Inge Johnsson Photography

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  • Bright green leaves on tree in El Chalten, Patagonia
    ElChaltenFoliage1.jpg
  • Bright green leaves on tree in El Chalten, Patagonia
    ElChaltenFoliage1.jpg
  • Farm fields from Steptoe Butte in the Palouse region of eastern Washington state
    PalouseGreenSea.jpg
  • Point of the Arches is located on Shi-Shi Beach in Washington state's Olympic National Park
    PointOfArchesGreenRock1.jpg
  • Plitvice Lakes National Park is one of the oldest national parks in Southeast Europe and the largest national park in Croatia. In 1979, Plitvice Lakes National Park was added to the UNESCO World Heritage register. The national park was founded in 1949 and is situated in the mountainous karst area of central Croatia, at the border to Bosnia and Herzegovina. The important north-south road connection, which passes through the national park area, connects the Croatian inland with the Adriatic coastal region.<br />
<br />
The national park is world famous for its lakes arranged in cascades. Currently, 16 lakes can be seen from the surface. These lakes are a result of the confluence of several small rivers and subterranean karst rivers. The lakes are all interconnected and follow the water flow. They are separated by natural dams of travertine, which is deposited by the action of moss, algae, and bacteria. The particularly sensitive travertine barriers are the result of an interplay between water, air and plants. The encrusted plants and bacteria accumulate on top of each other, forming travertine barriers which grow at the rate of about 1 cm (0.4 in) per year.<br />
<br />
The lakes are renowned for their distinctive colors, ranging from azure to green, grey or blue. The colors change constantly depending on the quantity of minerals or organisms in the water and the angle of sunlight.
    PlitvicePanorama1.jpg
  • Plitvice Lakes National Park is one of the oldest national parks in Southeast Europe and the largest national park in Croatia. In 1979, Plitvice Lakes National Park was added to the UNESCO World Heritage register. The national park was founded in 1949 and is situated in the mountainous karst area of central Croatia, at the border to Bosnia and Herzegovina. The important north-south road connection, which passes through the national park area, connects the Croatian inland with the Adriatic coastal region.<br />
<br />
The national park is world famous for its lakes arranged in cascades. Currently, 16 lakes can be seen from the surface. These lakes are a result of the confluence of several small rivers and subterranean karst rivers. The lakes are all interconnected and follow the water flow. They are separated by natural dams of travertine, which is deposited by the action of moss, algae, and bacteria. The particularly sensitive travertine barriers are the result of an interplay between water, air and plants. The encrusted plants and bacteria accumulate on top of each other, forming travertine barriers which grow at the rate of about 1 cm (0.4 in) per year.<br />
<br />
The lakes are renowned for their distinctive colors, ranging from azure to green, grey or blue. The colors change constantly depending on the quantity of minerals or organisms in the water and the angle of sunlight.
    PlitviceLake1.jpg
  • One of my images from a two day visit to the Fly Geyser in Nevada, near the Black Rock Desert.  This image was made with a Canon EOS-1N and a Canon TS-E 24/3.5L lens on Fujichrome Velvia.  It was quite interesting exploring this natural phenomenon for such a prolonged time and to stand in the hot water surrounding the geyser.<br />
.....<br />
The continuous Fly Geyser of Fly Ranch is on private land in Nevada and began during 1916 when a water well drilling operation accidentally penetrated a geothermal source.<br />
Fly Geyser, also known as Fly Ranch Geyser is a small geothermal geyser that is located approximately 20 miles (32 km) north of Gerlach, in Washoe County, Nevada. The Geyser is located in Hualapai Flat, about 1/3 of a mile from State Route 34. It is large enough to be seen from the road.<br />
.....<br />
Fly Geyser is a little-known tourist attraction, even to Nevada residents. It is located near the edge of Fly Reservoir and is only about 5 feet (1.5 m) high, (12 feet (3.7 m) counting the mound on which it sits). The water well functioned normally for several decades, but in the 1960s geothermally heated water found a weak spot in the wall and began escaping to the surface. Dissolved minerals started rising and accumulating, creating the mount on which the geyser sits, which continues growing. Today water is constantly spewing, reaching 5 feet (1.5 m) in the air. The geyser contains several terraces discharging water into 30 to 40 pools over an area of 30 hectares (74 acres). The geyser is made up of a series of different minerals, which gives it its magnificent coloration.<br />
.....<br />
There are two additional geysers in the area that were created in a way similar to Fly Geyser. The first geyser is approximately three feet high and is shaped like a miniature volcano. The second geyser is cone-shaped and is of the same approximate size as Fly Geyser. Like Fly Geyser, these geysers are continually growing.
    FlyGeyserGreenTavertines-new.jpg
  • Grapes on the vine in Chelan wine country in Washington state
    LakeChelanGrapes3.jpg
  • Grapes on the vine in Chelan wine country in Washington state
    LakeChelanGrapes3.jpg
  • Lupinus texensis, the Texas bluebonnet, is a species of lupine endemic to Texas. With other related species of lupines also called bluebonnets, it is the state flower of Texas. It is a biennial plant which begins its life as a small, gravel-like seed. The seed has a hard seed coat that must be penetrated by wind, rain, and weather over the course of a few months (but sometimes several years). In the fall, the bluebonnets emerge as small seedings with two cotyledons, and later a rosette of leaves that are palmately compound with 5-7 leaflets 3-10 cm long, green with a faint white edge and hair. Growth continues over the mild winter months and then in the spring will take off and rapidly grow larger, before sending up a 20-50 cm tall plume of blue flowers (with bits of white and occasionally a tinge of pinkish-red). The scent of these blossoms has been diversely described; many people say they give off no scent at all, while a few have described the scent as 'sickly sweet'. It has been found in the wild with isolated mutations in other colors, most notably all-white flowers, pink, and maroon. These mutations have since been selectively bred to produce different color strains that are available commercially.
    BluebonnetPond7.jpg
  • Lupinus texensis, the Texas bluebonnet, is a species of lupine endemic to Texas. With other related species of lupines also called bluebonnets, it is the state flower of Texas. It is a biennial plant which begins its life as a small, gravel-like seed. The seed has a hard seed coat that must be penetrated by wind, rain, and weather over the course of a few months (but sometimes several years). In the fall, the bluebonnets emerge as small seedings with two cotyledons, and later a rosette of leaves that are palmately compound with 5-7 leaflets 3-10 cm long, green with a faint white edge and hair. Growth continues over the mild winter months and then in the spring will take off and rapidly grow larger, before sending up a 20-50 cm tall plume of blue flowers (with bits of white and occasionally a tinge of pinkish-red). The scent of these blossoms has been diversely described; many people say they give off no scent at all, while a few have described the scent as 'sickly sweet'. It has been found in the wild with isolated mutations in other colors, most notably all-white flowers, pink, and maroon. These mutations have since been selectively bred to produce different color strains that are available commercially.
