"Email" is the e-mail address you used when you registered.

"Password" is case sensitive.

If you need additional assistance, please contact .

Enter the e-mail address you used when enrolling for Britannica Premium Service and we will e-mail your password to you.

Pacific Ocean

ARTICLE
from the
Encyclopædia Britannica
Get involved Share

Pacific Ocean, The Pacific Ocean, with depth contours and submarine features.
[Credit: Encyclop?dia Britannica, Inc.]body of salt water extending from the Antarctic region in the south to the Arctic in the north and lying between the continents of Asia and Australia on the west and North and South America on the east.

Of the three oceans that extend northward from the Antarctic continent, the Pacific is by far the largest, occupying about a third of the surface of the globe. Its area, excluding adjacent seas, encompasses about 63.8 million square miles (165.25 million square km). It has double the area and more than double the water volume of the Atlantic Ocean—the next largest division of the hydrosphere—and its area more than exceeds that of the whole land surface of the globe. The Pacific Ocean stretches from the shores of Antarctica to the Bering Strait through 135° of latitude, some 9,600 miles (15,500 km). Its greatest longitudinal extent measures some 12,000 miles (19,300 km) along latitude 5° N, between the coasts of Colombia in South America and the Malay Peninsula in Asia. The mean depth of the Pacific (excluding adjacent seas) is 14,040 feet (4,280 metres), and its greatest known depth is 36,201 feet (11,034 metres)—in the Mariana Trench—also the greatest depth found in any ocean.

In the Northern Hemisphere the Pacific Ocean meets the Arctic Ocean in the Bering Sea. In the Southern Hemisphere the Pacific and Atlantic mix in the relatively narrow Drake Passage between Tierra del Fuego in South America and Graham Land in Antarctica. The separation between the Pacific and Indian oceans is less distinct, but generally it is considered to lie along the line of islands extending eastward from Sumatra, through Java to Timor, thence across the Timor Sea to Cape Londonderry in Australia. To the south of Australia the boundary extends across the Bass Strait and thence from Tasmania to Antarctica. The portion of the Pacific near Antarctica sometimes is considered to be part of the Southern Ocean.

Because of the pattern of major mountain systems of the globe, a relatively small proportion (one-seventh) of the total continental drainage enters the Pacific—a total drainage area of less than about three times the total area of Australia. Of the rivers that drain into the Pacific, those of China and Southeast Asia are of the greatest importance; the basins of those rivers support more than one-fourth of the world’s population.

The eastern boundary of the Pacific is associated with the American cordilleran system, which stretches from Alaska in the north to Tierra del Fuego in the south. Except for its extreme northern and southern sections, which are characterized by fjords and their numerous off-lying islands, and except for the deeply indented Gulf of California, the coastal boundary is relatively regular and the continental shelf narrow. The western, or Asiatic, coastal boundary, in contrast, is irregular. Although the mountain systems there lie roughly parallel to the coast, as they do on the eastern Pacific coastlands, the western Pacific is noted for its many marginal seas. From north to south they include the Bering Sea, the Sea of Okhotsk, the Sea of Japan (East Sea), the Yellow Sea, the East China Sea, and the South China Sea. Their eastern boundaries are formed by southward-jutting peninsulas or island arcs or both. It is of oceanographic significance that the great rivers of eastern Asia—including the Amur, the Huang He (Yellow River), the Yangtze, the Xi and Pearl (Zhu), and the Mekong—enter the Pacific indirectly by way of the marginal seas.

This article treats the physical and human geography of the Pacific Ocean. For discussion of the physical and chemical oceanography and marine geology of the Pacific, see ocean.

LINKS
Related Articles

Aspects of the topic Pacific Ocean are discussed in the following places at Britannica.

Assorted References

exploration

physiography

tropical storms

 (in  tropical storm)
LINKS
Other Britannica Sites

Articles from Britannica encyclopedias for elementary and high school students.

Pacific Ocean - Children's Encyclopedia (Ages 8-11)

The Pacific is the largest of Earth’s oceans. It covers more of Earth’s surface than all the dry land put together. The explorer Ferdinand Magellan named the ocean El Mar pacifico, which means "the peaceful sea."

