Inge Johnsson Photography

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  • Weathered old barn in the Palouse area of eastern Washington
    PalouseBarn3-2.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
  • 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
  • Rock formations in the South Coyote Buttes unit of the Vermillion Cliffs National Monument
    SouthCoyoteButtesGargoyle.jpg
  • Rock formations in the South Coyote Buttes unit of the Vermillion Cliffs National Monument
    SouthCoyoteButtesSunrise1.jpg
  • Rock formations in the North Coyote Buttes unit of the Vermillion Cliffs National Monument
    SecondWave6.jpg
  • Rock formations in the North Coyote Buttes unit of the Vermillion Cliffs National Monument
    TopRockHamburger1.jpg
  • The Vermilion Cliffs are the second "step" up in the five-step Grand Staircase of the Colorado Plateau. Reddish or vermilion-colored cliffs are found along U.S. Highway 89 and U.S. Highway 89A near Kanab, Utah (and near Navajo Bridge in Arizona). 112,500 acres (45,500 ha) of the region were designated as the Paria Canyon-Vermilion Cliffs Wilderness in 1984, and an even greater area was proclaimed Vermilion Cliffs National Monument in 2000. Famous locations in the cliff area include Lee's Ferry, Glen Canyon (a national recreational area), The Wave, Coyote Buttes, and others.
    ClingingToEarth.jpg
  • Abstract patterns in Lower Antelope Canyon, Page, Arizona
    AntelopeAbstractCurve1.jpg
  • The Colorado River meandering through the Marble Canyon section of Grand Canyon National Park
    GrandCanyonMarbleCanyon2.jpg
  • Ancient Anaszi ruins high above the Colorado River in the Marble Canyon section of Grand Canyon National Park
    NankoweapRuins3.jpg
  • The Wahweap Hoodoos, a congregation of impossibly white rock spires topped with reddish-brown capstones, are quickly becoming one of Grand Staircase-Escalante National Monument’s most recognized formations. The hoodoos are generally described as three separate groupings—the White Hoodoo, Hoodoo Central, and the Towers of Silence.
    WahweapSingleHoodoo2.jpg
  • The Wahweap Hoodoos, a congregation of impossibly white rock spires topped with reddish-brown capstones, are quickly becoming one of Grand Staircase-Escalante National Monument’s most recognized formations. The hoodoos are generally described as three separate groupings—the White Hoodoo, Hoodoo Central, and the Towers of Silence.
    WahweapSky3.jpg
  • Ray of light coming down from the top of the narrow Upper Antelope Canyon
    AntelopeCanyonBeamOfLight.jpg
  • Ray of light coming down through a natural "keyhole" in the Lower Antelope Canyon
    AntelopeKeyhole-New.jpg
  • Classic view of the Mittens and Merrick Butte in Monument Valley, AZ
    JohnFordPoint.jpg
  • Typical Southwestern adobe home in Rancho de Taos, New Mexico
    RanchoDeTaosHome2.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
  • The Colorado River meandering through the Marble Canyon section of Grand Canyon National Park
    GrandCanyonMarbleCanyon3.jpg
  • Ancient Anaszi ruins high above the Colorado River in the Marble Canyon section of Grand Canyon National Park
    NankoweapRuins3.jpg
  • Colorado River at North Canyon
    GrandCanyonNorthCanyon2.jpg
  • Vespa on side street in Arles, Provence, France
    ArlesStreet2.jpg
  • Mystery Valley in the Monument Valley Navajo tribal park.  Monument Valley is a region of the Colorado Plateau characterized by a cluster of vast sandstone buttes, the largest reaching 1,000 ft above the valley floor. It is located on the southern border of Utah with northern Arizona near the Four Corners area.Mystery Valley in the Monument Valley Navajo tribal park.  Monument Valley is a region of the Colorado Plateau characterized by a cluster of vast sandstone buttes, the largest reaching 1,000 ft above the valley floor. It is located on the southern border of Utah with northern Arizona near the Four Corners area.
