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  • The walls of an open area of Upper Antelope Canyon on Navajo Nation land near Page, Arizona, take on different colors based on how much direct sunlight they receive. Sections near the slot canyon ceiling appear yellow and gold, while portions in deep shadow are purple. Violent flash floods sculpt the sandstone, leaving undulating, layered walls. The Navajo people call the canyon Tsé bighánílíní dóó Hazdistazí, which means "the place where water runs through rocks."
    Antelope-Canyon_Textured-Walls_6218c.jpg
  • The walls of an open area of Upper Antelope Canyon on Navajo Nation land near Page, Arizona, take on different colors based on how much direct sunlight they receive. Sections near the slot canyon ceiling appear yellow and gold, while portions in deep shadow are purple. Violent flash floods sculpt the sandstone, leaving undulating, layered walls. The Navajo people call the canyon Tsé bighánílíní dóó Hazdistazí, which means "the place where water runs through rocks."
    Antelope-Canyon_Colorful-Chamber_709...jpg
  • The walls of an open area of Upper Antelope Canyon on Navajo Nation land near Page, Arizona, take on different colors based on how much direct sunlight they receive. Sections near the slot canyon ceiling appear yellow and gold, while portions in deep shadow are purple. Violent flash floods sculpt the sandstone, leaving undulating, layered walls. The Navajo people call the canyon Tsé bighánílíní dóó Hazdistazí, which means "the place where water runs through rocks."
    Antelope-Canyon_Colorful-Chamber_622...jpg
  • The walls of a particularly narrow passage of Upper Antelope Canyon in Page, Arizona, take on different colors based on how much direct sunlight they receive. Sections near the slot canyon ceiling appear yellow and gold, while portions in deep shadow are purple. Violent flash floods sculpt the sandstone, leaving undulating, layered walls. The Navajo people call the canyon Tsé bighánílíní dóó Hazdistazí, which means "the place where water runs through rocks."
    Antelope-Canyon-Beam_S2574-01.jpg
  • The walls of a particularly narrow passage of Upper Antelope Canyon in Page, Arizona, take on different colors based on how much direct sunlight they receive. Sections near the slot canyon ceiling appear yellow and gold, while portions in deep shadow are purple. Violent flash floods sculpt the sandstone, leaving undulating, layered walls. The Navajo people call the canyon Tsé bighánílíní dóó Hazdistazí, which means "the place where water runs through rocks."
    Antelope-Canyon_Narrow-Passage_Looki...jpg
  • Bright streaks fall down the curved walls of Upper Antelope Canyon in the Navajo Nation, Arizona. Violent flash floods sculpt the sandstone, leaving undulating, layered walls. The Navajo people call the canyon Tsé bighánílíní dóó Hazdistazí, which means "the place where water runs through rocks."
    Antelope-Canyon_Streaks_6235.jpg
  • The walls of an open area of Upper Antelope Canyon on Navajo Nation land near Page, Arizona, take on different colors based on how much direct sunlight they receive. Sections near the slot canyon ceiling appear yellow and gold, while portions in deep shadow are purple. Violent flash floods sculpt the sandstone, leaving undulating, layered walls. The Navajo people call the canyon Tsé bighánílíní dóó Hazdistazí, which means "the place where water runs through rocks."
    Antelope-Canyon_Colorful-Chamber_622...jpg
  • A passage bends through a very narrow section of Upper Antelope Canyon on Navajo Nation land near Page, Arizona. Violent flash floods sculpt the sandstone, leaving undulating, layered walls. The Navajo people call the canyon Tsé bighánílíní dóó Hazdistazí, which means "the place where water runs through rocks."
    Antelope-Canyon_Narrow-Passage_6255.jpg
  • A narrow path winds through the tall undulating walls of Upper Antelope Canyon on Navajo Nation land in northern Arizona. Antelope Canyon is a slot canyon, a small sandstone canyon that is carved by violent flash floods. The Navajo people call the canyon Tsé bighánílíní dóó Hazdistazí, which means "the place where water runs through rocks."
    Antelope-Canyon_Narrow-Passage_6243.jpg
  • Sand falls from a ledge in Upper Antelope Canyon on Navajo Nation land near Page, Arizona. Antelope Canyon is a narrow sandstone canyon, known as a slot canyon. Violent flash floods sculpt the sandstone, leaving undulating, layered walls. The Navajo people call the canyon Tsé bighánílíní dóó Hazdistazí, which means "the place where water runs through rocks."
