Inge Johnsson Photography

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  • Little Colorado River confluence with the Colorado River
    GrandCanyonLittleColorado3.jpg
  • Little Colorado River confluence with the Colorado River
    GrandCanyonLittleColorado2.jpg
  • Little Colorado River confluence with the Colorado River
    GrandCanyonLittleColorado1.jpg
  • Little Colorado River confluence with the Colorado River
    GrandCanyonLittleColorado2.jpg
  • View of the canyon walls ofthe Grand Canyon seen from a raft on the Colorado River
    GrandCanyonRiver1.jpg
  • Horseshoe Bend on the Colorado River near Page, Arizona
    HorseshoeBendLeft.jpg
  • View of the canyon walls ofthe Grand Canyon seen from a raft on the Colorado River
    GrandCanyonRiver1.jpg
  • Horseshoe Bend on the Colorado River near Page, Arizona
    HorseshoeBendLeft.jpg
  • Canyon walls as seen from the Colorado River<br />
.....<br />
The Grand Canyon is a steep-sided canyon carved by the Colorado River in the state of Arizona in the United States. It is contained within and managed by Grand Canyon National Park, the Hualapai Tribal Nation, the Havasupai Tribe and the Navajo Nation. President Theodore Roosevelt was a major proponent of preservation of the Grand Canyon area, and visited it on numerous occasions to hunt and enjoy the scenery.<br />
The Grand Canyon is 277 miles long, up to 18 miles wide and attains a depth of over a mile. Nearly two billion years of Earth's geological history have been exposed as the Colorado River and its tributaries cut their channels through layer after layer of rock while the Colorado Plateau was uplifted. While the specific geologic processes and timing that formed the Grand Canyon are the subject of debate by geologists, recent evidence suggests that the Colorado River established its course through the canyon at least 17 million years ago. Since that time, the Colorado River continued to erode and form the canyon to its present-day configuration.<br />
For thousands of years, the area has been continuously inhabited by Native Americans who built settlements within the canyon and its many caves. The Pueblo people considered the Grand Canyon ("Ongtupqa" in the Hopi language) a holy site, and made pilgrimages to it. The first European known to have viewed the Grand Canyon was García López de Cárdenas from Spain, who arrived in 1540.
    GrandCanyonInterior1.jpg
  • Matkatamiba Canyon is a side canyon to the Grand Canyon accessible from the Colorado River<br />
.....<br />
The Grand Canyon is a steep-sided canyon carved by the Colorado River in the state of Arizona in the United States. It is contained within and managed by Grand Canyon National Park, the Hualapai Tribal Nation, the Havasupai Tribe and the Navajo Nation. President Theodore Roosevelt was a major proponent of preservation of the Grand Canyon area, and visited it on numerous occasions to hunt and enjoy the scenery.<br />
The Grand Canyon is 277 miles long, up to 18 miles wide and attains a depth of over a mile. Nearly two billion years of Earth's geological history have been exposed as the Colorado River and its tributaries cut their channels through layer after layer of rock while the Colorado Plateau was uplifted. While the specific geologic processes and timing that formed the Grand Canyon are the subject of debate by geologists, recent evidence suggests that the Colorado River established its course through the canyon at least 17 million years ago. Since that time, the Colorado River continued to erode and form the canyon to its present-day configuration.<br />
For thousands of years, the area has been continuously inhabited by Native Americans who built settlements within the canyon and its many caves. The Pueblo people considered the Grand Canyon ("Ongtupqa" in the Hopi language) a holy site, and made pilgrimages to it. The first European known to have viewed the Grand Canyon was García López de Cárdenas from Spain, who arrived in 1540.
    GrandCanyonMatkatamiba4.jpg
  • Reflection in the Colorado River at Lava Falls, in the Grand Canyon National Park<br />
.....<br />
The Grand Canyon is a steep-sided canyon carved by the Colorado River in the state of Arizona in the United States. It is contained within and managed by Grand Canyon National Park, the Hualapai Tribal Nation, the Havasupai Tribe and the Navajo Nation. President Theodore Roosevelt was a major proponent of preservation of the Grand Canyon area, and visited it on numerous occasions to hunt and enjoy the scenery.<br />
The Grand Canyon is 277 miles long, up to 18 miles wide and attains a depth of over a mile. Nearly two billion years of Earth's geological history have been exposed as the Colorado River and its tributaries cut their channels through layer after layer of rock while the Colorado Plateau was uplifted. While the specific geologic processes and timing that formed the Grand Canyon are the subject of debate by geologists, recent evidence suggests that the Colorado River established its course through the canyon at least 17 million years ago. Since that time, the Colorado River continued to erode and form the canyon to its present-day configuration.<br />
For thousands of years, the area has been continuously inhabited by Native Americans who built settlements within the canyon and its many caves. The Pueblo people considered the Grand Canyon ("Ongtupqa" in the Hopi language) a holy site, and made pilgrimages to it. The first European known to have viewed the Grand Canyon was García López de Cárdenas from Spain, who arrived in 1540.
    _MG_9397.jpg
  • Canyon walls as seen from the Colorado River<br />
.....<br />
The Grand Canyon is a steep-sided canyon carved by the Colorado River in the state of Arizona in the United States. It is contained within and managed by Grand Canyon National Park, the Hualapai Tribal Nation, the Havasupai Tribe and the Navajo Nation. President Theodore Roosevelt was a major proponent of preservation of the Grand Canyon area, and visited it on numerous occasions to hunt and enjoy the scenery.<br />
The Grand Canyon is 277 miles long, up to 18 miles wide and attains a depth of over a mile. Nearly two billion years of Earth's geological history have been exposed as the Colorado River and its tributaries cut their channels through layer after layer of rock while the Colorado Plateau was uplifted. While the specific geologic processes and timing that formed the Grand Canyon are the subject of debate by geologists, recent evidence suggests that the Colorado River established its course through the canyon at least 17 million years ago. Since that time, the Colorado River continued to erode and form the canyon to its present-day configuration.<br />
For thousands of years, the area has been continuously inhabited by Native Americans who built settlements within the canyon and its many caves. The Pueblo people considered the Grand Canyon ("Ongtupqa" in the Hopi language) a holy site, and made pilgrimages to it. The first European known to have viewed the Grand Canyon was García López de Cárdenas from Spain, who arrived in 1540.
    GrandCanyonInterior1.jpg
  • Matkatamiba Canyon is a side canyon to the Grand Canyon accessible from the Colorado River<br />
.....<br />
The Grand Canyon is a steep-sided canyon carved by the Colorado River in the state of Arizona in the United States. It is contained within and managed by Grand Canyon National Park, the Hualapai Tribal Nation, the Havasupai Tribe and the Navajo Nation. President Theodore Roosevelt was a major proponent of preservation of the Grand Canyon area, and visited it on numerous occasions to hunt and enjoy the scenery.<br />
The Grand Canyon is 277 miles long, up to 18 miles wide and attains a depth of over a mile. Nearly two billion years of Earth's geological history have been exposed as the Colorado River and its tributaries cut their channels through layer after layer of rock while the Colorado Plateau was uplifted. While the specific geologic processes and timing that formed the Grand Canyon are the subject of debate by geologists, recent evidence suggests that the Colorado River established its course through the canyon at least 17 million years ago. Since that time, the Colorado River continued to erode and form the canyon to its present-day configuration.<br />
For thousands of years, the area has been continuously inhabited by Native Americans who built settlements within the canyon and its many caves. The Pueblo people considered the Grand Canyon ("Ongtupqa" in the Hopi language) a holy site, and made pilgrimages to it. The first European known to have viewed the Grand Canyon was García López de Cárdenas from Spain, who arrived in 1540.
    GrandCanyonMatkatamiba4.jpg
  • Havasu Creek is a side stream to the Colorado River in the interior of the Grand Canyon<br />
.....<br />
The Grand Canyon is a steep-sided canyon carved by the Colorado River in the state of Arizona in the United States. It is contained within and managed by Grand Canyon National Park, the Hualapai Tribal Nation, the Havasupai Tribe and the Navajo Nation. President Theodore Roosevelt was a major proponent of preservation of the Grand Canyon area, and visited it on numerous occasions to hunt and enjoy the scenery.<br />
The Grand Canyon is 277 miles long, up to 18 miles wide and attains a depth of over a mile. Nearly two billion years of Earth's geological history have been exposed as the Colorado River and its tributaries cut their channels through layer after layer of rock while the Colorado Plateau was uplifted. While the specific geologic processes and timing that formed the Grand Canyon are the subject of debate by geologists, recent evidence suggests that the Colorado River established its course through the canyon at least 17 million years ago. Since that time, the Colorado River continued to erode and form the canyon to its present-day configuration.<br />
For thousands of years, the area has been continuously inhabited by Native Americans who built settlements within the canyon and its many caves. The Pueblo people considered the Grand Canyon ("Ongtupqa" in the Hopi language) a holy site, and made pilgrimages to it. The first European known to have viewed the Grand Canyon was García López de Cárdenas from Spain, who arrived in 1540.
    GrandCanyonHavasuCreek2.jpg
  • Matkatamiba Canyon is a side canyon to the Grand Canyon accessible from the Colorado River<br />
.....<br />
The Grand Canyon is a steep-sided canyon carved by the Colorado River in the state of Arizona in the United States. It is contained within and managed by Grand Canyon National Park, the Hualapai Tribal Nation, the Havasupai Tribe and the Navajo Nation. President Theodore Roosevelt was a major proponent of preservation of the Grand Canyon area, and visited it on numerous occasions to hunt and enjoy the scenery.<br />
The Grand Canyon is 277 miles long, up to 18 miles wide and attains a depth of over a mile. Nearly two billion years of Earth's geological history have been exposed as the Colorado River and its tributaries cut their channels through layer after layer of rock while the Colorado Plateau was uplifted. While the specific geologic processes and timing that formed the Grand Canyon are the subject of debate by geologists, recent evidence suggests that the Colorado River established its course through the canyon at least 17 million years ago. Since that time, the Colorado River continued to erode and form the canyon to its present-day configuration.<br />
For thousands of years, the area has been continuously inhabited by Native Americans who built settlements within the canyon and its many caves. The Pueblo people considered the Grand Canyon ("Ongtupqa" in the Hopi language) a holy site, and made pilgrimages to it. The first European known to have viewed the Grand Canyon was García López de Cárdenas from Spain, who arrived in 1540.
