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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
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/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.
Die Einzelblüten sind schräg abwärts gerichtet. Es handelt sich um „Rachenblumen“ mit der Innenwand dicht anliegenden Staubbeuteln und Narben. Der Eingang in die Blüten wird kleineren Insekten durch senkrecht hochstehende Sperrhaare verwehrt; gewöhnlich können nur Hummeln eindringen („Einkriechblume“). Ihnen dient der vorstehende untere Teil der Blütenglocke als Landeplattform. Wenn das Insekt zum Nektar vordringt, streift es die Staubgefäße mit dem Rücken, der dabei mit Pollen beladen werden kann.
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"
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
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.
nl.m.wikipedia.org/wiki/Utrechtse_schip
English:
The Utrecht ship, sometimes also referred to as Utrecht 1 or Utrecht ship, concerns the archaeological find of an approximately 1000 year old cargo ship. It was found in 1930 in the Dutch city of Utrecht.
Dated 997-1027
Collection Central Museum
The ship measures 17.8 by 3.8 meters and had a load capacity of approximately 13 tons. Fully loaded it had a draft of 0.7 metres. The ship was made of oak wood, which came from the area. By means of annual ring research it has been established that the ship was built between 997 and approximately 1027. At that time, with the Stathe trading district, Utrecht was an important trading center on the rivers Rhine and Vecht. A large oak tree was hollowed out to serve as the bottom of the ship, after which a superstructure of planks and beams was placed.
After the discovery on December 5, 1930 at the Van Hoornekade, the ship was preserved with creosote and linseed oil. The Utrecht ship has been exhibited in the Centraal Museum in Utrecht since 1936.
Out of the darkness came this wagon. I jumped out of the way just in time, but still managed this photo before I fell to the ground.
Excerpt from en.wikipedia.org/wiki/Studio_City_(Macau):
Studio City is a hotel casino resort on the Cotai Strip in Cotai, Macau. The Hollywood studio-themed leisure resort is the first in Asia to integrate television and film production facilities, retail, gaming and hotels. It is majority-owned by Melco Resorts & Entertainment and its subsidiary Studio City International Holdings Limited (SCIHL), Its two towers are connected by the world's first and highest figure-8 ferris wheel.
Inspired by the Golden Age of Hollywood, the cinematic-themed resort comprises a 30,000-square-foot Family Entertainment Center in collaboration with Time Warner Inc. subsidiaries Warner Bros and DC Comics. The entertainment center features DC Comics characters, such as Superman, Wonder Woman and The Flash.
Studio City features an Art Deco design inspired by two asteroids shooting through a Gotham City building. The resort was designed by Goddard Group, a Los Angeles–based entertainment design firm that also designed Galaxy Macau.
The resort's two hotel towers – Star Tower and Celebrity Tower – are connected by the Golden Reel, the world's first and highest figure-8 ferris wheel. Boarding at the hotel's 23rd floor, the wheel features 17 steampunk-themed cabins holding up to 10 passengers each, also designed by the Goddard Group, with hardware manufactured by Liechtenstein's Intamin Amusement Rides. Batman Dark Flight is a 4D flight simulation theatre attraction, along with a 40,000 square foot children's playground, the Warner Brothers Fun Zone.
Facilities include Legend Heroes Park, an immersive tech-based entertainment park (TBE), a 5,000-seat live performance arena, an indoor/outdoor water park, opened in May 2021, indoor and outdoor swimming pools, a fitness centre and meeting rooms. Star Tower is rated 5-star by Forbes Travel Guide and houses several award-winning restaurants, the Zensa Spa and Pacha Macau nightclub, as well as 1,233 gaming machines and about 250 gaming tables. Studio City Event Center hosts concerts and sporting events.
Guests may also view space through giant portal windows at the Cosmos Food Station food court. Restaurants at Studio City include Michelin-starred Pearl Dragon, Bi Ying, Rossi Trattoria and Hide Yamamoto.
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
Excerpt from en.wikipedia.org/wiki/Our_Lady_of_Mount_Carmel_Church_(Hong_Kong):
Our Lady of Mount Carmel Church (聖母聖衣堂) is a Roman Catholic church in the Diocese of Hong Kong. It is located in the Wanchai district at 1 Star Street. The church is unique being located within a private multi-storey residential building, rather than a stand-alone structure.
The current church situated in the historical site of St. Francis Xavier Chapel, which was the place of worship for Catholic faithful in the Wanchai area as early as 1845. There were religious communities, Catholic hospital, and homes for abandoned babies and blind women. As the number of faithful grew, the parish priest, Father James Zilioli, and the Wanchai faithful were determined to build a new church.
The preparation effort started from 1934, but due to financial difficulty, construction work could only be able to start by the end of February 1949. The new church, named as named “Holy Souls Church”, was finally opened on 19 July 1950, which was the feast day of Our Lady of Mount Carmel. In 1957, the church was renamed to "Our Lady of Mount Carmel Church”.
In the 1990s, the Diocese sold the property to secure funding for other purposes. With the dedication of the Diocese and assistance of local parishioners, agreement was reached with the developer to accommodate a church within the new premises.
The new church was officially opened and consecrated on 10 November 2001 by Cardinal John Baptist Wu Cheng-chung. The Bishop of Hong Kong.
The signature design of the church is a big skylight above the altar, with small sparkling pieces of crystal beads hanging down and a suspended golden cross. On the wall behind the altar, there is a mosaic depicting the scene in the Wedding at Cana by Mexican artist, Francisco Borboa. There are also flowing water running from the altar to the baptismal font at the entrance of the church.
PLASENCIA (Wiki): de.wikipedia.org/wiki/Plasencia
PLASENCIA (Tourismus): reisen-nach-spanien.com/extremadura/plasencia#9/40.0423/-...
Fazanul auriu
The golden pheasant or Chinese pheasant, (Chrysolophus pictus) is a gamebird of the order Galliformes (gallinaceous birds) and the family Phasianidae (pheasants). It is native to forests in mountainous areas of western China, but feral populations have been established in the United Kingdom and elsewhere. In England they may be found in East Anglia in the dense forest landscape of the Breckland.
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/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".
Wiki - The Historic Villages of Shirakawa-gō and Gokayama are one of Japan's UNESCO World Heritage Sites. The site is located in the Shogawa river valley stretching across the border of Gifu and Toyama Prefectures in central Japan. Shirakawa-gō (白川郷, "White River Old-District") is located in the village of Shirakawa in Gifu Prefecture.
These villages are well known for their houses constructed in the architectural style known as gasshō-zukuri (合掌造り). The Gasshō-zukuri, "prayer-hands construction" style is characterized by a thatched and steeply slanting roof resembling two hands joined in prayer. The design is exceptionally strong and, in combination with the unique properties of the thatching, allow the houses to withstand and shed the weight of the region's heavy snowfalls in winter.
