About: Tevaria   Sponge Permalink

An Entity of Type : dbkwik:resource/rs6aU8n6HOYGNXs2Pg7kzA==, within Data Space : 134.155.108.49:8890 associated with source dataset(s)

Tevaria is the smallest of the traditional eight continents in the English conception. The continent lies on a continental shelf overlain by shallow seas which divide the mainland from the various smaller islands making up the greater continent. When sea levels were lower during the Last Glacial Maximum, the entirety of the continent was connected by dry land. Over the past ten thousand years, sea levels have risen, separating the mainland from the various outlying areas of high elevation which would eventually become large islands.

AttributesValues
rdf:type
rdfs:label
  • Tevaria
rdfs:comment
  • Tevaria is the smallest of the traditional eight continents in the English conception. The continent lies on a continental shelf overlain by shallow seas which divide the mainland from the various smaller islands making up the greater continent. When sea levels were lower during the Last Glacial Maximum, the entirety of the continent was connected by dry land. Over the past ten thousand years, sea levels have risen, separating the mainland from the various outlying areas of high elevation which would eventually become large islands.
dcterms:subject
dbkwik:conworld/pr...iPageUsesTemplate
Cities
Population
  • 108168000(xsd:integer)
Title
  • Tevaria
Area
  • 2940132(xsd:double)
Demonym
  • Tevarian
GDP nominal
  • 6.13E12
GDP PPP
  • 5.898E12
Time
  • UTC +4, +5, +6
Density
  • 36(xsd:double)
abstract
  • Tevaria is the smallest of the traditional eight continents in the English conception. The continent lies on a continental shelf overlain by shallow seas which divide the mainland from the various smaller islands making up the greater continent. When sea levels were lower during the Last Glacial Maximum, the entirety of the continent was connected by dry land. Over the past ten thousand years, sea levels have risen, separating the mainland from the various outlying areas of high elevation which would eventually become large islands. The continent was formed by the Tevarian tectonic plate, which broke off from the Antarctic plate during the separation of Gondwana some 200 million years ago. The continent gradually expanded through intense volcanic activity, reaching its present size around 2 million years ago. Much of the biota of the continent is resultant of separation from India with influences from Africa and Australia, but the comparatively temperate climate of Tevene has led to distinct endemic developments on the continent. Humans have not lived on the continent until modern times, when humanity was introduced through colonisation following the discovery of the continent by the Portuguese in 1514. Following its discovery, it was explored and settled by Venice, France, and England. Each of the four contemporary countries are the result of a mixture of older groups of settlers, with Lindarens being descendants of the Austrians, Antesians being descendants of the French and the Venetians, Duchers being descendants of the Austrians, the French, and the English, and Frathensiens beings descendants of the English.
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