    BluebonnetPond7.jpg
  • Plitvice Lakes National Park is one of the oldest national parks in Southeast Europe and the largest national park in Croatia. In 1979, Plitvice Lakes National Park was added to the UNESCO World Heritage register. The national park was founded in 1949 and is situated in the mountainous karst area of central Croatia, at the border to Bosnia and Herzegovina. The important north-south road connection, which passes through the national park area, connects the Croatian inland with the Adriatic coastal region.<br />
<br />
The national park is world famous for its lakes arranged in cascades. Currently, 16 lakes can be seen from the surface. These lakes are a result of the confluence of several small rivers and subterranean karst rivers. The lakes are all interconnected and follow the water flow. They are separated by natural dams of travertine, which is deposited by the action of moss, algae, and bacteria. The particularly sensitive travertine barriers are the result of an interplay between water, air and plants. The encrusted plants and bacteria accumulate on top of each other, forming travertine barriers which grow at the rate of about 1 cm (0.4 in) per year.<br />
<br />
The lakes are renowned for their distinctive colors, ranging from azure to green, grey or blue. The colors change constantly depending on the quantity of minerals or organisms in the water and the angle of sunlight.
    PlitvicePanorama1.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
  • Plitvice Lakes National Park is one of the oldest national parks in Southeast Europe and the largest national park in Croatia. In 1979, Plitvice Lakes National Park was added to the UNESCO World Heritage register. The national park was founded in 1949 and is situated in the mountainous karst area of central Croatia, at the border to Bosnia and Herzegovina. The important north-south road connection, which passes through the national park area, connects the Croatian inland with the Adriatic coastal region.<br />
<br />
The national park is world famous for its lakes arranged in cascades. Currently, 16 lakes can be seen from the surface. These lakes are a result of the confluence of several small rivers and subterranean karst rivers. The lakes are all interconnected and follow the water flow. They are separated by natural dams of travertine, which is deposited by the action of moss, algae, and bacteria. The particularly sensitive travertine barriers are the result of an interplay between water, air and plants. The encrusted plants and bacteria accumulate on top of each other, forming travertine barriers which grow at the rate of about 1 cm (0.4 in) per year.<br />
<br />
The lakes are renowned for their distinctive colors, ranging from azure to green, grey or blue. The colors change constantly depending on the quantity of minerals or organisms in the water and the angle of sunlight.
    Plitvice1.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
  • Plitvice Lakes National Park is one of the oldest national parks in Southeast Europe and the largest national park in Croatia. In 1979, Plitvice Lakes National Park was added to the UNESCO World Heritage register. The national park was founded in 1949 and is situated in the mountainous karst area of central Croatia, at the border to Bosnia and Herzegovina. The important north-south road connection, which passes through the national park area, connects the Croatian inland with the Adriatic coastal region.<br />
<br />
The national park is world famous for its lakes arranged in cascades. Currently, 16 lakes can be seen from the surface. These lakes are a result of the confluence of several small rivers and subterranean karst rivers. The lakes are all interconnected and follow the water flow. They are separated by natural dams of travertine, which is deposited by the action of moss, algae, and bacteria. The particularly sensitive travertine barriers are the result of an interplay between water, air and plants. The encrusted plants and bacteria accumulate on top of each other, forming travertine barriers which grow at the rate of about 1 cm (0.4 in) per year.<br />
<br />
The lakes are renowned for their distinctive colors, ranging from azure to green, grey or blue. The colors change constantly depending on the quantity of minerals or organisms in the water and the angle of sunlight.
    PlitvicePanorama1.jpg
  • Plitvice Lakes National Park is one of the oldest national parks in Southeast Europe and the largest national park in Croatia. In 1979, Plitvice Lakes National Park was added to the UNESCO World Heritage register. The national park was founded in 1949 and is situated in the mountainous karst area of central Croatia, at the border to Bosnia and Herzegovina. The important north-south road connection, which passes through the national park area, connects the Croatian inland with the Adriatic coastal region.<br />
<br />
The national park is world famous for its lakes arranged in cascades. Currently, 16 lakes can be seen from the surface. These lakes are a result of the confluence of several small rivers and subterranean karst rivers. The lakes are all interconnected and follow the water flow. They are separated by natural dams of travertine, which is deposited by the action of moss, algae, and bacteria. The particularly sensitive travertine barriers are the result of an interplay between water, air and plants. The encrusted plants and bacteria accumulate on top of each other, forming travertine barriers which grow at the rate of about 1 cm (0.4 in) per year.<br />
<br />
The lakes are renowned for their distinctive colors, ranging from azure to green, grey or blue. The colors change constantly depending on the quantity of minerals or organisms in the water and the angle of sunlight.
    PlitvicePanorama1.jpg
  • Lower Proxy Falls in Proxy Falls state park in the Three Sisters Wilderness
    ProxyFalls7.jpg
  • Point of the Arches is located on Shi-Shi Beach in Washington state's Olympic National Park
    PointOfArchesGreenRock1.jpg
  • Plitvice Lakes National Park is one of the oldest national parks in Southeast Europe and the largest national park in Croatia. In 1979, Plitvice Lakes National Park was added to the UNESCO World Heritage register. The national park was founded in 1949 and is situated in the mountainous karst area of central Croatia, at the border to Bosnia and Herzegovina. The important north-south road connection, which passes through the national park area, connects the Croatian inland with the Adriatic coastal region.<br />
<br />
The national park is world famous for its lakes arranged in cascades. Currently, 16 lakes can be seen from the surface. These lakes are a result of the confluence of several small rivers and subterranean karst rivers. The lakes are all interconnected and follow the water flow. They are separated by natural dams of travertine, which is deposited by the action of moss, algae, and bacteria. The particularly sensitive travertine barriers are the result of an interplay between water, air and plants. The encrusted plants and bacteria accumulate on top of each other, forming travertine barriers which grow at the rate of about 1 cm (0.4 in) per year.<br />
<br />
The lakes are renowned for their distinctive colors, ranging from azure to green, grey or blue. The colors change constantly depending on the quantity of minerals or organisms in the water and the angle of sunlight.
    Plitvice6.jpg
  • Plitvice Lakes National Park is one of the oldest national parks in Southeast Europe and the largest national park in Croatia. In 1979, Plitvice Lakes National Park was added to the UNESCO World Heritage register. The national park was founded in 1949 and is situated in the mountainous karst area of central Croatia, at the border to Bosnia and Herzegovina. The important north-south road connection, which passes through the national park area, connects the Croatian inland with the Adriatic coastal region.<br />
<br />
The national park is world famous for its lakes arranged in cascades. Currently, 16 lakes can be seen from the surface. These lakes are a result of the confluence of several small rivers and subterranean karst rivers. The lakes are all interconnected and follow the water flow. They are separated by natural dams of travertine, which is deposited by the action of moss, algae, and bacteria. The particularly sensitive travertine barriers are the result of an interplay between water, air and plants. The encrusted plants and bacteria accumulate on top of each other, forming travertine barriers which grow at the rate of about 1 cm (0.4 in) per year.<br />
<br />
The lakes are renowned for their distinctive colors, ranging from azure to green, grey or blue. The colors change constantly depending on the quantity of minerals or organisms in the water and the angle of sunlight.
