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| Untitled #93 is a color photograph created by Cindy Sherman in 1981. It is part of her Centerfolds series of 12 photographs made for the Artforum magazine. They were never published there but went to be exhibited publicly the same year, to critical acclaim. (Full article...) | Untitled #93 is a color photograph created by Cindy Sherman in 1981. It is part of her Centerfolds series of 12 photographs made for the Artforum magazine. They were never published there but went to be exhibited publicly the same year, to critical acclaim. (Full article...) |
Basic
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| Nico Ditch is a six-mile (9.7 km) long linear earthwork between Ashton-under-Lyne and Stretford in Greater Manchester, England. It was dug as a defensive fortification, or possibly a boundary marker, between the 5th and 11th century. The ditch is still visible in short sections, such as a 330-yard (300 m) stretch in Denton Golf Course. For the parts which survived, the ditch is 4–5 yards (3.7–4.6 m) wide and up to 5 feet (1.5 m) deep. Part of the earthwork is protected as a Scheduled Ancient Monument. (Full article...) | Nico Ditch is a six-mile (9.7 km) long linear earthwork between Ashton-under-Lyne and Stretford in Greater Manchester, England. It was dug as a defensive fortification, or possibly a boundary marker, between the 5th and 11th century. The ditch is still visible in short sections, such as a 330-yard (300 m) stretch in Denton Golf Course. For the parts which survived, the ditch is 4–5 yards (3.7–4.6 m) wide and up to 5 feet (1.5 m) deep. Part of the earthwork is protected as a Scheduled Ancient Monument. (Full article...) |
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The Church of St John of the Collachium was a medieval church built by the Knights Hospitaller in Rhodes, capital of the island of the same name. It was built in the first half of the fourteenth century and dedicated to the order's patron, John the Baptist. It was the conventual church of the Hospitallers, immediately adjacent to the Palace of the Grand Master, and presided over by the order's most senior religious official. It was used for religious services and processions, meetings of the order's chapter general, and for the elections and funerals of its grand masters. Architecturally, the church was in the Gothic style, 48–50 metres (157–164 ft) long and 15–18 m (49–59 ft) wide. It was expanded in several phases, adding underground areas and a total of eight annexes, including several chapels. At least six Hospitaller grand masters were buried in the church, including Fabrizio del Carretto, whose elaborate funerary slab was placed in its central part. The church became famous for its collection of relics, which included objects associated with John the Baptist, Jesus, the Virgin Mary, and various other saints. After the Ottoman conquest of Rhodes in 1522, the church became the town's main mosque. The building was damaged by two earthquakes in the nineteenth century, and destroyed on 6 November 1856 by a lightning strike which ignited gunpowder stored in its cellars, killing at least 200 people. In modern times, only small parts of the northern and eastern foundations remain, and the site has been built over with a school. Archaeological investigations of the site took place in 1932 and 1934 under Pietro Lojacono, in 1988, and under Anna-Maria Kasdagli in 1995. (Full article...) |
The Church of St John of the Collachium was a medieval church built by the Knights Hospitaller in Rhodes, capital of the island of the same name. It was built in the first half of the fourteenth century and dedicated to the order's patron, John the Baptist. It was the conventual church of the Hospitallers, immediately adjacent to the Palace of the Grand Master, and presided over by the order's most senior religious official. It was used for religious services and processions, meetings of the order's chapter general, and for the elections and funerals of its grand masters. Architecturally, the church was in the Gothic style, 48–50 metres (157–164 ft) long and 15–18 m (49–59 ft) wide. It was expanded in several phases, adding underground areas and a total of eight annexes, including several chapels. At least six Hospitaller grand masters were buried in the church, including Fabrizio del Carretto, whose elaborate funerary slab was placed in its central part. The church became famous for its collection of relics, which included objects associated with John the Baptist, Jesus, the Virgin Mary, and various other saints. After the Ottoman conquest of Rhodes in 1522, the church became the town's main mosque. The building was damaged by two earthquakes in the nineteenth century, and destroyed on 6 November 1856 by a lightning strike which ignited gunpowder stored in its cellars, killing at least 200 people. In modern times, only small parts of the northern and eastern foundations remain, and the site has been built over with a school. Archaeological investigations of the site took place in 1932 and 1934 under Pietro Lojacono, in 1988, and under Anna-Maria Kasdagli in 1995. (Full article...) |
