We started at Beaver Meadows Visitor Center and scored some hats at a great price. The park rangers were really nice and provided maps and advice on where to hike. Then it was off to Sheep Lakes. Not much to see here unless you get to see some of the big horn sheep that live in the area. No such luck for us this time around, but it was fun to see photos and read about those who had made an appearance in the days prior to our arrival.
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.
Apart from elk, many other ungulates reside in the park, including bighorn sheep, moose, and mule deer. Bison were eliminated from the park in the 1800s, as were pronghorn and moose, the latter of which was restored to the area in 1978. Moose are now frequently seen in the park, especially on the park's west side. The park's bighorn sheep population has recovered and is estimated at 350 animals.
The Swiftcurrent Lodge is small in size but huge in personal attention. We have 12 units in the summer, 6 in the winter. The advantage of being small, bordering Rocky Mountain National Park and being on the river gives one the sense of seclusion and offers a quiet, peaceful atmosphere. With these attributes plus your own custom package, the Swiftcurrent Lodge is the ideal location for your Romantic Getaway.
The park was designated a World Biosphere Reserve by the United Nations in 1976 to protect its natural resources. The park's biodiversity includes afforestation and reforestation, ecology, inland bodies of water, and mammals, while its ecosystems are managed for nature conservation, environmental education and public recreation purposes. The areas of research and monitoring include ungulate ecology and management, high-altitude revegetation, global change, acid precipitation effects, and aquatic ecology and management.
Horace Albright, director of the National Park Service between 1929 and 1933, once said about Trail Ridge Road, "It's hard to describe what a sensation this new road is going to make. You will have the whole sweep of the Rockies before you in all directions." Trail Ridge Road was a sensation when it debuted back in 1932 and it remains so today for the travelers that make the 48-mile drive from Estes Park to Grand Lake, rising above the tree line for 11 miles at an elevation of nearly 11,500 feet. Visitors should keep that in mind when they're stopping at the lookout points that the road experiences temperatures that are 20 and even 30 degrees lower than both Estes Park and Grand Park.
Escape to this cozy log cabin that is surrounded by beautiful scenery and is nearby many popular attractions in Southern Colorado. The cabin boasts high-speed wifi, which you may not be using too much with the Mesa Verde cliff dwellings only 25 minutes away. The private property is also only 50 minutes from Durango and 90 from Telluride, making this retreat the perfect home-base for day trips!
Highlights of our trip were stopping and eating lunch at Hidden Valley, where we saw a bull Elk up close grazing. Hiking the beautiful Bear Lake, Nymph Lake and then on to the breathtaking Dream Lake. Fly fishing in Moraine Park on the Big Thompson River, with Elk surrounding us. Seeing a Moose for the first time at Forest Canyon. Seeing two Big Horn sheep at Sheeps Lake.
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.
Our warm and inviting Beaver Creek accommodations feature premium amenities that will make guests feel right at home, such as our Hyatt Grand Beds® with crisp linens, large flat-screen TVs, free Wi-Fi, and rich alpine views. Indulge in one of our luxury suites and enjoy extra perks, like a 500 sq. ft. terrace overlooking the entire valley, a kitchenette, and cozy fireplace for chilly nights.
Autumn Gold Festival – Celebrate your new marriage and the new fall season during the Autumn Gold Festival in late September. This year, the festival coincides with a fee-free day for Rocky Mountain National Park on Saturday, September 26! With free entrance to the park and to the festival, you can save that money for a visit to the spa or a nice romantic dinner out on the town. Did we mention the dancing and live music?
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.
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. 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. Many sedimentary rocks from the Paleozoic and Mesozoic eras exist in the basins surrounding the park.
Experience the beauty of Rocky Mountain National Park from your front porch or hot tub! Timber Creek Chalets provides the perfect setting for comfort and relaxation. Following a day of shopping or hiking in the park, refresh yourself in our outdoor heated pool (seasonal), or perhaps just soak in our year-round hot tub. Our chalets sleep from two to ten people � some with personal hot tubs � and are ideal for romantic getaways or family reunions.
This 5-bedroom residence features a stunning family room with a massive gas fireplace and a professional chef’s kitchen with dining area and breakfast nook. No expense was spared on the multi-zone sound system and other electronics throughout the home. Guests can settle into the cozy library/TV room or be blown away by the mineshaft themed cinema with a state-of-the-art digital projector and 11.1-point channel sound and hundreds of first-run movies and TV – all complimentary!