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  • The Atlanta Marriott Marquis is a Marriott hotel and the 14th tallest skyscraper in Atlanta, Georgia, United States. Designed by Atlanta architect John C. Portman, Jr., It is probably one of the most recognized buildings in the city. Construction was completed on the building in 1985, and because of its bulging base, it is often referred to as the "Pregnant Building".<br />
<br />
One of the defining features of the Marriott Marquis is its large atrium. It was the largest in the world upon its completion in 1985, at 470 feet (143 m) high. The atrium spans the entire height of the building and consists of two vertical chambers divided by elevator shafts and bridges.
    AtlantaMarriott2.jpg
  • The Atlanta Marriott Marquis is a Marriott hotel and the 14th tallest skyscraper in Atlanta, Georgia, United States. Designed by Atlanta architect John C. Portman, Jr., It is probably one of the most recognized buildings in the city. Construction was completed on the building in 1985, and because of its bulging base, it is often referred to as the "Pregnant Building".<br />
<br />
One of the defining features of the Marriott Marquis is its large atrium. It was the largest in the world upon its completion in 1985, at 470 feet (143 m) high. The atrium spans the entire height of the building and consists of two vertical chambers divided by elevator shafts and bridges.
    AtlantaMarriott1.jpg
  • Hoh Rainforest in Olympic National Park, in autumn
    HohLeavesAndMoss.jpg
  • Trinitatis Church is located in central Copenhagen, Denmark. It is part of the 17th century Trinitatis Complex, which includes the Rundetårn astronomical observatory tower and the Copenhagen University Library, in addition to the church. Built in the time of Christian IV, the church initially served the students of Copenhagen University. The interior was seriously damaged in the fire of 1728 but was rebuilt in 1731. The Rundetaarn, or Rundetårn (Round Tower in English), is a 17th-century tower located in central Copenhagen, Denmark. One of the many architectural projects of Christian IV, it was built as an astronomical observatory. It is most noted for its equestrian staircase, a 7.5-turn helical corridor leading to the top, and for the expansive views it affords over Copenhagen.
    CopenhagenTrinitatis1.jpg
  • Trinitatis Church is located in central Copenhagen, Denmark. It is part of the 17th century Trinitatis Complex, which includes the Rundetårn astronomical observatory tower and the Copenhagen University Library, in addition to the church. Built in the time of Christian IV, the church initially served the students of Copenhagen University. The interior was seriously damaged in the fire of 1728 but was rebuilt in 1731. The Rundetaarn, or Rundetårn (Round Tower in English), is a 17th-century tower located in central Copenhagen, Denmark. One of the many architectural projects of Christian IV, it was built as an astronomical observatory. It is most noted for its equestrian staircase, a 7.5-turn helical corridor leading to the top, and for the expansive views it affords over Copenhagen.
    CopenhagenTrinitatis2.jpg
  • Classroom in an old school in Dallas, Texas that was in use from 1888 to 1919.
    OldCityParkSchool2.jpg
  • The Palace of Versailles, or simply Versailles, is a royal château in Versailles in the Île-de-France region of France. In French it is the Château de Versailles.<br />
When the château was built, Versailles was a country village; today, however, it is a suburb of Paris, some 20 kilometres southwest of the French capital. The court of Versailles was the centre of political power in France from 1682, when Louis XIV moved from Paris, until the royal family was forced to return to the capital in October 1789 after the beginning of the French Revolution. Versailles is therefore famous not only as a building, but as a symbol of the system of absolute monarchy of the Ancien Régime.
    ParisVersaillesHallway1.jpg
  • The Owens–Thomas House & Slave Quarters is a historic home in Savannah, Georgia, that is operated as a historic house museum by Telfair Museums. It is located at 124 Abercorn Street, on the northeast corner of Oglethorpe Square. The Owens–Thomas House was designated a National Historic Landmark in 1976, as one of the nation's finest examples of English Regency architecture.<br />
<br />
Renovations in the 1990s uncovered and restored one of the oldest and best preserved urban slave quarters in the American South.
    OwensThomasHouse2.jpg
  • The Teatro Juarez is one of the most architectural stunning buildings in Guanajuato. Its main entrance is straight from ancient Rome while the flamboyant interior is oriental inspired. Teatro Juarez is regarded as one of Mexico's premier theaters. The initial construction of Teatro Juarez was started in 1872 based on the design by architect José Noriega. The theatre follows the neoclassical styling of eclecticism which was very popular within Mexico at the end of the 19th century. This design style was inspired by stories of ancient Rome and Greece and examples can be seen throughout the wondrous exterior. The rows of steps which lead up to the grand entrance with the 12 stately pillars so closely resembles the Pantheon of Rome. At the top of the roof stand 8 bronze statues from Greek mythology. The interior of the theatre was based on common European designs with four tiers of boxes and the stalls are based around a horseshoe shape. The theatre was inaugurated on the 27th of October 1903 by President Porfirio Diaz but the heyday of Teatro Juarez was a few years later between 1907 and 1910 when patrons would travel from all over the state to view the latest performances. During this period the Teatro Juarez was regarded as the most magnificent and prestigious theatre in the whole of Mexico. Since 1972 the Juarez Theater has been the focal point for the International Cervantes Festival.<br />
<br />
Guanajuato is a city and municipality in central Mexico and the capital of the state of the same name. It is part of the macroregion of Bajío. It is in a narrow valley, which makes its streets narrow and winding. Most are alleys that cars cannot pass through, and some are long sets of stairs up the mountainsides. Many of the city’s thoroughfares are partially or fully underground. The historic center has numerous small plazas and colonial-era mansions, churches and civil constructions built using pink or green sandstone.
    TeatroJuarezInterior1.jpg
  • The Teatro Juarez is one of the most architectural stunning buildings in Guanajuato. Its main entrance is straight from ancient Rome while the flamboyant interior is oriental inspired. Teatro Juarez is regarded as one of Mexico's premier theaters. The initial construction of Teatro Juarez was started in 1872 based on the design by architect José Noriega. The theatre follows the neoclassical styling of eclecticism which was very popular within Mexico at the end of the 19th century. This design style was inspired by stories of ancient Rome and Greece and examples can be seen throughout the wondrous exterior. The rows of steps which lead up to the grand entrance with the 12 stately pillars so closely resembles the Pantheon of Rome. At the top of the roof stand 8 bronze statues from Greek mythology. The interior of the theatre was based on common European designs with four tiers of boxes and the stalls are based around a horseshoe shape. The theatre was inaugurated on the 27th of October 1903 by President Porfirio Diaz but the heyday of Teatro Juarez was a few years later between 1907 and 1910 when patrons would travel from all over the state to view the latest performances. During this period the Teatro Juarez was regarded as the most magnificent and prestigious theatre in the whole of Mexico. Since 1972 the Juarez Theater has been the focal point for the International Cervantes Festival.<br />
<br />
Guanajuato is a city and municipality in central Mexico and the capital of the state of the same name. It is part of the macroregion of Bajío. It is in a narrow valley, which makes its streets narrow and winding. Most are alleys that cars cannot pass through, and some are long sets of stairs up the mountainsides. Many of the city’s thoroughfares are partially or fully underground. The historic center has numerous small plazas and colonial-era mansions, churches and civil constructions built using pink or green sandstone.
    TeatroJuarezInterior3.jpg
  • The Teatro Juarez is one of the most architectural stunning buildings in Guanajuato. Its main entrance is straight from ancient Rome while the flamboyant interior is oriental inspired. Teatro Juarez is regarded as one of Mexico's premier theaters. The initial construction of Teatro Juarez was started in 1872 based on the design by architect José Noriega. The theatre follows the neoclassical styling of eclecticism which was very popular within Mexico at the end of the 19th century. This design style was inspired by stories of ancient Rome and Greece and examples can be seen throughout the wondrous exterior. The rows of steps which lead up to the grand entrance with the 12 stately pillars so closely resembles the Pantheon of Rome. At the top of the roof stand 8 bronze statues from Greek mythology. The interior of the theatre was based on common European designs with four tiers of boxes and the stalls are based around a horseshoe shape. The theatre was inaugurated on the 27th of October 1903 by President Porfirio Diaz but the heyday of Teatro Juarez was a few years later between 1907 and 1910 when patrons would travel from all over the state to view the latest performances. During this period the Teatro Juarez was regarded as the most magnificent and prestigious theatre in the whole of Mexico. Since 1972 the Juarez Theater has been the focal point for the International Cervantes Festival.<br />
<br />
Guanajuato is a city and municipality in central Mexico and the capital of the state of the same name. It is part of the macroregion of Bajío. It is in a narrow valley, which makes its streets narrow and winding. Most are alleys that cars cannot pass through, and some are long sets of stairs up the mountainsides. Many of the city’s thoroughfares are partially or fully underground. The historic center has numerous small plazas and colonial-era mansions, churches and civil constructions built using pink or green sandstone.
    TeatroJuarezInterior4.jpg
  • The Teatro Juarez is one of the most architectural stunning buildings in Guanajuato. Its main entrance is straight from ancient Rome while the flamboyant interior is oriental inspired. Teatro Juarez is regarded as one of Mexico's premier theaters. The initial construction of Teatro Juarez was started in 1872 based on the design by architect José Noriega. The theatre follows the neoclassical styling of eclecticism which was very popular within Mexico at the end of the 19th century. This design style was inspired by stories of ancient Rome and Greece and examples can be seen throughout the wondrous exterior. The rows of steps which lead up to the grand entrance with the 12 stately pillars so closely resembles the Pantheon of Rome. At the top of the roof stand 8 bronze statues from Greek mythology. The interior of the theatre was based on common European designs with four tiers of boxes and the stalls are based around a horseshoe shape. The theatre was inaugurated on the 27th of October 1903 by President Porfirio Diaz but the heyday of Teatro Juarez was a few years later between 1907 and 1910 when patrons would travel from all over the state to view the latest performances. During this period the Teatro Juarez was regarded as the most magnificent and prestigious theatre in the whole of Mexico. Since 1972 the Juarez Theater has been the focal point for the International Cervantes Festival.<br />
<br />
Guanajuato is a city and municipality in central Mexico and the capital of the state of the same name. It is part of the macroregion of Bajío. It is in a narrow valley, which makes its streets narrow and winding. Most are alleys that cars cannot pass through, and some are long sets of stairs up the mountainsides. Many of the city’s thoroughfares are partially or fully underground. The historic center has numerous small plazas and colonial-era mansions, churches and civil constructions built using pink or green sandstone.
    TeatroJuarezInterior2.jpg
  • The Papal Basilica of Saint Peter, officially known in Italian as the Basilica Papale di San Pietro in Vaticano and commonly known as St. Peter's Basilica, is a Late Renaissance church located within the Vatican City.
    RomeStPetersDome1.jpg
  • Villa Cimbrone is a historic building in Ravello, on the Amalfi coast of southern Italy. Dating from at least the 11th century AD, it is famous for its scenic belvedere, the Terrazzo dell'lnfinito (the Terrace of Infinity).<br />
<br />
Much altered and extended in the early twentieth century by Ernest William Beckett (later Lord Grimthorpe), the villa is today composed of many salvaged architectural elements from other parts of Italy and elsewhere; little of the original structure remains visible.<br />
<br />
The gardens were redeveloped by Beckett at the same time. The villa is now a hotel, its gardens open to the public.
