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Source: en.wikipedia.org/wiki/Cliffs_of_Moher
The Cliffs of Moher (Irish: Aillte an Mhothair) are sea cliffs located at the southwestern edge of the Burren region in County Clare, Ireland. They run for about 14 kilometres. At their southern end, they rise 120 metres (390 ft) above the Atlantic Ocean at Hag's Head, and, eight kilometres to the north, they reach their maximum height of 214 metres (702 ft) just north of O'Brien's Tower, a round stone tower near the midpoint of the cliffs, built in 1835 by Sir Cornelius O'Brien, then continue at lower heights. The closest settlements are Liscannor (6 km south) and Doolin (7 km north).
From the cliffs, and from atop the tower, visitors can see the Aran Islands in Galway Bay, the Maumturks and Twelve Pins mountain ranges to the north in County Galway, and Loop Head to the south. The cliffs rank among the most visited tourist sites in Ireland, with around 1.5 million visits per annum.
Source: en.wikipedia.org/wiki/Monument_Valley
Monument Valley (Navajo: Tsé Biiʼ Ndzisgaii, pronounced [tsʰépìːʔ ǹtsɪ̀skɑ̀ìː], meaning "valley of the rocks") is a region of the Colorado Plateau characterized by a cluster of sandstone buttes, with the largest reaching 1,000 ft (300 m) above the valley floor. The most famous butte formations are located in northeastern Arizona along the Utah–Arizona state line. The valley is considered sacred by the Navajo Nation, the Native American people within whose reservation it lies.
Monument Valley has been featured in many forms of media since the 1930s. Famed director John Ford used the location for a number of his Westerns. Film critic Keith Phipps wrote that "its five square miles [13 km2] have defined what decades of moviegoers think of when they imagine the American West".
Sourc: navajonationparks.org/navajo-tribal-parks/monument-valley/
History
Before human existence, the Park was once a lowland basin. For hundreds of millions of years, materials that eroded from the early Rock Mountains deposited layer upon layer of sediment which cemented a slow and gentle uplift, generated by ceaseless pressure from below the surface, elevating these horizontal strata quite uniformly one to three miles above sea level. What was once a basin became a plateau.
Natural forces of wind and water that eroded the land spent the last 50 million years cutting into and peeling away at the surface of the plateau. The simple wearing down of altering layers of soft and hard rock slowly revealed the natural wonders of Monument Valley today.
From the visitor center, you see the world-famous panorama of the Mitten Buttes and Merrick Butte. You can also purchase guided tours from Navajo tour operators, who take you down into the valley in Jeeps for a narrated cruise through these mythical formations. Places such as Ear of the Wind and other landmarks can only be accessed via guided tours. During the summer months, the visitor center also features Haskenneini Restaurant, which specializes in both native Navajo and American cuisines, and a film/snack/souvenir shop. There are year-round restroom facilities. One mile before the center, numerous Navajo vendors sell arts, crafts, native food, and souvenirs at roadside stands.
Additional Foreign Language Tags:
(United States) "الولايات المتحدة" "Vereinigte Staaten" "アメリカ" "米国" "美国" "미국" "Estados Unidos" "États-Unis" "ארצות הברית" "संयुक्त राज्य" "США"
(Arizona) "أريزونا" "亚利桑那州" "אריזונה" "एरिजोना" "アリゾナ州" "애리조나" "Аризона"
(Utah) "يوتا" "犹他州" "יוטה" "यूटा" "ユタ州" "유타" "Юта"
(Monument Valley) "وادي النصب التذكاري" "纪念碑谷" "Vallée des monuments" "מוניומנט ואלי" "स्मारक घाटी" "モニュメントバレー" "모뉴먼트 밸리" "Долина Монументов" "Valle de los Monumentos"
Source: en.wikipedia.org/wiki/Monument_Valley
Monument Valley (Navajo: Tsé Biiʼ Ndzisgaii, pronounced [tsʰépìːʔ ǹtsɪ̀skɑ̀ìː], meaning "valley of the rocks") is a region of the Colorado Plateau characterized by a cluster of sandstone buttes, with the largest reaching 1,000 ft (300 m) above the valley floor. The most famous butte formations are located in northeastern Arizona along the Utah–Arizona state line. The valley is considered sacred by the Navajo Nation, the Native American people within whose reservation it lies.
Monument Valley has been featured in many forms of media since the 1930s. Famed director John Ford used the location for a number of his Westerns. Film critic Keith Phipps wrote that "its five square miles [13 km2] have defined what decades of moviegoers think of when they imagine the American West".
Sourc: navajonationparks.org/navajo-tribal-parks/monument-valley/
History
Before human existence, the Park was once a lowland basin. For hundreds of millions of years, materials that eroded from the early Rock Mountains deposited layer upon layer of sediment which cemented a slow and gentle uplift, generated by ceaseless pressure from below the surface, elevating these horizontal strata quite uniformly one to three miles above sea level. What was once a basin became a plateau.
Natural forces of wind and water that eroded the land spent the last 50 million years cutting into and peeling away at the surface of the plateau. The simple wearing down of altering layers of soft and hard rock slowly revealed the natural wonders of Monument Valley today.
From the visitor center, you see the world-famous panorama of the Mitten Buttes and Merrick Butte. You can also purchase guided tours from Navajo tour operators, who take you down into the valley in Jeeps for a narrated cruise through these mythical formations. Places such as Ear of the Wind and other landmarks can only be accessed via guided tours. During the summer months, the visitor center also features Haskenneini Restaurant, which specializes in both native Navajo and American cuisines, and a film/snack/souvenir shop. There are year-round restroom facilities. One mile before the center, numerous Navajo vendors sell arts, crafts, native food, and souvenirs at roadside stands.
Additional Foreign Language Tags:
(United States) "الولايات المتحدة" "Vereinigte Staaten" "アメリカ" "米国" "美国" "미국" "Estados Unidos" "États-Unis" "ארצות הברית" "संयुक्त राज्य" "США"
(Arizona) "أريزونا" "亚利桑那州" "אריזונה" "एरिजोना" "アリゾナ州" "애리조나" "Аризона"
(Utah) "يوتا" "犹他州" "יוטה" "यूटा" "ユタ州" "유타" "Юта"
(Monument Valley) "وادي النصب التذكاري" "纪念碑谷" "Vallée des monuments" "מוניומנט ואלי" "स्मारक घाटी" "モニュメントバレー" "모뉴먼트 밸리" "Долина Монументов" "Valle de los Monumentos"
The sun was on its way to setting over Manhattan, creating a light orange hue in this view from the Top of the Rock, featuring the Empire State Building and the Bank of America Tower (in the foreground) and the One World Trade Center further South (in the background).
A caminho das seis da tarde, o sol estava a pôr-se sobre Manhattan, criando um tom alaranjado claro nesta vista a partir do Top of the Rock, com o Empire State Building e a Bank of America Tower (em primeiro plano) e o One World Trade Center mais a Sul (em segundo plano).
en.wikipedia.org/wiki/Elora,_Ontario
The Historic Village of Elora is a community in the township of Centre Wellington (Wellington County) in the Province of Ontario, Canada. It is well known for its 19th-century limestone architecture and its geographically, historically, and culturally significant limestone gorge.
Elora is no longer an incorporated municipality in its own right, although it is the seat of the municipal government which succeeded it. The Township of Centre Wellington was formed in 1999 when, on the advice of the Province, the County amalgamated the Town of Fergus; the Village of Elora; and the surrounding townships of Nichol, Pilkington, and West Garafraxa (along with the northwestern part of Eramosa.)[2] The decision — along with the Ontario government’s role therein — remains highly controversial among Elora’s inhabitants.
In 2011, the Village was estimated to have had a population of approximately 7,756.[1]
History
Roman Catholic missionaries first visited the area in the early to mid 1600s attempting to Christianize the indigenous people, particularly the Neutral Nation on the Attiwandaronk Lands. The first European settlers arrived in 1817, and Roswell Matthews built a home here the next year.[3][4]
Captain William Gilkison (1777–1833) was born in Ayrshire, Scotland, and emigrated to North America in 1796. He served with the British forces in the War of 1812 as an assistant quartermaster-general, and in 1832 purchased some 14,000 acres of land in Nichol Township. He selected this area near the falls of the Grand River as a town site for his proposed settlement and named it Elora. It was laid out by Lewis Burwell, deputy provincial land surveyor, late in 1832, and the following year Gilkison established a sawmill and a general store. The founder of Elora died in April, 1833, before the full results of his foresight and enterprise were achieved.
Source: en.wikipedia.org/wiki/Monument_Valley
Monument Valley (Navajo: Tsé Biiʼ Ndzisgaii, pronounced [tsʰépìːʔ ǹtsɪ̀skɑ̀ìː], meaning "valley of the rocks") is a region of the Colorado Plateau characterized by a cluster of sandstone buttes, with the largest reaching 1,000 ft (300 m) above the valley floor. The most famous butte formations are located in northeastern Arizona along the Utah–Arizona state line. The valley is considered sacred by the Navajo Nation, the Native American people within whose reservation it lies.
Monument Valley has been featured in many forms of media since the 1930s. Famed director John Ford used the location for a number of his Westerns. Film critic Keith Phipps wrote that "its five square miles [13 km2] have defined what decades of moviegoers think of when they imagine the American West".
Sourc: navajonationparks.org/navajo-tribal-parks/monument-valley/
History
Before human existence, the Park was once a lowland basin. For hundreds of millions of years, materials that eroded from the early Rock Mountains deposited layer upon layer of sediment which cemented a slow and gentle uplift, generated by ceaseless pressure from below the surface, elevating these horizontal strata quite uniformly one to three miles above sea level. What was once a basin became a plateau.
Natural forces of wind and water that eroded the land spent the last 50 million years cutting into and peeling away at the surface of the plateau. The simple wearing down of altering layers of soft and hard rock slowly revealed the natural wonders of Monument Valley today.
From the visitor center, you see the world-famous panorama of the Mitten Buttes and Merrick Butte. You can also purchase guided tours from Navajo tour operators, who take you down into the valley in Jeeps for a narrated cruise through these mythical formations. Places such as Ear of the Wind and other landmarks can only be accessed via guided tours. During the summer months, the visitor center also features Haskenneini Restaurant, which specializes in both native Navajo and American cuisines, and a film/snack/souvenir shop. There are year-round restroom facilities. One mile before the center, numerous Navajo vendors sell arts, crafts, native food, and souvenirs at roadside stands.
Additional Foreign Language Tags:
(United States) "الولايات المتحدة" "Vereinigte Staaten" "アメリカ" "米国" "美国" "미국" "Estados Unidos" "États-Unis" "ארצות הברית" "संयुक्त राज्य" "США"
(Arizona) "أريزونا" "亚利桑那州" "אריזונה" "एरिजोना" "アリゾナ州" "애리조나" "Аризона"
(Utah) "يوتا" "犹他州" "יוטה" "यूटा" "ユタ州" "유타" "Юта"
(Monument Valley) "وادي النصب التذكاري" "纪念碑谷" "Vallée des monuments" "מוניומנט ואלי" "स्मारक घाटी" "モニュメントバレー" "모뉴먼트 밸리" "Долина Монументов" "Valle de los Monumentos"
Source: en.wikipedia.org/wiki/Boston
Boston, officially the City of Boston, is the capital and largest city of the Commonwealth of Massachusetts and the cultural and financial center of the New England region of the Northeastern United States. The city boundaries encompass an area of about 48.4 sq mi (125 km2) and a population of 675,647 as of 2020. The city is the economic and cultural anchor of a substantially larger metropolitan area known as Greater Boston, a metropolitan statistical area (MSA) home to 4,941,632 people as of 2020, ranking as the eleventh-largest MSA in the country. A broader combined statistical area (CSA), generally corresponding to the commuting area and including Worcester, Massachusetts and Providence, Rhode Island, is home to approximately 8.2 million people, making it the seventh-most populous in the United States.
