Estes Park has long billed itself as "The Gateway to the Rockies." This little town has a lot of charm of its own. For the many people who feel that the best part of the Rockies is the view, Estes Park is the best of both worlds. It is the perfect romantic getaway for those who would rather avoid the mountain roads and bone-chilling temperatures of Vail and Aspen during the winter.
Where your Rocky Mountain Adventure begins! Our conveniently located, 1910 rambling mountain inn is snuggled in amidst towering pine and aspen with an expansive view of the Estes Valley. The inn consists of four luxury suite, all with private baths with fireplaces and whirlpool tubs for two. Two luxury cabins sleep up to six and have a full kitchen.
Many visitors end up shopping or going to restaurants in Estes Park. Dickey said his sales are higher this week compared to a year ago. On Christmas Eve, he did twice as much business as he did on Christmas Eve 2017. Dickey, president of the Estes Valley Partners for Commerce board, said other store owners told him they had not noticed any downturns.
Colorado Cabin Adventures is the perfect mix of comfortable and rustic. For the outdoor enthusiast who loves to explore and wants to climb the highest peak, we are ideally located. For the aficionado of all things fabulous, who hopes to find inspiration, we are nicely decorated. For the rest of the crew, who goes with the flow and wants to just have fun, we are Colorado Cabin Adventures.
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.
Gem Lake is high among the rounded granite domes of Lumpy Ridge. Untouched by glaciation, this outcrop of 1.8 billion-year-old granite has been sculpted by wind and chemical erosion into a backbone-like ridge. Pillars, potholes, and balanced rocks are found around the midpoint of the trail, along with views of the Estes Valley and Continental Divide. Potts Puddle trail is accessible from the Black Canyon trail.
Features: Take a quick hike around Lake Irene. Lake Irene is one of the highest lakes in the park; it’s just below the continental divide. This secluded little lake is surrounded by pine trees, and the trail is fairly flat along its entire length. However, once again, since this lake is at elevation, it can be a bit winding—you’ll notice that the trees don’t grow quite so high around the lake since you’ll be near tree line. Take note, the parking lot is the highest point on this hike, so be prepared for the uphill jaunt back to your car! Halfway through the trail, you can also visit an overlook on the trail that displays a vista of Lake Irene and a nearby meadow (this portion of the trail is not part of the length calculation above). It’s about an hour drive from the resort to the Lake Irene Picnic Area.
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.