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The Aineta aryballos is an Ancient Greek aryballos, made in Corinth between approximately 625 and 570 BCE. Approximately 6.35 centimetres (2.50 in) in both height and diameter, it was intended to contain perfumed oil, and is likely to have been owned by a high-class courtesan (hetaira) by the name of Aineta, who may be portrayed in a drawing on its handle. The vase's illegal sale to the British Museum in 1865 led to the prosecution of its seller, the Athenian art dealer Athanasios Rhousopoulos, and exposed the latter's widespread involvement in antiquities crime. The vase is inscribed with a portrait, generally agreed to be that of a woman and probably that of Aineta, who is named in the inscription upon the vase. Below the portrait are the names of several men, generally taken to be Aineta's admirers or lovers. It is likely to have been found in a grave, probably that of Aineta herself. According to Rhousopoulos, it was discovered in Corinth around 1852. In 1877, Panagiotis Efstratiadis, the Ephor General of Antiquities in charge of the Greek Archaeological Service, had Rhousopoulos fined for selling the vase in contravention of Greek law. The case has been called "a milestone in the trafficking of Greek antiquities", in that it represented a relatively rare successful use of state power against the illegal trade in Ancient Greek artefacts. (Full article...) |
The Aineta aryballos is an Ancient Greek aryballos, made in Corinth between approximately 625 and 570 BCE. Approximately 6.35 centimetres (2.50 in) in both height and diameter, it was intended to contain perfumed oil, and is likely to have been owned by a high-class courtesan (hetaira) by the name of Aineta, who may be portrayed in a drawing on its handle. The vase's illegal sale to the British Museum in 1865 led to the prosecution of its seller, the Athenian art dealer Athanasios Rhousopoulos, and exposed the latter's widespread involvement in antiquities crime. The vase is inscribed with a portrait, generally agreed to be that of a woman and probably that of Aineta, who is named in the inscription upon the vase. Below the portrait are the names of several men, generally taken to be Aineta's admirers or lovers. It is likely to have been found in a grave, probably that of Aineta herself. According to Rhousopoulos, it was discovered in Corinth around 1852. In 1877, Panagiotis Efstratiadis, the Ephor General of Antiquities in charge of the Greek Archaeological Service, had Rhousopoulos fined for selling the vase in contravention of Greek law. The case has been called "a milestone in the trafficking of Greek antiquities", in that it represented a relatively rare successful use of state power against the illegal trade in Ancient Greek artefacts. (Full article...) |
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Georg Heinrich Karo (11 January 1872 – 12 November 1963) was a German archaeologist, known for his research into the Mycenaean and Etruscan cultures. He was twice director of the German Archaeological Institute at Athens (DAI), in which capacity he excavated the Mycenaean site of Tiryns and the Temple of Artemis on Corfu. A colleague of Wilhelm Dörpfeld, who had worked with Heinrich Schliemann at Troy, Karo published the findings from Schliemann's excavations of Grave Circle A at Mycenae, a work considered his greatest contribution to scholarship. Initially educated in philology, Karo became interested in archaeology as a student of Georg Loeschcke at the University of Bonn. Following his receipt of his doctorate from Bonn in 1896, Karo travelled widely in the Mediterranean region, developing interests in Minoan civilisation, the Etruscans and on ancient biblical commentaries. He taught briefly at Bonn between 1902 and 1905, before moving to the DAI in Athens as Dörpfeld's deputy. Known for his urbane manner and fluency in several languages, he became well connected in the international circles of Greek archaeology, and maintained the favour of both the Greek and the German royal families. His outspoken German nationalism led to his dismissal from the DAI in 1916: he spent some time in the Ottoman Empire, where he worked to conserve cultural heritage and was linked with various efforts to appropriate ancient artefacts and bring them to Germany. Karo's views made him unpopular with the Entente-backed government that ruled in Greece after the First World War, and he took an academic post at the University of Halle, which he held until 1930. That year, he returned to Athens as director of the DAI. Although an early supporter of the Nazi government of Germany, Karo was forced from his post in 1936 by antisemitism against his Jewish ancestry. In 1939, he fled to the United States, supported by American associates including Carl Blegen and Bert Hodge Hill, and obtained a series of visiting professorships at the University of Cincinnati, Oberlin College and Claremont Colleges. However, he was also accused of collaborating with the Nazi regime: though no evidence for this allegation was proven, he was denied US citizenship and listed as an "Enemy Alien". He returned to Germany in 1952, and became an honorary professor at the University of Freiburg. (Full article...) |
