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  • Ófærufoss is a waterfall situated in the Eldgjá chasm in central Iceland. Until the early 1990s a natural bridge spanned the falls, but it collapsed from natural causes.
    Ofaerufoss1.jpg
  • Glacier National Park is a national park located in the U.S. state of Montana, on the Canada–United States border with the Canadian provinces of Alberta and British Columbia. The park encompasses over 1 million acres and includes parts of two mountain ranges (sub-ranges of the Rocky Mountains), over 130 named lakes, more than 1,000 different species of plants, and hundreds of species of animals. This vast pristine ecosystem is the centerpiece of what has been referred to as the "Crown of the Continent Ecosystem", a region of protected land encompassing 16,000 square miles.<br />
<br />
The region that became Glacier National Park was first inhabited by Native Americans. Upon the arrival of European explorers, it was dominated by the Blackfeet in the east and the Flathead in the western regions. Soon after the establishment of the park on May 11, 1910, a number of hotels and chalets were constructed by the Great Northern Railway. These historic hotels and chalets are listed as National Historic Landmarks and a total of 350 locations are on the National Register of Historic Places. By 1932 work was completed on the Going-to-the-Sun Road, later designated a National Historic Civil Engineering Landmark, which provided greater accessibility for automobiles into the heart of the park.<br />
<br />
The mountains of Glacier National Park began forming 170 million years ago when ancient rocks were forced eastward up and over much younger rock strata. Known as the Lewis Overthrust, these sedimentary rocks are considered to have some of the finest fossilized examples of extremely early life found anywhere on Earth. The current shapes of the Lewis and Livingston mountain ranges and positioning and size of the lakes show the telltale evidence of massive glacial action, which carved U-shaped valleys and left behind moraines which impounded water, creating lakes. Of the estimated 150 glaciers which existed in the park in the mid-19th century, only 25 active glaciers remained by 2010. Scientists studyin
    GlacierLoganPassSunset2.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
  • Fjaðrárgljúfur is a canyon in south east Iceland which is up to 100 m deep and about 2 kilometers long, with the Fjaðrá river flowing through it .The canyon has steep walls and winding water.
    Fjadrargljufur8.jpg
  • Fjaðrárgljúfur is a canyon in south east Iceland which is up to 100 m deep and about 2 kilometers long, with the Fjaðrá river flowing through it .The canyon has steep walls and winding water.
    Fjadrargljufur2.jpg
  • Glacier National Park is a national park located in the U.S. state of Montana, on the Canada–United States border with the Canadian provinces of Alberta and British Columbia. The park encompasses over 1 million acres and includes parts of two mountain ranges (sub-ranges of the Rocky Mountains), over 130 named lakes, more than 1,000 different species of plants, and hundreds of species of animals. This vast pristine ecosystem is the centerpiece of what has been referred to as the "Crown of the Continent Ecosystem", a region of protected land encompassing 16,000 square miles.<br />
<br />
The region that became Glacier National Park was first inhabited by Native Americans. Upon the arrival of European explorers, it was dominated by the Blackfeet in the east and the Flathead in the western regions. Soon after the establishment of the park on May 11, 1910, a number of hotels and chalets were constructed by the Great Northern Railway. These historic hotels and chalets are listed as National Historic Landmarks and a total of 350 locations are on the National Register of Historic Places. By 1932 work was completed on the Going-to-the-Sun Road, later designated a National Historic Civil Engineering Landmark, which provided greater accessibility for automobiles into the heart of the park.<br />
<br />
The mountains of Glacier National Park began forming 170 million years ago when ancient rocks were forced eastward up and over much younger rock strata. Known as the Lewis Overthrust, these sedimentary rocks are considered to have some of the finest fossilized examples of extremely early life found anywhere on Earth. The current shapes of the Lewis and Livingston mountain ranges and positioning and size of the lakes show the telltale evidence of massive glacial action, which carved U-shaped valleys and left behind moraines which impounded water, creating lakes. Of the estimated 150 glaciers which existed in the park in the mid-19th century, only 25 active glaciers remained by 2010. Scientists studyin
    GlacierLoganPassSunset2.jpg
  • The Empire State Building is a 102-story landmark Art Deco skyscraper in New York City, United States, at the intersection of Fifth Avenue and West 34th Street. It is 1,250 ft (381 meters) tall.[6] Its name is derived from the nickname for New York, the Empire State. It stood as the world's tallest building for more than 40 years, from its completion in 1931 until construction of the World Trade Center's North Tower was completed in 1972. Following the destruction of the World Trade Center in 2001, the Empire State Building once again became the tallest building in New York City.
    NYCEmpireState12.jpg
  • The Empire State Building is a 102-story landmark Art Deco skyscraper in New York City, United States, at the intersection of Fifth Avenue and West 34th Street. It is 1,250 ft (381 meters) tall.[6] Its name is derived from the nickname for New York, the Empire State. It stood as the world's tallest building for more than 40 years, from its completion in 1931 until construction of the World Trade Center's North Tower was completed in 1972. Following the destruction of the World Trade Center in 2001, the Empire State Building once again became the tallest building in New York City.
    NYCEmpireState9.jpg
  • The Empire State Building is a 102-story landmark Art Deco skyscraper in New York City, United States, at the intersection of Fifth Avenue and West 34th Street. It is 1,250 ft (381 meters) tall.[6] Its name is derived from the nickname for New York, the Empire State. It stood as the world's tallest building for more than 40 years, from its completion in 1931 until construction of the World Trade Center's North Tower was completed in 1972. Following the destruction of the World Trade Center in 2001, the Empire State Building once again became the tallest building in New York City.
    NYC_HudsonRiver1.jpg
  • Manhattan is the most densely populated of the five boroughs of New York City. The borough is coterminous with New York County, founded on November 1, 1683 as an original county of the U.S. state of New York. The borough consists mostly of Manhattan Island, bounded by the East, Hudson, and Harlem Rivers, but also includes several small adjacent islands, as well as Marble Hill, a small neighborhood on the U.S. mainland.
    NYCTopOfTheRock6.jpg
  • View from Torre LatinoAmericana. Mexico City is the densely populated, high-altitude capital of Mexico. It's known for its Templo Mayor (a 13th-century Aztec temple), the baroque Catedral Metropolitana of the Spanish conquistadors and the Palacio Nacional, which houses historic murals by Diego Rivera. All of this resides in and around the Plaza de la Constitución, the massive main square also known as the Zócalo.
    MexicoCity3.jpg
  • The National Museum of Anthropology (Spanish: Museo Nacional de Antropología, MNA) is a national museum of Mexico. It is the largest and most visited museum in Mexico. Located in the area between Paseo de la Reforma and Mahatma Gandhi Street within Chapultepec Park in Mexico City, the museum contains significant archaeological and anthropological artifacts from the Mexico's pre-Columbian heritage, such as the Stone of the Sun (or the Aztec calendar stone) and the 16th-century Aztec Xochipilli statue. Designed in 1964 by Pedro Ramírez Vázquez, Jorge Campuzano, and Rafael Mijares Alcérreca, the monumental building contains exhibition halls surrounding a courtyard with a huge pond and a vast square concrete umbrella supported by a single slender pillar (known as "el paraguas", Spanish for "the umbrella"). The halls are ringed by gardens, many of which contain outdoor exhibits. The museum has 23 rooms for exhibits and covers an area of 79,700 square meters (almost 8 hectares) or 857,890 square feet (almost 20 acres).
    Teotihuacan1.jpg
  • Glacier National Park is a national park located in the U.S. state of Montana, on the Canada–United States border with the Canadian provinces of Alberta and British Columbia. The park encompasses over 1 million acres and includes parts of two mountain ranges (sub-ranges of the Rocky Mountains), over 130 named lakes, more than 1,000 different species of plants, and hundreds of species of animals. This vast pristine ecosystem is the centerpiece of what has been referred to as the "Crown of the Continent Ecosystem", a region of protected land encompassing 16,000 square miles.<br />
<br />
The region that became Glacier National Park was first inhabited by Native Americans. Upon the arrival of European explorers, it was dominated by the Blackfeet in the east and the Flathead in the western regions. Soon after the establishment of the park on May 11, 1910, a number of hotels and chalets were constructed by the Great Northern Railway. These historic hotels and chalets are listed as National Historic Landmarks and a total of 350 locations are on the National Register of Historic Places. By 1932 work was completed on the Going-to-the-Sun Road, later designated a National Historic Civil Engineering Landmark, which provided greater accessibility for automobiles into the heart of the park.<br />
<br />
The mountains of Glacier National Park began forming 170 million years ago when ancient rocks were forced eastward up and over much younger rock strata. Known as the Lewis Overthrust, these sedimentary rocks are considered to have some of the finest fossilized examples of extremely early life found anywhere on Earth. The current shapes of the Lewis and Livingston mountain ranges and positioning and size of the lakes show the telltale evidence of massive glacial action, which carved U-shaped valleys and left behind moraines which impounded water, creating lakes. Of the estimated 150 glaciers which existed in the park in the mid-19th century, only 25 active glaciers remained by 2010. Scientists studyin
    GlacierLoganPassStorm1.jpg
  • Ófærufoss is a waterfall situated in the Eldgjá chasm in central Iceland. Until the early 1990s a natural bridge spanned the falls, but it collapsed from natural causes.
    Ofaerufoss1.jpg
  • Death Valley is a desert located in Eastern California. Situated within the Mojave Desert, it features the lowest, driest, and hottest locations in North America.
    DeathValleyDuneAndSky2-LAB.jpg
  • Ófærufoss is a waterfall situated in the Eldgjá chasm in central Iceland. Until the early 1990s a natural bridge spanned the falls, but it collapsed from natural causes.
