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Verteba Cave (Ukrainian: Печера Вертеба, romanized: Pechera Verteba) is a karstic cave near the village of Bilche-Zolote, Chortkiv Raion, Ternopil Oblast, Ukraine. It sits near the Seret river, on a high plateau known as the Podolian Upland, and is one of several such caves in the region formed in gypsum. Verteba is the only cave in this cluster to show signs of prehistoric occupation. In Copper Age Europe, the cave was inhabited periodically by the Cucuteni–Trypillia culture. Thousands of artefacts, including ceramic vessels, clay figurines, bones, and tools, have been found inside. Human remains—which mainly consist of disembodied skulls—have been found bearing injuries consistent with having been intentionally killed. Between October 1942 and April 1943, 28 Jews from Bilche-Zolote and Korolivka hid in the cave to escape the Holocaust. When the Gestapo stormed the cave, the group was forced to relocate to Priest's Grotto; most survived the war, having hidden underground for nearly two years. Their ordeal was the subject of a 2007 book, The Secret of Priest's Grotto: A Holocaust Survival Story; and a 2012 documentary, No Place on Earth. Verteba partially opened to the public as a show cave in 2004. Inside, the cave hosts the Museum of Trypillian Culture, displaying archaeological finds from the past 200 years. (Full article...)

Verteba Cave (Ukrainian: Печера Вертеба, romanized: Pechera Verteba) is a karstic cave near the village of Bilche-Zolote, Chortkiv Raion, Ternopil Oblast, Ukraine. It sits near the Seret river, on a high plateau known as the Podolian Upland, and is one of several such caves in the region formed in gypsum. Verteba is the only cave in this cluster to show signs of prehistoric occupation. In Copper Age Europe, the cave was inhabited periodically by the Cucuteni–Trypillia culture. Thousands of artefacts, including ceramic vessels, clay figurines, bones, and tools, have been found inside. Human remains—which mainly consist of disembodied skulls—have been found bearing injuries consistent with having been intentionally killed. Between October 1942 and April 1943, 28 Jews from Bilche-Zolote and Korolivka hid in the cave to escape the Holocaust. When the Gestapo stormed the cave, the group was forced to relocate to Priest's Grotto; most survived the war, having hidden underground for nearly two years. Their ordeal was the subject of a 2007 book, The Secret of Priest's Grotto: A Holocaust Survival Story; and a 2012 documentary, No Place on Earth. Verteba partially opened to the public as a show cave in 2004. Inside, the cave hosts the Museum of Trypillian Culture, displaying archaeological finds from the past 200 years. (Full article...)

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The remains of Richard III, the last English king killed in battle and last king of the House of York, were discovered within the site of the former Grey Friars Priory in Leicester, England, in September 2012. Following extensive anthropological and genetic testing, the remains were reinterred at Leicester Cathedral on 26 March 2015. Richard III, the final ruler of the Plantagenet dynasty, was killed on 22 August 1485 in the Battle of Bosworth Field, the last significant battle of the Wars of the Roses. His body was taken to Greyfriars, Leicester, where it was buried in a crude grave in the friary church. Following the friary's dissolution in 1538 and subsequent demolition, Richard's tomb was lost. An erroneous account arose that Richard's bones had been thrown into the River Soar at the nearby Bow Bridge. A search for Richard's body began in August 2012, initiated by Philippa Langley and the Looking for Richard project with the support of the Richard III Society. The archaeological excavation was led by University of Leicester Archaeological Services, working in partnership with Leicester City Council. On the first day a human skeleton belonging to a man in his thirties was uncovered showing signs of severe injuries. The skeleton, which had several unusual physical features, most notably scoliosis, a severe curvature of the back, was exhumed to allow scientific analysis. Examination showed that the man had probably been killed either by a blow from a large bladed weapon, probably a halberd, which cut off the back of his skull and exposed the brain, or by a sword thrust that penetrated all the way through the brain. Other wounds on the skeleton had probably occurred after death as "humiliation injuries", inflicted as a form of posthumous revenge. The age of the bones at death matched that of Richard when he was killed; they were dated to about the period of his death and were mostly consistent with physical descriptions of the king. Preliminary DNA analysis showed that mitochondrial DNA extracted from the bones matched that of two matrilineal descendants, one 17th-generation and the other 19th-generation, of Richard's sister Anne of York. Taking these findings into account along with other historical, scientific and archaeological evidence, the University of Leicester announced on 4 February 2013 that it had concluded beyond reasonable doubt that the skeleton was that of Richard III. As a condition of being allowed to disinter the skeleton, the archaeologists agreed that, if Richard were found, his remains would be reburied in Leicester Cathedral. A controversy arose as to whether an alternative reburial site, York Minster or Westminster Abbey, would be more suitable. A legal challenge confirmed there were no public law grounds for the courts to be involved in that decision. Reinterment took place in Leicester on 26 March 2015, during a televised memorial service held in the presence of the Archbishop of Canterbury and senior members of other Christian denominations. (Full article...)

