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  • Sossussvlei is located in the Namib Desert in southern Namibia and forms part of the Namib-Naukluft National Park. The desert is Africa's second largest and contains some of the largest dunes in the world (over 300 meters). The area is considered to be one of the oldest deserts in the world, has less than 10 mm (0.4 inches) of rain annually and is almost completely barren.
    091101A-35.jpg
  • Sossussvlei is located in the Namib Desert in southern Namibia and forms part of the Namib-Naukluft National Park. The desert is Africa's second largest and contains some of the largest dunes in the world (over 300 meters). The area is considered to be one of the oldest deserts in the world, has less than 10 mm (0.4 inches) of rain annually and is almost completely barren.
    091201F-07.jpg
  • Sossussvlei is located in the Namib Desert in southern Namibia and forms part of the Namib-Naukluft National Park. The desert is Africa's second largest and contains some of the largest dunes in the world (over 300 meters). The area is considered to be one of the oldest deserts in the world, has less than 10 mm (0.4 inches) of rain annually and is almost completely barren.
    091201E-35.jpg
  • Sossussvlei is located in the Namib Desert in southern Namibia and forms part of the Namib-Naukluft National Park. The desert is Africa's second largest and contains some of the largest dunes in the world (over 300 meters). The area is considered to be one of the oldest deserts in the world, has less than 10 mm (0.4 inches) of rain annually and is almost completely barren.
    091201D-07.jpg
  • Sossussvlei is located in the Namib Desert in southern Namibia and forms part of the Namib-Naukluft National Park. The desert is Africa's second largest and contains some of the largest dunes in the world (over 300 meters). The area is considered to be one of the oldest deserts in the world, has less than 10 mm (0.4 inches) of rain annually and is almost completely barren.
    091101A-04.jpg
  • Sossussvlei is located in the Namib Desert in southern Namibia and forms part of the Namib-Naukluft National Park. The desert is Africa's second largest and contains some of the largest dunes in the world (over 300 meters). The area is considered to be one of the oldest deserts in the world, has less than 10 mm (0.4 inches) of rain annually and is almost completely barren.
    091201E-10.jpg
  • Sossussvlei is located in the Namib Desert in southern Namibia and forms part of the Namib-Naukluft National Park. The desert is Africa's second largest and contains some of the largest dunes in the world (over 300 meters). The area is considered to be one of the oldest deserts in the world, has less than 10 mm (0.4 inches) of rain annually and is almost completely barren.
    091201D-27.jpg
  • Sossussvlei is located in the Namib Desert in southern Namibia and forms part of the Namib-Naukluft National Park. The desert is Africa's second largest and contains some of the largest dunes in the world (over 300 meters). The area is considered to be one of the oldest deserts in the world, has less than 10 mm (0.4 inches) of rain annually and is almost completely barren.
    091201D-11.jpg
  • Sossussvlei is located in the Namib Desert in southern Namibia and forms part of the Namib-Naukluft National Park. The desert is Africa's second largest and contains some of the largest dunes in the world (over 300 meters). The area is considered to be one of the oldest deserts in the world, has less than 10 mm (0.4 inches) of rain annually and is almost completely barren.
    091101A-01.jpg
  • Sossussvlei is located in the Namib Desert in southern Namibia and forms part of the Namib-Naukluft National Park. The desert is Africa's second largest and contains some of the largest dunes in the world (over 300 meters). The area is considered to be one of the oldest deserts in the world, has less than 10 mm (0.4 inches) of rain annually and is almost completely barren.
    091201F-17.jpg
  • Sossussvlei is located in the Namib Desert in southern Namibia and forms part of the Namib-Naukluft National Park. The desert is Africa's second largest and contains some of the largest dunes in the world (over 300 meters). The area is considered to be one of the oldest deserts in the world, has less than 10 mm (0.4 inches) of rain annually and is almost completely barren.
    091201E-04.jpg
  • Sossussvlei is located in the Namib Desert in southern Namibia and forms part of the Namib-Naukluft National Park. The desert is Africa's second largest and contains some of the largest dunes in the world (over 300 meters). The area is considered to be one of the oldest deserts in the world, has less than 10 mm (0.4 inches) of rain annually and is almost completely barren.