    Antelope-Canyon_Sand-Falls_7097.jpg
  • A heart shape appears among the curves of the ceiling of Upper Antelope Canyon on Navajo land near Page, Arizona. Violent flash floods sculpt the sandstone slot canyon, leaving undulating, layered walls. The Navajo people call the canyon Tsé bighánílíní dóó Hazdistazí, which means "the place where water runs through rocks."
    Antelope-Canyon_Heart_7109.jpg
  • A heart shape appears among the curves of the ceiling of Upper Antelope Canyon on Navajo land near Page, Arizona. Violent flash floods sculpt the sandstone slot canyon, leaving undulating, layered walls. The Navajo people call the canyon Tsé bighánílíní dóó Hazdistazí, which means "the place where water runs through rocks."
    Antelope-Canyon_Heart_7110.jpg
  • With just a narrow crack in the ceiling of Upper Antelope Canyon near Page, Arizona, little sunlight reaches the floor by mid-afternoon. Violent flash floods sculpt the sandstone, leaving undulating, layered walls that appear violet or purple in the very faint indirect afternoon light. The Navajo people call Antelope Canyon Tsé bighánílíní dóó Hazdistazí, which means "the place where water runs through rocks." The light in the canyon was so dim at the time that this image was captured that it required a more than one-minute exposure to reveal the detail of the canyon walls.
    Antelope-Canyon_Texture_S2571-05.jpg
  • Pegmatite, a light-colored granite, forms bright stripes on the otherwise dark walls of the Black Canyon of the Gunnison in Colorado. These stripes were found on the Painted Wall, an especially dramatic part of the national park and the highest cliff in all of Colorado. Pegmatite is the result of especially water-rich magma, which is the last to cool and harden. Because it remains fluid longer, it is able to squeeze into cracks in rocks, resulting in the light-colored lines here.
    CO_PaintedWall_GunnisonNP_1965.jpg
  • Pegmatite, a light-colored granite, forms bright stripes on the otherwise dark walls of the Black Canyon of the Gunnison in Colorado. These stripes were found on the Painted Wall, an especially dramatic part of the national park and the highest cliff in all of Colorado. Pegmatite is the result of especially water-rich magma, which is the last to cool and harden. Because it remains fluid longer, it is able to squeeze into cracks in rocks, resulting in the light-colored lines here.
    CO_PaintedWall_GunnisonNP_1966.jpg
  • The steep canyon walls of Wall Street frame a tall hoodoo in Bryce Canyon National Park, Utah.
    BryceWallStreetFramed.jpg
  • Spray from Snoqualmie Falls, located near Snoqualmie, Washington, freezes to the walls of the gorge downstream on a frigid 17°F (-8°C) morning.
    Snoqualmie-Falls_Ice_Gorge_8455.jpg
  • The Kalalau Valley on the island of Kauai, Hawaii is bordered by towering cliffs, about 4,000 feet fall. The low-angled light of the nearly setting sun brings out the texture on one of the valley's walls.
    kauai-kalalau-texture2.jpg
  • Towering icicles cling to a steep, rock wall next to Clear Creek Falls near White Pass in Washington state. Some of the icicles in this image are 30-40 feet (10-12 meters) long.
    Clear-Creek-Falls_Icicles_2011.jpg
  • Abstract shapes are left behind on an eroded sandstone wall near Landscape Arches National Park, Utah.
    Arches_Sandstone-Wall_Texture_5060.jpg
  • Tall pine trees cast shadows on the towering hoodoos along the Wall Street Trail, which winds through the tall spires that make up the Bryce Canyon amphitheatre in Utah.
    BryceWallStreetPineTree.jpg
  • The curved walls of Rattlesnake Canyon join to form abstract patterns on Navajo Nation land near Page, Arizona. Rattlesnake Canyon is a slot canyon — a narrow sandstone canyon that's carved by flash floods.
    AZ_Rattlesnake-Canyon_Curved-Walls_6...jpg
  • The curved walls of Rattlesnake Canyon join to form abstract patterns on Navajo Nation land near Page, Arizona. Rattlesnake Canyon is a slot canyon — a narrow sandstone canyon that's carved by flash floods.