    MysteryValleyRock1.jpg
  • First light over Monument Valley from atop Hunts Mesa
    HuntsMesaPano1.jpg
  • Dead tree on Hunt's Mesa in Monument Valley, AZ
    MonumentValleyHuntsMesaDeadTree1.jpg
  • Sand Springs in Monument Valley, shadow of nearby tree
    MonumentValleySandSprings1.jpg
  • Grille on a vintage John Deere tractor on ranch in eastern Wyoming
    JDtractorGrille3.jpg
  • Door in Arles, Provence, France
    ArlesDoor1.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
  • Rock formations in the South Coyote Buttes unit of the Vermillion Cliffs National Monument
    SouthCoyoteButtesSunset2.jpg
  • Rock formations in the South Coyote Buttes unit of the Vermillion Cliffs National Monument
    SouthCoyoteButtesFins3.jpg
  • Rock formations in the South Coyote Buttes unit of the Vermillion Cliffs National Monument
    SouthCoyoteButtesFlakes.jpg
  • Rock formations in the North Coyote Buttes unit of the Vermillion Cliffs National Monument
    SecondWave3.jpg
  • Striated sandstone at South Coyote Buttes, Arizona
    RainbowRocksStriations5.jpg
  • Slickrock ridges at South Coyote Buttes, Arizona
    RainbowRocksStriations4.jpg
  • Lower Antelope Canyon "tunnel"
    AntelopeOpenings.jpg
  • San Juan River at Mexican Hat, Utah
    MexicanHatSanJuanRiver1.jpg
  • The Wahweap Hoodoos, a congregation of impossibly white rock spires topped with reddish-brown capstones, are quickly becoming one of Grand Staircase-Escalante National Monument’s most recognized formations. The hoodoos are generally described as three separate groupings—the White Hoodoo, Hoodoo Central, and the Towers of Silence.
    WahweapSingleHoodoo1.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
  • Horseshoe Bend on the Colorado River near Page, Arizona
    HorseshoeBendLeft.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
  • Sandstone hoodoos in the Glen Canyon Nation Recreation Area
    StudhorseHoodoosSunset2.jpg
  • Slickrock ridges at White Pocket
    WhitePocketSunrise1.jpg
  • Rock formations in the White Pocket unit of the Vermillion Cliffs National Monument
    WhitePocketLoneJuniper.jpg
  • Rock formations in the South Coyote Buttes unit of the Vermillion Cliffs National Monument
    SouthCoyoteButtesSunset2.jpg
  • Rock formations in the South Coyote Buttes unit of the Vermillion Cliffs National Monument
    SouthCoyoteButtesDeadJuniper1.jpg
  • Dead juniper in the South Coyote Buttes unit of the Vermillion Cliffs National Monument
    SouthCoyoteButtesDeadBranch.jpg
  • Rock formations in the South Coyote Buttes unit of the Vermillion Cliffs National Monument
    SouthCoyoteButtesSnail.jpg
  • Rock formations in the South Coyote Buttes unit of the Vermillion Cliffs National Monument
    SouthCoyoteButtesFins3.jpg
  • Rock formations in the South Coyote Buttes unit of the Vermillion Cliffs National Monument
    SouthCoyoteButtesFinRoom1.jpg
  • Rock formations in the South Coyote Buttes unit of the Vermillion Cliffs National Monument
    SouthCoyoteButtesLongFin.jpg
  • Rock formations in the South Coyote Buttes unit of the Vermillion Cliffs National Monument
    SouthCoyoteButtesFlakes.jpg
  • Sandstone hoodoos in the Glen Canyon Nation Recreation Area
    StudhorseHoodoosSunrise1.jpg
  • Juniper tree and rock formations in the North Coyote Buttes unit of the Vermillion Cliffs National Monument
    NorthCoyoteButtesJuniper.jpg
  • Rock formations in the North Coyote Buttes unit of the Vermillion Cliffs National Monument
    SecondWave3.jpg
  • Rocks in the North Coyote Buttes unit of the Vermillion Cliffs National Monument
    BoneYard3.jpg
  • Rock formations in the North Coyote Buttes unit of the Vermillion Cliffs National Monument
    TopArch1.jpg
