| Rocky Mountain National Park | |
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IUCN Category II (National Park)
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![]() Bierstadt Lake in Rocky Mountain National Park |
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| Location | Larimer, Grand, & Boulder counties, Colorado, USA |
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| Nearest city | Estes Park |
| Coordinates | 40°24′0″N 105°35′0″W / 40.4°N 105.583333°WCoordinates: 40°24′0″N 105°35′0″W / 40.4°N 105.583333°W |
| Area | 265,769 acres (1,075.53 km²) |
| Established | January 26, 1915 |
| Visitors | 2,991,528[1] (in 2009) |
| Governing body | National Park Service |
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, 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.[2]
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. 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 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.
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Rocky Mountain National Park encompasses approximately 265,770 acres (1,076 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.[citation needed]
The park contains 359 miles (578 km) of trails, 150 lakes, and 450 miles (720 km) of streams. The park contains over 60 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) [1]) above sea level. Longs Peak is the only fourteen thousand foot peak in the park.[citation needed]
Several small glaciers and permanent snowfields are found in the high mountain cirques, including Andrews Glacier, Sprague Glacier, Tyndall Glacier, Taylor Glacier, Rowe Glacier, Mills Glacier, and Moomaw Glacier.
The lowest elevations in the park are montane forests and grassland. The ponderosa pine, which prefers drier areas, dominates, though at higher elevations douglas fir trees are found. Above 9,000 feet (2,700 m) the montane forests give way to the subalpine forest. Engelmann Spruce and Subalpine Fir trees are common in this zone. These forests tend to have more moisture than the montane and tend to be denser. Above tree line, at approximately 11,500 feet (3,500 m), trees disappear and the vast alpine tundra takes over. Due to harsh winds and weather, the plants in the tundra are short with very limited growing seasons. Streams have created lush riparian wetlands across the park.
July and August are the warmest months in the park, where temperatures can reach the 80s although it is not uncommon to drop to below freezing at night. Thunderstorms often appear in the afternoons, and visitors should plan on staying below tree line when they occur. Heavy winter snows begin around mid-October, and last into May. While the snow can melt away from the lowest elevations of the park, deep snow is found above 9,000 feet (2,700 m) in the winter, causing the closure of Trail Ridge and Fall River roads during the winter and spring. Most of the trails are under snow this time of the year, and snowshoeing and skiing become popular. Springs tend to be wet, alternating between rain and possibly heavy snows. These snows can occur as late as July. The west side of the park typically receives more precipitation than the drier east side.[citation needed]
The park is dominated by Longs Peak, which is visible from many vantage points, 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, however due to snow and ice the Keyhole Route is impassable to regular hikers in all but the hottest summer months. This eight-mile one-way hike 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 displays 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.
Bear Lake, in the heart of the park, is a popular destination and trailhead. The lake lies below Hallett's 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 adverse weather conditions.
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 is popular there.
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 very craggy and, more often than not, covered in deep snow. This area saw the most extensive mining activity in the park, and trails lead past old mines and ghost towns.
Paradise Park is hidden in the peaks above Grand Lake. This area has no trails penetrating it, and is extremely rugged and wild.
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.[citation needed]
The Long Expedition, led by Stephen H Long, for whom Longs Peak was named,[citation needed] visited the area in 1820, though they never entered the mountains.
In 1859, while on a hunting expedition, Joel Estes and his son stumbled across 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 the majority 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. However, much of this land was favored for mining, logging and other operations, 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 somewhat 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. During the Great Depression, the Civilian Conservation Corps handled several building projects. Remnants of their camps can be found in the park today.[citation needed]
Rocky Mountain National Park was also a place for downhill skiing. Hidden Valley (Ski Estes Park) operated between 1955 - 1991 along U.S. 34, five miles (8 km) west of Estes Park. The area had been skied by locals long before it opened as a ski area[3]
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Rocky Mountain National Park [1] is a United States National Park that is located in the Front Range region of the state of Colorado. The park's borders lie within three counties, Larimer, Boulder, and Grand and it is surrounded by Roosevelt, Arapaho, and Routt National Forests. The Continental Divide cuts almost directly through the center of the park, creating two areas with very different landscapes - a drier and heavily glaciated eastern side, and a wetter, more forested western side. Both areas offer excellent spots for high altitude alpine hiking, backpacking and rock climbing as well as ample opportunity for spotting wildlife. The park is dominated by Longs Peak one of Colorado's 54 "Fourteeners" at 14,259 feet, and dubbed the "Monarch of the Front Range."
