Ware Formation | |
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Stratigraphic range: Late Miocene-Early Pleistocene, typically Pliocene ~ | |
Type | Geological formation |
Unit of | Cocinetas Basin |
Underlies | Alluvium |
Overlies | Castilletes Formation |
Thickness | up to 25 m (82 ft) |
Lithology | |
Primary | Sandstone, mudstone |
Other | Conglomerate |
Location | |
Coordinates | 11°51′4.32″N 71°19′26.4″W / 11.8512000°N 71.324000°W |
Approximate paleocoordinates | 11°42′N 70°48′W / 11.7°N 70.8°W |
Region | La Guajira Caribbean region |
Country | Colombia |
Type section | |
Named for | Wayuunaiki: "friend" |
Named by | Moreno et al. |
Location | Uribia |
Year defined | 2015 |
Coordinates | 11°51′4.32″N 71°19′26.4″W / 11.8512000°N 71.324000°W |
Region | La Guajira |
Country | Colombia |
Type locality of the formation in La Guajira |
The Ware Formation (Spanish: Formación Ware) is a fossiliferous geological formation of the Cocinetas Basin in the northernmost department of La Guajira. The formation consists of fine lithic to quartzitic sandstones, mudstones, pebbly conglomerates with sedimentary and metamorphic rock fragments, fossiliferous packstones and sandy to conglomeratic beds with high fossil content. The Ware Formation dates to the Neogene and Quaternary periods; Late Miocene to Early Pleistocene epochs, typically Pliocene (3.5 to 2.8 Ma), Uquian, Chapadmalalan and Montehermosan in the SALMA classification, and has a maximum thickness of 25 metres (82 ft).