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  • 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.
    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.
    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.
    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.
    PortlandJapaneseGarden4.jpg
  • Moraine Lake is a glacially fed lake in Banff National Park, 14 kilometres (8.7 mi) outside the Village of Lake Louise, Alberta, Canada. It is situated in the Valley of the Ten Peaks, at an elevation of approximately 6,183 feet (1,885 m). The lake has a surface area of 50 hectares (120 acres). The lake, being glacially fed, does not reach its crest until mid to late June. When it is full, it reflects a distinctive shade of blue. The colour is due to the refraction of light off the rock flour deposited in the lake on a continual basis.
    MoraineLake3.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.
    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.
    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.
    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.
    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.
    PortlandJapaneseGarden6.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.
    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.
    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
  • Mount Assiniboine Provincial Park is a provincial park in British Columbia, Canada, located around Mount Assiniboine. The park was established 1922. Some of the more recent history that is explorable within the park include Wheeler's Wonder Lodge (Naiset) (1924), Assiniboine Lodge (1928), the first ski lodge in the Canadian Rockies, and Sunburst (1928). In 1990, this park was included within the Canadian Rocky Mountain Parks UNESCO World Heritage Site. Together with the other national and provincial parks that comprise the Canadian Rocky Mountain Parks, the park was recognized for its natural beauty and the geological and ecological significance of its mountain landscapes containing the habitats of rare and endangered species, mountain peaks, glaciers, lakes, waterfalls, canyons, limestone caves and fossils.
    AssiniboineTarn3.jpg
  • Mount Assiniboine Provincial Park is a provincial park in British Columbia, Canada, located around Mount Assiniboine. The park was established 1922. Some of the more recent history that is explorable within the park include Wheeler's Wonder Lodge (Naiset) (1924), Assiniboine Lodge (1928), the first ski lodge in the Canadian Rockies, and Sunburst (1928). In 1990, this park was included within the Canadian Rocky Mountain Parks UNESCO World Heritage Site. Together with the other national and provincial parks that comprise the Canadian Rocky Mountain Parks, the park was recognized for its natural beauty and the geological and ecological significance of its mountain landscapes containing the habitats of rare and endangered species, mountain peaks, glaciers, lakes, waterfalls, canyons, limestone caves and fossils.
    AssiniboineTarn3.jpg
  • Herbert Lake in Banff National Park in Alberta, Canada. Banff National Park is Canada's oldest national park and was established in 1885. Located in the Rocky Mountains, 110–180 kilometres (68–112 mi) west of Calgary in the province of Alberta, Banff encompasses 6,641 square kilometres (2,564 sq mi) of mountainous terrain, with numerous glaciers and ice fields, dense coniferous forest, and alpine landscapes. The Icefields Parkway extends from Lake Louise, connecting to Jasper National Park in the north. Provincial forests and Yoho National Park are neighbours to the west, while Kootenay National Park is located to the south and Kananaskis Country to the southeast. The main commercial centre of the park is the town of Banff, in the Bow River valley.
    HerbertLake_Panorama.jpg
  • Herbert Lake in Banff National Park in Alberta, Canada. Banff National Park is Canada's oldest national park and was established in 1885. Located in the Rocky Mountains, 110–180 kilometres (68–112 mi) west of Calgary in the province of Alberta, Banff encompasses 6,641 square kilometres (2,564 sq mi) of mountainous terrain, with numerous glaciers and ice fields, dense coniferous forest, and alpine landscapes. The Icefields Parkway extends from Lake Louise, connecting to Jasper National Park in the north. Provincial forests and Yoho National Park are neighbours to the west, while Kootenay National Park is located to the south and Kananaskis Country to the southeast. The main commercial centre of the park is the town of Banff, in the Bow River valley.
    HerbertLake4.jpg
  • Mount Assiniboine Provincial Park is a provincial park in British Columbia, Canada, located around Mount Assiniboine. The park was established 1922. Some of the more recent history that is explorable within the park include Wheeler's Wonder Lodge (Naiset) (1924), Assiniboine Lodge (1928), the first ski lodge in the Canadian Rockies, and Sunburst (1928). In 1990, this park was included within the Canadian Rocky Mountain Parks UNESCO World Heritage Site. Together with the other national and provincial parks that comprise the Canadian Rocky Mountain Parks, the park was recognized for its natural beauty and the geological and ecological significance of its mountain landscapes containing the habitats of rare and endangered species, mountain peaks, glaciers, lakes, waterfalls, canyons, limestone caves and fossils.
    AssiniboineTarn2.jpg
  • Mount Assiniboine Provincial Park is a provincial park in British Columbia, Canada, located around Mount Assiniboine. The park was established 1922. Some of the more recent history that is explorable within the park include Wheeler's Wonder Lodge (Naiset) (1924), Assiniboine Lodge (1928), the first ski lodge in the Canadian Rockies, and Sunburst (1928). In 1990, this park was included within the Canadian Rocky Mountain Parks UNESCO World Heritage Site. Together with the other national and provincial parks that comprise the Canadian Rocky Mountain Parks, the park was recognized for its natural beauty and the geological and ecological significance of its mountain landscapes containing the habitats of rare and endangered species, mountain peaks, glaciers, lakes, waterfalls, canyons, limestone caves and fossils.
    AssiniboineTarn4.jpg
  • Herbert Lake in Banff National Park in Alberta, Canada. Banff National Park is Canada's oldest national park and was established in 1885. Located in the Rocky Mountains, 110–180 kilometres (68–112 mi) west of Calgary in the province of Alberta, Banff encompasses 6,641 square kilometres (2,564 sq mi) of mountainous terrain, with numerous glaciers and ice fields, dense coniferous forest, and alpine landscapes. The Icefields Parkway extends from Lake Louise, connecting to Jasper National Park in the north. Provincial forests and Yoho National Park are neighbours to the west, while Kootenay National Park is located to the south and Kananaskis Country to the southeast. The main commercial centre of the park is the town of Banff, in the Bow River valley.
    HerbertLake6.jpg
  • Herbert Lake in Banff National Park in Alberta, Canada. Banff National Park is Canada's oldest national park and was established in 1885. Located in the Rocky Mountains, 110–180 kilometres (68–112 mi) west of Calgary in the province of Alberta, Banff encompasses 6,641 square kilometres (2,564 sq mi) of mountainous terrain, with numerous glaciers and ice fields, dense coniferous forest, and alpine landscapes. The Icefields Parkway extends from Lake Louise, connecting to Jasper National Park in the north. Provincial forests and Yoho National Park are neighbours to the west, while Kootenay National Park is located to the south and Kananaskis Country to the southeast. The main commercial centre of the park is the town of Banff, in the Bow River valley.
    HerbertLake1.jpg
  • Mount Assiniboine Provincial Park is a provincial park in British Columbia, Canada, located around Mount Assiniboine. The park was established 1922. Some of the more recent history that is explorable within the park include Wheeler's Wonder Lodge (Naiset) (1924), Assiniboine Lodge (1928), the first ski lodge in the Canadian Rockies, and Sunburst (1928). In 1990, this park was included within the Canadian Rocky Mountain Parks UNESCO World Heritage Site. Together with the other national and provincial parks that comprise the Canadian Rocky Mountain Parks, the park was recognized for its natural beauty and the geological and ecological significance of its mountain landscapes containing the habitats of rare and endangered species, mountain peaks, glaciers, lakes, waterfalls, canyons, limestone caves and fossils.
    AssiniboineTarn1.jpg
  • Herbert Lake in Banff National Park in Alberta, Canada. Banff National Park is Canada's oldest national park and was established in 1885. Located in the Rocky Mountains, 110–180 kilometres (68–112 mi) west of Calgary in the province of Alberta, Banff encompasses 6,641 square kilometres (2,564 sq mi) of mountainous terrain, with numerous glaciers and ice fields, dense coniferous forest, and alpine landscapes. The Icefields Parkway extends from Lake Louise, connecting to Jasper National Park in the north. Provincial forests and Yoho National Park are neighbours to the west, while Kootenay National Park is located to the south and Kananaskis Country to the southeast. The main commercial centre of the park is the town of Banff, in the Bow River valley.
    HerbertLake5.jpg
  • Mount Assiniboine Provincial Park is a provincial park in British Columbia, Canada, located around Mount Assiniboine. The park was established 1922. Some of the more recent history that is explorable within the park include Wheeler's Wonder Lodge (Naiset) (1924), Assiniboine Lodge (1928), the first ski lodge in the Canadian Rockies, and Sunburst (1928). In 1990, this park was included within the Canadian Rocky Mountain Parks UNESCO World Heritage Site. Together with the other national and provincial parks that comprise the Canadian Rocky Mountain Parks, the park was recognized for its natural beauty and the geological and ecological significance of its mountain landscapes containing the habitats of rare and endangered species, mountain peaks, glaciers, lakes, waterfalls, canyons, limestone caves and fossils.
