Guadalupe Hill
| Guadalupe Hill | |
|---|---|
| Cerro de Guadalupe | |
Guadalupe Hill seen from Monserrate
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| Highest point | |
| Elevation | 3,317 m (10,883 ft) |
| Coordinates | 4°35′31″N 74°03′15″W / 4.59194°N 74.05417°WCoordinates: 4°35′31″N 74°03′15″W / 4.59194°N 74.05417°W |
| Geography | |
 Guadalupe Hill
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| City | Bogotá, Colombia |
| Parent range | |
| Geology | |
| Age of rock |
Guadalupe Group (type locality) Campanian-Maastrichtian |
| Mountain type | Thrusted mountain |
| Climbing | |
| First ascent | Pre-Columbian era |
| Easiest route | Pilgrimage trail Avenida Circunvalar→Road to Choachí |
Guadalupe Hill is a 3,317-metre (10,883 ft) high hill located in the Eastern Hills, uphill from the centre of Bogotá, Colombia. Together with its neighbouring hill Monserrate it is one of the landmarks of Bogotá. At the top of the hill a hermitage and a 15-metre (49 ft) high statue has been erected. The statue was elaborated by sculptor Gustavo Arcila Uribe in 1946 and is accompanied by a chapel dedicated to Our Lady of Guadalupe.
Guadalupe Hill is the type locality of the Guadalupe Group, a Late Cretaceous sedimentary sequence of sandstones and shales of 750 metres (2,460 ft) thick. The formation is thrusted on top of younger strata by the reverse Bogotá Fault during the Andean orogeny. The hill is the source for the Manzanares and El Chuscal creeks that flow westwards onto the Bogotá savanna.
Historically, Guadalupe Hill was an important sacred site for the indigenous Muisca, who inhabited the Bogotá savanna and surrounding regions before the Spanish conquest. During the colonial period, Guadalupe Hill contained a cross and the hermitage that was destroyed by various earthquakes in the eighteenth, nineteenth and twentieth centuries. On Sundays, Guadalupe Hill and its chapel and statue are visited by tourists and pilgrims from Bogotá, accessing the hill either by road and public transport or via a walking trail to the hilltop.
Guadalupe Hill is named after Our Lady of Guadalupe of Badajoz, not -as is commonly believed- after the famous Our Lady of Guadalupe in Mexico.
The Guadalupe Hill is the type locality for the Campanian-Maastrichtian Guadalupe Group, a sequence of three formations of sandstones and shales; Arenisca Dura, Plaeners, Arenisca de Labor and Arenisca Tierna. The thickness of the Guadalupe Group, defined as formation by some authors, at Guadalupe Hill is 750 metres (2,460 ft). Approximately 53% of the Eastern Hills consists of the Guadalupe Group.
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Wikipedia