ScenicNH Photography - White Mountains New Hampshire

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  • A hiker uses a water filtering system on Meader Ridge Trail during the spring months.  Located in the White Mountains, New Hampshire USA. .Note:
    MD075040.tif
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  • A hiker uses a water filtering system at Unknown Pond in Kilkenny, New Hampshire.
    MD077922.tif
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  • Northern Water Snake (Nerodia sipedon sipedon) in wetlands area in Sandown, New Hampshire
    M092486.jpg
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  • Northern Water Snake (Nerodia sipedon sipedon) in wetlands area in Sandown, New Hampshire
    M092487.jpg
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  • Water Lily during the summer months in a New Hampshire USA pond .  This plant  is part of the  Water-Liiy family .Notes:
    FD076970.tif
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  • Pink water shoes strapped to backpack in the White Mountains, New Hampshire USA
    MD078072.tif
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  • Hiker crossing footbridge along the Thoreau Falls Trail in the Pemigewasset Wilderness of New Hampshire during the winter months. This bridge is in an area referred to as North Fork Junction and crosses the East Branch of the Pemigewasset River. Just beyond this bridge was the location of a timber trestle of the old East Branch & Lincoln railroad (1893-1948). Update: the bridge seen in this photograph is no longer standing, and hikers now have to ford this water crossing.
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  • During the Lincoln, New Hampshire mill era (originally built by James E. Henry and Sons) in order to generate electric power for the mill, water at the Number 1 and Number 2 dams was diverted through large diameter wooden and steel penstock to turbines at the mill. These round steel hoops held the Number 1 Dam wooden penstock together.
    NH177601.jpg
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  • Remnants of the old Crib Dam (also may have be known as the Diversion Dam) on the East Branch of the Pemigewasset River during the spring months in Lincoln, New Hampshire. This dam was one of at least four dams on the East Branch of the Pemi during the Lincoln mill era. And this one was used to control water flow into the mill pond. Most of these timbers were washed away and / or buried during Tropical Storm Irene in 2011.
    NH133826.jpg
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  • A hiker uses a water filtering system on Meader Ridge Trail in the White Mountains, New Hampshire USA during the spring months.
    MD075039.tif
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  • Water chute along Harvard Brook in Lincoln, New Hampshire USA.  This brook is located on the side of the Georgiana Falls Path.
    WM5995-03.jpg
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  • Oak Falls along Black Brook (the Mikaseota) in Warren, New Hampshire during the summer months when the water levels were very low.
    NH168620.jpg
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  • Oak Falls along Black Brook (the Mikaseota) in Warren, New Hampshire during the summer months when the water levels were very low.
    NH168643.jpg
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  • In 2011, high waters from Tropical Storm Irene damaged the Thoreau Falls Trail bridge in the Pemigewasset Wilderness of New Hampshire. This is how the ramp to the bridge looked just days after Tropical Storm Irene. Update: the bridge seen in this photograph is no longer standing, and hikers now have to ford this water crossing.
    SC1113201.jpg
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  • In 2011, high waters from Tropical Storm Irene damaged the Thoreau Falls Trail bridge in the Pemigewasset Wilderness of New Hampshire. This is how the ramp to the bridge looked just days after Irene. Update: the bridge seen in this photograph is no longer standing, and hikers now have to ford this water crossing.
    SC1113223.jpg
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  • Water shoes on rock along the Swift River. This river is located along the Kancamagus Highway (route 112) which is one of New England's scenic byways. Located in the White Mountains, New Hampshire USA
    SC109045.jpg
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  • Piping along the Crawford Path, near Gibbs Brook, in the New Hampshire White Mountains. This piping system and dam (out of sight) supplied water to the old Crawford House. The Crawford House was located where the AMC Highland Center is today. The Crawford Path is the oldest continuously used mountain trail in America, passes by this dam.
    NH184367.jpg
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  • A crane places large sandbags into the East Branch of the Pemigewasset River in Lincoln, New Hampshire USA during the summer months. The sandbags are being used to divert water away from an area along the river that workers will be working in.
    NH1410400.jpg
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  • Pemigewasset Wilderness - High waters from flash floods from Tropical Storm Irene in 2011 cause peeling to the bottom of a footbridge, which crosses the East Branch of the Pemigewasset River along the Thoreau Falls Trail at North Fork Junction in Lincoln, New Hampshire USA. The bridge is supported by two large logs and they look to have received some damage. This tropical storm 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. Update: the bridge seen in this photograph is no longer standing, and hikers now have to ford this water crossing.
