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Pemigewasset River
The Pemigewasset River , known locally as "The Pemi", is a river in the state of New Hampshire, the United States. It is in length and (with its tributaries) drains approximately . The name "Pemigewasset" comes from the Abenaki word ''bemijijoasek'' əmidzidzoasək meaning "where side (entering) current is". Geography The Pemigewasset originates at Profile Lake in Franconia Notch State Park, in the town of Franconia. It flows south through the White Mountains and merges with the Winnipesaukee River to form the Merrimack River at Franklin. The Merrimack then flows through southern New Hampshire, northeastern Massachusetts and into the Atlantic Ocean. The Interstate 93 highway runs parallel with the river between Franconia Notch and New Hampton. The river passes through the communities of Lincoln, North Woodstock, Woodstock, Thornton, Campton, Plymouth, Holderness, Ashland, Bridgewater, Bristol, New Hampton, Hill, Sanbornton, and Franklin. The river descends over water ...
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Franconia Notch
Franconia Notch (elev. ) is a major mountain pass through the White Mountains of New Hampshire. Dominated by Cannon Mountain to the west and Mount Lafayette to the east, it lies principally within Franconia Notch State Park and is traversed by the Franconia Notch Parkway (Interstate 93 and U.S. Route 3). The parkway required a special act of Congress to sidestep design standards for the Interstate highway system because it is only one lane in each direction. Kimberly A. Jarvis, ''From the Mountains to the Sea: Protecting Nature in Postwar New Hampshire'' (University of Massachusetts Press, 2020online review/ref> The notch was home to the Old Man of the Mountain, a rock formation which collapsed in 2003 but whose profile remains a symbol of the state of New Hampshire. The notch is located primarily in the town of Franconia but extends south into Lincoln. It is bordered to the east by Franconia Ridge, comprising Mount Lafayette (), Mount Lincoln (), and Little Haystack Mountai ...
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Hill, New Hampshire
Hill is a town in Merrimack County, New Hampshire, United States. The population was 1,017 at the 2020 census. It is home to William Thomas State Forest. History Originally granted as "New Chester" in 1753, the town took the name "Hill" in 1837 in honor of Isaac Hill, governor of New Hampshire from 1836 to 1839. To accommodate the construction of the Franklin Falls Dam, the village of Hill was relocated in 1941. Geography According to the United States Census Bureau, the town has a total area of , of which are land and are water, comprising 0.66% of the town. The Pemigewasset River forms the eastern boundary of the town, and its tributary the Smith River forms two portions of the northern boundary. The southwest corner of the town drains south via Mountain Brook to the Blackwater River in neighboring Andover, a tributary of the Contoocook River. Via the Pemigewasset and Contoocook rivers, Hill lies fully within the Merrimack River watershed. The highest point in town is ...
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Smith River (Pemigewasset River Tributary)
The Smith River is a river located in central New Hampshire in the United States. It is a tributary of the Pemigewasset River, part of the Merrimack River watershed. The Smith River begins at the outlet of Tewksbury Pond in Grafton, New Hampshire. The river flows southwest and then southeast through Grafton, passing through Kilton Pond. Continuing through Danbury, the river remains generally flat until shortly before reaching the Alexandria-Hill town line, where it enters a narrow valley and produces several miles of whitewater. Passing under the New Hampshire Route 3A bridge at the Bristol-Hill town line, the Smith River drops over Profile Falls and arrives at the Pemigewasset River. U.S. Route 4 follows the Smith River from its source to Danbury. NH-104 follows the river from Danbury to the east side of Alexandria. 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" ...
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Newfound River (New Hampshire)
The Newfound River is a river in central New Hampshire in the United States. It is a tributary of the Pemigewasset River, part of the Merrimack River watershed. The Newfound River begins at the outlet of Newfound Lake in Bristol, New Hampshire. The river drops rapidly through the town of Bristol, passing over several hydroelectric dams before reaching the Pemigewasset. Major tributaries of the Newfound River (via Newfound Lake) are the Fowler River and the Cockermouth River. 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 either subject to thNew Hampshire Comprehensive Shoreland ... References Tributaries of the Merrimack River Rivers of New Hampshire Rivers of Grafton County, New Hampshire {{NewHampshire-river-stub ...
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Baker River (New Hampshire)
The Baker River, or ''Asquamchumauke'' (an Abenaki word meaning "salmon spawning place"), is a river in the White Mountains region of New Hampshire in the United States. It rises on the south side of Mount Moosilauke and runs south and east to empty into the Pemigewasset River in Plymouth. The river traverses the towns of Warren, Wentworth, and Rumney. It is part of the Merrimack River watershed. The Baker River's name recalls Lt. Thomas Baker (1682–1753), whose company of 34 scouts from Northampton, Massachusetts, passed down the river's valley in 1712 and destroyed a Pemigewasset Indian village. Along this river on April 28, 1752, John Stark and Amos Eastman were captured by Abenaki warriors and taken to Saint-François-du-Lac, Quebec, near Montreal. John Stark's brother William Stark escaped, and David Stinson was killed during the ambush. On the 1835 Thomas Bradford map of New Hampshire, the river is shown as "Bakers" River, originating on "Mooshillock Mtn." Major t ...
