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  • Moss and scenery in the Southern Region of Iceland
    IcelandMoss2.jpg
  • Moss and scenery in the Southern Region of Iceland
    IcelandMoss1.jpg
  • Moss and scenery in the Southern Region of Iceland
    IcelandMoss1.jpg
  • Moss, rocks, and cascading water at Thakgil Canyon
    Thakgil3.jpg
  • Moss, rocks, and cascading water at Thakgil Canyon
    Thakgil2.jpg
  • Moss, rocks, and cascading water at Thakgil Canyon
    Thakgil1.jpg
  • The Hoh Rainforest is located on the Olympic Peninsula in western Washington state, USA. It is one of the few temperate rainforests in the U.S., and also one of the largest.  It was formed thousands of years ago by glaciers.
    HohHallMossesTrail1.jpg
  • The Hoh Rainforest is located on the Olympic Peninsula in western Washington state, USA. It is one of the few temperate rainforests in the U.S., and also one of the largest.  It was formed thousands of years ago by glaciers.
    HohHallMossesTrail2.jpg
  • The Hoh Rainforest is located on the Olympic Peninsula in western Washington state, USA. It is one of the few temperate rainforests in the U.S., and also one of the largest.  It was formed thousands of years ago by glaciers.
    HohHallMossesTrail2.jpg
  • The Hoh Rainforest is located on the Olympic Peninsula in western Washington state, USA. It is one of the few temperate rainforests in the U.S., and also one of the largest.  It was formed thousands of years ago by glaciers.
    HohHallMossesTrail1.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.
    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.
    OneontaGorge2.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.
    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.
    OneontaFalls7.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
  • 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.
    OneontaGorge1.jpg
  • Hoh Rainforest in Olympic National Park, in autumn
    HohMossyTrunk1.jpg
  • Hoh Rainforest in Olympic National Park, in autumn
    HohMapleTrunks-LAB.jpg
  • Caddo Lake (French: Lac Caddo) is a 25,400 acres (10,300 ha) lake and wetland located on the border between Texas and Louisiana, in northern Harrison County and southern Marion County in Texas and western Caddo Parish in Louisiana. The lake is named after the Southeastern culture of Native Americans called Caddoans or Caddo, who lived in the area until their expulsion in the 19th century. It is an internationally protected wetland under the RAMSAR treaty and features the largest Cypress forest in the world. Caddo is one of Texas' few non-oxbow natural lakes and is the 2nd largest in the South; however, it was artificially altered by the addition of a dam in the 1900s.
    CaddoDawnTrunks1.jpg
  • Glacier National Park is a national park located in the U.S. state of Montana, on the Canada–United States border with the Canadian provinces of Alberta and British Columbia. The park encompasses over 1 million acres and includes parts of two mountain ranges (sub-ranges of the Rocky Mountains), over 130 named lakes, more than 1,000 different species of plants, and hundreds of species of animals. This vast pristine ecosystem is the centerpiece of what has been referred to as the "Crown of the Continent Ecosystem", a region of protected land encompassing 16,000 square miles.<br />
<br />
The region that became Glacier National Park was first inhabited by Native Americans. Upon the arrival of European explorers, it was dominated by the Blackfeet in the east and the Flathead in the western regions. Soon after the establishment of the park on May 11, 1910, a number of hotels and chalets were constructed by the Great Northern Railway. These historic hotels and chalets are listed as National Historic Landmarks and a total of 350 locations are on the National Register of Historic Places. By 1932 work was completed on the Going-to-the-Sun Road, later designated a National Historic Civil Engineering Landmark, which provided greater accessibility for automobiles into the heart of the park.<br />
<br />
The mountains of Glacier National Park began forming 170 million years ago when ancient rocks were forced eastward up and over much younger rock strata. Known as the Lewis Overthrust, these sedimentary rocks are considered to have some of the finest fossilized examples of extremely early life found anywhere on Earth. The current shapes of the Lewis and Livingston mountain ranges and positioning and size of the lakes show the telltale evidence of massive glacial action, which carved U-shaped valleys and left behind moraines which impounded water, creating lakes. Of the estimated 150 glaciers which existed in the park in the mid-19th century, only 25 active glaciers remained by 2010. Scientists studyin
    GlacierLoganPassPanorama1.jpg
  • The waterfall Háifoss is situated near the volcano Hekla in the south of Iceland. The river Fossá, a tributary of Þjórsá, drops here from a height of 122 m. This is the third highest waterfall of the island.<br />
<br />
From the historical farm Þjóðveldisbærinn Stöng, which was destroyed by a volcanic eruption of Hekla in the Middle Ages and reconstructed, it is possible to hike to the waterfall along the Fossá (5 to 6 hours both directions). Above the waterfall, there is also a parking lot, so the hiking can also be made in the other direction.
    Haifoss3.jpg
  • Fjaðrárgljúfur is a canyon in south east Iceland which is up to 100 m deep and about 2 kilometers long, with the Fjaðrá river flowing through it .The canyon has steep walls and winding water.
