An Entity of Type: military unit, from Named Graph: http://dbpedia.org, within Data Space: dbpedia.org

The Great Escarpment in Brazil is a major geological formation that runs along much of the eastern coast of Brazil south of the city of Salvador. The escarpment runs along the central and south Atlantic coasts of Brazil, rising sharply and separating the highland plateau from the coast.

Property Value
dbo:abstract
  • The Great Escarpment in Brazil is a major geological formation that runs along much of the eastern coast of Brazil south of the city of Salvador. The escarpment runs along the central and south Atlantic coasts of Brazil, rising sharply and separating the highland plateau from the coast. The escarpment rises steeply from the coastal plain to as much as 9,000 feet (2,700 m) in height.The top of the escarpment forms a drainage divide between the interior and the coastal plains.Apart from the São Francisco River, most streams flow into the central basin rather than to the coast.The escarpment defines the eastern edge of the Serra do Mar and other mountain ranges. (en)
  • ブラジル大断崖(ブラジルだいだんがい、英語: Great Escarpment, Brazil)は、ブラジルのバイーア州サルヴァドールの南にあるブラジルの東海岸の大部分に沿って南下する主要な断崖である。この断崖はブラジルの中央および南大西洋岸に沿って走り、急上昇し、ブラジル高原を海岸から分離している。 ブラジル大断崖は海岸平野から高さ2,700メートルまで急上昇する。断崖の上部は、内部と海岸平野の間に分水界を形成する。サンフランシスコ川を除いて、ほとんどの川は海岸ではなく中央流域に流れ込んでいる。この大断崖はセーハ・ド・マール山脈と他の山脈の東端になっている。 (ja)
  • La Grande scarpata del Brasile è la più grande formazione geologica che corre lungo gran parte della costa orientale del Brasile a sud della città di Salvador di Bahia.Corre lungo la costa centrale e meridionale dell'oceano Atlantico, in forte pendenza, separando l'altopiano dalla costa. La scarpata sale ripida dalla pianura costiera fino ai 2 700 metri s.l.m. dell'altopiano.La parte superiore della scarpata forma uno spartiacque tra l'interno e le pianure costiere.Ad eccezione del São Francisco, gran parte dei fiumi drenano nel bacino centrale invece che sulla costa.La scarpata definisce il bordo orientale della Serra do Mar e di altre catene montuose. (it)
dbo:thumbnail
dbo:wikiPageExternalLink
dbo:wikiPageID
  • 37798062 (xsd:integer)
dbo:wikiPageLength
  • 2321 (xsd:nonNegativeInteger)
dbo:wikiPageRevisionID
  • 1056064095 (xsd:integer)
dbo:wikiPageWikiLink
dbp:wikiPageUsesTemplate
dcterms:subject
gold:hypernym
rdf:type
rdfs:comment
  • ブラジル大断崖(ブラジルだいだんがい、英語: Great Escarpment, Brazil)は、ブラジルのバイーア州サルヴァドールの南にあるブラジルの東海岸の大部分に沿って南下する主要な断崖である。この断崖はブラジルの中央および南大西洋岸に沿って走り、急上昇し、ブラジル高原を海岸から分離している。 ブラジル大断崖は海岸平野から高さ2,700メートルまで急上昇する。断崖の上部は、内部と海岸平野の間に分水界を形成する。サンフランシスコ川を除いて、ほとんどの川は海岸ではなく中央流域に流れ込んでいる。この大断崖はセーハ・ド・マール山脈と他の山脈の東端になっている。 (ja)
  • The Great Escarpment in Brazil is a major geological formation that runs along much of the eastern coast of Brazil south of the city of Salvador. The escarpment runs along the central and south Atlantic coasts of Brazil, rising sharply and separating the highland plateau from the coast. (en)
  • La Grande scarpata del Brasile è la più grande formazione geologica che corre lungo gran parte della costa orientale del Brasile a sud della città di Salvador di Bahia.Corre lungo la costa centrale e meridionale dell'oceano Atlantico, in forte pendenza, separando l'altopiano dalla costa. (it)
rdfs:label
  • Great Escarpment, Brazil (en)
  • Grande scarpata (Brasile) (it)
  • ブラジル大断崖 (ja)
owl:sameAs
prov:wasDerivedFrom
foaf:depiction
foaf:isPrimaryTopicOf
is dbo:wikiPageDisambiguates of
is dbo:wikiPageWikiLink of
is foaf:primaryTopic of
Powered by OpenLink Virtuoso    This material is Open Knowledge     W3C Semantic Web Technology     This material is Open Knowledge    Valid XHTML + RDFa
This content was extracted from Wikipedia and is licensed under the Creative Commons Attribution-ShareAlike 3.0 Unported License