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The Itombe Formation is a geological formation of the Kwanza Basin in Angola dated to the Coniacian stage of the Late Cretaceous. The environment of deposition is shallow marine. Reptile fossils have been recovered from the Tadi beds locality within the formation, including the dinosaur Angolatitan, the mosasaurs Angolasaurus and Mosasaurus iembeensis and the turtle Angolachelys.The Itombe formation was formerly considered Turonian in age, but new data suggests to be Coniacian.

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rdf:type
rdfs:label
  • Itombe Formation (en)
rdfs:comment
  • The Itombe Formation is a geological formation of the Kwanza Basin in Angola dated to the Coniacian stage of the Late Cretaceous. The environment of deposition is shallow marine. Reptile fossils have been recovered from the Tadi beds locality within the formation, including the dinosaur Angolatitan, the mosasaurs Angolasaurus and Mosasaurus iembeensis and the turtle Angolachelys.The Itombe formation was formerly considered Turonian in age, but new data suggests to be Coniacian. (en)
name
  • Itombe Formation (en)
geo:lat
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Wikipage page ID
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Link from a Wikipage to another Wikipage
sameAs
subunits
  • Tadi Beds (en)
underlies
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country
  • Angola (en)
period
  • Coniacian (en)
region
Thickness
  • up to (en)
type
georss:point
  • -8.2 13.2
has abstract
  • The Itombe Formation is a geological formation of the Kwanza Basin in Angola dated to the Coniacian stage of the Late Cretaceous. The environment of deposition is shallow marine. Reptile fossils have been recovered from the Tadi beds locality within the formation, including the dinosaur Angolatitan, the mosasaurs Angolasaurus and Mosasaurus iembeensis and the turtle Angolachelys.The Itombe formation was formerly considered Turonian in age, but new data suggests to be Coniacian. (en)
extent
otherlithology
overlies
  • Cabo Ledo & Massangano Formations (en)
prilithology
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page length (characters) of wiki page
foaf:isPrimaryTopicOf
geo:geometry
  • POINT(13.199999809265 -8.1999998092651)
is Link from a Wikipage to another Wikipage of
is Wikipage redirect of
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