    Fjadrargljufur8.jpg
  • Fjaðrárgljúfur is a canyon in south east Iceland which is up to 100 m deep and about 2 kilometers long, with the Fjaðrá river flowing through it .The canyon has steep walls and winding water.
    Fjadrargljufur2.jpg
  • Landmannalaugar is a place in the Fjallabak Nature Reserve in the Highlands of Iceland. It is at the edge of Laugahraun lava field, which was formed in an eruption around the year 1477. It is known for its natural geothermal hot springs and surrounding landscape.
    Landmannalaugar6.jpg
  • Hof, in Öræfi, is a cluster of farms in the municipality of Sveitarfélagið Hornafjörður in southeast Iceland, close to Vatnajökull glacier, and twenty two kilometres south of Skaftafell in Vatnajökull National Park. It is located on the Route 1 southwest of Höfn, in the narrow strip between the sea coast and the glacier.<br />
<br />
A notаble building in Hof is a turf church, which was built in 1883 and is the youngest turf church in Iceland. Since 1951, it belongs to the National Museum of Iceland.
    Hofskirkja4.jpg
  • Glacier National Park is a national park located in the U.S. state of Montana, on the Canada–United States border with the Canadian provinces of Alberta and British Columbia. The park encompasses over 1 million acres and includes parts of two mountain ranges (sub-ranges of the Rocky Mountains), over 130 named lakes, more than 1,000 different species of plants, and hundreds of species of animals. This vast pristine ecosystem is the centerpiece of what has been referred to as the "Crown of the Continent Ecosystem", a region of protected land encompassing 16,000 square miles.<br />
<br />
The region that became Glacier National Park was first inhabited by Native Americans. Upon the arrival of European explorers, it was dominated by the Blackfeet in the east and the Flathead in the western regions. Soon after the establishment of the park on May 11, 1910, a number of hotels and chalets were constructed by the Great Northern Railway. These historic hotels and chalets are listed as National Historic Landmarks and a total of 350 locations are on the National Register of Historic Places. By 1932 work was completed on the Going-to-the-Sun Road, later designated a National Historic Civil Engineering Landmark, which provided greater accessibility for automobiles into the heart of the park.<br />
<br />
The mountains of Glacier National Park began forming 170 million years ago when ancient rocks were forced eastward up and over much younger rock strata. Known as the Lewis Overthrust, these sedimentary rocks are considered to have some of the finest fossilized examples of extremely early life found anywhere on Earth. The current shapes of the Lewis and Livingston mountain ranges and positioning and size of the lakes show the telltale evidence of massive glacial action, which carved U-shaped valleys and left behind moraines which impounded water, creating lakes. Of the estimated 150 glaciers which existed in the park in the mid-19th century, only 25 active glaciers remained by 2010. Scientists studyin
    GlacierAvalancheCreek4.jpg
  • Glacier National Park is a national park located in the U.S. state of Montana, on the Canada–United States border with the Canadian provinces of Alberta and British Columbia. The park encompasses over 1 million acres and includes parts of two mountain ranges (sub-ranges of the Rocky Mountains), over 130 named lakes, more than 1,000 different species of plants, and hundreds of species of animals. This vast pristine ecosystem is the centerpiece of what has been referred to as the "Crown of the Continent Ecosystem", a region of protected land encompassing 16,000 square miles.<br />
<br />
The region that became Glacier National Park was first inhabited by Native Americans. Upon the arrival of European explorers, it was dominated by the Blackfeet in the east and the Flathead in the western regions. Soon after the establishment of the park on May 11, 1910, a number of hotels and chalets were constructed by the Great Northern Railway. These historic hotels and chalets are listed as National Historic Landmarks and a total of 350 locations are on the National Register of Historic Places. By 1932 work was completed on the Going-to-the-Sun Road, later designated a National Historic Civil Engineering Landmark, which provided greater accessibility for automobiles into the heart of the park.<br />
<br />
The mountains of Glacier National Park began forming 170 million years ago when ancient rocks were forced eastward up and over much younger rock strata. Known as the Lewis Overthrust, these sedimentary rocks are considered to have some of the finest fossilized examples of extremely early life found anywhere on Earth. The current shapes of the Lewis and Livingston mountain ranges and positioning and size of the lakes show the telltale evidence of massive glacial action, which carved U-shaped valleys and left behind moraines which impounded water, creating lakes. Of the estimated 150 glaciers which existed in the park in the mid-19th century, only 25 active glaciers remained by 2010. Scientists studyin
    GlacierAvalancheCreek3.jpg
  • Sol Duc Falls.  The name Sol Duc means "magic waters". The Sol Duc River is divided into 3 or 4 separate streams (depending on flow) by an irregular rocky ledge. The water drops about 25 feet over the ledge into a tight cleft, making a 90 degree angle turn. The river passes beneath a footbridge, then drops about 10 feet into a deep teal pool.