    AZ_Rattlesnake-Canyon_Curved-Walls_6...jpg
  • Flash floods eroded a wavy pattern into the narrow walls of this slot canyon in the Coyote Gulch of the Grand Staircase-Escalante National Monument in Utah.
    Grand-Staircase-Escalante_Wall-Curve...jpg
  • Flash floods eroded a wavy pattern into the narrow walls of this slot canyon in the Coyote Gulch of the Grand Staircase-Escalante National Monument in Utah.
    Grand-Staircase-Escalante_Wall-Curve...jpg
  • Flash floods eroded a wavy pattern into the narrow walls of this slot canyon in the Coyote Gulch of the Grand Staircase Escalante, Utah.
    CoyoteGulchWavyWalls.jpg
  • Numerous caves are visible a soft rock cliff wall in Bandelier National Monument, New Mexico. The national monument protects caves that were used by humans for shelters more than 11,000 years ago.
    NM_Bandelier_Wall-Texture_1635.jpg
  • Numerous caves are visible a soft rock cliff wall in Bandelier National Monument, New Mexico. The national monument protects caves that were used by humans for shelters more than 11,000 years ago.
    NM_Bandelier_Wall-Texture_1633.jpg
  • Several prominent peaks in Zion National Park, Utah, including the Towers of the Virgin, are lit by alpenglow about a half hour before sunrise. The peaks, from left-to-right: The Watchman, The West Temple, The Sundial, The Altar of Sacrifice, The Sentinel, The Streaked Wall, and the East Temple.
    ZionCanyonAlpenglow.jpg
  • Grasses, tiny rocks and other debris is trapped in several small holes eroded in a sandstone wall in the Valley of Fire, Nevada.
    vof-sandstone-holes.jpg
  • During a high tide, Paciifc Ocean waves crash into a rock wall along a natural bridge at Second Beach in Olympic National Park, Washington.
    OlympicNP_Second-Beach_Waves-Crashin...jpg
  • A natural bridge spans two towering hoodoos in the Wall Street section of Bryce Canyon National Park, Utah. Bryce Canyon, which is actually a natural amphitheater, consists of dozens of spires separated by canyons. This span remains despite constant erosion.
    BryceCanyonArch.jpg
  • The rising sun lights up several prominent peaks in Zion National Park, Utah, including the Towers of the Virgin. The peaks, from left-to-right: The Watchman, The West Temple, The Sundial, The Altar of Sacrifice, The Sentinel, The Streaked Wall, and the East Temple. The Zion Canyon overlook overlooks both the Zion Canyon at the back of the frame and the Pine Creek Canyon near the foreground.
    ZionCanyonOverlook.jpg
  • The Grand Canyon of Yellowstone is filled with mist from Lower Yellowstone Falls, backlit by the morning sun.
    Yellowstone_Canyon-Wall_Mist_1158.jpg
  • Ice lines the sides of Yosemite Falls on a cold winter morning in Yosemite National Park, California. At 2,425 feet (739 meters), Yosemite Falls is the highest measured waterfall in North America and the fifth-highest in the world.
    Yosemite_Yosemite-Falls_Ice_9535.jpg
  • Petroglyphs carved by members of the Fremont Culture are visible in a sheer sandstone face in the Fremont River canyon in Capitol Reef National Park, Utah. The rock face includes symbols of bighorn sheep and other animals as well as people. The Fremont Culture lived in the area from 300-1300 Common Era (CE).
    Capitol-Reef_Petroglyphs_1278.jpg
  • Ice lines the sides of Yosemite Falls on a cold winter morning in Yosemite National Park, California. At 2,425 feet (739 meters), Yosemite Falls is the highest measured waterfall in North America and the fifth-highest in the world.
    Yosemite_Yosemite-Falls_Ice_Detail_9...jpg
  • Stars shine above the steep walls of the Tuweep Overlook, also spelled Toroweap, which provides one of the most dramatic views of teh Grand Canyon in Arizona. Lit by the full moon, the walls of the canyon are 3,000 feet tall. Here, the canyon is also a mile wide. It's one of the few places on the Grand Canyon rim where you can see both the Colorado River and the other side of the canyon.
