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A group of paintings created by Mark Rothko now known as a series including works on canvas and paper produced before the artists' death by suicide. The series has works which used both a combination of black and grey, or are monotone black, or with only a small quantity of color. The artists' works include an expression of color as more wholly dark, absent in previous works, from sometime during the 1950s. Some of the serial of works were gifted by The Mark Rothko Foundation Incorporated to various city galleries in the United States, including: The Museum of Contemporary Art, Los Angeles, the Guggenheim and Museum of Modern Art of New York, the National Gallery of Art in Washington. Altogether during 1970 the artist Rothko output three works of these $[$ ACCESSION 85.27$]$ is possessed by MoCA LA: Untitled the final in the grey-black serial painting. Although black with or without grey was the theme of Rothko's end works his penultimate painting Untitled included blue. The termination of Rothko's art and life in 1970 was death, his final product, red only. (Full article...)

A group of paintings created by Mark Rothko now known as a series including works on canvas and paper produced before the artists' death by suicide. The series has works which used both a combination of black and grey, or are monotone black, or with only a small quantity of color. The artists' works include an expression of color as more wholly dark, absent in previous works, from sometime during the 1950s. Some of the serial of works were gifted by The Mark Rothko Foundation Incorporated to various city galleries in the United States, including: The Museum of Contemporary Art, Los Angeles, the Guggenheim and Museum of Modern Art of New York, the National Gallery of Art in Washington. Altogether during 1970 the artist Rothko output three works of these $[$ ACCESSION 85.27$]$ is possessed by MoCA LA: Untitled the final in the grey-black serial painting. Although black with or without grey was the theme of Rothko's end works his penultimate painting Untitled included blue. The termination of Rothko's art and life in 1970 was death, his final product, red only. (Full article...)

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The Archaeology of Ritual and Magic is an archaeological study of the material evidence for ritual and magical practices in Europe, containing a particular emphasis on London and South East England. It was written by the English archaeologist Ralph Merrifield, the former deputy director of the Museum of London, and first published by B.T. Batsford in 1987. Merrifield opens The Archaeology of Ritual and Magic by discussing how archaeologists have understood magic and ritual practices in past societies, opining that on the whole it had been a neglected area of study. Looking at the archaeological evidence for ritual activity in the pre-Roman Iron Age and the Roman Iron Age of Britain, he discusses animal and human sacrifice, as well as the offering of votive deposits in rivers and other bodies of water. He moves on to explore the rituals surrounding death and burial, suggesting areas where this ritual activity is visible in the burial record of multiple societies. Merrifield goes on to discuss the archaeological evidence for ritual practices in Christian Europe, highlighting areas of ritual continuance from earlier pagan periods, in particular the deposition of metal goods in water. Looking at the evidence for foundation deposits in European buildings that likely had magico-religious purposes, he then looks at several examples of written charms and spells which have survived in the archaeological record. Upon publication, The Archaeology of Ritual and Magic received predominantly positive reviews in academic peer-reviewed journals such as Folklore and The Antiquaries Journal. In the ensuing years, the book has been widely cited by scholars as an influential and pioneering text in the study of the archaeology of ritual and magic. (Full article...)

The Archaeology of Ritual and Magic is an archaeological study of the material evidence for ritual and magical practices in Europe, containing a particular emphasis on London and South East England. It was written by the English archaeologist Ralph Merrifield, the former deputy director of the Museum of London, and first published by B.T. Batsford in 1987. Merrifield opens The Archaeology of Ritual and Magic by discussing how archaeologists have understood magic and ritual practices in past societies, opining that on the whole it had been a neglected area of study. Looking at the archaeological evidence for ritual activity in the pre-Roman Iron Age and the Roman Iron Age of Britain, he discusses animal and human sacrifice, as well as the offering of votive deposits in rivers and other bodies of water. He moves on to explore the rituals surrounding death and burial, suggesting areas where this ritual activity is visible in the burial record of multiple societies. Merrifield goes on to discuss the archaeological evidence for ritual practices in Christian Europe, highlighting areas of ritual continuance from earlier pagan periods, in particular the deposition of metal goods in water. Looking at the evidence for foundation deposits in European buildings that likely had magico-religious purposes, he then looks at several examples of written charms and spells which have survived in the archaeological record. Upon publication, The Archaeology of Ritual and Magic received predominantly positive reviews in academic peer-reviewed journals such as Folklore and The Antiquaries Journal. In the ensuing years, the book has been widely cited by scholars as an influential and pioneering text in the study of the archaeology of ritual and magic. (Full article...)

