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Great Sand Dunes

Great Sand Dunes National Park and Preserve
IUCN category II (national park)
A544, Great Sand Dunes National Park, Colorado, USA, climber ascending high dune, 2016.jpg
Hiker ascending the 700' tall "High Dune"
Map showing the location of Great Sand Dunes National Park and Preserve
Map showing the location of Great Sand Dunes National Park and Preserve
Map showing the location of Great Sand Dunes National Park and Preserve
Map showing the location of Great Sand Dunes National Park and Preserve
Location Alamosa and Saguache Counties, Colorado, United States
Nearest city Alamosa
Coordinates 37°43′58″N 105°30′44″W / 37.732870°N 105.512120°W / 37.732870; -105.512120Coordinates: 37°43′58″N 105°30′44″W / 37.732870°N 105.512120°W / 37.732870; -105.512120
Area 149,028 acres (603.09 km2)
Established September 24, 2004
Visitors 486,935 (in 2017)
Governing body National Park Service
Website Great Sand Dunes National Park and Preserve

Great Sand Dunes National Park and Preserve is a national park that conserves an area of large sand dunes up to 750 feet (229 m) tall on the eastern edge of the San Luis Valley, and an adjacent national preserve located in the Sangre de Cristo Range, in south-central Colorado, United States. The park was originally designated Great Sand Dunes National Monument on March 17, 1932 by President Herbert Hoover. The original boundaries protected an area of 35,528 acres (55.5 sq mi). A boundary change and redesignation as a national park and preserve was authorized on November 22, 2000 and then established by an act of Congress on September 24, 2004. The park encompasses 107,342 acres (167.7 sq mi) while the preserve protects an additional 41,686 acres (65.1 sq mi) for a total of 149,028 acres (232.9 sq mi). The recreational visitor total was 486,935 in 2017, about 25% more than the 388,308 visitors of 2016.

The park contains the tallest sand dunes in North America. The dunes cover an area of about 30 sq mi (78 km2) and are estimated to contain over 5 billion cubic meters of sand. Sediments from the surrounding mountains filled the valley over geologic time periods. After lakes within the valley receded, exposed sand was blown by the predominant southwest winds toward the Sangre de Cristos, eventually forming the dunefield over an estimated tens of thousands of years. The four primary components of the Great Sand Dunes system are the mountain watershed, the dunefield, the sand sheet, and the sabkha. Ecosystems within the mountain watershed include alpine tundra, subalpine forests, montane woodlands, and riparian zones.


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