    SolDucTripleFalls.jpg
  • Hoh Rainforest in Olympic National Park, in autumn
    HohGrove1.jpg
  • Rocks along the Skagit River in Washington state
    CascadesRiverRocks1.jpg
  • Glacier National Park is a national park located in the U.S. state of Montana, on the Canada–United States border with the Canadian provinces of Alberta and British Columbia. The park encompasses over 1 million acres and includes parts of two mountain ranges (sub-ranges of the Rocky Mountains), over 130 named lakes, more than 1,000 different species of plants, and hundreds of species of animals. This vast pristine ecosystem is the centerpiece of what has been referred to as the "Crown of the Continent Ecosystem", a region of protected land encompassing 16,000 square miles.<br />
<br />
The region that became Glacier National Park was first inhabited by Native Americans. Upon the arrival of European explorers, it was dominated by the Blackfeet in the east and the Flathead in the western regions. Soon after the establishment of the park on May 11, 1910, a number of hotels and chalets were constructed by the Great Northern Railway. These historic hotels and chalets are listed as National Historic Landmarks and a total of 350 locations are on the National Register of Historic Places. By 1932 work was completed on the Going-to-the-Sun Road, later designated a National Historic Civil Engineering Landmark, which provided greater accessibility for automobiles into the heart of the park.<br />
<br />
The mountains of Glacier National Park began forming 170 million years ago when ancient rocks were forced eastward up and over much younger rock strata. Known as the Lewis Overthrust, these sedimentary rocks are considered to have some of the finest fossilized examples of extremely early life found anywhere on Earth. The current shapes of the Lewis and Livingston mountain ranges and positioning and size of the lakes show the telltale evidence of massive glacial action, which carved U-shaped valleys and left behind moraines which impounded water, creating lakes. Of the estimated 150 glaciers which existed in the park in the mid-19th century, only 25 active glaciers remained by 2010. Scientists studyin
    GlacierAvalancheCreek3.jpg
  • Glacier National Park is a national park located in the U.S. state of Montana, on the Canada–United States border with the Canadian provinces of Alberta and British Columbia. The park encompasses over 1 million acres and includes parts of two mountain ranges (sub-ranges of the Rocky Mountains), over 130 named lakes, more than 1,000 different species of plants, and hundreds of species of animals. This vast pristine ecosystem is the centerpiece of what has been referred to as the "Crown of the Continent Ecosystem", a region of protected land encompassing 16,000 square miles.<br />
<br />
The region that became Glacier National Park was first inhabited by Native Americans. Upon the arrival of European explorers, it was dominated by the Blackfeet in the east and the Flathead in the western regions. Soon after the establishment of the park on May 11, 1910, a number of hotels and chalets were constructed by the Great Northern Railway. These historic hotels and chalets are listed as National Historic Landmarks and a total of 350 locations are on the National Register of Historic Places. By 1932 work was completed on the Going-to-the-Sun Road, later designated a National Historic Civil Engineering Landmark, which provided greater accessibility for automobiles into the heart of the park.<br />
<br />
The mountains of Glacier National Park began forming 170 million years ago when ancient rocks were forced eastward up and over much younger rock strata. Known as the Lewis Overthrust, these sedimentary rocks are considered to have some of the finest fossilized examples of extremely early life found anywhere on Earth. The current shapes of the Lewis and Livingston mountain ranges and positioning and size of the lakes show the telltale evidence of massive glacial action, which carved U-shaped valleys and left behind moraines which impounded water, creating lakes. Of the estimated 150 glaciers which existed in the park in the mid-19th century, only 25 active glaciers remained by 2010. Scientists studyin
    GlacierAvalancheCreek5.jpg
  • Small creek near Sol Duc Falls.  The name Sol Duc means "magic waters". The Sol Duc River is divided into 3 or 4 separate streams (depending on flow) by an irregular rocky ledge. The water drops about 25 feet over the ledge into a tight cleft, making a 90 degree angle turn. The river passes beneath a footbridge, then drops about 10 feet into a deep teal pool.
    SolDucStream.jpg
  • Latourell Falls is a waterfall along the Columbia River Gorge in Oregon, within Guy W. Talbot State Park.<br />
<br />
The Historic Columbia River Highway passes nearby, and at certain locations the Lower falls are visible from the road. Near the base of the falls, a parking lot and path were erected to assist visitors to the site. Visitors must hike along the 2.1 mile loop trail to see the upper falls.
    LatourellFalls1.jpg
  • Lower Proxy Falls in Proxy Falls state park in the Three Sisters Wilderness
    ProxyFallsWall6.jpg
  • Caddo Lake (French: Lac Caddo) is a 25,400 acres (10,300 ha) lake and wetland located on the border between Texas and Louisiana, in northern Harrison County and southern Marion County in Texas and western Caddo Parish in Louisiana. The lake is named after the Southeastern culture of Native Americans called Caddoans or Caddo, who lived in the area until their expulsion in the 19th century. It is an internationally protected wetland under the RAMSAR treaty and features the largest Cypress forest in the world. Caddo is one of Texas' few non-oxbow natural lakes and is the 2nd largest in the South; however, it was artificially altered by the addition of a dam in the 1900s.