    GrandCanyonMatkatamiba5.jpg
  • Matkatamiba Canyon is a side canyon to the Grand Canyon accessible from the Colorado River<br />
.....<br />
The Grand Canyon is a steep-sided canyon carved by the Colorado River in the state of Arizona in the United States. It is contained within and managed by Grand Canyon National Park, the Hualapai Tribal Nation, the Havasupai Tribe and the Navajo Nation. President Theodore Roosevelt was a major proponent of preservation of the Grand Canyon area, and visited it on numerous occasions to hunt and enjoy the scenery.<br />
The Grand Canyon is 277 miles long, up to 18 miles wide and attains a depth of over a mile. Nearly two billion years of Earth's geological history have been exposed as the Colorado River and its tributaries cut their channels through layer after layer of rock while the Colorado Plateau was uplifted. While the specific geologic processes and timing that formed the Grand Canyon are the subject of debate by geologists, recent evidence suggests that the Colorado River established its course through the canyon at least 17 million years ago. Since that time, the Colorado River continued to erode and form the canyon to its present-day configuration.<br />
For thousands of years, the area has been continuously inhabited by Native Americans who built settlements within the canyon and its many caves. The Pueblo people considered the Grand Canyon ("Ongtupqa" in the Hopi language) a holy site, and made pilgrimages to it. The first European known to have viewed the Grand Canyon was García López de Cárdenas from Spain, who arrived in 1540.
    GrandCanyonMatkatamiba2.jpg
  • The Maroon Bells are two peaks in the Elk Mountains, Maroon Peak and North Maroon Peak, separated by about a third of a mile. The mountains are about 12 miles southwest of Aspen. Both peaks are fourteeners. Maroon Peak, at 14,156 feet, is the 27th highest peak in Colorado; North Maroon Peak, at 14,014 feet, is the 50th highest. The view of the Maroon Bells to the southwest from the Maroon Creek valley is one of the most famous scenes in Colorado, and is reputed to be the "most-photographed spot in Colorado" and one of Colorado's premier scenic overlooks. The peaks are located in the Maroon Bells-Snowmass Wilderness of White River National Forest.<br />
<br />
A US Forest Service sign on the access trail refers to these mountains as "The Deadly Bells" and warns would-be climbers of "downsloping, loose, rotten and unstable" rock that "kills without warning". Unlike other mountains in the Rockies that are composed of granite and limestone, the Bells are composed of metamorphic sedimentary mudstone that has hardened into rock over millions of years. Mudstone is weak and fractures readily, giving rise to dangerously loose rock along almost any route. The mudstone is responsible for the Bells' distinctive maroon color. The Bells got their "deadly" name in 1965 when eight people died in five separate accidents.<br />
<br />
Maroon Lake (9,580') occupies a basin that was sculpted by Ice-Age glaciers and later dammed by landslide and rockfall debris from the steep slopes above the valley floor.
    MaroonBells6.jpg
  • The Maroon Bells are two peaks in the Elk Mountains, Maroon Peak and North Maroon Peak, separated by about a third of a mile. The mountains are about 12 miles southwest of Aspen. Both peaks are fourteeners. Maroon Peak, at 14,156 feet, is the 27th highest peak in Colorado; North Maroon Peak, at 14,014 feet, is the 50th highest. The view of the Maroon Bells to the southwest from the Maroon Creek valley is one of the most famous scenes in Colorado, and is reputed to be the "most-photographed spot in Colorado" and one of Colorado's premier scenic overlooks. The peaks are located in the Maroon Bells-Snowmass Wilderness of White River National Forest.<br />
<br />
A US Forest Service sign on the access trail refers to these mountains as "The Deadly Bells" and warns would-be climbers of "downsloping, loose, rotten and unstable" rock that "kills without warning". Unlike other mountains in the Rockies that are composed of granite and limestone, the Bells are composed of metamorphic sedimentary mudstone that has hardened into rock over millions of years. Mudstone is weak and fractures readily, giving rise to dangerously loose rock along almost any route. The mudstone is responsible for the Bells' distinctive maroon color. The Bells got their "deadly" name in 1965 when eight people died in five separate accidents.<br />
<br />
Maroon Lake (9,580') occupies a basin that was sculpted by Ice-Age glaciers and later dammed by landslide and rockfall debris from the steep slopes above the valley floor.
    MaroonBells3.jpg
  • The Maroon Bells are two peaks in the Elk Mountains, Maroon Peak and North Maroon Peak, separated by about a third of a mile. The mountains are about 12 miles southwest of Aspen. Both peaks are fourteeners. Maroon Peak, at 14,156 feet, is the 27th highest peak in Colorado; North Maroon Peak, at 14,014 feet, is the 50th highest. The view of the Maroon Bells to the southwest from the Maroon Creek valley is one of the most famous scenes in Colorado, and is reputed to be the "most-photographed spot in Colorado" and one of Colorado's premier scenic overlooks. The peaks are located in the Maroon Bells-Snowmass Wilderness of White River National Forest.<br />
<br />
A US Forest Service sign on the access trail refers to these mountains as "The Deadly Bells" and warns would-be climbers of "downsloping, loose, rotten and unstable" rock that "kills without warning". Unlike other mountains in the Rockies that are composed of granite and limestone, the Bells are composed of metamorphic sedimentary mudstone that has hardened into rock over millions of years. Mudstone is weak and fractures readily, giving rise to dangerously loose rock along almost any route. The mudstone is responsible for the Bells' distinctive maroon color. The Bells got their "deadly" name in 1965 when eight people died in five separate accidents.<br />
<br />
Maroon Lake (9,580') occupies a basin that was sculpted by Ice-Age glaciers and later dammed by landslide and rockfall debris from the steep slopes above the valley floor.
    MaroonBells1.jpg
  • Grand Canyon from Toroweap Point<br />
.....<br />
The Grand Canyon is a steep-sided canyon carved by the Colorado River in the state of Arizona in the United States. It is contained within and managed by Grand Canyon National Park, the Hualapai Tribal Nation, the Havasupai Tribe and the Navajo Nation. President Theodore Roosevelt was a major proponent of preservation of the Grand Canyon area, and visited it on numerous occasions to hunt and enjoy the scenery.<br />
The Grand Canyon is 277 miles long, up to 18 miles wide and attains a depth of over a mile. Nearly two billion years of Earth's geological history have been exposed as the Colorado River and its tributaries cut their channels through layer after layer of rock while the Colorado Plateau was uplifted. While the specific geologic processes and timing that formed the Grand Canyon are the subject of debate by geologists, recent evidence suggests that the Colorado River established its course through the canyon at least 17 million years ago. Since that time, the Colorado River continued to erode and form the canyon to its present-day configuration.<br />
For thousands of years, the area has been continuously inhabited by Native Americans who built settlements within the canyon and its many caves. The Pueblo people considered the Grand Canyon ("Ongtupqa" in the Hopi language) a holy site, and made pilgrimages to it. The first European known to have viewed the Grand Canyon was García López de Cárdenas from Spain, who arrived in 1540.
    GrandCanyonToroweap.jpg
  • Havasu Creek is a side stream to the Colorado River in the interior of the Grand Canyon<br />
.....<br />
The Grand Canyon is a steep-sided canyon carved by the Colorado River in the state of Arizona in the United States. It is contained within and managed by Grand Canyon National Park, the Hualapai Tribal Nation, the Havasupai Tribe and the Navajo Nation. President Theodore Roosevelt was a major proponent of preservation of the Grand Canyon area, and visited it on numerous occasions to hunt and enjoy the scenery.<br />
The Grand Canyon is 277 miles long, up to 18 miles wide and attains a depth of over a mile. Nearly two billion years of Earth's geological history have been exposed as the Colorado River and its tributaries cut their channels through layer after layer of rock while the Colorado Plateau was uplifted. While the specific geologic processes and timing that formed the Grand Canyon are the subject of debate by geologists, recent evidence suggests that the Colorado River established its course through the canyon at least 17 million years ago. Since that time, the Colorado River continued to erode and form the canyon to its present-day configuration.<br />
For thousands of years, the area has been continuously inhabited by Native Americans who built settlements within the canyon and its many caves. The Pueblo people considered the Grand Canyon ("Ongtupqa" in the Hopi language) a holy site, and made pilgrimages to it. The first European known to have viewed the Grand Canyon was García López de Cárdenas from Spain, who arrived in 1540.
    GrandCanyonHavasuCreek2.jpg
  • Matkatamiba Canyon is a side canyon to the Grand Canyon accessible from the Colorado River<br />
.....<br />
The Grand Canyon is a steep-sided canyon carved by the Colorado River in the state of Arizona in the United States. It is contained within and managed by Grand Canyon National Park, the Hualapai Tribal Nation, the Havasupai Tribe and the Navajo Nation. President Theodore Roosevelt was a major proponent of preservation of the Grand Canyon area, and visited it on numerous occasions to hunt and enjoy the scenery.<br />
The Grand Canyon is 277 miles long, up to 18 miles wide and attains a depth of over a mile. Nearly two billion years of Earth's geological history have been exposed as the Colorado River and its tributaries cut their channels through layer after layer of rock while the Colorado Plateau was uplifted. While the specific geologic processes and timing that formed the Grand Canyon are the subject of debate by geologists, recent evidence suggests that the Colorado River established its course through the canyon at least 17 million years ago. Since that time, the Colorado River continued to erode and form the canyon to its present-day configuration.<br />
For thousands of years, the area has been continuously inhabited by Native Americans who built settlements within the canyon and its many caves. The Pueblo people considered the Grand Canyon ("Ongtupqa" in the Hopi language) a holy site, and made pilgrimages to it. The first European known to have viewed the Grand Canyon was García López de Cárdenas from Spain, who arrived in 1540.
    GrandCanyonMatkatamiba2.jpg
  • The Maroon Bells are two peaks in the Elk Mountains, Maroon Peak and North Maroon Peak, separated by about a third of a mile. The mountains are about 12 miles southwest of Aspen. Both peaks are fourteeners. Maroon Peak, at 14,156 feet, is the 27th highest peak in Colorado; North Maroon Peak, at 14,014 feet, is the 50th highest. The view of the Maroon Bells to the southwest from the Maroon Creek valley is one of the most famous scenes in Colorado, and is reputed to be the "most-photographed spot in Colorado" and one of Colorado's premier scenic overlooks. The peaks are located in the Maroon Bells-Snowmass Wilderness of White River National Forest.<br />
<br />
A US Forest Service sign on the access trail refers to these mountains as "The Deadly Bells" and warns would-be climbers of "downsloping, loose, rotten and unstable" rock that "kills without warning". Unlike other mountains in the Rockies that are composed of granite and limestone, the Bells are composed of metamorphic sedimentary mudstone that has hardened into rock over millions of years. Mudstone is weak and fractures readily, giving rise to dangerously loose rock along almost any route. The mudstone is responsible for the Bells' distinctive maroon color. The Bells got their "deadly" name in 1965 when eight people died in five separate accidents.<br />
<br />
Maroon Lake (9,580') occupies a basin that was sculpted by Ice-Age glaciers and later dammed by landslide and rockfall debris from the steep slopes above the valley floor.
