The Trail Ridge Road, which itself reaches an altitude of more than 12,000 feet, is the main driving route through the park and offers easy access to this incredible terrain. You can sightsee from the comfort of your car or stop off along the way for a hike or easy walk. The park has an extensive system of hiking trails that range from paths of less than a half-mile to full-day and multi-day hikes. If you're lucky, you may see elk, bighorn sheep, deer, and other critters.
Glacial geology in Rocky Mountain National Park can be seen from the mountain peaks to the valley floors. Ice is a powerful sculptor of this natural environment and large masses of moving ice are the most powerful tools. Telltale marks of giant glaciers can be seen all throughout the park. Streams and glaciations during the Quaternary period cut through the older sediment, creating mesa tops and alluvial plains, and revealing the present Rocky Mountains.[61] The glaciation removed as much as 5,000 feet (1,500 m) of sedimentary rocks from earlier inland sea deposits. This erosion exposed the basement rock of the Ancestral Rockies. Evidence of the uplifting and erosion can be found on the way to Rocky Mountain National Park in the hogbacks of the Front Range foothills.[60] Many sedimentary rocks from the Paleozoic and Mesozoic eras exist in the basins surrounding the park.[62]
Trail Ridge Road is 48 miles (77 km) long and connects the entrances in Grand Lake and Estes Park.[92][93] Running generally east–west through many hairpin turns,[5] the road crosses Milner Pass through the Continental Divide[93] at an elevation of 10,758 ft (3,279 m).[92][94] The highest point of the road is 12,183 feet (3,713 m),[93] with eleven miles of the road being above tree line which is approximately 11,500 feet (3,505 m).[92] The road is the highest continuously paved highway in the country,[93] and includes many large turnouts at key points to stop and observe the scenery.[92]
^ This article incorporates public domain material from the Library of Congress document: "Majestic view from the old, one-way, dirt Fall River Road in Rocky Mountain National Park in the Front Range of the spectacular and high Rockies in north-central Colorado". Library of Congress - Prints & Photographs Online Catalog. Retrieved October 28, 2016.
Your first stop should be the Quarry Visitors Center from where you can access the main attraction at the park, the Quarry Exhibit Hall, built over the Carnegie Dinosaur Quarry. A huge wall of windows allows in natural light, making it feel more like an excavation site than a museum. Fossils are in various states, from still encased in the stone wall to fully assembled skeletons.
Enos Mills, the main figure behind the creation of Rocky Mountain National Park, enjoyed walking to Lily Lake from his nearby cabin. Wildflowers are common in the spring and early summer. In the winter, the trail around the lake is often suitable for walking in boots, or as a short snowshoe or ski. Other lakes in the Wild Basin include Chasm Lake, Snowbank Lake, Lion Lakes 1 and 2, Thunder Lake, Ouzel Lake, Finch Lake, Bluebird Lake, Pear Lake, and Sandbeach Lake. Many of the lakes have backcountry campsites. Waterfalls include Ouzel Falls, Trio Falls, Copeland Falls, and Calypso Cascades.[47]
While it is possible to travel through Rocky Mountain National Park and not catch sight of any wildlife, we venture to say that is an unlikely experience. From everyday sightings of chipmunks and mule deer to the moving experience of viewing elk in rut (the mating season), the animals in the park let you know that you are part of something truly wild. Some of these critters are harder to spot than others - they might camouflage themselves in the trees or hide in the underbrush - but look closely and you may have an encounter unlike any other.
