|Chaco Culture National Historical Park|
|IUCN Category V (Protected Landscape/Seascape)|
|Location:||San Juan County, New Mexico, USA|
|Nearest city:||Farmington, New Mexico|
|Established:||March 11, 1907|
|Visitation:||45,539 (in 2005)|
|Governing body:||National Park Service|
Chaco Culture National Historical Park is a United States National Historical Park and a UNESCO World Heritage Site hosting the densest and most exceptional concentration of pueblos in the American Southwest. The 34,000-acre park is located in northwestern New Mexico, in a relatively inaccessible valley cut by the Chaco Wash. Containing the most sweeping collection of ancient ruins north of Mexico, the park preserves one of America's most fascinating cultural and historic areas.
Between 900 and 1150 C.E., Chaco Canyon was a major center of culture for the Ancient Pueblo Peoples. Chacoans quarried sandstone blocks and hauled timber from great distances, assembling 15 major complexes which remained the largest buildings in North America until the nineteenth century. Many Chacoan buildings were aligned to capture the solar and lunar cycles, requiring generations of astronomical observations and centuries of skillfully coordinated construction.
The sites are considered sacred ancestral homelands of the Hopi, Navajo, and Pueblo peoples, who continue to maintain oral traditions recounting their historical migration from Chaco and their spiritual relationship to the land. While park preservation efforts often conflict with native religious beliefs, tribal representatives work closely with the National Park Service to share their knowledge and respect the heritage of the Chacoan culture.
While we most often appreciate National Parks for their present natural beauty, Chaco is appreciated most for its mysterious past.
Chaco Canyon lies within the San Juan Basin, atop the vast Colorado Plateau, surrounded by the Chuska Mountains in the west, the San Juan Mountains to the north, and the San Pedro Mountains in the east. Ancient Chacoans relied upon their dense forests of oak, piñon, ponderosa pine, and juniper to obtain timber and other resources. The canyon itself, located within lowlands circumscribed by dune fields, ridges, and mountains, runs in a roughly northwest-to-southeast direction and is rimmed by flat massifs known as mesas. Large gaps between the southwestern cliff faces (side canyons known as rincons) were critical in funneling rain-bearing storms into the canyon, boosting local precipitation levels. The principal Chacoan complexes, such as Pueblo Bonito, Nuevo Alto, and Kin Kletso, have elevations of 6,200 to 6,440 feet (1,890 to 1,963 m).
The alluvial canyon floor, which slopes downward to the northeast at a gentle grade of 30 feet per mile (6 meters per kilometer), is bisected by the Chaco Wash, an arroyo that only infrequently carries water. Of the canyon's aquifers, the largest are located at a depth that precluded the ancient Chacoans from tapping their groundwater; only a few smaller, shallower sources supported small springs. Significant surface water is virtually non-existent except in the guise of storm runoff flowing intermittently through arroyos.
Chaco Canyon's flora is typical of that found in the high deserts of North America: sagebrush and several species of cactus are interspersed with dry scrub forests of piñon and juniper, the latter primarily on mesa tops. The canyon receives less precipitation than many other parts of New Mexico located at similar latitudes and elevations; consequently, it does not have the temperate coniferous forests that are plentiful in areas to the east. The prevailing sparseness of both plants and wildlife was echoed in ancient times, when overpopulation, expanding cultivation, overhunting, habitat destruction, and drought may have led the Chacoans to strip the canyon of wild plants and game. As such, even during wet periods, the canyon was only able to sustain around 2,000 people.
The canyon's most notable mammalian species include the coyote, mule deer, elk, and antelope. Important smaller carnivores include the bobcats, badgers, foxes, and two species of skunk. The park hosts abundant populations of rabbits, porcupines, rodents—including several prairie dog towns—and small colonies of bats, which are present during the summer.