    SC1113228.jpg
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  • This how the underside of the Thoreau Falls Trail bridge looked days after Tropical Storm Irene in 2011. High waters from Irene caused peeling to the bottom of the two logs that support the bridge. It crosses the East Branch of the Pemigewasset River in the Pemigewasset Wilderness of New Hampshire. Tropical Storm Irene caused heavy destruction to the White Mountains Trail System. Update: the bridge seen in this photograph is no longer standing, and hikers now have to ford this water crossing.
    SC1113231.jpg
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  • The Thoreau Falls Trail bridge site days after Tropical Storm Irene in 2011. The bridge is supported by two large trees, and high waters from Irene caused peeling to the bottom of the footbridge. It crosses the East Branch of the Pemigewasset River in the Pemigewasset Wilderness of New Hampshire Update: the bridge seen in this photograph is no longer standing, and hikers now have to ford this water crossing.
    SC1112874.jpg
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  • Rushing water flowing over and around the rocks in the White Mountain National Forest of New Hampshire USA which is part of New England
    WM948-04.jpg
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  • Arrowhead- Sagittaria latifolia-in a New England swamp during the summer months. This plant is part of the Water Plantain Family, and its found in shallow water; slow streams, shorelines of lakes and ponds, marshes, and ditches.
    FD076977.jpg
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  • Arrowhead- Sagittaria latifolia-in a New England swamp during the summer months. This plant is part of the Water Plantain Family, and its found in shallow water; slow streams, shorelines of lakes and ponds, marshes, and ditches.
    FD076975.jpg
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  • Kinsman Notch - Remnants of a dam at Beaver Pond in the White Mountains, New Hampshire USA during the spring months.
    SC1210762.jpg
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  • Thoreau Falls Trail bridge days after Tropical Storm Irene in 2011. This bridge crosses the East Branch of the Pemigewasset River at North Fork Junction in the Pemigewasset Wilderness of New Hampshire. This scene shows some of the damage done to the bridge during Tropical Storm Irene. Update: the bridge seen in this photograph is no longer standing, and hikers now have to ford this water crossing.
    SC1113197.jpg
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  • Arrowhead- Sagittaria latifolia-in a New England swamp during the summer months. This plant is part of the Water Plantain Family, and its found in shallow water; slow streams, shorelines of lakes and ponds, marshes, and ditches.
    FD076950.jpg
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  • An old dam on Gibbs Brook near Crawford Path in the New Hampshire White Mountains during the spring months. This dam and piping system (out of sight) supplied water to the old Crawford House. The Crawford House was located where the AMC Highland Center is today. When the Crawford House rebuilt this dam in the 1960s, they reinforced the dam with old iron cots that were in the basement of the Crawford House. These iron cots can be seen in the dam today.
    NH184310.jpg
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  • Shell Cascade in Waterville Valley, New Hampshire during the spring months. Located on Hardy Brook, visitors to the Waterville Valley area have been visiting this waterfall since the 1800s. But no official trail leads to this waterfall today, and during times of high water it can be difficult to reach Hardy Brook.
    NH163368.jpg
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  • Shell Cascade in Waterville Valley, New Hampshire during the spring months. Located on Hardy Brook, visitors to the Waterville Valley area have been visiting this waterfall since the 1800s. But no official trail leads to this waterfall today, and during times of high water it can be difficult to reach Hardy Brook.
    NH163366.jpg
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  • Franconia Notch State Park - The Baby Flume along the Pemigewasset River in Lincoln, New Hampshire during the spring months. This water feature is located below the “Basin” viewing area.
    NH134076.jpg
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  • Water shoes on rocks along the East Branch of the Pemigewasset River in the Pemigewasset Wilderness of Lincoln, New Hampshire USA.
    SC124654.jpg
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  • The Baby Flume on the Pemigewasset River in Franconia Notch State Park in Lincoln, New Hampshire covered in snow. This water feature is located a short ways down river from the “The Basin" viewing area.
    SC123727.jpg
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  • Side view of the Thoreau Falls Trail bridge days after Tropical Storm Irene in 2011. This bridge crosses the East Branch of the Pemigewasset River at North Fork Junction in the Pemigewasset Wilderness of New Hampshire. Tropical Storm Irene caused destruction along the East coast of the United States, and the White Mountain National Forest was officially closed during the storm. Update: the bridge seen in this photograph is no longer standing, and hikers now have to ford this water crossing.