    MaroonBells1.jpg
  • Havasu Creek is a side stream to the Colorado River in the interior of the Grand Canyon<br />
.....<br />
The Grand Canyon is a steep-sided canyon carved by the Colorado River in the state of Arizona in the United States. It is contained within and managed by Grand Canyon National Park, the Hualapai Tribal Nation, the Havasupai Tribe and the Navajo Nation. President Theodore Roosevelt was a major proponent of preservation of the Grand Canyon area, and visited it on numerous occasions to hunt and enjoy the scenery.<br />
The Grand Canyon is 277 miles long, up to 18 miles wide and attains a depth of over a mile. Nearly two billion years of Earth's geological history have been exposed as the Colorado River and its tributaries cut their channels through layer after layer of rock while the Colorado Plateau was uplifted. While the specific geologic processes and timing that formed the Grand Canyon are the subject of debate by geologists, recent evidence suggests that the Colorado River established its course through the canyon at least 17 million years ago. Since that time, the Colorado River continued to erode and form the canyon to its present-day configuration.<br />
For thousands of years, the area has been continuously inhabited by Native Americans who built settlements within the canyon and its many caves. The Pueblo people considered the Grand Canyon ("Ongtupqa" in the Hopi language) a holy site, and made pilgrimages to it. The first European known to have viewed the Grand Canyon was García López de Cárdenas from Spain, who arrived in 1540.
    GrandCanyonHavasuCreek2.jpg
  • Matkatamiba Canyon is a side canyon to the Grand Canyon accessible from the Colorado River<br />
.....<br />
The Grand Canyon is a steep-sided canyon carved by the Colorado River in the state of Arizona in the United States. It is contained within and managed by Grand Canyon National Park, the Hualapai Tribal Nation, the Havasupai Tribe and the Navajo Nation. President Theodore Roosevelt was a major proponent of preservation of the Grand Canyon area, and visited it on numerous occasions to hunt and enjoy the scenery.<br />
The Grand Canyon is 277 miles long, up to 18 miles wide and attains a depth of over a mile. Nearly two billion years of Earth's geological history have been exposed as the Colorado River and its tributaries cut their channels through layer after layer of rock while the Colorado Plateau was uplifted. While the specific geologic processes and timing that formed the Grand Canyon are the subject of debate by geologists, recent evidence suggests that the Colorado River established its course through the canyon at least 17 million years ago. Since that time, the Colorado River continued to erode and form the canyon to its present-day configuration.<br />
For thousands of years, the area has been continuously inhabited by Native Americans who built settlements within the canyon and its many caves. The Pueblo people considered the Grand Canyon ("Ongtupqa" in the Hopi language) a holy site, and made pilgrimages to it. The first European known to have viewed the Grand Canyon was García López de Cárdenas from Spain, who arrived in 1540.
    GrandCanyonMatkatamiba2.jpg
  • The nightsky and Milky Way over Point Sublime on the North Rim of the Grand Canyon, Arizona<br />
.....<br />
The Grand Canyon is a steep-sided canyon carved by the Colorado River in the state of Arizona in the United States. It is contained within and managed by Grand Canyon National Park, the Hualapai Tribal Nation, the Havasupai Tribe and the Navajo Nation. President Theodore Roosevelt was a major proponent of preservation of the Grand Canyon area, and visited it on numerous occasions to hunt and enjoy the scenery.<br />
The Grand Canyon is 277 miles long, up to 18 miles wide and attains a depth of over a mile. Nearly two billion years of Earth's geological history have been exposed as the Colorado River and its tributaries cut their channels through layer after layer of rock while the Colorado Plateau was uplifted. While the specific geologic processes and timing that formed the Grand Canyon are the subject of debate by geologists, recent evidence suggests that the Colorado River established its course through the canyon at least 17 million years ago. Since that time, the Colorado River continued to erode and form the canyon to its present-day configuration.<br />
For thousands of years, the area has been continuously inhabited by Native Americans who built settlements within the canyon and its many caves. The Pueblo people considered the Grand Canyon ("Ongtupqa" in the Hopi language) a holy site, and made pilgrimages to it. The first European known to have viewed the Grand Canyon was García López de Cárdenas from Spain, who arrived in 1540.
    PointSublimeMilkyWay2.jpg
  • Grand Canyon from Toroweap Point<br />
.....<br />
The Grand Canyon is a steep-sided canyon carved by the Colorado River in the state of Arizona in the United States. It is contained within and managed by Grand Canyon National Park, the Hualapai Tribal Nation, the Havasupai Tribe and the Navajo Nation. President Theodore Roosevelt was a major proponent of preservation of the Grand Canyon area, and visited it on numerous occasions to hunt and enjoy the scenery.<br />
The Grand Canyon is 277 miles long, up to 18 miles wide and attains a depth of over a mile. Nearly two billion years of Earth's geological history have been exposed as the Colorado River and its tributaries cut their channels through layer after layer of rock while the Colorado Plateau was uplifted. While the specific geologic processes and timing that formed the Grand Canyon are the subject of debate by geologists, recent evidence suggests that the Colorado River established its course through the canyon at least 17 million years ago. Since that time, the Colorado River continued to erode and form the canyon to its present-day configuration.<br />
For thousands of years, the area has been continuously inhabited by Native Americans who built settlements within the canyon and its many caves. The Pueblo people considered the Grand Canyon ("Ongtupqa" in the Hopi language) a holy site, and made pilgrimages to it. The first European known to have viewed the Grand Canyon was García López de Cárdenas from Spain, who arrived in 1540.
    ToroweapPano1.jpg
  • Grand Canyon from Toroweap Point<br />
.....<br />
The Grand Canyon is a steep-sided canyon carved by the Colorado River in the state of Arizona in the United States. It is contained within and managed by Grand Canyon National Park, the Hualapai Tribal Nation, the Havasupai Tribe and the Navajo Nation. President Theodore Roosevelt was a major proponent of preservation of the Grand Canyon area, and visited it on numerous occasions to hunt and enjoy the scenery.<br />
The Grand Canyon is 277 miles long, up to 18 miles wide and attains a depth of over a mile. Nearly two billion years of Earth's geological history have been exposed as the Colorado River and its tributaries cut their channels through layer after layer of rock while the Colorado Plateau was uplifted. While the specific geologic processes and timing that formed the Grand Canyon are the subject of debate by geologists, recent evidence suggests that the Colorado River established its course through the canyon at least 17 million years ago. Since that time, the Colorado River continued to erode and form the canyon to its present-day configuration.<br />
For thousands of years, the area has been continuously inhabited by Native Americans who built settlements within the canyon and its many caves. The Pueblo people considered the Grand Canyon ("Ongtupqa" in the Hopi language) a holy site, and made pilgrimages to it. The first European known to have viewed the Grand Canyon was García López de Cárdenas from Spain, who arrived in 1540.
    Toroweap5.jpg
  • Birch Trees on the North Rim of the Grand Canyon<br />
.....<br />
The Grand Canyon is a steep-sided canyon carved by the Colorado River in the state of Arizona in the United States. It is contained within and managed by Grand Canyon National Park, the Hualapai Tribal Nation, the Havasupai Tribe and the Navajo Nation. President Theodore Roosevelt was a major proponent of preservation of the Grand Canyon area, and visited it on numerous occasions to hunt and enjoy the scenery.<br />
The Grand Canyon is 277 miles long, up to 18 miles wide and attains a depth of over a mile. Nearly two billion years of Earth's geological history have been exposed as the Colorado River and its tributaries cut their channels through layer after layer of rock while the Colorado Plateau was uplifted. While the specific geologic processes and timing that formed the Grand Canyon are the subject of debate by geologists, recent evidence suggests that the Colorado River established its course through the canyon at least 17 million years ago. Since that time, the Colorado River continued to erode and form the canyon to its present-day configuration.<br />
For thousands of years, the area has been continuously inhabited by Native Americans who built settlements within the canyon and its many caves. The Pueblo people considered the Grand Canyon ("Ongtupqa" in the Hopi language) a holy site, and made pilgrimages to it. The first European known to have viewed the Grand Canyon was García López de Cárdenas from Spain, who arrived in 1540.
    PointSublimeBirches1.jpg
  • The Maroon Bells are two peaks in the Elk Mountains, Maroon Peak and North Maroon Peak, separated by about a third of a mile. The mountains are about 12 miles southwest of Aspen. Both peaks are fourteeners. Maroon Peak, at 14,156 feet, is the 27th highest peak in Colorado; North Maroon Peak, at 14,014 feet, is the 50th highest. The view of the Maroon Bells to the southwest from the Maroon Creek valley is one of the most famous scenes in Colorado, and is reputed to be the "most-photographed spot in Colorado" and one of Colorado's premier scenic overlooks. The peaks are located in the Maroon Bells-Snowmass Wilderness of White River National Forest.<br />
<br />
A US Forest Service sign on the access trail refers to these mountains as "The Deadly Bells" and warns would-be climbers of "downsloping, loose, rotten and unstable" rock that "kills without warning". Unlike other mountains in the Rockies that are composed of granite and limestone, the Bells are composed of metamorphic sedimentary mudstone that has hardened into rock over millions of years. Mudstone is weak and fractures readily, giving rise to dangerously loose rock along almost any route. The mudstone is responsible for the Bells' distinctive maroon color. The Bells got their "deadly" name in 1965 when eight people died in five separate accidents.<br />
<br />
Maroon Lake (9,580') occupies a basin that was sculpted by Ice-Age glaciers and later dammed by landslide and rockfall debris from the steep slopes above the valley floor.
    MaroonBells5.jpg
  • The Maroon Bells are two peaks in the Elk Mountains, Maroon Peak and North Maroon Peak, separated by about a third of a mile. The mountains are about 12 miles southwest of Aspen. Both peaks are fourteeners. Maroon Peak, at 14,156 feet, is the 27th highest peak in Colorado; North Maroon Peak, at 14,014 feet, is the 50th highest. The view of the Maroon Bells to the southwest from the Maroon Creek valley is one of the most famous scenes in Colorado, and is reputed to be the "most-photographed spot in Colorado" and one of Colorado's premier scenic overlooks. The peaks are located in the Maroon Bells-Snowmass Wilderness of White River National Forest.<br />
<br />
A US Forest Service sign on the access trail refers to these mountains as "The Deadly Bells" and warns would-be climbers of "downsloping, loose, rotten and unstable" rock that "kills without warning". Unlike other mountains in the Rockies that are composed of granite and limestone, the Bells are composed of metamorphic sedimentary mudstone that has hardened into rock over millions of years. Mudstone is weak and fractures readily, giving rise to dangerously loose rock along almost any route. The mudstone is responsible for the Bells' distinctive maroon color. The Bells got their "deadly" name in 1965 when eight people died in five separate accidents.<br />
<br />
Maroon Lake (9,580') occupies a basin that was sculpted by Ice-Age glaciers and later dammed by landslide and rockfall debris from the steep slopes above the valley floor.
