Beckley Park was first enclosed in the 12th century from land held by Roger d'Ivry and later by Richard, Duke of Cornwall, who built a palace on Beckley Hill around which grew the village. He then limited the area of the park by a stone wall, partly extant, and stocked with deer. The hunting lodge was built on a Saxon site at this spot in the centre of the enclosure. First mentioned in 1347, the lodge was re-built in 1376 for King Edward III; the moats, hall buttresses date from the late 14th century. The park was crown property and its keepers appointed by the King for two centuries: notable families were the Hamdens, the Verneys; and Sir John, later Lord Williams of Thame who in 1550 held the park by grant, rebuilt the lodge to probably the present structure.
The park and lodge passed to the Norreys family, whose head in the late 17th  was created Earl of Abingdon. In the early 17th Century also a family of Ledwells lived there for generations. The Estate was sold by the son of the seventh Earl of Abingdon to the grandmother of the present owner in 1920. (HM Land Registry, Gloucester Office: Title Number ON145383 Beckley Park: The Title Register refers on Page 7 to a conveyance dated 18 November 1920 made between 1. The Right Hon Vere Frederick Viscount Bertie of Thame (grandson of the Earl of Abingdon), 2. The Rev Hon Alberic Edward Bertie & others and 3. Clotilde Kate Feilding.)
The house remains unaltered and 'unmodernised' to an unusual extent. It has been a Grade I listed building (with some Grade II listed areas) of historic interest since 1984 (List Entry Number: 1001087). The listing offers this summary:
 Formal early C20 gardens surrounding a mid C16 hunting lodge, incorporating the remains of three concentric medieval moats, formerly enclosing a medieval royal hunting lodge. The moats were probably part of medieval garden features, which possibly extended into the wider landscape of the surrounding former deer park.
The Listing document provides a summary of the history of the property including this coverage of the early years:
Beckley Park, known as Lower Park Farm in the C19 and early C20, is first recorded in 1175-6, having been for some time part of the capital seat of the Honour of St Valery, that is, the main property of the St Valery family. In the 1190s the park was refurbished and enclosed by a stone wall. In 1227, the park having come into the hands of the Crown, Henry III granted the manor and park to his brother the Earl of Cornwall who restocked the park with deer and constructed a deer leap. The park subsequently passed through the hands of several members of the Royal Family during the Middle Ages. Beckley Park formed the site of the park hunting lodge, situated at the centre of the c 300ha park, probably initially built in the early C13 and by 1300 being used as a centre for royal hunting parties and other entertainments. The site contained a hall, chambers, chapel, kitchen and stables, together with a garden and vineyard, all possibly contained within a moat. The lodge was rebuilt on a more lavish scale for Edward II over several years from 1373, and included an outer moat, planted around its outer perimeter with a hedge, with two gates and a porter's lodge. This work is assumed to have resulted in the present triple moats (VCH 1957; Taylor 1996).
After numerous years in ruin, the property was bought on November 18, 1920, by the first international woman architect Clotilde Kate Feilding (1874-1937) and restored by Clotilde and her husband, Percy. Clotilde was the daughter of Henry Bennet Brewster of the Palazzo Mattei in Rome and the Baroness Julia von Stockhausen. Among other work, Clotilde Brewster, as she was known then, was the architect of two palaces in Rome: the Palazzo Soderini and the Palazzo Frankenstein. Percy Henry Feilding (1867-1929) was the son of Sir Percy Robert Basil Feilding.


As part of BedZED's eco friendly low-energy-emission concept, cars are discouraged; the project encourages public transport, cycling and walking, and has limited parking space. There are good rail and bus links in the immediate area. They also have a car-share scheme.


Pits dating from the 4th millennium BC indicate that the site of Beeston Castle was inhabited or used as a communal gathering place during the Neolithic period. Archaeologists have discovered Neolithic flint arrow heads on the crag, as well as the remains of a Bronze Age community, and of an Iron Age hill fort. The rampart associated with the Bronze Age activity on the crag has been dated to around 1270–830 BC; seven circular buildings were identified as being either late Bronze Age or early Iron Age in origin. It may have been a specialist metalworking site.


Begnas Lake area with a number of resorts is a popular destination for tourists visiting Pokhara. The water from the lake is used for irrigation and some parts of the lake are used as caged fisheries. The Begnas lake area has a number of swampy areas around it, many of which have been converted to paddy fields. Annapurna and Manaslu Range can be seen very clearly from the lake.


The Belfry of Bruges (Dutch: Belfort van Brugge) is a medieval bell tower in the
centre of Bruges, Belgium. One of the city's most prominent symbols, the belfry formerly housed a treasury and the municipal archives, and served as an observation post for spotting fires and other dangers.


According to the National Weather Service, the warmest month at Big Bear is July, with a daily average temperature of  64.7 °F (18.2 °C).  The coolest month is January, with a daily average temperature of 34.1 °F (1.2 °C). There are an average of 1.7 days each year with highs of 90 °F (32 °C) or higher. Freezing temperatures have occurred in every month and occur on an average of 186 days each year, on average from September 24 to June 4. With a period of record dating only back to 1960, the highest temperature recorded was 94 °F (34 °C), last recorded on July 15, 1998, while lowest was −25 °F (−32 °C) on January 29, 1979.
Due to the 6,790 to 7,200 ft (2,070 to 2,190 m) elevation of the weather station, precipitation is greater than in the lowlands of San Bernardino County, averaging 21.15 in (537 mm) a year. The maximum 24-hour precipitation was 9.43 in (240 mm) on December 6, 1966.  Measurable precipitation normally occurs 44.9 days a year. Mountain thunderstorms occasionally produce heavy rainfall, even in midsummer (when most southern California lowland locations are quite dry). Big Bear Lake's climate is Csb (Warm-summer Mediterranean) under the Köppen climate classification.
In contrast to most of southern California, the Big Bear Lake region normally receives significant winter snow because of its high elevation. Snowfall, as measured at lake level, averages 72 in (180 cm) per season; upwards of 100 in (250 cm) can accumulate on the forested ridges bordering the lake, at elevation above 8,000 ft (2,400 m). In February 1990, 59.5 in (151 cm) of snow were recorded. The most snow in 24 hours was 27.0 in (69 cm) on March 27, 1991. The greatest snow depth was 58 in (150 cm) on February 3, 1979.  Snow has fallen in every month except July and August. There are normally 18 days each year with measurable snow of .1 in (0.25 cm) or more.


The Bingham Canyon Mine, more commonly known as Kennecott Copper Mine among locals, is an open-pit mining operation extracting a large porphyry copper deposit southwest of Salt Lake City, Utah, in the Oquirrh Mountains. The mine is the largest man-made excavation, and deepest open-pit mine in the world, which is considered to have produced more copper than any other mine in history – more than 19,000,000 short tons (17,000,000 long tons; 17,000,000 t). The mine is owned by Rio Tinto Group, a British-Australian multinational corporation.  The copper operations at Bingham Canyon Mine are managed through Kennecott Utah Copper Corporation which operates the mine, a concentrator plant, a smelter, and a refinery. The mine has been in production since 1906, and has resulted in the creation of a pit over 0.75 miles (1,210 m) deep, 2.5 miles (4 km) wide, and covering 1,900 acres (3.0 sq mi; 770 ha; 7.7 km²). It was designated a National Historic Landmark in 1966 under the name Bingham Canyon Open Pit Copper Mine. The mine experienced a massive landslide in April 2013 and a smaller slide in September 2013.


Minerals, in the form of copper ore, were first discovered in Bingham Canyon in 1848 by two brothers, Sanford and Thomas Bingham, sons of Erastus Bingham, Latter-Day Saint pioneers of September 1847, who grazed their cattle there. They reported their find to their leader, Brigham Young, who advised against pursuing mining operations because the survival and establishment of settlements was of paramount importance at that time. The brothers applied themselves to that purpose as directed and did not stake a claim. In 1850, the Bingham family went to settle what is now Weber County, leaving the canyon still today known by their name.
It was not until September 17, 1863, that extraction of ore began and the potential of the canyon's mineral resources began to be widely recognized. That was when George B. Ogilvie and 23 others "located the West Jordan claim", soon followed by the Vidette claim.  At first, mining was confined to placer gold, lead-silver and copper-gold. Porphyry copper required processing and a railroad, which reached the canyon in 1873.
Enos Andrew Wall started working claims in 1887.  His extensive tunnels and test pits, on his 200-acre (81 ha), indicated ore containing 2% copper.
The canyon's 19th Century mines were relatively small, and it wasn't until the end of the century that very large-scale exploitation of the canyon's ore bodies began to develop with open-pit mining.  In 1896, Samuel Newhouse and Thomas Weir acquired the Highland Boy Mine, which was rich in copper, silver and gold.  Together they formed the Utah Consolidated Gold Mines, Ltd. with English investors.  They then formed the Boston Consolidated Gold and Copper Co., Ltd., for development of low-grade copper ore adjacent to the Utah Copper Company site.
Another significant development took place in 1903, when Daniel C. Jackling and Enos A. Wall organized the Utah Copper Company. Utah Copper immediately began construction of a pilot mill at Copperton, just beyond the mouth of the canyon, and the company actually started mining in 1906.
The success of Utah Copper in mining the huge but low-grade porphyry copper type ore body at Bingham Canyon was based on Jacklin's 1904 decision to use open-pit mining, steam shovels and the railroad.  The mine became a showplace for "railroad-pit operations" and the industrial complex defined by the mine and the ASARCO smelting operation made it the "largest industrial mining complex in the world" by 1912.
Utah Copper and Boston Consolidated merged after their separate surface operations approached each other in 1906.  The Kennecott Copper Corporation, established to operate mines in Kennecott, Alaska, purchased a 25 percent financial interest in Utah Copper in 1915, which they increased to 75 percent in 1923.
Bingham's Canyon mine expanded rapidly, and by the 1920s the region was a beehive of activity. Some 15,000 people of widely varying ethnicity lived in the canyon, in large residential communities constructed on the steep canyon walls.  The population declined rapidly as mining techniques improved, and several of the mining camps were swallowed up by the ever-expanding mine. By 1980, when Lark was dismantled, only Copperton, at the mouth of Bingham Canyon and with a population of 800, remained.
The 21 separate mining operations in existence by 1911 were consolidated into two in 1970: Kennecott and The Anaconda Minerals Company.  In 1985 open-pit mining operations were halted by Kennecott's Utah Copper.  In 1986, Kennecott discovered gold in nearby Barney's Canyon.
KCC was purchased by Sohio in 1981 and the mine reopened in 1987 after BP Minerals purchased the assets.  In 1989 the Rio Tinto Group acquired the asset, who modernized the mine, mill and smelter.
The open-pit owners replaced an antiquated 1000-car railroad with conveyor belts and pipelines for transporting the ore and waste, which reduced costs by nearly 30% and returned the operation to profitability.