The remains of Richard III, the last English king killed in battle and last king of the House of York, were discovered within the site of the former Grey Friars Priory in Leicester, England, in September 2012. Following extensive anthropological and genetic testing, the remains were reinterred at Leicester Cathedral on 26 March 2015. Richard III, the final ruler of the Plantagenet dynasty, was killed on 22 August 1485 in the Battle of Bosworth Field, the last significant battle of the Wars of the Roses. His body was taken to Greyfriars, Leicester, where it was buried in a crude grave in the friary church. Following the friary's dissolution in 1538 and subsequent demolition, Richard's tomb was lost. An erroneous account arose that Richard's bones had been thrown into the River Soar at the nearby Bow Bridge. A search for Richard's body began in August 2012, initiated by Philippa Langley and the Looking for Richard project with the support of the Richard III Society. The archaeological excavation was led by University of Leicester Archaeological Services, working in partnership with Leicester City Council. On the first day a human skeleton belonging to a man in his thirties was uncovered showing signs of severe injuries. The skeleton, which had several unusual physical features, most notably scoliosis, a severe curvature of the back, was exhumed to allow scientific analysis. Examination showed that the man had probably been killed either by a blow from a large bladed weapon, probably a halberd, which cut off the back of his skull and exposed the brain, or by a sword thrust that penetrated all the way through the brain. Other wounds on the skeleton had probably occurred after death as "humiliation injuries", inflicted as a form of posthumous revenge. The age of the bones at death matched that of Richard when he was killed; they were dated to about the period of his death and were mostly consistent with physical descriptions of the king. Preliminary DNA analysis showed that mitochondrial DNA extracted from the bones matched that of two matrilineal descendants, one 17th-generation and the other 19th-generation, of Richard's sister Anne of York. Taking these findings into account along with other historical, scientific and archaeological evidence, the University of Leicester announced on 4 February 2013 that it had concluded beyond reasonable doubt that the skeleton was that of Richard III. As a condition of being allowed to disinter the skeleton, the archaeologists agreed that, if Richard were found, his remains would be reburied in Leicester Cathedral. A controversy arose as to whether an alternative reburial site, York Minster or Westminster Abbey, would be more suitable. A legal challenge confirmed there were no public law grounds for the courts to be involved in that decision. Reinterment took place in Leicester on 26 March 2015, during a televised memorial service held in the presence of the Archbishop of Canterbury and senior members of other Christian denominations. (Full article...)

