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An island or isle is a piece of land, distinct from a continent, completely surrounded by water. There are continental islands, which were formed by being split from a continent by plate tectonics, and oceanic islands, which have never been part of a continent. Oceanic islands can be formed from volcanic activity, grow into atolls from coral reefs, and form from sediment along shorelines, creating barrier islands. River islands can also form from sediment and debris in rivers. Artificial islands are those made by humans, including small rocky outcroppings built out of lagoons and large-scale land reclamation projects used for development.
Islands are host to diverse plant and animal life. Oceanic islands have the sea as a natural barrier to the introduction of new species, causing the species that do reach the island to evolve in isolation. Continental islands share animal and plant life with the continent they split from. Depending on how long ago the continental island formed, the life on that island may have diverged greatly from the mainland due to natural selection.
Humans have lived on and traveled between islands for thousands of years at a minimum. Some islands became host to humans due to a land bridge or a continental island splitting from the mainland, or by boat travel. In the far north or south some islands are joined by seasonal or glacial ice. Today, up to 10% of the world's population lives on islands. Islands are popular targets for tourism due to their perceived natural beauty, isolation, and unique cultures.
Islands became the target of colonization by Europeans, resulting in the majority of islands in the Pacific being put under European control. Decolonization has resulted in some but not all island nations becoming self-governing, with lasting effects related to industrialisation, invasive species, nuclear weapons testing, and tourism. Islands and island countries are threatened by climate change. Sea level rise threatens to submerge nations such as Maldives, the Marshall Islands, and Tuvalu completely. Increases in the frequency and intensity of tropical cyclones can cause widespread destruction of infrastructure and animal habitats. Species that live exclusively on islands are some of those most threatened by extinction.
DefinitionEdit
Template:Fuller projection with largest islands.svg An island is an area of land surrounded by water on all sides that is distinct from a continent.<ref name=":5" /> There is no standard of size that distinguishes islands and continents. Continents have an accepted geological definition – they are the largest landmass of a particular tectonic plate.<ref name=":6">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> Islands can occur in any body of water, including lakes, rivers, seas.<ref name=":24">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> Low-tide elevations, areas of land that are not above the surface during a high tide, are generally not considered islands.<ref name=":21">Template:Cite book</ref> Islands that have been bridged or otherwise joined to a mainland with land reclamation are sometimes considered "de-islanded", but not in every case.<ref>Template:Cite journal</ref>
EtymologyEdit
The word island derives from Middle English Template:Linktext, from Old English igland (from ig or ieg, similarly meaning 'island' when used independently, and -land carrying its contemporary meaning. Old English ieg is actually a cognate of Swedish ö and German Aue, and more distantly related to Latin Template:Linktext (water).<ref>Template:Cite Q</ref>
The spelling of the word was modified in the 15th century because of a false etymology caused by an association with the Old French loanword isle, which itself comes from the Latin word insula.<ref name=":5">Template:Cite dictionary</ref><ref>Template:Cite journal</ref>
GeologyEdit
Formation in oceansEdit
Islands often are found in archipelagos or island chains, which are collections of islands. These chains are thought to form from volcanic hotspots, areas of the lithosphere where the mantle is hotter than the surrounding area.<ref name=":1">Template:Cite journal</ref><ref name=":0" /> These hotspots would give rise to volcanoes whose lava would form the rock the islands are made of.<ref name=":1" /> For some islands, the movement of tectonic plates above stationary hotspots would form islands in a linear chain, with the islands further away from the hotspot being progressively older and more eroded, before disappearing under the sea entirely.<ref name=":2">Template:Cite journal</ref> An example is the Hawaiian Islands,<ref name=":2" /> with the oldest island being 25 million years old, and the youngest, Hawaii, still being an active volcano.<ref name=":0" /> However, not all island chains are formed this way. Some may be formed all at once by fractures in the tectonic plates themselves, simultaneously creating multiple islands. One supporting piece of evidence is that of the Line Islands, which are all estimated to be 8 million years old, rather than being different ages.<ref name=":0">Template:Cite journal</ref>
Other island chains form due to being separated from existing continents. The Japanese archipelago may have been separated from Eurasia due to seafloor spreading, a phenomenon where new oceanic crust is formed, pushing away older crust.<ref name=":0" /> Islands sitting on the continental shelf may be called continental islands.<ref name=":24" /> Other islands, like those that make up New Zealand, are what remains of continents that shrank and sunk beneath the sea.<ref name=":3">Template:Cite journal</ref> It was estimated that Zealandia, the continent-like area of crust that New Zealand sits on, has had 93% of its original surface area submerged.<ref name=":3" />
Some islands are formed when coral reefs grow on volcanic islands that have submerged beneath the surface.<ref name=":4">Template:Cite journal</ref> When these coral islands encircle a central lagoon, the island is known as an atoll.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> The formation of reefs and islands related to those reefs is aided by the buildup of sediment in shallow patches of water. In some cases, tectonic movements lifting a reef out of the water by as little as 1 meter can cause sediment to accumulate and an island to form.<ref name=":4" />
Barrier islands are long, sandy bars that form along shorelines due to the deposition of sediment by waves. These islands erode and grow as the wind and waves shift. Barrier islands have the effect of protecting coastal areas from severe weather because they absorb some of the energy of large waves before they can reach the shore.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
Antarctic islands, are sometimes permanently connected to another land mass by sea or glacial ice. An example of this is Ross Island in Antarctica.