    GrandCanyon_Tuweep_Night_4774.jpg
  • Large icicles form on a steep wall near Snoqualmie Falls, Snoqualmie, Washington after several days of subfreezing temperatures. During periods of extreme cold, mist from the waterfall freezes to the canyon walls. The Snoqualmie River is visible flowing across the bottom of the image.
    Icicles_SnoqualmieFalls_5661.jpg
  • Large icicles form on a steep wall near Snoqualmie Falls, Snoqualmie, Washington after several days of subfreezing temperatures. During periods of extreme cold, mist from the waterfall freezes to the canyon walls.
    Icicles_SnoqualmieFalls_5541.jpg
  • Large icicles form on a steep wall near Snoqualmie Falls, Snoqualmie, Washington after several days of subfreezing temperatures. During periods of extreme cold, mist from the waterfall freezes to the canyon walls.
    Icicles_SnoqualmieFalls_5578.jpg
  • Large icicles form on a steep wall near Snoqualmie Falls, Snoqualmie, Washington after several days of subfreezing temperatures. During periods of extreme cold, mist from the waterfall freezes to the canyon walls.
    Icicles_SnoqualmieFalls_5670.jpg
  • Large icicles form on a steep wall near Snoqualmie Falls, Snoqualmie, Washington after several days of subfreezing temperatures. During periods of extreme cold, mist from the waterfall freezes to the canyon walls.
    Icicles_SnoqualmieFalls_5667.jpg
  • Large icicles form on a steep wall near Snoqualmie Falls, Snoqualmie, Washington after several days of subfreezing temperatures. During periods of extreme cold, mist from the waterfall freezes to the canyon walls.
    Icicles_SnoqualmieFalls_5562.jpg
  • Lichen grows on the walls near the entrance of Beauty Cave, a 300-foot (100-meter) long lava tube in the Craters of the Moon National Monument, Idaho.
    CratersOfTheMoon_Beauty-Cave_2519.jpg
  • The setting sun lights up the rugged walls of the Kalalau Valley, located on Kauai's Na Pali coast. The cliffs that line the valley are more than 2,000 feet tall.
    kauai-kalalau-wide.jpg
  • Palouse Falls plunges 180 feet (55 meters) into a giant natural amphitheater surrounded by towering columnar basalt walls near Washtucna, Washington. Palouse Falls was formed at the end of the last ice age when a mammoth ice dam in Montana regularly collapsed, releasing a torrent of water that carved this winding gorge.
    WA_PalouseFalls_Gorge_9389.jpg
  • Light filters into a lava tube known as Skylight Cave in Deschutes National Forest in Oregon, revealing the texture of its walls.
    Skylight-Cave_Texture_2686.jpg
  • The golden light of sunset colors the walls of Mont Saint-Michel, a former monastery on a tidal island in Normandy, France. Mont Saint-Michel was known as Mont-Tombe until the 8th century when St. Aubert built a church there after having a vision of the archangel St. Michael. It soon became a pilgrimage center and a Benedictine abbey was built there in 966. After it was partially burned in 1203 during a takeover attempt by King Philip II of France, a monastery, known as La Merveille (“The Wonder”), was built and later fortified. The Mont Saint-Michel monastery was dissolved during the French Revolution (1787–99) and became a prison under Napoleon’s reign before the site was restored as a historic monument in 1874. Mont Saint-Michel was designated a UNESCO World Heritage site in 1979. Mont Saint-Michel lies at the mouth of the Couesnon River, which is visible at on the left side of the image. Mont Saint-Michel is cut off from the mainland by sea water during very high tides.
    Mont-Saint-Michel_Sunset_9726.jpg
  • The granite walls of the Yosemite Valley, turned golden at sunrise, are reflected on a textured layer of ice that covers Sentinel Meadow in Yosemite National Park, California.
    Yosemite_Sentinel-Meadow_Ice_9142fs.jpg
  • Camera movement during a long exposure resulted in this impressionistic view of a fallen tree over Yosemite Creek in Yosemite National Park, California. Neighboring granite walls, turned golden by the rising sun, are reflected on the surface of the water.
    Yosemite_YosemiteCreek_FallenTree_Im...jpg
  • Remnants of a fallen tree stretch across Yosemite Creek in Yosemite National Park, California. The surface of the creek reflects the golden color of the neighboring granite walls at sunrise.
