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   » » Wiki: El Abra
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El Abra is the name given to an extensive archeological site, located in the valley of the same name. El Abra is situated in the east of the municipality Zipaquirá extending to the westernmost part of Tocancipá in the department of Cundinamarca, . The several hundred metres long series of is in the north of the Bogotá savanna on the Altiplano Cundiboyacense, Eastern Ranges of the Colombian at an altitude of . The rock shelter and system is one of the first evidences of in the , dated at 12,400 ± 160 years . The site was used by the of the epoch.


Etymology
The name El Abra is taken from a large of that name at the foot of the western portion of the rock formation. The eastern side of the outcropping sandstones is accessible. Climbing activities at these Rocas de Sevilla are organised.


Stratigraphy
The first research in the place was conducted in 1967, and the stratigraphy of lithic instruments, and vegetal with radiocarbon dating established the date of the settlement in 12,400 ± 160 years . Nivel Paleoindio. Abrigos rocosos del Tequendama Gómez Mejía, 2012, p.153


Archaeological research
In the late 1960s, the Indiana University collaborated in a deeper research. In 1970, the Foundation for the Advancement of Tropical Research (NWO-WOTRO) discovered four new preceramic sites and the analysis of lacustrine sediments allowed a more accurate understanding of the paleoclimate and flora.


Fúquene stadial
The Fúquene stadial, named after Lake Fúquene, close to the village of the same name, is defined from 15,000 to 12,500 BP. It is characterized by a cold climate, flora typical of páramo ecosystems, and .


Guantivá interstadial
About 12,500 years ago, a gradual rise of temperature allowed the return of and the settlement of many animal species, making easier. Artefacts of this period are called abriense: flint (tool)s, and . As the climate was more benign, the cave system was gradually abandoned.


Tibitó stadial
The excavations of this period, near Tocancipá at Tibitó, dated at 11,400 years BP, show lithic instruments, bone tools and remains of Pleistocene megafauna, such as ( and ), American ( Equus amerhipuus lasallei), and deer ( Odocoileus virginianus) with traces of ritual ceremonies.


El Abra stadial
Dated 11,000 BP, it is characterized by a new cooling of the climate, recession of the forests and a last period of extending . From this period the archaeological site of in shows lithic instruments ( Tequendamenses tools) with a more smooth manufacture, many of them made with materials brought to this place from the valley, such as . At Tequendama, evidence for domestication of has been uncovered.


Holocene
Around 10,000 years BP, the last glaciation ended and the Andean forests appeared again. The lithic instruments show a rise in recollecting activities, with and consumed, and lower amounts of large animals hunted. The El Abra caves were abandoned gradually, while other nearby rock shelters like Nemocón and open area settlements as were populated.


Aguazuque
. In Aguazuque, around 5,000 BP, agriculture was established on elevated terraces, grinding stone instruments can be observed in association with itinerant habits. The abriense type instruments disappear.


Tourism
While access to the western Zipaquirá part of the rock formation is restricted as it is located on private lands, the eastern area in Tocancipá is accessible and around 20 climbing routes have been constructed. The climbing is comparable but more challenging than the famous routes of , due to the overhanging character of the formation. Las Rocas del Abra (Cundinamarca) climbing activities


Gallery
File:Rocas del abra zipaquira.jpg|Hacienda El Abra File:Rocas del abra zipaquira area rural.jpg|Rock formation of El Abra File:El Abra - Climbing Activities - Tocancipá, Cundinamarca, Colombia.jpg|Climbing at El Abra


See also


Bibliography

Further reading
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