manuel cohen

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  • View from below of the pediment of the Galerie de Mineralogie, de Geologie et de Paleobotanique (Gallery of Minerology, Geology and Paleobotany), built from 1833 to 1841 by Charles Rohault de Fleury and located in the Jardin des Plantes, Paris, 5th arrondissement, France. Founded in 1626 by Guy de La Brosse, Louis XIII's physician, the Jardin des Plantes, originally known as the Jardin du Roi, opened to the public in 1640. It became the Museum National d'Histoire Naturelle in 1793 during the French Revolution. Picture by Manuel Cohen
    LC_JDP_10_MC215.jpg
  • General view of the entrance to the Galerie de Mineralogie, de Geologie et de Paleobotanique (Gallery of Minerology, Geology and Paleobotany), built from 1833 to 1841 by Charles Rohault de Fleury and located in the Jardin des Plantes, Paris, 5th arrondissement, France. Founded in 1626 by Guy de La Brosse, Louis XIII's physician, the Jardin des Plantes, originally known as the Jardin du Roi, opened to the public in 1640. It became the Museum National d'Histoire Naturelle in 1793 during the French Revolution. Picture by Manuel Cohen
    LC_JDP_10_MC212.jpg
  • View from below of the pediment of the Galerie de Mineralogie, de Geologie et de Paleobotanique (Gallery of Minerology, Geology and Paleobotany), built from 1833 to 1841 by Charles Rohault de Fleury and located in the Jardin des Plantes, Paris, 5th arrondissement, France. Founded in 1626 by Guy de La Brosse, Louis XIII's physician, the Jardin des Plantes, originally known as the Jardin du Roi, opened to the public in 1640. It became the Museum National d'Histoire Naturelle in 1793 during the French Revolution. Picture by Manuel Cohen
    LC_JDP_10_MC216.jpg
  • View from below of the pediment of the Galerie de Mineralogie, de Geologie et de Palobotanique (Gallery of Minerology, Geology and Paleobotany), built from 1833 to 1841 by Charles Rohault de Fleury and located in the Jardin des Plantes, Paris, 5th arrondissement, France. Founded in 1626 by Guy de La Brosse, Louis XIII's physician, the Jardin des Plantes, originally known as the Jardin du Roi, opened to the public in 1640. It became the Museum National d'Histoire Naturelle in 1793 during the French Revolution. Picture by Manuel Cohen
    LC_JDP_10_MC220.jpg
  • Early morning view, from the Grande Galerie de l'Evolution (Great Gallery of Evolution), of the entrance to the Galerie de Mineralogie, de Geologie et de Paleobotanique (Gallery of Minerology, Geology and Paleobotany), built from 1833 to 1841 by Charles Rohault de Fleury and located in the Jardin des Plantes, Paris, 5th arrondissement, France. Founded in 1626 by Guy de La Brosse, Louis XIII's physician, the Jardin des Plantes, originally known as the Jardin du Roi, opened to the public in 1640. It became the Museum National d'Histoire Naturelle in 1793 during the French Revolution. Picture by Manuel Cohen
    LC_JDP_10_MC323.jpg
  • View from below of the pediment of the Galerie de Mineralogie, de Geologie et de Paleobotanique (Gallery of Minerology, Geology and Paleobotany), built from 1833 to 1841 by Charles Rohault de Fleury and located in the Jardin des Plantes, Paris, 5th arrondissement, France. Founded in 1626 by Guy de La Brosse, Louis XIII's physician, the Jardin des Plantes, originally known as the Jardin du Roi, opened to the public in 1640. It became the Museum National d'Histoire Naturelle in 1793 during the French Revolution. Picture by Manuel Cohen
    LC_JDP_10_MC219.jpg
  • Early morning view of the entrance to the Galerie de Mineralogie, de Geologie et de Paleobotanique (Gallery of Minerology, Geology and Paleobotany), built from 1833 to 1841 by Charles Rohault de Fleury and located in the Jardin des Plantes, Paris, 5th arrondissement, France. Founded in 1626 by Guy de La Brosse, Louis XIII's physician, the Jardin des Plantes, originally known as the Jardin du Roi, opened to the public in 1640. It became the Museum National d'Histoire Naturelle in 1793 during the French Revolution. Picture by Manuel Cohen
    LC_JDP_10_MC332.jpg
  • Early morning view, from the Grande Galerie de l'Evolution (Great Gallery of Evolution), of the entrance to the Galerie de Mineralogie, de Geologie et de Paleobotanique (Gallery of Minerology, Geology and Paleobotany) with the staircase of the Grande Galerie de l'Evolution in the foreground, built from 1833 to 1841 by Charles Rohault de Fleury and located in the Jardin des Plantes, Paris, 5th arrondissement, France. Founded in 1626 by Guy de La Brosse, Louis XIII's physician, the Jardin des Plantes, originally known as the Jardin du Roi, opened to the public in 1640. It became the Museum National d'Histoire Naturelle in 1793 during the French Revolution.
    JDP_MCohen_MNHN_Choix07.jpg
  • Low angle mid-length view of the statue called Venus genitrix or Venus animant l'univers, created by Louis-Charles Dupaty in 1810 and located in the Rose Garden of the Jardin des Plantes, Paris, 5th arrondissement, France. In the background can be seen the Galerie de Mineralogie, de Geologie et de Paleobotanique (Gallery of Minerology, Geology and Paleobotany). Founded in 1626 by Guy de La Brosse, Louis XIII's physician, the Jardin des Plantes, originally known as the Jardin du Roi, opened to the public in 1640. It became the Museum National d'Histoire Naturelle in 1793 during the French Revolution. Venus Genitrix was given to the Museum National d'Histoire Naturelle circa 1818 and was classified as Historical Monuments in 1982.
