Laja Falls
The Laja Falls (Spanish: Salto del Laja) is a waterfall located in the Laja River in southcentral Chile. It lies next to the old Pan-American Highway, between the cities of Los Ángeles and Chillán. Below the falls Laja River has formed a narrow canyon. The surroundings of the waterfall are very commercialized.
Two eastern falls from above
Laja Falls consist of four horseshoe shaped falls - one on each arm of Laja River. The tallest (35 m) is the easternmost fall, but the western falls are 20 m tall. Total width of all four falls - approximately 455 m.
Iguazu Falls, Brazil Side
Iguazu Falls, are waterfalls of the Iguazu River on the border of the Argentina province of Misiones and the Brazilian state of Paraná. The falls divide the river into the upper and lower Iguazu. The Iguazu River rises near the city of Curitiba. For most of its course, the river flows through Brazil, however, most of the falls are on the Argentine side. Below its confluence with the San Antonio River, the Iguazu River forms the boundary between Argentina and Brazil.
Iguazu Falls are located where the Iguazu River tumbles over the edge of the Paraná Plateau, 23 kilometres (14 mi) upriver from the Iguazu's confluence with the Paraná River. Numerous islands along the 2.7-kilometre-long (1.7 mi) edge divide the falls into many separate waterfalls and cataracts, varying between 60 to 82 metres (197 to 269 ft) high. The number of these smaller waterfalls fluctuates from 150 to 300, depending on the water level.[3] Approximately half of the river's flow falls into a long and narrow chasm called the Devil's Throat (Garganta del Diablo in Spanish or Garganta do Diabo in Portuguese). The Devil's Throat is U-shaped, 82 metres high, 150 m wide, and 700 m long (269×492×2,297 ft). Placenames have been given also to many other smaller falls, such as San Martín Falls, Bossetti Falls, and many others.
Iguazú Falls from the Argentine side
About 900 metres (2,950 ft) of the 2.7-kilometre (1.7 mi) length does not have water flowing over it. The edge of the basalt cap recedes by 3 mm (0.1 in) per year. The water of the lower Iguazu collects in a canyon that drains into the Paraná River, a short distance downstream from the Itaipu Dam. The junction of the water flows marks the border between Brazil, Argentina, and Paraguay. There are points in the cities of Foz do Iguaçu, Brazil, Puerto Iguazú, Argentina, and Ciudad del Este, Paraguay, which have access to the Iguazu River, where the borders of all three nations may be seen, a popular tourist attraction for visitors to the three cities.
Iguazu Falls, are waterfalls of the Iguazu River on the border of the Argentina province of Misiones and the Brazilian state of Paraná. The falls divide the river into the upper and lower Iguazu. The Iguazu River rises near the city of Curitiba. For most of its course, the river flows through Brazil, however, most of the falls are on the Argentine side. Below its confluence with the San Antonio River, the Iguazu River forms the boundary between Argentina and Brazil.
Iguazu Falls are located where the Iguazu River tumbles over the edge of the Paraná Plateau, 23 kilometres (14 mi) upriver from the Iguazu's confluence with the Paraná River. Numerous islands along the 2.7-kilometre-long (1.7 mi) edge divide the falls into many separate waterfalls and cataracts, varying between 60 to 82 metres (197 to 269 ft) high. The number of these smaller waterfalls fluctuates from 150 to 300, depending on the water level.[3] Approximately half of the river's flow falls into a long and narrow chasm called the Devil's Throat (Garganta del Diablo in Spanish or Garganta do Diabo in Portuguese). The Devil's Throat is U-shaped, 82 metres high, 150 m wide, and 700 m long (269×492×2,297 ft). Placenames have been given also to many other smaller falls, such as San Martín Falls, Bossetti Falls, and many others.
Iguazú Falls from the Argentine side
About 900 metres (2,950 ft) of the 2.7-kilometre (1.7 mi) length does not have water flowing over it. The edge of the basalt cap recedes by 3 mm (0.1 in) per year. The water of the lower Iguazu collects in a canyon that drains into the Paraná River, a short distance downstream from the Itaipu Dam. The junction of the water flows marks the border between Brazil, Argentina, and Paraguay. There are points in the cities of Foz do Iguaçu, Brazil, Puerto Iguazú, Argentina, and Ciudad del Este, Paraguay, which have access to the Iguazu River, where the borders of all three nations may be seen, a popular tourist attraction for visitors to the three cities.
Moraine Lake is a glacially-fed lake in Banff National Park, 14 kilometres (8.7 mi) outside the Village of Lake Louise, Alberta, Canada. It is situated in the Valley of the Ten Peaks, at an elevation of approximately 6,183 feet (1,885 m). The lake has a surface area of .5 square kilometres (0.19 sq mi).
The lake, being glacially fed, does not reach its crest until mid to late June. When it is full, it reflects a distinct shade of blue. The colour is due to the refraction of light off the rock flour deposited in the lake on a continual basis.
Grand Canyon
The Grand Canyon (Hopi: Ongtupqa; Yavapai: Wi:kaʼi:la, Spanish: Gran Cañón), is a steep-sided canyon carved by the Colorado River in the state of Arizona in the United States. It is contained within and managed by Grand Canyon National Park, the Hualapai Tribal Nation, the Havasupai Tribe and the Navajo Nation. President Theodore Roosevelt was a major proponent of preservation of the Grand Canyon area, and visited it on numerous occasions to hunt and enjoy the scenery.
