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Abaucan River
Topics: Rivers of Argentina
The Abaucan River is a river in Argentina which flows through the provinces of Catamarca and La Rioja, areas with very low precipitation.
It begins in the north of the Tinogasta Department of Catamarca Province, at the confluence of several rivers created by the melting of snow and precipitation in the high Andean peaks, such as the volcano Nevado Incahuasi , Cerro El Muerto and Cerro Negro of Laguna Verde , which dominates in addition the basin of Salina of Laguna Verde. At first it is called Rio Chascuil, then, after having received a stream on the right, the collector of Cerro Cenizo , it becomes the Rio Guanchin down to the spa town of Fiambala where there are hot springs. There, it receives on its left the Rio Fiambala, a periodic stream coming from the north which drains all the southern part of the Cordillera of San Buenaventura and the Sierra of Culampaja, very dry areas. It there takes the name Rio Abaucan, and makes its final orientation toward the south-east. It passes close to the town of Tinogasta, then constitutes the south-southeastern border of the basin of the Salar of Pipanaco, with which it happens that there is an interaction. From this section of its course, it is called the Rio Salado or Colorado or Bermejo. It passes into the province of La Rioja. Leaving the basin of Pipanaco, it threads its way between the Sierra of Ambato and the Sierra of Velasco. A little later it finishes its course by losing itself in a salt semi-desert called Desagues del Rio Salado.
Measurements made over nearly 40 years during the 20th century reveal a very reduced flow compared to the importance of its basin. In Tinogasta, it was an average of 2.54 m a second, with a daily maximum of 85 m. At this place, its basin already measures about 28,300 km, about the area of Belgium. The area of Tinogasta is an oasis well supplied with water by the Abaucan, as well as by aquifers, and is famous for its vineyards. Below Tinogasta, the flow of the river steadily decreases, it not receiving any further influx worth mentioning and losing its water by infiltration in highly permeable sandy zones and by evaporation due to the high temperatures on the plain. Nevertheless, it by and large provides enough water to supply the few human establishments located along its course.
In the part of its course where it delimits the southern zone of the basin of the Salar of Pipanaco, its bed is at about the same level as the salar. In the event of significant rising of the streams of the salar, this last can overflow and send its water surplus into the Rio Abaucan, contributing greatly to its salinity. The opposite interaction can also occur.
The important trunk road Route National 60, which connects Cordoba to Chile through the Paso de San Francisco , follows the course of the Rio Abaucan for almost its entire length.
Its mode is purely nival, tied to the snow melt of the Andean tops. Its basin has an area of 43,386 square kilometres, a little more than that of Switzerland.
This article is licensed under the GNU Free Documentation License. It uses material from the Wikipedia article Abaucan River
