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(1058 images)
Your search yielded 1058 images
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  • This is the landslide path just above the Willey Boulders in Crawford Notch in Hart’s Location, New Hampshire. The Willey Boulders saved the Willey House from destruction on August 28, 1826 when a massive landslide came down Mount Willey. These boulders were located just above the house and caused the landslide to split into two debris flows around the house. The house was said to be untouched, but all seven members of the family and two hired men perished in the slide while trying to escape to a safe area.
    SC1124579.jpg
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  • The "Willey Boulders" in Crawford Notch State Park in Hart’s Location, New Hampshire. These boulders saved the Willey House from destruction on August 28, 1826 when a massive landslide came down Mount Willey. These boulders located just above the house caused the landslide to split into two debris flows around the house. The house was said to be untouched, but all seven members of the family and two hired men perished in the slide while trying to escape to a safe area.
    SC1124559.jpg
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  • Jefferson Brook, along Jefferson Notch Road in the New Hampshire White Mountains during the summer months. Built in 1901-1902, the purpose of the Jefferson Notch Road was to connect the Crawford House with Jefferson Highlands.
    W088587.jpg
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  • Wadley Falls during the autumn months which is located along the Lamprey River in Lee, New Hampshire USA
    W0811908.jpg
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  • Wadley Falls during the autumn months which is located along the Lamprey River in Lee, New Hampshire USA
    W0811909.jpg
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  • Wadley Falls during the autumn months which is located along the Lamprey River in Lee, New Hampshire USA
    W0811906.jpg
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  • Wadley Falls during the autumn months which is located along the Lamprey River in Lee, New Hampshire USA
    W0811905.jpg
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  • Wadley Falls during the autumn months which is located along the Lamprey River in Lee, New Hampshire USA
    W0811902.jpg
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  • Jefferson Brook, along Jefferson Notch Road in the New Hampshire White Mountains during the summer months. Built in 1901-1902, the purpose of the Jefferson Notch Road was to connect the Crawford House with Jefferson Highlands.
    W088596.jpg
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  • Jefferson Brook, along Jefferson Notch Road in the New Hampshire White Mountains during the summer months. Built in 1901-1902, the purpose of the Jefferson Notch Road was to connect the Crawford House with Jefferson Highlands.
    W088586.jpg
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  • Small cascade on Stony Brook in Hart’s Location, New Hampshire during the spring months. This brook is on the side of Mount Tremont Trail.
    NH146772.jpg
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  • Small cascade on Stony Brook in Hart’s Location, New Hampshire during the spring months. This brook is on the side of Mount Tremont Trail.
    NH146766.jpg
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  • Swift River in the White Mountain National Forest of  New Hampshire USA
    SC1123517.jpg
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  • Zeacliff Pond Brook in the Pemigewasset Wilderness of Lincoln, New Hampshire USA during the spring months
    W095641.jpg
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  • Zeacliff Pond Brook in the Pemigewasset Wilderness of Lincoln, New Hampshire during the spring months.
    W095638.jpg
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  • Small cascade on Stony Brook in Hart’s Location, New Hampshire during the summer months. This brook is on the side of Mount Tremont Trail.
    W088636.jpg
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  • Small cascade on Stony Brook in Hart’s Location, New Hampshire during the summer months. This brook is on the side of Mount Tremont Trail.
    W088631.jpg
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  • The Basin along the Pemigewasset River in Franconia Notch State Park in Lincoln, New Hampshire. This 20 foot wide pothole is a natural feature along the Pemigewasset River.
    W2789-03.jpg
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  • Brook surrounded by ice and snow. Located in Auburn, New Hampshire, USA.
    WM327-06.jpg
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  • The Basin along the Pemigewasset River in Franconia Notch State Park in Lincoln, New Hampshire surrounded by snow. This 20 foot wide pothole is a natural feature along the Pemigewasset River.
