manuel cohen

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  • Les Orgues d'Ille-sur-Tet, fairy chimneys of rock created by erosion, at Ille-sur-Tet, Pyrenees-Orientales, France. The site is listed as a natural monument. Picture by Manuel Cohen
    LC20_FRANCE_MC_1657.jpg
  • Les Orgues d'Ille-sur-Tet, fairy chimneys of rock created by erosion, at Ille-sur-Tet, Pyrenees-Orientales, France. The cliffs of sand and clay have been sculpted by rainwater to create bulbous forms, tall spires and hoodoos, where harder rock sits on top of a column. The site is listed as a natural monument. Picture by Manuel Cohen
    LC20_FRANCE_MC_1643.jpg
  • Les Orgues d'Ille-sur-Tet, fairy chimneys of rock created by erosion, at Ille-sur-Tet, Pyrenees-Orientales, France. The cliffs of sand and clay have been sculpted by rainwater to create bulbous forms, tall spires and hoodoos, where harder rock sits on top of a column. The site is listed as a natural monument. Picture by Manuel Cohen
    LC20_FRANCE_MC_1641.jpg
  • Les Orgues d'Ille-sur-Tet, fairy chimneys of rock created by erosion, at Ille-sur-Tet, Pyrenees-Orientales, France. The site is listed as a natural monument. In the distance is the Pic du Canigou. The Canigou stands at 2784m and is the highest of the Eastern peaks of the Pyrenees. Picture by Manuel Cohen
    LC20_FRANCE_MC_1476.jpg
  • Les Orgues d'Ille-sur-Tet, fairy chimneys of rock created by erosion, at Ille-sur-Tet, Pyrenees-Orientales, France. The site is listed as a natural monument. In the distance is the Pic du Canigou. Picture by Manuel Cohen
    LC20_FRANCE_MC_1658.jpg
  • Les Orgues d'Ille-sur-Tet, fairy chimneys of rock created by erosion, aerial view, at Ille-sur-Tet, Pyrenees-Orientales, France. The site is listed as a natural monument. In the distance is the Pic du Canigou. The Canigou stands at 2784m and is the highest of the Eastern peaks of the Pyrenees. Picture by Manuel Cohen
    DRN_LC20_FRANCE_MC_1724.jpg
  • Les Orgues d'Ille-sur-Tet, fairy chimneys of rock created by erosion, at Ille-sur-Tet, Pyrenees-Orientales, France. The cliffs of sand and clay have been sculpted by rainwater to create bulbous forms, tall spires and hoodoos, where harder rock sits on top of a column. The site is listed as a natural monument. In the distance is the Pic du Canigou. The Canigou stands at 2784m and is the highest of the Eastern peaks of the Pyrenees. Picture by Manuel Cohen
    LC20_FRANCE_MC_1642.jpg
  • Rainbow over Les Orgues d'Ille-sur-Tet, fairy chimneys of rock created by erosion, at Ille-sur-Tet, Pyrenees-Orientales, France. The site is listed as a natural monument. Picture by Manuel Cohen
    LC20_FRANCE_MC_1562.jpg
  • Les Orgues d'Ille-sur-Tet, fairy chimneys of rock created by erosion, at Ille-sur-Tet, Pyrenees-Orientales, France. The site is listed as a natural monument. Picture by Manuel Cohen
    LC20_FRANCE_MC_1561.jpg
  • Les Orgues d'Ille-sur-Tet, fairy chimneys of rock created by erosion, at Ille-sur-Tet, Pyrenees-Orientales, France. The site is listed as a natural monument. Picture by Manuel Cohen
    LC20_FRANCE_MC_1659.jpg
  • Hoodoo at Les Orgues d'Ille-sur-Tet, fairy chimneys of rock created by erosion, at Ille-sur-Tet, Pyrenees-Orientales, France. The cliffs of sand and clay have been sculpted by rainwater to create bulbous forms, tall spires and hoodoos, where harder rock sits on top of a column. The site is listed as a natural monument. Picture by Manuel Cohen
    LC20_FRANCE_MC_1645.jpg
  • Hoodoo at Les Orgues d'Ille-sur-Tet, fairy chimneys of rock created by erosion, at Ille-sur-Tet, Pyrenees-Orientales, France. The cliffs of sand and clay have been sculpted by rainwater to create bulbous forms, tall spires and hoodoos, where harder rock sits on top of a column. The site is listed as a natural monument. Picture by Manuel Cohen
    LC20_FRANCE_MC_1644.jpg
  • Les Orgues d'Ille-sur-Tet, fairy chimneys of rock created by erosion, aerial view, at Ille-sur-Tet, Pyrenees-Orientales, France. The site is listed as a natural monument. In the distance is the Pic du Canigou. The Canigou stands at 2784m and is the highest of the Eastern peaks of the Pyrenees. Picture by Manuel Cohen
    DRN_LC20_FRANCE_MC_1740.jpg
  • Les Orgues d'Ille-sur-Tet, fairy chimneys of rock created by erosion, aerial view, at Ille-sur-Tet, Pyrenees-Orientales, France. The site is listed as a natural monument. Picture by Manuel Cohen
    DRN_LC20_FRANCE_MC_1736.jpg