The houses are large, with three to four stories encompassed between the low eaves, and historically intended to house large extended families and a highly efficient space for a variety of industries. The densely forested mountains of the region still occupy 96% of all land in the area, and prior to the introduction of heavy earth-moving machinery, the narrow bands of flat lands running the length of the river valley limited the area available for agriculture and homestead development. The upper storeys of the gasshō houses were usually set aside for sericulture, while the areas below the first (ground) floor were often used for the production of nitre, one of the raw materials needed for the production of gunpowder.
All Rights Reserved. Please do not reproduce, copy, edit, publish, transmit or upload material in my gallery without my permission.
Source: en.wikipedia.org/wiki/Arizona
Arizona is a state in the Southwestern region of the United States, sharing the Four Corners region of the western United States with Colorado, New Mexico, and Utah. Its other neighboring states are Nevada to the northwest and California to the west. It also shares an international border with the Mexican states of Sonora and Baja California to the south and southwest. It is the 6th-largest and the 14th-most-populous of the 50 states. Its capital and largest city is Phoenix, which is the most populous state capital in the United States.
Arizona is the 48th state and last of the contiguous states to be admitted to the Union, achieving statehood on February 14, 1912. Historically part of the territory of Alta California and Nuevo México in New Spain, it became part of independent Mexico in 1821. After being defeated in the Mexican–American War, Mexico ceded much of this territory to the United States in 1848, where the area became part of the territory of New Mexico. The southernmost portion of the state was acquired in 1853 through the Gadsden Purchase.
Southern Arizona is known for its desert climate, with extremely hot summers and mild winters. Northern Arizona features forests of pine, Douglas fir, and spruce trees; the Colorado Plateau; mountain ranges (such as the San Francisco Mountains); as well as large, deep canyons, with much more moderate summer temperatures and significant winter snowfalls. There are ski resorts in the areas of Flagstaff, Sunrise, and Tucson. In addition to the internationally known Grand Canyon National Park, which is one of the world's seven natural wonders, there are several national forests, national parks, and national monuments.
Arizona is home to a diverse population. About one-quarter of the state is made up of Indian reservations that serve as the home of 27 federally recognized Native American tribes, including the Navajo Nation, the largest in the state and the country, with more than 300,000 citizens. Since the 1980s, the proportion of Hispanics has grown significantly owing to migration from Mexico and Central America. A substantial portion of the population are followers of the Roman Catholic Church and the Church of Jesus Christ of Latter-day Saints. Arizona's population and economy have grown dramatically since the 1950s because of inward migration, and the state is now a major hub of the Sun Belt. Cities such as Phoenix and Tucson have developed large, sprawling suburban areas. Many large companies, such as PetSmart and Circle K, have headquarters in the state, and Arizona is home to major universities, including the University of Arizona, Arizona State University, and Northern Arizona University. The state is known for a history of conservative politicians such as Barry Goldwater and John McCain, though it has become a swing state in recent years.
Source: en.wikipedia.org/wiki/Page,_Arizona
Page is a city in Coconino County, Arizona, United States, near the Glen Canyon Dam and Lake Powell. As of the 2010 census, the population of the city was 7,247.
Source: en.wikipedia.org/wiki/Horseshoe_Bend_(Arizona)
Horseshoe Bend is a horseshoe-shaped incised meander of the Colorado River located near the town of Page, Arizona, United States. It is also referred to as the "east rim of the Grand Canyon."
Horseshoe Bend is located 5 miles (8 km) downstream from the Glen Canyon Dam and Lake Powell within Glen Canyon National Recreation Area, about 4 miles (6 km) southwest of Page.]
It is accessible via hiking a 1.5-mile (2.4 km) round trip from a parking area just off U.S. Route 89 within southwestern Page. The land south of the Bend's parking area, trail, and overlook are on the Navajo Nation territory.
Horseshoe Bend can be viewed from the steep cliff above.
The overlook is 4,200 feet (1,300 m) above sea level, and the Colorado River is at 3,200 feet (1,000 m) above sea level, making it a 1,000-foot (300 m) drop.
Source: www.nps.gov/glca/planyourvisit/horseshoe-bend.htm
A social media darling, Horseshoe Bend has become one of the most recognized and visited places in Glen Canyon National Recreation Area. The parking lot and trailhead is located off US Highway 89, approximately 5 miles (8 km) south of the Carl Hayden Visitor Center.
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"
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"
wiki ----The President is a giant sequoia located in the Giant Forest of Sequoia National Park in the United States, east of Visalia, California. It is not the tallest giant sequoia tree in the world with a height of about 247 feet (75 m), nor the widest at about 27 feet (8.2 m) in diameter at the base, but it is the third-largest tree in the world, measured by volume of trunk, and the oldest-known living sequoia, about 3,200 years old.[1] As of 2012, the volume of its trunk measured at about 45,000 cubic feet (1,300 m3), with an additional 9,000 cubic feet (250 m3) of branches.[2]
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"
en.wikipedia.org/wiki/Palace_of_Culture_and_Science
Thank you everyone for your visits, faves and comments, they are always appreciated :)
The Church of St. Lawrence was originally built in 1450. en.wikipedia.org/wiki/Church_of_St._Lawrence,_Vantaa
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"
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"
"Bungaroo" near the present day suburbs of Saint Ives and Davidson.
This was the site of the first of many inland explorations of the colony of New South Wales. A group of ten? men, searching for arable land on April 16, 1788. They found nothing good here.
That grumpy curmudgeon Surgeon White said of this place "the most desert, wild and solitary seclusion that the imagination can form any idea of".
Also present was the colonial governor, Captain Arthur Phillip. his deputy the Lieutenant Governor David Collins, a future Lieutenant Governor George Johnston, a sailor and a soldier.. So, it was nice to reconnect at the camping spot where those famous people slept. At the same time, a long way away in Vienna. Mozart was preparing to write his famous last three symphonies.
The camping spot here would be familiar to the ten men, back in 1788. They were the governor, naval Lieutenant Ball, Lieutenant George Johnston of the marines, David Collins the judge advocate, Surgeon White, three soldiers and two seamen.
Johnston later became lieutenant governor and was influential in the Rum Rebellion. Collins name is for Collins Street in Melbourne. Ball's pyramid at Lord Howe Island. White's Bay named after the doctor. And many things named for the governor, Arthur Phillip.
The reports from this trip say the campers were tormented by mosquitos, which is easy to understand. They can be ferocious outdoors in most months of the year. Particularly in April at night.
Lieutenant Ball, a marine and two fatigued seamen here left the main party to return to Sydney Cove via the North shore. Looks like they didn't camp here at Bungaroo.
This place has probably changed little. Surgeon White was a talented man, but he had a bad and cranky view of Australia. Surgeon White had a duel with another of the colonial doctors, Dr William Balmain. They both shot each other. The young scot receiving minor injuries to his thigh. White was also slightly injured.
The governor was horrified about this event, complaining how his doctors were trying to kill each other.
In 1790, Balmain saved Governor Phillip's life when he was speared at Manly.
Surgeon White was not an easy man to get on with. He is considered a man of many virtues as well as his rather poor record in other areas.
Yesterday I photographed a plant not far from the camping site. Collected by Surgeon White a few years later in Sydney. Here's the photo and new article: Leptospermum parvifolium.
