The CIA World Factbook Every edition, 1990 to 2021 Oceans
Terrain Pacific Ocean, in 32 editions.
The entry for Pacific Ocean published Terrain in 32 editions of 36, from 1990 to 2021. The text changed in 13 editions. Each is shown as published. Terrain in every entry.
- editions changed the text
- 13
- the first edition with it
- 1990
- the latest edition with it
- 2021
Published as “Terrain” (1990 to 2021).
field in that editiontext changed from the edition beforenot in that editionthe edition shownChoose an edition on the strip beside the text, or step through them with the arrows. Mark changes compares it with the edition before: the marks are ours, words added and words removed.
2021 edition
Changed since 2020The same text in 1990 and 1991.
- surface in the northern Pacific dominated by a clockwise, warm water gyre (broad, circular system of currents) and in the southern Pacific by a counterclockwise, cool water gyre;
- sea ice occurs in the Bering Sea and Sea of Okhotsk during winter and reaches maximum northern extent from Antarctica in October;
- the ocean floor in the eastern Pacific is dominated by the East Pacific Rise, while the western Pacific is dissected by deep trenches;
- the world's greatest depth is 10,924 meters in the Marianas Trench
surface in the northern Pacific dominated by a clockwise, warm water gyre (broad, circular system of currents) and in the southern Pacific by a counterclockwise, cool water gyre; sea ice occurs in the Bering Sea and Sea of Okhotsk during winter and reaches maximum northern extent from Antarctica in October; the ocean floor in the eastern Pacific is dominated by the East Pacific Rise, while the western Pacific is dissected by deep trenches; the world's greatest depth is 10,924 meters in the Marianas Trench
- surface in the northern Pacific dominated by a clockwise, warm-water gyre (broad, circular system of currents) and in the southern Pacific by a counterclockwise, cool-water gyre;
- sea ice occurs in the Bering Sea and Sea of Okhotsk during winter and reaches maximum northern extent from Antarctica in October;
- the ocean floor in the eastern Pacific is dominated by the East Pacific Rise, while the western Pacific is dissected by deep trenches;
- the world's greatest depth is 10,924 meters in the Marianas Trench
surface in the northern Pacific dominated by a clockwise, warm water warm-water gyre
(broad, circular system of currents) and in the southern Pacific by a
counterclockwise, cool water cool-water gyre; sea ice occurs in the Bering Sea and Sea
of Okhotsk during winter and reaches maximum northern extent from Antarctica
in October; the ocean floor in the eastern Pacific is dominated by the East
Pacific Rise, while the western Pacific is dissected by deep trenches; the
world's greatest depth is 10,924 meters in the Marianas Trench
- surface currents in the northern Pacific are dominated by a clockwise, warm-water gyre (broad circular system of currents) and in the southern Pacific by a counterclockwise, cool-water gyre;
- in the northern Pacific sea ice forms in the Bering Sea and Sea of Okhotsk in winter;
- in the southern Pacific sea ice from Antarctica reaches its northernmost extent in October;
- the ocean floor in the eastern Pacific is dominated by the East Pacific Rise, while the western Pacific is dissected by deep trenches, including the world's deepest, the 10,924 meter Marianas Trench
surface currents in the northern Pacific are dominated by a clockwise,
warm-water gyre (broad circular system of currents) and in the southern
(broad,
Pacific by acounterclockwise, cool-water gyre; in the northern Pacific sea
ice occurs forms in the Bering Sea and Seaof Okhotsk during winter and reaches maximum northern extent in winter; in the southern
