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]
Pikes Peak – “America’s Mountain” is one of the most iconic and beautiful vacation destinations in the West. Rising over 14,000 (making it one of Colorado’s many 14-er’s) feet, Pikes Peak has inspired Americans, including Katharine Lee Bates – who wrote “America the Beautiful” after summiting, for generations. There are a number of ways to enjoy it on your Colorado vacation, including by bicycle (ask us about our exciting mountain biking / rafting packages!) Or ride the historic Cog Railway to the top, where a new visitor’s center is being planned. Our tip: try the donuts – they’re amazing! 
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.

Since it’s just the two of you, a tiny house would be a great choice for the most romantic vacation. The small house known as “Dreamy Romance Parisian Honeymoon Cottage” in Colorado is the perfect option for lovebirds. In addition to the comfortable bed and beautiful decor, there is a small, beautiful, private garden where you can have a glass of wine with your partner and watch the changing colors of the gorgeous sunset.
Durango - very popular for romantic getaways in Colorado during the summer, and for good reason. The gorgeously restored Main Ave combines Victorian-era Hotels and Wild-West Saloons, giving the city a remarkable atmosphere. There's plenty of scenic drives nearby, and the steam-engine narrow gauge rail journey up to Silverton is a wonderful daytrip.
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.
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]
Chapin Pass trail traverses a dense forest to beautiful views of the Chapin Creek valley, proceeding onward above timberline to the western flank of Mount Chapin. Tundra Communities Trail, accessible from Trail Ridge Road, is a hike offering tundra views and alpine wildflowers. Other trails are Tombstone Ridge and Ute Trail, which starts at the tundra and is mostly downhill from Ute Crossing to Upper Beaver Meadows, with one backcountry camping site. Cache La Poudre River trail begins north of Poudre Lake on the west side of the valley near Milner Pass and heads downward toward the Mummy Pass trail junction. Lake Irene is a recreation and picnic area.[40]
Situated in Southern Colorado, the Great Sand Dunes National Park is an impressive sight. Shaped by winds blowing from and against the nearby Sangre de Cristo Mountains, the piles of sand climb to more than 750 feet (230 meters), making them the tallest dunes in North America. Sand-boarding, skiing and sledding on the dunes are the park’s most popular activities, and there are medium-size slopes to slide on located near the main parking area. A longer hike to the north brings thrill seekers to a 300-foot (90 meter) slope that tumbles onto into Medano Creek.
The Mummy Range is a short mountain range in the north of the park. The Mummies tend to be gentler and more forested than the other peaks in the park, though some slopes are rugged and heavily glaciated, particularly around Ypsilon Mountain and Mummy Mountain. Bridal Veil Falls is a scenic point and trail accessible from the Cow Creek trailhead, at the Continental Divide Research Center.[41] West Creek Falls and Chasm Falls, near Old Fall River Road, are also in this region. The Alluvial Fan trail leads to a bridge over the river that had been the site of the Lawn Lake Flood.[42]

The Alps Boulder Canyon Inn is an award-winning boutique bed and breakfast in the heart of scenic Boulder Canyon. Offering an unforgettable Boulder experience, the Inn features luxurious accommodations, excellent cuisine, and outstanding service. Surrounding by Boulder's magnificent mountain parks and just a short stroll from downtown Boulder and all its attractions, the Inn is an ideal place for both business and leisure travelers to take advantage of everything the town has to offer.


We really enjoyed our stay at the Solitude Cabins! We stayed in the Dalton's cabin which had very comfortable and clean accommodations with lots of room. The kitchen was complete with everything we needed. With our stay being in December, we were especially excited to see our cabin so adorably decorated for the Holidays, it was so festive! It totally exceeded our expectations! We will most definitely be back!


About 300 million years ago, the land was uplifted creating the ancestral Rocky Mountains.[55] Fountain Formation was deposited during the Pennsylvanian period of the Paleozoic era, 290–296 million years ago. Over the next 150 million years, the mountains uplifted, continued to erode, and covered themselves in their own sediment. Wind, gravity, rainwater, snow, and glacial ice eroded the granite mountains over geologic time scales.[56] The Ancestral Rockies were eventually buried under subsequent strata.[57]
Brian and I descended back to ~7,000 feet for dinner in a small-town Indian restaurant in Nederland, Colorado, west of Boulder. By then, both our heads ached like a bad hangover, and my lungs literally burned when I tried to inhale anything but shallow breaths. Add generalized joint pain, and I had a full-blown case of altitude sickness. Given that I am a noted hypochondriac, I expected the worst. 
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