    AssiniboineTarn3.jpg
  • Johnston Creek is a tributary of the Bow River in Canada's Rocky Mountains. The creek is located in Banff National Park. As Johnston Creek approaches the Bow River, it flows through a large canyon formed by erosion over thousands of years. The creek has cut through the limestone rock to form sheer canyon walls, as well as waterfalls, tunnels, and pools.
    JohnstonCanyon10.jpg
  • Meadow full of lupines in Mount Rainier National Park
    MountRainierNachesFlowers6.jpg
  • Lupines and sunflowers along Naches Peak trail in Mount Rainier National Park
    MountRainierNachesFlowers1.jpg
  • Lupines and sunflowers along Naches Peak trail in Mount Rainier National Park
    MountRainierNachesFlowers3.jpg
  • Kandestederne beach near Skagen on Jylland in Denmark
    SkagenSkiverenBeach1.jpg
  • The very northern tip of Denmark's Jylland province is called "Grenen", and divides the Kattegatt sea from the Skagerack sea
    SkagenGrenen1.jpg
  • Lupines and sunflowers along Naches Peak trail in Mount Rainier National Park
    MountRainierNachesFlowers3.jpg
  • Portland, Oregon skyline from the Pittock Mansion.<br />
<br />
Portland, officially the City of Portland, is the largest and most populous city in the U.S. state of Oregon and the seat of Multnomah County. It is a major port in the Willamette Valley region of the Pacific Northwest, at the confluence of the Willamette and Columbia rivers. Approximately 2.4 million people live in the Portland metropolitan statistical area (MSA), making it the 25th most populous in the United States. Named after Portland, Maine, the Oregon settlement began to be populated in the 1830s near the end of the Oregon Trail. Its water access provided convenient transportation of goods, and the timber industry was a major force in the city's early economy. At the turn of the 20th century, the city had a reputation as one of the most dangerous port cities in the world, a hub for organized crime and racketeering. After the city's economy experienced an industrial boom during World War II, its hard-edged reputation began to dissipate. Beginning in the 1960s, Portland became noted for its growing progressive political values, earning it a reputation as a bastion of counterculture.<br />
<br />
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.
    PortlandPittockMansion3.jpg
  • Portland, Oregon skyline from the Pittock Mansion.<br />
<br />
Portland, officially the City of Portland, is the largest and most populous city in the U.S. state of Oregon and the seat of Multnomah County. It is a major port in the Willamette Valley region of the Pacific Northwest, at the confluence of the Willamette and Columbia rivers. Approximately 2.4 million people live in the Portland metropolitan statistical area (MSA), making it the 25th most populous in the United States. Named after Portland, Maine, the Oregon settlement began to be populated in the 1830s near the end of the Oregon Trail. Its water access provided convenient transportation of goods, and the timber industry was a major force in the city's early economy. At the turn of the 20th century, the city had a reputation as one of the most dangerous port cities in the world, a hub for organized crime and racketeering. After the city's economy experienced an industrial boom during World War II, its hard-edged reputation began to dissipate. Beginning in the 1960s, Portland became noted for its growing progressive political values, earning it a reputation as a bastion of counterculture.<br />
<br />
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.
    PortlandPittockMansion1.jpg
  • Portland, Oregon skyline from the Portland Japanese Gardens.<br />
<br />
Portland, officially the City of Portland, is the largest and most populous city in the U.S. state of Oregon and the seat of Multnomah County. It is a major port in the Willamette Valley region of the Pacific Northwest, at the confluence of the Willamette and Columbia rivers. Approximately 2.4 million people live in the Portland metropolitan statistical area (MSA), making it the 25th most populous in the United States. Named after Portland, Maine, the Oregon settlement began to be populated in the 1830s near the end of the Oregon Trail. Its water access provided convenient transportation of goods, and the timber industry was a major force in the city's early economy. At the turn of the 20th century, the city had a reputation as one of the most dangerous port cities in the world, a hub for organized crime and racketeering. After the city's economy experienced an industrial boom during World War II, its hard-edged reputation began to dissipate. Beginning in the 1960s, Portland became noted for its growing progressive political values, earning it a reputation as a bastion of counterculture.<br />
<br />
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.
    PortlandJapaneseGarden19.jpg
  • Grand Canyon from Toroweap Point<br />
.....<br />
The Grand Canyon is a steep-sided canyon carved by the Colorado River in the state of Arizona in the United States. It is contained within and managed by Grand Canyon National Park, the Hualapai Tribal Nation, the Havasupai Tribe and the Navajo Nation. President Theodore Roosevelt was a major proponent of preservation of the Grand Canyon area, and visited it on numerous occasions to hunt and enjoy the scenery.<br />
The Grand Canyon is 277 miles long, up to 18 miles wide and attains a depth of over a mile. Nearly two billion years of Earth's geological history have been exposed as the Colorado River and its tributaries cut their channels through layer after layer of rock while the Colorado Plateau was uplifted. While the specific geologic processes and timing that formed the Grand Canyon are the subject of debate by geologists, recent evidence suggests that the Colorado River established its course through the canyon at least 17 million years ago. Since that time, the Colorado River continued to erode and form the canyon to its present-day configuration.<br />
For thousands of years, the area has been continuously inhabited by Native Americans who built settlements within the canyon and its many caves. The Pueblo people considered the Grand Canyon ("Ongtupqa" in the Hopi language) a holy site, and made pilgrimages to it. The first European known to have viewed the Grand Canyon was García López de Cárdenas from Spain, who arrived in 1540.
    Toroweap1.jpg
  • View of the canyon walls ofthe Grand Canyon seen from a raft on the Colorado River
    GrandCanyonRiver1.jpg
  • Grand Canyon from Toroweap Point<br />
.....<br />
The Grand Canyon is a steep-sided canyon carved by the Colorado River in the state of Arizona in the United States. It is contained within and managed by Grand Canyon National Park, the Hualapai Tribal Nation, the Havasupai Tribe and the Navajo Nation. President Theodore Roosevelt was a major proponent of preservation of the Grand Canyon area, and visited it on numerous occasions to hunt and enjoy the scenery.<br />
The Grand Canyon is 277 miles long, up to 18 miles wide and attains a depth of over a mile. Nearly two billion years of Earth's geological history have been exposed as the Colorado River and its tributaries cut their channels through layer after layer of rock while the Colorado Plateau was uplifted. While the specific geologic processes and timing that formed the Grand Canyon are the subject of debate by geologists, recent evidence suggests that the Colorado River established its course through the canyon at least 17 million years ago. Since that time, the Colorado River continued to erode and form the canyon to its present-day configuration.<br />
For thousands of years, the area has been continuously inhabited by Native Americans who built settlements within the canyon and its many caves. The Pueblo people considered the Grand Canyon ("Ongtupqa" in the Hopi language) a holy site, and made pilgrimages to it. The first European known to have viewed the Grand Canyon was García López de Cárdenas from Spain, who arrived in 1540.
    ToroweapPano1.jpg
  • The Oneonta Gorge is in the Columbia River Gorge in the American state of Oregon. The U.S. Forest Service has designated it as a botanical area because of the unique aquatic and woodland plants that grow there. The basalt walls are home to a wide variety of ferns, mosses, hepatics and lichens, many of which grow only in the Columbia River Gorge.
    OneontaFalls4.jpg
  • The north face of Mount Rainier from a tarn at Spray Park
    MtRainierSprayParkTarn2.jpg
  • Farm fields from Steptoe Butte in the Palouse region of eastern Washington state
    PalouseGreenSea.jpg
  • Farm buildings in the palouse area of eastern Washington
    PalouseBarn2Hor.jpg
  • The Palouse is a region of the northwestern United States, encompassing parts of southeastern Washington, north central Idaho and, in some definitions, extending south into northeast Oregon. It is a major agricultural area, primarily producing wheat and legumes.
