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Nemocón rock shelter[edit]

Nemocón 1-4
Tisquesusa/sandbox2 is located in Colombia
Tisquesusa/sandbox2
Location within Colombia
LocationNemocón, Cundinamarca
RegionBogotá savanna
Altiplano Cundiboyacense
 Colombia
Coordinates5°08′30.2″N 73°52′05.3″W / 5.141722°N 73.868139°W / 5.141722; -73.868139
Altitude2,620 m (8,596 ft)[1]
TypeRock shelter
Part ofPre-Muisca sites
Area24 m2 (260 sq ft)
History
MaterialStone & bone tools
Carbon
Human remains
Founded7530 ± 100 BP
PeriodsLithic-Herrera
CulturesPreceramic-Herrera
Site notes
ArchaeologistsGonzalo Correal Urrego
[2][3]

The rock shelter of Nemocón is an archaeological site in the north of the Bogotá savanna on the Altiplano Cundiboyacense, Colombia.[3] The rock shelter is located in the north of municipality Nemocón, Cundinamarca, Colombia. At Nemocón, bone and stone tools (waste material of tool making mostly and knives and scrapers) and carbon have been found. The site has been dated at 7530 ± 100 years BP.

Main researcher of Nemocón rock shelter is Colombian archaeologist Gonzalo Correal Urrego, who also analysed other early sites Tequendama, Aguazuque, Sueva, Tibitó and El Abra.[2].

Background[edit]

The Altiplano Cundiboyacense, and its southeastern flat portion the Bogotá savanna were populated by the first humans in the late Pleistocene, as evidenced by finds in Pubenza (16,000 years BP), El Abra, Tibitó and others. Until roughly 30,000 years BP, the Bogotá savanna was covered by a large lake; Lake Humboldt. This glacial lake surrounded by snowy peaks was fed by the glaciers of Sumapaz in the south, based on analysis of debris flow deposits close to Fusagasugá, yielding ages between 40,000 and 7000 years BP.[4] The approximately 4,500 square kilometres (1,700 sq mi) large lake contained an island, presently known as the Suba Hills (Cerros de Suba), in Bogotá. Surrounding the lake, Pleistocene megafauna as Glyptodonts, giant sloths, mastodons and deer foraged. The lake retreated during the last 30,000 years, but remnants still existing today are the Bogotá River and its tributaries, Lake Herrera and the many Wetlands of Bogotá. The timber line around Lake Humboldt, in older texts named Lake Bogotá, has been estimated to have been 1,000 metres (3,300 ft) lower than today.[5]

During the latest Pleistocene and early Holocene, the first humans arrived on the Andean high plateau at 2,650 metres (8,690 ft) above sea level. They settled in caves and rock shelters in various locations on the Altiplano and had a hunter-gatherer lifestyle. The main ingredient of the early diet existing until colonial times was white tailed deer (Odocoileus virginianus). Fishing in the many lakes that existed in those times was another source of food for the people.

Timeline of inhabitation of the Altiplano Cundiboyacense, Colombia
TequendamaAguazuquePiedras del Tunjo Archaeological ParkGalindo, BojacáBD BacatáLake HerreraChía (Cundinamarca)ZipaquiráEl AbraChecuaTibitóSuevaEl InfiernitoHistory of ColombiaSpanish EmpireSpanish conquest of the MuiscaMuisca peopleHerrera PeriodMuisca Confederation#PrehistoryBochicaMuisca mummificationCeramicAndean preceramicMuisca agricultureHunter-gatherer





Description[edit]

Class Frequency
cores 109
cantos rodados 104
hammers 18
waste 1929
lascas 902
scrapers 178
knives 7
choppers 1
bone scrapers 194
bone points 31
bone frags and microfrags 20,000+

See also[edit]

List of Muisca and pre-Muisca sites
Aguazuque, Tequendama, Checua, Sueva
El Abra, Tibitó, Gonzalo Correal Urrego

References[edit]

  1. ^ Correal Urrego, 1979, p.31
  2. ^ a b Correal Urrego, 1979
  3. ^ a b (in Spanish) Caracterización de los sitios arqueológicos Sabana de Bogotá - ICANH
  4. ^ Hoyos et al., 2015, p.265
  5. ^ Zonneveld, 1968, p.205

Bibliography[edit]

  • Correal Urrego, Gonzalo. 1979. Investigaciones Arqueológicas en Abrigos Rocosos de Nemocón y Sueva, 1-264. Fundación de Investigaciones Arqueológicas Nacionales - Banco de la República.
  • Montes, Natalia; O. Monsalve; G.W. Berger; J.L. Antinao; H. Giraldo; C. Silva; G. Ojeda; G. Bayona, and J. Escobar. 2015. A climatic trigger for catastrophic Pleistocene–Holocene debris flows in the Eastern Andean Cordillera of Colombia. Journal of Quaternary Science 30(3). 258-270. .
  • Prado, José Luis; María Teresa Alberdi; Begoña Sánchez, and Beatríz Azanza. 2003. Diversity of the Pleistocene Gomphotheres (Gomphotheriidae, Proboscidea) from South America. Deinsea 9. 347-363. .
  • Scott, David A., and Pieter Meyers. 1994. Archaeometry of Pre-Columbian sites and artifacts, 1-437. The Getty Conservation Institute.
  • Villarroel, Carlos; Ana Elena Concha, and Carlos Macía. 2001. El Lago Pleistoceno de Soatá (Boyacá, Colombia): Consideraciones estratigráficas, paleontológicas y paleoecológicas. Geología Colombiana 26. 79-93. .
  • Vogel, J.C., and J.C Lerman. 1969. Groningen Radiocarbon Dates VIII. Radiocarbon II(2). 351-390. .
  • Zonneveld, Jan Isaak Samuel. 1968. Quaternary climatic changes in the Caribbean and N. South America, 203-208.