  • Les Orgues d'Ille-sur-Tet, fairy chimneys of rock created by erosion, aerial view, at Ille-sur-Tet, Pyrenees-Orientales, France. The site is listed as a natural monument. In the distance is the Pic du Canigou. The Canigou stands at 2784m and is the highest of the Eastern peaks of the Pyrenees. Picture by Manuel Cohen
    DRN_LC20_FRANCE_MC_1727.jpg
  • Les Orgues d'Ille-sur-Tet, fairy chimneys of rock created by erosion, aerial view, at Ille-sur-Tet, Pyrenees-Orientales, France. The site is listed as a natural monument. In the distance is the Pic du Canigou. The Canigou stands at 2784m and is the highest of the Eastern peaks of the Pyrenees. Picture by Manuel Cohen
    DRN_LC20_FRANCE_MC_1711.jpg
  • Les Orgues d'Ille-sur-Tet, fairy chimneys of rock created by erosion, aerial view, at Ille-sur-Tet, Pyrenees-Orientales, France. The site is listed as a natural monument. Picture by Manuel Cohen
    DRN_LC20_FRANCE_MC_1729.jpg
  • Les Orgues d'Ille-sur-Tet, fairy chimneys of rock created by erosion, aerial view, at Ille-sur-Tet, Pyrenees-Orientales, France. The site is listed as a natural monument. In the distance is the Pic du Canigou. The Canigou stands at 2784m and is the highest of the Eastern peaks of the Pyrenees. Picture by Manuel Cohen
    DRN_LC20_FRANCE_MC_1728.jpg
  • Les Orgues d'Ille-sur-Tet, fairy chimneys of rock created by erosion, aerial view, at Ille-sur-Tet, Pyrenees-Orientales, France. The site is listed as a natural monument. In the distance is the Pic du Canigou. The Canigou stands at 2784m and is the highest of the Eastern peaks of the Pyrenees. Picture by Manuel Cohen
    DRN_LC20_FRANCE_MC_1714.jpg
  • Parque Natural de Bardenas Reales, aerial view, an arid region of semi-desert eroded landscape, in the Ebro valley depression, in Navarre, Northern Spain. The area covers 42,000 hectares between Tudela and Carcastillo, featuring badlands created by the erosion of the clay, chalk and sandstone soils by occasional heavy rains and a strong wind called cierzo. The area is listed as a UNESCO Biosphere Reserve. Picture by Manuel Cohen
    DRN_LC19_SPAIN_MC132.jpg
  • Castildetierra, a cabezo or fairy chimney, aerial view, in the Parque Natural de Bardenas Reales, an arid region of semi-desert eroded landscape, in the Ebro valley depression, in Navarre, Northern Spain. The area covers 42,000 hectares between Tudela and Carcastillo, featuring badlands created by the erosion of the clay, chalk and sandstone soils by occasional heavy rains and a strong wind called cierzo. The area is listed as a UNESCO Biosphere Reserve. Picture by Manuel Cohen
    DRN_LC19_SPAIN_MC124.jpg
  • Castildetierra, a cabezo or fairy chimney, aerial view, in the Parque Natural de Bardenas Reales, an arid region of semi-desert eroded landscape, in the Ebro valley depression, in Navarre, Northern Spain. The area covers 42,000 hectares between Tudela and Carcastillo, featuring badlands created by the erosion of the clay, chalk and sandstone soils by occasional heavy rains and a strong wind called cierzo. The area is listed as a UNESCO Biosphere Reserve. Picture by Manuel Cohen
    DRN_LC19_SPAIN_MC120.jpg
  • Parque Natural de Bardenas Reales, aerial view, an arid region of semi-desert eroded landscape, in the Ebro valley depression, in Navarre, Northern Spain. The area covers 42,000 hectares between Tudela and Carcastillo, featuring badlands created by the erosion of the clay, chalk and sandstone soils by occasional heavy rains and a strong wind called cierzo. The area is listed as a UNESCO Biosphere Reserve. Picture by Manuel Cohen
    DRN_LC19_SPAIN_MC115.jpg
  • Parque Natural de Bardenas Reales, aerial view, an arid region of semi-desert eroded landscape, in the Ebro valley depression, in Navarre, Northern Spain. The area covers 42,000 hectares between Tudela and Carcastillo, featuring badlands created by the erosion of the clay, chalk and sandstone soils by occasional heavy rains and a strong wind called cierzo. The area is listed as a UNESCO Biosphere Reserve. Picture by Manuel Cohen
    DRN_LC19_SPAIN_MC113.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_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
  • 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_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_020.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_048.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_052.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_063.jpg
