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Bogotá savanna

Coordinates:4°45′0″N74°10′30″W / 4.75000°N 74.17500°W /4.75000; -74.17500
From Wikipedia, the free encyclopedia
Motane savanna in Altiplano Cundiboyacense
Bogotá savanna
Sabana de Bogotá
The Bogotá savanna near the city of Bogotá
Topography and outline of the Bogotá savanna
Area4,251.6 km2 (1,641.6 sq mi)
Geology
TypeMontane savanna
Geography
CountryColombia
StateCundinamarca
RegionAndean region
Population centerBogotá
Borders onEast:Eastern Hills
South:Sumapaz mountains
North: Hills ofTausa andSuesca
West: Western hills
Coordinates4°45′0″N74°10′30″W / 4.75000°N 74.17500°W /4.75000; -74.17500
RiverBogotá,Teusacá,Torca,Juan Amarillo,Fucha,Tunjuelo
[1]
All but the southernmost localitySumapaz of Bogotá is located on the Bogotá savanna

TheBogotá savanna is amontane savanna, located in the southwestern part of theAltiplano Cundiboyacense in the center ofColombia. The Bogotá savanna has an extent of 4,251.6 square kilometres (1,641.6 sq mi) and an average altitude of 2,650 metres (8,690 ft). The savanna is situated in theEastern Ranges of the ColombianAndes.

The Bogotá savanna is crossed from northeast to southwest by the 375 kilometres (233 mi) longBogotá River, which at the southwestern edge of the plateau forms theTequendama Falls (Salto del Tequendama). Other rivers, such as theSubachoque,Bojacá,Fucha,Soacha andTunjuelo Rivers, tributaries of the Bogotá River, form smaller valleys with very fertile soils dedicated to agriculture and cattle-breeding.

Before theSpanish conquest of the Bogotá savanna, the area was inhabited by the indigenousMuisca, who formed a loose confederation of variouscaciques, named theMuisca Confederation. The Bogotá savanna, known asMuyquytá, was ruled by thezipa. The people specialised inagriculture, the mining ofemeralds,trade and especially the extraction ofrock salt from rocks inZipaquirá,Nemocón,Tausa and other areas on the Bogotá savanna. The salt extraction, a task exclusively of theMuisca women, gave the Muisca the name "The Salt People".

In April 1536, a group of around 800conquistadors left the relative safety of the Caribbean coastal city ofSanta Marta to start a strenuous expedition up theMagdalena River, the main fluvial artery of Colombia. Word got around among the Spanish colonisers that deep in the unknown Andes, a rich area with an advanced civilisation must exist. These tales bore the -not so much- legend ofEl Dorado; the city or man of gold. The Muisca, skilledgoldworkers, held a ritual inLake Guatavita where the newzipa would cover himself in gold dust and jump from araft into the cold waters of the 3,000 metres (9,800 ft) high lake to the northeast of the Bogotá savanna.

After a journey of almost a year, where the Spanish lost over 80% of their soldiers, the conquistadors following theSuárez River, reached the Bogotá savanna in March 1537. Thezipa who ruled the Bogotá savanna at the arrival of the Spanish wasTisquesusa. The Muisca posed little resistance to the Spanish strangers and Tisquesusa was defeated in April 1537 inFunza, in the centre of the savanna. He fled towards the western hills and died of his wounds inFacatativá, on the southwestern edge of the Bogotá savanna. The Spanish conquistadorGonzalo Jiménez de Quesada established theNew Kingdom of Granada with capital Santa Fe de Bogotá on August 6, 1538. This started a process of colonisation, evangelisation and submittance of the Muisca to the new rule. Between 65 and 80% of the indigenous people perished due to European diseases assmallpox andtyphus. The Spanish introduced new crops, replacing many of theNew World crops that the Muisca cultivated.

Over the course of the 16th to early 20th century, the Bogotá savanna was sparsely populated and industrialised. The rise in population during the twentieth century and the expansion of agriculture and urbanisation reduced the biodiversity and natural habitat of the Bogotá savanna severely. Today, theMetropolitan Area of Bogotá on the Bogotá savanna hosts more than ten million people. Bogotá is the biggest city worldwide at altitudes above 2,500 metres (8,200 ft). The many rivers on the savanna are highly contaminated and efforts to solve the environmental problems are conducted in the 21st century.

