Inge Johnsson Photography

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  • Located at the western gateway to Downtown Los Angeles, 10.5-acre Vista Hermosa Park is an urban natural park developed by the MRCA that boldly returns the serenity and diversity of nature the Los Angeles urban core. Operated in collaboration with the Los Angeles Unified School District and the City of Los Angeles, Vista Hermosa Natural Park is a popular destination for residents of this densely populated neighborhood.<br />
<br />
The park features walking trails, streams, meadows, oak savannahs, picnic grounds, and a nature-themed playground amidst native Mediterranean vegetation. A FIFA-regulation soccer field is jointly used by the adjacent Edward R. Roybal Learning Center and the L.A. Department of Recreation and Parks. An outdoor amphitheater in a grotto provides an ideal setting for environmental and natural history education, and other public events.
    VistaHermosa1.jpg
  • Located at the western gateway to Downtown Los Angeles, 10.5-acre Vista Hermosa Park is an urban natural park developed by the MRCA that boldly returns the serenity and diversity of nature the Los Angeles urban core. Operated in collaboration with the Los Angeles Unified School District and the City of Los Angeles, Vista Hermosa Natural Park is a popular destination for residents of this densely populated neighborhood.<br />
<br />
The park features walking trails, streams, meadows, oak savannahs, picnic grounds, and a nature-themed playground amidst native Mediterranean vegetation. A FIFA-regulation soccer field is jointly used by the adjacent Edward R. Roybal Learning Center and the L.A. Department of Recreation and Parks. An outdoor amphitheater in a grotto provides an ideal setting for environmental and natural history education, and other public events.
    VistaHermosa3.jpg
  • Located at the western gateway to Downtown Los Angeles, 10.5-acre Vista Hermosa Park is an urban natural park developed by the MRCA that boldly returns the serenity and diversity of nature the Los Angeles urban core. Operated in collaboration with the Los Angeles Unified School District and the City of Los Angeles, Vista Hermosa Natural Park is a popular destination for residents of this densely populated neighborhood.<br />
<br />
The park features walking trails, streams, meadows, oak savannahs, picnic grounds, and a nature-themed playground amidst native Mediterranean vegetation. A FIFA-regulation soccer field is jointly used by the adjacent Edward R. Roybal Learning Center and the L.A. Department of Recreation and Parks. An outdoor amphitheater in a grotto provides an ideal setting for environmental and natural history education, and other public events.
    VistaHermosa4.jpg
  • Located at the western gateway to Downtown Los Angeles, 10.5-acre Vista Hermosa Park is an urban natural park developed by the MRCA that boldly returns the serenity and diversity of nature the Los Angeles urban core. Operated in collaboration with the Los Angeles Unified School District and the City of Los Angeles, Vista Hermosa Natural Park is a popular destination for residents of this densely populated neighborhood.<br />
<br />
The park features walking trails, streams, meadows, oak savannahs, picnic grounds, and a nature-themed playground amidst native Mediterranean vegetation. A FIFA-regulation soccer field is jointly used by the adjacent Edward R. Roybal Learning Center and the L.A. Department of Recreation and Parks. An outdoor amphitheater in a grotto provides an ideal setting for environmental and natural history education, and other public events.
    VistaHermosa2.jpg
  • The Portland Japanese Garden is a traditional Japanese garden occupying 12 acres, located within Washington Park in the West Hills of Portland, Oregon, United States. It is operated as a private non-profit organization, which leased the site from the city in the early 1960s. Stephen D. Bloom has been the chief executive officer of the Portland Japanese Garden since 2005. <br />
<br />
The Garden Pavilion was built in 1980 in Japanese style by local builders: it has a tiled roof, wooden verandas, and Shōji sliding doors. It is the center of several Japanese cultural festivals, art exhibitions, and other events. The west veranda faces the Flat Garden, and the east veranda overlooks downtown Portland and Mount Hood, which resembles Mount Fuji. Dozens of stone lanterns are present throughout the garden. The lower entrance features a 100-year-old temple gate, a 1976 gift of the Japanese Ancestral Society of Portland Oregon.<br />
<br />
As a Japanese garden, the desired effect is to realize a sense of peace, harmony, and tranquility and to experience the feeling of being a part of nature. Three of the essential elements used to create the garden are stone, the "bones" of the landscape; water, the life-giving force; and plants, the tapestry of the four seasons. Japanese garden designers feel that good stone composition is one of the most important elements in creating a well-designed garden. Secondary elements include pagodas, stone lanterns, water basins, arbors, and bridges. Japanese gardens are asymmetrical in design and reflect nature in idealized form. Traditionally, human scale is maintained throughout so that one always feels part of the environment and not overpowered by it.<br />
<br />
The Japanese rock garden (枯山水 karesansui) or "dry landscape" garden, often called a zen garden, creates a miniature stylized landscape through carefully composed arrangements of rocks, water features, moss, pruned trees and bushes, and uses gravel or sand that is raked to represent ripples in water. A zen gar
    PortlandJapaneseGarden3.jpg
  • The Portland Japanese Garden is a traditional Japanese garden occupying 12 acres, located within Washington Park in the West Hills of Portland, Oregon, United States. It is operated as a private non-profit organization, which leased the site from the city in the early 1960s. Stephen D. Bloom has been the chief executive officer of the Portland Japanese Garden since 2005. <br />
<br />
The Garden Pavilion was built in 1980 in Japanese style by local builders: it has a tiled roof, wooden verandas, and Shōji sliding doors. It is the center of several Japanese cultural festivals, art exhibitions, and other events. The west veranda faces the Flat Garden, and the east veranda overlooks downtown Portland and Mount Hood, which resembles Mount Fuji. Dozens of stone lanterns are present throughout the garden. The lower entrance features a 100-year-old temple gate, a 1976 gift of the Japanese Ancestral Society of Portland Oregon.<br />
<br />
As a Japanese garden, the desired effect is to realize a sense of peace, harmony, and tranquility and to experience the feeling of being a part of nature. Three of the essential elements used to create the garden are stone, the "bones" of the landscape; water, the life-giving force; and plants, the tapestry of the four seasons. Japanese garden designers feel that good stone composition is one of the most important elements in creating a well-designed garden. Secondary elements include pagodas, stone lanterns, water basins, arbors, and bridges. Japanese gardens are asymmetrical in design and reflect nature in idealized form. Traditionally, human scale is maintained throughout so that one always feels part of the environment and not overpowered by it.
    PortlandJapaneseGarden17.jpg
  • The Portland Japanese Garden is a traditional Japanese garden occupying 12 acres, located within Washington Park in the West Hills of Portland, Oregon, United States. It is operated as a private non-profit organization, which leased the site from the city in the early 1960s. Stephen D. Bloom has been the chief executive officer of the Portland Japanese Garden since 2005. <br />
<br />
The Garden Pavilion was built in 1980 in Japanese style by local builders: it has a tiled roof, wooden verandas, and Shōji sliding doors. It is the center of several Japanese cultural festivals, art exhibitions, and other events. The west veranda faces the Flat Garden, and the east veranda overlooks downtown Portland and Mount Hood, which resembles Mount Fuji. Dozens of stone lanterns are present throughout the garden. The lower entrance features a 100-year-old temple gate, a 1976 gift of the Japanese Ancestral Society of Portland Oregon.<br />
<br />
As a Japanese garden, the desired effect is to realize a sense of peace, harmony, and tranquility and to experience the feeling of being a part of nature. Three of the essential elements used to create the garden are stone, the "bones" of the landscape; water, the life-giving force; and plants, the tapestry of the four seasons. Japanese garden designers feel that good stone composition is one of the most important elements in creating a well-designed garden. Secondary elements include pagodas, stone lanterns, water basins, arbors, and bridges. Japanese gardens are asymmetrical in design and reflect nature in idealized form. Traditionally, human scale is maintained throughout so that one always feels part of the environment and not overpowered by it.
    PortlandJapaneseGarden8.jpg
  • The Portland Japanese Garden is a traditional Japanese garden occupying 12 acres, located within Washington Park in the West Hills of Portland, Oregon, United States. It is operated as a private non-profit organization, which leased the site from the city in the early 1960s. Stephen D. Bloom has been the chief executive officer of the Portland Japanese Garden since 2005. <br />
<br />
The Garden Pavilion was built in 1980 in Japanese style by local builders: it has a tiled roof, wooden verandas, and Shōji sliding doors. It is the center of several Japanese cultural festivals, art exhibitions, and other events. The west veranda faces the Flat Garden, and the east veranda overlooks downtown Portland and Mount Hood, which resembles Mount Fuji. Dozens of stone lanterns are present throughout the garden. The lower entrance features a 100-year-old temple gate, a 1976 gift of the Japanese Ancestral Society of Portland Oregon.<br />
<br />
As a Japanese garden, the desired effect is to realize a sense of peace, harmony, and tranquility and to experience the feeling of being a part of nature. Three of the essential elements used to create the garden are stone, the "bones" of the landscape; water, the life-giving force; and plants, the tapestry of the four seasons. Japanese garden designers feel that good stone composition is one of the most important elements in creating a well-designed garden. Secondary elements include pagodas, stone lanterns, water basins, arbors, and bridges. Japanese gardens are asymmetrical in design and reflect nature in idealized form. Traditionally, human scale is maintained throughout so that one always feels part of the environment and not overpowered by it.
    PortlandJapaneseGarden4.jpg
  • The Portland Japanese Garden is a traditional Japanese garden occupying 12 acres, located within Washington Park in the West Hills of Portland, Oregon, United States. It is operated as a private non-profit organization, which leased the site from the city in the early 1960s. Stephen D. Bloom has been the chief executive officer of the Portland Japanese Garden since 2005. <br />
<br />
The Garden Pavilion was built in 1980 in Japanese style by local builders: it has a tiled roof, wooden verandas, and Shōji sliding doors. It is the center of several Japanese cultural festivals, art exhibitions, and other events. The west veranda faces the Flat Garden, and the east veranda overlooks downtown Portland and Mount Hood, which resembles Mount Fuji. Dozens of stone lanterns are present throughout the garden. The lower entrance features a 100-year-old temple gate, a 1976 gift of the Japanese Ancestral Society of Portland Oregon.<br />
<br />
As a Japanese garden, the desired effect is to realize a sense of peace, harmony, and tranquility and to experience the feeling of being a part of nature. Three of the essential elements used to create the garden are stone, the "bones" of the landscape; water, the life-giving force; and plants, the tapestry of the four seasons. Japanese garden designers feel that good stone composition is one of the most important elements in creating a well-designed garden. Secondary elements include pagodas, stone lanterns, water basins, arbors, and bridges. Japanese gardens are asymmetrical in design and reflect nature in idealized form. Traditionally, human scale is maintained throughout so that one always feels part of the environment and not overpowered by it.
    PortlandJapaneseGarden2.jpg
  • The Portland Japanese Garden is a traditional Japanese garden occupying 12 acres, located within Washington Park in the West Hills of Portland, Oregon, United States. It is operated as a private non-profit organization, which leased the site from the city in the early 1960s. Stephen D. Bloom has been the chief executive officer of the Portland Japanese Garden since 2005. <br />
<br />
The Garden Pavilion was built in 1980 in Japanese style by local builders: it has a tiled roof, wooden verandas, and Shōji sliding doors. It is the center of several Japanese cultural festivals, art exhibitions, and other events. The west veranda faces the Flat Garden, and the east veranda overlooks downtown Portland and Mount Hood, which resembles Mount Fuji. Dozens of stone lanterns are present throughout the garden. The lower entrance features a 100-year-old temple gate, a 1976 gift of the Japanese Ancestral Society of Portland Oregon.<br />
<br />
As a Japanese garden, the desired effect is to realize a sense of peace, harmony, and tranquility and to experience the feeling of being a part of nature. Three of the essential elements used to create the garden are stone, the "bones" of the landscape; water, the life-giving force; and plants, the tapestry of the four seasons. Japanese garden designers feel that good stone composition is one of the most important elements in creating a well-designed garden. Secondary elements include pagodas, stone lanterns, water basins, arbors, and bridges. Japanese gardens are asymmetrical in design and reflect nature in idealized form. Traditionally, human scale is maintained throughout so that one always feels part of the environment and not overpowered by it.