But this is a magnificent spot. The tidal limit of Middle Harbour creek where the colonials camped. Four famous men supported by two others. Upstream was land unsuited to agriculture. Very poor sandstone soils. So, this trip in 1788 failed to find suitable land.
North see beach where shrimp fishing with Belgian horses tradition since the 1500 , Martin’s photographs , Oostduinkerke , now Koksijde , West Vlaanderen , West Flanders , Belgium June 8. 2019
( en.m.wikipedia.org/wiki/Oostduinkerke)
Belgium
Belgie
Flags waving in the wind
Martin’s photographs
June 2019
Favourites
iPhone 6
shrimp fishing with Belgian horses tradition since the 1500
Koksijde
Oostduinkerke
West Vlaanderen
West Flanders
North see beach where shrimp fishing with Belgian horses
North see beach where shrimp fishing
Belgian horses
North see beach in Oostduinkerke
North see
Beach
Noord Zee kust
Shrimp
Belgian horses
Noord zee
Strandt
See Gulls
(en.m.wikipedia.org/wiki/Oostduinkerke)
Kavala (Greek: Καβάλα) is a city in northern Greece, the principal seaport of eastern Macedonia and the capital of Kavala regional unit. It is situated on the Bay of Kavala, across from the island of Thasos. Kavala is located on the Egnatia motorway and is a one and a half-hour drive to Thessaloniki (160 kilometres (99 miles) west) and a forty-minute drive to Drama (37 km (23 miles) north) and Xanthi (56 km (35 miles) east). Its nickname is The cyan city (Η γαλάζια πόλη).
History
Antiquity
The city was founded at about the end of the 7th century BC by settlers from Thassos, who called it Neapolis (Νεάπολις; "new city" in Greek). It was one of the colonies that the Thassians founded along the coastline in order to take advantage of the rich gold and silver mines of the territory, especially those located in the nearby Pangaion mountain (which were eventually exploited by Phillip the Second of Macedonia).
The worship of "Parthenos", a female deity of Greek–Ionian origin, is archaeologically attested in the archaic period. At the end of the 6th century BC Neapolis claimed its independence from Thassos and cut its own silver coins with the head of Gorgo (γοργὀνειο) on the one side. At the beginning of the 5th century BC a large Ionic temple made from thassian marble replaced the archaic one. Parts of it can now be seen in the archaeological museum of Kavala.
In 411 BC, during the Peloponnesian War, Neapolis was besieged by the allied armies of the Spartans and the Thassians but remained faithful to Athens. Two Athenian honorary decrees in 410 and 407 BC rewarded Neapolis for its loyalty.
Neapolis was a town of Macedonia, located 14 km (9 mi) from the harbor of Philippi. Neapolis was a member of the Athenian League; a pillar found in Athens mentions the contribution of Neapolis to the alliance.
Roman Era
The military Roman road Via Egnatia passed through the city helped commerce to flourish. It became a Roman civitas in 168 BC, and was a base for Brutus and Cassius in 42 BC, before their defeat in the Battle of Philippi. (Appian, B.C. iv. 106; Dion Cass. xlvii. 35.). The Apostle Paul landed at Kavala on his first voyage to Europe (Acts, xvi. 11).
Byzantine Era
In the 6th century, Byzantine emperor Justinian I fortified the city in an effort to protect it from barbaric raids. In later Byzantine times the city was called Christoupolis (Χριστούπολις, "city of Christ") and belonged to the theme of Macedonia. The first mention of the new name is recorded in a taktikon of the early 9th century. The city is also mentioned in the "Life of St. Gregory of Dekapolis". In the 8th and 9th century, Bulgarian attacks forced the Byzantines to reorganize the defense of the area, giving great care to Christoupolis with fortifications and a notable garrison. In 926 the Byzantine general (strategos) Basil Klaudon reconstructed the fallen walls of the city, ("τα πριν φθαρέντα και πεπτωκότα τείχη") according to an inscription that is now in the archaeological museum of Kavala. Due to the location of Christoupolis, the city experienced an economic resurgence, securing the contact between Constantinople and Thessaloniki. During the Norman raid of Macedonia in 1185, the city was captured and burned. In 1302, the Catalans failed to capture the city. In order to prevent them from coming back, the Byzantine emperor Andronikos III Palaiologos built a new long defensive wall ("το παρά την Χριστούπολιν τείχισμα"). In the 13th century the Byzantine Greek historian George Akropolites writes that the city and the area around the city is highly populated with Bulgarians and this makes it more difficult to keep the city as a part of Bizantium.[2] In 1357 it is mentioned that the Byzantine officers and brothers Alexios and John controlled the city and its territory. Recent excavations have revealed the ruins of an early Byzantine basilica under an old Ottoman mosque in the old part of the city (Panagia peninsula). This Christian temple was used until the late Byzantine era, as the also recently revealed small cemetery around it shows. The Ottoman Turks first captured the city in 1387 and completely destroyed it in 1391, as a Mount Athos chronicle testifies.
Ottoman Era
Kavala was part of the Ottoman Empire from 1387 to 1912. In the middle of the 16th century, Ibrahim Pasha, Grand Vizier of Suleiman the Magnificent, contributed to the prosperity and growth of Kavala by the construction of an aqueduct.[3] The Ottomans also extended the Byzantine fortress on the hill of Panagia. Both landmarks are among the most recognizable symbols of the city today.
Mehmet Ali, the founder of a dynasty that ruled Egypt, was born in Kavala in 1769. His house has been preserved as a museum.
Modern Kavala
Kavala was briefly occupied by the Bulgarians during the first Balkan War in 1912, but was finally captured by Greece in 1913 during a successful landing operation by the Greek Navy that was commanded by the famous admiral Pavlos Kountouriotis. During World War I Kavala suffered from the Bulgarian military occupation with many victims among its Greek population.[citation needed] After the Greco-Turkish War of 1919–1922, the city entered a new era of prosperity because of the labour offered by the thousands of refugees that moved to the area from Asia Minor. The development was both industrial and agricultural. Kavala became greatly involved in the processing and trading of tobacco. Many buildings related to the storage and processing of tobacco from that era are preserved in the city.
During World War II and after the fall of Athens, the Nazis awarded Kavala to their Bulgarian allies in 1941, causing the city to suffer once again, but finally was liberated in 1944.
In the late 1950s Kavala expanded towards the sea by reclaiming land from the area west of the port.
In 1967, King Constantine II left Athens for Kavala in an unsuccessful attempt to launch a counter-coup against the military junta.
Etymology
In antiquity the name of the city was Neapolis. During the Middle Ages it was Christoupolis. The etymology of the modern name of the city is disputed. There are some explanations, either from the Italian cavallo (=horse), or from the Hebrew Kabbalah due to the large Jewish population of the city.
Climate
Kavala has a humid subtropical climate (Köppen climate classification "Cfa") that borders on an semi-arid climate (Köppen climate classification "BSk" or "BSh" depending on the system used) with annual average precipitation of 460 mm (18.1 in). Snowfalls are sporadic, but happen more or less every year. The humidity is always very high
The absolute maximum temperature ever recorded was 38.0 °C (100 °F), while the absolute minimum ever recorded was −5.8 °C (22 °F).
