Mesa Verde National Park
|Mesa Verde National Park|
Mesa Verde from the northeast
|Location||Montezuma County, Colorado,
|Area||52,485 acres (21,240 ha)|
|Established||June 29, 1906|
|Visitors||572,329 (in 2011)|
|Governing body||National Park Service|
|Designated||1978 (2nd session)|
|State Party||United States|
|Region||Europe and North America|
|Designated||October 15, 1966|
Mesa Verde National Park is a U.S. National Park and UNESCO World Heritage Site located in Montezuma County, Colorado. It protects some of the best preserved Ancestral Puebloan archeological sites in the United States.
The park was created by President Theodore Roosevelt in 1906. It occupies 52,485 acres (21,240 ha) near the Four Corners region, and with more than 4,000 sites and 600 cliff dwellings, it is the largest archeological preserve in the US. Mesa Verde (Spanish for "green table") is best known for structures such as Cliff Palace, thought to be the largest cliff dwelling in North America.
Starting c. 7,500 BCE, Mesa Verde was seasonally inhabited by a group of nomadic Paleo-Indians known as the Foothills Mountain Complex. The variety of projectile points found in the region indicates they were influenced by surrounding areas, including the Great Basin, the San Juan Basin, and the Rio Grande Valley. Later, Archaic people established semi-permanent rockshelters in and around the mesa. By 1,000, the Basketmaker culture emerged from the local Archaic population, and by 500 CE the Ancestral Puebloans had developed from the Basketmaker culture.
The Mesa Verdeans survived by utilizing a combination of hunting, gathering, and subsistence farming of crops such as corn, beans, and squash. They built the mesa's first pueblos sometime after 650, and by the end of the 12th century they began to construct the massive cliff dwellings for which the park is best known. By 1285, following a period of social and environmental instability driven by a series of severe and prolonged droughts, they abandoned the area and moved south to locations in Arizona and New Mexico, including Rio Chama, Pajarito Plateau, and Santa Fe.
- 1 Background
- 2 Rediscovery
- 3 National Park
- 4 Geology
- 5 Geography and anthropogenic ecology
- 6 Climate
- 7 Key sites
- 8 Image gallery
- 9 See also
- 10 References
- 11 Further reading
- 12 External links
The first occupants of the Mesa Verde region, which spans from southeastern Utah to northwestern New Mexico, were nomadic Paleo-Indians who arrived in the area c. 9,500 BCE. They followed herds of big game and camped near rivers and streams, many of which dried up as the glaciers that once covered parts of the San Juan Mountains receded. The earliest Paleo-Indians were the Clovis culture and Folsom tradition, defined largely by the way in which they fashioned projectile points. Although they left evidence of their presence throughout the region, there is little indication that they lived in central Mesa Verde during this time.
After 9,600 the area's environment grew warmer and drier, which brought pine forests and the animals that thrive in them to central Mesa Verde. Paleo-Indians began inhabiting the mesa in increasing numbers c. 7500, though it is unclear whether they were seasonal occupants or year-round residents. Development of the atlatl during this period made it easier for them to hunt smaller game, a crucial advance at a time when most of the region's big game had disappeared from the landscape.
6,000 BCE marks the beginning of the Archaic period in North America. Archeologists differ as to the origin of the Mesa Verde Archaic population; some believe they developed exclusively from local Paleo-Indians, called the Foothills Mountain Complex, but others suggest that the variety of projectile points found in Mesa Verde indicates influence from surrounding areas, including the Great Basin, the San Juan Basin, and the Rio Grande Valley. The Archaic people probably developed locally, but were also influenced by contact, trade, and intermarriage with immigrants from these outlying areas.
The early Archaic people living near Mesa Verde utilized the atlatl and harvested a wider variety of plants and animals than the Paleo-Indians had, but retained their primarily nomadic lifestyle. They inhabited the outlying areas of the Mesa Verde region, but also the mountains, mesa tops, and canyons, where they created rockshelters and rock art, and left evidence of animal processing and chert knapping. Environmental stability during the period drove population expansion and migration. Significant warming and drying from 5,000 to 2,500 might have led middle Archaic people to seek the cooler climate of Mesa Verde, whose higher elevation brought increased snowpack that, when coupled with spring rains, provided relatively plentiful amounts of water.
By the late Archaic more people were living in semi-permanent rockshelters, which preserved perishable goods such as baskets, sandals, and mats. They started to make a variety of twig figurines that usually resembled sheep or deer. The late Archaic is marked by increased trade in exotic materials such as obsidian and turquoise. Marine shells and abalone from the Pacific coast made their way to Mesa Verde from Arizona, and the Archaic people worked them into necklaces and pendants. Rock art flourished, and people lived in rudimentary houses made of mud and wood. They also made early attempts at plant domestication that would eventually develop into the sustained agriculture that marked the end of the Archaic period, c. 1000.