    VillaCimbrone2.jpg
  • Amalfi Cathedral (Italian: Duomo di Amalfi; Cattedrale di Sant'Andrea) is a 9th-century Roman Catholic cathedral in the Piazza del Duomo, Amalfi, Italy. It is dedicated to the Apostle Saint Andrew whose relics are kept here. Formerly the episcopal seat of the Diocese of Amalfi, it has been since 1986 that of the Diocese of Amalfi-Cava de' Tirreni.<br />
<br />
Predominantly of Arab-Norman Romanesque[citation needed] architectural style, it has been remodeled several times, adding Romanesque, Byzantine, Gothic, and Baroque elements. The cathedral includes the adjoining 9th-century Basilica of the Crucifix. Leading from the basilica are steps into the Crypt of St. Andrew
    AmalfiCathedral3.jpg
  • Amalfi Cathedral (Italian: Duomo di Amalfi; Cattedrale di Sant'Andrea) is a 9th-century Roman Catholic cathedral in the Piazza del Duomo, Amalfi, Italy. It is dedicated to the Apostle Saint Andrew whose relics are kept here. Formerly the episcopal seat of the Diocese of Amalfi, it has been since 1986 that of the Diocese of Amalfi-Cava de' Tirreni.<br />
<br />
Predominantly of Arab-Norman Romanesque[citation needed] architectural style, it has been remodeled several times, adding Romanesque, Byzantine, Gothic, and Baroque elements. The cathedral includes the adjoining 9th-century Basilica of the Crucifix. Leading from the basilica are steps into the Crypt of St. Andrew
    AmalfiCathedral2.jpg
  • Amalfi Cathedral (Italian: Duomo di Amalfi; Cattedrale di Sant'Andrea) is a 9th-century Roman Catholic cathedral in the Piazza del Duomo, Amalfi, Italy. It is dedicated to the Apostle Saint Andrew whose relics are kept here. Formerly the episcopal seat of the Diocese of Amalfi, it has been since 1986 that of the Diocese of Amalfi-Cava de' Tirreni.<br />
<br />
Predominantly of Arab-Norman Romanesque[citation needed] architectural style, it has been remodeled several times, adding Romanesque, Byzantine, Gothic, and Baroque elements. The cathedral includes the adjoining 9th-century Basilica of the Crucifix. Leading from the basilica are steps into the Crypt of St. Andrew
    AmalfiCathedral1.jpg
  • Trinitatis Church is located in central Copenhagen, Denmark. It is part of the 17th century Trinitatis Complex, which includes the Rundetårn astronomical observatory tower and the Copenhagen University Library, in addition to the church. Built in the time of Christian IV, the church initially served the students of Copenhagen University. The interior was seriously damaged in the fire of 1728 but was rebuilt in 1731. The Rundetaarn, or Rundetårn (Round Tower in English), is a 17th-century tower located in central Copenhagen, Denmark. One of the many architectural projects of Christian IV, it was built as an astronomical observatory. It is most noted for its equestrian staircase, a 7.5-turn helical corridor leading to the top, and for the expansive views it affords over Copenhagen.
    CopenhagenTrinitatis2.jpg
  • Trinitatis Church is located in central Copenhagen, Denmark. It is part of the 17th century Trinitatis Complex, which includes the Rundetårn astronomical observatory tower and the Copenhagen University Library, in addition to the church. Built in the time of Christian IV, the church initially served the students of Copenhagen University. The interior was seriously damaged in the fire of 1728 but was rebuilt in 1731. The Rundetaarn, or Rundetårn (Round Tower in English), is a 17th-century tower located in central Copenhagen, Denmark. One of the many architectural projects of Christian IV, it was built as an astronomical observatory. It is most noted for its equestrian staircase, a 7.5-turn helical corridor leading to the top, and for the expansive views it affords over Copenhagen.
    CopenhagenTrinitatis1.jpg
  • Villa Cimbrone is a historic building in Ravello, on the Amalfi coast of southern Italy. Dating from at least the 11th century AD, it is famous for its scenic belvedere, the Terrazzo dell'lnfinito (the Terrace of Infinity).<br />
<br />
Much altered and extended in the early twentieth century by Ernest William Beckett (later Lord Grimthorpe), the villa is today composed of many salvaged architectural elements from other parts of Italy and elsewhere; little of the original structure remains visible.<br />
<br />
The gardens were redeveloped by Beckett at the same time. The villa is now a hotel, its gardens open to the public.
    VillaCimbrone4.jpg
  • The Bullock Texas State History Museum, is a history museum in Austin, Texas. The museum is a division of the Texas State Preservation Board. Its stated mission is to tell "the Story of Texas." The history museum is named after former Texas Lieutenant Governor Bob Bullock, who championed its creation. The museum is located at 1800 North Congress Avenue in Austin, a few blocks north of the Texas State Capitol. The museum has three floors of interactive exhibits; the first floor theme is "land," the second floor theme "identity," and the third floor theme "opportunity." On the second floor of the museum, 'The Spirit Theater' host a feature presentation entitled 'Star of Destiny.' Designed by award winning experience designer Bob Rogers (designer) and the design team BRC Imagination Arts, the special effects theater presentation takes audiences on an epic journey through the history of Texas, narrated by the character of Sam Houston. In addition to playing several shows, daily, the 200 seat Texas Spirit Theater is also used by the museum as a multimedia special effects theater for alternate film and lecture presentations The museum also has a 70mm film-based IMAX theater. The theater seats 400 and has a projector with both 2-D and 3-D capability.
    AustinHistoryMuseum2.jpg
  • The Bullock Texas State History Museum, is a history museum in Austin, Texas. The museum is a division of the Texas State Preservation Board. Its stated mission is to tell "the Story of Texas." The history museum is named after former Texas Lieutenant Governor Bob Bullock, who championed its creation. The museum is located at 1800 North Congress Avenue in Austin, a few blocks north of the Texas State Capitol. The museum has three floors of interactive exhibits; the first floor theme is "land," the second floor theme "identity," and the third floor theme "opportunity." On the second floor of the museum, 'The Spirit Theater' host a feature presentation entitled 'Star of Destiny.' Designed by award winning experience designer Bob Rogers (designer) and the design team BRC Imagination Arts, the special effects theater presentation takes audiences on an epic journey through the history of Texas, narrated by the character of Sam Houston. In addition to playing several shows, daily, the 200 seat Texas Spirit Theater is also used by the museum as a multimedia special effects theater for alternate film and lecture presentations The museum also has a 70mm film-based IMAX theater. The theater seats 400 and has a projector with both 2-D and 3-D capability.
    AustinHistoryMuseum1.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
  • The Royal Palace of Madrid (Spanish: Palacio Real de Madrid) is the official residence of the Spanish royal family at the city of Madrid, although now only used for state ceremonies. The palace has 135,000 square meters of floor space and contains 3,418 rooms. It is the largest functioning royal palace and the largest by floor area in Europe. King Felipe VI and the royal family do not reside in the palace, choosing instead the significantly more modest Palace of Zarzuela on the outskirts of Madrid. The palace is owned by the Spanish state and administered by the Patrimonio Nacional, a public agency of the Ministry of the Presidency. <br />
<br />
The palace is located on the site of a 9th-century Alcázar ("Muslim-era fortress"), near the town of Magerit, constructed as an outpost by Muhammad I of Córdoba and inherited after 1036 by the independent Moorish Taifa of Toledo. After Madrid fell to King Alfonso VI of Castile in 1083, the edifice was only rarely used by the kings of Castile. In 1329, King Alfonso XI of Castile convened the cortes of Madrid for the first time. King Felipe II moved his court to Madrid in 1561. The old Alcázar was built on the location in the 16th century. After it burned 24 December 1734, King Felipe V ordered a new palace built on the same site. Construction spanned the years 1738 to 1755 and followed a Berniniesque design by Filippo Juvarra and Giovanni Battista Sacchetti in cooperation with Ventura Rodríguez, Francesco Sabatini, and Martín Sarmiento. King Carlos III first occupied the new palace in 1764.<br />
<br />
The interior of the palace is notable for its wealth of art and the use of many types of fine materials in the construction and the decoration of its rooms. It includes paintings by artists such as Caravaggio, Juan de Flandes, Francisco de Goya, and Velázquez, and frescoes by Giovanni Battista Tiepolo, Corrado Giaquinto, and Anton Raphael Mengs. Other collections of great historical and artistic importance preserved in the building include the
    MadridPalacioReal4.jpg
  • The Royal Palace of Madrid (Spanish: Palacio Real de Madrid) is the official residence of the Spanish royal family at the city of Madrid, although now only used for state ceremonies. The palace has 135,000 square meters of floor space and contains 3,418 rooms. It is the largest functioning royal palace and the largest by floor area in Europe. King Felipe VI and the royal family do not reside in the palace, choosing instead the significantly more modest Palace of Zarzuela on the outskirts of Madrid. The palace is owned by the Spanish state and administered by the Patrimonio Nacional, a public agency of the Ministry of the Presidency. <br />
<br />
The palace is located on the site of a 9th-century Alcázar ("Muslim-era fortress"), near the town of Magerit, constructed as an outpost by Muhammad I of Córdoba and inherited after 1036 by the independent Moorish Taifa of Toledo. After Madrid fell to King Alfonso VI of Castile in 1083, the edifice was only rarely used by the kings of Castile. In 1329, King Alfonso XI of Castile convened the cortes of Madrid for the first time. King Felipe II moved his court to Madrid in 1561. The old Alcázar was built on the location in the 16th century. After it burned 24 December 1734, King Felipe V ordered a new palace built on the same site. Construction spanned the years 1738 to 1755 and followed a Berniniesque design by Filippo Juvarra and Giovanni Battista Sacchetti in cooperation with Ventura Rodríguez, Francesco Sabatini, and Martín Sarmiento. King Carlos III first occupied the new palace in 1764.<br />
<br />
The interior of the palace is notable for its wealth of art and the use of many types of fine materials in the construction and the decoration of its rooms. It includes paintings by artists such as Caravaggio, Juan de Flandes, Francisco de Goya, and Velázquez, and frescoes by Giovanni Battista Tiepolo, Corrado Giaquinto, and Anton Raphael Mengs. Other collections of great historical and artistic importance preserved in the building include the
    MadridPalacioReal1.jpg
  • The Royal Palace of Madrid (Spanish: Palacio Real de Madrid) is the official residence of the Spanish royal family at the city of Madrid, although now only used for state ceremonies. The palace has 135,000 square meters of floor space and contains 3,418 rooms. It is the largest functioning royal palace and the largest by floor area in Europe. King Felipe VI and the royal family do not reside in the palace, choosing instead the significantly more modest Palace of Zarzuela on the outskirts of Madrid. The palace is owned by the Spanish state and administered by the Patrimonio Nacional, a public agency of the Ministry of the Presidency. <br />
