th century. With high emissions it would instead accelerate further, and could rise by 1.0 m (3+1⁄3 ft) or even 1.6 m (5+1⁄3 ft) by 2100.^{[67][65]: 1302} In the long run, sea level rise would amount to 2–3 m (7–10 ft) over the next 2000 years if warming stays to its current 1.5 °C (2.7 °F) over the pre-industrial past. It would be 19–22 metres (62–72 ft) if warming peaks at 5 °C (9.0 °F).^[67]: 21

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.^[8] Likewise, the United Nations has declared 2021–2030 the UN Decade on Ecosystem Restoration, but restoration of coastal ecosystems has received insufficient attention.^[9]

See also

• Bank (geography)
• Beach cleaning
• Coastal and Estuarine Research Federation
• European Atlas of the Seas
• Intertidal zone
• Land reclamation
• List of countries by length of coastline
• List of U.S. states by coastline
• Offshore or Intertidal zone
• Ballantine Scale
• Coastal path
• Shorezone

References

1. "coast". The American Heritage Dictionary of the English Language (5th ed.). HarperCollins. Retrieved 2024-07-19.
2. "coastline". Merriam-Webster.com Dictionary. Merriam-Webster. Retrieved 2024-07-19.
3. Nagelkerken, Ivan, ed. (2009). Ecological Connectivity Among Tropical Coastal Ecosystems. Dordrecht: Springer Netherlands. doi:10.1007/978-90-481-2406-0. ISBN 978-90-481-2405-3.
4. Nagelkerken, I.; Blaber, S.J.M.; Bouillon, S.; Green, P.; Haywood, M.; Kirton, L.G.; Meynecke, J.-O.; Pawlik, J.; Penrose, H.M.; Sasekumar, A.; Somerfield, P.J. (2008). "The habitat function of mangroves for terrestrial and marine fauna: A review". Aquatic Botany. 89 (2): 155–185. Bibcode:2008AqBot..89..155N. doi:10.1016/j.aquabot.2007.12.007.
5. Pickard, George L.; Emery, William J. (1990). Descriptive Physical Oceanography (5th (illustrated) ed.). Elsevier. pp. 7–8. ISBN 0-7506-2759-X.
6. "UN Atlas of the Oceans". CoastalChallenges.com. Archived from the original on 2 November 2013. Retrieved 2013-10-31.
7. "Climate change and the coasts". World Ocean Review. Retrieved 2020-12-19.
8. United Nations (2017) Resolution adopted by the General Assembly on 6 July 2017, Work of the Statistical Commission pertaining to the 2030 Agenda for Sustainable Development (A/RES/71/313)
9. Waltham, Nathan J.; Elliott, Michael; Lee, Shing Yip; Lovelock, Catherine; Duarte, Carlos M.; Buelow, Christina; Simenstad, Charles; Nagelkerken, Ivan; Claassens, Louw; Wen, Colin K-C; Barletta, Mario (2020). "UN Decade on Ecosystem Restoration 2021–2030—What Chance for Success in Restoring Coastal Ecosystems?". Frontiers in Marine Science. 7: 71. doi:10.3389/fmars.2020.00071. hdl:2440/123896. ISSN 2296-7745.
10. Nelson, Stephen A. (2007). "Coastal Zones". Archived from the original on 2013-03-16. Retrieved 2008-12-11.
11. "The Indian Ocean Coast of Somalia". Marine Pollution Bulletin. 41 (1–6): 141–159. December 2000. doi: 10.1016/S0025-326X(00)00107-7
12. "Ocean Habitats". Oceans, Coasts & Seashores. National Park Service. 1 December 2016. Retrieved 25 September 2021.
13. Lellis-Dibble, K.A.; McGlynn, K.E.; Bigford, T.E. (2008). "Estuarine fish and shellfish species in US commercial and recreational fisheries: economic value as an incentive to protect and restore estuarine habitat". NOAA Technical Memo. NMFS-F/SPO. Retrieved 24 September 2021.
14. "Global Ocean Protection: Present Status and Future Possibilities". Iucn.org. 2010-11-23. Archived from the original on 2012-03-19. Retrieved 2012-06-07.
15. ""The Coast" is Complicated: A Model to Consistently Describe the Nation's Coastal Population" (PDF). NOAA. Archived (PDF) from the original on June 14, 2023. Retrieved June 13, 2023.