    MaroonBells4.jpg
  • The Maroon Bells are two peaks in the Elk Mountains, Maroon Peak and North Maroon Peak, separated by about a third of a mile. The mountains are about 12 miles southwest of Aspen. Both peaks are fourteeners. Maroon Peak, at 14,156 feet, is the 27th highest peak in Colorado; North Maroon Peak, at 14,014 feet, is the 50th highest. The view of the Maroon Bells to the southwest from the Maroon Creek valley is one of the most famous scenes in Colorado, and is reputed to be the "most-photographed spot in Colorado" and one of Colorado's premier scenic overlooks. The peaks are located in the Maroon Bells-Snowmass Wilderness of White River National Forest.<br />
<br />
A US Forest Service sign on the access trail refers to these mountains as "The Deadly Bells" and warns would-be climbers of "downsloping, loose, rotten and unstable" rock that "kills without warning". Unlike other mountains in the Rockies that are composed of granite and limestone, the Bells are composed of metamorphic sedimentary mudstone that has hardened into rock over millions of years. Mudstone is weak and fractures readily, giving rise to dangerously loose rock along almost any route. The mudstone is responsible for the Bells' distinctive maroon color. The Bells got their "deadly" name in 1965 when eight people died in five separate accidents.<br />
<br />
Maroon Lake (9,580') occupies a basin that was sculpted by Ice-Age glaciers and later dammed by landslide and rockfall debris from the steep slopes above the valley floor.
    MaroonBells2.jpg
  • The Maroon Bells are two peaks in the Elk Mountains, Maroon Peak and North Maroon Peak, separated by about a third of a mile. The mountains are about 12 miles southwest of Aspen. Both peaks are fourteeners. Maroon Peak, at 14,156 feet, is the 27th highest peak in Colorado; North Maroon Peak, at 14,014 feet, is the 50th highest. The view of the Maroon Bells to the southwest from the Maroon Creek valley is one of the most famous scenes in Colorado, and is reputed to be the "most-photographed spot in Colorado" and one of Colorado's premier scenic overlooks. The peaks are located in the Maroon Bells-Snowmass Wilderness of White River National Forest.<br />
<br />
A US Forest Service sign on the access trail refers to these mountains as "The Deadly Bells" and warns would-be climbers of "downsloping, loose, rotten and unstable" rock that "kills without warning". Unlike other mountains in the Rockies that are composed of granite and limestone, the Bells are composed of metamorphic sedimentary mudstone that has hardened into rock over millions of years. Mudstone is weak and fractures readily, giving rise to dangerously loose rock along almost any route. The mudstone is responsible for the Bells' distinctive maroon color. The Bells got their "deadly" name in 1965 when eight people died in five separate accidents.<br />
<br />
Maroon Lake (9,580') occupies a basin that was sculpted by Ice-Age glaciers and later dammed by landslide and rockfall debris from the steep slopes above the valley floor.
    MaroonBells5.jpg
  • The Maroon Bells are two peaks in the Elk Mountains, Maroon Peak and North Maroon Peak, separated by about a third of a mile. The mountains are about 12 miles southwest of Aspen. Both peaks are fourteeners. Maroon Peak, at 14,156 feet, is the 27th highest peak in Colorado; North Maroon Peak, at 14,014 feet, is the 50th highest. The view of the Maroon Bells to the southwest from the Maroon Creek valley is one of the most famous scenes in Colorado, and is reputed to be the "most-photographed spot in Colorado" and one of Colorado's premier scenic overlooks. The peaks are located in the Maroon Bells-Snowmass Wilderness of White River National Forest.<br />
<br />
A US Forest Service sign on the access trail refers to these mountains as "The Deadly Bells" and warns would-be climbers of "downsloping, loose, rotten and unstable" rock that "kills without warning". Unlike other mountains in the Rockies that are composed of granite and limestone, the Bells are composed of metamorphic sedimentary mudstone that has hardened into rock over millions of years. Mudstone is weak and fractures readily, giving rise to dangerously loose rock along almost any route. The mudstone is responsible for the Bells' distinctive maroon color. The Bells got their "deadly" name in 1965 when eight people died in five separate accidents.<br />
<br />
Maroon Lake (9,580') occupies a basin that was sculpted by Ice-Age glaciers and later dammed by landslide and rockfall debris from the steep slopes above the valley floor.
    MaroonBells1.jpg
  • The Maroon Bells are two peaks in the Elk Mountains, Maroon Peak and North Maroon Peak, separated by about a third of a mile. The mountains are about 12 miles southwest of Aspen. Both peaks are fourteeners. Maroon Peak, at 14,156 feet, is the 27th highest peak in Colorado; North Maroon Peak, at 14,014 feet, is the 50th highest. The view of the Maroon Bells to the southwest from the Maroon Creek valley is one of the most famous scenes in Colorado, and is reputed to be the "most-photographed spot in Colorado" and one of Colorado's premier scenic overlooks. The peaks are located in the Maroon Bells-Snowmass Wilderness of White River National Forest.<br />
<br />
A US Forest Service sign on the access trail refers to these mountains as "The Deadly Bells" and warns would-be climbers of "downsloping, loose, rotten and unstable" rock that "kills without warning". Unlike other mountains in the Rockies that are composed of granite and limestone, the Bells are composed of metamorphic sedimentary mudstone that has hardened into rock over millions of years. Mudstone is weak and fractures readily, giving rise to dangerously loose rock along almost any route. The mudstone is responsible for the Bells' distinctive maroon color. The Bells got their "deadly" name in 1965 when eight people died in five separate accidents.<br />
<br />
Maroon Lake (9,580') occupies a basin that was sculpted by Ice-Age glaciers and later dammed by landslide and rockfall debris from the steep slopes above the valley floor.
    MaroonBells6.jpg
  • The Maroon Bells are two peaks in the Elk Mountains, Maroon Peak and North Maroon Peak, separated by about a third of a mile. The mountains are about 12 miles southwest of Aspen. Both peaks are fourteeners. Maroon Peak, at 14,156 feet, is the 27th highest peak in Colorado; North Maroon Peak, at 14,014 feet, is the 50th highest. The view of the Maroon Bells to the southwest from the Maroon Creek valley is one of the most famous scenes in Colorado, and is reputed to be the "most-photographed spot in Colorado" and one of Colorado's premier scenic overlooks. The peaks are located in the Maroon Bells-Snowmass Wilderness of White River National Forest.<br />
<br />
A US Forest Service sign on the access trail refers to these mountains as "The Deadly Bells" and warns would-be climbers of "downsloping, loose, rotten and unstable" rock that "kills without warning". Unlike other mountains in the Rockies that are composed of granite and limestone, the Bells are composed of metamorphic sedimentary mudstone that has hardened into rock over millions of years. Mudstone is weak and fractures readily, giving rise to dangerously loose rock along almost any route. The mudstone is responsible for the Bells' distinctive maroon color. The Bells got their "deadly" name in 1965 when eight people died in five separate accidents.<br />
<br />
Maroon Lake (9,580') occupies a basin that was sculpted by Ice-Age glaciers and later dammed by landslide and rockfall debris from the steep slopes above the valley floor.
    MaroonBells2.jpg
  • The Maroon Bells are two peaks in the Elk Mountains, Maroon Peak and North Maroon Peak, separated by about a third of a mile. The mountains are about 12 miles southwest of Aspen. Both peaks are fourteeners. Maroon Peak, at 14,156 feet, is the 27th highest peak in Colorado; North Maroon Peak, at 14,014 feet, is the 50th highest. The view of the Maroon Bells to the southwest from the Maroon Creek valley is one of the most famous scenes in Colorado, and is reputed to be the "most-photographed spot in Colorado" and one of Colorado's premier scenic overlooks. The peaks are located in the Maroon Bells-Snowmass Wilderness of White River National Forest.<br />
<br />
A US Forest Service sign on the access trail refers to these mountains as "The Deadly Bells" and warns would-be climbers of "downsloping, loose, rotten and unstable" rock that "kills without warning". Unlike other mountains in the Rockies that are composed of granite and limestone, the Bells are composed of metamorphic sedimentary mudstone that has hardened into rock over millions of years. Mudstone is weak and fractures readily, giving rise to dangerously loose rock along almost any route. The mudstone is responsible for the Bells' distinctive maroon color. The Bells got their "deadly" name in 1965 when eight people died in five separate accidents.<br />
<br />
Maroon Lake (9,580') occupies a basin that was sculpted by Ice-Age glaciers and later dammed by landslide and rockfall debris from the steep slopes above the valley floor.
    MaroonBells4.jpg
  • The Maroon Bells are two peaks in the Elk Mountains, Maroon Peak and North Maroon Peak, separated by about a third of a mile. The mountains are about 12 miles southwest of Aspen. Both peaks are fourteeners. Maroon Peak, at 14,156 feet, is the 27th highest peak in Colorado; North Maroon Peak, at 14,014 feet, is the 50th highest. The view of the Maroon Bells to the southwest from the Maroon Creek valley is one of the most famous scenes in Colorado, and is reputed to be the "most-photographed spot in Colorado" and one of Colorado's premier scenic overlooks. The peaks are located in the Maroon Bells-Snowmass Wilderness of White River National Forest.<br />
<br />
A US Forest Service sign on the access trail refers to these mountains as "The Deadly Bells" and warns would-be climbers of "downsloping, loose, rotten and unstable" rock that "kills without warning". Unlike other mountains in the Rockies that are composed of granite and limestone, the Bells are composed of metamorphic sedimentary mudstone that has hardened into rock over millions of years. Mudstone is weak and fractures readily, giving rise to dangerously loose rock along almost any route. The mudstone is responsible for the Bells' distinctive maroon color. The Bells got their "deadly" name in 1965 when eight people died in five separate accidents.<br />
<br />
Maroon Lake (9,580') occupies a basin that was sculpted by Ice-Age glaciers and later dammed by landslide and rockfall debris from the steep slopes above the valley floor.
    MaroonBells3.jpg
  • Horseshoe Bend on the Colorado River near Page, Arizona ..... Horseshoe Bend is a horseshoe-shaped meander of the Colorado River located near the town of Page, Arizona, in the United States. Horseshoe Bend is located 5 miles downstream from the Glen Canyon Dam and Lake Powell within Glen Canyon National Recreation Area, about 4 miles southwest of Page. It is accessible via hiking a 1.5-mile round trip from U.S. Route 89, but an access road also reaches the geological structure, as it is part of a state park. Horseshoe Bend can be viewed from the steep cliff above. The overlook is 4,200 feet (1,300 m) above sea level, and the Colorado River is at 3,200 feet (980 m) above sea level, making it a 1,000-foot (300 m) drop
    HorseshoeBendSunrise1.jpg
  • Austin is the capital of Texas and the seat of Travis County. Located in Central Texas and the American Southwest, it is the 11th-largest city in the United States of America and the fourth-largest city in the state of Texas. It was the third-fastest-growing large city in the nation from 2000 to 2006. Austin is also the second largest state capital in the United States. Austin has a population of 842,592 (2012 estimate). The city is the cultural and economic center of the five-county Austin–Round Rock metropolitan area, which had an estimated population 1,834,303 (2012 U.S. Census). In the 1830s, pioneers began to settle the area in central Austin along the Colorado River. After Republic of Texas Vice President Mirabeau B. Lamar visited the area during a buffalo-hunting expedition between 1837 and 1838, he proposed that the republic's capital then located in Houston, Texas, be relocated to the area situated on the north bank of the Colorado River near the present-day Congress Avenue Bridge. In 1839, the site was officially chosen as the republic's new capital (the republic's seventh and final location) and was incorporated under the name Waterloo. Shortly thereafter, the name was changed to Austin in honor of Stephen F. Austin, the "Father of Texas" and the republic's first secretary of state. The city grew throughout the 19th century and became a center for government and education with the construction of the Texas State Capitol and the University of Texas at Austin. After a lull in growth from the Great Depression, Austin resumed its development into a major city and, by the 1980s, it emerged as a center for technology and business. A number of Fortune 500 companies have headquarters or regional offices in Austin including Advanced Micro Devices, Apple Inc., eBay, Google, IBM, Intel, Texas Instruments, 3M, and Whole Foods Market. Dell's worldwide headquarters is located in nearby Round Rock, a suburb of Austin.