    PortlandJapaneseGarden15.jpg
  • The Portland Japanese Garden is a traditional Japanese garden occupying 12 acres, located within Washington Park in the West Hills of Portland, Oregon, United States. It is operated as a private non-profit organization, which leased the site from the city in the early 1960s. Stephen D. Bloom has been the chief executive officer of the Portland Japanese Garden since 2005. <br />
<br />
The Garden Pavilion was built in 1980 in Japanese style by local builders: it has a tiled roof, wooden verandas, and Shōji sliding doors. It is the center of several Japanese cultural festivals, art exhibitions, and other events. The west veranda faces the Flat Garden, and the east veranda overlooks downtown Portland and Mount Hood, which resembles Mount Fuji. Dozens of stone lanterns are present throughout the garden. The lower entrance features a 100-year-old temple gate, a 1976 gift of the Japanese Ancestral Society of Portland Oregon.<br />
<br />
As a Japanese garden, the desired effect is to realize a sense of peace, harmony, and tranquility and to experience the feeling of being a part of nature. Three of the essential elements used to create the garden are stone, the "bones" of the landscape; water, the life-giving force; and plants, the tapestry of the four seasons. Japanese garden designers feel that good stone composition is one of the most important elements in creating a well-designed garden. Secondary elements include pagodas, stone lanterns, water basins, arbors, and bridges. Japanese gardens are asymmetrical in design and reflect nature in idealized form. Traditionally, human scale is maintained throughout so that one always feels part of the environment and not overpowered by it.
    PortlandJapaneseGarden13.jpg
  • The Portland Japanese Garden is a traditional Japanese garden occupying 12 acres, located within Washington Park in the West Hills of Portland, Oregon, United States. It is operated as a private non-profit organization, which leased the site from the city in the early 1960s. Stephen D. Bloom has been the chief executive officer of the Portland Japanese Garden since 2005. <br />
<br />
The Garden Pavilion was built in 1980 in Japanese style by local builders: it has a tiled roof, wooden verandas, and Shōji sliding doors. It is the center of several Japanese cultural festivals, art exhibitions, and other events. The west veranda faces the Flat Garden, and the east veranda overlooks downtown Portland and Mount Hood, which resembles Mount Fuji. Dozens of stone lanterns are present throughout the garden. The lower entrance features a 100-year-old temple gate, a 1976 gift of the Japanese Ancestral Society of Portland Oregon.<br />
<br />
As a Japanese garden, the desired effect is to realize a sense of peace, harmony, and tranquility and to experience the feeling of being a part of nature. Three of the essential elements used to create the garden are stone, the "bones" of the landscape; water, the life-giving force; and plants, the tapestry of the four seasons. Japanese garden designers feel that good stone composition is one of the most important elements in creating a well-designed garden. Secondary elements include pagodas, stone lanterns, water basins, arbors, and bridges. Japanese gardens are asymmetrical in design and reflect nature in idealized form. Traditionally, human scale is maintained throughout so that one always feels part of the environment and not overpowered by it.
    PortlandJapaneseGarden12.jpg
  • The Portland Japanese Garden is a traditional Japanese garden occupying 12 acres, located within Washington Park in the West Hills of Portland, Oregon, United States. It is operated as a private non-profit organization, which leased the site from the city in the early 1960s. Stephen D. Bloom has been the chief executive officer of the Portland Japanese Garden since 2005. <br />
<br />
The Garden Pavilion was built in 1980 in Japanese style by local builders: it has a tiled roof, wooden verandas, and Shōji sliding doors. It is the center of several Japanese cultural festivals, art exhibitions, and other events. The west veranda faces the Flat Garden, and the east veranda overlooks downtown Portland and Mount Hood, which resembles Mount Fuji. Dozens of stone lanterns are present throughout the garden. The lower entrance features a 100-year-old temple gate, a 1976 gift of the Japanese Ancestral Society of Portland Oregon.<br />
<br />
As a Japanese garden, the desired effect is to realize a sense of peace, harmony, and tranquility and to experience the feeling of being a part of nature. Three of the essential elements used to create the garden are stone, the "bones" of the landscape; water, the life-giving force; and plants, the tapestry of the four seasons. Japanese garden designers feel that good stone composition is one of the most important elements in creating a well-designed garden. Secondary elements include pagodas, stone lanterns, water basins, arbors, and bridges. Japanese gardens are asymmetrical in design and reflect nature in idealized form. Traditionally, human scale is maintained throughout so that one always feels part of the environment and not overpowered by it.
    PortlandJapaneseGarden11.jpg
  • The Portland Japanese Garden is a traditional Japanese garden occupying 12 acres, located within Washington Park in the West Hills of Portland, Oregon, United States. It is operated as a private non-profit organization, which leased the site from the city in the early 1960s. Stephen D. Bloom has been the chief executive officer of the Portland Japanese Garden since 2005. <br />
<br />
The Garden Pavilion was built in 1980 in Japanese style by local builders: it has a tiled roof, wooden verandas, and Shōji sliding doors. It is the center of several Japanese cultural festivals, art exhibitions, and other events. The west veranda faces the Flat Garden, and the east veranda overlooks downtown Portland and Mount Hood, which resembles Mount Fuji. Dozens of stone lanterns are present throughout the garden. The lower entrance features a 100-year-old temple gate, a 1976 gift of the Japanese Ancestral Society of Portland Oregon.<br />
<br />
As a Japanese garden, the desired effect is to realize a sense of peace, harmony, and tranquility and to experience the feeling of being a part of nature. Three of the essential elements used to create the garden are stone, the "bones" of the landscape; water, the life-giving force; and plants, the tapestry of the four seasons. Japanese garden designers feel that good stone composition is one of the most important elements in creating a well-designed garden. Secondary elements include pagodas, stone lanterns, water basins, arbors, and bridges. Japanese gardens are asymmetrical in design and reflect nature in idealized form. Traditionally, human scale is maintained throughout so that one always feels part of the environment and not overpowered by it.
    PortlandJapaneseGarden9.jpg
  • The Portland Japanese Garden is a traditional Japanese garden occupying 12 acres, located within Washington Park in the West Hills of Portland, Oregon, United States. It is operated as a private non-profit organization, which leased the site from the city in the early 1960s. Stephen D. Bloom has been the chief executive officer of the Portland Japanese Garden since 2005. <br />
<br />
The Garden Pavilion was built in 1980 in Japanese style by local builders: it has a tiled roof, wooden verandas, and Shōji sliding doors. It is the center of several Japanese cultural festivals, art exhibitions, and other events. The west veranda faces the Flat Garden, and the east veranda overlooks downtown Portland and Mount Hood, which resembles Mount Fuji. Dozens of stone lanterns are present throughout the garden. The lower entrance features a 100-year-old temple gate, a 1976 gift of the Japanese Ancestral Society of Portland Oregon.<br />
<br />
As a Japanese garden, the desired effect is to realize a sense of peace, harmony, and tranquility and to experience the feeling of being a part of nature. Three of the essential elements used to create the garden are stone, the "bones" of the landscape; water, the life-giving force; and plants, the tapestry of the four seasons. Japanese garden designers feel that good stone composition is one of the most important elements in creating a well-designed garden. Secondary elements include pagodas, stone lanterns, water basins, arbors, and bridges. Japanese gardens are asymmetrical in design and reflect nature in idealized form. Traditionally, human scale is maintained throughout so that one always feels part of the environment and not overpowered by it.
    PortlandJapaneseGarden5.jpg
  • The Portland Japanese Garden is a traditional Japanese garden occupying 12 acres, located within Washington Park in the West Hills of Portland, Oregon, United States. It is operated as a private non-profit organization, which leased the site from the city in the early 1960s. Stephen D. Bloom has been the chief executive officer of the Portland Japanese Garden since 2005. <br />
<br />
The Garden Pavilion was built in 1980 in Japanese style by local builders: it has a tiled roof, wooden verandas, and Shōji sliding doors. It is the center of several Japanese cultural festivals, art exhibitions, and other events. The west veranda faces the Flat Garden, and the east veranda overlooks downtown Portland and Mount Hood, which resembles Mount Fuji. Dozens of stone lanterns are present throughout the garden. The lower entrance features a 100-year-old temple gate, a 1976 gift of the Japanese Ancestral Society of Portland Oregon.<br />
<br />
As a Japanese garden, the desired effect is to realize a sense of peace, harmony, and tranquility and to experience the feeling of being a part of nature. Three of the essential elements used to create the garden are stone, the "bones" of the landscape; water, the life-giving force; and plants, the tapestry of the four seasons. Japanese garden designers feel that good stone composition is one of the most important elements in creating a well-designed garden. Secondary elements include pagodas, stone lanterns, water basins, arbors, and bridges. Japanese gardens are asymmetrical in design and reflect nature in idealized form. Traditionally, human scale is maintained throughout so that one always feels part of the environment and not overpowered by it.
    PortlandJapaneseGarden1.jpg
  • The Portland Japanese Garden is a traditional Japanese garden occupying 12 acres, located within Washington Park in the West Hills of Portland, Oregon, United States. It is operated as a private non-profit organization, which leased the site from the city in the early 1960s. Stephen D. Bloom has been the chief executive officer of the Portland Japanese Garden since 2005. <br />
<br />
The Garden Pavilion was built in 1980 in Japanese style by local builders: it has a tiled roof, wooden verandas, and Shōji sliding doors. It is the center of several Japanese cultural festivals, art exhibitions, and other events. The west veranda faces the Flat Garden, and the east veranda overlooks downtown Portland and Mount Hood, which resembles Mount Fuji. Dozens of stone lanterns are present throughout the garden. The lower entrance features a 100-year-old temple gate, a 1976 gift of the Japanese Ancestral Society of Portland Oregon.<br />
<br />
As a Japanese garden, the desired effect is to realize a sense of peace, harmony, and tranquility and to experience the feeling of being a part of nature. Three of the essential elements used to create the garden are stone, the "bones" of the landscape; water, the life-giving force; and plants, the tapestry of the four seasons. Japanese garden designers feel that good stone composition is one of the most important elements in creating a well-designed garden. Secondary elements include pagodas, stone lanterns, water basins, arbors, and bridges. Japanese gardens are asymmetrical in design and reflect nature in idealized form. Traditionally, human scale is maintained throughout so that one always feels part of the environment and not overpowered by it.
    PortlandJapaneseGarden10.jpg
  • The Portland Japanese Garden is a traditional Japanese garden occupying 12 acres, located within Washington Park in the West Hills of Portland, Oregon, United States. It is operated as a private non-profit organization, which leased the site from the city in the early 1960s. Stephen D. Bloom has been the chief executive officer of the Portland Japanese Garden since 2005. <br />
<br />
The Garden Pavilion was built in 1980 in Japanese style by local builders: it has a tiled roof, wooden verandas, and Shōji sliding doors. It is the center of several Japanese cultural festivals, art exhibitions, and other events. The west veranda faces the Flat Garden, and the east veranda overlooks downtown Portland and Mount Hood, which resembles Mount Fuji. Dozens of stone lanterns are present throughout the garden. The lower entrance features a 100-year-old temple gate, a 1976 gift of the Japanese Ancestral Society of Portland Oregon.<br />
<br />
As a Japanese garden, the desired effect is to realize a sense of peace, harmony, and tranquility and to experience the feeling of being a part of nature. Three of the essential elements used to create the garden are stone, the "bones" of the landscape; water, the life-giving force; and plants, the tapestry of the four seasons. Japanese garden designers feel that good stone composition is one of the most important elements in creating a well-designed garden. Secondary elements include pagodas, stone lanterns, water basins, arbors, and bridges. Japanese gardens are asymmetrical in design and reflect nature in idealized form. Traditionally, human scale is maintained throughout so that one always feels part of the environment and not overpowered by it.