    CaddoLakeTree2.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
    ProxyFallsWall1-LAB.jpg
  • Lower Proxy Falls in Proxy Falls state park in the Three Sisters Wilderness
    ProxyFalls1.jpg
  • Horsetail Falls on the Columbia River Gorge, Oregon
    WahkeenaFalls1.jpg
  • Sol Duc Falls.  The name Sol Duc means "magic waters". The Sol Duc River is divided into 3 or 4 separate streams (depending on flow) by an irregular rocky ledge. The water drops about 25 feet over the ledge into a tight cleft, making a 90 degree angle turn. The river passes beneath a footbridge, then drops about 10 feet into a deep teal pool.
    SolDucTripleFalls.jpg
  • Small creek near Sol Duc Falls.  The name Sol Duc means "magic waters". The Sol Duc River is divided into 3 or 4 separate streams (depending on flow) by an irregular rocky ledge. The water drops about 25 feet over the ledge into a tight cleft, making a 90 degree angle turn. The river passes beneath a footbridge, then drops about 10 feet into a deep teal pool.
    SolDucCascades2.jpg
  • The Hoh Rainforest is located on the Olympic Peninsula in western Washington state, USA. It is one of the few temperate rainforests in the U.S., and also one of the largest.  It was formed thousands of years ago by glaciers.
    HohMapleGrove5.jpg
  • The Hoh Rainforest is located on the Olympic Peninsula in western Washington state, USA. It is one of the few temperate rainforests in the U.S., and also one of the largest.  It was formed thousands of years ago by glaciers.
    OlympicHohStump2.jpg
  • Caddo Lake (French: Lac Caddo) is a 25,400 acres (10,300 ha) lake and wetland located on the border between Texas and Louisiana, in northern Harrison County and southern Marion County in Texas and western Caddo Parish in Louisiana. The lake is named after the Southeastern culture of Native Americans called Caddoans or Caddo, who lived in the area until their expulsion in the 19th century. It is an internationally protected wetland under the RAMSAR treaty and features the largest Cypress forest in the world. Caddo is one of Texas' few non-oxbow natural lakes and is the 2nd largest in the South; however, it was artificially altered by the addition of a dam in the 1900s.
    CaddoDawnFog1.jpg
  • Caddo Lake (French: Lac Caddo) is a 25,400 acres (10,300 ha) lake and wetland located on the border between Texas and Louisiana, in northern Harrison County and southern Marion County in Texas and western Caddo Parish in Louisiana. The lake is named after the Southeastern culture of Native Americans called Caddoans or Caddo, who lived in the area until their expulsion in the 19th century. It is an internationally protected wetland under the RAMSAR treaty and features the largest Cypress forest in the world. Caddo is one of Texas' few non-oxbow natural lakes and is the 2nd largest in the South; however, it was artificially altered by the addition of a dam in the 1900s.
    CaddoSunstar4.jpg
  • The waterfall Háifoss is situated near the volcano Hekla in the south of Iceland. The river Fossá, a tributary of Þjórsá, drops here from a height of 122 m. This is the third highest waterfall of the island.<br />
<br />
From the historical farm Þjóðveldisbærinn Stöng, which was destroyed by a volcanic eruption of Hekla in the Middle Ages and reconstructed, it is possible to hike to the waterfall along the Fossá (5 to 6 hours both directions). Above the waterfall, there is also a parking lot, so the hiking can also be made in the other direction.
    Haifoss2.jpg
  • Hof, in Öræfi, is a cluster of farms in the municipality of Sveitarfélagið Hornafjörður in southeast Iceland, close to Vatnajökull glacier, and twenty two kilometres south of Skaftafell in Vatnajökull National Park. It is located on the Route 1 southwest of Höfn, in the narrow strip between the sea coast and the glacier.<br />
<br />
A notаble building in Hof is a turf church, which was built in 1883 and is the youngest turf church in Iceland. Since 1951, it belongs to the National Museum of Iceland.