16. Steinhaus, Hugo (1954). "Length, shape and area". Colloquium Mathematicum. 3 (1): 1–13. doi:10.4064/cm-3-1-1-13. The left bank of the Vistula, when measured with increased precision would furnish lengths ten, hundred and even thousand times as great as the length read off the school map. A statement nearly adequate to reality would be to call most arcs encountered in nature not rectifiable.
17. Vulpiani, Angelo (2014). "Lewis Fry Richardson: scientist, visionary and pacifist". Lettera Matematica. 2 (3): 121–128. doi:10.1007/s40329-014-0063-z. MR 3344519. S2CID 128975381.
18. Richardson, L. F. (1961). "The problem of contiguity: An appendix to statistics of deadly quarrels". General Systems Yearbook. Vol. 6. pp. 139–187.
19. Mandelbrot, B. (1967). "How Long is the Coast of Britain? Statistical Self-Similarity and Fractional Dimension". Science. 156 (3775): 636–638. Bibcode:1967Sci...156..636M. doi:10.1126/science.156.3775.636. PMID 17837158. S2CID 15662830. Archived from the original on 2021-10-19. Retrieved 2021-05-21.
20. Mandelbrot, Benoit (1983). The Fractal Geometry of Nature. W. H. Freeman and Co. pp. 25–33. ISBN 978-0-7167-1186-5.
21. "Spiaggia Rosa" (in Italian). Retrieved 27 December 2024.
22. Davidson, Jon P. (2002). Exploring earth: an introduction to physical geology. Walter E. Reed, Paul M. Davis (2nd ed.). Upper Saddle River, NJ: Prentice Hall. ISBN 0-13-018372-5. OCLC 45917172.
23. Blatt, Harvey; Middleton, Gerard; Murray, Raymond (1980). Origin of sedimentary rocks (2d ed.). Englewood Cliffs, N.J.: Prentice-Hall. pp. 656–659. ISBN 0-13-642710-3.
24. Easterbrook, Don J. (1999). Surface processes and landforms (2nd ed.). Upper Saddle River, N.J.: Prentice Hall. ISBN 0-13-860958-6. OCLC 39890526.
25. "How is beach sand created? - Woods Hole Oceanographic Institution". Woods Hole Oceanographic Institution. Archived from the original on 2021-06-28. Retrieved 2021-08-10.
26. Goudarzi, Sara (July 18, 2006). "Flocking to the Coast: World's Population Migrating into Danger". Live Science. Retrieved 2008-12-14.
27. "Bay of Naples & Amalfi Coast History". Unique Costiera. Archived from the original on 31 October 2011. Retrieved 28 June 2011.
28. "Costiera Amalfitana". UNESCO World Heritage Centre. Retrieved 14 September 2015.
29. US EPA, ORD (2017-11-02). "Coastal Waters". US EPA. Retrieved 2020-05-04.
30. "High energy coasts". www.field-studies-council.org. Retrieved 13 April 2024.
31. "Classification of Coasts". www.vaia.com. Retrieved 13 April 2024.
32. Guisado-Pintado, E; Jackson, D.W.T. (2019). "Coastal Impact From High-Energy Events and the Importance of Concurrent Forcing Parameters: The Cases of Storm Ophelia (2017) and Storm Hector (2018) in NW Ireland". Front. Earth Sci. 7 (190). Bibcode:2019FrEaS...7..190G. doi:10.3389/feart.2019.00190.
33. "Method for high energy coasts". www.field-studies-council.org. Retrieved 13 April 2024.
34. "Coastal processes - AQA, Wave types - constructive and destructive". www.bbc.co.uk. Retrieved 13 April 2024.
35. "riviera". Chambers Concise Dictionary. New Delhi: Allied Chambers. 2004. p. 1045. ISBN 978-81-86062-36-4.
36. Kolb, Martina (2013). Nietzsche, Freud, Benn, and the Azure Spell of Liguria. Toronto, Ontario: University of Toronto Press. p. 30. ISBN 978-1-4426-4329-1.
37. The more common ones are puntellare and litorale.
38. Baughan, Rosa (1880). Winter havens in the sunny South, a complete handbook to the Riviera. London: The Bazaar. Archived from the original on 2017-02-02.
39. Black, Charles B. (1887). The Riviera, Or The Coast from Marseilles to Leghorn, Including Carrara, Lucca, Pisa, Pistoja and Florence (Third ed.). Edinburgh: Adam and Charles Black. Archived from the original on 2017-02-02.