    PortlandJapaneseGarden16.jpg
  • The Portland Japanese Garden is a traditional Japanese garden occupying 12 acres, located within Washington Park in the West Hills of Portland, Oregon, United States. It is operated as a private non-profit organization, which leased the site from the city in the early 1960s. Stephen D. Bloom has been the chief executive officer of the Portland Japanese Garden since 2005. <br />
<br />
The Garden Pavilion was built in 1980 in Japanese style by local builders: it has a tiled roof, wooden verandas, and Shōji sliding doors. It is the center of several Japanese cultural festivals, art exhibitions, and other events. The west veranda faces the Flat Garden, and the east veranda overlooks downtown Portland and Mount Hood, which resembles Mount Fuji. Dozens of stone lanterns are present throughout the garden. The lower entrance features a 100-year-old temple gate, a 1976 gift of the Japanese Ancestral Society of Portland Oregon.<br />
<br />
As a Japanese garden, the desired effect is to realize a sense of peace, harmony, and tranquility and to experience the feeling of being a part of nature. Three of the essential elements used to create the garden are stone, the "bones" of the landscape; water, the life-giving force; and plants, the tapestry of the four seasons. Japanese garden designers feel that good stone composition is one of the most important elements in creating a well-designed garden. Secondary elements include pagodas, stone lanterns, water basins, arbors, and bridges. Japanese gardens are asymmetrical in design and reflect nature in idealized form. Traditionally, human scale is maintained throughout so that one always feels part of the environment and not overpowered by it.
    PortlandJapaneseGarden7.jpg
  • The Portland Japanese Garden is a traditional Japanese garden occupying 12 acres, located within Washington Park in the West Hills of Portland, Oregon, United States. It is operated as a private non-profit organization, which leased the site from the city in the early 1960s. Stephen D. Bloom has been the chief executive officer of the Portland Japanese Garden since 2005. <br />
<br />
The Garden Pavilion was built in 1980 in Japanese style by local builders: it has a tiled roof, wooden verandas, and Shōji sliding doors. It is the center of several Japanese cultural festivals, art exhibitions, and other events. The west veranda faces the Flat Garden, and the east veranda overlooks downtown Portland and Mount Hood, which resembles Mount Fuji. Dozens of stone lanterns are present throughout the garden. The lower entrance features a 100-year-old temple gate, a 1976 gift of the Japanese Ancestral Society of Portland Oregon.<br />
<br />
As a Japanese garden, the desired effect is to realize a sense of peace, harmony, and tranquility and to experience the feeling of being a part of nature. Three of the essential elements used to create the garden are stone, the "bones" of the landscape; water, the life-giving force; and plants, the tapestry of the four seasons. Japanese garden designers feel that good stone composition is one of the most important elements in creating a well-designed garden. Secondary elements include pagodas, stone lanterns, water basins, arbors, and bridges. Japanese gardens are asymmetrical in design and reflect nature in idealized form. Traditionally, human scale is maintained throughout so that one always feels part of the environment and not overpowered by it.
    PortlandJapaneseGarden14.jpg
  • The Portland Japanese Garden is a traditional Japanese garden occupying 12 acres, located within Washington Park in the West Hills of Portland, Oregon, United States. It is operated as a private non-profit organization, which leased the site from the city in the early 1960s. Stephen D. Bloom has been the chief executive officer of the Portland Japanese Garden since 2005. <br />
<br />
The Garden Pavilion was built in 1980 in Japanese style by local builders: it has a tiled roof, wooden verandas, and Shōji sliding doors. It is the center of several Japanese cultural festivals, art exhibitions, and other events. The west veranda faces the Flat Garden, and the east veranda overlooks downtown Portland and Mount Hood, which resembles Mount Fuji. Dozens of stone lanterns are present throughout the garden. The lower entrance features a 100-year-old temple gate, a 1976 gift of the Japanese Ancestral Society of Portland Oregon.<br />
<br />
As a Japanese garden, the desired effect is to realize a sense of peace, harmony, and tranquility and to experience the feeling of being a part of nature. Three of the essential elements used to create the garden are stone, the "bones" of the landscape; water, the life-giving force; and plants, the tapestry of the four seasons. Japanese garden designers feel that good stone composition is one of the most important elements in creating a well-designed garden. Secondary elements include pagodas, stone lanterns, water basins, arbors, and bridges. Japanese gardens are asymmetrical in design and reflect nature in idealized form. Traditionally, human scale is maintained throughout so that one always feels part of the environment and not overpowered by it.
    PortlandJapaneseGarden6.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
  • 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.
    Landmannalaugar1.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.
    Landmannalaugar4.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.
    Landmannalaugar2.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.
    Landmannalaugar5.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.
    Landmannalaugar3.jpg
  • Kerlingarfjöll is a 1,477 m (4,846 ft)) tall mountain range in Iceland situated in the Highlands of Iceland near the Kjölur highland road. They are part of a large tuya volcano system of 100 km2 (39 sq mi). The volcanic origin of these mountains is evidenced by the numerous hot springs and rivulets in the area, as well as red volcanic rhyolite stone the mountains are composed of. Minerals that have emerged from the hot springs also color the ground yellow, red and green.<br />
<br />
The area was formerly known for its summer ski resort, but this was dismantled in 2000. From 2000 Kerlingarfjöll have been operated as a highland resort, offering accommodation and food services to the guests in the area.<br />
<br />
It was on March 17 in 2017 that the Iceland Monitor wrote that Kerlingarfjöll Mountains and geothermal area were being turned into a nature reserve. Although parts of the place already had protection, after made into reserve, all the whole 367 square kilometres are to be under the protection of the state of Iceland. Earlier, there had been thoughts of using the 140 degree Celsius hot springs as a geothermal power plant. It had already been popular of course with hiking and the tourists.
    KerlingarfjollAurora1.jpg
  • Kerlingarfjöll is a 1,477 m (4,846 ft)) tall mountain range in Iceland situated in the Highlands of Iceland near the Kjölur highland road. They are part of a large tuya volcano system of 100 km2 (39 sq mi). The volcanic origin of these mountains is evidenced by the numerous hot springs and rivulets in the area, as well as red volcanic rhyolite stone the mountains are composed of. Minerals that have emerged from the hot springs also color the ground yellow, red and green.<br />
<br />
The area was formerly known for its summer ski resort, but this was dismantled in 2000. From 2000 Kerlingarfjöll have been operated as a highland resort, offering accommodation and food services to the guests in the area.<br />
<br />
It was on March 17 in 2017 that the Iceland Monitor wrote that Kerlingarfjöll Mountains and geothermal area were being turned into a nature reserve. Although parts of the place already had protection, after made into reserve, all the whole 367 square kilometres are to be under the protection of the state of Iceland. Earlier, there had been thoughts of using the 140 degree Celsius hot springs as a geothermal power plant. It had already been popular of course with hiking and the tourists[
    Kerlingarfjoll5.jpg
  • Kerlingarfjöll is a 1,477 m (4,846 ft)) tall mountain range in Iceland situated in the Highlands of Iceland near the Kjölur highland road. They are part of a large tuya volcano system of 100 km2 (39 sq mi). The volcanic origin of these mountains is evidenced by the numerous hot springs and rivulets in the area, as well as red volcanic rhyolite stone the mountains are composed of. Minerals that have emerged from the hot springs also color the ground yellow, red and green.<br />
<br />
The area was formerly known for its summer ski resort, but this was dismantled in 2000. From 2000 Kerlingarfjöll have been operated as a highland resort, offering accommodation and food services to the guests in the area.<br />
<br />
It was on March 17 in 2017 that the Iceland Monitor wrote that Kerlingarfjöll Mountains and geothermal area were being turned into a nature reserve. Although parts of the place already had protection, after made into reserve, all the whole 367 square kilometres are to be under the protection of the state of Iceland. Earlier, there had been thoughts of using the 140 degree Celsius hot springs as a geothermal power plant. It had already been popular of course with hiking and the tourists[
    KerlingarfjollSteam6.jpg
  • Kerlingarfjöll is a 1,477 m (4,846 ft)) tall mountain range in Iceland situated in the Highlands of Iceland near the Kjölur highland road. They are part of a large tuya volcano system of 100 km2 (39 sq mi). The volcanic origin of these mountains is evidenced by the numerous hot springs and rivulets in the area, as well as red volcanic rhyolite stone the mountains are composed of. Minerals that have emerged from the hot springs also color the ground yellow, red and green.<br />
<br />
The area was formerly known for its summer ski resort, but this was dismantled in 2000. From 2000 Kerlingarfjöll have been operated as a highland resort, offering accommodation and food services to the guests in the area.<br />
<br />
It was on March 17 in 2017 that the Iceland Monitor wrote that Kerlingarfjöll Mountains and geothermal area were being turned into a nature reserve. Although parts of the place already had protection, after made into reserve, all the whole 367 square kilometres are to be under the protection of the state of Iceland. Earlier, there had been thoughts of using the 140 degree Celsius hot springs as a geothermal power plant. It had already been popular of course with hiking and the tourists[
    Kerlingarfjoll2.jpg
  • Kerlingarfjöll is a 1,477 m (4,846 ft)) tall mountain range in Iceland situated in the Highlands of Iceland near the Kjölur highland road. They are part of a large tuya volcano system of 100 km2 (39 sq mi). The volcanic origin of these mountains is evidenced by the numerous hot springs and rivulets in the area, as well as red volcanic rhyolite stone the mountains are composed of. Minerals that have emerged from the hot springs also color the ground yellow, red and green.<br />
<br />
The area was formerly known for its summer ski resort, but this was dismantled in 2000. From 2000 Kerlingarfjöll have been operated as a highland resort, offering accommodation and food services to the guests in the area.<br />
<br />
It was on March 17 in 2017 that the Iceland Monitor wrote that Kerlingarfjöll Mountains and geothermal area were being turned into a nature reserve. Although parts of the place already had protection, after made into reserve, all the whole 367 square kilometres are to be under the protection of the state of Iceland. Earlier, there had been thoughts of using the 140 degree Celsius hot springs as a geothermal power plant. It had already been popular of course with hiking and the tourists[
    KerlingarfjollRiver1.jpg
  • Kerlingarfjöll is a 1,477 m (4,846 ft)) tall mountain range in Iceland situated in the Highlands of Iceland near the Kjölur highland road. They are part of a large tuya volcano system of 100 km2 (39 sq mi). The volcanic origin of these mountains is evidenced by the numerous hot springs and rivulets in the area, as well as red volcanic rhyolite stone the mountains are composed of. Minerals that have emerged from the hot springs also color the ground yellow, red and green.<br />
<br />
The area was formerly known for its summer ski resort, but this was dismantled in 2000. From 2000 Kerlingarfjöll have been operated as a highland resort, offering accommodation and food services to the guests in the area.<br />
<br />
It was on March 17 in 2017 that the Iceland Monitor wrote that Kerlingarfjöll Mountains and geothermal area were being turned into a nature reserve. Although parts of the place already had protection, after made into reserve, all the whole 367 square kilometres are to be under the protection of the state of Iceland. Earlier, there had been thoughts of using the 140 degree Celsius hot springs as a geothermal power plant. It had already been popular of course with hiking and the tourists[
    Kerlingarfjoll1.jpg
  • The Giant's Causeway (known in Irish as Clochán an Aifir or Clochán na bhFómharach) is an area of about 40,000 interlocking basalt columns, the result of an ancient volcanic eruption. It is located in County Antrim on the northeast coast of Northern Ireland, about three miles (4.8 km) northeast of the town of Bushmills. It was declared a World Heritage Site by UNESCO in 1986, and a National Nature Reserve in 1987 by the Department of the Environment for Northern Ireland. In a 2005 poll of Radio Times readers, the Giant's Causeway was named as the fourth greatest natural wonder in the United Kingdom. The tops of the columns form stepping stones that lead from the cliff foot and disappear under the sea. Most of the columns are hexagonal, although there are also some with four, five, seven and eight sides. The tallest are about 12 metres (39 ft) high, and the solidified lava in the cliffs is 28 metres thick in places.
