Inge Johnsson Photography

Show Navigation
  • Portfolio
  • Galleries
    • All Galleries
    • Search
    • Cart
    • Lightbox
    • Client Area
  • Buy artwork at Fine Art America
  • About
  • Contact

Search Results

Refine Search
Match all words
Match any word
Prints
Personal Use
Royalty-Free
Rights-Managed
(leave unchecked to
search all images)
{ 3966 images found }

Loading ()...

  • Deadvlei is a white clay pan located near the more famous salt pan of Sossusvlei, inside the Namib-Naukluft Park in Namibia. Also written DeadVlei or Dead Vlei, its name means "dead marsh" (from English dead, and Afrikaans vlei, a lake or marsh in a valley between the dunes). The pan also is referred to as "Dooie Vlei" which is the (presumably original) fully Afrikaans name. <br />
<br />
Dead Vlei has been claimed to be surrounded by the highest sand dunes in the world, the highest reaching 300-400 meters (350m on average, named "Big Daddy" or "Crazy Dune"), which rest on a sandstone terrace.<br />
<br />
The clay pan was formed after rainfall, when the Tsauchab river flooded, creating temporary shallow pools where the abundance of water allowed camel thorn trees to grow. When the climate changed, drought hit the area, and sand dunes encroached on the pan, which blocked the river from the area.<br />
<br />
The trees died, as there no longer was enough water to survive. There are some species of plants remaining, such as salsola and clumps of !nara, adapted to surviving off the morning mist and very rare rainfall. The remaining skeletons of the trees, which are believed to have died 600-700 years ago (1340- 1430), are now black because the intense sun has scorched them. Though not petrified, the wood does not decompose because it is so dry.
    Deadvlei9.jpg
  • Deadvlei is a white clay pan located near the more famous salt pan of Sossusvlei, inside the Namib-Naukluft Park in Namibia. Also written DeadVlei or Dead Vlei, its name means "dead marsh" (from English dead, and Afrikaans vlei, a lake or marsh in a valley between the dunes). The pan also is referred to as "Dooie Vlei" which is the (presumably original) fully Afrikaans name. <br />
<br />
Dead Vlei has been claimed to be surrounded by the highest sand dunes in the world, the highest reaching 300-400 meters (350m on average, named "Big Daddy" or "Crazy Dune"), which rest on a sandstone terrace.<br />
<br />
The clay pan was formed after rainfall, when the Tsauchab river flooded, creating temporary shallow pools where the abundance of water allowed camel thorn trees to grow. When the climate changed, drought hit the area, and sand dunes encroached on the pan, which blocked the river from the area.<br />
<br />
The trees died, as there no longer was enough water to survive. There are some species of plants remaining, such as salsola and clumps of !nara, adapted to surviving off the morning mist and very rare rainfall. The remaining skeletons of the trees, which are believed to have died 600-700 years ago (1340- 1430), are now black because the intense sun has scorched them. Though not petrified, the wood does not decompose because it is so dry.
    Deadvlei4.jpg
  • Deadvlei is a white clay pan located near the more famous salt pan of Sossusvlei, inside the Namib-Naukluft Park in Namibia. Also written DeadVlei or Dead Vlei, its name means "dead marsh" (from English dead, and Afrikaans vlei, a lake or marsh in a valley between the dunes). The pan also is referred to as "Dooie Vlei" which is the (presumably original) fully Afrikaans name. <br />
<br />
Dead Vlei has been claimed to be surrounded by the highest sand dunes in the world, the highest reaching 300-400 meters (350m on average, named "Big Daddy" or "Crazy Dune"), which rest on a sandstone terrace.<br />
<br />
The clay pan was formed after rainfall, when the Tsauchab river flooded, creating temporary shallow pools where the abundance of water allowed camel thorn trees to grow. When the climate changed, drought hit the area, and sand dunes encroached on the pan, which blocked the river from the area.<br />
<br />
The trees died, as there no longer was enough water to survive. There are some species of plants remaining, such as salsola and clumps of !nara, adapted to surviving off the morning mist and very rare rainfall. The remaining skeletons of the trees, which are believed to have died 600-700 years ago (1340- 1430), are now black because the intense sun has scorched them. Though not petrified, the wood does not decompose because it is so dry.
    Deadvlei3.jpg
  • Deadvlei is a white clay pan located near the more famous salt pan of Sossusvlei, inside the Namib-Naukluft Park in Namibia. Also written DeadVlei or Dead Vlei, its name means "dead marsh" (from English dead, and Afrikaans vlei, a lake or marsh in a valley between the dunes). The pan also is referred to as "Dooie Vlei" which is the (presumably original) fully Afrikaans name. <br />
<br />
Dead Vlei has been claimed to be surrounded by the highest sand dunes in the world, the highest reaching 300-400 meters (350m on average, named "Big Daddy" or "Crazy Dune"), which rest on a sandstone terrace.<br />
<br />
The clay pan was formed after rainfall, when the Tsauchab river flooded, creating temporary shallow pools where the abundance of water allowed camel thorn trees to grow. When the climate changed, drought hit the area, and sand dunes encroached on the pan, which blocked the river from the area.<br />
<br />
The trees died, as there no longer was enough water to survive. There are some species of plants remaining, such as salsola and clumps of !nara, adapted to surviving off the morning mist and very rare rainfall. The remaining skeletons of the trees, which are believed to have died 600-700 years ago (1340- 1430), are now black because the intense sun has scorched them. Though not petrified, the wood does not decompose because it is so dry.
    Deadvlei5.jpg
  • The Quiver Tree Forest (Kokerboom Woud in Afrikaans) is a forest and tourist attraction of southern Namibia. It is located about 14 km north-east of Keetmanshoop, on the road to Koës, on the Gariganus farm. It comprises about 250 specimens of Aloe dichotoma, a species of aloe that is also locally known as "quiver tree" (Afrikaans: kokerboom) because bushmen traditionally used its branches to make quivers. The forest is spontaneous; the tallest quiver trees are two to three centuries old. The forest was declared a national monument of Namibia on June 1, 1995.<br />
Aloe dichotoma (the quiver tree or kokerboom) is a tall, branching species of aloe, indigenous to Southern Africa, specifically in the Northern Cape region of South Africa, and parts of Southern Namibia.
    QuiverTrees9.jpg
  • The Quiver Tree Forest (Kokerboom Woud in Afrikaans) is a forest and tourist attraction of southern Namibia. It is located about 14 km north-east of Keetmanshoop, on the road to Koës, on the Gariganus farm. It comprises about 250 specimens of Aloe dichotoma, a species of aloe that is also locally known as "quiver tree" (Afrikaans: kokerboom) because bushmen traditionally used its branches to make quivers. The forest is spontaneous; the tallest quiver trees are two to three centuries old. The forest was declared a national monument of Namibia on June 1, 1995.<br />
Aloe dichotoma (the quiver tree or kokerboom) is a tall, branching species of aloe, indigenous to Southern Africa, specifically in the Northern Cape region of South Africa, and parts of Southern Namibia.
    QuiverTrees12.jpg
  • The Quiver Tree Forest (Kokerboom Woud in Afrikaans) is a forest and tourist attraction of southern Namibia. It is located about 14 km north-east of Keetmanshoop, on the road to Koës, on the Gariganus farm. It comprises about 250 specimens of Aloe dichotoma, a species of aloe that is also locally known as "quiver tree" (Afrikaans: kokerboom) because bushmen traditionally used its branches to make quivers. The forest is spontaneous; the tallest quiver trees are two to three centuries old. The forest was declared a national monument of Namibia on June 1, 1995.<br />
Aloe dichotoma (the quiver tree or kokerboom) is a tall, branching species of aloe, indigenous to Southern Africa, specifically in the Northern Cape region of South Africa, and parts of Southern Namibia.