At 9:30 pm on April 10, 2013, a landslide occurred at the mine. Around 2.3–2.5 billion cubic feet (65×10⁶–70×10⁶ m³) of dirt and rock thundered down the side of the pit. It is possibly the largest historic, non-volcanic landslide in North America. On the basis that the mine's steep walls made it a high risk for landslides, an interferometric radar system had been previously installed to monitor the ground's stability. As a result of warnings produced by this system, mining operations had been shut down the previous day in anticipation of the slide and there were no injuries. The massive slide was expected to cut production of mined copper by 100,000 tonnes (98,000 long tons; 110,000 short tons). A second slide caused an evacuation of 100 workers on September 11, 2013. Another, less severe slide occurred on May 31, 2021.


The Bingham Canyon ore deposits occur in the Bingham nappe.  They are a porphyry copper deposit, formed by a quartz monzonite porphyry intruded into sedimentary rocks.  They exhibit a concentric alteration pattern and mineralogic zonation around the Bingham stock.  These zones include a central core containing magnetite, followed by "a molybdenite zone low in copper, a bornite-chalcopyrite-gold higher grade copper zone, a pyrite-chalcopyrite zone, a pyrite zone, and an outermost lead-zinc zone."
Structurally, Late Paleozoic rocks were thrust faulted over the Precambrian craton during the Cretaceous Sevier orogeny.  These rocks were later intruded and altered in the Tertiary by granitoid rocks.  This igneous event was the source of deposition of gold, silver and other base metals.
Copper and molybdenum sulfide minerals are dispersed in the intruded stock and in the adjoining carbonate sedimentary skarns. The main stratigraphic rocks in Bingham Canyon are Upper Pennsylvanian sandstones, quartzites, and limestones known as the Bingham Mine Formation in the Oquirrh Group.  The central porphyry ores formed from mantle hydrothermal circulation while the outer vein and deposits in the sedimentary rocks formed at lower temperature when magmatic and meteoric waters mixed.


The extracted ore is treated at the Kennecott smelter at nearby Magna, Utah. The ore is run through a concentrator, where grinding mills reduce it to the consistency of face powder. Flotation then separates the gangue from the metalliferous particles, which float off as a 28-percent concentrate of copper along with lesser amounts of silver, gold, lead, molybdenum, platinum and palladium. A selective flotation step separates the molybdenite (molybdenum disulfide) from the chalcopyrite.
The filtered concentrate slurry is piped 17 miles (27 km) to the smelter, where it is dried, and then injected along with oxygen into a flash smelting furnace to oxidize the iron and sulfur. The oxidized iron is skimmed off, while the sulfur dioxide gas is captured and sent to an on-site acid plant for conversion to valuable sulfuric acid – a million tons of it each year.
Left behind is a molten copper sulfide called matte. The 70-percent-copper matte is water-quenched to form a sand-like solid, then injected, with oxygen, into a flash-converting furnace that produces molten, 98.6-percent-pure copper. This copper is then cast into 700-pound (320 kg) anode plates and shipped by rail to the refinery.
At the refinery, the anode plates are pressed flat and interleaved with stainless steel cathode blanks. Automated robotic vehicles place the prepared anodes in cells containing an acidic electrolyte. When the cells are electrified, the anodes slowly dissolve, freeing copper ions that are deposited on the cathode as 99.99-percent-pure copper.
Impurities and precious metals settle to the bottom of the electrolytic cells as anode slimes. A chlorination leaching process recovers the gold and silver, which is melted in induction furnaces.


Bingham Canyon has proven to be one of the world's most productive mines. As of 2004, its ore yielded more than 17 million tons (15.4 Mt) of copper, 23 million ounces (715 t) of gold, 190 million ounces (5,900 t) of silver, and 850 million pounds (386 kt) of molybdenum.  The value of the resources extracted from the Bingham Canyon Mine is greater than the Comstock Lode, Klondike, and California gold rush mining regions combined.  Mines in Chile, Indonesia, Arizona,  and New Mexico now exceed Bingham Canyon's annual production rate.  High molybdenum prices in 2005 made the molybdenum produced at Bingham Canyon in that year worth more than the copper. The value of metals produced in 2006 at Bingham Canyon was US$1.8 billion.


In 1990, homes that had been built on former flood plains were discovered to be contaminated with high levels of lead and arsenic.  Activities to clean up 100 years of accumulated impacts began in the 1990s, under state Utah Department of Environmental Quality and federal oversight and are ongoing.
The EPA lists "Kennecott South Zone/Bingham" on its superfund webpage, after it was proposed to be listed as a superfund site in 1994. The South Zone includes the Bingham Mining District in the Oquirrh Mountains, about 25 mi (40 km) southwest of Salt Lake City, the open pit, waste rock dumps, Copperton Mill and other historic sites. The company avoided regulatory issues of being on the NPL by voluntarily cleaning up the contaminated lands, the Superfund Alternative Approach. The listing proposal was withdrawn in 2008. More than 25 million tons of mining wastes have been removed; sludge with elevated sulfate concentrations was consolidated and capped on site.


Sources from Birka are mainly archaeological remains. No texts survive from this area, though the written text Vita Ansgari ("The Life of Ansgar") by Rimbert (c. 865) describes the missionary work of Ansgar around 830 at Birka, and Gesta Hammaburgensis Ecclesiae Pontificum (Deeds of Bishops of the Hamburg Church) by Adam of Bremen in 1075 describes the Archbishop Unni, who died at Birka in 936. Saint Ansgar's work was the first attempt to convert the people of Birka from the Norse religion to Christianity. It was unsuccessful.
Both Rimbert and Adam were German clergymen writing in Latin. There are no known Norse sources mentioning the name of the settlement, or even the settlement itself, and the original Norse name of Birka is unknown. Birca is the Latinised form given in the written sources by Rimbert and Adam; and Birka is the contemporary, unhistorical Swedish form. The Latin name is probably derived from an Old Norse word "birk" which probably means a market place. Related to this was the Bjärköa law (bjärköarätt) which regulated the life of market places in Denmark, Norway and Sweden. Birka and similar spellings are very common in Scandinavian place names still today leading to speculation that all references to Birka, especially those by Adam of Bremen, were not about the same location.
Both publications are silent on Birka's size, layout, and appearance. Based on Rimbert's account, Birka was significant because it had a port and it was the location of the regional ting. Adam only mentions the port, but otherwise, Birka seems to have been significant to him because it was the start of Ansgar's Christian mission and because Archbishop Unni was buried there.
Vita Ansgari and Gesta are sometimes ambiguous, which has caused some controversy as to whether Birka and the Björkö settlement are the same location. Many other locations have been suggested through the years. However, Björkö is the only location that shows remains of a town of Birka's significance, which is why the vast majority of scholars regard Björkö as the location of Birka.
Birka was abandoned during the latter half of the 10th century. Based on the dating of the coins, the city seems to have died out around 960. Roughly around the same time, the nearby settlement of Sigtuna supplanted Birka as the main trading center in the Mälaren area. The reasons for Birka's decline are disputed. A contributing factor may have been the post-glacial rebound, which lowered the water level of Mälaren changing it from an arm of the sea into a lake and cutting Birka off from the nearest (southern) access to the Baltic Sea.  The Baltic island of Gotland was also in a better strategic position for Russian-Byzantine trade and was gaining eminence as a mercantile stronghold. Historian Neil Kent has speculated that the area may have been the victim of an enemy assault.
The Varangian trade stations in Russia suffered a serious decline at roughly the same date.


On 15 June 2022, it was announced that archaeologists from Stockholm University's Archaeological Research Laboratory had found a Viking Age shipyard in Lake Mälaren. It was the first time a site like the shipyard had been found.
"The site found consisted of a stone-lined depression in the Viking Age shore zone with a wooden boat slip at the bottom. The finds at the site consist of large quantities of both unused and used boat rivets, whetstones made from slate and woodworking tools."


Black Moshannon State Park is a 3,480-acre (1,410 ha) Pennsylvania state park in Rush Township, Centre County, Pennsylvania, United States. It surrounds Black Moshannon Lake, formed by a dam on Black Moshannon Creek, which has given its name to the lake and park. The park is just west of the Allegheny Front, 9 miles (14 km) east of Philipsburg on Pennsylvania Route 504, and is largely surrounded by Moshannon State Forest. A bog in the park provides a habitat for diverse wildlife not common in other areas of the state, such as carnivorous plants, orchids, and species normally found farther north. As home to the "largest reconstituted bog in Pennsylvania", it was chosen by the Pennsylvania Department of Conservation and Natural Resources for its "25 Must-see Pennsylvania State Parks" list.
Humans have long used the Black Moshannon area for recreational, industrial, and subsistence purposes. The Seneca tribe used it as hunting and fishing grounds. European settlers cleared some land for farming, then clear-cut the vast stands of old-growth white pine and eastern hemlock. Black Moshannon State Park rose from the ashes of a depleted forest which had been largely destroyed by wildfire in the years following the lumber era. The forests were rehabilitated by the Civilian Conservation Corps during the Great Depression in the 1930s. Many of the buildings built by the Civilian Conservation Corps stand in the park today and are protected on the list of National Register of Historic Places in three historic districts.
Black Moshannon State Park is open year-round for recreation and has an extensive network of trails which allow hiking, biking, and viewing the bog habitat at the Black Moshannon State Natural Area. The park is in a Pennsylvania Important Bird Area, where bird watchers have recorded 175 species. It is also home to many rare and unusual plants and animals due to its location atop the Allegheny Plateau; the lake is at an elevation of about 1,900 feet (580 m). Much of the park is open for hunting and the lake and creek are open for fishing, boating, and swimming. In winter it is a popular destination for cross-country skiing, and was home to a small downhill skiing area from 1965 to 1982. Picnics and camping are also popular, and the "Friends of Black Moshannon State Park" group promotes the park and all the recreational activities associated with it.


