Located in in southwestern Colorado, Mesa Verde is home to the famous cliff dwellings of the ancient Anasazi people. It is one of the most significant archeological preserve of Native American culture in the US. In the 12th century, the Anasazi start building houses in shallow caves and under rock overhangs along the canyon walls. The most famous of these is Cliff Palace. The Ancient Puebloans constructed it from sandstone bricks, and mortar made from ash, clay and water. It encompassed 150 rooms and 76 open areas. Climatic change and increased population placed the communities under stress and by the late 1270s, the Ancestral Puebloan population began migrating to what is now New Mexico and Arizona.
The Signature Jill's Restaurant has an outdoor terrace with mountain views and serves contemporary American & French cuisine with organic ingredients. The T-Zero Lounge serves signature martinis, cocktails and fine wine. Live entertainment is offered almost every night. If you are celebrating a special occasion, the private dining room can seat up to 25 guests. The terrace can be reserved for private parties in the summer. Room rates start at $249 per night. Things to Do in Boulder
Explore the nearby great outdoors at the Horsetooth Mountain Open Space or get your adrenaline pumping by rafting on Cache La Poudre River with the Mountain Whitewater Descents Company. Visit Global Village Museum of Arts and Cultures to learn about folk art from all over the world. Take the kids to the Farm at Lee Martinez Park to learn about the farm life and play with baby farm animals.
Located in southwestern Colorado, close to the Four Corners Monument where Colorado, New Mexico, Arizona and Utah meet, Durango is perfectly positioned for sightseeing and year-round outdoor activities. The town also has a vibrant art scene and you can spend many happy hours visiting a fascinating array of art galleries and live theater attractions.
Whether you like to ski, hike, or just take in the jaw-dropping mountain scenery with a craft beer in hand, you’ll find the perfect weekend getaway in Colorado. From lively cities like Denver and Boulder, to more laid-back locales like Golden and Pagosa Springs—and plenty of world-class ski resorts in between—we’ve compiled a list of 17 of the best weekend getaways in The Centennial State.
Perched on the banks of the San Juan River in Pagosa Springs, this hot-springs haven offers a Relaxation Terrace with five pools that are only accessible to the of-age crowd. The terrace is tucked above the kid-friendly main springs area, and includes a waterfall, fire pit, roman shower, jetted tub and river overlook, along with blissful quiet time. Access to the terrace is complimentary for hotel guests and is available to day visitors for a small fee.
The park is home to many predatory animals, including Canadian lynx, foxes, bobcat, cougar, black bear, and coyotes. Wolves and grizzly bears were extirpated in the early 1900s. Most of these predators kill smaller animals, but mountain lions and coyotes kill deer and occasionally elk. Bears also eat larger prey. Moose have no predators in the park. Black bears are relatively uncommon in the park, numbering only 24-35 animals. They also have fewer cubs and the bears seem skinnier than they do in most areas.[79] Canadian lynx are quite rare within the park, and they have probably spread north from the San Juan Mountains, where they were reintroduced in 1999. Cougars feed mainly on mule deer in the park, and live 10–13 years. Cougar territories can be as large as 500 square miles.[80] Coyotes hunt both alone and in pairs, but occasionally hunt in packs. They mainly feed on rodents but occasionally bring down larger animals, including deer, and especially fawns and elk calves. Scat studies in Moraine Park showed that their primary foods were deer and rodents. They form strong family bonds and are very vocal.[81]
The first week of the park shutdown brought little financial impact, said town manager Frank Lancaster, probably because most tourists had already booked their Christmas stays and couldn't cancel. Along the town's main street Wednesday, tourists peered in candy store windows, shopped for T-shirts and rented snowshoes, and there was little sign the nearby park is largely inaccessible.