    PalousePanorama1.jpg
  • Forest at Sol Duc Falls in Olympic National Park, Washington
    SolDucEnchantedForest3.jpg
  • Birch Trees on the North Rim of the Grand Canyon<br />
.....<br />
The Grand Canyon is a steep-sided canyon carved by the Colorado River in the state of Arizona in the United States. It is contained within and managed by Grand Canyon National Park, the Hualapai Tribal Nation, the Havasupai Tribe and the Navajo Nation. President Theodore Roosevelt was a major proponent of preservation of the Grand Canyon area, and visited it on numerous occasions to hunt and enjoy the scenery.<br />
The Grand Canyon is 277 miles long, up to 18 miles wide and attains a depth of over a mile. Nearly two billion years of Earth's geological history have been exposed as the Colorado River and its tributaries cut their channels through layer after layer of rock while the Colorado Plateau was uplifted. While the specific geologic processes and timing that formed the Grand Canyon are the subject of debate by geologists, recent evidence suggests that the Colorado River established its course through the canyon at least 17 million years ago. Since that time, the Colorado River continued to erode and form the canyon to its present-day configuration.<br />
For thousands of years, the area has been continuously inhabited by Native Americans who built settlements within the canyon and its many caves. The Pueblo people considered the Grand Canyon ("Ongtupqa" in the Hopi language) a holy site, and made pilgrimages to it. The first European known to have viewed the Grand Canyon was García López de Cárdenas from Spain, who arrived in 1540.
    PointSublimeBirches1.jpg
  • Point Sublime on the North Rim of the Grand Canyon, Arizona<br />
.....<br />
The Grand Canyon is a steep-sided canyon carved by the Colorado River in the state of Arizona in the United States. It is contained within and managed by Grand Canyon National Park, the Hualapai Tribal Nation, the Havasupai Tribe and the Navajo Nation. President Theodore Roosevelt was a major proponent of preservation of the Grand Canyon area, and visited it on numerous occasions to hunt and enjoy the scenery.<br />
The Grand Canyon is 277 miles long, up to 18 miles wide and attains a depth of over a mile. Nearly two billion years of Earth's geological history have been exposed as the Colorado River and its tributaries cut their channels through layer after layer of rock while the Colorado Plateau was uplifted. While the specific geologic processes and timing that formed the Grand Canyon are the subject of debate by geologists, recent evidence suggests that the Colorado River established its course through the canyon at least 17 million years ago. Since that time, the Colorado River continued to erode and form the canyon to its present-day configuration.<br />
For thousands of years, the area has been continuously inhabited by Native Americans who built settlements within the canyon and its many caves. The Pueblo people considered the Grand Canyon ("Ongtupqa" in the Hopi language) a holy site, and made pilgrimages to it. The first European known to have viewed the Grand Canyon was García López de Cárdenas from Spain, who arrived in 1540.
    PointSublimeSunset2.jpg
  • Point Sublime on the North Rim of the Grand Canyon, Arizona<br />
.....<br />
The Grand Canyon is a steep-sided canyon carved by the Colorado River in the state of Arizona in the United States. It is contained within and managed by Grand Canyon National Park, the Hualapai Tribal Nation, the Havasupai Tribe and the Navajo Nation. President Theodore Roosevelt was a major proponent of preservation of the Grand Canyon area, and visited it on numerous occasions to hunt and enjoy the scenery.<br />
The Grand Canyon is 277 miles long, up to 18 miles wide and attains a depth of over a mile. Nearly two billion years of Earth's geological history have been exposed as the Colorado River and its tributaries cut their channels through layer after layer of rock while the Colorado Plateau was uplifted. While the specific geologic processes and timing that formed the Grand Canyon are the subject of debate by geologists, recent evidence suggests that the Colorado River established its course through the canyon at least 17 million years ago. Since that time, the Colorado River continued to erode and form the canyon to its present-day configuration.<br />
For thousands of years, the area has been continuously inhabited by Native Americans who built settlements within the canyon and its many caves. The Pueblo people considered the Grand Canyon ("Ongtupqa" in the Hopi language) a holy site, and made pilgrimages to it. The first European known to have viewed the Grand Canyon was García López de Cárdenas from Spain, who arrived in 1540.
    PointSublime8.jpg
  • Sunset at Bright Angel Point on the North Rim of the Grand Canyon, Arizona<br />
.....<br />
The Grand Canyon is a steep-sided canyon carved by the Colorado River in the state of Arizona in the United States. It is contained within and managed by Grand Canyon National Park, the Hualapai Tribal Nation, the Havasupai Tribe and the Navajo Nation. President Theodore Roosevelt was a major proponent of preservation of the Grand Canyon area, and visited it on numerous occasions to hunt and enjoy the scenery.<br />
The Grand Canyon is 277 miles long, up to 18 miles wide and attains a depth of over a mile. Nearly two billion years of Earth's geological history have been exposed as the Colorado River and its tributaries cut their channels through layer after layer of rock while the Colorado Plateau was uplifted. While the specific geologic processes and timing that formed the Grand Canyon are the subject of debate by geologists, recent evidence suggests that the Colorado River established its course through the canyon at least 17 million years ago. Since that time, the Colorado River continued to erode and form the canyon to its present-day configuration.<br />
For thousands of years, the area has been continuously inhabited by Native Americans who built settlements within the canyon and its many caves. The Pueblo people considered the Grand Canyon ("Ongtupqa" in the Hopi language) a holy site, and made pilgrimages to it. The first European known to have viewed the Grand Canyon was García López de Cárdenas from Spain, who arrived in 1540.
    BrightAngelTree1.jpg
  • Birch Trees on the North Rim of the Grand Canyon<br />
.....<br />
The Grand Canyon is a steep-sided canyon carved by the Colorado River in the state of Arizona in the United States. It is contained within and managed by Grand Canyon National Park, the Hualapai Tribal Nation, the Havasupai Tribe and the Navajo Nation. President Theodore Roosevelt was a major proponent of preservation of the Grand Canyon area, and visited it on numerous occasions to hunt and enjoy the scenery.<br />
The Grand Canyon is 277 miles long, up to 18 miles wide and attains a depth of over a mile. Nearly two billion years of Earth's geological history have been exposed as the Colorado River and its tributaries cut their channels through layer after layer of rock while the Colorado Plateau was uplifted. While the specific geologic processes and timing that formed the Grand Canyon are the subject of debate by geologists, recent evidence suggests that the Colorado River established its course through the canyon at least 17 million years ago. Since that time, the Colorado River continued to erode and form the canyon to its present-day configuration.<br />
For thousands of years, the area has been continuously inhabited by Native Americans who built settlements within the canyon and its many caves. The Pueblo people considered the Grand Canyon ("Ongtupqa" in the Hopi language) a holy site, and made pilgrimages to it. The first European known to have viewed the Grand Canyon was García López de Cárdenas from Spain, who arrived in 1540.
    NorthRimBirches1.jpg
  • Sunrise at Point Imperial on the North Rim of the Grand Canyon, Arizona<br />
.....<br />
The Grand Canyon is a steep-sided canyon carved by the Colorado River in the state of Arizona in the United States. It is contained within and managed by Grand Canyon National Park, the Hualapai Tribal Nation, the Havasupai Tribe and the Navajo Nation. President Theodore Roosevelt was a major proponent of preservation of the Grand Canyon area, and visited it on numerous occasions to hunt and enjoy the scenery.<br />
The Grand Canyon is 277 miles long, up to 18 miles wide and attains a depth of over a mile. Nearly two billion years of Earth's geological history have been exposed as the Colorado River and its tributaries cut their channels through layer after layer of rock while the Colorado Plateau was uplifted. While the specific geologic processes and timing that formed the Grand Canyon are the subject of debate by geologists, recent evidence suggests that the Colorado River established its course through the canyon at least 17 million years ago. Since that time, the Colorado River continued to erode and form the canyon to its present-day configuration.<br />
For thousands of years, the area has been continuously inhabited by Native Americans who built settlements within the canyon and its many caves. The Pueblo people considered the Grand Canyon ("Ongtupqa" in the Hopi language) a holy site, and made pilgrimages to it. The first European known to have viewed the Grand Canyon was García López de Cárdenas from Spain, who arrived in 1540.
    PointImperial4.jpg
  • Sunrise at Point Imperial on the North Rim of the Grand Canyon, Arizona<br />
.....<br />
The Grand Canyon is a steep-sided canyon carved by the Colorado River in the state of Arizona in the United States. It is contained within and managed by Grand Canyon National Park, the Hualapai Tribal Nation, the Havasupai Tribe and the Navajo Nation. President Theodore Roosevelt was a major proponent of preservation of the Grand Canyon area, and visited it on numerous occasions to hunt and enjoy the scenery.<br />
The Grand Canyon is 277 miles long, up to 18 miles wide and attains a depth of over a mile. Nearly two billion years of Earth's geological history have been exposed as the Colorado River and its tributaries cut their channels through layer after layer of rock while the Colorado Plateau was uplifted. While the specific geologic processes and timing that formed the Grand Canyon are the subject of debate by geologists, recent evidence suggests that the Colorado River established its course through the canyon at least 17 million years ago. Since that time, the Colorado River continued to erode and form the canyon to its present-day configuration.<br />
For thousands of years, the area has been continuously inhabited by Native Americans who built settlements within the canyon and its many caves. The Pueblo people considered the Grand Canyon ("Ongtupqa" in the Hopi language) a holy site, and made pilgrimages to it. The first European known to have viewed the Grand Canyon was García López de Cárdenas from Spain, who arrived in 1540.