The canyon is able to support relatively few bird species due to its short supply of water. Roadrunners, large hawks (such as Cooper's Hawks and American Kestrels), owls, vultures, and ravens are some of the larger birds that make their home there. Sizeable populations of smaller birds, including warblers, sparrows, and house finches are common. Three species of hummingbirds are present, including the tiny Rufous Hummingbird who competes with the more mild-tempered Black-chinned Hummingbirds for breeding habitat in shrubs or trees located near water. Western (prairie) Rattlesnakes are occasionally seen in the backcountry, though various lizards and skinks are far more abundant.
An arid region of high scrubland and desert steppe, the canyon and wider basin average 8 inches (20 cm) of rainfall annually; the park averages 9.1 inches (231.1 mm). Chaco Canyon lies on the leeward side of extensive mountain ranges to the south and west, resulting in a rainshadow effect that leads to the prevailing lack of moisture in the region. Four distinct seasons define the region, with rainfall most likely between July and September; May and June are the driest months. Orographic precipitation, resulting from moisture wrung out of storm systems ascending mountain ranges around Chaco Canyon, is responsible for most precipitation in both summer and winter; rainfall increases with higher elevation.
The Chaco Canyon area is also characterized by remarkable climatic extremes: recorded temperatures range between −38 °F (−39 °C) to 102 °F (39 °C), and temperature swings of up to 60 °F in a single day are not unknown. The region averages less than 150 days without frost per year, and the local climate can swing wildly from years of plentiful rainfall to extended droughts. The heavy influence of the El Niño-Southern Oscillation phenomenon on the canyon's weather contributes to the extreme climatic variability.
After the supercontinent of Pangaea split apart during the Cretaceous period, the region became part of a shifting transition zone between a shallow inland sea, the Western Interior Seaway, and a band of plains and low hills to the west. A sandy and swampy coastline repeatedly shifted east and west, alternately submerging and uncovering the canyon's portion of what is now the Colorado Plateau.
As the Chaco Wash flowed across the upper strata of what is now the 400-foot (122 m) Chacra Mesa, it cut into it, gouging out the broad canyon over the course of millions of years. The mesa itself comprises sandstone and shale formations dating from the late Cretaceous, which are of the Mesa Verde formation. The canyon's bottomlands were later further eroded, exposing Menefee Shale bedrock; this was subsequently buried under approximately 125 feet (38 m) of deposited sediment. The canyon and mesa lie within the "Chaco Core," distinct from the wider Chaco Plateau; it is a relatively flat region of grassland with infrequent and interspersed stands of trees. Especially because the Continental Divide is only 15.5 miles (25 km) west of the canyon, geological characteristics and different patterns of drainage differentiate these two regions both from each other and from the nearby Chaco Slope, the Gobernador Slope, and the Chuska Valley.
Archaeologists identify the first people in the broader San Juan Basin as hunter-gatherers designated as the Archaic; they in turn descended from nomadic Clovis hunters who arrived in the Southwest around 10,000 B.C.E. By approximately 900 B.C.E., these people lived at sites such as Atlatl Cave. The Archaic people left very little evidence of their presence in Chaco Canyon itself. However, by approximately 490 C.E., their descendants, designated as Basketmakers, were continuously farming within the canyon, living in Shabik'eshchee Village and other pithouse settlements.
A small population of Basketmakers remained in the Chaco Canyon area and developed through several cultural stages until around 800, when they were building crescent-shaped stone complexes, each comprising four to five residential suites abutting subterranean kivas, large enclosed areas set aside for religious observances and ceremonies. These structures have been identified as characteristic of the Early Pueblo People. By 850, the Pueblo population, also known as the "Anasazi," had rapidly expanded, with members residing in larger, denser pueblos. There is strong evidence of a canyon-wide turquoise processing and trading industry dating from the tenth century. At this time, the first section of the massive Pueblo Bonito complex was built, beginning with a curved row of 50 rooms near its present north wall.
