Emigration Canyon is a metro township and canyon in Salt Lake County, Utah, United States, located east of Salt Lake City in the Wasatch Range. Beginning at the southern end of the University of Utah, the canyon itself heads east and northeast between Salt Lake City and Morgan County. The boundaries of the metro township do not extend to the county line, nor do they encompass all of Emigration Canyon, as parts of it are within Salt Lake City. As of the 2010 census, the population was 1,568. A portion of Emigration Canyon, located in This Is the Place Heritage Park, was declared a National Historic Landmark in 1961 for the canyon's significance in the Mormon migration of the 19th century.

The City of Fruita is a home rule municipality located in western Mesa County, Colorado, United States. Fruita is part of the Grand Junction, CO Metropolitan Statistical Area and within the Grand Valley. The geography is identified by the bordering Colorado River (historically known as the Grand River) on the southern edge of town, the Uncompahgre Plateau known for its pinyon-juniper landscape, and the Book Cliffs range on the northern edge of the Grand Valley. The population was 12,646 at the 2010 census. Originally home to the Ute people, white farmers settled the town after founder William Pabor in 1884. Ten years later, Fruita was incorporated. Economically, it started out as a fruit-producing region, but today it is well known for its outdoor sports such as mountain biking, hiking, and rafting, its proximity to the Colorado National Monument, and its annual festivals. Fruita has been the winner of the Governor's Smart Growth and Development Award for four consecutive years. The city motto is "Honor the Past, Envision the Future".

The San Rafael Swell is a large geologic feature located in south-central Utah, United States about 16 miles (26 km) west of Green River. The San Rafael Swell, measuring approximately 75 by 40 miles (121 by 64 km), consists of a giant dome-shaped anticline of sandstone, shale, and limestone that was pushed up during the Paleocene Laramide Orogeny 60–40 million years ago. Since that time, infrequent but powerful flash floods have eroded the sedimentary rocks into numerous valleys, canyons, gorges, mesas, buttes, and badlands. The swell is part of the Colorado Plateau physiographic region.

There is no other place in Colorado where visitors experience the intersection of so many prized ecosystems: Mountains, rivers, canyons, lakes, forests and high desert.