Formation in freshwaterEdit
A fluvial island is an island that forms from the erosion and sedimentation of debris in rivers; almost all rivers have some form of fluvial islands.<ref name=":7">Template:Cite journal</ref> These islands may only be a few meters high, and are usually temporary. Changes in the flow speed, water level, and sediment content of the river may effect the rate of fluvial island formation and depletion.<ref name=":7" /> Permanent river islands also exist, the largest of which (that is completely inland) is Bananal Island in the Tocantins of Brazil, which has a maximum width of 55 kilometers.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
Lakes form for a variety of reasons, including glaciers, plate tectonics, and volcanism.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> Lake islands can form as part of these processes.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
Life on islandsEdit
The field of insular biogeography studies the ecological processes that take place on islands, with a focus on what factors effect the evolution, extinction, and richness of species. Scientists often study islands as an isolated model of how the process of natural selection takes place.<ref>Template:Cite journal</ref><ref name=":27">Template:Cite journal</ref> Island ecology studies organisms on islands and their environment. It has yielded important insights for its parent field of ecology since the time of Charles Darwin.<ref name=":27" />
EndemismEdit
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In biology, endemism is defined as the phenomenon where species or genus is only found in a certain geographical area. Islands isolate land organisms from others with water, and isolate aquatic organisms living on them with land.<ref name=":27" /> Island ecosystems have the highest rates of endemism globally. This means that islands contribute heavily to global biodiversity.<ref>Template:Cite journal</ref> Areas with high lives of biodiversity are a priority target of conservation efforts, to prevent the extinction of these species.<ref>Template:Cite journal</ref> Despite high levels of endemism, the total species richness, the total number of unique species in a region, is lower on islands than on mainlands.<ref>Template:Cite journal</ref> The level of species richness on islands is proportional to the area of that island, a phenomenon known as the species-area relationship. This is because larger areas have more resources and thus can support more organisms. Populations with a higher carrying capacity also have more genetic diversity, which promotes speciation.<ref name=":27" />
DispersalEdit
Oceanic islands, ones that have never been connected to shore, are only populated by life that can cross the sea. This means that any animals present on the island had to have flown there, in the case of birds or bats, were carried by such animals, or were carried in a sea current in what is known as a "rafting event". This phenomenon is known as oceanic dispersal.<ref name=":28">Template:Cite journal</ref> Tropical cyclones have the capacity to transport species over great distances.<ref name=":23">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> Animals like tortoises can live for weeks without food or water, and are able to survive floating on debris in the sea.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> One case study showed that in 1995, fifteen iguanas survived a 300 km journey to Anguilla in the Caribbean, an island which no iguana had lived on previously. They survived floating on a mass of uprooted trees from a storm.<ref>Template:Cite journal</ref> Plant species are thought to be able to travel great distances of ocean. New Zealand and Australia share 200 native plant species, despite being separated by 1500 km.<ref name=":28" />
Continental islands, islands that were at one point connected to a continent, are expected to share a common history of plant and animal life up until the point that the island broke away from the continent.<ref name=":28" /> For example, the presence of freshwater fish on an island surrounded by ocean would indicate that it once was attached to a continent, since these fish cannot traverse the ocean on their own.<ref name=":27" /> Over the course of time, evolution and extinction changes the nature of animal life on a continental island, but only once it splits from the mainland. An example is that of the southern beech, a tree that is present in Australia, New Zealand, parts of South American, and New Guinea, places that today are geographically distant. A possible explanation for this phenomenon is that these landmasses were once all part of the continent Gondwana and separated by tectonic drift. However, there are competing theories that suggest this species may have reached faraway places by way of oceanic dispersal.<ref name=":28" />
Evolution on island groupsEdit
Species that colonize island archipelagos exhibit a specific property known as adaptive radiation. In this process, a species that arrives on a group of islands rapidly becomes more diverse over time, splitting off into new species or subspecies. A species that reaches an island ecosystem may face little competition for resources, or may find that the resources that they found in their previous habitat are not available. These factors together result in individual evolutionary branches with different means of survival.<ref name=":29">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