The cohesive system that characterized Chacoan society began disintegrating around 1140, perhaps in response to a severe 50-year drought that began in 1130; chronic climatic instability, including a series of severe droughts, again struck the region between 1250 and 1450. Other factors included water management patterns (leading to arroyo cutting) and deforestation. Outlying communities began to disappear and, by the end of the century, the buildings in the central canyon had been carefully sealed and abandoned. Archaeological and cultural evidence leads scientists to believe people from this region migrated south, east, and west into the valleys and drainages of the Little Colorado River, the Rio Puerco, and the Rio Grande.
Numic-speaking peoples, such as the Ute and Shoshone, were present on the Colorado Plateau beginning in the twelfth century. Nomadic Southern Athabaskan speaking peoples, such as the Apache and Navajo, succeeded the Pueblo people in this region by the fifteenth century; in the process, they acquired Chacoan customs and agricultural skills. Ute tribal groups also frequented the region, primarily during hunting and raiding expeditions. The modern Navajo Nation lies west of Chaco Canyon, and many Navajo live in surrounding areas. The arrival of the Spanish in the seventeenth century inaugurated an era of subjugation and rebellion, with the Chaco Canyon area absorbing Puebloan and Navajo refugees fleeing Spanish rule. In succession, as first Mexico, then the U.S., gained sovereignty over the canyon, military campaigns were launched against the region's remaining inhabitants.
The trader Josiah Gregg was, in 1832, the first to write about the ruins of Chaco Canyon, referring to Pueblo Bonito as "built of fine-grit sandstone." In 1849, a U.S. Army detachment passed through and surveyed the ruins. The location was so remote, however, that over the next 50 years the canyon was scarcely visited. After a brief reconnaissance by Smithsonian scholars in the 1870s, formal archaeological work began in 1896, when a party from the American Museum of Natural History (the Hyde Exploring Expedition) began excavating in Pueblo Bonito. They spent five summers in the region, sent over 60,000 artifacts back to New York, and operated a series of trading posts.
In 1901 Richard Wetherill, who worked for the Hyde brothers and their expedition, claimed a homestead of 161 acres of land that included Pueblo Bonito, Pueblo del Arroyo, and Chetro Ketl. While investigating Wetherill's land claim, federal land agent Samuel J. Holsinger reported the physical setting of the canyon and the sites, noted prehistoric road segments and stairways above Chetro Ketl, and documented prehistoric dams and irrigation systems. His report (which went unpublished) strongly recommended the creation of a national park to encompass and preserve Chacoan sites. The next year, Edgar Lee Hewett, who was president of New Mexico Normal University, mapped many Chacoan sites. Hewett and others helped to enact the Federal Antiquities Act of 1906, which was the first U.S. law protecting antiquities; it was, in effect, a direct consequence of controversy surrounding Wetherill's activities in the Chaco Canyon area. The Act also allowed the President to establish national monuments. President Theodore Roosevelt thus proclaimed Chaco Canyon National Monument on March 11, 1907; Wetherill relinquished his claim on several parcels of land he held in Chaco Canyon.
In 1949, Chaco Canyon National Monument was expanded with lands deeded from the University of New Mexico. In return, the university maintained scientific research rights to the area. By 1959, the National Park Service had constructed a park visitor center, staff housing, and campgrounds. As a historic property of the National Park Service, the National Monument was listed on the National Register of Historic Places on October 15, 1966. In 1971, researchers Robert Lister and James Judge established the Chaco Center, a division for cultural research that functioned as a joint project between the University of New Mexico and the National Park Service. A number of multi-disciplinary research projects, archaeological surveys, and limited excavations began during this time. The Chaco Center extensively surveyed the Chacoan roads, well-constructed paths radiating from the central canyon. The results from such research conducted at Pueblo Alto and other sites dramatically altered accepted academic interpretations of both the Chacoan culture and the Four Corners region of the American Southwest.
The richness of the cultural remains at park sites led to the expansion of the small National Monument into the Chaco Culture National Historical Park on December 19, 1980, when an additional 13,000 acres (53 km²) were added to the protected area. In 1987, the park was designated a World Heritage Site by UNESCO. To safeguard Chacoan sites on adjacent Bureau of Land Management and Navajo Nation lands, the Park Service developed the multi-agency Chaco Culture Archaeological Protection Site program. These initiatives have detailed the presence of more than 2,400 archeological sites within the current park's boundaries; only a small percentage of these have been excavated.