    091601D-12.jpg
  • Sossussvlei is located in the Namib Desert in southern Namibia and forms part of the Namib-Naukluft National Park. The desert is Africa's second largest and contains some of the largest dunes in the world (over 300 meters). The area is considered to be one of the oldest deserts in the world, has less than 10 mm (0.4 inches) of rain annually and is almost completely barren.
    091301B-01.jpg
  • Sossussvlei is located in the Namib Desert in southern Namibia and forms part of the Namib-Naukluft National Park. The desert is Africa's second largest and contains some of the largest dunes in the world (over 300 meters). The area is considered to be one of the oldest deserts in the world, has less than 10 mm (0.4 inches) of rain annually and is almost completely barren.
    091201E-07.jpg
  • Sossussvlei is located in the Namib Desert in southern Namibia and forms part of the Namib-Naukluft National Park. The desert is Africa's second largest and contains some of the largest dunes in the world (over 300 meters). The area is considered to be one of the oldest deserts in the world, has less than 10 mm (0.4 inches) of rain annually and is almost completely barren.
    091201D-27.jpg
  • Sossussvlei is located in the Namib Desert in southern Namibia and forms part of the Namib-Naukluft National Park. The desert is Africa's second largest and contains some of the largest dunes in the world (over 300 meters). The area is considered to be one of the oldest deserts in the world, has less than 10 mm (0.4 inches) of rain annually and is almost completely barren.
    091301B-28.jpg
  • This view from Weeping Rock in Zion National Park affords views of massive canyon walls ascending toward a brilliant blue sky. To experience Zion, you need to walk among the towering cliffs, or challenge your courage in a small narrow canyon. These unique sandstone cliffs range in color from cream, to pink, to red. They could be described as sand castles crowning desert canyons. Zion's unique geographic location and variety of life zones combine to create a variety of habitats for a surprising array of plant and animal species. Located on the Colorado Plateau, but bordering the Great Basin and Mojave Desert Provinces, Zion is home to plants from each region.
    062798B-02.jpg
  • The Navajo name for Upper Antelope Canyon is Tsé bighánílíní, which means "the place where water runs through rocks." <br />
<br />
Antelope Canyon was formed by erosion of Navajo Sandstone, primarily due to flash flooding and secondarily due to other sub-aerial processes. Rainwater, especially during monsoon season, runs into the extensive basin above the slot canyon sections, picking up speed and sand as it rushes into the narrow passageways. Over time the passageways eroded away, making the corridors deeper and smoothing hard edges in such a way as to form characteristic 'flowing' shapes in the rock.
    062315-066b.jpg
  • Monument Valley (Navajo: Tsé Biiʼ Ndzisgaii, meaning valley of the rocks) is a region of the Colorado Plateau characterized by a cluster of vast sandstone buttes, the largest reaching 1,000 ft (300 m) above the valley floor. It is located on the Arizona-Utah state line near the Four Corners area. The valley lies within the range of the Navajo Nation Reservation.  The area is part of the Colorado Plateau. The elevation of the valley floor ranges from 5,000 to 6,000 feet (1,500 to 1,800 m) above sea level. The floor is largely siltstone of the Cutler Group, or sand derived from it, deposited by the meandering rivers that carved the valley. The valley's vivid red color comes from iron oxide exposed in the weathered siltstone. The darker, blue-gray rocks in the valley get their color from manganese oxide.  The buttes are clearly stratified, with three principal layers. The lowest layer is the Organ Rock Shale, the middle is de Chelly Sandstone, and the top layer is the Moenkopi Formation capped by Shinarump Conglomerate. The valley includes large stone structures including the famed "Eye of the Sun".
    091615-052.jpg
  • The Navajo name for Upper Antelope Canyon is Tsé bighánílíní, which means "the place where water runs through rocks." <br />
<br />
Antelope Canyon was formed by erosion of Navajo Sandstone, primarily due to flash flooding and secondarily due to other sub-aerial processes. Rainwater, especially during monsoon season, runs into the extensive basin above the slot canyon sections, picking up speed and sand as it rushes into the narrow passageways. Over time the passageways eroded away, making the corridors deeper and smoothing hard edges in such a way as to form characteristic 'flowing' shapes in the rock.