    Hofskirkja1.jpg
  • Glacier National Park is a national park located in the U.S. state of Montana, on the Canada–United States border with the Canadian provinces of Alberta and British Columbia. The park encompasses over 1 million acres and includes parts of two mountain ranges (sub-ranges of the Rocky Mountains), over 130 named lakes, more than 1,000 different species of plants, and hundreds of species of animals. This vast pristine ecosystem is the centerpiece of what has been referred to as the "Crown of the Continent Ecosystem", a region of protected land encompassing 16,000 square miles.<br />
<br />
The region that became Glacier National Park was first inhabited by Native Americans. Upon the arrival of European explorers, it was dominated by the Blackfeet in the east and the Flathead in the western regions. Soon after the establishment of the park on May 11, 1910, a number of hotels and chalets were constructed by the Great Northern Railway. These historic hotels and chalets are listed as National Historic Landmarks and a total of 350 locations are on the National Register of Historic Places. By 1932 work was completed on the Going-to-the-Sun Road, later designated a National Historic Civil Engineering Landmark, which provided greater accessibility for automobiles into the heart of the park.<br />
<br />
The mountains of Glacier National Park began forming 170 million years ago when ancient rocks were forced eastward up and over much younger rock strata. Known as the Lewis Overthrust, these sedimentary rocks are considered to have some of the finest fossilized examples of extremely early life found anywhere on Earth. The current shapes of the Lewis and Livingston mountain ranges and positioning and size of the lakes show the telltale evidence of massive glacial action, which carved U-shaped valleys and left behind moraines which impounded water, creating lakes. Of the estimated 150 glaciers which existed in the park in the mid-19th century, only 25 active glaciers remained by 2010. Scientists studyin
    GlacierAvalancheCreek3.jpg
  • Johnston Creek is a tributary of the Bow River in Canada's Rocky Mountains. The creek is located in Banff National Park. As Johnston Creek approaches the Bow River, it flows through a large canyon formed by erosion over thousands of years. The creek has cut through the limestone rock to form sheer canyon walls, as well as waterfalls, tunnels, and pools.
    JohnstonCanyon1.jpg
  • Johnston Creek is a tributary of the Bow River in Canada's Rocky Mountains. The creek is located in Banff National Park. As Johnston Creek approaches the Bow River, it flows through a large canyon formed by erosion over thousands of years. The creek has cut through the limestone rock to form sheer canyon walls, as well as waterfalls, tunnels, and pools.
    JohnstonCanyon2.jpg
  • Punchbowl Falls on Eagle Creek, Oregon
    PunchbowlFalls1.jpg
  • Fjaðrárgljúfur is a canyon in south east Iceland which is up to 100 m deep and about 2 kilometers long, with the Fjaðrá river flowing through it .The canyon has steep walls and winding water.
    Fjadrargljufur9.jpg
  • Fjaðrárgljúfur is a canyon in south east Iceland which is up to 100 m deep and about 2 kilometers long, with the Fjaðrá river flowing through it .The canyon has steep walls and winding water.
    Fjadrargljufur5.jpg
  • Frostastaðavatn (Icelandic for lake of the frosty place) is a lake in Iceland. It is situated in the Highlands of Iceland, not far from the famous mountains of Landmannalaugar and the volcano Hekla. <br />
Evidence of volcanism shows around this lake; for example, green and blue water is often found around volcanoes. Two highland roads run along its shore, Fjallabaksleið nyrðri (F 208) and Landmannaleið.
    Frostastadavatn1.jpg
  • The waterfall Háifoss is situated near the volcano Hekla in the south of Iceland. The river Fossá, a tributary of Þjórsá, drops here from a height of 122 m. This is the third highest waterfall of the island.<br />
<br />
From the historical farm Þjóðveldisbærinn Stöng, which was destroyed by a volcanic eruption of Hekla in the Middle Ages and reconstructed, it is possible to hike to the waterfall along the Fossá (5 to 6 hours both directions). Above the waterfall, there is also a parking lot, so the hiking can also be made in the other direction.
    Haifoss2.jpg
  • The waterfall Háifoss is situated near the volcano Hekla in the south of Iceland. The river Fossá, a tributary of Þjórsá, drops here from a height of 122 m. This is the third highest waterfall of the island.<br />
<br />
From the historical farm Þjóðveldisbærinn Stöng, which was destroyed by a volcanic eruption of Hekla in the Middle Ages and reconstructed, it is possible to hike to the waterfall along the Fossá (5 to 6 hours both directions). Above the waterfall, there is also a parking lot, so the hiking can also be made in the other direction.
    Haifoss1.jpg
  • Ófærufoss is a waterfall situated in the Eldgjá chasm in central Iceland. Until the early 1990s a natural bridge spanned the falls, but it collapsed from natural causes.
    Ofaerufoss1.jpg
  • Ófærufoss is a waterfall situated in the Eldgjá chasm in central Iceland. Until the early 1990s a natural bridge spanned the falls, but it collapsed from natural causes.
    Ofaerufoss4.jpg
  • Fjaðrárgljúfur is a canyon in south east Iceland which is up to 100 m deep and about 2 kilometers long, with the Fjaðrá river flowing through it .The canyon has steep walls and winding water.
    _A1A6441-HDR.jpg
  • Hof, in Öræfi, is a cluster of farms in the municipality of Sveitarfélagið Hornafjörður in southeast Iceland, close to Vatnajökull glacier, and twenty two kilometres south of Skaftafell in Vatnajökull National Park. It is located on the Route 1 southwest of Höfn, in the narrow strip between the sea coast and the glacier.<br />
<br />
A notаble building in Hof is a turf church, which was built in 1883 and is the youngest turf church in Iceland. Since 1951, it belongs to the National Museum of Iceland.
