Rocky Mountain National Park is a national park of the United States located approximately northwest of Denver in north-central Colorado, within the Front Range of the Rocky Mountains. The park is situated between the towns of Estes Park to the east and Grand Lake to the west. The eastern and western slopes of the Continental Divide run directly through the center of the park with the headwaters of the Colorado River located in the park's northwestern region. The main features of the park include mountains, alpine lakes and a wide variety of wildlife within various climates and environments, from wooded forests to mountain tundra.
The Rocky Mountain National Park Act was signed by President Woodrow Wilson on January 26, 1915, establishing the park boundaries and protecting the area for future generations. In 2023, 4.1 million recreational visitors entered the park. The park is one of the most visited in the National Park System, ranking as the third most visited national park in 2015. In 2019, the park saw record attendance yet again with 4,678,804 visitors, a 44% increase since 2012.
The park has five visitor centers, with park headquarters located at the Beaver Meadows Visitor Centera National Historic Landmark designed by the Frank Lloyd Wright School of Architecture at Taliesin West. National forest lands surround the park on all sides, including Roosevelt National Forest to the north and east, Routt National Forest to the north and west, and Arapaho National Forest to the west and south, with the Indian Peaks Wilderness area located directly south of the park. The 1920s saw a boom in building lodges, including the Bear Lake Trail School, and roads in the park, culminating with the construction of Trail Ridge Road to Fall River Pass between 1929 and 1932, then to Grand Lake by 1938.
Prominent individuals in the effort to create a national park included Enos Mills from the Estes Park area, James Grafton Rogers from Denver, and J. Horace McFarland of Pennsylvania. The national park was established on January 26, 1915. The Continental Divide runs generally northsouth through the center of the park,
A geographical anomaly is found along the slopes of the Never Summer Mountains where the Continental Divide forms a horseshoeshaped bend for about , heading from southtonorth but then curving sharply southward and westward out of the park. The sharp bend results in streams on the eastern slopes of the range joining the headwaters of the Colorado River that flow south and west, eventually reaching the Pacific. Meanwhile, streams on the western slopes join rivers that flow north and then east and south, eventually reaching the Atlantic.
Rocky Mountain National Park is one of the highest national parks in the nation, with elevations from , Sixty mountain peaks over high provide scenic vistas. Several small glaciers and permanent snowfields are found in the high mountain cirques.a drainage that feeds streams and rivers that drain into the Gulf of Mexico. Other mountain passes are La Poudre Pass and Thunder Pass, which was once used by stage coaches and is a route to Michigan Lakes.
Climate
According to the Köppen climate classification system, Rocky Mountain National Park has a Subarctic climate with cool summers and year around precipitation (Dfc). According to the United States Department of Agriculture, the Plant Hardiness zone at Bear Lake Ranger Station (9492 ft / 2893 m) is 5a with an average annual extreme minimum temperature of -15.2 °F (-26.2 °C), and 5a with an average annual extreme minimum temperature of -16.1 °F (-26.7 °C) at Beaver Meadows Visitor Center (7825 ft / 2385 m).
The complex interactions of elevation, slope, exposure and regional-scale air masses determine the climate within the park, A "collision of air masses" from several directions produces some of the key weather events in the region. When cold arctic air from the north meets warm moist air from the Gulf of Mexico at the Front Range, "intense, very wet snowfalls with total snow depth measured in the feet" accumulate in the park.
Elevation
Higher elevation areas within the park receive twice as much precipitation as lower elevation areas, generally in the form of deep winter snowfall. Arctic conditions are prevalent during the winter, with sudden blizzards, high winds, and deep snowpack. High country overnight trips require gear suitable for -35 °F or below. The study began in 2011, orchestrated by members of the academic scientific community in cooperation with the National Park Service and the National Aeronautics and Space Administration (NASA).
thumb|upright|Trees killed by [[mountain pine beetles.]]
, the preceding one hundred years of records indicated an increase in the average annual temperature of approximately .