    QuiverTrees8.jpg
  • The Quiver Tree Forest (Kokerboom Woud in Afrikaans) is a forest and tourist attraction of southern Namibia. It is located about 14 km north-east of Keetmanshoop, on the road to Koës, on the Gariganus farm. It comprises about 250 specimens of Aloe dichotoma, a species of aloe that is also locally known as "quiver tree" (Afrikaans: kokerboom) because bushmen traditionally used its branches to make quivers. The forest is spontaneous; the tallest quiver trees are two to three centuries old. The forest was declared a national monument of Namibia on June 1, 1995.<br />
Aloe dichotoma (the quiver tree or kokerboom) is a tall, branching species of aloe, indigenous to Southern Africa, specifically in the Northern Cape region of South Africa, and parts of Southern Namibia.
    QuiverTrees3.jpg
  • The Quiver Tree Forest (Kokerboom Woud in Afrikaans) is a forest and tourist attraction of southern Namibia. It is located about 14 km north-east of Keetmanshoop, on the road to Koës, on the Gariganus farm. It comprises about 250 specimens of Aloe dichotoma, a species of aloe that is also locally known as "quiver tree" (Afrikaans: kokerboom) because bushmen traditionally used its branches to make quivers. The forest is spontaneous; the tallest quiver trees are two to three centuries old. The forest was declared a national monument of Namibia on June 1, 1995.<br />
Aloe dichotoma (the quiver tree or kokerboom) is a tall, branching species of aloe, indigenous to Southern Africa, specifically in the Northern Cape region of South Africa, and parts of Southern Namibia.
    QuiverTrees2.jpg
  • The Quiver Tree Forest (Kokerboom Woud in Afrikaans) is a forest and tourist attraction of southern Namibia. It is located about 14 km north-east of Keetmanshoop, on the road to Koës, on the Gariganus farm. It comprises about 250 specimens of Aloe dichotoma, a species of aloe that is also locally known as "quiver tree" (Afrikaans: kokerboom) because bushmen traditionally used its branches to make quivers. The forest is spontaneous; the tallest quiver trees are two to three centuries old. The forest was declared a national monument of Namibia on June 1, 1995.<br />
Aloe dichotoma (the quiver tree or kokerboom) is a tall, branching species of aloe, indigenous to Southern Africa, specifically in the Northern Cape region of South Africa, and parts of Southern Namibia.
    QuiverTrees13.jpg
  • The Quiver Tree Forest (Kokerboom Woud in Afrikaans) is a forest and tourist attraction of southern Namibia. It is located about 14 km north-east of Keetmanshoop, on the road to Koës, on the Gariganus farm. It comprises about 250 specimens of Aloe dichotoma, a species of aloe that is also locally known as "quiver tree" (Afrikaans: kokerboom) because bushmen traditionally used its branches to make quivers. The forest is spontaneous; the tallest quiver trees are two to three centuries old. The forest was declared a national monument of Namibia on June 1, 1995.<br />
Aloe dichotoma (the quiver tree or kokerboom) is a tall, branching species of aloe, indigenous to Southern Africa, specifically in the Northern Cape region of South Africa, and parts of Southern Namibia.
    QuiverTrees11.jpg
  • The Quiver Tree Forest (Kokerboom Woud in Afrikaans) is a forest and tourist attraction of southern Namibia. It is located about 14 km north-east of Keetmanshoop, on the road to Koës, on the Gariganus farm. It comprises about 250 specimens of Aloe dichotoma, a species of aloe that is also locally known as "quiver tree" (Afrikaans: kokerboom) because bushmen traditionally used its branches to make quivers. The forest is spontaneous; the tallest quiver trees are two to three centuries old. The forest was declared a national monument of Namibia on June 1, 1995.<br />
Aloe dichotoma (the quiver tree or kokerboom) is a tall, branching species of aloe, indigenous to Southern Africa, specifically in the Northern Cape region of South Africa, and parts of Southern Namibia.
    QuiverTrees5.jpg
  • The Quiver Tree Forest (Kokerboom Woud in Afrikaans) is a forest and tourist attraction of southern Namibia. It is located about 14 km north-east of Keetmanshoop, on the road to Koës, on the Gariganus farm. It comprises about 250 specimens of Aloe dichotoma, a species of aloe that is also locally known as "quiver tree" (Afrikaans: kokerboom) because bushmen traditionally used its branches to make quivers. The forest is spontaneous; the tallest quiver trees are two to three centuries old. The forest was declared a national monument of Namibia on June 1, 1995.<br />
Aloe dichotoma (the quiver tree or kokerboom) is a tall, branching species of aloe, indigenous to Southern Africa, specifically in the Northern Cape region of South Africa, and parts of Southern Namibia.
    QuiverTrees14.jpg
  • The Quiver Tree Forest (Kokerboom Woud in Afrikaans) is a forest and tourist attraction of southern Namibia. It is located about 14 km north-east of Keetmanshoop, on the road to Koës, on the Gariganus farm. It comprises about 250 specimens of Aloe dichotoma, a species of aloe that is also locally known as "quiver tree" (Afrikaans: kokerboom) because bushmen traditionally used its branches to make quivers. The forest is spontaneous; the tallest quiver trees are two to three centuries old. The forest was declared a national monument of Namibia on June 1, 1995.<br />
Aloe dichotoma (the quiver tree or kokerboom) is a tall, branching species of aloe, indigenous to Southern Africa, specifically in the Northern Cape region of South Africa, and parts of Southern Namibia.
    QuiverTrees6.jpg
  • The Quiver Tree Forest (Kokerboom Woud in Afrikaans) is a forest and tourist attraction of southern Namibia. It is located about 14 km north-east of Keetmanshoop, on the road to Koës, on the Gariganus farm. It comprises about 250 specimens of Aloe dichotoma, a species of aloe that is also locally known as "quiver tree" (Afrikaans: kokerboom) because bushmen traditionally used its branches to make quivers. The forest is spontaneous; the tallest quiver trees are two to three centuries old. The forest was declared a national monument of Namibia on June 1, 1995.<br />
Aloe dichotoma (the quiver tree or kokerboom) is a tall, branching species of aloe, indigenous to Southern Africa, specifically in the Northern Cape region of South Africa, and parts of Southern Namibia.
    QuiverTrees4.jpg
  • The Quiver Tree Forest (Kokerboom Woud in Afrikaans) is a forest and tourist attraction of southern Namibia. It is located about 14 km north-east of Keetmanshoop, on the road to Koës, on the Gariganus farm. It comprises about 250 specimens of Aloe dichotoma, a species of aloe that is also locally known as "quiver tree" (Afrikaans: kokerboom) because bushmen traditionally used its branches to make quivers. The forest is spontaneous; the tallest quiver trees are two to three centuries old. The forest was declared a national monument of Namibia on June 1, 1995.<br />
Aloe dichotoma (the quiver tree or kokerboom) is a tall, branching species of aloe, indigenous to Southern Africa, specifically in the Northern Cape region of South Africa, and parts of Southern Namibia.
    QuiverTrees1.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.