    JDP_MCohen_MNHN+_Choix24.jpg
  • Illustrated information panel depicting past geological volcanic activity, with hot springs, mud pools, lava flows and volcanic eruptions, at the Garden of the Gods Visitor and Nature Center, at the Garden of The Gods, an area of geological rock formations protected as a public park, near Colorado Springs, Colorado, USA. The Garden of the Gods was listed as a National Natural Landmark in 1971. Picture by Manuel Cohen
    LC16_COLORADO_MC_134.jpg
  • Cathedral Valley with hogback formations and sentinels, Garden of The Gods, an area of geological rock formations protected as a public park, near Colorado Springs, Colorado, USA. The formations are the result of vertical tilting due to the uplift forces of the Rocky Mountains and the Pikes Peak massif, of the horizontal layers of sandstones, conglomerates and limestones, resulting after erosion in the formation of fins and pinnacles. Native Americans have visited the area since 1330 BC and camped here since 250 BC, sheltering under the cliffs and producing rock art. The Garden of the Gods was listed as a National Natural Landmark in 1971. Picture by Manuel Cohen
    LC16_COLORADO_MC_159.jpg
  • Cathedral Valley with hogback formations and sentinels, Garden of The Gods, an area of geological rock formations protected as a public park, near Colorado Springs, Colorado, USA. The formations are the result of vertical tilting due to the uplift forces of the Rocky Mountains and the Pikes Peak massif, of the horizontal layers of sandstones, conglomerates and limestones, resulting after erosion in the formation of fins and pinnacles. Native Americans have visited the area since 1330 BC and camped here since 250 BC, sheltering under the cliffs and producing rock art. The Garden of the Gods was listed as a National Natural Landmark in 1971. Picture by Manuel Cohen
    LC16_COLORADO_MC_164.jpg
  • Gray Rock (left) and South Gateway Rock (right), with the Manitou Springs incline behind and Pikes Peak above, at the Garden of The Gods, an area of geological rock formations protected as a public park, near Colorado Springs, Colorado, USA. The formations are the result of vertical tilting due to the uplift forces of the Rocky Mountains and the Pikes Peak massif, of the horizontal layers of  sandstones, conglomerates and limestones, resulting after erosion in the formation of fins and pinnacles. Native Americans have visited the area since 1330 BC and camped here since 250 BC, sheltering under the cliffs and producing rock art. The Garden of the Gods was listed as a National Natural Landmark in 1971. Picture by Manuel Cohen
    LC16_COLORADO_MC_161.jpg
  • Gray Rock (left) and South Gateway Rock (right), with the Manitou Springs incline behind and Pikes Peak above, at the Garden of The Gods, an area of geological rock formations protected as a public park, near Colorado Springs, Colorado, USA. The formations are the result of vertical tilting due to the uplift forces of the Rocky Mountains and the Pikes Peak massif, of the horizontal layers of sandstones, conglomerates and limestones, resulting after erosion in the formation of fins and pinnacles. Native Americans have visited the area since 1330 BC and camped here since 250 BC, sheltering under the cliffs and producing rock art. The Garden of the Gods was listed as a National Natural Landmark in 1971. Picture by Manuel Cohen
    LC16_COLORADO_MC_162.jpg
  • Gray Rock (left) and South Gateway Rock (right), with the Manitou Springs incline behind and Pikes Peak above, at the Garden of The Gods, an area of geological rock formations protected as a public park, near Colorado Springs, Colorado, USA. The formations are the result of vertical tilting due to the uplift forces of the Rocky Mountains and the Pikes Peak massif, of the horizontal layers of sandstones, conglomerates and limestones, resulting after erosion in the formation of fins and pinnacles. Native Americans have visited the area since 1330 BC and camped here since 250 BC, sheltering under the cliffs and producing rock art. The Garden of the Gods was listed as a National Natural Landmark in 1971. Picture by Manuel Cohen
    LC16_COLORADO_MC_160.jpg
  • Narrow vertical fin formations with rock climbers, at the Garden of The Gods, an area of geological rock formations protected as a public park, near Colorado Springs, Colorado, USA. The formations are the result of vertical tilting due to the uplift forces of the Rocky Mountains and the Pikes Peak massif, of the horizontal layers of sandstones, conglomerates and limestones, resulting after erosion in the formation of fins and pinnacles. Native Americans have visited the area since 1330 BC and camped here since 250 BC, sheltering under the cliffs and producing rock art. The Garden of the Gods was listed as a National Natural Landmark in 1971. Picture by Manuel Cohen
    LC16_COLORADO_MC_156.jpg
  • Cathedral Valley with hogback formations and sentinels, Garden of The Gods, an area of geological rock formations protected as a public park, near Colorado Springs, Colorado, USA. The formations are the result of vertical tilting due to the uplift forces of the Rocky Mountains and the Pikes Peak massif, of the horizontal layers of sandstones, conglomerates and limestones, resulting after erosion in the formation of fins and pinnacles. Native Americans have visited the area since 1330 BC and camped here since 250 BC, sheltering under the cliffs and producing rock art. The Garden of the Gods was listed as a National Natural Landmark in 1971. Picture by Manuel Cohen
    LC16_COLORADO_MC_154.jpg
  • Cathedral Valley with hogback formations and sentinels, Garden of The Gods, an area of geological rock formations protected as a public park, near Colorado Springs, Colorado, USA. The formations are the result of vertical tilting due to the uplift forces of the Rocky Mountains and the Pikes Peak massif, of the horizontal layers of sandstones, conglomerates and limestones, resulting after erosion in the formation of fins and pinnacles. Native Americans have visited the area since 1330 BC and camped here since 250 BC, sheltering under the cliffs and producing rock art. The Garden of the Gods was listed as a National Natural Landmark in 1971. Picture by Manuel Cohen
    LC16_COLORADO_MC_151.jpg
  • Fin formations in Cathedral Valley, at the Garden of The Gods, an area of geological rock formations protected as a public park, near Colorado Springs, Colorado, USA. The formations are the result of vertical tilting due to the uplift forces of the Rocky Mountains and the Pikes Peak massif, of the horizontal layers of sandstones, conglomerates and limestones, resulting after erosion in the formation of fins and pinnacles. Native Americans have visited the area since 1330 BC and camped here since 250 BC, sheltering under the cliffs and producing rock art. The Garden of the Gods was listed as a National Natural Landmark in 1971. Picture by Manuel Cohen
    LC16_COLORADO_MC_153.jpg