    GiantsCausewayEgg.jpg
  • The Giant's Causeway (known in Irish as Clochán an Aifir or Clochán na bhFómharach) is an area of about 40,000 interlocking basalt columns, the result of an ancient volcanic eruption. It is located in County Antrim on the northeast coast of Northern Ireland, about three miles (4.8 km) northeast of the town of Bushmills. It was declared a World Heritage Site by UNESCO in 1986, and a National Nature Reserve in 1987 by the Department of the Environment for Northern Ireland. In a 2005 poll of Radio Times readers, the Giant's Causeway was named as the fourth greatest natural wonder in the United Kingdom. The tops of the columns form stepping stones that lead from the cliff foot and disappear under the sea. Most of the columns are hexagonal, although there are also some with four, five, seven and eight sides. The tallest are about 12 metres (39 ft) high, and the solidified lava in the cliffs is 28 metres thick in places.
    GiantsCausewayPool.jpg
  • The Giant's Causeway (known in Irish as Clochán an Aifir or Clochán na bhFómharach) is an area of about 40,000 interlocking basalt columns, the result of an ancient volcanic eruption. It is located in County Antrim on the northeast coast of Northern Ireland, about three miles (4.8 km) northeast of the town of Bushmills. It was declared a World Heritage Site by UNESCO in 1986, and a National Nature Reserve in 1987 by the Department of the Environment for Northern Ireland. In a 2005 poll of Radio Times readers, the Giant's Causeway was named as the fourth greatest natural wonder in the United Kingdom. The tops of the columns form stepping stones that lead from the cliff foot and disappear under the sea. Most of the columns are hexagonal, although there are also some with four, five, seven and eight sides. The tallest are about 12 metres (39 ft) high, and the solidified lava in the cliffs is 28 metres thick in places.
    GiantsCausewayWetHexagons.jpg
  • Kerlingarfjöll is a 1,477 m (4,846 ft)) tall mountain range in Iceland situated in the Highlands of Iceland near the Kjölur highland road. They are part of a large tuya volcano system of 100 km2 (39 sq mi). The volcanic origin of these mountains is evidenced by the numerous hot springs and rivulets in the area, as well as red volcanic rhyolite stone the mountains are composed of. Minerals that have emerged from the hot springs also color the ground yellow, red and green.<br />
<br />
The area was formerly known for its summer ski resort, but this was dismantled in 2000. From 2000 Kerlingarfjöll have been operated as a highland resort, offering accommodation and food services to the guests in the area.<br />
<br />
It was on March 17 in 2017 that the Iceland Monitor wrote that Kerlingarfjöll Mountains and geothermal area were being turned into a nature reserve. Although parts of the place already had protection, after made into reserve, all the whole 367 square kilometres are to be under the protection of the state of Iceland. Earlier, there had been thoughts of using the 140 degree Celsius hot springs as a geothermal power plant. It had already been popular of course with hiking and the tourists[
    KerlingarfjollSteam5.jpg
  • Kerlingarfjöll is a 1,477 m (4,846 ft)) tall mountain range in Iceland situated in the Highlands of Iceland near the Kjölur highland road. They are part of a large tuya volcano system of 100 km2 (39 sq mi). The volcanic origin of these mountains is evidenced by the numerous hot springs and rivulets in the area, as well as red volcanic rhyolite stone the mountains are composed of. Minerals that have emerged from the hot springs also color the ground yellow, red and green.<br />
<br />
The area was formerly known for its summer ski resort, but this was dismantled in 2000. From 2000 Kerlingarfjöll have been operated as a highland resort, offering accommodation and food services to the guests in the area.<br />
<br />
It was on March 17 in 2017 that the Iceland Monitor wrote that Kerlingarfjöll Mountains and geothermal area were being turned into a nature reserve. Although parts of the place already had protection, after made into reserve, all the whole 367 square kilometres are to be under the protection of the state of Iceland. Earlier, there had been thoughts of using the 140 degree Celsius hot springs as a geothermal power plant. It had already been popular of course with hiking and the tourists[
    KerlingarfjollSteam2.jpg
  • Kerlingarfjöll is a 1,477 m (4,846 ft)) tall mountain range in Iceland situated in the Highlands of Iceland near the Kjölur highland road. They are part of a large tuya volcano system of 100 km2 (39 sq mi). The volcanic origin of these mountains is evidenced by the numerous hot springs and rivulets in the area, as well as red volcanic rhyolite stone the mountains are composed of. Minerals that have emerged from the hot springs also color the ground yellow, red and green.<br />
<br />
The area was formerly known for its summer ski resort, but this was dismantled in 2000. From 2000 Kerlingarfjöll have been operated as a highland resort, offering accommodation and food services to the guests in the area.<br />
<br />
It was on March 17 in 2017 that the Iceland Monitor wrote that Kerlingarfjöll Mountains and geothermal area were being turned into a nature reserve. Although parts of the place already had protection, after made into reserve, all the whole 367 square kilometres are to be under the protection of the state of Iceland. Earlier, there had been thoughts of using the 140 degree Celsius hot springs as a geothermal power plant. It had already been popular of course with hiking and the tourists.
    KerlingarfjollAurora3.jpg
  • Kerlingarfjöll is a 1,477 m (4,846 ft)) tall mountain range in Iceland situated in the Highlands of Iceland near the Kjölur highland road. They are part of a large tuya volcano system of 100 km2 (39 sq mi). The volcanic origin of these mountains is evidenced by the numerous hot springs and rivulets in the area, as well as red volcanic rhyolite stone the mountains are composed of. Minerals that have emerged from the hot springs also color the ground yellow, red and green.<br />
<br />
The area was formerly known for its summer ski resort, but this was dismantled in 2000. From 2000 Kerlingarfjöll have been operated as a highland resort, offering accommodation and food services to the guests in the area.<br />
<br />
It was on March 17 in 2017 that the Iceland Monitor wrote that Kerlingarfjöll Mountains and geothermal area were being turned into a nature reserve. Although parts of the place already had protection, after made into reserve, all the whole 367 square kilometres are to be under the protection of the state of Iceland. Earlier, there had been thoughts of using the 140 degree Celsius hot springs as a geothermal power plant. It had already been popular of course with hiking and the tourists[
    Kerlingarfjoll6.jpg
  • Kerlingarfjöll is a 1,477 m (4,846 ft)) tall mountain range in Iceland situated in the Highlands of Iceland near the Kjölur highland road. They are part of a large tuya volcano system of 100 km2 (39 sq mi). The volcanic origin of these mountains is evidenced by the numerous hot springs and rivulets in the area, as well as red volcanic rhyolite stone the mountains are composed of. Minerals that have emerged from the hot springs also color the ground yellow, red and green.<br />
<br />
The area was formerly known for its summer ski resort, but this was dismantled in 2000. From 2000 Kerlingarfjöll have been operated as a highland resort, offering accommodation and food services to the guests in the area.<br />
<br />
It was on March 17 in 2017 that the Iceland Monitor wrote that Kerlingarfjöll Mountains and geothermal area were being turned into a nature reserve. Although parts of the place already had protection, after made into reserve, all the whole 367 square kilometres are to be under the protection of the state of Iceland. Earlier, there had been thoughts of using the 140 degree Celsius hot springs as a geothermal power plant. It had already been popular of course with hiking and the tourists[
    Kerlingarfjoll3.jpg
  • Kerlingarfjöll is a 1,477 m (4,846 ft)) tall mountain range in Iceland situated in the Highlands of Iceland near the Kjölur highland road. They are part of a large tuya volcano system of 100 km2 (39 sq mi). The volcanic origin of these mountains is evidenced by the numerous hot springs and rivulets in the area, as well as red volcanic rhyolite stone the mountains are composed of. Minerals that have emerged from the hot springs also color the ground yellow, red and green.<br />
<br />
The area was formerly known for its summer ski resort, but this was dismantled in 2000. From 2000 Kerlingarfjöll have been operated as a highland resort, offering accommodation and food services to the guests in the area.<br />
<br />
It was on March 17 in 2017 that the Iceland Monitor wrote that Kerlingarfjöll Mountains and geothermal area were being turned into a nature reserve. Although parts of the place already had protection, after made into reserve, all the whole 367 square kilometres are to be under the protection of the state of Iceland. Earlier, there had been thoughts of using the 140 degree Celsius hot springs as a geothermal power plant. It had already been popular of course with hiking and the tourists[
    Kerlingarfjoll7.jpg
  • Kerlingarfjöll is a 1,477 m (4,846 ft)) tall mountain range in Iceland situated in the Highlands of Iceland near the Kjölur highland road. They are part of a large tuya volcano system of 100 km2 (39 sq mi). The volcanic origin of these mountains is evidenced by the numerous hot springs and rivulets in the area, as well as red volcanic rhyolite stone the mountains are composed of. Minerals that have emerged from the hot springs also color the ground yellow, red and green.<br />
<br />
The area was formerly known for its summer ski resort, but this was dismantled in 2000. From 2000 Kerlingarfjöll have been operated as a highland resort, offering accommodation and food services to the guests in the area.<br />
<br />
It was on March 17 in 2017 that the Iceland Monitor wrote that Kerlingarfjöll Mountains and geothermal area were being turned into a nature reserve. Although parts of the place already had protection, after made into reserve, all the whole 367 square kilometres are to be under the protection of the state of Iceland. Earlier, there had been thoughts of using the 140 degree Celsius hot springs as a geothermal power plant. It had already been popular of course with hiking and the tourists[
    KerlingarfjollPano1.jpg
  • The Giant's Causeway (known in Irish as Clochán an Aifir or Clochán na bhFómharach) is an area of about 40,000 interlocking basalt columns, the result of an ancient volcanic eruption. It is located in County Antrim on the northeast coast of Northern Ireland, about three miles (4.8 km) northeast of the town of Bushmills. It was declared a World Heritage Site by UNESCO in 1986, and a National Nature Reserve in 1987 by the Department of the Environment for Northern Ireland. In a 2005 poll of Radio Times readers, the Giant's Causeway was named as the fourth greatest natural wonder in the United Kingdom. The tops of the columns form stepping stones that lead from the cliff foot and disappear under the sea. Most of the columns are hexagonal, although there are also some with four, five, seven and eight sides. The tallest are about 12 metres (39 ft) high, and the solidified lava in the cliffs is 28 metres thick in places.
    GiantsCausewayMountain.jpg
  • The Giant's Causeway (known in Irish as Clochán an Aifir or Clochán na bhFómharach) is an area of about 40,000 interlocking basalt columns, the result of an ancient volcanic eruption. It is located in County Antrim on the northeast coast of Northern Ireland, about three miles (4.8 km) northeast of the town of Bushmills. It was declared a World Heritage Site by UNESCO in 1986, and a National Nature Reserve in 1987 by the Department of the Environment for Northern Ireland. In a 2005 poll of Radio Times readers, the Giant's Causeway was named as the fourth greatest natural wonder in the United Kingdom. The tops of the columns form stepping stones that lead from the cliff foot and disappear under the sea. Most of the columns are hexagonal, although there are also some with four, five, seven and eight sides. The tallest are about 12 metres (39 ft) high, and the solidified lava in the cliffs is 28 metres thick in places.