    Ofaerufoss2.jpg
  • Fjaðrárgljúfur is a canyon in south east Iceland which is up to 100 m deep and about 2 kilometers long, with the Fjaðrá river flowing through it .The canyon has steep walls and winding water.
    Fjadrargljufur6.jpg
  • Fjaðrárgljúfur is a canyon in south east Iceland which is up to 100 m deep and about 2 kilometers long, with the Fjaðrá river flowing through it .The canyon has steep walls and winding water.
    Fjadrargljufur5.jpg
  • Fjaðrárgljúfur is a canyon in south east Iceland which is up to 100 m deep and about 2 kilometers long, with the Fjaðrá river flowing through it .The canyon has steep walls and winding water.
    _A1A6410-HDR.jpg
  • Fjaðrárgljúfur is a canyon in south east Iceland which is up to 100 m deep and about 2 kilometers long, with the Fjaðrá river flowing through it .The canyon has steep walls and winding water.
    _A1A6402-HDR.jpg
  • Ófærufoss is a waterfall situated in the Eldgjá chasm in central Iceland. Until the early 1990s a natural bridge spanned the falls, but it collapsed from natural causes.
    Ofaerufoss1.jpg
  • Fjaðrárgljúfur is a canyon in south east Iceland which is up to 100 m deep and about 2 kilometers long, with the Fjaðrá river flowing through it .The canyon has steep walls and winding water.
    Fjadrargljufur1.jpg
  • Fort Griffin State Historic Site was a Cavalry fort established 29 July 1867 by four companies of the Sixth Cavalry under the command of Lt. Col. S.D. Sturgis, in the northern part of West Texas, specifically northwestern Shackelford County, to give settlers protection from early Comanche and Kiowa raids. Originally called Camp Wilson, it was finally named for Charles Griffin, a former Civil War Union general who had commanded the Department of Texas during the early years of Reconstruction.<br />
<br />
Other forts in the frontier fort system were Forts Richardson, Concho, Belknap, Chadbourne, Fort Stockton, Fort Davis, Fort Bliss, McKavett, Clark, Fort McIntosh, Fort Inge and Phantom Hill in Texas, and Fort Sill in Oklahoma. There were "sub posts or intermediate stations" including Bothwick's Station on Salt Creek between Fort Richardson and Fort Belknap, Camp Wichita near Buffalo Springs between Fort Richardson and Red River Station, and Mountain Pass between Fort Concho and Fort Griffin.
    FrontierHouse1.jpg
  • Fort Griffin State Historic Site was a Cavalry fort established 29 July 1867 by four companies of the Sixth Cavalry under the command of Lt. Col. S.D. Sturgis, in the northern part of West Texas, specifically northwestern Shackelford County, to give settlers protection from early Comanche and Kiowa raids. Originally called Camp Wilson, it was finally named for Charles Griffin, a former Civil War Union general who had commanded the Department of Texas during the early years of Reconstruction.<br />
<br />
Other forts in the frontier fort system were Forts Richardson, Concho, Belknap, Chadbourne, Fort Stockton, Fort Davis, Fort Bliss, McKavett, Clark, Fort McIntosh, Fort Inge and Phantom Hill in Texas, and Fort Sill in Oklahoma. There were "sub posts or intermediate stations" including Bothwick's Station on Salt Creek between Fort Richardson and Fort Belknap, Camp Wichita near Buffalo Springs between Fort Richardson and Red River Station, and Mountain Pass between Fort Concho and Fort Griffin.
    _D3_7641.jpg
  • Glacier National Park is a national park located in the U.S. state of Montana, on the Canada–United States border with the Canadian provinces of Alberta and British Columbia. The park encompasses over 1 million acres and includes parts of two mountain ranges (sub-ranges of the Rocky Mountains), over 130 named lakes, more than 1,000 different species of plants, and hundreds of species of animals. This vast pristine ecosystem is the centerpiece of what has been referred to as the "Crown of the Continent Ecosystem", a region of protected land encompassing 16,000 square miles.<br />
<br />
The region that became Glacier National Park was first inhabited by Native Americans. Upon the arrival of European explorers, it was dominated by the Blackfeet in the east and the Flathead in the western regions. Soon after the establishment of the park on May 11, 1910, a number of hotels and chalets were constructed by the Great Northern Railway. These historic hotels and chalets are listed as National Historic Landmarks and a total of 350 locations are on the National Register of Historic Places. By 1932 work was completed on the Going-to-the-Sun Road, later designated a National Historic Civil Engineering Landmark, which provided greater accessibility for automobiles into the heart of the park.<br />
<br />
The mountains of Glacier National Park began forming 170 million years ago when ancient rocks were forced eastward up and over much younger rock strata. Known as the Lewis Overthrust, these sedimentary rocks are considered to have some of the finest fossilized examples of extremely early life found anywhere on Earth. The current shapes of the Lewis and Livingston mountain ranges and positioning and size of the lakes show the telltale evidence of massive glacial action, which carved U-shaped valleys and left behind moraines which impounded water, creating lakes. Of the estimated 150 glaciers which existed in the park in the mid-19th century, only 25 active glaciers remained by 2010. Scientists studyin
    GlacierLoganPassSunset1.jpg
  • The Empire State Building is a 102-story landmark Art Deco skyscraper in New York City, United States, at the intersection of Fifth Avenue and West 34th Street. It is 1,250 ft (381 meters) tall.[6] Its name is derived from the nickname for New York, the Empire State. It stood as the world's tallest building for more than 40 years, from its completion in 1931 until construction of the World Trade Center's North Tower was completed in 1972. Following the destruction of the World Trade Center in 2001, the Empire State Building once again became the tallest building in New York City.
    NYCEmpireState11.jpg
  • The Empire State Building is a 102-story landmark Art Deco skyscraper in New York City, United States, at the intersection of Fifth Avenue and West 34th Street. It is 1,250 ft (381 meters) tall.[6] Its name is derived from the nickname for New York, the Empire State. It stood as the world's tallest building for more than 40 years, from its completion in 1931 until construction of the World Trade Center's North Tower was completed in 1972. Following the destruction of the World Trade Center in 2001, the Empire State Building once again became the tallest building in New York City.
    NYCEmpireState8.jpg
  • The Empire State Building is a 102-story landmark Art Deco skyscraper in New York City, United States, at the intersection of Fifth Avenue and West 34th Street. It is 1,250 ft (381 meters) tall.[6] Its name is derived from the nickname for New York, the Empire State. It stood as the world's tallest building for more than 40 years, from its completion in 1931 until construction of the World Trade Center's North Tower was completed in 1972. Following the destruction of the World Trade Center in 2001, the Empire State Building once again became the tallest building in New York City.
    NYCEmpireState7.jpg
  • The Empire State Building is a 102-story landmark Art Deco skyscraper in New York City, United States, at the intersection of Fifth Avenue and West 34th Street. It is 1,250 ft (381 meters) tall.[6] Its name is derived from the nickname for New York, the Empire State. It stood as the world's tallest building for more than 40 years, from its completion in 1931 until construction of the World Trade Center's North Tower was completed in 1972. Following the destruction of the World Trade Center in 2001, the Empire State Building once again became the tallest building in New York City.
    NYCEmpireState5.jpg
  • Manhattan is the most densely populated of the five boroughs of New York City. The borough is coterminous with New York County, founded on November 1, 1683 as an original county of the U.S. state of New York. The borough consists mostly of Manhattan Island, bounded by the East, Hudson, and Harlem Rivers, but also includes several small adjacent islands, as well as Marble Hill, a small neighborhood on the U.S. mainland.
    NYCTopOfTheRock7.jpg
  • Glacier National Park is a national park located in the U.S. state of Montana, on the Canada–United States border with the Canadian provinces of Alberta and British Columbia. The park encompasses over 1 million acres and includes parts of two mountain ranges (sub-ranges of the Rocky Mountains), over 130 named lakes, more than 1,000 different species of plants, and hundreds of species of animals. This vast pristine ecosystem is the centerpiece of what has been referred to as the "Crown of the Continent Ecosystem", a region of protected land encompassing 16,000 square miles.<br />
<br />
The region that became Glacier National Park was first inhabited by Native Americans. Upon the arrival of European explorers, it was dominated by the Blackfeet in the east and the Flathead in the western regions. Soon after the establishment of the park on May 11, 1910, a number of hotels and chalets were constructed by the Great Northern Railway. These historic hotels and chalets are listed as National Historic Landmarks and a total of 350 locations are on the National Register of Historic Places. By 1932 work was completed on the Going-to-the-Sun Road, later designated a National Historic Civil Engineering Landmark, which provided greater accessibility for automobiles into the heart of the park.<br />
<br />
The mountains of Glacier National Park began forming 170 million years ago when ancient rocks were forced eastward up and over much younger rock strata. Known as the Lewis Overthrust, these sedimentary rocks are considered to have some of the finest fossilized examples of extremely early life found anywhere on Earth. The current shapes of the Lewis and Livingston mountain ranges and positioning and size of the lakes show the telltale evidence of massive glacial action, which carved U-shaped valleys and left behind moraines which impounded water, creating lakes. Of the estimated 150 glaciers which existed in the park in the mid-19th century, only 25 active glaciers remained by 2010. Scientists studyin
    GlacierLoganPassStorm1.jpg
  • Fort Griffin State Historic Site was a Cavalry fort established 29 July 1867 by four companies of the Sixth Cavalry under the command of Lt. Col. S.D. Sturgis, in the northern part of West Texas, specifically northwestern Shackelford County, to give settlers protection from early Comanche and Kiowa raids. Originally called Camp Wilson, it was finally named for Charles Griffin, a former Civil War Union general who had commanded the Department of Texas during the early years of Reconstruction.<br />
<br />
Other forts in the frontier fort system were Forts Richardson, Concho, Belknap, Chadbourne, Fort Stockton, Fort Davis, Fort Bliss, McKavett, Clark, Fort McIntosh, Fort Inge and Phantom Hill in Texas, and Fort Sill in Oklahoma. There were "sub posts or intermediate stations" including Bothwick's Station on Salt Creek between Fort Richardson and Fort Belknap, Camp Wichita near Buffalo Springs between Fort Richardson and Red River Station, and Mountain Pass between Fort Concho and Fort Griffin.