The classical example of this is Darwin's finches, a group of up to fifteen tanager species that are endemic to the Galápagos Islands.<ref>Template:Cite journal</ref> These birds evolved different beaks in order to eat different kinds of food available on the islands. The large ground finch has a large bill used to crack seeds and eat fruit. The Genovesa cactus finch prefers cacti as a food source, and has a beak adapted for removing pulp and flowers from cacti. The green warbler-finch (in the habit of true warbler species) consumes spiders and insects that live on plants.<ref name=":29" /> Other examples of this phenomenon exist worldwide, including in Hawaii and Madagascar, and are not limited to island ecosystems.<ref name=":29" />
The island ruleEdit
Species endemic to islands show a common evolutionary trajectory. Foster's rule (also known as the island rule), states that small mammals such as rodents evolve to become larger, known as island gigantism. One such example is the giant tortoise of the Seychelles, though it is unknown if it grew in size before or after reaching the island. Larger animals such as the hippopotamus tend to become smaller, such as in the case of the pygmy hippopotamus. This is known as insular dwarfism.<ref name=":30">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> In the case of smaller animals, it has been hypothesized that animals on islands may have fewer predators and competitors, resulting in selection pressure towards larger animals. Larger animals may exhaust food resources quickly due to their size, causing malnutrition in their young, resulting in a selection pressure for smaller animals that require less food. Having fewer predators would mean these animals did not need not be large to survive.<ref name=":30" />
Darwin, the Galápagos, and natural selectionEdit
Charles Darwin formulated the theory of natural selection through the study of island ecology.<ref name=":27" /> The species he observed on the Galápagos Islands, including tanager birds, contributed to his understanding of how evolution works.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> He first traveled to the islands as a naturalist on HMS Beagle in 1835, as part of a five-year circumnavigation of Earth. He wrote that "the different islands to a considerable extent are inhabited by a different set of beings".<ref name=":22">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> Through the study of the finches and other animals he realized that organisms survive by changing to adapt to their habitat.<ref name=":22" /> It would be over twenty years before he published his theories in On the Origin of Species.<ref name=":31">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
Humans and islandsEdit
History of explorationEdit
The first evidence of humans colonizing islands probably occurred in the Paleolithic era, 100,000 to 200,000 years ago. Reaching the Indonesian islands of Flores and Timor would have required crossing distances of water of at least Template:Cvt.<ref name=":9">Template:Citation</ref> Some islands, such as Honshu, were probably connected to the mainland with a land bridge that allowed humans to colonize it before it became an island.<ref name=":9" />
The first people to colonize distant oceanic islands were the Polynesians.<ref name=":10" /> Many of the previous island settlements required traveling distances of less than Template:Cvt, whereas Polynesians may have traveled Template:Convert to settle islands such as Tahiti.<ref name=":9" /> They would send navigators to sail the ocean without the aid of navigational instruments to discover new islands for settlement.<ref name=":10">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref><ref name=":20">Template:Cite book</ref> Between 1100 and 800 BC, Polynesians sailed East from New Guinea and the Solomon Islands and reached the islands that make up the modern-day Fiji and Samoa.<ref>Template:Cite book</ref> The furthest extent of this migration would be Easter Island in the East, and New Zealand in the South, with New Zealand's first settlements between 1250 and 1300.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
Historians have sought to understand why some remote islands have always been uninhabited, while others, especially in the Pacific Ocean, have long been populated by humans.<ref name=":9" /> Generally, larger islands are more likely to be able to sustain humans and thus are more likely to have been settled. Small islands that cannot sustain populations on their own can still be habitable if they are within a "commuting" distance to an island that has enough resources to be sustainable.<ref name=":9" /> The presence of an island is marked by seabirds, differences in cloud and weather patterns, as well as changes in the direction of waves.<ref name=":20" /><ref name=":10" /> It is also possible for human populations to have gone extinct on islands, evidenced by explorers finding islands that show evidence of habitation but no life.<ref name=":9" />
Not all islands were or are inhabited by maritime cultures.<ref name=":9" /><ref name=":8" /> In the past, some societies were found to have lost their seafaring ability over time, such as the case of the Canary Islands, which were occupied by an indigenous people since the island's first discovery in the first century until being conquered by the Spanish Empire in 1496.<ref name=":8">Template:Cite journal</ref> It has been hypothesized that since the inhabitants had little incentive for trade and had little to any contact with the mainland, they had no need for boats.<ref name=":8" />