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Martin Rundkvist (born 4 April 1972) is a Swedish archaeologist and associate professor at the University of Łódź in Poland. His research focuses on the Bronze, Iron, and Middle Ages of Scandinavia, including significant excavations in the province of Östergötland. Rundkvist has studied and excavated various sites in Sweden, particularly in the country's south. In 2003 and 2004, he published a three-volume work which doubled as his PhD dissertation, cataloguing the finds from Barshalder, the largest prehistoric cemetery on the Swedish island of Gotland. A subsequent book identified nine possible regional power centres in Östergötland, and attempted to determine where the "Beowulfian mead halls" of the day once stood. Excavating years later at one of these sites, Aska, Rundkvist uncovered the foundations of a large mead hall, and 30 ornate gold figures that might have represented gods or royals. In other works, Rundkvist has excavated a Viking boat grave, and analysed both the placement of deposited artefacts in the landscape and the lifestyles of the Scandinavian élite during the Middle Ages. Rundkvist has worked in archaeology since 1992, including research and lecture posts at the universities of Exeter, Chester, Linnaeus, and Tallinn. He spent two decades as managing editor of Fornvännen, a journal on archaeology and medieval art, and authors the blog Aardvarchaeology, which the James Randi Educational Foundation termed "the most-read archaeology blog on the Internet". Rundkvist served as chair for the Swedish Skeptics' Association for four years, and edited its quarterly magazine Folkvett. (Full article...)

Martin Rundkvist (born 4 April 1972) is a Swedish archaeologist and associate professor at the University of Łódź in Poland. His research focuses on the Bronze, Iron, and Middle Ages of Scandinavia, including significant excavations in the province of Östergötland. Rundkvist has studied and excavated various sites in Sweden, particularly in the country's south. In 2003 and 2004, he published a three-volume work which doubled as his PhD dissertation, cataloguing the finds from Barshalder, the largest prehistoric cemetery on the Swedish island of Gotland. A subsequent book identified nine possible regional power centres in Östergötland, and attempted to determine where the "Beowulfian mead halls" of the day once stood. Excavating years later at one of these sites, Aska, Rundkvist uncovered the foundations of a large mead hall, and 30 ornate gold figures that might have represented gods or royals. In other works, Rundkvist has excavated a Viking boat grave, and analysed both the placement of deposited artefacts in the landscape and the lifestyles of the Scandinavian élite during the Middle Ages. Rundkvist has worked in archaeology since 1992, including research and lecture posts at the universities of Exeter, Chester, Linnaeus, and Tallinn. He spent two decades as managing editor of Fornvännen, a journal on archaeology and medieval art, and authors the blog Aardvarchaeology, which the James Randi Educational Foundation termed "the most-read archaeology blog on the Internet". Rundkvist served as chair for the Swedish Skeptics' Association for four years, and edited its quarterly magazine Folkvett. (Full article...)

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Under the Köppen–Geiger classification, Sydney has a humid subtropical climate (Cfa) with "warm, sometimes hot" summers and "generally mild", to "cool" winters. The El Niño–Southern Oscillation, the Indian Ocean Dipole and the Southern Annular Mode play an important role in determining Sydney's weather patterns: drought and bushfire on the one hand, and storms and flooding on the other, associated with the opposite phases of the oscillation in Australia. The weather is moderated by proximity to the ocean, and more extreme temperatures are recorded in the inland western suburbs because Sydney CBD is more affected by the oceanic climate drivers than the western suburbs. At Sydney's primary weather station at Observatory Hill, extreme temperatures have ranged from 45.8 °C (114.4 °F) on 18 January 2013 to 2.1 °C (35.8 °F) on 22 June 1932. An average of 14.9 days a year have temperatures at or above 30 °C (86 °F) in the central business district (CBD). In contrast, the metropolitan area averages between 35 and 65 days, depending