Education/Research
The Technological Educational Institute (panoramic view).TEI of Kavala: The Technological Educational Institute of Kavala (Greek: ΤΕΙ Καβάλας) is a public institute providing education at university level in the region of Eastern Macedonia and Thrace. The main campus of the institute located in St. Lukas, Kavala and is approximately 132,000 m2 with buildings covering an area of 36,000 m2.The campus is home for 2 faculties (Faculty of Engineering Sciences and Faculty of Business and Economics) with totally 9 departments.
Fisheries Research Institute:[5] Fisheries Research Institute (F.R.I) is one of the five specialized research institutes of N.AG.RE.F, being responsible to conduct research and to promote technological development in the fishery sector. The Institute is located 17 km (11 mi) away from Kavala, in Nea Peramos, at the centre of a marine area with rich fishery grounds and high biodiversity in the surrounding lagoons, lakes and rivers.
Institute of Mohamed Ali for the Research of the Eastern Tradition (I.M.A.R.E.T.):[6] I.M.A.R.E.T. is a registered NGO with the Hellenic Ministry of Foreign Affairs, which was established several months ago by concerned citizens in Kavala, Greece. Its aims include the study of the Egyptian influence in Greece and vice versa. The intra-cultural exchange and dialogue, as well as the promotion of art as a means of intra-cultural understanding. The first major co-operation partner is Cultnat of Bibliotheca Alaxandrina with the aim of documenting and digitizing the architectural heritage of the Mohamed Ali era in Egypt and Greece. Most important event that take place every year at the institute is the International Roman Law Moot Court Competition.
Historical & Literary Archives of Kavala:[7] It is purely a non-profiteering, public utility foundation. The foundation of the Historical & Literary Archives of Kavala is not subsidized by the Greek State, neither by any other enterprise of the private sector. Its operational cost is covered only by its founders and by infrequent aids of the local self-government.
Egnatia Aviation:[8] It is a private training college for pilots that started training in Greece in July 2006. The facilities of Egnatia Aviation mostly located in the former passenger’s terminal of the Kavala International Airport "Alexander the Great".
Culture
Festivals and events
Kavala hosts a wide array of cultural events, which mostly take place during the summer months. The top festival is the Festival of Philippi,[9] which lasts from July to September and includes theatrical performances and music concerts. Since 1957, it has been the city's most important cultural event and one of the most important of Greece.
Cosmopolis is an International Festival held in the Old Town of Kavala that offers an acquaintance with cultures around the world through dancing and musical groups, traditional national cuisines, cinema, and exhibits at the kiosks of the participant countries.
Giannis Papaioannou’s Festival includes concerts and music seminars.[10]
Ilios ke Petra (Sun and Stone)(July): a Festival held in “Akontisma” of Nea Karvali. The event is of folkloric character, with the participation of traditional dancing groups from all over the world.
Wood Water Wild Festival:[11] Wood Water Wild is an outdoor activities festival, inspired by nature. It includes live bands & DJ sets, body&mind activities, a book fair, outdoor theatre, ecology, camping, and debates.
Kavala AirSea Show:[12] An annual air show, which takes place during the last days of June
Besides, various cultural events are held in all municipalities of Kavala during the summer months.
Cuisine
Fish and sea food, as well as the products of the local livestock breeding and agricultural sectors are the prevailing elements of Kavala courses. In Kavala, the traditional local recipes have been influenced by the cuisine of the refugees from Pontos, Asia Minor and Kappadokia. Fresh fish and sea food, salted food, mackerel "gouna" (sun dried mackerel on the grill), sardine pantremeni, mussels with rice, herring saganaki, anchovies wrapped in grape leaves, Stuffed eggplant: these are some very renowned recipes in Kavala and the coastal settlements of the region. The grapes, wine and tsipouro produced in the area, as well as the kourabiedes (sugar-coated almond biscuits) from Nea Karvali are particularly famous.
Municipality
The municipality of Kavala was formed at the 2011 local government reform by the merger of the following 2 former municipalities, that became municipal units:[13]
Municipal units (former municipalities):
Kavala
Filippoi
Municipal unit
Kavala 58,790
Filippoi 11,711
The population of the new municipality is 70,501 and the area is 350,61 km2. The seat of the municipality is in Kavala. Some of the most important communities inside new municipality are:
Population
Kavala 56,371
Krinides 3,365
Amigdaleonas 2,724
Nea Karvali 2,225
Zygos 2,057
Subdivisions
Kavala is built amphitheatrically, with most residents enjoying superb views of the coast and sea. Some of the regions inside Kavala are:
Agia Varvara Agios Athanasios Agios Ioannis Agios Loukas Chilia
Dexameni Kalamitsa Kentro Neapolis Panagia
Perigiali Potamoudia Profitis Ilias Timios Stavros Vyronas
Province
The province of Kavala (Greek: Επαρχία Καβάλας) was one of the provinces of the Kavala Prefecture. Its territory corresponded with that of the current municipality Kavala, and part of the municipal unit Eleftheroupoli.[14] It was abolished in 2006.
Transport
Highway Network
European route E90 runs through the city and connects Kavala with the other cities. The Egnatia Motorway (A2) lies north of the city. One can enter the city from one of two Junctions; 'Kavala West' and 'Kavala East'.Kavala has regular connection with Interregional Bus Lines (KTEL) from and to Thessaloniki and Athens.
Airport
The Kavala International Airport "Alexander the Great" (27 km (17 mi) from Kavala) is connected with Athens by regularly scheduled flights and with many European cities by scheduled and charter flights.
Port
Kavala is connected with all the islands of the Northern Aegean Sea with frequent itineraries of various ferry lines.
Bus
The city is connected with all of the large Greek cities such as Thessaloniki and Athens. All of the local villages are also connected via bus lines. The cost of tickets is very cheap. There is also a shuttle bus in Kavala with these lines : 1. Vironas - Kallithea 2. Dexameni 3. Cemetery 4. Kipoupoli - Technological Institute 5. Agios Loukas 6. Profitis Ilias 7. Stadium 8. Kalamitsa - Batis ( only in summer ) 9. Agios Konstantinos 10. Neapoli 11. Hospital - Perigiali
Sports
Kavala F.C.: AO Kavala (Greek: Athlitikos Omilos Kavala, Αθλητικός Όμιλος Καβάλα), the Athletic Club Kavala, is a professional association football club based in the city of Kavala, Greece.The club plays in the Municipal Kavala Stadium "Anthi Karagianni".[15]
Kavala B.C.: Enosi Kalathosfairisis Kavalas (Greek: Ένωση Καλαθοσφαίρισης Καβάλας - Basketball Union of Kavala) is a Greek professional basketball club that is located in Kavala, Greece. The club is also known as E.K. Kavalas. The club's full Greek name is Ένωση Καλαθοσφαίρισης Καβάλας. Which means, Kavala Basketball Union or Kavala Basketball Association in English. The club competes in the Greek League.