The motivation for island exploration has been the subject of research and debate. Some early historians previously argued that early island colonization was unintentional, perhaps by a raft being swept out to sea.<ref>Template:Cite journal</ref> Others compare the motivations of Polynesian and similar explorers with those of Christopher Columbus, the explorer who sailed westward over the Atlantic Ocean in search of an alternate route to the East Indies.<ref name=":9" /> These historians theorize that successful explorers were rewarded with recognition and wealth, leading others to attempt possibly dangerous expeditions to discover more islands, usually with poor results.<ref name=":9" />
LifestyleEdit
About 10% of the world's population lives on islands.<ref name=":11">Template:Cite journal</ref> The study of the culture of islands is known as island studies. The interest in the study of islands is due to their unique cultures and natural environments that differ from mainland cultures.<ref name=":11" /> This is for a few reasons: First, the obvious political and geographic isolation from mainland cultures.<ref name=":11" /> Second, unique restraints on resources and ecology creating marine-focused cultures with a focus on fishing and sailing.<ref name=":11" /> Third, a lasting historical and political significance of islands.<ref name=":11" />
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DietEdit
The Polynesian diet got most of its protein from fishing.<ref>Template:Cite journal</ref> Polynesians were known to fish close to shore, as well as in deep water. It was reported that Rapa Nui people were known to fish as far as Template:Cvt from shore at coral reefs.<ref name=":12">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> Spear, line, and net fishing were all used,<ref name=":25">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> to catch tuna as well as sharks and stingrays.<ref name=":12" /> Island cultures also cultivate native and non-native crops.<ref name=":8" /> Polynesians grew the native yam, taro, breadfruit, banana, coconut and other fruits and vegetables.<ref>Template:Cite book</ref> Different island climates made different resources more important, such as the Hawaiian islands being home to irrigated fields of taro,<ref name=":25" /> whereas in some islands, like Tahiti, breadfruit was more widely cultivated and fermented in order to preserve it.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> There is archeological evidence that Canary Islanders would chew the roots of ferns for sustenance, a practice that wore heavily on their molars.<ref name=":8" /> These islanders would also grow barley and raised livestock such as goats.<ref name=":8" />
Island nations and territoriesEdit
Template:Further Many island nations have little land and a restricted set of natural resources. However, these nations control some of the largest fisheries in the world, deposits of copper, gold, and nickel, as well as oil deposits. The natural beauty of island nations also makes them a magnet for tourism. Islands also have geopolitical value for naval bases, weapons testing, and general territorial control. One such example is French Polynesia, a territory that receives substantial military expenditure and aid from France.<ref>Template:Cite book</ref> Three others, Palau, Federated States of Micronesia, and the Marshall Islands, are island nations of the Pacific region that maintain a defense, aid, and immigration agreement with the United States called a Compact of Free Association.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
ColonizationEdit
Since the first discoveries of Polynesian, Micronesian, and other islands by Westerners, these nations have been the subject of colonization.<ref name=":14">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> Islands were the target of Christian missionaries. These missionaries faced resistance, but found success when some local chiefs used European support to centralize power. Beginning in the 16th century, European states placed most of Oceania in under colonial administration.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> Pohnpei was colonized by Spain as early as 1526. It changed hands from Germany to Japan to the United States before joining the Federated States of Micronesia in 1982, maintaining a "free association" status with the U.S.<ref>Template:Cite journal</ref> Guam was a Spanish territory until 1898, and now is a unincorporated territory of the U.S.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
The decolonization era saw many island states achieve independence or some form of self-governance.<ref name=":13">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> Nuclear weapons testing on the Marshall Islands left many atolls destroyed or uninhabitable, causing the forced displacement of people from their home islands as well as increases in cancer rates due to radiation.<ref name=":14" /> Colonization has resulted in a decline of observance of traditional cultural practices in places such as Hawaii, where Native Hawaiians are now a minority. Cultural attitudes related to communal ownership of land as well as a lack of individualistic decision-making may make some island cultures less compatible with the global capitalist economy, causing these nations to experience less economic growth.<ref name=":13" />
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TourismEdit