With the introduction of corn to the Mesa Verde region c. 1000 BCE and the trend away from nomadism toward permanent pithouse settlements, the Archaic Mesa Verdeans transitioned into what archeologists call the Basketmaker culture. Basketmaker II people are characterized by their combination of foraging and farming skills, use of the atlatl, and creation of finely woven baskets in the absence of earthen pottery. By 300, corn had become the preeminent staple of the Basketmaker II people's diet, which relied less and less on wild food sources and more on domesticated crops.[a]
In addition to the fine basketry for which they were named, Basketmaker II people fashioned a variety of household items from plant and animal materials, including sandals, robes, pouches, mats, and blankets. They also made clay pipes and gaming pieces. Basketmaker men were relatively short and muscular, averaging less than 5.5 feet (1.7 m) tall. Their skeletal remains reveal signs of hard labor and extensive travel, including degenerative joint disease, healed fractures, and moderate anemia associated with iron deficiency. They buried the dead near or amongst their settlements, and often included luxury items as gifts, which might indicate differences in relative social status. Basketmaker II people are also known for their distinctive rock art, which can be found throughout Mesa Verde. They depicted animals and people, in both abstract and realistic forms, in single works and more elaborate panels. A common subject was the hunchbacked flute player that the Hopi call Kokopelli. Modern Hopi have interpreted the petroglyphs at Mesa Verde's Petroglyph Point as depictions of various clans of people.
By 500 CE atlatls were being supplanted by the bow and arrow and baskets by pottery, marking the end of the Basketmaker II Era and the beginning of the Basketmaker III Era.[b] Year-round settlements first appear at the beginning of the 7th century. The population of the San Juan Basin increased markedly after 575, when there were very few Basketmaker III sites in Mesa Verde; by the early 600s there were many such sites in the mesa. For the next 150 years villages typically consisted of small groups of one to three residences. The population of Mesa Verde c. 675 was approximately 1,000 to 1,500 people.
Beans and new varieties of corn were introduced to the region c. 700. By 775, some settlements had grown to accommodate more than one hundred people; the construction of large, above ground storage buildings began around this time. Basketmakers endeavored to store enough food for their family for one year, but also retained residential mobility so they could quickly relocate their dwellings in the event of resource depletion or consistently inadequate crop yields. By the end of the 8th century, the smaller hamlets, which were typically occupied for ten to forty years, had been supplanted by larger ones that saw continuous occupation for as many as two generations. Basketmaker III people established a tradition of holding large ceremonial gatherings near community pit structures.
Pueblo I: 750 to 900
750 marks the end of the Basketmaker III Era and the beginning of the Pueblo I Era. The transition is characterized by significant changes in the design and construction of buildings and the organization of household activities. Pueblo I people doubled their capacity for food storage from one year to two and built interconnected, year-round residences called pueblos. Household activities that had previously been reserved for pithouses were moved to the new dwellings; this changed the function of pithouses from multi-purpose spaces to ones used primarily for ceremonies. During the late 8th century, Mesa Verdeans started building square pit structures that archeologists call protokivas. They were typically 3 or 4 feet (0.91 or 1.22 m) deep and 12 to 20 feet (3.7 to 6.1 m) in diameter.
The first pueblos appeared at Mesa Verde sometime after 650; by 850 more than half of Mesa Verdeans lived in them. As local populations grew, Puebloans found it difficult to survive on hunting, foraging, and gardening, which made them increasingly reliant on domesticated corn. This shift from semi-nomadism to a "sedentary and communal way of life changed ancestral Pueblo society forever". Within a generation the average number of households in these settlements grew from one to three to fifteen to twenty, with average populations of two hundred people. Population density increased dramatically, with as many as a dozen families occupying roughly the same space that had formerly housed two. This brought increased security against raids and encouraged greater cooperation amongst residents. It also facilitated trade and intermarriage between clans, and by the late 8th century, as Mesa Verde's population was being augmented by settlers from the south, four distinct cultural groups occupied the same villages.
Large Pueblo I settlements laid claim to the resources found within 15 to 30 square miles (39 to 78 km2). They were typically organized in groups of at least three and spaced about 1 mile (1.6 km) apart. By 860, there were approximately 8,000 people living in Mesa Verde. Within the plazas of larger villages, the Pueblo I people dug massive pit structures of 800 square feet (74 m2) that became central gathering places. These structures represent early architectural expressions of what would eventually develop into the Pueblo II Era great houses of Chaco Canyon. Despite robust growth during the early and mid-9th century, unpredictable rainfall and periodic drought led to a dramatic reversal of settlement trends in the area. Many late Pueblo I villages were abandoned after less than forty years of occupation. By 880, Mesa Verde's population was in steady decline. The beginning of the 10th century saw widespread depopulation of the region, as people emigrated south of the San Juan River to Chaco Canyon in search of reliable rains for farming. As Mesa Verdeans migrated south, to where many of their ancestors had emigrated two hundred years before, the influence of Chaco Canyon grew, and by 950 Chaco had supplanted Mesa Verde as the region's cultural center.