    PointSublimeBirches3.jpg
  • Mt Rainier at Reflection Lakes with three small trees
    MtRainierThreeTrees1.jpg
  • Mt Rainier at Reflection Lakes with three small trees
    MtRainierThreeTrees1.jpg
  • Palm trees on Promenade des Anglais in Nice, France on the French riviera
    NiceBeachSunsetPalms1.jpg
  • Mt Rainier at Reflection Lakes with three small trees
    MtRainierThreeTrees1.jpg
  • Mt Rainier at Reflection Lakes with three small trees
    MtRainierThreeTrees1.jpg
  • Palm trees along Las Vegas Boulevard, Las Vegas, Nevada
    LasVegasPalms1.jpg
  • Mt Rainier at Reflection Lakes with three small trees
    MtRainierThreeTrees1.jpg
  • Hoar frost on trees along Mazama Ridge at Mount Rainier in the winter
    MazamaTrees1.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.
    NorthRimBirches2.jpg
  • Mt Rainier at Reflection Lakes with three small trees
    MtRainierThreeTrees1.jpg
  • Mt Rainier at Reflection Lakes with three small trees
    MtRainierThreeTrees1.jpg
  • Mt Rainier at Reflection Lakes with three small trees
    MtRainierThreeTrees1.jpg
  • Snow covered trees 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.
    MoraineLakeTrees1.jpg
  • The Boulevard Oaks Historic District is one of the finest residential neighborhoods constructed during Houston’s building boom in the 1920s. It consists of seven different subdivisions, built between 1923 and 1940; the homes were designed by some of Houston’s most prominent architects. Today, the neighborhood is best known for its esplanades lined with giant oak trees, along North and South Boulevards. It is listed in the National Register of Historic Places.
    HoustonTrees1.jpg
  • The Fort Worth Japanese Garden is a 7.5-acre Japanese Garden in the Fort Worth Botanic Garden. The garden was built in 1973 and many of the plants and construction materials were donated by Fort Worth's sister city Nagaoka, Japan. Attractions at the garden include a zen garden, a moon viewing (tsukimi) deck, waterfalls, cherry trees, Japanese maples, a pagoda, and fishfood dispensers to feed the hundreds of koi in the Japanese Garden's three ponds. The garden hosts two annual events, the Spring Festival and the Fall Festival, featuring demonstrations of Japanese art and culture.
    FortWorthJapaneseGardens8.jpg
  • Trees at rim of Crater Lake, Oregon, at sunrise
    CraterLakeTrees.jpg
  • The Fort Worth Japanese Garden is a 7.5-acre Japanese Garden in the Fort Worth Botanic Garden. The garden was built in 1973 and many of the plants and construction materials were donated by Fort Worth's sister city Nagaoka, Japan. Attractions at the garden include a zen garden, a moon viewing (tsukimi) deck, waterfalls, cherry trees, Japanese maples, a pagoda, and fishfood dispensers to feed the hundreds of koi in the Japanese Garden's three ponds. The garden hosts two annual events, the Spring Festival and the Fall Festival, featuring demonstrations of Japanese art and culture.
    FortWorthJapaneseGardens8.jpg
  • Trees at rim of Crater Lake, Oregon, at sunrise
    CraterLakeTrees.jpg
  • Trees at rim of Crater Lake, Oregon, at sunrise
    CraterLakeTrees.jpg
  • The Fort Worth Japanese Garden is a 7.5-acre Japanese Garden in the Fort Worth Botanic Garden. The garden was built in 1973 and many of the plants and construction materials were donated by Fort Worth's sister city Nagaoka, Japan. Attractions at the garden include a zen garden, a moon viewing (tsukimi) deck, waterfalls, cherry trees, Japanese maples, a pagoda, and fishfood dispensers to feed the hundreds of koi in the Japanese Garden's three ponds. The garden hosts two annual events, the Spring Festival and the Fall Festival, featuring demonstrations of Japanese art and culture.
    FortWorthJapaneseGardens8.jpg
  • The Boulevard Oaks Historic District is one of the finest residential neighborhoods constructed during Houston’s building boom in the 1920s. It consists of seven different subdivisions, built between 1923 and 1940; the homes were designed by some of Houston’s most prominent architects. Today, the neighborhood is best known for its esplanades lined with giant oak trees, along North and South Boulevards. It is listed in the National Register of Historic Places.
    HoustonTrees1.jpg
  • The Fort Worth Japanese Garden is a 7.5-acre Japanese Garden in the Fort Worth Botanic Garden. The garden was built in 1973 and many of the plants and construction materials were donated by Fort Worth's sister city Nagaoka, Japan. Attractions at the garden include a zen garden, a moon viewing (tsukimi) deck, waterfalls, cherry trees, Japanese maples, a pagoda, and fishfood dispensers to feed the hundreds of koi in the Japanese Garden's three ponds. The garden hosts two annual events, the Spring Festival and the Fall Festival, featuring demonstrations of Japanese art and culture.
    FortWorthJapaneseGardens8.jpg
  • The Fort Worth Japanese Garden is a 7.5-acre Japanese Garden in the Fort Worth Botanic Garden. The garden was built in 1973 and many of the plants and construction materials were donated by Fort Worth's sister city Nagaoka, Japan. Attractions at the garden include a zen garden, a moon viewing (tsukimi) deck, waterfalls, cherry trees, Japanese maples, a pagoda, and fishfood dispensers to feed the hundreds of koi in the Japanese Garden's three ponds. The garden hosts two annual events, the Spring Festival and the Fall Festival, featuring demonstrations of Japanese art and culture.
    FortWorthJapaneseGardens8.jpg
  • The Boulevard Oaks Historic District is one of the finest residential neighborhoods constructed during Houston’s building boom in the 1920s. It consists of seven different subdivisions, built between 1923 and 1940; the homes were designed by some of Houston’s most prominent architects. Today, the neighborhood is best known for its esplanades lined with giant oak trees, along North and South Boulevards. It is listed in the National Register of Historic Places.
    HoustonTrees1.jpg
  • Black sand beach and palm trees in Hana Bay on the northeast coast of Maui, in the town of Hana.
    HanaPalmTrees2-2.jpg
  • The Boulevard Oaks Historic District is one of the finest residential neighborhoods constructed during Houston’s building boom in the 1920s. It consists of seven different subdivisions, built between 1923 and 1940; the homes were designed by some of Houston’s most prominent architects. Today, the neighborhood is best known for its esplanades lined with giant oak trees, along North and South Boulevards. It is listed in the National Register of Historic Places.
    HoustonTrees1.jpg
  • The Boulevard Oaks Historic District is one of the finest residential neighborhoods constructed during Houston’s building boom in the 1920s. It consists of seven different subdivisions, built between 1923 and 1940; the homes were designed by some of Houston’s most prominent architects. Today, the neighborhood is best known for its esplanades lined with giant oak trees, along North and South Boulevards. It is listed in the National Register of Historic Places.
    HoustonTrees1.jpg
  • Huangshan (Chinese: 黄山, literal meaning: Yellow Mountain) is a mountain range in southern Anhui province in eastern China. Vegetation on the range is thickest below 1,100 meters (3,600 ft), with trees growing up to the treeline at 1,800 meters (5,900 ft).<br />
<br />
The area is well known for its scenery, sunsets, peculiarly-shaped granite peaks, Huangshan pine trees, hot springs, winter snow, and views of the clouds from above. Huangshan is a frequent subject of traditional Chinese paintings and literature, as well as modern photography. It is a UNESCO World Heritage Site, and one of China's major tourist destinations.
    HuangshanTree1.jpg
  • The Quiver Tree Forest (Kokerboom Woud in Afrikaans) is a forest and tourist attraction of southern Namibia. It is located about 14 km north-east of Keetmanshoop, on the road to Koës, on the Gariganus farm. It comprises about 250 specimens of Aloe dichotoma, a species of aloe that is also locally known as "quiver tree" (Afrikaans: kokerboom) because bushmen traditionally used its branches to make quivers. The forest is spontaneous; the tallest quiver trees are two to three centuries old. The forest was declared a national monument of Namibia on June 1, 1995.<br />
Aloe dichotoma (the quiver tree or kokerboom) is a tall, branching species of aloe, indigenous to Southern Africa, specifically in the Northern Cape region of South Africa, and parts of Southern Namibia.