The Chacoans built their complexes along a nine-mile (14 km) stretch of canyon floor, with the walls of some structures aligned cardinally and others aligned with the 18.6-year cycle of minimum and maximum moonrise and moonset.
Immense complexes known as "Great Houses" were key centers exemplifying Chacoan architectural and worship styles. Although forms evolved as the centuries passed, the houses maintained several core characteristics. Most notable is their sheer bulk; most complexes in Chaco Canyon averaged more than 200 rooms each, with some reaching up to 700 rooms. The sizes of individual rooms were also substantial, with high ceilings when compared to buildings erected in preceding Anasazi periods. They were also well-planned, with vast sections or wings erected in a single stage, rather than in increments.
Ceremonial structures known as kivas were built in proportion to the number of rooms in a pueblo. On average, one small kiva was built for every 29 rooms. Nine complexes also each hosted an oversized Great Kiva, which could range up to 63 feet (19 m) in diameter. All Chacoan kivas share distinctive architectural features, including T-shaped doorways and stone lintels.
Nine Great Houses are positioned along the north side of Chaco Wash, at the base of massive sandstone mesas. Other Great Houses are found on mesa tops or in nearby washes and drainage areas. There are 14 recognized Great Houses, which are grouped below according to geographic positioning with respect to the canyon.
The central portion of the canyon contains the largest Chacoan complexes.
In Chaco Canyon's northern reaches lies another cluster of Great Houses.
Directly north are communities that are even more remote, including Salmon Ruins and Aztec Ruins, which are located along the San Juan and Animas Rivers near Farmington; these were built during a 30-year wet period that began in 1100. Located 60 miles (100 km) directly south of Chaco Canyon, on the Great South Road, lies another cluster of outlying communities. The largest of these is Kin Nizhoni, which stands atop a 7,000-foot (2,100 m) mesa surrounded by marsh-like bottomlands.
The park also provides other activities in addition to exploration of the ruins.
Open from April to October, the Chaco Night Sky Program presents astronomy programs and telescope viewing of the spectacular dark night sky.
United States World Heritage Periodic Report: Chaco Culture National Historical Park (Section II). Retrieved June 23, 2007.
All links retrieved January 25, 2017.
|National Historical Parks of the United States|
|Adams • Appomattox Court House • Boston • Cane River Creole • Cedar Creek and Belle Grove • Chaco Culture • Chesapeake and Ohio Canal • Colonial • Cumberland Gap • Dayton Aviation Heritage • George Rogers Clark • Harpers Ferry • Hopewell Culture • Independence • Jean Lafitte • Kalaupapa • Kaloko-Honokohau • Keweenaw • Klondike Gold Rush • Lewis and Clark • Lowell • Lyndon B. Johnson • Marsh-Billings-Rockefeller • Minute Man • Morristown • Natchez • New Bedford Whaling • New Orleans Jazz • Nez Perce • Pecos • Pu'uhonua o Honaunau • Rosie the Riveter/World War II Home Front • Salt River Bay • San Antonio Missions • San Francisco Maritime • San Juan Island • Saratoga • Sitka • Tumacácori • Valley Forge • War in the Pacific • Women's Rights|
Cahokia | Carlsbad Caverns | Chaco Culture | Everglades | Grand Canyon | Great Smoky Mountains | Hawaii Volcanoes | Independence Hall | Kluane / Wrangell-St. Elias / Glacier Bay / Tatshenshini-Alsek (w/ Canada) | La Fortaleza and San Juan National Historic Site, Puerto Rico | Mammoth Cave | Mesa Verde | Monticello and University of Virginia | Olympic | Pueblo de Taos | Redwood | Statue of Liberty | Waterton Glacier International Peace Park (w/ Canada) | Yellowstone | Yosemite
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