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  • The Aldeyjarfoss waterfall is situated in the north of Iceland at the northern part of the Sprengisandur Highland Road which means it is to be found within the Highlands of Iceland.<br />
<br />
One of the most interesting features of the waterfall is the contrast between the black basalt columns and the white waters of the fall. In this, it is similar to the much smaller Icelandic waterfall Svartifoss in Skaftafell.<br />
<br />
The river Skjálfandafljót drops here from a height of 20 m. The basalt belongs to a lava field called Frambruni or Suðurárhraun, hraun being the Icelandic designation for lava.
    Aldeyjarfoss3.jpg
  • The Aldeyjarfoss waterfall is situated in the north of Iceland at the northern part of the Sprengisandur Highland Road which means it is to be found within the Highlands of Iceland.<br />
<br />
One of the most interesting features of the waterfall is the contrast between the black basalt columns and the white waters of the fall. In this, it is similar to the much smaller Icelandic waterfall Svartifoss in Skaftafell.<br />
<br />
The river Skjálfandafljót drops here from a height of 20 m. The basalt belongs to a lava field called Frambruni or Suðurárhraun, hraun being the Icelandic designation for lava.
    Aldeyjarfoss2.jpg
  • The Aldeyjarfoss waterfall is situated in the north of Iceland at the northern part of the Sprengisandur Highland Road which means it is to be found within the Highlands of Iceland.<br />
<br />
One of the most interesting features of the waterfall is the contrast between the black basalt columns and the white waters of the fall. In this, it is similar to the much smaller Icelandic waterfall Svartifoss in Skaftafell.<br />
<br />
The river Skjálfandafljót drops here from a height of 20 m. The basalt belongs to a lava field called Frambruni or Suðurárhraun, hraun being the Icelandic designation for lava.
    Aldeyjarfoss1.jpg
  • The Aldeyjarfoss waterfall is situated in the north of Iceland at the northern part of the Sprengisandur Highland Road which means it is to be found within the Highlands of Iceland.<br />
<br />
One of the most interesting features of the waterfall is the contrast between the black basalt columns and the white waters of the fall. In this, it is similar to the much smaller Icelandic waterfall Svartifoss in Skaftafell.<br />
<br />
The river Skjálfandafljót drops here from a height of 20 m. The basalt belongs to a lava field called Frambruni or Suðurárhraun, hraun being the Icelandic designation for lava.
    Aldeyjarfoss4.jpg
  • The Giant's Causeway (known in Irish as Clochán an Aifir or Clochán na bhFómharach) is an area of about 40,000 interlocking basalt columns, the result of an ancient volcanic eruption. It is located in County Antrim on the northeast coast of Northern Ireland, about three miles (4.8 km) northeast of the town of Bushmills. It was declared a World Heritage Site by UNESCO in 1986, and a National Nature Reserve in 1987 by the Department of the Environment for Northern Ireland. In a 2005 poll of Radio Times readers, the Giant's Causeway was named as the fourth greatest natural wonder in the United Kingdom. The tops of the columns form stepping stones that lead from the cliff foot and disappear under the sea. Most of the columns are hexagonal, although there are also some with four, five, seven and eight sides. The tallest are about 12 metres (39 ft) high, and the solidified lava in the cliffs is 28 metres thick in places.
    GiantsCausewayPool.jpg
  • The Giant's Causeway (known in Irish as Clochán an Aifir or Clochán na bhFómharach) is an area of about 40,000 interlocking basalt columns, the result of an ancient volcanic eruption. It is located in County Antrim on the northeast coast of Northern Ireland, about three miles (4.8 km) northeast of the town of Bushmills. It was declared a World Heritage Site by UNESCO in 1986, and a National Nature Reserve in 1987 by the Department of the Environment for Northern Ireland. In a 2005 poll of Radio Times readers, the Giant's Causeway was named as the fourth greatest natural wonder in the United Kingdom. The tops of the columns form stepping stones that lead from the cliff foot and disappear under the sea. Most of the columns are hexagonal, although there are also some with four, five, seven and eight sides. The tallest are about 12 metres (39 ft) high, and the solidified lava in the cliffs is 28 metres thick in places.
    GiantsCausewayMountain.jpg
  • The Giant's Causeway (known in Irish as Clochán an Aifir or Clochán na bhFómharach) is an area of about 40,000 interlocking basalt columns, the result of an ancient volcanic eruption. It is located in County Antrim on the northeast coast of Northern Ireland, about three miles (4.8 km) northeast of the town of Bushmills. It was declared a World Heritage Site by UNESCO in 1986, and a National Nature Reserve in 1987 by the Department of the Environment for Northern Ireland. In a 2005 poll of Radio Times readers, the Giant's Causeway was named as the fourth greatest natural wonder in the United Kingdom. The tops of the columns form stepping stones that lead from the cliff foot and disappear under the sea. Most of the columns are hexagonal, although there are also some with four, five, seven and eight sides. The tallest are about 12 metres (39 ft) high, and the solidified lava in the cliffs is 28 metres thick in places.
    GiantsCausewayCircle.jpg
  • The Giant's Causeway (known in Irish as Clochán an Aifir or Clochán na bhFómharach) is an area of about 40,000 interlocking basalt columns, the result of an ancient volcanic eruption. It is located in County Antrim on the northeast coast of Northern Ireland, about three miles (4.8 km) northeast of the town of Bushmills. It was declared a World Heritage Site by UNESCO in 1986, and a National Nature Reserve in 1987 by the Department of the Environment for Northern Ireland. In a 2005 poll of Radio Times readers, the Giant's Causeway was named as the fourth greatest natural wonder in the United Kingdom. The tops of the columns form stepping stones that lead from the cliff foot and disappear under the sea. Most of the columns are hexagonal, although there are also some with four, five, seven and eight sides. The tallest are about 12 metres (39 ft) high, and the solidified lava in the cliffs is 28 metres thick in places.