  • Garden of The Gods, an area of geological rock formations protected as a public park, near Colorado Springs, Colorado, USA. The formations are the result of vertical tilting due to the uplift forces of the Rocky Mountains and the Pikes Peak massif, of the horizontal layers of sandstones, conglomerates and limestones, resulting after erosion in the formation of fins and pinnacles. Native Americans have visited the area since 1330 BC and camped here since 250 BC, sheltering under the cliffs and producing rock art. The Garden of the Gods was listed as a National Natural Landmark in 1971. Picture by Manuel Cohen
    LC16_COLORADO_MC_149.jpg
  • Pinnacles of the Garden of The Gods, an area of geological rock formations protected as a public park, near Colorado Springs, Colorado, USA. The formations are the result of vertical tilting due to the uplift forces of the Rocky Mountains and the Pikes Peak massif, of the horizontal layers of sandstones, conglomerates and limestones, resulting after erosion in the formation of fins and pinnacles. Native Americans have visited the area since 1330 BC and camped here since 250 BC, sheltering under the cliffs and producing rock art. The Garden of the Gods was listed as a National Natural Landmark in 1971. Picture by Manuel Cohen
    LC16_COLORADO_MC_148.jpg
  • Gray Rock (left) and South Gateway Rock (right), with the Manitou Springs incline behind and Pikes Peak above, at the Garden of The Gods, an area of geological rock formations protected as a public park, near Colorado Springs, Colorado, USA. The formations are the result of vertical tilting due to the uplift forces of the Rocky Mountains and the Pikes Peak massif, of the horizontal layers of sandstones, conglomerates and limestones, resulting after erosion in the formation of fins and pinnacles. Native Americans have visited the area since 1330 BC and camped here since 250 BC, sheltering under the cliffs and producing rock art. The Garden of the Gods was listed as a National Natural Landmark in 1971. Picture by Manuel Cohen
    LC16_COLORADO_MC_147.jpg
  • Cathedral Valley with hogback formations and sentinels, Garden of The Gods, an area of geological rock formations protected as a public park, near Colorado Springs, Colorado, USA. The formations are the result of vertical tilting due to the uplift forces of the Rocky Mountains and the Pikes Peak massif, of the horizontal layers of sandstones, conglomerates and limestones, resulting after erosion in the formation of fins and pinnacles. Native Americans have visited the area since 1330 BC and camped here since 250 BC, sheltering under the cliffs and producing rock art. The Garden of the Gods was listed as a National Natural Landmark in 1971. Picture by Manuel Cohen
    LC16_COLORADO_MC_145.jpg
  • Gray Rock (left) and South Gateway Rock (right), with the Manitou Springs incline behind and Pikes Peak above, at the Garden of The Gods, an area of geological rock formations protected as a public park, near Colorado Springs, Colorado, USA. The formations are the result of vertical tilting due to the uplift forces of the Rocky Mountains and the Pikes Peak massif, of the horizontal layers of sandstones, conglomerates and limestones, resulting after erosion in the formation of fins and pinnacles. Native Americans have visited the area since 1330 BC and camped here since 250 BC, sheltering under the cliffs and producing rock art. The Garden of the Gods was listed as a National Natural Landmark in 1971. Picture by Manuel Cohen
    LC16_COLORADO_MC_157.jpg
  • Gray Rock (left) and South Gateway Rock (right), with the Manitou Springs incline behind and Pikes Peak above, at the Garden of The Gods, an area of geological rock formations protected as a public park, near Colorado Springs, Colorado, USA. The formations are the result of vertical tilting due to the uplift forces of the Rocky Mountains and the Pikes Peak massif, of the horizontal layers of sandstones, conglomerates and limestones, resulting after erosion in the formation of fins and pinnacles. Native Americans have visited the area since 1330 BC and camped here since 250 BC, sheltering under the cliffs and producing rock art. The Garden of the Gods was listed as a National Natural Landmark in 1971. Picture by Manuel Cohen
    LC16_COLORADO_MC_158.jpg
  • Cathedral Valley with hogback formations and sentinels, Garden of The Gods, an area of geological rock formations protected as a public park, near Colorado Springs, Colorado, USA. The formations are the result of vertical tilting due to the uplift forces of the Rocky Mountains and the Pikes Peak massif, of the horizontal layers of sandstones, conglomerates and limestones, resulting after erosion in the formation of fins and pinnacles. Native Americans have visited the area since 1330 BC and camped here since 250 BC, sheltering under the cliffs and producing rock art. The Garden of the Gods was listed as a National Natural Landmark in 1971. Picture by Manuel Cohen
    LC16_COLORADO_MC_155.jpg
  • Fin formations at the Garden of The Gods, an area of geological rock formations protected as a public park, near Colorado Springs, Colorado, USA. The formations are the result of vertical tilting due to the uplift forces of the Rocky Mountains and the Pikes Peak massif, of the horizontal layers of sandstones, conglomerates and limestones, resulting after erosion in the formation of fins and pinnacles. Native Americans have visited the area since 1330 BC and camped here since 250 BC, sheltering under the cliffs and producing rock art. The Garden of the Gods was listed as a National Natural Landmark in 1971. Picture by Manuel Cohen
    LC16_COLORADO_MC_152.jpg
  • Garden of The Gods, with the Three Graces formation (left), an area of geological rock formations protected as a public park, near Colorado Springs, Colorado, USA. The formations are the result of vertical tilting due to the uplift forces of the Rocky Mountains and the Pikes Peak massif, of the horizontal layers of sandstones, conglomerates and limestones, resulting after erosion in the formation of fins and pinnacles. Native Americans have visited the area since 1330 BC and camped here since 250 BC, sheltering under the cliffs and producing rock art. The Garden of the Gods was listed as a National Natural Landmark in 1971. Picture by Manuel Cohen
    LC16_COLORADO_MC_146.jpg
  • Pinnacles of the Garden of The Gods, an area of geological rock formations protected as a public park, near Colorado Springs, Colorado, USA. The formations are the result of vertical tilting due to the uplift forces of the Rocky Mountains and the Pikes Peak massif, of the horizontal layers of sandstones, conglomerates and limestones, resulting after erosion in the formation of fins and pinnacles. Native Americans have visited the area since 1330 BC and camped here since 250 BC, sheltering under the cliffs and producing rock art. The Garden of the Gods was listed as a National Natural Landmark in 1971. Picture by Manuel Cohen
    LC16_COLORADO_MC_144.jpg
  • Cathedral Valley with hogback formations and sentinels, Garden of The Gods, an area of geological rock formations protected as a public park, near Colorado Springs, Colorado, USA. The formations are the result of vertical tilting due to the uplift forces of the Rocky Mountains and the Pikes Peak massif, of the horizontal layers of sandstones, conglomerates and limestones, resulting after erosion in the formation of fins and pinnacles. Native Americans have visited the area since 1330 BC and camped here since 250 BC, sheltering under the cliffs and producing rock art. The Garden of the Gods was listed as a National Natural Landmark in 1971. Picture by Manuel Cohen