Pueblo II: 900 to 1150
The Pueblo II Era is marked by the growth and outreach of communities centered around the great houses of Chaco Canyon. Despite their participation in the vast Chacoan system, Mesa Verdeans retained a distinct cultural identity while melding regional innovation with ancient tradition, inspiring further architectural advancements; the 9th century Mesa Verdean pueblos influenced two hundred years of Chacoan great house construction. Droughts during the late 9th century rendered Mesa Verdean dry land farming unreliable, which led to their growing crops only near drainages for the next 150 years. During the early 11th century, crop yields returned to healthy levels. By 1050 the population of Mesa Verde began to rebound, as agricultural prosperity increased and people returned from the south. 
Mesa Verdean farmers increasingly relied on masonry reservoirs during the Pueblo II Era. During the 11th century, they built check dams and terraces near drainages and slopes in an effort to conserve soil and runoff. These fields offset the danger of crop failures in the larger dry land fields. By the mid-10th and early 11th centuries, protokivas had evolved into smaller circular structures called kivas, which were usually 12 to 15 feet (3.7 to 4.6 m) across. These Mesa Verde-style kivas included a feature from earlier times called a sipapu, which is a hole dug in the north of the chamber that symbolizes the Ancestral Puebloan's place of emergence from the underworld. During this period, Mesa Verdeans began to move away from the post and mud jacal-style buildings that marked the Pueblo I Era toward masonry construction, which had been utilized in the region as early as 700, but was not widespread until the 11th and 12th centuries. Chacoan influence manifested in the form of Chaco-style great houses that became the focal point of many Mesa Verdean villages after 1075. These timber-and-earth Pueblo II dwellings were typically inhabited for about twenty years. During the early 12th century, the locus of regional control shifted away from Chaco to Aztec, New Mexico, in the southern Mesa Verde region.[c] By 1150, drought had once again stressed the region's inhabitants, leading to a temporary cessation of great house construction at Mesa Verde.
Pueblo III: 1150 to 1300
A severe drought from 1130 to 1180 caused rapid depopulation in many parts of the San Juan Basin, particularly at Chaco Canyon. As the extensive Chacoan system collapsed, people increasingly migrated to Mesa Verde, causing significant population growth in the area. This led to much larger settlements of six to eight hundred people, which reduced mobility for Mesa Verdeans, who had in the past frequently relocated their dwellings and fields as part of their agriculture strategy. In order to sustain these larger populations, they dedicated more and more of their labor to farming. Population increases also led to expanded tree felling that reduced habitat for many wild plant and animal specie that the Mesa Verdeans had replied on, further deepening their dependency on domesticated crops that were susceptible to drought-related failure.
The Chacoan system brought large quantities of imported goods to Mesa Verde during the late 11th and early 12th centuries, including pottery, shells, and turquoise, but by the late 12th century, as the system collapsed, the amount of goods imported by the mesa quickly declined, and Mesa Verde became isolated from the surrounding region. For approximately six hundred years, most Mesa Verdean farmers lived in small, mesa-top homesteads of one or two families. They were typically located near their fields and walking distance to sources of water. This practice continued into the mid- to late 12th century, but by the start of the 13th century they began living in canyon locations that were close to water sources and within walking distance of their fields.
Mesa Verdean villages thrived during the mid-Pueblo III Era, when architects constructed impressive multi-story buildings and artisans adorned pottery with elaborate designs. Structures built during this period have been described as "among the world's greatest archaeological treasures". Pueblo III masonry buildings were usually occupied for approximately fifty years, more than double the usable lifespan of the Pueblo II jacal structures. Others were continuously inhabited for two hundred years or more. Architectural innovations such as towers and multi-walled structures also appear during the Pueblo III Era. Mesa Verde's population remained fairly stable during the 12th century drought. At the start of the 13th century, approximately 22,000 people lived there. The area saw moderate population increases during the following decades, and dramatic ones from 1225 to 1260. Most of the people in the region lived in the plains west of the mesa at locations such as Yellow Jacket Pueblo, near Cortez, Colorado. Others colonized canyon rims and slopes in multi-family structures that grew to unprecedented size as populations swelled. By 1260, the majority of Mesa Verdeans lived in large pueblos that housed several families and more than one hundred people.
The 13th century saw 69 years of below average rainfall in the Mesa Verde region, and after 1270 the area suffered from especially cold temperatures. Dendrochronology indicates that the last tree felled for construction on the mesa was cut in 1281. There was a significant decline in ceramic imports to the region during this time, but local production remained steady. Despite challenging conditions, the Puebloans continued to farm the area until a severely dry period from 1276 to 1299 ended seven hundred years of continuous human occupation at Mesa Verde. The last inhabitants of the mesa left the area c. 1285.
