"White House Ruin" by U.S. National Park Service , public domain

Canyon de Chelly

National Monument - Arizona

Canyon de Chelly National Monument was established on April 1, 1931 as a unit of the National Park Service. Located in northeastern Arizona, it is within the boundaries of the Navajo Nation and lies in the Four Corners region.

maps

Official visitor map of Canyon de Chelly National Monument (NM) in Arizona. Published by the National Park Service (NPS).Canyon de Chelly - Visitor Map

Official visitor map of Canyon de Chelly National Monument (NM) in Arizona. Published by the National Park Service (NPS).

Map of the U.S. National Park System. Published by the National Park Service (NPS).National Park System - National Park Units

Map of the U.S. National Park System. Published by the National Park Service (NPS).

Map of the U.S. National Park System with Unified Regions. Published by the National Park Service (NPS).National Park System - National Park Units and Regions

Map of the U.S. National Park System with Unified Regions. Published by the National Park Service (NPS).

Map of the U.S. National Heritage Areas. Published by the National Park Service (NPS).National Park System - National Heritage Areas

Map of the U.S. National Heritage Areas. Published by the National Park Service (NPS).

Apache and Navaja County Map of Arizona Surface Management Responsibility. Published by Arizona State Land Department and U.S. Bureau of Land Management (BLM).AZ Surface Management Responsibility - Apache and Navaja County

Apache and Navaja County Map of Arizona Surface Management Responsibility. Published by Arizona State Land Department and U.S. Bureau of Land Management (BLM).

Statewide Map of Arizona Surface Management Responsibility. Published by Arizona State Land Department and U.S. Bureau of Land Management (BLM).AZ Surface Management Responsibility - Arizona State

Statewide Map of Arizona Surface Management Responsibility. Published by Arizona State Land Department and U.S. Bureau of Land Management (BLM).

