Geological formation in the Colombian Andes
The Cacho Formation (Spanish : Formación Cacho , E1 C, Tpc, Tec) is a geological formation of the Altiplano Cundiboyacense , Eastern Ranges of the Colombian Andes . The predominantly sandstone formation with thin intercalated beds of shales dates to the Paleogene period; Middle to Late Paleocene epochs, and has a maximum thickness of 400 metres (1,300 ft).
The formation was first described by Hubach in 1931 and 1957 and named by Campbell in 1962 and Julivert in 1963.[ 1] [ 2]
The Cacho Formation consists of white, yellow and reddish fine to coarse cross-bedded sandstones in thick banks intercalated with reddish and grey shales .[ 1] [ 3]
Stratigraphy and depositional environment [ edit ] The 50 to 400 metres (160 to 1,310 ft) thick Cacho Formation overlies the Guaduas Formation and is overlain by the Bogotá Formation .[ 3] The age has been estimated to be Late Paleocene , based on paleoflora studied by Thomas van der Hammen in 1957. The formation is laterally equivalent to the Lower Socha and Barco Formations .[ 4]
Type locality of the Cacho Formation in the south of the Bogotá savanna
The Cacho Formation is apart from its type locality in Soacha , found in the Eastern Hills of Bogotá , and many other locations in the Eastern Ranges up until the south of Boyacá .[ 2] The synclinals of the Río Frío , Checua -Lenguazaque , Sesquilé , Sisga , Subachoque , Teusacá , Siecha , and the anticlinal of Guatavita are composed of the Cacho Formation.[ 1]
^ a b c Montoya & Reyes, 2005, p.55
^ a b Acosta & Ulloa, 2002, p.58
^ a b Guerrero Uscátegui, 1992, p.5
^ Montoya & Reyes, 2005, p.57
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Guerrero Uscátegui, Alberto Lobo (1992), Geología e Hidrogeología de Santafé de Bogotá y su Sabana , Sociedad Colombiana de Ingenieros, pp. 1– 20
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