    AustinNightSkyline3.jpg
  • The Durango and Silverton Narrow Gauge Railroad (D&SNG) is a narrow gauge heritage railroad that operates 45 miles of 3 ft track between Durango and Silverton, in the US state of Colorado. The railway is a federally designated National Historic Landmark and is also designated by the American Society of Civil Engineers as a Historic Civil Engineering Landmark.<br />
The route was originally built between 1881 and 1882, by the Denver and Rio Grande Railway, in order to carry supplies and people to and silver and gold ore from mines in the San Juan Mountains. The line was an extension of the D&RG narrow gauge from Antonito, Colorado to Durango. The last train to operate into Durango from the east was on December 6, 1968. The States of New Mexico and Colorado purchased 64 miles of the line between Antonito and Chama, New Mexico in 1970 and operates today as the Cumbres and Toltec Scenic Railroad. The trackage between Chama and Durango was abandoned and rails were removed by 1971.
    DurangoTrainNight1.jpg
  • The Strater Hotel in Durango, Colorado. The City of Durango is a Home Rule Municipality that is the county seat and the most populous city of La Plata County, Colorado, United States.[6] The United States Census Bureau reported a population of 16,887 in the 2010 census.
    DurangoStreet2.jpg
  • The Durango and Silverton Narrow Gauge Railroad (D&SNG) is a narrow gauge heritage railroad that operates 45 miles of 3 ft track between Durango and Silverton, in the US state of Colorado. The railway is a federally designated National Historic Landmark and is also designated by the American Society of Civil Engineers as a Historic Civil Engineering Landmark.<br />
The route was originally built between 1881 and 1882, by the Denver and Rio Grande Railway, in order to carry supplies and people to and silver and gold ore from mines in the San Juan Mountains. The line was an extension of the D&RG narrow gauge from Antonito, Colorado to Durango. The last train to operate into Durango from the east was on December 6, 1968. The States of New Mexico and Colorado purchased 64 miles of the line between Antonito and Chama, New Mexico in 1970 and operates today as the Cumbres and Toltec Scenic Railroad. The trackage between Chama and Durango was abandoned and rails were removed by 1971.
    DurangoStationNight2.jpg
  • The Durango and Silverton Narrow Gauge Railroad (D&SNG) is a narrow gauge heritage railroad that operates 45 miles of 3 ft track between Durango and Silverton, in the US state of Colorado. The railway is a federally designated National Historic Landmark and is also designated by the American Society of Civil Engineers as a Historic Civil Engineering Landmark.<br />
The route was originally built between 1881 and 1882, by the Denver and Rio Grande Railway, in order to carry supplies and people to and silver and gold ore from mines in the San Juan Mountains. The line was an extension of the D&RG narrow gauge from Antonito, Colorado to Durango. The last train to operate into Durango from the east was on December 6, 1968. The States of New Mexico and Colorado purchased 64 miles of the line between Antonito and Chama, New Mexico in 1970 and operates today as the Cumbres and Toltec Scenic Railroad. The trackage between Chama and Durango was abandoned and rails were removed by 1971.
    DurangoBowenRanch1.jpg
  • The Durango and Silverton Narrow Gauge Railroad (D&SNG) is a narrow gauge heritage railroad that operates 45 miles of 3 ft track between Durango and Silverton, in the US state of Colorado. The railway is a federally designated National Historic Landmark and is also designated by the American Society of Civil Engineers as a Historic Civil Engineering Landmark.<br />
The route was originally built between 1881 and 1882, by the Denver and Rio Grande Railway, in order to carry supplies and people to and silver and gold ore from mines in the San Juan Mountains. The line was an extension of the D&RG narrow gauge from Antonito, Colorado to Durango. The last train to operate into Durango from the east was on December 6, 1968. The States of New Mexico and Colorado purchased 64 miles of the line between Antonito and Chama, New Mexico in 1970 and operates today as the Cumbres and Toltec Scenic Railroad. The trackage between Chama and Durango was abandoned and rails were removed by 1971.
    DurangoTrain2.jpg
  • The Durango and Silverton Narrow Gauge Railroad (D&SNG) is a narrow gauge heritage railroad that operates 45 miles of 3 ft track between Durango and Silverton, in the US state of Colorado. The railway is a federally designated National Historic Landmark and is also designated by the American Society of Civil Engineers as a Historic Civil Engineering Landmark.<br />
The route was originally built between 1881 and 1882, by the Denver and Rio Grande Railway, in order to carry supplies and people to and silver and gold ore from mines in the San Juan Mountains. The line was an extension of the D&RG narrow gauge from Antonito, Colorado to Durango. The last train to operate into Durango from the east was on December 6, 1968. The States of New Mexico and Colorado purchased 64 miles of the line between Antonito and Chama, New Mexico in 1970 and operates today as the Cumbres and Toltec Scenic Railroad. The trackage between Chama and Durango was abandoned and rails were removed by 1971.
    DurangoElkPark1.jpg
  • The Durango and Silverton Narrow Gauge Railroad (D&SNG) is a narrow gauge heritage railroad that operates 45 miles of 3 ft track between Durango and Silverton, in the US state of Colorado. The railway is a federally designated National Historic Landmark and is also designated by the American Society of Civil Engineers as a Historic Civil Engineering Landmark.<br />
The route was originally built between 1881 and 1882, by the Denver and Rio Grande Railway, in order to carry supplies and people to and silver and gold ore from mines in the San Juan Mountains. The line was an extension of the D&RG narrow gauge from Antonito, Colorado to Durango. The last train to operate into Durango from the east was on December 6, 1968. The States of New Mexico and Colorado purchased 64 miles of the line between Antonito and Chama, New Mexico in 1970 and operates today as the Cumbres and Toltec Scenic Railroad. The trackage between Chama and Durango was abandoned and rails were removed by 1971.
    DurangoNeedleton1.jpg
  • The Durango and Silverton Narrow Gauge Railroad (D&SNG) is a narrow gauge heritage railroad that operates 45 miles of 3 ft track between Durango and Silverton, in the US state of Colorado. The railway is a federally designated National Historic Landmark and is also designated by the American Society of Civil Engineers as a Historic Civil Engineering Landmark.<br />
The route was originally built between 1881 and 1882, by the Denver and Rio Grande Railway, in order to carry supplies and people to and silver and gold ore from mines in the San Juan Mountains. The line was an extension of the D&RG narrow gauge from Antonito, Colorado to Durango. The last train to operate into Durango from the east was on December 6, 1968. The States of New Mexico and Colorado purchased 64 miles of the line between Antonito and Chama, New Mexico in 1970 and operates today as the Cumbres and Toltec Scenic Railroad. The trackage between Chama and Durango was abandoned and rails were removed by 1971.
    DurangoNeedleCreek3.jpg
  • The Durango and Silverton Narrow Gauge Railroad (D&SNG) is a narrow gauge heritage railroad that operates 45 miles of 3 ft track between Durango and Silverton, in the US state of Colorado. The railway is a federally designated National Historic Landmark and is also designated by the American Society of Civil Engineers as a Historic Civil Engineering Landmark.<br />
The route was originally built between 1881 and 1882, by the Denver and Rio Grande Railway, in order to carry supplies and people to and silver and gold ore from mines in the San Juan Mountains. The line was an extension of the D&RG narrow gauge from Antonito, Colorado to Durango. The last train to operate into Durango from the east was on December 6, 1968. The States of New Mexico and Colorado purchased 64 miles of the line between Antonito and Chama, New Mexico in 1970 and operates today as the Cumbres and Toltec Scenic Railroad. The trackage between Chama and Durango was abandoned and rails were removed by 1971.
    DurangoNeedleCreek1.jpg
  • Navajo Bridge crosses the Colorado River's Marble Canyon near Lee's Ferry in the US state of Arizona. Apart from the Glen Canyon Bridge a few miles upstream at Page, Arizona, it is the only roadway crossing of the river and the Grand Canyon for nearly 600 miles (970 km). Spanning Marble Canyon, the bridge carries northbound travelers to southern Utah and to the Arizona Strip, the otherwise inaccessible portion of Arizona north of the Colorado River, which includes the North Rim of Grand Canyon National Park.<br />
Prior to the construction of the first Navajo Bridge, the only river crossing from Arizona to Utah was at nearby Lee's Ferry, where the canyon walls are low and getting vehicles onto the water is relatively convenient. The ferry offered only unreliable service, however, as adverse weather and flooding regularly prevented its operation.
    NavajoBridge1.jpg
  • Horseshoe Bend on the Colorado River near Page, Arizona ..... Horseshoe Bend is a horseshoe-shaped meander of the Colorado River located near the town of Page, Arizona, in the United States. Horseshoe Bend is located 5 miles downstream from the Glen Canyon Dam and Lake Powell within Glen Canyon National Recreation Area, about 4 miles southwest of Page. It is accessible via hiking a 1.5-mile round trip from U.S. Route 89, but an access road also reaches the geological structure, as it is part of a state park. Horseshoe Bend can be viewed from the steep cliff above. The overlook is 4,200 feet (1,300 m) above sea level, and the Colorado River is at 3,200 feet (980 m) above sea level, making it a 1,000-foot (300 m) drop
    HorseshoeBendSunrise1.jpg
  • Navajo Bridge crosses the Colorado River's Marble Canyon near Lee's Ferry in the US state of Arizona. Apart from the Glen Canyon Bridge a few miles upstream at Page, Arizona, it is the only roadway crossing of the river and the Grand Canyon for nearly 600 miles (970 km). Spanning Marble Canyon, the bridge carries northbound travelers to southern Utah and to the Arizona Strip, the otherwise inaccessible portion of Arizona north of the Colorado River, which includes the North Rim of Grand Canyon National Park.<br />
Prior to the construction of the first Navajo Bridge, the only river crossing from Arizona to Utah was at nearby Lee's Ferry, where the canyon walls are low and getting vehicles onto the water is relatively convenient. The ferry offered only unreliable service, however, as adverse weather and flooding regularly prevented its operation.