    PointImperial3.jpg
  • Cape Royal at the North Rim of the Grand Canyon, Arizona<br />
.....<br />
The Grand Canyon is a steep-sided canyon carved by the Colorado River in the state of Arizona in the United States. It is contained within and managed by Grand Canyon National Park, the Hualapai Tribal Nation, the Havasupai Tribe and the Navajo Nation. President Theodore Roosevelt was a major proponent of preservation of the Grand Canyon area, and visited it on numerous occasions to hunt and enjoy the scenery.<br />
The Grand Canyon is 277 miles long, up to 18 miles wide and attains a depth of over a mile. Nearly two billion years of Earth's geological history have been exposed as the Colorado River and its tributaries cut their channels through layer after layer of rock while the Colorado Plateau was uplifted. While the specific geologic processes and timing that formed the Grand Canyon are the subject of debate by geologists, recent evidence suggests that the Colorado River established its course through the canyon at least 17 million years ago. Since that time, the Colorado River continued to erode and form the canyon to its present-day configuration.<br />
For thousands of years, the area has been continuously inhabited by Native Americans who built settlements within the canyon and its many caves. The Pueblo people considered the Grand Canyon ("Ongtupqa" in the Hopi language) a holy site, and made pilgrimages to it. The first European known to have viewed the Grand Canyon was García López de Cárdenas from Spain, who arrived in 1540.
    CapeRoyalAfterglow2.jpg
  • Cape Royal at the North Rim of the Grand Canyon, Arizona<br />
.....<br />
The Grand Canyon is a steep-sided canyon carved by the Colorado River in the state of Arizona in the United States. It is contained within and managed by Grand Canyon National Park, the Hualapai Tribal Nation, the Havasupai Tribe and the Navajo Nation. President Theodore Roosevelt was a major proponent of preservation of the Grand Canyon area, and visited it on numerous occasions to hunt and enjoy the scenery.<br />
The Grand Canyon is 277 miles long, up to 18 miles wide and attains a depth of over a mile. Nearly two billion years of Earth's geological history have been exposed as the Colorado River and its tributaries cut their channels through layer after layer of rock while the Colorado Plateau was uplifted. While the specific geologic processes and timing that formed the Grand Canyon are the subject of debate by geologists, recent evidence suggests that the Colorado River established its course through the canyon at least 17 million years ago. Since that time, the Colorado River continued to erode and form the canyon to its present-day configuration.<br />
For thousands of years, the area has been continuously inhabited by Native Americans who built settlements within the canyon and its many caves. The Pueblo people considered the Grand Canyon ("Ongtupqa" in the Hopi language) a holy site, and made pilgrimages to it. The first European known to have viewed the Grand Canyon was García López de Cárdenas from Spain, who arrived in 1540.
    CapeRoyalAfterglow1.jpg
  • Cape Royal at the North Rim of the Grand Canyon, Arizona<br />
.....<br />
The Grand Canyon is a steep-sided canyon carved by the Colorado River in the state of Arizona in the United States. It is contained within and managed by Grand Canyon National Park, the Hualapai Tribal Nation, the Havasupai Tribe and the Navajo Nation. President Theodore Roosevelt was a major proponent of preservation of the Grand Canyon area, and visited it on numerous occasions to hunt and enjoy the scenery.<br />
The Grand Canyon is 277 miles long, up to 18 miles wide and attains a depth of over a mile. Nearly two billion years of Earth's geological history have been exposed as the Colorado River and its tributaries cut their channels through layer after layer of rock while the Colorado Plateau was uplifted. While the specific geologic processes and timing that formed the Grand Canyon are the subject of debate by geologists, recent evidence suggests that the Colorado River established its course through the canyon at least 17 million years ago. Since that time, the Colorado River continued to erode and form the canyon to its present-day configuration.<br />
For thousands of years, the area has been continuously inhabited by Native Americans who built settlements within the canyon and its many caves. The Pueblo people considered the Grand Canyon ("Ongtupqa" in the Hopi language) a holy site, and made pilgrimages to it. The first European known to have viewed the Grand Canyon was García López de Cárdenas from Spain, who arrived in 1540.
    CapeRoyalAfternoon2.jpg
  • Lake Louise, named Lake of the Little Fishes by the Stoney Nakota First Nations people, is a glacial lake within Banff National Park in Alberta, Canada. It is located 5 km (3.1 mi) west of the Hamlet of Lake Louise and the Trans-Canada Highway (Highway 1). Lake Louise is named after the Princess Louise Caroline Alberta (1848–1939), the fourth daughter of Queen Victoria and the wife of the Marquess of Lorne, who was the Governor General of Canada from 1878 to 1883. The emerald colour of the water comes from rock flour carried into the lake by melt-water from the glaciers that overlook the lake. The lake has a surface of 0.8 km2 (0.31 sq mi) and is drained through the 3 km long Louise Creek into the Bow River.<br />
Fairmont's Chateau Lake Louise, one of Canada's grand railway hotels, is located on Lake Louise's eastern shore. It is a luxury resort hotel built in the early decades of the 20th century by the Canadian Pacific Railway.<br />
Moraine Lake and Lake Agnes are also accessible from Lake Louise.
    LakeLouiseRedCanoes1.jpg
  • Mount Assiniboine, also known as Assiniboine Mountain, is a pyramidal peak mountain located on the Great Divide, on the British Columbia/Alberta border in Canada. At 11,870 ft, it is the highest peak in the Southern Continental Ranges of the Canadian Rockies. Mt. Assiniboine rises nearly 1,525 m (5,003 ft) above Lake Magog. Because of its resemblance to the Matterhorn in the Alps, it is nicknamed the "Matterhorn of the Rockies". Mt. Assiniboine was named by George M. Dawson in 1885. When Dawson saw Mt. Assiniboine from Copper Mountain, he saw a plume of clouds trailing away from the top. This reminded him of the plumes of smoke emanating from the teepees of Assiniboine Indians. Mt. Assiniboine lies on the border between Mount Assiniboine Provincial Park, in British Columbia, and Banff National Park, in Alberta. The park does not have any roads and thus can only be reached by a six-hour hike or horse-pack 27 km, three-hour bike ride (now disallowed to reduce human / grizzly encounters) or helicopter. The usual approach is via Bryant Creek. From Canmore follow the Smith-Dorien road to the Mount Shark parking lot. The trail is well signed. A helipad is also here.
    MtAssiniboine3.jpg
  • Mount Assiniboine Provincial Park is a provincial park in British Columbia, Canada, located around Mount Assiniboine. The park was established 1922. Some of the more recent history that is explorable within the park include Wheeler's Wonder Lodge (Naiset) (1924), Assiniboine Lodge (1928), the first ski lodge in the Canadian Rockies, and Sunburst (1928). In 1990, this park was included within the Canadian Rocky Mountain Parks UNESCO World Heritage Site. Together with the other national and provincial parks that comprise the Canadian Rocky Mountain Parks, the park was recognized for its natural beauty and the geological and ecological significance of its mountain landscapes containing the habitats of rare and endangered species, mountain peaks, glaciers, lakes, waterfalls, canyons, limestone caves and fossils.
    LakeMagogMountainLight4.jpg
  • Mount Assiniboine Provincial Park is a provincial park in British Columbia, Canada, located around Mount Assiniboine. The park was established 1922. Some of the more recent history that is explorable within the park include Wheeler's Wonder Lodge (Naiset) (1924), Assiniboine Lodge (1928), the first ski lodge in the Canadian Rockies, and Sunburst (1928). In 1990, this park was included within the Canadian Rocky Mountain Parks UNESCO World Heritage Site. Together with the other national and provincial parks that comprise the Canadian Rocky Mountain Parks, the park was recognized for its natural beauty and the geological and ecological significance of its mountain landscapes containing the habitats of rare and endangered species, mountain peaks, glaciers, lakes, waterfalls, canyons, limestone caves and fossils.