    GiantsCausewaySurf.jpg
  • The Giant's Causeway (known in Irish as Clochán an Aifir or Clochán na bhFómharach) is an area of about 40,000 interlocking basalt columns, the result of an ancient volcanic eruption. It is located in County Antrim on the northeast coast of Northern Ireland, about three miles (4.8 km) northeast of the town of Bushmills. It was declared a World Heritage Site by UNESCO in 1986, and a National Nature Reserve in 1987 by the Department of the Environment for Northern Ireland. In a 2005 poll of Radio Times readers, the Giant's Causeway was named as the fourth greatest natural wonder in the United Kingdom. The tops of the columns form stepping stones that lead from the cliff foot and disappear under the sea. Most of the columns are hexagonal, although there are also some with four, five, seven and eight sides. The tallest are about 12 metres (39 ft) high, and the solidified lava in the cliffs is 28 metres thick in places.
    GiantsCausewayStairs.jpg
  • The Giant's Causeway (known in Irish as Clochán an Aifir or Clochán na bhFómharach) is an area of about 40,000 interlocking basalt columns, the result of an ancient volcanic eruption. It is located in County Antrim on the northeast coast of Northern Ireland, about three miles (4.8 km) northeast of the town of Bushmills. It was declared a World Heritage Site by UNESCO in 1986, and a National Nature Reserve in 1987 by the Department of the Environment for Northern Ireland. In a 2005 poll of Radio Times readers, the Giant's Causeway was named as the fourth greatest natural wonder in the United Kingdom. The tops of the columns form stepping stones that lead from the cliff foot and disappear under the sea. Most of the columns are hexagonal, although there are also some with four, five, seven and eight sides. The tallest are about 12 metres (39 ft) high, and the solidified lava in the cliffs is 28 metres thick in places.
    GiantsCausewayHexagons2.jpg
  • The Giant's Causeway (known in Irish as Clochán an Aifir or Clochán na bhFómharach) is an area of about 40,000 interlocking basalt columns, the result of an ancient volcanic eruption. It is located in County Antrim on the northeast coast of Northern Ireland, about three miles (4.8 km) northeast of the town of Bushmills. It was declared a World Heritage Site by UNESCO in 1986, and a National Nature Reserve in 1987 by the Department of the Environment for Northern Ireland. In a 2005 poll of Radio Times readers, the Giant's Causeway was named as the fourth greatest natural wonder in the United Kingdom. The tops of the columns form stepping stones that lead from the cliff foot and disappear under the sea. Most of the columns are hexagonal, although there are also some with four, five, seven and eight sides. The tallest are about 12 metres (39 ft) high, and the solidified lava in the cliffs is 28 metres thick in places.
    GiantsCausewayBricks.jpg
  • The Giant's Causeway (known in Irish as Clochán an Aifir or Clochán na bhFómharach) is an area of about 40,000 interlocking basalt columns, the result of an ancient volcanic eruption. It is located in County Antrim on the northeast coast of Northern Ireland, about three miles (4.8 km) northeast of the town of Bushmills. It was declared a World Heritage Site by UNESCO in 1986, and a National Nature Reserve in 1987 by the Department of the Environment for Northern Ireland. In a 2005 poll of Radio Times readers, the Giant's Causeway was named as the fourth greatest natural wonder in the United Kingdom. The tops of the columns form stepping stones that lead from the cliff foot and disappear under the sea. Most of the columns are hexagonal, although there are also some with four, five, seven and eight sides. The tallest are about 12 metres (39 ft) high, and the solidified lava in the cliffs is 28 metres thick in places.
    GiantsCausewayEgg.jpg
  • The Giant's Causeway (known in Irish as Clochán an Aifir or Clochán na bhFómharach) is an area of about 40,000 interlocking basalt columns, the result of an ancient volcanic eruption. It is located in County Antrim on the northeast coast of Northern Ireland, about three miles (4.8 km) northeast of the town of Bushmills. It was declared a World Heritage Site by UNESCO in 1986, and a National Nature Reserve in 1987 by the Department of the Environment for Northern Ireland. In a 2005 poll of Radio Times readers, the Giant's Causeway was named as the fourth greatest natural wonder in the United Kingdom. The tops of the columns form stepping stones that lead from the cliff foot and disappear under the sea. Most of the columns are hexagonal, although there are also some with four, five, seven and eight sides. The tallest are about 12 metres (39 ft) high, and the solidified lava in the cliffs is 28 metres thick in places.
    GiantsCausewayWetHexagons.jpg
  • The Giant's Causeway (known in Irish as Clochán an Aifir or Clochán na bhFómharach) is an area of about 40,000 interlocking basalt columns, the result of an ancient volcanic eruption. It is located in County Antrim on the northeast coast of Northern Ireland, about three miles (4.8 km) northeast of the town of Bushmills. It was declared a World Heritage Site by UNESCO in 1986, and a National Nature Reserve in 1987 by the Department of the Environment for Northern Ireland. In a 2005 poll of Radio Times readers, the Giant's Causeway was named as the fourth greatest natural wonder in the United Kingdom. The tops of the columns form stepping stones that lead from the cliff foot and disappear under the sea. Most of the columns are hexagonal, although there are also some with four, five, seven and eight sides. The tallest are about 12 metres (39 ft) high, and the solidified lava in the cliffs is 28 metres thick in places.
    GiantsCausewayHexagons3.jpg
  • The Giant's Causeway (known in Irish as Clochán an Aifir or Clochán na bhFómharach) is an area of about 40,000 interlocking basalt columns, the result of an ancient volcanic eruption. It is located in County Antrim on the northeast coast of Northern Ireland, about three miles (4.8 km) northeast of the town of Bushmills. It was declared a World Heritage Site by UNESCO in 1986, and a National Nature Reserve in 1987 by the Department of the Environment for Northern Ireland. In a 2005 poll of Radio Times readers, the Giant's Causeway was named as the fourth greatest natural wonder in the United Kingdom. The tops of the columns form stepping stones that lead from the cliff foot and disappear under the sea. Most of the columns are hexagonal, although there are also some with four, five, seven and eight sides. The tallest are about 12 metres (39 ft) high, and the solidified lava in the cliffs is 28 metres thick in places.