  • Rock formations in the North Coyote Buttes unit of the Vermillion Cliffs National Monument
    WaveBowl1.jpg
  • Rock formations in the North Coyote Buttes unit of the Vermillion Cliffs National Monument
    BoneYard1.jpg
  • Sandstone formations in bowl in the interior of Rainbow Rocks
    SandstoneAnvils.jpg
  • Slickrock ridges at South Coyote Buttes, Arizona
    RainbowRocksStriations4.jpg
  • Swirl in the sandstone at White Pocket, AZ
    WhitePocketsSwirl1.jpg
  • Canyon wall in Buckskin Gulch, Paria Canyon Wilderness. The Buckskin Gulch, a canyon in southern Utah, is one of the main tributaries of the Paria River, which is itself a minor tributary of the Colorado River. It is the longest and deepest slot canyon in the southwest United States and may very well be the longest in the world. As such it is one of the premier destinations for slot canyon hikers, and receives a high amount of foot traffic.<br />
At over 13 miles (21 km) in length it is often visited in conjunction with the longer Paria Canyon, although some prefer to make a long day trip out of the hike. With a distance of 20 miles (32 km), hiking this canyon in one day is possible. Wire Pass, a short tributary to the Buckskin, is an ideal alternative for a short day hike that still takes hikers through the narrow, curving features that are the hallmark of slot canyons
    BuckskinRoughSea.jpg
  • Mystery Valley in the Monument Valley Navajo tribal park.  Monument Valley is a region of the Colorado Plateau characterized by a cluster of vast sandstone buttes, the largest reaching 1,000 ft above the valley floor. It is located on the southern border of Utah with northern Arizona near the Four Corners area.
    MysteryValleyPancake1.jpg
  • Sunrise at the far end of Hunt's Mesa above Monument Valley, Arizona
    MonumentValleyFirstRays1.jpg
  • First light at Yei-bi-Chai rocks in Monument Valley
    MonumentValleyYeibicheiSunrise2.jpg
  • First light at Yei-bi-Chai rocks in Monument Valley
    MonumentValleyYeibicheiSunrise3.jpg
  • View of the canyon walls ofthe Grand Canyon seen from a raft on the Colorado River
    GrandCanyonRiver1.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
  • Havasu Creek is a side stream to the Colorado River in the interior of the Grand Canyon
    GrandCanyonHavasuCreekPool1.jpg
  • Slot canyon in Deer Creek patio.  Deer Creek is a side stream to the Colorado River in the interior of the Grand Canyon.
    GrandCanyonDeerCreekSlot1.jpg
  • Slot canyon in Deer Creek patio.  Deer Creek is a side stream to the Colorado River in the interior of the Grand Canyon.
    GrandCanyonDeerCreekSlot3.jpg
  • Blacktail Canyon, a side canyon to the Grand Canyon.
    GrandCanyonBlacktail2.jpg
  • Elves Chasm waterfall in the interior of the Grand Canyon.
    GrandCanyonElvesChasm1.jpg
  • Small waterfall on Clear Creek, a side stream to the Colorado River in the interior of the Grand Canyon
    GrandCanyonClearCreek1.jpg
  • Small waterfall on Clear Creek, a side stream to the Colorado River in the interior of the Grand Canyon
    GrandCanyonClearCreek2.jpg
  • The Colorado River meandering through the Marble Canyon section of Grand Canyon National Park
    GrandCanyonMarbleCanyon3.jpg
  • The Colorado River meandering through the Marble Canyon section of Grand Canyon National Park
    GrandCanyonMarbleCanyon1.jpg
  • Colorado River at North Canyon
    GrandCanyonNorthCanyon1.jpg
  • The Wahweap Hoodoos, a congregation of impossibly white rock spires topped with reddish-brown capstones, are quickly becoming one of Grand Staircase-Escalante National Monument’s most recognized formations. The hoodoos are generally described as three separate groupings—the White Hoodoo, Hoodoo Central, and the Towers of Silence.
