Dog Canyon, on the northern park boundary at the Texas-New Mexico State line is reached by driving through
Carlsbad, New Mexico or
Dell City, Texas. There is a campground which accommodates tent campers, recreational vehicles, and horse trailers. There is a public corral for livestock available by reservation.
On the west side of the park near Dell City lie impressive gypsum sand dunes. Another attraction is the Williams Ranch.
[citation needed]
History[edit]
Map of Guadalupe Mountains National Park
For thousands of years, the
Guadalupe Mountains have had a tumultuous history. Archaeological evidence has shown that people lived over 10,000 years ago in and among the many
caves and
alcoves. Hunter-gatherers followed large game and collected edible vegetation. This conclusion is supported by the discovery of projectile points, baskets, pottery, and rock art.
[3]
The first Europeans to arrive in the area were the
Spanish in the 16th century, but they did not make serious attempts to settle in the area. The Spanish introduced horses; nomadic indigenous tribes like the Apaches soon found them an asset for hunting and migrating.
Mescalero Apaches followed game and harvested the agave (or mescal) for food and fiber (Mescalero is Spanish for mescal-maker). Agave roasting pits and other artifacts of Mescalero culture can be found in the park.
The Mescalero Apaches remained in the mountains through the mid-19th century, but they were challenged by an American transportation route at the end of the
American Civil War. During the 1840s and 1850s many people immigrating west crossed the area. In 1858,
Pinery Station was constructed near Pine Springs for the
Butterfield Overland Mail. The Butterfield Overland Mail traveled over Guadalupe Pass located at 5,534 ft (1,687 m) above sea level. The
9th Cavalry Regiment was ordered to the area to stop Indian raids on settlements and mail stage route. During the winter of 1869, Lt. H.B. Cushing led his troops into the Guadalupe Mountains and destroyed two Mescalero Apache camps. They were eventually driven out of the area and into US
reservations.
Felix McKittrick was one of the first European settlers in the Guadalupe Mountains; he worked cattle during the 1870s.
McKittrick Canyon is thought to be named after him.
Frijole Ranch was the first permanent ranch house; it was constructed in 1876 by the Rader brothers. Frijole Ranch House was the only major building in the region; it served as a community center and regional post office from 1916 to 1942. Today, the Frijole Ranch House has been restored and serves as a cultural museum. In 1908 Williams Ranch House was built, and it was named after one of its inhabitants, James Adolphus Williams. Judge J.C. Hunter from
Van Horn,
Texas consolidated most of the smaller ranches in the area into the
Guadalupe Mountain Ranch. In 1921,
Wallace Pratt, a geologist for
Humble Oil and Refining Company, was impressed by the beauty of
McKittrick Canyon and bought the land to build two houses there. Both were used as summer homes by Pratt and his family up until 1960. Wallace Pratt donated about 6,000 acres (2,400 ha) of McKittrick Canyon which became part of Guadalupe Mountains National Park, which was dedicated and formally opened to the public in September, 1972.
[3]
Geography and climate[edit]
The Guadalupe Mountains reach their highest point at Guadalupe Peak, the highest point in
Texas,
[4] with an elevation of 8,751 feet (2,667 m).
[5]The range lies southeast of the
Sacramento Mountains and east of the Brokeoff Mountains. The mountain range extends north-northwest and northeast from Guadalupe Peak in Texas into New Mexico.
[6] The northeastern extension ends about 10 miles (16 km) southwest of
Carlsbad, near White's City and
Carlsbad Caverns National Park; the southwest tip ends with
El Capitan about 90 miles (140 km) east of
El Paso. The mountains rise more than 3,000 feet (910 m) above the arid floor of the
Chihuahuan Desert.
[4] The Guadalupe Mountains are surrounded by the
South Plainsto the east and north,
Delaware Mountains to the south, and
Sacramento Mountains to the west.
The northwestern extension, bounded by a dramatic escarpment known as "The Rim", extends much further into New Mexico, to near the Sacramento Mountains. The range is bounded on the north by Four Mile Canyon; on the east by the valley of the
Pecos River; and on the west by Piñon Creek, Big Dog Canyon, Valley Canyon, Middle Dog Canyon and West Dog Canyon. Much of the range is built from the ancient Capitán Reef that formed at the margins of a shallow sea during the
Permian Period. For detail on the area's geology, see
Delaware Basin. As the range is built up almost entirely of
limestone, upland areas have little or no surface water. The only significant surface water is McKittrick Creek, in
McKittrick Canyon, which emerges from the eastern side of the massif, just south of the New Mexico border. Elevations at the base of the range vary from 4,000 feet (1,200 m) above
sea level on the western side to 5,000 feet (1,500 m) on the east. Several peaks on the southern end exceed 8,000 feet (2,400 m).
The Guadalupe Mountains experience relatively hot summers, calm, mild autumn weather, and cool to cold weather in winter and early spring. Snow storms, freezing rain, or fog may occur in winter or early spring. Frequent high wind warnings are issued during winter through spring. Late summer monsoons produce thunderstorms. Nights are cool, even in summer.