    GiantsCausewayHexagons4.jpg
  • Toketee Falls is a waterfall in Douglas County, Oregon, United States, on the North Umpqua River at its confluence with the Clearwater River. It is located approximately 58 miles east of Roseburg near Oregon Route 138.<br />
<br />
Toketee (pronounced TOKE-uh-tee), is a Chinook Jargon word meaning "pretty" or "graceful". The falls was officially named by a United States Board on Geographic Names decision in 1916, over alternate names Ireland Falls and Toketie Falls. Carved from ancient columnar basalt, Toketee Falls drops approximately 120 feet in two stages.<br />
<br />
With a reliable water flow on the North Umpqua River, the falls avoids the seasonal fluctuations of other creek-fed waterfalls in Oregon. The waterfall is regulated by a dam built just upstream by PacifiCorp, which now regulates and reduces the water flow over the falls. The damming forms a reservoir called Toketee Lake. Previously the full volume of the North Umpqua River was allowed to flow over the falls, but the flow has been reduced by a penstock that utilizes the drop of the falls to generate hydroelectricity.
    ToketeeFalls2.jpg
  • Toketee Falls is a waterfall in Douglas County, Oregon, United States, on the North Umpqua River at its confluence with the Clearwater River. It is located approximately 58 miles east of Roseburg near Oregon Route 138.<br />
<br />
Toketee (pronounced TOKE-uh-tee), is a Chinook Jargon word meaning "pretty" or "graceful". The falls was officially named by a United States Board on Geographic Names decision in 1916, over alternate names Ireland Falls and Toketie Falls. Carved from ancient columnar basalt, Toketee Falls drops approximately 120 feet in two stages.<br />
<br />
With a reliable water flow on the North Umpqua River, the falls avoids the seasonal fluctuations of other creek-fed waterfalls in Oregon. The waterfall is regulated by a dam built just upstream by PacifiCorp, which now regulates and reduces the water flow over the falls. The damming forms a reservoir called Toketee Lake. Previously the full volume of the North Umpqua River was allowed to flow over the falls, but the flow has been reduced by a penstock that utilizes the drop of the falls to generate hydroelectricity.
    ToketeeFalls1.jpg
  • The Giant's Causeway (known in Irish as Clochán an Aifir or Clochán na bhFómharach) is an area of about 40,000 interlocking basalt columns, the result of an ancient volcanic eruption. It is located in County Antrim on the northeast coast of Northern Ireland, about three miles (4.8 km) northeast of the town of Bushmills. It was declared a World Heritage Site by UNESCO in 1986, and a National Nature Reserve in 1987 by the Department of the Environment for Northern Ireland. In a 2005 poll of Radio Times readers, the Giant's Causeway was named as the fourth greatest natural wonder in the United Kingdom. The tops of the columns form stepping stones that lead from the cliff foot and disappear under the sea. Most of the columns are hexagonal, although there are also some with four, five, seven and eight sides. The tallest are about 12 metres (39 ft) high, and the solidified lava in the cliffs is 28 metres thick in places.
    GiantsCausewayCove1.jpg
  • The Giant's Causeway (known in Irish as Clochán an Aifir or Clochán na bhFómharach) is an area of about 40,000 interlocking basalt columns, the result of an ancient volcanic eruption. It is located in County Antrim on the northeast coast of Northern Ireland, about three miles (4.8 km) northeast of the town of Bushmills. It was declared a World Heritage Site by UNESCO in 1986, and a National Nature Reserve in 1987 by the Department of the Environment for Northern Ireland. In a 2005 poll of Radio Times readers, the Giant's Causeway was named as the fourth greatest natural wonder in the United Kingdom. The tops of the columns form stepping stones that lead from the cliff foot and disappear under the sea. Most of the columns are hexagonal, although there are also some with four, five, seven and eight sides. The tallest are about 12 metres (39 ft) high, and the solidified lava in the cliffs is 28 metres thick in places.
    GiantsCausewayCoveWaves1.jpg
  • The Giant's Causeway (known in Irish as Clochán an Aifir or Clochán na bhFómharach) is an area of about 40,000 interlocking basalt columns, the result of an ancient volcanic eruption. It is located in County Antrim on the northeast coast of Northern Ireland, about three miles (4.8 km) northeast of the town of Bushmills. It was declared a World Heritage Site by UNESCO in 1986, and a National Nature Reserve in 1987 by the Department of the Environment for Northern Ireland. In a 2005 poll of Radio Times readers, the Giant's Causeway was named as the fourth greatest natural wonder in the United Kingdom. The tops of the columns form stepping stones that lead from the cliff foot and disappear under the sea. Most of the columns are hexagonal, although there are also some with four, five, seven and eight sides. The tallest are about 12 metres (39 ft) high, and the solidified lava in the cliffs is 28 metres thick in places.
    GiantsCausewayHexagons1.jpg
  • The Giant's Causeway (known in Irish as Clochán an Aifir or Clochán na bhFómharach) is an area of about 40,000 interlocking basalt columns, the result of an ancient volcanic eruption. It is located in County Antrim on the northeast coast of Northern Ireland, about three miles (4.8 km) northeast of the town of Bushmills. It was declared a World Heritage Site by UNESCO in 1986, and a National Nature Reserve in 1987 by the Department of the Environment for Northern Ireland. In a 2005 poll of Radio Times readers, the Giant's Causeway was named as the fourth greatest natural wonder in the United Kingdom. The tops of the columns form stepping stones that lead from the cliff foot and disappear under the sea. Most of the columns are hexagonal, although there are also some with four, five, seven and eight sides. The tallest are about 12 metres (39 ft) high, and the solidified lava in the cliffs is 28 metres thick in places.
    GiantsCausewaySunset.jpg
  • The Giant's Causeway (known in Irish as Clochán an Aifir or Clochán na bhFómharach) is an area of about 40,000 interlocking basalt columns, the result of an ancient volcanic eruption. It is located in County Antrim on the northeast coast of Northern Ireland, about three miles (4.8 km) northeast of the town of Bushmills. It was declared a World Heritage Site by UNESCO in 1986, and a National Nature Reserve in 1987 by the Department of the Environment for Northern Ireland. In a 2005 poll of Radio Times readers, the Giant's Causeway was named as the fourth greatest natural wonder in the United Kingdom. The tops of the columns form stepping stones that lead from the cliff foot and disappear under the sea. Most of the columns are hexagonal, although there are also some with four, five, seven and eight sides. The tallest are about 12 metres (39 ft) high, and the solidified lava in the cliffs is 28 metres thick in places.
