License: CC BY-ND 2.0 This picture is licensed under CC BY-ND 2.0.Picture by rosario fiore
Dunguaire Castle, Ireland
Dunguaire Castle (Irish: Dún Guaire) is a 16th-century tower house on the southeastern shore of Galway Bay in County Galway, Ireland, near Kinvarra (also spelled Kinvara). The name derives from the Dun of King Guaire, the legendary king of Connacht. The castle's 75-foot tower and its defensive wall have been restored, and the grounds are open to tourists during the summer.
License: CC BY 2.0 This picture is licensed under CC BY 2.0.Picture by Nicolas Raymond
Dunguaire Castle, Ireland
Dunguaire Castle (Irish: Dún Guaire) is a 16th-century tower house on the southeastern shore of Galway Bay in County Galway, Ireland, near Kinvarra (also spelled Kinvara). The name derives from the Dun of King Guaire, the legendary king of Connacht. The castle's 75-foot tower and its defensive wall have been restored, and the grounds are open to tourists during the summer.
License: CC BY 2.0 This picture is licensed under CC BY 2.0.Picture by Christopher Michel
Lake Pehoé, Chile
Lake Pehoé and Cordillera del Paine at sunrise. Lake Pehoé (Spanish pronunciation: [peoˈe]) is a surface water body located in Torres del Paine National Park, in the Magallanes Region of southern Chile. The lake is fed mainly by Paine River through the Nordenskjöld Lake, but it also receives the waters of the outlet of Skottsberg Lake.
License: CC BY 2.0 This picture is licensed under CC BY 2.0.Picture by Christopher Michel
Lake Pehoé, Chile
Lake Pehoé and Cordillera del Paine at sunrise. Lake Pehoé (Spanish pronunciation: [peoˈe]) is a surface water body located in Torres del Paine National Park, in the Magallanes Region of southern Chile. The lake is fed mainly by Paine River through the Nordenskjöld Lake, but it also receives the waters of the outlet of Skottsberg Lake.
License: CC BY 2.0 This picture is licensed under CC BY 2.0.Picture by Christopher Michel
Lake Pehoé, Chile
Lake Pehoé and Cordillera del Paine at sunrise. Lake Pehoé (Spanish pronunciation: [peoˈe]) is a surface water body located in Torres del Paine National Park, in the Magallanes Region of southern Chile. The lake is fed mainly by Paine River through the Nordenskjöld Lake, but it also receives the waters of the outlet of Skottsberg Lake.
License: CC BY 2.0 This picture is licensed under CC BY 2.0.Picture by Taro Taylor
Tavurvur (223 m), Papua New Guinea
Tavurvur is an active stratovolcano that lies near Rabaul, on the island of New Britain, in Papua New Guinea. It is a sub-vent of the Rabaul caldera and lies on the eastern rim of the larger feature. An eruption of the volcano largely destroyed the nearby town of Rabaul in 1994. Mount Tavurvur is the most active volcano in Rabaul caldera.
License: CC BY 2.0 This picture is licensed under CC BY 2.0.Picture by Taro Taylor
Tavurvur (223 m), Papua New Guinea
Tavurvur is an active stratovolcano that lies near Rabaul, on the island of New Britain, in Papua New Guinea. It is a sub-vent of the Rabaul caldera and lies on the eastern rim of the larger feature. An eruption of the volcano largely destroyed the nearby town of Rabaul in 1994. Mount Tavurvur is the most active volcano in Rabaul caldera.
License: CC BY-SA 2.0 This picture is licensed under CC BY-SA 2.0.Picture by Leonora Enking
Salar de Uyuni, Bolivia
Sunset over the Salar de Uyuni. Salar de Uyuni (or Salar de Tunupa) is the world's largest salt flat at 10,582 square kilometers. It is located in the Potosí and Oruro departments in southwest Bolivia, near the crest of the Andes and is at an elevation of 3656 m above mean sea level. The Salar was formed as a result of transformations between several prehistoric lakes. It is covered by a few meters of salt crust, which has an extraordinary flatness with the average altitude variations within one meter over the entire area of the Salar.
