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About: Timor Trough

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

The Timor Trough is an oceanic trough that is a continuation of the Sunda Trench (Java Trench) that marks the boundary between the Indo-Australian Plate and the Timor Plate. It is separated from the Sunda Trench by a sag near Sumba Island at the and the , and on the other end becomes the Tanimbar Trough southeast of the Tanimbar Islands, continuing on to the Aru Trough east of the Kai Islands near the Bird's Head Peninsula on New Guinea. Lining the north of the trough are numerous islands, of which Timor is the largest. Further west are the and the . Oil and natural gas have been found in the Bonaparte Basin south of the trough and the region is geologically active with numerous earthquakes.

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dbo:abstract
  • Der Timorgraben ist eine bis 3310 m tiefe Tiefseerinne im äußersten Nordosten des Indischen Ozeans. (de)
  • The Timor Trough is an oceanic trough that is a continuation of the Sunda Trench (Java Trench) that marks the boundary between the Indo-Australian Plate and the Timor Plate. It is separated from the Sunda Trench by a sag near Sumba Island at the and the , and on the other end becomes the Tanimbar Trough southeast of the Tanimbar Islands, continuing on to the Aru Trough east of the Kai Islands near the Bird's Head Peninsula on New Guinea. Lining the north of the trough are numerous islands, of which Timor is the largest. Further west are the and the . Oil and natural gas have been found in the Bonaparte Basin south of the trough and the region is geologically active with numerous earthquakes. (en)
  • De Timortrog is een 3300 m diepe diepzeekloof in het uiterste noordoosten van de Indische Oceaan: de Timorzee. Zij bevindt zich tussen Timor in het noorden, de Tanimbar-eilanden in het noordoosten, de Arafurazee in het oosten, de eigenlijke Timorzee in het zuiden en het Roti-eiland in het westen. De Timortrog is ontstaan door platentektoniek: het is een deel van het subductiegebied tussen de Euraziatische plaat en de Australische plaat waarbij deze laatste onder de eerste schuift. (nl)
  • Rów Timorski znajduje się na morzu Timor. Ma głębokość 3310 m. Temperatura wód powierzchniowych wynosi 23-29 °C. Zasolenie waha się w granicach 34,5-34,7‰. (pl)
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  • Der Timorgraben ist eine bis 3310 m tiefe Tiefseerinne im äußersten Nordosten des Indischen Ozeans. (de)
  • The Timor Trough is an oceanic trough that is a continuation of the Sunda Trench (Java Trench) that marks the boundary between the Indo-Australian Plate and the Timor Plate. It is separated from the Sunda Trench by a sag near Sumba Island at the and the , and on the other end becomes the Tanimbar Trough southeast of the Tanimbar Islands, continuing on to the Aru Trough east of the Kai Islands near the Bird's Head Peninsula on New Guinea. Lining the north of the trough are numerous islands, of which Timor is the largest. Further west are the and the . Oil and natural gas have been found in the Bonaparte Basin south of the trough and the region is geologically active with numerous earthquakes. (en)
  • De Timortrog is een 3300 m diepe diepzeekloof in het uiterste noordoosten van de Indische Oceaan: de Timorzee. Zij bevindt zich tussen Timor in het noorden, de Tanimbar-eilanden in het noordoosten, de Arafurazee in het oosten, de eigenlijke Timorzee in het zuiden en het Roti-eiland in het westen. De Timortrog is ontstaan door platentektoniek: het is een deel van het subductiegebied tussen de Euraziatische plaat en de Australische plaat waarbij deze laatste onder de eerste schuift. (nl)
  • Rów Timorski znajduje się na morzu Timor. Ma głębokość 3310 m. Temperatura wód powierzchniowych wynosi 23-29 °C. Zasolenie waha się w granicach 34,5-34,7‰. (pl)
rdfs:label
  • Timorgraben (de)
  • Timortrog (nl)
  • Rów Timorski (pl)
  • Timor Trough (en)
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