The Civilian Conservation Corps (CCC) was a work relief program for young men from unemployed families, established in 1933. As part of President Franklin D. Roosevelt's New Deal legislation, it was designed to combat unemployment during the Great Depression. The CCC operated in every U.S. state. The original facilities at Black Moshannon State Park were constructed by the CCC from 1933 to 1937, one of many projects it undertook throughout central Pennsylvania.
Beaver Meadow CCC Camp S-71 was built in May 1933 near the abandoned village of Beaver Mills, and was one of the first to expand recreational facilities in Pennsylvania. More than 200 young men moved in and began the work of conserving soil, water, and timber in the area. They cut roads through the growing forest to aid in fighting the wildfires that sprang up, and planted many acres of red pines as part of the reforestation effort.
Most of the CCC-built park facilities are still in use today, including log cabins, picnic pavilions, a food concession stand, and miles of trails. Early on, the CCC constructed a dam at Black Moshannon Lake, on the site of the former mill pond dam. CCC Camp S-71 closed in January 1937 and Black Moshannon State Park officially opened that same year.


The bogs at the park contain large amounts of sphagnum moss; this decomposes very slowly, causing layers of dead moss to build up at the bottom of the bog, creating peat. In 1994, 1,592 acres (644 ha) of bog at the state park were protected as the "Black Moshannon Bog Natural Area"; this was originally conceived as part of the State Parks 2000 strategic plan of the DCNR, and fourteen years later the total area of bog protected as a Natural Area had increased to 1,992 acres (806 ha).
Most bogs exist in glaciated areas, but Black Moshannon State Park is on the Allegheny Plateau. This area was not covered by glaciers during the last ice age. The bogs formed here because of the beds of sandstone that lie flat, a short distance below the surface of the earth. The sandstone formations in the park do not absorb water very well, so any depression in them will collect water, as has happened here. The bogs extend the shores of the lake. Migratory shorebirds that visit here include greater and lesser yellowlegs, least sandpiper, solitary sandpiper, and the spotted sandpiper, which has been confirmed as using the IBA as a breeding grounds.
The water in the bog is low in nutrients and high in acidity, which makes it difficult for most plants to live there. Only specialized plants can thrive in the park bogs: there are three species of carnivorous plants and seventeen varieties of orchid. Wild cranberries and blueberries grow in the bog along with sedges, leatherleaf shrubs, Arctic cotton grass, and viburnums. The bogs are all protected by the state of Pennsylvania.


White-tailed deer, wild turkey, ruffed grouse, opossum, raccoon, hawks, chipmunks, porcupine, woodpeckers, and flying, red, and eastern gray squirrels are all fairly common in the park. Black bears also inhabit Black Moshannon State Park. Many of these animals were decimated due to the effects of deforestation, pollution and unregulated hunting and trapping during the late 19th century. Hunting controls established by the Pennsylvania Game Commission and the work of the Civilian Conservation Corps and Pennsylvania Department of Conservation and Natural Resources in re-establishing the second growth forest have led to the strong comeback of game species at Black Moshannon State Park and throughout the forests of Pennsylvania.
The lake is home to American beavers, as well as great blue heron, swans, snow geese, common loons, and many other types of waterfowl, with Canada goose, ring-necked duck, mallard, and wood duck the most commonly seen. The bogs, marshes, and swamps contain frogs and salamanders, and provide a habitat for carnivorous plants like the pitcher plant and sundew. Black Moshannon State Park is home to many common species of songbirds, including ovenbirds.
The conifer and mixed-forests of the park and its surroundings provide habitats for northern saw-whet owl, blue-headed vireo, hermit thrush, dark-eyed junco, and magnolia, pine, yellow-rumped, Blackburnian, and black-throated green warblers. The deciduous forests provide habitats for songbirds, such as scarlet tanager and red-eyed vireo.
An outbreak of the non-native gypsy moth in the mid-1980s nearly devastated the woods in a small valley. Selective timber cuts harvested the trees that were affected by species of moth. Today the 1.2-mile (1.9 km) Sleepy Hollow Trail for hiking, biking, and cross-country skiing loops through the new growth in the area, which provides an ideal habitat for populations of white-tailed deer and wild turkey.


Twenty-one cabins can be used by visitors at Black Moshannon State Park. Thirteen are rustic cabins, built by the CCC, with electric lights, a kitchen stove and a wood-burning stove, refrigerator, and bunk beds. Six are modern cabins, including the former ski lodge, with electric heat, a bedroom, living room, kitchen, and bath. There are also two deluxe camping cottages with electric heat and similar amenities as the rustic cabins. All cabin renters need to bring their own household items such as linens and cookware. Pets are prohibited in all cabins in the park.
There are seventy-two campsites at Black Moshannon State Park. Each campsite has access to washhouses with flush toilets, showers, and laundry tubs. The campsites also have fire rings and picnic tables. There is also an organized group tenting area, which can accommodate up to 60 persons. Some sites allow pets; there are also twelve full hook-up sites available. These have electric service, water and sewer hook-ups as well. Nine sites are tent-only.
The sandy beach on Black Moshannon Lake is open from Memorial Day weekend through Labor Day weekend, and the beach bathhouse was built by the CCC. Beginning in 2008, lifeguards will not be posted at the beach.
There are eight picnic pavilions built by the CCC in the park, which can be reserved for a fee. In addition to the pavilions, Black Moshannon State Park has 250 picnic tables in four large picnic areas. The use of these picnic tables and unreserved pavilions is first come, first served, and they are free of charge.
Some modern activities are prohibited in Black Moshannon State Park. The operation of drones and similar radio controlled devices is prohibited. All-terrain vehicle usage is also prohibited and closely monitored by DCNR. Further, removing any natural items is illegal as is firewood cutting without a permit.


There are 21 miles (34 km) of trails at Black Moshannon State Park; all are open to hiking, most are open to cross-country skiing during the winter months, and select trails are open to snowmobiles and mountain bikes. The park is especially popular among cross-country skiing enthusiasts due to its high elevation. Skiers will find trails that are largely free of rocks, with a layer of grass beneath the snow. Sleepy Hollow, Seneca, Indian, and Hay Road Trails are most frequently used. Eight of the park's fourteen trails are described above, the remaining six follow.
Allegheny Front Trail is a 41.8-mile (67.3 km) hiking trail that passes through Black Moshannon State Park and Moshannon State Forest. It was built in the late 1990s and offers several vistas looking out from atop the Allegheny Front.
Blueberry Trail is a 1-mile (1,600 m) loop between the airport and bog with "abundant berries".
Bog Trail is a 0.5-mile (800 m) boardwalk hiking trail that was built by the Pennsylvania Conservation Corps and has received awards for its handicapped accessibility. Bog Trail loops through the bog at the park passing by lilies, sedges, rushes, Leatherleaf, and various carnivorous plants. Visitors may observe waterfowl and wildlife in the bogs. Access for the handicapped is provided at the boating area.
Lake Loop Trail is a 0.7-mile (1,100 m) loop which crosses the Pennsylvania Route 504 bridge over the lake and the bridge over Black Moshannon Creek just below the dam.
Moss-Hanne Trail is an 7.7-mile (12.4 km) trail through the Black Moshannon Bog Natural Area. It is open to hiking and cross-country skiing. The trail passes through pine plantations, hardwood forests, spruce groves, hemlock-filled bottomlands, patches of wild blueberries, and by beaver ponds. The area is marshy; waterproof footwear is recommended and parts of the trail are boardwalks. Bikes are prohibited on the Moss-Hanne trail.
Snowmobile Trail is a 1.1-mile (1.8 km) trail that departs the park area behind Pavilion 6. It provides access to the many miles of trails in Moshannon State Forest that are open to recreational snowmobiling. It is open during summer months for hiking and mountain biking.


The High Blauen Road (Hochblauenstraße) was opened to private vehicles in 1928. About half the route is in the county of Freiburg-Hochschwarzwald. In its northwestern section it thus bears the designation K 4948, in the southeastern section it runs under the number K 6314, where the Wollbach highway agency is responsible. Winter clearance of the whole route is undertaken by the Müllheim highway agency by arrangement between the counties. The road runs to the top. Since 2011 during the summer months there has also been a bus route that links the summit on Sundays and holidays via Marzell and Kandern with Basle. In addition, variant A of the West Way, a long-distance path maintained by the Black Forest Club that runs for 280 kilometres (170 mi) from Pforzheim to Basle, goes over Blauen.
Between 1957 and 1980 there was a reallocation of land in the mountain forest which, after comprehensive and expensive survey work, resulted in 42 small parcels of land being consolidated into twelve larger ones. To commemorate this, a monument was erected in 2007 with a brass plate that records the names of all the participants.
Tourist facilities on Blauen first appeared in 1872 when a covered forest inn (Waldschenke) was opened. In June 1875 the first house was opened; it bore the name Krone des Blauen ("Crown of Blauen"). It was expanded in 1890 and again in 1965–1966, in order to handle the increase number of tourists.
The water main installed in 1898 is still used and runs 150 metres (490 ft) down to a spring. Since 1925, when a cable was laid to Blauen from Marzell there has been electricity at the summit. Three years later the first motorised vehicles made their way up the mountain road.
At the summit is the Berghaus Hochblauen (also called the Blauenhaus), an inn with overnight accommodation. Since spring 2013 the inn has been closed. In 2015 it was being modified and should be open in 2016.


Also at the peak stands a 93-metre-high Deutsche Telekom VHF and microwave radio relay tower. The tower is a reinforced concrete Typenturm, built in 1985. The following radio stations are broadcast from this tower: SWR1 Baden-Württemberg (89.2 FM/8.4 kW), SWR2 (92.6 FM/8.4 kW), SWR3 (97.0 FM/8,4 kW), Deutschlandfunk (105.1 FM/10 kW), Radio Regenbogen (101.1 FM/8,4 kW) und baden.fm (106.0 FM/8,4 kW). The tower is also used by the amateur radio repeater DB0YE.
The tower serves mainly the southern Upper Rhine valley as well as a large portion of the Breisgau-Hochschwarzwald and Lörrach rural districts. The stations transmitted from Blauen are also easily received in northwestern Switzerland. Until the end of the 1980s the former SWF broadcast could be heard well beyond the Vosges mountains to the west. Since then the power of the transmissions toward France have been limited by international agreements.