    LakeMagogMountainLight3.jpg
  • Mount Assiniboine Provincial Park is a provincial park in British Columbia, Canada, located around Mount Assiniboine. The park was established 1922. Some of the more recent history that is explorable within the park include Wheeler's Wonder Lodge (Naiset) (1924), Assiniboine Lodge (1928), the first ski lodge in the Canadian Rockies, and Sunburst (1928). In 1990, this park was included within the Canadian Rocky Mountain Parks UNESCO World Heritage Site. Together with the other national and provincial parks that comprise the Canadian Rocky Mountain Parks, the park was recognized for its natural beauty and the geological and ecological significance of its mountain landscapes containing the habitats of rare and endangered species, mountain peaks, glaciers, lakes, waterfalls, canyons, limestone caves and fossils.
    LakeMagogMountainLight1.jpg
  • Mount Assiniboine Provincial Park is a provincial park in British Columbia, Canada, located around Mount Assiniboine. The park was established 1922. Some of the more recent history that is explorable within the park include Wheeler's Wonder Lodge (Naiset) (1924), Assiniboine Lodge (1928), the first ski lodge in the Canadian Rockies, and Sunburst (1928).
    SunburstPeak3.jpg
  • Mount Assiniboine Provincial Park is a provincial park in British Columbia, Canada, located around Mount Assiniboine. The park was established 1922. Some of the more recent history that is explorable within the park include Wheeler's Wonder Lodge (Naiset) (1924), Assiniboine Lodge (1928), the first ski lodge in the Canadian Rockies, and Sunburst (1928). In 1990, this park was included within the Canadian Rocky Mountain Parks UNESCO World Heritage Site. Together with the other national and provincial parks that comprise the Canadian Rocky Mountain Parks, the park was recognized for its natural beauty and the geological and ecological significance of its mountain landscapes containing the habitats of rare and endangered species, mountain peaks, glaciers, lakes, waterfalls, canyons, limestone caves and fossils.
    MtAssiniboineHut5.jpg
  • Mount Assiniboine Provincial Park is a provincial park in British Columbia, Canada, located around Mount Assiniboine. The park was established 1922. Some of the more recent history that is explorable within the park include Wheeler's Wonder Lodge (Naiset) (1924), Assiniboine Lodge (1928), the first ski lodge in the Canadian Rockies, and Sunburst (1928). In 1990, this park was included within the Canadian Rocky Mountain Parks UNESCO World Heritage Site. Together with the other national and provincial parks that comprise the Canadian Rocky Mountain Parks, the park was recognized for its natural beauty and the geological and ecological significance of its mountain landscapes containing the habitats of rare and endangered species, mountain peaks, glaciers, lakes, waterfalls, canyons, limestone caves and fossils.
    AssiniboineWinterTrees1.jpg
  • Mount Assiniboine, also known as Assiniboine Mountain, is a pyramidal peak mountain located on the Great Divide, on the British Columbia/Alberta border in Canada. At 11,870 ft, it is the highest peak in the Southern Continental Ranges of the Canadian Rockies. Mt. Assiniboine rises nearly 1,525 m (5,003 ft) above Lake Magog. Because of its resemblance to the Matterhorn in the Alps, it is nicknamed the "Matterhorn of the Rockies". Mt. Assiniboine was named by George M. Dawson in 1885. When Dawson saw Mt. Assiniboine from Copper Mountain, he saw a plume of clouds trailing away from the top. This reminded him of the plumes of smoke emanating from the teepees of Assiniboine Indians. Mt. Assiniboine lies on the border between Mount Assiniboine Provincial Park, in British Columbia, and Banff National Park, in Alberta. The park does not have any roads and thus can only be reached by a six-hour hike or horse-pack 27 km, three-hour bike ride (now disallowed to reduce human / grizzly encounters) or helicopter. The usual approach is via Bryant Creek. From Canmore follow the Smith-Dorien road to the Mount Shark parking lot. The trail is well signed. A helipad is also here.
    MtAssiniboineHut3.jpg
  • Mount Assiniboine Provincial Park is a provincial park in British Columbia, Canada, located around Mount Assiniboine. The park was established 1922. Some of the more recent history that is explorable within the park include Wheeler's Wonder Lodge (Naiset) (1924), Assiniboine Lodge (1928), the first ski lodge in the Canadian Rockies, and Sunburst (1928). In 1990, this park was included within the Canadian Rocky Mountain Parks UNESCO World Heritage Site. Together with the other national and provincial parks that comprise the Canadian Rocky Mountain Parks, the park was recognized for its natural beauty and the geological and ecological significance of its mountain landscapes containing the habitats of rare and endangered species, mountain peaks, glaciers, lakes, waterfalls, canyons, limestone caves and fossils.
    MtAssiniboineHut1.jpg
  • Mount Assiniboine, also known as Assiniboine Mountain, is a pyramidal peak mountain located on the Great Divide, on the British Columbia/Alberta border in Canada. At 11,870 ft, it is the highest peak in the Southern Continental Ranges of the Canadian Rockies. Mt. Assiniboine rises nearly 1,525 m (5,003 ft) above Lake Magog. Because of its resemblance to the Matterhorn in the Alps, it is nicknamed the "Matterhorn of the Rockies". Mt. Assiniboine was named by George M. Dawson in 1885. When Dawson saw Mt. Assiniboine from Copper Mountain, he saw a plume of clouds trailing away from the top. This reminded him of the plumes of smoke emanating from the teepees of Assiniboine Indians. Mt. Assiniboine lies on the border between Mount Assiniboine Provincial Park, in British Columbia, and Banff National Park, in Alberta. The park does not have any roads and thus can only be reached by a six-hour hike or horse-pack 27 km, three-hour bike ride (now disallowed to reduce human / grizzly encounters) or helicopter. The usual approach is via Bryant Creek. From Canmore follow the Smith-Dorien road to the Mount Shark parking lot. The trail is well signed. A helipad is also here.
    MtAssiniboineLodgeNight2.jpg
  • Mount Assiniboine, also known as Assiniboine Mountain, is a pyramidal peak mountain located on the Great Divide, on the British Columbia/Alberta border in Canada. At 11,870 ft, it is the highest peak in the Southern Continental Ranges of the Canadian Rockies. Mt. Assiniboine rises nearly 1,525 m (5,003 ft) above Lake Magog. Because of its resemblance to the Matterhorn in the Alps, it is nicknamed the "Matterhorn of the Rockies". Mt. Assiniboine was named by George M. Dawson in 1885. When Dawson saw Mt. Assiniboine from Copper Mountain, he saw a plume of clouds trailing away from the top. This reminded him of the plumes of smoke emanating from the teepees of Assiniboine Indians. Mt. Assiniboine lies on the border between Mount Assiniboine Provincial Park, in British Columbia, and Banff National Park, in Alberta. The park does not have any roads and thus can only be reached by a six-hour hike or horse-pack 27 km, three-hour bike ride (now disallowed to reduce human / grizzly encounters) or helicopter. The usual approach is via Bryant Creek. From Canmore follow the Smith-Dorien road to the Mount Shark parking lot. The trail is well signed. A helipad is also here.
    LakeMagogCabins1.jpg
  • Mount Assiniboine, also known as Assiniboine Mountain, is a pyramidal peak mountain located on the Great Divide, on the British Columbia/Alberta border in Canada. At 11,870 ft, it is the highest peak in the Southern Continental Ranges of the Canadian Rockies. Mt. Assiniboine rises nearly 1,525 m (5,003 ft) above Lake Magog. Because of its resemblance to the Matterhorn in the Alps, it is nicknamed the "Matterhorn of the Rockies". Mt. Assiniboine was named by George M. Dawson in 1885. When Dawson saw Mt. Assiniboine from Copper Mountain, he saw a plume of clouds trailing away from the top. This reminded him of the plumes of smoke emanating from the teepees of Assiniboine Indians. Mt. Assiniboine lies on the border between Mount Assiniboine Provincial Park, in British Columbia, and Banff National Park, in Alberta. The park does not have any roads and thus can only be reached by a six-hour hike or horse-pack 27 km, three-hour bike ride (now disallowed to reduce human / grizzly encounters) or helicopter. The usual approach is via Bryant Creek. From Canmore follow the Smith-Dorien road to the Mount Shark parking lot. The trail is well signed. A helipad is also here.