    GiantsCausewayPeak2.jpg
  • The Giant's Causeway (known in Irish as Clochán an Aifir or Clochán na bhFómharach) is an area of about 40,000 interlocking basalt columns, the result of an ancient volcanic eruption. It is located in County Antrim on the northeast coast of Northern Ireland, about three miles (4.8 km) northeast of the town of Bushmills. It was declared a World Heritage Site by UNESCO in 1986, and a National Nature Reserve in 1987 by the Department of the Environment for Northern Ireland. In a 2005 poll of Radio Times readers, the Giant's Causeway was named as the fourth greatest natural wonder in the United Kingdom. The tops of the columns form stepping stones that lead from the cliff foot and disappear under the sea. Most of the columns are hexagonal, although there are also some with four, five, seven and eight sides. The tallest are about 12 metres (39 ft) high, and the solidified lava in the cliffs is 28 metres thick in places.
    GiantsCausewayCove.jpg
  • The Giant's Causeway (known in Irish as Clochán an Aifir or Clochán na bhFómharach) is an area of about 40,000 interlocking basalt columns, the result of an ancient volcanic eruption. It is located in County Antrim on the northeast coast of Northern Ireland, about three miles (4.8 km) northeast of the town of Bushmills. It was declared a World Heritage Site by UNESCO in 1986, and a National Nature Reserve in 1987 by the Department of the Environment for Northern Ireland. In a 2005 poll of Radio Times readers, the Giant's Causeway was named as the fourth greatest natural wonder in the United Kingdom. The tops of the columns form stepping stones that lead from the cliff foot and disappear under the sea. Most of the columns are hexagonal, although there are also some with four, five, seven and eight sides. The tallest are about 12 metres (39 ft) high, and the solidified lava in the cliffs is 28 metres thick in places.
    GiantsCausewayPeak1.jpg
  • The Giant's Causeway (known in Irish as Clochán an Aifir or Clochán na bhFómharach) is an area of about 40,000 interlocking basalt columns, the result of an ancient volcanic eruption. It is located in County Antrim on the northeast coast of Northern Ireland, about three miles (4.8 km) northeast of the town of Bushmills. It was declared a World Heritage Site by UNESCO in 1986, and a National Nature Reserve in 1987 by the Department of the Environment for Northern Ireland. In a 2005 poll of Radio Times readers, the Giant's Causeway was named as the fourth greatest natural wonder in the United Kingdom. The tops of the columns form stepping stones that lead from the cliff foot and disappear under the sea. Most of the columns are hexagonal, although there are also some with four, five, seven and eight sides. The tallest are about 12 metres (39 ft) high, and the solidified lava in the cliffs is 28 metres thick in places.
    GiantsCausewayShore.jpg
  • The Giant's Causeway (known in Irish as Clochán an Aifir or Clochán na bhFómharach) is an area of about 40,000 interlocking basalt columns, the result of an ancient volcanic eruption. It is located in County Antrim on the northeast coast of Northern Ireland, about three miles (4.8 km) northeast of the town of Bushmills. It was declared a World Heritage Site by UNESCO in 1986, and a National Nature Reserve in 1987 by the Department of the Environment for Northern Ireland. In a 2005 poll of Radio Times readers, the Giant's Causeway was named as the fourth greatest natural wonder in the United Kingdom. The tops of the columns form stepping stones that lead from the cliff foot and disappear under the sea. Most of the columns are hexagonal, although there are also some with four, five, seven and eight sides. The tallest are about 12 metres (39 ft) high, and the solidified lava in the cliffs is 28 metres thick in places.
    GiantsCausewayRockway1.jpg
  • Lower Proxy Falls in Proxy Falls state park in the Three Sisters Wilderness
    ProxyFalls2.jpg
  • Lower Proxy Falls in Proxy Falls state park in the Three Sisters Wilderness
    ProxyFalls7.jpg
  • Lower Proxy Falls in Proxy Falls state park in the Three Sisters Wilderness
    ProxyFalls2.jpg
  • Lower Proxy Falls in Proxy Falls state park in the Three Sisters Wilderness
    ProxyFalls2.jpg
  • Lower Proxy Falls in Proxy Falls state park in the Three Sisters Wilderness
    ProxyFallsWall6.jpg
  • Lower Proxy Falls in Proxy Falls state park in the Three Sisters Wilderness
    ProxyFalls1.jpg
  • Lower Proxy Falls in Proxy Falls state park in the Three Sisters Wilderness
    ProxyFalls7.jpg
  • Lower Proxy Falls in Proxy Falls state park in the Three Sisters Wilderness
    ProxyFalls3.jpg
  • Lower Proxy Falls in Proxy Falls state park in the Three Sisters Wilderness
    ProxyFalls2.jpg
  • Lower Proxy Falls in Proxy Falls state park in the Three Sisters Wilderness
    ProxyFalls2.jpg
  • Lower Proxy Falls in Proxy Falls state park in the Three Sisters Wilderness
    ProxyFalls6.jpg
  • Lower Proxy Falls in Proxy Falls state park in the Three Sisters Wilderness
    ProxyFallsWall6.jpg
  • Lower Proxy Falls in Proxy Falls state park in the Three Sisters Wilderness
    ProxyFallsCascade1.jpg
  • Lower Proxy Falls in Proxy Falls state park in the Three Sisters Wilderness
    ProxyFalls7.jpg
  • Lower Proxy Falls in Proxy Falls state park in the Three Sisters Wilderness
    ProxyFalls2.jpg
  • Lower Proxy Falls in Proxy Falls state park in the Three Sisters Wilderness
    ProxyFalls7.jpg
  • Lower Proxy Falls in Proxy Falls state park in the Three Sisters Wilderness
    ProxyFalls7.jpg
  • Lower Proxy Falls in Proxy Falls state park in the Three Sisters Wilderness
    ProxyFallsWall4.jpg
  • Lower Proxy Falls in Proxy Falls state park in the Three Sisters Wilderness
    ProxyFallsWall1-LAB.jpg
  • Lower Proxy Falls in Proxy Falls state park in the Three Sisters Wilderness
    ProxyFalls3.jpg
  • Dettifoss is a waterfall in Vatnajökull National Park in Northeast Iceland, and is reputed to be the most powerful waterfall in Europe. The water comes from the nearby Vatnajökull glacier, whose sediment-rich runoff colors the water a greyish white. The superlative of "most powerful" comes from its water flow times its fall distance. The water of the wide Jökulsá á Fjöllum river falls for more than 44 metres, causing a massive, crashing spray.
