Tuesday, October 1, 2013

Rocky Mountain National Park

Rocky Mountain National Park is a national park located in the north-central region of the U.S. state of Colorado. It features majestic mountain views, mountain lakes, a variety of wildlife, varied climates and environments—from wooded forests to mountain tundra—and easy access to back-country trails and campsites. The park is located northwest of Boulder, Colorado, in the Rockies, and includes the Continental Divide and the headwaters of the Colorado River.

The park has five visitor centers. The park headquarters, Beaver Meadows Visitor Center, is a National Historic Landmark, designed by the Frank Lloyd Wright School of Architecture at Taliesin West. The park may be accessed by three roads: U.S. Highway 34, 36, and State Highway 7. Highway 7 enters the park for less than a mile, where it provides access to the Lily Lake Visitor Center which is closed indefinitely. Farther south, spurs from route 7 lead to campgrounds and trail heads around Longs Peak and Wild Basin. Highway 36 enters the park on the east side, where it terminates after a few miles at Highway 34. Highway 34, known as Trail Ridge Road through the park, runs from the town of Estes Park on the east to Grand Lake on the southwest. The road reaches an elevation of 12,183 feet (3,713 m), and is closed by snow in winter.

The California Zephyr serves Granby (near the west entrance of the park) by rail from Denver, crossing the Continental Divide through the Moffat Tunnel well south of the park. The park's website suggests Granby as an appropriate rail terminus for visitors, although it lies about sixteen miles from the park without public transportation connections. The park is surrounded by Roosevelt National Forest on the north and east, Routt National Forest on the northwest, and Arapaho National Forest on the southwest.


Geography

Map of Colorado. The area of the Rocky Mountain National Park is in dark red.
Rocky Mountain National Park encompasses 265,761 acres (415.25 sq mi; 1,075.50 km2) of land in Colorado's northern Front Range. The park is split by the Continental Divide, which gives the eastern and western portions of the park a different character. The east side of the park tends to be drier, with heavily glaciated peaks and cirques. The west side of the park is wetter and more lush, with deep forests dominating. The park contains 359 miles (578 km) of trails, 150 lakes, and 450 miles (720 km) of streams. The park contains 72 named peaks higher than 12,000 feet (3,700 m), and over one fourth of the park resides above tree line. The highest point of the park is Longs Peak, which rises to 14,259 feet (4,346 m; surveys before 2002 show 14,255 feet (4,345 m)) above sea level. On the north side of the park, the Mummy Range contains a number of smaller thirteener peaks, including Hagues Peak, Mummy Mountain, Fairchild Mountain, Ypsilon Mountain, and Mount Chiquita. Several small glaciers and permanent snowfields are found in the high mountain cirques, including Andrews, Sprague, Tyndall, Taylor, Rowe, Mills, and Moomaw Glaciers.


History

Evidence has shown that Native Americans have visited the area of the park for the last 10,000 years. Their influence in the region was limited, however, and their visits often transitory. The Ute Tribe visited the west side of the park, particularly around Grand Lake. The Arapaho visited and hunted in the Estes Park region. The Long Expedition, led by Stephen H. Long, for whom Longs Peak was named,visited the area in 1820, though they never entered the mountains.
In 1859 while on a hunting expedition, Joel Estes and his son discovered the meadows that eventually became Estes Park. He moved his family there in 1860 and raised cattle. He stayed only until 1866, forced out by long, harsh winters. In the next years, settlers and homesteaders staked their claims in the Estes Park region. Tourists, particularly those interested in climbing the high peaks of the region, appeared after this time.

In 1880 a small mining rush began in the Never Summer Mountains. The mining town of Lulu City was established with great fanfare and promotion by the media, particularly by Fort Collins newspapers. The ore mined, however, was low grade; by 1883 the rush went bust, and most of the residents moved on. A satellite town, Dutchtown, was abandoned by 1884.

Enos Mills, then a 14-year-old boy, moved to Estes Park in 1884. He explored the mountains of the area and wrote many books and articles describing the region. He later supported the creation of Rocky Mountain National Park, and he split his time between the mountains he loved and the cities of the eastern United States, where he lobbied for the legislation to create the park. The legislation was drafted by James Grafton Rogers, a Denver lawyer and avid outdoorsman. Mills' original proposal for park boundaries went from Wyoming all the way down to the Mount Evans area, including areas such as the Indian Peaks Wilderness. Much of the land was favored for mining, logging, and other operations, however, so the proposed park was reduced to an area approximating the current park borders. The bill passed Congress and was signed by President Woodrow Wilson on January 26, 1915. A formal dedication ceremony was held on September 4, 1915 in Horseshoe Park. The park has expanded over the years, with the largest parcel — the Never Summer Range — added in 1929.

The 1920s saw a boom in building lodges and roads in the park, culminating with the construction of Trail Ridge Road between 1929 and 1933. The Civilian Conservation Corps handled several building projects during the Great Depression and remnants of their camps can be found in the park today. On June 24, 2010, a wildfire burned over 1,500 acres (6.1 km2) of the park in Larimer County near Estes Park. Estes Park Fire Department believed that lightning may have started the fire.


Popular areas

Longs Peak seen from Dream Lake trail

The park is dominated by Longs Peak, which is visible from many vantage points, and has an elevation of 14,259 feet (4,346 m). Each year thousands of people attempt to scale it. The easiest route is the Keyhole Route, impassable to regular hikers in all but the hottest summer months due to snow and ice. This eight-mile (13 km) one-way climb has an elevation gain of 4,850 ft (1,480 m). The vast east face, including the area known as The Diamond, is home to many classic big wall rock climbing routes. Not all leave Longs Peak alive and safe. There is a stone gazebo at the Keyhole formation with a plaque memorializing Agnes Vaille, a well-known climber in the 1920s. In January 1925, Vaille fell 100 ft (30 m) while descending the North Face. Vaille survived the fall with minor injuries, but was unable to walk. Her climbing partner, professional mountaineering guide Walter Kiener, went for help; but when rescuers arrived, Vaille had died of fatigue and hypothermia. One of the rescuers, Herbert Sortland, froze to death after breaking his hip while trying to rescue her.


Hallett Peak

Bear Lake, in the heart of the park, is a popular destination and trailhead. The lake lies below Hallett Peak and the Continental Divide. Several trails start from the lake, ranging from easy strolls to strenuous hikes. Bear Lake Road is open year round, though it may close temporarily due to bad weather.


Grand Lake

Trail Ridge Road connects the town of Estes Park in the east with Grand Lake in the west. The road reaches an altitude of 12,183 feet (3,713 m), with long stretches above tree line. It passes the Alpine Visitors' Center, a popular destination, and crosses the Continental Divide at Milner Pass. Numerous short interpretive trails and pullouts along the road serve to educate the visitor on the history, geography, and ecology of the park. The southern area of the park is Wild Basin, a wild and remote region. Several trails cross the area and backpacking it is popular. 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.

The snow-capped Never Summer Mountains are found in the west side of the park. Here the south-trending Continental Divide takes a brief sharp northward loop, which creates an interesting reverse scenario, where the Pacific Basin is on the east side of the divide and the Atlantic Basin on the west. The mountains themselves, the result of volcanic activity, are craggy and, more often than not, covered in deep snow. This area saw the most extensive mining in the park, and trails lead past old mines and ghost towns.


Paradise Park is hidden in the peaks above Grand Lake. This rugged and wild area has no trails penetrating it.

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