ScenicNH Photography - White Mountains New Hampshire

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(1749 images)
Your search yielded 1749 images
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  • Saco River in Bartlett, New Hampshire during the spring months. In 2011, Tropical Storm Irene caused major erosion damage along the Saco River. The storm pushed massive amounts of rocks onto the riverbank and changed the path of the river channel in some areas.
    SC129757.jpg
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  • Dry River Wilderness - Foot bridge which crosses the Dry River along the Dry River Trail in Cutt’s Grant of the New Hampshire White Mountains.
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  • Dry River Falls on Dry River in Cutt's Grant in the New Hampshire White Mountains during the summer months. Dry River Falls is located along the Dry River near the Dry River Trail.
    W089152.jpg
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  • Dry River No. 3 shelter along the Dry River Trail in Cutt’s Grant, New Hampshire. This Adirondack-style shelter is located within the Presidential Range - Dry River Wilderness. The original Dry River No. 3 shelter was one of three shelters built along the Dry River Trail in the 1930s; the No.1 shelter and No. 2 shelter were removed, and the No. 3 shelter, seen here in 2008, was rebuilt in 1963.
    SC089179.jpg
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  • Dry River No. 3 shelter along the Dry River Trail in Cutt’s Grant, New Hampshire. This Adirondack-style shelter is located within the Presidential Range - Dry River Wilderness. The original Dry River No. 3 shelter was one of three shelters built along the Dry River Trail in the 1930s; the No.1 shelter and No. 2 shelter were removed, and the No. 3 shelter, seen here in 2008, was rebuilt in 1963.
    SC089177.jpg
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  • Dry River No. 3 shelter along the Dry River Trail in Cutt’s Grant, New Hampshire. This Adirondack-style shelter is located within the Presidential Range - Dry River Wilderness. The original Dry River No. 3 shelter was one of three shelters built along the Dry River Trail in the 1930s; the No.1 shelter and No. 2 shelter were removed, and the No. 3 shelter, seen here in 2008, was rebuilt in 1963.
    SC089171.jpg
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  • Dry River No. 3 shelter along the Dry River Trail in Cutt’s Grant, New Hampshire. This Adirondack-style shelter is located within the Presidential Range - Dry River Wilderness. The original Dry River No. 3 shelter was one of three shelters built along the Dry River Trail in the 1930s; the No.1 shelter and No. 2 shelter were removed, and the No. 3 shelter, seen here in 2008, was rebuilt in 1963.
    SC089170.jpg
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  • Side view of foot bridge along the Dry River Trail in Cutt’s Grant in the New Hampshire White Mountains. Located within the Dry River Wilderness this bridge crosses the Dry River.
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  • Pemigewasset River in Woodstock, New Hampshire USA during the spring months.
    SC1210066.jpg
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  • Pemigewasset River in Woodstock, New Hampshire USA during the spring months.
    SC1210069.jpg
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  • Saco River in Bartlett, New Hampshire during the spring months. In 2011, Tropical Storm Irene caused major erosion damage along the Saco River. The storm pushed massive amounts of rocks onto the riverbank and changed the path of the river channel in some areas.
    SC129772.jpg
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  • Saco River in the Bartlett, New Hampshire during the spring months. In 2011, Tropical Storm Irene caused major erosion damage along the Saco River. The storm pushed massive amounts of rocks onto the riverbank and changed the path of the river channel in some areas.
    SC129761.jpg
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  • Looking upstream at the foot bridge that crosses the Dry River along the Dry River Trail in Cutt’s Grant of the New Hampshire White Mountains.
    SC1140185.jpg
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  • Dry River Wilderness - Foot bridge which crosses the Dry River along the Dry River Trail in Cutt’s Grant of the New Hampshire White Mountains.
    SC117817.jpg
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  • Flash floods from Tropical Storm Irene in 2011 rerouted sections of the Saco River in the New Hampshire White Mountains. This image shows how a section of the Saco River in Bartlett looks today, after Tropical Storm Irene. This storm caused destruction along the East Coast of the United States, and the White Mountain National Forest was officially closed during the storm.
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  • Swift River in Albany, New Hampshire during the summer months. Located in the White Mountains region of New Hampshire, the Swift River originates in Livermore, and flows east for roughly 26 miles before joining the Saco River in Conway.