    Plitvice2.jpg
  • Lupinus texensis, the Texas bluebonnet, is a species of lupine endemic to Texas. With other related species of lupines also called bluebonnets, it is the state flower of Texas. It is a biennial plant which begins its life as a small, gravel-like seed. The seed has a hard seed coat that must be penetrated by wind, rain, and weather over the course of a few months (but sometimes several years). In the fall, the bluebonnets emerge as small seedings with two cotyledons, and later a rosette of leaves that are palmately compound with 5-7 leaflets 3-10 cm long, green with a faint white edge and hair. Growth continues over the mild winter months and then in the spring will take off and rapidly grow larger, before sending up a 20-50 cm tall plume of blue flowers (with bits of white and occasionally a tinge of pinkish-red). The scent of these blossoms has been diversely described; many people say they give off no scent at all, while a few have described the scent as 'sickly sweet'. It has been found in the wild with isolated mutations in other colors, most notably all-white flowers, pink, and maroon. These mutations have since been selectively bred to produce different color strains that are available commercially.
    BluebonnetPond7.jpg
  • Rocks in the Sol Duc River in Washington state's Olympic National Park, river reflecting the surrounding spring green foliage
    SolDucGreenRocks.jpg
  • Farm tractor near the town of Palouse in the agricultural area of The Palouse in eastern Washington state.
    PalouseTractor1.jpg
  • Bluebonnets in Ennis, Texas. Lupinus texensis, the Texas bluebonnet, is a species of lupine endemic to Texas. With other related species of lupines also called bluebonnets, it is the state flower of Texas. It is a biennial plant which begins its life as a small, gravel-like seed. The seed has a hard seed coat that must be penetrated by wind, rain, and weather over the course of a few months (but sometimes several years). In the fall, the bluebonnets emerge as small seedings with two cotyledons, and later a rosette of leaves that are palmately compound with 5-7 leaflets 3-10 cm long, green with a faint white edge and hair. Growth continues over the mild winter months and then in the spring will take off and rapidly grow larger, before sending up a 20-50 cm tall plume of blue flowers (with bits of white and occasionally a tinge of pinkish-red). The scent of these blossoms has been diversely described; many people say they give off no scent at all, while a few have described the scent as 'sickly sweet'. It has been found in the wild with isolated mutations in other colors, most notably all-white flowers, pink, and maroon. These mutations have since been selectively bred to produce different color strains that are available commercially.
    EnnisBluebonnets13.jpg
  • Lupinus texensis, the Texas bluebonnet, is a species of lupine endemic to Texas. With other related species of lupines also called bluebonnets, it is the state flower of Texas. It is a biennial plant which begins its life as a small, gravel-like seed. The seed has a hard seed coat that must be penetrated by wind, rain, and weather over the course of a few months (but sometimes several years). In the fall, the bluebonnets emerge as small seedings with two cotyledons, and later a rosette of leaves that are palmately compound with 5-7 leaflets 3-10 cm long, green with a faint white edge and hair. Growth continues over the mild winter months and then in the spring will take off and rapidly grow larger, before sending up a 20-50 cm tall plume of blue flowers (with bits of white and occasionally a tinge of pinkish-red). The scent of these blossoms has been diversely described; many people say they give off no scent at all, while a few have described the scent as 'sickly sweet'. It has been found in the wild with isolated mutations in other colors, most notably all-white flowers, pink, and maroon. These mutations have since been selectively bred to produce different color strains that are available commercially.
    BluebonnetPond7.jpg
  • Bluebonnets in Ennis, Texas. Lupinus texensis, the Texas bluebonnet, is a species of lupine endemic to Texas. With other related species of lupines also called bluebonnets, it is the state flower of Texas. It is a biennial plant which begins its life as a small, gravel-like seed. The seed has a hard seed coat that must be penetrated by wind, rain, and weather over the course of a few months (but sometimes several years). In the fall, the bluebonnets emerge as small seedings with two cotyledons, and later a rosette of leaves that are palmately compound with 5-7 leaflets 3-10 cm long, green with a faint white edge and hair. Growth continues over the mild winter months and then in the spring will take off and rapidly grow larger, before sending up a 20-50 cm tall plume of blue flowers (with bits of white and occasionally a tinge of pinkish-red). The scent of these blossoms has been diversely described; many people say they give off no scent at all, while a few have described the scent as 'sickly sweet'. It has been found in the wild with isolated mutations in other colors, most notably all-white flowers, pink, and maroon. These mutations have since been selectively bred to produce different color strains that are available commercially.
    EnnisBluebonnets13.jpg
  • Point of the Arches is located on Shi-Shi Beach in Washington state's Olympic National Park
    PointOfArchesGreenRock1.jpg
  • Point of the Arches is located on Shi-Shi Beach in Washington state's Olympic National Park
    PointOfArchesGreenRock1.jpg
  • Point of the Arches is located on Shi-Shi Beach in Washington state's Olympic National Park
    PointOfArchesGreenRock1.jpg
  • Rocks in the Sol Duc River in Washington state's Olympic National Park, river reflecting the surrounding spring green foliage
    SolDucGreenRocks.jpg
  • The wood duck or Carolina duck (Aix sponsa) is a species of perching duck found in North America. It is one of the most colorful North American waterfowl. The adult male has distinctive multicolored iridescent plumage and red eyes,with a distinctive white flare down the neck. The female, less colorful, has a white eye-ring and a whitish throat. Both adults have crested heads.
    _R6C2166.jpg
  • Point of the Arches is located on Shi-Shi Beach in Washington state's Olympic National Park
    PointOfArchesGreenRock1.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
    ProxyFalls3.jpg
  • Plitvice Lakes National Park is one of the oldest national parks in Southeast Europe and the largest national park in Croatia. In 1979, Plitvice Lakes National Park was added to the UNESCO World Heritage register. The national park was founded in 1949 and is situated in the mountainous karst area of central Croatia, at the border to Bosnia and Herzegovina. The important north-south road connection, which passes through the national park area, connects the Croatian inland with the Adriatic coastal region.<br />
<br />
The national park is world famous for its lakes arranged in cascades. Currently, 16 lakes can be seen from the surface. These lakes are a result of the confluence of several small rivers and subterranean karst rivers. The lakes are all interconnected and follow the water flow. They are separated by natural dams of travertine, which is deposited by the action of moss, algae, and bacteria. The particularly sensitive travertine barriers are the result of an interplay between water, air and plants. The encrusted plants and bacteria accumulate on top of each other, forming travertine barriers which grow at the rate of about 1 cm (0.4 in) per year.<br />
<br />
The lakes are renowned for their distinctive colors, ranging from azure to green, grey or blue. The colors change constantly depending on the quantity of minerals or organisms in the water and the angle of sunlight.