Blickling Hall is a Jacobean stately home situated in 5,000 acres of parkland in a loop of the River Bure, near the village of Blickling north of Aylsham in Norfolk, England. The mansion was built on the ruins of a Tudor building for Sir Henry Hobart from 1616 and designed by Robert Lyminge. The library at Blickling Hall contains one of the most historically significant collections of manuscripts and books in England, containing an estimated 13,000 to 14,000 volumes. The core collection was formed by Sir Richard Ellys. The property passed into the care of the National Trust in 1940.


During World War II the house was requisitioned and served as the Officers' Mess of nearby RAF Oulton. After the death of Philip Kerr, 11th Marquess of Lothian (the last private owner of Blickling) in December 1940, the Blickling estate passed into the care of the National Trust as part of his bequest, under the terms of the Country Houses Scheme. RAF servicemen and women were billeted within the grounds in Nissen huts, whilst officers were housed in the house itself. The adjacent lake was used by RAF service personnel to practise dinghy drills during the Second World War. The National Trust has created the RAF Oulton Museum on site in tribute to the RAF pilots and ground crew who served in the Second World War, and this may be visited for no additional entrance fee.
At the end of the war, the house was de-requisitioned. The National Trust again let it to tenants until 1960, when the Trust began work to restore the house to a style reflecting its history. The house and grounds were opened to the public in 1962 and remain open under the name of "Blickling Estate". During 2019, the site received 225,624 visitors.
In 2015 the National Trust marked the 75th anniversary of Philip Kerr's death with a celebration of his life and times.
Work began in October 2015 to introduce a heat pump system, using residual warmth from the lake. A raft of tubes, filled with a plant-based glycol, would be sunk into the lake and the liquid pumped into the main boiler-room for conversion to a higher temperature to heat the hall and west wing of the building. The new system would allow the removal of two oil tanks, and produce an annual saving of more than 25,000 litres of oil, and £16,000.
In February 2021, it was reported that the parasitic wasp species Trichogramma evanescens was being deployed to the hall in an attempt to prevent damage to various artworks there, including a tapestry from Catherine the Great, caused by difficulties controlling the common clothes moth. In conjunction with this, chemicals to confuse the moths' mating behaviour would also be used.


Bloomingdale is in the southwestern part of Ward 5, currently represented on the City Council by Councilmember Kenyan McDuffie. Bloomingdale is a part of Advisory Neighborhood Commission 5E, currently represented by commissioners Robert Vinson Brannum, Bertha Holliday, Karla Lewis, and Dianne Barnes.


The lands that comprise Bloomingdale first began as large estates and orchards. Boundary Street, today Florida Avenue, was the dividing line between paved, planned streets (to the south), laid out in the original L'Enfant Plan, and rural country (to the north of Boundary), where landowners maintained orchards, large country estates and, later, a mixture of commercial properties.
In 1823, George Beale and his wife Emily Truxton Beale bought a 10-acre (40,000 m²) parcel of land north of the Capitol, along the City boundary, for $600.00 from William Bradley. They named it the "Bloomingdale Estate," and it grew to 50 acres (200,000 m²).
As late as the 1870s, the land where Bloomingdale now sits was largely a collection of undeveloped private estates and farming properties, most prominently those of the Beales and of the Moores.


Following Emily Truxton Beale's death in 1885, her heirs began to sell large tracts of the estate to developers. The old Bloomingdale estate rapidly changed into the modern neighborhood configuration as developers and land speculators transformed the undeveloped lands for denser residential development, between the established residential LeDroit Park and Eckington neighborhoods. By 1887, city planners had proposed extending the city's paved street grid into Bloomingdale.
In 1891, the 45-acre (180,000 m²) Moore farm, north and west of the former Beale estate and representing some of the last undeveloped property in the area, was sold to private developers. It was incorporated into the already-underway Bloomingdale neighborhood.
By 1892, the reconfiguration of Bloomingdale was underway, as large estates were consolidated and reconfigured into the predecessor to the modern neighborhood, with further development by 1894. During this time, roads corresponding to the grid system of Washington's streets were improved, curbed, and paved. Streams and creeks were buried or re-directed—most notably the Tiber Creek, many of which had been buried south of Bloomingdale in the original City of Washington. One section of the Tiber Creek in Bloomingdale ran along what is now Flagler Place.
Construction on some of the earliest homes was completed between 1892 and 1900. In the early 1900s, the remainder of the surrounding blocks had been built in a speculative nature by such developers as Harry Wardman, Francis Blundon, and S. H. Meyers in the following decade. The neighborhood website contains a list of Bloomingdale's Wardman built homes. Many of Wardman's first homes incorporate elements of Richardson Romanesque architecture (a sub-category of Victorian). This can be seen in the ornate floral and vine-like stone carving around doors and windows of many Bloomingdale homes. His later homes, like those on Adams and Bryant Streets, are in an architectural style for which he is most prominently known, brick homes that incorporate a deeper setback from the street and large covered front porch. Blundon built several homes along 1st Street including 100 W Street, NW, which he occupied with his family.
Development continued and, in 1904, the neighborhood's first school, the Nathaniel Parker Gage School, was built on the 2000 block of 2nd Street. (The school has been converted to private condominiums.) By 1909, the old estates had been sold and divided, the Tiber Creek had been buried, and the neighborhood street layout had been fully developed into its present form.
Many homes in the northern section of Bloomingdale retain carriage houses in the block interiors. Some have been converted to private residences.


Like many D.C. neighborhoods since the early 2000s, Bloomingdale has undergone substantial gentrification, with the neighborhood's once-numerous vacant properties being repurposed, sharp rises in property values, and rapidly shifting demographics. The population is nearly evenly split between White residents, many of whom have moved to the neighborhood since the 2000s, and African American residents, who have historically constituted a majority in the community.
During this period of rapid change, new businesses have opened in the neighborhood, primarily restaurants, bars, and food markets. These include Windows Market, Big Bear Cafe, Yoga District, El Camino, Bacio Pizzeria, FieldToCity, Rustik Tavern, Boundary Stone, Aroi Thai Sushi Bar, Grassroots Gourmet, Red Hen, Showtime Lounge, and Crisp Kitchen & Bar. Every summer, the Bloomingdale Farmers' Market operates on Sundays on R St between Florida Ave and 1st Street, N.W.
On May 22, 2010, the city officially dedicated a new street, Bloomingdale Court, N.W., the name given by local resident and novelist Frederick Louis Richardson for the alley system between the 100 block of U and V Streets, N.W., and the 2000 block of 1st Street and Flagler Place, N.W.
On July 27, 2018, the D.C. Historic Preservation Review Board voted to designate Bloomingdale a historic district. It was listed on the National Register of Historic Places on November 26 of the same year.
The neighborhood has several active neighborhood groups and associations including the Bloomingdale Civic Association.


Bloomingdale has its own community-managed and community-owned greenspace, Crispus Attucks Park. The acre-and-a-quarter park, in the court bounded by First, U, V, and North Capitol streets NW, was previously the site of a warehouse built in 1910 and used as a telephone-switching station and cable yard for the Chesapeake & Potomac Telephone Company.
Chesapeake & Potomac Telephone Company stopped using the property in 1974 and tried to sell it, but no one wanted to buy it, largely because the only access was by way of an alley off of V Street NW. In 1976, a neighborhood organization, V Street Block Club, approached the Chesapeake & Potomac Telephone Company to donate the property. The neighborhood organization asked the Chesapeake & Potomac Telephone Company to use the warehouse to teach children to play music in the warehouse. Chesapeake & Potomac Telephone Company said it would prefer to donate the property to the government of the District of Columbia, which would then donate the property to the neighborhood organization. The District government declined the offer, because it did not have the funds to renovate the building, and nothing happened for a few months. In December 1976, Hyman Construction Company learned about the issue, and it agreed to renovate the warehouse, Chesapeake & Potomac Telephone Company agreed to donate the land and the warehouse to a newly incorporated neighborhood organization, then called NUV-1, an acronym for each street that surrounds the property.
Hyman Construction Company paid its employees to renovate the warehouse, and employees of a few other construction companies donated their time as well. National Capital United Presbytery donated $7,500, and architect Ward Bucher donated his time to create the plans. Renovation began in July 1977, and the building officially opened as a neighborhood arts center on April 2, 1978.
The neighborhood arts center offered photography, martial arts, and bicycle-repair classes, lectures, musical events, dances, and day-care. In 1987, the District government reduced funding through the Recreation Department, and the six of the center's eight staff members were let go, significantly reducing the activities at the center.
The neighborhood organization became the Crispus Attucks Development Corporation, a 501(c)(3) nonprofit organization.
The park is named after Crispus Attucks, an African American who was killed in the Boston Massacre and is often regarded as the first person killed in the American Revolution. Crispus Attucks Park is privately owned and open to the public. It is maintained through charitable donations and volunteer labor coordinated by the Crispus Attucks Development Corporation.


Although the series House of Cards was filmed in Baltimore, its  opening credits sequence features several prominent shots of the Bloomingdale neighborhood along North Capitol Street, between R Street and T Street.


The square was developed for the 4th Earl of Southampton in the early 1660s and was initially known as Southampton Square. It was one of the earliest London squares. The Earl's own house, then known as Southampton House and later as Bedford House after the square and the rest of the Bloomsbury Estate passed by marriage from the Earls of Southampton to the Dukes of Bedford, occupied the whole of the north side of the square, where Bedford Place is now located. The other sides were lined with typical terraced houses of the time, which were initially occupied by members of the aristocracy and gentry.
On 9 April 1694 Bloomsbury Square was the setting for an infamous duel. The then 23-year-old Scottish economist and financier John Law fought Edward 'Beau' Wilson, killing him with a single pass and thrust of his sword. Law would be convicted of murder and sentenced to death, but would escape his condemned cell and go on to become the founder of the Mississippi Company and the de facto prime minister of France.
By the early 19th century, Bloomsbury was no longer fashionable with the upper classes. Consequently, the Duke of Bedford of the day moved out of Bedford House, which was demolished and replaced with further terraced houses. In the 19th century the square was occupied mainly by middle class professionals. The writer Isaac D'Israeli lived at No. 6 from 1817 to 1829 and for part of that time his son, the future Prime Minister Benjamin Disraeli lived with him. In the 20th century most of the buildings came to be used as offices.
Bloomsbury Square's garden contains a bronze statue by Richard Westmacott of Charles James Fox, who was a Whig associate of the Dukes of Bedford.  None of the original 17th-century buildings survive, but there are many handsome 18th- and early 19th-century houses. The Royal Pharmaceutical Society of Great Britain was based in an 18th-century building on the southern side of the square partly credited to John Nash. The eastern side of the square is occupied by a large early 20th-century office building called Victoria House, built for, and for many decades occupied by, Liverpool Victoria Friendly Society. The garden is open to the public and was refurbished in 2003.
The garden is Grade II listed on the Register of Historic Parks and Gardens.