    WM475-06.jpg
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  • Ellen's Falls which are located along Hobbs Brook in Albany, New Hampshire USA
    SC1120737.jpg
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  • Zeacliff Pond Brook in the Pemigewasset Wilderness of Lincoln, New Hampshire during the spring months. This forest was logged during the East Branch & Lincoln Logging Railroad era (1893-1948).
    W095635.jpg
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  • A seasonal waterfall in an old landslide path on the western flank of Mount Lafayette in Franconia Notch, New Hampshire during the spring months. This landslide slide in 1948 and again in 1959, and buried the old Route 3 both times.
    NH183323.jpg
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  • A plastic PVC pipe and metal tag in an old landslide path on the western flank of Mount Lafayette in Franconia Notch, New Hampshire. This landslide slid in 1948 and in 1959, and this pipe and metal tag are possibly remnants of an old study that was done on the landslide. The study focused on the forests recovery from landslides.
    NH183215.jpg
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  • Landslide path on the side of the Hancock Mountain Range in the Pemigewasset Wilderness in Lincoln, New Hampshire in November 2011. Heavy rains from Tropical Storm Irene in August 2011 caused an old landslide that was in the process of being natural regenerated to slide again. The new landslide looks to follow the track of the old one. The natural process of regeneration must start all over.
    SC1120193.jpg
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  • Looking up a landslide on the side of the Hancock Mountain Range in the Pemigewasset Wilderness in Lincoln, New Hampshire in November 2011. Heavy rains from Tropical Storm Irene in 2011 caused an old landslide that was in the process of being natural regenerated to slide again. The new landslide looks to follow the track of the old one. This storm caused extensive damage in the New Hampshire White Mountains.
    SC1120230_103MR.jpg
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  • Landslide on the side of the Hancock Mountain Range in the Pemigewasset Wilderness of Lincoln, New Hampshire in November 2011. Heavy rains from Tropical Storm Irene in 2011 caused a old landslide that was in the process of being natural regenerated to slide again. The natural process of regeneration must start all over. The new landslide looks to follow the track of the old one. This storm caused extensive damage along the East coast of the United States and the White Mountains, New Hampshire.
    SC1120200.jpg
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  • Landslide on the side of the Hancock Mountain Range in the Pemigewasset Wilderness in Lincoln, New Hampshire in November 2011. Heavy rains from Tropical Storm Irene in 2011 caused an old landslide that was in the process of being natural regenerated to slide again. The natural process of regeneration must start all over. The new landslide looks to follow the track of the old one. This storm caused extensive damage along the East coast of the United States and the White Mountains, New Hampshire.
    SC1120169.jpg
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  • Confluence of the North and East Branches of the Pemigewasset River at North Fork Junction in the Pemigewasset Wilderness in Lincoln, New Hampshire. The foreground is the general location of where a trestle, along a spur line, of the East Branch & Lincoln Railroad (1893-1948) crossed the river.
    SC118293.jpg
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  • Confluence of the North and East Branches of the Pemigewasset River at North Fork Junction in the Pemigewasset Wilderness in Lincoln, New Hampshire. This is the general location of where a trestle, along a spur line, of the East Branch & Lincoln Railroad (1893-1948) crossed the river.
    SC118295.jpg
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  • Landslide path on the side of Whitewall Mountain during the autumn months in the White Mountains, New Hampshire USA.
    SC089402.jpg
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  • Skookumchuck Brook during the early summer months which runs on the side of Skookumchuck Trail in the White Mountains, New Hampshire  USA. .
    WD075078.tif
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  • Odiorne Point State Park - The remains of an old rusted pipe on the shoreline of Fort Dearborn, which is an old fort located in Rye, New Hampshire
    SF22-06.tif
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  • Waves crashing over rocks along the New Hampshire USA coast.
    S227-06.tif
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  • A seasonal waterfall in an old landslide path on the western flank of Mount Lafayette in Franconia Notch, New Hampshire during the spring months. This landslide slide in 1948 and again in 1959, and buried the old Route 3 both times.
