The Pool is a large turbulent water pocket formed below where Spruce and Fern Creeks join the Big Thompson River. The winter route is along a gravel road, which leads to a trail at the Fern Lake trailhead. Along the route are beaver-cut aspen, frozen waterfalls on the cliffs, and the Arch Rocks. The trail to Alberta Falls runs by Glacier Creek and Glacier Gorge.
Hypothermia, or loss of body heat through exposure, is a danger that can be encountered any time of the year. If anyone exhibits shivering, slurred speech, incoherence, stumbling, or drowsiness, get the person out of the wet, cold. and wind, and into shelter and dry, woolen clothing. The quickest way to warm the victim is to place the person in a dry sleeping bag with another person.
The spacious Grand Ballroom – attached directly to the hotel – can accommodate as many as 400 guests, or, reserve just enough space to party in the Latitude 105 Restaurant for a more intimate gathering with your closest friends and family. The Aspen Courtyard makes an open and inviting venue with a fire pit circled by Adirondack chairs and covered dining for up to 250 guests where everyone can enjoy Colorado’s fresh mountain air, with dinner and dancing under the stars.
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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. 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.
Horace Albright, director of the National Park Service between 1929 and 1933, once said about Trail Ridge Road, "It's hard to describe what a sensation this new road is going to make. You will have the whole sweep of the Rockies before you in all directions." Trail Ridge Road was a sensation when it debuted back in 1932 and it remains so today for the travelers that make the 48-mile drive from Estes Park to Grand Lake, rising above the tree line for 11 miles at an elevation of nearly 11,500 feet. Visitors should keep that in mind when they're stopping at the lookout points that the road experiences temperatures that are 20 and even 30 degrees lower than both Estes Park and Grand Park.
If driving Trail Ridge Road or Old Fall River Road is on the top of your list and you have limited time, you may want to enter the park via the Fall River Entrance on the park’s east side. It also is just a few minutes from Estes Park’s downtown. You’ll reach Trail Ridge Road a lot faster than those waiting in line at the Beaver Meadows Entrance during the summer and fall seasons.