    FortGriffinTree1.jpg
  • The Empire State Building is a 102-story landmark Art Deco skyscraper in New York City, United States, at the intersection of Fifth Avenue and West 34th Street. It is 1,250 ft (381 meters) tall.[6] Its name is derived from the nickname for New York, the Empire State. It stood as the world's tallest building for more than 40 years, from its completion in 1931 until construction of the World Trade Center's North Tower was completed in 1972. Following the destruction of the World Trade Center in 2001, the Empire State Building once again became the tallest building in New York City.
    NYCEmpireState1.jpg
  • Manhattan is the most densely populated of the five boroughs of New York City. The borough is coterminous with New York County, founded on November 1, 1683 as an original county of the U.S. state of New York. The borough consists mostly of Manhattan Island, bounded by the East, Hudson, and Harlem Rivers, but also includes several small adjacent islands, as well as Marble Hill, a small neighborhood on the U.S. mainland.
    NYCTopOfTheRock2.jpg
  • Death Valley is a desert located in Eastern California. Situated within the Mojave Desert, it features the lowest, driest, and hottest locations in North America.
    DeathValleyDuneAndSky2-LAB.jpg
  • Fort Griffin State Historic Site was a Cavalry fort established 29 July 1867 by four companies of the Sixth Cavalry under the command of Lt. Col. S.D. Sturgis, in the northern part of West Texas, specifically northwestern Shackelford County, to give settlers protection from early Comanche and Kiowa raids. Originally called Camp Wilson, it was finally named for Charles Griffin, a former Civil War Union general who had commanded the Department of Texas during the early years of Reconstruction.<br />
<br />
Other forts in the frontier fort system were Forts Richardson, Concho, Belknap, Chadbourne, Fort Stockton, Fort Davis, Fort Bliss, McKavett, Clark, Fort McIntosh, Fort Inge and Phantom Hill in Texas, and Fort Sill in Oklahoma. There were "sub posts or intermediate stations" including Bothwick's Station on Salt Creek between Fort Richardson and Fort Belknap, Camp Wichita near Buffalo Springs between Fort Richardson and Red River Station, and Mountain Pass between Fort Concho and Fort Griffin.
    FrontierHouse1.jpg
  • Ófærufoss is a waterfall situated in the Eldgjá chasm in central Iceland. Until the early 1990s a natural bridge spanned the falls, but it collapsed from natural causes.
    Ofaerufoss1.jpg
  • Ófærufoss is a waterfall situated in the Eldgjá chasm in central Iceland. Until the early 1990s a natural bridge spanned the falls, but it collapsed from natural causes.
    Ofaerufoss1.jpg
  • Glacier National Park is a national park located in the U.S. state of Montana, on the Canada–United States border with the Canadian provinces of Alberta and British Columbia. The park encompasses over 1 million acres and includes parts of two mountain ranges (sub-ranges of the Rocky Mountains), over 130 named lakes, more than 1,000 different species of plants, and hundreds of species of animals. This vast pristine ecosystem is the centerpiece of what has been referred to as the "Crown of the Continent Ecosystem", a region of protected land encompassing 16,000 square miles.<br />
<br />
The region that became Glacier National Park was first inhabited by Native Americans. Upon the arrival of European explorers, it was dominated by the Blackfeet in the east and the Flathead in the western regions. Soon after the establishment of the park on May 11, 1910, a number of hotels and chalets were constructed by the Great Northern Railway. These historic hotels and chalets are listed as National Historic Landmarks and a total of 350 locations are on the National Register of Historic Places. By 1932 work was completed on the Going-to-the-Sun Road, later designated a National Historic Civil Engineering Landmark, which provided greater accessibility for automobiles into the heart of the park.<br />
<br />
The mountains of Glacier National Park began forming 170 million years ago when ancient rocks were forced eastward up and over much younger rock strata. Known as the Lewis Overthrust, these sedimentary rocks are considered to have some of the finest fossilized examples of extremely early life found anywhere on Earth. The current shapes of the Lewis and Livingston mountain ranges and positioning and size of the lakes show the telltale evidence of massive glacial action, which carved U-shaped valleys and left behind moraines which impounded water, creating lakes. Of the estimated 150 glaciers which existed in the park in the mid-19th century, only 25 active glaciers remained by 2010. Scientists studyin
    GlacierLoganPassSunset1.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
  • Ófærufoss is a waterfall situated in the Eldgjá chasm in central Iceland. Until the early 1990s a natural bridge spanned the falls, but it collapsed from natural causes.
    Ofaerufoss5.jpg
  • Ófærufoss is a waterfall situated in the Eldgjá chasm in central Iceland. Until the early 1990s a natural bridge spanned the falls, but it collapsed from natural causes.
    Ofaerufoss3.jpg
  • Fjaðrárgljúfur is a canyon in south east Iceland which is up to 100 m deep and about 2 kilometers long, with the Fjaðrá river flowing through it .The canyon has steep walls and winding water.
    Fjadrargljufur9.jpg
  • Ófærufoss is a waterfall situated in the Eldgjá chasm in central Iceland. Until the early 1990s a natural bridge spanned the falls, but it collapsed from natural causes.
    Ofaerufoss4.jpg
  • Fjaðrárgljúfur is a canyon in south east Iceland which is up to 100 m deep and about 2 kilometers long, with the Fjaðrá river flowing through it .The canyon has steep walls and winding water.
    _A1A6441-HDR.jpg
  • The Fontana del Pantheon fountain in front of the Pantheon in Rome, Italy. The Fontana del Pantheon was commissioned by Pope Gregory XIII and is located in the Piazza della Rotonda, Rome, in front of the Roman Pantheon. It was designed by Giacomo Della Porta in 1575 and sculpted out of marble by Leonardo Sormani.<br />
In 1711, Pope Clement XI requested that the fountain be modified and had Filippo Barigioni design a new layout, which included a different basin, made of stone, and the Macuteo obelisk, created during the period of Ramses II, set in the centre on a plinth with four dolphins decorating the base.<br />
In 1886, the original marble figures were removed, and replaced with copies by Luigi Amici. Today, the originals can be seen in the Museum of Rome.<br />
Fontana del Pantheon was the model to Francesco Robba for the Robba fountain, which stands at Town Square in Ljubljana, the capital of Slovenia. It is one of the city's most recognizable symbols.
    RomePantheon1.jpg
  • Death Valley is a desert located in Eastern California. Situated within the Mojave Desert, it features the lowest, driest, and hottest locations in North America.
    DeathValleyDuneAndSky2-LAB.jpg
  • The Empire State Building is a 102-story landmark Art Deco skyscraper in New York City, United States, at the intersection of Fifth Avenue and West 34th Street. It is 1,250 ft (381 meters) tall.[6] Its name is derived from the nickname for New York, the Empire State. It stood as the world's tallest building for more than 40 years, from its completion in 1931 until construction of the World Trade Center's North Tower was completed in 1972. Following the destruction of the World Trade Center in 2001, the Empire State Building once again became the tallest building in New York City.
    NYCEmpireState10.jpg
  • The Empire State Building is a 102-story landmark Art Deco skyscraper in New York City, United States, at the intersection of Fifth Avenue and West 34th Street. It is 1,250 ft (381 meters) tall.[6] Its name is derived from the nickname for New York, the Empire State. It stood as the world's tallest building for more than 40 years, from its completion in 1931 until construction of the World Trade Center's North Tower was completed in 1972. Following the destruction of the World Trade Center in 2001, the Empire State Building once again became the tallest building in New York City.
    NYCEmpireState6.jpg
  • Manhattan is the most densely populated of the five boroughs of New York City. The borough is coterminous with New York County, founded on November 1, 1683 as an original county of the U.S. state of New York. The borough consists mostly of Manhattan Island, bounded by the East, Hudson, and Harlem Rivers, but also includes several small adjacent islands, as well as Marble Hill, a small neighborhood on the U.S. mainland.
    NYCTopOfTheRock3.jpg
  • Manhattan is the most densely populated of the five boroughs of New York City. The borough is coterminous with New York County, founded on November 1, 1683 as an original county of the U.S. state of New York. The borough consists mostly of Manhattan Island, bounded by the East, Hudson, and Harlem Rivers, but also includes several small adjacent islands, as well as Marble Hill, a small neighborhood on the U.S. mainland.
    NYCTopOfTheRock5.jpg
  • View from Torre LatinoAmericana. Mexico City is the densely populated, high-altitude capital of Mexico. It's known for its Templo Mayor (a 13th-century Aztec temple), the baroque Catedral Metropolitana of the Spanish conquistadors and the Palacio Nacional, which houses historic murals by Diego Rivera. All of this resides in and around the Plaza de la Constitución, the massive main square also known as the Zócalo.
    MexicoCity2.jpg
  • View from Torre LatinoAmericana. Mexico City is the densely populated, high-altitude capital of Mexico. It's known for its Templo Mayor (a 13th-century Aztec temple), the baroque Catedral Metropolitana of the Spanish conquistadors and the Palacio Nacional, which houses historic murals by Diego Rivera. All of this resides in and around the Plaza de la Constitución, the massive main square also known as the Zócalo.