<br />
The palace is located on the site of a 9th-century Alcázar ("Muslim-era fortress"), near the town of Magerit, constructed as an outpost by Muhammad I of Córdoba and inherited after 1036 by the independent Moorish Taifa of Toledo. After Madrid fell to King Alfonso VI of Castile in 1083, the edifice was only rarely used by the kings of Castile. In 1329, King Alfonso XI of Castile convened the cortes of Madrid for the first time. King Felipe II moved his court to Madrid in 1561. The old Alcázar was built on the location in the 16th century. After it burned 24 December 1734, King Felipe V ordered a new palace built on the same site. Construction spanned the years 1738 to 1755 and followed a Berniniesque design by Filippo Juvarra and Giovanni Battista Sacchetti in cooperation with Ventura Rodríguez, Francesco Sabatini, and Martín Sarmiento. King Carlos III first occupied the new palace in 1764.<br />
<br />
The interior of the palace is notable for its wealth of art and the use of many types of fine materials in the construction and the decoration of its rooms. It includes paintings by artists such as Caravaggio, Juan de Flandes, Francisco de Goya, and Velázquez, and frescoes by Giovanni Battista Tiepolo, Corrado Giaquinto, and Anton Raphael Mengs. Other collections of great historical and artistic importance preserved in the building include the
    MadridPalacioReal7.jpg
  • The Royal Palace of Madrid (Spanish: Palacio Real de Madrid) is the official residence of the Spanish royal family at the city of Madrid, although now only used for state ceremonies. The palace has 135,000 square meters of floor space and contains 3,418 rooms. It is the largest functioning royal palace and the largest by floor area in Europe. King Felipe VI and the royal family do not reside in the palace, choosing instead the significantly more modest Palace of Zarzuela on the outskirts of Madrid. The palace is owned by the Spanish state and administered by the Patrimonio Nacional, a public agency of the Ministry of the Presidency. <br />
<br />
The palace is located on the site of a 9th-century Alcázar ("Muslim-era fortress"), near the town of Magerit, constructed as an outpost by Muhammad I of Córdoba and inherited after 1036 by the independent Moorish Taifa of Toledo. After Madrid fell to King Alfonso VI of Castile in 1083, the edifice was only rarely used by the kings of Castile. In 1329, King Alfonso XI of Castile convened the cortes of Madrid for the first time. King Felipe II moved his court to Madrid in 1561. The old Alcázar was built on the location in the 16th century. After it burned 24 December 1734, King Felipe V ordered a new palace built on the same site. Construction spanned the years 1738 to 1755 and followed a Berniniesque design by Filippo Juvarra and Giovanni Battista Sacchetti in cooperation with Ventura Rodríguez, Francesco Sabatini, and Martín Sarmiento. King Carlos III first occupied the new palace in 1764.<br />
<br />
The interior of the palace is notable for its wealth of art and the use of many types of fine materials in the construction and the decoration of its rooms. It includes paintings by artists such as Caravaggio, Juan de Flandes, Francisco de Goya, and Velázquez, and frescoes by Giovanni Battista Tiepolo, Corrado Giaquinto, and Anton Raphael Mengs. Other collections of great historical and artistic importance preserved in the building include the
    MadridPalacioReal3.jpg
  • The Royal Palace of Madrid (Spanish: Palacio Real de Madrid) is the official residence of the Spanish royal family at the city of Madrid, although now only used for state ceremonies. The palace has 135,000 square meters of floor space and contains 3,418 rooms. It is the largest functioning royal palace and the largest by floor area in Europe. King Felipe VI and the royal family do not reside in the palace, choosing instead the significantly more modest Palace of Zarzuela on the outskirts of Madrid. The palace is owned by the Spanish state and administered by the Patrimonio Nacional, a public agency of the Ministry of the Presidency. <br />
<br />
The palace is located on the site of a 9th-century Alcázar ("Muslim-era fortress"), near the town of Magerit, constructed as an outpost by Muhammad I of Córdoba and inherited after 1036 by the independent Moorish Taifa of Toledo. After Madrid fell to King Alfonso VI of Castile in 1083, the edifice was only rarely used by the kings of Castile. In 1329, King Alfonso XI of Castile convened the cortes of Madrid for the first time. King Felipe II moved his court to Madrid in 1561. The old Alcázar was built on the location in the 16th century. After it burned 24 December 1734, King Felipe V ordered a new palace built on the same site. Construction spanned the years 1738 to 1755 and followed a Berniniesque design by Filippo Juvarra and Giovanni Battista Sacchetti in cooperation with Ventura Rodríguez, Francesco Sabatini, and Martín Sarmiento. King Carlos III first occupied the new palace in 1764.<br />
<br />
The interior of the palace is notable for its wealth of art and the use of many types of fine materials in the construction and the decoration of its rooms. It includes paintings by artists such as Caravaggio, Juan de Flandes, Francisco de Goya, and Velázquez, and frescoes by Giovanni Battista Tiepolo, Corrado Giaquinto, and Anton Raphael Mengs. Other collections of great historical and artistic importance preserved in the building include the
    MadridPalacioReal2.jpg
  • The Royal Palace of Madrid (Spanish: Palacio Real de Madrid) is the official residence of the Spanish royal family at the city of Madrid, although now only used for state ceremonies. The palace has 135,000 square meters of floor space and contains 3,418 rooms. It is the largest functioning royal palace and the largest by floor area in Europe. King Felipe VI and the royal family do not reside in the palace, choosing instead the significantly more modest Palace of Zarzuela on the outskirts of Madrid. The palace is owned by the Spanish state and administered by the Patrimonio Nacional, a public agency of the Ministry of the Presidency. <br />
<br />
The palace is located on the site of a 9th-century Alcázar ("Muslim-era fortress"), near the town of Magerit, constructed as an outpost by Muhammad I of Córdoba and inherited after 1036 by the independent Moorish Taifa of Toledo. After Madrid fell to King Alfonso VI of Castile in 1083, the edifice was only rarely used by the kings of Castile. In 1329, King Alfonso XI of Castile convened the cortes of Madrid for the first time. King Felipe II moved his court to Madrid in 1561. The old Alcázar was built on the location in the 16th century. After it burned 24 December 1734, King Felipe V ordered a new palace built on the same site. Construction spanned the years 1738 to 1755 and followed a Berniniesque design by Filippo Juvarra and Giovanni Battista Sacchetti in cooperation with Ventura Rodríguez, Francesco Sabatini, and Martín Sarmiento. King Carlos III first occupied the new palace in 1764.<br />
<br />
The interior of the palace is notable for its wealth of art and the use of many types of fine materials in the construction and the decoration of its rooms. It includes paintings by artists such as Caravaggio, Juan de Flandes, Francisco de Goya, and Velázquez, and frescoes by Giovanni Battista Tiepolo, Corrado Giaquinto, and Anton Raphael Mengs. Other collections of great historical and artistic importance preserved in the building include the
    MadridPalacioReal6.jpg
  • The Royal Palace of Madrid (Spanish: Palacio Real de Madrid) is the official residence of the Spanish royal family at the city of Madrid, although now only used for state ceremonies. The palace has 135,000 square meters of floor space and contains 3,418 rooms. It is the largest functioning royal palace and the largest by floor area in Europe. King Felipe VI and the royal family do not reside in the palace, choosing instead the significantly more modest Palace of Zarzuela on the outskirts of Madrid. The palace is owned by the Spanish state and administered by the Patrimonio Nacional, a public agency of the Ministry of the Presidency. <br />
<br />
The palace is located on the site of a 9th-century Alcázar ("Muslim-era fortress"), near the town of Magerit, constructed as an outpost by Muhammad I of Córdoba and inherited after 1036 by the independent Moorish Taifa of Toledo. After Madrid fell to King Alfonso VI of Castile in 1083, the edifice was only rarely used by the kings of Castile. In 1329, King Alfonso XI of Castile convened the cortes of Madrid for the first time. King Felipe II moved his court to Madrid in 1561. The old Alcázar was built on the location in the 16th century. After it burned 24 December 1734, King Felipe V ordered a new palace built on the same site. Construction spanned the years 1738 to 1755 and followed a Berniniesque design by Filippo Juvarra and Giovanni Battista Sacchetti in cooperation with Ventura Rodríguez, Francesco Sabatini, and Martín Sarmiento. King Carlos III first occupied the new palace in 1764.<br />
<br />
The interior of the palace is notable for its wealth of art and the use of many types of fine materials in the construction and the decoration of its rooms. It includes paintings by artists such as Caravaggio, Juan de Flandes, Francisco de Goya, and Velázquez, and frescoes by Giovanni Battista Tiepolo, Corrado Giaquinto, and Anton Raphael Mengs. Other collections of great historical and artistic importance preserved in the building include the
    MadridPalacioReal5.jpg
  • El Capitan is a peak in Culberson County, Texas, United States, within Guadalupe Mountains National Park. It is the eighth highest peak in Texas, and rises abruptly out of the Chihuahuan Desert floor; it is considered the "signature peak" of West Texas.
    GuadalupeElCapitan4.jpg
  • The Maroon Bells are two peaks in the Elk Mountains, Maroon Peak and North Maroon Peak, separated by about a third of a mile. The mountains are about 12 miles southwest of Aspen. Both peaks are fourteeners. Maroon Peak, at 14,156 feet, is the 27th highest peak in Colorado; North Maroon Peak, at 14,014 feet, is the 50th highest. The view of the Maroon Bells to the southwest from the Maroon Creek valley is one of the most famous scenes in Colorado, and is reputed to be the "most-photographed spot in Colorado" and one of Colorado's premier scenic overlooks. The peaks are located in the Maroon Bells-Snowmass Wilderness of White River National Forest.<br />
<br />
A US Forest Service sign on the access trail refers to these mountains as "The Deadly Bells" and warns would-be climbers of "downsloping, loose, rotten and unstable" rock that "kills without warning". Unlike other mountains in the Rockies that are composed of granite and limestone, the Bells are composed of metamorphic sedimentary mudstone that has hardened into rock over millions of years. Mudstone is weak and fractures readily, giving rise to dangerously loose rock along almost any route. The mudstone is responsible for the Bells' distinctive maroon color. The Bells got their "deadly" name in 1965 when eight people died in five separate accidents.<br />
<br />
Maroon Lake (9,580') occupies a basin that was sculpted by Ice-Age glaciers and later dammed by landslide and rockfall debris from the steep slopes above the valley floor.