    LC16_COLORADO_MC_163.jpg
  • Cathedral Valley with hogback formations and sentinels, Garden of The Gods, an area of geological rock formations protected as a public park, near Colorado Springs, Colorado, USA. The formations are the result of vertical tilting due to the uplift forces of the Rocky Mountains and the Pikes Peak massif, of the horizontal layers of sandstones, conglomerates and limestones, resulting after erosion in the formation of fins and pinnacles. Native Americans have visited the area since 1330 BC and camped here since 250 BC, sheltering under the cliffs and producing rock art. The Garden of the Gods was listed as a National Natural Landmark in 1971. Picture by Manuel Cohen
    LC16_COLORADO_MC_150.jpg
  • The Iglesia de la Ermita Nueva, rebuilt in the 20th century and dedicated to the Virgen de Gracia or Our Lady of Grace, in the Barrio de la cuevas or Barrio troglodyte, an area housing half the population of Guadix in troglodyte dwellings, underground cave homes dug into the rock built to keep out the heat of the summer and the cold of the winter, Guadix, Andalusia, Southern Spain. The strange rock formations or badlands are formed by erosion of marine geological deposits. Picture by Manuel Cohen
    LC14_GRANADA_MC318.jpg
  • Barrio de la cuevas or Barrio troglodyte, an area housing half the population of Guadix in troglodyte dwellings, underground cave homes dug into the rock built to keep out the heat of the summer and the cold of the winter, Guadix, Andalusia, Southern Spain. The strange rock formations or badlands are formed by erosion of marine geological deposits. Picture by Manuel Cohen
    LC14_GRANADA_MC315.jpg
  • Barrio de la cuevas or Barrio troglodyte, an area housing half the population of Guadix in troglodyte dwellings, underground cave homes dug into the rock built to keep out the heat of the summer and the cold of the winter, Guadix, Andalusia, Southern Spain. The strange rock formations or badlands are formed by erosion of marine geological deposits. Picture by Manuel Cohen
    LC14_GRANADA_MC310.jpg
  • Barrio de la cuevas or Barrio troglodyte, an area housing half the population of Guadix in troglodyte dwellings, underground cave homes dug into the rock built to keep out the heat of the summer and the cold of the winter, Guadix, Andalusia, Southern Spain. The strange rock formations or badlands are formed by erosion of marine geological deposits. Picture by Manuel Cohen
    LC14_GRANADA_MC333.jpg
  • Barrio de la cuevas or Barrio troglodyte, an area housing half the population of Guadix in troglodyte dwellings, underground cave homes dug into the rock built to keep out the heat of the summer and the cold of the winter, Guadix, Andalusia, Southern Spain. The strange rock formations or badlands are formed by erosion of marine geological deposits. Picture by Manuel Cohen
    LC14_GRANADA_MC324.jpg
  • Barrio de la cuevas or Barrio troglodyte, an area housing half the population of Guadix in troglodyte dwellings, underground cave homes dug into the rock built to keep out the heat of the summer and the cold of the winter, Guadix, Andalusia, Southern Spain. The strange rock formations or badlands are formed by erosion of marine geological deposits. Picture by Manuel Cohen
    LC14_GRANADA_MC323.jpg
  • The Iglesia de la Ermita Nueva, rebuilt in the 20th century and dedicated to the Virgen de Gracia or Our Lady of Grace, in the Barrio de la cuevas or Barrio troglodyte, an area housing half the population of Guadix in troglodyte dwellings, underground cave homes dug into the rock built to keep out the heat of the summer and the cold of the winter, Guadix, Andalusia, Southern Spain. The strange rock formations or badlands are formed by erosion of marine geological deposits. Picture by Manuel Cohen
    LC14_GRANADA_MC317.jpg
  • The Iglesia de la Ermita Nueva, rebuilt in the 20th century and dedicated to the Virgen de Gracia or Our Lady of Grace, in the Barrio de la cuevas or Barrio troglodyte, an area housing half the population of Guadix in troglodyte dwellings, underground cave homes dug into the rock built to keep out the heat of the summer and the cold of the winter, Guadix, Andalusia, Southern Spain. The strange rock formations or badlands are formed by erosion of marine geological deposits. Picture by Manuel Cohen
    LC14_GRANADA_MC316.jpg
  • Barrio de la cuevas or Barrio troglodyte, an area housing half the population of Guadix in troglodyte dwellings, underground cave homes dug into the rock built to keep out the heat of the summer and the cold of the winter, Guadix, Andalusia, Southern Spain. The strange rock formations or badlands are formed by erosion of marine geological deposits. Picture by Manuel Cohen
    LC14_GRANADA_MC313.jpg
  • Small troglodyte church in the Barrio de la cuevas or Barrio troglodyte, an area housing half the population of Guadix in troglodyte dwellings, underground cave homes dug into the rock built to keep out the heat of the summer and the cold of the winter, Guadix, Andalusia, Southern Spain. The strange rock formations or badlands are formed by erosion of marine geological deposits. Picture by Manuel Cohen
    LC14_GRANADA_MC325.jpg
  • Barrio de la cuevas or Barrio troglodyte, an area housing half the population of Guadix in troglodyte dwellings, underground cave homes dug into the rock built to keep out the heat of the summer and the cold of the winter, Guadix, Andalusia, Southern Spain. The strange rock formations or badlands are formed by erosion of marine geological deposits. Picture by Manuel Cohen
    LC14_GRANADA_MC322.jpg
  • Nuestra Senora de Gracia or Our Lady of Grace, patron of the cave dwellers of Guadix, painted 4th October 1960 on tiles by J Gabarron, on the wall of a house in the Barrio de la cuevas or Barrio troglodyte, an area housing half the population of Guadix in troglodyte dwellings, underground cave homes dug into the rock built to keep out the heat of the summer and the cold of the winter, Guadix, Andalusia, Southern Spain. The strange rock formations or badlands are formed by erosion of marine geological deposits. Picture by Manuel Cohen
    LC14_GRANADA_MC320.jpg
  • Eroded rocks of the Bardenas Reales, a 42,000 hectare area of semi-desert and badlands, forming a UNESCO Biosphere Reserve, the Bardenas Reales Nature Reserve, in Navarre, Spain. The desert area is in the Ebro valley at the foot of the Yugo mountains and the Zaragoza region of Cinco Villas. Clay, chalk and sandstone terrain has been eroded by water and wind creating canyons, plateaus, tabular structures and isolated hills, called cabezos. Picture by Manuel Cohen
    LC19_SPAIN_MC284.jpg