License: CC BY-SA 2.0 This picture is licensed under CC BY-SA 2.0.Picture by Leonora Enking
Salar de Uyuni, Bolivia
Sunset over the Salar de Uyuni. Salar de Uyuni (or Salar de Tunupa) is the world's largest salt flat at 10,582 square kilometers. It is located in the Potosí and Oruro departments in southwest Bolivia, near the crest of the Andes and is at an elevation of 3656 m above mean sea level. The Salar was formed as a result of transformations between several prehistoric lakes. It is covered by a few meters of salt crust, which has an extraordinary flatness with the average altitude variations within one meter over the entire area of the Salar.
License: CC BY-SA 2.0 This picture is licensed under CC BY-SA 2.0.Picture by Leonora Enking
Salar de Uyuni, Bolivia
Sunset over the Salar de Uyuni. Salar de Uyuni (or Salar de Tunupa) is the world's largest salt flat at 10,582 square kilometers. It is located in the Potosí and Oruro departments in southwest Bolivia, near the crest of the Andes and is at an elevation of 3656 m above mean sea level. The Salar was formed as a result of transformations between several prehistoric lakes. It is covered by a few meters of salt crust, which has an extraordinary flatness with the average altitude variations within one meter over the entire area of the Salar.
License: CC BY-SA 2.0 This picture is licensed under CC BY-SA 2.0.Picture by kris krüg
Salar de Uyuni, Bolivia
Sunrise over the Salar de Uyuni. Salar de Uyuni (or Salar de Tunupa) is the world's largest salt flat at 10,582 square kilometers. It is located in the Potosí and Oruro departments in southwest Bolivia, near the crest of the Andes and is at an elevation of 3656 m above mean sea level. The Salar was formed as a result of transformations between several prehistoric lakes. It is covered by a few meters of salt crust, which has an extraordinary flatness with the average altitude variations within one meter over the entire area of the Salar.
License: CC BY-SA 2.0 This picture is licensed under CC BY-SA 2.0.Picture by kris krüg
Salar de Uyuni, Bolivia
Sunrise over the Salar de Uyuni. Salar de Uyuni (or Salar de Tunupa) is the world's largest salt flat at 10,582 square kilometers. It is located in the Potosí and Oruro departments in southwest Bolivia, near the crest of the Andes and is at an elevation of 3656 m above mean sea level. The Salar was formed as a result of transformations between several prehistoric lakes. It is covered by a few meters of salt crust, which has an extraordinary flatness with the average altitude variations within one meter over the entire area of the Salar.
License: CC BY 2.0 This picture is licensed under CC BY 2.0.Picture by Colin Bowern
Mount Ngauruhoe (2291 m), New Zealand
Mount Ngauruhoe at sunset. Mount Ngauruhoe is an active stratovolcano or composite cone in New Zealand, made from layers of lava and tephra. It is the youngest vent in the Tongariro volcanic complex on the Central Plateau of the North Island, and first erupted about 2,500 years ago. Although seen by most as a volcano in its own right, it is technically a secondary cone of Mount Tongariro.
License: CC BY 2.0 This picture is licensed under CC BY 2.0.Picture by Jeff P
Mount Ngauruhoe (2291 m), New Zealand
Mount Ngauruhoe at sunset. Mount Ngauruhoe is an active stratovolcano or composite cone in New Zealand, made from layers of lava and tephra. It is the youngest vent in the Tongariro volcanic complex on the Central Plateau of the North Island, and first erupted about 2,500 years ago. Although seen by most as a volcano in its own right, it is technically a secondary cone of Mount Tongariro.
License: CC BY-SA 2.0 This picture is licensed under CC BY-SA 2.0.Picture by Mark Fischer
Angkor Wat, Cambodia
Angkor Wat in afternoon. Angkor Wat is the largest Hindu temple complex and the largest religious monument in the world. The temple was built by a king Suryavarman II in the early 12th century in Yasodharapura, the capital of the Khmer Empire, as his state temple and eventual mausoleum. Breaking from the Shaivism tradition of previous kings, Angkor Wat was instead dedicated to Vishnu.
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