"North Pacific", "Pacific", and "Pacific region" redirect here.
For the region in Colombia, see Pacific Region, Colombia.
|Surface area||165,250,000 km (63,800,000 sq mi)|
|Average depth||4,280 m (14,040 ft)|
|Max. depth||10,911 m (35,797 ft)|
|Water volume||710,000,000 km (170,000,000 cu mi)|
|Islands||List of islands|
|Settlements||Anchorage, Auckland, Brisbane, Busan, Buenaventura, Guayaquil, Hong Kong, Honolulu, Lima, Los Angeles, Magadan, Manila, Melbourne, Osaka, Panama City, Papeete, San Francisco Bay Area, San Diego, Seattle, Shanghai, Singapore, Suva, Sydney, Tijuana, Tokyo, Valparaíso, Vancouver, Vladivostok, Christchurch,|
It extends from the Arctic Ocean in the north to the Southern Ocean (or, depending on definition, to Antarctica) in the south and is bounded by the continents of Asia and Oceania in the west and the Americas in the east.
At 165,250,000 square kilometers (63,800,000 square miles) in area (as defined with an Antarctic southern border), this largest division of the World Ocean—and, in turn, the hydrosphere—covers about 46% of Earth's water surface and about 32% of its total surface area, making it larger than all of Earth's land area combined (148,000,000 square kilometers).
Ocean circulation (caused by the Coriolis effect) subdivides it into two largely independent volumes of water, which meet at the equator: the North(ern) Pacific Ocean and South(ern) Pacific Ocean.
Its mean depth is 4,000 meters (13,000 feet).
The third deepest point on Earth, the Sirena Deep, is also located in the Mariana Trench.
Though the peoples of Asia and Oceania have traveled the Pacific Ocean since prehistoric times, the eastern Pacific was first sighted by Europeans in the early 16th century when Spanish explorer Vasco Núñez de Balboa crossed the Isthmus of Panama in 1513 and discovered the great "southern sea" which he named Mar del Sur (in Spanish).
Biggest seas in Pacific Ocean
Top large seas:
Important human migrations occurred in the Pacific in prehistoric times.
About 3000 BC, the Austronesian peoples on the island of Taiwan mastered the art of long-distance canoe travel and spread themselves and their languages south to the Philippines, Indonesia, and maritime Southeast Asia; west towards Madagascar; southeast towards New Guinea and Melanesia (intermarrying with native Papuans); and east to the islands of Micronesia, Oceania and Polynesia.
Trade, and therefore knowledge, extended to the Indonesian islands but apparently not Australia.
In 219 BC Xu Fu sailed out into the Pacific searching for the elixir of immortality.
By at least 878 when there was a significant Islamic settlement in Canton much of this trade was controlled by Arabs or Muslims.
Main article: Exploration of the Pacific
The first contact of European navigators with the western edge of the Pacific Ocean was made by the Portuguese expeditions of António de Abreu and Francisco Serrão, via the Lesser Sunda Islands, to the Maluku Islands, in 1512, and with Jorge Álvares's expedition to southern China in 1513, both ordered by Afonso de Albuquerque from Malacca.
He named it Mar del Sur (literally, "Sea of the South" or "South Sea") because the ocean was to the south of the coast of the isthmus where he first observed the Pacific.
Magellan called the ocean Pacífico (or "Pacific" meaning, "peaceful") because, after sailing through the stormy seas off Cape Horn, the expedition found calm waters.
The ocean was often called the Sea of Magellan in his honor until the eighteenth century.
Magellan stopped at one uninhabited Pacific island before stopping at Guam in March 1521.
Although Magellan himself died in the Philippines in 1521, Spanish navigator Juan Sebastián Elcano led the remains of the expedition back to Spain across the Indian Ocean and round the Cape of Good Hope, completing the first world circumnavigation in 1522.
In 1542–43 the Portuguese also reached Japan.
For the remainder of the 16th century, Spanish influence was paramount, with ships sailing from Mexico and Peru across the Pacific Ocean to the Philippines via Guam, and establishing the Spanish East Indies.