The castle was built between two arms of the River Würm for Duke Albert III, Duke of Bavaria in 1438–39 as a hunting-lodge, replacing an older castle burned down in war. The origin of this castle is a moated castle of the 13th century. The core of this castle was a residential tower, the remains of which were uncovered in 1981. The fortress was first mentioned in writing only in 1432.
Albert's son, Duke Sigismund of Bavaria, ordered extensions of the castle beginning in 1488 and later died here in 1501. The main building became derelict during the Thirty Years War, but was rebuilt in 1680–81. The castle is still surrounded by a ring wall with three towers and a gate tower. The defensive character of the castle, however, was with the reconstruction in 17th century significantly reduced. The plant was already at that time no longer defensible.


The walls of the chapel are focused according to the sides of the world. Entablature creates the external appearance of the walls, which revolves around them, breaking down in accordance with their relief.
The southern side is closed with a residential house, which is attached to the chapel. It was built in the 19th century.
The eastern wall is divided by five pilasters and decorated with two mural portraits of Georgy Boim and his wife, Jadwiga. The portraits were created in 1617, by Jan Gianni.
The northern wall is also divided by pilasters. Two fresco images are located there: the Virgin and Jesus Christ. A bas-relief of Saint George (the name saint of Georgy Boim) fighting the dragon is situated on the wall of the octagonal tambour.


An eight-storey watchtower, 58 metres (190 ft) high, dominates the complex. The buildings are grouped around it in the form of a horseshoe, and the castle is enhanced by a number of towers, and among other things, bastions, battlements, oriel windows and loopholes. The two long bridges, ending with a short drawbridge, span the deep dry moat around the castle. The knights' hall, armoury, which is in one of the few original rooms with preserved Gothic vaulting, bedrooms of the knights and a neo-gothic chapel with its Gothic altar and tombs occupy the central part of the castle. The valuable furniture comes from the private collection of Eugen von Habsburg and the collection of the Order of the Teutonic Knights. Since 1999 the castle has been a national monument.


As the size of the congregation grew, a new synagogue was built, designed by the architectural firm of Edelman and Barnett.  The original wood structure was moved to the back of the lot to make room for the new brick structure which opened in 1923.  The new synagogue was built from unreinforced masonry with veneer brick and cast stone embellishments on the facade.  The façade includes alternating bands of dichromatic brickwork, "dense prickly foliage carving", other organic motifs, and Stars of David in bas-relief cast stone detail.


In 1988, the building was designated as a City of Los Angeles Historic-Cultural Monument. The building fell into disrepair in the 1990s, and the City of Los Angeles foreclosed on the property after recording an assessment for barricading and protection. In 1998, Hillary Clinton visited the Shul as part of her Save America's Treasures campaign. In July 2000, the City quitclaimed the property to Breed Street Shul Project, Inc., a subsidiary of the Jewish Historical Society of Southern California.  The organization plans to rehabilitate the buildings as a county museum, educational and cultural center.  It was listed on the National Register of Historic Places in 2001.


Bricktown is an entertainment district just east of downtown Oklahoma City, Oklahoma, United States. It was formerly a major warehouse district. The major attractions of the district are the Chickasaw Bricktown Ballpark, the navigable Bricktown Canal, and the 16-screen Harkins movie theatre.


Bricktown Entertainment District includes some 50 square city blocks bounded between the Oklahoma River on the south, I-235 on the east, Deep Deuce District to the North, and the Oklahoma City Central Business District to the West. The general boundary of the Bricktown Core Development District (also known as Upper Bricktown) is as follows: An area bordered generally by the BNSF Railway; Reno Avenue; Centennial Expressway; and the railroad right-of-way between Main and NE 1st.
The district is administered by the Bricktown Urban Design Committee which was established by the City of Oklahoma City to oversee modifications to the buildings and new construction within the district. Downtown Oklahoma City Inc. (an arm of the Greater Oklahoma City Chamber of Commerce) is charged with maintenance and operations of the district and oversees promotion alongside the Oklahoma City Tourism and Visitors Bureau. All entities are united with the ultimate goal of preserving Bricktown's historic 'warehouse district' flavor while allowing modern entertainment, commercial, retail, and residential development to flourish.


Four railroad companies had freight operations east of the Santa Fe tracks in what is now Bricktown in the late 19th and early 20th century. The first brick structures, which were typically only one or two stories, appeared between 1898 and 1903. Larger brick buildings were constructed between 1903 and 1911, and the tallest brick buildings were built between 1911 and 1930. Working-class houses were built nearby.
Oklahoma City's first black newspaper, the Black Dispatch, was located in Bricktown at 228 E. First; it reported on the struggle to end racially segregated housing in the city. Also in that area was the first local chapter of the National Association for the Advancement of Colored People (NAACP), founded in the early 20th century to work for the civil rights of African Americans.
The decline of the area began with the onset of the Great Depression, which diminished businesses in the area. The growth of eastern suburbs and subsidized highways during and after World War II attracted many residents to newer housing. Railroads restructured and freight traffic moved to trucks and highways. By 1980, Bricktown had become a cluster of abandoned buildings.
In the 1990s, mayor Ron Norick persuaded Oklahoma City residents to approve a series of tax incentives to lure new businesses, but these were not sufficient. A visit to Indianapolis, Indiana, which had recently beat the city in a competition for a new airline maintenance plant, led him to believe that Oklahoma City needed a vibrant downtown. It lacked the range of activities and amenities to attract more residents and visitors. Along with Greater Oklahoma City Chamber President Ray Ackerman, Norick and their staffs developed the Metropolitan Area Projects or MAPS, which approval led to the construction of the Bricktown ballpark and a tree-lined, mile-long canal through the district, as well as other projects in downtown. The ballpark opened in 1998 and the canal opened in July 1999. Water taxis carry visitors to different stops along the canal, including many restaurants, shops and nightclubs.


The district contains a number of public sculptures and murals, including a monument to the Oklahoma Land Run. The Centennial Land Run Monument, a large bronze sculpture by artist Paul Moore, is at the south end of Bricktown Canal. It commemorates the Land Run of 1889, which marked the opening of the Unassigned Lands area to settlement. This area is now a city park, open 24 hours a day, year round, and there is no admission fee.
An annual Bricktown Art Festival is held in mid-July.


The Brighton Palace Pier, commonly known as Brighton Pier or the Palace Pier, is a Grade II* listed pleasure pier in Brighton, England, located in the city centre opposite the Old Steine. Established in 1899, it was the third pier to be constructed in Brighton after the Royal Suspension Chain Pier and the West Pier, but is now the only one still in operation. It is managed and operated by the Eclectic Bar Group.
The Palace Pier was intended as a replacement for the Chain Pier, which collapsed in 1896 during construction of the new pier. It quickly became popular, and had become a frequently-visited theatre and entertainment venue by 1911. Aside from closures owing to war, it continued to hold regular entertainment up to the 1970s. The theatre was damaged in 1973 and following a buy-out was demolished in 1986, changing the pier's character from seaside entertainment to an amusement park, with various fairground rides and roller coasters.
The pier remains popular with the public, with over four million visitors in 2016, and has been featured in many works of British culture, including the gangster thriller Brighton Rock, the comedy Carry On at Your Convenience and the Who's concept album and film Quadrophenia.


The pier was listed at Grade II* on 20 August 1971. As of February 2001, it was one of 70 Grade II*-listed buildings and structures, and 1,218 listed buildings of all grades, in the city of Brighton and Hove.
During a storm in 1973, a 70-long-ton (71 t) barge moored at the pier's landing stage broke loose and began to damage the pier head, particularly the theatre. Despite fears that the pier would be destroyed, the storm eased and the barge was removed. The landing pier was demolished in 1975, and the damaged theatre was never used again, despite protests from the Theatres Trust.
The pier was sold to the Noble Organisation in 1984. The theatre was removed two years later, on the understanding that it would be replaced; however a domed amusement arcade was put in place instead. Consequently, the seaward end of the pier was filled with fairground rides, including thrill rides, children's rides and roller coasters. Entertainment continued to be popular at the pier; the Spice Girls made an early live performance there in 1996 and returned the following year after achieving commercial success.
On 13 August 1994, a bomb planted by the IRA near the pier was defused by a controlled explosion. A similar bomb by the same perpetrators had exploded in Bognor Regis on the same day. The bombing was intended to mark the 25th anniversary of the start of The Troubles. The pier was closed for several days owing to police investigation.


The pier was renamed as "Brighton Pier" in 2000, although this legal change was not recognised by the National Piers Society nor some residents of Brighton and Hove. The local newspaper, The Argus, continued to refer to the structure as the Palace Pier.
The Palace Pier caught fire on 4 February 2003 but damage was limited and most of the pier was able to reopen the next day. Police suspected arson.
In 2004, the Brighton Marine Palace Pier Company (owned by the Noble Organisation), admitted an offence of breaching public safety under the Health and Safety at Work Act and had to pay fines and costs of £37,000 after a fairground ride was operated with part of its track missing. A representative from the Health and Safety Executive said that inadequate procedures were to blame for the fact that nothing had been done to alert staff or passengers that the ride would be dangerous to use. The pier management came into criticism from Brighton and Hove City Council, who thought they were relying too much on fairground rides, some of which were being built too high.
In 2011, the Noble Organisation put the pier for sale, with an expected price of £30 million. It was rumoured that the council wanted to buy the pier, but this was quickly ruled out. It was taken off the market the following year, due to lack of interest in suitable buyers. In 2016, it was sold to the Eclectic Bar Group, headed by former PizzaExpress owner Luke Johnson, who renamed the pier back to Brighton Palace Pier in July.
The Palace Pier remains a popular tourist attraction into the 21st century, particularly with day visitors to the city. In contrast to the redevelopment and liberal culture in Brighton generally, it has retained a traditional down-market "bucket and spade" seaside atmosphere. In 2016, the Brighton Fringe festival director Julian Caddy criticised the pier as "a massive public relations problem".