on the suburb. The hottest day in the metropolitan area occurred in Penrith on 4 January 2020, where a high of 48.9 °C (120.0 °F) was recorded. The average annual temperature of the sea ranges from 18.5 °C (65.3 °F) in September to 23.7 °C (74.7 °F) in February. Sydney has an average of 7.2 hours of sunshine per day and 109.5 clear days annually. Due to the inland location, frost is recorded early in the morning in Western Sydney a few times in winter. Autumn and spring are the transitional seasons, with spring showing a larger temperature variation than autumn. Sydney experiences an urban heat island effect. This makes certain parts of the city more vulnerable to extreme heat, including coastal suburbs. In late spring and summer, temperatures over 35 °C (95 °F) are not uncommon, though hot, dry conditions are usually ended by a southerly buster, a powerful southerly that brings gale winds and a rapid fall in temperature. Since Sydney is downwind of the Great Dividing Range, it occasionally experiences dry, westerly foehn winds typically in winter and early spring (which are the reason for its warm maximum temperatures). Westerly winds are intense when the Roaring Forties (or the Southern Annular Mode) shift towards southeastern Australia, where they may damage homes and affect flights, in addition to making the temperature seem colder than it actually is. Rainfall has a moderate to low variability and has historically been fairly uniform throughout the year, although in recent years it has been more summer-dominant and erratic. Precipitation is usually higher in summer through to autumn, and lower in late winter to early spring. In late autumn and winter, east coast lows may bring large amounts of rainfall, especially in the CBD. In the warm season black nor'easters are usually the cause of heavy rain events, though other forms of low-pressure areas, including remnants of ex-cyclones, may also bring heavy deluge and afternoon thunderstorms. 'Snow' was last alleged in 1836, more than likely a fall of graupel, or soft hail; and in July 2008 the Upper North Shore saw a fall of graupel that was mistaken by many for 'snow'. In 2009, dry conditions brought a severe dust storm towards the city. Climate data for Sydney (Observatory Hill) 1991–2020 averages, 1861–present extremes Month Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Year Record high °C (°F) 45.8 (114.4) 42.1 (107.8) 39.8 (103.6) 35.4 (95.7) 30.0 (86.0) 26.9 (80.4) 26.5 (79.7) 31.3 (88.3) 34.6 (94.3) 38.2 (100.8) 41.8 (107.2) 42.2 (108.0) 45.8 (114.4) Mean maximum °C (°F) 36.8 (98.2) 34.1 (93.4) 32.2 (90.0) 29.7 (85.5) 26.2 (79.2) 22.3 (72.1) 22.9 (73.2) 25.4 (77.7) 29.9 (85.8) 33.6 (92.5) 34.1 (93.4) 34.4 (93.9) 38.8 (101.8) Mean daily maximum °C (°F) 27.0 (80.6) 26.8 (80.2) 25.7 (78.3) 23.6 (74.5) 20.9 (69.6) 18.3 (64.9) 17.9 (64.2) 19.3 (66.7) 21.6 (70.9) 23.2 (73.8) 24.2 (75.6) 25.7 (78.3) 22.8 (73.0) Daily mean °C (°F) 23.5 (74.3) 23.4 (74.1) 22.1 (71.8) 19.5 (67.1) 16.6 (61.9) 14.2 (57.6) 13.4 (56.1) 14.5 (58.1) 17.0 (62.6) 18.9 (66.0) 20.4 (68.7) 22.1 (71.8) 18.8 (65.8) Mean daily minimum °C (°F) 20.0 (68.0) 19.9 (67.8) 18.4 (65.1) 15.3 (59.5) 12.3 (54.1) 10.0 (50.0) 8.9 (48.0) 9.7 (49.5) 12.3 (54.1) 14.6 (58.3) 16.6 (61.9) 18.4 (65.1) 14.7 (58.5) Mean minimum °C (°F) 16.1 (61.0) 16.1 (61.0) 14.2 (57.6) 11.0 (51.8) 8.3 (46.9) 6.5 (43.7) 5.7 (42.3) 6.1 (43.0) 8.0 (46.4) 9.8 (49.6) 12.0 (53.6) 13.9 (57.0) 5.3 (41.5) Record low °C (°F) 10.6 (51.1) 9.6 (49.3) 9.3 (48.7) 7.0 (44.6) 4.4 (39.9) 2.1 (35.8) 2.2 (36.0) 2.7 (36.9) 4.9 (40.8) 5.7 (42.3) 7.7 (45.9) 9.1 (48.4) 2.1 (35.8) Average rainfall mm (inches) 91.1 (3.59) 131.5 (5.18) 117.5 (4.63) 114.1 (4.49) 100.8 (3.97) 142.0 (5.59) 80.3 (3.16) 75.1 (2.96) 63.4 (2.50) 67.7 (2.67) 90.6 (3.57) 73.0 (2.87) 1,149.7 (45.26) Average rainy days (≥ 1 mm) 8.2 9.0 10.1 7.9 7.9 9.3 7.2 5.6 5.8 7.6 8.7 7.9 95.2 Average afternoon relative humidity (%) 60 62 59 58 58 56 52 47 49 53 57 58 56 Average dew point °C (°F) 16.5 (61.7) 17.2 (63.0) 15.4 (59.7) 12.7 (54.9) 10.3 (50.5) 7.8 (46.0) 6.1 (43.0) 5.4 (41.7) 7.8 (46.0) 10.2 (50.4) 12.6 (54.7) 14.6 (58.3) 11.4 (52.5) Mean monthly sunshine hours 232.5 205.9 210.8 213.0 204.6 171.0 207.7 248.0 243.0 244.9 222.0 235.6 2,639 Percent possible sunshine 53 54 55 63 63 57 66 72 67 61 55 55 60 Source 1: Bureau of Meteorology Source 2: Bureau of Meteorology, Sydney Airport (sunshine hours) (Full article...)