    MaroonBells3.jpg
  • 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
  • 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
  • The Maroon Bells are two peaks in the Elk Mountains, Maroon Peak and North Maroon Peak, separated by about a third of a mile. The mountains are about 12 miles southwest of Aspen. Both peaks are fourteeners. Maroon Peak, at 14,156 feet, is the 27th highest peak in Colorado; North Maroon Peak, at 14,014 feet, is the 50th highest. The view of the Maroon Bells to the southwest from the Maroon Creek valley is one of the most famous scenes in Colorado, and is reputed to be the "most-photographed spot in Colorado" and one of Colorado's premier scenic overlooks. The peaks are located in the Maroon Bells-Snowmass Wilderness of White River National Forest.<br />
<br />
A US Forest Service sign on the access trail refers to these mountains as "The Deadly Bells" and warns would-be climbers of "downsloping, loose, rotten and unstable" rock that "kills without warning". Unlike other mountains in the Rockies that are composed of granite and limestone, the Bells are composed of metamorphic sedimentary mudstone that has hardened into rock over millions of years. Mudstone is weak and fractures readily, giving rise to dangerously loose rock along almost any route. The mudstone is responsible for the Bells' distinctive maroon color. The Bells got their "deadly" name in 1965 when eight people died in five separate accidents.<br />
<br />
Maroon Lake (9,580') occupies a basin that was sculpted by Ice-Age glaciers and later dammed by landslide and rockfall debris from the steep slopes above the valley floor.
    MaroonBells6.jpg
  • The Maroon Bells are two peaks in the Elk Mountains, Maroon Peak and North Maroon Peak, separated by about a third of a mile. The mountains are about 12 miles southwest of Aspen. Both peaks are fourteeners. Maroon Peak, at 14,156 feet, is the 27th highest peak in Colorado; North Maroon Peak, at 14,014 feet, is the 50th highest. The view of the Maroon Bells to the southwest from the Maroon Creek valley is one of the most famous scenes in Colorado, and is reputed to be the "most-photographed spot in Colorado" and one of Colorado's premier scenic overlooks. The peaks are located in the Maroon Bells-Snowmass Wilderness of White River National Forest.<br />
<br />
A US Forest Service sign on the access trail refers to these mountains as "The Deadly Bells" and warns would-be climbers of "downsloping, loose, rotten and unstable" rock that "kills without warning". Unlike other mountains in the Rockies that are composed of granite and limestone, the Bells are composed of metamorphic sedimentary mudstone that has hardened into rock over millions of years. Mudstone is weak and fractures readily, giving rise to dangerously loose rock along almost any route. The mudstone is responsible for the Bells' distinctive maroon color. The Bells got their "deadly" name in 1965 when eight people died in five separate accidents.<br />
<br />
Maroon Lake (9,580') occupies a basin that was sculpted by Ice-Age glaciers and later dammed by landslide and rockfall debris from the steep slopes above the valley floor.
    MaroonBells3.jpg
  • The Maroon Bells are two peaks in the Elk Mountains, Maroon Peak and North Maroon Peak, separated by about a third of a mile. The mountains are about 12 miles southwest of Aspen. Both peaks are fourteeners. Maroon Peak, at 14,156 feet, is the 27th highest peak in Colorado; North Maroon Peak, at 14,014 feet, is the 50th highest. The view of the Maroon Bells to the southwest from the Maroon Creek valley is one of the most famous scenes in Colorado, and is reputed to be the "most-photographed spot in Colorado" and one of Colorado's premier scenic overlooks. The peaks are located in the Maroon Bells-Snowmass Wilderness of White River National Forest.<br />
<br />
A US Forest Service sign on the access trail refers to these mountains as "The Deadly Bells" and warns would-be climbers of "downsloping, loose, rotten and unstable" rock that "kills without warning". Unlike other mountains in the Rockies that are composed of granite and limestone, the Bells are composed of metamorphic sedimentary mudstone that has hardened into rock over millions of years. Mudstone is weak and fractures readily, giving rise to dangerously loose rock along almost any route. The mudstone is responsible for the Bells' distinctive maroon color. The Bells got their "deadly" name in 1965 when eight people died in five separate accidents.<br />
<br />
Maroon Lake (9,580') occupies a basin that was sculpted by Ice-Age glaciers and later dammed by landslide and rockfall debris from the steep slopes above the valley floor.
    MaroonBells1.jpg
  • The Maroon Bells are two peaks in the Elk Mountains, Maroon Peak and North Maroon Peak, separated by about a third of a mile. The mountains are about 12 miles southwest of Aspen. Both peaks are fourteeners. Maroon Peak, at 14,156 feet, is the 27th highest peak in Colorado; North Maroon Peak, at 14,014 feet, is the 50th highest. The view of the Maroon Bells to the southwest from the Maroon Creek valley is one of the most famous scenes in Colorado, and is reputed to be the "most-photographed spot in Colorado" and one of Colorado's premier scenic overlooks. The peaks are located in the Maroon Bells-Snowmass Wilderness of White River National Forest.<br />
<br />
A US Forest Service sign on the access trail refers to these mountains as "The Deadly Bells" and warns would-be climbers of "downsloping, loose, rotten and unstable" rock that "kills without warning". Unlike other mountains in the Rockies that are composed of granite and limestone, the Bells are composed of metamorphic sedimentary mudstone that has hardened into rock over millions of years. Mudstone is weak and fractures readily, giving rise to dangerously loose rock along almost any route. The mudstone is responsible for the Bells' distinctive maroon color. The Bells got their "deadly" name in 1965 when eight people died in five separate accidents.<br />
<br />
Maroon Lake (9,580') occupies a basin that was sculpted by Ice-Age glaciers and later dammed by landslide and rockfall debris from the steep slopes above the valley floor.
    MaroonBells5.jpg
  • 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 />
<br />
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 />
<br />
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 />
<br />
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.
    DeathValleyBush.jpg
  • The Maroon Bells are two peaks in the Elk Mountains, Maroon Peak and North Maroon Peak, separated by about a third of a mile. The mountains are about 12 miles southwest of Aspen. Both peaks are fourteeners. Maroon Peak, at 14,156 feet, is the 27th highest peak in Colorado; North Maroon Peak, at 14,014 feet, is the 50th highest. The view of the Maroon Bells to the southwest from the Maroon Creek valley is one of the most famous scenes in Colorado, and is reputed to be the "most-photographed spot in Colorado" and one of Colorado's premier scenic overlooks. The peaks are located in the Maroon Bells-Snowmass Wilderness of White River National Forest.<br />
<br />
A US Forest Service sign on the access trail refers to these mountains as "The Deadly Bells" and warns would-be climbers of "downsloping, loose, rotten and unstable" rock that "kills without warning". Unlike other mountains in the Rockies that are composed of granite and limestone, the Bells are composed of metamorphic sedimentary mudstone that has hardened into rock over millions of years. Mudstone is weak and fractures readily, giving rise to dangerously loose rock along almost any route. The mudstone is responsible for the Bells' distinctive maroon color. The Bells got their "deadly" name in 1965 when eight people died in five separate accidents.<br />
<br />
Maroon Lake (9,580') occupies a basin that was sculpted by Ice-Age glaciers and later dammed by landslide and rockfall debris from the steep slopes above the valley floor.
    MaroonBells1.jpg
  • The Boston Public Library McKim Building (built 1895) in Copley Square contains the library's research collection, exhibition rooms and administrative offices. When it opened in 1895, the new Boston Public Library was proclaimed a "palace for the people." The building includes lavish decorations, a children's room (the first in the nation), and a central courtyard surrounded by an arcaded gallery in the manner of a Renaissance cloister. The library regularly displays its rare works, often in exhibits that will combine works on paper, rare books, and works of art. Several galleries in the third floor of the McKim building are maintained for exhibits.
    BostonPublicLibrary2.jpg
  • Monument Valley (Navajo: Tsé Biiʼ Ndzisgaii, meaning valley of the rocks) is a region of the Colorado Plateau characterized by a cluster of vast sandstone buttes, the largest reaching 1,000 ft above the valley floor. It is located on the Arizona-Utah state line, near the Four Corners area. The valley lies within the range of the Navajo Nation Reservation and is accessible from U.S. Highway 163. 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."
    Highway163-Alt2.jpg
  • El Capitan is a peak in Culberson County, Texas, United States, within Guadalupe Mountains National Park. It is the eighth highest peak in Texas, and rises abruptly out of the Chihuahuan Desert floor; it is considered the "signature peak" of West Texas.
    GuadalupeElCapitan4.jpg
  • El Capitan is a peak in Culberson County, Texas, United States, within Guadalupe Mountains National Park. It is the eighth highest peak in Texas, and rises abruptly out of the Chihuahuan Desert floor; it is considered the "signature peak" of West Texas.
    GuadalupeElCapitan4.jpg
  • El Capitan is a peak in Culberson County, Texas, United States, within Guadalupe Mountains National Park. It is the eighth highest peak in Texas, and rises abruptly out of the Chihuahuan Desert floor; it is considered the "signature peak" of West Texas.
    GuadalupeElCapitan3-Blend.jpg
  • El Capitan is a peak in Culberson County, Texas, United States, within Guadalupe Mountains National Park. It is the eighth highest peak in Texas, and rises abruptly out of the Chihuahuan Desert floor; it is considered the "signature peak" of West Texas.
    GuadalupeElCapitan3.jpg
  • El Capitan is a peak in Culberson County, Texas, United States, within Guadalupe Mountains National Park. It is the eighth highest peak in Texas, and rises abruptly out of the Chihuahuan Desert floor; it is considered the "signature peak" of West Texas.
    GuadalupeElCapitan2.jpg
  • El Capitan is a peak in Culberson County, Texas, United States, within Guadalupe Mountains National Park. It is the eighth highest peak in Texas, and rises abruptly out of the Chihuahuan Desert floor; it is considered the "signature peak" of West Texas.
    GuadalupeElCapitan3-Blend.jpg
  • The Dordogne (French: La Dordogne) is a river in south-central and southwest France. The Dordogne and its watershed were designated Biosphere Reserve by UNESCO on July 11 2012. The river rises on the flanks of the Puy de Sancy in the mountains of Auvergne, from the confluence of two small torrents above the town of Le Mont-Dore: the Dore and the Dogne. It flows generally west through the Limousin and Périgord regions before flowing into the Gironde, its common estuary with the Garonne, at the Bec d'Ambès ("Ambès beak"), north of the city of Bordeaux. The Dordogne is one of the few rivers in the world that exhibit the phenomenon of a tidal bore, known as a mascaret.<br />
<br />
The upper valley of the Dordogne is a series of deep gorges. The cliffs, steep banks, fast flowing water and high bridges attract both walkers and drivers. In several places the river is dammed to form long, deep lakes. Camp sites and holiday homes have proliferated wherever the valley floor is wide enough to accommodate them.<br />
<br />
Below Argentat and around Beaulieu-sur-Dordogne, the valley widens to accommodate fertile farmland, well-watered pasture and orchards. In the towns, which are major tourist attractions because of their history and architecture, the quaysides are lined with eating and drinking places. In Périgord, the valley widens further to encompass one of France's main gastronomic regions, with vineyards, poultry farms and truffle-rich woodlands.