Georg Heinrich Karo (11 January 1872 – 12 November 1963) was a German archaeologist, known for his research into the Mycenaean and Etruscan cultures. He was twice director of the German Archaeological Institute at Athens (DAI), in which capacity he excavated the Mycenaean site of Tiryns and the Temple of Artemis on Corfu. A colleague of Wilhelm Dörpfeld, who had worked with Heinrich Schliemann at Troy, Karo published the findings from Schliemann's excavations of Grave Circle A at Mycenae, a work considered his greatest contribution to scholarship. Initially educated in philology, Karo became interested in archaeology as a student of Georg Loeschcke at the University of Bonn. Following his receipt of his doctorate from Bonn in 1896, Karo travelled widely in the Mediterranean region, developing interests in Minoan civilisation, the Etruscans and on ancient biblical commentaries. He taught briefly at Bonn between 1902 and 1905, before moving to the DAI in Athens as Dörpfeld's deputy. Known for his urbane manner and fluency in several languages, he became well connected in the international circles of Greek archaeology, and maintained the favour of both the Greek and the German royal families. His outspoken German nationalism led to his dismissal from the DAI in 1916: he spent some time in the Ottoman Empire, where he worked to conserve cultural heritage and was linked with various efforts to appropriate ancient artefacts and bring them to Germany. Karo's views made him unpopular with the Entente-backed government that ruled in Greece after the First World War, and he took an academic post at the University of Halle, which he held until 1930. That year, he returned to Athens as director of the DAI. Although an early supporter of the Nazi government of Germany, Karo was forced from his post in 1936 by antisemitism against his Jewish ancestry. In 1939, he fled to the United States, supported by American associates including Carl Blegen and Bert Hodge Hill, and obtained a series of visiting professorships at the University of Cincinnati, Oberlin College and Claremont Colleges. However, he was also accused of collaborating with the Nazi regime: though no evidence for this allegation was proven, he was denied US citizenship and listed as an "Enemy Alien". He returned to Germany in 1952, and became an honorary professor at the University of Freiburg. (Full article...) |
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Lindow Man, also known as Lindow II and (in jest) as Pete Marsh, is the preserved bog body of a man discovered in a peat bog at Lindow Moss near Wilmslow in Cheshire, North West England. The remains were found on 1 August 1984 by commercial peat cutters. Lindow Man is not the only bog body to have been found in the moss; Lindow Woman was discovered the year before, and other body parts have also been recovered. The find was described as "one of the most significant archaeological discoveries of the 1980s" and caused a media sensation. It helped invigorate study of British bog bodies, which had previously been neglected. Dating the body has proven problematic, but it is thought that he was deposited into Lindow Moss, face down, some time between 2 BC and 119 AD, in either the Iron Age or Romano-British period. At the time of death, Lindow Man was a healthy male in his mid-20s, and may have been of high social status as his body shows little evidence of having done heavy or rough physical labour during his lifetime. There has been debate over the reason for his death; his death was violent and perhaps ritualistic. The recovered body has been preserved by freeze-drying and is on permanent display at the British Museum, although it occasionally travels to other venues such as the Manchester Museum. (Full article...) |
Lindow Man, also known as Lindow II and (in jest) as Pete Marsh, is the preserved bog body of a man discovered in a peat bog at Lindow Moss near Wilmslow in Cheshire, North West England. The remains were found on 1 August 1984 by commercial peat cutters. Lindow Man is not the only bog body to have been found in the moss; Lindow Woman was discovered the year before, and other body parts have also been recovered. The find was described as "one of the most significant archaeological discoveries of the 1980s" and caused a media sensation. It helped invigorate study of British bog bodies, which had previously been neglected. Dating the body has proven problematic, but it is thought that he was deposited into Lindow Moss, face down, some time between 2 BC and 119 AD, in either the Iron Age or Romano-British period. At the time of death, Lindow Man was a healthy male in his mid-20s, and may have been of high social status as his body shows little evidence of having done heavy or rough physical labour during his lifetime. There has been debate over the reason for his death; his death was violent and perhaps ritualistic. The recovered body has been preserved by freeze-drying and is on permanent display at the British Museum, although it occasionally travels to other venues such as the Manchester Museum. (Full article...) |
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Melbourne has a temperate oceanic climate (Köppen climate classification Cfb), bordering on a humid subtropical climate (Köppen climate classification Cfa), 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 south central Victorian standards, are nonetheless drizzly and overcast. The lack of winter rainfall is owed to 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 and/or the land mass, particularly in spring and autumn; this can set up a "bay effect", similar to the "lake effect" seen in colder climates, 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 around 425 mm (17 in) at Little River to 1,250 mm (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 is also prone to 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 predominately 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), bordering on a humid subtropical climate (Köppen climate classification Cfa), 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 south central Victorian standards, are nonetheless drizzly and overcast. The lack of winter rainfall is owed to 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 and/or the land mass, particularly in spring and autumn; this can set up a "bay effect", similar to the "lake effect" seen in colder climates, 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 around 425 mm (17 in) at Little River to 1,250 mm (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 is also prone to 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 predominately 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...) |
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