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Bluff (Navajo: Tséłgaii Deezʼáhí) is a town in San Juan County, Utah, United States. The population was 320 at the 2000 census . Bluff incorporated in 2018.
The Bluff Historic District, in Bluff, Utah, is a 225 acres (91 ha) historic district which was listed on the National Register of Historic Places in 1995. The district included 11 contributing buildings and six contributing sites. [1] The district is roughly bounded by Main St., U.S. Route 191, 2nd E. St., and the bluffs. [2]
This is intended to be a complete list of the properties and districts on the National Register of Historic Places in San Juan County, Utah, United States. Latitude and longitude coordinates are provided for many National Register properties and districts; these locations may be seen together in a map. [1]
Bluff Ruins located in Hovenweep National Monument. Hackberry Anasazi Bluff Ruins located in Hovenweep National Monument. Holly: Anasazi Bluff Ruins located in Hovenweep National Monument. Cajon: Anasazi Bluff Ruins located in Hovenweep National Monument. Monarch Cave: Anasazi Bluff Ruins located in Butler Wash, Utah. Hovenweep House: Anasazi Bluff
The trail follows a 180-mile (290 km) route starting near Escalante, Utah, and ending in Bluff, Utah, and is named for the place where the San Juan Mission of Mormon pioneers constructed a descent to the Colorado River. The natural crevice on the 1,000-foot (300 m) cliff above the Colorado was enlarged by the party to lower the wagons down to ...
Bluff Fort is a small, fenced settlement from the 19th century in southeast Utah in the United States, an area that was uninhabited until that time. The settlement in situ took place at the end of the 6-month San Juan Expedition .
The Joseph Frederick Adams House, at approximately 150 N. 700 East off U.S. Route 163), in Bluff, Utah, was built in 1895. It was listed on the National Register of Historic Places in 1985. [1] It is also a contributing building in the National Register-listed Bluff Historic District. [2]
The Bluff Formation consists of massive wind-deposited sandstone beds at its type location at Bluff, Utah. These cap the cliffs north of town and are 100–350 feet (30–107 m) thick. [ 1 ] Further to the southeast, the sandstone beds lack high-angle cross beds , being dominated instead by horizontal bed forms, and are overlain by mixed ...
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