    Hofskirkja3.jpg
  • Hof, in Öræfi, is a cluster of farms in the municipality of Sveitarfélagið Hornafjörður in southeast Iceland, close to Vatnajökull glacier, and twenty two kilometres south of Skaftafell in Vatnajökull National Park. It is located on the Route 1 southwest of Höfn, in the narrow strip between the sea coast and the glacier.<br />
<br />
A notаble building in Hof is a turf church, which was built in 1883 and is the youngest turf church in Iceland. Since 1951, it belongs to the National Museum of Iceland.
    Hofskirkja1.jpg
  • Rocks along the Skagit River in Washington state
    CascadesRiverRocks1.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
    ProxyFalls6.jpg
  • Hoh Rainforest in Olympic National Park, in autumn
    HohGrove2.jpg
  • Glacier National Park is a national park located in the U.S. state of Montana, on the Canada–United States border with the Canadian provinces of Alberta and British Columbia. The park encompasses over 1 million acres and includes parts of two mountain ranges (sub-ranges of the Rocky Mountains), over 130 named lakes, more than 1,000 different species of plants, and hundreds of species of animals. This vast pristine ecosystem is the centerpiece of what has been referred to as the "Crown of the Continent Ecosystem", a region of protected land encompassing 16,000 square miles.<br />
<br />
The region that became Glacier National Park was first inhabited by Native Americans. Upon the arrival of European explorers, it was dominated by the Blackfeet in the east and the Flathead in the western regions. Soon after the establishment of the park on May 11, 1910, a number of hotels and chalets were constructed by the Great Northern Railway. These historic hotels and chalets are listed as National Historic Landmarks and a total of 350 locations are on the National Register of Historic Places. By 1932 work was completed on the Going-to-the-Sun Road, later designated a National Historic Civil Engineering Landmark, which provided greater accessibility for automobiles into the heart of the park.<br />
<br />
The mountains of Glacier National Park began forming 170 million years ago when ancient rocks were forced eastward up and over much younger rock strata. Known as the Lewis Overthrust, these sedimentary rocks are considered to have some of the finest fossilized examples of extremely early life found anywhere on Earth. The current shapes of the Lewis and Livingston mountain ranges and positioning and size of the lakes show the telltale evidence of massive glacial action, which carved U-shaped valleys and left behind moraines which impounded water, creating lakes. Of the estimated 150 glaciers which existed in the park in the mid-19th century, only 25 active glaciers remained by 2010. Scientists studyin
    GlacierAvalancheCreek2.jpg
  • Glacier National Park is a national park located in the U.S. state of Montana, on the Canada–United States border with the Canadian provinces of Alberta and British Columbia. The park encompasses over 1 million acres and includes parts of two mountain ranges (sub-ranges of the Rocky Mountains), over 130 named lakes, more than 1,000 different species of plants, and hundreds of species of animals. This vast pristine ecosystem is the centerpiece of what has been referred to as the "Crown of the Continent Ecosystem", a region of protected land encompassing 16,000 square miles.<br />
<br />
The region that became Glacier National Park was first inhabited by Native Americans. Upon the arrival of European explorers, it was dominated by the Blackfeet in the east and the Flathead in the western regions. Soon after the establishment of the park on May 11, 1910, a number of hotels and chalets were constructed by the Great Northern Railway. These historic hotels and chalets are listed as National Historic Landmarks and a total of 350 locations are on the National Register of Historic Places. By 1932 work was completed on the Going-to-the-Sun Road, later designated a National Historic Civil Engineering Landmark, which provided greater accessibility for automobiles into the heart of the park.<br />
<br />
The mountains of Glacier National Park began forming 170 million years ago when ancient rocks were forced eastward up and over much younger rock strata. Known as the Lewis Overthrust, these sedimentary rocks are considered to have some of the finest fossilized examples of extremely early life found anywhere on Earth. The current shapes of the Lewis and Livingston mountain ranges and positioning and size of the lakes show the telltale evidence of massive glacial action, which carved U-shaped valleys and left behind moraines which impounded water, creating lakes. Of the estimated 150 glaciers which existed in the park in the mid-19th century, only 25 active glaciers remained by 2010. Scientists studyin
    GlacierAvalancheCreek4.jpg
  • Glacier National Park is a national park located in the U.S. state of Montana, on the Canada–United States border with the Canadian provinces of Alberta and British Columbia. The park encompasses over 1 million acres and includes parts of two mountain ranges (sub-ranges of the Rocky Mountains), over 130 named lakes, more than 1,000 different species of plants, and hundreds of species of animals. This vast pristine ecosystem is the centerpiece of what has been referred to as the "Crown of the Continent Ecosystem", a region of protected land encompassing 16,000 square miles.<br />
<br />