    QuiverTrees16.jpg
  • The Quiver Tree Forest (Kokerboom Woud in Afrikaans) is a forest and tourist attraction of southern Namibia. It is located about 14 km north-east of Keetmanshoop, on the road to Koës, on the Gariganus farm. It comprises about 250 specimens of Aloe dichotoma, a species of aloe that is also locally known as "quiver tree" (Afrikaans: kokerboom) because bushmen traditionally used its branches to make quivers. The forest is spontaneous; the tallest quiver trees are two to three centuries old. The forest was declared a national monument of Namibia on June 1, 1995.<br />
Aloe dichotoma (the quiver tree or kokerboom) is a tall, branching species of aloe, indigenous to Southern Africa, specifically in the Northern Cape region of South Africa, and parts of Southern Namibia.
    QuiverTrees10.jpg
  • Hoar frost on trees along Mazama Ridge at Mount Rainier in the winter
    MazamaTrees3.jpg
  • Hoar frost on trees along Mazama Ridge at Mount Rainier in the winter
    MazamaTrees3.jpg
  • Hongcun (Chinese: 宏村; pinyin: Hóngcūn; literally: "Hong village") is a village in Hongcun Town (宏村镇), Yi County, Huangshan City in the historical Huizhou region of southern Anhui Province, China, near the southwest slope of Mount Huangshan.<br />
<br />
The village is arranged in the shape of an ox with the nearby hill (Leigang Hill) interpreted as the head, and two trees standing on it as the horns. Four bridges across the Jiyin stream can be seen as the legs whilst the houses of the village form the body. Inside the “body”, the Jiyin stream represents the intestines and various lakes such as the “South Lake” (Nanhu) form the other internal organs.<br />
<br />
The architecture and carvings of the approximately 150 residences dating back to the Ming and Qing Dynasties are said to be among the best of their kind in China.[citation needed] One of the biggest of the residences open to visitors, Chenzhi Hall, also contains a small museum.<br />
<br />
Together with Xidi, the village became a UNESCO World Heritage Site in 2000. Scenes from the film Crouching Tiger, Hidden Dragon were filmed on location in Hongcun.
    HongcunBuildings1.jpg
  • Leavenworth is a city in Chelan County, Washington, in Eastern Washington United States. The entire town center is modelled on a Bavarian village.  In December Leavenworth puts on the ultimate Christmas Festival: Leavenworth’s Town and Tree Lighting.
    LeavenworthXmas-8.jpg
  • Leavenworth is a city in Chelan County, Washington, in Eastern Washington United States. The entire town center is modelled on a Bavarian village.  In December Leavenworth puts on the ultimate Christmas Festival: Leavenworth’s Town and Tree Lighting.
    LeavenworthXmas-8.jpg
  • Leavenworth is a city in Chelan County, Washington, in Eastern Washington United States. The entire town center is modelled on a Bavarian village.  In December Leavenworth puts on the ultimate Christmas Festival: Leavenworth's Town and Tree Lighting.
    LeavenworthXmas-8.jpg
  • Leavenworth is a city in Chelan County, Washington, in Eastern Washington United States. The entire town center is modelled on a Bavarian village.  In December Leavenworth puts on the ultimate Christmas Festival: Leavenworth’s Town and Tree Lighting.
    LeavenworthXmas-8.jpg
  • Leavenworth is a city in Chelan County, Washington, in Eastern Washington United States. The entire town center is modelled on a Bavarian village.  In December Leavenworth puts on the ultimate Christmas Festival: Leavenworth’s Town and Tree Lighting.
    LeavenworthXmas-8.jpg
  • Leavenworth is a city in Chelan County, Washington, in Eastern Washington United States. The entire town center is modelled on a Bavarian village.  In December Leavenworth puts on the ultimate Christmas Festival: Leavenworth’s Town and Tree Lighting.
    LeavenworthXmas-1.jpg
  • Leavenworth is a city in Chelan County, Washington, in Eastern Washington United States. The entire town center is modelled on a Bavarian village.  In December Leavenworth puts on the ultimate Christmas Festival: Leavenworth’s Town and Tree Lighting.
    LeavenworthXmas-7-Edit.jpg
  • Leavenworth is a city in Chelan County, Washington, in Eastern Washington United States. The entire town center is modelled on a Bavarian village.  In December Leavenworth puts on the ultimate Christmas Festival: Leavenworth’s Town and Tree Lighting.
    LeavenworthXmas-1.jpg
  • Deadvlei is a white clay pan located near the more famous salt pan of Sossusvlei, inside the Namib-Naukluft Park in Namibia. Also written DeadVlei or Dead Vlei, its name means "dead marsh" (from English dead, and Afrikaans vlei, a lake or marsh in a valley between the dunes). The pan also is referred to as "Dooie Vlei" which is the (presumably original) fully Afrikaans name. <br />
<br />
Dead Vlei has been claimed to be surrounded by the highest sand dunes in the world, the highest reaching 300-400 meters (350m on average, named "Big Daddy" or "Crazy Dune"), which rest on a sandstone terrace.<br />
<br />
The clay pan was formed after rainfall, when the Tsauchab river flooded, creating temporary shallow pools where the abundance of water allowed camel thorn trees to grow. When the climate changed, drought hit the area, and sand dunes encroached on the pan, which blocked the river from the area.<br />
<br />
The trees died, as there no longer was enough water to survive. There are some species of plants remaining, such as salsola and clumps of !nara, adapted to surviving off the morning mist and very rare rainfall. The remaining skeletons of the trees, which are believed to have died 600-700 years ago (1340- 1430), are now black because the intense sun has scorched them. Though not petrified, the wood does not decompose because it is so dry.
    Deadvlei12.jpg
  • Deadvlei is a white clay pan located near the more famous salt pan of Sossusvlei, inside the Namib-Naukluft Park in Namibia. Also written DeadVlei or Dead Vlei, its name means "dead marsh" (from English dead, and Afrikaans vlei, a lake or marsh in a valley between the dunes). The pan also is referred to as "Dooie Vlei" which is the (presumably original) fully Afrikaans name. <br />
<br />
Dead Vlei has been claimed to be surrounded by the highest sand dunes in the world, the highest reaching 300-400 meters (350m on average, named "Big Daddy" or "Crazy Dune"), which rest on a sandstone terrace.<br />
<br />
The clay pan was formed after rainfall, when the Tsauchab river flooded, creating temporary shallow pools where the abundance of water allowed camel thorn trees to grow. When the climate changed, drought hit the area, and sand dunes encroached on the pan, which blocked the river from the area.<br />
<br />
The trees died, as there no longer was enough water to survive. There are some species of plants remaining, such as salsola and clumps of !nara, adapted to surviving off the morning mist and very rare rainfall. The remaining skeletons of the trees, which are believed to have died 600-700 years ago (1340- 1430), are now black because the intense sun has scorched them. Though not petrified, the wood does not decompose because it is so dry.
