Kilikas Sea: Difference between revisions
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| elevation = | | elevation = | ||
| frozen = | | frozen = | ||
| islands = [[Islas Nubes]], [[ | | islands = [[Islas Nubes]], [[Koskenkorva]], [[Wintergen]], [[Scapa]] | ||
| cities = | | cities = | ||
{{flag|Faneria}} | |||
* Myshall | |||
* Dunmach | |||
* Farranfore | |||
* Dunderrow | |||
* Banagher | |||
* Port na Habhainnsk | |||
* Lansgadh | |||
* Glenhest | |||
* Aberavon | |||
| reference = | | reference = | ||
}} | }} | ||
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The '''Kilikas Sea''' is a {{wp|sea}} surrounded by the [[Kilikas_Sea#Extent|Kilikas Basin]] and is pass-through for waters from the [[Levantine Ocean]] to the [[Coscivian Sea]], and then onto the [[Sea of Odoneru]]. The sea is bound by the Arctic in the north and [[Levantia]] in the south. The northern 40% of the sea freezes over from January to March. This much colder water, moving southward, conflicting with the warmer winds moving up the western [[Levantia|Levantine]] coast from the equator in the southern [[Sea of Odoneru]] have caused a phenomenon known as the Kilikas Storm Belt, which encompasses the southwestern quadrant of the sea, particularly in the transitional waters of the Kilikas into the [[Coscivian Sea]]. | The '''Kilikas Sea''' is a {{wp|sea}} surrounded by the [[Kilikas_Sea#Extent|Kilikas Basin]] and is pass-through for waters from the [[Levantine Ocean]] to the [[Coscivian Sea]], and then onto the [[Sea of Odoneru]]. The sea is bound by the Arctic in the north and [[Levantia]] in the south. The northern 40% of the sea freezes over from January to March. This much colder water, moving southward, conflicting with the warmer winds moving up the western [[Levantia|Levantine]] coast from the equator in the southern [[Sea of Odoneru]] have caused a phenomenon known as the Kilikas Storm Belt, which encompasses the southwestern quadrant of the sea, particularly in the transitional waters of the Kilikas into the [[Coscivian Sea]]. | ||
The Kilikas Sea has an average depth of {{convert|1054|m|ft|abbr=on}} and the deepest recorded point is {{convert|6357|m|ft|abbr=on}} about 650 nm due east of [[Wintergen]], known as the Phistual Trench. Because of the Kilikas Storm Belt, the sea has only become an important route for merchants and travelers of in the last few centuries, following the development of safer maritime modes of transport. This has led to the development of slightly isolated cultures, like the [[Bergendii]] who otherwise would have been part of a larger Latinic civilization. The [[Kilikas_Sea#History|history of the Kilikas region]] is crucial to understanding the origins and development of | The Kilikas Sea has an average depth of {{convert|1054|m|ft|abbr=on}} and the deepest recorded point is {{convert|6357|m|ft|abbr=on}} about 650 nm due east of [[Wintergen]], known as the Phistual Trench. Because of the Kilikas Storm Belt, the sea has only become an important route for merchants and travelers of in the last few centuries, following the development of safer maritime modes of transport. This has led to the development of slightly isolated cultures, like the [[Bergendii]] who otherwise would have been part of a larger Latinic civilization. The [[Kilikas_Sea#History|history of the Kilikas region]] is crucial to understanding the origins and development of [[Kiravia]], and the origins of globalization. | ||
The countries with coastlines on the Kilikas Sea are [[Burgundie]], [[Kiravia]], [[Fiannria]]. | The countries with coastlines on the Kilikas Sea are [[Burgundie]], [[Kiravia]], [[Fiannria]]. | ||
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==History== | ==History== | ||
===Ancient civilisations=== | ===Ancient civilisations=== | ||
Pretannic Celts, ??? | |||
Later civilizations | Later civilizations | ||
[[Bergendii]], | [[Bergendii]], [[Coscivians]] | ||
===Middle Ages and empires=== | ===Middle Ages and empires=== | ||
| Line 46: | Line 56: | ||
===Oceanography=== | ===Oceanography=== | ||
===Coastal countries=== | ===Coastal countries=== | ||