    062315-017.jpg
  • The Navajo name for Upper Antelope Canyon is Tsé bighánílíní, which means "the place where water runs through rocks." Antelope Canyon was formed by erosion of Navajo Sandstone, primarily due to flash flooding and secondarily due to other sub-aerial processes. Rainwater, especially during monsoon season, runs into the extensive basin above the slot canyon sections, picking up speed and sand as it rushes into the narrow passageways. Over time the passageways eroded away, making the corridors deeper and smoothing hard edges in such a way as to form characteristic 'flowing' shapes in the rock.
    091415-189.jpg
  • The Navajo name for Upper Antelope Canyon is Tsé bighánílíní, which means "the place where water runs through rocks." <br />
<br />
Antelope Canyon was formed by erosion of Navajo Sandstone, primarily due to flash flooding and secondarily due to other sub-aerial processes. Rainwater, especially during monsoon season, runs into the extensive basin above the slot canyon sections, picking up speed and sand as it rushes into the narrow passageways. Over time the passageways eroded away, making the corridors deeper and smoothing hard edges in such a way as to form characteristic 'flowing' shapes in the rock.
    062315-070.jpg
  • The Navajo name for Upper Antelope Canyon is Tsé bighánílíní, which means "the place where water runs through rocks." Antelope Canyon was formed by erosion of Navajo Sandstone, primarily due to flash flooding and secondarily due to other sub-aerial processes. Rainwater, especially during monsoon season, runs into the extensive basin above the slot canyon sections, picking up speed and sand as it rushes into the narrow passageways. Over time the passageways eroded away, making the corridors deeper and smoothing hard edges in such a way as to form characteristic 'flowing' shapes in the rock.
    091415-132.jpg
  • Monument Valley (Navajo: Tsé Biiʼ Ndzisgaii, meaning valley of the rocks) is a region of the Colorado Plateau characterized by a cluster of vast sandstone buttes, the largest reaching 1,000 ft (300 m) above the valley floor. It is located on the Arizona-Utah state line near the Four Corners area. The valley lies within the range of the Navajo Nation Reservation.  The area is part of the Colorado Plateau. The elevation of the valley floor ranges from 5,000 to 6,000 feet (1,500 to 1,800 m) above sea level. The floor is largely siltstone of the Cutler Group, or sand derived from it, deposited by the meandering rivers that carved the valley. The valley's vivid red color comes from iron oxide exposed in the weathered siltstone. The darker, blue-gray rocks in the valley get their color from manganese oxide.  The buttes are clearly stratified, with three principal layers. The lowest layer is the Organ Rock Shale, the middle is de Chelly Sandstone, and the top layer is the Moenkopi Formation capped by Shinarump Conglomerate. The valley includes large stone structures including the famed "Eye of the Sun".
    091615-062.jpg
  • Monument Valley (Navajo: Tsé Biiʼ Ndzisgaii, meaning valley of the rocks) is a region of the Colorado Plateau characterized by a cluster of vast sandstone buttes, the largest reaching 1,000 ft (300 m) above the valley floor. It is located on the Arizona-Utah state line near the Four Corners area. The valley lies within the range of the Navajo Nation Reservation.  The area is part of the Colorado Plateau. The elevation of the valley floor ranges from 5,000 to 6,000 feet (1,500 to 1,800 m) above sea level. The floor is largely siltstone of the Cutler Group, or sand derived from it, deposited by the meandering rivers that carved the valley. The valley's vivid red color comes from iron oxide exposed in the weathered siltstone. The darker, blue-gray rocks in the valley get their color from manganese oxide.  The buttes are clearly stratified, with three principal layers. The lowest layer is the Organ Rock Shale, the middle is de Chelly Sandstone, and the top layer is the Moenkopi Formation capped by Shinarump Conglomerate. The valley includes large stone structures including the famed "Eye of the Sun".