Subsection
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Fort Dobbs was an 18th-century fort in the Yadkin–Pee Dee River Basin region of the Province of North Carolina, near what is now Statesville in Iredell County. Used for frontier defense during and after the French and Indian War, the fort was built to protect the American settlers of the western frontier of North Carolina, and served as a vital outpost for soldiers. Fort Dobbs' primary structure was a blockhouse with log walls, surrounded by a shallow ditch, and by 1759, a palisade. It was intended to provide protection from French-allied Native Americans such as the Shawnee raids into western North Carolina. The fort's name honored Arthur Dobbs, the Royal Governor of North Carolina from 1755 to 1765, who played a role in designing the fort and authorized its construction. Between 1756 and 1761, the fort was garrisoned by a variable number of soldiers, many of whom were sent to fight in Pennsylvania and the Ohio River Valley during the French and Indian War. On February 27, 1760, the fort was the site of an engagement between Cherokee warriors and Provincial soldiers that ended in a victory for the Provincials. Fort Dobbs was abandoned in March, 1761, and disappeared from the landscape. Archaeology and historical research led to the discovery of the fort's exact location and probable appearance. The site on which the fort sat is now operated by North Carolina's Division of State Historic Sites and Properties as Fort Dobbs State Historic Site. The reconstruction of the fort was completed on September 21, 2019. (Full article...) |
Fort Dobbs was an 18th-century fort in the Yadkin–Pee Dee River Basin region of the Province of North Carolina, near what is now Statesville in Iredell County. Used for frontier defense during and after the French and Indian War, the fort was built to protect the American settlers of the western frontier of North Carolina, and served as a vital outpost for soldiers. Fort Dobbs' primary structure was a blockhouse with log walls, surrounded by a shallow ditch, and by 1759, a palisade. It was intended to provide protection from French-allied Native Americans such as the Shawnee raids into western North Carolina. The fort's name honored Arthur Dobbs, the Royal Governor of North Carolina from 1755 to 1765, who played a role in designing the fort and authorized its construction. Between 1756 and 1761, the fort was garrisoned by a variable number of soldiers, many of whom were sent to fight in Pennsylvania and the Ohio River Valley during the French and Indian War. On February 27, 1760, the fort was the site of an engagement between Cherokee warriors and Provincial soldiers that ended in a victory for the Provincials. Fort Dobbs was abandoned in March, 1761, and disappeared from the landscape. Archaeology and historical research led to the discovery of the fort's exact location and probable appearance. The site on which the fort sat is now operated by North Carolina's Division of State Historic Sites and Properties as Fort Dobbs State Historic Site. The reconstruction of the fort was completed on September 21, 2019. (Full article...) |
List with sections
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Melbourne has a temperate oceanic climate (Köppen climate classification Cfb), with warm summers and cool winters. Melbourne is well known for its changeable weather conditions, mainly due to it being located on the boundary of hot inland areas and the cool southern ocean. This temperature differential is most pronounced in the spring and summer months and can cause strong cold fronts to form. These cold fronts can be responsible for varied forms of severe weather from gales to thunderstorms and hail, large temperature drops and heavy rain. Winters, while exceptionally dry by southern Victorian standards, are often cloudy. The lack of winter rainfall is because of Melbourne's rain shadowed location between the Otway and Macedon Ranges, which block much of the rainfall arriving from the north and west. Port Phillip is often warmer than the surrounding oceans or the land mass, particularly in spring and autumn; this can set up a "bay effect rain", where showers are intensified leeward of the bay. Relatively narrow streams of heavy showers can often affect the same places (usually the eastern suburbs) for an extended period, while the rest of Melbourne and surrounds stays dry. Overall, the area around Melbourne is, owing to its rain shadow, nonetheless significantly drier than average for southern Victoria. Within the city and surrounds, rainfall varies widely, from about 425 millimetres (16.7 in) at Little River to 1,250 