    MexicoCity1.jpg
  • The National Museum of Anthropology (Spanish: Museo Nacional de Antropología, MNA) is a national museum of Mexico. It is the largest and most visited museum in Mexico. Located in the area between Paseo de la Reforma and Mahatma Gandhi Street within Chapultepec Park in Mexico City, the museum contains significant archaeological and anthropological artifacts from the Mexico's pre-Columbian heritage, such as the Stone of the Sun (or the Aztec calendar stone) and the 16th-century Aztec Xochipilli statue. Designed in 1964 by Pedro Ramírez Vázquez, Jorge Campuzano, and Rafael Mijares Alcérreca, the monumental building contains exhibition halls surrounding a courtyard with a huge pond and a vast square concrete umbrella supported by a single slender pillar (known as "el paraguas", Spanish for "the umbrella"). The halls are ringed by gardens, many of which contain outdoor exhibits. The museum has 23 rooms for exhibits and covers an area of 79,700 square meters (almost 8 hectares) or 857,890 square feet (almost 20 acres).
    Aztec3.jpg
  • The Empire State Building is a 102-story landmark Art Deco skyscraper in New York City, United States, at the intersection of Fifth Avenue and West 34th Street. It is 1,250 ft (381 meters) tall.[6] Its name is derived from the nickname for New York, the Empire State. It stood as the world's tallest building for more than 40 years, from its completion in 1931 until construction of the World Trade Center's North Tower was completed in 1972. Following the destruction of the World Trade Center in 2001, the Empire State Building once again became the tallest building in New York City.
    NYCEmpireState3.jpg
  • Death Valley is a desert valley located in Eastern California. Situated within the Mojave Desert, it is the lowest and driest area in North America. The Mesquite Flat Sand Dunes are at the northern end of the valley floor and are nearly surrounded by mountains on all sides. Due to their easy access from the road and the overall proximity of Death Valley to Hollywood, these dunes have been used to film sand dune scenes for several movies including films in the Star Wars series. The largest dune is called Star Dune and is relatively stable and stationary because it is at a point where the various winds that shape the dunes converge. The depth of the sand at its crest is 130–140 feet but this is small compared to other dunes in the area that have sand depths of up to 600–700 feet deep.<br />
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The primary source of the dune sands is probably the Cottonwood Mountains which lie to the north and northwest. The tiny grains of quartz and feldspar that form the sinuous sculptures that make up this dune field began as much larger pieces of solid rock.<br />
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In between many of the dunes are stands of creosote bush and some mesquite on the sand and on dried mud, which used to cover this part of the valley before the dunes intruded (mesquite was the dominant plant here before the sand dunes but creosote does much better in the sand dune conditions).<br />
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Located near the border of California and Nevada, in the Great Basin, east of the Sierra Nevada mountains, Death Valley constitutes much of Death Valley National Park and is the principal feature of the Mojave and Colorado Deserts Biosphere Reserve. It is located mostly in Inyo County, California. It runs from north to south between the Amargosa Range on the east and the Panamint Range on the west; the Sylvania Mountains and the Owlshead Mountains form its northern and southern boundaries, respectively.
    DeathValleyDuneAndSky1-LAB.jpg
  • The guanaco (Lama guanicoe) is a camelid native to South America that stands between 1 and 1.2 metres (3 ft 3 in and 3 ft 11 in) at the shoulder and weighs about 90 kg (200 lb). The colour varies very little (unlike the domestic llama), ranging from a light brown to dark cinnamon and shading to white underneath. Guanacos have grey faces and small straight ears. The name guanaco comes from the South American language Quechua word wanaku (old spelling, huanaco). Young guanacos are called chulengo(s). These guanacos were photographed in Torres del Paine, Chile.
    Guanacos2.jpg
  • Lost Maples State Natural Area is located about 5 miles north of Vanderpool, Texas and 71 miles west of San Antonio. The park sits along the Sabinal River in western Bandera County and far eastern Real County. The land for Lost Maples State Natural Area was acquired by the state of Texas in 1973 and 1974, and the park was opened to the public in 1979. In 1980, the Heritage Conservation and Recreation Service made the park a National Natural Landmark. This area along the upper Sabinal River was inhabited in prehistoric times. The recorded history of the area, beginning with Spanish explorations in the 17th century, identified a number of Indian groups, including the Apache, Lipan Apache and Comanche.<br />
<br />
Much of the park's limestone bedrock is exposed on elevated terrain, which has a shallow, discontinuous cover of dark gray stony clay (Eckrant series). Most valley bottoms have deep, dark brown silty clay (Krum series) or clay loam (Pratley series). Deposits of gravel, sand, and loam (Orif-Boerne association) lie within a few hundred feet of the Sabinal River. All of these soils have free calcium carbonate throughout their profiles and are moderately alkaline. Despite a high clay content in most cases, poorly drained soils are too inextensive to be mapped.<br />
<br />
Among the trees are American Sycamore (Platanus occidentalis), Bald Cypress (Taxodium distichum), Black Walnut (Juglans nigra), Pecan (Carya illinoinensis), Green Ash (Fraxinus pennsylvanica), Black Willow (Salix nigra), Chinkapin Oak (Quercus muehlenbergii), Lacey Oak (Quercus laceyi), Texas Red Oak (Quercus buckleyi), Juniper, Florida Basswood (Tilia caroliniana) and Bigtooth Maple (Acer grandidentatum) (the latter of which was discovered far removed from any maple forest, and thus gave the area the name "lost maples"). Maple colors are brilliant unless autumn is mild; the Texas red oak gives a good display almost every year. This park is most crowded when the fall colors peak in November. Evidence suggests that th
    LostMaplesReflection.jpg
  • Lost Maples State Natural Area is located about 5 miles north of Vanderpool, Texas and 71 miles west of San Antonio. The park sits along the Sabinal River in western Bandera County and far eastern Real County. The land for Lost Maples State Natural Area was acquired by the state of Texas in 1973 and 1974, and the park was opened to the public in 1979. In 1980, the Heritage Conservation and Recreation Service made the park a National Natural Landmark. This area along the upper Sabinal River was inhabited in prehistoric times. The recorded history of the area, beginning with Spanish explorations in the 17th century, identified a number of Indian groups, including the Apache, Lipan Apache and Comanche.<br />
<br />
Much of the park's limestone bedrock is exposed on elevated terrain, which has a shallow, discontinuous cover of dark gray stony clay (Eckrant series). Most valley bottoms have deep, dark brown silty clay (Krum series) or clay loam (Pratley series). Deposits of gravel, sand, and loam (Orif-Boerne association) lie within a few hundred feet of the Sabinal River. All of these soils have free calcium carbonate throughout their profiles and are moderately alkaline. Despite a high clay content in most cases, poorly drained soils are too inextensive to be mapped.<br />
<br />
Among the trees are American Sycamore (Platanus occidentalis), Bald Cypress (Taxodium distichum), Black Walnut (Juglans nigra), Pecan (Carya illinoinensis), Green Ash (Fraxinus pennsylvanica), Black Willow (Salix nigra), Chinkapin Oak (Quercus muehlenbergii), Lacey Oak (Quercus laceyi), Texas Red Oak (Quercus buckleyi), Juniper, Florida Basswood (Tilia caroliniana) and Bigtooth Maple (Acer grandidentatum) (the latter of which was discovered far removed from any maple forest, and thus gave the area the name "lost maples"). Maple colors are brilliant unless autumn is mild; the Texas red oak gives a good display almost every year. This park is most crowded when the fall colors peak in November. Evidence suggests that th
    LostMaplesReflection.jpg
  • Lost Maples State Natural Area is located about 5 miles north of Vanderpool, Texas and 71 miles west of San Antonio. The park sits along the Sabinal River in western Bandera County and far eastern Real County. The land for Lost Maples State Natural Area was acquired by the state of Texas in 1973 and 1974, and the park was opened to the public in 1979. In 1980, the Heritage Conservation and Recreation Service made the park a National Natural Landmark. This area along the upper Sabinal River was inhabited in prehistoric times. The recorded history of the area, beginning with Spanish explorations in the 17th century, identified a number of Indian groups, including the Apache, Lipan Apache and Comanche.<br />
<br />
Much of the park's limestone bedrock is exposed on elevated terrain, which has a shallow, discontinuous cover of dark gray stony clay (Eckrant series). Most valley bottoms have deep, dark brown silty clay (Krum series) or clay loam (Pratley series). Deposits of gravel, sand, and loam (Orif-Boerne association) lie within a few hundred feet of the Sabinal River. All of these soils have free calcium carbonate throughout their profiles and are moderately alkaline. Despite a high clay content in most cases, poorly drained soils are too inextensive to be mapped.<br />
<br />
Among the trees are American Sycamore (Platanus occidentalis), Bald Cypress (Taxodium distichum), Black Walnut (Juglans nigra), Pecan (Carya illinoinensis), Green Ash (Fraxinus pennsylvanica), Black Willow (Salix nigra), Chinkapin Oak (Quercus muehlenbergii), Lacey Oak (Quercus laceyi), Texas Red Oak (Quercus buckleyi), Juniper, Florida Basswood (Tilia caroliniana) and Bigtooth Maple (Acer grandidentatum) (the latter of which was discovered far removed from any maple forest, and thus gave the area the name "lost maples"). Maple colors are brilliant unless autumn is mild; the Texas red oak gives a good display almost every year. This park is most crowded when the fall colors peak in November. Evidence suggests that th
    LostMaplesReflection.jpg
  • Lost Maples State Natural Area is located about 5 miles north of Vanderpool, Texas and 71 miles west of San Antonio. The park sits along the Sabinal River in western Bandera County and far eastern Real County. The land for Lost Maples State Natural Area was acquired by the state of Texas in 1973 and 1974, and the park was opened to the public in 1979. In 1980, the Heritage Conservation and Recreation Service made the park a National Natural Landmark. This area along the upper Sabinal River was inhabited in prehistoric times. The recorded history of the area, beginning with Spanish explorations in the 17th century, identified a number of Indian groups, including the Apache, Lipan Apache and Comanche.<br />
<br />
Much of the park's limestone bedrock is exposed on elevated terrain, which has a shallow, discontinuous cover of dark gray stony clay (Eckrant series). Most valley bottoms have deep, dark brown silty clay (Krum series) or clay loam (Pratley series). Deposits of gravel, sand, and loam (Orif-Boerne association) lie within a few hundred feet of the Sabinal River. All of these soils have free calcium carbonate throughout their profiles and are moderately alkaline. Despite a high clay content in most cases, poorly drained soils are too inextensive to be mapped.<br />
<br />
Among the trees are American Sycamore (Platanus occidentalis), Bald Cypress (Taxodium distichum), Black Walnut (Juglans nigra), Pecan (Carya illinoinensis), Green Ash (Fraxinus pennsylvanica), Black Willow (Salix nigra), Chinkapin Oak (Quercus muehlenbergii), Lacey Oak (Quercus laceyi), Texas Red Oak (Quercus buckleyi), Juniper, Florida Basswood (Tilia caroliniana) and Bigtooth Maple (Acer grandidentatum) (the latter of which was discovered far removed from any maple forest, and thus gave the area the name "lost maples"). Maple colors are brilliant unless autumn is mild; the Texas red oak gives a good display almost every year. This park is most crowded when the fall colors peak in November. Evidence suggests that th
    LostMaplesReflection.jpg
  • The (southern) pale chanting goshawk (Melierax canorus) is a bird of prey in the family Accipitridae. This hawk breeds in southern Africa. It is a resident species of dry, open semi-desert . It is commonly seen perched on roadside telephone poles.<br />
<br />
This species is 56–65 cm long. The adult has grey upperparts with a white rump. The central tail feathers are black tipped with white, and the outer feathers are barred grey and white. The head and upper breast are pale grey; the rest of the underparts are finely barred in dark grey and white. Its eyes are yellow, the bill is mostly orange, and it has long orange legs. It is paler than the grey-rumped dark chanting goshawk, Melierax metabates.<br />
<br />
The pale chanting goshawk eats a variety of vertebrate prey, mainly lizards, but also small mammals and birds, and large insects. It often walks on the ground.
