Glenwood Canyon

Geology

The canyon was formed relatively recently in Pleistocene time by the rapid cutting of the Colorado down through layers of sedimentary rock. The upper layers of the canyon are sandstone from Pennsylvanian and Mississippian. Sections of the lower canyon walls are made of Cambrian rock. The Mississippian layer that is prominent throughout much of the upper rim sections of the canyon is part of the Leadville Formation.

Railroads

In 1906, the canyon provided the route of the Taylor State Road, a gravel road that was the first route for automobiles through the Colorado Rockies. The canyon also provided the route for the Denver and Rio Grande Western Railroad in the late 19th century. Through acquisitions, the line is currently part of the Union Pacific system, comprising part of its Central Corridor between Denver and Grand Junction.

As Glenwood Canyon was one of the iconic scenic views along the California Zephyr passenger train, a monument to the dome car design was originally installed in the canyon. In the 1990s, the monument was relocated to the Colorado Railroad Museum in Golden to make way for the construction on Interstate 70.

Interstate 70

The canyon is widely considered one of the most scenic natural features on the Interstate Highway System of the United States. Foot access to the canyon is available at four rest areas along Interstate 70 in the canyon. The Hanging Lake Rest Area (exit 125) provides access to the canyon along a stretch where I-70 is concealed in the Hanging Lake Tunnel. The freeway is also prone to rockslides in the canyon, such as the ones that closed it in February 2016 and July 2021.