millimetres (49 in) on the eastern fringe at Gembrook. Melbourne receives 48.6 clear days annually. Dewpoint temperatures in the summer range from 9.5 to 11.7 °C (49.1 to 53.1 °F). Melbourne rarely receives widespread or continuous rainfall (as experienced in other Australian cities, such as Sydney or Brisbane) and instead experiences precipitation through fleeting showers that can vary in intensity, Melbourne is particularly prone to these isolated convective showers forming when a cold pool crosses the state, especially if there is considerable daytime heating. These showers are often heavy and can include hail, squalls, and significant drops in temperature, but they often pass through very quickly with a rapid clearing trend to sunny and relatively calm weather and the temperature rising back to what it was before the shower. This can occur in the space of minutes and can be repeated many times a day, giving Melbourne a reputation for having "four seasons in one day", a phrase that is part of local popular culture. The lowest temperature on record is −2.8 °C (27.0 °F), on 21 July 1869. The highest temperature recorded in Melbourne city was 46.4 °C (115.5 °F), on 7 February 2009. While snow is occasionally seen at higher elevations in the outskirts of the city, and dustings were observed in 2020, it has not been recorded in the central business district since 1986. The sea temperature in Melbourne is warmer than the surrounding ocean during the summer months, and colder during the winter months. This is predominantly due to Port Phillip Bay being an enclosed and shallow bay that is largely protected from the ocean, resulting in greater temperature variation across seasons. (Full article...) |
Melbourne has a temperate oceanic climate (Köppen climate classification Cfb), with warm summers and cool winters. Melbourne is well known for its changeable weather conditions, mainly due to it being located on the boundary of hot inland areas and the cool southern ocean. This temperature differential is most pronounced in the spring and summer months and can cause strong cold fronts to form. These cold fronts can be responsible for varied forms of severe weather from gales to thunderstorms and hail, large temperature drops and heavy rain. Winters, while exceptionally dry by southern Victorian standards, are often cloudy. The lack of winter rainfall is because of Melbourne's rain shadowed location between the Otway and Macedon Ranges, which block much of the rainfall arriving from the north and west. Port Phillip is often warmer than the surrounding oceans or the land mass, particularly in spring and autumn; this can set up a "bay effect rain", where showers are intensified leeward of the bay. Relatively narrow streams of heavy showers can often affect the same places (usually the eastern suburbs) for an extended period, while the rest of Melbourne and surrounds stays dry. Overall, the area around Melbourne is, owing to its rain shadow, nonetheless significantly drier than average for southern Victoria. Within the city and surrounds, rainfall varies widely, from about 425 millimetres (16.7 in) at Little River to 1,250 millimetres (49 in) on the eastern fringe at Gembrook. Melbourne receives 48.6 clear days annually. Dewpoint temperatures in the summer range from 9.5 to 11.7 °C (49.1 to 53.1 °F). Melbourne rarely receives widespread or continuous rainfall (as experienced in other Australian cities, such as Sydney or Brisbane) and instead experiences precipitation through fleeting showers that can vary in intensity, Melbourne is particularly prone to these isolated convective showers forming when a cold pool crosses the state, especially if there is considerable daytime heating. These showers are often heavy and can include hail, squalls, and significant drops in temperature, but they often pass through very quickly with a rapid clearing trend to sunny and relatively calm weather and the temperature rising back to what it was before the shower. This can occur in the space of minutes and can be repeated many times a day, giving Melbourne a reputation for having "four seasons in one day", a phrase that is part of local popular culture. The lowest temperature on record is −2.8 °C (27.0 °F), on 21 July 1869. The highest temperature recorded in Melbourne city was 46.4 °C (115.5 °F), on 7 February 2009. While snow is occasionally seen at higher elevations in the outskirts of the city, and dustings were observed in 2020, it has not been recorded in the central business district since 1986. The sea temperature in Melbourne is warmer than the surrounding ocean during the summer months, and colder during the winter months. This is predominantly due to Port Phillip Bay being an enclosed and shallow bay that is largely protected from the ocean, resulting in greater temperature variation across seasons. (Full article...) |
References
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