Under the Köppen–Geiger classification, Sydney has a humid subtropical climate (Cfa) with "warm, sometimes hot" summers and "generally mild", to "cool" winters. The El Niño–Southern Oscillation, the Indian Ocean Dipole and the Southern Annular Mode play an important role in determining Sydney's weather patterns: drought and bushfire on the one hand, and storms and flooding on the other, associated with the opposite phases of the oscillation in Australia. The weather is moderated by proximity to the ocean, and more extreme temperatures are recorded in the inland western suburbs because Sydney CBD is more affected by the oceanic climate drivers than the western suburbs. At Sydney's primary weather station at Observatory Hill, extreme temperatures have ranged from 45.8 °C (114.4 °F) on 18 January 2013 to 2.1 °C (35.8 °F) on 22 June 1932. An average of 14.9 days a year have temperatures at or above 30 °C (86 °F) in the central business district (CBD). In contrast, the metropolitan area averages between 35 and 65 days, depending on the suburb. The hottest day in the metropolitan area occurred in Penrith on 4 January 2020, where a high of 48.9 °C (120.0 °F) was recorded. The average annual temperature of the sea ranges from 18.5 °C (65.3 °F) in September to 23.7 °C (74.7 °F) in February. Sydney has an average of 7.2 hours of sunshine per day and 109.5 clear days annually. Due to the inland location, frost is recorded early in the morning in Western Sydney a few times in winter. Autumn and spring are the transitional seasons, with spring showing a larger temperature variation than autumn. Sydney experiences an urban heat island effect. This makes certain parts of the city more vulnerable to extreme heat, including coastal suburbs. In late spring and summer, temperatures over 35 °C (95 °F) are not uncommon, though hot, dry conditions are usually ended by a southerly buster, a powerful southerly that brings gale winds and a rapid fall in temperature. Since Sydney is downwind of the Great Dividing Range, it occasionally experiences dry, westerly foehn winds typically in winter and early spring (which are the reason for its warm maximum temperatures). Westerly winds are intense when the Roaring Forties (or the Southern Annular Mode) shift towards southeastern Australia, where they may damage homes and affect flights, in addition to making the temperature seem colder than it actually is. Rainfall has a moderate to low variability and has historically been fairly uniform throughout the year, although in recent years it has been more summer-dominant and erratic. Precipitation is usually higher in summer through to autumn, and lower in late winter to early spring. In late autumn and winter, east coast lows may bring large amounts of rainfall, especially in the CBD. In the warm season black nor'easters are usually the cause of heavy rain events, though other forms of low-pressure areas, including remnants of ex-cyclones, may also bring heavy deluge and afternoon thunderstorms. 