Evidence of Native American peoples visiting the park date back almost 10,000 years, mainly from the Ute and Arapaho communities. Several expeditions visited the area in the early to mid 19th century, including one by Joel Estes in 1859 after which he and his family established a homestead that would soon become Estes Park, the resort town that currently sits on the east side of the park. After a small mining rush on the western side of the park in the early 1880s, a 14 year old boy by the name of Enos Mills moved to the area and began to extensively document the region's geography and ecology through essays and books. He began to lobby Congress to establish a national park in the area surrounding Longs Peak, a mountain he had climbed over 40 times by himself. On January 26, 1915, President Woodrow Wilson signed a bill that established the creation of Rocky Mountain National Park. The 1930s brought a building boom to the park during the Great Depression, during which time the Trail Ridge Road was constructed through the park, which remains today the highest continuous stretch of highway in the United States.
Rocky Mountain National Park sits on the Continental Divide, separating the park into two distinct regions. The eastern and more developed side of the park is dominated by striking valleys and cirques that were formed through heavy glaciation and is a good starting point for first-time visitors. The western side of the park is wetter, is heavily forested and is less developed, but still contains excellent trekking and backcountry opportunities. Most areas of the park sit well above 9,000 feet with mountains along the Continental Divide topping off at above 12,000 feet. The 13,000 foot Mummy Range rests on the northern side of Rocky Mountain National Park with two roads skirting long it's southern edges; a one-way, dirt road that winds up the Fall River called the Old Fall River Road; and a section of Highway 34 famously known as the Trail Ridge Road. The Never Summer Mountains sit on the western side of the park and consist of 10 distinct peaks, all rising well over 12,000 feet, and contain the headwaters for the Colorado River. One of the most dominating features in the southeast area of the park is Longs Peak at 14,259 feet, which is surrounded on all sides by several peaks well about 13,000 feet, including Mt. Meeker, Mount Lady Washington, and Storm Peak.
For wildlife seekers, Rocky Mountain National Park offers some fantastic opportunities to view the variety of animals that live inside its borders. Elk, deer, chipmunks, ground squirrels, beavers, porcupines, foxes, and coyotes are all commonly seen in meadows and in and around lakes and streams. Marmots seem to be ubiquitous above the tree line, especially on well-hiked trails around Longs Peak. Hawks and eagles are often seen soaring above the glacier gorges in search of critters that hide among the rocks and colorful tree birds such as blue jays and cardinals fly in the lower altitudes. Hummingbirds have a tendency to close to where people - and their food - are sitting. Less common animal sightings include black bears and the rare mountain lions, although the former will manage to hang out if human food is accessible. Moose mainly stay on the western side of the park and Bighorn Sheep - a rare but exciting find - stay above the tree line and can sometimes be seen off the Trail Ridge Road.
Wildflowers seem to be everywhere throughout the park, including the popular Indian Paintbrush and Columbine, Colorado's state flower. One of the most spectacular sights in the mid to late fall is to walk through a grove of Aspen trees as their leaves change from green to gold. Ponderosa and Lodgepole pines are the dominate conifer trees in the area, although they have been recently dying in large numbers due to an outbreak of pine beetle infestation.
| Climate | Jan | Feb | Mar | Apr | May | Jun | Jul | Aug | Sep | Oct | Nov | Dec |
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| Daily highs (°F) | 38 | 40 | 44 | 53 | 62 | 72 | 78 | 76 | 70 | 60 | 46 | 39 |
| Nightly lows (°F) | 16 | 17 | 20 | 27 | 34 | 41 | 46 | 44 | 37 | 30 | 22 | 17 |
| Precipitation (in) | <1 | <1 | <1 | 1 | 2 | 2 | 2 | 2 | 1 | <1 | <1 | <1 |
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The above measurements are for Estes Park. Temperatures in the mountains can be 10-15°F (5-7°C). |
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Considering the park's high altitude, the weather trends closer toward moderate four-season climate than edging on the extremes. Winters bring heavy snowfall, and although there is rarely a deep-freeze the park gets significantly less visitors. Summer are the high season with warm temperatures ranging in from mid 70s-80°F during the day, but dropping into the low 40s°F to near freezing. Thunderstorms are constantly looming in the early to mid afternoon during the summer, but clear off quickly by evening, bringing crisp and cool weather.
Highway 34 connects Grand Lake and Estes Park across the Continental Divide, giving you awesome views of the western and eastern sides of the park. A great stopping point along the road is the Alpine Visitor Center at the Fall River Pass, which sits at almost 11,800 feet. Colorado Route 7 runs from Estes Park to the south, passing by several trailheads, including those for Lily Mountain, the Twin Sisters, the Longs Peak Ranger Station and the Wild Basin. Many visitors use Bear Lake or Glacier Gorge as their starting point into the park, both of which can be accessed via the Bear Lake Road. The Beaver Meadows and Moraine Park visitor centers are popular destinations for getting oriented with the park's layout, the former having been designed by students of American architect Frank Lloyd Wright.