    WahweapHoodoos2.jpg
  • The Wahweap Hoodoos, a congregation of impossibly white rock spires topped with reddish-brown capstones, are quickly becoming one of Grand Staircase-Escalante National Monument’s most recognized formations. The hoodoos are generally described as three separate groupings—the White Hoodoo, Hoodoo Central, and the Towers of Silence.
    WahweapSingleHoodoo1.jpg
  • The Wahweap Hoodoos, a congregation of impossibly white rock spires topped with reddish-brown capstones, are quickly becoming one of Grand Staircase-Escalante National Monument’s most recognized formations. The hoodoos are generally described as three separate groupings—the White Hoodoo, Hoodoo Central, and the Towers of Silence.
    WahweapSky1.jpg
  • Sandstone patterns in Lower Antelope Canyon near Page, Arizona
    AntelopeRidge2a.jpg
  • TurtleBackRocks.jpg
  • Entrance to Upper Antelope Canyon near Page, Arizona
    AntelopeEntranceDrapery.jpg
  • Sandstone patterns in Lower Antelope Canyon near Page, Arizona
    AntelopeRidge1.jpg
  • Sandstone patterns in Lower Antelope Canyon near Page, Arizona
    AntelopeSandstonePatterns2.jpg
  • Swirls in sandstone walls
    AntelopeSandstoneWavesVetical.jpg
  • Monument Valley is a region of the Colorado Plateau characterized by a cluster of vast sandstone buttes, the largest reaching 1,000 ft above the valley floor. It is located on the Arizona–Utah border, near the Four Corners area. The valley lies within the range of the Navajo Nation Reservation and is accessible from U.S. Highway 163.<br />
<br />
Monument Valley has been featured in many forms of media since the 1930s. Director John Ford used the location for a number of his best-known films and thus, in the words of critic Keith Phipps, "its five square miles have defined what decades of moviegoers think of when they imagine the American West
    MonumentVallleyWheel1.jpg
  • Monument Valley is a region of the Colorado Plateau characterized by a cluster of vast sandstone buttes, the largest reaching 1,000 ft above the valley floor. It is located on the Arizona–Utah border, near the Four Corners area. The valley lies within the range of the Navajo Nation Reservation and is accessible from U.S. Highway 163.<br />
<br />
Monument Valley has been featured in many forms of media since the 1930s. Director John Ford used the location for a number of his best-known films and thus, in the words of critic Keith Phipps, "its five square miles have defined what decades of moviegoers think of when they imagine the American West
    MonumentValleyStagecoach1.jpg
  • Santa Fe is the capital of the state of New Mexico. This area was occupied for at least several thousand years by indigenous peoples who built villages several hundred years ago on the current site of the city. It was known by the Tewa inhabitants as Ogha Po'oge ("White Shell Water Place"). The city of Santa Fe, founded by Spanish colonists in 1610, is the oldest city in the state and the oldest state capital city in the United States. Santa Fe (meaning "holy faith" in Spanish) had a population of 69,204 in 2012.  After the mainline of the railroad bypassed Santa Fe, it lost population. However artists and writers, as well as retirees, were attracted to the cultural richness of the area, the beauty of the landscapes, and its dry climate. Local leaders began promoting the city as a tourist attraction. The city sponsored architectural restoration projects and erected new buildings according to traditional techniques and styles, thus creating the Santa Fe Style. Edgar L. Hewett, founder and first director of the School of American Research and the Museum of New Mexico in Santa Fe, was a leading promoter. He began the Santa Fe Fiesta in 1919 and the Southwest Indian Fair in 1922 (now known as the Indian Market).
    SantaFeClouds1.jpg
  • Santa Fe is the capital of the state of New Mexico. This area was occupied for at least several thousand years by indigenous peoples who built villages several hundred years ago on the current site of the city. It was known by the Tewa inhabitants as Ogha Po'oge ("White Shell Water Place"). The city of Santa Fe, founded by Spanish colonists in 1610, is the oldest city in the state and the oldest state capital city in the United States. Santa Fe (meaning "holy faith" in Spanish) had a population of 69,204 in 2012.  After the mainline of the railroad bypassed Santa Fe, it lost population. However artists and writers, as well as retirees, were attracted to the cultural richness of the area, the beauty of the landscapes, and its dry climate. Local leaders began promoting the city as a tourist attraction. The city sponsored architectural restoration projects and erected new buildings according to traditional techniques and styles, thus creating the Santa Fe Style. Edgar L. Hewett, founder and first director of the School of American Research and the Museum of New Mexico in Santa Fe, was a leading promoter. He began the Santa Fe Fiesta in 1919 and the Southwest Indian Fair in 1922 (now known as the Indian Market).