Kavala '86: A women football club, founded in 1986, with panhellenic titles in Greek women football.
Kavala Chess Club:[16] Chess is very popular in Kavala and the local chess club ranks top in Greece, enjoying plenty of success both domestically and internationally. The highlight has to be the club's annual International Open, that takes place every August in Kavala and attracts the biggest names in chess from all over the globe
Nautical Club of Kavala (1945, Ναυτικός Ομιλος Καβάλας, ΝΟΚ). Sports of sea (swimming, yachting,water-polo,diving e.t.c.)
Kavala Titans (2009, Τιτάνες Καβάλας). Rugby Union
International relations
Twin towns – Sister cities
Kavala is twinned with:
Bulgaria Gabrovo, Bulgaria (1975)
Bosnia and Herzegovina Gradiška, Bosnia and Herzegovina (1994)
Germany Nuremberg, Germany (1998)
Partnerships
Morocco Agadir, Morocco (2001)
Armenia Martuni, Armenia (2001)
Turkey Tekirdağ, Turkey (2003)
Bulgaria Gotse Delchev, Bulgaria (2003)
Serbia Vranje, Serbia (2009)
Postage stamps
Austria opened a post office in Kavala before 1864.[18] Between 1893 and 1903, the French post office in the city issued its own postage stamps; at first stamps of France overprinted with "Cavalle" and a value in piasters, then in 1902 the French designs inscribed "CAVALLE".
Historical population
1961 44,517 44,978 -
1971 46,234 46,887 -
1981 56,375 56,705 -
1991 56,571 58,025 -
2001 58,663 63,293 -
2011 54,027 58,790 70,501
Notable figures
Muhammad Ali Pasha of Kavala, the Albanian Wali (governor) of Egypt between 1805–1848 and founder of the modern state of Egypt
Theodore Kavalliotis, Greek Orthodox priest, teacher and a figure of the Greek Enlightenment
Vassilis Vassilikos, Greek writer and diplomat
George Georgiadis, Greek footballer
Giorgos Heimonas (1938–2000), writer and translator
Nikos Karageorgiou, (born December 9, 1962) Manager of Greek football team Ergotelis, based in Heraklion, Crete
Anthi Karagianni, silver medalist in the Athens 2004 and Beijing 2008 Paralympic Games; the city's Municipal stadium is named after her
Vasilis Karas, Greek singer
Nikos Kourkoulis, Greek singer
Mitsos Partsalidis, first elected "red" (communist) mere in modern Greek history, back in 1.4.1934
Antigone Valakou, actress
Despina Vandi, a Top Greek singer
Thanasis Euthimiadis, a Greek actor
Anna Verouli, 1982 Gold Medalist, European Championship, javelin thrower
Zisis Vryzas (born November 9, 1973), former footballer, currently vicepresident of PAOK FC
Theodoros Zagorakis (born October 27, 1971), former footballer, captain of national team of Greece-European champion 2004, currently president of PAOK FC
Anna Gerasimou, a Greek tennis player
Kleon Krantonellis, Αrchitect
Wiki: The creator of the cartoon character Wiley Coyote, Chuck Jones, based the character on Mark Twain's book Roughing It, in which Twain described the coyote as "a long, slim, sick and sorry-looking skeleton" that is "a living, breathing allegory of Want. He is always hungry."
en.wikipedia.org/wiki/Red-tailed_wheatear
The red-tailed wheatear (Oenanthe chrysopygia), also known as the rusty-tailed wheatear, Persian wheatear or Afghan wheatear, is a small passerine bird breeding in mountainous areas of south-west and central Asia. It belongs to the wheatear genus Oenanthe which was formerly placed in the thrush family Turdidae but is now in the Old World flycatcher family Muscicapidae. The red-tailed wheatear used to be considered a subspecies of the Kurdish wheatear (O. xanthoprymna) but is now often regarded as a separate species.
Description
It is 14.5 cm long with a wingspan of 26–27 cm and a weight of about 20-27 g.[2] The plumage is fairly drab, mainly grey-brown above and greyish-white below. It has a faint pale stripe over the eye, a rufous tinge to the ear-coverts and silvery-white underwing-coverts.[3] The rump and bases of the outer tail-feathers are reddish while the rest of the tail is black forming a T-shaped pattern.[4] There is little difference between males and females but the male has black between the eye and bill.[5]
The female Kurdistan wheatear can be very similar but usually has white bases to the outer tail-feathers. Adult males and some females of the Kurdistan wheatear are quite different with a black face and throat and greyer upperparts.
The song is a simple repeated whistle. The bird has several clicking, rasping and whistling calls.[2]
Taxonomy
The species was described in 1863 by the Italian zoologist Filippo de Filippi who named it Dromolaea chrysopgyia. It was later treated as a subspecies of the Kurdish wheatear (O. xanthoprymna) after birds with an appearance intermediate between the two ("O. x. cummingi") were found, suggesting that they could interbreed. However, these hybrid birds may in fact be first-winter Kurdish wheatears.[6]
Red-tailed wheatears in the eastern part of the range are slightly paler and are sometimes regarded as a separate subspecies, O. c. kingi.
Distribution and habitat
Its breeding range extends from north-east Turkey, Armenia and Azerbaijan eastwards through Iran to Afghanistan, southern Tajikistan and western Pakistan. It migrates south to winter in the Arabian Peninsula, Eritrea, southern parts of Iraq and Iran, Pakistan and north-west India. It has occurred as a vagrant in Israel, Ethiopia, Djibouti and Nepal.
It breeds in mountainous areas from 1,200—4,000 m above sea-level. It nests on steep, barren, rocky ground with little vegetation. It winters at lower levels occurring on rocky hills, steppe, scrubland and semi-desert.
Behaviour
It usually forages on bare ground, feeding mainly on insects such as ants, beetles and caterpillars. It will pick food from vegetation, dig with its bill for beetle larvae and launch attacks from an exposed perch on a rock or stone.[2]
It breeds from late March or April to June, raising two broods. The nest is a cup of grass and other plant material built in a hole in rocks, stones or a wall. Four to six eggs are laid and are incubated for 13 days. The eggs are pale bluish-white, sometimes with reddish-brown spots.[
en.wikipedia.org/wiki/Sefton_Park
Sefton Park is a public park in south Liverpool, England. The park is in a district of the same name within the Liverpool City Council Ward of Mossley Hill, and roughly within the historic bounds of the large area of Toxteth Park. Neighbouring districts include modern-day Toxteth, Aigburth, Mossley Hill, and St Michael's Hamlet.
The park is 235 acres (0.95 km2) in area[1] and has been designated a Grade II* Historic Park by English Heritage[citation needed] making it one of three such parks in the city, along with the nearby Princes Park and St James Cemetery.
History
The site of the park was once within the boundaries of the 2,300-acre (9.3 km2) Royal Deer Park of Toxteth which became "disparked" in 1591. The land eventually came under the control of the Earl of Sefton.
