Old Fall River Road will be closed in 2014 due to flood damage
Damages on Old Fall River Road are extensive and the road will remain closed to vehicles through 2014. It is unknown at this time whether hikers and bicyclists will be allowed on the road. More »
Impacts from September 2013 Flood
Due to recent flooding, there are still some closures in the park that could affect your visit. More »
The road system of Rocky Mountain National Park offers visitors access to diverse ecosystems characterizing the higher regions of the central Rocky Mountains. The roads take visitors through lowland meadows and aspen groves, along swift-flowing rivers and up through subalpine forests to more than 12,000 feet in elevation. No other national park roads offer the dramatic experience of a long drive across alpine tundra region, and few offer such a wide variety of experiences.
The careful relationship of the park roads to the landscape results in a road system that generally harmonizes with the environment. Roadway alignments were chosen to highlight natural features, and scenic vistas and overlooks were provided to allow visitors to take in the magnificent terrain. The stone parapet walls and road-related structures, constructed in the National Park Service's distinctive rustic style of architecture, relate well to their natural surroundings and help evoke a distinctive experience. Not surprisingly, the park roads are the principal attraction for most of the nearly three million visitors who flock to Rocky Mountain National Park each year.
Old Fall River Road gives todays visitor the opportunity to experience the park by automobile in much the same way as early visitors. Trail Ridge Road is one of ten America's Byways and a national designated All American Road. Like to see as many byways as you can? On the outskirts of Rocky is the oldest Colorado Scenic Byway, Peak to Peak, and another America's Byway, the Colorado River Headwaters. To learn more about other Colorado Scenic Byways click here.
Did You Know?
The oldest rocks in the park are metamorphic (biotite schist and gneiss) estimated at 1.7 billion years old, making them some of the oldest rocks within the National Park System.