La Quinta Formation

http://dbpedia.org/resource/La_Quinta_Formation an entity of type: WikicatMesozoicPaleontologicalSitesOfSouthAmerica

La formación la quinta es un yacimiento fósil del periodo jurásico inferior hace aproximadamente 224 y 196 millones de años en el pasado.​Este yacimiento preserva una de las mayores diversidades fósiles más grandes de Sudamérica, se destaca de las demás formaciones geológicas por tener fósiles enterrados a más de un metro debajo del suelo.​ rdf:langString
The La Quinta Formation is a Jurassic geologic formation which crops out in the Cordillera de Mérida and Serranía del Perijá of western Venezuela and northeastern Colombia. The formation is also present in the subsurface of the Cesar-Ranchería and Maracaibo Basins. At its type locality near La Grita, Táchira, it consists of a basal dacitic tuff followed by interlayered sandstones, tuffs, siltstones and rare limestones. Dinosaur remains including Laquintasaura, Tachiraptor, and Perijasaurus are among the fossils that have been recovered from the formation. rdf:langString
rdf:langString Formación La Quinta
rdf:langString La Quinta Formation
rdf:langString La Quinta Formation
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rdf:langString The La Quinta Formation near its type section in Táchira, Venezuela
rdf:langString Early Jurassic
rdf:langString Cesar-Ranchería & Maracaibo Basins
rdf:langString up to
xsd:string 8.15 -72.02
rdf:langString La formación la quinta es un yacimiento fósil del periodo jurásico inferior hace aproximadamente 224 y 196 millones de años en el pasado.​Este yacimiento preserva una de las mayores diversidades fósiles más grandes de Sudamérica, se destaca de las demás formaciones geológicas por tener fósiles enterrados a más de un metro debajo del suelo.​
rdf:langString The La Quinta Formation is a Jurassic geologic formation which crops out in the Cordillera de Mérida and Serranía del Perijá of western Venezuela and northeastern Colombia. The formation is also present in the subsurface of the Cesar-Ranchería and Maracaibo Basins. At its type locality near La Grita, Táchira, it consists of a basal dacitic tuff followed by interlayered sandstones, tuffs, siltstones and rare limestones. Dinosaur remains including Laquintasaura, Tachiraptor, and Perijasaurus are among the fossils that have been recovered from the formation. U–Pb zircon analysis demonstrates that the formation dates to 200.91+0.55 Ma at its base and a maximum age of 174.8 Ma.
rdf:langString La Quinta quarry
xsd:nonNegativeInteger 7661
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