    Beynac7.jpg
  • The Maroon Bells are two peaks in the Elk Mountains, Maroon Peak and North Maroon Peak, separated by about a third of a mile. The mountains are about 12 miles southwest of Aspen. Both peaks are fourteeners. Maroon Peak, at 14,156 feet, is the 27th highest peak in Colorado; North Maroon Peak, at 14,014 feet, is the 50th highest. The view of the Maroon Bells to the southwest from the Maroon Creek valley is one of the most famous scenes in Colorado, and is reputed to be the "most-photographed spot in Colorado" and one of Colorado's premier scenic overlooks. The peaks are located in the Maroon Bells-Snowmass Wilderness of White River National Forest.<br />
<br />
A US Forest Service sign on the access trail refers to these mountains as "The Deadly Bells" and warns would-be climbers of "downsloping, loose, rotten and unstable" rock that "kills without warning". Unlike other mountains in the Rockies that are composed of granite and limestone, the Bells are composed of metamorphic sedimentary mudstone that has hardened into rock over millions of years. Mudstone is weak and fractures readily, giving rise to dangerously loose rock along almost any route. The mudstone is responsible for the Bells' distinctive maroon color. The Bells got their "deadly" name in 1965 when eight people died in five separate accidents.<br />
<br />
Maroon Lake (9,580') occupies a basin that was sculpted by Ice-Age glaciers and later dammed by landslide and rockfall debris from the steep slopes above the valley floor.
    MaroonBells2.jpg
  • El Capitan is a peak in Culberson County, Texas, United States, within Guadalupe Mountains National Park. It is the eighth highest peak in Texas, and rises abruptly out of the Chihuahuan Desert floor; it is considered the "signature peak" of West Texas.
    GuadalupeElCapitan1.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
  • 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 />
<br />
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 />
<br />
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 />
<br />
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.
    DeathValleyBush.jpg
  • The Maroon Bells are two peaks in the Elk Mountains, Maroon Peak and North Maroon Peak, separated by about a third of a mile. The mountains are about 12 miles southwest of Aspen. Both peaks are fourteeners. Maroon Peak, at 14,156 feet, is the 27th highest peak in Colorado; North Maroon Peak, at 14,014 feet, is the 50th highest. The view of the Maroon Bells to the southwest from the Maroon Creek valley is one of the most famous scenes in Colorado, and is reputed to be the "most-photographed spot in Colorado" and one of Colorado's premier scenic overlooks. The peaks are located in the Maroon Bells-Snowmass Wilderness of White River National Forest.<br />
<br />
A US Forest Service sign on the access trail refers to these mountains as "The Deadly Bells" and warns would-be climbers of "downsloping, loose, rotten and unstable" rock that "kills without warning". Unlike other mountains in the Rockies that are composed of granite and limestone, the Bells are composed of metamorphic sedimentary mudstone that has hardened into rock over millions of years. Mudstone is weak and fractures readily, giving rise to dangerously loose rock along almost any route. The mudstone is responsible for the Bells' distinctive maroon color. The Bells got their "deadly" name in 1965 when eight people died in five separate accidents.<br />
<br />
Maroon Lake (9,580') occupies a basin that was sculpted by Ice-Age glaciers and later dammed by landslide and rockfall debris from the steep slopes above the valley floor.
    MaroonBells5.jpg
  • The Maroon Bells are two peaks in the Elk Mountains, Maroon Peak and North Maroon Peak, separated by about a third of a mile. The mountains are about 12 miles southwest of Aspen. Both peaks are fourteeners. Maroon Peak, at 14,156 feet, is the 27th highest peak in Colorado; North Maroon Peak, at 14,014 feet, is the 50th highest. The view of the Maroon Bells to the southwest from the Maroon Creek valley is one of the most famous scenes in Colorado, and is reputed to be the "most-photographed spot in Colorado" and one of Colorado's premier scenic overlooks. The peaks are located in the Maroon Bells-Snowmass Wilderness of White River National Forest.<br />
<br />
A US Forest Service sign on the access trail refers to these mountains as "The Deadly Bells" and warns would-be climbers of "downsloping, loose, rotten and unstable" rock that "kills without warning". Unlike other mountains in the Rockies that are composed of granite and limestone, the Bells are composed of metamorphic sedimentary mudstone that has hardened into rock over millions of years. Mudstone is weak and fractures readily, giving rise to dangerously loose rock along almost any route. The mudstone is responsible for the Bells' distinctive maroon color. The Bells got their "deadly" name in 1965 when eight people died in five separate accidents.<br />
<br />
Maroon Lake (9,580') occupies a basin that was sculpted by Ice-Age glaciers and later dammed by landslide and rockfall debris from the steep slopes above the valley floor.
    MaroonBells4.jpg
  • El Capitan is a peak in Culberson County, Texas, United States, within Guadalupe Mountains National Park. It is the eighth highest peak in Texas, and rises abruptly out of the Chihuahuan Desert floor; it is considered the "signature peak" of West Texas.
    GuadalupeElCapitan3.jpg
  • El Capitan is a peak in Culberson County, Texas, United States, within Guadalupe Mountains National Park. It is the eighth highest peak in Texas, and rises abruptly out of the Chihuahuan Desert floor; it is considered the "signature peak" of West Texas.
    GuadalupeElCapitan2.jpg
  • El Capitan is a peak in Culberson County, Texas, United States, within Guadalupe Mountains National Park. It is the eighth highest peak in Texas, and rises abruptly out of the Chihuahuan Desert floor; it is considered the "signature peak" of West Texas.
    GuadalupeElCapitan1.jpg
  • The Maroon Bells are two peaks in the Elk Mountains, Maroon Peak and North Maroon Peak, separated by about a third of a mile. The mountains are about 12 miles southwest of Aspen. Both peaks are fourteeners. Maroon Peak, at 14,156 feet, is the 27th highest peak in Colorado; North Maroon Peak, at 14,014 feet, is the 50th highest. The view of the Maroon Bells to the southwest from the Maroon Creek valley is one of the most famous scenes in Colorado, and is reputed to be the "most-photographed spot in Colorado" and one of Colorado's premier scenic overlooks. The peaks are located in the Maroon Bells-Snowmass Wilderness of White River National Forest.<br />
<br />
A US Forest Service sign on the access trail refers to these mountains as "The Deadly Bells" and warns would-be climbers of "downsloping, loose, rotten and unstable" rock that "kills without warning". Unlike other mountains in the Rockies that are composed of granite and limestone, the Bells are composed of metamorphic sedimentary mudstone that has hardened into rock over millions of years. Mudstone is weak and fractures readily, giving rise to dangerously loose rock along almost any route. The mudstone is responsible for the Bells' distinctive maroon color. The Bells got their "deadly" name in 1965 when eight people died in five separate accidents.<br />
<br />
Maroon Lake (9,580') occupies a basin that was sculpted by Ice-Age glaciers and later dammed by landslide and rockfall debris from the steep slopes above the valley floor.
    MaroonBells1.jpg
  • 4 Times Square, formerly known as the Condé Nast Building, is a skyscraper in Times Square in Midtown Manhattan, New York City. Located on Broadway between West 42nd and 43rd Streets, the structure was finished in January 2000 as part of a larger project to redevelop 42nd Street. The architects were Fox & Fowle, who also designed the Reuters Building as part of the larger project. The 809-foot, 48-story building is the 12th tallest building in New York City and the 41st tallest in the United States. Owned by the Durst Organization, the building contains 1,600,000 square feet of floor space. The major office space tenants are Skadden, Arps, Slate, Meagher & Flom, a prominent U.S. law firm. Duane Reade is a major retail tenant. H&M has leased the space formerly occupied by ESPNZone; in August 2013, the retailer announced that it would be installing four illuminated panels bearing the company logo atop the tower.
    NYC_HMBuilding3.jpg
  • The New York Stock Exchange (abbreviated as NYSE and nicknamed "The Big Board"), is an American stock exchange located at 11 Wall Street, Lower Manhattan, New York City, New York. It is by far the world's largest stock exchange by market capitalization of its listed companies at US$19.69 trillion as of May 2015. The average daily trading value was approximately US$169 billion in 2013. The NYSE trading floor is located at 11 Wall Street and is composed of 21 rooms used for the facilitation of trading. A fifth trading room, located at 30 Broad Street, was closed in February 2007. The main building and the 11 Wall Street building were designated National Historic Landmarks in 1978.
    NYC_StockExchange1.jpg
  • Jal Mahal (meaning "Water Palace") is a palace located in the middle of the Man Sagar Lake in Jaipur city, the capital of the state of Rajasthan, India. The palace and the lake around it were renovated and enlarged in the 18th century by Maharaja Jai Singh II of Amber. The Jal Mahal palace has got an eye-popping makeover. Traditional boat-makers from Vrindavan have crafted the Rajput style wooden boats. A gentle splashing of oars on the clear lake waters takes you to Jal Mahal. You move past decorated hallways and chambers on the first floor to climb all the way up to the fragrant Chameli Bagh. Across the lake, you can view the Aravalli hills, dotted with temples and ancient forts, and on the other side, bustling Jaipur. The most remarkable change is in the lake itself. The drains were diverted, two million tonnes of toxic silt were dredged from the bottom, increasing its depth by over a metre, a water treatment system was developed, local vegetation and fish reintroduced, the surrounding wetlands regenerated and five nesting islands created to attract migratory birds.
    JalMahal1.jpg
  • Stepwells, also called kalyani or pushkarani , bawdi or baoli are wells or ponds in which the water may be reached by descending a set of steps. They may be covered and protected and are often of architectural significance. They also may be multi-storied having a bullock which turns the water wheel ("rehat") to raise the water in the well to the first or second floor.<br />
They are most common in western India. They may be also found in the other more arid regions of the South Asia, extending into Pakistan. The construction may be utilitarian, but sometimes includes significant architectural embellishments.
    Abhaneri1.jpg
  • Stepwells, also called kalyani or pushkarani , bawdi or baoli are wells or ponds in which the water may be reached by descending a set of steps. They may be covered and protected and are often of architectural significance. They also may be multi-storied having a bullock which turns the water wheel ("rehat") to raise the water in the well to the first or second floor.<br />
They are most common in western India. They may be also found in the other more arid regions of the South Asia, extending into Pakistan. The construction may be utilitarian, but sometimes includes significant architectural embellishments.
    Abhaneri2.jpg
  • Mount Shasta is located at the southern end of the Cascade Range in Siskiyou County, California and at 14,179 feet is the second highest peak in the Cascades and the fifth highest in California. Mount Shasta has an estimated volume of 85 cubic miles which makes it the most voluminous stratovolcano in the Cascade Volcanic Arc.<br />
<br />
The mountain and its surrounding area are managed by the U.S. Forest Service, Shasta-Trinity National Forest.<br />
<br />
Mount Shasta is not connected to any nearby mountain and dominates the northern California landscape. It rises abruptly and stands nearly 10,000 ft above the surrounding terrain. On a clear winter day snowy Mount Shasta can be seen from the floor of the valley 140 miles south. The mountain has attracted the attention of poets, authors, and presidents.<br />
The mountain consists of four overlapping volcanic cones which have built a complex shape, including the main summit and the prominent satellite cone of 12,330 ft Shastina, which has a visibly conical form. If Shastina were a separate mountain, it would rank as the fourth-highest peak of the Cascade Range (after Mt. Rainier, Rainier's Liberty Cap, and Mt. Shasta itself).<br />
<br />
Mount Shasta's surface is relatively free of deep glacial erosion except, paradoxically, for its south side where Sargents Ridge runs parallel to the U-shaped Avalanche Gulch. This is the largest glacial valley on the volcano, although it does not presently have a glacier in it. There are seven named glaciers on Mount Shasta, with the four largest (Whitney, Bolam, Hotlum, and Wintun) radiating down from high on the main summit cone to below 10,000 ft primarily on the north and east sides. The Whitney Glacier is the longest and the Hotlum is the most voluminous glacier in the state of California. Three of the smaller named glaciers occupy cirques near and above 11,000 ft on the south and southeast sides, including the Watkins, Konwakiton, and Mud Creek Glaciers.
