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The Rio Grande Gorge Bridge, locally known as the "Gorge Bridge" or the "High Bridge", [2] is a steel deck arch bridge across the Rio Grande Gorge 10 miles (16 km) northwest of Taos, New Mexico, United States. Roughly 600 feet (180 m) above the Rio Grande, it is the seventh highest bridge in the United States. [3]
near Anthony, New Mexico: S.H. 226 Bridge NM 226 near Berino, New Mexico: Six Mile Road Bridge Six Mile Road near Vado, New Mexico: S.H. 227 Bridge NM 227 Vado, New Mexico to La Mesa, New Mexico: S.H. 192 Bridge NM 192 Mesquite, New Mexico: S.H. 28 Bridge NM 28 South of Las Cruces, New Mexico: Calle Del Norte Bridge: Old Mesilla, New Mexico: I ...
The Rio Grande Bridge at Radium Springs is a historic timber beam bridge built in 1933. As of 1997, it still carried NM 185 over the Rio Grande, about 1 mile (1.6 km) south of Radium Springs, New Mexico. It was listed on the National Register of Historic Places in 1997. [1]
The New Mexico Department of Transportation is reminding people about work on another part of the Interstate 25 improvements project . ... An inspection on the Rio Grande Gorge Bridge recently began.
Rio Arriba 36°57′20″N 106°32′28″W / 36.95556°N 106.54111°W / 36.95556; -106.54111 ( Denver & Rio Grande Railroad, San Juan Extension, Wolf Creek NM-29
Warren type steel deck truss bridge, removed from service in 1995 but preserved Felix Bridge at Hagerman: 1926 1997-07-15 Hagerman: Chaves: Pratt through truss bridge Rio Grande Bridge at Radium Springs: 1933 1997-07-15 Radium Springs
The Rio Grande Bridge at San Juan Pueblo, crossing the Rio Grande near Alcalde, New Mexico, is a Parker pony truss bridge built in 1925. It was listed on the National Register of Historic Places in 1997. [1] It is a four-span bridge located about 200 yards (180 m) south of New Mexico State Road 74, about .5 miles (0.80 km) west of San Juan ...
Rio Grande Gorge Bridge. Geologically, the Rio Grande Gorge is a canyon, [1] carved out by erosion over the last several million years. [2] The Rio Grande Gorge and its river follow a topographical low within the larger Rio Grande Rift; a mixture of volcanic activity, shifting tectonic plates, and erosion of layers of gravels and lava yielded the recognizable narrow, deep gorge visible today.