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Thomas Charles Lethbridge (23 March 1901 – 30 September 1971), better known as T. C. Lethbridge, was an English archaeologist, parapsychologist, and explorer. A specialist in Anglo-Saxon archaeology, he was honorary Keeper of Anglo-Saxon Antiquities at the Cambridge University Museum of Archaeology and Ethnology from 1923 to 1957, and wrote twenty-four books on various subjects, becoming known for his advocacy of dowsing. Born in Somerset to a wealthy family, Lethbridge was educated at Trinity College, Cambridge, during the course of which he attended an expedition to Jan Mayen island, becoming part of the first group to successfully climb the Beerenberg. After a failed second expedition to the Arctic Circle, he became involved in archaeology. In his capacity as Keeper of Anglo-Saxon Antiquities at the Cambridge University Museum of Archaeology and Ethnology, Lethbridge carried out excavations at sites around Britain. His claims regarding the existence of Iron Age hill figures on Wandlebury Hill in Cambridgeshire caused controversy within the archaeological community, with most archaeologists concluding that he had misidentified a natural feature. Lethbridge's methodology and theories were widely deemed unorthodox, and in turn he became increasingly critical of the archaeological profession. After resigning from the museum in 1957, Lethbridge devoted himself to researching paranormal phenomena, publishing a string of books on the subject for a popular rather than academic audience. Several books involved his research into the use of pendulums for dowsing, although in other publications he championed the witch-cult hypothesis of Margaret Murray, articulated the Stone Tape theory as an explanation for ghost sightings, and argued that extraterrestrial species were involved in shaping human evolution; in this he came to embrace and perpetuate the esoteric ideas of the Earth mysteries movement. Although his work in parapsychology was derided and ignored as pseudo-scientific by the academic establishment, he attracted a cult following, and his work was posthumously championed by esotericists including Colin Wilson and Julian Cope. In 2011 he was the subject of a biography by Terry Welbourn. (Full article...) |
Thomas Charles Lethbridge (23 March 1901 – 30 September 1971), better known as T. C. Lethbridge, was an English archaeologist, parapsychologist, and explorer. A specialist in Anglo-Saxon archaeology, he was honorary Keeper of Anglo-Saxon Antiquities at the Cambridge University Museum of Archaeology and Ethnology from 1923 to 1957, and wrote twenty-four books on various subjects, becoming known for his advocacy of dowsing. Born in Somerset to a wealthy family, Lethbridge was educated at Trinity College, Cambridge, during the course of which he attended an expedition to Jan Mayen island, becoming part of the first group to successfully climb the Beerenberg. After a failed second expedition to the Arctic Circle, he became involved in archaeology. In his capacity as Keeper of Anglo-Saxon Antiquities at the Cambridge University Museum of Archaeology and Ethnology, Lethbridge carried out excavations at sites around Britain. His claims regarding the existence of Iron Age hill figures on Wandlebury Hill in Cambridgeshire caused controversy within the archaeological community, with most archaeologists concluding that he had misidentified a natural feature. Lethbridge's methodology and theories were widely deemed unorthodox, and in turn he became increasingly critical of the archaeological profession. After resigning from the museum in 1957, Lethbridge devoted himself to researching paranormal phenomena, publishing a string of books on the subject for a popular rather than academic audience. Several books involved his research into the use of pendulums for dowsing, although in other publications he championed the witch-cult hypothesis of Margaret Murray, articulated the Stone Tape theory as an explanation for ghost sightings, and argued that extraterrestrial species were involved in shaping human evolution; in this he came to embrace and perpetuate the esoteric ideas of the Earth mysteries movement. Although his work in parapsychology was derided and ignored as pseudo-scientific by the academic establishment, he attracted a cult following, and his work was posthumously championed by esotericists including Colin Wilson and Julian Cope. In 2011 he was the subject of a biography by Terry Welbourn. (Full article...) |
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The Nine Stones, also known as the Devil's Nine Stones, the Nine Ladies, or Lady Williams and her Dog, is a stone circle located near to the village of Winterbourne Abbas in the southwestern English county of Dorset. Archaeologists believe that it was likely erected during the Bronze Age. The Nine Stones is part of a tradition of stone circle construction that spread through much of Great Britain, Ireland, and Brittany between 3,300 and 900 BCE, during the Late Neolithic and Early Bronze Age. The stone circle tradition was accompanied by the construction of timber circles and earthen henges, reflecting a growing emphasis on circular monuments. The purpose of such rings is unknown, although archaeologists speculate that the stones represented supernatural entities for the circle's builders. At least nine of these stone circles are known to have been constructed near modern Dorset. They are smaller than those found elsewhere in Great Britain and are typically built from sarsen stone. Located in the bottom of a narrow valley, the Nine Stones circle has a diameter of 9.1 by 7.8 metres (29 feet 10 inches by 25 feet 7 inches). It consists of nine irregularly spaced sarsen megaliths, with a small opening on its northern side. Two of the stones on the northwestern side of the monument are considerably larger than the other seven. This architectural feature has parallels with various stone circles in southwestern Scotland, and was potentially a deliberate choice of the circle's builders, to whom it may have had symbolic meaning. Antiquarians like John Aubrey and William Stukeley first took an interest in the site during the eighteenth century. It later received archaeological attention, although it has not been excavated. Local folklore has grown up around the circle, associating it with the Devil and with children petrified into rock. The Nine Stones are regarded as a sacred site by local Druids, who perform religious ceremonies there. The circle is adjacent to the A35 road and encircled by trees. The site is owned by English Heritage and is open without charge to visitors. (Full article...) |