    PlitvicePanorama1.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
  • Lower Proxy Falls in Proxy Falls state park in the Three Sisters Wilderness
    ProxyFalls7.jpg
  • Plitvice Lakes National Park is one of the oldest national parks in Southeast Europe and the largest national park in Croatia. In 1979, Plitvice Lakes National Park was added to the UNESCO World Heritage register. The national park was founded in 1949 and is situated in the mountainous karst area of central Croatia, at the border to Bosnia and Herzegovina. The important north-south road connection, which passes through the national park area, connects the Croatian inland with the Adriatic coastal region.<br />
<br />
The national park is world famous for its lakes arranged in cascades. Currently, 16 lakes can be seen from the surface. These lakes are a result of the confluence of several small rivers and subterranean karst rivers. The lakes are all interconnected and follow the water flow. They are separated by natural dams of travertine, which is deposited by the action of moss, algae, and bacteria. The particularly sensitive travertine barriers are the result of an interplay between water, air and plants. The encrusted plants and bacteria accumulate on top of each other, forming travertine barriers which grow at the rate of about 1 cm (0.4 in) per year.<br />
<br />
The lakes are renowned for their distinctive colors, ranging from azure to green, grey or blue. The colors change constantly depending on the quantity of minerals or organisms in the water and the angle of sunlight.
    Plitvice8.jpg
  • Plitvice Lakes National Park is one of the oldest national parks in Southeast Europe and the largest national park in Croatia. In 1979, Plitvice Lakes National Park was added to the UNESCO World Heritage register. The national park was founded in 1949 and is situated in the mountainous karst area of central Croatia, at the border to Bosnia and Herzegovina. The important north-south road connection, which passes through the national park area, connects the Croatian inland with the Adriatic coastal region.<br />
<br />
The national park is world famous for its lakes arranged in cascades. Currently, 16 lakes can be seen from the surface. These lakes are a result of the confluence of several small rivers and subterranean karst rivers. The lakes are all interconnected and follow the water flow. They are separated by natural dams of travertine, which is deposited by the action of moss, algae, and bacteria. The particularly sensitive travertine barriers are the result of an interplay between water, air and plants. The encrusted plants and bacteria accumulate on top of each other, forming travertine barriers which grow at the rate of about 1 cm (0.4 in) per year.<br />
<br />
The lakes are renowned for their distinctive colors, ranging from azure to green, grey or blue. The colors change constantly depending on the quantity of minerals or organisms in the water and the angle of sunlight.
    Plitvice5.jpg
  • Plitvice Lakes National Park is one of the oldest national parks in Southeast Europe and the largest national park in Croatia. In 1979, Plitvice Lakes National Park was added to the UNESCO World Heritage register. The national park was founded in 1949 and is situated in the mountainous karst area of central Croatia, at the border to Bosnia and Herzegovina. The important north-south road connection, which passes through the national park area, connects the Croatian inland with the Adriatic coastal region.<br />
<br />
The national park is world famous for its lakes arranged in cascades. Currently, 16 lakes can be seen from the surface. These lakes are a result of the confluence of several small rivers and subterranean karst rivers. The lakes are all interconnected and follow the water flow. They are separated by natural dams of travertine, which is deposited by the action of moss, algae, and bacteria. The particularly sensitive travertine barriers are the result of an interplay between water, air and plants. The encrusted plants and bacteria accumulate on top of each other, forming travertine barriers which grow at the rate of about 1 cm (0.4 in) per year.<br />
<br />
The lakes are renowned for their distinctive colors, ranging from azure to green, grey or blue. The colors change constantly depending on the quantity of minerals or organisms in the water and the angle of sunlight.
    Plitvice4.jpg
  • Plitvice Lakes National Park is one of the oldest national parks in Southeast Europe and the largest national park in Croatia. In 1979, Plitvice Lakes National Park was added to the UNESCO World Heritage register. The national park was founded in 1949 and is situated in the mountainous karst area of central Croatia, at the border to Bosnia and Herzegovina. The important north-south road connection, which passes through the national park area, connects the Croatian inland with the Adriatic coastal region.<br />
<br />
The national park is world famous for its lakes arranged in cascades. Currently, 16 lakes can be seen from the surface. These lakes are a result of the confluence of several small rivers and subterranean karst rivers. The lakes are all interconnected and follow the water flow. They are separated by natural dams of travertine, which is deposited by the action of moss, algae, and bacteria. The particularly sensitive travertine barriers are the result of an interplay between water, air and plants. The encrusted plants and bacteria accumulate on top of each other, forming travertine barriers which grow at the rate of about 1 cm (0.4 in) per year.<br />
<br />
The lakes are renowned for their distinctive colors, ranging from azure to green, grey or blue. The colors change constantly depending on the quantity of minerals or organisms in the water and the angle of sunlight.
    PlitviceBoat1.jpg
  • Lower Proxy Falls in Proxy Falls state park in the Three Sisters Wilderness
    ProxyFalls2.jpg
  • Farm fields from Steptoe Butte in the Palouse region of eastern Washington state
    PalouseGreenSea.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
  • Burano is an island in the Venetian Lagoon, although like Venice itself it could more correctly be called an archipelago of islands linked by bridges. Burano is also known for its small, brightly-painted houses, popular with artists.
    Burano2.jpg
  • Bluebonnets in Ennis, Texas. Lupinus texensis, the Texas bluebonnet, is a species of lupine endemic to Texas. With other related species of lupines also called bluebonnets, it is the state flower of Texas. It is a biennial plant which begins its life as a small, gravel-like seed. The seed has a hard seed coat that must be penetrated by wind, rain, and weather over the course of a few months (but sometimes several years). In the fall, the bluebonnets emerge as small seedings with two cotyledons, and later a rosette of leaves that are palmately compound with 5-7 leaflets 3-10 cm long, green with a faint white edge and hair. Growth continues over the mild winter months and then in the spring will take off and rapidly grow larger, before sending up a 20-50 cm tall plume of blue flowers (with bits of white and occasionally a tinge of pinkish-red). The scent of these blossoms has been diversely described; many people say they give off no scent at all, while a few have described the scent as 'sickly sweet'. It has been found in the wild with isolated mutations in other colors, most notably all-white flowers, pink, and maroon. These mutations have since been selectively bred to produce different color strains that are available commercially.
    EnnisBluebonnets13.jpg
  • Lupinus texensis, the Texas bluebonnet, is a species of lupine endemic to Texas. With other related species of lupines also called bluebonnets, it is the state flower of Texas. It is a biennial plant which begins its life as a small, gravel-like seed. The seed has a hard seed coat that must be penetrated by wind, rain, and weather over the course of a few months (but sometimes several years). In the fall, the bluebonnets emerge as small seedings with two cotyledons, and later a rosette of leaves that are palmately compound with 5-7 leaflets 3-10 cm long, green with a faint white edge and hair. Growth continues over the mild winter months and then in the spring will take off and rapidly grow larger, before sending up a 20-50 cm tall plume of blue flowers (with bits of white and occasionally a tinge of pinkish-red). The scent of these blossoms has been diversely described; many people say they give off no scent at all, while a few have described the scent as 'sickly sweet'. It has been found in the wild with isolated mutations in other colors, most notably all-white flowers, pink, and maroon. These mutations have since been selectively bred to produce different color strains that are available commercially.
