^ Jump up to: a b "Landscape Climate Change Vulnerability Project; Using NASA Resources to Inform Climate and Land Use Adaptation; Ecological Forecasting, Vulnerability Assessment, and Evaluation of Management Options Across Two US DOI Landscape Conservation Cooperatives" (PDF). montana.edu. Montana State University. August 2011. pp. 2, 5. Retrieved February 5, 2017.
The park's climate is also affected by the Continental Divide, which runs northwest to southeast through the center of the park atop the high peaks. The Continental Divide creates two distinct climate patterns - one typical of the east side near Estes Park and the other associated with the Grand Lake area on the park's west side.[49] The west side of the park experiences more snow, less wind, and clear cold days during the winter months.[49]
Classic Estes Park cabins are a popular choice for visitors to this Front Range mountain town. From cozy and rustic to something a little more luxurious, FlipKey has something to suit every style and budget. Many cabin rentals in Estes Park are equipped with full kitchens and fireplaces, and some have luxury touches such as hot tubs and underfloor heating. Condos in Estes Park are a good alternative to a hotel, offering many of the same amenities but with a more personal touch.
Located near the towns of Cortez and Mancos, Mesa Verde is reached by a long road that leads high up above the surrounding landscape. The drive from the highway up to the site takes about 45 minutes. Near the highway is one of the visitor centers, where you can get information on the park and road conditions before driving up. You can book a ranger-led tour of Cliff Palace when you arrive so you know what time to show up for the one-hour tour.
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]
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]
Stay in 1 of our 5 renovated riverfront cabins for a romantic atmosphere away from daily routine. With a private hot tub overlooking Fall River & a jetted spa tub for 2 in the living area, fireplace, full kitchen & gas grill on the deck, you can rest & reconnect. Nestled among tall Ponderosa pines just 1 mi. west of downtown, with easy access to RMNP. Fall River Cabins Details
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.