    SC1110625.jpg
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  • Swift River in Albany, New Hampshire during the summer months. Table Mountain is off in the distance. Located in the White Mountains region of New Hampshire, the Swift River originates in Livermore, and flows east for roughly 26 miles before joining the Saco River in Conway.
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  • Saco River in Bartlett, New Hampshire during the summer months. This is an example of boulder - cobble river channel.
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  • Saco River in Bartlett, New Hampshire during the summer months. This is an example of boulder - cobble river channel.
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  • Saco River in Bartlett, New Hampshire during the summer months. This is an example of boulder - cobble river channel.
    SC119968.jpg
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  • Saco River in Bartlett, New Hampshire during the summer months. This is an example of boulder - cobble river channel.
    SC119952.jpg
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  • Cascade just above Dry River Falls in Cutt's Grant in the New Hampshire White Mountains during the summer months. Dry River is located near the Dry River Trail.
    W089124.jpg
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  • East Branch of the Pemigewasset River in Lincoln, New Hampshire covered in snow at sunrise  on a cloudy winter morning. This river begins deep in the Pemigewasset Wilderness in the area of Stillwater Junction and travels roughly 15.5 miles before joining the Pemigewasset River.
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  • Remnants (railroad spike) of the abandoned railroad at the Gale River Settlement in Bethlehem, New Hampshire. From 1874-1921 a railroad traveled through this area; the railroad was first used by the Gale River Railroad. This logging railroad was in operation from 1874-1878, and it ended at the Gale River Settlement. The Profile & Franconia Notch Railroad would then take over the line and extend it to the Profile House in Franconia Notch. In operation from 1879-1921, this passenger railroad only serviced the Profile House.
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  • Remnants of the railroad bed in the area of the where the old sawmill may have been at the Gale River Settlement in Bethlehem, New Hampshire. From 1874-1921 a railroad traveled through this area; the railroad was first used by the Gale River Railroad. This logging railroad was in operation from 1874-1878, and it ended at the Gale River Settlement, where a sawmill was located. The Profile & Franconia Notch Railroad would then take over the line and extend it to the Profile House in Franconia Notch. In operation from 1879-1921, this passenger railroad only serviced the Profile House. The removal of historic artifacts from federal lands without a permit is a violation of federal law.
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  • Remnants of the abandoned railroad bed at the Gale River Settlement in Bethlehem, New Hampshire. From 1874-1921 a railroad traveled through this area; the railroad was first used by the Gale River Railroad. This was a logging railroad in operation from 1874-1878, and it ended at the Gale River Settlement. The Profile & Franconia Notch Railroad would then take over the line and extend it to the Profile House in Franconia Notch. In operation from 1879-1921, this passenger railroad only serviced the Profile House.
    NH2111337.jpg
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  • East Branch of the Pemigewasset River in Lincoln, New Hampshire covered in snow at sunrise on a cold and cloudy winter morning. This river begins deep in the Pemigewasset Wilderness in the area of Stillwater Junction and travels roughly 15.5 miles before joining the Pemigewasset River.
    NH211743-2.jpg
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  • The Pemigewasset River near the Flume Visitor Center in Franconia Notch State Park in Lincoln, New Hampshire covered in snow on a cloudy autumn day. The 65 mile long Pemigewasset River begins at Profile Lake in Franconia Notch; it travels south and merges with the Winnipesaukee River at Franklin to form the Merrimack River.
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  • The Pemigewasset River near the Flume Visitor Center in Franconia Notch State Park in Lincoln, New Hampshire covered in snow on a cloudy autumn day. The 65 mile long Pemigewasset River begins at Profile Lake in Franconia Notch; it travels south and merges with the Winnipesaukee River at Franklin to form the Merrimack River.
    NH208012.jpg
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  • The Wild Ammonoosuc River in Landaff, New Hampshire during the spring months. During the 1800s, log drives were done on this river down to the Connecticut River.
    NH183710.jpg
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  • Location of where the Number 1 Dam was on the East Branch of the Pemigewasset River in Lincoln, New Hampshire. Built in the early 1900s, this dam was located downstream from today’s Loon Mt. Bridge. Historical references refer to this dam by different names, but the No. 1 Dam seems to be the name most used.