  • Castildetierra, a large rock pinnacle or cabezo, in the Bardenas Reales, a 42,000 hectare area of semi-desert and badlands, forming a UNESCO Biosphere Reserve, the Bardenas Reales Nature Reserve, in Navarre, Spain. The desert area is in the Ebro valley at the foot of the Yugo mountains and the Zaragoza region of Cinco Villas. Clay, chalk and sandstone terrain has been eroded by water and wind creating canyons, plateaus, tabular structures and isolated hills, called cabezos. Picture by Manuel Cohen
    LC19_SPAIN_MC293.jpg
  • Bardenas Reales, a 42,000 hectare area of semi-desert and badlands, forming a UNESCO Biosphere Reserve, the Bardenas Reales Nature Reserve, in Navarre, Spain. The desert area is in the Ebro valley at the foot of the Yugo mountains and the Zaragoza region of Cinco Villas. Clay, chalk and sandstone terrain has been eroded by water and wind creating canyons, plateaus, tabular structures and isolated hills, called cabezos. Picture by Manuel Cohen
    LC19_SPAIN_MC296.jpg
  • Pasabag Valley or Monks' Valley, in Goreme National Park, near Goreme, in Nevsehir province, Cappadocia, Central Anatolia, Turkey. The rock formations here were made by erosion of the volcanic tuff created by ash from volcanic eruptions millions of years ago. Some of the chimneys in this valley were carved out to form hermitages for early christian monks. This area forms part of the Goreme National Park and the Rock Sites of Cappadocia UNESCO World Heritage Site. Picture by Manuel Cohen
    LC18_Cappadocia_MC_008.jpg
  • Twin fairy chimneys above the town of Urgup, in Nevsehir province, Cappadocia, Central Anatolia, Turkey. The chimneys were formed by erosion of the volcanic tuff created by ash from volcanic eruptions millions of years ago, and have caps of basalt on top which is slower to erode. Many of the chimneys have been hollowed out to form dwellings. Urgup was one of the first areas to be settled in the region and is now a tourist centre and home to the Cappadocian wine trade. This area forms part of the Goreme National Park and the Rock Sites of Cappadocia UNESCO World Heritage Site. Picture by Manuel Cohen
    LC18_Cappadocia_MC_011.jpg
  • Lunar landscape around the twin fairy chimneys above the town of Urgup, in Nevsehir province, Cappadocia, Central Anatolia, Turkey. The chimneys were formed by erosion of the volcanic tuff created by ash from volcanic eruptions millions of years ago, and have caps of basalt on top which is slower to erode. Many of the chimneys have been hollowed out to form dwellings. Urgup was one of the first areas to be settled in the region and is now a tourist centre and home to the Cappadocian wine trade. This area forms part of the Goreme National Park and the Rock Sites of Cappadocia UNESCO World Heritage Site. Picture by Manuel Cohen
    LC18_Cappadocia_MC_012.jpg
  • Kasabasi Kizil Vadi, or Red Valley, in Nevsehir province, Cappadocia, Central Anatolia, Turkey. The rock formations here were made by erosion of the volcanic tuff created by ash from volcanic eruptions millions of years ago. The valley contains many cave houses and churches, carved out of the rock by early christians fleeing persecution by the Romans. The colour of the rock changes dramatically with sunlight and the valley is popular for hiking and hot air balloon flights. This area forms part of the Goreme National Park and the Rock Sites of Cappadocia UNESCO World Heritage Site. Picture by Manuel Cohen
    LC18_Cappadocia_MC_020.jpg
  • Pancarlik Kilise or Pancarlik Church, early 11th century, in the Pancarlik Valley, Nevsehir province, Cappadocia, Central Anatolia, Turkey. The churches are carved from the soft volcanic tuff created by ash from volcanic eruptions millions of years ago. Early christians came here to flee persecution by the Romans and others settled here under the influence of early saints. This area forms part of the Goreme National Park and the Rock Sites of Cappadocia UNESCO World Heritage Site. Picture by Manuel Cohen
    LC18_Cappadocia_MC_035.jpg
  • Devrent Valley, known as Imagination Valley, near Goreme in Nevsehir province, Cappadocia, Central Anatolia, Turkey. The rock formations here were made by erosion of the volcanic tuff created by ash from volcanic eruptions millions of years ago, and many resemble figures or animals, such as camels, snakes, seals and dolphins. This area forms part of the Goreme National Park and the Rock Sites of Cappadocia UNESCO World Heritage Site. Picture by Manuel Cohen
    LC18_Cappadocia_MC_049.jpg
  • Devrent Valley, known as Imagination Valley, near Goreme in Nevsehir province, Cappadocia, Central Anatolia, Turkey. The rock formations here were made by erosion of the volcanic tuff created by ash from volcanic eruptions millions of years ago, and many resemble figures or animals, such as camels, snakes, seals and dolphins. This area forms part of the Goreme National Park and the Rock Sites of Cappadocia UNESCO World Heritage Site. Picture by Manuel Cohen
    LC18_Cappadocia_MC_053.jpg
  • Devrent Valley, known as Imagination Valley, near Goreme in Nevsehir province, Cappadocia, Central Anatolia, Turkey. The rock formations here were made by erosion of the volcanic tuff created by ash from volcanic eruptions millions of years ago, and many resemble figures or animals, such as camels, snakes, seals and dolphins. This area forms part of the Goreme National Park and the Rock Sites of Cappadocia UNESCO World Heritage Site. Picture by Manuel Cohen
    LC18_Cappadocia_MC_054.jpg
  • Devrent Valley, known as Imagination Valley, near Goreme in Nevsehir province, Cappadocia, Central Anatolia, Turkey. The rock formations here were made by erosion of the volcanic tuff created by ash from volcanic eruptions millions of years ago, and many resemble figures or animals, such as camels, snakes, seals and dolphins. This area forms part of the Goreme National Park and the Rock Sites of Cappadocia UNESCO World Heritage Site. Picture by Manuel Cohen
    LC18_Cappadocia_MC_061.jpg
  • Devrent Valley, known as Imagination Valley, near Goreme in Nevsehir province, Cappadocia, Central Anatolia, Turkey. The rock formations here were made by erosion of the volcanic tuff created by ash from volcanic eruptions millions of years ago, and many resemble figures or animals, such as camels, snakes, seals and dolphins. This area forms part of the Goreme National Park and the Rock Sites of Cappadocia UNESCO World Heritage Site. Picture by Manuel Cohen
    LC18_Cappadocia_MC_064.jpg
  • Devrent Valley, known as Imagination Valley, near Goreme in Nevsehir province, Cappadocia, Central Anatolia, Turkey. The rock formations here were made by erosion of the volcanic tuff created by ash from volcanic eruptions millions of years ago, and many resemble figures or animals, such as camels, snakes, seals and dolphins. This area forms part of the Goreme National Park and the Rock Sites of Cappadocia UNESCO World Heritage Site. Picture by Manuel Cohen
    LC18_Cappadocia_MC_065.jpg
  • Devrent Valley, known as Imagination Valley, near Goreme in Nevsehir province, Cappadocia, Central Anatolia, Turkey. The rock formations here were made by erosion of the volcanic tuff created by ash from volcanic eruptions millions of years ago, and many resemble figures or animals, such as camels, snakes, seals and dolphins. This area forms part of the Goreme National Park and the Rock Sites of Cappadocia UNESCO World Heritage Site. Picture by Manuel Cohen