    Dettifoss2.jpg
  • The Oneonta Gorge is in the Columbia River Gorge in the American state of Oregon. The U.S. Forest Service has designated it as a botanical area because of the unique aquatic and woodland plants that grow there. The basalt walls are home to a wide variety of ferns, mosses, hepatics and lichens, many of which grow only in the Columbia River Gorge.
    OneontaFalls4.jpg
  • The Oneonta Gorge is in the Columbia River Gorge in the American state of Oregon. The U.S. Forest Service has designated it as a botanical area because of the unique aquatic and woodland plants that grow there. The basalt walls are home to a wide variety of ferns, mosses, hepatics and lichens, many of which grow only in the Columbia River Gorge.
    OneontaGorge1.jpg
  • The Oneonta Gorge is in the Columbia River Gorge in the American state of Oregon. The U.S. Forest Service has designated it as a botanical area because of the unique aquatic and woodland plants that grow there. The basalt walls are home to a wide variety of ferns, mosses, hepatics and lichens, many of which grow only in the Columbia River Gorge.
    OneontaGorge1.jpg
  • Mount Shuksan in Washington state's North Cascades National Park reflecting in Picture Lake. Mount Shuksan is a glaciated massif in the North Cascades National Park. Shuksan rises in Whatcom County, Washington immediately to the east of Mount Baker, and 11.6 miles  south of the Canadian border. The mountain's name Shuksan is derived from the Lummi word, said to mean "high peak". The highest point on the mountain is a three sided peak known as Summit Pyramid. There are two named subsidiary peaks: Nooksack Tower and The Hourglass. The mountain is composed of Shuksan greenschist, oceanic basalt that was metamorphosed when the Easton terrane collided with the west coast of North America, approximately 120 million years ago. The mountain is an eroded remnant of a thrust plate formed by the Easton collision.
    MtShuksanPictureLake3.jpg
  • The Oneonta Gorge is in the Columbia River Gorge in the American state of Oregon. The U.S. Forest Service has designated it as a botanical area because of the unique aquatic and woodland plants that grow there. The basalt walls are home to a wide variety of ferns, mosses, hepatics and lichens, many of which grow only in the Columbia River Gorge.
    OneontaGorge1.jpg
  • Harpa is a concert hall and conference centre in Reykjavík, Iceland. The opening concert was held on May 4, 2011. The building features a distinctive colored glass facade inspired by the basalt landscape of Iceland.
    _Y6A5785.jpg
  • The Oneonta Gorge is in the Columbia River Gorge in the American state of Oregon. The U.S. Forest Service has designated it as a botanical area because of the unique aquatic and woodland plants that grow there. The basalt walls are home to a wide variety of ferns, mosses, hepatics and lichens, many of which grow only in the Columbia River Gorge.
    OneontaFalls1.jpg
  • Crooked River and Smith Rock<br />
.....<br />
Smith Rock State Park is an American state park located in central Oregon's high desert near the communities of Redmond and Terrebonne. Its sheer cliffs of tuff and basalt are ideal for rock climbing of all difficulty levels. Smith Rock is generally considered the birthplace of modern American sport climbing, and is host to cutting-edge climbing routes. There is sport climbing, traditional climbing, multi-pitch climbing, and bouldering.<br />
<br />
The park contains the first U.S. climb rated 5.14. The area is well known for its challenging climbing routes so eventually all top climbers visit. In 1983, Allan Watts began to use sport climbing ethics which pushed American climbing to new levels. Shortly after, between 1992 and 2009, about 500 new climbing routes were added. This brought climbers from all over the world as Smith Rock became the world capital for sport climbing. To this day the park still attracts climbers from all over the world. The winter tends to be too cold (below freezing) for climbing and the summer months regularly reach the 100s °F. In addition to the world-famous rock climbing, Smith Rock State Park is host to many miles of hiking trails, the meandering Crooked River and views of the volcanic peaks of Oregon's Cascade Range.
    SmithRockBend1-LAB.jpg
  • The Oneonta Gorge is in the Columbia River Gorge in the American state of Oregon. The U.S. Forest Service has designated it as a botanical area because of the unique aquatic and woodland plants that grow there. The basalt walls are home to a wide variety of ferns, mosses, hepatics and lichens, many of which grow only in the Columbia River Gorge.
    OneontaGorge4.jpg
  • The Oneonta Gorge is in the Columbia River Gorge in the American state of Oregon. The U.S. Forest Service has designated it as a botanical area because of the unique aquatic and woodland plants that grow there. The basalt walls are home to a wide variety of ferns, mosses, hepatics and lichens, many of which grow only in the Columbia River Gorge.
    OneontaFalls7.jpg
  • Crooked River and Smith Rock<br />
.....<br />
Smith Rock State Park is an American state park located in central Oregon's high desert near the communities of Redmond and Terrebonne. Its sheer cliffs of tuff and basalt are ideal for rock climbing of all difficulty levels. Smith Rock is generally considered the birthplace of modern American sport climbing, and is host to cutting-edge climbing routes. There is sport climbing, traditional climbing, multi-pitch climbing, and bouldering.<br />
<br />
The park contains the first U.S. climb rated 5.14. The area is well known for its challenging climbing routes so eventually all top climbers visit. In 1983, Allan Watts began to use sport climbing ethics which pushed American climbing to new levels. Shortly after, between 1992 and 2009, about 500 new climbing routes were added. This brought climbers from all over the world as Smith Rock became the world capital for sport climbing. To this day the park still attracts climbers from all over the world. The winter tends to be too cold (below freezing) for climbing and the summer months regularly reach the 100s °F. In addition to the world-famous rock climbing, Smith Rock State Park is host to many miles of hiking trails, the meandering Crooked River and views of the volcanic peaks of Oregon's Cascade Range.