    BluebonnetPond7.jpg
  • Bluebonnets in Ennis, Texas. Lupinus texensis, the Texas bluebonnet, is a species of lupine endemic to Texas. With other related species of lupines also called bluebonnets, it is the state flower of Texas. It is a biennial plant which begins its life as a small, gravel-like seed. The seed has a hard seed coat that must be penetrated by wind, rain, and weather over the course of a few months (but sometimes several years). In the fall, the bluebonnets emerge as small seedings with two cotyledons, and later a rosette of leaves that are palmately compound with 5-7 leaflets 3-10 cm long, green with a faint white edge and hair. Growth continues over the mild winter months and then in the spring will take off and rapidly grow larger, before sending up a 20-50 cm tall plume of blue flowers (with bits of white and occasionally a tinge of pinkish-red). The scent of these blossoms has been diversely described; many people say they give off no scent at all, while a few have described the scent as 'sickly sweet'. It has been found in the wild with isolated mutations in other colors, most notably all-white flowers, pink, and maroon. These mutations have since been selectively bred to produce different color strains that are available commercially.
    EnnisBluebonnets13.jpg
  • Plitvice Lakes National Park is one of the oldest national parks in Southeast Europe and the largest national park in Croatia. In 1979, Plitvice Lakes National Park was added to the UNESCO World Heritage register. The national park was founded in 1949 and is situated in the mountainous karst area of central Croatia, at the border to Bosnia and Herzegovina. The important north-south road connection, which passes through the national park area, connects the Croatian inland with the Adriatic coastal region.<br />
<br />
The national park is world famous for its lakes arranged in cascades. Currently, 16 lakes can be seen from the surface. These lakes are a result of the confluence of several small rivers and subterranean karst rivers. The lakes are all interconnected and follow the water flow. They are separated by natural dams of travertine, which is deposited by the action of moss, algae, and bacteria. The particularly sensitive travertine barriers are the result of an interplay between water, air and plants. The encrusted plants and bacteria accumulate on top of each other, forming travertine barriers which grow at the rate of about 1 cm (0.4 in) per year.<br />
<br />
The lakes are renowned for their distinctive colors, ranging from azure to green, grey or blue. The colors change constantly depending on the quantity of minerals or organisms in the water and the angle of sunlight.
    Plitvice1.jpg
  • Point of the Arches is located on Shi-Shi Beach in Washington state's Olympic National Park
    PointOfArchesGreenRock1.jpg
  • Point of the Arches is located on Shi-Shi Beach in Washington state's Olympic National Park
    PointOfArchesGreenRock1.jpg
  • Lower Proxy Falls in Proxy Falls state park in the Three Sisters Wilderness
    ProxyFalls2.jpg
  • Point of the Arches is located on Shi-Shi Beach in Washington state's Olympic National Park
    PointOfArchesGreenRock1.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
  • The Seattle Great Wheel is a giant Ferris wheel at Pier 57 on Elliott Bay in Seattle, Washington, United States. With an overall height of 175 feet, it became the tallest Ferris wheel on the west coast of the United States when it opened on June 29, 2012. Seattle was the third city in North America to offer a wheel of this design, following the Niagara SkyWheel at Clifton Hill, Niagara Falls, Canada, which is also 175 feet tall, and the larger Myrtle Beach SkyWheel in South Carolina, which is 187 feet tall. The Seattle wheel is the only one of the three to be built over water. The Seattle Great Wheel has 42 climate-controlled gondolas, each able to carry up to eight passengers (except the "VIP" gondola, seating four), giving a maximum capacity of over 300. The 12-minute ride extends 40 feet out over Elliott Bay. Seattle businessman and waterfront developer Hal Griffith has envisioned a Ferris wheel on Elliott Bay for nearly 30 years. Along with his family, he is the owner of the Pier 57 upon which the Seattle Great Wheel is located. In addition to the wheel, the pier is the location of Miner's Landing, which consists of souvenir gift shops, tourist attractions, and variety of seafood restaurants. During the 1980s, Griffith began developing plans to ensure the perpetual existence and success of the family's business ventures on the pier. His plans had long included continual development of the waterfront on Puget Sound to provide entertainment and recreational opportunities for tourists and local residents. His goal was to drive success through innovative ideas, staying a step ahead of the competition. Griffith often met logistical and political roadblocks that inhibited development on the waterfront, but he was determined to build the Ferris wheel on Pier 57, located adjacent to the Alaskan Way Viaduct.
    GreatWheel1.jpg
  • Point of the Arches is located on Shi-Shi Beach in Washington state's Olympic National Park
    PointOfArchesGreenRock1.jpg
  • Plitvice Lakes National Park is one of the oldest national parks in Southeast Europe and the largest national park in Croatia. In 1979, Plitvice Lakes National Park was added to the UNESCO World Heritage register. The national park was founded in 1949 and is situated in the mountainous karst area of central Croatia, at the border to Bosnia and Herzegovina. The important north-south road connection, which passes through the national park area, connects the Croatian inland with the Adriatic coastal region.<br />
<br />
The national park is world famous for its lakes arranged in cascades. Currently, 16 lakes can be seen from the surface. These lakes are a result of the confluence of several small rivers and subterranean karst rivers. The lakes are all interconnected and follow the water flow. They are separated by natural dams of travertine, which is deposited by the action of moss, algae, and bacteria. The particularly sensitive travertine barriers are the result of an interplay between water, air and plants. The encrusted plants and bacteria accumulate on top of each other, forming travertine barriers which grow at the rate of about 1 cm (0.4 in) per year.<br />
<br />
The lakes are renowned for their distinctive colors, ranging from azure to green, grey or blue. The colors change constantly depending on the quantity of minerals or organisms in the water and the angle of sunlight.
    _R6C7044_HDR.jpg
  • Plitvice Lakes National Park is one of the oldest national parks in Southeast Europe and the largest national park in Croatia. In 1979, Plitvice Lakes National Park was added to the UNESCO World Heritage register. The national park was founded in 1949 and is situated in the mountainous karst area of central Croatia, at the border to Bosnia and Herzegovina. The important north-south road connection, which passes through the national park area, connects the Croatian inland with the Adriatic coastal region.<br />
<br />
The national park is world famous for its lakes arranged in cascades. Currently, 16 lakes can be seen from the surface. These lakes are a result of the confluence of several small rivers and subterranean karst rivers. The lakes are all interconnected and follow the water flow. They are separated by natural dams of travertine, which is deposited by the action of moss, algae, and bacteria. The particularly sensitive travertine barriers are the result of an interplay between water, air and plants. The encrusted plants and bacteria accumulate on top of each other, forming travertine barriers which grow at the rate of about 1 cm (0.4 in) per year.<br />
<br />
The lakes are renowned for their distinctive colors, ranging from azure to green, grey or blue. The colors change constantly depending on the quantity of minerals or organisms in the water and the angle of sunlight.
    PlitvicePanorama1.jpg
  • Plitvice Lakes National Park is one of the oldest national parks in Southeast Europe and the largest national park in Croatia. In 1979, Plitvice Lakes National Park was added to the UNESCO World Heritage register. The national park was founded in 1949 and is situated in the mountainous karst area of central Croatia, at the border to Bosnia and Herzegovina. The important north-south road connection, which passes through the national park area, connects the Croatian inland with the Adriatic coastal region.<br />
<br />
The national park is world famous for its lakes arranged in cascades. Currently, 16 lakes can be seen from the surface. These lakes are a result of the confluence of several small rivers and subterranean karst rivers. The lakes are all interconnected and follow the water flow. They are separated by natural dams of travertine, which is deposited by the action of moss, algae, and bacteria. The particularly sensitive travertine barriers are the result of an interplay between water, air and plants. The encrusted plants and bacteria accumulate on top of each other, forming travertine barriers which grow at the rate of about 1 cm (0.4 in) per year.<br />
<br />
The lakes are renowned for their distinctive colors, ranging from azure to green, grey or blue. The colors change constantly depending on the quantity of minerals or organisms in the water and the angle of sunlight.
