Cañón de Santa Elena

History

The arrowheads, the mortars and paintings found at the site indicate the following human occupation periods: Paleo-Indian (15,000-6,500 BC), Archaic (6500 BC-900 AD), early Postclassic (900 to 1500 AD), and late Postclassic (1300 to 1680). These populations were dispersed with seasonal movements, allowing the use of resources. They engaged in fishing, the collection, hunting, and agriculture. Among the groups transiting this area they highlight Conchos, the Jumano, the Chisos and Apaches, the Chiricahua, the Mezcaleros and Lipanenes

The Spanish and Comanche arrived at the same time, and ended with the Mescalero and Lipan. The colonial government established the Rio Grande as a line of defense, where he built small fortifications, which were guarded by a garrison of soldiers. These were San Carlos, in Chihuahua, and the Board of Rivers, San Vicente, Santa Rosa and San Juan Bautista, in Coahuila. Until 1890 the region remained virtually uninhabited due to attacks by Apaches and Comanche tribes.

From 1784, the fort of San Carlos was abandoned and was only used by travelers, who were protected from attack by Apaches and bandits. The first council of municipality of Ojinaga was built in 1824, and was annexed in 1831, as a section of San Carlos, which bears the name of Manuel Benavides.

Geography

The protected area is within the known as Chihuahuan desert ecosystem, which highlights a number of mountain ranges separated by valleys and wavy plains, home calcium and volcanic areas. It has great diversity of vegetation types because of the large differences in altitude, from seven to two thousand four hundred meters above sea level.

Location

Santa Elena Canyon is to the northeast of Chihuahua, bounded to the north by Rio Grande and east by Coahuila. 80% of the reserve is located in the municipalities of Manuel Benavides and Ojinaga. It covers a strip of thirty km wide by one hundred km long, ranging from this to west. Has a height above sea level ranging from seven m. Until 2400 m, on the highest part of their guns

Geology

The area has a base of Cretaceous limestone on which developed volcanic in mid-Tertiary. Volcanism caused folds between the plates, because the fragment into blocks of lifts formed and depression. In areas are metamorphic rocks Palaeozoic granitic and igneous intrusions.

The area of Santa Elena Canyon includes the sierras of El Ranchito, Sierra Rica and El Mulatto, among which are the valleys of Alamo, Chapó, El Mulato, and Rancho Blanco. Also they highlight the low hills of Manuel Benavides, Paso Lajitas and San Antonio. The area has two canyons: La Gaviota (the Seagull), 656 meters deep, and Santa Elena, with a depth of 467 meters. Much of the area is flat, with slopes less than 8% and bigoted hills and formations

Climate

The area has an extremely dry and hot climate. The climatic conditions are very extreme, with temperatures up to 50 °C in summer. In addition, there is a contrast between the desert and cold temperate ecosystems. The climate is arid, with little rain in summer.

Demographics

The main villages of the area are Manuel Benavides, which is the county seat, Loma de Juárez, El Mulato, Area Montoya, Paso Lajitas, New Lajitas, Santa Elena, Altares, Paso de San Antonio, San Antonio Alamos, Providence, Jars of Wizards and Alamos Marquez. In addition, the towns of Ojinaga, La Mula, Mahijoma and Morita is located in the area of influence. It is estimated that in the 2578 inhabitants live protected area.

Within the protected area there are 125 properties, which occupy 34.8% of the area, 13 ejido s, which occupy 59.4%, and foundations and centers of population and public lands occupy 5.8 Remaining%. The soils of the area and the area of influence are used for agriculture, the livestock and mining.

Flora and fauna

In the area there are several species, of which seventy-nine are protected. Thirteen of these are species of plants, mostly cacti, while the rest are sixty-six species of wildlife, among which include the black bear, the golden eagle, the peregrine and beaver

The area has a great diversity of vegetation, highlighting the scrub desert microphyll, scrub desert rosetophilous, the pasture, the oak forest and vegetation riparian, and also scrub Guamis, mariola, cenixo and guayacán in addition to mesquite, feline and huizaches. In the region with a resetófila vegetation, which is made up of lechugilla, Sotol and various species of cactus develops. Moreover, there is riparian vegetation consisting of poplars and willows.

In the desert scrub microphyll you can find species such as Guamis ( Larrea tridentata ), hojasén ( Flourensia cernua ), mariola ( Parthenium incanum ), mesquite ( Prosopis glandulosa ), ocotillo ( Founquieria splendens ) and reed ( Koeberlinia spinosa ), among others. In the desert scrub rosetophilous can find species such as palm ( Yucca rostrata ), lechuguilla ( Agave lechugilla ), maguey ( Agave spp ), among others. On the other hand, in the grasslands there are species such as penknives (Bouteloua gracilis) or the Chinese grass (Hilaria belangeri), among others. This table groups vegetation protection area are based on its altitude and its botanical composition

The fauna of the region is composed by birds and mammals that have adapted to aridity. Among the species that inhabit the area are the hare black-tailed ( black-tailed jackrabbit ), the bobcat ( Lynx rufus ), the whitetail deer ( Odocoileus virginianus ), the mule deer, the collared peccary ( Tayassu tajacu ), the doves ( mourning dove '), some ducks and coyotes. There are also birds of prey like peregrine (' 'Falcao peregrinus ), the kestrel ( Falco sparverius ) and the golden eagle ( Aquila chrysaetos ). In addition the presence of songbirds stands out and ornamental of beaver is and several species of fish.

Creating the protected area

In 1990 was initiated at the request of the Government of the State of Chihuahua, the process for creating a Biosphere Reserve in Northwest state of Chihuahua, limiting with the Big Bend National Park in United States. After some meetings with villagers and local authorities, the region was declared a Protected Area of Flora and Fauna in 1994. This protected area was included within the area of the Forest Protected Area, and declared in 1934, with the aim of conserving irrigation watersheds, protecting the flow of the Presa La Amistad in Coahuila

The Federal government of the United States had pushed, since 1934, for the creation of a protected area in Mexico to be the counterpart of Big Bend National Park. These initiatives were not considered for various reasons until 1994, except for the creation of the Department of Forest Protection enacted in 1934.

Threats to the reserve

The protected area is affected by various threats, all being caused by humans. These may be environmental, due to the excesses committed by the settlers on the resources of pasture, with an overload of ranching and cattle. Also, some people are clearing land for new crops, thus losing native plant species. Another threat is the mining exploitation, using materials extracted for works and services. There is also the ant smuggling, especially cactuss, fossil is and other archaeological artifacts used by the ancient inhabitants of the area. A looming threat is unchecked tourism, which can inadvertently damage parts of the reserve.

Goals

This reserve was created with the aim of having a protected area that represented the ecological area known as Chihuahuan desert, where counterpart of protected areas border of State of Texas, being able to extend the protection of ecosystem s and conducting joint actions in ecological matters. A study of Autonomous University of Chihuahua conducted in 1994 also argues that the region It is protected because it has a considerable amount of endangered species (thirteen species of flora and sixty six of fauna) and a large geological, hydrological and historical heritage, and a striking contrast between the ecosystems of desert and forest.