    PaleChantingGoshawk1.jpg
  • Lost Maples State Natural Area is located about 5 miles north of Vanderpool, Texas and 71 miles west of San Antonio. The park sits along the Sabinal River in western Bandera County and far eastern Real County. The land for Lost Maples State Natural Area was acquired by the state of Texas in 1973 and 1974, and the park was opened to the public in 1979. In 1980, the Heritage Conservation and Recreation Service made the park a National Natural Landmark. This area along the upper Sabinal River was inhabited in prehistoric times. The recorded history of the area, beginning with Spanish explorations in the 17th century, identified a number of Indian groups, including the Apache, Lipan Apache and Comanche.<br />
<br />
Much of the park's limestone bedrock is exposed on elevated terrain, which has a shallow, discontinuous cover of dark gray stony clay (Eckrant series). Most valley bottoms have deep, dark brown silty clay (Krum series) or clay loam (Pratley series). Deposits of gravel, sand, and loam (Orif-Boerne association) lie within a few hundred feet of the Sabinal River. All of these soils have free calcium carbonate throughout their profiles and are moderately alkaline. Despite a high clay content in most cases, poorly drained soils are too inextensive to be mapped.<br />
<br />
Among the trees are American Sycamore (Platanus occidentalis), Bald Cypress (Taxodium distichum), Black Walnut (Juglans nigra), Pecan (Carya illinoinensis), Green Ash (Fraxinus pennsylvanica), Black Willow (Salix nigra), Chinkapin Oak (Quercus muehlenbergii), Lacey Oak (Quercus laceyi), Texas Red Oak (Quercus buckleyi), Juniper, Florida Basswood (Tilia caroliniana) and Bigtooth Maple (Acer grandidentatum) (the latter of which was discovered far removed from any maple forest, and thus gave the area the name "lost maples"). Maple colors are brilliant unless autumn is mild; the Texas red oak gives a good display almost every year. This park is most crowded when the fall colors peak in November. Evidence suggests that th
    LostMaplesReflection.jpg
  • Oppède is a commune in the Vaucluse department in the Provence-Alpes-Côte d'Azur region in southeastern France. Oppidum is the Latin word for 'town'. It is in fact two villages: Oppède-le-Vieux ("the old" in French), built against the Petit Luberon and dating back to the 12th century, and Oppède-les-Poulivets ("nice view" in Provençal), today known as "le village", down in the valley.<br />
<br />
The old village, built on a rocky hill, has narrow streets. In winter, the Petit Luberon starts casting its shadow early in the afternoon. Houses beyond the medieval ramparts are dark, humid and tricky to maintain. From below the village is dominated by the restored church of Notre-Dame-Dalidon and the ruins of the castle. In the 19th century, the inhabitants had enough and started to move down in the valley, dismantling the roof of their houses to stop paying property taxes.<br />
<br />
By the beginning of the 20th century, Oppède-le-Vieux was a ghost village and a new community was officially established in the valley, with larger streets, cosier houses and farmers closer to their fields.<br />
<br />
Following the armistice of June 1940, architect Bernard Zehrfuss founded a commune of artists in the old town, a project that attracted French sculptor François Stahly and the writer and artist Consuelo de Saint Exupéry. The commune proved short-lived. It was the basis for Saint Exupéry's fictionalized account, published in 1946, called "Kingdom of the Rocks".[2]
    OppedeLeVieux9.jpg
  • Oppède is a commune in the Vaucluse department in the Provence-Alpes-Côte d'Azur region in southeastern France. Oppidum is the Latin word for 'town'. It is in fact two villages: Oppède-le-Vieux ("the old" in French), built against the Petit Luberon and dating back to the 12th century, and Oppède-les-Poulivets ("nice view" in Provençal), today known as "le village", down in the valley.<br />
<br />
The old village, built on a rocky hill, has narrow streets. In winter, the Petit Luberon starts casting its shadow early in the afternoon. Houses beyond the medieval ramparts are dark, humid and tricky to maintain. From below the village is dominated by the restored church of Notre-Dame-Dalidon and the ruins of the castle. In the 19th century, the inhabitants had enough and started to move down in the valley, dismantling the roof of their houses to stop paying property taxes.<br />
<br />
By the beginning of the 20th century, Oppède-le-Vieux was a ghost village and a new community was officially established in the valley, with larger streets, cosier houses and farmers closer to their fields.<br />
<br />
Following the armistice of June 1940, architect Bernard Zehrfuss founded a commune of artists in the old town, a project that attracted French sculptor François Stahly and the writer and artist Consuelo de Saint Exupéry. The commune proved short-lived. It was the basis for Saint Exupéry's fictionalized account, published in 1946, called "Kingdom of the Rocks".[2]
    OppedeLeVieux1.jpg
  • The springbok (Antidorcas marsupialis) is a medium-sized antelope found mainly in southern and southwestern Africa. The sole member of the genus Antidorcas, this bovid was first described by the German zoologist Eberhard August Wilhelm von Zimmermann in 1780. Three subspecies are identified. A slender, long-legged antelope, the springbok reaches 71 to 86 cm (28 to 34 in) at the shoulder and weighs between 27 and 42 kg (60 and 93 lb). Both sexes have a pair of black, 35-to-50-centimetre (14 to 20 in) long horns that curve backward. The springbok is characterised by a white face, a dark stripe running from the eyes to the mouth, a light brown coat marked by a reddish brown stripe that runs from the upper foreleg to the buttocks across the flanks, and a white rump flap.<br />
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Active mainly at dawn and dusk, springbok form harems (mixed-sex herds). In earlier times, springbok of the Kalahari desert and Karoo would migrate in large numbers across the countryside, a practice known as trekbokken. A feature unique to the springbok is pronking, in which the springbok performs multiple leaps into the air, up to 2 metres (6.6 ft) above the ground, in a stiff-legged posture, with the back bowed and the white flap lifted. Primarily a browser, the springbok feeds on shrubs and succulents; this antelope can live without drinking water for years, meeting its requirements through eating succulent vegetation. Breeding takes place year-round, and peaks in the rainy season, when forage is most abundant. A single calf is born after a five to six month long pregnancy; weaning occurs at nearly six months of age, and the calf leaves its mother a few months later.
    Springbok4.jpg
  • The springbok (Antidorcas marsupialis) is a medium-sized antelope found mainly in southern and southwestern Africa. The sole member of the genus Antidorcas, this bovid was first described by the German zoologist Eberhard August Wilhelm von Zimmermann in 1780. Three subspecies are identified. A slender, long-legged antelope, the springbok reaches 71 to 86 cm (28 to 34 in) at the shoulder and weighs between 27 and 42 kg (60 and 93 lb). Both sexes have a pair of black, 35-to-50-centimetre (14 to 20 in) long horns that curve backward. The springbok is characterised by a white face, a dark stripe running from the eyes to the mouth, a light brown coat marked by a reddish brown stripe that runs from the upper foreleg to the buttocks across the flanks, and a white rump flap.<br />
<br />
Active mainly at dawn and dusk, springbok form harems (mixed-sex herds). In earlier times, springbok of the Kalahari desert and Karoo would migrate in large numbers across the countryside, a practice known as trekbokken. A feature unique to the springbok is pronking, in which the springbok performs multiple leaps into the air, up to 2 metres (6.6 ft) above the ground, in a stiff-legged posture, with the back bowed and the white flap lifted. Primarily a browser, the springbok feeds on shrubs and succulents; this antelope can live without drinking water for years, meeting its requirements through eating succulent vegetation. Breeding takes place year-round, and peaks in the rainy season, when forage is most abundant. A single calf is born after a five to six month long pregnancy; weaning occurs at nearly six months of age, and the calf leaves its mother a few months later.