Following the 2010–2013 redevelopment, City Hall's role is primarily to support public gatherings, although it was the major Brisbane venue for classical concerts and arts events for decades, hosting such singers as Richard Tauber and Peter Dawson. In addition to the main auditorium, reception rooms that had been converted to administration spaces over the years have been restored to their original purpose. An industrial kitchen installed in the basement during the renovations provides catering support for events; previously external caterers had to be used, however now City Hall is managed on behalf of Brisbane City Council by EPICURE. Functions, concerts and events can still be hosted by contacting EPICURE.
The Museum of Brisbane is now relocated into a purpose-built facility on the rooftop. In addition to a changing program of exhibitions, the museum also operates tours of the building and tours of the clock tower.
There are two privately operated cafes in City Hall, the Red Cross Cafe and the Shingle Inn. The Shingle Inn cafe was originally not part of City Hall but was located in Edward Street and was demolished as part of the Queen's Plaza development. However, the iconic interior fittings of the Shingle Inn Cafe were removed and put into storage, allowing it to be reconstructed within the City Hall.
The only administrative functions remaining in the city hall are the Council Chambers (located on second floor of the Adelaide Street side of the building) and the Lord Mayor's and Deputy Lord Mayor's offices.


During the evening of 23 May 1970, the bridge was heavily damaged when boys playing inside the structure dropped a burning torch, setting alight the tar-coated wooden roof of the tubes. Despite the best efforts of the Caernarfonshire and Anglesey fire brigades, the bridge's height, construction, and the lack of an adequate water supply meant they were unable to control the fire, which spread all the way across from the mainland to the Anglesey side. After the fire had burned itself out, the bridge was still standing. However, the structural integrity of the iron tubes had been critically compromised by the intense heat; they had visibly split open at the three towers and had begun to sag. It was recognised that there was still danger of the structure collapsing. As a consequence, the bridge was rendered unusable without the enactment of major restorative work.
In light of events, the chief civil engineer of British Railways' London Midland region, W.F. Beatty, sought structural advice from consulting engineering company Husband & Co. Following an in-depth investigation of the site performed by the company, it was determined that the cast iron beams inside the towers had suffered substantial cracking and tilting, meaning that the tubes required immediate support at all three towers. The Royal Engineers were quickly brought in to save the bridge, rapidly deploying vertical Bailey bridge units to fill the original jacking slots in the masonry towers. By the end of July 1970, a total of eight Bailey bridge steel towers had been erected, each being capable of bearing a vertical load of around 200 tonnes.
Further analysis showed that the wrought iron tubes had been too badly damaged to be retained. In light of this discovery, it was decided to dismantle the tubes in favour of replacing them with a new deck at the same level as the original tracks. With the exception of the original stone substructure, the structure was completely rebuilt by Cleveland Bridge & Engineering Company. The superstructure of the new bridge was to include two decks: a lower rail deck supported by steel arches and an upper deck constructed out of reinforced concrete, to carry a new road crossing over the strait. Concrete supports were built under the approach spans and steel archways constructed under the long spans on either side of the central Britannia Tower. The two long spans are supported by arches, which had not been an option for the original structure as a result of the clearance needed for tall-masted vessels; modern navigational requirements require much less headroom.
The bridge was rebuilt in stages. The first stage was to erect the new steel arches under the two original wrought-iron tubes. The arches were completed, and single-line working was restored to the railway on 30 January 1972 by reusing one of the tubes. The next stage was to dismantle and remove the other tube and replace it with a concrete deck for the other rail track. Then the single-line working was transferred to the new track (on the west side); this allowed the other tube to be removed and replaced with a concrete deck (which is used only for service access) by 1974. Finally the upper road deck was installed and by July 1980, over 10 years after the fire, the new road crossing was completed, and formally opened by the Prince of Wales, carrying a single-carriageway section of the A5 road (now the A55).
During 2011, national railway infrastructure owner Network Rail, the Welsh Assembly Government and the English Highways Agency undertook a £4 million joint programme to strengthen the 160-year-old structure and improve its reliability. The work involved the replacement of eroded steelwork, repairs to the drainage system, restoration of the parapets and stonework, and the painting of the steel approach portals of the bridge. The programme included a detailed inspection of the internal chambers of the three towers and the construction of a special walkway to enable easier and safer access to the structure for future inspections of the masonry piers; special protective efforts adopted for the work included the use of special pollution-minimising paint and the decontamination of all equipment before being brought onsite.


The developer for the site was British Land. In February 2005 Broadgate Plaza Ltd, a subsidiary of British Land, submitted a planning application to the City of London for the construction of two buildings of 33 stories and 13 stories. Broadgate Tower, which was designed by Skidmore, Owings & Merrill and built by Bovis Lend Lease, was completed in 2008. It was constructed at the same time as the neighbouring building, 201 Bishopsgate, and the two are separated by a covered pedestrian area.
The building was used in the James Bond Skyfall movie to represent a Shanghai skyscraper.


The Nuu-chah-nulth (pronounced [nuːʧanˀuɬ]), are indigenous peoples in Canada. Their traditional home is on the west coast of Vancouver Island. In pre-contact and early post-contact times, the number of nations was much greater, but as in the rest of the region, smallpox and other consequences of contact resulted in the disappearance of some groups, and the absorption of others into neighbouring groups.
They were among the first Pacific peoples north of California to come into contact with Europeans, as the Spanish, Americans and British attempted to secure control of Pacific Northwest and the trade in otter pelts, with Nootka Sound becoming a focus of these rivalries. The Nuu-chah-nulth speak a Southern Wakashan language and are closely related to the Makah of the Olympic Peninsula, Washington state and the Ditidaht.


Acacias in Australia probably evolved their fire resistance about 20 million years ago when fossilised charcoal deposits show a large increase, indicating that fire was a factor even then. With no major mountain ranges or rivers to prevent their spread, the wattles began to spread all over the continent as it dried and fires became more common. They began to form dry, open forests with species of the genera Allocasuarina, Eucalyptus and Callitris (cypress-pines).
The southernmost species in the genus are Acacia dealbata (silver wattle), Acacia longifolia (coast wattle or Sydney golden wattle), Acacia mearnsii (black wattle), and Acacia melanoxylon (blackwood), reaching 43°30' S in Tasmania, Australia.


The Albanian Renaissance was a period with its roots in the late 18th century and continuing into the 19th century, during which the Albanian people gathered spiritual and intellectual strength for an independent cultural and political life within an independent nation. Modern Albanian culture flourished too, especially Albanian literature and arts, and was frequently linked to the influences of the Romanticism and Enlightenment principles.
Prior to the rise of nationalism, Albania was under the rule of the Ottoman Empire for almost five centuries, and Ottoman authorities suppressed any expression of national unity or conscience by the Albanian people. Through literature, Albanians started to make a conscious effort to awaken feelings of pride and unity among their people that would call to mind the rich history and hopes for a more decent future.
The victory of Russia over the Ottoman Empire following the Russian-Ottoman Wars resulted the execution of the Treaty of San Stefano which overlooked to assign Albanian-populated lands to the Slavic and Greek neighbours. However, the United Kingdom and Austro-Hungarian Empire consequently blocked the arrangement and caused the Treaty of Berlin. From this point, Albanians started to organise themselves with the goal to protect and unite the Albanian-populated lands into a unitary nation, leading to the formation of the League of Prizren.
The league had initially the assistance of the Ottoman authorities whose position was based on the religious solidarity of Muslim people and landlords connected with the Ottoman administration. They favoured and protected the Muslim solidarity and called for defence of Muslim lands simultaneously constituting the reason for titling the league Committee of the Real Muslims.
Approximately 300 Muslims participated in the assembly composed by delegates from Bosnia, the administrator of the Sanjak of Prizren as representatives of the central authorities and no delegates from Vilayet of Scutari. Signed by only 47 Muslim deputies, the league issued the Kararname that contained a proclamation that the people from northern Albania, Epirus and Bosnia and Herzegovina are willing to defend the territorial integrity of the Ottoman Empire by all possible means against the troops of Bulgaria, Serbia and Montenegro.
Ottomans authorities cancelled their assistance when the league, under Abdyl Frashëri, became focused on working towards Albanian autonomy and requested merging four vilayets, including Kosovo, Shkodër, Monastir and Ioannina, into an unified vilayet, the Albanian Vilayet. The league used military force to prevent the annexing areas of Plav and Gusinje assigned to Montenegro. After several successful battles with Montenegrin troops, such as the Battle of Novšiće, the league was forced to retreat from their contested regions. The league was later defeated by the Ottoman army sent by the sultan.


The word "habitat" has been in use since about 1755 and derives from the Latin habitāre, to inhabit, from habēre, to have or to hold. Habitat can be defined as the natural environment of an organism, the type of place in which it is natural for it to live and grow. It is similar in meaning to a biotope; an area of uniform environmental conditions associated with a particular community of plants and animals.


A cultivar is a type of plant that people have bred for desired traits, which are reproduced in each new generation by a method such as grafting, tissue culture, or carefully controlled seed production. Most cultivars arise from purposeful human manipulation, but some originate from wild plants that have distinctive characteristics. Cultivar names are chosen according to rules of the International Code of Nomenclature for Cultivated Plants (ICNCP), and not all cultivated plants qualify as cultivars. Horticulturists generally believe the word cultivar was coined as a term meaning "cultivated variety".
Popular ornamental plants like roses, camellias, daffodils, rhododendrons, and azaleas are commonly cultivars produced by breeding and selection or as sports, for floral colour or size, plant form, or other desirable characteristics. Similarly, the world's agricultural food crops are almost exclusively cultivars that have been selected for characters such as improved yield, flavour, and resistance to disease, and very few wild plants are now used as food sources. Trees used in forestry are also special selections grown for their enhanced quality and yield of timber.
Cultivars form a major part of Liberty Hyde Bailey's broader group, the cultigen, which is defined as a plant whose origin or selection is primarily due to intentional human activity. A cultivar is not the same as a botanical variety, which is a taxonomic rank below subspecies, and there are differences in the rules for creating and using the names of botanical varieties and cultivars.  In recent times, the naming of cultivars has been complicated by the use of statutory patents for plants and recognition of plant breeders' rights.
The International Union for the Protection of New Varieties of Plants (UPOV – French: Union internationale pour la protection des obtentions végétales) offers legal protection of plant cultivars to persons or organisations that introduce new cultivars to commerce. UPOV requires that a cultivar be "distinct, uniform", and "stable". To be "distinct", it must have characters that easily distinguish it from any other known cultivar. To be "uniform" and "stable", the cultivar must retain these characters in repeated propagation.
The naming of cultivars is an important aspect of cultivated plant taxonomy, and the correct naming of a cultivar is prescribed by the Rules and Recommendations of the International Code of Nomenclature for Cultivated Plants (ICNCP, commonly denominated the Cultivated Plant Code). A cultivar is given a cultivar name, which consists of the scientific Latin botanical name followed by a cultivar epithet. The cultivar epithet is usually in a vernacular language.


