The Densuș-Ciula Formation is a geological formation in Romania whose strata date back to the Late Cretaceous. It forms part of the Hațeg Island assemblage. Dinosaur remains are among the fossils that have been recovered from the formation. It is divided up into three members, the lower member is noted for high content of volcanogenic material and is poorly fossiliferous. While the Middle member consists of silty mudstones, sandstones and conglomerates containing volcanogenic clasts and is richly fossiliferous, while the upper member consists of matrix supported red conglomerates and is poorly fossiliferous.
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| - Formación Densus Ciula (es)
- Densuș-Ciula Formation (en)
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| - La Formación Densus Ciula es una formación geológica en Rumania que corresponde al período Cretácico Superior. Los restos de dinosaurios se encuentran entre los fósiles que se han recuperado de la formación. (es)
- The Densuș-Ciula Formation is a geological formation in Romania whose strata date back to the Late Cretaceous. It forms part of the Hațeg Island assemblage. Dinosaur remains are among the fossils that have been recovered from the formation. It is divided up into three members, the lower member is noted for high content of volcanogenic material and is poorly fossiliferous. While the Middle member consists of silty mudstones, sandstones and conglomerates containing volcanogenic clasts and is richly fossiliferous, while the upper member consists of matrix supported red conglomerates and is poorly fossiliferous. (en)
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| - Densuş-Ciula Formation (en)
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| - Lower, Middle and Upper Members (en)
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| - La Formación Densus Ciula es una formación geológica en Rumania que corresponde al período Cretácico Superior. Los restos de dinosaurios se encuentran entre los fósiles que se han recuperado de la formación. (es)
- The Densuș-Ciula Formation is a geological formation in Romania whose strata date back to the Late Cretaceous. It forms part of the Hațeg Island assemblage. Dinosaur remains are among the fossils that have been recovered from the formation. It is divided up into three members, the lower member is noted for high content of volcanogenic material and is poorly fossiliferous. While the Middle member consists of silty mudstones, sandstones and conglomerates containing volcanogenic clasts and is richly fossiliferous, while the upper member consists of matrix supported red conglomerates and is poorly fossiliferous. (en)
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| - Northwest Hațeg Basin (en)
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