Mount Hood Wilderness
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Mount Hood Wilderness
The Mount Hood Wilderness is a protected wilderness area inside the Mount Hood National Forest, in the U.S. state of Oregon. The area, covering , includes the peak of Mount Hood and its upper slopes, and ranges from temperate rain forests at the lower elevations, to glaciers and rocky ridges at higher elevations. The wilderness wraps around the mountain from west to northeast, and borders Timberline Lodge and Mount Hood Meadows ski lifts on some of the south and east slopes of the mountain. Trails Journeys to the summit are popular. There are opportunities for experienced and novice mountaineers to traverse glaciers, snowfields and steep volcanic soil, and to deal with rapidly changing and difficult to predict weather. More than 10,000 climbers annually make the attempt, making Mount Hood's summit the most visited snowclad peak in America. Numerous trails circle the mountain, from Lolo Pass on the northwest (which the Pacific Crest Trail crosses) to Cloud Cap on the northeast ...
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Ladd Glacier
Ladd Glacier is an alpine glacier on the north slope of Mount Hood in the U.S. state of Oregon. It lies at an average elevation of . The glacier lies entirely within Mount Hood Wilderness. Between 1907 and 2004, Ladd Glacier lost 37% of its surface area and the glacier terminus retreated over the same time period. See also *List of glaciers in the United States This is a list of glaciers existing in the United States, currently or in recent centuries. These glaciers are located in nine states, all in the Rocky Mountains or farther west. The southernmost named glacier among them is the Lilliput Glacier ... References Glaciers of Mount Hood Glaciers of Hood River County, Oregon Mount Hood National Forest Glaciers of Oregon {{HoodRiverCountyOR-geo-stub ...
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Cloud Cap
In meteorology, a cloud is an aerosol consisting of a visible mass of miniature liquid drop (liquid), droplets, ice crystals, frozen crystals, or other particulates, particles suspended in the atmosphere of a planetary body or similar space. Water or various other chemicals may compose the droplets and crystals. On Earth, clouds are formed as a result of saturation of the air when it is cooled to its dew point, or when it gains sufficient moisture (usually in the form of water vapor) from an adjacent source to raise the dew point to the ambient temperature. They are seen in the Earth's homosphere, which includes the troposphere, stratosphere, and mesosphere. Nephology is the science of clouds, which is undertaken in the cloud physics branch of meteorology. There are two methods of naming clouds in their respective layers of the homosphere, Latin and common name. Genus types in the troposphere, the atmospheric layer closest to Earth's surface, have Latin names because of the ...
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