Pacific sea ice from Antarcticareaches its northernmost extent in October;
the ocean floor in the eastern Pacific is dominated by the EastPacific
Rise, while the western Pacific is dissected by deep trenches; trenches, including the
world's greatest depth is 10,924 meters in deepest, the 10,924 meter Marianas Trench
- surface currents in the northern Pacific are dominated by a clockwise, warm-water gyre (broad circular system of currents) and in the southern Pacific by a counterclockwise, cool-water gyre;
- in the northern Pacific sea ice forms in the Bering Sea and Sea of Okhotsk in winter;
- in the southern Pacific sea ice from Antarctica reaches its northernmost extent in October;
- the ocean floor in the eastern Pacific is dominated by the East Pacific Rise, while the western Pacific is dissected by deep trenches, including the world's deepest, the 10,924 meter Marianas Trench
surface currents in the northern Pacific are dominated by a clockwise,
warm-water gyre (broad circular system of currents) and in the southern
southern Pacific by a counterclockwise, cool-water gyre; in the
northern Pacific seaice forms in the Bering Sea and Sea of Okhotsk in
winter; in the southernPacific sea ice from Antarctica reaches its
northernmost extent in October;the ocean floor in the eastern Pacific
is dominated by the East PacificRise, while the western Pacific is
dissected by deep trenches, including theworld's deepest, the 10,924
meter Marianas Trench
- surface currents in the northern Pacific are dominated by a clockwise, warm-water gyre (broad circular system of currents) and in the southern Pacific by a counterclockwise, cool-water gyre;
- in the northern Pacific sea ice forms in the Bering Sea and Sea of Okhotsk in winter;
- in the southern Pacific sea ice from Antarctica reaches its northernmost extent in October;
- the ocean floor in the eastern Pacific is dominated by the East Pacific Rise, while the western Pacific is dissected by deep trenches, including the world's deepest, the 10,924 meter Marianas Trench
surface currents in the northern Pacific are dominated by a clockwise,
clockwise, warm-water gyre (broad circular system of currents) and in the
the southern Pacific by a counterclockwise, cool-water gyre; in the
northern Pacific sea ice forms in the Bering Sea and Sea of Okhotsk in
winter; in the southern Pacific sea ice from Antarctica reaches its
northernmost extent in October; the ocean floor in the eastern Pacific
is dominated by the East Pacific Rise, while the western Pacific is
dissected by deep trenches, including the world's deepest, the 10,924
meter Marianas Trench
- surface currents in the northern Pacific are dominated by a clockwise, warm-water gyre (broad circular system of currents) and in the southern Pacific by a counterclockwise, cool-water gyre;
- in the northern Pacific, sea ice forms in the Bering Sea and Sea of Okhotsk in winter;
- in the southern Pacific, sea ice from Antarctica reaches its northernmost extent in October;
- the ocean floor in the eastern Pacific is dominated by the East Pacific Rise, while the western Pacific is dissected by deep trenches, including the Marianas Trench, which is the world's deepest
- lowest point:
- Marianas Trench -10,924 m
- highest point:
- sea level 0 m
surface currents in the northern Pacific are dominated by a
a clockwise, warm-water gyre (broad circular system of currents) and in
in the southern Pacific by a counterclockwise, cool-water gyre; in the
the northern Pacific Pacific, sea ice forms in the Bering Sea and Sea of
Okhotsk inwinter; in the southern Pacific Pacific, sea ice from Antarctica
reaches itsnorthernmost extent in October; the ocean floor in the
eastern Pacificis dominated by the East Pacific Rise, while the
