Malargue, Mendoza, Argentina Malargue, Mendoza, Argentina
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GEOGRAPHICAL FEATURES

Malargue is the largest district in Mendoza Province. The total surface is very similar to that of the whole of Tucumán Province with 41,500 square kilometres. Being as it is very close to the Andes, the average altitude is about 1,400 metres above sea level.

DIFFERENT ENVIRONMENTS IN THE DISTRICT OF MALARGUE

It is not easy to talk about Malargue if one does not take into account two very central components of nature, which are water and high point formations. These two components have modelled and influenced very significantly not only the landscape and its richness but also the lives of those who chose this land to live here and enjoy it.

But, the most striking feature for those visiting is the modelling of the territory, especially the majestic Central Cordillera, the many valleys and canyons, the unbeatable volcanic fields in La Payunia and the central flat lands ending in the Llancanelo Lake amongst many other geo-formations. 

The Central Cordillera (the only chain of mountains separating the district from the Republic of Chile) is actually the geological history of Mendoza and of Argentina. It is a very young chain since it started to be formed around 65 million years ago and it has an average height of 3,500 metres.

 It shelters many glacier and river valleys with huge water wealth which is tremendously important for the province, such as the basins of the Salado, Grande and Malargue Rivers.

This massive chain includes many young volcanoes which work as great glacier and snow reservoirs. Amongst these volcanoes, we can mention the volcanic family including: the “Planchón”, “Peteroa”, “Azufre”, “Descabezado Grande,” “Azul” and “Quizapu” Volcanoes.

 Volcanic records confirm the presence of eruptions since the year 1500; however, there is evidence of intense activity much before that year.

Zona Volcánica, Malargüe

As an example of this and acting as a witness of that activity, we can mention the presence of ashes all around the district due to an eruption of the Quizapu in 1932 which covered with ashes a large surface of the Mendoza Province as well important chunks of other provinces.

The climatic conditions are dominated by air masses coming over from the Pacific Ocean generating snow fall in winter which feed the above mentioned river systems. During summer, and depending on the intensity of the air masses, it receives humid winds from the Atlantic Ocean which bring torrential rains and swell the streams and rivers coming down from the mountains and the lower hills.

The climate, the kind of relief and the soils, all have an influence on the vegetation growth adapted to altitude conditions, low temperatures and the dryness of the air.

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