Etymology

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Bogotá savanna is named after Bogotá, which is derived fromMuysccubunBacatá, which means "(Enclosure) outside of the farm fields".[2]

Geography

[edit]
Hills of Sesquilé in the northeast of the Bogotá savanna
The climber's paradiseRocas de Suesca form the northeastern boundary of the Bogotá savanna
Main article:Altiplano Cundiboyacense

The Bogotá savanna is the southwestern part of the larger Andean plateau, the Altiplano Cundiboyacense. The savanna is amontane savanna, bordered to the east by theEastern Hills, theSumapaz mountains in the south, the hills ofTausa andSuesca in the north and western hills of Cundinamarca in the west. The total surface area is 4,251.6 square kilometres (1,641.6 sq mi).[1]

Climate

[edit]

The average temperature of the plateau is 14 °C (57 °F), but this can fluctuate between 0 and 24 °C (32 and 75 °F). The dry and rainy seasons alternate frequently during the year. The driest months are December, January, February and March. During the rainy months, the temperature tends to be more stable with variations between 9 and 20 °C (48 and 68 °F). June, July and August are the months that present the largest variations of temperature, and during the morning frost in the higher terrains surrounding the savanna is possible. Sometimes also ground frost is present, which has a negative impact on agriculture. Hail is a relatively common phenomenon on the savanna.[3][4]

Hydrology

[edit]
The Bogotá River separating Cota, Cundinamarca (top) from Bogotá
The Bogotá River is the main river of the Bogotá savanna

Rivers

[edit]

Lakes

[edit]
Natural
[edit]
Artificial
[edit]
  • Tominé Reservoir - northeast, biggest waterbody on the Bogotá savanna - 690 cubic megametres (2.4×1022 cu ft)
  • Neusa Reservoir - north - 102 cubic megametres (3.6×1021 cu ft)
  • El Muña Reservoir - south - 42 cubic megametres (1.5×1021 cu ft)
  • Lake Herrera (since 1973)[5]

Waterfalls

[edit]

Wetlands

[edit]
Main article:Wetlands of Bogotá

There is a system ofwetlands (humedales) that regulate the soil moisture acting like sponges for the rain waters. Fifteen wetlands have a protected status, with various wetlands as unprotected. In 1950, the total surface area of the wetlands amounted to 150,000 hectares (370,000 acres), but due to the urbanisation of the Colombian capital the total area has been reduced to 1,500 hectares (3,700 acres).[6]

Map
WetlandLocationAltitude (m)Area (ha)NotesImage
Guaymaral y TorcaUsaquén
Suba
254773[7][8]
La ConejeraSuba254458.9[9]
CórdobaSuba254840.51[10]
Tibabuyes
Juan Amarillo
Suba
Engativá
2539222.58[11]
JaboqueEngativá2539148[12]
Santa María del LagoEngativá254912[13]
El BurroKennedy254118.84[14]
La VacaKennedy25487.96[15]
TechoTecho, Kennedy254511.46[16]
CapellaníaFontibón254227.05[17]
Meandro del SayFontibón
Mosquera
254813.6[18]
TibanicaBosa
Soacha
254228.8[19]
El SalitreBarrios Unidos25586.4[20]
La IslaBosa25507.7[21]
La FloridaFunza254226[22]

Biodiversity

[edit]
See also:Biodiversity of Colombia

Despite the continuous urbanisation and industrial activities, the Bogotá savanna is a rich biodiverse area with many bird species registered.[23] The diversity of mammals, amphibians and reptiles is much lower.[24] Before the arrival of the European colonisers, the savanna was populated predominantly bywhite-tailed deer, the main ingredient of theMuisca cuisine. Today, this species of deer, as well as the once commonspectacled bear, is restricted to protected areas surrounding the Bogotá savanna. TheThomas van der Hammen Natural Reserve is aprotected area in the north of Bogotá.