From the west: The Kawuneeche Visitor Center is one mile north of the town of Grand Lake on US-34. Grand Lake can be reached from I-70 via US-40 which runs through Empire and over the Berthoud Pass.
From the east: The Beaver Meadows Visitor Center is three miles from downtown Estes Park near the terminus of US-36 and can be reached via several roads. SR-7 runs from Boulder via Lyons and Allenspark along the east side of the park, passing the Longs Peak Ranger Station and intersects US-36 in Estes Park. SR-66/US-36 run from Denver through Longmont up the Big Thompson River canyon. US-34 also intersects US-36 in Estes Park via Loveland and continues on into the park toward the Fall River Visitor Center.
Rental cars are available at the Denver International Airport. If you aren't driving, the Estes Park Shuttle [2] offers reasonable one-way and round-trip rates from DEN to downtown Estes Park.
NOTE: While the park is open year-round, the Trail Ridge Road closes in the winter and may not open until the late spring or early summer, depending on the snowpack.
The nearest major airport is Denver International Airport (IATA: DEN) [3] located about 1 hour and 45 minutes away from the park, with connecting service to most major US cities. A smaller option is Eagle County Regional Airport (IATA: EGE) [4] located near the skiing resorts of Vail and Beaver Creek; however, service to this airport is usually seasonal and confined to the winter months.
Entrance fees are $20 per private vehicle or $10 for individuals on foot or on bicycle, valid for seven days. Holders of the National Park Pass ($50, allows entry to all national park areas for one year) do not need to pay an entrance fee. In addition, there is a $35 pass available that allows entry into Rocky Mountain National Park for one year.
If you drive in early in the morning or late at night the fee booth will probably be unmanned. It is rumored that local Larimer County and Grand County residents can pass through the park without paying a fee if they mention that intention to the entrance guards.
Most of the major trailheads in the park are accessible by car and have parking lots depending on the popularity of the route. While parking is relatively ample in the early mornings, many lots are full by mid-morning during the peak summer months. The Trail Ridge Road and Old Fall River Roads are closed during the winter and usually don't reopen till late spring at the earliest. Access to Moraine Park and Bear Lake via the Bear Lake Road are open year-round and plowed.
There are several entrances to the park which do not have fees on the east side of the park:
Starting around Memorial Day Weekend and going through the end of September, Rocky Mountain National Park operates a free shuttle bus service which enables you to access many destination and loop hikes along Bear Lake Road, including Sprague Lake and Glacier Gorge to cut down on traffic congestion and limited parking. Shuttle buses run between many trailheads, Moraine Park Visitor Center, and Moraine Park and Glacier Basin Campgrounds.
There are two routes: The Bear Lake Route and the Moraine Park Route. Both routes are based at the Park & Ride shuttle bus parking area across from the Glacier Basin Campground. The first bus departs from Park & Ride at 7PM. and the last bus leaves at 7PM. The last bus of the day leaves Bear Lake and Fern Lake Trailheads at 7:30PM. The Bear Lake Route shuttle makes the round trip between the Park & Ride and Bear Lake. These buses run every 10 to 15 minutes. The Moraine Park Route shuttle makes the round trip between the Park & Ride and the Fern Lake Trailhead bus stop. These buses run every 30 minutes.
To experience the true beauty of Rocky Mountain National Park means getting out onto some of the 355 miles of trail that wind in, around and over the Continental Divide, Wild Basin, Mummy Range, and more.
Cycling through the park offers riders a chance to take in some of the scenery and striking vistas at a casual pace; however, some may be daunted by the high altitudes and steep climbs on the main roads. Elevations range from 8,000 feet to 12,183 feet (2,400 to 3,700 m). There are 60 miles (97 km) of hard-surfaced road with a five to seven percent grade. Most of the roads in the park have little to no shoulder, with the added challenge of dealing with heavy summer traffic. Early mornings or late evening rides may minimize conflict with other vehicles. Be vigilant for thunderstorms in the early to late afternoons, where lightning can create a serious hazard.
Winter cyclists will have access to Upper Beaver Meadows Road, Moraine Park Campground, Endovalley Road, Aspenglen Campground and High Drive. For a unique cycling experience, check with the park information office for specifics on the Old Fall River Road (gravel surface) and Trail Ridge Road (paved), which are open to bicycles early in the summer season, before they open to vehicles.
Off-road mountain biking is prohibited inside the park.
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