    SmithRockBend2.jpg
  • The Oneonta Gorge is in the Columbia River Gorge in the American state of Oregon. The U.S. Forest Service has designated it as a botanical area because of the unique aquatic and woodland plants that grow there. The basalt walls are home to a wide variety of ferns, mosses, hepatics and lichens, many of which grow only in the Columbia River Gorge.
    OneontaGorge3.jpg
  • The Oneonta Gorge is in the Columbia River Gorge in the American state of Oregon. The U.S. Forest Service has designated it as a botanical area because of the unique aquatic and woodland plants that grow there. The basalt walls are home to a wide variety of ferns, mosses, hepatics and lichens, many of which grow only in the Columbia River Gorge.
    OneontaFalls4.jpg
  • Mount Shuksan in Washington state's North Cascades National Park reflecting in Picture Lake. Mount Shuksan is a glaciated massif in the North Cascades National Park. Shuksan rises in Whatcom County, Washington immediately to the east of Mount Baker, and 11.6 miles  south of the Canadian border. The mountain's name Shuksan is derived from the Lummi word, said to mean "high peak". The highest point on the mountain is a three sided peak known as Summit Pyramid. There are two named subsidiary peaks: Nooksack Tower and The Hourglass. The mountain is composed of Shuksan greenschist, oceanic basalt that was metamorphosed when the Easton terrane collided with the west coast of North America, approximately 120 million years ago. The mountain is an eroded remnant of a thrust plate formed by the Easton collision.
    MtShuksanPictureLake7.jpg
  • The Oneonta Gorge is in the Columbia River Gorge in the American state of Oregon. The U.S. Forest Service has designated it as a botanical area because of the unique aquatic and woodland plants that grow there. The basalt walls are home to a wide variety of ferns, mosses, hepatics and lichens, many of which grow only in the Columbia River Gorge.
    OneontaFalls4.jpg
  • Harpa is a concert hall and conference centre in Reykjavík, Iceland. The opening concert was held on May 4, 2011. The building features a distinctive colored glass facade inspired by the basalt landscape of Iceland.
    _Y6A5796.jpg
  • Harpa is a concert hall and conference centre in Reykjavík, Iceland. The opening concert was held on May 4, 2011. The building features a distinctive colored glass facade inspired by the basalt landscape of Iceland.
    Harpa1.jpg
  • Mount Shuksan in Washington state's North Cascades National Park reflecting in Picture Lake. Mount Shuksan is a glaciated massif in the North Cascades National Park. Shuksan rises in Whatcom County, Washington immediately to the east of Mount Baker, and 11.6 miles  south of the Canadian border. The mountain's name Shuksan is derived from the Lummi word, said to mean "high peak". The highest point on the mountain is a three sided peak known as Summit Pyramid. There are two named subsidiary peaks: Nooksack Tower and The Hourglass. The mountain is composed of Shuksan greenschist, oceanic basalt that was metamorphosed when the Easton terrane collided with the west coast of North America, approximately 120 million years ago. The mountain is an eroded remnant of a thrust plate formed by the Easton collision.
    MtShuksanPictureLake3.jpg
  • Mount Shuksan in Washington state's North Cascades National Park reflecting in Picture Lake. Mount Shuksan is a glaciated massif in the North Cascades National Park. Shuksan rises in Whatcom County, Washington immediately to the east of Mount Baker, and 11.6 miles  south of the Canadian border. The mountain's name Shuksan is derived from the Lummi word, said to mean "high peak". The highest point on the mountain is a three sided peak known as Summit Pyramid. There are two named subsidiary peaks: Nooksack Tower and The Hourglass. The mountain is composed of Shuksan greenschist, oceanic basalt that was metamorphosed when the Easton terrane collided with the west coast of North America, approximately 120 million years ago. The mountain is an eroded remnant of a thrust plate formed by the Easton collision.
    MtShuksanPictureLake3.jpg
  • Mount Shuksan in Washington state's North Cascades National Park reflecting in Picture Lake. Mount Shuksan is a glaciated massif in the North Cascades National Park. Shuksan rises in Whatcom County, Washington immediately to the east of Mount Baker, and 11.6 miles  south of the Canadian border. The mountain's name Shuksan is derived from the Lummi word, said to mean "high peak". The highest point on the mountain is a three sided peak known as Summit Pyramid. There are two named subsidiary peaks: Nooksack Tower and The Hourglass. The mountain is composed of Shuksan greenschist, oceanic basalt that was metamorphosed when the Easton terrane collided with the west coast of North America, approximately 120 million years ago. The mountain is an eroded remnant of a thrust plate formed by the Easton collision.
    MtShuksanPictureLake3.jpg
  • The Oneonta Gorge is in the Columbia River Gorge in the American state of Oregon. The U.S. Forest Service has designated it as a botanical area because of the unique aquatic and woodland plants that grow there. The basalt walls are home to a wide variety of ferns, mosses, hepatics and lichens, many of which grow only in the Columbia River Gorge.
    OneontaGorge2.jpg
  • Multnomah Falls in Columbia River Gorge, Oregon.<br />
---<br />
Multnomah Falls is a waterfall located on Multnomah Creek in the Columbia River Gorge, east of Troutdale, between Corbett and Dodson, Oregon, United States. The waterfall is accessible from the Historic Columbia River Highway and Interstate 84. Spanning two tiers on basalt cliffs, it is the tallest waterfall in the state of Oregon at 620 ft in height.<br />
<br />
The land surrounding the falls was developed by Simon Benson in the early-twentieth century, with a pathway, viewing bridge, and adjacent lodge being constructed in 1925. The Multnomah Falls Lodge and the surrounding footpaths at the falls were added to the National Register of Historic Places in 1981. Contemporarily, the state of Oregon maintains a switchback trail that ascends to a talus slope 100 feet above the falls, and descends to an observation deck that overlooks the falls' edge. The falls attract over two million visitors each year, making it the most-visited natural recreation site in the U.S. Pacific Northwest.