    NavajoBridge1.jpg
  • The Durango and Silverton Narrow Gauge Railroad (D&SNG) is a narrow gauge heritage railroad that operates 45 miles of 3 ft track between Durango and Silverton, in the US state of Colorado. The railway is a federally designated National Historic Landmark and is also designated by the American Society of Civil Engineers as a Historic Civil Engineering Landmark.<br />
The route was originally built between 1881 and 1882, by the Denver and Rio Grande Railway, in order to carry supplies and people to and silver and gold ore from mines in the San Juan Mountains. The line was an extension of the D&RG narrow gauge from Antonito, Colorado to Durango. The last train to operate into Durango from the east was on December 6, 1968. The States of New Mexico and Colorado purchased 64 miles of the line between Antonito and Chama, New Mexico in 1970 and operates today as the Cumbres and Toltec Scenic Railroad. The trackage between Chama and Durango was abandoned and rails were removed by 1971.
    DurangoTwinBridge1.jpg
  • The Durango and Silverton Narrow Gauge Railroad (D&SNG) is a narrow gauge heritage railroad that operates 45 miles of 3 ft track between Durango and Silverton, in the US state of Colorado. The railway is a federally designated National Historic Landmark and is also designated by the American Society of Civil Engineers as a Historic Civil Engineering Landmark.<br />
The route was originally built between 1881 and 1882, by the Denver and Rio Grande Railway, in order to carry supplies and people to and silver and gold ore from mines in the San Juan Mountains. The line was an extension of the D&RG narrow gauge from Antonito, Colorado to Durango. The last train to operate into Durango from the east was on December 6, 1968. The States of New Mexico and Colorado purchased 64 miles of the line between Antonito and Chama, New Mexico in 1970 and operates today as the Cumbres and Toltec Scenic Railroad. The trackage between Chama and Durango was abandoned and rails were removed by 1971.
    DurangoBowenRanch2.jpg
  • Austin is the capital of Texas and the seat of Travis County. Located in Central Texas and the American Southwest, it is the 11th-largest city in the United States of America and the fourth-largest city in the state of Texas. It was the third-fastest-growing large city in the nation from 2000 to 2006. Austin is also the second largest state capital in the United States. Austin has a population of 842,592 (2012 estimate). The city is the cultural and economic center of the five-county Austin–Round Rock metropolitan area, which had an estimated population 1,834,303 (2012 U.S. Census). In the 1830s, pioneers began to settle the area in central Austin along the Colorado River. After Republic of Texas Vice President Mirabeau B. Lamar visited the area during a buffalo-hunting expedition between 1837 and 1838, he proposed that the republic's capital then located in Houston, Texas, be relocated to the area situated on the north bank of the Colorado River near the present-day Congress Avenue Bridge. In 1839, the site was officially chosen as the republic's new capital (the republic's seventh and final location) and was incorporated under the name Waterloo. Shortly thereafter, the name was changed to Austin in honor of Stephen F. Austin, the "Father of Texas" and the republic's first secretary of state. The city grew throughout the 19th century and became a center for government and education with the construction of the Texas State Capitol and the University of Texas at Austin. After a lull in growth from the Great Depression, Austin resumed its development into a major city and, by the 1980s, it emerged as a center for technology and business. A number of Fortune 500 companies have headquarters or regional offices in Austin including Advanced Micro Devices, Apple Inc., eBay, Google, IBM, Intel, Texas Instruments, 3M, and Whole Foods Market. Dell's worldwide headquarters is located in nearby Round Rock, a suburb of Austin.
    AustinNightSkyline2.jpg
  • Austin is the capital of Texas and the seat of Travis County. Located in Central Texas and the American Southwest, it is the 11th-largest city in the United States of America and the fourth-largest city in the state of Texas. It was the third-fastest-growing large city in the nation from 2000 to 2006. Austin is also the second largest state capital in the United States. Austin has a population of 842,592 (2012 estimate). The city is the cultural and economic center of the five-county Austin–Round Rock metropolitan area, which had an estimated population 1,834,303 (2012 U.S. Census). In the 1830s, pioneers began to settle the area in central Austin along the Colorado River. After Republic of Texas Vice President Mirabeau B. Lamar visited the area during a buffalo-hunting expedition between 1837 and 1838, he proposed that the republic's capital then located in Houston, Texas, be relocated to the area situated on the north bank of the Colorado River near the present-day Congress Avenue Bridge. In 1839, the site was officially chosen as the republic's new capital (the republic's seventh and final location) and was incorporated under the name Waterloo. Shortly thereafter, the name was changed to Austin in honor of Stephen F. Austin, the "Father of Texas" and the republic's first secretary of state. The city grew throughout the 19th century and became a center for government and education with the construction of the Texas State Capitol and the University of Texas at Austin. After a lull in growth from the Great Depression, Austin resumed its development into a major city and, by the 1980s, it emerged as a center for technology and business. A number of Fortune 500 companies have headquarters or regional offices in Austin including Advanced Micro Devices, Apple Inc., eBay, Google, IBM, Intel, Texas Instruments, 3M, and Whole Foods Market. Dell's worldwide headquarters is located in nearby Round Rock, a suburb of Austin.
    AustinNightSkyline1.jpg
  • The Durango and Silverton Narrow Gauge Railroad (D&SNG) is a narrow gauge heritage railroad that operates 45 miles of 3 ft track between Durango and Silverton, in the US state of Colorado. The railway is a federally designated National Historic Landmark and is also designated by the American Society of Civil Engineers as a Historic Civil Engineering Landmark.<br />
The route was originally built between 1881 and 1882, by the Denver and Rio Grande Railway, in order to carry supplies and people to and silver and gold ore from mines in the San Juan Mountains. The line was an extension of the D&RG narrow gauge from Antonito, Colorado to Durango. The last train to operate into Durango from the east was on December 6, 1968. The States of New Mexico and Colorado purchased 64 miles of the line between Antonito and Chama, New Mexico in 1970 and operates today as the Cumbres and Toltec Scenic Railroad. The trackage between Chama and Durango was abandoned and rails were removed by 1971.
    DurangoTwinBridge1.jpg
  • The Durango and Silverton Narrow Gauge Railroad (D&SNG) is a narrow gauge heritage railroad that operates 45 miles of 3 ft track between Durango and Silverton, in the US state of Colorado. The railway is a federally designated National Historic Landmark and is also designated by the American Society of Civil Engineers as a Historic Civil Engineering Landmark.<br />
The route was originally built between 1881 and 1882, by the Denver and Rio Grande Railway, in order to carry supplies and people to and silver and gold ore from mines in the San Juan Mountains. The line was an extension of the D&RG narrow gauge from Antonito, Colorado to Durango. The last train to operate into Durango from the east was on December 6, 1968. The States of New Mexico and Colorado purchased 64 miles of the line between Antonito and Chama, New Mexico in 1970 and operates today as the Cumbres and Toltec Scenic Railroad. The trackage between Chama and Durango was abandoned and rails were removed by 1971.
    DurangoTrainNight4.jpg
  • The Durango and Silverton Narrow Gauge Railroad (D&SNG) is a narrow gauge heritage railroad that operates 45 miles of 3 ft track between Durango and Silverton, in the US state of Colorado. The railway is a federally designated National Historic Landmark and is also designated by the American Society of Civil Engineers as a Historic Civil Engineering Landmark.<br />
The route was originally built between 1881 and 1882, by the Denver and Rio Grande Railway, in order to carry supplies and people to and silver and gold ore from mines in the San Juan Mountains. The line was an extension of the D&RG narrow gauge from Antonito, Colorado to Durango. The last train to operate into Durango from the east was on December 6, 1968. The States of New Mexico and Colorado purchased 64 miles of the line between Antonito and Chama, New Mexico in 1970 and operates today as the Cumbres and Toltec Scenic Railroad. The trackage between Chama and Durango was abandoned and rails were removed by 1971.
    DurangoTrainNight3.jpg
  • The Durango and Silverton Narrow Gauge Railroad (D&SNG) is a narrow gauge heritage railroad that operates 45 miles of 3 ft track between Durango and Silverton, in the US state of Colorado. The railway is a federally designated National Historic Landmark and is also designated by the American Society of Civil Engineers as a Historic Civil Engineering Landmark.<br />
The route was originally built between 1881 and 1882, by the Denver and Rio Grande Railway, in order to carry supplies and people to and silver and gold ore from mines in the San Juan Mountains. The line was an extension of the D&RG narrow gauge from Antonito, Colorado to Durango. The last train to operate into Durango from the east was on December 6, 1968. The States of New Mexico and Colorado purchased 64 miles of the line between Antonito and Chama, New Mexico in 1970 and operates today as the Cumbres and Toltec Scenic Railroad. The trackage between Chama and Durango was abandoned and rails were removed by 1971.
    DurangoHighLine1.jpg
  • The Durango and Silverton Narrow Gauge Railroad (D&SNG) is a narrow gauge heritage railroad that operates 45 miles of 3 ft track between Durango and Silverton, in the US state of Colorado. The railway is a federally designated National Historic Landmark and is also designated by the American Society of Civil Engineers as a Historic Civil Engineering Landmark.<br />
The route was originally built between 1881 and 1882, by the Denver and Rio Grande Railway, in order to carry supplies and people to and silver and gold ore from mines in the San Juan Mountains. The line was an extension of the D&RG narrow gauge from Antonito, Colorado to Durango. The last train to operate into Durango from the east was on December 6, 1968. The States of New Mexico and Colorado purchased 64 miles of the line between Antonito and Chama, New Mexico in 1970 and operates today as the Cumbres and Toltec Scenic Railroad. The trackage between Chama and Durango was abandoned and rails were removed by 1971.
    DurangoHighline3.jpg
  • The Durango and Silverton Narrow Gauge Railroad (D&SNG) is a narrow gauge heritage railroad that operates 45 miles of 3 ft track between Durango and Silverton, in the US state of Colorado. The railway is a federally designated National Historic Landmark and is also designated by the American Society of Civil Engineers as a Historic Civil Engineering Landmark.<br />
The route was originally built between 1881 and 1882, by the Denver and Rio Grande Railway, in order to carry supplies and people to and silver and gold ore from mines in the San Juan Mountains. The line was an extension of the D&RG narrow gauge from Antonito, Colorado to Durango. The last train to operate into Durango from the east was on December 6, 1968. The States of New Mexico and Colorado purchased 64 miles of the line between Antonito and Chama, New Mexico in 1970 and operates today as the Cumbres and Toltec Scenic Railroad. The trackage between Chama and Durango was abandoned and rails were removed by 1971.