Boston is one of the nation's oldest municipalities, founded on the Shawmut Peninsula in 1630 by Puritan settlers from the English town of the same name. During the American Revolution and the nation's founding, Boston was the location of several key events, including the Boston Massacre, the Boston Tea Party, the hanging of Paul Revere's lantern signal in Old North Church, the Battle of Bunker Hill, and the siege of Boston. Following American independence from Great Britain, the city continued to play an important role as a port, manufacturing hub, and center for American education and culture. The city has expanded beyond the original peninsula through land reclamation and municipal annexation. Its rich history attracts many tourists, with Faneuil Hall alone drawing more than 20 million visitors per year. Boston's many firsts include the United States' first public park (Boston Common, 1634), the first public school (Boston Latin School, 1635), the first subway system (Tremont Street subway, 1897), and the first large public library (Boston Public Library, 1848).
In the 21st century, Boston has emerged as a global leader in higher education and academic research. Greater Boston's many colleges and universities include Harvard University and MIT, both located in suburban Cambridge and both routinely included among the world's most highly ranked universities. The city is also a national leader in scientific research, law, medicine, engineering, and business. With nearly 5,000 startup companies, the city is considered a global pioneer in innovation and entrepreneurship. Boston's economic base also includes finance, professional and business services, biotechnology, information technology, and government activities. Households in the city claim the highest average rate of philanthropy in the United States. Boston businesses and institutions rank among the top in the country for environmental sustainability and new investment.
Source: en.wikipedia.org/wiki/Beacon_Hill,_Boston
Beacon Hill is a historic neighborhood in Boston, Massachusetts, United States. It is also the location of the Massachusetts State House. The term "Beacon Hill" is used locally as a metonym to refer to the state government or the legislature itself, much like Washington, D.C.'s Capitol Hill does at the federal level.
Federal-style rowhouses, narrow gaslit streets and brick sidewalks run through the neighborhood, which is generally regarded as one of the more desirable and expensive in Boston. As of the 2010 U.S. Census, the population of Boston's Beacon Hill neighborhood was 9,023.
Source: en.wikipedia.org/wiki/Massachusetts_State_House
The Massachusetts State House, also known as the Massachusetts Statehouse or the New State House, is the state capitol and seat of government for the Commonwealth of Massachusetts, located in the Beacon Hill neighborhood of Boston. The building houses the Massachusetts General Court (state legislature) and the offices of the Governor of Massachusetts. The building, designed by architect Charles Bulfinch, was completed in January 1798 at a cost of $133,333 (more than five times the budget), and has repeatedly been enlarged since. It is one of the oldest state capitols in current use. It is considered a masterpiece of Federal architecture and among Bulfinch's finest works, and was designated a National Historic Landmark for its architectural significance.
Additional Foreign Language Tags:
(United States) "الولايات المتحدة" "Vereinigte Staaten" "アメリカ" "美国" "미국" "Estados Unidos" "États-Unis"
(Massachusetts) "ماساتشوستس" "麻萨诸塞州" "मैसाचुसेट्स" "マサチューセッツ" "매사추세츠 주" "Массачусетс"
(Boston) "بوسطن" "波士顿" "बोस्टन" "ボストン" "보스턴" "Бостон"
Yeah I think it turn out pretty well.
As always I will give the files and instructions for free once I build it.
Undine Falls is four miles east of Mammoth, near the roadway, and accessible by an easy, short hike. Lava Creek spills over the cliff face of a basalt lava flow that was emplaced about 700,000 years ago. The falls is approximately 60 feet in height, descending in three plunges. Originally called “East Gardner Falls,” “Cascade Falls of the East Gardiner,” or “Gardiner River Falls,” Undine received its present name in 1885 from geologist Arnold Hague. Undine (Webster says it is pronounced UN deen) was named for wise, usually female water spirits from German mythology who lived around waterfalls and who could gain souls by marrying mortal men. Undine Falls was featured on the cover of the July 1977 edition of National Geographic magazine. [Source: yellowstone.net/waterfalls/yellowstones-waterfalls/undine...]
www.world-of-waterfalls.com/yellowstone-undine-falls.html
www.gowaterfalling.com/waterfalls/undine.shtml
Yellowstone National Park is a national park located in the U.S. states of Wyoming, Montana, and Idaho. It was established by the U.S. Congress and signed into law by President Ulysses S. Grant on March 1, 1872. Yellowstone was the first National Park in the U.S. and is also widely held to be the first national park in the world. The park is known for its wildlife and its many geothermal features, especially Old Faithful Geyser, one of its most popular features. It has many types of ecosystems, but the subalpine forest is the most abundant. It is part of the South Central Rockies forests ecoregion. [Source: en.wikipedia.org/wiki/Yellowstone_National_Park]
en.wikipedia.org/wiki/Duke%27s_Dock
Duke's Dock[3][4] is a dock on the River Mersey, England, and part of the Port of Liverpool. It is in the southern dock system, connected to Salthouse Dock and Wapping Dock to the east. The Albert Dock is located immediately north, although not directly accessible by water.
History
The land for the dock was obtained in 1768.[5] Opening in 1773, Duke's Dock was built privately for the Duke of Bridgewater as a Liverpool-based facility for traffic using the Bridgewater Canal from Manchester.[6][7] The dock was probably designed by James Brindley, who also built the Bridgewater Canal.[2] The first dockside warehouse on the Mersey was built at the dock in 1783, and the dock was extended in the 1790s due to growth in the cotton industry.[2] In 1811, a large six-storey warehouse was built on the southern side of the dock.[5] Barges were able to enter the warehouse from the dock, and the building lasted until the 1960s.[5] In 1845, a small half-tide dock was constructed between Duke's Dock and the river and, at the opposite end of the dock, Wapping Basin was added in 1855.[5] The dock was purchased by the MD&HB in 1900, and the warehouses remained until 1960.[2] The dock had a southern branch which was filled in 1967, and warehouses were removed from the north and south quaysides.[5] The dock closed in 1972.[2]
After closure
After the closure of Duke's Dock, the dock silted up during the following decade and the quayside was in a state of considerable dereliction by 1980.[5] In 1980, disused buildings including one of the Liverpool Lighterage Company, a training school and a customs house still remained on the north quayside.[5]
Water balling at Duke's Dock. The Albert Dock warehouses are to the left, with Liverpool Metropolitan Cathedral beyond the footbridge in the background.
In 1981, the Merseyside Development Corporation was established to rejuvenate the South Docks, and the dock was dredged between 1981-5.[8] The river entrance was filled in during the 1980s, and replaced with a permanent roadway leading to a large temporary car park on the site of King's Dock.[citation needed] Footbridges across the dock, leading from the King's Dock car park to the rejuvenated Albert Dock, were also installed at this time. The remaining buildings on the north quayside were also removed, to create permanent car parking space for the Albert Dock.[citation needed]
Present use
Direct river access to the west is no longer provided, with the only remains of the river entrance being markings on the dock wall. The dock is still accessible from Wapping Basin.
The water depth varies from around 6 ft (1.8 m) up to 20 ft (6.1 m). The dock is sometimes used by sport scuba divers. Its water is clear and it has much underwater sealife.[citation needed] The waterspace, of this and the other docks in the southern system, was owned by British Waterways from 2003 to 2012 and now transferred to the Canal & River Trust.[1] Water balling is now allowed on the dock.
Source: en.wikipedia.org/wiki/Monument_Valley
Monument Valley (Navajo: Tsé Biiʼ Ndzisgaii, pronounced [tsʰépìːʔ ǹtsɪ̀skɑ̀ìː], meaning "valley of the rocks") is a region of the Colorado Plateau characterized by a cluster of sandstone buttes, with the largest reaching 1,000 ft (300 m) above the valley floor. The most famous butte formations are located in northeastern Arizona along the Utah–Arizona state line. The valley is considered sacred by the Navajo Nation, the Native American people within whose reservation it lies.
Monument Valley has been featured in many forms of media since the 1930s. Famed director John Ford used the location for a number of his Westerns. Film critic Keith Phipps wrote that "its five square miles [13 km2] have defined what decades of moviegoers think of when they imagine the American West".
Sourc: navajonationparks.org/navajo-tribal-parks/monument-valley/
History
Before human existence, the Park was once a lowland basin. For hundreds of millions of years, materials that eroded from the early Rock Mountains deposited layer upon layer of sediment which cemented a slow and gentle uplift, generated by ceaseless pressure from below the surface, elevating these horizontal strata quite uniformly one to three miles above sea level. What was once a basin became a plateau.
Natural forces of wind and water that eroded the land spent the last 50 million years cutting into and peeling away at the surface of the plateau. The simple wearing down of altering layers of soft and hard rock slowly revealed the natural wonders of Monument Valley today.
From the visitor center, you see the world-famous panorama of the Mitten Buttes and Merrick Butte. You can also purchase guided tours from Navajo tour operators, who take you down into the valley in Jeeps for a narrated cruise through these mythical formations. Places such as Ear of the Wind and other landmarks can only be accessed via guided tours. During the summer months, the visitor center also features Haskenneini Restaurant, which specializes in both native Navajo and American cuisines, and a film/snack/souvenir shop. There are year-round restroom facilities. One mile before the center, numerous Navajo vendors sell arts, crafts, native food, and souvenirs at roadside stands.
Additional Foreign Language Tags:
(United States) "الولايات المتحدة" "Vereinigte Staaten" "アメリカ" "米国" "美国" "미국" "Estados Unidos" "États-Unis" "ארצות הברית" "संयुक्त राज्य" "США"
(Arizona) "أريزونا" "亚利桑那州" "אריזונה" "एरिजोना" "アリゾナ州" "애리조나" "Аризона"
(Utah) "يوتا" "犹他州" "יוטה" "यूटा" "ユタ州" "유타" "Юта"
(Monument Valley) "وادي النصب التذكاري" "纪念碑谷" "Vallée des monuments" "מוניומנט ואלי" "स्मारक घाटी" "モニュメントバレー" "모뉴먼트 밸리" "Долина Монументов" "Valle de los Monumentos"
Source: en.wikipedia.org/wiki/Grand_Canyon
The Grand Canyon is a steep-sided canyon carved by the Colorado River in Arizona, United States. The Grand Canyon is 277 miles (446 km) long, up to 18 miles (29 km) wide and attains a depth of over a mile (6,093 feet or 1,857 meters).
The canyon and adjacent rim are contained within Grand Canyon National Park, the Kaibab National Forest, Grand Canyon–Parashant National Monument, the Hualapai Indian Reservation, the Havasupai Indian Reservation and the Navajo Nation. The surrounding area is contained within the Baaj Nwaavjo I'tah Kukveni – Ancestral Footprints of the Grand Canyon National Monument. President Theodore Roosevelt was a major proponent of the preservation of the Grand Canyon area and visited it on numerous occasions to hunt and enjoy the scenery.
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 some aspects about the history of incision of the canyon are debated by geologists, several recent studies support the hypothesis that the Colorado River established its course through the area about 5 to 6 million years ago. Since that time, the Colorado River has driven the down-cutting of the tributaries and retreat of the cliffs, simultaneously deepening and widening the canyon.
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 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.
Source: en.wikipedia.org/wiki/Grand_Canyon_National_Park
Grand Canyon National Park is a national park of the United States located in northwestern Arizona, the 15th site to have been named as a national park. The park's central feature is the Grand Canyon, a gorge of the Colorado River, which is often considered one of the Wonders of the World. The park, which covers 1,217,262 acres (1,901.972 sq mi; 4,926.08 km2) of unincorporated area in Coconino and Mohave counties, received more than 4.7 million recreational visitors in 2023. The Grand Canyon was designated a World Heritage Site by UNESCO in 1979. The park celebrated its 100th anniversary on February 26, 2019.
