Mérida, officially known as Santiago de los Caballeros de Mérida, is the capital of the municipality of Libertador and the state of Mérida, and is one of the main cities of the Venezuelan Andes. It was founded in 1558 by Captain Juan Rodríguez Suárez, forming part of Nueva Granada, but later became part of the Captaincy General of Venezuela and played an active role in the War of Independence.
The capital city's population is 204,879 inhabitants, and the metropolitan area, that includes the municipality of Libertador, reaches 345,489 people (Census 2001). The city accounts for 28% of the total population of Mérida State, which has more than 750,000 inhabitants (Census 2001). It is home to the University of Los Andes and the Archdiocese of Mérida. It also has the highest and longest cable car in the world. It is the largest student and tourist center of western Venezuela. The mass transit system (Trolebús Mérida) is available as a means of tourist transport.
This city sits on a plateau nestled in the valley of the Chama River, which runs from end to end. The town of Mérida is located at an altitude of 1,600 metres (5,200 feet). As background on the horizon rises the country's highest summit: the Pico Bolívar with an altitude of 4,981 metres (16,342 feet).
Geography:
The city is located in the center of the Venezuelan Andes, in a wide plain in the valley of the Chama River, between the Sierra Nevada de Mérida to the southeast and the Sierra La Culata to the northwest. The old quarter of the city is on the alluvial plain known as Tatuy.
Mérida has four principal rivers and some smaller seasonal streams in the less urbanized parts of the city, these last ones have a significant water flow only in times of heavy precipitation. The most important river is the Chama, followed by the Albarregas, which cross the plain and divide it into two parts: the Banda Occidental (west bank) and the Banda Oriental (east bank). These two rivers run from one end of the city to the other. The other two principal rivers are the Mucujún and the Milla, which flow into the Chama and Albarregas. In the lower part of the city is found the La Rosa lake, one of some 200 lakes in Mérida State.
In the center of the city the terrain, located on a plain, is almost flat. Nonetheless, there is an average incline of 3 to 7 degrees, which causes a difference in altitude between the high and low parts of the city of more than 400 m (1,300 ft), the average being 1,630 m (5,350 ft) above sea level at the Plaza Bolívar. However, the areas surrounding the city are rough and uneven, situated in the valleys formed by the Chama and Albarregas rivers and the Sierra Nevada and Sierra de La Culata ranges.
The valley in which the city is located was formed approximately 40 to 60 million years ago with the creation of the Venezuelan Andes and its continuous erosion by the area's water systems. Its soils consist of alluvial sediment and clay. Below the city runs the major tectonic fault in the western part of the country, the Boconó fault, which forms part of the South American Plate.
The vegetation in the interior of the city consists of medium to tall trees, and ferns (Pteridophyte), located mainly near the basin of the Albarregas river. On the outskirts of Mérida, one finds non-urbanized areas, where sub-mountainous and seasonal jungle vegetation predominates. On the other hand, vast coniferous forests extend toward the south, where they were planted some years ago. Toward the north and east, one finds cloud forests.
Significant among the local fauna are important populations of certain small and medium-sized birds such as hummingbirds and parrots (Psittacidae), spread particularly to the south of the city.