    Yosemite_YosemiteCreek_FallenTree_09...jpg
  • The John Day River flows past the tall columnar basalt walls that make up Picture Gorge in John Day National Monument, Oregon. The white stains on the columns illustrate how high the water level has been.
    OR_JohnDay_PictureGorge_ColumnarBasa...jpg
  • The granite walls of the Yosemite Valley, turned golden at sunrise, are reflected on a textured layer of ice that covers Sentinel Meadow in Yosemite National Park, California.
    Yosemite_Sentinel-Meadow_Ice_9134fs.jpg
  • The sandstone that forms the upper walls of the Valley of Fire Narrows was deposited in colorful layers. The Narrows are located along the White Dome trail in the Nevada state park.
    Valley-Of-Fire_Sandstone-Layers_9335.jpg
  • Several large cracks, some caused by rocks tumbling from the steep, rocky walls that surround the lake, are visible in the ice on Lake Crowley, located near Mammoth Lakes in Mono County, California.
    CA_Lake-Crowley_Cracks-In-Ice_6761.jpg
  • The layers that make up the eroding walls of the Grand Canyon are visible from the Desert View vantage point on the south rim of Grand Canyon National Park, Arizona.
    GrandCanyon_DesertView_8607.jpg
  • Pacific Goose Barnacles (Mitella polymerus) cling to the walls of a natural sea tunnel at Devil's Punchbowl on the central Oregon coast.
    OR_DevilsPunchbowl_Barnacles_Tunnel_...jpg
  • A northern plateau lizard (Sceloporus undulates elongatus) blends in with the rocks along the rim of the Black Canyon of the Gunnison in Colorado. The northern plateau lizard, which lives in rock outcrops and canyon walls, feeds on grasshoppers, crickets, leaf hoppers, flying ants, moths and other insects.
    Lizard_NorthernPlateau_GunnisonNP_20...jpg
  • A tiny waterfall flows through a talus cave located next to the Index Town Wall near the town of Index, Washington. Talus is a pile of rocks that broke off a nearby mountain face. Occasionally the rocks break off and land in such a way that it forms a natural cave. The falls is illuminated by a skylight in the cave.
    WA_TalusCaveFalls_Index_4219.jpg
  • The Potomac River runs through a gorge in Great Falls Park located on the border of Virginia and Maryland. The northern gorge wall (on the right of this image) as well as the Potomac River are located in Maryland; the southern wall and most of the national park facilities are located in Virginia.
    Great-Falls-Park_Potomac-River_4219.jpg
  • The Potomac River runs through a gorge in Great Falls Park located on the border of Virginia and Maryland. The northern gorge wall (at the top of this image) as well as the Potomac River are located in Maryland; the southern wall and most of the national park facilities are located in Virginia.
    Great-Falls-Park_Potomac-River_4196.jpg
  • The texture of the main cave in Carlsbad Caverns National Park, New Mexico, shows folds, curtains, terraces and other decorative features. The decorations, known as speleothems, are formed when groundwater containing calcium bicarbonate solution seeps into the cave. Then that solution is exposed to the air in the cave, carbon dioxide gas is released and calcite is deposited.
    CarlsbadCaverns_Wall-Texture_1159.jpg
  • A variety of petroglyphs, including symbols depicting a hunter chasing a deer, are visible on a rock wall at Newspaper Rock State Historic Monument in San Juan County, Utah. The oldest symbols on the rock were made about 2,000 years ago by Archaic, Anasazi, Fremont, Navajo, Anglo and Pueblo people. The oldest petroglyphs on the sandstone appear to be fading, re-covered by desert varnish, a natural manganese-rich coating. In Navajo, the rock is called Tse' Hone, which means a rock that tells a story.
    Petroglyphs_Newspaper-Rock_Utah_0977.jpg
  • A Plains bison (Bison bison) stands in a heavy snow storm next to a canyon wall over the Gibbon River in Yellowstone National Park, Wyoming. American bison are sometimes mistakenly referred to as buffalo; they are only distantly related to true buffalo.
    Bison_Yellowstone_Snow-Storm_4089.jpg
  • Mist at the top of Snoqualmie Falls near Snoqualmie, Washington is turned golden by the rising sun, while the wall below is encased in thick winter ice. At Snoqualmie Falls, the Snoqualmie River drops 268 feet (82 meters).