    LC18_Cappadocia_MC_066.jpg
  • Devrent Valley, known as Imagination Valley, near Goreme in Nevsehir province, Cappadocia, Central Anatolia, Turkey. The rock formations here were made by erosion of the volcanic tuff created by ash from volcanic eruptions millions of years ago, and many resemble figures or animals, such as camels, snakes, seals and dolphins. This area forms part of the Goreme National Park and the Rock Sites of Cappadocia UNESCO World Heritage Site. Picture by Manuel Cohen
    LC18_Cappadocia_MC_075.jpg
  • Devrent Valley, known as Imagination Valley, near Goreme in Nevsehir province, Cappadocia, Central Anatolia, Turkey. The rock formations here were made by erosion of the volcanic tuff created by ash from volcanic eruptions millions of years ago, and many resemble figures or animals, such as camels, snakes, seals and dolphins. This area forms part of the Goreme National Park and the Rock Sites of Cappadocia UNESCO World Heritage Site. Picture by Manuel Cohen
    LC18_Cappadocia_MC_077.jpg
  • Fairy chimneys and cliffs in the Devrent Valley, known as Imagination Valley, near Goreme in Nevsehir province, Cappadocia, Central Anatolia, Turkey. The rock formations here were made by erosion of the volcanic tuff created by ash from volcanic eruptions millions of years ago, and many resemble figures or animals, such as camels, snakes, seals and dolphins. This area forms part of the Goreme National Park and the Rock Sites of Cappadocia UNESCO World Heritage Site. Picture by Manuel Cohen
    LC18_Cappadocia_MC_078.jpg
  • Eroded landscape of the Devrent Valley, known as Imagination Valley, near Goreme in Nevsehir province, Cappadocia, Central Anatolia, Turkey. The rock formations here were made by erosion of the volcanic tuff created by ash from volcanic eruptions millions of years ago, and many resemble figures or animals, such as camels, snakes, seals and dolphins. This area forms part of the Goreme National Park and the Rock Sites of Cappadocia UNESCO World Heritage Site. Picture by Manuel Cohen
    LC18_Cappadocia_MC_081.jpg
  • Landscape between Urgup in Nevsehir province and Ortahisar in Trabzon province, Cappadocia, Central Anatolia, Turkey. The rock formations here were made by erosion of the volcanic tuff created by ash from volcanic eruptions millions of years ago. Some of the formations have been carved out to form dwellings by early christians who came here to flee persecution by the Romans. This area forms part of the Goreme National Park and the Rock Sites of Cappadocia UNESCO World Heritage Site. Picture by Manuel Cohen
    LC18_Cappadocia_MC_083.jpg
  • Eroded rocks in the Goreme Valley, in Goreme National Park, between Goreme and Uchisar, in Nevsehir province, Cappadocia, Central Anatolia, Turkey. The rock formations here were made by erosion of the soft volcanic tuff created by ash from volcanic eruptions millions of years ago. The Goreme Valley also contains cave dwellings, underground towns and churches, carved out of the rock in the Byzantine period. This area forms part of the Goreme National Park and the Rock Sites of Cappadocia UNESCO World Heritage Site. Picture by Manuel Cohen
    LC18_Cappadocia_MC_090.jpg
  • Goreme Open Air Museum, consisting of many 10th - 12th century rock-cut monasteries, refectories, churches and monks' cells, and the town of Goreme in the distance, Goreme National Park, in Nevsehir province, Cappadocia, Central Anatolia, Turkey. The churches in Goreme are carved from the soft volcanic tuff created by ash from volcanic eruptions millions of years ago. Early christians came here to flee persecution by the Romans and others settled here under the influence of early saints. This area forms part of the Goreme National Park and the Rock Sites of Cappadocia UNESCO World Heritage Site. Picture by Manuel Cohen
    LC18_Cappadocia_MC_091.jpg
  • Ortahisar, a town in Trabzon province, Cappadocia, Central Anatolia, Turkey, with Ortahisar Castle, carved from what is known as the 'tallest fairy chimney in Cappadocia'. Surrounding the town are caves cut into the soft volcanic rock, used for storing locally produced fruits and vegetables. This area forms part of the Goreme National Park and the Rock Sites of Cappadocia UNESCO World Heritage Site. Picture by Manuel Cohen
    LC18_Cappadocia_MC_097.jpg
  • Ortahisar, a town in Trabzon province, Cappadocia, Central Anatolia, Turkey, with Ortahisar Castle, carved from what is known as the 'tallest fairy chimney in Cappadocia'. Surrounding the town are caves cut into the soft volcanic rock, used for storing locally produced fruits and vegetables. This area forms part of the Goreme National Park and the Rock Sites of Cappadocia UNESCO World Heritage Site. Picture by Manuel Cohen
    LC18_Cappadocia_MC_100.jpg
  • Landscape surrounding Ortahisar, in Trabzon province, Cappadocia, Central Anatolia, Turkey. The rock formations here were made by erosion of the volcanic tuff created by ash from volcanic eruptions millions of years ago. This area forms part of the Goreme National Park and the Rock Sites of Cappadocia UNESCO World Heritage Site. Picture by Manuel Cohen
    LC18_Cappadocia_MC_101.jpg
  • Landscape surrounding Ortahisar, in Trabzon province, Cappadocia, Central Anatolia, Turkey. The rock formations here were made by erosion of the volcanic tuff created by ash from volcanic eruptions millions of years ago. This area forms part of the Goreme National Park and the Rock Sites of Cappadocia UNESCO World Heritage Site. Picture by Manuel Cohen
    LC18_Cappadocia_MC_104.jpg
  • Landscape surrounding Ortahisar, in Trabzon province, Cappadocia, Central Anatolia, Turkey. The rock formations here were made by erosion of the volcanic tuff created by ash from volcanic eruptions millions of years ago. This area forms part of the Goreme National Park and the Rock Sites of Cappadocia UNESCO World Heritage Site. Picture by Manuel Cohen
    LC18_Cappadocia_MC_103.jpg
  • Hot air balloon flying above the Goreme Valley, in Goreme National Park, between Goreme and Uchisar, in Nevsehir province, Cappadocia, Central Anatolia, Turkey. The rock formations here were made by erosion of the soft volcanic tuff created by ash from volcanic eruptions millions of years ago. The Goreme Valley also contains cave dwellings, underground towns and churches, carved out of the rock in the Byzantine period. This area forms part of the Goreme National Park and the Rock Sites of Cappadocia UNESCO World Heritage Site. Picture by Manuel Cohen
    LC18_Cappadocia_MC_125.jpg
  • Fairy chimneys at Pasabag Valley or Monks' Valley, in Goreme National Park, near Goreme, in Nevsehir province, Cappadocia, Central Anatolia, Turkey. The rock formations here were made by erosion of the volcanic tuff created by ash from volcanic eruptions millions of years ago. Some of the chimneys in this valley were carved out to form hermitages for early christian monks. This area forms part of the Goreme National Park and the Rock Sites of Cappadocia UNESCO World Heritage Site. Picture by Manuel Cohen
    LC18_Cappadocia_MC_137.jpg