    MultnomahFalls1.jpg
  • The Oneonta Gorge is in the Columbia River Gorge in the American state of Oregon. The U.S. Forest Service has designated it as a botanical area because of the unique aquatic and woodland plants that grow there. The basalt walls are home to a wide variety of ferns, mosses, hepatics and lichens, many of which grow only in the Columbia River Gorge.
    OneontaFalls6.jpg
  • Mount Shuksan in Washington state's North Cascades National Park reflecting in Picture Lake. Mount Shuksan is a glaciated massif in the North Cascades National Park. Shuksan rises in Whatcom County, Washington immediately to the east of Mount Baker, and 11.6 miles  south of the Canadian border. The mountain's name Shuksan is derived from the Lummi word, said to mean "high peak". The highest point on the mountain is a three sided peak known as Summit Pyramid. There are two named subsidiary peaks: Nooksack Tower and The Hourglass. The mountain is composed of Shuksan greenschist, oceanic basalt that was metamorphosed when the Easton terrane collided with the west coast of North America, approximately 120 million years ago. The mountain is an eroded remnant of a thrust plate formed by the Easton collision.
    MtShuksanPictureLake3.jpg
  • Multnomah Falls in Columbia River Gorge, Oregon.<br />
---<br />
Multnomah Falls is a waterfall located on Multnomah Creek in the Columbia River Gorge, east of Troutdale, between Corbett and Dodson, Oregon, United States. The waterfall is accessible from the Historic Columbia River Highway and Interstate 84. Spanning two tiers on basalt cliffs, it is the tallest waterfall in the state of Oregon at 620 ft in height.<br />
<br />
The land surrounding the falls was developed by Simon Benson in the early-twentieth century, with a pathway, viewing bridge, and adjacent lodge being constructed in 1925. The Multnomah Falls Lodge and the surrounding footpaths at the falls were added to the National Register of Historic Places in 1981. Contemporarily, the state of Oregon maintains a switchback trail that ascends to a talus slope 100 feet above the falls, and descends to an observation deck that overlooks the falls' edge. The falls attract over two million visitors each year, making it the most-visited natural recreation site in the U.S. Pacific Northwest.
    MultnomahAutumn1.jpg
  • Multnomah Falls in Columbia River Gorge, Oregon.<br />
---<br />
Multnomah Falls is a waterfall located on Multnomah Creek in the Columbia River Gorge, east of Troutdale, between Corbett and Dodson, Oregon, United States. The waterfall is accessible from the Historic Columbia River Highway and Interstate 84. Spanning two tiers on basalt cliffs, it is the tallest waterfall in the state of Oregon at 620 ft in height.<br />
<br />
The land surrounding the falls was developed by Simon Benson in the early-twentieth century, with a pathway, viewing bridge, and adjacent lodge being constructed in 1925. The Multnomah Falls Lodge and the surrounding footpaths at the falls were added to the National Register of Historic Places in 1981. Contemporarily, the state of Oregon maintains a switchback trail that ascends to a talus slope 100 feet above the falls, and descends to an observation deck that overlooks the falls' edge. The falls attract over two million visitors each year, making it the most-visited natural recreation site in the U.S. Pacific Northwest.
    UpperMultnomah1.jpg
  • The Oneonta Gorge is in the Columbia River Gorge in the American state of Oregon. The U.S. Forest Service has designated it as a botanical area because of the unique aquatic and woodland plants that grow there. The basalt walls are home to a wide variety of ferns, mosses, hepatics and lichens, many of which grow only in the Columbia River Gorge.
    OneontaGorge1.jpg
  • Mount Shuksan in Washington state's North Cascades National Park reflecting in Picture Lake. Mount Shuksan is a glaciated massif in the North Cascades National Park. Shuksan rises in Whatcom County, Washington immediately to the east of Mount Baker, and 11.6 miles  south of the Canadian border. The mountain's name Shuksan is derived from the Lummi word, said to mean "high peak". The highest point on the mountain is a three sided peak known as Summit Pyramid. There are two named subsidiary peaks: Nooksack Tower and The Hourglass. The mountain is composed of Shuksan greenschist, oceanic basalt that was metamorphosed when the Easton terrane collided with the west coast of North America, approximately 120 million years ago. The mountain is an eroded remnant of a thrust plate formed by the Easton collision.
    MtShuksanPictureLake3.jpg
  • Crooked River and Smith Rock<br />
.....<br />
Smith Rock State Park is an American state park located in central Oregon's high desert near the communities of Redmond and Terrebonne. Its sheer cliffs of tuff and basalt are ideal for rock climbing of all difficulty levels. Smith Rock is generally considered the birthplace of modern American sport climbing, and is host to cutting-edge climbing routes. There is sport climbing, traditional climbing, multi-pitch climbing, and bouldering.<br />
<br />
The park contains the first U.S. climb rated 5.14. The area is well known for its challenging climbing routes so eventually all top climbers visit. In 1983, Allan Watts began to use sport climbing ethics which pushed American climbing to new levels. Shortly after, between 1992 and 2009, about 500 new climbing routes were added. This brought climbers from all over the world as Smith Rock became the world capital for sport climbing. To this day the park still attracts climbers from all over the world. The winter tends to be too cold (below freezing) for climbing and the summer months regularly reach the 100s °F. In addition to the world-famous rock climbing, Smith Rock State Park is host to many miles of hiking trails, the meandering Crooked River and views of the volcanic peaks of Oregon's Cascade Range.
    SmithRockBend2.jpg
  • Mount Shuksan in Washington state's North Cascades National Park reflecting in Picture Lake. Mount Shuksan is a glaciated massif in the North Cascades National Park. Shuksan rises in Whatcom County, Washington immediately to the east of Mount Baker, and 11.6 miles  south of the Canadian border. The mountain's name Shuksan is derived from the Lummi word, said to mean "high peak". The highest point on the mountain is a three sided peak known as Summit Pyramid. There are two named subsidiary peaks: Nooksack Tower and The Hourglass. The mountain is composed of Shuksan greenschist, oceanic basalt that was metamorphosed when the Easton terrane collided with the west coast of North America, approximately 120 million years ago. The mountain is an eroded remnant of a thrust plate formed by the Easton collision.