Source: www.nps.gov/grca/index.htm
Entirely within the state of Arizona, the park encompasses 278 miles (447 km) of the Colorado River and adjacent uplands. Located on the ancestral homelands of 11 present day Tribal Communities, Grand Canyon is one of the most spectacular examples of erosion anywhere in the world—a mile deep canyon unmatched in the incomparable vistas it offers visitors from both north and south rims.
Additional Foreign Language Tags:
(United States) "الولايات المتحدة" "Vereinigte Staaten" "アメリカ" "米国" "美国" "미국" "Estados Unidos" "États-Unis" "ארצות הברית" "संयुक्त राज्य" "США"
(Arizona) "أريزونا" "亚利桑那州" "אריזונה" "एरिजोना" "アリゾナ州" "애리조나" "Аризона"
(Grand Canyon) "جراند كانيون" "大峡谷" "גרנד קניון" "ग्रांड कैन्यन" "グランドキャニオン" "그랜드 캐니언" "Гранд-Каньон" "Gran Cañón"
ODC topic 'Soft & Sharp.' Cats' whiskers are so sharp and strong at the thick end you can puncture your finger with it and draw blood. At the fine, thin end it is so soft it is impossible to feel it. Please see photo below
From Wiki:
The yellow-rumped cacique has benefited from the more open habitat created by forest clearance and ranching. It is not considered threatened. It is a colonial breeder, with up to 100 bag-shaped nests in a tree, which usually also contains an active wasp nest. The females build the nests, incubate, and care for the young. Each nest is 30–45 cm long and widens at the base, and is suspended from the end of a branch. Females compete for the best sites near the protection of the wasp nest. The normal clutch is two dark-blotched pale blue or white eggs. Females begin incubating after laying the second egg; hatching occurs after 13 or 14 days. The young fledge in 34 to 40 days, usually only one per nest. Eats large insects, spiders, fruit, and nectar.
Excerpt from en.wikipedia.org/wiki/Sacramento_Valley_Station:
Sacramento Valley Station is an Amtrak railway station in the city of Sacramento, California, at 401 I Street on the corner of Fifth Street, built in 1926 on the site of China Slough. It is the thirteenth busiest Amtrak station in the country, and the second busiest in the Western United States. It is served by four different Amtrak train routes and connecting Amtrak Thruway motorcoaches. It is also the western terminus for the Gold Line of the SacRT light rail system and the Route 30 bus serving California State University, Sacramento.
The original Sacramento station was the terminal of the Central Pacific Railroad. The present building, designed by the San Francisco architectural firm of Bliss and Faville for the Southern Pacific Railroad, was built in 1926 on the site of China Slough in the Renaissance Revival style. Decorative features include a red tile roof and terracotta trim, as well as large arches on the main facade. Inside, the waiting room has a mural by artist John A. MacQuarrie that depicts the celebration of the groundbreaking for the First transcontinental railroad on January 8, 1863, in Sacramento. The Central Pacific started from Sacramento and built east to Promontory Summit, Utah, where it met the Union Pacific Railroad. The station is now owned by the City of Sacramento. With the creation of Amtrak on May 1, 1971, the station became Amtrak-only. The station was listed on the National Register of Historic Places in 1975 as "Southern Pacific Railroad Company's Sacramento Depot".
For most of Amtrak's first two decades, the only trains calling at Sacramento were long-distance routes. The California Zephyr and its predecessors have served the station from Amtrak's inception; several pre-Amtrak predecessors of the Zephyr stopped in Sacramento from the 1930s onward. The Coast Starlight arrived in 1982. From 1981, the Spirit of California ran as a sleeper to Los Angeles along the far southern leg of the Coast Starlight route. Service expanded dramatically in 1991 with the introduction of the Capitols service, now the Capitol Corridor. Partly due to its success, it is now the second-busiest station in the Western United States, behind only Los Angeles Union Station, and the seventh-busiest station overall.
The Sacramento Regional Transit Gold Line service was extended 0.5 miles (0.80 km) to Sacramento Valley Station on December 8, 2006.
en.wikipedia.org/wiki/Taj_building,_Nowshera
The Taj Building is an architectural jewel on the main Grand Trunk Road in Nowshera, Khyber Pakhtunkhwa, Pakistan.
Built in the 1920s, the imposing structure has endured the ravages of time despite lack of any concerted attempts in the past to preserve it. The facade of the three-storey building is highly decorated with floral and vine patterns in intricate stucco. The sweeping round arches and numerous embellished columns represent a charming architectural blend of Roman, Gothic and Oriental. An arched gateway on the side of the building with beautiful jharoka-styled (elevated window balcony) features leads into the main compound.[1] The building was constructed by Khan Bahadur Taj Muhammad Khan OBE MLC of Badrashi Village, Nowshera. He was a famous colonial-era contractor and landlord whose father KB Abdul Hamid Khan had been in the service of the British Empire as well. Therefore, all the bricks used in construction of this building are marked with the word KB (Khan Bahadur). He was a wealthy man and was particularly fond of racehorses. He used to travel extensively in India and had built several grand mansions for his own comfort. The present National Defence College building in New Delhi, India was also his personal mansion.
Mammoth Hot Springs is a large complex of hot springs on a hill of travertine in Yellowstone National Park adjacent to Fort Yellowstone and the Mammoth Hot Springs Historic District. It was created over thousands of years as hot water from the spring cooled and deposited calcium carbonate (over two tons flow into Mammoth each day in a solution). Because of the huge amount of geothermal vents, travertine flourishes. Although these springs lie outside the caldera boundary, their energy has been attributed to the same magmatic system that fuels other Yellowstone geothermal areas. The hot water that feeds Mammoth comes from Norris Geyser Basin after traveling underground via a fault line that runs through limestone and roughly parallel to the Norris-to-Mammoth road. The limestone from rock formations along the fault is the source of the calcium carbonate. Shallow circulation along this corridor allows Norris' superheated water to slightly cool before surfacing at Mammoth, generally at about 170 °F (80 °C). Algae living in the warm pools have tinted the travertine shades of brown, orange, red, and green. Thermal activity here is extensive both over time and distance. The thermal flows show much variability with some variations taking place over periods ranging from decades to days. Terrace Mountain at Mammoth Hot Springs is the largest known carbonate-depositing spring in the world. The most famous feature at the springs is the Minerva Terrace, a series of travertine terraces. The terraces have been deposited by the spring over many years but, due to recent minor earthquake activity, the spring vent has shifted, rendering the terraces dry. The Mammoth Terraces extend all the way from the hillside, across the Parade Ground, and down to Boiling River. The Mammoth Hotel, as well as all of Fort Yellowstone, is built upon an old terrace formation known as Hotel Terrace. There was some concern when construction began in 1891 on the fort site that the hollow ground would not support the weight of the buildings. Several large sink holes (fenced off) can be seen out on the Parade Ground. This area has been thermally active for several thousand years. The Mammoth area exhibits much evidence of glacial activity from the Pinedale Glaciation. The summit of Terrace Mountain is covered with glacial till, thereby dating the travertine formation there to earlier than the end of the Pinedale Glaciation. Several thermal kames, including Capitol Hill and Dude Hill, are major features of the Mammoth Village area. Ice-marginal stream beds are in evidence in the small, narrow valleys where Floating Island Lake and Phantom Lake are found. In Gardner Canyon one can see the old, sorted gravel bed of the Gardner River covered by unsorted glacial till. [Source: en.wikipedia.org/wiki/Mammoth_Hot_Springs]
Yellowstone National Park is a national park located in the U.S. states of Wyoming, Montana, and Idaho. It was established by the U.S. Congress and signed into law by President Ulysses S. Grant on March 1, 1872. Yellowstone was the first National Park in the U.S. and is also widely held to be the first national park in the world. The park is known for its wildlife and its many geothermal features, especially Old Faithful Geyser, one of its most popular features. It has many types of ecosystems, but the subalpine forest is the most abundant. It is part of the South Central Rockies forests ecoregion. [Source: en.wikipedia.org/wiki/Yellowstone_National_Park]
en.wikipedia.org/wiki/Glossy_ibis
The glossy ibis (Plegadis falcinellus) is a wading bird in the ibis family Threskiornithidae.
Distribution
This is the most widespread ibis species, breeding in scattered sites in warm regions of Europe, Asia, Africa, Australia, and the Atlantic and Caribbean[2] regions of the Americas. It is thought to have originated in the Old World and spread naturally from Africa to northern South America in the 19th century, from where it spread to North America.[3] This species is migratory; most European birds winter in Africa, and in North America[4] birds from north of the Carolinas winter farther south. Birds from other populations may disperse widely outside the breeding season. While generally declining in Europe, it has recently established a breeding colony in southern Spain, and there appears to be a growing trend for the Spanish birds to winter in Britain and Ireland, with at least 22 sightings in 2010.[5] In 2014, a pair attempted to breed in Lincolnshire, the first such attempt in Britain [6]
Behaviour
Glossy ibises undertake dispersal movements after breeding and are very nomadic. The more northerly populations are fully migratory and travel on a broad front, for example across the Sahara Desert. Populations in temperate regions breed during the local spring, while tropical populations nest to coincide with the rainy season. Nesting is often in mixed-species colonies. When not nesting, flocks of over 100 individuals may occur on migration, and during the winter or dry seasons the species is usually found foraging in small flocks. Glossy ibises often roost communally at night in large flocks, with other species, occasionally in trees which can be some distance from wetland feeding areas.
Habitat
Glossy ibises feed in very shallow water and nest in freshwater or brackish wetlands with tall dense stands of emergent vegetation such as reeds, papyrus or rushes) and low trees or bushes. They show a preference for marshes at the margins of lakes and rivers but can also be found at lagoons, flood-plains, wet meadows, swamps, reservoirs, sewage ponds, paddies and irrigated farmland. It is less commonly found in coastal locations such as estuaries, deltas, salt marshes and coastal lagoons. Preferred roosting sites are normally in large trees which may be distant from the feeding areas.
The nests are usually a platform of twigs and vegetation positioned at least 1 m (3.3 ft) above water, sometimes up to 7 m (23 ft) in tall, dense stands of emergent vegetation, low trees or bushes.[1]
Diet
The diet of the glossy ibis is variable according to the season and is very dependent on what is available. Prey includes adult and larval insects such as aquatic beetles, dragonflies, damselflies, grasshoppers, crickets, flies and caddisflies, Annelida including leeches, molluscs (e.g. snails and mussels), crustaceans (e.g. crabs and crayfish) and occasionally fish, amphibians, lizards, small snakes and nestling birds.[1]
Description
This species is a mid-sized ibis. It is 48–66 cm (19–26 in) long, averaging around 59.4 cm (23.4 in) with an 80–105 cm (31–41 in) wingspan.[7][8] The culmen measures 9.7 to 14.4 cm (3.8 to 5.7 in) in length, each wing measures 24.8–30.6 cm (9.8–12.0 in), the tail is 9–11.2 cm (3.5–4.4 in) and the tarsus measures 6.8–11.3 cm (2.7–4.4 in).[8] The body mass of this ibis can range from 485 to 970 g (1.069 to 2.138 lb).[8] Breeding adults have reddish-brown bodies and shiny bottle-green wings. Non-breeders and juveniles have duller bodies. This species has a brownish bill, dark facial skin bordered above and below in blue-gray (non-breeding) to cobalt blue (breeding), and red-brown legs. Unlike herons, ibises fly with necks outstretched, their flight being graceful and often in V formation.
