El Abra

Etymology

The name El Abra is taken from a large hacienda 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, bones and vegetal charcoal with radiocarbon dating established the date of the settlement in 12,400 ± 160 years BP.

Archaeological research

In the late 1960s, the Indiana University collaborated in a deeper research. In 1970, the Dutch 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 lithic tools.

Guantivá interstadial

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

Tibitó stadial

Main article: Tibitó

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 mastodons (Haplomastodon waringi and Cuvieronius hyodon), American horse (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 glaciations. From this period the archaeological site of Tequendama in Soacha shows lithic instruments (Tequendamenses tools) with a more smooth manufacture, many of them made with materials brought to this place from the Magdalena River valley, such as quartzite. At Tequendama, evidence for domestication of guinea pigs 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 rodents and vegetables 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 Checua were populated.

Aguazuque

Main article: 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 Suesca, due to the overhanging character of the formation.

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

References

Bibliography

References

1. {{in lang. es [http://aplicaciones.virtual.unal.edu.co/blogs/hacolombia/2011/03/13/1-nivel-paleoindio-abrigos-rocosos-del-tequendama/ Nivel Paleoindio. Abrigos rocosos del Tequendama] {{webarchive. link. (2016-04-29)
2. Gómez Mejía, 2012, p.153
3. {{in lang. es [http://monodedo.com/md%20colombia/mdcolombia/dondeEscalar/topos/zipaquira.htm Las Rocas del Abra (Cundinamarca) climbing activities]