Further reading[edit]


Sueva[edit]

Sueva
Tisquesusa/sandbox2 is located in Colombia
Tisquesusa/sandbox2
Location within Colombia
LocationJunín & Guasca, Cundinamarca
RegionAltiplano Cundiboyacense
 Colombia
Coordinates4°49′22.9″N 73°45′42.4″W / 4.823028°N 73.761778°W / 4.823028; -73.761778
Altitude2,560 m (8,399 ft)[1]
TypeRock shelter
Part ofPre-Muisca sites
Area22 m2 (240 sq ft)
History
MaterialStone & bone tools
Carbon
Founded10,090 ± 90 BP
PeriodsPrehistory-Herrera
CulturesPreceramic-Herrera
Site notes
ArchaeologistsGonzalo Correal Urrego
[2]

Sueva is the third-oldest dated archaeological site on the Altiplano Cundiboyacense, Colombia.[3] The rock shelter is located in the extreme west of municipality Junín at the border with Guasca, Cundinamarca, Colombia. At Sueva, bone and stone tools (knives and scrapers mostly) and carbon have been found. Carbon from the deepest human trace containing layer of the site is carbon dated to be 10,090 ± 90 years old.

Main researcher of Sueva is Colombian archaeologist Gonzalo Correal Urrego, who also analysed other early sites Tequendama, Aguazuque, Nemocón, Tibitó and El Abra.[2]

Background[edit]

Sueva and other prehistoric sites on the Bogotá savanna

The Altiplano Cundiboyacense, and its southeastern flat portion the Bogotá savanna were populated by the first humans in the late Pleistocene, as evidenced by finds in Pubenza (16,000 years BP), El Abra, Tibitó and others. Until roughly 30,000 years BP, the Bogotá savanna was covered by a large lake; Lake Humboldt. This glacial lake surrounded by snowy peaks was fed by the glaciers of Sumapaz in the south, based on analysis of debris flow deposits close to Fusagasugá, yielding ages between 40,000 and 7000 years BP.[4]

During the latest Pleistocene and early Holocene, the first humans arrived on the Andean high plateau at 2,650 metres (8,690 ft) above sea level. They settled in caves and rock shelters in various locations on the Altiplano and had a hunter-gatherer lifestyle. The main ingredient of the early diet existing until colonial times was white tailed deer (Odocoileus virginianus). Fishing in the many lakes that existed in those times was another source of food for the people.

Timeline of inhabitation of the Altiplano Cundiboyacense, Colombia
TequendamaAguazuquePiedras del Tunjo Archaeological ParkGalindo, BojacáBD BacatáLake HerreraChía (Cundinamarca)ZipaquiráEl AbraChecuaTibitóSuevaEl InfiernitoHistory of ColombiaSpanish EmpireSpanish conquest of the MuiscaMuisca peopleHerrera PeriodMuisca Confederation#PrehistoryBochicaMuisca mummificationCeramicAndean preceramicMuisca agricultureHunter-gatherer





Description[edit]

See also[edit]

List of Muisca and pre-Muisca sites
Aguazuque, Tequendama, Checua, Nemocón
El Abra, Tibitó, Gonzalo Correal Urrego

References[edit]

  1. ^ Correal Urrego, 1979, p.141
  2. ^ a b Correal Urrego, 1979
  3. ^ (in Spanish) Caracterización de los sitios arqueológicos Sabana de Bogotá - ICANH
  4. ^ Hoyos et al., 2015, p.265

Bibliography[edit]

  • Correal Urrego, Gonzalo. 1979. Investigaciones Arqueológicas en Abrigos Rocosos de Nemocón y Sueva, 1-264. Fundación de Investigaciones Arqueológicas Nacionales - Banco de la República.
  • Montes, Natalia; O. Monsalve; G.W. Berger; J.L. Antinao; H. Giraldo; C. Silva; G. Ojeda; G. Bayona, and J. Escobar. 2015. A climatic trigger for catastrophic Pleistocene–Holocene debris flows in the Eastern Andean Cordillera of Colombia. Journal of Quaternary Science 30(3). 258-270. .
  • Prado, José Luis; María Teresa Alberdi; Begoña Sánchez, and Beatríz Azanza. 2003. Diversity of the Pleistocene Gomphotheres (Gomphotheriidae, Proboscidea) from South America. Deinsea 9. 347-363. .
  • Scott, David A., and Pieter Meyers. 1994. Archaeometry of Pre-Columbian sites and artifacts, 1-437. The Getty Conservation Institute.
  • Villarroel, Carlos; Ana Elena Concha, and Carlos Macía. 2001. El Lago Pleistoceno de Soatá (Boyacá, Colombia): Consideraciones estratigráficas, paleontológicas y paleoecológicas. Geología Colombiana 26. 79-93. .
  • Vogel, J.C., and J.C Lerman. 1969. Groningen Radiocarbon Dates VIII. Radiocarbon II(2). 351-390. .
  • Zonneveld, Jan Isaak Samuel. 1968. Quaternary climatic changes in the Caribbean and N. South America, 203-208.

Further reading[edit]