Warfare and migration
Evidence of violence and cannibalism dating to the mid-12th century has been found in the central Mesa Verde region. Periodic warfare occurred on the mesa throughout the 13th century. Economic and social uncertainty during the century's final decades led to widespread conflict. Evidence of partly burned villages and post-mortem trauma has been uncovered, and the residents of one village appear to have been the victims of a site-wide massacre. While most of the violence, which peaked between 1275 and 1285, is generally ascribed to in-fighting amongst Mesa Verdeans, archeological evidence found at Sand Canyon Pueblo, in Canyons of the Ancients National Monument, suggests that violent interactions also occurred between Mesa Verdeans and people from outside the region.
After 1260, there was a rapid depopulation of Mesa Verde, as "tens of thousands of people" emigrated or died from starvation. Many smaller communities in the Four Corners region were also abandoned during this period. The Ancestral Puebloans had a long history of migration in the face of environmental instability, but the depopulation of Mesa Verde at the end of the 13th century was different in that the region was almost completely emptied, and no descendants returned to build permanent settlements.
After leaving Mesa Verde, many people relocated to southern Arizona and New Mexico. Although the rate of settlement is unclear, significant increases in previously sparsely populated areas such as Rio Chama, Pajarito Plateau, and Santa Fe, New Mexico, correspond directly with the period of migration from Mesa Verde. Archeologists believe the Mesa Verdeans who settled in the areas near the Rio Grande, where Mesa Verde Black-on-white pottery became widespread during the 14th century, were likely related to the households they joined and not unwelcome intruders. Archeologists view this migration as a continuation, versus a dissolution, of Ancestral Puebloan society and culture.
Mesa Verde is best known for a large number of well-preserved cliff dwellings, houses built in alcoves, or rock overhangs along the canyon walls. The structures contained within these alcoves were mostly blocks of hard sandstone, held together and plastered with adobe mortar. Specific constructions had many similarities but were generally unique in form due to the individual topography of different alcoves along the canyon walls. In marked contrast to earlier constructions and villages on top of the mesas, the cliff dwellings of Mesa Verde reflected a region-wide trend towards the aggregation of growing regional populations into close, highly defensible quarters during the 13th century.
Pueblo buildings were built with stone, windows facing south, and in U, E and L shapes. The buildings were located more closely together and reflected deepening religious celebration. Towers were built near kivas and likely used for lookouts. Pottery became more versatile, including pitchers, ladles, bowls, jars and dishware for food and drink. White pottery with black designs emerged, the pigments coming from plants. Water management and conservation techniques, including the use of reservoirs and silt-retaining dams, also emerged during this period. Decorative motifs for these sandstone/mortar constructions, both surface and cliff dwellings, included T-shaped windows and doors. This has been taken by some archaeologists, such as Stephen H. Lekson, as evidence of the continuing reach of the Chacoan system. Other researchers see these motifs as part of a more generalized Puebloan style and/or spiritual significance, rather than evidence of a continuing specific elite socioeconomic system.
While much of the construction in these sites is consistent with common Pueblo architectural forms, including kivas, towers, and pit-houses, the space constrictions of these alcoves necessitated what seems to have been a far denser concentration of their populations. Mug House, a typical cliff dwelling of the period, was home to around 100 people who shared 94 small rooms and eight kivas built against each other and sharing many of their walls; builders in these areas maximized space in any way they could, with no areas considered off-limits to construction.
Starting in the 6th century, the farmers living in central Mesa Verde cultivated corn, beans, squash, and gourds. The combination of corn and beans provided the Mesa Verdeans with the amino acids of a complete protein. When conditions were good, 3 or 4 acres (1.2 or 1.6 ha) of land would provide enough food for a family of three or four individuals for one year, providing they supplemented with game and wild plants. As Mesa Verdeans increasingly relied on corn as a dietary staple, the success or failure of crop yields factored heavily into their lives. The mesa tilts slightly to the south, which increased its exposure to the sun.
The majority of Mesa Verdeans practiced dry farming, which relied on rain to water their crops, but others utilized runoff, springs, seeps, and natural collection pools. Starting in the 9th century, they dug and maintained reservoirs that caught runoff from summer showers and spring snowmelt; some crops were watered by hand.
Hunting and foraging
The Mesa Verdeans harvested primarily local small game, but sometimes organized hunting parties that traveled long distances. Their main source of animal protein came from mule deer and rabbits, but they also ate domesticated turkeys. They occasionally hunted Bighorn sheep, antelope, and elk. They wove blankets from turkey feathers and rabbit fur, and made implements such as awls and needles from turkey and deer bones. Despite the availability of fish in the area's rivers and streams, archeological evidence suggests that Mesa Verdeans rarely if ever ate or caught them.