    Springbok2.jpg
  • The guanaco (Lama guanicoe) is a camelid native to South America that stands between 1 and 1.2 metres (3 ft 3 in and 3 ft 11 in) at the shoulder and weighs about 90 kg (200 lb). The colour varies very little (unlike the domestic llama), ranging from a light brown to dark cinnamon and shading to white underneath. Guanacos have grey faces and small straight ears. The name guanaco comes from the South American language Quechua word wanaku (old spelling, huanaco). Young guanacos are called chulengo(s). These guanacos were photographed in Torres del Paine, Chile.
    _D3_3555.jpg
  • The guanaco (Lama guanicoe) is a camelid native to South America that stands between 1 and 1.2 metres (3 ft 3 in and 3 ft 11 in) at the shoulder and weighs about 90 kg (200 lb). The colour varies very little (unlike the domestic llama), ranging from a light brown to dark cinnamon and shading to white underneath. Guanacos have grey faces and small straight ears. The name guanaco comes from the South American language Quechua word wanaku (old spelling, huanaco). Young guanacos are called chulengo(s). These guanacos were photographed in Torres del Paine, Chile.
    _D3_3450.jpg
  • The guanaco (Lama guanicoe) is a camelid native to South America that stands between 1 and 1.2 metres (3 ft 3 in and 3 ft 11 in) at the shoulder and weighs about 90 kg (200 lb). The colour varies very little (unlike the domestic llama), ranging from a light brown to dark cinnamon and shading to white underneath. Guanacos have grey faces and small straight ears. The name guanaco comes from the South American language Quechua word wanaku (old spelling, huanaco). Young guanacos are called chulengo(s). These guanacos were photographed in Torres del Paine, Chile.
    _D3_3425-2.jpg
  • Cattle drive through the Fort Worth Stockyards<br />
.....<br />
The Texas Longhorn is a breed of cattle known for its characteristic horns, which can extend to 7 ft tip to tip for steers and exceptional cows, and 36 to 80 in tip to tip for bulls. Similar cattle were imported by Spanish colonists into other parts of North America, including California and Florida. Horns can have a slight upward turn at their tips or even triple twist. Texas Longhorns are known for their diverse coloring. A longhorn can be any color or mix of colors but dark red and white color mixes are the most dominant. Texas Longhorns with elite genetics can often fetch $40,000 or more at auction with the record of $170,000 in recent history for a cow. Due to their innate gentle disposition and intelligence, Texas Longhorns are increasingly being trained as riding steers.
    TexasLonghorns1.jpg
  • Phalacrocoracidae is a family of some 40 species of aquatic birds commonly known as cormorants and shags. The majority of species have dark feathers. The bill is long, thin and hooked. Their feet have webbing between all four toes. All species are fish-eaters, catching the prey by diving from the surface. They are excellent divers, and under water they propel themselves with their feet with help from their wings; some cormorant species have been found to dive as deep as 45 metres. They have relatively short wings due to their need for economical movement underwater, and consequently have the highest flight costs of any bird.<br />
<br />
Cormorants nest in colonies around the shore, on trees, islets or cliffs. They are coastal rather than oceanic birds, and some have colonised inland waters – indeed, the original ancestor of cormorants seems to have been a fresh-water bird. They range around the world, except for the central Pacific islands.
    GalvestonCormorants1.jpg
  • Oppède is a commune in the Vaucluse department in the Provence-Alpes-Côte d'Azur region in southeastern France. Oppidum is the Latin word for 'town'. It is in fact two villages: Oppède-le-Vieux ("the old" in French), built against the Petit Luberon and dating back to the 12th century, and Oppède-les-Poulivets ("nice view" in Provençal), today known as "le village", down in the valley.<br />
<br />
The old village, built on a rocky hill, has narrow streets. In winter, the Petit Luberon starts casting its shadow early in the afternoon. Houses beyond the medieval ramparts are dark, humid and tricky to maintain. From below the village is dominated by the restored church of Notre-Dame-Dalidon and the ruins of the castle. In the 19th century, the inhabitants had enough and started to move down in the valley, dismantling the roof of their houses to stop paying property taxes.<br />
<br />
By the beginning of the 20th century, Oppède-le-Vieux was a ghost village and a new community was officially established in the valley, with larger streets, cosier houses and farmers closer to their fields.<br />
<br />
Following the armistice of June 1940, architect Bernard Zehrfuss founded a commune of artists in the old town, a project that attracted French sculptor François Stahly and the writer and artist Consuelo de Saint Exupéry. The commune proved short-lived. It was the basis for Saint Exupéry's fictionalized account, published in 1946, called "Kingdom of the Rocks".[2]
    OppedeLeVieux13.jpg
  • Oppède is a commune in the Vaucluse department in the Provence-Alpes-Côte d'Azur region in southeastern France. Oppidum is the Latin word for 'town'. It is in fact two villages: Oppède-le-Vieux ("the old" in French), built against the Petit Luberon and dating back to the 12th century, and Oppède-les-Poulivets ("nice view" in Provençal), today known as "le village", down in the valley.<br />
<br />
The old village, built on a rocky hill, has narrow streets. In winter, the Petit Luberon starts casting its shadow early in the afternoon. Houses beyond the medieval ramparts are dark, humid and tricky to maintain. From below the village is dominated by the restored church of Notre-Dame-Dalidon and the ruins of the castle. In the 19th century, the inhabitants had enough and started to move down in the valley, dismantling the roof of their houses to stop paying property taxes.<br />
<br />
By the beginning of the 20th century, Oppède-le-Vieux was a ghost village and a new community was officially established in the valley, with larger streets, cosier houses and farmers closer to their fields.<br />
<br />
Following the armistice of June 1940, architect Bernard Zehrfuss founded a commune of artists in the old town, a project that attracted French sculptor François Stahly and the writer and artist Consuelo de Saint Exupéry. The commune proved short-lived. It was the basis for Saint Exupéry's fictionalized account, published in 1946, called "Kingdom of the Rocks".[2]
    OppedeLeVieux10.jpg
  • Oppède is a commune in the Vaucluse department in the Provence-Alpes-Côte d'Azur region in southeastern France. Oppidum is the Latin word for 'town'. It is in fact two villages: Oppède-le-Vieux ("the old" in French), built against the Petit Luberon and dating back to the 12th century, and Oppède-les-Poulivets ("nice view" in Provençal), today known as "le village", down in the valley.<br />
<br />
The old village, built on a rocky hill, has narrow streets. In winter, the Petit Luberon starts casting its shadow early in the afternoon. Houses beyond the medieval ramparts are dark, humid and tricky to maintain. From below the village is dominated by the restored church of Notre-Dame-Dalidon and the ruins of the castle. In the 19th century, the inhabitants had enough and started to move down in the valley, dismantling the roof of their houses to stop paying property taxes.<br />
<br />
By the beginning of the 20th century, Oppède-le-Vieux was a ghost village and a new community was officially established in the valley, with larger streets, cosier houses and farmers closer to their fields.<br />
<br />
Following the armistice of June 1940, architect Bernard Zehrfuss founded a commune of artists in the old town, a project that attracted French sculptor François Stahly and the writer and artist Consuelo de Saint Exupéry. The commune proved short-lived. It was the basis for Saint Exupéry's fictionalized account, published in 1946, called "Kingdom of the Rocks".[2]
    OppedeLeVieux8.jpg
  • Oppède is a commune in the Vaucluse department in the Provence-Alpes-Côte d'Azur region in southeastern France. Oppidum is the Latin word for 'town'. It is in fact two villages: Oppède-le-Vieux ("the old" in French), built against the Petit Luberon and dating back to the 12th century, and Oppède-les-Poulivets ("nice view" in Provençal), today known as "le village", down in the valley.<br />
<br />
The old village, built on a rocky hill, has narrow streets. In winter, the Petit Luberon starts casting its shadow early in the afternoon. Houses beyond the medieval ramparts are dark, humid and tricky to maintain. From below the village is dominated by the restored church of Notre-Dame-Dalidon and the ruins of the castle. In the 19th century, the inhabitants had enough and started to move down in the valley, dismantling the roof of their houses to stop paying property taxes.<br />
<br />
By the beginning of the 20th century, Oppède-le-Vieux was a ghost village and a new community was officially established in the valley, with larger streets, cosier houses and farmers closer to their fields.<br />
<br />
Following the armistice of June 1940, architect Bernard Zehrfuss founded a commune of artists in the old town, a project that attracted French sculptor François Stahly and the writer and artist Consuelo de Saint Exupéry. The commune proved short-lived. It was the basis for Saint Exupéry's fictionalized account, published in 1946, called "Kingdom of the Rocks".[2]
    OppedeLeVieux5.jpg
  • The springbok (Antidorcas marsupialis) is a medium-sized antelope found mainly in southern and southwestern Africa. The sole member of the genus Antidorcas, this bovid was first described by the German zoologist Eberhard August Wilhelm von Zimmermann in 1780. Three subspecies are identified. A slender, long-legged antelope, the springbok reaches 71 to 86 cm (28 to 34 in) at the shoulder and weighs between 27 and 42 kg (60 and 93 lb). Both sexes have a pair of black, 35-to-50-centimetre (14 to 20 in) long horns that curve backward. The springbok is characterised by a white face, a dark stripe running from the eyes to the mouth, a light brown coat marked by a reddish brown stripe that runs from the upper foreleg to the buttocks across the flanks, and a white rump flap.<br />
<br />
Active mainly at dawn and dusk, springbok form harems (mixed-sex herds). In earlier times, springbok of the Kalahari desert and Karoo would migrate in large numbers across the countryside, a practice known as trekbokken. A feature unique to the springbok is pronking, in which the springbok performs multiple leaps into the air, up to 2 metres (6.6 ft) above the ground, in a stiff-legged posture, with the back bowed and the white flap lifted. Primarily a browser, the springbok feeds on shrubs and succulents; this antelope can live without drinking water for years, meeting its requirements through eating succulent vegetation. Breeding takes place year-round, and peaks in the rainy season, when forage is most abundant. A single calf is born after a five to six month long pregnancy; weaning occurs at nearly six months of age, and the calf leaves its mother a few months later.
