TheCentral Cordillera of Colombia It is a mountain range that forms the axis of the Colombian Andes together with the Eastern Cordillera and the Western Cordillera. In its development starting in the south in the Colombian massif and up to the San Lucas mountain range to the north, it manages to travel approximately 1023 km, occupying an approximate total area of 129 737 km2 with a maximum width of 449 km.
On this mountain range of high snow-capped mountains and active volcanoes is the so-called Eje Cafetero de Colombia and on its way it crosses several important Colombian departments, where some of the main cities of the country have settled..
As expected, this mountain range presents a range of possibilities in terms of fauna and flora, climate and resources, all this enhanced by its changing relief that goes from the plains, passing through the level of tropical forest to climb to heights of perpetual snow..
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Along with the Occidental and the Oriental, the Central Cordillera of Colombia supports 70% of the total population of the country. While it is true that the abrupt topography of the landscape has been a limiting factor in the growth of the population on a larger scale, it is also true that it has brought out the best in its inhabitants to adapt and seek their resources..
Delimited to the west by the Cauca River and to the east by the Magdalena River, there are important cities in Colombia. Some of them are: Medellín, Popayán, San Juan de Pasto, Ibagué, Armenia, Manizales and Pereira.
This activity has been developed since 1986, and is the basis of the current economy of the country.
Up to 1000 meters above sea level, bananas, plantains, rice, cotton, tobacco, cocoa and sugar cane are grown..
Between 1000 and 2000 meters above sea level, corn, coffee, and fruits such as citrus fruits, pears, pineapples and tomatoes are grown; and between 2000 and 3000 meters above sea level wheat, barley, potatoes and flowers are grown.
Emeralds, platinum, silver and gold for export stand out. For the domestic market, cement, coal, clay, salt, sand, gravel and silica are produced..
This activity is one of the most prosperous in this region, given its biodiversity and that it is an obvious tourist attraction.
The surface of our planet is in constant motion, and from the movement and encounter of tectonic plates all the topographic features that we can see around us have arisen..
It is this orogenesis that is responsible for the creation of the Andes and the Colombian mountain ranges. This geological process of folding of the earth's crust along a vast expanse is what provides the opportunity to enjoy perpetual snow or deep crevices near the plains where it disappears..
The last orogenic folding was the Andean-Alpine, which is estimated to have occurred in the Middle and Upper Cretaceous period. The first Colombian mountain range to emerge was the Central, during the Triassic-Jurassic period between 225 and 145 million years ago.
During the time that this mountain range rose (it was Mesozoic), the mega-continent Pangea was separated on the world stage. Other geological processes occurred in parallel due to the intense volcanic activity; currently these are noted in the thick stripes of deep red or black colors in exposed areas of the mountainous structure.
This formation allows you to go from 0 to almost 6000 meters above sea level, where its highest point known as the Nevado de Huila is located..
The formation begins to the south, in the so-called Nudo de Almaguer or Colombian massif, and descends towards the north to disappear in the plains and plains of the San Lucas mountain range..
On this road from south to north, and while it separates into the three mountain ranges that make up the Colombian Andes, it leaves different accidents, peaks, snow-capped mountains and volcanoes. We will describe the most prominent ones below:
It is an active volcano located between the departments Huila, Tolima and Cauca.
It is a volcano located in the homonymous department and is part of the Los Nevados National Park.
Dormant volcano that is also part of Los Nevados National Park
Mountainous formation located between the departments of Risaralda, Caldas and Tolima. It is part of the Los Nevados National Park
It is an inactive volcano, also part of the Los Nevados National Park.
Active volcano located in the department of Cauca. It is part of the Puracé National Park.
Dormant volcano located in the department of Huila
Also called Nudo de Almaguer, it is the starting point of the Colombian mountain range and of a large part of the rivers that bathe the region. There are heights that range between 2,600 and 4,700 meters above sea level..
It is located in the department of Antioquia, with altitudes between 1000 and 3000 meters above sea level.
It is a mountainous formation whose heights range from 0 to 2600 meters above sea level. It is located between the departments of Antioquia and Bolívar.
The Central Cordillera of Colombia gives the possibility of enjoying all possible climates, going from an intense heat to a freezing climate just by traveling along its valleys and mountains. We can identify the following types of weather:
It is present up to 1000 meters above sea level and has an average temperature that exceeds 24 ⁰C. It is dominant in the plains of the mountain range and is key to the production of certain fruits.
It implies temperatures that exceed 27 ⁰C and with a very high humidity. These areas are preferably located towards the north face of the geological formation.
The areas of low mountains between 1000 and 2000 meters above sea level are those that have this type of climate, under which temperatures can be between 17 and 24 ⁰C.
Between 2000 and 3000 meters above sea level we will find the temperatures that define this climate band: they range from 12 to 17 ⁰C.
Upon exceeding 3000 and up to 4000 meters above sea level, we will find temperatures between 6 and 12 ⁰C. Humidity is low at these heights and it is noticeable in the predominant type of vegetation.
Those travelers who dare to exceed 4000 meters above sea level will find temperatures below 6 ⁰C and breathing difficulties.
The richness of the biodiversity of the area goes hand in hand with the rivers and bodies of water that are found along the length and breadth of the mountain range. Many of these see their birth in the Colombian massif and leave their nutrients for thousands of kilometers.
There are several hydrographic slopes that are identified in their journey from south to north. The main one is the so-called Caribbean slope, the longest and most important for the country.
In this there are several holes, which are nothing other than the set of rivers and bodies of water that flow in this slope.
Some of the most important rivers in the central mountain range of Colombia are the following:
- Magdalena (main river of Colombia).
- Cauca.
- Caquetá.
- Patia.
- Saldana.
- Nima.
- Love me.
- Tulúa.
- Amoyá
- Cambrín.
- Anamichú.
- Otún.
- Totarito.
- Mills.
- Medellin.
It is worth noting that these bodies of water constitute a vital communication channel for the growth of the economy, and with the construction of dams and reservoirs an additional boost is given to the quality of life of the inhabitants of the areas they serve..
The electrical energy produced by the aforementioned dams is practically an inexhaustible natural source of resources that would only be affected if the necessary ecological and maintenance measures were not taken..
Another interesting point is the existence of many underground, mineral and volcanic water currents. The former function as providers of the vital liquid in optimal conditions for consumption; the others are a source of supply for sulfur mines.
The hot springs, very frequent thanks to the volcanic activity of various elements in the area, are a source of income thanks to tourist exploitation.
Life flourishes without restrictions thanks to the existence of several bodies of fresh water that see their birth in this mountain range, the same ones that in the past allowed the emergence of the many populations that today are maintained and grow thanks to the resources of that land..
The greatest threat to the region is the intensive illegal hunting and exploitation of resources without recovery plans for the affected areas. Large areas of forests are gradually disappearing and the diversity of the fauna is diminishing.
However, the creation of protection areas and national parks together with stricter regulations will help in the medium and long term to reforestation of the most sensitive sites and the return of species that guarantee the balance of biodiversity..
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