    PlitviceLake2.jpg
  • Plitvice Lakes National Park is one of the oldest national parks in Southeast Europe and the largest national park in Croatia. In 1979, Plitvice Lakes National Park was added to the UNESCO World Heritage register. The national park was founded in 1949 and is situated in the mountainous karst area of central Croatia, at the border to Bosnia and Herzegovina. The important north-south road connection, which passes through the national park area, connects the Croatian inland with the Adriatic coastal region.<br />
<br />
The national park is world famous for its lakes arranged in cascades. Currently, 16 lakes can be seen from the surface. These lakes are a result of the confluence of several small rivers and subterranean karst rivers. The lakes are all interconnected and follow the water flow. They are separated by natural dams of travertine, which is deposited by the action of moss, algae, and bacteria. The particularly sensitive travertine barriers are the result of an interplay between water, air and plants. The encrusted plants and bacteria accumulate on top of each other, forming travertine barriers which grow at the rate of about 1 cm (0.4 in) per year.<br />
<br />
The lakes are renowned for their distinctive colors, ranging from azure to green, grey or blue. The colors change constantly depending on the quantity of minerals or organisms in the water and the angle of sunlight.
    Plitvice7.jpg
  • Plitvice Lakes National Park is one of the oldest national parks in Southeast Europe and the largest national park in Croatia. In 1979, Plitvice Lakes National Park was added to the UNESCO World Heritage register. The national park was founded in 1949 and is situated in the mountainous karst area of central Croatia, at the border to Bosnia and Herzegovina. The important north-south road connection, which passes through the national park area, connects the Croatian inland with the Adriatic coastal region.<br />
<br />
The national park is world famous for its lakes arranged in cascades. Currently, 16 lakes can be seen from the surface. These lakes are a result of the confluence of several small rivers and subterranean karst rivers. The lakes are all interconnected and follow the water flow. They are separated by natural dams of travertine, which is deposited by the action of moss, algae, and bacteria. The particularly sensitive travertine barriers are the result of an interplay between water, air and plants. The encrusted plants and bacteria accumulate on top of each other, forming travertine barriers which grow at the rate of about 1 cm (0.4 in) per year.<br />
<br />
The lakes are renowned for their distinctive colors, ranging from azure to green, grey or blue. The colors change constantly depending on the quantity of minerals or organisms in the water and the angle of sunlight.
    Plitvice3.jpg
  • Plitvice Lakes National Park is one of the oldest national parks in Southeast Europe and the largest national park in Croatia. In 1979, Plitvice Lakes National Park was added to the UNESCO World Heritage register. The national park was founded in 1949 and is situated in the mountainous karst area of central Croatia, at the border to Bosnia and Herzegovina. The important north-south road connection, which passes through the national park area, connects the Croatian inland with the Adriatic coastal region.<br />
<br />
The national park is world famous for its lakes arranged in cascades. Currently, 16 lakes can be seen from the surface. These lakes are a result of the confluence of several small rivers and subterranean karst rivers. The lakes are all interconnected and follow the water flow. They are separated by natural dams of travertine, which is deposited by the action of moss, algae, and bacteria. The particularly sensitive travertine barriers are the result of an interplay between water, air and plants. The encrusted plants and bacteria accumulate on top of each other, forming travertine barriers which grow at the rate of about 1 cm (0.4 in) per year.<br />
<br />
The lakes are renowned for their distinctive colors, ranging from azure to green, grey or blue. The colors change constantly depending on the quantity of minerals or organisms in the water and the angle of sunlight.
    Plitvice1.jpg
  • Old door in Zagreb, Croatia
    ZagrebDoor1.jpg
  • Bluebonnets in Ennis, Texas. Lupinus texensis, the Texas bluebonnet, is a species of lupine endemic to Texas. With other related species of lupines also called bluebonnets, it is the state flower of Texas. It is a biennial plant which begins its life as a small, gravel-like seed. The seed has a hard seed coat that must be penetrated by wind, rain, and weather over the course of a few months (but sometimes several years). In the fall, the bluebonnets emerge as small seedings with two cotyledons, and later a rosette of leaves that are palmately compound with 5-7 leaflets 3-10 cm long, green with a faint white edge and hair. Growth continues over the mild winter months and then in the spring will take off and rapidly grow larger, before sending up a 20-50 cm tall plume of blue flowers (with bits of white and occasionally a tinge of pinkish-red). The scent of these blossoms has been diversely described; many people say they give off no scent at all, while a few have described the scent as 'sickly sweet'. It has been found in the wild with isolated mutations in other colors, most notably all-white flowers, pink, and maroon. These mutations have since been selectively bred to produce different color strains that are available commercially.
    EnnisBluebonnets13.jpg
  • Rocks in creek on the the north side of Mount Rainier, near Carbon Glacier
    MtRainierGreenRocks.jpg
  • Farm tractor near the town of Palouse in the agricultural area of The Palouse in eastern Washington state.
    PalouseTractor1.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
  • Rocks in creek on the the north side of Mount Rainier, near Carbon Glacier
    MtRainierGreenRocks.jpg
  • The Seattle Great Wheel is a giant Ferris wheel at Pier 57 on Elliott Bay in Seattle, Washington, United States. With an overall height of 175 feet, it became the tallest Ferris wheel on the west coast of the United States when it opened on June 29, 2012. Seattle was the third city in North America to offer a wheel of this design, following the Niagara SkyWheel at Clifton Hill, Niagara Falls, Canada, which is also 175 feet tall, and the larger Myrtle Beach SkyWheel in South Carolina, which is 187 feet tall. The Seattle wheel is the only one of the three to be built over water. The Seattle Great Wheel has 42 climate-controlled gondolas, each able to carry up to eight passengers (except the "VIP" gondola, seating four), giving a maximum capacity of over 300. The 12-minute ride extends 40 feet out over Elliott Bay. Seattle businessman and waterfront developer Hal Griffith has envisioned a Ferris wheel on Elliott Bay for nearly 30 years. Along with his family, he is the owner of the Pier 57 upon which the Seattle Great Wheel is located. In addition to the wheel, the pier is the location of Miner's Landing, which consists of souvenir gift shops, tourist attractions, and variety of seafood restaurants. During the 1980s, Griffith began developing plans to ensure the perpetual existence and success of the family's business ventures on the pier. His plans had long included continual development of the waterfront on Puget Sound to provide entertainment and recreational opportunities for tourists and local residents. His goal was to drive success through innovative ideas, staying a step ahead of the competition. Griffith often met logistical and political roadblocks that inhibited development on the waterfront, but he was determined to build the Ferris wheel on Pier 57, located adjacent to the Alaskan Way Viaduct.