    091515-128.jpg
  • The Navajo name for Upper Antelope Canyon is Tsé bighánílíní, which means "the place where water runs through rocks." <br />
<br />
Antelope Canyon was formed by erosion of Navajo Sandstone, primarily due to flash flooding and secondarily due to other sub-aerial processes. Rainwater, especially during monsoon season, runs into the extensive basin above the slot canyon sections, picking up speed and sand as it rushes into the narrow passageways. Over time the passageways eroded away, making the corridors deeper and smoothing hard edges in such a way as to form characteristic 'flowing' shapes in the rock.
    062315-503.jpg
  • The Navajo name for Upper Antelope Canyon is Tsé bighánílíní, which means "the place where water runs through rocks." <br />
<br />
Antelope Canyon was formed by erosion of Navajo Sandstone, primarily due to flash flooding and secondarily due to other sub-aerial processes. Rainwater, especially during monsoon season, runs into the extensive basin above the slot canyon sections, picking up speed and sand as it rushes into the narrow passageways. Over time the passageways eroded away, making the corridors deeper and smoothing hard edges in such a way as to form characteristic 'flowing' shapes in the rock.
    062315-010.jpg
  • Monument Valley (Navajo: Tsé Biiʼ Ndzisgaii, meaning valley of the rocks) is a region of the Colorado Plateau characterized by a cluster of vast sandstone buttes, the largest reaching 1,000 ft (300 m) above the valley floor. It is located on the Arizona-Utah state line near the Four Corners area. The valley lies within the range of the Navajo Nation Reservation.  The area is part of the Colorado Plateau. The elevation of the valley floor ranges from 5,000 to 6,000 feet (1,500 to 1,800 m) above sea level. The floor is largely siltstone of the Cutler Group, or sand derived from it, deposited by the meandering rivers that carved the valley. The valley's vivid red color comes from iron oxide exposed in the weathered siltstone. The darker, blue-gray rocks in the valley get their color from manganese oxide.  The buttes are clearly stratified, with three principal layers. The lowest layer is the Organ Rock Shale, the middle is de Chelly Sandstone, and the top layer is the Moenkopi Formation capped by Shinarump Conglomerate. The valley includes large stone structures including the famed "Eye of the Sun".
    091615-044.jpg
  • The Navajo name for Upper Antelope Canyon is Tsé bighánílíní, which means "the place where water runs through rocks." <br />
<br />
Antelope Canyon was formed by erosion of Navajo Sandstone, primarily due to flash flooding and secondarily due to other sub-aerial processes. Rainwater, especially during monsoon season, runs into the extensive basin above the slot canyon sections, picking up speed and sand as it rushes into the narrow passageways. Over time the passageways eroded away, making the corridors deeper and smoothing hard edges in such a way as to form characteristic 'flowing' shapes in the rock.
    062315-275.jpg
  • The Navajo name for Upper Antelope Canyon is Tsé bighánílíní, which means "the place where water runs through rocks." <br />
<br />
Antelope Canyon was formed by erosion of Navajo Sandstone, primarily due to flash flooding and secondarily due to other sub-aerial processes. Rainwater, especially during monsoon season, runs into the extensive basin above the slot canyon sections, picking up speed and sand as it rushes into the narrow passageways. Over time the passageways eroded away, making the corridors deeper and smoothing hard edges in such a way as to form characteristic 'flowing' shapes in the rock.
    062315-057.jpg
  • Monument Valley (Navajo: Tsé Biiʼ Ndzisgaii, meaning valley of the rocks) is a region of the Colorado Plateau characterized by a cluster of vast sandstone buttes, the largest reaching 1,000 ft (300 m) above the valley floor. It is located on the Arizona-Utah state line near the Four Corners area. The valley lies within the range of the Navajo Nation Reservation.  The area is part of the Colorado Plateau. The elevation of the valley floor ranges from 5,000 to 6,000 feet (1,500 to 1,800 m) above sea level. The floor is largely siltstone of the Cutler Group, or sand derived from it, deposited by the meandering rivers that carved the valley. The valley's vivid red color comes from iron oxide exposed in the weathered siltstone. The darker, blue-gray rocks in the valley get their color from manganese oxide.  The buttes are clearly stratified, with three principal layers. The lowest layer is the Organ Rock Shale, the middle is de Chelly Sandstone, and the top layer is the Moenkopi Formation capped by Shinarump Conglomerate. The valley includes large stone structures including the famed "Eye of the Sun".