western Pacific isdissected by deep trenches, including the world's deepest,
Marianas Trench, which is the 10,924 world's deepestmeter lowest point: Marianas Trench -10,924 m
highest point: sea level 0 m
- surface currents in the northern Pacific are dominated by a clockwise, warm-water gyre (broad circular system of currents) and in the southern Pacific by a counterclockwise, cool-water gyre;
- in the northern Pacific, sea ice forms in the Bering Sea and Sea of Okhotsk in winter;
- in the southern Pacific, sea ice from Antarctica reaches its northernmost extent in October;
- the ocean floor in the eastern Pacific is dominated by the East Pacific Rise, while the western Pacific is dissected by deep trenches, including the Marianas Trench, which is the world's deepest
surface currents in the northern Pacific are dominated bya
clockwise, warm-water gyre (broad circular system of currents) andin
the southern Pacific by a counterclockwise, cool-water gyre; inthe
northern Pacific, sea ice forms in the Bering Sea and Sea ofOkhotsk
in winter; in the southern Pacific, sea ice from Antarcticareaches
its northernmost extent in October; the ocean floor in theeastern
Pacific is dominated by the East Pacific Rise, while thewestern
Pacific is dissected by deep trenches, including theMarianas Trench,
which is the world's deepest
lowest point: Marianas Trench -10,924 m
highest point: sea level 0 m
- surface currents in the northern Pacific are dominated by a clockwise, warm-water gyre (broad circular system of currents) and in the southern Pacific by a counterclockwise, cool-water gyre;
- in the northern Pacific, sea ice forms in the Bering Sea and Sea of Okhotsk in winter;
- in the southern Pacific, sea ice from Antarctica reaches its northernmost extent in October;
- the ocean floor in the eastern Pacific is dominated by the East Pacific Rise, while the western Pacific is dissected by deep trenches, including the Mariana Trench, which is the world's deepest
surface currents in the northern Pacific are dominated by a
clockwise, warm-water gyre (broad circular system of currents) and in
the southern Pacific by a counterclockwise, cool-water gyre; in the
northern Pacific, sea ice forms in the Bering Sea and Sea of Okhotsk
in winter; in the southern Pacific, sea ice from Antarctica reaches
its northernmost extent in October; the ocean floor in the eastern
Pacific is dominated by the East Pacific Rise, while the western
Pacific is dissected by deep trenches, including the Marianas Mariana Trench,
which is the world's deepest
- surface currents in the northern Pacific are dominated by a clockwise, warm-water gyre (broad circular system of currents) and in the southern Pacific by a counterclockwise, cool-water gyre;
- in the northern Pacific, sea ice forms in the Bering Sea and Sea of Okhotsk in winter;
- in the southern Pacific, sea ice from Antarctica reaches its northernmost extent in October;
- the ocean floor in the eastern Pacific is dominated by the East Pacific Rise, while the western Pacific is dissected by deep trenches, including the Mariana Trench, which is the world's deepest
surface currents in the northern Pacific are dominated
by aclockwise, warm-water gyre (broad circular system of currents)
and inthe southern Pacific by a counterclockwise, cool-water gyre;
in thenorthern Pacific, sea ice forms in the Bering Sea and Sea of Okhotsk
Okhotsk in winter; in the southern Pacific, sea ice from Antarctica reaches
reaches its northernmost extent in October; the ocean floor in the eastern
eastern Pacific is dominated by the East Pacific Rise, while the western
western Pacific is dissected by deep trenches, including the Mariana Trench,
Trench, which is the world's deepest
The same text in 17 editions, 2000 to 2016.