Sounds made by this rather quiet ibis include a variety of croaks and grunts, including a hoarse grrrr made when breeding.
Conservation
The glossy ibis is one of the species to which the Agreement on the Conservation of African-Eurasian Migratory Waterbirds (AEWA) applies. Glossy ibises are threatened by wetland habitat degradation and loss through drainage, increased salinity, groundwater extraction and invasion by exotic plants.[1]
The common name black curlew may be a reference to the glossy ibis and this name appears in Anglo-Saxon literature, indicating that it may have bred in early medieval England but Yalden and Albarella do not mention this species.[9]
Mormon Row Historic District - Mormon Row is a line of homestead complexes along the Jackson-Moran Road near the southeast corner of Grand Teton National Park, in the valley called Jackson Hole. The rural historic landscape's period of significance includes the construction of the Andy Chambers, T.A. Moulton and John Moulton farms from 1908 to the 1950s. Six building clusters and a separate ruin illustrate Mormon settlement in the area and comprise such features as drainage systems, barns, fields and corrals. Apart from John and T.A. Moulton, other settlers in the area were Joseph Eggleston, Albert Gunther, Henry May, Thomas Murphy and George Riniker. The area is also known as Antelope Flats, situated between the towns of Moose and Kelly. It is a popular destination for tourists and photographers on account of the historic buildings, the herds of bison, and the spectacular Teton Range rising in the background. The alluvial soil to the east of Blacktail Butte was more suitable than most locations in Jackson Hole for farming, somewhat hampered by a lack of readily available water. The Mormon homesteaders began to arrive in the 1890s from Idaho, creating a community called "Gros Ventre", with a total of 27 homesteads. The Mormon settlers tended to create clustered communities, in contrast to the isolated homesteads more typical of Jackson Hole. Mormon Row was placed on the National Register of Historic Places in 1997. [Source: en.wikipedia.org/wiki/Mormon_Row_Historic_District]
Grand Teton National Park is a United States National Park in northwestern Wyoming. At approximately 310,000 acres (480 sq mi; 130,000 ha; 1,300 km2), the park includes the major peaks of the 40-mile-long (64 km) Teton Range as well as most of the northern sections of the valley known as Jackson Hole. It is only 10 miles (16 km) south of Yellowstone National Park, to which it is connected by the National Park Service-managed John D. Rockefeller, Jr. Memorial Parkway. Along with surrounding National Forests, these three protected areas constitute the almost 18,000,000-acre (7,300,000 ha) Greater Yellowstone Ecosystem, one of the largest intact mid-latitude temperate ecosystems in the world. Human history of the Grand Teton region dates back at least 11,000 years, when the first nomadic hunter-gatherer Paleo-Indians began migrating into the region during warmer months pursuing food and supplies. In the early 19th century, the first White explorers encountered the eastern Shoshone natives. Between 1810 and 1840, the region attracted fur trading companies that vied for control of the lucrative beaver pelt trade. U.S. Government expeditions to the region commenced in the mid-19th century as an offshoot of exploration in Yellowstone, with the first permanent white settlers in Jackson Hole arriving in the 1880s. Efforts to preserve the region as a national park commenced in the late 19th century, and in 1929 Grand Teton National Park was established, protecting the major peaks of the Teton Range. The valley of Jackson Hole remained in private ownership until the 1930s, when conservationists led by John D. Rockefeller, Jr. began purchasing land in Jackson Hole to be added to the existing national park. Against public opinion and with repeated Congressional efforts to repeal the measures, much of Jackson Hole was set aside for protection as Jackson Hole National Monument in 1943. The monument was abolished in 1950 and most of the monument land was added to Grand Teton National Park. Grand Teton National Park is named for Grand Teton, the tallest mountain in the Teton Range. The naming of the mountains is attributed to early 19th-century French-speaking trappers—les trois tétons (the three teats) was later anglicized and shortened to Tetons. At 13,775 feet (4,199 m), Grand Teton abruptly rises more than 7,000 feet (2,100 m) above Jackson Hole, almost 850 feet (260 m) higher than Mount Owen, the second-highest summit in the range. The park has numerous lakes, including 15-mile-long (24 km) Jackson Lake as well as streams of varying length and the upper main stem of the Snake River. Though in a state of recession, a dozen small glaciers persist at the higher elevations near the highest peaks in the range. Some of the rocks in the park are the oldest found in any U.S. National Park and have been dated at nearly 2.7 billion years. Grand Teton National Park is an almost pristine ecosystem and the same species of flora and fauna that have existed since prehistoric times can still be found there. More than 1,000 species of vascular plants, dozens of species of mammals, 300 species of birds, more than a dozen fish species and a few species of reptiles and amphibians exist. Due to various changes in the ecosystem, some of them human-induced, efforts have been made to provide enhanced protection to some species of native fish and the increasingly threatened whitebark pine. Grand Teton National Park is a popular destination for mountaineering, hiking, fishing and other forms of recreation. There are more than 1,000 drive-in campsites and over 200 miles (320 km) of hiking trails that provide access to backcountry camping areas. Noted for world-renowned trout fishing, the park is one of the few places to catch Snake River fine-spotted cutthroat trout. Grand Teton has several National Park Service-run visitor centers, and privately operated concessions for motels, lodges, gas stations and marinas.
[source: en.wikipedia.org/wiki/Grand_Teton_National_Park]
Website: www.nps.gov/grte/index.htm
Wiki: Die Forschungseinrichtung für experimentelle Medizin der Charité, ehemals Zentrale Tierlaboratorien der Freien Universität Berlin, ist ein wissenschaftliches Forschungsgebäude. Das Gebäude gehört seit 2003 zur Charité und beherbergte bis 2019 den Hauptsitz der gleichnamigen Zentraleinrichtung.[1] Umgangssprachlich ist das Gebäude als Mäusebunker bekannt.
Im November 2019 erklärte der Landesdenkmalrat, beide Gebäude stellten „unbestreitbar bedeutende bauliche Manifestationen ihrer Zeit dar“, und empfahl den Erhalt des Ensembles.
Información en WIKIPEDIA:
🇪🇸 Colmar
🇫🇷 Colmar
Tomada a 193 m.s.n.m.
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AATV L03 - The Tremendous 3000s ()
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en.wikipedia.org/wiki/Thirlmere
Thirlmere is a reservoir in the Borough of Allerdale in Cumbria and the English Lake District. It runs roughly south to north, with a dam at the northern end, and is bordered on the eastern side by the A591 road and on the western side by a minor road.
Thirlmere was constructed in the 19th century by the Manchester Corporation to provide the burgeoning industrial city of Manchester with water supplies. The 96 mile-long Thirlmere Aqueduct still provides water to the Manchester area.
History
Prior to the construction of the reservoir the site was occupied by two smaller lakes - Leathes Water and Wythburn Water. The growth of the industrial city of Manchester during the 19th century had led to an increased demand for water. The water level was raised by construction of a dam by the Manchester Corporation at the northern end of Thirlmere, in 1890–1894. The reservoir was then able to supply water to Manchester via the Thirlmere Aqueduct, roughly 100 miles long. John Frederick Bateman acted as advisor to the corporation for both projects.
There was strong local opposition to the construction of the lake and the Thirlmere Defence Association (TDA) was formed to oppose the parliamentary act which was required before work could begin. The TDA opposed on the basis that raising the water level by 50 feet would submerge the dramatic cliffs which then surrounded the lake and a receding shoreline in summer would expose the smelly and unsightly lake bed. The organisation managed to stall the reading of the act in parliament in 1878 but the act was passed at the second reading in 1879.[
Etymology
" ...Leathes-Water' called also 'Thirlmere' or 'Wythburn-water' 1769...Probably 'the lake with/at the narrowing' from OE 'þyrel' 'aperture', pierced hole' plus OE 'mere' 'lake'. The lake had an especially narrow 'waist', spanned by a cuaseway and bridges," [2] before the dam was built. (OE= Old English).
Geography
The name is sometimes also applied to the whole valley, which connects Grasmere in the south with the Vale of Keswick in the north. The highest point in the valley is Dunmail Raise. The A591 runs the length of the valley and goes over Dunmail Raise.
The Helvellyn ridge lies to the east of Thirlmere. To the west of Thirlmere are a number of fells; for instance, Armboth Fell and Raven Crag both of which give views of the lake.
Management
The reservoir and surrounding forested valley is owned and managed by United Utilities, a private water and waste water company.
Every five years, since 1815, the inhabitants of a small town, Sordevolo, play the Passion of the Christ, putting in an amphitheatre the last days of the terrain life of Jesus Christ. The inhabitants are all non-professional actors, so they put their best to recall those biblical scenes with the utmost accuracy and attention to details. Two hours and a half of play in poetry reassured to move you, whether you're a believer or not.
Here's the scene of the Flagellation of Jesus.
You find me on - Mi trovate su
en.wikipedia.org/wiki/Cattle_Egret
The Cattle Egret (Bubulcus ibis) is a cosmopolitan species of heron (family Ardeidae) found in the tropics, subtropics and warm temperate zones. It is the only member of the monotypic genus Bubulcus, although some authorities regard its two subspecies as full species, the Western Cattle Egret and the Eastern Cattle Egret. Despite the similarities in plumage to the egrets of the genus Egretta, it is more closely related to the herons of Ardea. Originally native to parts of Asia, Africa and Europe, it has undergone a rapid expansion in its distribution and successfully colonised much of the rest of the world.
It is a white bird adorned with buff plumes in the breeding season. It nests in colonies, usually near bodies of water and often with other wading birds. The nest is a platform of sticks in trees or shrubs. Cattle Egrets exploit drier and open habitats more than other heron species. Their feeding habitats include seasonally inundated grasslands, pastures, farmlands, wetlands and rice paddies. They often accompany cattle or other large mammals, catching insect and small vertebrate prey disturbed by these animals. Some populations of the Cattle Egret are migratory and others show post-breeding dispersal.
The adult Cattle Egret has few predators, but birds or mammals may raid its nests, and chicks may be lost to starvation, calcium deficiency or disturbance from other large birds. This species maintains a special relationship with cattle, which extends to other large grazing mammals. The cattle egret removes ticks and flies from cattle and consumes them. This benefits both species, but it has been implicated in the spread of tick-borne animal diseases.
The Cattle Egret was first described in 1758 by Linnaeus in his Systema naturae as Ardea ibis,[2] but was moved to its current genus by Charles Lucien Bonaparte in 1855.[3] Its genus name Bubulcus is Latin for herdsman, referring, like the English name, to this species' association with cattle.[4] Ibis is a Latin and Greek word which originally referred to another white wading bird, the Sacred Ibis.[5]
The Cattle Egret has two geographical races which are sometimes classified as full species, the Western Cattle Egret, B. ibis, and Eastern Cattle Egret, B. coromandus. The two forms were split by McAllan and Bruce,[6] but were regarded as conspecific by almost all other recent authors until the publication of the influential Birds of South Asia.[7] The eastern subspecies B. (i.) coromandus, described by Pieter Boddaert in 1783, breeds in Asia and Australasia, and the western nominate form occupies the rest of the species range, including the Americas.[8] Some authorities recognise a third Seychelles subspecies, B. i. seychellarum, which was first described by Finn Salomonsen in 1934.[9]
Despite superficial similarities in appearance, the Cattle Egret is more closely related to the genus Ardea, which comprises the great or typical herons and the Great Egret (A. alba), than to the majority of species termed egrets in the genus Egretta.[10] Rare cases of hybridization with Little Blue Heron Egretta caerulea, Little Egret Egretta garzetta and Snowy Egret Egretta thula have been recorded.
