Mount Washington , the highest peak in the northeastern United States at 1.917 meters above sea level, is the most prominent mountain east of the Mississippi River. It is known for its dangerously erratic weather patterns. For 76 years, until 2010, the Summit Weather Observatory held the record for the highest wind gust measured directly on the Earth's surface, 372 km/h (103 m/s), on the afternoon of April 12, 1934. Before the arrival of European settlers, the mountain was known as Agiocochook, or "Home of the Great Spirit."
In this article we are going to tell you everything you need to know about Mount Washington, its characteristics and origin.
History of Mount Washington

The mountain is located in the Presidential Range in the White Mountains, Sargent Procurement Township, Coos County, New Hampshire. While almost the entire mountain is in the White Mountains National Forest, the 0,24 square kilometer area that surrounds Mount Washington State Park, including the summit.
The first European to mention the mountain was Giovanni da Verrazano. In 1524, he saw it from the Atlantic Ocean, describing what he saw as a "high inland mountain ." The Abenaki people, who lived in the area at the time of European contact, believed the summit was the abode of the gods and, therefore, among other things, did not climb to the summit out of religious respect for the gods. Darbyfield claims the first ascent of Mount Washington in 1642.
Field climbed the mountain in June of that year, demonstrating to Chief Abenaki Pasakonaway that Europeans were not bound by the gods believed to dwell on the mountaintop—a pivotal political move to further the expansion of northern settlers. In October 1642, Field again summited Agiocochook during one of the earliest reconnaissance expeditions to map lands as far away as Maine, aiding a delegation from the Massachusetts colony in seeking to occupy the more arable coastal areas.
In 1784, a geological team led by Manasseh Cutler named the mountain. The Crawford Trail is the oldest hiking trail in the United States, paved in 1819 as a bridle path from Crawford Notch to the summit and still in use today. Ethan Alan Crawford built a hilltop home in 1821 and continued to live there until 1826, the year of a storm.
historical climbs

Little happened to the summit itself until the mid-19th century, when it became one of America's first tourist destinations, with more horse trails and two hotels under construction. Opened in 1852, Summit House is a 60-foot-long stone hotel with a roof secured by four heavy chains. In 1853, the "needle house" was erected for competition. Rebuilt with wood in 1872–1873, Summit House had 91 rooms, burned down in 1908, and was rebuilt with granite in 1915.
For forty years, Henry M. Burt published an intermittent journal called Among the Clouds every summer on the summit until 1917. Copies were distributed to surrounding hotels and other stores by rack and stagecoach.
In November 2010, it was revealed that Orlando, Florida-based CNL Financial, owner of the Mount Washington Hotel at the base of the mountain, had officially applied for a trademark for the name "Mount Washington ." CNL officials said they were targeting other hotels that use the mountain's name, not the many businesses in the area that use it. CNL filed an application with the USPTO seeking to register the "Mount Washington" trademark for any retail service, any restaurant service, and any entertainment service.
Geographic characteristics

Although the western slope ascended by the cog railway is a straight line from the base of the mountain to the summit, the other side is more complicated. To the north, the Great Bay, the mountain's largest glacial ice crater, forms an amphitheater surrounded by the Presidential Mountains to the north: the Clay, Jefferson, Adams, and Madison Mountains. These interconnected peaks spread out across the treeless alpine terrain. The massive Chandler Ridge extends northeast from Mount Washington to form the amphitheater's southern wall and serves as an access ramp to the freeway.
East of the summit, a plateau known as Alpine Gardens extends southward from Chandler Ridge at about 5,000 feet to the south. It is worth noting that both plant species endemic to the alpine meadows of the White Mountains and atypical plant species of the far north Arctic are found here. Alpine Gardens drops sharply into two prominent glacial craters. The rugged Huntington Canyon offers rock and ice climbing in an alpine setting. More rounded, Tuckerman Canyon is New England's premier jurisdiction for backcountry skiing from spring through June, followed by scenic hiking trails. It lies about 500 meters above the alpine tree line.
South of the summit is the second largest alpine plateau, Bigelow Lawn, between 1.500m and 1.700m above sea level. The satellite peaks of the Boott Spur, then Montalban Ridge, which includes Mount Isolation and Mount Davis, extend to the south, while the higher Presidential Mountains (Mount Monroe, Franklin Mountains, Mount Eisenhower, Mount Pierce, Jackson and Webster) they extend southwest to Crawford Canyon and Oaks Bay separates two high ridges.
Hiking Mount Washington
The most popular hike to the summit is via the 4-mile (6,6-kilometer) Tuckerman Canyon Trail. It begins at Pinkham Notch Campground and reaches 4,000 feet, leading directly to the top of Tuckerman Canyon Bowl through a series of steep rock passages that offer spectacular views of the canyon and, through the canyon, to Wildcat Mountain. Skiing accidents and hypothermia have been fatal on the trail. Water bottles can be refilled at the bottom of a pump pit 2 miles (3,4 kilometers) from the trailhead, near a small hiker store that offers snacks, restrooms, and shelter.
At the top is a center that houses the museum, gift shop, gazebo, and cafe. There is a bus service (summer) back to Pinkham Notch Campground for a fee. Other trails that climb the side of the mountain include the Lion Head, Boot Spur, Huntington Ravine, and Nelson Crag trails, and the Great Gulf Trail that climbs from the northeast. Western Slope trails include the Ammonoosuc Ravine and Jewell Trails and the Crawford Trail and Gulfside Trail (which coincide with the Southwest and North Appalachian Trails, respectively).
There are many differences between climbing Mount Washington in summer and climbing it in winter. Of course, the weather and terrain conditions vary widely, but there are also significant differences in the level of services available to visitors. There are no public facilities at the summit in winter. In winter, the most popular route is the Lion's Head Winter Route, which begins in Tuckerman Canyon and turns north to climb Lion's Head to 5,534 feet (1534 meters) above sea level. Route changes are recommended in winter to help climbers avoid avalanche hazards.
Exactly where the trail diverges from the Tuckerman Canyon Trail depends on snow conditions. The Lion's Head Summer Trail may be open if there isn't enough snow. After a 2.2-mile (3,7 km) hike from the Pinkham Notch Visitor Center, the trail will turn right onto the Lion's Head Summer Trail . If there is sufficient snow on the Lion's Head Summer Trail, the Forest Service will open the Lion's Head Winter Trail, which ends in about 1.7 miles (2,7 km).
I hope that with this information you can learn more about the bush in Washington and its characteristics.