Later, in the quest for Terra Australis ("the [great] Southern Land"), Spanish explorations in the 17th century, such as the expedition led by the Portuguese navigator Pedro Fernandes de Queirós, discovered the Pitcairn and Vanuatu archipelagos, and sailed the Torres Strait between Australia and New Guinea, named after navigator Luís Vaz de Torres.
Dutch explorers, sailing around southern Africa, also engaged in discovery and trade; Willem Janszoon, made the first completely documented European landing in Australia (1606), in Cape York Peninsula, and Abel Janszoon Tasman circumnavigated and landed on parts of the Australian continental coast and discovered Tasmania and New Zealand in 1642.
In the 16th and 17th centuries, Spain considered the Pacific Ocean a mare clausum—a sea closed to other naval powers.
As the only known entrance from the Atlantic, the Strait of Magellan was at times patrolled by fleets sent to prevent entrance of non-Spanish ships.
On the western side of the Pacific Ocean the Dutch threatened the Spanish Philippines.
The 18th century marked the beginning of major exploration by the Russians in Alaska and the Aleutian Islands, such as the First Kamchatka expedition and the Great Northern Expedition, led by the Danish Russian navy officer Vitus Bering.
In 1768, Pierre-Antoine Véron, a young astronomer accompanying Louis Antoine de Bougainville on his voyage of exploration, established the width of the Pacific with precision for the first time in history.
One of the earliest voyages of scientific exploration was organized by Spain in the Malaspina Expedition of 1789–1794.
It sailed vast areas of the Pacific, from Cape Horn to Alaska, Guam and the Philippines, New Zealand, Australia, and the South Pacific.
See also: New Imperialism
Growing imperialism during the 19th century resulted in the occupation of much of Oceania by European powers, and later Japan and the United States.
Significant contributions to oceanographic knowledge were made by the voyages of HMS Beagle in the 1830s, with Charles Darwin aboard; HMS Challenger during the 1870s; the USS Tuscarora (1873–76); and the German Gazelle (1874–76).
By occupying Easter Island, Chile joined the imperial nations.
By 1900 nearly all Pacific islands were in control of Britain, France, United States, Germany, Japan, and Chile.
Although the United States gained control of Guam and the Philippines from Spain in 1898, Japan controlled most of the western Pacific by 1914 and occupied many other islands during the Pacific War; however, by the end of that war, Japan was defeated and the U.S. was the virtual master of the ocean. Pacific Fleet
The Japanese-ruled Northern Mariana Islands came under the control of the United States.
Since the end of World War II, many former colonies in the Pacific have become independent states.
The Pacific separates Asia and Australia from the Americas.
It may be further subdivided by the equator into northern (North Pacific) and southern (South Pacific) portions.
The Pacific Ocean encompasses approximately one-third of the Earth's surface, having an area of 165,200,000 km (63,800,000 sq mi)— larger than Earth's entire landmass combined, 150,000,000 km (58,000,000 sq mi).
Extending approximately 15,500 km (9,600 mi) from the Bering Sea in the Arctic to the northern extent of the circumpolar Southern Ocean at 60°S (older definitions extend it to Antarctica's Ross Sea), the Pacific reaches its greatest east–west width at about 5°N latitude, where it stretches approximately 19,800 km (12,300 mi) from Indonesia to the coast of Colombia—halfway around the world, and more than five times the diameter of the Moon.
Its average depth is 4,280 m (14,040 ft; 2,340 fathoms), putting the total water volume at roughly 710,000,000 km (170,000,000 cu mi).
Due to the effects of plate tectonics, the Pacific Ocean is currently shrinking by roughly 2.5 cm (1 in) per year on three sides, roughly averaging 0.52 km (0.20 sq mi) a year.
By contrast, the Atlantic Ocean is increasing in size.
Along the Pacific Ocean's irregular western margins lie many seas, the largest of which are the Celebes Sea, Coral Sea, East China Sea (East Sea), Philippine Sea, Sea of Japan, South China Sea (South Sea), Sulu Sea, Tasman Sea, and Yellow Sea (West Sea of Korea).