Mesa Verde's Puebloans supplemented their diet by gathering the seeds and fruits of wild plants. They sometimes searched large expanses of land while procuring these resources. Depending on the season, they collected piñon nuts and juniper berries, weedy goosefoot, pigweed, purslane, tomatillo, tansy mustard, globe mallow, sunflower seeds, and yuka, as well as various specie of grass and cacti. Prickly pear fruits provided a rare source of natural sugar. Wild seeds were cooked and ground up into porridge. They used sagebrush and mountain mahogany, along with piñon and juniper, for firewood. They also smoked wild tobacco.
Neutron activation analysis indicates that much of the Black-on-white pottery found at Mesa Verde was produced locally. Cretaceous clays from both the Dakota and Menefee Formations were used in Black-on-white wares, and Mancos Formation clays for corrugated jars. Evidence that pottery of both types moved between several locations around the Mesa Verde region suggests interaction between groups of ancient potters, or they might have shared a common source of raw materials.
The Mesa Verde Black-on-white pottery was produced at three locations: Sand Canyon, Castle Rock, and Mesa Verde. Because the corrugated wares were probably made using clay from formations other than Menefee, this suggests the ancient potters selected different clays for different styles. Another interpretation is that all corrugated wares were produced at a location where no Black-on-white pottery was fired.
The area in and around Mesa Verde had been home to the Utes. In 1868, a treaty between the United States government and the Ute tribe recognized Ute ownership of Colorado land by identifying land west of the Continental Divide as Ute land. After there had become an interest in land in western Colorado, a new treaty in 1873 left the Ute with a strip of land in southwestern Colorado between the border with New Mexico and 15 miles north. Most of Mesa Verde lies within this strip of land. The Ute wintered in the warm, deep canyons and found sanctuary there and the high plateaus of Mesa Verde. Believing the cliff dwellings to be sacred ancestral sites, they did not live in the ancient dwellings.
Mexican-Spanish missionaries and explorers Francisco Atanasio Domínguez and Silvestre Vélez de Escalante, seeking a route from Santa Fe to California, faithfully recorded their travels in 1776. They reached the Mesa Verde (green plateau) region, which they named after its high, tree-covered plateaus, but they never got close enough, or into the needed angle, to see the ancient stone villages. They were the first white men to travel the route through much of the Colorado Plateau into Utah and back through Arizona to New Mexico.
Occasional trappers and prospectors visited, with one prospector, John Moss, making his observations known in 1873. The following year, Moss led eminent photographer William Henry Jackson through Mancos Canyon, at the base of Mesa Verde. There, Jackson both photographed and publicized a typical stone cliff dwelling. In 1875, geologist William H. Holmes retraced Jackson's route.
Reports by both Jackson and Holmes were included in the 1876 report of the Hayden Survey, one of the four federally financed efforts to explore the American West. These and other publications led to proposals to study Southwestern archeological sites systematically.
Virginia McClurg, a journalist for the New York Daily Graphic, visited Mesa Verde in 1882 and 1885 in her quest to find Ancestral Puebloan settlements. In 1885, her party found Echo Cliff House, Three Tier House and Balcony House, and these findings induced her future work to protect the dwellings and artifacts.
A family of cattle ranchers, the Wetherills, befriended members of the Ute tribe near their ranch southwest of Mancos, Colorado. With the Ute tribe's approval, the Wetherills were allowed to bring cattle into the lower, warmer plateaus of the present Ute Mountain Ute Tribe in the winter. Word had spread of the dwellings of Ancestral Puebloans. Acowitz, a member of the Ute tribe, told the Wetherills of a special dwelling in Mesa Verde: "Deep in that canyon and near its head are many houses of the old people – the Ancient Ones. One of those houses, high, high in the rocks, is bigger than all the others. Utes never go there, it is a sacred place." On December 18, 1888, Richard Wetherill and Charlie Mason, cowboys from Mancos, found Cliff Palace in Mesa Verde after spotting the ruins from the top of the mesa. Wetherill gave the ruin its present-day name. Richard Wetherill, family and friends explored the ruins and gathered artifacts, some of which they sold to the Historical Society of Colorado and much of which they kept. Among the people who stayed with the Wetherills and explored the cliff dwellings was mountaineer, photographer, and author Frederick H. Chapin, who visited the region during 1889 and 1890. He described the landscape and ruins in an 1890 article and later in an 1892 book, The Land of the Cliff-Dwellers, which he illustrated with hand-drawn maps and personal photographs.
The Wetherills also hosted Gustaf Nordenskiöld, the son of polar explorer Adolf Erik Nordenskiöld, in 1891. Nordenskiöld was a trained mineralogist who introduced scientific methods to artifact collection, recorded locations, photographed extensively, diagrammed sites, and correlated what he observed with existing archeological literature as well as the home-grown expertise of the Wetherills.He removed a lot of artifacts and sent them to Sweden, where they eventually went to the National Museum of Finland. Nordenskiöld published, in 1893, The Cliff Dwellers of the Mesa Verde. When Nordenskiöld shipped the collection that he made of Mesa Verde artifacts, the event initiated concerns about the need to protect Mesa Verde land and its resources.