    Springbok1.jpg
  • The gemsbok or gemsbuck (Oryx gazella) is a large antelope in the Oryx genus. It is native to the arid regions of Southern Africa, such as the Kalahari Desert. The gemsbok is depicted on the coat of arms of Namibia, where the current population of the species is estimated at 373,000 individuals. Gemsbok are light brownish-grey to tan in colour, with lighter patches toward the bottom rear of the rump. Their tails are long and black in colour. A blackish stripe extends from the chin down the lower edge of the neck, through the juncture of the shoulder and leg along the lower flank of each side to the blackish section of the rear leg. They have muscular necks and shoulders, and their legs have white 'socks' with a black patch on the front of both the front legs, and both genders have long, straight horns. Comparably, the East African oryx lacks a dark patch at the base of the tail, has less black on the legs (none on the hindlegs), and less black on the lower flanks. One very rare condition is the "Golden Oryx", in which the Gemsboks black markings are muted and now appear golden.
    Oryx3.jpg
  • The guanaco (Lama guanicoe) is a camelid native to South America that stands between 1 and 1.2 metres (3 ft 3 in and 3 ft 11 in) at the shoulder and weighs about 90 kg (200 lb). The colour varies very little (unlike the domestic llama), ranging from a light brown to dark cinnamon and shading to white underneath. Guanacos have grey faces and small straight ears. The name guanaco comes from the South American language Quechua word wanaku (old spelling, huanaco). Young guanacos are called chulengo(s). These guanacos were photographed in Torres del Paine, Chile.
    Guanacos1.jpg
  • Oppède is a commune in the Vaucluse department in the Provence-Alpes-Côte d'Azur region in southeastern France. Oppidum is the Latin word for 'town'. It is in fact two villages: Oppède-le-Vieux ("the old" in French), built against the Petit Luberon and dating back to the 12th century, and Oppède-les-Poulivets ("nice view" in Provençal), today known as "le village", down in the valley.<br />
<br />
The old village, built on a rocky hill, has narrow streets. In winter, the Petit Luberon starts casting its shadow early in the afternoon. Houses beyond the medieval ramparts are dark, humid and tricky to maintain. From below the village is dominated by the restored church of Notre-Dame-Dalidon and the ruins of the castle. In the 19th century, the inhabitants had enough and started to move down in the valley, dismantling the roof of their houses to stop paying property taxes.<br />
<br />
By the beginning of the 20th century, Oppède-le-Vieux was a ghost village and a new community was officially established in the valley, with larger streets, cosier houses and farmers closer to their fields.<br />
<br />
Following the armistice of June 1940, architect Bernard Zehrfuss founded a commune of artists in the old town, a project that attracted French sculptor François Stahly and the writer and artist Consuelo de Saint Exupéry. The commune proved short-lived. It was the basis for Saint Exupéry's fictionalized account, published in 1946, called "Kingdom of the Rocks".[2]
    OppedeLeVieux3.jpg
  • The springbok (Antidorcas marsupialis) is a medium-sized antelope found mainly in southern and southwestern Africa. The sole member of the genus Antidorcas, this bovid was first described by the German zoologist Eberhard August Wilhelm von Zimmermann in 1780. Three subspecies are identified. A slender, long-legged antelope, the springbok reaches 71 to 86 cm (28 to 34 in) at the shoulder and weighs between 27 and 42 kg (60 and 93 lb). Both sexes have a pair of black, 35-to-50-centimetre (14 to 20 in) long horns that curve backward. The springbok is characterised by a white face, a dark stripe running from the eyes to the mouth, a light brown coat marked by a reddish brown stripe that runs from the upper foreleg to the buttocks across the flanks, and a white rump flap.<br />
<br />
Active mainly at dawn and dusk, springbok form harems (mixed-sex herds). In earlier times, springbok of the Kalahari desert and Karoo would migrate in large numbers across the countryside, a practice known as trekbokken. A feature unique to the springbok is pronking, in which the springbok performs multiple leaps into the air, up to 2 metres (6.6 ft) above the ground, in a stiff-legged posture, with the back bowed and the white flap lifted. Primarily a browser, the springbok feeds on shrubs and succulents; this antelope can live without drinking water for years, meeting its requirements through eating succulent vegetation. Breeding takes place year-round, and peaks in the rainy season, when forage is most abundant. A single calf is born after a five to six month long pregnancy; weaning occurs at nearly six months of age, and the calf leaves its mother a few months later.
    Springbok7.jpg
  • The springbok (Antidorcas marsupialis) is a medium-sized antelope found mainly in southern and southwestern Africa. The sole member of the genus Antidorcas, this bovid was first described by the German zoologist Eberhard August Wilhelm von Zimmermann in 1780. Three subspecies are identified. A slender, long-legged antelope, the springbok reaches 71 to 86 cm (28 to 34 in) at the shoulder and weighs between 27 and 42 kg (60 and 93 lb). Both sexes have a pair of black, 35-to-50-centimetre (14 to 20 in) long horns that curve backward. The springbok is characterised by a white face, a dark stripe running from the eyes to the mouth, a light brown coat marked by a reddish brown stripe that runs from the upper foreleg to the buttocks across the flanks, and a white rump flap.<br />
<br />
Active mainly at dawn and dusk, springbok form harems (mixed-sex herds). In earlier times, springbok of the Kalahari desert and Karoo would migrate in large numbers across the countryside, a practice known as trekbokken. A feature unique to the springbok is pronking, in which the springbok performs multiple leaps into the air, up to 2 metres (6.6 ft) above the ground, in a stiff-legged posture, with the back bowed and the white flap lifted. Primarily a browser, the springbok feeds on shrubs and succulents; this antelope can live without drinking water for years, meeting its requirements through eating succulent vegetation. Breeding takes place year-round, and peaks in the rainy season, when forage is most abundant. A single calf is born after a five to six month long pregnancy; weaning occurs at nearly six months of age, and the calf leaves its mother a few months later.
    Springbok6.jpg
  • The springbok (Antidorcas marsupialis) is a medium-sized antelope found mainly in southern and southwestern Africa. The sole member of the genus Antidorcas, this bovid was first described by the German zoologist Eberhard August Wilhelm von Zimmermann in 1780. Three subspecies are identified. A slender, long-legged antelope, the springbok reaches 71 to 86 cm (28 to 34 in) at the shoulder and weighs between 27 and 42 kg (60 and 93 lb). Both sexes have a pair of black, 35-to-50-centimetre (14 to 20 in) long horns that curve backward. The springbok is characterised by a white face, a dark stripe running from the eyes to the mouth, a light brown coat marked by a reddish brown stripe that runs from the upper foreleg to the buttocks across the flanks, and a white rump flap.<br />
<br />
Active mainly at dawn and dusk, springbok form harems (mixed-sex herds). In earlier times, springbok of the Kalahari desert and Karoo would migrate in large numbers across the countryside, a practice known as trekbokken. A feature unique to the springbok is pronking, in which the springbok performs multiple leaps into the air, up to 2 metres (6.6 ft) above the ground, in a stiff-legged posture, with the back bowed and the white flap lifted. Primarily a browser, the springbok feeds on shrubs and succulents; this antelope can live without drinking water for years, meeting its requirements through eating succulent vegetation. Breeding takes place year-round, and peaks in the rainy season, when forage is most abundant. A single calf is born after a five to six month long pregnancy; weaning occurs at nearly six months of age, and the calf leaves its mother a few months later.
    Springbok5.jpg
  • The springbok (Antidorcas marsupialis) is a medium-sized antelope found mainly in southern and southwestern Africa. The sole member of the genus Antidorcas, this bovid was first described by the German zoologist Eberhard August Wilhelm von Zimmermann in 1780. Three subspecies are identified. A slender, long-legged antelope, the springbok reaches 71 to 86 cm (28 to 34 in) at the shoulder and weighs between 27 and 42 kg (60 and 93 lb). Both sexes have a pair of black, 35-to-50-centimetre (14 to 20 in) long horns that curve backward. The springbok is characterised by a white face, a dark stripe running from the eyes to the mouth, a light brown coat marked by a reddish brown stripe that runs from the upper foreleg to the buttocks across the flanks, and a white rump flap.<br />
<br />
Active mainly at dawn and dusk, springbok form harems (mixed-sex herds). In earlier times, springbok of the Kalahari desert and Karoo would migrate in large numbers across the countryside, a practice known as trekbokken. A feature unique to the springbok is pronking, in which the springbok performs multiple leaps into the air, up to 2 metres (6.6 ft) above the ground, in a stiff-legged posture, with the back bowed and the white flap lifted. Primarily a browser, the springbok feeds on shrubs and succulents; this antelope can live without drinking water for years, meeting its requirements through eating succulent vegetation. Breeding takes place year-round, and peaks in the rainy season, when forage is most abundant. A single calf is born after a five to six month long pregnancy; weaning occurs at nearly six months of age, and the calf leaves its mother a few months later.