    NH183310.jpg
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  • A seasonal waterfall in an old landslide path on the western flank of Mount Lafayette in Franconia Notch, New Hampshire during the spring months. This landslide slide in 1948 and again in 1959, and buried the old Route 3 both times.
    NH183308.jpg
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  • A seasonal waterfall in an old landslide path on the western flank of Mount Lafayette in Franconia Notch, New Hampshire during the spring months. This landslide slide in 1948 and again in 1959, and buried the old Route 3 both times.
    NH183350.jpg
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  • Franconia Notch State Park - Franconia Ridge from along Kinsman Ridge Trail in the White Mountains, New Hampshire. This trail leads to the summit of Cannon Mountain.
    SC122664.jpg
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  • Looking up a landslide on the side of the Hancock Mountain Range in the Pemigewasset Wilderness in Lincoln, New Hampshire in November 2011. Heavy rains from Tropical Storm Irene in 2011 caused an old landslide that was in the process of being natural regenerated to slide again. The natural process of regeneration must start all over. The new landslide looks to follow the track of the old one. This storm caused extensive damage along the East Coast of the United States and the White Mountains, New Hampshire.
    SC1120214.jpg
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  • Looking up landslide on the side of the Hancock Mountain Range in the Pemigewasset Wilderness of Lincoln, New Hampshire in November 2011. Heavy rains from Tropical Storm Irene in 2011 caused an old landslide that was in the process of being natural regenerated to slide again. The natural process of regeneration must start all over. The new landslide looks to follow the track of the old one. This storm caused extensive damage along the East coast of the United States and the White Mountains, New Hampshire.
    SC1120185.jpg
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  • Looking up a landslide on the side of the Hancock Mountain Range in the Pemigewasset Wilderness in Lincoln, New Hampshire in November 2011. Heavy rains from Tropical Storm Irene in 2011 caused an old landslide that was in the process of being natural regenerated to slide again. The natural process of regeneration must start all over. The new landslide looks to follow the track of the old one. This storm caused extensive damage along the East coast of the United States and the White Mountains, New Hampshire.
    SC1120183.jpg
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  • Looking up a landslide on the side of the Hancock Mountain Range in the Pemigewasset Wilderness in Lincoln, New Hampshire in November 2011. Heavy rains from Tropical Storm Irene in 2011 caused an old landslide that was in the process of being natural regenerated to slide again. The natural process of regeneration must start all over. The new landslide looks to follow the track of the old one. This storm caused extensive damage along the East Coast of the United States and the White Mountains, New Hampshire.
    SC1120217.jpg
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  • Swift River along the side of Sawyer River Trail. This river is near the Kancamagus Highway (route 112) in the White Mountains, New Hampshire USA.
    WD077233.tif
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  • Skookumchuck Brook during the early summer months which runs on the side of Skookumchuck Trail in the White Mountains, New Hampshire  USA. .
    WD075082.tif
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  • Ice flowing down the East Branch of the Pemigewasset River in the area of the Lincoln levee in Lincoln, New Hampshire during a rainy and snowy winter day in January 2014.
    NH141183.jpg
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  • Ice flowing down the East Branch of the Pemigewasset River in the area of the Lincoln levee in Lincoln, New Hampshire during a rainy and snowy winter day in January 2014.
    NH141147.jpg
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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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  • 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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  • The Pemigewasset River near the Flume Visitor Center in Lincoln, New Hampshire USA during the spring months. The Pemigewasset River originates at Profile Lake in Franconia Notch; it flows south for about 65 miles to Franklin, New Hampshire, where it merges with the Winnipesaukee River to form the Merrimack River.
    NH172639.jpg
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  • Cascade along the Pemigewasset River near the Flume Visitor Center in Franconia Notch State Park in Lincoln, New Hampshire during the spring months. The Pemigewasset River originates at Profile Lake in Franconia Notch; it flows south for about 65 miles to Franklin, New Hampshire, where it merges with the Winnipesaukee River to form the Merrimack River.
    NH172656.jpg
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