    Deadvlei15.jpg
  • Deadvlei is a white clay pan located near the more famous salt pan of Sossusvlei, inside the Namib-Naukluft Park in Namibia. Also written DeadVlei or Dead Vlei, its name means "dead marsh" (from English dead, and Afrikaans vlei, a lake or marsh in a valley between the dunes). The pan also is referred to as "Dooie Vlei" which is the (presumably original) fully Afrikaans name. <br />
<br />
Dead Vlei has been claimed to be surrounded by the highest sand dunes in the world, the highest reaching 300-400 meters (350m on average, named "Big Daddy" or "Crazy Dune"), which rest on a sandstone terrace.<br />
<br />
The clay pan was formed after rainfall, when the Tsauchab river flooded, creating temporary shallow pools where the abundance of water allowed camel thorn trees to grow. When the climate changed, drought hit the area, and sand dunes encroached on the pan, which blocked the river from the area.<br />
<br />
The trees died, as there no longer was enough water to survive. There are some species of plants remaining, such as salsola and clumps of !nara, adapted to surviving off the morning mist and very rare rainfall. The remaining skeletons of the trees, which are believed to have died 600-700 years ago (1340- 1430), are now black because the intense sun has scorched them. Though not petrified, the wood does not decompose because it is so dry.
    Deadvlei7.jpg
  • Deadvlei is a white clay pan located near the more famous salt pan of Sossusvlei, inside the Namib-Naukluft Park in Namibia. Also written DeadVlei or Dead Vlei, its name means "dead marsh" (from English dead, and Afrikaans vlei, a lake or marsh in a valley between the dunes). The pan also is referred to as "Dooie Vlei" which is the (presumably original) fully Afrikaans name. <br />
<br />
Dead Vlei has been claimed to be surrounded by the highest sand dunes in the world, the highest reaching 300-400 meters (350m on average, named "Big Daddy" or "Crazy Dune"), which rest on a sandstone terrace.<br />
<br />
The clay pan was formed after rainfall, when the Tsauchab river flooded, creating temporary shallow pools where the abundance of water allowed camel thorn trees to grow. When the climate changed, drought hit the area, and sand dunes encroached on the pan, which blocked the river from the area.<br />
<br />
The trees died, as there no longer was enough water to survive. There are some species of plants remaining, such as salsola and clumps of !nara, adapted to surviving off the morning mist and very rare rainfall. The remaining skeletons of the trees, which are believed to have died 600-700 years ago (1340- 1430), are now black because the intense sun has scorched them. Though not petrified, the wood does not decompose because it is so dry.
    Deadvlei2.jpg
  • Deadvlei is a white clay pan located near the more famous salt pan of Sossusvlei, inside the Namib-Naukluft Park in Namibia. Also written DeadVlei or Dead Vlei, its name means "dead marsh" (from English dead, and Afrikaans vlei, a lake or marsh in a valley between the dunes). The pan also is referred to as "Dooie Vlei" which is the (presumably original) fully Afrikaans name. <br />
<br />
Dead Vlei has been claimed to be surrounded by the highest sand dunes in the world, the highest reaching 300-400 meters (350m on average, named "Big Daddy" or "Crazy Dune"), which rest on a sandstone terrace.<br />
<br />
The clay pan was formed after rainfall, when the Tsauchab river flooded, creating temporary shallow pools where the abundance of water allowed camel thorn trees to grow. When the climate changed, drought hit the area, and sand dunes encroached on the pan, which blocked the river from the area.<br />
<br />
The trees died, as there no longer was enough water to survive. There are some species of plants remaining, such as salsola and clumps of !nara, adapted to surviving off the morning mist and very rare rainfall. The remaining skeletons of the trees, which are believed to have died 600-700 years ago (1340- 1430), are now black because the intense sun has scorched them. Though not petrified, the wood does not decompose because it is so dry.
    Deadvlei1.jpg
  • Deadvlei is a white clay pan located near the more famous salt pan of Sossusvlei, inside the Namib-Naukluft Park in Namibia. Also written DeadVlei or Dead Vlei, its name means "dead marsh" (from English dead, and Afrikaans vlei, a lake or marsh in a valley between the dunes). The pan also is referred to as "Dooie Vlei" which is the (presumably original) fully Afrikaans name. <br />
<br />
Dead Vlei has been claimed to be surrounded by the highest sand dunes in the world, the highest reaching 300-400 meters (350m on average, named "Big Daddy" or "Crazy Dune"), which rest on a sandstone terrace.<br />
<br />
The clay pan was formed after rainfall, when the Tsauchab river flooded, creating temporary shallow pools where the abundance of water allowed camel thorn trees to grow. When the climate changed, drought hit the area, and sand dunes encroached on the pan, which blocked the river from the area.<br />
<br />
The trees died, as there no longer was enough water to survive. There are some species of plants remaining, such as salsola and clumps of !nara, adapted to surviving off the morning mist and very rare rainfall. The remaining skeletons of the trees, which are believed to have died 600-700 years ago (1340- 1430), are now black because the intense sun has scorched them. Though not petrified, the wood does not decompose because it is so dry.
    Deadvlei17.jpg
  • Deadvlei is a white clay pan located near the more famous salt pan of Sossusvlei, inside the Namib-Naukluft Park in Namibia. Also written DeadVlei or Dead Vlei, its name means "dead marsh" (from English dead, and Afrikaans vlei, a lake or marsh in a valley between the dunes). The pan also is referred to as "Dooie Vlei" which is the (presumably original) fully Afrikaans name. <br />
<br />
Dead Vlei has been claimed to be surrounded by the highest sand dunes in the world, the highest reaching 300-400 meters (350m on average, named "Big Daddy" or "Crazy Dune"), which rest on a sandstone terrace.<br />
<br />
The clay pan was formed after rainfall, when the Tsauchab river flooded, creating temporary shallow pools where the abundance of water allowed camel thorn trees to grow. When the climate changed, drought hit the area, and sand dunes encroached on the pan, which blocked the river from the area.<br />
<br />
The trees died, as there no longer was enough water to survive. There are some species of plants remaining, such as salsola and clumps of !nara, adapted to surviving off the morning mist and very rare rainfall. The remaining skeletons of the trees, which are believed to have died 600-700 years ago (1340- 1430), are now black because the intense sun has scorched them. Though not petrified, the wood does not decompose because it is so dry.
    Deadvlei6.jpg
  • Deadvlei is a white clay pan located near the more famous salt pan of Sossusvlei, inside the Namib-Naukluft Park in Namibia. Also written DeadVlei or Dead Vlei, its name means "dead marsh" (from English dead, and Afrikaans vlei, a lake or marsh in a valley between the dunes). The pan also is referred to as "Dooie Vlei" which is the (presumably original) fully Afrikaans name. <br />
<br />
Dead Vlei has been claimed to be surrounded by the highest sand dunes in the world, the highest reaching 300-400 meters (350m on average, named "Big Daddy" or "Crazy Dune"), which rest on a sandstone terrace.<br />
<br />
The clay pan was formed after rainfall, when the Tsauchab river flooded, creating temporary shallow pools where the abundance of water allowed camel thorn trees to grow. When the climate changed, drought hit the area, and sand dunes encroached on the pan, which blocked the river from the area.<br />
<br />
The trees died, as there no longer was enough water to survive. There are some species of plants remaining, such as salsola and clumps of !nara, adapted to surviving off the morning mist and very rare rainfall. The remaining skeletons of the trees, which are believed to have died 600-700 years ago (1340- 1430), are now black because the intense sun has scorched them. Though not petrified, the wood does not decompose because it is so dry.
    Deadvlei8.jpg
  • Huangshan (Chinese: 黄山, literal meaning: Yellow Mountain) is a mountain range in southern Anhui province in eastern China. Vegetation on the range is thickest below 1,100 meters (3,600 ft), with trees growing up to the treeline at 1,800 meters (5,900 ft).<br />
<br />
The area is well known for its scenery, sunsets, peculiarly-shaped granite peaks, Huangshan pine trees, hot springs, winter snow, and views of the clouds from above. Huangshan is a frequent subject of traditional Chinese paintings and literature, as well as modern photography. It is a UNESCO World Heritage Site, and one of China's major tourist destinations.