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The tomb of Tutankhamun was discovered in the Valley of the Kings in 1922 by excavators led by the Egyptologist Howard Carter, more than 3,300 years after Tutankhamun's death and burial. Whereas the tombs of most pharaohs were plundered by graverobbers in ancient times, Tutankhamun's tomb was hidden by debris for most of its existence and therefore not extensively robbed. It thus became the only known near-intact royal burial from ancient Egypt. The tomb was opened beginning on 4 November 1922 during an excavation by Carter and his patron, the 5th Earl of Carnarvon. The burial consisted of more than five thousand objects, many of which were in a highly fragile state, so conserving the burial goods for removal from the tomb required an unprecedented effort. The opulence of the burial goods inspired a media frenzy and popularised ancient Egyptian-inspired designs with the Western public. To the Egyptians, who had recently become partially independent of British rule, the tomb became a symbol of national pride, strengthening Pharaonism, a nationalist ideology that emphasised modern Egypt's ties to the ancient civilisation, and creating friction between Egyptians and the British-led excavation team. The publicity surrounding the excavation intensified when Carnarvon died of an infection, giving rise to speculation that his death and other misfortunes connected with the tomb were the result of an ancient curse. After Carnarvon's death, tensions arose between Carter and the Egyptian government over who should control access to the tomb. In early 1924, Carter stopped work in protest, beginning a dispute that lasted until the end of the year. Under the agreement that resolved the dispute, the artefacts from the tomb would not be divided between the government and the dig's sponsors, as was standard practice in previous Egyptological digs, and most of the tomb's contents went to the Egyptian Museum in Cairo. In later seasons media attention waned, apart from coverage of the removal of Tutankhamun's mummy from its coffin in 1925. The last of the burial goods were conserved and shipped to Cairo in 1932. The tomb's discovery did not reveal as much about the history of Tutankhamun's time as Egyptologists had initially hoped, but it established the length of his reign and gave clues about the end of the Amarna Period, which preceded his reign. It was more informative about the material culture of Tutankhamun's time, demonstrating what a complete royal burial was like and providing evidence about the lifestyles of wealthy Egyptians and the behaviour of ancient tomb robbers. The interest generated by the find stimulated efforts to train Egyptians in Egyptology. Since the discovery, the Egyptian government has capitalised on its enduring fame by using exhibitions of the burial goods for purposes of fundraising and diplomacy, and Tutankhamun has become a symbol of ancient Egypt itself. (Full article...)

The tomb of Tutankhamun was discovered in the Valley of the Kings in 1922 by excavators led by the Egyptologist Howard Carter, more than 3,300 years after Tutankhamun's death and burial. Whereas the tombs of most pharaohs were plundered by graverobbers in ancient times, Tutankhamun's tomb was hidden by debris for most of its existence and therefore not extensively robbed. It thus became the only known near-intact royal burial from ancient Egypt. The tomb was opened beginning on 4 November 1922 during an excavation by Carter and his patron, the 5th Earl of Carnarvon. The burial consisted of more than five thousand objects, many of which were in a highly fragile state, so conserving the burial goods for removal from the tomb required an unprecedented effort. The opulence of the burial goods inspired a media frenzy and popularised ancient Egyptian-inspired designs with the Western public. To the Egyptians, who had recently become partially independent of British rule, the tomb became a symbol of national pride, strengthening Pharaonism, a nationalist ideology that emphasised modern Egypt's ties to the ancient civilisation, and creating friction between Egyptians and the British-led excavation team. The publicity surrounding the excavation intensified when Carnarvon died of an infection, giving rise to speculation that his death and other misfortunes connected with the tomb were the result of an ancient curse. After Carnarvon's death, tensions arose between Carter and the Egyptian government over who should control access to the tomb. In early 1924, Carter stopped work in protest, beginning a dispute that lasted until the end of the year. Under the agreement that resolved the dispute, the artefacts from the tomb would not be divided between the government and the dig's sponsors, as was standard practice in previous Egyptological digs, and most of the tomb's contents went to the Egyptian Museum in Cairo. In later seasons media attention waned, apart from coverage of the removal of Tutankhamun's mummy from its coffin in 1925. The last of the burial goods were conserved and shipped to Cairo in 1932. The tomb's discovery did not reveal as much about the history of Tutankhamun's time as Egyptologists had initially hoped, but it established the length of his reign and gave clues about the end of the Amarna Period, which preceded his reign. It was more informative about the material culture of Tutankhamun's time, demonstrating what a complete royal burial was like and providing evidence about the lifestyles of wealthy Egyptians and the behaviour of ancient tomb robbers. The interest generated by the find stimulated efforts to train Egyptians in Egyptology. Since the discovery, the Egyptian government has capitalised on its enduring fame by using exhibitions of the burial goods for purposes of fundraising and diplomacy, and Tutankhamun has become a symbol of ancient Egypt itself. (Full article...)

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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 nonetheless drizzly and overcast. 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 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 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 nonetheless drizzly and overcast. 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 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 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...)

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