  • Eroded landscape of Goreme National Park, between Goreme and Uchisar, 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 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_067.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_070.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_076.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_079.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_082.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_085.jpg
  • Fairy chimneys and cave dwellings 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_089.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
  • 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
  • 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', and rock formations formed by erosion of the tuff. 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_106.jpg
  • Town of Uchisar, in Pigeon Valley near Goreme, in Nevsehir province, Cappadocia, Central Anatolia, Turkey. In the centre is Uchisar Castle, the highest point in Cappadocia, with many rooms carved out of the rock. Many of the houses are carved into the soft volcanic rock, and the rock formations surrounding the town 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_114.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_132.jpg
  • Cueva de San Gabriel, created by limestone erosion, containing precolumbian petroglyphs of the Tainos culture, in the Parque Nacional de los Haitises, or Los Haitises National Park, on the North East coast of the Dominican Republic, in the Caribbean. The park was established in 1976 and consists of limestone karst scenery, mountains, subtropical forest and mangrove forests along the coast. Picture by Manuel Cohen
    LC18_DominicanRepublic_MC_049.jpg
  • Entrance to Merlin's Cave at low tide, at Tintagel Castle, built by Richard, 1st Earl of Cornwall in the 13th century, Tintagel Island, Cornwall, England. This is a sea cave caused by wave erosion and passes through Tintagel Island from Tintagel Haven on the East to West Cove on the West. In Tennyson's Idylls of the King, he describes waves bringing the infant King Arthur to shore and Merlin carrying him to safety. The ruined castle is also linked with Arthurian Legend, as Geoffrey of Monmouth cited it as the place of conception of King Arthur in his 12th century book, History of the Kings of England. The site is managed by English Heritage. Picture by Manuel Cohen
    LC17_ENGLAND_MC_103.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_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
  • 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
  • Parque Natural de Bardenas Reales, an arid region of semi-desert eroded landscape, in the Ebro valley depression, in Navarre, Northern Spain. The area covers 42,000 hectares between Tudela and Carcastillo, featuring badlands created by the erosion of the clay, chalk and sandstone soils by occasional heavy rains and a strong wind called cierzo. The area is listed as a UNESCO Biosphere Reserve. Picture by Manuel Cohen
    DRN_LC19_SPAIN_MC125.jpg
  • Gullies in the Parque Natural de Bardenas Reales, aerial view, an arid region of semi-desert eroded landscape, in the Ebro valley depression, in Navarre, Northern Spain. The area covers 42,000 hectares between Tudela and Carcastillo, featuring badlands created by the erosion of the clay, chalk and sandstone soils by occasional heavy rains and a strong wind called cierzo. The area is listed as a UNESCO Biosphere Reserve. Picture by Manuel Cohen
    DRN_LC19_SPAIN_MC123.jpg
  • Castildetierra, a cabezo or fairy chimney, aerial view, in the Parque Natural de Bardenas Reales, an arid region of semi-desert eroded landscape, in the Ebro valley depression, in Navarre, Northern Spain. The area covers 42,000 hectares between Tudela and Carcastillo, featuring badlands created by the erosion of the clay, chalk and sandstone soils by occasional heavy rains and a strong wind called cierzo. The area is listed as a UNESCO Biosphere Reserve. Picture by Manuel Cohen
    DRN_LC19_SPAIN_MC121.jpg
  • Parque Natural de Bardenas Reales, aerial view, an arid region of semi-desert eroded landscape, in the Ebro valley depression, in Navarre, Northern Spain. The area covers 42,000 hectares between Tudela and Carcastillo, featuring badlands created by the erosion of the clay, chalk and sandstone soils by occasional heavy rains and a strong wind called cierzo. The area is listed as a UNESCO Biosphere Reserve. Picture by Manuel Cohen
    DRN_LC19_SPAIN_MC118.jpg