History

[edit]
Preceramic sites on the Bogotá savanna
Ab -El Abra
Ti -Tibitó
Te -Tequendama
P -Piedras del Tunjo
Ag -Aguazuque
C -Checua
H -Lake Herrera
See also:Muisca Confederation § Prehistory,Herrera Period, andTimeline of Bogotá

The earliest confirmed inhabitation of present-day Colombia was on the Bogotá savanna withsitesEl Abra,Tequendama andTibitó, where semi-nomadichunter-gatherers lived in caves and rock shelters. One of the first evidences of settlement in open area space wasAguazuque, whose oldest dated remains are analysed to be 5000 years old. This prehistoricalpreceramic period was followed by theHerrera Period, commonly defined from 800 BCE to 800 AD.

Muisca Confederation

[edit]
Main article:Muisca Confederation

At the arrival of theSpanishconquistadors, the region was inhabited by theMuisca who lived in hundreds of small villages scattered across the plateau. These villages were individually ruled bycaciques who at the same time paid tribute to thezipa, ruler of Bacatá. The Muisca were known as "The Salt People", thanks to their extraction ofrock salt from brines in large pots heated over fires. This process was the exclusive task of theMuisca women.

Theeconomy of the Muisca, meaning "person" or "people" in their indigenous version ofChibcha;Muysccubun, was self-sufficient due to the advancedagriculture on the fertile soils of the frequently flooding Bogotá savanna. More tropical and subtropical agricultural products asavocadoes andcotton weretraded with their neighbours, in particular theGuane andLache in the north and northeast and theGuayupe,Achagua andTegua in the east.

The Muisca were known as skilledgoldworkers, represented in the famousMuisca raft, that symbolises the initiation ritual of the newzipa inLake Guatavita. This ritual, where thezipa covered himself in gold dust and jumped in the 3,000 metres (9,800 ft) altitude lake, gave rise to the -not so much- legend ofEl Dorado.

Spanish conquest

[edit]
IndigenousMuiscafishermen in Funza
Litho in 1860 byRamón Torres Méndez[25]
Pottery producingMuisca in Tocancipá
Litho in 1860 by Ramón Torres Méndez[25]
Main article:Spanish conquest of the Muisca

In April 1536, a group of around 800conquistadors left the relative safety of the Caribbean coastal city ofSanta Marta to start a strenuous expedition up theMagdalena River, the main fluvial artery of Colombia. Word got around among the Spanish colonisers that deep in the unknown Andes, a rich area with an advanced civilisation must exist. These tales bore the -not so much- legend ofEl Dorado; the city or man of gold. The Muisca, skilledgoldworkers, held a ritual inLake Guatavita where the newzipa would cover himself in gold dust and jump from araft into the cold waters of the 3,000 metres (9,800 ft) high lake to the northeast of the Bogotá savanna.

After a journey of almost a year, where the Spanish lost over 80% of their soldiers, the conquistadors following theSuárez River, reached the Bogotá savanna in March 1537. Thezipa who ruled the Bogotá savanna at the arrival of the Spanish wasTisquesusa. The Muisca posed little resistance to the Spanish strangers and Tisquesusa was defeated in April 1537 inFunza, in the centre of the savanna. He fled towards the western hills and died of his wounds inFacatativá, on the southwestern edge of the Bogotá savanna. The Spanish conquistadorGonzalo Jiménez de Quesada established theNew Kingdom of Granada with capital Santa Fe de Bogotá on August 6, 1538. This started a process of colonisation, evangelisation and submittance of the Muisca to the new rule. Between 65 and 80% of the indigenous people perished due to European diseases assmallpox andtyphus. The Spanish introduced new crops, replacing many of theNew World crops that the Muisca cultivated.

The Spanish colonizers engaged in the construction of Spanish-style towns to replace all the indigenous villages and in the process of assimilation and religious convert of the Muisca. The majority of those villages kept their indigenous names, but some were slightly modified in time, likeSuacha which becameSoacha,Hyntiba becomingFontibón andBacatá becomingBogotá.