The default color of vertebrate eggs is the white of the calcium carbonate from which the shells are made, but some birds, mainly passerines, produce colored eggs. The pigment biliverdin and its zinc chelate give a green or blue ground color, and protoporphyrin produces reds and browns as a ground color or as spotting.
Non-passerines typically have white eggs, except in some ground-nesting groups such as the Charadriiformes, sandgrouse and nightjars, where camouflage is necessary, and some parasitic cuckoos which have to match the passerine host's egg. Most passerines, in contrast, lay colored eggs, even if there is no need of cryptic colors.
However some have suggested that the protoporphyrin markings on passerine eggs actually act to reduce brittleness by acting as a solid-state lubricant. If there is insufficient calcium available in the local soil, the egg shell may be thin, especially in a circle around the broad end. Protoporphyrin speckling compensates for this, and increases inversely to the amount of calcium in the soil.
For the same reason, later eggs in a clutch are more spotted than early ones as the female's store of calcium is depleted.
The color of individual eggs is also genetically influenced, and appears to be inherited through the mother only, suggesting that the gene responsible for pigmentation is on the sex-determining W chromosome (female birds are WZ, males ZZ).
It used to be thought that color was applied to the shell immediately before laying, but subsequent research shows that coloration is an integral part of the development of the shell, with the same protein responsible for depositing calcium carbonate, or protoporphyrins when there is a lack of that mineral.
In species such as the common guillemot, which nest in large groups, each female's eggs have very different markings, making it easier for females to identify their own eggs on the crowded cliff ledges on which they breed.


A lichen consists of a simple photosynthesizing organism, usually a green alga or cyanobacterium, surrounded by filaments of a fungus. Generally, most of a lichen's bulk is made of interwoven fungal filaments, but this is reversed in filamentous and gelatinous lichens. The fungus is called a mycobiont. The photosynthesizing organism is called a photobiont. Algal photobionts are called phycobionts. Cyanobacteria photobionts are called cyanobionts.
The part of a lichen that is not involved in reproduction, the "body" or "vegetative tissue" of a lichen, is called the thallus. The thallus form is very different from any form where the fungus or alga are growing separately. The thallus is made up of filaments of the fungus called hyphae. The filaments grow by branching then rejoining to create a mesh, which is called being "anastomosed". The mesh of fungal filaments may be dense or loose.
Generally, the fungal mesh surrounds the algal or cyanobacterial cells, often enclosing them within complex fungal tissues that are unique to lichen associations. The thallus may or may not have a protective "skin" of densely packed fungal filaments, often containing a second fungal species, which is called a cortex. Fruticose lichens have one cortex layer wrapping around the "branches". Foliose lichens have an upper cortex on the top side of the "leaf", and a separate lower cortex on the bottom side. Crustose and squamulose lichens have only an upper cortex, with the "inside" of the lichen in direct contact with the surface they grow on (the substrate). Even if the edges peel up from the substrate and appear flat and leaf-like, they lack a lower cortex, unlike foliose lichens. Filamentous, byssoid, leprose, gelatinous, and other lichens do not have a cortex, which is called being ecorticate.
Fruticose, foliose, crustose, and squamulose lichens generally have up to three different types of tissue, differentiated by having different densities of fungal filaments. The top layer, where the lichen contacts the environment, is called a cortex. The cortex is made of densely tightly woven, packed, and glued together (agglutinated) fungal filaments. The dense packing makes the cortex act like a protective "skin", keeping other organisms out, and reducing the intensity of sunlight on the layers below. The cortex layer can be up to several hundred micrometers (μm) in thickness (less than a millimeter). The cortex may be further topped by an epicortex of secretions, not cells, 0.6–1 μm thick in some lichens. This secretion layer may or may not have pores.
Below the cortex layer is a layer called the photobiontic layer or symbiont layer. The symbiont layer has less densely packed fungal filaments, with the photosynthetic partner embedded in them. The less dense packing allows air circulation during photosynthesis, similar to the anatomy of a leaf. Each cell or group of cells of the photobiont is usually individually wrapped by hyphae, and in some cases penetrated by a haustorium. In crustose and foliose lichens, algae in the photobiontic layer are diffuse among the fungal filaments, decreasing in gradation into the layer below. In fruticose lichens, the photobiontic layer is sharply distinct from the layer below.
The layer beneath the symbiont layer called is called the medulla. The medulla is less densely packed with fungal filaments than the layers above. In foliose lichens, there is usually, as in Peltigera, another densely packed layer of fungal filaments called the lower cortex. Root-like fungal structures called rhizines (usually) grow from the lower cortex to attach or anchor the lichen to the substrate. Fruticose lichens have a single cortex wrapping all the way around the "stems" and "branches". The medulla is the lowest layer, and may form a cottony white inner core for the branchlike thallus, or it may be hollow. Crustose and squamulose lichens lack a lower cortex, and the medulla is in direct contact with the substrate that the lichen grows on.
In crustose areolate lichens, the edges of the areolas peel up from the substrate and appear leafy. In squamulose lichens the part of the lichen thallus that is not attached to the substrate may also appear leafy. But these leafy parts lack a lower cortex, which distinguishes crustose and squamulose lichens from foliose lichens. Conversely, foliose lichens may appear flattened against the substrate like a crustose lichen, but most of the leaf-like lobes can be lifted up from the substrate because it is separated from it by a tightly packed lower cortex.
Gelatinous, byssoid, and leprose lichens lack a cortex (are ecorticate), and generally have only undifferentiated tissue, similar to only having a symbiont layer.
In lichens that include both green algal and cyanobacterial symbionts, the cyanobacteria may be held on the upper or lower surface in small pustules called cephalodia.
Pruinia is a whitish coating on top of an upper surface. An epinecral layer is "a layer of horny dead fungal hyphae with indistinct lumina in or near the cortex above the algal layer".
In August 2016, it was reported that some macrolichens have more than one species of fungus in their tissues.


Mexican liberals were concerned that the Roman Catholic Church retained too much power in the post-independence period and sought to undermine it by mandating the secularization of missions in 1833. In the aftermath of the Mexican American War (1846–1848) and the Treaty of Guadalupe Hidalgo, the United States gained sovereignty over territory previously held first by New Spain and then Mexico, most of which was sparsely settled. Alta California was incorporated into the U.S., and during the California Gold Rush, quickly gained enough population to be admitted to the union as a state. Baja California remained under Mexican control. In 1853, soldier of fortune (mercenary) William Walker captured La Paz, declaring himself president of the Republic of Baja California. The Mexican government forced his retreat after several months.


Oregon is 295 miles (475 km) north to south at longest distance, and 395 miles (636 km) east to west. With an area of 98,381 square miles (254,810 km²), Oregon is slightly larger than the United Kingdom. It is the ninth largest state in the United States. Oregon's highest point is the summit of Mount Hood, at 11,249 feet (3,429 m), and its lowest point is the sea level of the Pacific Ocean along the Oregon Coast. Oregon's mean elevation is 3,300 feet (1,006 m). Crater Lake National Park, the state's only national park, is the site of the deepest lake in the United States at 1,943 feet (592 m). Oregon claims the D River as the shortest river in the world, though the state of Montana makes the same claim of its Roe River. Oregon is also home to Mill Ends Park (in Portland), the smallest park in the world at 452 square inches (0.29 m²).
Oregon is split into eight geographical regions. In Western Oregon: Oregon Coast (west of the Coast Range), the Willamette Valley, Rogue Valley, Cascade Range and Klamath Mountains; and in Central and Eastern Oregon: the Columbia Plateau, the High Desert, and the Blue Mountains.
Oregon lies in two time zones. Most of Malheur County is in the Mountain Time Zone, while the rest of the state lies in the Pacific Time Zone.


In 1874, the Brooks-Baxter War, a political struggle between factions of the Republican Party shook Little Rock and the state governorship. It was settled only when President Ulysses S. Grant ordered Joseph Brooks to disperse his militant supporters.
Following the Brooks-Baxter War, a new state constitution was ratified, re-enfranchising former Confederates.
In 1881, the Arkansas state legislature enacted a bill that adopted an official pronunciation of the state's name, to combat a controversy then simmering. (See Law and Government below.)
After Reconstruction, the state began to receive more immigrants and migrants. Chinese, Italian, and Syrian men were recruited for farm labor in the developing Delta region. None of these nationalities stayed long at farm labor; the Chinese especially quickly became small merchants in towns around the Delta. Many Chinese became such successful merchants in small towns that they were able to educate their children at college.
Construction of railroads enabled more farmers to get their products to market. It also brought new development into different parts of the state, including the Ozarks, where some areas were developed as resorts. In a few years at the end of the 19th century, for instance, Eureka Springs in Carroll County grew to 10,000 people, rapidly becoming a tourist destination and the fourth-largest city of the state. It featured newly constructed, elegant resort hotels and spas planned around its natural springs, considered to have healthful properties. The town's attractions included horse racing and other entertainment. It appealed to a wide variety of classes, becoming almost as popular as Hot Springs.


In 1500, King Manuel I of Portugal sent Gaspar Corte-Real to Greenland in search of a Northwest Passage to Asia which, according to the Treaty of Tordesillas, was part of Portugal's sphere of influence. In 1501, Corte-Real returned with his brother, Miguel Corte-Real. Finding the sea frozen, they headed south and arrived in Labrador and Newfoundland. Upon the brothers' return to Portugal, the cartographic information supplied by Corte-Real was incorporated into a new map of the world which was presented to Ercole I d'Este, Duke of Ferrara, by Alberto Cantino in 1502. The Cantino planisphere, made in Lisbon, accurately depicts the southern coastline of Greenland.
In 1605–1607, King Christian IV of Denmark sent a series of expeditions to Greenland and Arctic waterways to locate the lost eastern Norse settlement and assert Danish sovereignty over Greenland. The expeditions were mostly unsuccessful, partly due to leaders who lacked experience with the difficult Arctic ice and weather conditions, and partly because the expedition leaders were given instructions to search for the Eastern Settlement on the east coast of Greenland just north of Cape Farewell, which is almost inaccessible due to southward drifting ice. The pilot on all three trips was English explorer James Hall.
After the Norse settlements died off, Greenland came under the de facto control of various Inuit groups, but the Danish government never forgot or relinquished the claims to Greenland that it had inherited from the Norse. When it re-established contact with Greenland in the early 17th century, Denmark asserted its sovereignty over the island. In 1721, a joint mercantile and clerical expedition led by Danish-Norwegian missionary Hans Egede was sent to Greenland, not knowing whether a Norse civilization remained there. This expedition is part of the Dano-Norwegian colonization of the Americas. After 15 years in Greenland, Hans Egede left his son Paul Egede in charge of the mission there and returned to Denmark, where he established a Greenland Seminary. This new colony was centred at Godthåb ("Good Hope") on the southwest coast. Gradually, Greenland was opened up to Danish merchants, but closed to those from other countries.