The Indonesian Seaway (including the Strait of Malacca and Torres Strait) joins the Pacific and the Indian Ocean to the west, and Drake Passage and the Strait of Magellan link the Pacific with the Atlantic Ocean on the east.
As the Pacific straddles the 180th meridian, the West Pacific (or western Pacific, near Asia) is in the Eastern Hemisphere, while the East Pacific (or eastern Pacific, near the Americas) is in the Western Hemisphere.
The Southern Pacific Ocean harbors the Southeast Indian Ridge crossing from south of Australia turning into the Pacific-Antarctic Ridge (north of the South Pole) and merges with another ridge (south of South America) to form the East Pacific Rise which also connects with another ridge (south of North America) which overlooks the Juan de Fuca Ridge.
Many tropical storms batter the islands of the Pacific.
Tsunamis, caused by underwater earthquakes, have devastated many islands and in some cases destroyed entire towns.
The Martin Waldseemüller map of 1507 was the first to show the Americas separating two distinct oceans.
Later, the Diogo Ribeiro map of 1529 was the first to show the Pacific at about its proper size.
Bordering countries and territories
Landmasses and islands
Main article: Pacific Islands
The Pacific Ocean has most of the islands in the world.
There are about 25,000 islands in the Pacific Ocean.
Micronesia, which lies north of the equator and west of the International Date Line, includes the Mariana Islands in the northwest, the Caroline Islands in the center, the Marshall Islands to the east and the islands of Kiribati in the southeast.
The largest area, Polynesia, stretching from Hawaii in the north to New Zealand in the south, also encompasses Tuvalu, Tokelau, Samoa, Tonga and the Kermadec Islands to the west, the Cook Islands, Society Islands and Austral Islands in the center, and the Marquesas Islands, Tuamotu, Mangareva Islands, and Easter Island to the east.
Islands in the Pacific Ocean are of four basic types: continental islands, high islands, coral reefs and uplifted coral platforms.
Continental islands lie outside the andesite line and include New Guinea, the islands of New Zealand, and the Philippines.
Some of these islands are structurally associated with nearby continents.
High islands are of volcanic origin, and many contain active volcanoes.
Among these are Bougainville, Hawaii, and the Solomon Islands.
The coral reefs of the South Pacific are low-lying structures that have built up on basaltic lava flows under the ocean's surface.
A second island type formed of coral is the uplifted coral platform, which is usually slightly larger than the low coral islands.
The volume of the Pacific Ocean, representing about 50.1 percent of the world's oceanic water, has been estimated at some 714 million cubic kilometers (171 million cubic miles).
Surface water temperatures in the Pacific can vary from −1.4 °C (29.5 °F), the freezing point of sea water, in the poleward areas to about 30 °C (86 °F) near the equator.
Salinity also varies latitudinally, reaching a maximum of 37 parts per thousand in the southeastern area.
The water near the equator, which can have a salinity as low as 34 parts per thousand, is less salty than that found in the mid-latitudes because of abundant equatorial precipitation throughout the year.
The lowest counts of less than 32 parts per thousand are found in the far north as less evaporation of seawater takes place in these frigid areas.
The Aleutian Current branches as it approaches North America and forms the base of a counter-clockwise circulation in the Bering Sea.
Its southern arm becomes the chilled slow, south-flowing California Current.
The South Equatorial Current, flowing west along the equator, swings southward east of New Guinea, turns east at about 50°S, and joins the main westerly circulation of the South Pacific, which includes the Earth-circling Antarctic Circumpolar Current.
The climate patterns of the Northern and Southern Hemispheres generally mirror each other.
The trade winds in the southern and eastern Pacific are remarkably steady while conditions in the North Pacific are far more varied with, for example, cold winter temperatures on the east coast of Russia contrasting with the milder weather off British Columbia during the winter months due to the preferred flow of ocean currents.
In the tropical and subtropical Pacific, the El Niño Southern Oscillation (ENSO) affects weather conditions.
To determine the phase of ENSO, the most recent three-month sea surface temperature average for the area approximately 3,000 km (1,900 mi) to the southeast of Hawaii is computed, and if the region is more than 0.5 °C (0.9 °F) above or below normal for that period, then an El Niño or La Niña is considered in progress.