Description
The Cattle Egret is a stocky heron with a 88–96 cm (35–38 in) wingspan; it is 46–56 centimetres (18–22 in) long and weighs 270–512 grams (9.5–18.1 oz).[12] It has a relatively short thick neck, sturdy bill, and a hunched posture. The non-breeding adult has mainly white plumage, a yellow bill and greyish-yellow legs. During the breeding season, adults of the nominate western subspecies develop orange-buff plumes on the back, breast and crown, and the bill, legs and irises become bright red for a brief period prior to pairing.[13] The sexes are similar, but the male is marginally larger and has slightly longer breeding plumes than the female; juvenile birds lack coloured plumes and have a black bill.[12][14]
B. i. coromandus differs from the nominate subspecies in breeding plumage, when the buff colour on its head extends to the cheeks and throat, and the plumes are more golden in colour. This subspecies' bill and tarsus are longer on average than in B. i. ibis.[15] B. i. seychellarum is smaller and shorter-winged than the other forms. It has white cheeks and throat, like B. i. ibis, but the nuptial plumes are golden, as with B. i. coromandus.[9]
The positioning of the egret's eyes allows for binocular vision during feeding,[16] and physiological studies suggest that the species may be capable of crepuscular or nocturnal activity.[17] Adapted to foraging on land, they have lost the ability possessed by their wetland relatives to accurately correct for light refraction by water.[18]
This species gives a quiet, throaty "rick-rack" call at the breeding colony, but is otherwise largely silent.
Distribution and habitat
The Cattle Egret has undergone one of the most rapid and wide reaching natural expansions of any bird species.[19] It was originally native to parts of Southern Spain and Portugal, tropical and subtropical Africa and humid tropical and subtropical Asia. In the end of the 19th century it began expanding its range into southern Africa, first breeding in the Cape Province in 1908.[20] Cattle Egrets were first sighted in the Americas on the boundary of Guiana and Suriname in 1877, having apparently flown across the Atlantic Ocean.[8][12] It was not until the 1930s that the species is thought to have become established in that area.[21]
The species first arrived in North America in 1941 (these early sightings were originally dismissed as escapees), bred in Florida in 1953, and spread rapidly, breeding for the first time in Canada in 1962.[20] It is now commonly seen as far west as California. It was first recorded breeding in Cuba in 1957, in Costa Rica in 1958, and in Mexico in 1963, although it was probably established before that.[21] In Europe the species had historically declined in Spain and Portugal, but in the latter part of the 20th century it expanded back through the Iberian Peninsula, and then began to colonise other parts of Europe; southern France in 1958, northern France in 1981 and Italy in 1985.[20] Breeding in the United Kingdom was recorded for the first time in 2008 only a year after an influx seen in the previous year.[22][23] In 2008 cattle egrets were also reported as having moved into Ireland for the first time.[24]
In Australia the colonisation began in the 1940s, with the species establishing itself in the north and east of the continent.[25] It began to regularly visit New Zealand in the 1960s. Since 1948 the Cattle Egret has been permanently resident in Israel. Prior to 1948 it was only a winter visitor. [26]
The massive and rapid expansion of the Cattle Egret's range is due to its relationship with humans and their domesticated animals. Originally adapted to a commensal relationship with large browsing animals, it was easily able to switch to domesticated cattle and horses. As the keeping of livestock spread throughout the world, the Cattle Egret was able to occupy otherwise empty niches.[27] Many populations of Cattle Egrets are highly migratory and dispersive,[19] and this has helped the species' range expansion. The species has been seen as a vagrant in various sub-Antarctic islands, including South Georgia, Marion Island, the South Sandwich Islands and the South Orkney Islands.[28] A small flock of eight birds was also seen in Fiji in 2008.[29]
In addition to the natural expansion of its range, Cattle Egrets have been introduced into a few areas. The species was introduced to Hawaii in 1959, and to the Chagos Archipelago in 1955. Successful releases were also made in the Seychelles and Rodrigues, but attempts to introduce the species to Mauritius failed. Numerous birds were also released by Whipsnade Zoo in England, but the species was never established.[30]
Although the Cattle Egret sometimes feeds in shallow water, unlike most herons it is typically found in fields and dry grassy habitats, reflecting its greater dietary reliance on terrestrial insects rather than aquatic prey.
Migration and movements
Some populations of Cattle Egrets are migratory, others are dispersive, and distinguishing between the two can be difficult for this species.[19] In many areas populations can be both sedentary and migratory. In the northern hemisphere migration is from cooler climes to warmer areas, but Cattle Egrets nesting in Australia migrate to cooler Tasmania and New Zealand in the winter and return in the spring.[25] Migration in western Africa is in response to rainfall, and in South America migrating birds travel south of their breeding range in the non breeding season.[19] Populations in southern India appear to show local migrations in response to the monsoons. They move north from Kerala after September.[32][33] During winter, many birds have been seen flying at night with flocks of Indian Pond Herons (Ardeola grayii) on the southeastern coast of India[34] and a winter influx has also been noted in Sri Lanka.[7]
Young birds are known to disperse up to 5,000 km (3,100 mi) from their breeding area. Flocks may fly vast distances and have been seen over seas and oceans including in the middle of the Atlantic.
Status
This species has a large range, with an estimated global extent of occurrence of 10 million square kilometres (3.8 million square miles). Its global population estimated to be 3.8–6.7 million individuals. For these reasons, the species is evaluated as Least Concern.[1] On the other hand the expansion and establishment of the species over large ranges has led it to be classed as an invasive species (although little, if any impact has been noted yet).[
Behaviour
Breeding
The Cattle Egret nests in colonies, which are often, but not always, found around bodies of water.[19] The colonies are usually found in woodlands near lakes or rivers, in swamps, or on small inland or coastal islands, and are sometimes shared with other wetland birds, such as herons, egrets, ibises and cormorants. The breeding season varies within South Asia.[7] Nesting in northern India begins with the onset of monsoons in May.[37] The breeding season in Australia is November to early January, with one brood laid per season.[38] The North American breeding season lasts from April to October.[19] In the Seychelles, the breeding season of the subspecies B.i. seychellarum is April to October.[39]
The male displays in a tree in the colony, using a range of ritualised behaviours such as shaking a twig and sky-pointing (raising bill vertically upwards),[40] and the pair forms over three or four days. A new mate is chosen in each season and when re-nesting following nest failure.[41] The nest is a small untidy platform of sticks in a tree or shrub constructed by both parents. Sticks are collected by the male and arranged by the female, and stick-stealing is rife.[14] The clutch size can be anywhere from one to five eggs, although three or four is most common. The pale bluish-white eggs are oval-shaped and measure 45 mm × 53 mm. (1.8–2.1 in)[38] Incubation lasts around 23 days, with both sexes sharing incubation duties.[19] The chicks are partly covered with down at hatching, but are not capable of fending for themselves; they become capable of regulating their temperature at 9–12 days and are fully feathered in 13–21 days.[42] They begin to leave the nest and climb around at 2 weeks, fledge at 30 days and become independent at around the 45th day.[41]
The Cattle Egret engages in low levels of brood parasitism, and there are a few instances of Cattle Egret eggs being laid in the nests of Snowy Egrets and Little Blue Herons, although these eggs seldom hatch.[19] There is also evidence of low levels of intraspecific brood parasitism, with females laying eggs in the nests of other Cattle Egrets. As much as 30% extra-pair copulations have been noted.[43][44]
The dominant factor in nesting mortality is starvation. Sibling rivalry can be intense, and in South Africa third and fourth chicks inevitably starve.[41] In the dryer habitats with fewer amphibians the diet may lack sufficient vertebrate content and may cause bone abnormalities in growing chicks due to calcium deficiency.[45] In Barbados, nests were sometimes raided by vervet monkeys,[8] and a study in Florida reported the Fish Crow and black rat as other possible nest raiders. The same study attributed some nestling mortality to Brown Pelicans nesting in the vicinity, which accidentally, but frequently, dislodged nests or caused nestlings to fall.[46] In Australia, Torresian Crows, Wedge-tailed Eagles and White-bellied Sea Eagles take eggs or young, and tick infestation and viral infections may also be causes of mortality.
Feeding
The Cattle Egret feeds on a wide range of prey, particularly insects, especially grasshoppers, crickets, flies (adults and maggots [47]), and moths, as well as spiders, frogs, and earthworms.[48][49] In a rare instance they have been observed foraging along the branches of a Banyan tree for ripe figs.[50] The species is usually found with cattle and other large grazing and browsing animals, and catches small creatures disturbed by the mammals. Studies have shown that Cattle Egret foraging success is much higher when foraging near a large animal than when feeding singly.[51] When foraging with cattle, it has been shown to be 3.6 times more successful in capturing prey than when foraging alone. Its performance is similar when it follows farm machinery, but it is forced to move more.[52]
A Cattle Egret will weakly defend the area around a grazing animal against others of the same species, but if the area is swamped by egrets it will give up and continue foraging elsewhere. Where numerous large animals are present, Cattle Egrets selectively forage around species that move at around 5–15 steps per minute, avoiding faster and slower moving herds; in Africa, Cattle Egrets selectively forage behind Plains Zebras, Waterbuck, Blue Wildebeest and Cape Buffalo.[53] Dominant birds feed nearest to the host, and obtain more food.[14]
The Cattle Egret may also show versatility in its diet. On islands with seabird colonies, it will prey on the eggs and chicks of terns and other seabirds.[30] During migration it has also been reported to eat exhausted migrating landbirds.[54] Birds of the Seychelles race also indulge in some kleptoparasitism, chasing the chicks of Sooty Terns and forcing them to disgorge food.[
Relationship with humans
A conspicuous species, the Cattle Egret has attracted many common names. These mostly relate to its habit of following cattle and other large animals, and it is known variously as cow crane, cow bird or cow heron, or even elephant bird, rhinoceros egret.[19] Its Arabic name, abu qerdan, means "father of ticks", a name derived from the huge number of parasites such as avian ticks found in its breeding colonies.[19][56]
The Cattle Egret is a popular bird with cattle ranchers for its perceived role as a biocontrol of cattle parasites such as ticks and flies.[19] A study in Australia found that Cattle Egrets reduced the number of flies that bothered cattle by pecking them directly off the skin.[57] It was the benefit to stock that prompted ranchers and the Hawaiian Board of Agriculture and Forestry to release the species in Hawaii.[30][58]
Not all interactions between humans and Cattle Egrets are beneficial. The Cattle Egret can be a safety hazard to aircraft due to its habit of feeding in large groups in the grassy verges of airports,[59] and it has been implicated in the spread of animal infections such as heartwater, infectious bursal disease[60] and possibly Newcastle disease
Source: en.wikipedia.org/wiki/Pensacola,_Florida
Pensacola is the westernmost city in the Florida Panhandle, and the county seat of Escambia County, Florida. As of 2018, the population was estimated to be 52,713. Pensacola is the principal city of the Pensacola Metropolitan Area, which had an estimated 494,883 residents as of 2018. Pensacola is one of the largest metropolitan areas in the Gulf Coast region, the largest between New Orleans and Tampa.
Pensacola is the site of the first Spanish settlement within the borders of the continental United States in 1559, predating the establishment of St. Augustine by 6 years, although the settlement was abandoned due to a hurricane and not re-established until 1698. Pensacola is a seaport on Pensacola Bay, which is protected by the barrier island of Santa Rosa and connects to the Gulf of Mexico. A large United States Naval Air Station, the first in the United States, is located southwest of Pensacola near Warrington; it is the base of the Blue Angels flight demonstration team and the National Naval Aviation Museum. The main campus of the University of West Florida is situated north of the city center.