In 1886, a Denver Tribune Republican article printed on December 12, 1886, was the first known suggestion to create a National Park around the archeological site. In 1889, Goodman Point Pueblo became the first pre-Columbian archeological site in the Mesa Verde region to gain federal protection. It was the first such site to be protected in the US. Virginia McClurg was diligent in her efforts between 1887 and 1906 to inform the United States and European community of the importance of protecting the important historical material and dwellings in Mesa Verde. Her efforts included enlisting support from 250,000 women through the Federation of Women's Clubs, writing and having published poems in popular magazines, giving speeches domestically and internationally, and forming the Colorado Cliff Dwellers Association. The Colorado Cliff Dwellers' purpose was to protect the resources of Colorado cliff dwellings, reclaiming as much of the original artifacts as possible and sharing information about the people who dwelt there. A fellow activist for protection of Mesa Verde and prehistoric archeological sites included Lucy Peabody, who, located in Washington, D.C., met with members of Congress to further the cause.
Former Mesa Verde National Park superintendent Robert Heyder communicated his belief that the park might have been far more significant with the hundreds of artifacts taken by Nordenskiöld.
By the end of the 19th century, it was clear that Mesa Verde needed protection from people in general who came to Mesa Verde and created or sold their own collection of artifacts. In a report to the Secretary of the Interior, Smithsonian Institution Ethnologist J. Walter Fewkes described vandalism at Mesa Verde's Cliff Palace:
Parties of "curio seekers" camped on the ruin for several winters, and it is reported that many hundred specimens there have been carried down the mesa and sold to private individuals. Some of these objects are now in museums, but many are forever lost to science. In order to secure this valuable archeological material, walls were broken down [...] often simply to let light into the darker rooms; floors were invariably opened and buried kivas mutilated. To facilitate this work and get rid of the dust, great openings were broken through the five walls which form the front of the ruin. Beams were used for firewood to so great an extent that not a single roof now remains. This work of destruction, added to that resulting from erosion due to rain, left Cliff Palace in a sad condition.
Many artefacts from Mesa Verde are now located in museums and private collections in the USA and across the world. A representative selection of pottery vessels and other objects, for example, is now in the British Museum in London.
In 1906, President Teddy Roosevelt approved creation of the Mesa Verde National Park and the Federal Antiquities Act of 1906. The park was an effort to "preserve the works of man" and was the first of its kind. The park was named with the Spanish term for green table because of its forests of juniper and piñon trees. From 1908 to 1922, The Spruce Tree House, Cliff Palace, and Sun Temple ruins were stabilized. Most of the early efforts were led by J. Walter Fewkes.
During the 1930s and 40s, Civilian Conservation Corps workers, starting in 1932, played key roles in excavation efforts, building trails and roads, creating museum exhibits and constructing buildings at Mesa Verde. From 1958 to 1965, Wetherill Mesa Archeological Project included archeological excavations, stabilization of sites, and surveys. With excavation and study of eleven Wetherill Mesa sites, it is considered the largest archeological effort in the United States.
In 1966, as with all historical areas administered by the National Park Service, Mesa Verde was listed on the National Register of Historic Places. It was designated a World Heritage Site in 1978. In 1987, the Mesa Verde Administrative District was listed on the National Register of Historic Places.
During the years 1996, 2000 (twice), 2001, 2002, and 2003, the park, which is covered with piñon pine and Utah juniper forests, suffered from a large number of wildland fires. In its 2015 travel awards, Sunset magazine named Mesa Verde National Park "the best cultural attraction" in the Western United States.
Mesa Verde's park entrance is on U.S. Route 160, about 9 miles (14 km) east of the community of Cortez and about 7 miles (11 km) west of Mancos, Colorado. The park covers 52,485 acres (21,240 ha) It contains 4,372 documented sites. It is the largest archeological preserve in the US. It protects some of the most important and best preserved archeological sites in the country.
The park protects 600 separate cliff dwellings. Of the park's 600 separate cliff dwellings, 230 of them have been assessed for damage, and may be repaired in the coming years.
The Mesa Verde Visitor and Research Center is located just off of Highway 160 and is before the park entrance booths. The Visitor and Research Center opened in December 2012. Chapin Mesa (the most popular area) is 20 miles (32 km) beyond the visitor center.
Mesa Verde National Park is an area of federal exclusive jurisdiction. Because of this all law enforcement, emergency medical service, and wildland/structural fire duties are conducted by federal National Park Service Law Enforcement Rangers. The Mesa Verde National Park Post Office has the ZIP Code 81330.
Park facilities and access:
- The park's Chapin Mesa Archeological Museum is open all year.
- Three of the cliff dwellings on Chapin Mesa are open to the public.