    SantaFe304Door3.jpg
  • Santa Fe is the capital of the state of New Mexico. This area was occupied for at least several thousand years by indigenous peoples who built villages several hundred years ago on the current site of the city. It was known by the Tewa inhabitants as Ogha Po'oge ("White Shell Water Place"). The city of Santa Fe, founded by Spanish colonists in 1610, is the oldest city in the state and the oldest state capital city in the United States. Santa Fe (meaning "holy faith" in Spanish) had a population of 69,204 in 2012.  After the mainline of the railroad bypassed Santa Fe, it lost population. However artists and writers, as well as retirees, were attracted to the cultural richness of the area, the beauty of the landscapes, and its dry climate. Local leaders began promoting the city as a tourist attraction. The city sponsored architectural restoration projects and erected new buildings according to traditional techniques and styles, thus creating the Santa Fe Style. Edgar L. Hewett, founder and first director of the School of American Research and the Museum of New Mexico in Santa Fe, was a leading promoter. He began the Santa Fe Fiesta in 1919 and the Southwest Indian Fair in 1922 (now known as the Indian Market).
    SantaFeClouds1.jpg
  • Santa Fe is the capital of the state of New Mexico. This area was occupied for at least several thousand years by indigenous peoples who built villages several hundred years ago on the current site of the city. It was known by the Tewa inhabitants as Ogha Po'oge ("White Shell Water Place"). The city of Santa Fe, founded by Spanish colonists in 1610, is the oldest city in the state and the oldest state capital city in the United States. Santa Fe (meaning "holy faith" in Spanish) had a population of 69,204 in 2012.  After the mainline of the railroad bypassed Santa Fe, it lost population. However artists and writers, as well as retirees, were attracted to the cultural richness of the area, the beauty of the landscapes, and its dry climate. Local leaders began promoting the city as a tourist attraction. The city sponsored architectural restoration projects and erected new buildings according to traditional techniques and styles, thus creating the Santa Fe Style. Edgar L. Hewett, founder and first director of the School of American Research and the Museum of New Mexico in Santa Fe, was a leading promoter. He began the Santa Fe Fiesta in 1919 and the Southwest Indian Fair in 1922 (now known as the Indian Market).
    SantaFe304Door2.jpg
  • Santa Fe is the capital of the state of New Mexico. This area was occupied for at least several thousand years by indigenous peoples who built villages several hundred years ago on the current site of the city. It was known by the Tewa inhabitants as Ogha Po'oge ("White Shell Water Place"). The city of Santa Fe, founded by Spanish colonists in 1610, is the oldest city in the state and the oldest state capital city in the United States. Santa Fe (meaning "holy faith" in Spanish) had a population of 69,204 in 2012.  After the mainline of the railroad bypassed Santa Fe, it lost population. However artists and writers, as well as retirees, were attracted to the cultural richness of the area, the beauty of the landscapes, and its dry climate. Local leaders began promoting the city as a tourist attraction. The city sponsored architectural restoration projects and erected new buildings according to traditional techniques and styles, thus creating the Santa Fe Style. Edgar L. Hewett, founder and first director of the School of American Research and the Museum of New Mexico in Santa Fe, was a leading promoter. He began the Santa Fe Fiesta in 1919 and the Southwest Indian Fair in 1922 (now known as the Indian Market).