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Moosilauke Brook
Moosilauke Brook is a stream in the White Mountains of New Hampshire in the United States. It is the downstream continuation of the Lost River and is a tributary of the Pemigewasset River, part of the Merrimack River watershed. Moosilauke Brook begins in the eastern part of Kinsman Notch, where the Lost River, flowing out of the center of the notch, joins Jackman Brook entering from the south. Moosilauke Brook runs northeast, passing through the granite gorge of Agassiz Basin and joining the Pemigewasset River in the village of North Woodstock. New Hampshire Route 112 follows Moosilauke Brook for its entire course. 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 either subject to thNew Hampshire Comprehensive Shorelan ... References Tributaries of the Merrimack River Rivers of Ne ...
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Winnipesaukee River
The Winnipesaukee River is a river that connects Lake Winnipesaukee with the Pemigewasset and Merrimack rivers in Franklin, New Hampshire. The river is in the Lakes Region of central New Hampshire. The river's drainage area is approximately . The river has two distinct sections. The upstream section consists of a series of river courses connecting a chain of lakes, beginning with Lake Winnipesaukee. From the dam at the outlet of Lake Winnipesaukee in the Lakeport section of Laconia, the river almost immediately enters Opechee Bay. down the lake, the river exits over a dam and drops through the center of Laconia, its banks lined by industrial buildings from the 19th century that were constructed to take advantage of the river's power. The section through Laconia ends at Lake Winnisquam, the fourth-largest lake in New Hampshire. A stretch across Winnisquam leads to the dam at the lake's outlet and a short descent to Silver Lake. The river's lower section begins at the nat ...
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Squam River
The Squam River is a river located in central New Hampshire in the United States. The river is the outlet of Squam Lake, the second-largest lake in New Hampshire, and it is a tributary of the Pemigewasset River, which itself is a tributary of the Merrimack River. The Squam River first appears as a narrow channel in Holderness, New Hampshire, between Squam Lake and Little Squam Lake downstream. The two lakes have the same elevation, due to a dam below the outlet to Little Squam, so the river in Holderness village is not free-flowing. Below Little Squam Lake the river proceeds south for over a mile before reaching the dam which controls the two lakes' water level. Below this point, the river quickly reaches the backwater from a mill dam in the town of Ashland. In Ashland, the river drops in , sufficient to provide hydropower for numerous industries when the town originally grew in the 19th century. Below the center of town, the river wanders southeast under railroad tracks and ...
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Beebe River
The Beebe River is a river located in the White Mountains of New Hampshire in the United States. It is a tributary of the Pemigewasset River, part of the Merrimack River watershed. The Beebe River begins at Black Mountain Pond on the southern slopes of Sandwich Mountain, a summit in the southern White Mountains, in the town of Sandwich. The river drops off the mountain to the south, then turns west to travel through Sandwich Notch, staying in a wooded valley and entering the town of Campton. The valley broadens as the river approaches the village of Campton Hollow, where the river reaches New Hampshire Route 175 and drops over some small waterfalls. The river passes by the old industrial community of Beebe River and reaches the Pemigewasset River next to Interstate 93. 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 wel ...
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Mad River (Pemigewasset River Tributary)
The Mad River is a river in the White Mountains of New Hampshire in the United States. It is a tributary of the Pemigewasset River, part of the Merrimack River watershed. The Mad River begins at the Greeley Ponds in Mad River Notch, a mountain pass between Mount Osceola to the west and Mount Kancamagus to the east, in the township of Livermore. The river descends to the south, followed by the Greeley Pond Trail, to the town of Waterville Valley, where the West Branch enters. After winding through the Waterville Valley Resort community, the Mad River proceeds southwest over continuous boulder-strewn rapids into a corner of the town of Thornton, eventually settling out in Campton Pond in the town of Campton. Passing over a small hydroelectric dam at Campton Upper Village, the river descends over some small waterfalls and enters the floodplain of the Pemigewasset River, which it joins near Interstate 93. For most of the river's length below Waterville Valley, it is parall ...
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East Branch Pemigewasset River
The East Branch of the Pemigewasset River is a river located in the White Mountains of New Hampshire in the United States. It is a tributary of the Pemigewasset River, part of the Merrimack River watershed. The East Branch is a longer and larger river than the river that it flows into, but it is named a branch of the main stem because its source lies deep in the Pemigewasset Wilderness of the White Mountains, while the main Pemigewasset River flows directly from Franconia Notch, a major pass through the mountains. The East Branch begins in the locality known as Stillwater, in a wide valley north of Mount Carrigain and Mount Hancock, where several large brooks converge. The river flows west and southwest through the heart of the Pemigewasset Wilderness, picking up tributaries such as the North Fork of the Pemigewasset and Franconia Branch before reaching, at the Lincoln Woods Visitor Center, the Kancamagus Highway stretch of New Hampshire Route 112. Now into developed are ...
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Flume Gorge
The Flume Gorge (locally, just The Flume) is a natural gorge extending horizontally at the base of Mount Liberty in Franconia Notch State Park, New Hampshire, United States. Cut by Flume Brook, the gorge features walls of Conway granite that rise to a height of and are apart. Discovered in 1808 by 93-year-old "Aunt" Jess Guernsey, the Flume is now a paid attraction that allows visitors to walk through it from May 10 to October 20. Pets are not allowed. Geology Nearly 200 million years ago in the Jurassic period, the Conway granite that forms the walls of the Flume was deeply buried molten rock. As it cooled, the granite was broken by closely spaced vertical fractures that lay nearly parallel in a northeasterly direction. Sometime after the fractures were formed, small dikes of basalt were forced up along the fractures. The basalt came from deep within the earth as a fluid material, and because of pressure, was able to force the Conway granite aside. The basalt crystalli ...
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