    FrozenHuangshan1.jpg
  • Huangshan (Chinese: 黄山, literal meaning: Yellow Mountain) is a mountain range in southern Anhui province in eastern China. Vegetation on the range is thickest below 1,100 meters (3,600 ft), with trees growing up to the treeline at 1,800 meters (5,900 ft).<br />
<br />
The area is well known for its scenery, sunsets, peculiarly-shaped granite peaks, Huangshan pine trees, hot springs, winter snow, and views of the clouds from above. Huangshan is a frequent subject of traditional Chinese paintings and literature, as well as modern photography. It is a UNESCO World Heritage Site, and one of China's major tourist destinations.
    _Y6A6325-HDR-Edit.jpg
  • Huangshan (Chinese: 黄山, literal meaning: Yellow Mountain) is a mountain range in southern Anhui province in eastern China. Vegetation on the range is thickest below 1,100 meters (3,600 ft), with trees growing up to the treeline at 1,800 meters (5,900 ft).<br />
<br />
The area is well known for its scenery, sunsets, peculiarly-shaped granite peaks, Huangshan pine trees, hot springs, winter snow, and views of the clouds from above. Huangshan is a frequent subject of traditional Chinese paintings and literature, as well as modern photography. It is a UNESCO World Heritage Site, and one of China's major tourist destinations.
    HuangshanCirclePeaks1.jpg
  • Huangshan (Chinese: 黄山, literal meaning: Yellow Mountain) is a mountain range in southern Anhui province in eastern China. Vegetation on the range is thickest below 1,100 meters (3,600 ft), with trees growing up to the treeline at 1,800 meters (5,900 ft).<br />
<br />
The area is well known for its scenery, sunsets, peculiarly-shaped granite peaks, Huangshan pine trees, hot springs, winter snow, and views of the clouds from above. Huangshan is a frequent subject of traditional Chinese paintings and literature, as well as modern photography. It is a UNESCO World Heritage Site, and one of China's major tourist destinations.
    HuangshanCirclePeaks2.jpg
  • Huangshan (Chinese: 黄山, literal meaning: Yellow Mountain) is a mountain range in southern Anhui province in eastern China. Vegetation on the range is thickest below 1,100 meters (3,600 ft), with trees growing up to the treeline at 1,800 meters (5,900 ft).<br />
<br />
The area is well known for its scenery, sunsets, peculiarly-shaped granite peaks, Huangshan pine trees, hot springs, winter snow, and views of the clouds from above. Huangshan is a frequent subject of traditional Chinese paintings and literature, as well as modern photography. It is a UNESCO World Heritage Site, and one of China's major tourist destinations.
    HuangshanBench1.jpg
  • The Fort Worth Water Gardens, built in 1974, is located on the south end of downtown Fort Worth between Houston and Commerce Streets next to the Fort Worth Convention Center. The 4.3 acre (1.7 hectare) Water Gardens were designed by noted New York architects Philip Johnson and John Burgee and were dedicated to the City of Fort Worth by the Amon G. Carter Foundation.<br />
The urban park is frequently billed as a "cooling oasis in the concrete jungle" of downtown. Its focal points are three pools of water and a terraced knoll, which helps to shield the park from adjacent Interstate 30. The quiet meditation pool is encircled with trees and features a flat, still plane of water that cascades almost 90 degrees down to a sunken walkway. The aerating pool features multiple spray fountains. The main attraction of the Water Gardens is the active pool which has water cascading 38 feet (11 m) down terraces and steps into a small pool at the bottom. The park also contains over 500 species of plants and trees.<br />
The active pool was originally built for people to be able to walk down the terraced steps and experience the water tumbling around them. It was temporarily closed to the public after four people died there on June 16, 2004. Three children and one adult drowned after one of the children fell in the pool. The water was unusually deep due to a recirculating pump malfunction and heavy rains. The park was reopened on March 4, 2007 after being made safer by reducing the depth of the main pool from 9 ft (2.7 m) to 2 ft (0.61 m).
    FortWorthWaterGardens3.jpg
  • The Fort Worth Water Gardens, built in 1974, is located on the south end of downtown Fort Worth between Houston and Commerce Streets next to the Fort Worth Convention Center. The 4.3 acre (1.7 hectare) Water Gardens were designed by noted New York architects Philip Johnson and John Burgee and were dedicated to the City of Fort Worth by the Amon G. Carter Foundation.<br />
The urban park is frequently billed as a "cooling oasis in the concrete jungle" of downtown. Its focal points are three pools of water and a terraced knoll, which helps to shield the park from adjacent Interstate 30. The quiet meditation pool is encircled with trees and features a flat, still plane of water that cascades almost 90 degrees down to a sunken walkway. The aerating pool features multiple spray fountains. The main attraction of the Water Gardens is the active pool which has water cascading 38 feet (11 m) down terraces and steps into a small pool at the bottom. The park also contains over 500 species of plants and trees.<br />
The active pool was originally built for people to be able to walk down the terraced steps and experience the water tumbling around them. It was temporarily closed to the public after four people died there on June 16, 2004. Three children and one adult drowned after one of the children fell in the pool. The water was unusually deep due to a recirculating pump malfunction and heavy rains. The park was reopened on March 4, 2007 after being made safer by reducing the depth of the main pool from 9 ft (2.7 m) to 2 ft (0.61 m).
    FortWorthWaterGardens2.jpg
  • The Fort Worth Water Gardens, built in 1974, is located on the south end of downtown Fort Worth between Houston and Commerce Streets next to the Fort Worth Convention Center. The 4.3 acre (1.7 hectare) Water Gardens were designed by noted New York architects Philip Johnson and John Burgee and were dedicated to the City of Fort Worth by the Amon G. Carter Foundation.<br />
The urban park is frequently billed as a "cooling oasis in the concrete jungle" of downtown. Its focal points are three pools of water and a terraced knoll, which helps to shield the park from adjacent Interstate 30. The quiet meditation pool is encircled with trees and features a flat, still plane of water that cascades almost 90 degrees down to a sunken walkway. The aerating pool features multiple spray fountains. The main attraction of the Water Gardens is the active pool which has water cascading 38 feet (11 m) down terraces and steps into a small pool at the bottom. The park also contains over 500 species of plants and trees.<br />
The active pool was originally built for people to be able to walk down the terraced steps and experience the water tumbling around them. It was temporarily closed to the public after four people died there on June 16, 2004. Three children and one adult drowned after one of the children fell in the pool. The water was unusually deep due to a recirculating pump malfunction and heavy rains. The park was reopened on March 4, 2007 after being made safer by reducing the depth of the main pool from 9 ft (2.7 m) to 2 ft (0.61 m).
    FWWaterGardens3.jpg
  • Huangshan (Chinese: 黄山, literal meaning: Yellow Mountain) is a mountain range in southern Anhui province in eastern China. Vegetation on the range is thickest below 1,100 meters (3,600 ft), with trees growing up to the treeline at 1,800 meters (5,900 ft).<br />
<br />
The area is well known for its scenery, sunsets, peculiarly-shaped granite peaks, Huangshan pine trees, hot springs, winter snow, and views of the clouds from above. Huangshan is a frequent subject of traditional Chinese paintings and literature, as well as modern photography. It is a UNESCO World Heritage Site, and one of China's major tourist destinations.