    DurangoBowenRanch2.jpg
  • The Durango and Silverton Narrow Gauge Railroad (D&SNG) is a narrow gauge heritage railroad that operates 45 miles of 3 ft track between Durango and Silverton, in the US state of Colorado. The railway is a federally designated National Historic Landmark and is also designated by the American Society of Civil Engineers as a Historic Civil Engineering Landmark.<br />
The route was originally built between 1881 and 1882, by the Denver and Rio Grande Railway, in order to carry supplies and people to and silver and gold ore from mines in the San Juan Mountains. The line was an extension of the D&RG narrow gauge from Antonito, Colorado to Durango. The last train to operate into Durango from the east was on December 6, 1968. The States of New Mexico and Colorado purchased 64 miles of the line between Antonito and Chama, New Mexico in 1970 and operates today as the Cumbres and Toltec Scenic Railroad. The trackage between Chama and Durango was abandoned and rails were removed by 1971.
    DurangoTrain1.jpg
  • The Durango and Silverton Narrow Gauge Railroad (D&SNG) is a narrow gauge heritage railroad that operates 45 miles of 3 ft track between Durango and Silverton, in the US state of Colorado. The railway is a federally designated National Historic Landmark and is also designated by the American Society of Civil Engineers as a Historic Civil Engineering Landmark.<br />
The route was originally built between 1881 and 1882, by the Denver and Rio Grande Railway, in order to carry supplies and people to and silver and gold ore from mines in the San Juan Mountains. The line was an extension of the D&RG narrow gauge from Antonito, Colorado to Durango. The last train to operate into Durango from the east was on December 6, 1968. The States of New Mexico and Colorado purchased 64 miles of the line between Antonito and Chama, New Mexico in 1970 and operates today as the Cumbres and Toltec Scenic Railroad. The trackage between Chama and Durango was abandoned and rails were removed by 1971.
    DurangoColoradoTrail2.jpg
  • The Durango and Silverton Narrow Gauge Railroad (D&SNG) is a narrow gauge heritage railroad that operates 45 miles of 3 ft track between Durango and Silverton, in the US state of Colorado. The railway is a federally designated National Historic Landmark and is also designated by the American Society of Civil Engineers as a Historic Civil Engineering Landmark.<br />
The route was originally built between 1881 and 1882, by the Denver and Rio Grande Railway, in order to carry supplies and people to and silver and gold ore from mines in the San Juan Mountains. The line was an extension of the D&RG narrow gauge from Antonito, Colorado to Durango. The last train to operate into Durango from the east was on December 6, 1968. The States of New Mexico and Colorado purchased 64 miles of the line between Antonito and Chama, New Mexico in 1970 and operates today as the Cumbres and Toltec Scenic Railroad. The trackage between Chama and Durango was abandoned and rails were removed by 1971.
    DurangoSteamEngine1.jpg
  • The Durango and Silverton Narrow Gauge Railroad (D&SNG) is a narrow gauge heritage railroad that operates 45 miles of 3 ft track between Durango and Silverton, in the US state of Colorado. The railway is a federally designated National Historic Landmark and is also designated by the American Society of Civil Engineers as a Historic Civil Engineering Landmark.<br />
The route was originally built between 1881 and 1882, by the Denver and Rio Grande Railway, in order to carry supplies and people to and silver and gold ore from mines in the San Juan Mountains. The line was an extension of the D&RG narrow gauge from Antonito, Colorado to Durango. The last train to operate into Durango from the east was on December 6, 1968. The States of New Mexico and Colorado purchased 64 miles of the line between Antonito and Chama, New Mexico in 1970 and operates today as the Cumbres and Toltec Scenic Railroad. The trackage between Chama and Durango was abandoned and rails were removed by 1971.
    DurangoElkPark2.jpg
  • The Durango and Silverton Narrow Gauge Railroad (D&SNG) is a narrow gauge heritage railroad that operates 45 miles of 3 ft track between Durango and Silverton, in the US state of Colorado. The railway is a federally designated National Historic Landmark and is also designated by the American Society of Civil Engineers as a Historic Civil Engineering Landmark.<br />
The route was originally built between 1881 and 1882, by the Denver and Rio Grande Railway, in order to carry supplies and people to and silver and gold ore from mines in the San Juan Mountains. The line was an extension of the D&RG narrow gauge from Antonito, Colorado to Durango. The last train to operate into Durango from the east was on December 6, 1968. The States of New Mexico and Colorado purchased 64 miles of the line between Antonito and Chama, New Mexico in 1970 and operates today as the Cumbres and Toltec Scenic Railroad. The trackage between Chama and Durango was abandoned and rails were removed by 1971.
    DurangoNeedleCreek5.jpg
  • The Durango and Silverton Narrow Gauge Railroad (D&SNG) is a narrow gauge heritage railroad that operates 45 miles of 3 ft track between Durango and Silverton, in the US state of Colorado. The railway is a federally designated National Historic Landmark and is also designated by the American Society of Civil Engineers as a Historic Civil Engineering Landmark.<br />
The route was originally built between 1881 and 1882, by the Denver and Rio Grande Railway, in order to carry supplies and people to and silver and gold ore from mines in the San Juan Mountains. The line was an extension of the D&RG narrow gauge from Antonito, Colorado to Durango. The last train to operate into Durango from the east was on December 6, 1968. The States of New Mexico and Colorado purchased 64 miles of the line between Antonito and Chama, New Mexico in 1970 and operates today as the Cumbres and Toltec Scenic Railroad. The trackage between Chama and Durango was abandoned and rails were removed by 1971.
    DurangoTrainNeedleton2.jpg
  • The Durango and Silverton Narrow Gauge Railroad (D&SNG) is a narrow gauge heritage railroad that operates 45 miles of 3 ft track between Durango and Silverton, in the US state of Colorado. The railway is a federally designated National Historic Landmark and is also designated by the American Society of Civil Engineers as a Historic Civil Engineering Landmark.<br />
The route was originally built between 1881 and 1882, by the Denver and Rio Grande Railway, in order to carry supplies and people to and silver and gold ore from mines in the San Juan Mountains. The line was an extension of the D&RG narrow gauge from Antonito, Colorado to Durango. The last train to operate into Durango from the east was on December 6, 1968. The States of New Mexico and Colorado purchased 64 miles of the line between Antonito and Chama, New Mexico in 1970 and operates today as the Cumbres and Toltec Scenic Railroad. The trackage between Chama and Durango was abandoned and rails were removed by 1971.
    DurangoNeedleCreek2.jpg
  • The Durango and Silverton Narrow Gauge Railroad (D&SNG) is a narrow gauge heritage railroad that operates 45 miles of 3 ft track between Durango and Silverton, in the US state of Colorado. The railway is a federally designated National Historic Landmark and is also designated by the American Society of Civil Engineers as a Historic Civil Engineering Landmark.<br />
The route was originally built between 1881 and 1882, by the Denver and Rio Grande Railway, in order to carry supplies and people to and silver and gold ore from mines in the San Juan Mountains. The line was an extension of the D&RG narrow gauge from Antonito, Colorado to Durango. The last train to operate into Durango from the east was on December 6, 1968. The States of New Mexico and Colorado purchased 64 miles of the line between Antonito and Chama, New Mexico in 1970 and operates today as the Cumbres and Toltec Scenic Railroad. The trackage between Chama and Durango was abandoned and rails were removed by 1971.
    DurangoTrainHighBridge2.jpg
  • Austin is the capital of Texas and the seat of Travis County. Located in Central Texas and the American Southwest, it is the 11th-largest city in the United States of America and the fourth-largest city in the state of Texas. It was the third-fastest-growing large city in the nation from 2000 to 2006. Austin is also the second largest state capital in the United States. Austin has a population of 842,592 (2012 estimate). The city is the cultural and economic center of the five-county Austin–Round Rock metropolitan area, which had an estimated population 1,834,303 (2012 U.S. Census). In the 1830s, pioneers began to settle the area in central Austin along the Colorado River. After Republic of Texas Vice President Mirabeau B. Lamar visited the area during a buffalo-hunting expedition between 1837 and 1838, he proposed that the republic's capital then located in Houston, Texas, be relocated to the area situated on the north bank of the Colorado River near the present-day Congress Avenue Bridge. In 1839, the site was officially chosen as the republic's new capital (the republic's seventh and final location) and was incorporated under the name Waterloo. Shortly thereafter, the name was changed to Austin in honor of Stephen F. Austin, the "Father of Texas" and the republic's first secretary of state. The city grew throughout the 19th century and became a center for government and education with the construction of the Texas State Capitol and the University of Texas at Austin. After a lull in growth from the Great Depression, Austin resumed its development into a major city and, by the 1980s, it emerged as a center for technology and business. A number of Fortune 500 companies have headquarters or regional offices in Austin including Advanced Micro Devices, Apple Inc., eBay, Google, IBM, Intel, Texas Instruments, 3M, and Whole Foods Market. Dell's worldwide headquarters is located in nearby Round Rock, a suburb of Austin.
    AustinNightSkyline5.jpg
  • Austin is the capital of Texas and the seat of Travis County. Located in Central Texas and the American Southwest, it is the 11th-largest city in the United States of America and the fourth-largest city in the state of Texas. It was the third-fastest-growing large city in the nation from 2000 to 2006. Austin is also the second largest state capital in the United States. Austin has a population of 842,592 (2012 estimate). The city is the cultural and economic center of the five-county Austin–Round Rock metropolitan area, which had an estimated population 1,834,303 (2012 U.S. Census). In the 1830s, pioneers began to settle the area in central Austin along the Colorado River. After Republic of Texas Vice President Mirabeau B. Lamar visited the area during a buffalo-hunting expedition between 1837 and 1838, he proposed that the republic's capital then located in Houston, Texas, be relocated to the area situated on the north bank of the Colorado River near the present-day Congress Avenue Bridge. In 1839, the site was officially chosen as the republic's new capital (the republic's seventh and final location) and was incorporated under the name Waterloo. Shortly thereafter, the name was changed to Austin in honor of Stephen F. Austin, the "Father of Texas" and the republic's first secretary of state. The city grew throughout the 19th century and became a center for government and education with the construction of the Texas State Capitol and the University of Texas at Austin. After a lull in growth from the Great Depression, Austin resumed its development into a major city and, by the 1980s, it emerged as a center for technology and business. A number of Fortune 500 companies have headquarters or regional offices in Austin including Advanced Micro Devices, Apple Inc., eBay, Google, IBM, Intel, Texas Instruments, 3M, and Whole Foods Market. Dell's worldwide headquarters is located in nearby Round Rock, a suburb of Austin.
    AustinNightSkyline4.jpg
  • The Strater Hotel in Durango, Colorado. The City of Durango is a Home Rule Municipality that is the county seat and the most populous city of La Plata County, Colorado, United States.[6] The United States Census Bureau reported a population of 16,887 in the 2010 census.