  • Devrent Valley, known as Imagination Valley, near Goreme in Nevsehir province, Cappadocia, Central Anatolia, Turkey. The rock formations here were made by erosion of the volcanic tuff created by ash from volcanic eruptions millions of years ago, and many resemble figures or animals, such as camels, snakes, seals and dolphins. This area forms part of the Goreme National Park and the Rock Sites of Cappadocia UNESCO World Heritage Site. Picture by Manuel Cohen
    LC18_Cappadocia_MC_142.jpg
  • Gaetan Brindejonc, coast guard on the Cote Sauvage on the Quiberon Peninsula, Morbihan, Brittany, France. He is depicted beside the natural stone arch called Arche de Port Blanc (Port Blanc Arch), keeping watch over the Natura 2000 zone, a specially protected conservation area. Picture by Manuel Cohen
    27102017_Gaetan_Brindejonc_MC07.jpg
  • The Great Kiva, built c. 1084, a large round ceremonial room with central fire pit, diverting stone and ventilation shaft, rebuilt in 1972, at Chimney Rock National Monument, in Chimney Rock State Park, in San Juan National Forest, South West Colorado, USA. The ridge was an ancestral Puebloan site occupied 925-1125 AD by around 2000 Indians. Chimney Rock was made a National Monument in 2012 and is listed on the US National Register of Historic Places and the Colorado State Register of Historic Properties. Picture by Manuel Cohen
    LC16_COLORADO_MC_093.jpg
  • Chimney Rock (right) and Companion Rock (left) in the evening, at Chimney Rock National Monument, in Chimney Rock State Park, in San Juan National Forest, South West Colorado, USA. The ridge was an ancestral Puebloan site occupied 925-1125 AD by around 2000 Indians. Chimney Rock was made a National Monument in 2012 and is listed on the US National Register of Historic Places and the Colorado State Register of Historic Properties. Picture by Manuel Cohen
    LC16_COLORADO_MC_092.jpg
  • Chimney Rock (right) and Companion Rock (left), at Chimney Rock National Monument, in Chimney Rock State Park, in San Juan National Forest, South West Colorado, USA. The ridge was an ancestral Puebloan site occupied 925-1125 AD by around 2000 Indians. Chimney Rock was made a National Monument in 2012 and is listed on the US National Register of Historic Places and the Colorado State Register of Historic Properties. Picture by Manuel Cohen
    LC16_COLORADO_MC_089.jpg
  • Chimney Rock (right) and Companion Rock (left), at Chimney Rock National Monument, in Chimney Rock State Park, in San Juan National Forest, South West Colorado, USA. The ridge was an ancestral Puebloan site occupied 925-1125 AD by around 2000 Indians. Chimney Rock was made a National Monument in 2012 and is listed on the US National Register of Historic Places and the Colorado State Register of Historic Properties. Picture by Manuel Cohen
    LC16_COLORADO_MC_088.jpg
  • Chimney Rock (right) and Companion Rock (left), at Chimney Rock National Monument, in Chimney Rock State Park, in San Juan National Forest, South West Colorado, USA. The ridge was an ancestral Puebloan site occupied 925-1125 AD by around 2000 Indians. Chimney Rock was made a National Monument in 2012 and is listed on the US National Register of Historic Places and the Colorado State Register of Historic Properties. Picture by Manuel Cohen
    LC16_COLORADO_MC_083.jpg
  • Man taking a photograph on the ridge with Chimney Rock (right) and Companion Rock (left), at Chimney Rock National Monument, in Chimney Rock State Park, in San Juan National Forest, South West Colorado, USA. The ridge was an ancestral Puebloan site occupied 925-1125 AD by around 2000 Indians. Chimney Rock was made a National Monument in 2012 and is listed on the US National Register of Historic Places and the Colorado State Register of Historic Properties. Picture by Manuel Cohen
    LC16_COLORADO_MC_082.jpg
  • Chimney Rock (right) and Companion Rock (left), at Chimney Rock National Monument, in Chimney Rock State Park, in San Juan National Forest, South West Colorado, USA. The ridge was an ancestral Puebloan site occupied 925-1125 AD by around 2000 Indians. Chimney Rock was made a National Monument in 2012 and is listed on the US National Register of Historic Places and the Colorado State Register of Historic Properties. Picture by Manuel Cohen
    LC16_COLORADO_MC_081.jpg
  • La Foradada with its natural rock arch, in the archipelago of the Columbretes Islands, a group of small uninhabited volcanic islets in the Mediterranean Sea, 49km off Orpesa, Valencia, Spain. There are 4 groups of islands in the archipelago, Columbret Gran, La Ferrera, La Foradada and El Carallot, and in 1988 the archipelago was declared a wildlife reserve. Picture by Manuel Cohen
    LC21_SPAIN_MC_0193.jpg
  • La Foradada with its natural rock arch, in the archipelago of the Columbretes Islands, a group of small uninhabited volcanic islets in the Mediterranean Sea, 49km off Orpesa, Valencia, Spain. There are 4 groups of islands in the archipelago, Columbret Gran, La Ferrera, La Foradada and El Carallot, and in 1988 the archipelago was declared a wildlife reserve. Picture by Manuel Cohen
    LC21_SPAIN_MC_0194.JPG
  • Bardenas Reales, a 42,000 hectare area of semi-desert and badlands, forming a UNESCO Biosphere Reserve, the Bardenas Reales Nature Reserve, in Navarre, Spain. The desert area is in the Ebro valley at the foot of the Yugo mountains and the Zaragoza region of Cinco Villas. Clay, chalk and sandstone terrain has been eroded by water and wind creating canyons, plateaus, tabular structures and isolated hills, called cabezos. Picture by Manuel Cohen
    LC19_SPAIN_MC285.JPG
  • Child playing on the rocks of the Bardenas Reales, a 42,000 hectare area of semi-desert and badlands, forming a UNESCO Biosphere Reserve, the Bardenas Reales Nature Reserve, in Navarre, Spain. The desert area is in the Ebro valley at the foot of the Yugo mountains and the Zaragoza region of Cinco Villas. Clay, chalk and sandstone terrain has been eroded by water and wind creating canyons, plateaus, tabular structures and isolated hills, called cabezos. Picture by Manuel Cohen
    LC19_SPAIN_MC286.jpg
  • Castildetierra, a large rock pinnacle or cabezo, in the Bardenas Reales, a 42,000 hectare area of semi-desert and badlands, forming a UNESCO Biosphere Reserve, the Bardenas Reales Nature Reserve, in Navarre, Spain. The desert area is in the Ebro valley at the foot of the Yugo mountains and the Zaragoza region of Cinco Villas. Clay, chalk and sandstone terrain has been eroded by water and wind creating canyons, plateaus, tabular structures and isolated hills, called cabezos. Picture by Manuel Cohen
    LC19_SPAIN_MC287.jpg
  • Castildetierra, a large rock pinnacle or cabezo, in the Bardenas Reales, a 42,000 hectare area of semi-desert and badlands, forming a UNESCO Biosphere Reserve, the Bardenas Reales Nature Reserve, in Navarre, Spain. The desert area is in the Ebro valley at the foot of the Yugo mountains and the Zaragoza region of Cinco Villas. Clay, chalk and sandstone terrain has been eroded by water and wind creating canyons, plateaus, tabular structures and isolated hills, called cabezos. Picture by Manuel Cohen
    LC19_SPAIN_MC288.jpg