    GreatWheel1.jpg
  • The wood duck or Carolina duck (Aix sponsa) is a species of perching duck found in North America. It is one of the most colorful North American waterfowl. The adult male has distinctive multicolored iridescent plumage and red eyes,with a distinctive white flare down the neck. The female, less colorful, has a white eye-ring and a whitish throat. Both adults have crested heads.
    WoodDuck1.jpg
  • Lower Proxy Falls in Proxy Falls state park in the Three Sisters Wilderness
    ProxyFalls3.jpg
  • The continuous Fly Geyser of Fly Ranch is on private land in Nevada and began during 1916 when a water well drilling operation accidentally penetrated a geothermal source.<br />
Fly Geyser, also known as Fly Ranch Geyser is a small geothermal geyser that is located approximately 20 miles (32 km) north of Gerlach, in Washoe County, Nevada. The Geyser is located in Hualapai Flat, about 1/3 of a mile from State Route 34. It is large enough to be seen from the road.<br />
.....<br />
Fly Geyser is a little-known tourist attraction, even to Nevada residents. It is located near the edge of Fly Reservoir and is only about 5 feet (1.5 m) high, (12 feet (3.7 m) counting the mound on which it sits). The water well functioned normally for several decades, but in the 1960s geothermally heated water found a weak spot in the wall and began escaping to the surface. Dissolved minerals started rising and accumulating, creating the mount on which the geyser sits, which continues growing. Today water is constantly spewing, reaching 5 feet (1.5 m) in the air. The geyser contains several terraces discharging water into 30 to 40 pools over an area of 30 hectares (74 acres). The geyser is made up of a series of different minerals, which gives it its magnificent coloration.<br />
.....<br />
There are two additional geysers in the area that were created in a way similar to Fly Geyser. The first geyser is approximately three feet high and is shaped like a miniature volcano. The second geyser is cone-shaped and is of the same approximate size as Fly Geyser. Like Fly Geyser, these geysers are continually growing.
    FlyGeyserPanorama1.jpg
  • The continuous Fly Geyser of Fly Ranch is on private land in Nevada and began during 1916 when a water well drilling operation accidentally penetrated a geothermal source.<br />
Fly Geyser, also known as Fly Ranch Geyser is a small geothermal geyser that is located approximately 20 miles (32 km) north of Gerlach, in Washoe County, Nevada. The Geyser is located in Hualapai Flat, about 1/3 of a mile from State Route 34. It is large enough to be seen from the road.<br />
.....<br />
Fly Geyser is a little-known tourist attraction, even to Nevada residents. It is located near the edge of Fly Reservoir and is only about 5 feet (1.5 m) high, (12 feet (3.7 m) counting the mound on which it sits). The water well functioned normally for several decades, but in the 1960s geothermally heated water found a weak spot in the wall and began escaping to the surface. Dissolved minerals started rising and accumulating, creating the mount on which the geyser sits, which continues growing. Today water is constantly spewing, reaching 5 feet (1.5 m) in the air. The geyser contains several terraces discharging water into 30 to 40 pools over an area of 30 hectares (74 acres). The geyser is made up of a series of different minerals, which gives it its magnificent coloration.<br />
.....<br />
There are two additional geysers in the area that were created in a way similar to Fly Geyser. The first geyser is approximately three feet high and is shaped like a miniature volcano. The second geyser is cone-shaped and is of the same approximate size as Fly Geyser. Like Fly Geyser, these geysers are continually growing.
    FlyGeyserYellow2.jpg
  • Trillium Lake south of Mount Hood with view of the mountain, two people in a canoe on the lake
    TrilliumLakeBlueCanoe1.jpg
  • Mount Baker reflecting in tarn near Park Butte in the Mount Baker Wilderness <br />
..... <br />
Mount Baker, also known as Koma Kulshan or simply Kulshan, is an active glaciated andesitic stratovolcano in the Cascade Volcanic Arc and the North Cascades of Washington State in the United States. Mount Baker has the second-most thermally active crater in the Cascade Range after Mount Saint Helens. About 31 miles due east of the city of Bellingham, Whatcom County, Mount Baker is the youngest volcano in the Mount Baker volcanic field. While volcanism has persisted here for some 1.5 million years, the current glaciated cone is likely no more than 140,000 years old, and possibly no older than 80-90,000 years. <br />
After Mount Rainier, Mount Baker is the most heavily glaciated of the Cascade Range volcanoes; the volume of snow and ice on Mount Baker, 0.43 cu mi is greater than that of all the other Cascades volcanoes (except Rainier) combined. At 10,781 ft, it is the third-highest mountain in Washington State and the fifth-highest in the Cascade Range, if Little Tahoma Peak, a subpeak of Mount Rainier, and Shastina, a subpeak of Mount Shasta, are not counted. Located in the Mount Baker Wilderness, it is visible from much of Greater Victoria, Greater Vancouver, and, to the south, from Seattle (and on clear days Tacoma) in Washington. <br />
Indigenous natives have known the mountain for thousands of years, but the first written record of the mountain is from the Spanish. Spanish explorer Gonzalo Lopez de Haro mapped it in 1790 as the Gran Montana del Carmelo, "Great Mount Carmel". The explorer George Vancouver renamed the mountain for 3rd Lieutenant Joseph Baker of HMS Discovery, who saw it on April 30, 1792.
    MountBakerParkButteTarn4.jpg
  • Mount Rainier from Tipsoo Lake
    MtRainierUpperTipsoo2.jpg
  • Trillium Lake south of Mount Hood with view of the mountain, two people in a canoe on the lake
    TrilliumLakeBlueCanoe1.jpg
  • Mount Rainier from Tipsoo Lake
    MtRainierUpperTipsoo2.jpg
  • Mount Rainier from Tipsoo Lake
    MtRainierUpperTipsoo2.jpg
  • The continuous Fly Geyser of Fly Ranch is on private land in Nevada and began during 1916 when a water well drilling operation accidentally penetrated a geothermal source.<br />
Fly Geyser, also known as Fly Ranch Geyser is a small geothermal geyser that is located approximately 20 miles (32 km) north of Gerlach, in Washoe County, Nevada. The Geyser is located in Hualapai Flat, about 1/3 of a mile from State Route 34. It is large enough to be seen from the road.<br />
.....<br />
Fly Geyser is a little-known tourist attraction, even to Nevada residents. It is located near the edge of Fly Reservoir and is only about 5 feet (1.5 m) high, (12 feet (3.7 m) counting the mound on which it sits). The water well functioned normally for several decades, but in the 1960s geothermally heated water found a weak spot in the wall and began escaping to the surface. Dissolved minerals started rising and accumulating, creating the mount on which the geyser sits, which continues growing. Today water is constantly spewing, reaching 5 feet (1.5 m) in the air. The geyser contains several terraces discharging water into 30 to 40 pools over an area of 30 hectares (74 acres). The geyser is made up of a series of different minerals, which gives it its magnificent coloration.<br />
.....<br />
There are two additional geysers in the area that were created in a way similar to Fly Geyser. The first geyser is approximately three feet high and is shaped like a miniature volcano. The second geyser is cone-shaped and is of the same approximate size as Fly Geyser. Like Fly Geyser, these geysers are continually growing.