The Grand Canyon is 277 miles (446 km) long, up to 18 miles (29 km) wide and attains a depth of over a mile (6,000 feet or 1,800 meters). Nearly two billion years of Earth's geological history have been exposed as the Colorado River and its tributaries cut their channels through layer after layer of rock while the Colorado Plateau was uplifted. While the specific geologic processes and timing that formed the Grand Canyon are the subject of debate by geologists, recent evidence suggests that the Colorado River established its course through the canyon at least 17 million years ago. Since that time, the Colorado River continued to erode and form the canyon to its present-day configuration.
For thousands of years, the area has been continuously inhabited by Native Americans who built settlements within the canyon and its many caves. The Pueblo people considered the Grand Canyon ("Ongtupqa" in the Hopi language) a holy site, and made pilgrimages to it. The first European known to have viewed the Grand Canyon was García López de Cárdenas from Spain, who arrived in 1540.
The Grand Canyon is 277 miles (446 km) long, up to 18 miles (29 km) wide and attains a depth of over a mile (6,000 feet or 1,800 meters). Nearly two billion years of Earth's geological history have been exposed as the Colorado River and its tributaries cut their channels through layer after layer of rock while the Colorado Plateau was uplifted. While the specific geologic processes and timing that formed the Grand Canyon are the subject of debate by geologists, recent evidence suggests that the Colorado River established its course through the canyon at least 17 million years ago. Since that time, the Colorado River continued to erode and form the canyon to its present-day configuration.
For thousands of years, the area has been continuously inhabited by Native Americans who built settlements within the canyon and its many caves. The Pueblo people considered the Grand Canyon ("Ongtupqa" in the Hopi language) a holy site, and made pilgrimages to it. The first European known to have viewed the Grand Canyon was García López de Cárdenas from Spain, who arrived in 1540.
Preikestolen
Preikestolen or Prekestolen, also known by the English translations of Preacher's Pulpit or Pulpit Rock, is a famous tourist attraction in Forsand, Ryfylke, Norway. It consists of a steep cliff which rises 604 metres (1982 feet) above Lysefjorden, opposite the Kjerag plateau, with an almost flat top of approximately 25 by 25 metres (82 by 82 feet).
Tourism at the site has been increasing in recent years, with between 150,000 and 200,000 visitors in 2012 making it one of the most visited natural tourist attractions in Norway. Due to its increased popularity, there is currently a project under way to improve the path to the site, which is only accessible via a 3.8 km (2.4 mi.) hike.
Tourism at the site has been increasing in recent years, with between 150,000 and 200,000 visitors in 2012 making it one of the most visited natural tourist attractions in Norway. Due to its increased popularity, there is currently a project under way to improve the path to the site, which is only accessible via a 3.8 km (2.4 mi.) hike.
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The Apostle Islands are a result of the glaciers that once covered North America. “Geologically they are originally part of the main land at the edge of the great rift or fault which formed the depression to which the waters of Lake Superior collected.” When the glaciers melted, waves from the waters of Lake Superior caused erosion that formed the islands. The islands are composed of mostly red sandstone because of the glacial shift.
It is widely assumed that Indians were the first to inhabit the island. “There is some evidence that they were seen and possibly visited sometime in the fourteenth century by Indians who were making their way to Isle Royale near the north shore of the land in search of copper.” Not long after, the islands were visited by Étienne Brûlé, a French explorer who, like many French Canadians, was trying to discover a new way to the East Indies. "Historians believe that the Jesuits named the islands the Apostle Islands according to their practice of giving holy names to new places." It is said that fur traders were the first explorers to settle in the area, building a village from the money they brought in.
United States Senator Gaylord Nelson sponsored the federal legislation that established the Apostle Islands National Lakeshore. Public Law 91-424 was signed by the President on September 26, 1970. It included 20 islands, a 12-mile (19 km) strip of the mainland, and approximately 1/4 mile of Lake Superior jurisdiction adjacent to each land unit.
Public Law 99-497 in 1986 added Long Island to the National Lakeshore and transferred ownership of all the light stations from the U.S. Coast Guard to the National Park Service.
After the National Park Service completed a wilderness study in 2004, and received overwhelming support from the public, Congress designated 80 percent of the land area of the national lakeshore as the Gaylord Nelson Wilderness on December 8, 2004. (Public Law 108-447, Division E, Section 140)
The National Park Travelers Club held its 2012 convention at the Apostle Islands.
Lake Michigan Ice Balls
Fly Geyser
Fly Geyser, also known as Fly Ranch Geyser or the Green Geyser is a man-made small geothermal geyserlocated in Washoe County, Nevada approximately 20 miles (32 km) north of Gerlach. Fly Geyser is located near the edge of Fly Reservoir and is only about 5 feet (1.5 m) high, but 12 feet (3.7 m) wide, counting the mound on which it sits.
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Shining Hearts
Shining Hearts is a 2009 role-playing video game developed and published by Sega. It is the first Shining game to be released for the PlayStation Portable and is the third with characters designed by Tony Taka, the other two being Shining Tears and Shining Wind.
The game has been adapted into an anime television series titled Shining Hearts: Shiawase no Pan that premiered in April 2012.
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