    NH175486.jpg
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  • Big Coolidge Mountain from along the East Branch of the Pemigewasset River behind the Village of Lincoln in Lincoln, New Hampshire during the winter months. This river begins deep in the Pemigewasset Wilderness in the area of Stillwater Junction and travels roughly 15. 5 miles before joining the Pemigewasset River.
    NH131666.jpg
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  • Gale River Forest - Autumn foliage along Gale River Road in the Bethlehem, New Hampshire. Gale River Road is a seasonal road closed during the winter season.
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  • Route 302 bridge in Harts Location, New Hampshire from Forth Iron railroad bridge. These bridges cross the Sawyer River in the White Mountains. The Sawyer River Railroad (1877-1928), traveled along side of this river and through the village of Livermore.
    NH145305.jpg
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  • East Branch of the Pemigewasset River in Lincoln, New Hampshire on a winter morning. This river begins deep in the Pemigewasset Wilderness in the area known as Stillwater Junction and travels roughly 15.5 miles before joining the Pemigewasset River.
    NH141130.jpg
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  • East Branch of the Pemigewasset River in Lincoln, New Hampshire on a winter morning. This river begins deep in the Pemigewasset Wilderness in the area known as Stillwater Junction and travels roughly 15.5 miles before joining the Pemigewasset River.
    NH141123.jpg
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  • East Branch of the Pemigewasset River in Lincoln, New Hampshire on a winter morning. This river begins deep in the Pemigewasset Wilderness in the area known as Stillwater Junction and travels roughly 15.5 miles before joining the Pemigewasset River.
    NH141075-2.jpg
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  • East Branch of the Pemigewasset River behind the Village of Lincoln in Lincoln, New Hampshire during the winter months. This river begins deep in the Pemigewasset Wilderness in the area of Stillwater Junction and travels roughly 15. 5 miles before joining the Pemigewasset River.
    NH131673.jpg
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  • Pemigewasset River in Woodstock, New Hampshire USA during the spring months.
    SC1210063.jpg
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  • East Branch of the Pemigewasset River, near the Lincoln Woods Trail Suspension footbridge, in Lincoln, New Hampshire during the autumn months.
    SC1115496.jpg
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  • Flash floods from Tropical Storm Irene in 2011 rerouted sections of the Saco River in the New Hampshire White Mountains. This image shows how a section of the Saco River in Bartlett looks today, after Tropical Storm Irene. This storm caused destruction along the East Coast of the United States, and the White Mountain National Forest was officially closed during the storm.
    SC1114093.jpg
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  • Flash floods from Tropical Storm Irene in 2011 rerouted sections of the Swift River in the White Mountains, New Hampshire USA. This image shows a new section of the river. This tropical storm / hurricane caused destruction along the East coast of the United States and the White Mountain National Forest of New Hampshire was officially closed during the storm.
    SC1113546.jpg
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  • Before Tropical Storm Irene in 2011 this section was the main channel of the Swift River in the New Hampshire White Mountains. The floods from the storm rerouted this section of river, and it now travels in the forest on the right-hand side.
    SC1113529.jpg
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  • Swift River in Albany, New Hampshire during the summer months. Located in the New Hampshire White Mountains, this scenic river originates in Livermore, and it flows east along the Kancamagus Highway for roughly 26 miles before joining the Saco River in Conway.
    SC1110253.jpg
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  • Swift River in Albany, New Hampshire during the summer months. Located in the New Hampshire White Mountains, this scenic river originates in Livermore, and it flows east along the Kancamagus Highway for roughly 26 miles before joining the Saco River in Conway.
    SC1110251.jpg
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  • River bank erosion along the Swift River in Albany, New Hampshire USA.
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  • River bank erosion along the Swift River in Albany, New Hampshire USA.
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  • River bank erosion along the Swift River in Albany, New Hampshire USA.
    SC114108.jpg
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  • River bank erosion along the Swift River in Albany, New Hampshire USA.
    SC114103.jpg
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  • Mad River Logging Era - Remnants of a splash dam along Flume Brook near the old logging Camp 5 site in Waterville Valley, New Hampshire. Splash dams were used to hold back rushing water during spring melt. And when the gates were opened the strong flow of the brook would push four foot cut logs down the brook to the Mad River. From 1891-1946 +/- this area was logged, and up until 1933 log drives were done on the Mad River to move logs down to Campton Pond.
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