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Untitled is the title of the debut album from UK R&B / soul singer Terri Walker. The album was released in 2003 by Def Soul/Mercury Records and spawned 3 singles, "Guess You Didn't Love Me" (Featuring Mos Def), "Ching Ching (Lovin' You Still)" (her first and only UK top 40 hit to date) and "Drawing Board" (promo only). The album was nominated for a MOBO award and it was also nominated for the Mercury Music Prize for album of the year. (Full article...)

Untitled is the title of the debut album from UK R&B / soul singer Terri Walker. The album was released in 2003 by Def Soul/Mercury Records and spawned 3 singles, "Guess You Didn't Love Me" (Featuring Mos Def), "Ching Ching (Lovin' You Still)" (her first and only UK top 40 hit to date) and "Drawing Board" (promo only). The album was nominated for a MOBO award and it was also nominated for the Mercury Music Prize for album of the year. (Full article...)

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Pedra da Gávea is a mountain in Tijuca Forest, Rio de Janeiro, Brazil. Differential weathering on one side of the rock has created what is described as a stylized human face, and weathered markings on another face of the rock have been described as an inscription. Some individuals, such as Bernardo de Azevedo da Silva Ramos, have advanced the position that the inscription is of Phoenician origin and possibly proof of pre-Columbian contact from Old World cultures. Alternative theories proposed include that the rock was the site of a Norse colony or that it is connected with suspected UFO activity. Mainstream geologists and scientists are in agreement that the "inscription" is the result of erosion and that the "face" is a product of pareidolia. No credible evidence has ever been collected that backs up the idea that Pedra da Gávea was discovered by Phoenicians or any other civilization. Furthermore, the consensus of archaeologists and scholars in Brazil is that the mountain should not be viewed as an archaeological site, and hypotheses that regard it as such are fringe theories. (Full article...)

Pedra da Gávea is a mountain in Tijuca Forest, Rio de Janeiro, Brazil. Differential weathering on one side of the rock has created what is described as a stylized human face, and weathered markings on another face of the rock have been described as an inscription. Some individuals, such as Bernardo de Azevedo da Silva Ramos, have advanced the position that the inscription is of Phoenician origin and possibly proof of pre-Columbian contact from Old World cultures. Alternative theories proposed include that the rock was the site of a Norse colony or that it is connected with suspected UFO activity. Mainstream geologists and scientists are in agreement that the "inscription" is the result of erosion and that the "face" is a product of pareidolia. No credible evidence has ever been collected that backs up the idea that Pedra da Gávea was discovered by Phoenicians or any other civilization. Furthermore, the consensus of archaeologists and scholars in Brazil is that the mountain should not be viewed as an archaeological site, and hypotheses that regard it as such are fringe theories. (Full article...)

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Ralph Merrifield (22 August 1913 – 9 January 1995) was an English museum curator and archaeologist. Described as "the father of London's modern archaeology", Merrifield was a specialist in the archaeology of both Roman London and magical practices, publishing six books on these subjects over the course of his life. Merrifield began his career in 1930 as an assistant at Brighton Museum. In 1935 he gained an external degree in anthropology from the University of London. During the Second World War he served in the Royal Air Force. In 1950 he became assistant keeper of the Guildhall Museum in London. In 1956 he relocated to Accra to oversee the opening of the new National Museum of Ghana, before returning to work at the Guildhall Museum. He produced a synthesis of known material on the archaeology of Roman London, published as The Roman City of London in 1965. He was appointed senior keeper of the new Museum of London on its establishment in 1976, and soon after was promoted to deputy director. He retired in 1978 but remained active, lecturing, and publishing The Archaeology of Ritual and Magic (1987) and further studies of Roman London. He was a keen supporter of the Standing Conference on London Archaeology, a body designed to monitor the impact that English Heritage was having on the city's archaeology, which he believed to be negative. (Full article...)

Ralph Merrifield (22 August 1913 – 9 January 1995) was an English museum curator and archaeologist. Described as "the father of London's modern archaeology", Merrifield was a specialist in the archaeology of both Roman London and magical practices, publishing six books on these subjects over the course of his life. Merrifield began his career in 1930 as an assistant at Brighton Museum. In 1935 he gained an external degree in anthropology from the University of London. During the Second World War he served in the Royal Air Force. In 1950 he became assistant keeper of the Guildhall Museum in London. In 1956 he relocated to Accra to oversee the opening of the new National Museum of Ghana, before returning to work at the Guildhall Museum. He produced a synthesis of known material on the archaeology of Roman London, published as The Roman City of London in 1965. He was appointed senior keeper of the new Museum of London on its establishment in 1976, and soon after was promoted to deputy director. He retired in 1978 but remained active, lecturing, and publishing The Archaeology of Ritual and Magic (1987) and further studies of Roman London. He was a keen supporter of the Standing Conference on London Archaeology, a body designed to monitor the impact that English Heritage was having on the city's archaeology, which he believed to be negative. (Full article...)