The region that became Glacier National Park was first inhabited by Native Americans. Upon the arrival of European explorers, it was dominated by the Blackfeet in the east and the Flathead in the western regions. Soon after the establishment of the park on May 11, 1910, a number of hotels and chalets were constructed by the Great Northern Railway. These historic hotels and chalets are listed as National Historic Landmarks and a total of 350 locations are on the National Register of Historic Places. By 1932 work was completed on the Going-to-the-Sun Road, later designated a National Historic Civil Engineering Landmark, which provided greater accessibility for automobiles into the heart of the park.<br />
<br />
The mountains of Glacier National Park began forming 170 million years ago when ancient rocks were forced eastward up and over much younger rock strata. Known as the Lewis Overthrust, these sedimentary rocks are considered to have some of the finest fossilized examples of extremely early life found anywhere on Earth. The current shapes of the Lewis and Livingston mountain ranges and positioning and size of the lakes show the telltale evidence of massive glacial action, which carved U-shaped valleys and left behind moraines which impounded water, creating lakes. Of the estimated 150 glaciers which existed in the park in the mid-19th century, only 25 active glaciers remained by 2010. Scientists studyin
    GlacierLoganPass3.jpg
  • Glacier National Park is a national park located in the U.S. state of Montana, on the Canada–United States border with the Canadian provinces of Alberta and British Columbia. The park encompasses over 1 million acres and includes parts of two mountain ranges (sub-ranges of the Rocky Mountains), over 130 named lakes, more than 1,000 different species of plants, and hundreds of species of animals. This vast pristine ecosystem is the centerpiece of what has been referred to as the "Crown of the Continent Ecosystem", a region of protected land encompassing 16,000 square miles.<br />
<br />
The region that became Glacier National Park was first inhabited by Native Americans. Upon the arrival of European explorers, it was dominated by the Blackfeet in the east and the Flathead in the western regions. Soon after the establishment of the park on May 11, 1910, a number of hotels and chalets were constructed by the Great Northern Railway. These historic hotels and chalets are listed as National Historic Landmarks and a total of 350 locations are on the National Register of Historic Places. By 1932 work was completed on the Going-to-the-Sun Road, later designated a National Historic Civil Engineering Landmark, which provided greater accessibility for automobiles into the heart of the park.<br />
<br />
The mountains of Glacier National Park began forming 170 million years ago when ancient rocks were forced eastward up and over much younger rock strata. Known as the Lewis Overthrust, these sedimentary rocks are considered to have some of the finest fossilized examples of extremely early life found anywhere on Earth. The current shapes of the Lewis and Livingston mountain ranges and positioning and size of the lakes show the telltale evidence of massive glacial action, which carved U-shaped valleys and left behind moraines which impounded water, creating lakes. Of the estimated 150 glaciers which existed in the park in the mid-19th century, only 25 active glaciers remained by 2010. Scientists studyin
    GlacierLoganPass8.jpg
  • Lower Proxy Falls in Proxy Falls state park in the Three Sisters Wilderness
    ProxyFalls2.jpg
  • Sol Duc Falls.  The name Sol Duc means "magic waters". The Sol Duc River is divided into 3 or 4 separate streams (depending on flow) by an irregular rocky ledge. The water drops about 25 feet over the ledge into a tight cleft, making a 90 degree angle turn. The river passes beneath a footbridge, then drops about 10 feet into a deep teal pool.
    SolDucTripleFalls.jpg
  • Hoh Rainforest in Olympic National Park, in autumn
    HohGrove2.jpg
  • Hoh Rainforest in Olympic National Park, in autumn
    HohGrove1.jpg
  • Rocks along the Skagit River in Washington state
    CascadesRiverRocks1.jpg
  • Multnomah Falls in Columbia River Gorge, Oregon
    MultnomahFalls1.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
    ProxyFalls3.jpg
  • Small creek near Sol Duc Falls.  The name Sol Duc means "magic waters". The Sol Duc River is divided into 3 or 4 separate streams (depending on flow) by an irregular rocky ledge. The water drops about 25 feet over the ledge into a tight cleft, making a 90 degree angle turn. The river passes beneath a footbridge, then drops about 10 feet into a deep teal pool.
    SolDucStream-Alt.jpg
  • Hoh Rainforest in Olympic National Park, in autumn
    HohGrove2.jpg
  • Hoh Rainforest in Olympic National Park, in autumn
    HohGrove1.jpg
  • Punchbowl Falls on Eagle Creek, Oregon
    PunchBowlFalls3.jpg
  • Punchbowl Falls on Eagle Creek, Oregon
    PunchbowlFalls2.jpg
  • Latourell Falls is a waterfall along the Columbia River Gorge in Oregon, within Guy W. Talbot State Park.<br />
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The Historic Columbia River Highway passes nearby, and at certain locations the Lower falls are visible from the road. Near the base of the falls, a parking lot and path were erected to assist visitors to the site. Visitors must hike along the 2.1 mile loop trail to see the upper falls.