    MountShasta5.jpg
  • Mount Shasta is located at the southern end of the Cascade Range in Siskiyou County, California and at 14,179 feet is the second highest peak in the Cascades and the fifth highest in California. Mount Shasta has an estimated volume of 85 cubic miles which makes it the most voluminous stratovolcano in the Cascade Volcanic Arc.<br />
<br />
The mountain and its surrounding area are managed by the U.S. Forest Service, Shasta-Trinity National Forest.<br />
<br />
Mount Shasta is not connected to any nearby mountain and dominates the northern California landscape. It rises abruptly and stands nearly 10,000 ft above the surrounding terrain. On a clear winter day snowy Mount Shasta can be seen from the floor of the valley 140 miles south. The mountain has attracted the attention of poets, authors, and presidents.<br />
The mountain consists of four overlapping volcanic cones which have built a complex shape, including the main summit and the prominent satellite cone of 12,330 ft Shastina, which has a visibly conical form. If Shastina were a separate mountain, it would rank as the fourth-highest peak of the Cascade Range (after Mt. Rainier, Rainier's Liberty Cap, and Mt. Shasta itself).<br />
<br />
Mount Shasta's surface is relatively free of deep glacial erosion except, paradoxically, for its south side where Sargents Ridge runs parallel to the U-shaped Avalanche Gulch. This is the largest glacial valley on the volcano, although it does not presently have a glacier in it. There are seven named glaciers on Mount Shasta, with the four largest (Whitney, Bolam, Hotlum, and Wintun) radiating down from high on the main summit cone to below 10,000 ft primarily on the north and east sides. The Whitney Glacier is the longest and the Hotlum is the most voluminous glacier in the state of California. Three of the smaller named glaciers occupy cirques near and above 11,000 ft on the south and southeast sides, including the Watkins, Konwakiton, and Mud Creek Glaciers.
    MountShasta4.jpg
  • Mount Shasta is located at the southern end of the Cascade Range in Siskiyou County, California and at 14,179 feet is the second highest peak in the Cascades and the fifth highest in California. Mount Shasta has an estimated volume of 85 cubic miles which makes it the most voluminous stratovolcano in the Cascade Volcanic Arc.<br />
<br />
The mountain and its surrounding area are managed by the U.S. Forest Service, Shasta-Trinity National Forest.<br />
<br />
Mount Shasta is not connected to any nearby mountain and dominates the northern California landscape. It rises abruptly and stands nearly 10,000 ft above the surrounding terrain. On a clear winter day snowy Mount Shasta can be seen from the floor of the valley 140 miles south. The mountain has attracted the attention of poets, authors, and presidents.<br />
The mountain consists of four overlapping volcanic cones which have built a complex shape, including the main summit and the prominent satellite cone of 12,330 ft Shastina, which has a visibly conical form. If Shastina were a separate mountain, it would rank as the fourth-highest peak of the Cascade Range (after Mt. Rainier, Rainier's Liberty Cap, and Mt. Shasta itself).<br />
<br />
Mount Shasta's surface is relatively free of deep glacial erosion except, paradoxically, for its south side where Sargents Ridge runs parallel to the U-shaped Avalanche Gulch. This is the largest glacial valley on the volcano, although it does not presently have a glacier in it. There are seven named glaciers on Mount Shasta, with the four largest (Whitney, Bolam, Hotlum, and Wintun) radiating down from high on the main summit cone to below 10,000 ft primarily on the north and east sides. The Whitney Glacier is the longest and the Hotlum is the most voluminous glacier in the state of California. Three of the smaller named glaciers occupy cirques near and above 11,000 ft on the south and southeast sides, including the Watkins, Konwakiton, and Mud Creek Glaciers.
    MountShasta2.jpg
  • Mount Shasta is located at the southern end of the Cascade Range in Siskiyou County, California and at 14,179 feet is the second highest peak in the Cascades and the fifth highest in California. Mount Shasta has an estimated volume of 85 cubic miles which makes it the most voluminous stratovolcano in the Cascade Volcanic Arc.<br />
<br />
The mountain and its surrounding area are managed by the U.S. Forest Service, Shasta-Trinity National Forest.<br />
<br />
Mount Shasta is not connected to any nearby mountain and dominates the northern California landscape. It rises abruptly and stands nearly 10,000 ft above the surrounding terrain. On a clear winter day snowy Mount Shasta can be seen from the floor of the valley 140 miles south. The mountain has attracted the attention of poets, authors, and presidents.<br />
The mountain consists of four overlapping volcanic cones which have built a complex shape, including the main summit and the prominent satellite cone of 12,330 ft Shastina, which has a visibly conical form. If Shastina were a separate mountain, it would rank as the fourth-highest peak of the Cascade Range (after Mt. Rainier, Rainier's Liberty Cap, and Mt. Shasta itself).<br />
<br />
Mount Shasta's surface is relatively free of deep glacial erosion except, paradoxically, for its south side where Sargents Ridge runs parallel to the U-shaped Avalanche Gulch. This is the largest glacial valley on the volcano, although it does not presently have a glacier in it. There are seven named glaciers on Mount Shasta, with the four largest (Whitney, Bolam, Hotlum, and Wintun) radiating down from high on the main summit cone to below 10,000 ft primarily on the north and east sides. The Whitney Glacier is the longest and the Hotlum is the most voluminous glacier in the state of California. Three of the smaller named glaciers occupy cirques near and above 11,000 ft on the south and southeast sides, including the Watkins, Konwakiton, and Mud Creek Glaciers.
    MountShasta1.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
  • El Capitan is a peak in Culberson County, Texas, United States, within Guadalupe Mountains National Park. It is the eighth highest peak in Texas, and rises abruptly out of the Chihuahuan Desert floor; it is considered the "signature peak" of West Texas.
    GuadalupeElCapitan1.jpg
  • El Capitan is a peak in Culberson County, Texas, United States, within Guadalupe Mountains National Park. It is the eighth highest peak in Texas, and rises abruptly out of the Chihuahuan Desert floor; it is considered the "signature peak" of West Texas.
    _Y6A3113-Edit.jpg
  • El Capitan is a peak in Culberson County, Texas, United States, within Guadalupe Mountains National Park. It is the eighth highest peak in Texas, and rises abruptly out of the Chihuahuan Desert floor; it is considered the "signature peak" of West Texas.
    GuadalupeElCapitan1.jpg
  • The Dordogne (French: La Dordogne) is a river in south-central and southwest France. The Dordogne and its watershed were designated Biosphere Reserve by UNESCO on July 11 2012. The river rises on the flanks of the Puy de Sancy in the mountains of Auvergne, from the confluence of two small torrents above the town of Le Mont-Dore: the Dore and the Dogne. It flows generally west through the Limousin and Périgord regions before flowing into the Gironde, its common estuary with the Garonne, at the Bec d'Ambès ("Ambès beak"), north of the city of Bordeaux. The Dordogne is one of the few rivers in the world that exhibit the phenomenon of a tidal bore, known as a mascaret.<br />
<br />
The upper valley of the Dordogne is a series of deep gorges. The cliffs, steep banks, fast flowing water and high bridges attract both walkers and drivers. In several places the river is dammed to form long, deep lakes. Camp sites and holiday homes have proliferated wherever the valley floor is wide enough to accommodate them.<br />
<br />
Below Argentat and around Beaulieu-sur-Dordogne, the valley widens to accommodate fertile farmland, well-watered pasture and orchards. In the towns, which are major tourist attractions because of their history and architecture, the quaysides are lined with eating and drinking places. In Périgord, the valley widens further to encompass one of France's main gastronomic regions, with vineyards, poultry farms and truffle-rich woodlands.
    Beynac6.jpg
  • The Dordogne (French: La Dordogne) is a river in south-central and southwest France. The Dordogne and its watershed were designated Biosphere Reserve by UNESCO on July 11 2012. The river rises on the flanks of the Puy de Sancy in the mountains of Auvergne, from the confluence of two small torrents above the town of Le Mont-Dore: the Dore and the Dogne. It flows generally west through the Limousin and Périgord regions before flowing into the Gironde, its common estuary with the Garonne, at the Bec d'Ambès ("Ambès beak"), north of the city of Bordeaux. The Dordogne is one of the few rivers in the world that exhibit the phenomenon of a tidal bore, known as a mascaret.<br />
<br />
The upper valley of the Dordogne is a series of deep gorges. The cliffs, steep banks, fast flowing water and high bridges attract both walkers and drivers. In several places the river is dammed to form long, deep lakes. Camp sites and holiday homes have proliferated wherever the valley floor is wide enough to accommodate them.<br />
<br />
Below Argentat and around Beaulieu-sur-Dordogne, the valley widens to accommodate fertile farmland, well-watered pasture and orchards. In the towns, which are major tourist attractions because of their history and architecture, the quaysides are lined with eating and drinking places. In Périgord, the valley widens further to encompass one of France's main gastronomic regions, with vineyards, poultry farms and truffle-rich woodlands.
    Montfort12.jpg
  • Mount Shasta is located at the southern end of the Cascade Range in Siskiyou County, California and at 14,179 feet is the second highest peak in the Cascades and the fifth highest in California. Mount Shasta has an estimated volume of 85 cubic miles which makes it the most voluminous stratovolcano in the Cascade Volcanic Arc.<br />
<br />
The mountain and its surrounding area are managed by the U.S. Forest Service, Shasta-Trinity National Forest.<br />
<br />
Mount Shasta is not connected to any nearby mountain and dominates the northern California landscape. It rises abruptly and stands nearly 10,000 ft above the surrounding terrain. On a clear winter day snowy Mount Shasta can be seen from the floor of the valley 140 miles south. The mountain has attracted the attention of poets, authors, and presidents.<br />
The mountain consists of four overlapping volcanic cones which have built a complex shape, including the main summit and the prominent satellite cone of 12,330 ft Shastina, which has a visibly conical form. If Shastina were a separate mountain, it would rank as the fourth-highest peak of the Cascade Range (after Mt. Rainier, Rainier's Liberty Cap, and Mt. Shasta itself).<br />
<br />
Mount Shasta's surface is relatively free of deep glacial erosion except, paradoxically, for its south side where Sargents Ridge runs parallel to the U-shaped Avalanche Gulch. This is the largest glacial valley on the volcano, although it does not presently have a glacier in it. There are seven named glaciers on Mount Shasta, with the four largest (Whitney, Bolam, Hotlum, and Wintun) radiating down from high on the main summit cone to below 10,000 ft primarily on the north and east sides. The Whitney Glacier is the longest and the Hotlum is the most voluminous glacier in the state of California. Three of the smaller named glaciers occupy cirques near and above 11,000 ft on the south and southeast sides, including the Watkins, Konwakiton, and Mud Creek Glaciers.
