If you’re interested in visiting the iconic archaeological sites in Mesa Verde National Park, a trip to Durango is in order. This southwestern Colorado city is the closest town to the Puebloan cliff dwellings, and even offers convenient day trips for travelers who are strapped for time. While you’re in town, take the Million Dollar Highway through the San Juan National Forest for some of the best views in the region.
Estes Park vacation rentals are always worth considering, but be sure to check the calendar before you book and you could enjoy something even more special. Estes Park hosts a variety of events throughout the year, any of which would make a great addition to your vacation itinerary. For example, in early June, the Estes Park Jazz Fest takes place and features jazz musicians from across the country and beyond. 

With stunning Colorado surroundings and easy access to a national park, a visit to an Estes Park vacation rental will capture the whole family's imagination. Sitting at 7,522 feet above sea level, this town is a favorite Colorado getaway due to its proximity to the Rocky Mountain National Park, landmarks such as the historic Stanley Hotel, and a variety of galleries and family-friendly museums that are well worth a visit. Whether you're visiting in the summer or winter, our Estes Park cabin rentals are the perfect setting for an unforgettable trip. 
After your fireside meal, retreat to one of the private, wooden hot tubs tucked in the middle of the woods. A hand-held stroll along the forest path to a bubbling tub overlooking the city's lights will set the perfect mood. Take it to the next level and request a night's stay in the old firehouse on the tip-top of the mountain. There's no better view — maybe anywhere in the state.  

Estes Park is home to the headquarters of the Rocky Mountain National Park, and for many visitors, it’s the first stop en route to a Rocky Mountain vacation. Find yourself passing through to pick up maps and check trail conditions, or stay for a weekend getaway that offers unbeatable access to the Rockies, meaning you can hike all day and dine and unwind at night. The lively town has plenty of entertainment like the downtown Riverwalk,  Aspen and Evergreen Gallery, and the historic Stanley Hotel.
Colorado’s biggest city, Denver offers an eclectic mix of attractions, from its trendy eateries to its impressive museums. A combination of a cityscape and natural surroundings, Denver is more than just a base to explore Colorado’s other outdoor treasures. Boasting a laid-back ambiance, this Mile High City is centered around an outdoorsy culture of locals that welcome visitors to sample their delicious craft beer, vibrant shopping streets and beautiful hiking paths. Spend a day at the Denver Art Museum, Denver Museum of Nature & Science or the Denver Zoo, then browse Larimer Square and catch a game at Coors Field.
If you were any closer to the national park, you'd be in it! No street lights, power lines or major roads. Just peace, wilderness & wildlife, and sounds of the river! Each of our 12 cabins is unique & comfy. Walk to Park trails, or fish the Big Thompson River.  Just 2.5 miles west of downtown Estes Park, dining & shopping options are never far away.  Aspen Brook Details.
Observing wildlife is one of the most popular activities in the Rockies. A drive through the park at dusk during the summer is sure to guarantee viewing of herds of elk and mule deer. And throughout the rest of the year, moose, bighorn sheep, black bears, coyotes, cougars, eagles, hawks and scores of smaller animals like pikas and marmots delight wildlife-watchers of all ages.
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.
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]
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            “By 1900, the growing national conservation and preservation movement, led by Theodore Roosevelt, Gifford Pinchot, and John Muir, advocated an appreciation for nature. The Estes Park Protective and Improvement Association fostered local conservation efforts. "Those who pull flowers up by the roots will be condemned by all worthy people," they warned. In 1909, Enos Mills, a naturalist, nature guide, and lodge owner, championed the creation of the nation's tenth national park. He hoped that: "In years to come when I am asleep beneath the pines, thousands of families will find rest and hope in this park." Unleashing his diverse talents and inexhaustible energy, he spent several years lecturing across the nation, writing thousands of letters and articles, and lobbying Congress to create a new national park. Most civic leaders supported the idea, as did the Denver Chamber of Commerce and the Colorado Mountain Club. In general, mining, logging, and agricultural interests opposed it. On January 26, 1915, President Woodrow Wilson signed the Rocky Mountain National Park Act.”
The famous hot springs of Glenwood is a must-see and do for all romantics. Located in Glenwood Springs, less than 3 hours from Denver, the historic and local family-owned Hotel Denver spans more than 100 years with many stories to tell, including Colorado immigrants, prohibition, gangsters, world wars, and even a Wild West shooting or two. This Colorado hotel has bragging rights to prime real estate in historic downtown Glenwood Springs, close to the train, many restaurants, shopping, the Hot Springs Pool, and our personal favorite, the Iron Mountain Hot Springs.
Located one mile from the main entrance of Rocky Mountain National Park and two miles from Estes Park, Rams Horn Village Resort offers 46 luxury cabins, a heated outdoor swimming pool in the summer, three outdoor, year-round hot tubs, a fitness center and a playground on over seven acres of landscaped grounds. Every amenity at Rams Horn is free to use with your reservation and every cabin will turn into a second home.
Old-fashioned hospitality is the specialty at Sylvan Dale in Loveland. During August and September, the guest ranch offers great grown-up getaways complete with home-style meals and a personal horse for your stay, plus options for overnight trail rides, trap shooting and more. Guests lend a hand with ranch chores, but come nighttime, you can kick back by the campfire to toast s’mores and mingle with fellow guests who might just feel like family by the end of your stay. Find more dude ranches in Colorado >>

Would you like to stay in a historic red barn, a former milk room, or an original historic log cabin and get an idea of how the original Colorado settlers lived? Converted to the luxury Four Mile Creek Bed and Breakfast, this former 1885 homestead is a quaint reminder of the area’s adventurous past. With its main lodge building, old converted barn, and two log cabins, the Bed and Breakfast today offers rustic luxury and unparalleled comfort. The rooms are furnished with antique pieces and fireplaces, with luxurious bathrooms featuring claw foot tubs, conveying a sense of times gone by while providing entirely modern comfort and amenities.
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]
Above tree line, at approximately 11,000 ft (3,400 m), trees disappear and the vast alpine tundra takes over.[69] Over one third of the park resides above the tree line, an area which limits plant growth due to the cold climate and strong winds. The few plants that can survive under such extreme conditions are mostly perennials. Many alpine plants are dwarfed at high elevations, though their occasional blossoms may be full-sized.[73]
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