40. Mantoura, R. F. C; Martin, Jean-Marie; Wollast, R, eds. (1991). Ocean margin processes in global change: report of the Dahlem Workshop on Ocean Margin Processes in Global Change, Berlin, 1990, March 18-23. Chichester, New York: Wiley. ISBN 978-0-471-92673-3. OCLC 22765791.
41. "Coastal waters Definition: 255 Samples". Law Insider. Retrieved 2022-06-22.
42. Simpson, John H.; Sharples, Jonathan (2012). Introduction to the Physical and Biological Oceanography of Shelf Seas (1 ed.). Cambridge University Press. doi:10.1017/CBO9781139034098. ISBN 978-0-521-87762-6.
43. "coastal waters — European Environment Agency". www.eea.europa.eu. Retrieved 2022-06-29.
44. US EPA, ORD (2017-11-02). "Coastal Waters". www.epa.gov. Retrieved 2022-06-29.
45. USEPA (2001) Nutrient Criteria Technical Guidance Manual, Estuarine and Coastal Marine Waters, U.S. Environmental Protection Agency
46. Seekell, D.; Cael, B.; Norman, S.; Byström, P. (2021). "Patterns and variation of littoral habitat size among lakes". Geophysical Research Letters. 48 (20): e2021GL095046. Bibcode:2021GeoRL..4895046S. doi:10.1029/2021GL095046. ISSN 1944-8007. S2CID 244253181.
47. Maúre, Elígio de Raús; Terauchi, Genki; Ishizaka, Joji; Clinton, Nicholas; DeWitt, Michael (2021). "Globally consistent assessment of coastal eutrophication". Nature Communications. 12 (1): 6142. doi:10.1038/s41467-021-26391-9. ISSN 2041-1723. PMC 8536747. PMID 34686688.
48. Jickells, T. D. (1998). "Nutrient Biogeochemistry of the Coastal Zone". Science. 281 (5374): 217–222. doi:10.1126/science.281.5374.217. ISSN 0036-8075. PMID 9660744.
49. Glibert, Patricia; Burford, Michele (2017). "Globally Changing Nutrient Loads and Harmful Algal Blooms: Recent Advances, New Paradigms, and Continuing Challenges". Oceanography. 30 (1): 58–69. doi:10.5670/oceanog.2017.110. hdl:10072/377577.
50. Leeder, M. R. (2011). Sedimentology and sedimentary basins: from turbulence to tectonics (2nd ed.). Chichester, West Sussex, UK: Wiley-Blackwell. pp. 436–437. ISBN 978-1-4051-7783-2.
51. Blatt, Middleton & Murray 1980, pp. 673–674.
52. Moyle and Cech, 2004, page 585
53. Moyle and Cech, 2004, page 572
54. Sheppard, Charles, ed. (2019). World seas: an Environmental Evaluation. Vol. III, Ecological Issues and Environmental Impacts (Second ed.). London: Academic Press. ISBN 978-0-12-805204-4. OCLC 1052566532.
55. "Marine Pollution". Education | National Geographic Society. Retrieved 2023-06-19.
56. Duce, Robert; Galloway, J.; Liss, P. (2009). "The Impacts of Atmospheric Deposition to the Ocean on Marine Ecosystems and Climate WMO Bulletin Vol 58 (1)". Archived from the original on 18 December 2023. Retrieved 22 September 2020.
57. "What is the biggest source of pollution in the ocean?". National Ocean Service (US). Silver Spring, MD: National Oceanic and Atmospheric Administration. Retrieved 2022-09-21.
58. Graham, Rachel (10 July 2019). "Euronews Living | Watch: Italy's answer to the problem with plastic". living.
59. "Dumped fishing gear is biggest plastic polluter in ocean, finds report". The Guardian. 2019-11-06. Retrieved 2021-04-09.
60. "Facts about marine debris". US NOAA. Archived from the original on 13 February 2009. Retrieved 10 April 2008.
61. Wiggin, K. J.; Holland, E. B. (June 2019). "Validation and application of cost and time effective methods for the detection of 3–500 μm sized microplastics in the urban marine and estuarine environments surrounding Long Beach, California". Marine Pollution Bulletin. 143: 152–162. Bibcode:2019MarPB.143..152W. doi:10.1016/j.marpolbul.2019.03.060. ISSN 0025-326X. PMID 31789151. S2CID 150122831.