https://www.nps.gov/cach/index.htm https://en.wikipedia.org/wiki/Canyon_de_Chelly_National_Monument Canyon de Chelly National Monument was established on April 1, 1931 as a unit of the National Park Service. Located in northeastern Arizona, it is within the boundaries of the Navajo Nation and lies in the Four Corners region. For nearly 5,000 years, people have lived in these canyons - longer than anyone has lived uninterrupted anywhere on the Colorado Plateau. In the place called Tsegi, their homes and images tell us their stories. Today, Navajo families make their homes, raise livestock, and farm the lands in the canyons. A place like no other, the park and Navajo Nation work together to manage the land's resources. The recommended route to the park is from Highway 191 in Chinle then turning east on Route 7. The park entrance and Visitor Center is about 3 miles from Highway 191. An alternative is entering the park on the East side via Route 64. There are 3 overlooks to stop at along Route 64 before getting to the Visitor Center. Travel on Route 7 from the East is NOT RECOMMENDED since the road is unpaved and unmaintained between Sawmill and the Spider Rock turnoff. Visitor Center Pick up a park map at the Visitor Center which features a park store, orientation video and activity schedule. Visitor Center and parking lot gates open daily from 8 a.m. to 5 p.m. Closed on Thanksgiving, Christmas and New Year's Day. GPS units and cell phone services are unreliable throughout the Navajo Nation. The recommended route to the park is from Highway 191 in Chinle then turning east on Route 7. The park entrance and Visitor Center is about 3 miles from Highway 191. The alternative is entering the park on the East side via Route 64. There are 3 overlooks to stop at along Route 64 before getting to the Visitor Center. Travel on Route 7 from the East is NOT RECOMMENDED since the road is unpaved and unmaintained. Canyon Farm Farm in the canyon Navajo families continue to live and farm in the canyon they call Tsegi Canyon Hike Hiking in the canyon Visitors can enjoy a free ranger led hike into the canyon Spider Rock View of Spider Rock from the overlook Her home on top of Spider Rock, Spider Woman taught the Navajo people how to weave Canyon View View of the canyon from the White House Trail The Navajo people call the canyon Tsegi meaning "within the rocks" White House View of White House Ruin Ancient Puebloans built villages like White House that offered opportunities for trade, ceremony, and social gatherings. NPS Geodiversity Atlas—Canyon de Chelly National Monument, Arizona Each park-specific page in the NPS Geodiversity Atlas provides basic information on the significant geologic features and processes occurring in the park. [Site Under Development] spider rock pinnacle 2019 Connecting with our Homelands Awardees Hopa Mountain, in partnership with the National Park Service, is pleased to announce the 2019 awardees of the Connecting with our Homelands travel grants. Twenty-one Indigenous organizations, schools, and nonprofits have been awarded travel funds for trips to national park units across 12 states/territories within the United States. An elder and young student talk while sitting on a rock. 2011 SCPN-NAU Student Projects In spring 2011, the SCPN-NAU School of Communication collaboration began with a multimedia studies course focused on documenting park resources and resource projects. The class was taught by NAU professors Laura Camden and Peter Friederici. 2011 Student Projects The Colorado Plateau The Colorado Plateau is centered on the four corners area of the Southwest, and includes much of Arizona, Utah, Colorado, and New Mexico. Hazy Fajada Butte, Chaco Culture National Monument Monitoring Bird Communities on the Southern Colorado Plateau Bird communities can tell us a lot about changing environmental conditions. High on the food chain, and sensitive to climate and habitat changes, birds are monitored on the Southern Colorado Plateau as indicators of riparian and upland ecosystem health. Male Williamson’s sapsucker. Monitoring Night Skies and Natural Soundscapes on the Southern Colorado Plateau Many national parks in the Southern Colorado Plateau region contain large areas of wilderness, where dark night skies and natural soundscapes are important human values. Dark night skies, which depend upon the visibility of stars and other natural components, are diminishing resources in several park units because of anthropogenic activities. Natural soundscapes—that is, the natural sounds of wildlands—are degraded by sounds caused by humans or human technology. Clouds and sky turning red and orange over Navajo National Monument at sunset Monitoring Water Quality on the Southern Colorado Plateau Water quality data are used to characterize waters, detect trends over time, and identify emerging problems. In Southern Colorado Plateau Network parks, water quality is monitored as an indicator of aquatic ecosystem integrity, as a component of watershed condition, and to document water quality conditions in relation to state and federal regulations. Collecting water quality data Vegetation Characterization and Mapping on the Southern Colorado Plateau Vegetation mapping is a tool used by botanists, ecologists, and land managers to better understand the abundance, diversity, and distribution of different vegetation types across a landscape. Vegetation plots used for the classification and mapping of El Malpais NM Climate Change on the Southern Colorado Plateau The combination of high. elevation and a semi-arid climate makes the Colorado Plateau particularly vulnerable to climate change. Climate models predict that over the next 100 years, the Southwest will become warmer and even more arid, with more extreme droughts than the region has experienced in the recent past. One result of climate change may be more, larger floods, like this flash flood in Glen Canyon NRA Monitoring Spring Ecosystems on the Southern Colorado Plateau Springs are important water sources in arid landscapes, supporting unique plant associations and sustaining high levels of biotic diversity. Because springs rely on groundwater, they can serve as important indicators of change in local and regional aquifers. On the Colorado Plateau, spring ecosystems also provide vital habitat for both endemic and regionally rare species, including several types of orchids and declining populations of leopard frogs. A pool of water filled with vegetation and sheltered by large rocks Monitoring Aquatic Macroinvertebrates on the Southern Colorado Plateau Aquatic macroinvertebrates, such as insect larvae, snails, and worms, play a vital role in stream ecosystems, both as a food source and as consumers of algae and other organic matter. Because macroinvertebrates are sensitive to environmental change, monitoring them can help to detect chemical, physical, and biological impacts to aquatic ecosystems. Monitoring aquatic macroinvertebrates JROTC and NPS Collaboration – Expanding Our Stories Over the course of the 2018-19 academic years, the National Park Service’s Washington, DC Office of Interpretation, Education and Volunteers (WASO IEV), with support from Kutztown University, has overseen a series of pilot programs aimed to facilitate unique, place-based learning experiences in national parks for military youth throughout the United States. Series: Geologic Time Periods in the Mesozoic Era The Mesozoic Era (251.9 to 66 million years ago) was the "Age of Reptiles." During the Mesozoic, Pangaea began separating into the modern continents, and the modern Rocky Mountains rose. Dinosaurs, crocodiles, and pterosaurs ruled the land and air. As climate changed and rapid plate tectonics resulted in shallow ocean basins, sea levels rose world-wide and seas expanded across the center of North America. fossil dinosaur skull in rock face Series: National Park Service Geodiversity Atlas The servicewide Geodiversity Atlas provides information on <a href="https://www.nps.gov/subjects/geology/geoheritage-conservation.htm">geoheritage</a> and <a href="https://www.nps.gov/subjects/geology/geodiversity.htm">geodiversity</a> resources and values all across the National Park System to support science-based management and education. The <a href="https://www.nps.gov/orgs/1088/index.htm">NPS Geologic Resources Division</a> and many parks work with National and International <a href="https://www.nps.gov/subjects/geology/park-geology.htm">geoconservation</a> communities to ensure that NPS abiotic resources are managed using the highest standards and best practices available. park scene mountains Series: Defining the Southwest The Southwest has a special place in the American imagination – one filled with canyon lands, cacti, roadrunners, perpetual desert heat, a glaring sun, and the unfolding of history in places like Tombstone and Santa Fe. In the American mind, the Southwest is a place without boundaries – a land with its own style and its own pace – a land that ultimately defies a single definition. Maize agriculture is one component of a general cultural definition of the Southwest. Series: SCPN-NAU School of Communication Collaboration The Southern Colorado Plateau Network (SCPN) of the National Park Service has been partnering with the Northern Arizona University (NAU) School of Communication since 2011 to develop student multimedia projects that highlight resources and activities in network parks. This collaboration gives NAU students hands-on experience in creating multimedia projects and provides network parks with products that can help to promote their unique resources and scientific or educational project work. SCPN-NAU student projects Triassic Period—251.9 to 201.3 MYA The brightly colored Triassic rocks of Petrified Forest National Park yield not only the petrified trees but many other plant and animal fossils. fossil footprint on stone Mesozoic Era The Mesozoic Era (251.9 to 66 million years ago) was the "Age of Reptiles." During the Mesozoic, Pangaea began separating into the modern continents, and the modern Rocky Mountains rose. Dinosaurs, crocodiles, and pterosaurs ruled the land and air. As climate changed and rapid plate tectonics resulted in shallow ocean basins, sea levels rose world-wide and seas expanded across the center of North America. fossil dinosaur skull in rock face

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