    HuangshanCirclePeaks1.jpg
  • Huangshan (Chinese: 黄山, literal meaning: Yellow Mountain) is a mountain range in southern Anhui province in eastern China. Vegetation on the range is thickest below 1,100 meters (3,600 ft), with trees growing up to the treeline at 1,800 meters (5,900 ft).<br />
<br />
The area is well known for its scenery, sunsets, peculiarly-shaped granite peaks, Huangshan pine trees, hot springs, winter snow, and views of the clouds from above. Huangshan is a frequent subject of traditional Chinese paintings and literature, as well as modern photography. It is a UNESCO World Heritage Site, and one of China's major tourist destinations.
    HuangshanGrandCanyon1.jpg
  • The Fort Worth Water Gardens, built in 1974, is located on the south end of downtown Fort Worth between Houston and Commerce Streets next to the Fort Worth Convention Center. The 4.3 acre (1.7 hectare) Water Gardens were designed by noted New York architects Philip Johnson and John Burgee and were dedicated to the City of Fort Worth by the Amon G. Carter Foundation.<br />
The urban park is frequently billed as a "cooling oasis in the concrete jungle" of downtown. Its focal points are three pools of water and a terraced knoll, which helps to shield the park from adjacent Interstate 30. The quiet meditation pool is encircled with trees and features a flat, still plane of water that cascades almost 90 degrees down to a sunken walkway. The aerating pool features multiple spray fountains. The main attraction of the Water Gardens is the active pool which has water cascading 38 feet (11 m) down terraces and steps into a small pool at the bottom. The park also contains over 500 species of plants and trees.<br />
The active pool was originally built for people to be able to walk down the terraced steps and experience the water tumbling around them. It was temporarily closed to the public after four people died there on June 16, 2004. Three children and one adult drowned after one of the children fell in the pool. The water was unusually deep due to a recirculating pump malfunction and heavy rains. The park was reopened on March 4, 2007 after being made safer by reducing the depth of the main pool from 9 ft (2.7 m) to 2 ft (0.61 m).
    _D3_1758.jpg
  • The Fort Worth Water Gardens, built in 1974, is located on the south end of downtown Fort Worth between Houston and Commerce Streets next to the Fort Worth Convention Center. The 4.3 acre (1.7 hectare) Water Gardens were designed by noted New York architects Philip Johnson and John Burgee and were dedicated to the City of Fort Worth by the Amon G. Carter Foundation.<br />
The urban park is frequently billed as a "cooling oasis in the concrete jungle" of downtown. Its focal points are three pools of water and a terraced knoll, which helps to shield the park from adjacent Interstate 30. The quiet meditation pool is encircled with trees and features a flat, still plane of water that cascades almost 90 degrees down to a sunken walkway. The aerating pool features multiple spray fountains. The main attraction of the Water Gardens is the active pool which has water cascading 38 feet (11 m) down terraces and steps into a small pool at the bottom. The park also contains over 500 species of plants and trees.<br />
The active pool was originally built for people to be able to walk down the terraced steps and experience the water tumbling around them. It was temporarily closed to the public after four people died there on June 16, 2004. Three children and one adult drowned after one of the children fell in the pool. The water was unusually deep due to a recirculating pump malfunction and heavy rains. The park was reopened on March 4, 2007 after being made safer by reducing the depth of the main pool from 9 ft (2.7 m) to 2 ft (0.61 m).
    FortWorthWaterGardens4.jpg
  • The Fort Worth Water Gardens, built in 1974, is located on the south end of downtown Fort Worth between Houston and Commerce Streets next to the Fort Worth Convention Center. The 4.3 acre (1.7 hectare) Water Gardens were designed by noted New York architects Philip Johnson and John Burgee and were dedicated to the City of Fort Worth by the Amon G. Carter Foundation.<br />
The urban park is frequently billed as a "cooling oasis in the concrete jungle" of downtown. Its focal points are three pools of water and a terraced knoll, which helps to shield the park from adjacent Interstate 30. The quiet meditation pool is encircled with trees and features a flat, still plane of water that cascades almost 90 degrees down to a sunken walkway. The aerating pool features multiple spray fountains. The main attraction of the Water Gardens is the active pool which has water cascading 38 feet (11 m) down terraces and steps into a small pool at the bottom. The park also contains over 500 species of plants and trees.<br />
The active pool was originally built for people to be able to walk down the terraced steps and experience the water tumbling around them. It was temporarily closed to the public after four people died there on June 16, 2004. Three children and one adult drowned after one of the children fell in the pool. The water was unusually deep due to a recirculating pump malfunction and heavy rains. The park was reopened on March 4, 2007 after being made safer by reducing the depth of the main pool from 9 ft (2.7 m) to 2 ft (0.61 m).
    FortWorthWaterGardens1.jpg
  • The Fort Worth Water Gardens, built in 1974, is located on the south end of downtown Fort Worth between Houston and Commerce Streets next to the Fort Worth Convention Center. The 4.3 acre (1.7 hectare) Water Gardens were designed by noted New York architects Philip Johnson and John Burgee and were dedicated to the City of Fort Worth by the Amon G. Carter Foundation.<br />
The urban park is frequently billed as a "cooling oasis in the concrete jungle" of downtown. Its focal points are three pools of water and a terraced knoll, which helps to shield the park from adjacent Interstate 30. The quiet meditation pool is encircled with trees and features a flat, still plane of water that cascades almost 90 degrees down to a sunken walkway. The aerating pool features multiple spray fountains. The main attraction of the Water Gardens is the active pool which has water cascading 38 feet (11 m) down terraces and steps into a small pool at the bottom. The park also contains over 500 species of plants and trees.<br />
The active pool was originally built for people to be able to walk down the terraced steps and experience the water tumbling around them. It was temporarily closed to the public after four people died there on June 16, 2004. Three children and one adult drowned after one of the children fell in the pool. The water was unusually deep due to a recirculating pump malfunction and heavy rains. The park was reopened on March 4, 2007 after being made safer by reducing the depth of the main pool from 9 ft (2.7 m) to 2 ft (0.61 m).
    FWWaterGardens2.jpg
  • Bluebonnets and trees near Kingsland in the Texas Hill Country. Lupinus texensis, the Texas bluebonnet, is a species of lupine endemic to Texas. With other related species of lupines also called bluebonnets, it is the state flower of Texas. It is a biennial plant which begins its life as a small, gravel-like seed. The seed has a hard seed coat that must be penetrated by wind, rain, and weather over the course of a few months (but sometimes several years). In the fall, the bluebonnets emerge as small seedings with two cotyledons, and later a rosette of leaves that are palmately compound with 5-7 leaflets 3-10 cm long, green with a faint white edge and hair. Growth continues over the mild winter months and then in the spring will take off and rapidly grow larger, before sending up a 20-50 cm tall plume of blue flowers (with bits of white and occasionally a tinge of pinkish-red). The scent of these blossoms has been diversely described; many people say they give off no scent at all, while a few have described the scent as 'sickly sweet'. It has been found in the wild with isolated mutations in other colors, most notably all-white flowers, pink, and maroon. These mutations have since been selectively bred to produce different color strains that are available commercially.
    KingslandTree1.jpg
  • Bluebonnets and trees near Kingsland in the Texas Hill Country
    _D3_3855.jpg
  • Bluebonnets and trees near Kingsland in the Texas Hill Country. Lupinus texensis, the Texas bluebonnet, is a species of lupine endemic to Texas. With other related species of lupines also called bluebonnets, it is the state flower of Texas. It is a biennial plant which begins its life as a small, gravel-like seed. The seed has a hard seed coat that must be penetrated by wind, rain, and weather over the course of a few months (but sometimes several years). In the fall, the bluebonnets emerge as small seedings with two cotyledons, and later a rosette of leaves that are palmately compound with 5-7 leaflets 3-10 cm long, green with a faint white edge and hair. Growth continues over the mild winter months and then in the spring will take off and rapidly grow larger, before sending up a 20-50 cm tall plume of blue flowers (with bits of white and occasionally a tinge of pinkish-red). The scent of these blossoms has been diversely described; many people say they give off no scent at all, while a few have described the scent as 'sickly sweet'. It has been found in the wild with isolated mutations in other colors, most notably all-white flowers, pink, and maroon. These mutations have since been selectively bred to produce different color strains that are available commercially.
