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Geography of the Pacific Ocean

Learn Information about the World's Largest Ocean


Pacific Ocean

The Pacific Ocean

CIA World Factbook
Updated July 28, 2011

The Pacific Ocean is one of the world's five oceans. It is the largest with an area of 60.06 million square miles (155.557 million sq km) and it stretches from the Arctic Ocean in the north to the Southern Ocean in the south. It also sits between Asia and Australia as well as between Asia and North America and Australia and South America (map). With this area it covers about 28% of the Earth's surface and it is "almost equal to the total land area of the world" (CIA World Factbook). In addition the Pacific Ocean is also usually divided into the North and South Pacific regions with the equator serving as the division between the two.

Because of its large size, the Pacific Ocean, like the rest of the world's oceans, was formed millions of years ago and has a unique topography. It also plays a significant role in weather patterns around the globe and in today's economy.

Formation and Geology of the Pacific Ocean

It is believed that the Pacific Ocean formed millions of years ago after the break-up of Pangaea about 250 million years ago. It formed out of the Panthalassa Ocean that surrounded the Pangaea landmass. There is no specific date on when the Pacific Ocean developed, however because the ocean floor constantly recycles itself as it moves and is subducted, melted into the Earth's mantle and then forced up again at ocean ridges. Currently the oldest known Pacific Ocean floor is about 180 million years old.

In terms of its geology the area encompassing the Pacific Ocean is sometimes called the Pacific Ring of Fire. The region has this name because it is the world's largest area of volcanism and earthquakes. The Pacific is subject to this geologic activity because much of its seafloor sits above subduction zones where the edges of the Earth's plates are forced down below others after collision. In addition, there are some areas of hotspot volcanic activity where magma from the Earth's mantle is forced up through the crust creating underwater volcanoes which can eventually form islands and seamounts.

Topography of the Pacific Ocean

The Pacific Ocean has a highly varied topography that consists of oceanic ridges, trenches and long seamount chains that are formed by hotspot volcanoes under the Earth's surface (map). An example of these seamounts that are above the ocean's surface are the islands of Hawaii. Other seamounts are sometimes below the surface and they look like underwater islands such as the Davidson Seamount of the coast of Monterey, California.

Oceanic ridges are found in a few places in the Pacific Ocean and they are areas where new oceanic crust is being pushed up from below the Earth's surface. Once the new crust is pushed up, it spreads away from these locations. In these spots the ocean floor is not as deep and it is very young compared to other areas that are farther from the ridges. An example of a ridge in the Pacific is the East Pacific Rise.

By contrast there are also oceanic trenches in the Pacific that are home to very deep locations. As such, the Pacific is home to the deepest ocean point in the world - the Challenger Deep in the Mariana Trench. This trench is located in the western Pacific to the east of the Mariana Islands and it reaches a maximum depth of -35,840 feet (-10,924 m).

Finally, the topography of the Pacific Ocean varies even more where closer to large landmasses and islands. Some coastlines along the Pacific are rugged have high cliffs and nearby mountain ranges such as the west coast of the United States, while others have more gradual, gently sloping coastlines. In addition, some areas have deep, quickly dropping trenches near the coasts (such as the coast of Chile) while others are gradual.

The northern Pacific Ocean (and also the northern hemisphere) also has more land in it than the South Pacific. There are however many island chains and small islands like those in Micronesia and the Marshall Islands throughout the ocean. The largest island within the Pacific is the island of New Guinea.

Climate of the Pacific Ocean

The climate of the Pacific Ocean varies greatly based on latitude, the presence of landmasses and the types of air masses moving over its waters. The sea surface temperatures also play a role in the climate because it affects the availability of moisture in the different regions. Near the equator the climate is tropical, wet and warm throughout most of the year while the far North Pacific and far South Pacific are more temperate and have greater seasonal differences in weather patterns. In addition there are seasonal trade winds in some regions that impact climate as well as tropical cyclones in areas to the south of Mexico from June to October and typhoons in the South Pacific from May to December (CIA World Factbook).

Economy of the Pacific Ocean

Because it covers 28% of the Earth's surface, borders many different nations and is home to a wide variety of fish, plants and other animals, the Pacific Ocean plays a major role in the world's economy. It provides an easy way to ship goods from Asia to North America and vice versa, is a large part of the world's fishing industry and is a source of natural resources like oil and other minerals.

To learn more about the Pacific Ocean, visit Infoplease.com's page on the Pacific Ocean.


Central Intelligence Agency. (17 November 2010). CIA - The World Factbook - Pacific Ocean. Retrieved from: https://www.cia.gov/library/publications/the-world-factbook/geos/zn.html

Wikipedia.org. (26 July 2011). Pacific Ocean - Wikipedia, the Free Encyclopedia. Retrieved from: http://en.wikipedia.org/wiki/Pacific_Ocean

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