    Springbok3.jpg
  • The guanaco (Lama guanicoe) is a camelid native to South America that stands between 1 and 1.2 metres (3 ft 3 in and 3 ft 11 in) at the shoulder and weighs about 90 kg (200 lb). The colour varies very little (unlike the domestic llama), ranging from a light brown to dark cinnamon and shading to white underneath. Guanacos have grey faces and small straight ears. The name guanaco comes from the South American language Quechua word wanaku (old spelling, huanaco). Young guanacos are called chulengo(s). These guanacos were photographed in Torres del Paine, Chile.
    _D3_3438.jpg
  • Lunar eclipse April 15, 2014.<br />
<br />
A lunar eclipse occurs when the Moon passes directly behind the Earth into its umbra (shadow). This can occur only when the Sun, Earth, and Moon are aligned (in "syzygy") exactly, or very closely so, with the Earth in the middle. Hence, a lunar eclipse can only occur the night of a full moon. The type and length of an eclipse depend upon the Moon's location relative to its orbital nodes.<br />
<br />
Unlike a solar eclipse, which can only be viewed from a certain relatively small area of the world, a lunar eclipse may be viewed from anywhere on the night side of the Earth. A lunar eclipse lasts for a few hours, whereas a total solar eclipse lasts for only a few minutes at any given place, due to the smaller size of the moon's shadow. Also unlike solar eclipses, lunar eclipses are safe to view without any eye protection or special precautions, as they are dimmer than the full moon.<br />
<br />
The Moon does not completely disappear as it passes through the umbra because of the refraction of sunlight by the Earth’s atmosphere into the shadow cone; if the Earth had no atmosphere, the Moon would be completely dark during an eclipse. The red coloring arises because sunlight reaching the Moon must pass through a long and dense layer of the Earth’s atmosphere, where it is scattered. Shorter wavelengths are more likely to be scattered by the air molecules and the small particles, and so by the time the light has passed through the atmosphere, the longer wavelengths dominate. This resulting light we perceive as red. This is the same effect that causes sunsets and sunrises to turn the sky a reddish color; an alternative way of considering the problem is to realize that, as viewed from the Moon, the Sun would appear to be setting (or rising) behind the Earth. Such a total eclipse of the moon is sometimes referred to as a blood moon.
    LunarEclipse1.jpg
  • Cattle drive through the Fort Worth Stockyards<br />
.....<br />
The Texas Longhorn is a breed of cattle known for its characteristic horns, which can extend to 7 ft tip to tip for steers and exceptional cows, and 36 to 80 in tip to tip for bulls. Similar cattle were imported by Spanish colonists into other parts of North America, including California and Florida. Horns can have a slight upward turn at their tips or even triple twist. Texas Longhorns are known for their diverse coloring. A longhorn can be any color or mix of colors but dark red and white color mixes are the most dominant. Texas Longhorns with elite genetics can often fetch $40,000 or more at auction with the record of $170,000 in recent history for a cow. Due to their innate gentle disposition and intelligence, Texas Longhorns are increasingly being trained as riding steers.
    TexasLonghorns1.jpg
  • Oppède is a commune in the Vaucluse department in the Provence-Alpes-Côte d'Azur region in southeastern France. Oppidum is the Latin word for 'town'. It is in fact two villages: Oppède-le-Vieux ("the old" in French), built against the Petit Luberon and dating back to the 12th century, and Oppède-les-Poulivets ("nice view" in Provençal), today known as "le village", down in the valley.<br />
<br />
The old village, built on a rocky hill, has narrow streets. In winter, the Petit Luberon starts casting its shadow early in the afternoon. Houses beyond the medieval ramparts are dark, humid and tricky to maintain. From below the village is dominated by the restored church of Notre-Dame-Dalidon and the ruins of the castle. In the 19th century, the inhabitants had enough and started to move down in the valley, dismantling the roof of their houses to stop paying property taxes.<br />
<br />
By the beginning of the 20th century, Oppède-le-Vieux was a ghost village and a new community was officially established in the valley, with larger streets, cosier houses and farmers closer to their fields.<br />
<br />
Following the armistice of June 1940, architect Bernard Zehrfuss founded a commune of artists in the old town, a project that attracted French sculptor François Stahly and the writer and artist Consuelo de Saint Exupéry. The commune proved short-lived. It was the basis for Saint Exupéry's fictionalized account, published in 1946, called "Kingdom of the Rocks".[2]
    OppedeLeVieux12.jpg
  • The guanaco (Lama guanicoe) is a camelid native to South America that stands between 1 and 1.2 metres (3 ft 3 in and 3 ft 11 in) at the shoulder and weighs about 90 kg (200 lb). The colour varies very little (unlike the domestic llama), ranging from a light brown to dark cinnamon and shading to white underneath. Guanacos have grey faces and small straight ears. The name guanaco comes from the South American language Quechua word wanaku (old spelling, huanaco). Young guanacos are called chulengo(s). These guanacos were photographed in Torres del Paine, Chile.
    _D3_3546.jpg
  • Monte Fitz Roy (also known as Cerro Chaltén, Cerro Fitz Roy, or simply Mount Fitz Roy) is a mountain located near El Chaltén village, in the Southern Patagonian Ice Field in Patagonia, on the border between Argentina and Chile. First climbed in 1952 by French alpinists Lionel Terray and Guido Magnone, it remains among the most technically challenging mountains on Earth for mountaineers. Monte Fitz Roy is the basis for the Patagonia clothing logo following Yvon Chouinard's ascent and subsequent film in 1968.
    MtFitzRoyRiver11.jpg
  • Monte Fitz Roy (also known as Cerro Chaltén, Cerro Fitz Roy, or simply Mount Fitz Roy) is a mountain located near El Chaltén village, in the Southern Patagonian Ice Field in Patagonia, on the border between Argentina and Chile. First climbed in 1952 by French alpinists Lionel Terray and Guido Magnone, it remains among the most technically challenging mountains on Earth for mountaineers. Monte Fitz Roy is the basis for the Patagonia clothing logo following Yvon Chouinard's ascent and subsequent film in 1968.
    MtFitzRoyRiver11.jpg
  • San Francisco, officially the City and County of San Francisco, is the cultural center and a leading financial hub of the San Francisco Bay Area and Northern California. The only consolidated city-county in California, San Francisco encompasses a land area of about 46.9 square miles on the northern end of the San Francisco Peninsula. It is the most densely settled large city in the state of California and the second-most densely populated major city in the United States after New York City. San Francisco is the fourth-most populous city in California, after Los Angeles, San Diego and San Jose, and the 14th-most populous city in the United States—with a Census-estimated 2013 population of 837,442. <br />
<br />
San Francisco (Spanish for "Saint Francis") was founded on June 29, 1776, when colonists from Spain established a fort at the Golden Gate and a mission named for St. Francis of Assisi a few miles away. The California Gold Rush of 1849 brought rapid growth, making it the largest city on the West Coast at the time. Due to the growth of its population, San Francisco became a consolidated city-county in 1856. After three-quarters of the city was destroyed by the 1906 earthquake and fire,[17] San Francisco was quickly rebuilt, hosting the Panama-Pacific International Exposition nine years later. During World War II, San Francisco was the port of embarkation for service members shipping out to the Pacific Theater.[18] After the war, the confluence of returning servicemen, massive immigration, liberalizing attitudes, along with the rise of the "hippie" counterculture, the Sexual Revolution, the Peace Movement growing from opposition to United States involvement in the Vietnam War, and other factors led to the Summer of Love and the gay rights movement, cementing San Francisco as a center of liberal activism in the United States.<br />
<br />
San Francisco is a popular tourist destination, known for its cool summers, fog, steep rolling hills, eclectic mix of architecture, and landmarks inc
    SanFranciscoMandarin2.jpg
  • Sunrise at Mount Rainier's Sunrise area with the White River below
    MtRainierSunriseFlower1-Dark-HDR-Edi...jpg
  • Sunrise at Mount Rainier's Sunrise area with the White River below
    MtRainierSunriseFlower1-Dark-HDR-Edi...jpg
  • Mount Baker reflecting in tarn near Park Butte in the Mount Baker Wilderness <br />
..... <br />
Mount Baker, also known as Koma Kulshan or simply Kulshan, is an active glaciated andesitic stratovolcano in the Cascade Volcanic Arc and the North Cascades of Washington State in the United States. Mount Baker has the second-most thermally active crater in the Cascade Range after Mount Saint Helens. About 31 miles due east of the city of Bellingham, Whatcom County, Mount Baker is the youngest volcano in the Mount Baker volcanic field. While volcanism has persisted here for some 1.5 million years, the current glaciated cone is likely no more than 140,000 years old, and possibly no older than 80-90,000 years. <br />
After Mount Rainier, Mount Baker is the most heavily glaciated of the Cascade Range volcanoes; the volume of snow and ice on Mount Baker, 0.43 cu mi is greater than that of all the other Cascades volcanoes (except Rainier) combined. At 10,781 ft, it is the third-highest mountain in Washington State and the fifth-highest in the Cascade Range, if Little Tahoma Peak, a subpeak of Mount Rainier, and Shastina, a subpeak of Mount Shasta, are not counted. Located in the Mount Baker Wilderness, it is visible from much of Greater Victoria, Greater Vancouver, and, to the south, from Seattle (and on clear days Tacoma) in Washington. <br />
Indigenous natives have known the mountain for thousands of years, but the first written record of the mountain is from the Spanish. Spanish explorer Gonzalo Lopez de Haro mapped it in 1790 as the Gran Montana del Carmelo, "Great Mount Carmel". The explorer George Vancouver renamed the mountain for 3rd Lieutenant Joseph Baker of HMS Discovery, who saw it on April 30, 1792.
    MountBakerParkButteTarn2-Dark-HDR.jpg
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