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Leslie Valentine Grinsell OBE FSA (14 February 1907 – 28 February 1995) was an English archaeologist and museum curator. Publishing over twenty books on archaeology during his lifetime, he was renowned as a specialist on the prehistoric barrows of southern England. Born in London and raised largely in Brighton, Grinsell developed an early interest in archaeology through visits to Brighton Museum. Later working as a bank clerk in London, he embarked on archaeological research in an amateur capacity, visiting prehistoric barrows during his weekends and holidays to record their shape, dimensions, and location. On the basis of his research, he published a range of academic articles and books on barrows during the 1930s, gaining recognition as Britain's foremost expert on the subject. In 1933, he carried out his only archaeological excavation, at the Devil's Humps in Sussex. During the Second World War he joined the Royal Air Force and served in Egypt, where he acquainted himself with the archaeological remains of Ancient Egyptian society; after the war he published a book on the Egyptian pyramids. On his return to Britain, Grinsell became the treasurer of the Prehistoric Society, a position that he held from 1947 till 1970. Moving to Devizes, in 1949 he entered the archaeological profession as an assistant to Christopher Hawkes and Stuart Piggott at the Victoria County History project. From 1952 to 1972, Grinsell worked as Keeper of Anthropology and Archaeology at Bristol City Museum, during which time he continued his examination of barrows, focusing on those in south-west England. On retirement, he was appointed to the Order of the British Empire and a festschrift was published in his honour. Over the course of his lifetime, Grinsell examined and catalogued around 10,000 barrows and advanced the archaeological understanding of such monuments. His use of non-excavatory fieldwork influenced much British archaeology in the latter part of his 20th century, while his willingness to pay attention to other sources of information, such as folklore and place-names, has been deemed ahead of its time. (Full article...) |
Leslie Valentine Grinsell OBE FSA (14 February 1907 – 28 February 1995) was an English archaeologist and museum curator. Publishing over twenty books on archaeology during his lifetime, he was renowned as a specialist on the prehistoric barrows of southern England. Born in London and raised largely in Brighton, Grinsell developed an early interest in archaeology through visits to Brighton Museum. Later working as a bank clerk in London, he embarked on archaeological research in an amateur capacity, visiting prehistoric barrows during his weekends and holidays to record their shape, dimensions, and location. On the basis of his research, he published a range of academic articles and books on barrows during the 1930s, gaining recognition as Britain's foremost expert on the subject. In 1933, he carried out his only archaeological excavation, at the Devil's Humps in Sussex. During the Second World War he joined the Royal Air Force and served in Egypt, where he acquainted himself with the archaeological remains of Ancient Egyptian society; after the war he published a book on the Egyptian pyramids. On his return to Britain, Grinsell became the treasurer of the Prehistoric Society, a position that he held from 1947 till 1970. Moving to Devizes, in 1949 he entered the archaeological profession as an assistant to Christopher Hawkes and Stuart Piggott at the Victoria County History project. From 1952 to 1972, Grinsell worked as Keeper of Anthropology and Archaeology at Bristol City Museum, during which time he continued his examination of barrows, focusing on those in south-west England. On retirement, he was appointed to the Order of the British Empire and a festschrift was published in his honour. Over the course of his lifetime, Grinsell examined and catalogued around 10,000 barrows and advanced the archaeological understanding of such monuments. His use of non-excavatory fieldwork influenced much British archaeology in the latter part of his 20th century, while his willingness to pay attention to other sources of information, such as folklore and place-names, has been deemed ahead of its time. (Full article...) |
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| Potbelly sculptures (Spanish barrigones pl. or barrigón sing.) are in-the-round sculptures of obese human figures carved from boulders. They are a distinctive element of the sculptural tradition in the southern Maya area of Mesoamerica. The precise purpose of potbelly sculptures is unknown, although they appear to have been the focus of public veneration and ritual directed by the ruling elite. Although this sculptural tradition is found within the southern Maya area, it has been recognized that the sculptures themselves are non-Maya. (Full article...) | Potbelly sculptures (Spanish barrigones pl. or barrigón sing.) are in-the-round sculptures of obese human figures carved from boulders. They are a distinctive element of the sculptural tradition in the southern Maya area of Mesoamerica. The precise purpose of potbelly sculptures is unknown, although they appear to have been the focus of public veneration and ritual directed by the ruling elite. Although this sculptural tradition is found within the southern Maya area, it has been recognized that the sculptures themselves are non-Maya. (Full article...) |
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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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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 northwest, 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 southwest, providing relief from the hot northeasterly 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 southwest 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 northwest, 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 southwest, providing relief from the hot northeasterly 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 southwest 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...) |
References
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