    DurangoStreet1.jpg
  • The Durango and Silverton Narrow Gauge Railroad (D&SNG) is a narrow gauge heritage railroad that operates 45 miles of 3 ft track between Durango and Silverton, in the US state of Colorado. The railway is a federally designated National Historic Landmark and is also designated by the American Society of Civil Engineers as a Historic Civil Engineering Landmark.<br />
The route was originally built between 1881 and 1882, by the Denver and Rio Grande Railway, in order to carry supplies and people to and silver and gold ore from mines in the San Juan Mountains. The line was an extension of the D&RG narrow gauge from Antonito, Colorado to Durango. The last train to operate into Durango from the east was on December 6, 1968. The States of New Mexico and Colorado purchased 64 miles of the line between Antonito and Chama, New Mexico in 1970 and operates today as the Cumbres and Toltec Scenic Railroad. The trackage between Chama and Durango was abandoned and rails were removed by 1971.
    DurangoStationNight1.jpg
  • The Durango and Silverton Narrow Gauge Railroad (D&SNG) is a narrow gauge heritage railroad that operates 45 miles of 3 ft track between Durango and Silverton, in the US state of Colorado. The railway is a federally designated National Historic Landmark and is also designated by the American Society of Civil Engineers as a Historic Civil Engineering Landmark.<br />
The route was originally built between 1881 and 1882, by the Denver and Rio Grande Railway, in order to carry supplies and people to and silver and gold ore from mines in the San Juan Mountains. The line was an extension of the D&RG narrow gauge from Antonito, Colorado to Durango. The last train to operate into Durango from the east was on December 6, 1968. The States of New Mexico and Colorado purchased 64 miles of the line between Antonito and Chama, New Mexico in 1970 and operates today as the Cumbres and Toltec Scenic Railroad. The trackage between Chama and Durango was abandoned and rails were removed by 1971.
    DurangoHighline2.jpg
  • The Durango and Silverton Narrow Gauge Railroad (D&SNG) is a narrow gauge heritage railroad that operates 45 miles of 3 ft track between Durango and Silverton, in the US state of Colorado. The railway is a federally designated National Historic Landmark and is also designated by the American Society of Civil Engineers as a Historic Civil Engineering Landmark.<br />
The route was originally built between 1881 and 1882, by the Denver and Rio Grande Railway, in order to carry supplies and people to and silver and gold ore from mines in the San Juan Mountains. The line was an extension of the D&RG narrow gauge from Antonito, Colorado to Durango. The last train to operate into Durango from the east was on December 6, 1968. The States of New Mexico and Colorado purchased 64 miles of the line between Antonito and Chama, New Mexico in 1970 and operates today as the Cumbres and Toltec Scenic Railroad. The trackage between Chama and Durango was abandoned and rails were removed by 1971.
    DurangoHighline4.jpg
  • The Durango and Silverton Narrow Gauge Railroad (D&SNG) is a narrow gauge heritage railroad that operates 45 miles of 3 ft track between Durango and Silverton, in the US state of Colorado. The railway is a federally designated National Historic Landmark and is also designated by the American Society of Civil Engineers as a Historic Civil Engineering Landmark.<br />
The route was originally built between 1881 and 1882, by the Denver and Rio Grande Railway, in order to carry supplies and people to and silver and gold ore from mines in the San Juan Mountains. The line was an extension of the D&RG narrow gauge from Antonito, Colorado to Durango. The last train to operate into Durango from the east was on December 6, 1968. The States of New Mexico and Colorado purchased 64 miles of the line between Antonito and Chama, New Mexico in 1970 and operates today as the Cumbres and Toltec Scenic Railroad. The trackage between Chama and Durango was abandoned and rails were removed by 1971.
    DurangoColoradoTrail1.jpg
  • The Durango and Silverton Narrow Gauge Railroad (D&SNG) is a narrow gauge heritage railroad that operates 45 miles of 3 ft track between Durango and Silverton, in the US state of Colorado. The railway is a federally designated National Historic Landmark and is also designated by the American Society of Civil Engineers as a Historic Civil Engineering Landmark.<br />
The route was originally built between 1881 and 1882, by the Denver and Rio Grande Railway, in order to carry supplies and people to and silver and gold ore from mines in the San Juan Mountains. The line was an extension of the D&RG narrow gauge from Antonito, Colorado to Durango. The last train to operate into Durango from the east was on December 6, 1968. The States of New Mexico and Colorado purchased 64 miles of the line between Antonito and Chama, New Mexico in 1970 and operates today as the Cumbres and Toltec Scenic Railroad. The trackage between Chama and Durango was abandoned and rails were removed by 1971.
    DurangoTrainHighBridge1.jpg
  • Sunset in the lush valley around the small town of Orfir in the Colorado San Juan mountains
    _D3_0440-HDR-Edit.jpg
  • Aspens on hillside in the San Juan mountains of Colorado with Silver Mountain peak in the background
    ColoradoSilverMountain.jpg
  • Aspen grove in the San Juan mountains of Colorado
    ColoradoAspenSky1.jpg
  • Aspens grove in the San Juan mountains of Colorado
    ColoradoOrfirAspens2.jpg
  • Aspens grove in the San Juan mountains of Colorado with the Ulysses Grant Peak looming above the trees
    ColoradoOrfirMountain1.jpg
  • Aspens on hillside in the San Juan mountains of Colorado with small river in foreground
    ColoradoAspensRiver2.jpg
  • Mesa Verde National Park is a National Park and World Heritage Site located in Montezuma County, Colorado. It protects some of the best preserved Ancestral Puebloan archaeological sites in the United States.<br />
<br />
Created by President Theodore Roosevelt in 1906, the park occupies 52,485 acres  near the Four Corners region of the American Southwest. With more than 4,300 sites, including 600 cliff dwellings, it is the largest archaeological preserve in the U.S. Mesa Verde (Spanish for "green table") is best known for structures such as Cliff Palace, thought to be the largest cliff dwelling in North America.
    MesaVerde1.jpg
  • Snowden Peak in Colorado's Rocky Mountains
    SnowdonPeak3.jpg
  • Snowden Peak in Colorado's Rocky Mountains
    SnowdonPeak2.jpg
  • Austin is the capital of Texas and the seat of Travis County. Located in Central Texas and the American Southwest, it is the 11th-largest city in the United States of America and the fourth-largest city in the state of Texas. It was the third-fastest-growing large city in the nation from 2000 to 2006. Austin is also the second largest state capital in the United States. Austin has a population of 842,592 (2012 estimate). The city is the cultural and economic center of the five-county Austin–Round Rock metropolitan area, which had an estimated population 1,834,303 (2012 U.S. Census). In the 1830s, pioneers began to settle the area in central Austin along the Colorado River. After Republic of Texas Vice President Mirabeau B. Lamar visited the area during a buffalo-hunting expedition between 1837 and 1838, he proposed that the republic's capital then located in Houston, Texas, be relocated to the area situated on the north bank of the Colorado River near the present-day Congress Avenue Bridge. In 1839, the site was officially chosen as the republic's new capital (the republic's seventh and final location) and was incorporated under the name Waterloo. Shortly thereafter, the name was changed to Austin in honor of Stephen F. Austin, the "Father of Texas" and the republic's first secretary of state. The city grew throughout the 19th century and became a center for government and education with the construction of the Texas State Capitol and the University of Texas at Austin. After a lull in growth from the Great Depression, Austin resumed its development into a major city and, by the 1980s, it emerged as a center for technology and business. A number of Fortune 500 companies have headquarters or regional offices in Austin including Advanced Micro Devices, Apple Inc., eBay, Google, IBM, Intel, Texas Instruments, 3M, and Whole Foods Market. Dell's worldwide headquarters is located in nearby Round Rock, a suburb of Austin.
    AustinSkyline1.jpg
  • Aspens on hillside in the San Juan mountains of Colorado with small river in foreground
    ColoradoAspensRiver2.jpg
  • Sunset in the lush valley around the small town of Orfir in the Colorado San Juan mountains
    ColoradoOrfirSunset1.jpg
  • Austin is the capital of Texas and the seat of Travis County. Located in Central Texas and the American Southwest, it is the 11th-largest city in the United States of America and the fourth-largest city in the state of Texas. It was the third-fastest-growing large city in the nation from 2000 to 2006. Austin is also the second largest state capital in the United States. Austin has a population of 842,592 (2012 estimate). The city is the cultural and economic center of the five-county Austin–Round Rock metropolitan area, which had an estimated population 1,834,303 (2012 U.S. Census). In the 1830s, pioneers began to settle the area in central Austin along the Colorado River. After Republic of Texas Vice President Mirabeau B. Lamar visited the area during a buffalo-hunting expedition between 1837 and 1838, he proposed that the republic's capital then located in Houston, Texas, be relocated to the area situated on the north bank of the Colorado River near the present-day Congress Avenue Bridge. In 1839, the site was officially chosen as the republic's new capital (the republic's seventh and final location) and was incorporated under the name Waterloo. Shortly thereafter, the name was changed to Austin in honor of Stephen F. Austin, the "Father of Texas" and the republic's first secretary of state. The city grew throughout the 19th century and became a center for government and education with the construction of the Texas State Capitol and the University of Texas at Austin. After a lull in growth from the Great Depression, Austin resumed its development into a major city and, by the 1980s, it emerged as a center for technology and business. A number of Fortune 500 companies have headquarters or regional offices in Austin including Advanced Micro Devices, Apple Inc., eBay, Google, IBM, Intel, Texas Instruments, 3M, and Whole Foods Market. Dell's worldwide headquarters is located in nearby Round Rock, a suburb of Austin.
    AustinSkyline1.jpg
  • Aspen grove in the San Juan mountains of Colorado
    ColoradoAspenSky2.jpg
  • Aspen grove in the San Juan mountains of Colorado
    ColoradoAspenSky3.jpg
  • Aspens grove in the San Juan mountains of Colorado
    ColoradoOrfirAspens1.jpg
  • Aspens grove in the San Juan mountains of Colorado
    ColoradoOrfirAspens4.jpg
  • Aspens on hillside in the San Juan mountains of Colorado with small river in foreground
    ColoradoAspensRiver1.jpg
  • Aspens on hillside in the San Juan mountains of Colorado
    ColoradoAspens2.jpg
  • Aspens on hillside in the San Juan mountains of Colorado
    ColoradoAspens1.jpg
  • Mesa Verde National Park is a National Park and World Heritage Site located in Montezuma County, Colorado. It protects some of the best preserved Ancestral Puebloan archaeological sites in the United States.<br />
<br />
Created by President Theodore Roosevelt in 1906, the park occupies 52,485 acres  near the Four Corners region of the American Southwest. With more than 4,300 sites, including 600 cliff dwellings, it is the largest archaeological preserve in the U.S. Mesa Verde (Spanish for "green table") is best known for structures such as Cliff Palace, thought to be the largest cliff dwelling in North America.
    MesaVerde2.jpg
  • Snowden Peak in Colorado's Rocky Mountains
    SnowdonPeak4.jpg
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