Islands have long been a popular target for tourism, thanks to their unique climates, cultures, and natural beauty. However, islands may suffer from poor transportation connectivity from airplanes and boats and strains on infrastructure from tourist activity.<ref name=":15">Template:Cite journal</ref> Islands in colder climates often rely on seasonal tourists seeking to enjoy nature or local cultures, and may only be one aspect of an island's economy. In contrast, tourism on tropical islands can often make up the majority of the local economy and built environment. These islands sometimes also require consistent foreign aid on top of tourism in order to ensure economic growth. This reliance can result in social inequality and environmental degradation. During tourism downturns, these economies struggle to make up the lost inflow of cash with other industries.<ref name=":15" />
Threats to islandsEdit
Climate change threatens human development on islands due to sea level rise, more dangerous tropical cyclones, coral bleaching, and an increase in invasive species.<ref name=":16">Template:Citation</ref> For example, in 2017 Hurricane Maria caused a loss of almost all the infrastructure in Dominica. Sea level rise and other climate changes can reduce freshwater reserves, resulting in droughts.<ref name=":16" /> These risks are expected to decrease the habitability of islands, especially small ones. Beyond risks to human life, plant and animal life are threatened. It has been estimated that almost 50 percent of land species threatened by extinction live on islands.<ref name=":16" /> In 2017, a detailed review of 1,288 islands found that they were home to 1,189 highly-threatened vertebrate species, which was 41 percent of the global figure.<ref name=Spatz>Template:Citation</ref> Coral bleaching is expected to occur with more frequency, threatening marine ecosystems, some of which island economies are dependent on.<ref name=":16" />
Some islands that are low-lying may cease to exist given high enough amounts of sea level rise. Tuvalu received media attention for a press conference publicizing the ongoing submerging of the island country.<ref name=":17">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> Tuvalu signed a cooperation agreement with Australia agreeing to annually allow 280 of its citizens to become permanent residents of Australia. The Marshall Islands, a country of 1,156 islands, have also been identified as a country that may be existentially threatened by rising seas.<ref name=":17" />
Increasing intensity of tropical storms also increases the distances and frequency with which invasive species may be transported to islands. Floodwaters from these storms may also wash plants further inland than they would travel on their own, introducing them to new habitats.<ref name=":23" /> Agriculture and trade also have introduced non-native life to islands. These processes result in an introduction of invasive species to ecosystems that are especially small and fragile. One example is the apple snail, initially introduced to the U.S. by aquarium owners. It has since been transported by hurricanes across the Gulf Coast and neighboring islands.<ref name=":23" /> These species compete for resources with native animals, and some may grow so densely that they displace other forms of existing life.<ref name=":23" />
Artificial islandsEdit
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For hundreds of years, islands have been created through land reclamation.<ref name=":18">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> One of the first recorded instances of this when people of the Solomon Islands created eighty such islands by piling coral and rock in the Lau Lagoon.<ref name=":18" /> One traditional way of constructing islands is with the use of a revetment. Sandbags or stones are dropped with a barge into the sea to bring the land level slightly out of the water. The island area is then filled with sand or gravel, followed by a construction of this revetment to hold it together.<ref name=":19">Template:Cite book</ref> Islands have also been constructed with a permanent caisson, a steel or concrete structure built in a closed loop and then filled with sand.<ref name=":19" />
Some modern islands have been constructed by pouring millions of tons of sand into the sea, such as with Pearl Island in Qatar or the Palm Islands in Dubai.<ref name=":18" /> These islands are usually created for real estate development, and are sold for private ownership or construction of housing.<ref name=":18" /> Offshore oil platforms have also been described as a type of island. Some atolls have been covered in concrete to create artificial islands for military purposes, such as those created by China in the South China Sea.<ref name=":18" /><ref name=":26">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> These atolls were previously low-tide elevations, landmasses that are only above water during low tide. The United Nations Convention on the Law of the Sea indicates that these islands may not have the same legal status as a naturally occurring island, and as such may not confer the same legal rights.<ref name=":26" />
See alsoEdit
- Lists of islands
- List of archipelagos
- List of artificial islands
- List of divided islands
- List of fictional islands
- List of island countries
- List of islands by area
- List of islands by country
- List of islands by highest point
- List of islands by name
- List of islands by population
- List of islands by population density
- List of islands named after people
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