The area was originally inhabited by Muskogean-speaking peoples. The Pensacola people lived there at the time of European contact, and Creek people frequently visited and traded from present-day southern Alabama. Spanish explorer Tristán de Luna founded a short-lived settlement in 1559. In 1698 the Spanish established a presidio in the area, from which the modern city gradually developed. The area changed hands several times as European powers competed in North America. During Florida's British rule (1763–1781), fortifications were strengthened.
It is nicknamed "The City of Five Flags", due to the five governments that have ruled it during its history: the flags of Spain (Castile), France, Great Britain, the United States of America, and the Confederate States of America. Other nicknames include "World's Whitest Beaches" (due to the white sand of Florida panhandle beaches), "Cradle of Naval Aviation", "Western Gate to the Sunshine State", "America's First Settlement", "Emerald Coast", "Red Snapper Capital of the World", and "P-Cola".
Source: en.wikipedia.org/wiki/T._T._Wentworth_Jr._Florida_State_M...
The T. T. Wentworth Jr. Florida State Museum is a museum of history located at 330 Jefferson Street in the Plaza Ferdinand VII in Pensacola, Florida. It is part of the Historic Pensacola Village museum complex. The building, reminiscent of the Alamo mission style, was built in 1907 as the Pensacola City Hall and served as such until 1985 when the present city hall was built at 180 Governmental Center, also known as 222 West Main Street. In 1989, the building was listed as the Pensacola City Hall in A Guide to Florida's Historic Architecture, published by the University of Florida Press.
en.wikipedia.org/wiki/White_Cliffs_of_Dover
The White Cliffs of Dover are cliffs that form part of the English coastline facing the Strait of Dover and France. The cliffs are part of the North Downs formation. The cliff face, which reaches up to 350 feet (110 m),[1] owes its striking appearance to its composition of chalk accented by streaks of black flint. The cliffs stretch along the coastline for eight miles (13 km), spreading east and west from the town of Dover in the county of Kent, an ancient and still important English port.[2]
The cliffs have great symbolic value in Britain because they face towards continental Europe across the narrowest part of the English Channel, where invasions have historically threatened and against which the cliffs form a symbolic guard. The National Trust calls the cliffs "an icon of Britain", with "the white chalk face a symbol of home and war time defence."[3] Because crossing at Dover was the primary route to the continent before the advent of air travel, the white line of cliffs also formed the first or last sight of Britain for travellers. In World War II, thousands of allied troops on the little ships in the Dunkirk evacuation saw the welcoming sight of the cliffs.
Location
The cliffs are located along the coastline of England between approximately 51°06′N 1°14′E and 51°12′N 1°24′E. The White Cliffs are at one end of the Kent Downs designated Area of Outstanding Natural Beauty.[5]
During the summer of 1940, reporters gathered at Shakespeare Cliff to watch aerial dogfights between German and British aircraft during the Battle of Britain.[6] It marks the point where Great Britain most closely approaches continental Europe. On a clear day, the cliffs are easily visible from the French coast.
In 1999 a sustainable National Trust visitor centre was built in the area. The Gateway building was designed by van Heyningen and Haward Architects and houses a restaurant, an information centre on the work of the National Trust, and details of local archaeology, history and landscape.[7]
Geology
The cliffs themselves were formed at the same time as the Strait of Dover, by ice-age floods.
The cliffs are mainly soft white chalk with a very fine-grained texture, composed primarily of coccoliths, plates of calcium carbonate formed by coccolithophores, single-celled planktonic algae whose skeletal remains sank to the bottom of the ocean during the Cretaceous and, together with the remains of bottom-living creatures, formed sediments.[8] Flint and quartz are also found in the chalk.[9] White cliffs like those of Dover are also found on the Danish islands of Møn and Langeland and the island of Rügen in Germany. The chalk cliffs of the Alabaster Coast of Normandy, France, are part of the same geological system as Dover's cliffs. In a 2005 poll of Radio Times readers, the cliffs were named as the third greatest natural wonder in Britain.
The cliff face continues to weather at an average rate of 1 centimetre (0.4 in) per year, although occasionally large pieces will fall. This occurred in 2001, when a large chunk of the edge, as large as a football pitch, fell into the Channel.[10] A further large section collapsed into the Channel on 15 March 2012.[11] Visitors are, therefore, urged to remain well away from the cliff edge.
Ecology
Several species of cliff nesting birds nest on the cliff face, including fulmar and colonies of black-legged kittiwake. However, contrary to the words of the World War II song "White Cliffs of Dover", bluebirds are an American species not found in the UK.
PLASENCIA (Wiki): de.wikipedia.org/wiki/Plasencia
PLASENCIA (Tourismus): reisen-nach-spanien.com/extremadura/plasencia#9/40.0423/-...
en.wikipedia.org/wiki/River_Wharfe
The River Wharfe is a river in Yorkshire, England. For much of its length it is the county boundary between West Yorkshire and North Yorkshire. The name Wharfe is Celtic and means "twisting, winding".
The valley of the River Wharfe is known as Wharfedale. The river source is at Beckermonds, Langstrothdale in the Yorkshire Dales National Park and flows through Kettlewell, Grassington, Bolton Abbey, Addingham, Ilkley, Burley-in-Wharfedale, Otley, Wetherby and Tadcaster. It then flows into the River Ouse near Cawood. The section of the river from its source to around Addingham is known as Upper Wharfedale and has a very different character to the river downstream.
The river is approximately 97 km long before it joins the River Ouse. It is a public navigation from the weir at Tadcaster to its junction with the River Ouse near Cawood and tidal from Ulleskelf.
Course
The river source is the confluence of Oughtershaw Beck and Green Field Beck in Langstrothdale near Beckermonds. It flows east and south east taking the flows from many small streams, whose sources are the shake holes from Yockenthwaite Moor on the north bank and Horse Head Moor on the south bank. After Hubberholme, the river flows south past Buckden and Starbotton and then south east past Kettlewell before flowing south again. Near Conistone are the gentle waterfalls of Scar Lash. Near Grassington, the river turns south east over Linton Falls. South of Appletreewick, the river flows south west for a short distance until it reaches Gill Beck and returns southward. To the north of Bolton Bridge, the river narrows and goes over waterfalls in an area known as The Strid. The river winds south and south east towards Ilkley where it heads east through Otley and Collingham. It briefly flows north to Wetherby before turning south and then south east past Ulleskelf to the confluence with the River Ouse.
Water levels
Monitoring Station[1]
Station Elevation
Low water level
High water level
Record high level
Kettlewell 212 m (696 ft) 0.17 m (0.56 ft) 2 m (6.6 ft) 2.54 m (8.3 ft)
Grassington 171 m (561 ft) 0 m (0 ft) 1.5 m (4.9 ft) 2.79 m (9.2 ft)
Ilkley 78 m (256 ft) 0.09 m (0.30 ft) 2.9 m (9.5 ft) 3.88 m (12.7 ft)
Otley 56 m (184 ft) 0.36 m (1.2 ft) 1.5 m (4.9 ft) 2.46 m (8.1 ft)
Pool Bridge 46 m (151 ft) 0.09 m (0.30 ft) 2.9 m (9.5 ft) 3.77 m (12.4 ft)
Arthington 46 m (151 ft) 0.32 m (1.0 ft) 3.3 m (11 ft) 4.14 m (13.6 ft)
Collingham 25 m (82 ft) 0.35 m (1.1 ft) 1.59 m (5.2 ft) 4.7 m (15 ft)
Wetherby 25 m (82 ft) 0.4 m (1.3 ft) 1.8 m (5.9 ft) 3.10 m (10.2 ft)
Tadcaster 11 m (36 ft) 0.18 m (0.59 ft) 2.9 m (9.5 ft) 3.79 m (12.4 ft)
Cock Beck Sluices 6 m (20 ft) 3.44 m (11.3 ft) 7.3 m (24 ft) 9.26 m (30.4 ft)
Fleet Pumping Station 6 m (20 ft) 2 m (6.6 ft) 6.5 m (21 ft) 7.35 m (24.1 ft)
Low and High Water Levels are an average figure.
Natural history
Fauna
There are over 230 species of bird observed along the river valley including Eagle-Owl, Red Grouse, Stonechat, Whinchat, Golden Plover, Pied Flycatcher, Redstart, Wood Warbler, Common Sandpiper, Grey Wagtail, Dipper, Tawny Owl, Sparrowhawk, Greater Spotted Woodpecker, Nuthatch, Treecreeper and, in wetter places, Snipe and Woodcock, Chiffchaff, Willow Warbler, Garden Warbler, and Twite.[2]
The Wharfe has populations of Signal Crayfish and the few White-clawed Crayfish remaining are at great risk.[2]
There are populations of Rabbit, Red Fox, Grey Squirrel, Otter, Water Voles and deer.[2][3][4]
Flora
Ferns found here include Wall Rue, Maidenhair Spleenwort, Brittle Bladder-fern, Hart's-tongue and Hard Shield-fern. In Upper Wharfedale the scars and screes support a range of plants including the Alpine Cinquefoil and Hoary Whitlowgrass. Also to be found are Lesser Meadow-rue, Goldenrod, Scabious and Bloody Crane's-bill with, to a lesser extent, Mountain Melick, Limestone Fern, Wood Crane's-bill and Melancholy Thistle, Green Spleenwort, Wall Lettuce and Hairy Stonecrop.[2]
Lower down the valley, species including Alpine Cinquefoil, Lily-of-the-valley, Mountain Melick and Herb Paris, blue sesleria, Common Valerian and Wild Angelica. The limestone outcrops have uncommon species including Rock Whitebeam and Solomon's Seal as well as Bird's-eye Primrose, Butterwort, Rockrose, Dropwort and Limestone Bedstraw.
The limestone pavements of the area are a habitat for several species usually confined to woodlands, such as Dog's Mercury, Wood Anemone and Ramsons. Rarer species to be found in the grikes include Baneberry and Downy Currant. Ferns in the moist grikes include Rigid Buckler-fern. Also to be found are Alternate-leaved Golden Saxifrage, Reed Canary-grass and Stone Bramble.
Some of the inaccessible cliffs are home to ledge dwelling flora including mosses and liverworts, such as Red Leskea, Sharp Rock-bristle and the very rare Zygodon gracilis. The ledges also support Woodrush, Polypody and Water Avens, Purple Saxifrage, Yellow Saxifrage, Hoary Whitlowgrass and Roseroot.
Blue Moor-grass can also be found, with Sheep's-fescue and herbs such as Thyme, Salad Burnet and Common Rock-rose. There is Wild Thyme, Common Milkwort, Fairy Flax, Bird's-foot Trefoil, Autumn Gentian, Harebell, Eyebright.
Species of tree and shrub include Ash, Downy Birch, Hazel, Hawthorn, Yew and Rowan. In the woods shrubs such as Wild Privet and Spindle can be found. More rare is Dark Red Helleborine.[2][5]
Geology
Upper Wharfedale is an area from the Lower Carboniferous era and lies north-west of Burnsall. Its main features are the Great Scar Limestone which forms a base to the overlying Yoredale Beds, a 300-metre deep strata of hard limestones, sandstones and shale. These have been slightly tilted, toward the east. To the south-east of the area are the Millstone Grit laid down in the Upper Carboniferous era, and is covered by heather moorland, hard crags and tors.[6][7]
Weathering of the Yoredale Beds has produced a stepped profile to the valley sides, consisting of a shelf of limestone, sometimes grassy but often displaying such karst features as limestone pavement, gorges and sinkholes. During the last ice age, the local ice cap at the head of the Dales fed glaciers to produce the classic U-shaped profiles seen today.[8]
Where the river valley changes course into Lower Wharfedale, the change of underlying rock can be seen in the darker stone in the field walls. The Millstone Grit outcrops at the Cow and Calf Rocks near Ilkley form a rolling dissected plateau. Due to the impermeable nature of the rock, blanket bogs and mires form, and drier areas have wet and dry heaths and acid grasslands.[9]
Coarse sandstones in the area are known as Addingham Edge and Bramhope Grits. The Otley Shell Beds become exposed at Otley Chevin. At Great Dib Wood the Otley Shell Bed is sandwiched between two Namurian sandstones.