    GiantsCausewaySunset.jpg
  • The Giant's Causeway (known in Irish as Clochán an Aifir or Clochán na bhFómharach) is an area of about 40,000 interlocking basalt columns, the result of an ancient volcanic eruption. It is located in County Antrim on the northeast coast of Northern Ireland, about three miles (4.8 km) northeast of the town of Bushmills. It was declared a World Heritage Site by UNESCO in 1986, and a National Nature Reserve in 1987 by the Department of the Environment for Northern Ireland. In a 2005 poll of Radio Times readers, the Giant's Causeway was named as the fourth greatest natural wonder in the United Kingdom. The tops of the columns form stepping stones that lead from the cliff foot and disappear under the sea. Most of the columns are hexagonal, although there are also some with four, five, seven and eight sides. The tallest are about 12 metres (39 ft) high, and the solidified lava in the cliffs is 28 metres thick in places.
    GiantsCausewayCircle.jpg
  • The Giant's Causeway (known in Irish as Clochán an Aifir or Clochán na bhFómharach) is an area of about 40,000 interlocking basalt columns, the result of an ancient volcanic eruption. It is located in County Antrim on the northeast coast of Northern Ireland, about three miles (4.8 km) northeast of the town of Bushmills. It was declared a World Heritage Site by UNESCO in 1986, and a National Nature Reserve in 1987 by the Department of the Environment for Northern Ireland. In a 2005 poll of Radio Times readers, the Giant's Causeway was named as the fourth greatest natural wonder in the United Kingdom. The tops of the columns form stepping stones that lead from the cliff foot and disappear under the sea. Most of the columns are hexagonal, although there are also some with four, five, seven and eight sides. The tallest are about 12 metres (39 ft) high, and the solidified lava in the cliffs is 28 metres thick in places.
    GiantsCausewaySurf.jpg
  • The Giant's Causeway (known in Irish as Clochán an Aifir or Clochán na bhFómharach) is an area of about 40,000 interlocking basalt columns, the result of an ancient volcanic eruption. It is located in County Antrim on the northeast coast of Northern Ireland, about three miles (4.8 km) northeast of the town of Bushmills. It was declared a World Heritage Site by UNESCO in 1986, and a National Nature Reserve in 1987 by the Department of the Environment for Northern Ireland. In a 2005 poll of Radio Times readers, the Giant's Causeway was named as the fourth greatest natural wonder in the United Kingdom. The tops of the columns form stepping stones that lead from the cliff foot and disappear under the sea. Most of the columns are hexagonal, although there are also some with four, five, seven and eight sides. The tallest are about 12 metres (39 ft) high, and the solidified lava in the cliffs is 28 metres thick in places.
    GiantsCausewayBricks.jpg
  • The Giant's Causeway (known in Irish as Clochán an Aifir or Clochán na bhFómharach) is an area of about 40,000 interlocking basalt columns, the result of an ancient volcanic eruption. It is located in County Antrim on the northeast coast of Northern Ireland, about three miles (4.8 km) northeast of the town of Bushmills. It was declared a World Heritage Site by UNESCO in 1986, and a National Nature Reserve in 1987 by the Department of the Environment for Northern Ireland. In a 2005 poll of Radio Times readers, the Giant's Causeway was named as the fourth greatest natural wonder in the United Kingdom. The tops of the columns form stepping stones that lead from the cliff foot and disappear under the sea. Most of the columns are hexagonal, although there are also some with four, five, seven and eight sides. The tallest are about 12 metres (39 ft) high, and the solidified lava in the cliffs is 28 metres thick in places.
    GiantsCausewayStairs.jpg
  • The Giant's Causeway (known in Irish as Clochán an Aifir or Clochán na bhFómharach) is an area of about 40,000 interlocking basalt columns, the result of an ancient volcanic eruption. It is located in County Antrim on the northeast coast of Northern Ireland, about three miles (4.8 km) northeast of the town of Bushmills. It was declared a World Heritage Site by UNESCO in 1986, and a National Nature Reserve in 1987 by the Department of the Environment for Northern Ireland. In a 2005 poll of Radio Times readers, the Giant's Causeway was named as the fourth greatest natural wonder in the United Kingdom. The tops of the columns form stepping stones that lead from the cliff foot and disappear under the sea. Most of the columns are hexagonal, although there are also some with four, five, seven and eight sides. The tallest are about 12 metres (39 ft) high, and the solidified lava in the cliffs is 28 metres thick in places.
    GiantsCausewayShore.jpg
  • Kerlingarfjöll is a 1,477 m (4,846 ft)) tall mountain range in Iceland situated in the Highlands of Iceland near the Kjölur highland road. They are part of a large tuya volcano system of 100 km2 (39 sq mi). The volcanic origin of these mountains is evidenced by the numerous hot springs and rivulets in the area, as well as red volcanic rhyolite stone the mountains are composed of. Minerals that have emerged from the hot springs also color the ground yellow, red and green.<br />
<br />
The area was formerly known for its summer ski resort, but this was dismantled in 2000. From 2000 Kerlingarfjöll have been operated as a highland resort, offering accommodation and food services to the guests in the area.<br />
<br />
It was on March 17 in 2017 that the Iceland Monitor wrote that Kerlingarfjöll Mountains and geothermal area were being turned into a nature reserve. Although parts of the place already had protection, after made into reserve, all the whole 367 square kilometres are to be under the protection of the state of Iceland. Earlier, there had been thoughts of using the 140 degree Celsius hot springs as a geothermal power plant. It had already been popular of course with hiking and the tourists[
    KerlingarfjollSteam3.jpg
  • Kerlingarfjöll is a 1,477 m (4,846 ft)) tall mountain range in Iceland situated in the Highlands of Iceland near the Kjölur highland road. They are part of a large tuya volcano system of 100 km2 (39 sq mi). The volcanic origin of these mountains is evidenced by the numerous hot springs and rivulets in the area, as well as red volcanic rhyolite stone the mountains are composed of. Minerals that have emerged from the hot springs also color the ground yellow, red and green.<br />
<br />
The area was formerly known for its summer ski resort, but this was dismantled in 2000. From 2000 Kerlingarfjöll have been operated as a highland resort, offering accommodation and food services to the guests in the area.<br />
<br />
It was on March 17 in 2017 that the Iceland Monitor wrote that Kerlingarfjöll Mountains and geothermal area were being turned into a nature reserve. Although parts of the place already had protection, after made into reserve, all the whole 367 square kilometres are to be under the protection of the state of Iceland. Earlier, there had been thoughts of using the 140 degree Celsius hot springs as a geothermal power plant. It had already been popular of course with hiking and the tourists[
    KerlingarfjollSteam1.jpg
  • Kerlingarfjöll is a 1,477 m (4,846 ft)) tall mountain range in Iceland situated in the Highlands of Iceland near the Kjölur highland road. They are part of a large tuya volcano system of 100 km2 (39 sq mi). The volcanic origin of these mountains is evidenced by the numerous hot springs and rivulets in the area, as well as red volcanic rhyolite stone the mountains are composed of. Minerals that have emerged from the hot springs also color the ground yellow, red and green.<br />
<br />
The area was formerly known for its summer ski resort, but this was dismantled in 2000. From 2000 Kerlingarfjöll have been operated as a highland resort, offering accommodation and food services to the guests in the area.<br />
<br />
It was on March 17 in 2017 that the Iceland Monitor wrote that Kerlingarfjöll Mountains and geothermal area were being turned into a nature reserve. Although parts of the place already had protection, after made into reserve, all the whole 367 square kilometres are to be under the protection of the state of Iceland. Earlier, there had been thoughts of using the 140 degree Celsius hot springs as a geothermal power plant. It had already been popular of course with hiking and the tourists[
    _A1A7965.jpg
  • Kerlingarfjöll is a 1,477 m (4,846 ft)) tall mountain range in Iceland situated in the Highlands of Iceland near the Kjölur highland road. They are part of a large tuya volcano system of 100 km2 (39 sq mi). The volcanic origin of these mountains is evidenced by the numerous hot springs and rivulets in the area, as well as red volcanic rhyolite stone the mountains are composed of. Minerals that have emerged from the hot springs also color the ground yellow, red and green.<br />
<br />
The area was formerly known for its summer ski resort, but this was dismantled in 2000. From 2000 Kerlingarfjöll have been operated as a highland resort, offering accommodation and food services to the guests in the area.<br />
<br />
It was on March 17 in 2017 that the Iceland Monitor wrote that Kerlingarfjöll Mountains and geothermal area were being turned into a nature reserve. Although parts of the place already had protection, after made into reserve, all the whole 367 square kilometres are to be under the protection of the state of Iceland. Earlier, there had been thoughts of using the 140 degree Celsius hot springs as a geothermal power plant. It had already been popular of course with hiking and the tourists[
    Kerlingarfjoll8.jpg
  • Kerlingarfjöll is a 1,477 m (4,846 ft)) tall mountain range in Iceland situated in the Highlands of Iceland near the Kjölur highland road. They are part of a large tuya volcano system of 100 km2 (39 sq mi). The volcanic origin of these mountains is evidenced by the numerous hot springs and rivulets in the area, as well as red volcanic rhyolite stone the mountains are composed of. Minerals that have emerged from the hot springs also color the ground yellow, red and green.<br />
<br />
The area was formerly known for its summer ski resort, but this was dismantled in 2000. From 2000 Kerlingarfjöll have been operated as a highland resort, offering accommodation and food services to the guests in the area.<br />
<br />
It was on March 17 in 2017 that the Iceland Monitor wrote that Kerlingarfjöll Mountains and geothermal area were being turned into a nature reserve. Although parts of the place already had protection, after made into reserve, all the whole 367 square kilometres are to be under the protection of the state of Iceland. Earlier, there had been thoughts of using the 140 degree Celsius hot springs as a geothermal power plant. It had already been popular of course with hiking and the tourists[
    KerlingarfjollPeak1.jpg
  • Kerlingarfjöll is a 1,477 m (4,846 ft)) tall mountain range in Iceland situated in the Highlands of Iceland near the Kjölur highland road. They are part of a large tuya volcano system of 100 km2 (39 sq mi). The volcanic origin of these mountains is evidenced by the numerous hot springs and rivulets in the area, as well as red volcanic rhyolite stone the mountains are composed of. Minerals that have emerged from the hot springs also color the ground yellow, red and green.<br />
<br />
The area was formerly known for its summer ski resort, but this was dismantled in 2000. From 2000 Kerlingarfjöll have been operated as a highland resort, offering accommodation and food services to the guests in the area.<br />
<br />
It was on March 17 in 2017 that the Iceland Monitor wrote that Kerlingarfjöll Mountains and geothermal area were being turned into a nature reserve. Although parts of the place already had protection, after made into reserve, all the whole 367 square kilometres are to be under the protection of the state of Iceland. Earlier, there had been thoughts of using the 140 degree Celsius hot springs as a geothermal power plant. It had already been popular of course with hiking and the tourists[
    KerlingarfjollRange2.jpg
  • Kerlingarfjöll is a 1,477 m (4,846 ft)) tall mountain range in Iceland situated in the Highlands of Iceland near the Kjölur highland road. They are part of a large tuya volcano system of 100 km2 (39 sq mi). The volcanic origin of these mountains is evidenced by the numerous hot springs and rivulets in the area, as well as red volcanic rhyolite stone the mountains are composed of. Minerals that have emerged from the hot springs also color the ground yellow, red and green.<br />
<br />
The area was formerly known for its summer ski resort, but this was dismantled in 2000. From 2000 Kerlingarfjöll have been operated as a highland resort, offering accommodation and food services to the guests in the area.<br />
<br />
It was on March 17 in 2017 that the Iceland Monitor wrote that Kerlingarfjöll Mountains and geothermal area were being turned into a nature reserve. Although parts of the place already had protection, after made into reserve, all the whole 367 square kilometres are to be under the protection of the state of Iceland. Earlier, there had been thoughts of using the 140 degree Celsius hot springs as a geothermal power plant. It had already been popular of course with hiking and the tourists[
    KerlingarfjollRange1.jpg
  • The Giant's Causeway (known in Irish as Clochán an Aifir or Clochán na bhFómharach) is an area of about 40,000 interlocking basalt columns, the result of an ancient volcanic eruption. It is located in County Antrim on the northeast coast of Northern Ireland, about three miles (4.8 km) northeast of the town of Bushmills. It was declared a World Heritage Site by UNESCO in 1986, and a National Nature Reserve in 1987 by the Department of the Environment for Northern Ireland. In a 2005 poll of Radio Times readers, the Giant's Causeway was named as the fourth greatest natural wonder in the United Kingdom. The tops of the columns form stepping stones that lead from the cliff foot and disappear under the sea. Most of the columns are hexagonal, although there are also some with four, five, seven and eight sides. The tallest are about 12 metres (39 ft) high, and the solidified lava in the cliffs is 28 metres thick in places.