- Spruce Tree House is open all year, weather permitting.
- Balcony House, Long House and Cliff Palace require tour tickets for ranger-guided tours. Many other dwellings are visible from the road but not open to tourists.
- The park offers hiking trails, a campground, and, during peak season, facilities for food, fuel, and lodging; these are unavailable in the winter.
Culturally modified trees
Ute Mountain Tribal Park
The Ute Mountain Tribal Park, adjoining Mesa Verde National Park to the east of the mountains, is approximately 125,000 acres (51,000 ha) along the Mancos River. Hundreds of surface sites, cliff dwellings, petroglyphs, and wall paintings of Ancestral Puebloan and Ute cultures are preserved in the park. Native American Ute tour guides provide background information about the people, culture and history who lived in the park lands. National Geographic Traveler chose it as one of "80 World Destinations for Travel in the 21st Century", one of only nine places selected in the United States.
In the late Cretaceous Period, the Mancos Shale was deposited on top of the Dakota Sandstone, which is the rock formation that can be found under much of Colorado. The beds of the Mancos Shale are "fine-grained sand-stones, mudstones, and shales" which accumulated in the deep water of the Cretaceous Sea. It has a high clay content which causes it to expand when wet leading to sliding of the terrain. On top of this shale, there are three formations in the Mesaverde group which reflect the changes in depositional environment in the area over time. The first is the Point Lookout Sandstone, which is named for the Point Lookout feature in the park (elevation 8427 feet). This sandstone, which formed in the marine environment of shallow water when the Cretaceous sea was receding, is "massive, fine-grained, cross-bedded, and very resistant", in its layers reflecting waves and currents that were present during the time of its formation. Its sediments are approximately 400 feet thick, and its upper layers feature fossiliferous invertebrates.
Next is the Menefee Formation, the middle formation whose content features "interbedded carbonaceous shales, siltstones, and sandstones". These were deposited in a semi-marine environments of brackish water in "bays, lagoons, and swamps". Due to its depositional environment and the organic material in its composition, there are thin coal seams running through the Menefee Formation. At the top, this Formation is intruded upon or "inter fingers with" the Cliff House Sandstone.
The Cliff House Sandstone is the "youngest rock layer present in the area." It was formed after the Cretaceous sea had completely receded and as a result has a high sand content from beaches, dunes, etc. and from this receives its characteristic yellow tint to its canyon faces. Like the Point Lookout Sandstone, it is about 400 feet thick. It contains numerous fossil beds of different types of shells, fish teeth, and other invertebrate leftovers from the receded sea. The shale zones in this feature determine where alcoves formed where the Ancestral Puebloans constructed their dwellings.
Continuing through the Cretaceous period and into the early Tertiary, there was uplifting in the area of the Colorado Plateau, the San Juan Mountains, and the La Plata Mountains, which led to the formation of the Mesa Verde pediment with the help of erosion. Small channels of water ran across this formation depositing gravel. Later in the tertiary, the last period of uplift and rock tilting towards the south caused these streams to cut rapidly into the rock removing loose sediment and forming the vast canyons seen today. This caused the isolation of the Mesa Verde pediment from surrounding rock. Today, since the climate is more arid, these erosional processes are significantly slowed.
Geography and anthropogenic ecology
Mesa Verde's canyons were created by streams eroding the hard sandstone which covers the area. This resulted in Mesa Verde National Park elevations ranging from about 6,000 to 8,572 feet (1,829 to 2,613 m), the highest elevation at Park Point. The terrain in the park is now a transition zone between the low desert plateaus and the Rocky Mountains.
Anthropogenic ecology refers to the human impact on animals and plants in an ecosystem. A significant shift from medium and large game animals such as deer, bighorn sheep, and antelope to smaller ones like rabbits and turkey during the mid-10th to mid-13th centuries might indicate that Mesa Verdean subsistence hunting had dramatically altered faunal populations on the mesa.
Analysis of pack rat midden indicates that, with the exception of invasive species such as tumbleweed and clover, the flora and fauna in the area have remained relatively consistent for the past 4,000 years.
The climate is semi-arid. Water for farming and consumption by the was provided by summer rains, winter snowfall, and seeps and springs in and near the Mesa Verde villages. At 7,000 feet (2,100 m), the middle mesa areas were typically ten degrees cooler than the mesa top, which reduced the amount of water needed for farming. The cliff dwellings were built to take advantage of solar energy. The angle of the sun in winter warmed the masonry of the cliff dwellings, warm breezes blew from the valley, and the air was ten to twenty degrees warmer in the canyon alcoves than on the top of the mesa. In the summer, with the sun high overhead, much of the village was protected from direct sunlight in the high cliff dwellings.