    FlyGeyserYellow1.jpg
  • Mount Baker reflecting in tarn near Park Butte in the Mount Baker Wilderness <br />
..... <br />
Mount Baker, also known as Koma Kulshan or simply Kulshan, is an active glaciated andesitic stratovolcano in the Cascade Volcanic Arc and the North Cascades of Washington State in the United States. Mount Baker has the second-most thermally active crater in the Cascade Range after Mount Saint Helens. About 31 miles due east of the city of Bellingham, Whatcom County, Mount Baker is the youngest volcano in the Mount Baker volcanic field. While volcanism has persisted here for some 1.5 million years, the current glaciated cone is likely no more than 140,000 years old, and possibly no older than 80-90,000 years. <br />
After Mount Rainier, Mount Baker is the most heavily glaciated of the Cascade Range volcanoes; the volume of snow and ice on Mount Baker, 0.43 cu mi is greater than that of all the other Cascades volcanoes (except Rainier) combined. At 10,781 ft, it is the third-highest mountain in Washington State and the fifth-highest in the Cascade Range, if Little Tahoma Peak, a subpeak of Mount Rainier, and Shastina, a subpeak of Mount Shasta, are not counted. Located in the Mount Baker Wilderness, it is visible from much of Greater Victoria, Greater Vancouver, and, to the south, from Seattle (and on clear days Tacoma) in Washington. <br />
Indigenous natives have known the mountain for thousands of years, but the first written record of the mountain is from the Spanish. Spanish explorer Gonzalo Lopez de Haro mapped it in 1790 as the Gran Montana del Carmelo, "Great Mount Carmel". The explorer George Vancouver renamed the mountain for 3rd Lieutenant Joseph Baker of HMS Discovery, who saw it on April 30, 1792.
    MountBakerParkButteTarn4.jpg
  • Trillium Lake south of Mount Hood with view of the mountain, two people in a canoe on the lake
    TrilliumLakeBlueCanoe1.jpg
  • Trillium Lake south of Mount Hood with view of the mountain, two people in a canoe on the lake
    TrilliumLakeBlueCanoe1.jpg
  • Trillium Lake south of Mount Hood with view of the mountain, two people in a canoe on the lake
    TrilliumLakeBlueCanoe1.jpg
  • Trillium Lake south of Mount Hood with view of the mountain, two people in a canoe on the lake
    TrilliumLakeBlueCanoe1.jpg
  • Mount Rainier from Tipsoo Lake
    MtRainierUpperTipsoo2.jpg
  • Mount Baker reflecting in tarn near Park Butte in the Mount Baker Wilderness <br />
..... <br />
Mount Baker, also known as Koma Kulshan or simply Kulshan, is an active glaciated andesitic stratovolcano in the Cascade Volcanic Arc and the North Cascades of Washington State in the United States. Mount Baker has the second-most thermally active crater in the Cascade Range after Mount Saint Helens. About 31 miles due east of the city of Bellingham, Whatcom County, Mount Baker is the youngest volcano in the Mount Baker volcanic field. While volcanism has persisted here for some 1.5 million years, the current glaciated cone is likely no more than 140,000 years old, and possibly no older than 80-90,000 years. <br />
After Mount Rainier, Mount Baker is the most heavily glaciated of the Cascade Range volcanoes; the volume of snow and ice on Mount Baker, 0.43 cu mi is greater than that of all the other Cascades volcanoes (except Rainier) combined. At 10,781 ft, it is the third-highest mountain in Washington State and the fifth-highest in the Cascade Range, if Little Tahoma Peak, a subpeak of Mount Rainier, and Shastina, a subpeak of Mount Shasta, are not counted. Located in the Mount Baker Wilderness, it is visible from much of Greater Victoria, Greater Vancouver, and, to the south, from Seattle (and on clear days Tacoma) in Washington. <br />
Indigenous natives have known the mountain for thousands of years, but the first written record of the mountain is from the Spanish. Spanish explorer Gonzalo Lopez de Haro mapped it in 1790 as the Gran Montana del Carmelo, "Great Mount Carmel". The explorer George Vancouver renamed the mountain for 3rd Lieutenant Joseph Baker of HMS Discovery, who saw it on April 30, 1792.
    MountBakerParkButteTarn5.jpg
  • Trillium Lake south of Mount Hood with view of the mountain, two people in a canoe on the lake
    TrilliumLakeBlueCanoe1.jpg
  • Mount Rainier from Tipsoo Lake
    MtRainierUpperTipsoo2.jpg
  • Hoh Rainforest in Olympic National Park, in autumn
    HohGrove2.jpg
  • Vineyard in Chelan, Washington, with Lake Chelan below
    LakeChelanBensonVineyard1.jpg
  • Trillium Lake south of Mount Hood with view of the mountain, two people in a canoe on the lake
    TrilliumLakeBlueCanoe1.jpg
  • Mount Baker reflecting in tarn near Park Butte in the Mount Baker Wilderness <br />
..... <br />
Mount Baker, also known as Koma Kulshan or simply Kulshan, is an active glaciated andesitic stratovolcano in the Cascade Volcanic Arc and the North Cascades of Washington State in the United States. Mount Baker has the second-most thermally active crater in the Cascade Range after Mount Saint Helens. About 31 miles due east of the city of Bellingham, Whatcom County, Mount Baker is the youngest volcano in the Mount Baker volcanic field. While volcanism has persisted here for some 1.5 million years, the current glaciated cone is likely no more than 140,000 years old, and possibly no older than 80-90,000 years. <br />
After Mount Rainier, Mount Baker is the most heavily glaciated of the Cascade Range volcanoes; the volume of snow and ice on Mount Baker, 0.43 cu mi is greater than that of all the other Cascades volcanoes (except Rainier) combined. At 10,781 ft, it is the third-highest mountain in Washington State and the fifth-highest in the Cascade Range, if Little Tahoma Peak, a subpeak of Mount Rainier, and Shastina, a subpeak of Mount Shasta, are not counted. Located in the Mount Baker Wilderness, it is visible from much of Greater Victoria, Greater Vancouver, and, to the south, from Seattle (and on clear days Tacoma) in Washington. <br />
Indigenous natives have known the mountain for thousands of years, but the first written record of the mountain is from the Spanish. Spanish explorer Gonzalo Lopez de Haro mapped it in 1790 as the Gran Montana del Carmelo, "Great Mount Carmel". The explorer George Vancouver renamed the mountain for 3rd Lieutenant Joseph Baker of HMS Discovery, who saw it on April 30, 1792.
    MountBakerParkButteTarn5.jpg
  • Trillium Lake south of Mount Hood with view of the mountain, two people in a canoe on the lake
    TrilliumLakeBlueCanoe1.jpg
  • Sol Duc Falls in Olympic National Park, in autumn.  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.
    SolDucFallsAutumn1.jpg
  • Prusik Peak from an icy Gnome Tarn in the Enchantment Lakes area of the Alpine Lakes Wilderness, Washington
    EnchantmentsGnomeTarnIce2.jpg
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