As Toxteth rapidly grew, the green fields and woodland of Toxteth Park grew into narrow streets and courts packed tiny uninhabitable houses where the air was stagnant, there was little or no sanitation and running water consisted of one tap in the middle of the court. At the same time there was demand for large aristocratic mansions in the South of Liverpool. In 1862 the Borough Council Engineer recommended a site for this development. An Act of Parliament[which?] in 1864 permitted corporations to borrow sums of money up to half a million pounds to be repaid over thirty years. This allowed steps to be taken towards the purchase of land for Sefton Park. In 1867 the Council purchased 375 acres (1.52 km2) of land for the development of the park for £250,000 from the Earl of Sefton.
Even though it was recognised by politicians that clean, fresh open spaces were now regarded as necessity there was an outcry from the public that £250,000 was extravagant and wasteful. As with neighbouring Princes Park plots of land on the perimeter were sold for housing which helped in the funding of the layout of the park.
Soon after, a European competition was launched to design a grand park. 29 entries were received and the competition was won by a French landscape architect Édouard André with work on the design also undertaken by Liverpool architect Lewis Hornblower. The park was opened on 20 May 1872 by Prince Arthur who dedicated it "for the health and enjoyment of the townspeople".
The Park design is based on circular, oval and marginal footpaths, framing the green spaces, with two natural watercourses flowing into the 7-acre (0.028 km2) man-made lake. Hornblower’s designs for the park lodges and entrances were elaborate structures, and included follies[specify], shelters and boathouses. The parkland itself included a deer park and the strong water theme was reflected by the presence of pools, waterfalls and stepping stones. The Park, its exclusive villas and ornamentation reflected the grandeur of the City during its mid Victorian period when Liverpool was the second city of the Empire.
The perimeter road's outer edge is lined with Victorian buildings constructed to around 1890, and Edwardian houses. Additional development of the park continued with the construction of the iron bridge in 1873.
The park had a gallops[specify] which led to it being nicknamed "the Hyde Park of the North" but was always referred to by locals as "The Jockey Sands".[citation needed]
A major park improvement programme was undertaken in 1983 prior to International Garden Festival.
Sporting uses
Sefton Park Cricket Club moved their ground to the park in 1876 and WG Grace was amongst the three Gloucestershire players who made up a "South of England" team who won there in 1877. The park also has tennis courts, a bowling green, a popular jogging circuit and local league football is a regular weekend fixture. It is also used every November to hold the European Cross Country Championships trial races for the British team.
Entertainment uses
The park has also been a site for Royal Liverpool Philharmonic Orchestra's summer pops season, Africa Oyé and the Moscow State Circus. Bands have also played at the park in the 80s such as Echo and the Bunneymen.
Restoration
In 2005 the park received provisional approval for a major £5 million Heritage Lottery funded renovation project which involves the refurbishment and improvement of many of the park's features. The work began in June 2007 was expected to be completed in summer 2009. This work was very controversial with some regular users of the park as it included destroying trees and breeding sites of birds.[2] The work led to the formation of the "Friends of Sefton Park" campaigns.
Notable features of the park
Palm House
This is a Grade II* three-tier dome conservatory palm house designed and built by MacKenzie and Moncur of Edinburgh which opened in 1896. Liverpool millionaire Henry Yates Thompson (the great nephew of the founder of Princes Park) gifted £10,000 to the city to fund the construction. It was designed in the tradition of Joseph Paxton's glass houses and was stocked originally with a rich collection of exotic plants.
During the Liverpool Blitz of May 1941 a bomb fell nearby and shattered the glass. It was reglazed in 1950 at a cost of £6,163 with costs covered by War Restoration funds. A period of decline and deterioration culminated in its closure in the 1980s on grounds of safety.
In June 1992, a public meeting was held highlighting the dereliction and calling for restoration. A petition was presented to the City Council by what had become the "Save the Palm House" campaign. A public fund raising campaign was established, with a "sponsor a pane" programme generating over £35,000. This led directly to the conversion of Save the Palm House into a registered charity (Friends of Sefton Park Palm House). The Palm House was partially repaired and reopened in 1993. It was fully restored at a cost of £3.5 million with Heritage Lottery and European funding and reopened in September 2001. It is now both a popular visitor attraction offering free and paid-for public entertainment and is venue for hire.
The eight ‘corners’ of the Palm House are marked by statues by the French sculptor Leon-Joseph Chavalliaud. These include explorers Captain Cook, Christopher Columbus, navigators Gerardus Mercator and Henry the Navigator, botanists and explorers Charles Darwin, Carl Linnaeus and John Parkinson and landscape architect Andre le Notre. Inside the Palm House are two sculptures by Benjamin Edward Spence "Highland Mary" and "The Angel's Whisper".
The grounds of the Palm House feature a statue of Peter Pan which was one of the last works by the British sculptor Sir George Frampton. This is Grade II listed and is a replica of a similar statue given as a gift for the visiting public to Kensington Gardens by author J.M. Barrie. The statue was donated to the park by George Audley in 1928 and was unveiled in the presence of Barrie. It originally sat in Sefton Park but was damaged in the 1990s. It was restored at Liverpool's Conservation Centre, and returned to the more secure location of the Palm House's grounds in December 2005.
Shaftesbury Memorial and Eros Fountain
This is Grade II listed and situated in the centre of the Park next to the cafe and former site of the aviary. The fountain, made from bronze and aluminium, was unveiled in 1932 and is a replica of a memorial to Lord Shaftesbury created by Sir Alfred Gilbert in London's Piccadilly Circus. It was restored in 2008 with a new aluminium Eros statue replacing the original which now resides in Liverpool's Conservation Centre.
Grotto
An artificial cave also known as Old Nick's Caves. This was built around 1870 by French rockwork specialist M. Combaz. It includes a waterfall which flows into a mirror pond.
Other statues and facilities
The park features a Gothic drinking fountain and several prominent statues including a memorial to William Rathbone V by Sir Thomas Brock unveiled in 1887, and an obelisk, the Samuel Smith memorial located by the principal entrance to the Park. There is a bandstand, popular since the Victorian era, which is said[by whom?] to be the inspiration for The Beatles' song Sgt Peppers Lonely Hearts Club Band. An iron bridge was opened in 1873 which spans the Fairy Glen. There is a cafe in the centre of the park called the Aviary Cafe and a pirate themed children's play area opened in 2009.
Former features of the park
Aviary
An aviary was introduced to the park in 1901 and was home to many exotic birds. After falling into disuse in the 1990s, the old cages were removed during the restoration project and replaced with a new curved viewing point overlooking new outside planting.
The Concert
The park also boasted a small open-air theatre – "The Concert" – near the café which featured singers, magicians and talent contests to entertain local children during the summer holidays. This was removed in the 1970s.
Boating lake
The lake was a popular venue for boating until the 1970s, with a jetty and boat hire facilities. The lake was totally emptied in 2007 for the extensive renovation work and all of the fish (which included specimen weights of carp, tench, roach, pike and golden orf)[citation needed] were caught with large nets and sent to various locations across the UK. Following its restoration, the lake was refilled in 2010. Turtles have also been spotted in the lake.