    091615-287.jpg
  • The Navajo name for Upper Antelope Canyon is Tsé bighánílíní, which means "the place where water runs through rocks." Antelope Canyon was formed by erosion of Navajo Sandstone, primarily due to flash flooding and secondarily due to other sub-aerial processes. Rainwater, especially during monsoon season, runs into the extensive basin above the slot canyon sections, picking up speed and sand as it rushes into the narrow passageways. Over time the passageways eroded away, making the corridors deeper and smoothing hard edges in such a way as to form characteristic 'flowing' shapes in the rock.
    091415-084.jpg
  • The Navajo name for Upper Antelope Canyon is Tsé bighánílíní, which means "the place where water runs through rocks." Antelope Canyon was formed by erosion of Navajo Sandstone, primarily due to flash flooding and secondarily due to other sub-aerial processes. Rainwater, especially during monsoon season, runs into the extensive basin above the slot canyon sections, picking up speed and sand as it rushes into the narrow passageways. Over time the passageways eroded away, making the corridors deeper and smoothing hard edges in such a way as to form characteristic 'flowing' shapes in the rock.
    091415-087.jpg
  • The Navajo name for Upper Antelope Canyon is Tsé bighánílíní, which means "the place where water runs through rocks." <br />
<br />
Antelope Canyon was formed by erosion of Navajo Sandstone, primarily due to flash flooding and secondarily due to other sub-aerial processes. Rainwater, especially during monsoon season, runs into the extensive basin above the slot canyon sections, picking up speed and sand as it rushes into the narrow passageways. Over time the passageways eroded away, making the corridors deeper and smoothing hard edges in such a way as to form characteristic 'flowing' shapes in the rock.
    062315-305.jpg
  • The Navajo name for Upper Antelope Canyon is Tsé bighánílíní, which means "the place where water runs through rocks." <br />
<br />
Antelope Canyon was formed by erosion of Navajo Sandstone, primarily due to flash flooding and secondarily due to other sub-aerial processes. Rainwater, especially during monsoon season, runs into the extensive basin above the slot canyon sections, picking up speed and sand as it rushes into the narrow passageways. Over time the passageways eroded away, making the corridors deeper and smoothing hard edges in such a way as to form characteristic 'flowing' shapes in the rock.
    062315-127.jpg
  • Monument Valley (Navajo: Tsé Biiʼ Ndzisgaii, meaning valley of the rocks) is a region of the Colorado Plateau characterized by a cluster of vast sandstone buttes, the largest reaching 1,000 ft (300 m) above the valley floor. It is located on the Arizona-Utah state line near the Four Corners area. The valley lies within the range of the Navajo Nation Reservation.  The area is part of the Colorado Plateau. The elevation of the valley floor ranges from 5,000 to 6,000 feet (1,500 to 1,800 m) above sea level. The floor is largely siltstone of the Cutler Group, or sand derived from it, deposited by the meandering rivers that carved the valley. The valley's vivid red color comes from iron oxide exposed in the weathered siltstone. The darker, blue-gray rocks in the valley get their color from manganese oxide.  The buttes are clearly stratified, with three principal layers. The lowest layer is the Organ Rock Shale, the middle is de Chelly Sandstone, and the top layer is the Moenkopi Formation capped by Shinarump Conglomerate. The valley includes large stone structures including the famed "Eye of the Sun".
    091515-002.jpg
  • The Navajo name for Upper Antelope Canyon is Tsé bighánílíní, which means "the place where water runs through rocks." <br />
<br />
Antelope Canyon was formed by erosion of Navajo Sandstone, primarily due to flash flooding and secondarily due to other sub-aerial processes. Rainwater, especially during monsoon season, runs into the extensive basin above the slot canyon sections, picking up speed and sand as it rushes into the narrow passageways. Over time the passageways eroded away, making the corridors deeper and smoothing hard edges in such a way as to form characteristic 'flowing' shapes in the rock.
    062315-171.jpg