West Branch Peabody River
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West Branch Peabody River
The West Branch of the Peabody River is a river in the White Mountains of New Hampshire in the United States. It is a tributary of the Peabody River, which flows into the Androscoggin River, which in turn flows east and south into Maine, joining the Kennebec River near the Atlantic Ocean. The West Branch of the Peabody is within the Great Gulf Wilderness of the White Mountain National Forest for most of its length. It is paralleled by the Great Gulf Trail, a popular route for backpackers. The stream rises in Great Gulf, a large glacial cirque on the northern side of Mount Washington. The West Branch flows from the outlet of Spaulding Lake, a tarn seated at the foot of the east face of Mount Clay, and proceeds northeast deeper into the gulf, with Mount Jefferson of the Presidential Range to the west and Chandlers Ridge, a northern spur of Mount Washington, to the east. Upon reaching the outlet of Jefferson Ravine, the river turns east, with Mount Adams and Mount Madison rising a ...
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Peabody River
The Peabody River is a river in the White Mountains of New Hampshire in the United States. It is a tributary of the Androscoggin River, which flows south and east into Maine, joining the Kennebec River near the Atlantic Ocean. The Peabody River rises in Pinkham Notch, on the eastern slopes of Mount Washington. The river flows northeast to the Androscoggin River in Gorham, New Hampshire, collecting tributaries from the Presidential Range to the west and the Carter-Moriah Range to the east. Its most significant tributary is the West Branch of the Peabody River, emerging from Great Gulf, a deep and long glacial cirque surrounded by the peaks of the Presidential Range. New Hampshire Route 16 follows the Peabody River for most of the river's length. See also *List of rivers of New Hampshire This is a list of rivers and significant streams in the U.S. state of New Hampshire. All watercourses named "River" (freshwater or tidal) are listed here, as well as other streams which are eit ...
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White Mountain National Forest
The White Mountain National Forest (WMNF) is a federally managed forest contained within the White Mountains in the northeastern United States. It was established in 1918 as a result of the Weeks Act of 1911; federal acquisition of land had already begun in 1914. It has a total area of (1,225 sq mi). Most of the WMNF is in New Hampshire; a small part (about 5.65% of the forest) is in the neighboring state of Maine. While often casually referred to as a park, this is a national forest, used not only for hiking, camping, and skiing but for logging and other limited commercial purposes. The WMNF is the only national forest located in either New Hampshire or Maine, and is the most eastern national forest in the United States. Most of the major peaks over 4,000 feet high for peak-bagging in New Hampshire are located in the national forest. Over of the Appalachian Trail traverses the White Mountain National Forest. In descending order of land area the forest lies in parts of Graf ...
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List Of Rivers Of New Hampshire
This is a list of rivers and significant streams in the U.S. state of New Hampshire. All watercourses named "River" (freshwater or tidal) are listed here, as well as other streams which are either subject to thNew Hampshire Comprehensive Shoreland Protection Actor are more than long. New Hampshire rivers and streams qualify for state shoreland protection (and are listed here in bold) if they are ''fourth-order'' or larger water bodies, based on the Strahler method of stream order classification. Strahler, A. N. (1952). "Dynamic basis of geomorphology". ''Geological Society of America Bulletin'', 63, 923–938. By drainage basin All New Hampshire rivers ultimately flow to the Atlantic Ocean. The list is sorted by major drainage basin, running from north to south along the Atlantic coast, with respective tributaries arranged based on their entry into the main stream from mouth to source. Where several tributaries enter a single lake, they are listed running clockwise from the lak ...
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Mount Washington Auto Road
The Mount Washington Auto Road—originally the Mount Washington Carriage Road—is a toll road in southern Coos County, New Hampshire that extends from New Hampshire Route 16 in Green's Grant, just north of Pinkham Notch, westward across Pinkham's Grant and Thompson and Meserve's Purchase to the summit of Mount Washington in the White Mountains of the US state of New Hampshire. The road climbs from an altitude of at the bottom to at the top, an average gradient of 11.6%. The road was completed and opened to the public in 1861. Operations The Auto Road may be traversed by private vehicles, and there are also guided tours in vans, called stages. The toll on private cars includes a bumper sticker with the text, "THIS CAR CLIMBED MT. WASHINGTON". No bicycles are allowed on the road, except for participants during specific bicycle events (see below). Weather sensors The road has a series of sensors located at various altitudes along it. The sensors transmit weather data v ...
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Mount Madison
Mount Madison is a mountain in the Presidential Range of New Hampshire in the United States. It is named after the fourth U.S. President, James Madison. Mountains in the Presidential Range are named for U.S. presidents, with the tallest (Mount Washington) named for the first president, the second tallest ( Mount Adams) for the second president, and so on. However, due to a surveying error, Mount Monroe, named after the fifth president, James Monroe, is actually taller than Mount Madison. There are many hiking trails on the mountain. A stretch of the Appalachian Trail traverses just below its summit on the Osgood Trail. The Madison Spring Hut, maintained by the Appalachian Mountain Club, is nestled between Mount Madison and Mount Adams and provides rustic lodging in the summer. Reservations generally need to be made far in advance. Mount Madison is the northernmost peak in the Presidentials. Like most of the range, its summit is above treeline. Due to high winds and low te ...
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Mount Adams (New Hampshire)
Mount Adams, elevation above sea level, is a mountain in New Hampshire, the second highest peak in the Northeast United States after its nearby neighbor, Mount Washington. Located in the northern Presidential Range, Mount Adams was named after John Adams, the second President of the United States. It was given this name on July 31, 1820. To the northeast is Mount Madison and to the southwest is Mount Jefferson. From the summit, Mount Washington can be seen directly to the south. There are two major subsidiary peaks of Mount Adams: Mount Sam Adams and Mount Quincy Adams, named after John Adams' cousin, Revolutionary leader Samuel Adams, and son, President John Quincy Adams, respectively, and two minor sub-peaks, Abigail Adams (named for John Adams' wife Abigail) and Adams 5. The northern side of the mountain ridge is located in Low and Burbank's Grant, and the end of Durand Ridge, and King Ravine, on the north side of Mount Adams are in the town of Randolph (formerly ...
