The Oxford Club, Spa & Salon offers a full range of services, whether you are looking for a classical massage or a revitalizing facial. Head to the fitness center to work out with a Personal Trainer, practice yoga, take a spinning class or go indoor rowing. The salon at The Oxford is one of the best places in town for a haircut, blowout and highlights. The Urban Farmer Steakhouse by Sage Restaurant Group is scheduled to open in the summer of 2017. Before dinner, have drinks at the Cruise Room Martini Bar decorated in fun Art Deco style. Hotel guests receive complimentary Escalade car service within a two mile radius. Rooms start at USD $200 per night. Next read: 25 Best Things to Do in Denver and 15 Best Romantic Restaurants in Denver, one of the top Colorado destinations.
This three-story, immaculately furnished lodge can sleep up to 30 people and is located mere minutes from the entrance of Rocky Mountain National Park. It can be divided into two different suites for smaller groups. Overlooking the tranquil Trout Pond, the lodge has everything you need for a perfect family reunion, wedding, retreat or any large gathering.
Visitors come from far reaches to travel America’s highest continuous paved highway. Not for the queasy and open only between Memorial Day — pending the towering walls of winter snow have melted — and Labor Day, two-lane Trail Ridge Road takes explorers across the Continental Divide, past weathered tundra overlooking sweeping valleys and into the clouds at 12,183 feet. The ribbon of a road covers the 46-mile stretch between Estes Park on the park’s east side and the marine town of Grand Lake at the park’s western entrance. There Peak to Peak Highway is another byway near the park, starting in Estes and going through Nederland, Black Hawk and Central City.
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]
From luxury condos in major cities, to furnished beach rentals, cozy ski cabins and more, Tripping.com offers the widest variety of unique accommodations for your next trip. Whether you’re seeking a lakefront cabin for a quick getaway, a modern apartment in New York City, or a beachfront property with sunset views in Hawaii, Tripping.com can help you find and book it all.
It’s hard to beat the majestic setting at The Peaks Resort & Spa in Telluride. This property is surrounded by the dramatic peaks of the Rockies in the southwestern region of the state, and is particularly renowned for its spa. Here you can indulge in a variety of rejuvenating treatments like hot stone therapy, soak in the eucalyptus-filled Jacuzzis or take advantage of personal training sessions. Enjoy your days taking part in outdoor adventures like mountain biking or hiking the spectacular trails and then come back to enjoy a
Central ColoradoFind yourself in Colorado Springs at Pikes Peak. We have five historic trains to transport you back to the days of cowboys and gold mining. Endless trails allow you to enjoy the abundant sunshine and spectacular scenery. A family vacation in Colorado Springs is the smart choice – great lodging values, a long list of low-cost or no-cost activities, and adventure around every corner. Order your free guide today.
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 sun made us lazy, and after following Brian as he made his way upstream I found a wider expanse of sand and gravel, promptly plopping down on a pair of flip flops I had brought in my backpack as a make-shift seat. After identifying the northern harrier hawk over my head, and the savannas sparrows and red-winged blackbirds perched precariously on reeds across the water, I took out my knitting project. I didn’t have to worry about losing Brian; in the valley I could see for miles in both directions.