  • Parque Natural de Bardenas Reales, aerial view, an arid region of semi-desert eroded landscape, in the Ebro valley depression, in Navarre, Northern Spain. The area covers 42,000 hectares between Tudela and Carcastillo, featuring badlands created by the erosion of the clay, chalk and sandstone soils by occasional heavy rains and a strong wind called cierzo. The area is listed as a UNESCO Biosphere Reserve. Picture by Manuel Cohen
    DRN_LC19_SPAIN_MC117.jpg
  • Parque Natural de Bardenas Reales, aerial view, an arid region of semi-desert eroded landscape, in the Ebro valley depression, in Navarre, Northern Spain. The area covers 42,000 hectares between Tudela and Carcastillo, featuring badlands created by the erosion of the clay, chalk and sandstone soils by occasional heavy rains and a strong wind called cierzo. The area is listed as a UNESCO Biosphere Reserve. Picture by Manuel Cohen
    DRN_LC19_SPAIN_MC116.jpg
  • Parque Natural de Bardenas Reales, aerial view, an arid region of semi-desert eroded landscape, in the Ebro valley depression, in Navarre, Northern Spain. The area covers 42,000 hectares between Tudela and Carcastillo, featuring badlands created by the erosion of the clay, chalk and sandstone soils by occasional heavy rains and a strong wind called cierzo. The area is listed as a UNESCO Biosphere Reserve. Picture by Manuel Cohen
    DRN_LC19_SPAIN_MC114.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 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_006.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
  • 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
  • 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_014.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_016.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_017.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_018.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_019.jpg
  • Troglodyte hermit house within a fairy chimney, in 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. 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_022.jpg
  • Fairy chimneys in 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_051.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_050.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_056.jpg
  • Fairy chimney in 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_057.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_059.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_060.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_062.jpg
  • Fairy chimneys in the eroded landscape of Goreme National Park, between Goreme and Uchisar, 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 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_068.jpg
  • Fairy chimneys in the eroded landscape of Goreme National Park, between Goreme and Uchisar, 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 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_069.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_071.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_072.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_074.jpg
  • Fairy chimneys and cliffs in the Devrent Valley, known as Imagination Valley, near Goreme in Nevsehir province, Cappadocia, Central Anatolia, Turkey. Homes have been carved out of the rock in the formations along the bottom of the cliff. 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_080.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_084.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_086.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_087.jpg
  • Fairy chimneys and cave dwellings 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_096.jpg
  • Eroded rocks near 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_105.jpg
  • Twin fairy chimneys 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. 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_107.jpg
  • Twin fairy chimneys 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. 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_108.jpg
  • Town of Uchisar, in Pigeon Valley near Goreme, in Nevsehir province, Cappadocia, Central Anatolia, Turkey. In the centre is Uchisar Castle, the highest point in Cappadocia, with many rooms carved out of the rock. Many of the houses are carved into the soft volcanic rock, and the rock formations surrounding the town 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_120.jpg
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