Features: The Lily Lake Loop is one of the easiest hikes in the park, and the trailhead is only about 6 miles from our resort. On the Lily Lake Loop, you’ll enjoy vistas of Lily Lake, as it reflects the surrounding mountain range. Take a moment to soak in Longs Peak, Meeker, and Estes Cone. Hike, picnic, fish, and relax. At only 10 feet of elevation change across the entire trail, the Lily Lake Loop is more of a walk in The Park than a hike, and it offers breathtaking beauty that can only be found in RMNP. Lily Lake Loop is handicap accessible.
Region 5, known for waterfalls and backcountry, is south of Estes Park and contains Longs Peak—the park's iconic fourteener—and the Wild Basin area. Other peaks and passes include Lily Mountain, Estes Cone, Twin Sisters, Boulder-Grand Pass, and Granite Pass. Eugenia Mine operated about the late-19th to early-20th century, with some old equipment and a log cabin remaining. Sites and trails include Boulder Field, Wild Basin Trail, and Homer Rouse Memorial Trail.
Trail Ridge Road is 48 miles (77 km) long and connects the entrances in Grand Lake and Estes Park. Running generally east–west through many hairpin turns, the road crosses Milner Pass through the Continental Divide at an elevation of 10,758 ft (3,279 m). The highest point of the road is 12,183 feet (3,713 m), with eleven miles of the road being above tree line which is approximately 11,500 feet (3,505 m). The road is the highest continuously paved highway in the country, and includes many large turnouts at key points to stop and observe the scenery.
Features: If you’re looking for beautiful falls and a relatively easy hike, you’ve got to trek to Copeland Falls. Copeland Falls is about a 30 minute drive South from our resort. The trail is well shaded by pine trees, and it brings you to several cascading waterfalls, all along the North St. Vrain Creek. You can see both Upper Copeland Falls and Lower Copeland Falls on sections of this trail.
Skiiers: Have everything taken care of for you so that all you have to worry about is the snow. This cabin is just outside of Crested Butte, which was named Best Ski Town in North America by Powder Magazine. A free shuttle can get you to the base and you can store all of your skiing and outdoor equipment at the cabin. Check out that front porch swing with an amazing view of the mountains!
About 300 million years ago, the land was uplifted creating the ancestral Rocky Mountains. Fountain Formation was deposited during the Pennsylvanian period of the Paleozoic era, 290–296 million years ago. Over the next 150 million years, the mountains uplifted, continued to erode, and covered themselves in their own sediment. Wind, gravity, rainwater, snow, and glacial ice eroded the granite mountains over geologic time scales. The Ancestral Rockies were eventually buried under subsequent strata.
Rocky Mountain National Park was selected to participate in a climate change study, along with two other National Park Service areas in the Rocky Mountain region and three in the Appalachian Mountain region. The study began in 2011, orchestrated by members of the academic scientific community in cooperation with the National Park Service and the National Aeronautics and Space Administration (NASA). The stated objective: "develop and apply decision support tools that use NASA and other data and models to assess vulnerability of ecosystems and species to climate and land use change and evaluate management options."
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.