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 ====== The Altiplano Cundiboyacense Mountain Range ======
-The Altiplano Cundiboyacense is located in the central area of the Eastern Cordillera of the Colombian Andes and extends across the departments of Cundinamarca and Boyacá. It includes a series of interconnected high-mountain basins and plateaus—such as the Bogotá savanna and the Ubaté and Chiquinquirá valleys—with most elevations ranging between 2,500 and 3,000 meters.
+The Altiplano Cundiboyacense, situated in the central portion of the Eastern Cordillera of the Colombian Andes, represents a key geomorphological region composed of interconnected high-altitude basins and plateaus (Grokipedia, 2024). Spanning the departments of Cundinamarca and Boyacá, the plateau stands roughly 2,500 to 3,000 meters above sea level. Its main features include the Bogotá savanna, the Ubaté Valley, and the Chiquinquirá Valley, forming a relatively even highland area. Unlike much of the Andes, which are dominated by steep and fragmented terrain, this plateau offers favorable conditions for agriculture, human settlement, and urban expansion (World Bank, 2010).
-The flat and moderately elevated high plateau provides ideal space for urban development.
-In the Andes, most areas are steep and unsuitable for large settlements, but the Altiplano Cundiboyacense consists of a series of relatively level high-mountain basins, such as the Sabana de Bogotá. This makes it one of the easiest areas for cities to expand and settle, which is why Colombia’s largest city—Bogotá—is located here.
+Figure1 the view of Altiplano Cundiboyacense
-Its cool climate and fertile land encourage population concentration.
-With an elevation of about 2,500–3,000 meters, the plateau has a mild climate, fewer tropical diseases, and favorable agricultural conditions. As a result, it has been densely populated since pre-Hispanic times, leading many cities (such as Tunja, Zipaquirá, and Sogamoso) to develop along the plateau.
+{{:arcabuco_rural_detalle.jpg?400|}}
-Its role as the core area of the ancient Muisca civilization stimulated early urban formation.
-The Muisca people relied on the plateau’s salt mines, farmland, and trade routes to establish settlement centers. These locations later evolved into colonial and modern cities, causing today’s urban distribution to overlap significantly with ancient cultural centers.
+A significant environmental feature surrounding the plateau is the **[[18|Paramo de Sumapaz ecosystem]]**, which plays an essential role in sustaining water resources for the region (Instituto Humboldt, 2018). These high-altitude wetlands, typically located above 3,000 meters, are distinguished by unique vegetation such as tussock grasses, cushion bogs, and the emblematic Espeletia species. Functioning both as a biodiversity hotspot and a hydrological regulator, the páramo captures rainfall and atmospheric moisture, stores it within its organic soils, and gradually releases it into river systems. Consequently, it underpins the water supply for major urban centers, including Bogotá, which relies heavily on páramo-fed watersheds (World Bank, 2010).
-Natural corridors facilitate transportation, promoting a chain-like distribution of cities along valleys and basins.
-The internal basins of the plateau are connected by relatively gentle valleys that historically served as important transportation and trade routes. As a result, cities formed in linear or sequential patterns, such as the Bogotá—Facatativá—Tunja—Duitama—Sogamoso urban corridor.
+Spatially, the plateau is composed of gently sloping valleys that interconnect the basins, serving as natural corridors for transportation and communication (Grokipedia, 2024). This configuration has fostered linear or chain-like urban development, exemplified by the Bogotá–Tunja–Sogamoso axis (Wikipedia, 2024). Such corridors historically reduced infrastructure costs while facilitating regional trade, mobility, and economic integration.
-The páramo ecosystems surrounding the plateau provide abundant water resources that support large urban development.
-The páramo regions supply reliable water sources (for example, Bogotá’s water comes from the Chingaza and Sumapaz areas), enabling major cities to expand sustainably.
+Figure2: the range of Altiplano Cundiboyacense
+{{::altiplano_cundiboyacense_subdivisions_.png?400|}}
+The Altiplano Cundiboyacense is more than a geographical plateau; it is a dynamic socio-ecological landscape shaped by long-term interactions among geological processes, climatic factors, and human activity. Serving as the cradle of ancient civilizations, a vital agricultural hub, and a key ecological zone, it occupies a central role in Colombia’s natural and cultural framework. Given ongoing urban growth and environmental pressures, sustained research and responsible spatial planning are essential to ensure the long-term resilience and sustainability of this distinctive highland region.
+Reference：
+Grokipedia (2024) Altiplano Cundiboyacense. Available at: https://grokipedia.com/page/Altiplano_Cundiboyacense
+Instituto de Investigación de Recursos Biológicos Alexander von Humboldt (2018) Páramos de Colombia: biodiversidad y servicios ecosistémicos. Bogotá: IAvH.
+World Bank (2010) Colombia. Available at：https://www.worldbank.org/ext/en/country/colombia
+Wikipedia (2024) Altiplano Cundiboyacense. Available at: https://en.wikipedia.org/wiki/Altiplano_Cundiboyacense