    MtShuksanPictureLake3.jpg
  • The Oneonta Gorge is in the Columbia River Gorge in the American state of Oregon. The U.S. Forest Service has designated it as a botanical area because of the unique aquatic and woodland plants that grow there. The basalt walls are home to a wide variety of ferns, mosses, hepatics and lichens, many of which grow only in the Columbia River Gorge.
    OneontaGorge4.jpg
  • The Oneonta Gorge is in the Columbia River Gorge in the American state of Oregon. The U.S. Forest Service has designated it as a botanical area because of the unique aquatic and woodland plants that grow there. The basalt walls are home to a wide variety of ferns, mosses, hepatics and lichens, many of which grow only in the Columbia River Gorge.
    OneontaFalls1.jpg
  • The Oneonta Gorge is in the Columbia River Gorge in the American state of Oregon. The U.S. Forest Service has designated it as a botanical area because of the unique aquatic and woodland plants that grow there. The basalt walls are home to a wide variety of ferns, mosses, hepatics and lichens, many of which grow only in the Columbia River Gorge.
    OneontaFalls4.jpg
  • The Oneonta Gorge is in the Columbia River Gorge in the American state of Oregon. The U.S. Forest Service has designated it as a botanical area because of the unique aquatic and woodland plants that grow there. The basalt walls are home to a wide variety of ferns, mosses, hepatics and lichens, many of which grow only in the Columbia River Gorge.
    OneontaFalls4.jpg
  • The Oneonta Gorge is in the Columbia River Gorge in the American state of Oregon. The U.S. Forest Service has designated it as a botanical area because of the unique aquatic and woodland plants that grow there. The basalt walls are home to a wide variety of ferns, mosses, hepatics and lichens, many of which grow only in the Columbia River Gorge.
    OneontaGorge1.jpg
  • Mount Shuksan in Washington state's North Cascades National Park reflecting in Picture Lake. Mount Shuksan is a glaciated massif in the North Cascades National Park. Shuksan rises in Whatcom County, Washington immediately to the east of Mount Baker, and 11.6 miles  south of the Canadian border. The mountain's name Shuksan is derived from the Lummi word, said to mean "high peak". The highest point on the mountain is a three sided peak known as Summit Pyramid. There are two named subsidiary peaks: Nooksack Tower and The Hourglass. The mountain is composed of Shuksan greenschist, oceanic basalt that was metamorphosed when the Easton terrane collided with the west coast of North America, approximately 120 million years ago. The mountain is an eroded remnant of a thrust plate formed by the Easton collision.
    MtShuksanPictureLake7.jpg
  • Crooked River and Smith Rock<br />
.....<br />
Smith Rock State Park is an American state park located in central Oregon's high desert near the communities of Redmond and Terrebonne. Its sheer cliffs of tuff and basalt are ideal for rock climbing of all difficulty levels. Smith Rock is generally considered the birthplace of modern American sport climbing, and is host to cutting-edge climbing routes. There is sport climbing, traditional climbing, multi-pitch climbing, and bouldering.<br />
<br />
The park contains the first U.S. climb rated 5.14. The area is well known for its challenging climbing routes so eventually all top climbers visit. In 1983, Allan Watts began to use sport climbing ethics which pushed American climbing to new levels. Shortly after, between 1992 and 2009, about 500 new climbing routes were added. This brought climbers from all over the world as Smith Rock became the world capital for sport climbing. To this day the park still attracts climbers from all over the world. The winter tends to be too cold (below freezing) for climbing and the summer months regularly reach the 100s °F. In addition to the world-famous rock climbing, Smith Rock State Park is host to many miles of hiking trails, the meandering Crooked River and views of the volcanic peaks of Oregon's Cascade Range.
    SmithRockBend1-LAB.jpg
  • The Oneonta Gorge is in the Columbia River Gorge in the American state of Oregon. The U.S. Forest Service has designated it as a botanical area because of the unique aquatic and woodland plants that grow there. The basalt walls are home to a wide variety of ferns, mosses, hepatics and lichens, many of which grow only in the Columbia River Gorge.
    OneontaFalls3.jpg
  • Steptoe Butte is a quartzite island jutting out of the silty loess of the Palouse hills in Whitman County, Washington. It is contained by Steptoe Butte State Park. The rock that forms the butte is over 400 million years old, in contrast with the 15–7 million year old Columbia River basalts that underlie the rest of the Palouse. Steptoe Butte has become an archetype, as isolated protrusions of bedrock, such as summits of hills or mountains, in lava flows have come to be called steptoes.
    PalouseDawn.jpg
  • Steptoe Butte is a quartzite island jutting out of the silty loess of the Palouse hills in Whitman County, Washington. It is contained by Steptoe Butte State Park. The rock that forms the butte is over 400 million years old, in contrast with the 15–7 million year old Columbia River basalts that underlie the rest of the Palouse. Steptoe Butte has become an archetype, as isolated protrusions of bedrock, such as summits of hills or mountains, in lava flows have come to be called steptoes.
    PalouseDawn.jpg
  • Steptoe Butte is a quartzite island jutting out of the silty loess of the Palouse hills in Whitman County, Washington. It is contained by Steptoe Butte State Park. The rock that forms the butte is over 400 million years old, in contrast with the 15–7 million year old Columbia River basalts that underlie the rest of the Palouse. Steptoe Butte has become an archetype, as isolated protrusions of bedrock, such as summits of hills or mountains, in lava flows have come to be called steptoes.
    PalouseDawn.jpg
  • Steptoe Butte is a quartzite island jutting out of the silty loess of the Palouse hills in Whitman County, Washington. It is contained by Steptoe Butte State Park. The rock that forms the butte is over 400 million years old, in contrast with the 15–7 million year old Columbia River basalts that underlie the rest of the Palouse. Steptoe Butte has become an archetype, as isolated protrusions of bedrock, such as summits of hills or mountains, in lava flows have come to be called steptoes.
    PalouseDawn.jpg
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