Mitteleuropa may refer to an historical concept, or to a contemporary German definition of Central Europe. As an historical concept, the German term Mitteleuropa (or alternatively its literal translation into English, Middle Europe) is an ambiguous German concept. It is sometimes used in English to refer to an area somewhat larger than most conceptions of 'Central Europe'; it refers to territories under Germanic cultural hegemony until World War I (encompassing Austria–Hungary and Germany in their pre-war formations but usually excluding the Baltic countries north of East Prussia). According to Fritz Fischer Mitteleuropa was a scheme in the era of the Reich of 1871–1918 by which the old imperial elites had allegedly sought to build a system of German economic, military and political domination from the northern seas to the Near East and from the Low Countries through the steppes of Russia to the Caucasus.  Later on, professor Fritz Epstein argued the threat of a Slavic "Drang nach Westen" (Western expansion) had been a major factor in the emergence of a Mitteleuropa ideology before the Reich of 1871 ever came into being.
In Germany the connotation was also sometimes linked to the pre-war German provinces east of the Oder-Neisse line.
The term "Mitteleuropa" conjures up negative historical associations among some elderly people, although the Germans have not played an exclusively negative role in the region. Most Central European Jews embraced the enlightened German humanistic culture of the 19th century. German-speaking Jews from turn of the 20th century Vienna, Budapest and Prague became representatives of what many consider to be Central European culture at its best, though the Nazi version of "Mitteleuropa" destroyed this kind of culture instead. However, the term "Mitteleuropa" is now widely used again in German education and media without negative meaning, especially since the end of communism. In fact, many people from the new states of Germany do not identify themselves as being part of Western Europe and therefore prefer the term "Mitteleuropa".


In botanical terminology, a berry is a simple fruit with seeds and pulp produced from the ovary of a single flower. It is fleshy throughout, except for the seeds. It does not have a special "line of weakness" along which it splits to release the seeds when ripe (i.e. it is indehiscent). A berry may develop from an ovary with one or more carpels (the female reproductive structures of a flower). The seeds are usually embedded in the fleshy interior of the ovary, but there are some non-fleshy examples such as peppers, with air rather than pulp around their seeds. The differences between the everyday and botanical uses of "berry" results in three categories: those fruits that are berries under both definitions; those fruits that are botanical berries but not commonly known as berries; and those parts of plants commonly known as berries that are not botanical berries, and may not even be fruits.
Berries under both definitions include blueberries, cranberries, lingonberries, and the fruits of many other members of the heather family, as well as gooseberries, goji berries and elderberries. The fruits of some "currants" (Ribes species), such as blackcurrants, red currants and white currants, are botanical berries, and are treated as horticultural berries (or as soft fruit in the UK), even though their most commonly used names do not include the word "berry".
Botanical berries not commonly known as berries include bananas, tomatoes, grapes, eggplants (aubergines), persimmons, watermelons, and pumpkins.
There are several different kinds of fruits which are commonly called berries, but are not botanical berries. Blackberries, raspberries, and strawberries are kinds of aggregate fruit; they contain seeds from different ovaries of a single flower. In aggregate fruits like blackberries, the individual "fruitlets" making up the fruit can be clearly seen. The fruits of blackthorn may be called "sloe berries", but botanically are small stone fruits or drupes, like plums or apricots. Junipers and yews are commonly said to have berries, but these differ from botanical berries and are instead highly modified seed-bearing cones. In juniper berries, used to flavour gin, the cone scales, which are hard and woody in most conifers, are instead soft and fleshy when ripe. The bright red berries of yews consist of a fleshy outgrowth (aril) almost enclosing the poisonous seed.


Berries have been valuable as a food source for humans since before the start of agriculture, and remain among the primary food sources of other primates. They were a seasonal staple for early hunter-gatherers for thousands of years, and wild berry gathering remains a popular activity in Europe and North America today. In time, humans learned to store berries so that they could be used in the winter. They may be made into fruit preserves, and among Native Americans, mixed with meat and fats as pemmican.
Berries also began to be cultivated in Europe and other countries. Some species of blackberries and raspberries of the genus Rubus have been cultivated since the 17th century, while smooth-skinned blueberries and cranberries of the genus Vaccinium have been cultivated in the United States for over a century. In Japan, between the 10th and 18th centuries, the term ichibigo ichigo referred to many berry crops. The most widely cultivated berry of modern times, however, is the strawberry, which is produced globally at twice the amount of all other berry crops combined.
The strawberry was mentioned by ancient Romans, who thought it had medicinal properties, but it was then not a staple of agriculture. Woodland strawberries began to be grown in French gardens in the 14th century. The musk strawberry (F. moschata), also known as the hautbois strawberry, began to be grown in European gardens in the late 16th century. Later, the Virginia strawberry was grown in Europe and the United States. The most commonly consumed strawberry, the garden strawberry (F. ananassa), is an accidental hybrid of the Virginia strawberry and a Chilean variety Fragaria chiloensis. It was first noted by a French gardener around the mid 18th century that, when F. moschata and F. virginiana were planted in between rows of F. chiloensis, the Chilean strawberry would bear abundant and unusually large fruits. Soon after, Antoine Nicolas Duchesne began to study the breeding of strawberries and made several discoveries crucial to the science of plant breeding, such as the sexual reproduction of strawberry. Later, in the early 1800s, English breeders of strawberry made varieties of F. ananassa which were important in strawberry breeding in Europe, and hundreds of cultivars have since been produced through the breeding of strawberries.


In 1939, Nazi Germany and the Soviet Union invaded and occupied Poland, marking the beginning of World War II. The Soviets invaded and annexed much of eastern Poland, which had been part of the country since the Peace of Riga two decades earlier. Much of the northern section of this area was added to the Byelorussian SSR, and now constitutes West Belarus. The Soviet-controlled Byelorussian People's Council officially took control of the territories, whose populations consisted of a mixture of Poles, Ukrainians, Belarusians and Jews, on 28 October 1939 in Białystok. Nazi Germany invaded the Soviet Union in 1941. The defense of Brest Fortress was the first major battle of Operation Barbarossa.
The Byelorussian SSR was the hardest-hit Soviet republic in World War II; it remained in Nazi hands until 1944. The German Generalplan Ost called for the extermination, expulsion, or enslavement of most or all Belarusians for the purpose of providing more living space in the East for Germans. Most of Western Belarus became part of the Reichskommissariat Ostland in 1941, but in 1943 the German authorities allowed local collaborators to set up a client state, the Belarusian Central Council.
The German occupation in 1941–1944 and war on the Eastern Front devastated Belarus. During that time, 209 out of 290 towns and cities were destroyed, 85% of the republic's industry, and more than one million buildings. After the war, it was estimated that 2.2 million local inhabitants had died and of those some 810,000 were combatants—some foreign. This figure represented a staggering quarter of the prewar population. In the 1990s some raised the estimate even higher, to 2.7 million. The Jewish population of Belarus was devastated during the Holocaust and never recovered. The population of Belarus did not regain its pre-war level until 1971.


At 825,615 km² (318,772 sq mi), Namibia is the world's thirty-fourth largest country (after Venezuela). It lies mostly between latitudes 17° and 29°S (a small area is north of 17°), and longitudes 11° and 26°E.
Being situated between the Namib and the Kalahari deserts, Namibia has the least rainfall of any country in sub-Saharan Africa.
The Namibian landscape consists generally of five geographical areas, each with characteristic abiotic conditions and vegetation, with some variation within and overlap between them: the Central Plateau, the Namib, the Great Escarpment, the Bushveld, and the Kalahari Desert.
The Central Plateau runs from north to south, bordered by the Skeleton Coast to the northwest, the Namib Desert and its coastal plains to the southwest, the Orange River to the south, and the Kalahari Desert to the east. The Central Plateau is home to the highest point in Namibia at Königstein elevation 2,606 metres (8,550 ft).
The Namib is a broad expanse of hyper-arid gravel plains and dunes that stretches along Namibia's entire coastline. It varies between 100 and 200 kilometres (60 and 120 mi) in width. Areas within the Namib include the Skeleton Coast and the Kaokoveld in the north and the extensive Namib Sand Sea along the central coast.
The Great Escarpment swiftly rises to over 2,000 metres (7,000 ft). Average temperatures and temperature ranges increase further inland from the cold Atlantic waters, while the lingering coastal fogs slowly diminish. Although the area is rocky with poorly developed soils, it is significantly more productive than the Namib Desert. As summer winds are forced over the Escarpment, moisture is extracted as precipitation.
The Bushveld is found in north-eastern Namibia along the Angolan border and in the Caprivi Strip. The area receives a significantly greater amount of precipitation than the rest of the country, averaging around 400 mm (16 in) per year. The area is generally flat and the soils sandy, limiting their ability to retain water and support agriculture.
The Kalahari Desert, an arid region that extends into South Africa and Botswana, is one of Namibia's well-known geographical features. The Kalahari, while popularly known as a desert, has a variety of localised environments, including some verdant and technically non-desert areas. The Succulent Karoo is home to over 5,000 species of plants, nearly half of them endemic; approximately 10 percent of the world's succulents are found in the Karoo. The reason behind this high productivity and endemism may be the relatively stable nature of precipitation.
Namibia's Coastal Desert is one of the oldest deserts in the world. Its sand dunes, created by the strong onshore winds, are the highest in the world. Because of the location of the shoreline, at the point where the Atlantic's cold water reaches Africa's hot climate, often extremely dense fog forms along the coast. Near the coast there are areas where the dune-hummocks are vegetated. Namibia has rich coastal and marine resources that remain largely unexplored.