*[[Burgundie]] | *[[Wintergen]], [[Burgundie]] | ||
*[[Islas Nubes]], [[Cartadania]] | *[[Islas Nubes]], [[Cartadania]] | ||
*[[Fiannria]] | *[[Fiannria]] | ||
*[[ | *[[Koskenkorva]], [[Kiravia]] | ||
===Coastal cities=== | ===Coastal cities=== | ||
*[[ | *[[Hivernille]], [[Wintergen]], {{flag|Burgundie}} | ||
*[[Cities of Kiravia#Valkadun|Valkadun]] | *[[Cities of Kiravia#Valkadun|Valkadun]] | ||
===Subdivisions=== | ===Subdivisions=== | ||
====Other seas==== | ====Other seas==== | ||
====Other features==== | ====Other features==== | ||
===10 largest islands by area=== | ===10 largest islands by area=== | ||
*[[ | *[[Koskenkorva]], [[Kiravia]] | ||
*[[Wintergen]], [[Burgundie]] | *[[Wintergen]], [[Burgundie]] | ||
*[[Islas Nubes]], [[Cartadania]] | *[[Islas Nubes]], [[Cartadania]] | ||
| Line 109: | Line 112: | ||
==Gallery== | ==Gallery== | ||
==See also== | ==See also== | ||
[[Category: | [[Category:Fiannria]] | ||
[[Category:KRV]] | [[Category:KRV]] | ||
[[Category:Geography]] | [[Category:Geography]] | ||
[[Category:Bodies of water]] | |||
Latest revision as of 21:04, 24 March 2023
| Kilikas Sea | |
|---|---|
| File:Map highlighting the Kilikas Sea Map of the Kilikas Sea | |
| Type | Sea |
| Primary inflows | Levantine Ocean |
| Primary outflows | Coscivian Sea |
| Basin countries | Burgundie, Cartadania, Kiravia, Fiannria |
| Surface area | 7,247,823 km2 (2,798,400 sq mi) |
| Average depth | 1,054 m (3,458 ft) |
| Max. depth | 6,357 m (20,856 ft) |
| Water volume | 7,610,214 km3 (1,825,787 cu mi) |
| Islands | Islas Nubes, Koskenkorva, Wintergen, Scapa |
| Settlements |  Faneria
|
The Kilikas Sea is a sea surrounded by the Kilikas Basin and is pass-through for waters from the Levantine Ocean to the Coscivian Sea, and then onto the Sea of Odoneru. The sea is bound by the Arctic in the north and Levantia in the south. The northern 40% of the sea freezes over from January to March. This much colder water, moving southward, conflicting with the warmer winds moving up the western Levantine coast from the equator in the southern Sea of Odoneru have caused a phenomenon known as the Kilikas Storm Belt, which encompasses the southwestern quadrant of the sea, particularly in the transitional waters of the Kilikas into the Coscivian Sea.
The Kilikas Sea has an average depth of 1,054 m (3,458 ft) and the deepest recorded point is 6,357 m (20,856 ft) about 650 nm due east of Wintergen, known as the Phistual Trench. Because of the Kilikas Storm Belt, the sea has only become an important route for merchants and travelers of in the last few centuries, following the development of safer maritime modes of transport. This has led to the development of slightly isolated cultures, like the Bergendii who otherwise would have been part of a larger Latinic civilization. The history of the Kilikas region is crucial to understanding the origins and development of Kiravia, and the origins of globalization.
The countries with coastlines on the Kilikas Sea are Burgundie, Kiravia, Fiannria.
Name
History
Ancient civilisations
Pretannic Celts, ???
Later civilizations Bergendii, Coscivians
Middle Ages and empires
21st century and migrations
Geography
Extent
Oceanography
Coastal countries
Coastal cities
Subdivisions
Other seas
Other features
10 largest islands by area
- Koskenkorva, Kiravia
- Wintergen, Burgundie
- Islas Nubes, Cartadania
- Kuhls islands TBD
Climate
Sea temperature
Geology
Tectonics and paleoenvironmental analysis
Desiccation and exchanges of flora and fauna
Paleoclimate
Ecology and biota
Environmental history
Natural hazards
Kilikas Storm Belt
Biodiversity
Invasive species
- Basques
Arrival of new tropical species
Sea-level rise
Pollution
Shipping
Lighthouses
Weather Radar
AIS
Other
Tourism
Fishing
Overfishing
Aquaculture
Gallery
See also
Categories:
- Pages using duplicate arguments in template calls
- Pages with broken file links
- Articles using infobox body of water without alt
- Articles using infobox body of water without coordinates
- Articles using infobox body of water without pushpin map
- Articles using infobox body of water without image bathymetry
- Fiannria
- KRV
- Geography
- Bodies of water