Others
There was a small pirate ship located in one of the lakes until the early 1990s when it was removed due to falling into disrepair.
Source: en.wikipedia.org/wiki/Hoover_Dam
Hoover Dam is a concrete arch-gravity dam in the Black Canyon of the Colorado River, on the border between the U.S. states of Nevada and Arizona. Constructed between 1931 and 1936, during the Great Depression, it was dedicated on September 30, 1935, by President Franklin D. Roosevelt. Its construction was the result of a massive effort involving thousands of workers, and cost over 100 lives. In bills passed by Congress during its construction, it was referred to as the Hoover Dam, after President Herbert Hoover, but was named Boulder Dam by the Roosevelt administration. In 1947, the name Hoover Dam was restored by Congress.
Since about 1900, the Black Canyon and nearby Boulder Canyon had been investigated for their potential to support a dam that would control floods, provide irrigation water, and produce hydroelectric power. In 1928, Congress authorized the project. The winning bid to build the dam was submitted by a consortium named Six Companies, Inc., which began construction in early 1931. Such a large concrete structure had never been built before, and some of the techniques used were unproven. The torrid summer weather and lack of facilities near the site also presented difficulties. Nevertheless, Six Companies turned the dam over to the federal government on March 1, 1936, more than two years ahead of schedule.
Hoover Dam impounds Lake Mead and is located near Boulder City, Nevada, a municipality originally constructed for workers on the construction project, about 30 mi (48 km) southeast of Las Vegas, Nevada. The dam's generators provide power for public and private utilities in Nevada, Arizona, and California. Hoover Dam is a major tourist attraction, with 7 million tourists a year. The heavily traveled U.S. Route 93 (US 93) ran along the dam's crest until October 2010, when the Hoover Dam Bypass opened.
Source: hoover.archives.gov/hoovers/hoover-dam
85 years after its completion, Hoover dam is still considered an engineering marvel. It is named in honor of President Herbert Hoover, who played a crucial role in its creation.
For many years, residents of the American southwest sought to tame the unpredictable Colorado River. Disastrous floods during the early 1900’s led residents of the area to look to the federal government for aid, and experiments with irrigation on a limited scale had shown that this arid region could be transformed into fertile cropland, if only the river could be controlled. The greatest obstacle to the construction of such a dam was the allocation of water rights among the seven states comprising the Colorado River drainage basin. Meetings were held in 1918, 1919 and 1920, but the states could not reach a consensus.
Herbert Hoover had visited the Lower Colorado region in the years before World War I and was familiar with its problems and the potential for development. Upon becoming Secretary of Commerce in 1921, Hoover proposed the construction of a dam on the Colorado River. In addition to flood control and irrigation, it would provide a dependable supply of water for Los Angeles and Southern California. The project would be self-supporting, recovering its cost through the sale of hydroelectric power generated by the dam.
In 1921, the state legislatures of the Colorado River basin authorized commissioners to negotiate an interstate agreement. Congress authorized President Harding to appoint a representative for the federal government to serve as chair of the Colorado River Commission and on December 17, 1921, Harding appointed Hoover to that role.
When the commission assembled in Santa Fe in November 1922, the seven states still disagreed over the fair distribution of water. The upstream states feared that the downstream states, with their rapidly developing agricultural and power demands, would quickly preempt rights to the water by the “first in time, first in right” doctrine. Hoover suggested a compromise that the water be divided between the upper and lower basins without individual state quotas. The resulting Colorado River Compact was signed on November 24, 1922. It split the river basin into upper and lower halves with the states within each region deciding amongst themselves how the water would be allocated.
A series of bills calling for Federal funding to build the dam were introduced by Congressman Phil D. Swing and Senator Hiram W. Johnson between 1922 and 1928, all of which were rejected. The last Swing-Johnson bill, titled the Boulder Canyon Project Act, was largely written by Hoover and Secretary of the Interior Hubert Work. Congress finally agreed, and the bill was signed into law on December 21, 1928 by President Coolidge. The dream was about to become reality.
On June 25, 1929, less than four months after his inauguration, President Herbert Hoover signed a proclamation declaring the Colorado River Compact effective at last. Appropriations were approved and construction began in 1930. The dam was dedicated in 1935 and the hydroelectric generators went online in 1937. In 1947, Congress officially "restored" Hoover's name to the dam, after FDR's Secretary of the Interior tried to remove it. Hoover Dam was built for a cost of $49 million (approximately $1 billion adjusted for inflation). The power plant and generators cost an additional $71 million, more than the cost of the dam itself. The sale of electrical power generated by the dam paid back its construction cost, with interest, by 1987.
Today the Hoover Dam controls the flooding of the Colorado River, irrigates more than 1.5 million acres of land, and provides water to more than 16 million people. Lake Mead supports recreational activities and provides habitats to fish and wildlife. Power generated by the dam provides energy to power over 500,000 homes. The Hoover Compromise still governs how the water is shared.
Additional Foreign Language Tags:
(United States) "الولايات المتحدة" "Vereinigte Staaten" "アメリカ" "美国" "미국" "Estados Unidos" "États-Unis"
(Nevada) "نيفادا" "内华达州" "नेवादा" "ネバダ" "네바다" "Невада"
(Arizona) "أريزونا" "亚利桑那州" "एरिजोना" "アリゾナ州" "애리조나" "Аризона"
(Hoover Dam) "سد هوفر" "胡佛水坝" "हूवर बांध" "フーバーダム" "후버 댐" "Гувера" "Presa Hoover"
Wiki enjoys the little seasonal stream nearby. It runs between our house and our friend and neighbor's house part of the year when we have rain.
... die Bäume schlagen aus
München - Allee im Hofgarten vor der Nordseite der Residenz (Herkulessaal)
de.wikipedia.org/wiki/Hofgarten_(München)
I'll show this one to my barber next time I want something specific.
Okay, I lied, I don't go to the barber.
2,5x magnification of a robber fly
One shot, handheld, diffused twin flash.
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"
Source: en.wikipedia.org/wiki/Arizona
Arizona is a state in the Southwestern region of the United States, sharing the Four Corners region of the western United States with Colorado, New Mexico, and Utah. Its other neighboring states are Nevada to the northwest and California to the west. It also shares an international border with the Mexican states of Sonora and Baja California to the south and southwest. It is the 6th-largest and the 14th-most-populous of the 50 states. Its capital and largest city is Phoenix, which is the most populous state capital in the United States.
Arizona is the 48th state and last of the contiguous states to be admitted to the Union, achieving statehood on February 14, 1912. Historically part of the territory of Alta California and Nuevo México in New Spain, it became part of independent Mexico in 1821. After being defeated in the Mexican–American War, Mexico ceded much of this territory to the United States in 1848, where the area became part of the territory of New Mexico. The southernmost portion of the state was acquired in 1853 through the Gadsden Purchase.
Southern Arizona is known for its desert climate, with extremely hot summers and mild winters. Northern Arizona features forests of pine, Douglas fir, and spruce trees; the Colorado Plateau; mountain ranges (such as the San Francisco Mountains); as well as large, deep canyons, with much more moderate summer temperatures and significant winter snowfalls. There are ski resorts in the areas of Flagstaff, Sunrise, and Tucson. In addition to the internationally known Grand Canyon National Park, which is one of the world's seven natural wonders, there are several national forests, national parks, and national monuments.