    _A1A0967-HDR.jpg
  • Mount Assiniboine, also known as Assiniboine Mountain, is a pyramidal peak mountain located on the Great Divide, on the British Columbia/Alberta border in Canada. At 11,870 ft, it is the highest peak in the Southern Continental Ranges of the Canadian Rockies. Mt. Assiniboine rises nearly 1,525 m (5,003 ft) above Lake Magog. Because of its resemblance to the Matterhorn in the Alps, it is nicknamed the "Matterhorn of the Rockies". Mt. Assiniboine was named by George M. Dawson in 1885. When Dawson saw Mt. Assiniboine from Copper Mountain, he saw a plume of clouds trailing away from the top. This reminded him of the plumes of smoke emanating from the teepees of Assiniboine Indians. Mt. Assiniboine lies on the border between Mount Assiniboine Provincial Park, in British Columbia, and Banff National Park, in Alberta. The park does not have any roads and thus can only be reached by a six-hour hike or horse-pack 27 km, three-hour bike ride (now disallowed to reduce human / grizzly encounters) or helicopter. The usual approach is via Bryant Creek. From Canmore follow the Smith-Dorien road to the Mount Shark parking lot. The trail is well signed. A helipad is also here.
    _A1A0764.jpg
  • Mount Assiniboine, also known as Assiniboine Mountain, is a pyramidal peak mountain located on the Great Divide, on the British Columbia/Alberta border in Canada. At 11,870 ft, it is the highest peak in the Southern Continental Ranges of the Canadian Rockies. Mt. Assiniboine rises nearly 1,525 m (5,003 ft) above Lake Magog. Because of its resemblance to the Matterhorn in the Alps, it is nicknamed the "Matterhorn of the Rockies". Mt. Assiniboine was named by George M. Dawson in 1885. When Dawson saw Mt. Assiniboine from Copper Mountain, he saw a plume of clouds trailing away from the top. This reminded him of the plumes of smoke emanating from the teepees of Assiniboine Indians. Mt. Assiniboine lies on the border between Mount Assiniboine Provincial Park, in British Columbia, and Banff National Park, in Alberta. The park does not have any roads and thus can only be reached by a six-hour hike or horse-pack 27 km, three-hour bike ride (now disallowed to reduce human / grizzly encounters) or helicopter. The usual approach is via Bryant Creek. From Canmore follow the Smith-Dorien road to the Mount Shark parking lot. The trail is well signed. A helipad is also here.
    _A1A0721.jpg
  • Mount Assiniboine, also known as Assiniboine Mountain, is a pyramidal peak mountain located on the Great Divide, on the British Columbia/Alberta border in Canada. At 11,870 ft, it is the highest peak in the Southern Continental Ranges of the Canadian Rockies. Mt. Assiniboine rises nearly 1,525 m (5,003 ft) above Lake Magog. Because of its resemblance to the Matterhorn in the Alps, it is nicknamed the "Matterhorn of the Rockies". Mt. Assiniboine was named by George M. Dawson in 1885. When Dawson saw Mt. Assiniboine from Copper Mountain, he saw a plume of clouds trailing away from the top. This reminded him of the plumes of smoke emanating from the teepees of Assiniboine Indians. Mt. Assiniboine lies on the border between Mount Assiniboine Provincial Park, in British Columbia, and Banff National Park, in Alberta. The park does not have any roads and thus can only be reached by a six-hour hike or horse-pack 27 km, three-hour bike ride (now disallowed to reduce human / grizzly encounters) or helicopter. The usual approach is via Bryant Creek. From Canmore follow the Smith-Dorien road to the Mount Shark parking lot. The trail is well signed. A helipad is also here.
    MountAssiniboineTarn2.jpg
  • Mount Assiniboine, also known as Assiniboine Mountain, is a pyramidal peak mountain located on the Great Divide, on the British Columbia/Alberta border in Canada. At 11,870 ft, it is the highest peak in the Southern Continental Ranges of the Canadian Rockies. Mt. Assiniboine rises nearly 1,525 m (5,003 ft) above Lake Magog. Because of its resemblance to the Matterhorn in the Alps, it is nicknamed the "Matterhorn of the Rockies". Mt. Assiniboine was named by George M. Dawson in 1885. When Dawson saw Mt. Assiniboine from Copper Mountain, he saw a plume of clouds trailing away from the top. This reminded him of the plumes of smoke emanating from the teepees of Assiniboine Indians. Mt. Assiniboine lies on the border between Mount Assiniboine Provincial Park, in British Columbia, and Banff National Park, in Alberta. The park does not have any roads and thus can only be reached by a six-hour hike or horse-pack 27 km, three-hour bike ride (now disallowed to reduce human / grizzly encounters) or helicopter. The usual approach is via Bryant Creek. From Canmore follow the Smith-Dorien road to the Mount Shark parking lot. The trail is well signed. A helipad is also here.
    MountAssiniboineTarn1.jpg
  • Mount Assiniboine, also known as Assiniboine Mountain, is a pyramidal peak mountain located on the Great Divide, on the British Columbia/Alberta border in Canada. At 11,870 ft, it is the highest peak in the Southern Continental Ranges of the Canadian Rockies. Mt. Assiniboine rises nearly 1,525 m (5,003 ft) above Lake Magog. Because of its resemblance to the Matterhorn in the Alps, it is nicknamed the "Matterhorn of the Rockies". Mt. Assiniboine was named by George M. Dawson in 1885. When Dawson saw Mt. Assiniboine from Copper Mountain, he saw a plume of clouds trailing away from the top. This reminded him of the plumes of smoke emanating from the teepees of Assiniboine Indians. Mt. Assiniboine lies on the border between Mount Assiniboine Provincial Park, in British Columbia, and Banff National Park, in Alberta. The park does not have any roads and thus can only be reached by a six-hour hike or horse-pack 27 km, three-hour bike ride (now disallowed to reduce human / grizzly encounters) or helicopter. The usual approach is via Bryant Creek. From Canmore follow the Smith-Dorien road to the Mount Shark parking lot. The trail is well signed. A helipad is also here.
    MtAssinniboine1.jpg
  • Mount Assiniboine Provincial Park is a provincial park in British Columbia, Canada, located around Mount Assiniboine. The park was established 1922. Some of the more recent history that is explorable within the park include Wheeler's Wonder Lodge (Naiset) (1924), Assiniboine Lodge (1928), the first ski lodge in the Canadian Rockies, and Sunburst (1928). In 1990, this park was included within the Canadian Rocky Mountain Parks UNESCO World Heritage Site. Together with the other national and provincial parks that comprise the Canadian Rocky Mountain Parks, the park was recognized for its natural beauty and the geological and ecological significance of its mountain landscapes containing the habitats of rare and endangered species, mountain peaks, glaciers, lakes, waterfalls, canyons, limestone caves and fossils.
    MtAssinniboine4.jpg
  • Mount Assiniboine, also known as Assiniboine Mountain, is a pyramidal peak mountain located on the Great Divide, on the British Columbia/Alberta border in Canada. At 11,870 ft, it is the highest peak in the Southern Continental Ranges of the Canadian Rockies. Mt. Assiniboine rises nearly 1,525 m (5,003 ft) above Lake Magog. Because of its resemblance to the Matterhorn in the Alps, it is nicknamed the "Matterhorn of the Rockies". Mt. Assiniboine was named by George M. Dawson in 1885. When Dawson saw Mt. Assiniboine from Copper Mountain, he saw a plume of clouds trailing away from the top. This reminded him of the plumes of smoke emanating from the teepees of Assiniboine Indians. Mt. Assiniboine lies on the border between Mount Assiniboine Provincial Park, in British Columbia, and Banff National Park, in Alberta. The park does not have any roads and thus can only be reached by a six-hour hike or horse-pack 27 km, three-hour bike ride (now disallowed to reduce human / grizzly encounters) or helicopter. The usual approach is via Bryant Creek. From Canmore follow the Smith-Dorien road to the Mount Shark parking lot. The trail is well signed. A helipad is also here.
    AssiniboineMeadow1.jpg
  • Mount Assiniboine, also known as Assiniboine Mountain, is a pyramidal peak mountain located on the Great Divide, on the British Columbia/Alberta border in Canada. At 11,870 ft, it is the highest peak in the Southern Continental Ranges of the Canadian Rockies. Mt. Assiniboine rises nearly 1,525 m (5,003 ft) above Lake Magog. Because of its resemblance to the Matterhorn in the Alps, it is nicknamed the "Matterhorn of the Rockies". Mt. Assiniboine was named by George M. Dawson in 1885. When Dawson saw Mt. Assiniboine from Copper Mountain, he saw a plume of clouds trailing away from the top. This reminded him of the plumes of smoke emanating from the teepees of Assiniboine Indians. Mt. Assiniboine lies on the border between Mount Assiniboine Provincial Park, in British Columbia, and Banff National Park, in Alberta. The park does not have any roads and thus can only be reached by a six-hour hike or horse-pack 27 km, three-hour bike ride (now disallowed to reduce human / grizzly encounters) or helicopter. The usual approach is via Bryant Creek. From Canmore follow the Smith-Dorien road to the Mount Shark parking lot. The trail is well signed. A helipad is also here.