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Presidential Range
The Presidential Range is a mountain range located in the White Mountains of the U.S. state of New Hampshire. Containing the highest peaks of the Whites, its most notable summits are named for American presidents, followed by prominent public figures of the 18th and 19th centuries. The Presidential Range is notorious for having some of the worst weather on Earth, mainly because of the unpredictability of high wind speeds and whiteout conditions on the higher summits. Because of the poor weather conditions, the Presidential Range is often used for mountaineering training for those who go on to climb some of the world's highest mountains, including K2 and Everest. Mount Washington, long home of the highest winds recorded on the surface of the Earth at , is the tallest at , followed by neighboring peaks Mount Adams at and Mount Jefferson at . The range is almost entirely in Coos County. Notable summits The highest mountains in the Presidential Range are named principally fo ...
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Mount Jefferson (New Hampshire)
Mount Jefferson is located in Coos County, New Hampshire, and is the third highest mountain in the state. The mountain is named after Thomas Jefferson, the third president of the United States, and is part of the Presidential Range of the White Mountains. Mount Jefferson is flanked by Mount Adams (to the northeast) and Mount Clay (to the south). The mountain has several interesting features, making it a popular hike. Two distinct ridges lead to its summit: Ridge of the Caps and Castle Ridge. The mountain is surrounded by the three dramatic glacial cirques of Jefferson Ravine, Castle Ravine, and the Great Gulf. Finally, Monticello Lawn is a large expanse of alpine sedge and rush near the otherwise talus-covered summit cone. When viewed from the Mount Washington Auto Road, Jefferson features an arrow-shaped bald patch pointing to its summit. Mount Jefferson has a direct ascent along the Caps Ridge Trail, whose base, Jefferson Notch, is the highest point of any public road in ...
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Mount Clay
Mount Clay is a peak located in Thompson and Meserve's Purchase in Coos County in the Presidential Range of the White Mountains of New Hampshire. It is a rise about long and a few hundred feet tall, with summit elevation of ; it lies on the ridge joining the summits of Mount Washington, about to the south-southeast, with that of Mount Jefferson, about north. The Appalachian Trail, coinciding there with the Gulfside Trail, rises about a hundred feet approaching it northbound, and passes from the summit, below it. The Mt. Clay Loop passes over the summit. The Jewell Trail is a popular choice as a relatively less strenuous route to Mt. Washington's summit; hikers ascending it, eastbound, from the vicinity of the cog rail base station join the Gulfside Trail about from Clay's summit and about below, and give up about in descending the southern tail of Clay, before resuming the ascent of Washington. The mountain is named for Henry Clay, 19th-century senator and U.S. Sec ...
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Tarn (lake)
A tarn (or corrie loch) is a Proglacial lake, proglacial mountain lake, pond or pool, formed in a cirque excavated by a glacier. A moraine may form a natural dam below a tarn. Etymology The word is toponymy, derived from the Old Norse word ''tjörn'' ("a small mountain lake without tributaries") meaning pond. In parts of Northern England - predominantly Cumbria but also areas of North Lancashire and North Yorkshire - 'tarn' is widely used as the name for small lakes or ponds, regardless of their location and origin (e.g. Talkin Tarn, Urswick Tarn, Malham Tarn). Similarly, in Scandinavian languages, a ''tjern'' or ''tjørn'' (both Norwegian) or ''tjärn'' or ''tärn'' (both Swedish) is a small natural lake, often in a forest or with vegetation closely surrounding it or growing into the tarn. The specific technical use for a body of water in a glacial corrie comes from high number of tarns found in corries in the Lake District, an upland area in Cumbria. Nonetheless, there are ...
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Mount Washington (New Hampshire)
Mount Washington is the highest peak in the Northeastern United States at and the most topographically prominent mountain east of the Mississippi River. The mountain is notorious for its erratic weather. On the afternoon of April 12, 1934, the Mount Washington Observatory recorded a windspeed of at the summit, the world record from 1934 until 1996. Mount Washington still holds the record for highest measured wind speed not associated with a tornado or tropical cyclone. The mountain is located in the Presidential Range of the White Mountains, in Coös County, New Hampshire. The mountain is in several unincorporated townships, with the summit in the township of Sargent's Purchase. While nearly the whole mountain is in the White Mountain National Forest, an area of surrounding and including the summit is occupied by Mount Washington State Park. The Mount Washington Cog Railway ascends the western slope of the mountain, and the Mount Washington Auto Road climbs to the summ ...
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Cirque
A (; from the Latin word ') is an amphitheatre-like valley formed by glacial erosion. Alternative names for this landform are corrie (from Scottish Gaelic , meaning a pot or cauldron) and (; ). A cirque may also be a similarly shaped landform arising from fluvial erosion. The concave shape of a glacial cirque is open on the downhill side, while the cupped section is generally steep. Cliff-like slopes, down which ice and glaciated debris combine and converge, form the three or more higher sides. The floor of the cirque ends up bowl-shaped, as it is the complex convergence zone of combining ice flows from multiple directions and their accompanying rock burdens. Hence, it experiences somewhat greater erosion forces and is most often overdeepened below the level of the cirque's low-side outlet (stage) and its down-slope (backstage) valley. If the cirque is subject to seasonal melting, the floor of the cirque most often forms a tarn (small lake) behind a dam, which marks the down ...
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