The Nine Stones, also known as the Devil's Nine Stones, the Nine Ladies, or Lady Williams and her Dog, is a stone circle located near to the village of Winterbourne Abbas in the southwestern English county of Dorset. Archaeologists believe that it was likely erected during the Bronze Age. The Nine Stones is part of a tradition of stone circle construction that spread through much of Great Britain, Ireland, and Brittany between 3,300 and 900 BCE, during the Late Neolithic and Early Bronze Age. The stone circle tradition was accompanied by the construction of timber circles and earthen henges, reflecting a growing emphasis on circular monuments. The purpose of such rings is unknown, although archaeologists speculate that the stones represented supernatural entities for the circle's builders. At least nine of these stone circles are known to have been constructed near modern Dorset. They are smaller than those found elsewhere in Great Britain and are typically built from sarsen stone. Located in the bottom of a narrow valley, the Nine Stones circle has a diameter of 9.1 by 7.8 metres (29 feet 10 inches by 25 feet 7 inches). It consists of nine irregularly spaced sarsen megaliths, with a small opening on its northern side. Two of the stones on the northwestern side of the monument are considerably larger than the other seven. This architectural feature has parallels with various stone circles in southwestern Scotland, and was potentially a deliberate choice of the circle's builders, to whom it may have had symbolic meaning. Antiquarians like John Aubrey and William Stukeley first took an interest in the site during the eighteenth century. It later received archaeological attention, although it has not been excavated. Local folklore has grown up around the circle, associating it with the Devil and with children petrified into rock. The Nine Stones are regarded as a sacred site by local Druids, who perform religious ceremonies there. The circle is adjacent to the A35 road and encircled by trees. The site is owned by English Heritage and is open without charge to visitors. (Full article...) |
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The Beulé Gate (French pronunciation: [bœ'le]) is a fortified gate, constructed in the Roman period, leading to the Propylaia of the Acropolis of Athens. It was constructed almost entirely from repurposed materials (spolia) taken from the Choragic Monument of Nikias, a monument built in the fourth century BCE and demolished between the second and fourth centuries CE. The dedicatory inscription from Nikias's monument is still visible in the entablature of the Beulé Gate. The gate was integrated into the Post-Herulian Wall, a late Roman fortification built around the Acropolis in the years following the city's sack by the Germanic Heruli people in 267 or early 268 CE. Its construction marked the beginning of a new phase in the Acropolis's use, in which it came to be seen more as a potential defensive position than in the religious terms that had marked its use in the classical period. During the medieval period, the gate was further fortified and closed off, before being built over with a bastion in Ottoman times. The monument was discovered by the French archaeologist Charles Ernest Beulé in 1852, and excavated between 1852 and 1853. Its discovery was greeted enthusiastically in France among the scholarly community and the press, though archaeologists and Greek commentators criticised the aggressive means – particularly the use of explosives – by which Beulé had carried out the excavation. In modern times, the gate has served primarily as an exit for tourists from the Acropolis. (Full article...) |
The Beulé Gate (French pronunciation: [bœ'le]) is a fortified gate, constructed in the Roman period, leading to the Propylaia of the Acropolis of Athens. It was constructed almost entirely from repurposed materials (spolia) taken from the Choragic Monument of Nikias, a monument built in the fourth century BCE and demolished between the second and fourth centuries CE. The dedicatory inscription from Nikias's monument is still visible in the entablature of the Beulé Gate. The gate was integrated into the Post-Herulian Wall, a late Roman fortification built around the Acropolis in the years following the city's sack by the Germanic Heruli people in 267 or early 268 CE. Its construction marked the beginning of a new phase in the Acropolis's use, in which it came to be seen more as a potential defensive position than in the religious terms that had marked its use in the classical period. During the medieval period, the gate was further fortified and closed off, before being built over with a bastion in Ottoman times. The monument was discovered by the French archaeologist Charles Ernest Beulé in 1852, and excavated between 1852 and 1853. Its discovery was greeted enthusiastically in France among the scholarly community and the press, though archaeologists and Greek commentators criticised the aggressive means – particularly the use of explosives – by which Beulé had carried out the excavation. In modern times, the gate has served primarily as an exit for tourists from the Acropolis. (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...) |
References
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