Glacial lakes once filled Lower Wharfedale and deposited sand and gravel. These were quarried and now form the basis of the Otley Wetland Reserve, and Ben Rhydding and Knotford Nook gravel pits.[10]
Waterfalls
Linton Fall (Grid Reference: SE001633) are located just south of Grassington and can be accessed from the village down Sedber Lane. There is a footbridge straddling the falls for viewing.
The Strid (Grid Reference: SE064565) is a series of waterfalls and rapids associated with a deep underwater channel caused by the dramatic narrowing of the River Wharfe from approximately 30 ft (9 m) wide just to the north of the start of the Strid, to the width of a long stride less than 100 yd (91 m) later.[11] It is especially dangerous as both banks are undercut,[12][13] and it has been the scene of a number of fatalities including those of a honeymoon couple.[14] The Strid walk is very popular and is accessed from the car park at Bolton Abbey.[15]
History
Wharfe is a Celtic river name meaning the winding river.[16][17]
Iron Age fields and hut circles can still be seen in outline on the hills above Grassington and Kettlewell.[7] The Romans built a road through Wharfedale that went over Stake Moss into neighboring Wensleydale. The local tribe of Brigantes were subdued by the Romans in AD 74. The Romans mined lead in the hills on Greenhow Hill overlooking Appletreewick until AD 410.[7] After AD 620 the Celtic settlers were joined by Angles and increased the amount of forest clearing to establish fields for crops and animals. These were overrun by Danes initially before they too settled to farming near Burnsall and Thorpe. Vikings then settled the area in the 10th century, lending their language to some of the names of hamlets and landscape features of Upper Wharfedale, especially near the head of the valley.[7] During Anglo-Saxon times, large estates were established and the River Wharfe and its valley came under the protection of Earl Edwin of Bolton-in-Craven. After the Norman invasion, the lands were given to Robert Romilly.[7]
In medieval times low intensity methods were used to produce both crops and livestock but the great monasteries of Fountains, Rievaulx and Bolton Priory had large sheep flocks and sold their wool on the European market. In 1155, Alice de Romilly donated land for the establishment of Bolton Priory and land at Kilnsey to Fountains Abbey. The monasteries helped develop vast sheep farms and the founding of drove roads, which can still be seen and walked today. The success of the monasteries was also responsible for the growth of the market towns of Grassington and Kettlewell.[7]
When the monasteries were dissolved in 1539, and wool prices fell, many tenant farmers took to cattle and sheep rearing. However, at the end of the 17th century there was still small-scale arable production. By the early nineteenth century there was a demand for food from the growing industrial towns and farmers and many farms began to produce milk from the lower lands and use the higher fells for sheep.[18]
The river has had appearances in films. In 1992, the town of Grassington was used as a filming location for Wuthering Heights.[19] The 2003 film, Calendar Girls, was filmed at several locations in the river valley including Buckden, Burnsall, Kettlewell and Kilnsey.[20]
Economy
During the 1990s there had been an increase in the number of second home ownership, particularly in the Upper Wharfedale area. This had been partly due to subsidised Council Tax rates for a second property. The 1991 census had shown 13% of homes were classified as second properties, which had risen to 18% by late 1998.[21] The 2001 census showed that this figure had dropped to 15%[22] and further still to just 7% by 2011.[23]
The Upper Wharfedale area has been traditionally associated with farming, but there has been a change in the numbers and types of employment. Whilst there were declines in the number of people in this industry, farming accounted directly for 9.16%[24] of employment in 2001 but this had increased to 11.27% by 2011.[25]
Lead mining was once the main industry in Wharfedale. From the seventeenth century to the late nineteenth it employed hundreds of men and boys, exploiting the veins in the limestone at Greenhow, Hebden, Grassington, Linton and Conistone, Appletreewick and elsewhere. The heaps of mining waste remain, contaminated with lead, and on which little will grow. The few plants that will are known as 'lead plants' such as spring sandwort and alpine penny-cress.[26][27]
Tourism is big part of the rural economy in Wharfedale and there are many short, mid and long distance walks, with clear waymarkers. There are also other outdoor activities such as rock climbing, most notably at Kilnsey Crag, and canoeing. Other activities include cycling, mountain biking, horse riding and caving.[28] The following Long Distance Walks pass near or over the river:[29]
Dales Way (follows the river valley from Beckermonds to Ilkley)
Lady Anne's Way (enters the river valley near Hubberholme and leaves to the west of Bolton Abbey)
Inn Way to the Yorkshire Dales (part of walk from Grassington to Buckden)
The Way of the Roses (part of the cycle route from Appletreewick to Thorpe)
Lists
All lists are from the source of the river:-[30]
Tributaries
Deepdale Gill
Hagg Gill
Bowther Gill
Strans Gill
Kirk Gill
Cow Close Gill
Buckden Beck
Step Gill
Cam Gill Beck
Falcon Beard Beck
Hush Gutter
Kettlewell Beck
Black Geld
River Skirfane
How Beck
White Beck
Davy Keld
Dib Beck
Robin Hood's Beck
Captain Beck
Brow Well
Isingdale Beck
Howling Beck
Hebden Beck
Sandbed Beck
Barden Beck
The Old Gutter
Hall Wells Dike
Foul Sike
Fir Beck
Bumby Dike
Gill Beck
Hollin Beck
Posforth Gill
Cowpert Gill
Stead Dike
Pickles Beck
Raven's Gill Beck
Kex Beck
Lathehouse Beck
Wine Beck
West Hall Beck
Dean Beck
Mill Stream
West Beck
Mill Dam Beck
Boot's Beck
River Washburn
Weeton Beck
Stank Beck
Collingham Beck
Hay Dike
Cock Beck
Owl Sike
Pailbank Drain
The Fleet
Settlements
Beckermonds
Deepdale
Yockenthwaite
Hubberholme
Buckden
Starbotton
Kettlewell
Kilnsey
Conistone
Threshfield
Grassington
Linton
Hebden
Burnsall
Appletreewick
Bolton Abbey
Beamsley
Addingham
Nesfield
Ilkley
Burley in Wharfedale
Otley
Pool
Castley
Netherby
Chapel Hill
Collingham
Linton
Wetherby
Boston Spa
Thorp Arch
Newton Kyme
Tadcaster
Kirkby Wharfe
Ulleskelf
Ozendyke
Ryther
Crossings
New House Farm footbridge
Deepdale Bridge
Yockenthwaite Bridge
Hubberholme Bridge
Buckden Bridge
Starbotton footbridge
B6160 Kettlewell New Bridge
Conistone Bridge
B6265 Grassington Bridge
Tin Bridge (footbridge), Linton Falls
Linton stepping stones
Suspension Bridge (footbridge), Hebden
Burnsall Bridge
Drebley stepping stones
Barden Bridge
Barden Aqueduct and footbridge
Wooden Bridge (at Cavendish Pavilion)
Friars' Steps (stepping stones)
Waterfall Bridge (footbridge)
Bolton Bridge
A59 Bridge
Suspension Bridge (footbridge), Addingham
Old Bridge, Ilkley (footbridge)
New Bridge, Ilkley (New Brook Street)
Ilkley Susupension Bridge (footbridge)
Denton Bridge
Greenholme stepping stones
B6451 Otley Bridge
Footbridge
A658 Pool Bridge
Railway Bridge (Leeds-Harrogate railway line)
A61 Harewood Bridge
Woodhall Bridge (footbridge)
Linton Bridge, Collingham
Footbridge
A661 Wetherby Bridge
A58 bridge, Wetherby
A1(M) bridge, Wetherby
Thorp Arch Bridge, Boston Spa
Wharfe Bridge (dismantled railway)
Viaduct Walk, Tadcaster (footbridge)
A659 Tadcaster Bridge
A64 bridge (Tadcaster By-pass)
Railway Bridge (Dearne Valley Line)
East Coast Main Line Railway Bridge
de.wikipedia.org/wiki/Hain-B%C3%A4nderschnecke
Die Hain-Bänderschnecke (Cepaea nemoralis) – auch Hain-Schnirkelschnecke oder Schwarzmündige Bänderschnecke genannt – gehört zur Familie der Schnirkelschnecken (Helicidae), die zur Ordnung der Lungenschnecken (Pulmonata) gerechnet wird.
www.nabu.de/tiere-und-pflanzen/sonstige-arten/weichtiere/...
Färbung und Lebensraum bedingen sich
Wenn die Individuen einer Art ganz verschieden aussehen können, spricht die Wissenschaft von Polymorphismus. Der extreme Polymorphismus der Bänderschnecken ist schon seit Jahrhunderten Gegenstand wissenschaftlicher Forschungen. Besonders die Frage nach der genetischen Fixierung der verschiedenen Muster stand hier oft im Vordergrund. Spannend ist auch die Abhängigkeit der Farbe und Musterung vom Lebensraum. Ein wichtiger Punkt sind dabei die Prädatoren, also jene Tiere, die den Schnecken nachstellen. So ist es einleuchtend, dass in Gebüschen lebende Schnecken am besten getarnt sind, wenn sie ein kräftiges Streifenmuster aufweisen, womit sie zwischen den Schatten der Zweige optisch verschwinden. In Wäldern haben dunkle Farben Vorteile und in offenen Grasbiotopen dominieren oft helle Farben. Wer davon abweicht, kann am besten von Fressfeinden, zum Beispiel Singdrosseln, erbeutet und somit ausgelesen werden.
Lebensgrundlage für viele Tiere
Während wir uns nur an der Farbenpracht und Vielfalt der Bänderschnecken erfreuen, haben sie für eine Vielzahl von Tieren große Bedeutung. Manche Arten sind sogar zum Überleben auf Bänderschnecken, aber auch andere Schnecken-Arten, angewiesen.
Die Singdrossel als Schneckenjäger haben wir schon erwähnt. Doch auch für andere Vogelarten sind Schnecken lebenswichtige Nahrung, denn das Kalzium der Schneckenhäuser ist Baustoff für Eierschalen und Knochen. Vogelforscher haben herausgefunden, dass beim Rückgang der Schnecken auch die Qualität der Eierschale und in Folge der Bruterfolg von Singvögeln zurückging.
en.wikipedia.org/wiki/Forest_of_Bowland
The Forest of Bowland, also known as the Bowland Fells, is an area of barren gritstone fells, deep valleys and peat moorland, mostly in north-east Lancashire, England. A small part lies in North Yorkshire, and much of the area was historically part of the West Riding of Yorkshire. It has been designated an Area of Outstanding Natural Beauty (AONB) since 1964, and is used for grouse shooting, walking and cycling, though it is relatively unfrequented by tourists. One of the best known features of the area is Pendle Hill, which is separated from the main part of the Forest of Bowland AONB by the Ribble Valley.
13% of the AONB is designated a Site of Special Scientific Interest for its important areas of heather moorland and blanket bog. The area is nationally and internationally important for its upland bird populations – the hen harrier is the symbol of the AONB. There are over 500 listed buildings and 18 scheduled monuments within the AONB.
The name 'forest' is used in its traditional sense of 'a royal hunting ground', and much of the land still belongs to the British Crown as part of the Duchy of Lancaster. In the past wild boar, deer, wolves, wild cats and game roamed the forest.