    GiantsCausewayHexagons3.jpg
  • The Giant's Causeway (known in Irish as Clochán an Aifir or Clochán na bhFómharach) is an area of about 40,000 interlocking basalt columns, the result of an ancient volcanic eruption. It is located in County Antrim on the northeast coast of Northern Ireland, about three miles (4.8 km) northeast of the town of Bushmills. It was declared a World Heritage Site by UNESCO in 1986, and a National Nature Reserve in 1987 by the Department of the Environment for Northern Ireland. In a 2005 poll of Radio Times readers, the Giant's Causeway was named as the fourth greatest natural wonder in the United Kingdom. The tops of the columns form stepping stones that lead from the cliff foot and disappear under the sea. Most of the columns are hexagonal, although there are also some with four, five, seven and eight sides. The tallest are about 12 metres (39 ft) high, and the solidified lava in the cliffs is 28 metres thick in places.
    GiantsCausewayCove1.jpg
  • The Giant's Causeway (known in Irish as Clochán an Aifir or Clochán na bhFómharach) is an area of about 40,000 interlocking basalt columns, the result of an ancient volcanic eruption. It is located in County Antrim on the northeast coast of Northern Ireland, about three miles (4.8 km) northeast of the town of Bushmills. It was declared a World Heritage Site by UNESCO in 1986, and a National Nature Reserve in 1987 by the Department of the Environment for Northern Ireland. In a 2005 poll of Radio Times readers, the Giant's Causeway was named as the fourth greatest natural wonder in the United Kingdom. The tops of the columns form stepping stones that lead from the cliff foot and disappear under the sea. Most of the columns are hexagonal, although there are also some with four, five, seven and eight sides. The tallest are about 12 metres (39 ft) high, and the solidified lava in the cliffs is 28 metres thick in places.
    GiantsCausewayCoveWaves1.jpg
  • The Giant's Causeway (known in Irish as Clochán an Aifir or Clochán na bhFómharach) is an area of about 40,000 interlocking basalt columns, the result of an ancient volcanic eruption. It is located in County Antrim on the northeast coast of Northern Ireland, about three miles (4.8 km) northeast of the town of Bushmills. It was declared a World Heritage Site by UNESCO in 1986, and a National Nature Reserve in 1987 by the Department of the Environment for Northern Ireland. In a 2005 poll of Radio Times readers, the Giant's Causeway was named as the fourth greatest natural wonder in the United Kingdom. The tops of the columns form stepping stones that lead from the cliff foot and disappear under the sea. Most of the columns are hexagonal, although there are also some with four, five, seven and eight sides. The tallest are about 12 metres (39 ft) high, and the solidified lava in the cliffs is 28 metres thick in places.
    GiantsCausewayHexagons1.jpg
  • The Giant's Causeway (known in Irish as Clochán an Aifir or Clochán na bhFómharach) is an area of about 40,000 interlocking basalt columns, the result of an ancient volcanic eruption. It is located in County Antrim on the northeast coast of Northern Ireland, about three miles (4.8 km) northeast of the town of Bushmills. It was declared a World Heritage Site by UNESCO in 1986, and a National Nature Reserve in 1987 by the Department of the Environment for Northern Ireland. In a 2005 poll of Radio Times readers, the Giant's Causeway was named as the fourth greatest natural wonder in the United Kingdom. The tops of the columns form stepping stones that lead from the cliff foot and disappear under the sea. Most of the columns are hexagonal, although there are also some with four, five, seven and eight sides. The tallest are about 12 metres (39 ft) high, and the solidified lava in the cliffs is 28 metres thick in places.
    GiantsCausewayHexagons2.jpg
  • The Giant's Causeway (known in Irish as Clochán an Aifir or Clochán na bhFómharach) is an area of about 40,000 interlocking basalt columns, the result of an ancient volcanic eruption. It is located in County Antrim on the northeast coast of Northern Ireland, about three miles (4.8 km) northeast of the town of Bushmills. It was declared a World Heritage Site by UNESCO in 1986, and a National Nature Reserve in 1987 by the Department of the Environment for Northern Ireland. In a 2005 poll of Radio Times readers, the Giant's Causeway was named as the fourth greatest natural wonder in the United Kingdom. The tops of the columns form stepping stones that lead from the cliff foot and disappear under the sea. Most of the columns are hexagonal, although there are also some with four, five, seven and eight sides. The tallest are about 12 metres (39 ft) high, and the solidified lava in the cliffs is 28 metres thick in places.
    GiantsCausewayHexagons4.jpg
  • The Giant's Causeway (known in Irish as Clochán an Aifir or Clochán na bhFómharach) is an area of about 40,000 interlocking basalt columns, the result of an ancient volcanic eruption. It is located in County Antrim on the northeast coast of Northern Ireland, about three miles (4.8 km) northeast of the town of Bushmills. It was declared a World Heritage Site by UNESCO in 1986, and a National Nature Reserve in 1987 by the Department of the Environment for Northern Ireland. In a 2005 poll of Radio Times readers, the Giant's Causeway was named as the fourth greatest natural wonder in the United Kingdom. The tops of the columns form stepping stones that lead from the cliff foot and disappear under the sea. Most of the columns are hexagonal, although there are also some with four, five, seven and eight sides. The tallest are about 12 metres (39 ft) high, and the solidified lava in the cliffs is 28 metres thick in places.
    GiantsCausewayPeak2.jpg
  • The Giant's Causeway (known in Irish as Clochán an Aifir or Clochán na bhFómharach) is an area of about 40,000 interlocking basalt columns, the result of an ancient volcanic eruption. It is located in County Antrim on the northeast coast of Northern Ireland, about three miles (4.8 km) northeast of the town of Bushmills. It was declared a World Heritage Site by UNESCO in 1986, and a National Nature Reserve in 1987 by the Department of the Environment for Northern Ireland. In a 2005 poll of Radio Times readers, the Giant's Causeway was named as the fourth greatest natural wonder in the United Kingdom. The tops of the columns form stepping stones that lead from the cliff foot and disappear under the sea. Most of the columns are hexagonal, although there are also some with four, five, seven and eight sides. The tallest are about 12 metres (39 ft) high, and the solidified lava in the cliffs is 28 metres thick in places.
    GiantsCausewayCove.jpg
  • The Giant's Causeway (known in Irish as Clochán an Aifir or Clochán na bhFómharach) is an area of about 40,000 interlocking basalt columns, the result of an ancient volcanic eruption. It is located in County Antrim on the northeast coast of Northern Ireland, about three miles (4.8 km) northeast of the town of Bushmills. It was declared a World Heritage Site by UNESCO in 1986, and a National Nature Reserve in 1987 by the Department of the Environment for Northern Ireland. In a 2005 poll of Radio Times readers, the Giant's Causeway was named as the fourth greatest natural wonder in the United Kingdom. The tops of the columns form stepping stones that lead from the cliff foot and disappear under the sea. Most of the columns are hexagonal, although there are also some with four, five, seven and eight sides. The tallest are about 12 metres (39 ft) high, and the solidified lava in the cliffs is 28 metres thick in places.
    GiantsCausewayPeak1.jpg
  • The Giant's Causeway (known in Irish as Clochán an Aifir or Clochán na bhFómharach) is an area of about 40,000 interlocking basalt columns, the result of an ancient volcanic eruption. It is located in County Antrim on the northeast coast of Northern Ireland, about three miles (4.8 km) northeast of the town of Bushmills. It was declared a World Heritage Site by UNESCO in 1986, and a National Nature Reserve in 1987 by the Department of the Environment for Northern Ireland. In a 2005 poll of Radio Times readers, the Giant's Causeway was named as the fourth greatest natural wonder in the United Kingdom. The tops of the columns form stepping stones that lead from the cliff foot and disappear under the sea. Most of the columns are hexagonal, although there are also some with four, five, seven and eight sides. The tallest are about 12 metres (39 ft) high, and the solidified lava in the cliffs is 28 metres thick in places.
    GiantsCausewayRockway1.jpg
  • Kerlingarfjöll is a 1,477 m (4,846 ft)) tall mountain range in Iceland situated in the Highlands of Iceland near the Kjölur highland road. They are part of a large tuya volcano system of 100 km2 (39 sq mi). The volcanic origin of these mountains is evidenced by the numerous hot springs and rivulets in the area, as well as red volcanic rhyolite stone the mountains are composed of. Minerals that have emerged from the hot springs also color the ground yellow, red and green.<br />
<br />
The area was formerly known for its summer ski resort, but this was dismantled in 2000. From 2000 Kerlingarfjöll have been operated as a highland resort, offering accommodation and food services to the guests in the area.<br />
<br />
It was on March 17 in 2017 that the Iceland Monitor wrote that Kerlingarfjöll Mountains and geothermal area were being turned into a nature reserve. Although parts of the place already had protection, after made into reserve, all the whole 367 square kilometres are to be under the protection of the state of Iceland. Earlier, there had been thoughts of using the 140 degree Celsius hot springs as a geothermal power plant. It had already been popular of course with hiking and the tourists[
    KerlingarfjollSteam4.jpg
  • Kerlingarfjöll is a 1,477 m (4,846 ft)) tall mountain range in Iceland situated in the Highlands of Iceland near the Kjölur highland road. They are part of a large tuya volcano system of 100 km2 (39 sq mi). The volcanic origin of these mountains is evidenced by the numerous hot springs and rivulets in the area, as well as red volcanic rhyolite stone the mountains are composed of. Minerals that have emerged from the hot springs also color the ground yellow, red and green.<br />
<br />
The area was formerly known for its summer ski resort, but this was dismantled in 2000. From 2000 Kerlingarfjöll have been operated as a highland resort, offering accommodation and food services to the guests in the area.<br />
<br />
It was on March 17 in 2017 that the Iceland Monitor wrote that Kerlingarfjöll Mountains and geothermal area were being turned into a nature reserve. Although parts of the place already had protection, after made into reserve, all the whole 367 square kilometres are to be under the protection of the state of Iceland. Earlier, there had been thoughts of using the 140 degree Celsius hot springs as a geothermal power plant. It had already been popular of course with hiking and the tourists[
    Kerlingarfjoll4.jpg
  • Kerlingarfjöll is a 1,477 m (4,846 ft)) tall mountain range in Iceland situated in the Highlands of Iceland near the Kjölur highland road. They are part of a large tuya volcano system of 100 km2 (39 sq mi). The volcanic origin of these mountains is evidenced by the numerous hot springs and rivulets in the area, as well as red volcanic rhyolite stone the mountains are composed of. Minerals that have emerged from the hot springs also color the ground yellow, red and green.<br />
<br />
The area was formerly known for its summer ski resort, but this was dismantled in 2000. From 2000 Kerlingarfjöll have been operated as a highland resort, offering accommodation and food services to the guests in the area.<br />
<br />
It was on March 17 in 2017 that the Iceland Monitor wrote that Kerlingarfjöll Mountains and geothermal area were being turned into a nature reserve. Although parts of the place already had protection, after made into reserve, all the whole 367 square kilometres are to be under the protection of the state of Iceland. Earlier, there had been thoughts of using the 140 degree Celsius hot springs as a geothermal power plant. It had already been popular of course with hiking and the tourists[
    _A1A7917.jpg
  • Kerlingarfjöll is a 1,477 m (4,846 ft)) tall mountain range in Iceland situated in the Highlands of Iceland near the Kjölur highland road. They are part of a large tuya volcano system of 100 km2 (39 sq mi). The volcanic origin of these mountains is evidenced by the numerous hot springs and rivulets in the area, as well as red volcanic rhyolite stone the mountains are composed of. Minerals that have emerged from the hot springs also color the ground yellow, red and green.<br />
<br />
The area was formerly known for its summer ski resort, but this was dismantled in 2000. From 2000 Kerlingarfjöll have been operated as a highland resort, offering accommodation and food services to the guests in the area.<br />
<br />
It was on March 17 in 2017 that the Iceland Monitor wrote that Kerlingarfjöll Mountains and geothermal area were being turned into a nature reserve. Although parts of the place already had protection, after made into reserve, all the whole 367 square kilometres are to be under the protection of the state of Iceland. Earlier, there had been thoughts of using the 140 degree Celsius hot springs as a geothermal power plant. It had already been popular of course with hiking and the tourists[
    _A1A7916.jpg
  • Natural Bridge in Yoho National Park, British Columbia, Canada. <br />
<br />
Yoho National Park is located in the Canadian Rocky Mountains along the western slope of the Continental Divide of the Americas in southeastern British Columbia. Yoho NP is bordered by Kootenay National Park on the southern side and Banff National Park on the eastern side in Alberta. The name Yoho comes from the Cree word for awe and wonder.<br />
<br />
Yoho covers 1,313 km2 (507 mi2) and it is the smallest of the four contiguous national parks. Yoho, together with Jasper, Kootenay and Banff National Parks, along with three British Columbia provincial parks—Hamber Provincial Park, Mount Assiniboine Provincial Park, and Mount Robson Provincial Park—form the Canadian Rocky Mountain Parks World Heritage Site. The park's administrative and visitor centre are located in the town of Field, British Columbia, beside the Trans-Canada Highway.