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Spyridon Marinatos (Greek: Σπυρίδων Μαρινάτος; 17 November [O.S. 4 November] 1901 – 1 October 1974) was a Greek archaeologist who specialised in the Minoan and Mycenaean civilizations of the Aegean Bronze Age. He is best known for the excavation of the Minoan site of Akrotiri on Thera, which he conducted between 1967 and 1974. He received many honours in Greece and abroad, and was considered one of the most important Greek archaeologists of his day. A native of Kephallonia, Marinatos was educated at the University of Athens, the Friedrich Wilhelms University of Berlin, and the University of Halle. His early teachers included noted archaeologists such as Panagiotis Kavvadias, Christos Tsountas and Georg Karo. He joined the Greek Archaeological Service in 1919, and spent much of his early career on the island of Crete, where he excavated several Minoan sites, served as director of the Heraklion Museum, and formulated his theory that the collapse of Neopalatial Minoan society had been the result of the eruption of the volcanic island of Thera around 1600 BCE. In the 1940s and 1950s, Marinatos surveyed and excavated widely in the region of Messenia in south-west Greece, collaborating with Carl Blegen, who was engaged in the simultaneous excavation of the Palace of Nestor at Pylos. He also discovered the battlefield of Thermopylae and excavated the Mycenaean cemeteries at Tsepi and Vranas near Marathon in Attica. Marinatos was head of the Greek Archaeological Service from 1937 to 1939, from 1955 to 1958, and lastly from 1967 to 1974, under the Greek military junta. He was an enthusiastic supporter of the junta; in the late 1930s, he had been close to the quasi-fascist dictatorship of Ioannis Metaxas, under whom he initiated legislation to restrict the roles of women in Greek archaeology. His leadership of the Archaeological Service has been criticised for its cronyism and for promoting the pursuit of grand discoveries at the expense of good scholarship. Marinatos died while excavating at Akrotiri in 1974, and is buried at the site. (Full article...)

The Roman temple of Bziza is a well-preserved first century AD building dedicated to Azizos, a personification of the morning star in ancient Arab polytheism. This Roman temple lends the modern Lebanese town of Bziza its current name, as Bziza is a corruption of Beth Azizo meaning the house or temple of Azizos. Azizos was identified as Ares by Emperor Julian. The tetrastyle prostyle building has two doors that connect the pronaos to a square cella. To the back of the temple lie the remains of the adyton where images of the deity once stood. The ancient temple functioned as an aedes, the dwelling place of the deity. The temple of Bziza was converted into a church and underwent architectural modification during two phases of Christianization; in the Early Byzantine period and later in the Middle Ages. The church, colloquially known until modern times as the Lady of the Pillars, fell into disrepair. Despite the church's condition, Christian devotion was still maintained in the nineteenth century in one of the temple's niches. The temple of Bziza is featured on multiple stamps issued by the Lebanese state. (Full article...)