[hide]Climate data for Pine Springs weather station, Texas. (Elevation 5,600 ft or 1,700 m) |
Month | Jan | Feb | Mar | Apr | May | Jun | Jul | Aug | Sep | Oct | Nov | Dec | Year |
Record high °F (°C) | 74 (23) | 76 (24) | 83 (28) | 90 (32) | 97 (36) | 105 (41) | 103 (39) | 97 (36) | 96 (36) | 90 (32) | 82 (28) | 73 (23) | 105 (41) |
Average high °F (°C) | 53.7 (12.1) | 56.0 (13.3) | 62.7 (17.1) | 70.2 (21.2) | 78.5 (25.8) | 87.1 (30.6) | 86.2 (30.1) | 84.1 (28.9) | 79.0 (26.1) | 71.9 (22.2) | 60.9 (16.1) | 53.2 (11.8) | 70.3 (21.3) |
Average low °F (°C) | 31.7 (−0.2) | 34.7 (1.5) | 39.0 (3.9) | 46.3 (7.9) | 55.6 (13.1) | 62.5 (16.9) | 63.4 (17.4) | 62.4 (16.9) | 57.5 (14.2) | 48.9 (9.4) | 39.1 (3.9) | 31.1 (−0.5) | 47.7 (8.7) |
Record low °F (°C) | 4 (−16) | 3 (−16) | 9 (−13) | 19 (−7) | 31 (−1) | 43 (6) | 50 (10) | 49 (9) | 33 (1) | 18 (−8) | 15 (−9) | 0 (−18) | 0 (−18) |
Average precipitation inches (mm) | 0.69 (17.5) | 0.80 (20.3) | 0.65 (16.5) | 0.66 (16.8) | 1.05 (26.7) | 1.62 (41.1) | 3.25 (82.6) | 3.62 (91.9) | 2.65 (67.3) | 1.58 (40.1) | 0.74 (18.8) | 0.97 (24.6) | 18.29 (464.6) |
Source: The Western Regional Climate Center[7] |
Ecology[edit]
There are three major ecosystems contained within the mountain range. First of all,
deserts exhibit
salt flats on the western side of the National Park and
creosote desert, with low elevations on the east covered with
grassland, pinyon pine (
Pinus edulis) and
junipers such as alligator juniper (
J. deppeana) and one-seeded juniper (
J. monosperma). Secondly, canyon interiors such as
McKittrick, Bear, and Pine Springs Canyon on the southeast end exhibit
maple,
ash, chinquapin oak (
Quercus muehlenbergii), and other deciduous trees. These trees are able to grow in the desert due to
springs of water recharged by wet uplands. Finally, alpine uplands known as 'The Bowl' exceeding elevations of 7,000 ft (2,100 m) are clothed with denser forests of ponderosa pine (
Pinus ponderosa), southwestern white pine (
Pinus flexilis), and
Rocky Mountain Douglas-fir(
Pseudotsuga menziesii subsp.
glauca), with small stands of
aspen.
[8]
Animals that inhabit this national parks include
elk,
gray foxes,
black bears,
coyotes,
bobcats,
striped and
hog-nosed skunks,
badgers, sixteen species of
bats,
mule deer, and
cougars. Birds of this park include
great horned owls,
chickadees,
sparrows,
barn owls,
woodpeckers,
turkey vultures,
greater roadrunners,
hummingbirds,
peregrine falcons,
golden eagles,
wrens, and
grosbeaks.
See also[edit]
References[edit]
- ^ Jump up to:a b "Listing of acreage as of December 31, 2011". Land Resource Division, National Park Service. Retrieved 2012-03-07.
- Jump up^ "NPS Annual Recreation Visits Report". National Park Service. Retrieved 2018-02-26.
- ^ Jump up to:a b National Park Service. History of Guadalupe National Park. United States Department of the Interior.
- ^ Jump up to:a b "Elevations and Distances in the United States". United States Geological Survey. April 29, 2005. Archived from the original on January 16, 2008. Retrieved 2009-03-28.
- Jump up^ "El Capitan". NGS data sheet. U.S. National Geodetic Survey. Retrieved 2008-12-28.
- Jump up^ U.S. Geological Survey Geographic Names Information System: Guadalupe Mountains National Park
- Jump up^ "Seasonal Temperature and Precipitation Information". Western Regional Climate Center. Retrieved January 6, 2014.
- Jump up^ Powell, A. Michael. Trees and Shrubs of the Trans-Pecos and Adjacent Areas. University of Texas Press. p. 91; ISBN 978-0-292-76573-3
- Jump up^ Butterfield, Mike, and Greene, Peter, Mike Butterfield's Guide to the Mountains of New Mexico, New Mexico Magazine Press, 2006, ISBN 978-0-937206-88-1
External links[edit]
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