Worldwide, tropical cyclone activity peaks in late summer, when the difference between temperatures aloft and sea surface temperatures is the greatest; however, each particular basin has its own seasonal patterns.
On a worldwide scale, May is the least active month, while September is the most active month.
November is the only month in which all the tropical cyclone basins are active.
The Pacific hosts the two most active tropical cyclone basins, which are the northwestern Pacific and the eastern Pacific.
Pacific hurricanes form south of Mexico, sometimes striking the western Mexican coast and occasionally the southwestern United States between June and October, while typhoons forming in the northwestern Pacific moving into southeast and east Asia from May to December.
Tropical cyclones also form in the South Pacific basin, where they occasionally impact island nations.
In the arctic, icing from October to May can present a hazard for shipping while persistent fog occurs from June to December.
A climatological low in the Gulf of Alaska keeps the southern coast wet and mild during the winter months.
The Westerlies and associated jet stream within the Mid-Latitudes can be particularly strong, especially in the Southern Hemisphere, due to the temperature difference between the tropics and Antarctica, which records the coldest temperature readings on the planet.
In the Southern hemisphere, because of the stormy and cloudy conditions associated with extratropical cyclones riding the jet stream, it is usual to refer to the Westerlies as the Roaring Forties, Furious Fifties and Shrieking Sixties according to the varying degrees of latitude.
To Magellan, it seemed much more calm (pacific) than the Atlantic.
The andesite line is the most significant regional distinction in the Pacific.
The andesite line follows the western edge of the islands off California and passes south of the Aleutian arc, along the eastern edge of the Kamchatka Peninsula, the Kuril Islands, Japan, the Mariana Islands, the Solomon Islands, and New Zealand's North Island.
Indonesia, the Philippines, Japan, New Guinea, and New Zealand lie outside the andesite line.
Within the closed loop of the andesite line are most of the deep troughs, submerged volcanic mountains, and oceanic volcanic islands that characterize the Pacific basin.
Here basaltic lavas gently flow out of rifts to build huge dome-shaped volcanic mountains whose eroded summits form island arcs, chains, and clusters.
The Ring of Fire is named after the several hundred active volcanoes that sit above the various subduction zones.
The Pacific Ocean is the only ocean which is mostly bounded by subduction zones.
Only the Antarctic and Australian coasts have no nearby subduction zones.
The oldest Pacific Ocean floor is only around 180 Ma old, with older crust subducted by now.
The exploitation of the Pacific's mineral wealth is hampered by the ocean's great depths.
In shallow waters of the continental shelves off the coasts of Australia and New Zealand, petroleum and natural gas are extracted, and pearls are harvested along the coasts of Australia, Japan, Papua New Guinea, Nicaragua, Panama, and the Philippines, although in sharply declining volume in some cases.
Fish are an important economic asset in the Pacific.
Overfishing has become a serious problem in some areas.
For example, catches in the rich fishing grounds of the Okhotsk Sea off the Russian coast have been reduced by at least half since the 1990s as a result of overfishing.
Main article: Marine pollution
The quantity of small plastic fragments floating in the north-east Pacific Ocean increased a hundredfold between 1972 and 2012.
The ever-growing Great Pacific garbage patch between California and Japan is three times the size of France.
An estimated 80,000 metric tons of plastic inhabit the patch, totaling 1.8 trillion pieces.
Marine pollution is a generic term for the harmful entry into the ocean of chemicals or particles.
The main culprits are those using the rivers for disposing of their waste.
The rivers then empty into the ocean, often also bringing chemicals used as fertilizers in agriculture.
Marine debris, also known as marine litter, is human-created waste that has ended up floating in a lake, sea, ocean, or waterway.
Oceanic debris tends to accumulate at the center of gyres and coastlines, frequently washing aground where it is known as beach litter.
Major ports and harbors
Main article: List of ports and harbors of the Pacific Ocean
Credits to the contents of this page go to the authors of the corresponding Wikipedia page: en.wikipedia.org/wiki/Pacific Ocean.