62. Fendall, Lisa S.; Sewell, Mary A. (2009). "Contributing to marine pollution by washing your face: Microplastics in facial cleansers". Marine Pollution Bulletin. 58 (8): 1225–1228. Bibcode:2009MarPB..58.1225F. doi:10.1016/j.marpolbul.2009.04.025. PMID 19481226.
63. De-la-Torre, Gabriel E.; Dioses-Salinas, Diana C.; Castro, Jasmin M.; Antay, Rosabel; Fernández, Naomy Y.; Espinoza-Morriberón, D.; Saldaña-Serrano, Miguel (2020). "Abundance and distribution of microplastics on sandy beaches of Lima, Peru". Marine Pollution Bulletin. 151: 110877. Bibcode:2020MarPB.15110877D. doi:10.1016/j.marpolbul.2019.110877. PMID 32056653. S2CID 211112493.
64. Karlsson, Therese M.; Kärrman, Anna; Rotander, Anna; Hassellöv, Martin (2020). "Comparison between manta trawl and in situ pump filtration methods, and guidance for visual identification of microplastics in surface waters". Environmental Science and Pollution Research. 27 (5): 5559–5571. Bibcode:2020ESPR...27.5559K. doi:10.1007/s11356-019-07274-5. PMC 7028838. PMID 31853844.
65. Fox-Kemper, B.; Hewitt, Helene T.; Xiao, C.; Aðalgeirsdóttir, G.; Drijfhout, S. S.; Edwards, T. L.; Golledge, N. R.; Hemer, M.; Kopp, R. E.; Krinner, G.; Mix, A. (2021). Masson-Delmotte, V.; Zhai, P.; Pirani, A.; Connors, S. L.; Péan, C.; Berger, S.; Caud, N.; Chen, Y.; Goldfarb, L. (eds.). "Chapter 9: Ocean, Cryosphere and Sea Level Change" (PDF). Climate Change 2021: The Physical Science Basis. Contribution of Working Group I to the Sixth Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge University Press, Cambridge, UK and New York, US. Archived (PDF) from the original on 2022-10-24. Retrieved 2022-10-18.
66. "WMO annual report highlights continuous advance of climate change". World Meteorological Organization. 21 April 2023. Archived from the original on 17 December 2023. Retrieved 18 December 2023. Press Release Number: 21042023.
67. IPCC, 2021: Summary for Policymakers Archived 2021-08-11 at the Wayback Machine. In: Climate Change 2021: The Physical Science Basis. Contribution of Working Group I to the Sixth Assessment Report of the Intergovernmental Panel on Climate Change Archived 2023-05-26 at the Wayback Machine Masson-Delmotte, V., P. Zhai, A. Pirani, S.L. Connors, C. Péan, S. Berger, N. Caud, Y. Chen, L. Goldfarb, M. I. Gomis, M. Huang, K. Leitzell, E. Lonnoy, J. B. R. Matthews, T. K. Maycock, T. Waterfield, O. Yelekçi, R. Yu, and B. Zhou (eds.). Cambridge University Press, Cambridge, UK and New York, US, pp. 3−32, doi:10.1017/9781009157896.001.
68. WCRP Global Sea Level Budget Group (2018). "Global sea-level budget 1993–present". Earth System Science Data. 10 (3): 1551–1590. Bibcode:2018ESSD...10.1551W. doi:10.5194/essd-10-1551-2018. hdl:20.500.11850/287786. This corresponds to a mean sea-level rise of about 7.5 cm over the whole altimetry period. More importantly, the GMSL curve shows a net acceleration, estimated to be at 0.08mm/yr².
69. National Academies of Sciences, Engineering, and Medicine (2011). "Synopsis". Climate Stabilization Targets: Emissions, Concentrations, and Impacts over Decades to Millennia. Washington, DC: The National Academies Press. p. 5. doi:10.17226/12877. ISBN 978-0-309-15176-4. Archived from the original on 2023-06-30. Retrieved 2022-04-11. Box SYN-1: Sustained warming could lead to severe impacts

Further reading

• Scheffers, Anja M.; Scheffers, Sander R.; Kelletat, Dieter H. (2012). The Coastlines of the World with Google Earth: Understanding our Environment. New York: Springer. ISBN 978-94-007-0737-5.

External links

• Woods Hole Oceanographic Institution - organization dedicated to ocean research, exploration, and education