    LatourellFalls1.jpg
  • Rocks in creek on the the north side of Mount Rainier, near Carbon Glacier
    MtRainierGreenRocks.jpg
  • Caddo Lake (French: Lac Caddo) is a 25,400 acres (10,300 ha) lake and wetland located on the border between Texas and Louisiana, in northern Harrison County and southern Marion County in Texas and western Caddo Parish in Louisiana. The lake is named after the Southeastern culture of Native Americans called Caddoans or Caddo, who lived in the area until their expulsion in the 19th century. It is an internationally protected wetland under the RAMSAR treaty and features the largest Cypress forest in the world. Caddo is one of Texas' few non-oxbow natural lakes and is the 2nd largest in the South; however, it was artificially altered by the addition of a dam in the 1900s.
    CaddoSawmillPond2.jpg
  • Caddo Lake (French: Lac Caddo) is a 25,400 acres (10,300 ha) lake and wetland located on the border between Texas and Louisiana, in northern Harrison County and southern Marion County in Texas and western Caddo Parish in Louisiana. The lake is named after the Southeastern culture of Native Americans called Caddoans or Caddo, who lived in the area until their expulsion in the 19th century. It is an internationally protected wetland under the RAMSAR treaty and features the largest Cypress forest in the world. Caddo is one of Texas' few non-oxbow natural lakes and is the 2nd largest in the South; however, it was artificially altered by the addition of a dam in the 1900s.
    CaddoSawmillPond4.jpg
  • Caddo Lake (French: Lac Caddo) is a 25,400 acres (10,300 ha) lake and wetland located on the border between Texas and Louisiana, in northern Harrison County and southern Marion County in Texas and western Caddo Parish in Louisiana. The lake is named after the Southeastern culture of Native Americans called Caddoans or Caddo, who lived in the area until their expulsion in the 19th century. It is an internationally protected wetland under the RAMSAR treaty and features the largest Cypress forest in the world. Caddo is one of Texas' few non-oxbow natural lakes and is the 2nd largest in the South; however, it was artificially altered by the addition of a dam in the 1900s.
    CaddoSawmillPond1.jpg
  • Caddo Lake (French: Lac Caddo) is a 25,400 acres (10,300 ha) lake and wetland located on the border between Texas and Louisiana, in northern Harrison County and southern Marion County in Texas and western Caddo Parish in Louisiana. The lake is named after the Southeastern culture of Native Americans called Caddoans or Caddo, who lived in the area until their expulsion in the 19th century. It is an internationally protected wetland under the RAMSAR treaty and features the largest Cypress forest in the world. Caddo is one of Texas' few non-oxbow natural lakes and is the 2nd largest in the South; however, it was artificially altered by the addition of a dam in the 1900s.
    CaddoSawmillPond3.jpg
  • Caddo Lake (French: Lac Caddo) is a 25,400 acres (10,300 ha) lake and wetland located on the border between Texas and Louisiana, in northern Harrison County and southern Marion County in Texas and western Caddo Parish in Louisiana. The lake is named after the Southeastern culture of Native Americans called Caddoans or Caddo, who lived in the area until their expulsion in the 19th century. It is an internationally protected wetland under the RAMSAR treaty and features the largest Cypress forest in the world. Caddo is one of Texas' few non-oxbow natural lakes and is the 2nd largest in the South; however, it was artificially altered by the addition of a dam in the 1900s.
    CaddoCypressGrove1.jpg
  • The Hoh Rainforest is located on the Olympic Peninsula in western Washington state, USA. It is one of the few temperate rainforests in the U.S., and also one of the largest.  It was formed thousands of years ago by glaciers.
    HohHallMossesTrail3.jpg
  • Sol Duc Falls.  The name Sol Duc means "magic waters". The Sol Duc River is divided into 3 or 4 separate streams (depending on flow) by an irregular rocky ledge. The water drops about 25 feet over the ledge into a tight cleft, making a 90 degree angle turn. The river passes beneath a footbridge, then drops about 10 feet into a deep teal pool.
    SolDucTripleFalls.jpg
  • Small creek near Sol Duc Falls.  The name Sol Duc means "magic waters". The Sol Duc River is divided into 3 or 4 separate streams (depending on flow) by an irregular rocky ledge. The water drops about 25 feet over the ledge into a tight cleft, making a 90 degree angle turn. The river passes beneath a footbridge, then drops about 10 feet into a deep teal pool.
    SolDucCascades2.jpg
  • The Hoh Rainforest is located on the Olympic Peninsula in western Washington state, USA. It is one of the few temperate rainforests in the U.S., and also one of the largest.  It was formed thousands of years ago by glaciers.
    HohMapleGrove5.jpg
  • The Hoh Rainforest is located on the Olympic Peninsula in western Washington state, USA. It is one of the few temperate rainforests in the U.S., and also one of the largest.  It was formed thousands of years ago by glaciers.
    OlympicHohArches2.jpg
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