Inge Johnsson Photography

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  • Grey fox in Chile's Torres del Paine national park. The South American gray fox (Lycalopex griseus), also known as the Patagonian fox, the chilla, or the grey zorro, is a species of zorro, the "false" foxes. The South American gray fox is found in the Southern Cone of South America, particularly in Argentina and Chile. Its range comprises a stripe, both sides of the Andes Mountain Range between parallels 17ºS (northernmost Chile) and 54ºS (Tierra del Fuego).<br />
<br />
In Argentina, this species inhabits the western semiarid region of the country, from the Andean spurs (ca. 69ºW) to meridian 66ºW. South from the Río Grande, the distribution of the fox widens reaching the Atlantic coast. In Chile, it is present throughout the country. Its presence in Peru has been mentioned; to date, however, there has been no confirmation of it. The South American gray fox was introduced to the Falkland Islands in the late 1920s early 1930s and is still present in quite large numbers on Beaver and Weddell Islands plus several smaller islands.<br />
<br />
The South American gray fox occurs in a variety of habitats, from the warm, arid scrublands of the Argentine Monte and the cold, arid Patagonian steppe to the forest of southernmost Chile.
    _D3_3649.jpg
  • Grey fox in Chile's Torres del Paine national park. The South American gray fox (Lycalopex griseus), also known as the Patagonian fox, the chilla, or the grey zorro, is a species of zorro, the "false" foxes. The South American gray fox is found in the Southern Cone of South America, particularly in Argentina and Chile. Its range comprises a stripe, both sides of the Andes Mountain Range between parallels 17ºS (northernmost Chile) and 54ºS (Tierra del Fuego).<br />
<br />
In Argentina, this species inhabits the western semiarid region of the country, from the Andean spurs (ca. 69ºW) to meridian 66ºW. South from the Río Grande, the distribution of the fox widens reaching the Atlantic coast. In Chile, it is present throughout the country. Its presence in Peru has been mentioned; to date, however, there has been no confirmation of it. The South American gray fox was introduced to the Falkland Islands in the late 1920s early 1930s and is still present in quite large numbers on Beaver and Weddell Islands plus several smaller islands.<br />
<br />
The South American gray fox occurs in a variety of habitats, from the warm, arid scrublands of the Argentine Monte and the cold, arid Patagonian steppe to the forest of southernmost Chile.
    _D3_3658.jpg
  • Grey fox in Chile's Torres del Paine national park. The South American gray fox (Lycalopex griseus), also known as the Patagonian fox, the chilla, or the grey zorro, is a species of zorro, the "false" foxes. The South American gray fox is found in the Southern Cone of South America, particularly in Argentina and Chile. Its range comprises a stripe, both sides of the Andes Mountain Range between parallels 17ºS (northernmost Chile) and 54ºS (Tierra del Fuego).<br />
<br />
In Argentina, this species inhabits the western semiarid region of the country, from the Andean spurs (ca. 69ºW) to meridian 66ºW. South from the Río Grande, the distribution of the fox widens reaching the Atlantic coast. In Chile, it is present throughout the country. Its presence in Peru has been mentioned; to date, however, there has been no confirmation of it. The South American gray fox was introduced to the Falkland Islands in the late 1920s early 1930s and is still present in quite large numbers on Beaver and Weddell Islands plus several smaller islands.<br />
<br />
The South American gray fox occurs in a variety of habitats, from the warm, arid scrublands of the Argentine Monte and the cold, arid Patagonian steppe to the forest of southernmost Chile.
    _D3_3665.jpg
  • Grey fox in Chile's Torres del Paine national park. The South American gray fox (Lycalopex griseus), also known as the Patagonian fox, the chilla, or the grey zorro, is a species of zorro, the "false" foxes. The South American gray fox is found in the Southern Cone of South America, particularly in Argentina and Chile. Its range comprises a stripe, both sides of the Andes Mountain Range between parallels 17ºS (northernmost Chile) and 54ºS (Tierra del Fuego).<br />
<br />
In Argentina, this species inhabits the western semiarid region of the country, from the Andean spurs (ca. 69ºW) to meridian 66ºW. South from the Río Grande, the distribution of the fox widens reaching the Atlantic coast. In Chile, it is present throughout the country. Its presence in Peru has been mentioned; to date, however, there has been no confirmation of it. The South American gray fox was introduced to the Falkland Islands in the late 1920s early 1930s and is still present in quite large numbers on Beaver and Weddell Islands plus several smaller islands.<br />
<br />
The South American gray fox occurs in a variety of habitats, from the warm, arid scrublands of the Argentine Monte and the cold, arid Patagonian steppe to the forest of southernmost Chile.
