| Barzalosa Formation | |
| Period: | Oligocene |
| Age: | ~Mid Eocene-Oligocene or Oligocene-Early Miocene ~ |
| Type: | Geological formation |
| Prilithology: | Conglomerates |
| Otherlithology: | Sandstones, siltstones, shale, gypsum |
| Underlies: | Honda Gp., Carmen de Apicalá Conglomerate |
| Overlies: | La Tabla Fm., Olini Gp., Seca Fm. |
| Thickness: | ~360m (1,180feet) |
| Map: | Blakey 035Ma - COL.jpg |
| Coordinates: | 4.3639°N -74.7916°W |
| Paleocoordinates: | 2.7°N -71.2°W |
| Region: | Upper Magdalena Valley Central & Eastern Ranges Andes |
| Namedfor: | Barzalosa |
| Namedby: | Scheibe |
| Year Ts: | 1934 |
| Location Ts: | Girardot |
| Coordinates Ts: | 4.3639°N -74.7916°W |
| Region Ts: | Cundinamarca |
The Barzalosa Formation (Spanish; Castilian: Formación Barzalosa, Pgb, Pgba) is a fossiliferous geological formation of the Upper Magdalena Valley and the bounding foothills of the Central Ranges and Eastern Ranges of the Colombian Andes. The formation consists of conglomerates, sandstones and siltstones. The Barzalosa Formation probably dates to the Late Paleogene to Early Neogene period; Oligocene to Early Miocene epochs, and has an approximate thickness of 360m (1,180feet). Fossils of Balanerodus logimus, Lophiodolodus chaparralensis, Xenastrapotherium chaparralensis, Protheosodon sp. and Proadinotherium sp. have been uncovered from the formation in Chaparral, Tolima.
The formation was defined by Scheibe in 1934 and named after Barzalosa, a vereda of Girardot, Cundinamarca. Cáceres and Etayo elevated the "Pisos de Barzalosa" to a formation in 1969.[1]
The Barzalosa Formation consists of conglomerates, sandstones and siltstones.[2] In parts, the formation contains shale beds and gypsum.[3]
The approximately 360m (1,180feet) thick Barzalosa Formation overlies the Olini Group and the Seca Formation in the west and is overlain by the Honda Group.[2] In the east towards Fusagasugá, the formation overlies the La Tabla Formation and is overlain by the Carmen de Apicalá Conglomerate.[4] As the formation does not contain foraminifera, the age is difficult to establish, but has been estimated to be Oligocene to Early Miocene,[2] or Middle Eocene to Oligocene.[5] The depositional environment has been interpreted as alluvial fans and braided rivers.[6]
| Location | Department | Fossils | class=unsortable | Notes |
|---|---|---|---|---|
| Alto San José, Chaparral | Tolima | Balanerodus logimus | ||
| Lophiodolodus chaparralensis | ||||
| Xenastrapotherium chaparralensis | ||||
| Protheosodon sp. | ||||
| Proadinotherium sp. | ||||
The Barzalosa Formation is apart from its type locality found in Tocaima and to the east of Agua de Dios,[1] and on the western side of the Magdalena River around Chaparral, Tolima.
Geology of the Eastern Hills
Geology of the Altiplano Cundiboyacense