Carmen River

Carmen River
a map of the Guzmán Basin showing the lake and river between Chihuahua City and Ciudad Juárez
Native nameRio del Carmen (Spanish)
Location
CountryMexico
StateChihuahua
Physical characteristics
Source 
  coordinates30°01′32″N 106°58′44″W / 30.02556°N 106.97881°W / 30.02556; -106.97881 (Rio del Carmen headwaters)
Mouth 
  location
Laguna de los Patos
  coordinates
30°40′37″N 106°29′31″W / 30.677°N 106.492°W / 30.677; -106.492 (mouth of Rio del Carmen)

The Carmen River (Rio del Carmen) is a river in Chihuahua, Mexico that rises to the west of Lake St Martin and drains into Lake Patos (Laguna de los Patos).

Like other rivers in north-west Chihuahua, the river disappears at the lake because of the rainfall levels and the arid climate. It can very between being an intermittent stream in the dry season to a full-flowing river in the rainy season. The lake can be almost entirely dried out in some years.

The river flows past Villa Ahumada to the east.

In prehistoric times, this river alongside the Rio Casas Grandes and Rio Santa Maria to the west formed a river system with a significant population. Several archaeological finds along the river valley and in Lake Patas are indicative of worked turquoise at the time of the Casas Grandes.

Laguna de los Patos itself is 11 kilometres (6.8 miles) north of Villa Ahumada, at an elevation of 1,150 metres (1,260 yd) above mean sea level; and the Pan-American Highway runs to its west. It is so-named because of its historic reputation as a place where wildfowl gathered. However, both the river and the lake have been used by farmers for irrigation leaving the lake entirely dry during some parts of the year since the 1940s, and greatly diminished in size in general over the course of the middle 20th century. Wildfowl have been observed still gathering there in small numbers during that period, in the wet season and on the ice of the lake in the winter.

The lake's long axis runs north-south, with it being roughly 8 by 3 kilometres (5.0 by 1.9 miles) in size. In 1956 its area was measured at 2,400 hectares (5,900 acres), and in 1981 it was estimated to have a roughly maximal area of 5,500 hectares (14,000 acres) after heavy rainfall.

It is considered likely that the regular high wind levels and muddy nature of the lakebed, as well as heavy grazing, inhibit the growth of aquatic vegetation on the lake.