    KingslandTree1.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
  • 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
  • Snow and trees in Mount Rainier National Park in the winter.
    MountRainierWinter1.jpg
  • Bluebonnets and trees near Kingsland in the Texas Hill Country. Lupinus texensis, the Texas bluebonnet, is a species of lupine endemic to Texas. With other related species of lupines also called bluebonnets, it is the state flower of Texas. It is a biennial plant which begins its life as a small, gravel-like seed. The seed has a hard seed coat that must be penetrated by wind, rain, and weather over the course of a few months (but sometimes several years). In the fall, the bluebonnets emerge as small seedings with two cotyledons, and later a rosette of leaves that are palmately compound with 5-7 leaflets 3-10 cm long, green with a faint white edge and hair. Growth continues over the mild winter months and then in the spring will take off and rapidly grow larger, before sending up a 20-50 cm tall plume of blue flowers (with bits of white and occasionally a tinge of pinkish-red). The scent of these blossoms has been diversely described; many people say they give off no scent at all, while a few have described the scent as 'sickly sweet'. It has been found in the wild with isolated mutations in other colors, most notably all-white flowers, pink, and maroon. These mutations have since been selectively bred to produce different color strains that are available commercially.
    KingslandTree1.jpg
  • Bluebonnets and trees near Kingsland in the Texas Hill Country. Lupinus texensis, the Texas bluebonnet, is a species of lupine endemic to Texas. With other related species of lupines also called bluebonnets, it is the state flower of Texas. It is a biennial plant which begins its life as a small, gravel-like seed. The seed has a hard seed coat that must be penetrated by wind, rain, and weather over the course of a few months (but sometimes several years). In the fall, the bluebonnets emerge as small seedings with two cotyledons, and later a rosette of leaves that are palmately compound with 5-7 leaflets 3-10 cm long, green with a faint white edge and hair. Growth continues over the mild winter months and then in the spring will take off and rapidly grow larger, before sending up a 20-50 cm tall plume of blue flowers (with bits of white and occasionally a tinge of pinkish-red). The scent of these blossoms has been diversely described; many people say they give off no scent at all, while a few have described the scent as 'sickly sweet'. It has been found in the wild with isolated mutations in other colors, most notably all-white flowers, pink, and maroon. These mutations have since been selectively bred to produce different color strains that are available commercially.
    KingslandTree1.jpg
  • Bluebonnets and trees near Kingsland in the Texas Hill Country. Lupinus texensis, the Texas bluebonnet, is a species of lupine endemic to Texas. With other related species of lupines also called bluebonnets, it is the state flower of Texas. It is a biennial plant which begins its life as a small, gravel-like seed. The seed has a hard seed coat that must be penetrated by wind, rain, and weather over the course of a few months (but sometimes several years). In the fall, the bluebonnets emerge as small seedings with two cotyledons, and later a rosette of leaves that are palmately compound with 5-7 leaflets 3-10 cm long, green with a faint white edge and hair. Growth continues over the mild winter months and then in the spring will take off and rapidly grow larger, before sending up a 20-50 cm tall plume of blue flowers (with bits of white and occasionally a tinge of pinkish-red). The scent of these blossoms has been diversely described; many people say they give off no scent at all, while a few have described the scent as 'sickly sweet'. It has been found in the wild with isolated mutations in other colors, most notably all-white flowers, pink, and maroon. These mutations have since been selectively bred to produce different color strains that are available commercially.
    KingslandTree1.jpg
  • Bluebonnets and trees near Kingsland in the Texas Hill Country
    _D3_3859.jpg
  • Palm trees on Promenade des Anglais in Nice, France on the French riviera
    NicePromenade.jpg
  • Bluebonnets and trees near Kingsland in the Texas Hill Country. Lupinus texensis, the Texas bluebonnet, is a species of lupine endemic to Texas. With other related species of lupines also called bluebonnets, it is the state flower of Texas. It is a biennial plant which begins its life as a small, gravel-like seed. The seed has a hard seed coat that must be penetrated by wind, rain, and weather over the course of a few months (but sometimes several years). In the fall, the bluebonnets emerge as small seedings with two cotyledons, and later a rosette of leaves that are palmately compound with 5-7 leaflets 3-10 cm long, green with a faint white edge and hair. Growth continues over the mild winter months and then in the spring will take off and rapidly grow larger, before sending up a 20-50 cm tall plume of blue flowers (with bits of white and occasionally a tinge of pinkish-red). The scent of these blossoms has been diversely described; many people say they give off no scent at all, while a few have described the scent as 'sickly sweet'. It has been found in the wild with isolated mutations in other colors, most notably all-white flowers, pink, and maroon. These mutations have since been selectively bred to produce different color strains that are available commercially.
    KingslandTree1.jpg
  • Aspens grove in the San Juan mountains of Colorado with the Ulysses Grant Peak looming above the trees
    ColoradoOrfirMountain1.jpg
  • Bluebonnets and trees near Kingsland in the Texas Hill Country
    _D3_3848.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.
    PointSublimeBirches2.jpg
  • Mountain Larches at Maple Pass in North Cascades National Park
    LakeAnnLarches1.jpg
  • Larch trees at Crystal Lake in the Enchantment Lakes wilderness
    EnchantmentsCrystalLake1.jpg
  • Tamaracks and Prussik Peak in Washington's Enchantment Lakes wilderness area<br />
.....<br />
The Enchantments is an area comprising an upper and a lower basin, the lakes and tarns contained within them, and the peaks of the Stuart Range bounding the basins. The area is located entirely within the Alpine Lakes Wilderness about 15 miles southwest of Leavenworth, Washington in the United States. The Enchantments is regarded as one of the most spectacular locations in the Cascade Range. The first European American to discover the area and name it was A.H. Sylvester, topographer for the US Geological Survey and first supervisor of the Wenatchee National Forest. Sylvester visited the middle Enchantment basin and probably did not venture into the upper basin. Snow Creek Glacier covered more of the upper basin at the time than it does today, which may have discouraged him from exploring the higher areas. He is credited with naming some of the features in the region.<br />
<br />
By the 1940s climbers discovered the area and began naming the crags. Bill and Peg Stark of Leavenworth, became frequent visitors who drew upon various mythologies to name features of the landscape. When they made their first visit in the fall of 1959, they were captivated by the golden splendor of the larch trees in the fall, the numerous lakes and tarns, and jagged peaks towering above. They used fairy names such as Gnome Tarn, Troll Sink, Naiad Lake (officially Temple Lake), Sprite and King Arthur legends in the Lower Enchantment Basin because "the lower basin was not as austere as the upper basin," according to Peg. They used Norse names and mythology for features of the upper basin, for example Brynhild Lake (officially Inspiration Lake), Lake Freya (officially Tranquil Lake), and Valhalla Cirque because, Peg said, it felt "as if the Ice Age had just gone off."<br />
<br />
The official naming rulings of the US Board on Geographic Names in the 1960s resulted in a mixture of two name sets being adopted as official, particularly
    EnchantmentsRiver2.jpg
  • Two larch trees, or tamaracks, along the Maple Pass loop trail in North Cascades national park
    TwoLarches.jpg
  • Larch trees at Enchantment Lakes
    EnchantmentsPerfectionLakeLarches1.jpg
Next
  • Facebook
  • Twitter
x