    MountShasta6.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
  • Monument Valley (Navajo: Tsé Biiʼ Ndzisgaii, meaning valley of the rocks) is a region of the Colorado Plateau characterized by a cluster of vast sandstone buttes, the largest reaching 1,000 ft above the valley floor. It is located on the Arizona-Utah state line, near the Four Corners area. The valley lies within the range of the Navajo Nation Reservation and is accessible from U.S. Highway 163. 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."
    Highway163-Alt2.jpg
  • The Maroon Bells are two peaks in the Elk Mountains, Maroon Peak and North Maroon Peak, separated by about a third of a mile. The mountains are about 12 miles southwest of Aspen. Both peaks are fourteeners. Maroon Peak, at 14,156 feet, is the 27th highest peak in Colorado; North Maroon Peak, at 14,014 feet, is the 50th highest. The view of the Maroon Bells to the southwest from the Maroon Creek valley is one of the most famous scenes in Colorado, and is reputed to be the "most-photographed spot in Colorado" and one of Colorado's premier scenic overlooks. The peaks are located in the Maroon Bells-Snowmass Wilderness of White River National Forest.<br />
<br />
A US Forest Service sign on the access trail refers to these mountains as "The Deadly Bells" and warns would-be climbers of "downsloping, loose, rotten and unstable" rock that "kills without warning". Unlike other mountains in the Rockies that are composed of granite and limestone, the Bells are composed of metamorphic sedimentary mudstone that has hardened into rock over millions of years. Mudstone is weak and fractures readily, giving rise to dangerously loose rock along almost any route. The mudstone is responsible for the Bells' distinctive maroon color. The Bells got their "deadly" name in 1965 when eight people died in five separate accidents.<br />
<br />
Maroon Lake (9,580') occupies a basin that was sculpted by Ice-Age glaciers and later dammed by landslide and rockfall debris from the steep slopes above the valley floor.
    MaroonBells2.jpg
  • El Capitan is a peak in Culberson County, Texas, United States, within Guadalupe Mountains National Park. It is the eighth highest peak in Texas, and rises abruptly out of the Chihuahuan Desert floor; it is considered the "signature peak" of West Texas.
    GuadalupeElCapitan3-Blend.jpg
  • The Maroon Bells are two peaks in the Elk Mountains, Maroon Peak and North Maroon Peak, separated by about a third of a mile. The mountains are about 12 miles southwest of Aspen. Both peaks are fourteeners. Maroon Peak, at 14,156 feet, is the 27th highest peak in Colorado; North Maroon Peak, at 14,014 feet, is the 50th highest. The view of the Maroon Bells to the southwest from the Maroon Creek valley is one of the most famous scenes in Colorado, and is reputed to be the "most-photographed spot in Colorado" and one of Colorado's premier scenic overlooks. The peaks are located in the Maroon Bells-Snowmass Wilderness of White River National Forest.<br />
<br />
A US Forest Service sign on the access trail refers to these mountains as "The Deadly Bells" and warns would-be climbers of "downsloping, loose, rotten and unstable" rock that "kills without warning". Unlike other mountains in the Rockies that are composed of granite and limestone, the Bells are composed of metamorphic sedimentary mudstone that has hardened into rock over millions of years. Mudstone is weak and fractures readily, giving rise to dangerously loose rock along almost any route. The mudstone is responsible for the Bells' distinctive maroon color. The Bells got their "deadly" name in 1965 when eight people died in five separate accidents.<br />
<br />
Maroon Lake (9,580') occupies a basin that was sculpted by Ice-Age glaciers and later dammed by landslide and rockfall debris from the steep slopes above the valley floor.
    MaroonBells4.jpg
  • 4 Times Square, formerly known as the Condé Nast Building, is a skyscraper in Times Square in Midtown Manhattan, New York City. Located on Broadway between West 42nd and 43rd Streets, the structure was finished in January 2000 as part of a larger project to redevelop 42nd Street. The architects were Fox & Fowle, who also designed the Reuters Building as part of the larger project. The 809-foot, 48-story building is the 12th tallest building in New York City and the 41st tallest in the United States. Owned by the Durst Organization, the building contains 1,600,000 square feet of floor space. The major office space tenants are Skadden, Arps, Slate, Meagher & Flom, a prominent U.S. law firm. Duane Reade is a major retail tenant. H&M has leased the space formerly occupied by ESPNZone; in August 2013, the retailer announced that it would be installing four illuminated panels bearing the company logo atop the tower.
    NYC_HMBuilding4.jpg
  • 4 Times Square, formerly known as the Condé Nast Building, is a skyscraper in Times Square in Midtown Manhattan, New York City. Located on Broadway between West 42nd and 43rd Streets, the structure was finished in January 2000 as part of a larger project to redevelop 42nd Street. The architects were Fox & Fowle, who also designed the Reuters Building as part of the larger project. The 809-foot, 48-story building is the 12th tallest building in New York City and the 41st tallest in the United States. Owned by the Durst Organization, the building contains 1,600,000 square feet of floor space. The major office space tenants are Skadden, Arps, Slate, Meagher & Flom, a prominent U.S. law firm. Duane Reade is a major retail tenant. H&M has leased the space formerly occupied by ESPNZone; in August 2013, the retailer announced that it would be installing four illuminated panels bearing the company logo atop the tower.
    NYC_HMBuilding2.jpg
  • 4 Times Square, formerly known as the Condé Nast Building, is a skyscraper in Times Square in Midtown Manhattan, New York City. Located on Broadway between West 42nd and 43rd Streets, the structure was finished in January 2000 as part of a larger project to redevelop 42nd Street. The architects were Fox & Fowle, who also designed the Reuters Building as part of the larger project. The 809-foot, 48-story building is the 12th tallest building in New York City and the 41st tallest in the United States. Owned by the Durst Organization, the building contains 1,600,000 square feet of floor space. The major office space tenants are Skadden, Arps, Slate, Meagher & Flom, a prominent U.S. law firm. Duane Reade is a major retail tenant. H&M has leased the space formerly occupied by ESPNZone; in August 2013, the retailer announced that it would be installing four illuminated panels bearing the company logo atop the tower.
    NYC_HMBuilding1.jpg
  • The Maroon Bells are two peaks in the Elk Mountains, Maroon Peak and North Maroon Peak, separated by about a third of a mile. The mountains are about 12 miles southwest of Aspen. Both peaks are fourteeners. Maroon Peak, at 14,156 feet, is the 27th highest peak in Colorado; North Maroon Peak, at 14,014 feet, is the 50th highest. The view of the Maroon Bells to the southwest from the Maroon Creek valley is one of the most famous scenes in Colorado, and is reputed to be the "most-photographed spot in Colorado" and one of Colorado's premier scenic overlooks. The peaks are located in the Maroon Bells-Snowmass Wilderness of White River National Forest.<br />
<br />
A US Forest Service sign on the access trail refers to these mountains as "The Deadly Bells" and warns would-be climbers of "downsloping, loose, rotten and unstable" rock that "kills without warning". Unlike other mountains in the Rockies that are composed of granite and limestone, the Bells are composed of metamorphic sedimentary mudstone that has hardened into rock over millions of years. Mudstone is weak and fractures readily, giving rise to dangerously loose rock along almost any route. The mudstone is responsible for the Bells' distinctive maroon color. The Bells got their "deadly" name in 1965 when eight people died in five separate accidents.<br />
<br />
Maroon Lake (9,580') occupies a basin that was sculpted by Ice-Age glaciers and later dammed by landslide and rockfall debris from the steep slopes above the valley floor.
    MaroonBells6.jpg
  • The Maroon Bells are two peaks in the Elk Mountains, Maroon Peak and North Maroon Peak, separated by about a third of a mile. The mountains are about 12 miles southwest of Aspen. Both peaks are fourteeners. Maroon Peak, at 14,156 feet, is the 27th highest peak in Colorado; North Maroon Peak, at 14,014 feet, is the 50th highest. The view of the Maroon Bells to the southwest from the Maroon Creek valley is one of the most famous scenes in Colorado, and is reputed to be the "most-photographed spot in Colorado" and one of Colorado's premier scenic overlooks. The peaks are located in the Maroon Bells-Snowmass Wilderness of White River National Forest.<br />
<br />
A US Forest Service sign on the access trail refers to these mountains as "The Deadly Bells" and warns would-be climbers of "downsloping, loose, rotten and unstable" rock that "kills without warning". Unlike other mountains in the Rockies that are composed of granite and limestone, the Bells are composed of metamorphic sedimentary mudstone that has hardened into rock over millions of years. Mudstone is weak and fractures readily, giving rise to dangerously loose rock along almost any route. The mudstone is responsible for the Bells' distinctive maroon color. The Bells got their "deadly" name in 1965 when eight people died in five separate accidents.<br />
<br />
Maroon Lake (9,580') occupies a basin that was sculpted by Ice-Age glaciers and later dammed by landslide and rockfall debris from the steep slopes above the valley floor.
    MaroonBells3.jpg
  • The Maroon Bells are two peaks in the Elk Mountains, Maroon Peak and North Maroon Peak, separated by about a third of a mile. The mountains are about 12 miles southwest of Aspen. Both peaks are fourteeners. Maroon Peak, at 14,156 feet, is the 27th highest peak in Colorado; North Maroon Peak, at 14,014 feet, is the 50th highest. The view of the Maroon Bells to the southwest from the Maroon Creek valley is one of the most famous scenes in Colorado, and is reputed to be the "most-photographed spot in Colorado" and one of Colorado's premier scenic overlooks. The peaks are located in the Maroon Bells-Snowmass Wilderness of White River National Forest.<br />
<br />
A US Forest Service sign on the access trail refers to these mountains as "The Deadly Bells" and warns would-be climbers of "downsloping, loose, rotten and unstable" rock that "kills without warning". Unlike other mountains in the Rockies that are composed of granite and limestone, the Bells are composed of metamorphic sedimentary mudstone that has hardened into rock over millions of years. Mudstone is weak and fractures readily, giving rise to dangerously loose rock along almost any route. The mudstone is responsible for the Bells' distinctive maroon color. The Bells got their "deadly" name in 1965 when eight people died in five separate accidents.<br />
<br />
Maroon Lake (9,580') occupies a basin that was sculpted by Ice-Age glaciers and later dammed by landslide and rockfall debris from the steep slopes above the valley floor.