    SC1113237.jpg
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  • An old dam on Gibbs Brook in the New Hampshire White Mountains during the spring months. This dam, rebuilt in the 1960s, and piping system (out of sight) supplied water to the old Crawford House. The Crawford House was located where the AMC Highland Center is today. Crawford Path, the oldest continuously used mountain trail in America, passes by this dam.
    W093590.jpg
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  • An old dam on Gibbs Brook in the New Hampshire White Mountains during the spring months. This dam, rebuilt in the 1960s, and piping system (out of sight) supplied water to the old Crawford House. The Crawford House was located where the AMC Highland Center is today. Crawford Path, the oldest continuously used mountain trail in America, passes by this dam.
    NH184344.jpg
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  • An old dam on Gibbs Brook near Crawford Path in the New Hampshire White Mountains during the spring months. This dam and piping system (out of sight) supplied water to the old Crawford House. The Crawford House was located where the AMC Highland Center is today. When the Crawford House rebuilt this dam in the 1960s, they reinforced the dam with old iron cots that were in the basement of the Crawford House. These iron cots can be seen in the dam today
    NH184347.jpg
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  • The silhouette of a Black Hawk helicopter with hanging water bucket flying over forest fire on Dilly Cliff in Kinsman Notch, New Hampshire in October 2017. These cliffs are located behind the Lost River Gorge and Boulder Caves on Route 112 in North Woodstock.
    NH178432.jpg
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  • Shell Cascade in Waterville Valley, New Hampshire during the spring months. Located on Hardy Brook, visitors to the Waterville Valley area have been visiting this waterfall since the 1800s. But no official trail leads to this waterfall today, and during times of high water it can be difficult to reach Hardy Brook.
    NH163446.jpg
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  • Shell Cascade in Waterville Valley, New Hampshire during the spring months. Located on Hardy Brook, visitors to the Waterville Valley area have been visiting this waterfall since the 1800s. But no official trail leads to this waterfall today, and during times of high water it can be difficult to reach Hardy Brook.
    NH163443.jpg
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  • Water shoes on rocks along the East Branch of the Pemigewasset River in the Pemigewasset Wilderness of Lincoln, New Hampshire USA.
    SC124665.jpg
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  • The Baby Flume on the Pemigewasset River in Franconia Notch State Park in Lincoln, New Hampshire covered in snow. This water feature is located a short ways down river from the “The Basin" viewing area.
    SC123714-1.jpg
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  • Fleming Flume on Elephant Head Brook in Carroll, New Hampshire during the summer months when the water level was very low.
    NH168135.jpg
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  • Footbridge along the Thoreau Falls Trail days after Tropical Storm Irene. This bridge crosses the East Branch of the Pemigewasset River in the Pemigewasset Wilderness of New Hampshire. The White Mountain National Forest was officially closed during Tropical Storm Irene. Update: the bridge seen in this photograph is no longer standing, and hikers now have to ford this water crossing.
    SC1112872.jpg
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  • The Thoreau Falls Trail bridge, which crosses the East Branch of the Pemigewasset River, in the Pemigewasset Wilderness on October 31, 2017. On October 29-30 a storm consisting of heavy rain and strong winds caused extensive damage throughout New Hampshire. The East Branch of the Pemi River flooded around the Thoreau Falls Trail bridge, but the bridge looks to have been untouched. This bridge has a tilt to it that is visible in the photograph. Update: the bridge seen in this photograph is no longer standing, and hikers now have to ford this water crossing.
    NH1710304.jpg
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  • Water bar along the Mt Tecumseh Trail in the New Hampshire White Mountains in 2013. Update: 2018, this section of trail has been worked on and no longer looks like this.
    NH1318540.jpg
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  • Remnants of the water system in the abandoned village of Livermore during the autumn months. This was a logging village in the late 19th and early 20th centuries along the Sawyer River Logging Railroad in Livermore, New Hampshire USA. The town and railroad were owned by the Saunders family.
    NH1511557.jpg
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  • Stark Falls on Stark Falls Brook in North Woodstock, New Hampshire during the spring months. This small water is located in Kinsman Notch.
    NH136056.jpg
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  • Stark Falls on Stark Falls Brook in North Woodstock, New Hampshire during the spring months. This small water is located in Kinsman Notch.
    NH136041.jpg
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  • Non-conforming stone structures (wall) along the Mt Tecumseh Trail in the New Hampshire White Mountains during the summer of 2011. Water bar across trail is per guidelines. Trail maintenance handbooks suggest the best trails show little evidence of trail work and that work should blend in with the surroundings. After a trail inspection by Forest Service in June 2012, the walls on each side of the drainage may be removed because they have no real use.
    SC1113903.jpg
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