What is more romantic than spending the nights together with your partner in a private cottage located on a creek with views of waterfalls and Pike National Forest? It is more than possible to have a romantic getaway in this serene and beautiful Colorado cottage! Moreover, if you both love adventure, this vacation rental is perfect for hiking and biking together. Be healthy, be strong together!
During the winter most of Trail Ridge Road is closed due to heavy snow, limiting motorized access to the edges of the park.[68] Winter activities include snowshoeing and cross-country skiing which are possible from either the Estes Park or Grand Lake entrances. On the east side near Estes Park, skiing and snowshoeing trails are available off Bear Lake Road, such as the Bear Lake, Bierstadt Lake, and Sprague Lake trails and at Hidden Valley. Slopes for sledding are also available at Hidden Valley. The west side of the park near Grand Lake also has viable snowshoeing trails.[68][88] Backcountry skiing and snowboarding can be enjoyed after climbing up one of the higher slopes, especially late in the snow season after avalanche danger has subsided[89], and technical climbing remains also a possibility, although typically differing in style from the summer months[90].
In Michigan, more than half of the 24,313 accommodations are house rentals, which represent 53.55% of its available accommodations. In addition, these properties have a median size of 1,840 ft² as well as cost, on average, $332 a night. Moreover, these properties are optimal for 8 as that is the average number of vacationers house rentals can host in Michigan. If you are searching for another type of accommodation, you can look for many other offers, such as hotel rooms, which are the other very popular type of property in Michigan. While house rentals in Michigan have an average size of 1,840 ft², hotel rooms have an average size of 420 ft².
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]
Gem Lake is high among the rounded granite domes of Lumpy Ridge. Untouched by glaciation, this outcrop of 1.8 billion-year-old granite has been sculpted by wind and chemical erosion into a backbone-like ridge. Pillars, potholes, and balanced rocks are found around the midpoint of the trail, along with views of the Estes Valley and Continental Divide.[42] Potts Puddle trail is accessible from the Black Canyon trail.[42]
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]
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.
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]
When it comes to the best weekend getaways in Colorado, Colorado Springs is a top choice with a little bit of everything—numerous hiking trails, interesting museums, an artsy historic district, and plenty of restaurants and breweries. It’s also home to Garden of the Gods, a National Natural Landmark featuring hiking, climbing, and stunning views at the foot of Pikes Peak.