  • Castildetierra, a large rock pinnacle or cabezo, in the Bardenas Reales, a 42,000 hectare area of semi-desert and badlands, forming a UNESCO Biosphere Reserve, the Bardenas Reales Nature Reserve, in Navarre, Spain. The desert area is in the Ebro valley at the foot of the Yugo mountains and the Zaragoza region of Cinco Villas. Clay, chalk and sandstone terrain has been eroded by water and wind creating canyons, plateaus, tabular structures and isolated hills, called cabezos. Picture by Manuel Cohen
    LC19_SPAIN_MC290.jpg
  • Sunrise over the Bardenas Reales, a 42,000 hectare area of semi-desert and badlands, forming a UNESCO Biosphere Reserve, the Bardenas Reales Nature Reserve, in Navarre, Spain. The desert area is in the Ebro valley at the foot of the Yugo mountains and the Zaragoza region of Cinco Villas. Clay, chalk and sandstone terrain has been eroded by water and wind creating canyons, plateaus, tabular structures and isolated hills, called cabezos. Picture by Manuel Cohen
    LC19_SPAIN_MC291.jpg
  • Bardenas Reales, a 42,000 hectare area of semi-desert and badlands, forming a UNESCO Biosphere Reserve, the Bardenas Reales Nature Reserve, in Navarre, Spain. The desert area is in the Ebro valley at the foot of the Yugo mountains and the Zaragoza region of Cinco Villas. Clay, chalk and sandstone terrain has been eroded by water and wind creating canyons, plateaus, tabular structures and isolated hills, called cabezos. Picture by Manuel Cohen
    LC19_SPAIN_MC295.jpg
  • Fairy chimneys at Pasabag Valley or Monks' Valley, in Goreme National Park, near Goreme, in Nevsehir province, Cappadocia, Central Anatolia, Turkey. The rock formations here were made by erosion of the volcanic tuff created by ash from volcanic eruptions millions of years ago. Some of the chimneys in this valley were carved out to form hermitages for early christian monks. This area forms part of the Goreme National Park and the Rock Sites of Cappadocia UNESCO World Heritage Site. Picture by Manuel Cohen
    LC18_Cappadocia_MC_001.jpg
  • Fairy chimneys at Pasabag Valley or Monks' Valley, in Goreme National Park, near Goreme, in Nevsehir province, Cappadocia, Central Anatolia, Turkey. The rock formations here were made by erosion of the volcanic tuff created by ash from volcanic eruptions millions of years ago. Some of the chimneys in this valley were carved out to form hermitages for early christian monks. This area forms part of the Goreme National Park and the Rock Sites of Cappadocia UNESCO World Heritage Site. Picture by Manuel Cohen
    LC18_Cappadocia_MC_003.jpg
  • Fairy chimneys at Pasabag Valley or Monks' Valley, in Goreme National Park, near Goreme, in Nevsehir province, Cappadocia, Central Anatolia, Turkey. The rock formations here were made by erosion of the volcanic tuff created by ash from volcanic eruptions millions of years ago. Some of the chimneys in this valley were carved out to form hermitages for early christian monks. This area forms part of the Goreme National Park and the Rock Sites of Cappadocia UNESCO World Heritage Site. Picture by Manuel Cohen
    LC18_Cappadocia_MC_002.jpg
  • Fairy chimneys at Pasabag Valley or Monks' Valley, in Goreme National Park, near Goreme, in Nevsehir province, Cappadocia, Central Anatolia, Turkey. The rock formations here were made by erosion of the volcanic tuff created by ash from volcanic eruptions millions of years ago. Some of the chimneys in this valley were carved out to form hermitages for early christian monks. This area forms part of the Goreme National Park and the Rock Sites of Cappadocia UNESCO World Heritage Site. Picture by Manuel Cohen
    LC18_Cappadocia_MC_005.jpg
  • Fairy chimney at Pasabag Valley or Monks' Valley, in Goreme National Park, near Goreme, in Nevsehir province, Cappadocia, Central Anatolia, Turkey. The rock formations here were made by erosion of the volcanic tuff created by ash from volcanic eruptions millions of years ago. Some of the chimneys in this valley were carved out to form hermitages for early christian monks. This area forms part of the Goreme National Park and the Rock Sites of Cappadocia UNESCO World Heritage Site. Picture by Manuel Cohen
    LC18_Cappadocia_MC_004.jpg
  • Fairy chimneys at Pasabag Valley or Monks' Valley, in Goreme National Park, near Goreme, in Nevsehir province, Cappadocia, Central Anatolia, Turkey. The rock formations here were made by erosion of the volcanic tuff created by ash from volcanic eruptions millions of years ago. Some of the chimneys in this valley were carved out to form hermitages for early christian monks. This area forms part of the Goreme National Park and the Rock Sites of Cappadocia UNESCO World Heritage Site. Picture by Manuel Cohen
    LC18_Cappadocia_MC_007.jpg
  • Fairy chimneys at Pasabag Valley or Monks' Valley, in Goreme National Park, near Goreme, in Nevsehir province, Cappadocia, Central Anatolia, Turkey. The rock formations here were made by erosion of the volcanic tuff created by ash from volcanic eruptions millions of years ago. Some of the chimneys in this valley were carved out to form hermitages for early christian monks. This area forms part of the Goreme National Park and the Rock Sites of Cappadocia UNESCO World Heritage Site. Picture by Manuel Cohen
    LC18_Cappadocia_MC_009.jpg
  • Kasabasi Kizil Vadi, or Red Valley, in Nevsehir province, Cappadocia, Central Anatolia, Turkey. The rock formations here were made by erosion of the volcanic tuff created by ash from volcanic eruptions millions of years ago. The valley contains many cave houses and churches, carved out of the rock by early christians fleeing persecution by the Romans. The colour of the rock changes dramatically with sunlight and the valley is popular for hiking and hot air balloon flights. This area forms part of the Goreme National Park and the Rock Sites of Cappadocia UNESCO World Heritage Site. Picture by Manuel Cohen
    LC18_Cappadocia_MC_013.jpg
  • Kasabasi Kizil Vadi, or Red Valley, in Nevsehir province, Cappadocia, Central Anatolia, Turkey. The rock formations here were made by erosion of the volcanic tuff created by ash from volcanic eruptions millions of years ago. The valley contains many cave houses and churches, carved out of the rock by early christians fleeing persecution by the Romans. The colour of the rock changes dramatically with sunlight and the valley is popular for hiking and hot air balloon flights. This area forms part of the Goreme National Park and the Rock Sites of Cappadocia UNESCO World Heritage Site. Picture by Manuel Cohen
    LC18_Cappadocia_MC_015.jpg
  • Kasabasi Kizil Vadi, or Red Valley, in Nevsehir province, Cappadocia, Central Anatolia, Turkey. The rock formations here were made by erosion of the volcanic tuff created by ash from volcanic eruptions millions of years ago. The valley contains many cave houses and churches, carved out of the rock by early christians fleeing persecution by the Romans. The colour of the rock changes dramatically with sunlight and the valley is popular for hiking and hot air balloon flights. This area forms part of the Goreme National Park and the Rock Sites of Cappadocia UNESCO World Heritage Site. Picture by Manuel Cohen
    LC18_Cappadocia_MC_014.jpg
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