    GreyFox1.jpg
  • Dead branch creating a stark reflection in Rampart Lakes in the Alpine Lakes Wilderness area of Washington state
    RampartsLakesLimb.jpg
  • Dead branch creating a stark reflection in Rampart Lakes in the Alpine Lakes Wilderness area of Washington state
    RampartsLakesLimb.jpg
  • Chinese figurine at the Royal Palace in Bangkok, Thailand<br />
.....<br />
The Grand Palace is a complex of buildings at the heart of Bangkok, Thailand. The palace has been the official residence of the Kings of Siam (and later Thailand) since 1782. The king, his court and his royal government were based on the grounds of the palace until 1925. King Bhumibol Adulyadej (Rama IX), resided at Chitralada Royal Villa in the Dusit Palace, but the Grand Palace is still used for official events. Several royal ceremonies and state functions are held within the walls of the palace every year. The palace is one of the most popular tourist attractions in Thailand.<br />
Construction of the palace began on May 6, 1782, at the order of King Buddha Yodfa Chulaloke (Rama I), the founder of the Chakri Dynasty, when he moved the capital city from Thonburi to Bangkok. Throughout successive reigns, many new buildings and structures were added, especially during the reign of King Chulalongkorn (Rama V). By 1925, the king, the Royal Family and the government were no longer permanently settled at the palace, and had moved to other residences. After the abolition of absolute monarchy in 1932, all government agencies completely moved out of the palace.<br />
It is situated on the banks of the Chao Phraya River at the heart of the Rattanakosin Island, today in the Phra Nakhon District. Rather than being a single structure, the Grand Palace is made up of numerous buildings, halls, pavilions set around open lawns, gardens and courtyards. Its asymmetry and eclectic styles are due to its organic development, with additions and rebuilding being made by successive reigning kings over 200 years of history. It is divided into several quarters: the Temple of the Emerald Buddha; the Outer Court, with many public buildings; the Middle Court, including the Phra Maha Monthien Buildings, the Phra Maha Prasat Buildings and the Chakri Maha Prasat Buildings; the Inner Court and the Siwalai Gardens quarter. The Grand Palace is curr
    AmarindraWinitchaiStatue1.jpg
  • Neah Bay is a census-designated place (CDP) on the Makah Indian reservation in Clallam County, Washington, United States.
    NeahBay1.jpg
  • Lost Maples State Natural Area is located about 5 miles north of Vanderpool, Texas and 71 miles west of San Antonio. The park sits along the Sabinal River in western Bandera County and far eastern Real County. The land for Lost Maples State Natural Area was acquired by the state of Texas in 1973 and 1974, and the park was opened to the public in 1979. In 1980, the Heritage Conservation and Recreation Service made the park a National Natural Landmark. This area along the upper Sabinal River was inhabited in prehistoric times. The recorded history of the area, beginning with Spanish explorations in the 17th century, identified a number of Indian groups, including the Apache, Lipan Apache and Comanche.<br />
<br />
Much of the park's limestone bedrock is exposed on elevated terrain, which has a shallow, discontinuous cover of dark gray stony clay (Eckrant series). Most valley bottoms have deep, dark brown silty clay (Krum series) or clay loam (Pratley series). Deposits of gravel, sand, and loam (Orif-Boerne association) lie within a few hundred feet of the Sabinal River. All of these soils have free calcium carbonate throughout their profiles and are moderately alkaline. Despite a high clay content in most cases, poorly drained soils are too inextensive to be mapped.<br />
<br />
Among the trees are American Sycamore (Platanus occidentalis), Bald Cypress (Taxodium distichum), Black Walnut (Juglans nigra), Pecan (Carya illinoinensis), Green Ash (Fraxinus pennsylvanica), Black Willow (Salix nigra), Chinkapin Oak (Quercus muehlenbergii), Lacey Oak (Quercus laceyi), Texas Red Oak (Quercus buckleyi), Juniper, Florida Basswood (Tilia caroliniana) and Bigtooth Maple (Acer grandidentatum) (the latter of which was discovered far removed from any maple forest, and thus gave the area the name "lost maples"). Maple colors are brilliant unless autumn is mild; the Texas red oak gives a good display almost every year. This park is most crowded when the fall colors peak in November. Evidence suggests that th