'Snow' was last alleged in 1836, more than likely a fall of graupel, or soft hail; and in July 2008 the Upper North Shore saw a fall of graupel that was mistaken by many for 'snow'. In 2009, dry conditions brought a severe dust storm towards the city. Climate data for Sydney (Observatory Hill) 1991–2020 averages, 1861–present extremes Month Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Year Record high °C (°F) 45.8 (114.4) 42.1 (107.8) 39.8 (103.6) 35.4 (95.7) 30.0 (86.0) 26.9 (80.4) 26.5 (79.7) 31.3 (88.3) 34.6 (94.3) 38.2 (100.8) 41.8 (107.2) 42.2 (108.0) 45.8 (114.4) Mean maximum °C (°F) 36.8 (98.2) 34.1 (93.4) 32.2 (90.0) 29.7 (85.5) 26.2 (79.2) 22.3 (72.1) 22.9 (73.2) 25.4 (77.7) 29.9 (85.8) 33.6 (92.5) 34.1 (93.4) 34.4 (93.9) 38.8 (101.8) Mean daily maximum °C (°F) 27.0 (80.6) 26.8 (80.2) 25.7 (78.3) 23.6 (74.5) 20.9 (69.6) 18.3 (64.9) 17.9 (64.2) 19.3 (66.7) 21.6 (70.9) 23.2 (73.8) 24.2 (75.6) 25.7 (78.3) 22.8 (73.0) Daily mean °C (°F) 23.5 (74.3) 23.4 (74.1) 22.1 (71.8) 19.5 (67.1) 16.6 (61.9) 14.2 (57.6) 13.4 (56.1) 14.5 (58.1) 17.0 (62.6) 18.9 (66.0) 20.4 (68.7) 22.1 (71.8) 18.8 (65.8) Mean daily minimum °C (°F) 20.0 (68.0) 19.9 (67.8) 18.4 (65.1) 15.3 (59.5) 12.3 (54.1) 10.0 (50.0) 8.9 (48.0) 9.7 (49.5) 12.3 (54.1) 14.6 (58.3) 16.6 (61.9) 18.4 (65.1) 14.7 (58.5) Mean minimum °C (°F) 16.1 (61.0) 16.1 (61.0) 14.2 (57.6) 11.0 (51.8) 8.3 (46.9) 6.5 (43.7) 5.7 (42.3) 6.1 (43.0) 8.0 (46.4) 9.8 (49.6) 12.0 (53.6) 13.9 (57.0) 5.3 (41.5) Record low °C (°F) 10.6 (51.1) 9.6 (49.3) 9.3 (48.7) 7.0 (44.6) 4.4 (39.9) 2.1 (35.8) 2.2 (36.0) 2.7 (36.9) 4.9 (40.8) 5.7 (42.3) 7.7 (45.9) 9.1 (48.4) 2.1 (35.8) Average rainfall mm (inches) 91.1 (3.59) 131.5 (5.18) 117.5 (4.63) 114.1 (4.49) 100.8 (3.97) 142.0 (5.59) 80.3 (3.16) 75.1 (2.96) 63.4 (2.50) 67.7 (2.67) 90.6 (3.57) 73.0 (2.87) 1,149.7 (45.26) Average rainy days (≥ 1 mm) 8.2 9.0 10.1 7.9 7.9 9.3 7.2 5.6 5.8 7.6 8.7 7.9 95.2 Average afternoon relative humidity (%) 60 62 59 58 58 56 52 47 49 53 57 58 56 Average dew point °C (°F) 16.5 (61.7) 17.2 (63.0) 15.4 (59.7) 12.7 (54.9) 10.3 (50.5) 7.8 (46.0) 6.1 (43.0) 5.4 (41.7) 7.8 (46.0) 10.2 (50.4) 12.6 (54.7) 14.6 (58.3) 11.4 (52.5) Mean monthly sunshine hours 232.5 205.9 210.8 213.0 204.6 171.0 207.7 248.0 243.0 244.9 222.0 235.6 2,639 Percent possible sunshine 53 54 55 63 63 57 66 72 67 61 55 55 60 Source 1: Bureau of Meteorology Source 2: Bureau of Meteorology, Sydney Airport (sunshine hours) (Full article...)

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