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Perth receives moderate, though highly seasonal, winter-based rainfall. Summers are generally hot, sunny and dry, lasting from December to March, with February generally the hottest month. Winters are relatively mild and wet, giving Perth a hot-summer Mediterranean climate (Köppen climate classification Csa). Perth has an average of 8.8 hours of sunshine per day, which equates to around 3,200 hours of sunshine and 138.7 clear days annually, making it Australia's sunniest capital city. Summers are typically hot and dry but not completely devoid of rain, with sporadic rainfall in the form of short-lived thunderstorms, weak cold fronts and on occasions decaying tropical cyclones from Western Australia's north-west, which can bring heavy rain. Temperatures above 35 °C (95 °F) occur, on average, 26 days per year and rise above 40 °C (104 °F) on 5 days per year. The highest temperature recorded in Perth was 46.2 °C (115.2 °F) on 23 February 1991, although Perth Airport recorded 46.7 °C (116.1 °F) on the same day. On most summer afternoons a sea breeze, known locally as the Fremantle Doctor, blows from the south-west, providing relief from the hot north-easterly winds. Temperatures often fall below 30 °C (86 °F) a few hours after the arrival of the wind change. In the summer, the 3 p.m. dewpoint averages at around 12 °C (54 °F). Winters are mild and wet, with most of Perth's annual rainfall between May and September. Winters see significant rainfall as frontal systems move across the region, interspersed with clear and sunny days where minimum temperatures tend to drop below 5 °C (41 °F). The lowest temperature recorded in Perth was −0.7 °C (30.7 °F) on 17 June 2006. The lowest temperature within the Perth metropolitan area was −3.4 °C (25.9 °F) on the same day at Jandakot Airport, although temperatures at or below zero are rare occurrences. The lowest maximum temperature recorded in Perth is 8.8 °C (47.8 °F) on 26 June 1956. It occasionally gets cold enough for frost to form. While snow has never been recorded in the Perth CBD, light snowfalls have been reported in outer suburbs of Perth in the Perth Hills around Kalamunda, Roleystone and Mundaring. The most recent snowfall was in 1968. The rainfall pattern has changed in Perth and south-west Western Australia since the mid-1970s. A significant reduction in winter rainfall has been observed with a greater number of extreme rainfall events in the summer, such as the slow-moving storms on 8 February 1992 that brought 120.6 millimetres (4.75 in) of rain, heavy rainfall associated with a tropical low on 10 February 2017, which brought 114.4 millimetres (4.50 in) of rain, and the remnants of ex-Tropical Cyclone Joyce on 15 January 2018 with 96.2 millimetres (3.79 in). Perth was also hit by a severe thunderstorm on 22 March 2010, which brought 40.2 mm (1.58 in) of rain, and large hail and caused significant damage in the metropolitan area. The average sea temperature ranges from 18.9 °C (66.0 °F) in October to 23.4 °C (74.1 °F) in March. (Full article...)

Perth receives moderate, though highly seasonal, winter-based rainfall. Summers are generally hot, sunny and dry, lasting from December to March, with February generally the hottest month. Winters are relatively mild and wet, giving Perth a hot-summer Mediterranean climate (Köppen climate classification Csa). Perth has an average of 8.8 hours of sunshine per day, which equates to around 3,200 hours of sunshine and 138.7 clear days annually, making it Australia's sunniest capital city. Summers are typically hot and dry but not completely devoid of rain, with sporadic rainfall in the form of short-lived thunderstorms, weak cold fronts and on occasions decaying tropical cyclones from Western Australia's north-west, which can bring heavy rain. Temperatures above 35 °C (95 °F) occur, on average, 26 days per year and rise above 40 °C (104 °F) on 5 days per year. The highest temperature recorded in Perth was 46.2 °C (115.2 °F) on 23 February 1991, although Perth Airport recorded 46.7 °C (116.1 °F) on the same day. On most summer afternoons a sea breeze, known locally as the Fremantle Doctor, blows from the south-west, providing relief from the hot north-easterly winds. Temperatures often fall below 30 °C (86 °F) a few hours after the arrival of the wind change. In the summer, the 3 p.m. dewpoint averages at around 12 °C (54 °F). Winters are mild and wet, with most of Perth's annual rainfall between May and September. Winters see significant rainfall as frontal systems move across the region, interspersed with clear and sunny days where minimum temperatures tend to drop below 5 °C (41 °F). The lowest temperature recorded in Perth was −0.7 °C (30.7 °F) on 17 June 2006. The lowest temperature within the Perth metropolitan area was −3.4 °C (25.9 °F) on the same day at Jandakot Airport, although temperatures at or below zero are rare occurrences. The lowest maximum temperature recorded in Perth is 8.8 °C (47.8 °F) on 26 June 1956. It occasionally gets cold enough for frost to form. While snow has never been recorded in the Perth CBD, light snowfalls have been reported in outer suburbs of Perth in the Perth Hills around Kalamunda, Roleystone and Mundaring. The most recent snowfall was in 1968. The rainfall pattern has changed in Perth and south-west Western Australia since the mid-1970s. A significant reduction in winter rainfall has been observed with a greater number of extreme rainfall events in the summer, such as the slow-moving storms on 8 February 1992 that brought 120.6 millimetres (4.75 in) of rain, heavy rainfall associated with a tropical low on 10 February 2017, which brought 114.4 millimetres (4.50 in) of rain, and the remnants of ex-Tropical Cyclone Joyce on 15 January 2018 with 96.2 millimetres (3.79 in). Perth was also hit by a severe thunderstorm on 22 March 2010, which brought 40.2 mm (1.58 in) of rain, and large hail and caused significant damage in the metropolitan area. The average sea temperature ranges from 18.9 °C (66.0 °F) in October to 23.4 °C (74.1 °F) in March. (Full article...)

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