    LostMaplesReflection.jpg
  • Lost Maples State Natural Area is located about 5 miles north of Vanderpool, Texas and 71 miles west of San Antonio. The park sits along the Sabinal River in western Bandera County and far eastern Real County. The land for Lost Maples State Natural Area was acquired by the state of Texas in 1973 and 1974, and the park was opened to the public in 1979. In 1980, the Heritage Conservation and Recreation Service made the park a National Natural Landmark. This area along the upper Sabinal River was inhabited in prehistoric times. The recorded history of the area, beginning with Spanish explorations in the 17th century, identified a number of Indian groups, including the Apache, Lipan Apache and Comanche.<br />
<br />
Much of the park's limestone bedrock is exposed on elevated terrain, which has a shallow, discontinuous cover of dark gray stony clay (Eckrant series). Most valley bottoms have deep, dark brown silty clay (Krum series) or clay loam (Pratley series). Deposits of gravel, sand, and loam (Orif-Boerne association) lie within a few hundred feet of the Sabinal River. All of these soils have free calcium carbonate throughout their profiles and are moderately alkaline. Despite a high clay content in most cases, poorly drained soils are too inextensive to be mapped.<br />
<br />
Among the trees are American Sycamore (Platanus occidentalis), Bald Cypress (Taxodium distichum), Black Walnut (Juglans nigra), Pecan (Carya illinoinensis), Green Ash (Fraxinus pennsylvanica), Black Willow (Salix nigra), Chinkapin Oak (Quercus muehlenbergii), Lacey Oak (Quercus laceyi), Texas Red Oak (Quercus buckleyi), Juniper, Florida Basswood (Tilia caroliniana) and Bigtooth Maple (Acer grandidentatum) (the latter of which was discovered far removed from any maple forest, and thus gave the area the name "lost maples"). Maple colors are brilliant unless autumn is mild; the Texas red oak gives a good display almost every year. This park is most crowded when the fall colors peak in November. Evidence suggests that th
    LostMaplesReflection.jpg
  • Lost Maples State Natural Area is located about 5 miles north of Vanderpool, Texas and 71 miles west of San Antonio. The park sits along the Sabinal River in western Bandera County and far eastern Real County. The land for Lost Maples State Natural Area was acquired by the state of Texas in 1973 and 1974, and the park was opened to the public in 1979. In 1980, the Heritage Conservation and Recreation Service made the park a National Natural Landmark. This area along the upper Sabinal River was inhabited in prehistoric times. The recorded history of the area, beginning with Spanish explorations in the 17th century, identified a number of Indian groups, including the Apache, Lipan Apache and Comanche.<br />
<br />
Much of the park's limestone bedrock is exposed on elevated terrain, which has a shallow, discontinuous cover of dark gray stony clay (Eckrant series). Most valley bottoms have deep, dark brown silty clay (Krum series) or clay loam (Pratley series). Deposits of gravel, sand, and loam (Orif-Boerne association) lie within a few hundred feet of the Sabinal River. All of these soils have free calcium carbonate throughout their profiles and are moderately alkaline. Despite a high clay content in most cases, poorly drained soils are too inextensive to be mapped.<br />
<br />
Among the trees are American Sycamore (Platanus occidentalis), Bald Cypress (Taxodium distichum), Black Walnut (Juglans nigra), Pecan (Carya illinoinensis), Green Ash (Fraxinus pennsylvanica), Black Willow (Salix nigra), Chinkapin Oak (Quercus muehlenbergii), Lacey Oak (Quercus laceyi), Texas Red Oak (Quercus buckleyi), Juniper, Florida Basswood (Tilia caroliniana) and Bigtooth Maple (Acer grandidentatum) (the latter of which was discovered far removed from any maple forest, and thus gave the area the name "lost maples"). Maple colors are brilliant unless autumn is mild; the Texas red oak gives a good display almost every year. This park is most crowded when the fall colors peak in November. Evidence suggests that th