    SantaFeHydrant1.jpg
  • Santa Fe is the capital of the state of New Mexico. This area was occupied for at least several thousand years by indigenous peoples who built villages several hundred years ago on the current site of the city. It was known by the Tewa inhabitants as Ogha Po'oge ("White Shell Water Place"). The city of Santa Fe, founded by Spanish colonists in 1610, is the oldest city in the state and the oldest state capital city in the United States. Santa Fe (meaning "holy faith" in Spanish) had a population of 69,204 in 2012.  After the mainline of the railroad bypassed Santa Fe, it lost population. However artists and writers, as well as retirees, were attracted to the cultural richness of the area, the beauty of the landscapes, and its dry climate. Local leaders began promoting the city as a tourist attraction. The city sponsored architectural restoration projects and erected new buildings according to traditional techniques and styles, thus creating the Santa Fe Style. Edgar L. Hewett, founder and first director of the School of American Research and the Museum of New Mexico in Santa Fe, was a leading promoter. He began the Santa Fe Fiesta in 1919 and the Southwest Indian Fair in 1922 (now known as the Indian Market).
    SantaFeRedDoor1.jpg
  • Santa Fe is the capital of the state of New Mexico. This area was occupied for at least several thousand years by indigenous peoples who built villages several hundred years ago on the current site of the city. It was known by the Tewa inhabitants as Ogha Po'oge ("White Shell Water Place"). The city of Santa Fe, founded by Spanish colonists in 1610, is the oldest city in the state and the oldest state capital city in the United States. Santa Fe (meaning "holy faith" in Spanish) had a population of 69,204 in 2012.  After the mainline of the railroad bypassed Santa Fe, it lost population. However artists and writers, as well as retirees, were attracted to the cultural richness of the area, the beauty of the landscapes, and its dry climate. Local leaders began promoting the city as a tourist attraction. The city sponsored architectural restoration projects and erected new buildings according to traditional techniques and styles, thus creating the Santa Fe Style. Edgar L. Hewett, founder and first director of the School of American Research and the Museum of New Mexico in Santa Fe, was a leading promoter. He began the Santa Fe Fiesta in 1919 and the Southwest Indian Fair in 1922 (now known as the Indian Market).
    SantaFeTurqioseBench1.jpg
  • Santa Fe is the capital of the state of New Mexico. This area was occupied for at least several thousand years by indigenous peoples who built villages several hundred years ago on the current site of the city. It was known by the Tewa inhabitants as Ogha Po'oge ("White Shell Water Place"). The city of Santa Fe, founded by Spanish colonists in 1610, is the oldest city in the state and the oldest state capital city in the United States. Santa Fe (meaning "holy faith" in Spanish) had a population of 69,204 in 2012.  After the mainline of the railroad bypassed Santa Fe, it lost population. However artists and writers, as well as retirees, were attracted to the cultural richness of the area, the beauty of the landscapes, and its dry climate. Local leaders began promoting the city as a tourist attraction. The city sponsored architectural restoration projects and erected new buildings according to traditional techniques and styles, thus creating the Santa Fe Style. Edgar L. Hewett, founder and first director of the School of American Research and the Museum of New Mexico in Santa Fe, was a leading promoter. He began the Santa Fe Fiesta in 1919 and the Southwest Indian Fair in 1922 (now known as the Indian Market).
    SantaFe304Door1.jpg
  • Santa Fe is the capital of the state of New Mexico. This area was occupied for at least several thousand years by indigenous peoples who built villages several hundred years ago on the current site of the city. It was known by the Tewa inhabitants as Ogha Po'oge ("White Shell Water Place"). The city of Santa Fe, founded by Spanish colonists in 1610, is the oldest city in the state and the oldest state capital city in the United States. Santa Fe (meaning "holy faith" in Spanish) had a population of 69,204 in 2012.  After the mainline of the railroad bypassed Santa Fe, it lost population. However artists and writers, as well as retirees, were attracted to the cultural richness of the area, the beauty of the landscapes, and its dry climate. Local leaders began promoting the city as a tourist attraction. The city sponsored architectural restoration projects and erected new buildings according to traditional techniques and styles, thus creating the Santa Fe Style. Edgar L. Hewett, founder and first director of the School of American Research and the Museum of New Mexico in Santa Fe, was a leading promoter. He began the Santa Fe Fiesta in 1919 and the Southwest Indian Fair in 1922 (now known as the Indian Market).
    SantaFe304Door2.jpg
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