- surface currents in the northern Pacific are dominated by a clockwise, warm-water gyre (broad circular system of currents) and in the southern Pacific by a counterclockwise, cool-water gyre;
- in the northern Pacific, sea ice forms in the Bering Sea and Sea of Okhotsk in winter;
- in the southern Pacific, sea ice from Antarctica reaches its northernmost extent in October;
- the ocean floor in the eastern Pacific is dominated by the East Pacific Rise, while the western Pacific is dissected by deep trenches, including the Mariana Trench, which is the world's deepest
surface currents in the northern Pacific are dominatedby a clockwise, warm-water gyre (broad circular system of currents)and in the southern Pacific by a counterclockwise, cool-water gyre;in the northern Pacific, sea ice forms in the Bering Sea and Sea ofOkhotsk in winter; in the southern Pacific, sea ice from Antarcticareaches its northernmost extent in October; the ocean floor in theeastern Pacific is dominated by the East Pacific Rise, while thewestern Pacific is dissected by deep trenches, including the MarianaTrench, which is the world's deepest
- surface dominated by two large gyres (broad, circular systems of currents), one in the northern Pacific and another in the southern Pacific;
- in the northern Pacific, sea ice forms in the Bering Sea and Sea of Okhotsk in winter;
- in the southern Pacific, sea ice from Antarctica reaches its northernmost extent in October;
- the ocean floor in the eastern Pacific is dominated by the East Pacific Rise, while the western Pacific is dissected by deep trenches, including the Mariana Trench, which is the world's deepest at 10,924 m
- major surface currents:
- clockwise North Pacific Gyre formed by the warm Kuroshio Current in the west, the North Pacific Current in the north, the cold California Current in the east, and the North Equatorial Current in the south;
- the counterclockwise South Pacific Gyre composed of the warm East Australian Current in the west, the South Pacific Current in the south, the cold Peru (Humbolt) Current in the east, and the South Equatorial Current in the north
surface currents in the northern Pacific are dominated by a clockwise, warm-water gyre (broad two large gyres (broad, circular system systems of currents) currents), one in the northern Pacific and another in the southern Pacific by a counterclockwise, cool-water gyre; Pacific; in the northern Pacific, sea ice forms in the Bering Sea and Sea of Okhotsk in winter; in the southern Pacific, sea ice from Antarctica reaches its northernmost extent in October; the ocean floor in the eastern Pacific is dominated by the East Pacific Rise, while the western Pacific is dissected by deep trenches, including the Mariana Trench, which is the world's deepest at 10,924 m
major surface currents: clockwise North Pacific Gyre formed by the warm Kuroshio Current in the west, the North Pacific Current in the north, the cold California Current in the east, and the North Equatorial Current in the south; the counterclockwise South Pacific Gyre composed of the warm East Australian Current in the west, the South Pacific Current in the south, the cold Peru (Humbolt) Current in the east, and the South Equatorial Current in the north
surface dominated by two large gyres (broad, circular systems of currents), one in the northern Pacific and another in the southern Pacific; in the northern Pacific, sea ice forms in the Bering Sea and Sea of Okhotsk in winter; in the southern Pacific, sea ice from Antarctica reaches its northernmost extent in October; the ocean floor in the eastern Pacific is dominated by the East Pacific Rise, while the western Pacific is dissected by deep trenches, including the Mariana Trench, which is the world's deepest at 10,924 m major surface currents: clockwise North Pacific Gyre formed by the warm Kuroshio Current in the west, the North Pacific Current in the north, the cold California Current in the east, and the North Equatorial Current in the south; the counterclockwise South Pacific Gyre composed of the warm East Australian Current in the west, the South Pacific Current in the south, the cold Peru (Humbolt) Current in the east, and the South Equatorial Current in the north
surface dominated by two large gyres (broad, circular systems of currents), one in the northern Pacific and another in the southern Pacific; in the northern Pacific, sea ice forms in the Bering Sea and Sea of Okhotsk in winter; in the southern Pacific, sea ice from Antarctica reaches its northernmost extent in October; the ocean floor in the eastern Pacific is dominated by the East Pacific Rise, while the western Pacific is dissected by deep trenches, including the Mariana Trench, which is the world's deepest at 10,924 mmajor surface currents: clockwise North Pacific Gyre formed by the warm Kuroshio Current in the west, the North Pacific Current in the north, the cold California Current in the east, and the North Equatorial Current in the south; the counterclockwise South Pacific Gyre composed of the warm East Australian Current in the west, the South Pacific Current in the south, the cold Peru (Humbolt) Current in the east, and the South Equatorial Current in the north
The same text in 2019 and 2020.