    SnoqualmieFalls_Frozen_5534.jpg
  • A layered sandstone wall appears to have been twisted and folded by many thousands of years of geological forces in Harris Wash in Grand Staircase-Escalante National Monument, Utah.
    Grand-Staircase-Escalante_Harris-Was...jpg
  • Faded petroglyphs depicting wildlife are visible on a basalt rock wall in Hieroglyphic Canyon, located in the Superstition Wilderness in Arizona. The petroglyphs were carved by the Hohokam people who lived in central and southern Arizona as early as 500 A.D.
    Petroglyphs_Superstition-Wilderness_...jpg
  • Thin cirrus clouds mimick the shape of the Olympic Mountain Range in Washington state. The mountains are not especially high - Mount Olympus is the highest at 7,962 ft (2,427 m) - but they rise quickly from the Pacific Ocean and are densely packed. This wall of mountains traps ocean storms, resulting in a temperate rain forest at their western base. The Hoh Rain Forest records an average of 142 in (360 cm) of rainfall each year, making it the wettest area in the 48 contiguous states. This image was captured from near Hurricane Ridge in Olympic National Park.
    Olympics_HurricaneRidge_CirrusClouds...jpg
  • A basalt wall is partially reflected onto the water of McMannaman Lake in the Columbia National Wildlife Refuge in Washington state.
    WA_Columbia-NWR_McMannaman-Lake_8782.jpg
  • A common raven (Corvus corax) flies over Grand Canyon National Park in Arizona. A wall of the Grand Canyon is visible in the background and is partially reflected on the raven's shiny feathers.
    Grand-Canyon_Raven_Desert-View_6300.jpg
  • A bald eagle (Haliaeetus leucocephalus) regurgitates food for its two young eaglets, which are hidden behind the wall of the nest in Kirkland, Washington. Both bald eagle parents take turns protecting and feeding the eaglets.
    BaldEagles_Nest_Parents_Regurgitate_...jpg
  • A shape resembling a volcano is visible on the wall of Subway Cave, a lava tube formed 30,000 years ago in California's Hat Creek Valley. The tube itself was formed when the top portion of the lava flow cooled to a hard crust while allowing hot lava to flow underneath. Eventually, the lava flow stopped, leaving behind the shell. This formation resulted from hot lava dripping from the ceiling of the tube.
    CA_SubwayCave_VolcanoShape_3617.jpg
  • A few blades of grass trap winter ice from floating down Pine Creek in Zion National Park, Utah. The Streaked Wall, reddened by the sunrise is reflected in the waters.
    Zion_PineCreekIce_1864.jpg
  • A common raven (Corvus corax) flies over Grand Canyon National Park in Arizona. A wall of the Grand Canyon is visible in the background and is partially reflected on the raven's shiny feathers.
    Grand-Canyon_Raven_Desert-View_6872.jpg
  • The Potomac River forms a number of small cascades as it runs against a large gorge wall in Great Falls Park, Maryland.
    Great-Falls-Park_Potomac-River_5046.jpg
  • A family of mountain goats (Oreamnos americanus) climbs the steep rugged wall known as Goat Lick in Glacier National Park, Montana. The mountain goats travel for miles to lick the mineral-laden cliffs during the spring and early summer. The cliffs are full of calcium, potassium and magnesium and smaller amounts of sodium and phosphorous. Scientists believe the goats may lick the cliffs to replace minerals they lose from their bones over the long winter. The minerals may also serve as a digestive aid. It's also possible the goats have simply developed a taste for salt.
    Goats_Mountain_Goat-Lick_Glacier_013...jpg
  • A family of mountain goats (Oreamnos americanus) climbs the steep rugged wall known as Goat Lick in Glacier National Park, Montana. The mountain goats travel for miles to lick the mineral-laden cliffs during the spring and early summer. The cliffs are full of calcium, potassium and magnesium and smaller amounts of sodium and phosphorous. Scientists believe the goats may lick the cliffs to replace minerals they lose from their bones over the long winter. The minerals may also serve as a digestive aid. It's also possible the goats have simply developed a taste for salt.
    Goats_Mountain_Goat-Lick_Glacier_011...jpg
  • This close-up shows the texture of the steep rock wall behind Lower Twin Falls near North Bend, Washington. The entire waterfall drops 135 feet (41 meters).
    TwinFalls_NorthBend_CloseUp_7126.jpg
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