    NaturalBridge3.jpg
  • Natural Bridge in Yoho National Park, British Columbia, Canada. <br />
<br />
Yoho National Park is located in the Canadian Rocky Mountains along the western slope of the Continental Divide of the Americas in southeastern British Columbia. Yoho NP is bordered by Kootenay National Park on the southern side and Banff National Park on the eastern side in Alberta. The name Yoho comes from the Cree word for awe and wonder.<br />
<br />
Yoho covers 1,313 km2 (507 mi2) and it is the smallest of the four contiguous national parks. Yoho, together with Jasper, Kootenay and Banff National Parks, along with three British Columbia provincial parks—Hamber Provincial Park, Mount Assiniboine Provincial Park, and Mount Robson Provincial Park—form the Canadian Rocky Mountain Parks World Heritage Site. The park's administrative and visitor centre are located in the town of Field, British Columbia, beside the Trans-Canada Highway.
    NaturalBridge2.jpg
  • Natural Bridge in Yoho National Park, British Columbia, Canada. <br />
<br />
Yoho National Park is located in the Canadian Rocky Mountains along the western slope of the Continental Divide of the Americas in southeastern British Columbia. Yoho NP is bordered by Kootenay National Park on the southern side and Banff National Park on the eastern side in Alberta. The name Yoho comes from the Cree word for awe and wonder.<br />
<br />
Yoho covers 1,313 km2 (507 mi2) and it is the smallest of the four contiguous national parks. Yoho, together with Jasper, Kootenay and Banff National Parks, along with three British Columbia provincial parks—Hamber Provincial Park, Mount Assiniboine Provincial Park, and Mount Robson Provincial Park—form the Canadian Rocky Mountain Parks World Heritage Site. The park's administrative and visitor centre are located in the town of Field, British Columbia, beside the Trans-Canada Highway.
    NaturalBridge1.jpg
  • The Devil's Garden of the Grand Staircase-Escalante National Monument (GSENM) in south central Utah, the United States, is a protected area featuring hoodoos, natural arches and other sandstone formations. The United States Geological Survey (USGS) designated the name Devils Garden. The area is also known as the Devils Garden Outstanding Natural Area within the National Landscape Conservation System.<br />
<br />
The formations in the Devils Garden were created, and continue to be shaped, by various weathering and erosional processes. These natural processes have been shaping sandstone layers formed more than 166 million years ago during the Jurassic period's Middle epoch.
    _Y6A0497-HDR.jpg
  • The Devil's Garden of the Grand Staircase-Escalante National Monument (GSENM) in south central Utah, the United States, is a protected area featuring hoodoos, natural arches and other sandstone formations. The United States Geological Survey (USGS) designated the name Devils Garden. The area is also known as the Devils Garden Outstanding Natural Area within the National Landscape Conservation System.<br />
<br />
The formations in the Devils Garden were created, and continue to be shaped, by various weathering and erosional processes. These natural processes have been shaping sandstone layers formed more than 166 million years ago during the Jurassic period's Middle epoch.
    _Y6A0520.jpg
  • The Devil's Garden of the Grand Staircase-Escalante National Monument (GSENM) in south central Utah, the United States, is a protected area featuring hoodoos, natural arches and other sandstone formations. The United States Geological Survey (USGS) designated the name Devils Garden. The area is also known as the Devils Garden Outstanding Natural Area within the National Landscape Conservation System.<br />
<br />
The formations in the Devils Garden were created, and continue to be shaped, by various weathering and erosional processes. These natural processes have been shaping sandstone layers formed more than 166 million years ago during the Jurassic period's Middle epoch.
    _Y6A0489.jpg
  • The Devil's Garden of the Grand Staircase-Escalante National Monument (GSENM) in south central Utah, the United States, is a protected area featuring hoodoos, natural arches and other sandstone formations. The United States Geological Survey (USGS) designated the name Devils Garden. The area is also known as the Devils Garden Outstanding Natural Area within the National Landscape Conservation System.<br />
<br />
The formations in the Devils Garden were created, and continue to be shaped, by various weathering and erosional processes. These natural processes have been shaping sandstone layers formed more than 166 million years ago during the Jurassic period's Middle epoch.
    _Y6A0487.jpg
  • The Devil's Garden of the Grand Staircase-Escalante National Monument (GSENM) in south central Utah, the United States, is a protected area featuring hoodoos, natural arches and other sandstone formations. The United States Geological Survey (USGS) designated the name Devils Garden. The area is also known as the Devils Garden Outstanding Natural Area within the National Landscape Conservation System.<br />
<br />
The formations in the Devils Garden were created, and continue to be shaped, by various weathering and erosional processes. These natural processes have been shaping sandstone layers formed more than 166 million years ago during the Jurassic period's Middle epoch.
    MetateArch1.jpg
  • The Devil's Garden of the Grand Staircase-Escalante National Monument (GSENM) in south central Utah, the United States, is a protected area featuring hoodoos, natural arches and other sandstone formations. The United States Geological Survey (USGS) designated the name Devils Garden. The area is also known as the Devils Garden Outstanding Natural Area within the National Landscape Conservation System.<br />
<br />
The formations in the Devils Garden were created, and continue to be shaped, by various weathering and erosional processes. These natural processes have been shaping sandstone layers formed more than 166 million years ago during the Jurassic period's Middle epoch.
    _Y6A0494-HDR.jpg
  • The Devil's Garden of the Grand Staircase-Escalante National Monument (GSENM) in south central Utah, the United States, is a protected area featuring hoodoos, natural arches and other sandstone formations. The United States Geological Survey (USGS) designated the name Devils Garden. The area is also known as the Devils Garden Outstanding Natural Area within the National Landscape Conservation System.<br />
<br />
The formations in the Devils Garden were created, and continue to be shaped, by various weathering and erosional processes. These natural processes have been shaping sandstone layers formed more than 166 million years ago during the Jurassic period's Middle epoch.
    _Y6A0525.jpg
  • Zion National Park is a United States National Park located in southwestern Utah. A prominent feature of the 229-square-mile park is Zion Canyon, which is 15 miles long and up to half a mile deep, cut through the reddish and tan-colored Navajo Sandstone by the North Fork of the Virgin River. The lowest elevation is 3,666 ft  at Coalpits Wash and the highest elevation is 8,726 ft at Horse Ranch Mountain. Located at the junction of the Colorado Plateau, Great Basin, and Mojave Desert regions, the park's unique geography and variety of life zones allow for unusual plant and animal diversity. Numerous plant species as well as 289 species of birds, 75 mammals (including 19 species of bat), and 32 reptiles inhabit the park's four life zones: desert, riparian, woodland, and coniferous forest. Zion National Park includes mountains, canyons, buttes, mesas, monoliths, rivers, slot canyons, and natural arches.
    JacksTreeBent1.jpg
  • Multnomah Falls in Columbia River Gorge, Oregon.<br />
---<br />
Multnomah Falls is a waterfall located on Multnomah Creek in the Columbia River Gorge, east of Troutdale, between Corbett and Dodson, Oregon, United States. The waterfall is accessible from the Historic Columbia River Highway and Interstate 84. Spanning two tiers on basalt cliffs, it is the tallest waterfall in the state of Oregon at 620 ft in height.<br />
<br />
The land surrounding the falls was developed by Simon Benson in the early-twentieth century, with a pathway, viewing bridge, and adjacent lodge being constructed in 1925. The Multnomah Falls Lodge and the surrounding footpaths at the falls were added to the National Register of Historic Places in 1981. Contemporarily, the state of Oregon maintains a switchback trail that ascends to a talus slope 100 feet above the falls, and descends to an observation deck that overlooks the falls' edge. The falls attract over two million visitors each year, making it the most-visited natural recreation site in the U.S. Pacific Northwest.
    UpperMultnomah1.jpg
  • The Summer Palace (Chinese: 頤和園), is a vast ensemble of lakes, gardens and palaces in Beijing. It was an imperial garden in the Qing Dynasty. Mainly dominated by Longevity Hill (万寿山; 萬壽山) and Kunming Lake, it covers an expanse of 2.9 square kilometres, three-quarters of which is water.<br />
<br />
Longevity Hill is about 60 m high and has many buildings positioned in sequence. The front hill is rich with splendid halls and pavilions, while the back hill, in sharp contrast, is quiet with natural beauty. The central Kunming Lake, covering 2.2 square kilometres, was entirely man-made and the excavated soil was used to build Longevity Hill.<br />
<br />
In December 1998, UNESCO included the Summer Palace on its World Heritage List. It declared the Summer Palace "a masterpiece of Chinese landscape garden design. The natural landscape of hills and open water is combined with artificial features such as pavilions, halls, palaces, temples and bridges to form a harmonious ensemble of outstanding aesthetic value".
    SummerPalaceCeiling3.jpg
  • The Summer Palace (Chinese: 頤和園), is a vast ensemble of lakes, gardens and palaces in Beijing. It was an imperial garden in the Qing Dynasty. Mainly dominated by Longevity Hill (万寿山; 萬壽山) and Kunming Lake, it covers an expanse of 2.9 square kilometres, three-quarters of which is water.<br />
<br />
Longevity Hill is about 60 m high and has many buildings positioned in sequence. The front hill is rich with splendid halls and pavilions, while the back hill, in sharp contrast, is quiet with natural beauty. The central Kunming Lake, covering 2.2 square kilometres, was entirely man-made and the excavated soil was used to build Longevity Hill.<br />
<br />
In December 1998, UNESCO included the Summer Palace on its World Heritage List. It declared the Summer Palace "a masterpiece of Chinese landscape garden design. The natural landscape of hills and open water is combined with artificial features such as pavilions, halls, palaces, temples and bridges to form a harmonious ensemble of outstanding aesthetic value".