Pacific Ocean - Student Encyclopedia (Ages 11 and up)

The major feature of the Pacific Ocean is its enormous size: not only is it the largest ocean in the world, it is also the world’s largest single physical feature. With an area of about 64 million square miles (166 million square kilometers), it is twice the size of the Atlantic Ocean and occupies nearly a third of the surface of the Earth-more than the area of all the Earth’s land surfaces. The Pacific reaches about 9,300 miles (15,000 kilometers) from Antarctica almost to the Arctic Circle in the Bering Sea. Its greatest dimension stretches from east to west, with nearly half the length of the Equator lying across its surface-11,000 miles (18,000 kilometers).

The topic Pacific Ocean is discussed at the following external Web sites.

Citations

To cite this page:

MLA Style:

"Pacific Ocean." Encyclopædia Britannica. Encyclopædia Britannica Online. Encyclopædia Britannica Inc., 2012. Web. 28 Oct. 2012. <http://www.britannica.com/EBchecked/topic/437703/Pacific-Ocean>.

APA Style:

Pacific Ocean. (2012). In Encyclopædia Britannica. Retrieved from http://www.britannica.com/EBchecked/topic/437703/Pacific-Ocean

Harvard Style:

Pacific Ocean 2012. Encyclopædia Britannica Online. Retrieved 28 October, 2012, from http://www.britannica.com/EBchecked/topic/437703/Pacific-Ocean

Chicago Manual of Style:

Encyclopædia Britannica Online, s. v. "Pacific Ocean," accessed October 28, 2012, http://www.britannica.com/EBchecked/topic/437703/Pacific-Ocean.

 This feature allows you to export a Britannica citation in the RIS format used by many citation management software programs.
While every effort has been made to follow citation style rules, there may be some discrepancies. Please refer to the appropriate style manual or other sources if you have any questions.
VIDEOS
IMAGES
INTER
ACTIVES

Britannica's Web Search provides an algorithm that improves the results of a standard web search.

Try searching the web for the topic Pacific Ocean.

No results found.
Type a word or double click on any word to see a definition from the Merriam-Webster Online Dictionary.
Type a word or double click on any word to see a definition from the Merriam-Webster Online Dictionary.
No results found.
Type a word to see synonyms from the Merriam-Webster Online Thesaurus.
Type a word to see synonyms from the Merriam-Webster Online Thesaurus.
VIDEOS
IMAGES
INTER
ACTIVES
  • All of the media associated with this article appears on the left. Click an item to view it.
  • Mouse over the caption, credit, links or citations to learn more.
  • You can mouse over some images to magnify, or click on them to view full-screen.
  • Click on the Expand button to view this full-screen. Press Escape to return.
  • Click on audio player controls to interact.
JOIN COMMUNITY LOGIN
Join Free Community

Please join our community in order to save your work, create a new document, upload media files, recommend an article or submit changes to our editors.

Log In

"Email" is the e-mail address you used when you registered. "Password" is case sensitive.

If you need additional assistance, please contact customer support.

Enter the e-mail address you used when registering and we will e-mail your password to you. (or click on Cancel to go back).

Save to My Workspace
Share the full text of this article with your friends, associates, or readers by linking to it from your web site or social networking page.

Permalink
Copy Link
Britannica needs you! Become a part of more than two centuries of publishing tradition by contributing to this article. If your submission is accepted by our editors, you'll become a Britannica contributor and your name will appear along with the other people who have contributed to this article. View Submission Guidelines
View Changes:
Revised:
By:
Share
Feedback

Send us feedback about this topic, and one of our Editors will review your comments.

(Please limit to 900 characters)
(Please limit to 900 characters) Send

Copy and paste the HTML below to include this widget on your Web page.

Apply proxy prefix (optional):
Copy Link
The Britannica Store

Share This

Other users can view this at the following URL:
Copy

Create New Project

Done

Rename This Project

Done

Add or Remove from Projects

Add to project:
Add
Remove from Project:
Remove

Copy This Project

Copy

Import Projects

Please enter your user name and password
that you use to sign in to your workspace account on
Britannica Online Academic.