    LostMaplesReflection.jpg
  • Lost Maples State Natural Area is located about 5 miles north of Vanderpool, Texas and 71 miles west of San Antonio. The park sits along the Sabinal River in western Bandera County and far eastern Real County. The land for Lost Maples State Natural Area was acquired by the state of Texas in 1973 and 1974, and the park was opened to the public in 1979. In 1980, the Heritage Conservation and Recreation Service made the park a National Natural Landmark. This area along the upper Sabinal River was inhabited in prehistoric times. The recorded history of the area, beginning with Spanish explorations in the 17th century, identified a number of Indian groups, including the Apache, Lipan Apache and Comanche.<br />
<br />
Much of the park's limestone bedrock is exposed on elevated terrain, which has a shallow, discontinuous cover of dark gray stony clay (Eckrant series). Most valley bottoms have deep, dark brown silty clay (Krum series) or clay loam (Pratley series). Deposits of gravel, sand, and loam (Orif-Boerne association) lie within a few hundred feet of the Sabinal River. All of these soils have free calcium carbonate throughout their profiles and are moderately alkaline. Despite a high clay content in most cases, poorly drained soils are too inextensive to be mapped.<br />
<br />
Among the trees are American Sycamore (Platanus occidentalis), Bald Cypress (Taxodium distichum), Black Walnut (Juglans nigra), Pecan (Carya illinoinensis), Green Ash (Fraxinus pennsylvanica), Black Willow (Salix nigra), Chinkapin Oak (Quercus muehlenbergii), Lacey Oak (Quercus laceyi), Texas Red Oak (Quercus buckleyi), Juniper, Florida Basswood (Tilia caroliniana) and Bigtooth Maple (Acer grandidentatum) (the latter of which was discovered far removed from any maple forest, and thus gave the area the name "lost maples"). Maple colors are brilliant unless autumn is mild; the Texas red oak gives a good display almost every year. This park is most crowded when the fall colors peak in November. Evidence suggests that th
    LostMaplesReflection.jpg
  • Lost Maples State Natural Area is located about 5 miles north of Vanderpool, Texas and 71 miles west of San Antonio. The park sits along the Sabinal River in western Bandera County and far eastern Real County. The land for Lost Maples State Natural Area was acquired by the state of Texas in 1973 and 1974, and the park was opened to the public in 1979. In 1980, the Heritage Conservation and Recreation Service made the park a National Natural Landmark. This area along the upper Sabinal River was inhabited in prehistoric times. The recorded history of the area, beginning with Spanish explorations in the 17th century, identified a number of Indian groups, including the Apache, Lipan Apache and Comanche.<br />
<br />
Much of the park's limestone bedrock is exposed on elevated terrain, which has a shallow, discontinuous cover of dark gray stony clay (Eckrant series). Most valley bottoms have deep, dark brown silty clay (Krum series) or clay loam (Pratley series). Deposits of gravel, sand, and loam (Orif-Boerne association) lie within a few hundred feet of the Sabinal River. All of these soils have free calcium carbonate throughout their profiles and are moderately alkaline. Despite a high clay content in most cases, poorly drained soils are too inextensive to be mapped.<br />
<br />
Among the trees are American Sycamore (Platanus occidentalis), Bald Cypress (Taxodium distichum), Black Walnut (Juglans nigra), Pecan (Carya illinoinensis), Green Ash (Fraxinus pennsylvanica), Black Willow (Salix nigra), Chinkapin Oak (Quercus muehlenbergii), Lacey Oak (Quercus laceyi), Texas Red Oak (Quercus buckleyi), Juniper, Florida Basswood (Tilia caroliniana) and Bigtooth Maple (Acer grandidentatum) (the latter of which was discovered far removed from any maple forest, and thus gave the area the name "lost maples"). Maple colors are brilliant unless autumn is mild; the Texas red oak gives a good display almost every year. This park is most crowded when the fall colors peak in November. Evidence suggests that th
    LostMaplesReflection.jpg
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