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Sabana Formation information


Sabana Formation
Stratigraphic range: Mid to Late Pleistocene
(Ensenadan-Lujanian)
~1.2–0.01 Ma
PreꞒ
O
S
D
C
P
T
J
K
Pg
N
TypeGeological formation
UnderliesHolocene unconsolidated sediments
OverliesSubachoque Fm., Tilatá Fm.
Area~4,500 km2 (1,700 sq mi)
Thicknessup to 320 m (1,050 ft)
Lithology
PrimaryShale
OtherLignite, sandstone, volcanic ash
Location
Coordinates4°43′02.3″N 74°13′01.2″W / 4.717306°N 74.217000°W / 4.717306; -74.217000
RegionBogotá savanna, Altiplano Cundiboyacense
Eastern Ranges, Andes
CountrySabana Formation Colombia
Extent~90 km × 40 km (56 mi × 25 mi)
Type section
Named forBogotá savanna
Named byHelmens & Hammen
LocationFunza II well
Year defined1995
Coordinates4°43′02.3″N 74°13′01.2″W / 4.717306°N 74.217000°W / 4.717306; -74.217000
RegionCundinamarca
CountrySabana Formation Colombia
Thickness at type section317 m (1,040 ft)

Paleogeography of the Pleistocene
by Ron Blakey
The Altiplano Cundiboyacense was formed late in the Andean orogenic phase

The Sabana Formation (Spanish: Formación Sabana, Q1sa, QTs) is a geological formation of the Bogotá savanna, Altiplano Cundiboyacense, Eastern Ranges of the Colombian Andes. The formation consists mainly of shales with at the edges of the Bogotá savanna lignites and sandstones. The Sabana Formation dates to the Quaternary period; Middle to Late Pleistocene epoch, and has a maximum thickness of 320 metres (1,050 ft), varying greatly across the savanna. It is the uppermost formation of the lacustrine and fluvio-glacial sediments of paleolake Humboldt, that existed at the edge of the Eastern Hills until the latest Pleistocene.

The uppermost sediments of the Sabana Formation were deposited during the Last Glacial Maximum, a time when the first humans populated the Bogotá savanna. These hunter-gatherers used the bones of the still extant Pleistocene megafauna as Notiomastodon platensis, Cuvieronius hyodon and Equus neogeus, of which fossils have been found in the Sabana Formation.

Knowledge about the formation has been provided by geologists Alberto Guerrero, Thomas van der Hammen and others.

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