Valley of Toluca

The Toluca Valley is a valley in central Mexico, just west of the Valley of Mexico (Mexico City), the old name was Matlatzinco. The valley runs north south for about 35 km surrounded by mountains, the most imposing of which is the Nevado de Toluca Volcano. It is one of the highest valleys in Mexico and for this reason has a relatively cold climate. Since the 1940s, there has been significant environmental degradation in the valley, with the loss of forests, soil erosion, falling water tables and water pollution due to growth in industry and population. In the pre Hispanic period, it was a buffer region between the Aztec Empire and Purépecha Empire. From the Aztec period until the 19th century, it was part of the region controlled by Mexico City, but today it is the center of the State of Mexico, which has its capital in Toluca, the main city of the valley.

The Toluca Valley is a broad highland valley located immediately west of the Valley of Mexico. It is one of the highest valleys in Mexico with an average elevation of 2,570 meters above sea level ("masl"). The valley is part of the Trans-Mexican Volcanic Belt, with its soils of volcanic origin mostly dating from the Upper Cenozoic. Mountains sides have tertiary volcanic rock, mostly basalt and andesite along with pyroclastic matter and breaches. The valley floor is composed of lacustrine and sedimentary materials . The valley covers an area of about 700 square kilometres, running north south with a length of 35 km. Its width is about 20 km. Its northern border is marked by the Guadalupana Volcano, the Cerro el Aguila and the Sierra Monte Alto. Its southern extension is marked by the Tenango and Zempoala Volcanoes. Its eastern boundary is marked by the Sierra de Las Cruces and La Iglesia mountains and the west is defined by the Nevado de Toluca and the Sierra Morelos. These mountains, along with the elevation of the valley in general cause the area to experience cooler temperatures then the rest of the region.

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