|Climate data for Mesa Verde National Park (1981−2010 normals)|
|Record high °F (°C)||62
|Average high °F (°C)||39.6
|Average low °F (°C)||19.5
|Record low °F (°C)||−20
|Average precipitation inches (mm)||1.77
|Average snowfall inches (cm)||17.9
|Avg. precipitation days (≥ 0.01 in)||7.2||7.9||8.0||6.6||6.4||4.0||9.3||10.6||7.9||6.9||6.4||7.4||88.6|
|Avg. snowy days (≥ 0.1 in)||6.5||6.6||5.7||2.6||0.3||0||0||0||0||0.9||3.2||5.9||31.6|
|Source: NOAA (extremes 1922–present)|
Approximately 600 of the more than 4700 archeological sites found in Mesa Verde National Park are cliff dwellings. In addition to the cliff dwellings, Mesa Verde boasts a number of mesa-top ruins. Examples open to public access include the Far View Complex and Cedar Tree Tower on Chapin Mesa, and Badger House Community, on Wetherill Mesa.
Set on a high ledge facing east, Balcony House with 45 rooms and 2 kivas, would have been cold for its residents in the winter. The modern visitor enters by climbing a 32-foot ladder and a crawling through a 12-foot tunnel. The exit, a series of toe-holds in a cleft of the cliff, was believed to be the only entry and exit route for the cliff dwellers, which made the small village easy to defend and secure. One log was dated at 1278, so it was likely built not long before the Mesa Verde people migrated out of the area. It was officially excavated by Jesse Nusbaum, one of the first Superintendents of Mesa Verde National Park, in 1910. Visitors can enter Balcony House through ranger-guided tours.
This multi-storied ruin, the best-known cliff dwelling in Mesa Verde, is located in the largest alcove in the center of the Great Mesa. It was south- and southwest-facing, providing greater warmth from the sun in the winter. Dating back more than 700 years, the dwelling is constructed of sandstone, wooden beams, and mortar. Many of the rooms were brightly painted. Cliff Palace was home to approximately 125 people, but was likely an important part of a larger community of sixty nearby pueblos, which housed a combined six hundred or more people. With 23 kivas and 150 rooms, Cliff Palace is the largest cliff dwelling in Mesa Verde National Park.
Located on the Wetherill Mesa, Long House is the second-largest Mesa Verdean village; approximately 150 people lived there. The location was excavated from 1959 through 1961, as part of the Wetherhill Mesa Archeological Project. Long House was built c. 1200; it was occupied until 1280. The cliff dwelling features 150 rooms, a kiva, a tower, and a central plaza. Its rooms are not clustered like typical cliff dwellings. Stones were used without shaping for fit and stability. Two overhead ledges contain storage space for grain. One ledge seems to include an overlook with small holes in the wall to see the rest of the village below. A spring is accessible within several hundred feet, and seeps are located in the rear of the village.
Far View Reservoir
This ancient structure was originally identified as reservoir, to support the mesa top with water for drinking and irrigation. On September 26, 2004, it became a National Civil Engineering Historic Landmark. In 2014 geospatial analyses showed that neither collection nor retention of water was possible in the supposed structures. The new interpretation sees Far view reservoir as a ceremonial space with procession roads in an adaptation of Chacoan culture.
This ruin situated on Wetherill Mesa contains 94 rooms, a large kiva, and a nearby reservoir. It received its name from four mugs the Charles Mason and the Wetherill brothers found strung together on a string. This ceremonial structure has a keyhole shape, due to a recess behind the fireplace and a deflector, that is considered an element of the Mesa Verde style. The rooms clustered around the kiva formed part of the courtyard, indicating the kiva would have been roofed.
Oak Tree House
Oak Tree House and neighboring Fire Temple can be visited via a 2-hour ranger-guided hike.
Spruce Tree House
Spruce Tree House is the third-largest village, within several hundred feet of a spring, and had 130 rooms and eight kivas. It was constructed sometime between 1211 and 1278. It is believed anywhere from 60 to 80 people lived there at one time. Because of its protective location, it is well preserved. The short trail to Spruce House begins at the Chapin Mesa Archeological Museum.
Square Tower House
The Square Tower House is one of the stops on the Mesa Top Loop Road driving tour. The tower that gives this site its name is the tallest structure in Mesa Verde. This cliff dwelling was occupied between 1200 and 1300.
- Mesa Verde Wilderness
- Ute Mountain Tribal Park in Mesa Verde
- Yucca House National Monument administered by the Mesa Verde National Park
Other neighboring Ancestral Puebloan sites in Colorado
- Anasazi Heritage Center
- Canyons of the Ancients National Monument
- Crow Canyon Archeological Center
- Hovenweep National Monument
Other cultures in the Four Corners region
Early American cultures
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- Mesa Verde National Park (National Park Service)
- Interactive map of the National Park System
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- Mesa Verde Digital Media Archive (creative commons-licensed photos, laser scans, panoramas), data on Spruce Tree House, Fire Temple, and Square Tower House from a National Park Service/CyArk research partnership