    MaroonBells2.jpg
  • Jal Mahal (meaning "Water Palace") is a palace located in the middle of the Man Sagar Lake in Jaipur city, the capital of the state of Rajasthan, India. The palace and the lake around it were renovated and enlarged in the 18th century by Maharaja Jai Singh II of Amber. The Jal Mahal palace has got an eye-popping makeover. Traditional boat-makers from Vrindavan have crafted the Rajput style wooden boats. A gentle splashing of oars on the clear lake waters takes you to Jal Mahal. You move past decorated hallways and chambers on the first floor to climb all the way up to the fragrant Chameli Bagh. Across the lake, you can view the Aravalli hills, dotted with temples and ancient forts, and on the other side, bustling Jaipur. The most remarkable change is in the lake itself. The drains were diverted, two million tonnes of toxic silt were dredged from the bottom, increasing its depth by over a metre, a water treatment system was developed, local vegetation and fish reintroduced, the surrounding wetlands regenerated and five nesting islands created to attract migratory birds.
    JalMahal1.jpg
  • The Boston Public Library McKim Building (built 1895) in Copley Square contains the library's research collection, exhibition rooms and administrative offices. When it opened in 1895, the new Boston Public Library was proclaimed a "palace for the people." The building includes lavish decorations, a children's room (the first in the nation), and a central courtyard surrounded by an arcaded gallery in the manner of a Renaissance cloister. The library regularly displays its rare works, often in exhibits that will combine works on paper, rare books, and works of art. Several galleries in the third floor of the McKim building are maintained for exhibits.
    BostonPublicLibrary1.jpg
  • Mount Shasta is located at the southern end of the Cascade Range in Siskiyou County, California and at 14,179 feet is the second highest peak in the Cascades and the fifth highest in California. Mount Shasta has an estimated volume of 85 cubic miles which makes it the most voluminous stratovolcano in the Cascade Volcanic Arc.<br />
<br />
The mountain and its surrounding area are managed by the U.S. Forest Service, Shasta-Trinity National Forest.<br />
<br />
Mount Shasta is not connected to any nearby mountain and dominates the northern California landscape. It rises abruptly and stands nearly 10,000 ft above the surrounding terrain. On a clear winter day snowy Mount Shasta can be seen from the floor of the valley 140 miles south. The mountain has attracted the attention of poets, authors, and presidents.<br />
The mountain consists of four overlapping volcanic cones which have built a complex shape, including the main summit and the prominent satellite cone of 12,330 ft Shastina, which has a visibly conical form. If Shastina were a separate mountain, it would rank as the fourth-highest peak of the Cascade Range (after Mt. Rainier, Rainier's Liberty Cap, and Mt. Shasta itself).<br />
<br />
Mount Shasta's surface is relatively free of deep glacial erosion except, paradoxically, for its south side where Sargents Ridge runs parallel to the U-shaped Avalanche Gulch. This is the largest glacial valley on the volcano, although it does not presently have a glacier in it. There are seven named glaciers on Mount Shasta, with the four largest (Whitney, Bolam, Hotlum, and Wintun) radiating down from high on the main summit cone to below 10,000 ft primarily on the north and east sides. The Whitney Glacier is the longest and the Hotlum is the most voluminous glacier in the state of California. Three of the smaller named glaciers occupy cirques near and above 11,000 ft on the south and southeast sides, including the Watkins, Konwakiton, and Mud Creek Glaciers.
    MountShasta6.jpg
  • Mount Shasta is located at the southern end of the Cascade Range in Siskiyou County, California and at 14,179 feet is the second highest peak in the Cascades and the fifth highest in California. Mount Shasta has an estimated volume of 85 cubic miles which makes it the most voluminous stratovolcano in the Cascade Volcanic Arc.<br />
<br />
The mountain and its surrounding area are managed by the U.S. Forest Service, Shasta-Trinity National Forest.<br />
<br />
Mount Shasta is not connected to any nearby mountain and dominates the northern California landscape. It rises abruptly and stands nearly 10,000 ft above the surrounding terrain. On a clear winter day snowy Mount Shasta can be seen from the floor of the valley 140 miles south. The mountain has attracted the attention of poets, authors, and presidents.<br />
The mountain consists of four overlapping volcanic cones which have built a complex shape, including the main summit and the prominent satellite cone of 12,330 ft Shastina, which has a visibly conical form. If Shastina were a separate mountain, it would rank as the fourth-highest peak of the Cascade Range (after Mt. Rainier, Rainier's Liberty Cap, and Mt. Shasta itself).<br />
<br />
Mount Shasta's surface is relatively free of deep glacial erosion except, paradoxically, for its south side where Sargents Ridge runs parallel to the U-shaped Avalanche Gulch. This is the largest glacial valley on the volcano, although it does not presently have a glacier in it. There are seven named glaciers on Mount Shasta, with the four largest (Whitney, Bolam, Hotlum, and Wintun) radiating down from high on the main summit cone to below 10,000 ft primarily on the north and east sides. The Whitney Glacier is the longest and the Hotlum is the most voluminous glacier in the state of California. Three of the smaller named glaciers occupy cirques near and above 11,000 ft on the south and southeast sides, including the Watkins, Konwakiton, and Mud Creek Glaciers.
    MountShasta3.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
  • Kolmanskop (Afrikaans for Coleman's hill, German: Kolmannskuppe) is a ghost town in the Namib desert in southern Namibia, 10 kilometres inland from the port town of Lüderitz. It was named after a transport driver named Johnny Coleman who, during a sand storm, abandoned his ox wagon on a small incline opposite the settlement. Once a small but very rich mining village, it is now a popular tourist destination run by the joint firm NamDeb (Namibia-De Beers).<br />
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In 1908 the worker Zacharias Lewala found a diamond while working in this area and showed it to his supervisor, the German railway inspector August Stauch. Realizing the area was rich in diamonds, German miners began settlement, and soon after the German government declared a large area as a "Sperrgebiet", starting to exploit the diamond field. Driven by the enormous wealth of the first diamond miners, the residents built the village in the architectural style of a German town, with amenities and institutions including a hospital, ballroom, power station, school, skittle-alley, theatre and sport-hall, casino, ice factory and the first x-ray-station in the southern hemisphere, as well as the first tram in Africa. It had a railway link to Lüderitz.<br />
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The town declined after World War I when the diamond-field slowly exhausted and was ultimately abandoned in 1954. The geological forces of the desert mean that tourists now walk through houses knee-deep in sand.
    Kolmanskop10.jpg
  • The Secretariat Building or Central Secretariat is where the Cabinet Secretariat is housed, which administers the Government of India. Built in the 1910s, it is home to some of the most important ministries of the Cabinet of India. Situated on Raisina Hill, New Delhi, the Secretariat buildings are two blocks of symmetrical buildings (North Block and South Block) on opposite sides of the great axis of Rajpath, and flanking the Rashtrapati Bhavan (President's House).<br />
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The Secretariat Building was designed by the prominent British architect Herbert Baker in Indo-Saracenic Revival architecture. Both the identical building have four levels, each with about 1,000 rooms, in the inner courtyards to make space for future expansions. In continuation with the Viceroy's House, these buildings also used cream and red Dholpur sandstone from Rajasthan, with the red sandstone forming the base. Together the buildings were designed to form two squares. They have broad corridors between different wings and wide stairways to the four floors and each building is topped by a giant dome, while each wings end with colonnaded balcony.<br />
Much of the building is in classical architectural style, yet it incorporated from Mughal and Rajasthani architecture style and motifs in its architecture. These are visible in the use of Jali, perforated screens, to protect from scorching sun and monsoon rains of India. Another feature of the building is a dome-like structure known as the Chatri, a design unique to India, used in ancient times to give relief to travelers by providing shade from the hot Indian sun.<br />
The style of architecture used in Secretariat Building is unique to Raisina Hill. In front of the main gates on buildings are the four "dominion columns", given by Canada, Australia, New Zealand and South Africa. At the time of their unveiling in 1930, India also supposed to become a British dominion soon, however India became independent within the next 17 years and the Secretariat became the
    DelhiSecretariat3.jpg
  • The Secretariat Building or Central Secretariat is where the Cabinet Secretariat is housed, which administers the Government of India. Built in the 1910s, it is home to some of the most important ministries of the Cabinet of India. Situated on Raisina Hill, New Delhi, the Secretariat buildings are two blocks of symmetrical buildings (North Block and South Block) on opposite sides of the great axis of Rajpath, and flanking the Rashtrapati Bhavan (President's House).<br />
.....<br />
The Secretariat Building was designed by the prominent British architect Herbert Baker in Indo-Saracenic Revival architecture. Both the identical building have four levels, each with about 1,000 rooms, in the inner courtyards to make space for future expansions. In continuation with the Viceroy's House, these buildings also used cream and red Dholpur sandstone from Rajasthan, with the red sandstone forming the base. Together the buildings were designed to form two squares. They have broad corridors between different wings and wide stairways to the four floors and each building is topped by a giant dome, while each wings end with colonnaded balcony.<br />
Much of the building is in classical architectural style, yet it incorporated from Mughal and Rajasthani architecture style and motifs in its architecture. These are visible in the use of Jali, perforated screens, to protect from scorching sun and monsoon rains of India. Another feature of the building is a dome-like structure known as the Chatri, a design unique to India, used in ancient times to give relief to travelers by providing shade from the hot Indian sun.<br />
The style of architecture used in Secretariat Building is unique to Raisina Hill. In front of the main gates on buildings are the four "dominion columns", given by Canada, Australia, New Zealand and South Africa. At the time of their unveiling in 1930, India also supposed to become a British dominion soon, however India became independent within the next 17 years and the Secretariat became the
    DelhiSecretariat2.jpg
  • The Secretariat Building or Central Secretariat is where the Cabinet Secretariat is housed, which administers the Government of India. Built in the 1910s, it is home to some of the most important ministries of the Cabinet of India. Situated on Raisina Hill, New Delhi, the Secretariat buildings are two blocks of symmetrical buildings (North Block and South Block) on opposite sides of the great axis of Rajpath, and flanking the Rashtrapati Bhavan (President's House).<br />
.....<br />
The Secretariat Building was designed by the prominent British architect Herbert Baker in Indo-Saracenic Revival architecture. Both the identical building have four levels, each with about 1,000 rooms, in the inner courtyards to make space for future expansions. In continuation with the Viceroy's House, these buildings also used cream and red Dholpur sandstone from Rajasthan, with the red sandstone forming the base. Together the buildings were designed to form two squares. They have broad corridors between different wings and wide stairways to the four floors and each building is topped by a giant dome, while each wings end with colonnaded balcony.<br />
Much of the building is in classical architectural style, yet it incorporated from Mughal and Rajasthani architecture style and motifs in its architecture. These are visible in the use of Jali, perforated screens, to protect from scorching sun and monsoon rains of India. Another feature of the building is a dome-like structure known as the Chatri, a design unique to India, used in ancient times to give relief to travelers by providing shade from the hot Indian sun.<br />
The style of architecture used in Secretariat Building is unique to Raisina Hill. In front of the main gates on buildings are the four "dominion columns", given by Canada, Australia, New Zealand and South Africa. At the time of their unveiling in 1930, India also supposed to become a British dominion soon, however India became independent within the next 17 years and the Secretariat became the
    DelhiSecretariat1.jpg
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