Nature created a perfectly beautiful vacation spot right on Fall River, where you will find our lovely village of 20 cabin suites. They are sprinkled over 17 acres amid the Pine & Aspen with kitchens, fireplaces, decks, grills, Free Wi-Fi, & some private hot tubs overlooking the stocked fishing river. Streamside is perfect for your relaxing river-front getaway. Streamside on Fall River Details
Or enjoy a family wildflower hike to Gem Lake or Bridal Veil Falls. For a little more challenge, try the 2.8-mile Mills Lake trek. You’ll be rewarded with grand views of 14,259-foot-tall Longs Peak and the Keyboard of the Winds, a whimsical rock formation named for its shape. Pull over at Moraine Park for prime wildlife watching. More than 3,000 elk and 800 bighorn sheep live in the park, and this U-shaped valley is a regular gathering spot for bugling elk.
Precambrian metamorphic rock formed the core of the North American continent during the Precambrian eon 4.5–1 billion years ago. During the Paleozoic era, western North America was submerged beneath a shallow sea, with a seabed composed of limestone and dolomite deposits many kilometers thick. Pikes Peak granite formed during the late Precambrian eon, continuing well into the Paleozoic era, when mass quantities of molten rock flowed, amalgamated, and formed the continents about 1 billion–300 million years ago. Concurrently, in the period from 500–300 million years ago, the region began to sink while lime and mud sediments were deposited in the vacated space. Eroded granite produced sand particles that formed strata—layers of sediment—in the sinking basin.
Most visitors to the park drive over the famous Trail Ridge Road, but other roads include Fall River Road and Bear Lake Road. The park is open every day of the year, weather permitting. Due to the extended winter season in higher elevations, Trail Ridge Road between Many Parks Curve and the Colorado River Trailhead is closed much of the year. The road is usually open again by Memorial Day and closes in mid-October, generally after Columbus Day. Fall River Road does not open until about July 4 and closes by, or in, October for vehicular traffic. Snow may also fall in sufficient quantities in higher elevations to require temporary closure of the roads into July, which is reported on the road status site.
The Mummy Range is a short mountain range in the north of the park. The Mummies tend to be gentler and more forested than the other peaks in the park, though some slopes are rugged and heavily glaciated, particularly around Ypsilon Mountain and Mummy Mountain. Bridal Veil Falls is a scenic point and trail accessible from the Cow Creek trailhead, at the Continental Divide Research Center. West Creek Falls and Chasm Falls, near Old Fall River Road, are also in this region. The Alluvial Fan trail leads to a bridge over the river that had been the site of the Lawn Lake Flood.
Cow Creek Trail follows Cow Creek, with its many beaver ponds, extending past the Bridal Falls turnoff as the Dark Mountain trail, then joining the Black Canyon trail to intersect the Lawn Lake trail shortly below the lake. North Boundary Trail connects to the Lost Lake trail system. North Fork Trail begins outside of the park in the Comanche Peak Wilderness before reaching the park boundary and ending at Lost Lake. Stormy Peaks Trail connects Colorado State University's Pingree Park campus in the Comanche Peak Wilderness and the North Fork Trail inside the park.