Cordilian Sea (Pacifica)
| Cordilian Sea | |
|---|---|
 | |
| Surface area | 30,630,000 km2 (11,830,000 sq mi) |
| Average depth | 3,260 m (10,700 ft) |
| Max. depth | 6,540 m (21,460 ft) |
| Water volume | 200,320,200 km3 (48,059,400 cu mi) |
| Islands | List of islands |
| Settlements |
|
The Cordilian Sea stretches from the North Pacific Ocean in the north to the Southern Ocean in the south, and washes the shores of Cordilia to the east and the island continent to the west.
It encompasses 30,630,000 km2 (11,830,000 sq mi) in area, and covers about 6% of the total area of Pacifica. The Cordilian Sea splits into two regions with different and independent ocean currents at the equator due to the Coriolis Effect. It splits into the North Cordilian Sea and the South Cordilian Sea, this last one taking most of the area of the Cordilian Sea and being the main current in the occidental shore of Cordilia.
Its average depth is around of 3,300 m (10,800 ft). The Deep in the West Continent Trench, located west of Kosbareland, is the deepest point of the Cordilian Sea.
The Cordilian Sea has some marginal seas within it, including but not limited to the Sea of Frost, the Serevan Sea and the Astro Sea.
Etymology
Since ancient times, the Cordilian Sea has been navigated by diverse civilizations from all places. The name of Cordilian Sea was coined due to being the major sea at the west coasts of the Cordilia continent. Although the population of Viliakmon reclaims that the body of water is an ocean, due to their long history in relation with the body of water and great attachment to it.
Geography
The Cordilian Sea separates Cordilia from the West Pacific. It may be further subdivided by the equator into northern (North Cordilian) and southern (South Cordilian) portions. It extends from the Antarctic region in the South to the North Pacific Ocean in the north. The Cordilian Sea encompasses approximately 6% of Pacifica's surface, having an area of 30,630,000 km2 (11,830,000 sq mi)— larger than Cordilia itself.
Extending approximately 9,615 km (5,974 mi) from the West Pacific Island Chain in the north to the northern extent of the circumpolar Southern Ocean at 60°S, the Pacific reaches its greatest east–west width at about 3.5°N latitude. There it stretches approximately 5,075 km (3,153 mi) from the West Pacific Island Chain to the coast of Rock Island, TSSS. Its geographic center is at 15°S, 55.5°W. The lowest known point on the Cordilian Sea—The Deep—lies 6,540 m (21,460 ft; 3,580 fathoms) below sea level. Its average depth is 3,260 m (10,700 ft; 1,780 fathoms), putting the total water volume at roughly 200,320,200 km3 (48,059,400 cu mi).
The Gulf of Good Omen joins the Cordilian Sea, the Transcrabrian Sea and the South Pacific Ocean to the east, the Frost Sea links the Cordilian Sea with the North Pacific Ocean on the north. To the south, the Cordilian Sea connects directly to the Antarctic Ocean at latitude 60°S.
Bordering nations
Landmasses and islands
All the islands in the Cordilian Sea are islands that limit it or continental islands. There are about 85 islands in the Cordilian Sea.
Islands in the Cordilian Sea are of four basic types: continental islands and high islands. Continental islands lie outside the andesite line and include Kaly Theá, the many islands of Techganet, the island chains of Kosbareland and Qaweritoyu, and others. All of these islands are structurally associated with nearby continents. High islands are of volcanic origin, and many contain active volcanoes. Among these are Snolland, Bruuma, and others.
Water characteristics
The volume of the Cordilian Sea has been estimated at some 200,000,000 cubic kilometres (48,000,000 cubic miles). Surface water temperatures in the Cordilian Sea can vary from 10 °C (50 °F), in the southern borders with the Antarctic Ocean, to about 30 °C (86 °F) near the equator. Salinity also varies latitudinally, reaching a maximum of 37 parts per thousand in the southern 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 south, as less evaporation of seawater takes place in these frigid areas. The motion of Cordilian waters is generally clockwise in the Northern Hemisphere and counter-clockwise in the Southern Hemisphere.