    SummerPalaceBridge1.jpg
  • The Summer Palace (Chinese: 頤和園), is a vast ensemble of lakes, gardens and palaces in Beijing. It was an imperial garden in the Qing Dynasty. Mainly dominated by Longevity Hill (万寿山; 萬壽山) and Kunming Lake, it covers an expanse of 2.9 square kilometres, three-quarters of which is water.<br />
<br />
Longevity Hill is about 60 m high and has many buildings positioned in sequence. The front hill is rich with splendid halls and pavilions, while the back hill, in sharp contrast, is quiet with natural beauty. The central Kunming Lake, covering 2.2 square kilometres, was entirely man-made and the excavated soil was used to build Longevity Hill.<br />
<br />
In December 1998, UNESCO included the Summer Palace on its World Heritage List. It declared the Summer Palace "a masterpiece of Chinese landscape garden design. The natural landscape of hills and open water is combined with artificial features such as pavilions, halls, palaces, temples and bridges to form a harmonious ensemble of outstanding aesthetic value".
    HallOfBenevolentLongevity1.jpg
  • Mount St. Helens National Volcanic Monument is a U.S. National Monument that includes the area around Mount St. Helens in Washington. It was established on August 27, 1982 by U.S. President Ronald Reagan following the 1980 eruption of Mount St. Helens. The 110,000 acre National Volcanic Monument was set-aside for research, recreation, and education. Inside the Monument, the environment is left to respond naturally to the disturbance.
    MountSaintHelens3.jpg
  • The Summer Palace (Chinese: 頤和園), is a vast ensemble of lakes, gardens and palaces in Beijing. It was an imperial garden in the Qing Dynasty. Mainly dominated by Longevity Hill (万寿山; 萬壽山) and Kunming Lake, it covers an expanse of 2.9 square kilometres, three-quarters of which is water.<br />
<br />
Longevity Hill is about 60 m high and has many buildings positioned in sequence. The front hill is rich with splendid halls and pavilions, while the back hill, in sharp contrast, is quiet with natural beauty. The central Kunming Lake, covering 2.2 square kilometres, was entirely man-made and the excavated soil was used to build Longevity Hill.<br />
<br />
In December 1998, UNESCO included the Summer Palace on its World Heritage List. It declared the Summer Palace "a masterpiece of Chinese landscape garden design. The natural landscape of hills and open water is combined with artificial features such as pavilions, halls, palaces, temples and bridges to form a harmonious ensemble of outstanding aesthetic value".
    CircularGates1.jpg
  • The Summer Palace (Chinese: 頤和園), is a vast ensemble of lakes, gardens and palaces in Beijing. It was an imperial garden in the Qing Dynasty. Mainly dominated by Longevity Hill (万寿山; 萬壽山) and Kunming Lake, it covers an expanse of 2.9 square kilometres, three-quarters of which is water.<br />
<br />
Longevity Hill is about 60 m high and has many buildings positioned in sequence. The front hill is rich with splendid halls and pavilions, while the back hill, in sharp contrast, is quiet with natural beauty. The central Kunming Lake, covering 2.2 square kilometres, was entirely man-made and the excavated soil was used to build Longevity Hill.<br />
<br />
In December 1998, UNESCO included the Summer Palace on its World Heritage List. It declared the Summer Palace "a masterpiece of Chinese landscape garden design. The natural landscape of hills and open water is combined with artificial features such as pavilions, halls, palaces, temples and bridges to form a harmonious ensemble of outstanding aesthetic value".
    TowerBuddhistIncence3-Edit.jpg
  • Mount St. Helens National Volcanic Monument is a U.S. National Monument that includes the area around Mount St. Helens in Washington. It was established on August 27, 1982 by U.S. President Ronald Reagan following the 1980 eruption of Mount St. Helens. The 110,000 acre National Volcanic Monument was set-aside for research, recreation, and education. Inside the Monument, the environment is left to respond naturally to the disturbance.
    MountSaintHelens6.jpg
  • The Summer Palace (Chinese: 頤和園), is a vast ensemble of lakes, gardens and palaces in Beijing. It was an imperial garden in the Qing Dynasty. Mainly dominated by Longevity Hill (万寿山; 萬壽山) and Kunming Lake, it covers an expanse of 2.9 square kilometres, three-quarters of which is water.<br />
<br />
Longevity Hill is about 60 m high and has many buildings positioned in sequence. The front hill is rich with splendid halls and pavilions, while the back hill, in sharp contrast, is quiet with natural beauty. The central Kunming Lake, covering 2.2 square kilometres, was entirely man-made and the excavated soil was used to build Longevity Hill.<br />
<br />
In December 1998, UNESCO included the Summer Palace on its World Heritage List. It declared the Summer Palace "a masterpiece of Chinese landscape garden design. The natural landscape of hills and open water is combined with artificial features such as pavilions, halls, palaces, temples and bridges to form a harmonious ensemble of outstanding aesthetic value".
    _Y6A1093-HDR-Edit.jpg
  • The Summer Palace (Chinese: 頤和園), is a vast ensemble of lakes, gardens and palaces in Beijing. It was an imperial garden in the Qing Dynasty. Mainly dominated by Longevity Hill (万寿山; 萬壽山) and Kunming Lake, it covers an expanse of 2.9 square kilometres, three-quarters of which is water.<br />
<br />
Longevity Hill is about 60 m high and has many buildings positioned in sequence. The front hill is rich with splendid halls and pavilions, while the back hill, in sharp contrast, is quiet with natural beauty. The central Kunming Lake, covering 2.2 square kilometres, was entirely man-made and the excavated soil was used to build Longevity Hill.<br />
<br />
In December 1998, UNESCO included the Summer Palace on its World Heritage List. It declared the Summer Palace "a masterpiece of Chinese landscape garden design. The natural landscape of hills and open water is combined with artificial features such as pavilions, halls, palaces, temples and bridges to form a harmonious ensemble of outstanding aesthetic value".
    TowerBuddhistIncence1.jpg
  • The Summer Palace (Chinese: 頤和園), is a vast ensemble of lakes, gardens and palaces in Beijing. It was an imperial garden in the Qing Dynasty. Mainly dominated by Longevity Hill (万寿山; 萬壽山) and Kunming Lake, it covers an expanse of 2.9 square kilometres, three-quarters of which is water.<br />
<br />
Longevity Hill is about 60 m high and has many buildings positioned in sequence. The front hill is rich with splendid halls and pavilions, while the back hill, in sharp contrast, is quiet with natural beauty. The central Kunming Lake, covering 2.2 square kilometres, was entirely man-made and the excavated soil was used to build Longevity Hill.<br />
<br />
In December 1998, UNESCO included the Summer Palace on its World Heritage List. It declared the Summer Palace "a masterpiece of Chinese landscape garden design. The natural landscape of hills and open water is combined with artificial features such as pavilions, halls, palaces, temples and bridges to form a harmonious ensemble of outstanding aesthetic value".
    TowerBuddhistIncence2.jpg
  • Mount St. Helens National Volcanic Monument is a U.S. National Monument that includes the area around Mount St. Helens in Washington. It was established on August 27, 1982 by U.S. President Ronald Reagan following the 1980 eruption of Mount St. Helens. The 110,000 acre National Volcanic Monument was set-aside for research, recreation, and education. Inside the Monument, the environment is left to respond naturally to the disturbance.
    MountSaintHelens10.jpg
  • Zion National Park is a United States National Park located in southwestern Utah. A prominent feature of the 229-square-mile park is Zion Canyon, which is 15 miles long and up to half a mile deep, cut through the reddish and tan-colored Navajo Sandstone by the North Fork of the Virgin River. The lowest elevation is 3,666 ft  at Coalpits Wash and the highest elevation is 8,726 ft at Horse Ranch Mountain. Located at the junction of the Colorado Plateau, Great Basin, and Mojave Desert regions, the park's unique geography and variety of life zones allow for unusual plant and animal diversity. Numerous plant species as well as 289 species of birds, 75 mammals (including 19 species of bat), and 32 reptiles inhabit the park's four life zones: desert, riparian, woodland, and coniferous forest. Zion National Park includes mountains, canyons, buttes, mesas, monoliths, rivers, slot canyons, and natural arches.
    ZionWatchman1.jpg
  • The Summer Palace (Chinese: 頤和園), is a vast ensemble of lakes, gardens and palaces in Beijing. It was an imperial garden in the Qing Dynasty. Mainly dominated by Longevity Hill (万寿山; 萬壽山) and Kunming Lake, it covers an expanse of 2.9 square kilometres, three-quarters of which is water.<br />
<br />
Longevity Hill is about 60 m high and has many buildings positioned in sequence. The front hill is rich with splendid halls and pavilions, while the back hill, in sharp contrast, is quiet with natural beauty. The central Kunming Lake, covering 2.2 square kilometres, was entirely man-made and the excavated soil was used to build Longevity Hill.<br />
<br />
In December 1998, UNESCO included the Summer Palace on its World Heritage List. It declared the Summer Palace "a masterpiece of Chinese landscape garden design. The natural landscape of hills and open water is combined with artificial features such as pavilions, halls, palaces, temples and bridges to form a harmonious ensemble of outstanding aesthetic value".
    LongCorridor4.jpg
  • The Summer Palace (Chinese: 頤和園), is a vast ensemble of lakes, gardens and palaces in Beijing. It was an imperial garden in the Qing Dynasty. Mainly dominated by Longevity Hill (万寿山; 萬壽山) and Kunming Lake, it covers an expanse of 2.9 square kilometres, three-quarters of which is water.<br />
<br />
Longevity Hill is about 60 m high and has many buildings positioned in sequence. The front hill is rich with splendid halls and pavilions, while the back hill, in sharp contrast, is quiet with natural beauty. The central Kunming Lake, covering 2.2 square kilometres, was entirely man-made and the excavated soil was used to build Longevity Hill.<br />
<br />
In December 1998, UNESCO included the Summer Palace on its World Heritage List. It declared the Summer Palace "a masterpiece of Chinese landscape garden design. The natural landscape of hills and open water is combined with artificial features such as pavilions, halls, palaces, temples and bridges to form a harmonious ensemble of outstanding aesthetic value".
    KunmingLake1.jpg
  • Mount St. Helens National Volcanic Monument is a U.S. National Monument that includes the area around Mount St. Helens in Washington. It was established on August 27, 1982 by U.S. President Ronald Reagan following the 1980 eruption of Mount St. Helens. The 110,000 acre National Volcanic Monument was set-aside for research, recreation, and education. Inside the Monument, the environment is left to respond naturally to the disturbance.
    MountSaintHelens4.jpg
  • Mount St. Helens National Volcanic Monument is a U.S. National Monument that includes the area around Mount St. Helens in Washington. It was established on August 27, 1982 by U.S. President Ronald Reagan following the 1980 eruption of Mount St. Helens. The 110,000 acre National Volcanic Monument was set-aside for research, recreation, and education. Inside the Monument, the environment is left to respond naturally to the disturbance.
    MountSaintHelens8.jpg
  • Multnomah Falls in Columbia River Gorge, Oregon.<br />
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Multnomah Falls is a waterfall located on Multnomah Creek in the Columbia River Gorge, east of Troutdale, between Corbett and Dodson, Oregon, United States. The waterfall is accessible from the Historic Columbia River Highway and Interstate 84. Spanning two tiers on basalt cliffs, it is the tallest waterfall in the state of Oregon at 620 ft in height.<br />
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The land surrounding the falls was developed by Simon Benson in the early-twentieth century, with a pathway, viewing bridge, and adjacent lodge being constructed in 1925. The Multnomah Falls Lodge and the surrounding footpaths at the falls were added to the National Register of Historic Places in 1981. Contemporarily, the state of Oregon maintains a switchback trail that ascends to a talus slope 100 feet above the falls, and descends to an observation deck that overlooks the falls' edge. The falls attract over two million visitors each year, making it the most-visited natural recreation site in the U.S. Pacific Northwest.
    MultnomahAutumn1.jpg
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