Modern history

[edit]
See also:New Kingdom of Granada,Gran Colombia, andHistory of Bogotá

Over the course of the 16th to early 20th century, the Bogotá savanna was sparsely populated and industrialised. The rise in population during the twentieth century and the expansion of agriculture and urbanisation reduced the biodiversity and natural habitat of the Bogotá savanna severely. Today, theMetropolitan Area of Bogotá on the Bogotá savanna hosts more than ten million people. Bogotá is the biggest city worldwide at altitudes above 2,500 metres (8,200 ft). The many rivers on the savanna are highly contaminated and efforts to solve the environmental problems are conducted in the 21st century.

Timeline of inhabitation

[edit]
Timeline of inhabitation of the Bogotá savanna, Colombia




Cities

[edit]
The capital of Colombia, Bogotá, here seen at night fromMonserrate, is the main city on the Bogotá savanna. The flatland is clearly visible

The main cities of the Bogotá savanna, in addition to the capital city ofBogotá, are:Mosquera,Soacha,Madrid,Funza,Facatativá,Subachoque,El Rosal,Tabio,Tenjo,Cota,Chía,Cajicá,Zipaquirá,Nemocón,Sopó,Tocancipá,Gachancipá,Sesquilé,Suesca,Chocontá andGuatavita.[26]

List of municipalities

[edit]
Municipality
Locality
Altitude
urban centre (m)
Surface area
(km2)
Inhabitants[note 1]RemarksMap
Bogotá264015877,980,00116Named afterBacatá[note 2]
Capital of Colombia
Biggest city at altitudes
above 2,500 metres (8,200 ft)
Usaquén265065.31449,62116
Chapinero264038.15122,50707
Santa Fe264045.1796,24107
San Cristóbal264049.09404,35007
Usme2700119.04314,43107
Tunjuelito26009.91182,53207
Bosa260023.93637,28315
Kennedy270038.59979,91407
Fontibón260033.28317,17907
Engativá260035.88824,33707
Suba2700100.561,161,50016
Barrios Unidos260011.9230,06607
Teusaquillo260014.19139,29807
Los Mártires26006.5194,94407
Antonio Nariño26004.88119,56507
Puente Aranda260017.31250,71507
La Candelaria26402.0622,11507
Rafael Uribe Uribe260013.83378.78007
Ciudad Bolívar2700130593,93707
Soacha2565184.45522,44216Preceramic siteTequendama
Herrera site
Muisca ceramics production
Petrographs found
Sibaté2700125.638,41215Petrographs found
El Muña Reservoir
Mosquera251610782,75015Lake Herrera
Petrographs found
Bojacá259810911,25415Lake Herrera
Petrographs found
Chía256480129,65216Moon Temple
Herrera site
Petrographs found
Cota25665524,91615Petrographs found
Muisca community
Cajicá255850.456,87515Located in the funnel of the northern savanna
Facatativá2586158134,52215Piedras del Tunjo
Funza25487075,35015Muisca market town
Madrid2554120.577,62715Lake Herrera
Petrographs found
El Rosal268586.4817,25415
Zipacón255070557015Agriculture
Place of meditation for thezipa
Petrographs found
Subachoque2663211.5316,11715Petrographs found
Tabio256974.527,03315Hot springs used by the Muisca
Tenjo258710818,38715Petrographs found
Zipaquirá2650197124,37615El Abra
Muisca salt mines
Important market town
Petrographs and petroglyphs found
Nemocón258598.113,48815Muisca salt mines
Preceramic siteChecua
Petrographs found
Cogua260011322,36115Muisca ceramics production
Petrographs found
Neusa Reservoir
Tocancipá260573.5131,97515Preceramic siteTibitó
Muisca ceramics production
Important market town
Petrographs found
Gachancipá25684414,44215Muisca mummy found
Muisca ceramics production
Guasca271034614,75915Siecha Lakes
Muisca ceramics production
Petrographs found
Guatavita2680247.3689815Muisca ceramics production
Main goldworking town
Petrographs found
Tominé Reservoir
Sopó2650111.526,76915Herrera site
Sesquilé259514113,93615Lake Guatavita
Minor Muisca salt mines
Suesca258417717,31815150Muisca mummies found
Lake Suesca
Muisca ceramics production
Important market town
Petrographs found

Panoramas

[edit]
Panoramas
Panorama of the Tena Valley to the southwest of the Bogotá savanna, nearSan Antonio del Tequendama