    MtAssiniBoineCabin1.jpg
  • Lake Louise, named Lake of the Little Fishes by the Stoney Nakota First Nations people, is a glacial lake within Banff National Park in Alberta, Canada. It is located 5 km (3.1 mi) west of the Hamlet of Lake Louise and the Trans-Canada Highway (Highway 1). Lake Louise is named after the Princess Louise Caroline Alberta (1848–1939), the fourth daughter of Queen Victoria and the wife of the Marquess of Lorne, who was the Governor General of Canada from 1878 to 1883. The emerald colour of the water comes from rock flour carried into the lake by melt-water from the glaciers that overlook the lake. The lake has a surface of 0.8 km2 (0.31 sq mi) and is drained through the 3 km long Louise Creek into the Bow River.<br />
Fairmont's Chateau Lake Louise, one of Canada's grand railway hotels, is located on Lake Louise's eastern shore. It is a luxury resort hotel built in the early decades of the 20th century by the Canadian Pacific Railway.<br />
Moraine Lake and Lake Agnes are also accessible from Lake Louise.
    LakeLouiseRedCanoes3.jpg
  • Moraine Lake is a glacially fed lake in Banff National Park, 14 kilometres (8.7 mi) outside the Village of Lake Louise, Alberta, Canada. It is situated in the Valley of the Ten Peaks, at an elevation of approximately 6,183 feet (1,885 m). The lake has a surface area of 50 hectares (120 acres). The lake, being glacially fed, does not reach its crest until mid to late June. When it is full, it reflects a distinctive shade of blue. The colour is due to the refraction of light off the rock flour deposited in the lake on a continual basis.
    MoraineLakeClouds2.jpg
  • Highway 93 is a north-south highway in Alberta, Canada. It is also known as the Banff-Windermere Parkway south of the Trans-Canada Highway (Highway 1) and the Icefields Parkway north of the Trans-Canada Highway. It travels through Banff National Park and Jasper National Park and is maintained by Parks Canada for its entire length. It runs from the British Columbia border at Vermilion Pass in the south, where it becomes British Columbia Highway 93, to its terminus at the junction with the Yellowhead Highway (Highway 16) at Jasper. The route takes its number from U.S. Route 93, which runs uninterrupted south to central Arizona, and was initially designated as '93' in 1959.
    IcefieldsParkway10.jpg
  • Lake Louise, named Lake of the Little Fishes by the Stoney Nakota First Nations people, is a glacial lake within Banff National Park in Alberta, Canada. It is located 5 km (3.1 mi) west of the Hamlet of Lake Louise and the Trans-Canada Highway (Highway 1). Lake Louise is named after the Princess Louise Caroline Alberta (1848–1939), the fourth daughter of Queen Victoria and the wife of the Marquess of Lorne, who was the Governor General of Canada from 1878 to 1883. The emerald colour of the water comes from rock flour carried into the lake by melt-water from the glaciers that overlook the lake. The lake has a surface of 0.8 km2 (0.31 sq mi) and is drained through the 3 km long Louise Creek into the Bow River.<br />
Fairmont's Chateau Lake Louise, one of Canada's grand railway hotels, is located on Lake Louise's eastern shore. It is a luxury resort hotel built in the early decades of the 20th century by the Canadian Pacific Railway.<br />
Moraine Lake and Lake Agnes are also accessible from Lake Louise.
    LakeLouiseRedCanoes5.jpg
  • Peyto Lake is a glacier-fed lake in Banff National Park in the Canadian Rockies. The lake itself is easily accessed from the Icefields Parkway. It was named for Bill Peyto, an early trail guide and trapper in the Banff area. The lake is formed in a valley of the Waputik Range, between Caldron Peak, Peyto Peak and Mount Jimmy Simpson, at an elevation of 1,860 m (6,100 ft).<br />
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During the summer, significant amounts of glacial rock flour flow into the lake, and these suspended rock particles give the lake a bright, turquoise colour. Because of its bright colour, photos of the lake often appear in illustrated books, and the area around the lake is a popular sightseeing spot for tourists. The lake is best seen from Bow Summit, the highest point on the Icefields Parkway.<br />
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The lake is fed by Peyto Creek, which drains water from Caldron Lake and Peyto Glacier (part of the Wapta Icefield). Peyto Lake is the origin of the Mistaya River, which heads northwest from the lake's outflow.
    PeytoLake2.jpg
  • Nigel Creek is a short stream located in the Canadian Rockies of Alberta, Canada. It forms in the glacial meltwaters north of Sunwapta Pass and takes on streams flowing from Nigel Pass.<br />
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The creek flows South-Southeast, and parallels the Icefields Parkway for part of its course. It joins the North Saskatchewan River near the Big Bend. It plummets over Bridal Veil Falls before entering the North Saskatchewan. Nigel Creek is named after Nigel Vavasoeur, a packer who accompanied early climbing expeditions in the region.
    NIgelCreek2.jpg
  • Lake Louise, named Lake of the Little Fishes by the Stoney Nakota First Nations people, is a glacial lake within Banff National Park in Alberta, Canada. It is located 5 km (3.1 mi) west of the Hamlet of Lake Louise and the Trans-Canada Highway (Highway 1). Lake Louise is named after the Princess Louise Caroline Alberta (1848–1939), the fourth daughter of Queen Victoria and the wife of the Marquess of Lorne, who was the Governor General of Canada from 1878 to 1883. The emerald colour of the water comes from rock flour carried into the lake by melt-water from the glaciers that overlook the lake. The lake has a surface of 0.8 km2 (0.31 sq mi) and is drained through the 3 km long Louise Creek into the Bow River.<br />
Fairmont's Chateau Lake Louise, one of Canada's grand railway hotels, is located on Lake Louise's eastern shore. It is a luxury resort hotel built in the early decades of the 20th century by the Canadian Pacific Railway.<br />
Moraine Lake and Lake Agnes are also accessible from Lake Louise.
    LakeLouiseWinterMorning12.jpg
  • Lake Louise, named Lake of the Little Fishes by the Stoney Nakota First Nations people, is a glacial lake within Banff National Park in Alberta, Canada. It is located 5 km (3.1 mi) west of the Hamlet of Lake Louise and the Trans-Canada Highway (Highway 1). Lake Louise is named after the Princess Louise Caroline Alberta (1848–1939), the fourth daughter of Queen Victoria and the wife of the Marquess of Lorne, who was the Governor General of Canada from 1878 to 1883. The emerald colour of the water comes from rock flour carried into the lake by melt-water from the glaciers that overlook the lake. The lake has a surface of 0.8 km2 (0.31 sq mi) and is drained through the 3 km long Louise Creek into the Bow River.<br />
Fairmont's Chateau Lake Louise, one of Canada's grand railway hotels, is located on Lake Louise's eastern shore. It is a luxury resort hotel built in the early decades of the 20th century by the Canadian Pacific Railway.<br />
Moraine Lake and Lake Agnes are also accessible from Lake Louise.
    LakeLouiseWinterMorningPano1-Edit.jpg
  • Lake Louise, named Lake of the Little Fishes by the Stoney Nakota First Nations people, is a glacial lake within Banff National Park in Alberta, Canada. It is located 5 km (3.1 mi) west of the Hamlet of Lake Louise and the Trans-Canada Highway (Highway 1). Lake Louise is named after the Princess Louise Caroline Alberta (1848–1939), the fourth daughter of Queen Victoria and the wife of the Marquess of Lorne, who was the Governor General of Canada from 1878 to 1883. The emerald colour of the water comes from rock flour carried into the lake by melt-water from the glaciers that overlook the lake. The lake has a surface of 0.8 km2 (0.31 sq mi) and is drained through the 3 km long Louise Creek into the Bow River.<br />
Fairmont's Chateau Lake Louise, one of Canada's grand railway hotels, is located on Lake Louise's eastern shore. It is a luxury resort hotel built in the early decades of the 20th century by the Canadian Pacific Railway.<br />
Moraine Lake and Lake Agnes are also accessible from Lake Louise.
