Back to the Fall River Road, and it’s just another few hundred yards to the Sheep Lakes Information Station. From here you have about the best chance in the park to see the Rocky Mountain Bighorn Sheep, a truly impressive sheep species that is notable for its agility, as well as having enormous horns. Be sure to keep your distance from the sheep and any other animals here, they are wild animals and this is their home!

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.[54] 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.[55]


The rain started to head in, but we shifted plans a bit (the park is huge - one side can have rain while the other is sunny) and got to Alluvial Fan, Bear Lake, Nymph Lake and Dream Lake among some other spots. We also drove through most of the park and went to the Alpine  Visitor Center - 11,796 feet up! It's the highest elevation Visitor Center in the park. Great views. Such a different feel - it was cold and there was snow on the ground. In July!
A gourmet breakfast is included in the price of suites and cabins. A great room and sunny family room offer games, piano, movie library, trail guides and maps. The warmth of knotty pine walls, wood floors, a big sandstone fireplace and family heirlooms transport you back to a simpler era. Let us pamper you for your romantic getaway, elopement or any occasion when you chose Estes Park.
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.[41] 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.[42]
Located in the moose capital of Colorado — Colorado State Forest State Park — Never Summer Nordic has built and operates seven yurts and two huts inside the state land. Their headquarters is located in Walden on the outskirts of the park, but their backcountry yurts can be found in jaw-dropping, secluded locations throughout all 70,838 acres. Whether you’re looking for a weeklong backcountry ski trip or a romantic weekend getaway, Never Summer Nordic has the yurt for you. See them all here.

We invite you to Wildwood Inn where you can experience the beauty of the majestic surrounding mountains, the abundant wildlife away from the congested areas of Estes Park. Nestled within 7 acres of private land and the National Park, you will enjoy spectacular views, and star studded nights that can let your spirits soar. Indulge yourself in beautifully appointed suites all with luxurious 310 thread count linens and some with Deluxe Temper-Pedic mattresses. Most offer private outdoor hot tubs with spectacular views of the mountain ranges or fireside hot tubs with shimmering candles aglow, and even ones with both.
Features: Bear Lake Loop is one of the most popular hiking loops in The Park, and it’s one of the flattest hikes. Bear Lake provides phenomenal views of aspen, making it one of the best hikes to try during the fall months. Take a stroll around the lake, and gaze upon the beauty of Glacier Gorge. View Longs Peak, Half Mountain, and Hallet Peak looming over the undulating terrain. The trail hugs the lake, occasionally weaving through packs of pine trees. Since Bear Lake is one of the most popular natural monuments here at RMNP, you may want to take the shuttle, instead of your car, especially during summer when the park is most popular. It’s about a 30 minute drive from Rams Horn Village to the Bear Lake Ranger Station trailhead. Bear Lake
Campgrounds in Rocky Mountain National Park offer unique, wilderness-meets-community experiences for couples, families and groups. Camping fees are $26 per site, per night in the summer, and $18 in the winter (when the water is off) - some park passes include discounts. Campers may check in after 1 p.m. and are requested to check out by noon; abide by posted quiet hours.
Hypothermia, or loss of body heat through exposure, is a danger that can be encountered any time of the year. If anyone exhibits shivering, slurred speech, incoherence, stumbling, or drowsiness, get the person out of the wet, cold. and wind, and into shelter and dry, woolen clothing. The quickest way to warm the victim is to place the person in a dry sleeping bag with another person.
Alta Lakes is a pristine and secluded wilderness setting situated 30 minutes outside the charming mountain town of Telluride, Colorado.  The Observatory is nestled underneath the 13,000-foot peaks of the San Juan Mountains – it is one of only a few homes in the United States at 11,000+ feet! The backcountry cabin with charming rugged details serves as the perfect romantic mountain getaway for couples.
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.[54] 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.[55]
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.[42] 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.[42]
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