Bogotá on the savanna

Zipaquirá

School in Cota

The northwestern part of the ancient Lake Humboldt is artificially represented in theNeusa Reservoir



La Conejera wetland

See also

[edit]

References

[edit]
  1. ^abPérez Preciado, 2000, p.2
  2. ^(in Spanish)Etymology Bacatá - Banco de la República
  3. ^"Climate: Bogotá - Climate graph, Temperature graph, Climate table". Climate-Data.org. Retrieved2016-09-29.
  4. ^"Weatherbase: Historical Weather for Bogota, Colombia". Weatherbase. Retrieved2016-09-29.
  5. ^(in Spanish)Lake Herrera largest water reserve of the Bogotá savanna
  6. ^Moreno et al., s.a., p.2
  7. ^Humedal Guaymaral
  8. ^Humedal Torca
  9. ^Humedal La Conejera
  10. ^Humedal Córdoba
  11. ^Humedal Tibabuyes
  12. ^Humedal Jaboque
  13. ^Humedal Santa María del Lago
  14. ^Humedal El Burro
  15. ^Humedal La Vaca
  16. ^Humedal Techo
  17. ^Humedal Capellanía
  18. ^Humedal Meandro del Say
  19. ^Humedal Tibanica
  20. ^Humedal El Salitre
  21. ^Humedal La Isla
  22. ^Humedal La Florida
  23. ^Calvachi Zambrano, 2002, p.95
  24. ^Calvachi Zambrano, 2002, p.97
  25. ^abRamón Torres Méndez (1875).Costumbres santafereñas. E. V. Sperling.
  26. ^Cities on the Bogotá savannaArchived November 13, 2013, at theWayback Machine

Notes

[edit]
  1. ^07; 2007, 15; 2015, 16; 2016
  2. ^Bacatá refers to the southern part of the Bogotá savanna, ruled by thezipa based inFunza, but with various frequently visited other settlements, visibles in the namesNemocón (Nemequene),Zipacón,Zipaquirá,Tocancipá,Gachancipá

Bibliography

[edit]

Geology

[edit]

Wetlands

[edit]

Flora and fauna

[edit]

History

[edit]
Preceramic
[edit]
Muisca
[edit]
Conquest and colonial period
[edit]
General biota
Vertebrates
Other
Regional biota
Ecoregions
Tumbes
Chocó
Magdalena
Tropical
Andes
Other
Nature reserves
Organizations
Seal of BogotaBogotá, Capital DistrictFlag of Bogota
Administrative
subdivision
in 20 localities
Metropolitan Area
Geography
Sedimentary basins of Colombia
Onshore
Western Region
Central Region
Eastern Region
Bogotá savanna is located in Colombia
Amagá Basin
Cauca-Patía Basin
Chocó Basin
Sinú-San Jacinto Basin
Tumaco Basin
Urabá Basin
Catatumbo Basin
Cesar-Ranchería Basin
Cocinetas Basin
Eastern Cordillera Basin
Lower Magdalena Valley
Middle Magdalena Valley
Upper Magdalena Valley
Caguán-Putumayo Basin
Llanos Basin
Vaupés-Amazonas Basin
Chocó Offshore Basin
Guajira Offshore Basin
Sinú Offshore Basin
Tumaco Offshore Basin
Colombia Basin
Colombia Deep Pacific Basin
Los Cayos Basin
Offshore
Source
Barrero, Dario; Pardo, Andrés; Vargas, Carlos A.; Martínez, Juan F. (2007).Colombian Sedimentary Basins: Nomenclature, Boundaries and Petroleum Geology, a New Proposal.ANH. pp. 1–92.
Topics
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The Salt People
Geography and history
Altiplano
Cundiboyacense
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History
Prehistory(<10,000 BP)
Lithic(10,000 - 2800 BP)
Ceramic(>800 BC)
Religion and mythology
Deities
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Built
Natural
Mythology
Myths
Mythological figures
Caciques and neighbours
Northerncaciques
zaque ofHunza
iraca ofSuamox
cacique ofTundama 
Southerncaciques
zipa ofBacatá
cacique ofTurmequé
Neighbours
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Conquistadors
Major
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Neighbouring conquests
Research and collections
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