Heather moorland on Clougha, in the north west of the Forest of Bowland, looking towards the Yorkshire three peaks
Bowland remains as the northwestern remainder of the ancient wilderness that once stretched over a huge part of England, encompassing the Forest of Bowland, Sherwood Forest (Nottinghamshire), the New Forest (Hampshire) and Savernake Forest (Wiltshire). While the Trough of Bowland (the valley and high pass connecting the Wyre (at Marshaw) and Langden Brook and dividing the upland core of Bowland into two main blocks) represents the area, to many, on account of its popularity, it is in fact only a small part of the wider Forest of Bowland area.
The hills on the western side of the Forest of Bowland attract walkers from Lancaster and the surrounding area. Overlooking Lancaster is Clougha Pike, the western-most hill. The hills form a large horseshoe shape with its open end facing west. Clockwise from Lancaster the hills are Clougha Pike (413 m), Grit Fell (468 m), Ward's Stone (561 m), Wolfhole Crag (527 m), White Hill (544 m), Whins Brow (476 m), Totridge (496 m), Parlick (432 m), Fair Snape Fell (510 m), Bleasdale Moor (429 m), and Hawthornthwaite fell (478 m).
The area is home to the geographic centre of Great Britain which is close to the Whitendale Hanging Stones, around 4 miles (6.4 km) north of Dunsop Bridge.
The Forest of Bowland is home to an annual challenge event: The Bowland Challenge where teams of walkers navigate around a series of grid references over a ten hour period. Proceeds of the event go to support Bowland Pennine Mountain Rescue Team.
en.wikipedia.org/wiki/Durlston_Castle
Durlston Castle stands within Durlston Country Park, a 1.13 square-kilometre (280-acre) country park and nature reserve stretching along the coastline south of Swanage, on the Isle of Purbeck in Dorset.
History
John Mowlem[1] (1788-1868), a Swanage-born man, was a stonemason and builder. He was the founder of the quarrying and construction company Mowlem. He and his nephew and business partner George Burt[2] (1816-1894) wanted to give something back to their home town, which was the source of their Portland and Purbeck limestone, popular for building at the time. John Mowlem built the Mowlem Institute, a reading room and public library, in 1862. George Burt purchased an undulating tract of land covering Durlston Head during the same year. This estate, the Durlston Estate, included quarries that supplied their firm with limestone. Burt developed this estate as a tourist attraction.
Burt established the Durlston Estate upon the crest of the hill and here he built his folly Durlston Castle. The castle was designed by the Weymouth architect G.R. Crickmay (1830-1907) and built by W.M. Hardy in 1886-87 entirely of local stone. The 'castle' was never a real castle: it was purpose-built by Burt as a restaurant for the visitors to his estate.
The castle played a part in the evolution of radio and telecommunications. A team of Marconi's engineers used the roof of the castle in the 1890s for some of their early wireless experiments to transmit to the Isle of Wight.
The castle passed through the hands of many owners until in 1973 it was bought by Dorset County Council.
Description
The side wall of the castle features a sundial and two stone tablets inscribed with various statistics such as clock times and tides around the world. South of the castle is the Great Globe, built by Burt in 1887.[3] The footpaths around the Castle and Great Globe are lined with cast iron bollards that were brought from London. All around the estate there are further stone plaques carved with quotations from Shakespeare and the Bible, maps showing the English Channel and the United Kingdom, and further facts about the natural world. These surrounds were placed during the period 1887 to 1891.
Also within the Durlston Country Park and within walking distance of the Globe are Durlston Bay, the Tilly Whim Caves and the Anvil Point Lighthouse. The Park is part of the Jurassic Coast World Heritage Site.
Restoration
Durlston Castle and the Great Globe were both restored during 2010 and 2011 by the Council.[4][5] The castle now houses a new Visitor Centre to Durlston Country Park and National Nature Reserve, and stands as a gateway to the Jurassic Coast.
Source: en.wikipedia.org/wiki/Grand_Canyon
The Grand Canyon is a steep-sided canyon carved by the Colorado River in Arizona, United States. The Grand Canyon is 277 miles (446 km) long, up to 18 miles (29 km) wide and attains a depth of over a mile (6,093 feet or 1,857 meters).
The canyon and adjacent rim are contained within Grand Canyon National Park, the Kaibab National Forest, Grand Canyon–Parashant National Monument, the Hualapai Indian Reservation, the Havasupai Indian Reservation and the Navajo Nation. The surrounding area is contained within the Baaj Nwaavjo I'tah Kukveni – Ancestral Footprints of the Grand Canyon National Monument. President Theodore Roosevelt was a major proponent of the preservation of the Grand Canyon area and visited it on numerous occasions to hunt and enjoy the scenery.
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 some aspects about the history of incision of the canyon are debated by geologists, several recent studies support the hypothesis that the Colorado River established its course through the area about 5 to 6 million years ago. Since that time, the Colorado River has driven the down-cutting of the tributaries and retreat of the cliffs, simultaneously deepening and widening the canyon.
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 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.
Source: en.wikipedia.org/wiki/Grand_Canyon_National_Park
Grand Canyon National Park is a national park of the United States located in northwestern Arizona, the 15th site to have been named as a national park. The park's central feature is the Grand Canyon, a gorge of the Colorado River, which is often considered one of the Wonders of the World. The park, which covers 1,217,262 acres (1,901.972 sq mi; 4,926.08 km2) of unincorporated area in Coconino and Mohave counties, received more than 4.7 million recreational visitors in 2023. The Grand Canyon was designated a World Heritage Site by UNESCO in 1979. The park celebrated its 100th anniversary on February 26, 2019.
Source: www.nps.gov/grca/index.htm
Entirely within the state of Arizona, the park encompasses 278 miles (447 km) of the Colorado River and adjacent uplands. Located on the ancestral homelands of 11 present day Tribal Communities, Grand Canyon is one of the most spectacular examples of erosion anywhere in the world—a mile deep canyon unmatched in the incomparable vistas it offers visitors from both north and south rims.
Additional Foreign Language Tags:
(United States) "الولايات المتحدة" "Vereinigte Staaten" "アメリカ" "米国" "美国" "미국" "Estados Unidos" "États-Unis" "ארצות הברית" "संयुक्त राज्य" "США"
(Arizona) "أريزونا" "亚利桑那州" "אריזונה" "एरिजोना" "アリゾナ州" "애리조나" "Аризона"
(Grand Canyon) "جراند كانيون" "大峡谷" "גרנד קניון" "ग्रांड कैन्यन" "グランドキャニオン" "그랜드 캐니언" "Гранд-Каньон" "Gran Cañón"
Pont Beatus Rhenanus
fr.wikipedia.org/wiki/Pont_Beatus-Rhenanus
28, 29 et 30 avril 2017, fête franco allemande pour l'inauguration de la nouvelle ligne de tamway qui relie Strasbourg (France) à Kehl (Allemagne).
Un nouveau pont a été construit pour franchir le Rhin. Un pont exclusivement réservé au tramway, aux piétons et cyclistes.
A Strasbourg eurométropole, capitale de l'europe, "On préfère y construire des ponts que des murs" comme a dit le maire de Strasbourg Roland Ries.
La nuit l'eclairage des arches du pont sont aux couleurs de la france sur la partie française du pont, et, aux couleurs de l'allemagne sur la partie allemande...
Beatus Rhenanus brücke
28, 29. und 30. April 2017 der deutsch-französisches Festival für die Einweihung der neuen Linie von tamway verbindet Straßburg (Frankreich) Kehl (Deutschland).
Eine neue Brücke wurde gebaut, um den Rhein zu überqueren. Eine ausschließlich Brücke Straßenbahn, Fußgänger und Radfahrer.
In Straßburg Eurometropole , die Hauptstadt von Europa, „bevorzugt Brücken als Mauern zu bauen“, wie er sagte der Bürgermeister von Straßburg Roland Ries.
Nachts wird die Beleuchtung der Brückenbögen sind die Farben von Frankreich auf der Französisch Seite der Brücke, und die Farben von Deutschland auf der deutschen Seite ...
Beatus Rhenanus bridge
28, 29 and 30 April 2017, Franco-German celebration for the inauguration of the new Tamway line connecting Strasbourg (France) to Kehl (Germany).
A new bridge was built to cross the Rhine. A bridge exclusively reserved for tramway, pedestrians and cyclists.
In Strasbourg eurometropole, capital of europe, "We prefer to build bridges as walls" as the mayor of Strasbourg Roland Ries said.
At night the lighting of the arches of the bridge are in the colors of france on the French part of the bridge, and, in the colors of germany on the German part ...
Source: en.wikipedia.org/wiki/Pensacola,_Florida
Pensacola is the westernmost city in the Florida Panhandle, and the county seat of Escambia County, Florida. As of 2018, the population was estimated to be 52,713. Pensacola is the principal city of the Pensacola Metropolitan Area, which had an estimated 494,883 residents as of 2018. Pensacola is one of the largest metropolitan areas in the Gulf Coast region, the largest between New Orleans and Tampa.
Pensacola is the site of the first Spanish settlement within the borders of the continental United States in 1559, predating the establishment of St. Augustine by 6 years, although the settlement was abandoned due to a hurricane and not re-established until 1698. Pensacola is a seaport on Pensacola Bay, which is protected by the barrier island of Santa Rosa and connects to the Gulf of Mexico. A large United States Naval Air Station, the first in the United States, is located southwest of Pensacola near Warrington; it is the base of the Blue Angels flight demonstration team and the National Naval Aviation Museum. The main campus of the University of West Florida is situated north of the city center.
The area was originally inhabited by Muskogean-speaking peoples. The Pensacola people lived there at the time of European contact, and Creek people frequently visited and traded from present-day southern Alabama. Spanish explorer Tristán de Luna founded a short-lived settlement in 1559. In 1698 the Spanish established a presidio in the area, from which the modern city gradually developed. The area changed hands several times as European powers competed in North America. During Florida's British rule (1763–1781), fortifications were strengthened.
It is nicknamed "The City of Five Flags", due to the five governments that have ruled it during its history: the flags of Spain (Castile), France, Great Britain, the United States of America, and the Confederate States of America. Other nicknames include "World's Whitest Beaches" (due to the white sand of Florida panhandle beaches), "Cradle of Naval Aviation", "Western Gate to the Sunshine State", "America's First Settlement", "Emerald Coast", "Red Snapper Capital of the World", and "P-Cola".
Source: en.wikipedia.org/wiki/Pinckneyville,_Illinois
Pinckneyville is a city in and the county seat of Perry County, Illinois, United States. The population was 5,066 at the 2020 census. It is named for Charles Cotesworth Pinckney, an early American diplomat and presidential candidate.
Pinckneyville is the location of the Pinckneyville Power Plant, a combustion turbine generator (CTG)-type power plant run by Ameren.
Source: www.americanthresherman.com/history.html
ATA HISTORY
The American Thresherman Association (ATA) was organized in March of 1959.
At the annual meeting in 1962, Amos Rixman commented that the Association "organized three years ago this month for the purpose of furnishing some enjoyment to its members and to be the beginning of something very worthwhile." Already in its brief life the Association had earned such a reputation that three towns vied for the chance to become the permanent site for the show. The Pinckneyville Chamber of Commerce invited the ATA with open arms and pledges of support, and the Perry County community was chosen over Mascoutah and Highland for the 1962 show site.
Additional Foreign Language Tags:
(United States) "الولايات المتحدة" "Vereinigte Staaten" "アメリカ" "美国" "미국" "Estados Unidos" "États-Unis"
(Illinois) "الينوي" "伊利诺伊州" "इलिनोइस" "イリノイ" "일리노이" "Иллинойс"
(Pinckneyville) "بينكنيفيل" "平克尼维尔" "पिंकनीविले" "ピンクニービル" "핀크니빌" "Пинкнивилль"