    LakeLouiseWinterMorning10.jpg
  • Lake Louise, named Lake of the Little Fishes by the Stoney Nakota First Nations people, is a glacial lake within Banff National Park in Alberta, Canada. It is located 5 km (3.1 mi) west of the Hamlet of Lake Louise and the Trans-Canada Highway (Highway 1). Lake Louise is named after the Princess Louise Caroline Alberta (1848–1939), the fourth daughter of Queen Victoria and the wife of the Marquess of Lorne, who was the Governor General of Canada from 1878 to 1883. The emerald colour of the water comes from rock flour carried into the lake by melt-water from the glaciers that overlook the lake. The lake has a surface of 0.8 km2 (0.31 sq mi) and is drained through the 3 km long Louise Creek into the Bow River.<br />
Fairmont's Chateau Lake Louise, one of Canada's grand railway hotels, is located on Lake Louise's eastern shore. It is a luxury resort hotel built in the early decades of the 20th century by the Canadian Pacific Railway.<br />
Moraine Lake and Lake Agnes are also accessible from Lake Louise.
    LakeLouiseWinterMorning9-Edit.jpg
  • Natural Bridge in Yoho National Park, British Columbia, Canada. <br />
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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 />
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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 />
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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 />
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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
  • Creek near Moraine Lake in Banff National Park. Banff National Park is Canada's oldest national park and was established in 1885. Located in the Rocky Mountains, 110–180 kilometres (68–112 mi) west of Calgary in the province of Alberta, Banff encompasses 6,641 square kilometres (2,564 sq mi) of mountainous terrain, with numerous glaciers and ice fields, dense coniferous forest, and alpine landscapes. The Icefields Parkway extends from Lake Louise, connecting to Jasper National Park in the north. Provincial forests and Yoho National Park are neighbours to the west, while Kootenay National Park is located to the south and Kananaskis Country to the southeast. The main commercial centre of the park is the town of Banff, in the Bow River valley.
    MoraineCreek2.jpg
  • Lake Louise, named Lake of the Little Fishes by the Stoney Nakota First Nations people, is a glacial lake within Banff National Park in Alberta, Canada. It is located 5 km (3.1 mi) west of the Hamlet of Lake Louise and the Trans-Canada Highway (Highway 1). Lake Louise is named after the Princess Louise Caroline Alberta (1848–1939), the fourth daughter of Queen Victoria and the wife of the Marquess of Lorne, who was the Governor General of Canada from 1878 to 1883. The emerald colour of the water comes from rock flour carried into the lake by melt-water from the glaciers that overlook the lake. The lake has a surface of 0.8 km2 (0.31 sq mi) and is drained through the 3 km long Louise Creek into the Bow River.<br />
Fairmont's Chateau Lake Louise, one of Canada's grand railway hotels, is located on Lake Louise's eastern shore. It is a luxury resort hotel built in the early decades of the 20th century by the Canadian Pacific Railway.<br />
Moraine Lake and Lake Agnes are also accessible from Lake Louise.
    LakeLouiseWinterMorning3.jpg
  • Lake Louise, named Lake of the Little Fishes by the Stoney Nakota First Nations people, is a glacial lake within Banff National Park in Alberta, Canada. It is located 5 km (3.1 mi) west of the Hamlet of Lake Louise and the Trans-Canada Highway (Highway 1). Lake Louise is named after the Princess Louise Caroline Alberta (1848–1939), the fourth daughter of Queen Victoria and the wife of the Marquess of Lorne, who was the Governor General of Canada from 1878 to 1883. The emerald colour of the water comes from rock flour carried into the lake by melt-water from the glaciers that overlook the lake. The lake has a surface of 0.8 km2 (0.31 sq mi) and is drained through the 3 km long Louise Creek into the Bow River.<br />
Fairmont's Chateau Lake Louise, one of Canada's grand railway hotels, is located on Lake Louise's eastern shore. It is a luxury resort hotel built in the early decades of the 20th century by the Canadian Pacific Railway.<br />
Moraine Lake and Lake Agnes are also accessible from Lake Louise.
    LakeLouiseWinterMorning2.jpg
  • Moraine Lake is a glacially fed lake in Banff National Park, 14 kilometres (8.7 mi) outside the Village of Lake Louise, Alberta, Canada. It is situated in the Valley of the Ten Peaks, at an elevation of approximately 6,183 feet (1,885 m). The lake has a surface area of 50 hectares (120 acres). The lake, being glacially fed, does not reach its crest until mid to late June. When it is full, it reflects a distinctive shade of blue. The colour is due to the refraction of light off the rock flour deposited in the lake on a continual basis.
    MoraineLake7.jpg
  • Moraine Lake is a glacially fed lake in Banff National Park, 14 kilometres (8.7 mi) outside the Village of Lake Louise, Alberta, Canada. It is situated in the Valley of the Ten Peaks, at an elevation of approximately 6,183 feet (1,885 m). The lake has a surface area of 50 hectares (120 acres). The lake, being glacially fed, does not reach its crest until mid to late June. When it is full, it reflects a distinctive shade of blue. The colour is due to the refraction of light off the rock flour deposited in the lake on a continual basis.
    MoraineLake5.jpg
  • Moraine Lake is a glacially fed lake in Banff National Park, 14 kilometres (8.7 mi) outside the Village of Lake Louise, Alberta, Canada. It is situated in the Valley of the Ten Peaks, at an elevation of approximately 6,183 feet (1,885 m). The lake has a surface area of 50 hectares (120 acres). The lake, being glacially fed, does not reach its crest until mid to late June. When it is full, it reflects a distinctive shade of blue. The colour is due to the refraction of light off the rock flour deposited in the lake on a continual basis.
    MoraineLake2.jpg
  • Lake Louise, named Lake of the Little Fishes by the Stoney Nakota First Nations people, is a glacial lake within Banff National Park in Alberta, Canada. It is located 5 km (3.1 mi) west of the Hamlet of Lake Louise and the Trans-Canada Highway (Highway 1). Lake Louise is named after the Princess Louise Caroline Alberta (1848–1939), the fourth daughter of Queen Victoria and the wife of the Marquess of Lorne, who was the Governor General of Canada from 1878 to 1883. The emerald colour of the water comes from rock flour carried into the lake by melt-water from the glaciers that overlook the lake. The lake has a surface of 0.8 km2 (0.31 sq mi) and is drained through the 3 km long Louise Creek into the Bow River.<br />
Fairmont's Chateau Lake Louise, one of Canada's grand railway hotels, is located on Lake Louise's eastern shore. It is a luxury resort hotel built in the early decades of the 20th century by the Canadian Pacific Railway.<br />
Moraine Lake and Lake Agnes are also accessible from Lake Louise.
    LakeLouiseMistyDawn3.jpg
  • Lake Louise, named Lake of the Little Fishes by the Stoney Nakota First Nations people, is a glacial lake within Banff National Park in Alberta, Canada. It is located 5 km (3.1 mi) west of the Hamlet of Lake Louise and the Trans-Canada Highway (Highway 1). Lake Louise is named after the Princess Louise Caroline Alberta (1848–1939), the fourth daughter of Queen Victoria and the wife of the Marquess of Lorne, who was the Governor General of Canada from 1878 to 1883. The emerald colour of the water comes from rock flour carried into the lake by melt-water from the glaciers that overlook the lake. The lake has a surface of 0.8 km2 (0.31 sq mi) and is drained through the 3 km long Louise Creek into the Bow River.<br />
Fairmont's Chateau Lake Louise, one of Canada's grand railway hotels, is located on Lake Louise's eastern shore. It is a luxury resort hotel built in the early decades of the 20th century by the Canadian Pacific Railway.<br />
Moraine Lake and Lake Agnes are also accessible from Lake Louise.
    LakeLouiseMistyDawn2.jpg
  • Lake Louise, named Lake of the Little Fishes by the Stoney Nakota First Nations people, is a glacial lake within Banff National Park in Alberta, Canada. It is located 5 km (3.1 mi) west of the Hamlet of Lake Louise and the Trans-Canada Highway (Highway 1). Lake Louise is named after the Princess Louise Caroline Alberta (1848–1939), the fourth daughter of Queen Victoria and the wife of the Marquess of Lorne, who was the Governor General of Canada from 1878 to 1883. The emerald colour of the water comes from rock flour carried into the lake by melt-water from the glaciers that overlook the lake. The lake has a surface of 0.8 km2 (0.31 sq mi) and is drained through the 3 km long Louise Creek into the Bow River.<br />
Fairmont's Chateau Lake Louise, one of Canada's grand railway hotels, is located on Lake Louise's eastern shore. It is a luxury resort hotel built in the early decades of the 20th century by the Canadian Pacific Railway.<br />
Moraine Lake and Lake Agnes are also accessible from Lake Louise.
    LakeLouiseCanoes2.jpg
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