surface dominated by two large gyres (broad, circular systems of currents), one in the northern Pacific and another in the southern Pacific; in the northern Pacific, sea ice forms in the Bering Sea and Sea of Okhotsk in winter; in the southern Pacific, sea ice from Antarctica reaches its northernmost extent in October; the ocean floor in the eastern Pacific is dominated by the East Pacific Rise, while the western Pacific is dissected by deep trenches, including the Mariana Trench, which is the world's deepest at 10,924 m major surface currents: clockwise North Pacific Gyre formed by the warm northward flowing Kuroshio Current in the west, the eastward flowing North Pacific Current in the north, the southward flowing cold California Current in the east, and the westward flowing North Equatorial Current in the south; the counterclockwise South Pacific Gyre composed of the southward flowing warm East Australian Current in the west, the eastward flowing South Pacific Current in the south, the northward flowing cold Peru (Humbolt) Current in the east, and the westward flowing South Equatorial Current in the north
surface dominated by two large gyres (broad, circular systems of currents), one in the northern Pacific and another in the southern Pacific; in the northern Pacific, sea ice forms in the Bering Sea and Sea of Okhotsk in winter; in the southern Pacific, sea ice from Antarctica reaches its northernmost extent in October; the ocean floor in the eastern Pacific is dominated by the East Pacific Rise, while the western Pacific is dissected by deep trenches, including the Mariana Trench, which is the world's deepest at 10,924 m major surface currents: clockwise North Pacific Gyre formed by the warm northward flowing Kuroshio Current in the west, the eastward flowing North Pacific Current in the north, the southward flowing cold California Current in the east, and the westward flowing North Equatorial Current in the south; the counterclockwise South Pacific Gyre composed of the southward flowing warm East Australian Current in the west, the eastward flowing South Pacific Current in the south, the northward flowing cold Peru (Humbolt) Current in the east, and the westward flowing South Equatorial Current in the north
- surface dominated by two large gyres (broad, circular systems of currents), one in the northern Pacific and another in the southern Pacific;
- in the northern Pacific, sea ice forms in the Bering Sea and Sea of Okhotsk in winter;
- in the southern Pacific, sea ice from Antarctica reaches its northernmost extent in October;
- the ocean floor in the eastern Pacific is dominated by the East Pacific Rise, while the western Pacific is dissected by deep trenches, including the Mariana Trench, which is the world's deepest at 10,924 m
- major surface currents:
- clockwise North Pacific Gyre formed by the warm northward flowing Kuroshio Current in the west, the eastward flowing North Pacific Current in the north, the southward flowing cold California Current in the east, and the westward flowing North Equatorial Current in the south;
- the counterclockwise South Pacific Gyre composed of the southward flowing warm East Australian Current in the west, the eastward flowing South Pacific Current in the south, the northward flowing cold Peru (Humbolt) Current in the east, and the westward flowing South Equatorial Current in the north
surface dominated by two large gyres (broad, circular systems of currents), one in the northern Pacific and another in the southern Pacific; in the northern Pacific, sea ice forms in the Bering Sea and Sea of Okhotsk in winter; in the southern Pacific, sea ice from Antarctica reaches its northernmost extent in October; the ocean floor in the eastern Pacific is dominated by the East Pacific Rise, while the western Pacific is dissected by deep trenches, including the Mariana Trench, which is the world's deepest at 10,924 m
major surface currents: clockwise North Pacific Gyre formed by the warm northward flowing Kuroshio Current in the west, the eastward flowing North Pacific Current in the north, the southward flowing cold California Current in the east, and the westward flowing North Equatorial Current in the south; the counterclockwise South Pacific Gyre composed of the southward flowing warm East Australian Current in the west, the eastward flowing South Pacific Current in the south, the northward flowing cold Peru (Humbolt) Current in the east, and the westward flowing South Equatorial Current in the north
No edition has those words. Try a shorter word.
Cite this page
Central Intelligence Agency. “Pacific Ocean: Terrain.” The World Factbook, 1990–2021 editions. Archived by The Factbook, thefactbook.org/pacific-ocean/terrain.