Diana Rowe is a freelance writer living in suburbia Denver, 20 minutes from downtown and under an hour to the Colorado Rockies. Finding the perfect hotel, whether for leisure or business travel, is an important part of Diana’s travels. Her articles have been featured in Global Traveler Magazine, Business Traveler, Away.com, TripAdvisor.com, Latitudes (American Eagle in-flight), American Cowboy, Persimmon Hill Magazine, Prevue Magazine, and Corporate & Incentive Travel Magazine. She’s also a blogger/writer for TravelingMom.com, TravelShark.com and Cvent.com. Catch up with Diana at www.dianarowe.com or follow her adventures at www.TravelingInHeels.com, Facebook fan page or Twitter @dianarowe
There's more to Michigan than its natural legacies. Ann Arbor's University of Michigan is a must-visit for its Law Quadrangle, the Power Center for the Performing Arts, Natural History Museum, and a series of Gothic structures. One of the longest suspension bridges in the world is the Mackinac Bridge, which joins the Lower Peninsula at Mackinaw City to the Upper Peninsula at St. Ignace. Frankenmuth in mid-Michigan is an interesting replica of a German town, where visitors make a customary stop at Zehnder's or The Bavarian Inn, known for their luscious fried chicken.
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]
Get away and enjoy the surrounding beauty and frequent wildlife visits right from your cabin. Only 3 mi. from Estes Park, our quiet piece of paradise is set on 15 acres of pines & aspen next to RMNP. Full kitchen, living room, and fireplace in all cabins for evening relaxation. Private decks and gas grills. Some w/private hot tubs. Valhalla Resort Details
Region 2 is the alpine region of the park with accessible tundra trails at high elevations—an area known for its spectacular vistas.[35] Within the region are Mount Ida, with tundra slopes and a wide-open view of the Continental Divide, and Specimen Mountain, which has a steep trail and the opportunity to view bighorn sheep and marmots. Forest Canyon Pass is near the top of the Old Ute Trail that once linked villages across the Continental Divide.[40]
The montane ecosystem is at the lowest elevations in the park, between 5,600 to 9,500 feet (1,700 to 2,900 m), where the slopes and large meadow valleys support the widest range of plant and animal life,[69][70] including montane forests, grasslands, and shrublands. The area has meandering rivers[70] and during the summer, wildflowers grow in the open meadows. Ponderosa pine trees, grass, shrubs and herbs live on dry, south-facing slopes. North-facing slopes retain moisture better than those that face south. The soil better supports dense populations of trees, like Douglas fir, lodgepole pine, and ponderosa pine. There are also occasional Engelmann spruce and blue spruce trees. Quaking aspens thrive in high-moisture montane soils. Other water-loving small trees like willows, grey alder, and water birch may be found along streams or lakeshores. Water-logged soil in flat montane valleys may be unable to support growth of evergreen forests.[70] The following areas are part of the montane ecosystem: Moraine Park, Horseshoe Park, Kawuneeche Valley, and Upper Beaver Meadows.[70]
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]
Later in June is the Scandinavian Midsummer Festival, Estes Park's annual celebration of Scandinavian culture. This festival features many Scandinavian and Nordic traditions, such as raising the Maypole, as well as authentic food and drink from the region. There is also dancing, knitting, arts & crafts, and even a reenactment of a Viking camp complete with a Viking ship and sword fight!
The Experience: Hanging Lake in Glenwood Canyon is a summer dream (though it's also incredibly breathtaking in winter when the cascading water freezes). The Colorado River snakes through the center of town, and there's plenty to do outside of this park, making it a lovely destination on its own, but you can also make it a day trip if you're staying in Aspen.
Located just 45 minutes west of Denver, historic Georgetown annually attracts hundreds of visitors who come to experience the history and pioneering spirit of this 1875 mining town. Absorb the atmosphere at museums like the Hamill House Museum, the Georgetown Heritage Center and the Hotel de Paris. Learn all about silver mining as you take a ride to Silver Plume on the historic Georgetown Loop Railway - you can tour the Lebanon Silver Mine en-route.
