Kilikas Sea: Difference between revisions

From IxWiki
Jump to navigation Jump to search
m 1 revision imported: IXWB Import - Take 1
mNo edit summary
Tag: 2017 source edit
 
(8 intermediate revisions by 4 users not shown)
Line 10: Line 10:
| outflow            = [[Coscivian Sea]]
| outflow            = [[Coscivian Sea]]
| catchment          =
| catchment          =
| basin_countries    = [[Burgundie]], [[Cartadania]], [[Kiravia]], [[Kuhlfros]]
| basin_countries    = [[Burgundie]], [[Cartadania]], [[Kiravia]], [[Fiannria]]
| length            =  
| length            =  
| width              =
| width              =
Line 21: Line 21:
| elevation          =
| elevation          =
| frozen            =
| frozen            =
| islands            = [[Islas Nubes]], [[Isle of Burgundie|Burgundie]], [[Meridia]], [[Wintergen]]
| islands            = [[Islas Nubes]], [[Koskenkorva]], [[Wintergen]], [[Scapa]]
| cities            = [[Category:Kilikas Cities]]
| cities            =  
{{flag|Faneria}}
* Myshall
* Dunmach
* Farranfore
* Dunderrow
* Banagher
* Port na Habhainnsk
* Lansgadh
* Glenhest
* Aberavon
| reference          =
| reference          =
}}
}}
Line 28: Line 38:
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 [[Burgundie]], [[Kirav]], and the origins of globalization.
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]], [[Kuhlfros]].
The countries with coastlines on the Kilikas Sea are [[Burgundie]], [[Kiravia]], [[Fiannria]].


==Name==
==Name==
==History==
==History==
===Ancient civilisations===
===Ancient civilisations===
Lezevish (Basques), Impaxi (Picts), Prythonic Gaels, Brytonic Gaels, Finnics
Pretannic Celts, ???


Later civilizations
Later civilizations
[[Bergendii]], Kiravian Coscivians
[[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]]
*[[Kuhlfros]]
*[[Fiannria]]
*[[Meridia]], [[Kirav]]
*[[Koskenkorva]], [[Kiravia]]


===Coastal cities===
===Coastal cities===
*[[Bekshavn]]
*[[Hivernille]], [[Wintergen]], {{flag|Burgundie}}
*[[Dorft]]
*[[Granblaix]]
*[[Le Ax-Canbon]]
*[[NordHalle]]
*[[Vilauristre]]
*[[Cities of Kiravia#Valkadun|Valkadun]]
*[[Cities of Kiravia#Valkadun|Valkadun]]


===Subdivisions===
===Subdivisions===
*Strait of Burgundie
 
*Feradach Channel
====Other seas====
====Other seas====
====Other features====
====Other features====


===10 largest islands by area===
===10 largest islands by area===
*[[Meridia]], [[Kirav]]
*[[Koskenkorva]], [[Kiravia]]
*[[Isle of Burgundie]], [[Burgundie]]
*[[Wintergen]], [[Burgundie]]
*[[Wintergen]], [[Burgundie]]
*[[Islas Nubes]], [[Cartadania]]
*[[Islas Nubes]], [[Cartadania]]
Line 109: Line 112:
==Gallery==
==Gallery==
==See also==
==See also==
[[Category:Kuhlfros]]
[[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
TypeSea
Primary inflowsLevantine Ocean
Primary outflowsCoscivian Sea
Basin countriesBurgundie, Cartadania, Kiravia, Fiannria
Surface area7,247,823 km2 (2,798,400 sq mi)
Average depth1,054 m (3,458 ft)
Max. depth6,357 m (20,856 ft)
Water volume7,610,214 km3 (1,825,787 cu mi)
IslandsIslas Nubes, Koskenkorva, Wintergen, Scapa
Settlements Faneria
  • Myshall
  • Dunmach
  • Farranfore
  • Dunderrow
  • Banagher
  • Port na Habhainnsk
  • Lansgadh
  • Glenhest
  • Aberavon

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

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

Navigational Aides

Lighthouses
Weather Radar
AIS
Other

Tourism

Fishing

Overfishing

Aquaculture

Gallery

See also