The landlocked state boasts about four dozen major lakes where you'll find waterside recreation ranging from houseboating to fishing to waterskiing. In the southwest corner of the state, Navajo State Park boasts a 15,000-acre reservoir that extends into the state of New Mexico. Camp in one of 150 campsites, book a night at the Navajo Lodge, or explore the lake for days on a houseboat. Dillon Reservoir near Breckenridge tucks into pine-laden hills near some of the state's most renowned ski areas. Fish the lake for cutthroat trout, brookies or salmon, or take a sailing lesson at the Dillon Marina.
Rooms enjoy large beds, plush décor, kitchenettes with microwaves and fridges, and cable TV and free wireless Internet, and guests have access to a year-round indoor heated swimming pool and an outdoor hot tub. Sip complimentary morning coffee accompanied by muffins in front a crackling fire in the inviting lobby before heading out to enjoy some of the many outdoor activities in the area.
A cozy and warm studio accommodation is perfect for a romantic getaway. Waking up to the serenity of the nature and the beautiful views of the mountains provides a peaceful getaway from busy everyday life. The studio is conveniently located near historic downtown Breckenridge, making it perfect for local explorations. Have a romantic shopping trip followed by dinner in the downtown as there are many shops and restaurants to choose from. If you two happen to be ski lovers, you can enjoy skiing in the mountains, but if you don’t ski, just enjoy the snow.
Fort Collins is the perfect base camp for your trip, located just 35 miles from the peaks of Rocky Mountain National Park that soar to more than 13,000 feet and form the Continental Divide. The town of Estes Park sits at the eastern edge of the park. Rocky Mountain National Park covers 410 square miles and includes Longs Peak (14,255 feet high), 18 named peaks above 13,000 feet, 150 named lakes, and the highest continuously paved highway in the U.S. — Trail Ridge Road. The road is usually open from Memorial Day until early October. However, the park is open year-round and lower elevation roads are open during the winter.
Dunton Hot Springs is a luxury hideaway with authentic nineteenth century hand-hewn log cabins and a bath house with natural hot springs in Colorado. Dunton attracts outdoor adventure enthusiasts as well as guests who are looking for a quiet place to relax in natural surroundings. The cabins are located in the San Juan Range of the Colorado Rockies 8,700 feet above sea levels. Guests have access to a two story library and an open-air wedding chapel. Visitors can keep in touch with the outside world through high speed wireless internet access and video conferencing.
At about 68 million years ago, the Front Range began to rise again due to the Laramide orogeny in the west.[58][59] During the Cenozoic era, block uplift formed the present Rocky Mountains. The geologic composition of Rocky Mountain National Park was also affected by deformation and erosion during that era. The uplift disrupted the older drainage patterns and created the present drainage patterns.[60]
Built in 1866, the historic Dove Inn is a quiet, private bed and breakfast a block from Golden's Main Street that provides an ideal getaway for both business and leisure travelers. The inn offers a choice of luxurious guest rooms to suit every taste from historical accommodations overlooking the inn’s beautiful gardens to luxury rooms for the discerning traveler to multi-purpose rooms for larger families and group travelers.
Buena Vista is an historic mining and railroad town that resoundingly lives up to its Spanish name meaning “good views” – you are surrounded by towering mountain peaks that provide a wonderful year-round playground for adventure seekers. The area boasts some of the best river rafting adventures in the country and you can also go hiking, biking, horseback riding, fishing and zip-lining.
At about 68 million years ago, the Front Range began to rise again due to the Laramide orogeny in the west.[58][59] During the Cenozoic era, block uplift formed the present Rocky Mountains. The geologic composition of Rocky Mountain National Park was also affected by deformation and erosion during that era. The uplift disrupted the older drainage patterns and created the present drainage patterns.[60]
Garden of the Gods Park is a registered National Natural Landmark comprised of 1,300 acres of magnificent views and stunning red sandstone formations. TripAdvisor® users voted Garden of the Gods the #1 park in the U.S. and #2 park in the world. Make sure to snap some selfies of you and your partner smooching under Kissing Camels and holding up Balanced Rock.
Another one of the state’s most popular skiing and snowboarding destinations, Steamboat Springs may be a winter wonderland during the chillier months of the year, but the summer brings an endless landscape of green dotted with brilliant wildflowers. This is when this Wild West town really comes alive, with visitors enjoying fly fishing, inner tube rides and rafting trips on the Yampa River, endless scenic hiking and mountain biking trails, and natural hot springs that are ideal for soothing sore muscles afterward. If you can be here around late June/early July, you can attend the legendary annual Hot Air Balloon Rodeo and Art in the Park festival which boasts an extensive display of colorful hot air balloons along with some 50 artist vendors, live entertainment, food and drink vendors, and an interactive children’s art area.
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]
You’ll feel really spoiled (especially in Vail!) with complimentary WiFi, complimentary underground valet parking, free breakfast buffet included a surprisingly hefty selection of pastries, breads, fruits, meats, cheeses, cold cereals, and eggs, as well as juice, tea, and coffee. And the outdoor heated swimming pool is worth taking the plunge just for the view.
The Pierre Shale formation was deposited during the Paleogene and Cretaceous periods about 70 million years ago. The region was covered by a deep sea—the Cretaceous Western Interior Seaway—which deposited massive amounts of shale on the seabed. Both the thick stratum of shale and embedded marine life fossils—including ammonites and skeletons of fish and such marine reptiles as mosasaurs, plesiosaurs, and extinct species of sea turtles, along with rare dinosaur and bird remains—were created during this time period. The area now known as Colorado was eventually transformed from being at the bottom of an ocean to dry land again, giving yield to another fossiliferous rock layer known as the Denver Formation.[58]
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]
From 9,000 ft (2,700 m) to 11,000 ft (3,400 m),[72] the montane forests give way to subalpine forests.[69] Forests of fir and Engelmann spruce cover the mountainsides in subalpine areas. Trees grow straight and tall in the lower subalpine forests, but become shorter and more deformed the nearer they are to the tree line.[72] At the tree line, seedlings may germinate on the lee side of rocks and grow only as high as the rock provides wind protection, with any further growth being more horizontal than vertical. The low growth of dense trees is called krummholz, which may become well-established and live for several hundred to a thousand years old.[72]