Arizona is home to a diverse population. About one-quarter of the state is made up of Indian reservations that serve as the home of 27 federally recognized Native American tribes, including the Navajo Nation, the largest in the state and the country, with more than 300,000 citizens. Since the 1980s, the proportion of Hispanics has grown significantly owing to migration from Mexico and Central America. A substantial portion of the population are followers of the Roman Catholic Church and the Church of Jesus Christ of Latter-day Saints. Arizona's population and economy have grown dramatically since the 1950s because of inward migration, and the state is now a major hub of the Sun Belt. Cities such as Phoenix and Tucson have developed large, sprawling suburban areas. Many large companies, such as PetSmart and Circle K, have headquarters in the state, and Arizona is home to major universities, including the University of Arizona, Arizona State University, and Northern Arizona University. The state is known for a history of conservative politicians such as Barry Goldwater and John McCain, though it has become a swing state in recent years.
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"
In the Lower Belvedere in Vienna
The view from the monopteros of the English Garden.
A vista a partir do monóptero do Jardim Inglês.
en.wikipedia.org/wiki/Risley_Moss
Risley Moss is an area of peat bog situated near Birchwood in Warrington, England. It covers an area of 210.5 acres (85.2 ha) and is one of the last remaining fragments of the raised bogs that once covered large areas of South Lancashire and North Cheshire. Natural depressions in the glacial drift left by the ice sheets which covered the Cheshire–Shropshire plain during the last ice age, 10,000–15,000 years ago, filled with water, forming the meres and mosses characteristic of the area today. In some cases, like Risley Moss, peat accumulation filled the depression, allowing colonisation by bog mosses such as the Sphagnum varieties, thus giving rise to the name "moss".
Risley Moss is one of only two mosses in Cheshire where the water level has been deliberately raised in an attempt to encourage the regeneration of an active bog surface.[1] The long-term restoration project to re-wet the moss began in 1978 and was completed in 2002. This scheme was undertaken to create a series of scrapes and bunds to retain water and recreate the perfect conditions for bog flora such as cotton grass and sphagnum mosses to re-colonise the bogs.[2]
It was the former site of a large Royal Ordnance Factory. Today, it is managed by Cheshire County Council as a country park and an educational nature reserve. It was designated a Site of Special Scientific Interest in 1986.[1] Risley Moss, together with Astley and Bedford Mosses and Holcroft Moss, is also a European Union designated Special Area of Conservation, known as Manchester Mosses.[3]
Features
The main feature of Risley Moss is the large peat bog flats, overlooked by two observation points: a large watchtower, ideal for bird watching, and a smaller lookout. These points have additional information inside relating to bird species and landscape layouts. The Moss also has several smaller huts located inside the forested area for bird watching and nature enthusiasts.
Tours across the flats and nature reserve are available from the main information centre and are undertaken by local rangers.
In addition to the natural features and landscape, there are several sculptures around the site, usually with a natural theme.
Source: en.wikipedia.org/wiki/Devils_Tower
Devils Tower (also known as Bear Lodge Butte) is a butte, possibly laccolithic, composed of igneous rock in the Bear Lodge Ranger District of the Black Hills, near Hulett and Sundance in Crook County, northeastern Wyoming, above the Belle Fourche River. It rises 1,267 feet (386 m) above the Belle Fourche River, standing 867 feet (265 m) from summit to base. The summit is 5,112 feet (1,559 m) above sea level.
Devils Tower was the first United States national monument, established on September 24, 1906 by President Theodore Roosevelt. The monument's boundary encloses an area of 1,347 acres (545 ha).
Source: www.nps.gov/deto/index.htm
Many People, Many Stories, One Place
The Tower is an astounding geologic feature that protrudes out of the prairie surrounding the Black Hills. It is considered sacred by Northern Plains Indians and indigenous people. Hundreds of parallel cracks make it one of the finest crack climbing areas in North America. Devils Tower entices us to learn more, explore more and define our place in the natural and cultural world.
Source: www.blackhillsbadlands.com/parks-monuments/devils-tower-n...
Devils Tower National Monument, a unique and striking geologic wonder steeped in Native American legend, is a modern-day national park and climbers' challenge. Devils Tower sits across the state line in northeast Wyoming. The Tower is a solitary, stump-shaped granite formation that looms 1,267 feet above the tree-lined Belle Fourche River Valley, like a skyscraper in the country. Once hidden below the earth’s surface, erosion has stripped away the softer rock layers revealing the Tower.
The two-square-mile park surrounding the tower was proclaimed the nation’s first national monument by President Theodore Roosevelt in 1906. The park is covered with pine forests, woodlands, and grasslands. While visiting the park you are bound to see deer, prairie dogs, and other wildlife. The mountain’s markings are the basis for Native American legend. One legend has it that a giant bear clawed the grooves into the mountainside while chasing several young Indian maidens. Known by several northern plains tribes as Bears Lodge, it is a sacred site of worship for many American Indians. Devils Tower is also remembered as the movie location for “Close Encounters of the Third Kind.”
The stone pillar is about 1,000 feet in diameter at the bottom and 275 feet at the top and that makes it the premier rock climbing challenge in the Black Hills. Hikers enjoy the Monument’s trails. The 1.25-mile Tower Trail encircles the base. This self-guided hike offers close-up views of the forest and wildlife, not to mention spectacular views of the Tower itself. The Red Beds Trail covers a much wider three-mile loop around the tower.
Source: travelwyoming.com/places-to-go/destinations/national-park...
While America’s first national monument garnered significant attention as the backdrop to the 1977 Stephen Spielberg movie, Close Encounters of the Third Kind, the tower is sacred to Northern Plains Indian tribes and the Black Hills region Kiowa Tribe. With oral storytelling and a history that dates back thousands of years, today, American Indian tribes continue to hold sacred ceremonies at the tower, including sweat lodges and sun dances. There is more to this monument than its rich history. You can stop at the visitor’s center to learn about one of the ranger-led programs, night sky viewing, hiking and even climbing to the top of Devils Tower. If one day isn’t enough to explore this unforgettable area, bring your camping gear to stay within the monument, or stay just outside or in accommodations at one of the nearby towns.
Additional Foreign Language Tags:
(United States) "الولايات المتحدة" "Vereinigte Staaten" "アメリカ" "美国" "미국" "Estados Unidos" "États-Unis"
(Wyoming) "وايومنغ" "怀俄明州" "व्योमिंग" "ワイオミング州" "와이오밍" "Вайоминг"
(Devils Tower National Monument) "النصب التذكاري الوطني لبرج الشياطين" "魔鬼塔国家纪念碑" "डेविल्स टॉवर राष्ट्रीय स्मारक" "デビルズタワー国定公園" "데빌스 타워 국립천연기념물" "Национальный монумент «Башня дьявола»" "Monumento Nacional Torre del Diablo"