Übersetzung für 'Deccan Traps' von Englisch nach Deutsch
NOUN   - | the Deccan Traps
Deccan Traps {pl}
Dekkan-Trapp {m}
Deccan (crested) lark [Galerida deva]
Devalerche / Deva-Lerche {f}
Deccan rock bush quail [Perdicula argoondah]
Madraswachtel {f}
trapsFallen {pl}
to avoid trapsFallen aus dem Wege gehen
wave trapsSperrkreise {pl}
to set trapsFallen aufstellen
sb./sth. trapsjd./etw. fängt
traps {pl} [belongings­, luggage]Gepäck {n}
sb./sth. trapsjd./etw. fängt ein
Shut your traps! [coll.]
Haltet die Klappe! [ugs.]
until sb./sth. trapsbis jd./etw. einfängt
traps [coll.] [short for: trapezius]
Trapezmuskeln {pl}
tendelle traps [bird-trap hunting]Quetschfallen {pl}
tendelle traps [bird-trap hunting]Steinquetschfallen {pl}
deccan grass [Echinochloa colonum] [error: Echinochloa colona]
Schmale Igelhirse {f}
16 Übersetzungen
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Anwendungsbeispiele Englisch
  • Fossil wood is known from the Deccan Traps of India some 66 million years ago.
  • Part of it is overlaid with alluvium, and in the west it is overlaid with the igneous rocks of the Deccan Traps.
  • The Deccan Traps is a large igneous province of west-central India (17–24°N, 73–74°E). It is one of the largest volcanic features on Earth, taking the form of a large shield volcano.
  • At the time of the K-Pg extinction, the Deccan Traps flood basalts of India were actively erupting.
  • Among these works was the osteological description of "Oxyglossus pusillus", a fossil frog from the Deccan Traps of Bombay.

  • The plateau is an extension of the Deccan Traps, formed between 60 and 68 million years ago at the end of the Cretaceous period.
  • Large basaltic rock formations exists throughout Vidarbha, part of the 66-million-year-old volcanic Deccan Traps.
  • Ellora occupies a relatively flat rocky region of the Western Ghats, where ancient volcanic activity had created multilayered basalt formations, known as the Deccan Traps.
  • For example, the release of volcanic gases (particularly sulfur dioxide) during the formation of the Deccan Traps in India.
  • The Mesozoic Deccan Traps formation is seen over most of the northern Deccan; they are believed to be the result of sub-aerial volcanic activity.

  • The Réunion hotspot (active 70–40 million years ago) connects Réunion and the Mascarene Plateau to the Chagos-Laccadive Ridge and the Deccan Traps in north-western India; the Kerguelen hotspot (100–35 million years ago) connects the Kerguelen Islands and Kerguelen Plateau to the Ninety East Ridge and the Rajmahal Traps in north-eastern India; the Marion hotspot (100–70 million years ago) possibly connects Prince Edward Islands to the Eighty Five East Ridge.
  • If the Deccan Traps were the location of a verneshot event at the Cretaceous–Paleogene boundary, the strong iridium spike at the Cretaceous–Paleogene boundary could be explained by the iridium-rich nature of volatiles in the Reunion mantle plume, which is currently beneath Piton de la Fournaise, but during the end Cretaceous was located beneath India in the area of the Deccan Traps; the verneshot event could potentially distribute the iridium globally.
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