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The untitled sixth studio album by the Canadian rock band Trooper (informally known as Trooper 1980) was released on October 4, 1980. It remains the only Trooper album not to chart a hit single on Canada's RPM 100 Singles chart. (Full article...)	The untitled sixth studio album by the Canadian rock band Trooper (informally known as Trooper 1980) was released on October 4, 1980. It remains the only Trooper album not to chart a hit single on Canada's RPM 100 Singles chart. (Full article...)

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There are 37 scheduled monuments in Greater Manchester, a metropolitan county in North West England. In the United Kingdom, a scheduled monument is a "nationally important" archaeological site or historic building that has been given protection against unauthorised change by being placed on a list (or "schedule") by the Secretary of State for Digital Culture, Media and Sport; Historic England recommends sites for scheduling to the Secretary of State. Scheduled monuments are defined in the Ancient Monuments and Archaeological Areas Act 1979 and the National Heritage Act 1983. There are nearly 20,000 entries on the schedule, which is maintained by Historic England as part of the National Heritage List for England; more than one site can be included in a single entry. While a scheduled monument can also be recognised as a listed building, Historic England's aim is to set the most appropriate form of protection in place for the building or site. Applications to deschedule a site are administered Historic England, who will carry out an assessment and make a recommendation to the Secretary of State. The metropolitan county of Greater Manchester is composed of 10 metropolitan boroughs: Bolton, Bury, Manchester, Oldham, Rochdale, Salford, Stockport, Tameside, Trafford and Wigan. Rochdale has no scheduled monuments; those in the other boroughs are listed separately. They range from prehistoric structures – the oldest of which date from the Bronze Age – to more modern structures such as the Astley Green Colliery, from 1908. Greater Manchester has seven prehistoric monuments (i.e. Bronze or Iron Age), found in Bury, Oldham, Salford, Stockport, and Tameside. The Bronze Age sites are mainly cairns and barrows, and both the Iron Age sites are military in nature, promontory forts. The trend of military sites continues from the Iron Age into the Roman period; two Roman forts in Greater Manchester are scheduled monuments and were the two main areas of Roman activity in the county. Of the nine castles in Greater Manchester, four are scheduled monuments: Buckton Castle, Watch Hill Castle, Bury Castle, and Radcliffe Tower. The last two are fortified manor houses, and although defined as castles were not exclusively military in nature; they probably acted as the administrative centre of the manors they were in. There are several other manor houses and country houses – some with moats – in the county that are protected as scheduled monuments. The Astley Green Colliery, the Marple Aqueduct, Oldknows Limekilns, and the Worsley Delph are scheduled relics of Greater Manchester's industrial history. (Full article...)

There are 37 scheduled monuments in Greater Manchester, a metropolitan county in North West England. In the United Kingdom, a scheduled monument is a "nationally important" archaeological site or historic building that has been given protection against unauthorised change by being placed on a list (or "schedule") by the Secretary of State for Digital Culture, Media and Sport; Historic England recommends sites for scheduling to the Secretary of State. Scheduled monuments are defined in the Ancient Monuments and Archaeological Areas Act 1979 and the National Heritage Act 1983. There are nearly 20,000 entries on the schedule, which is maintained by Historic England as part of the National Heritage List for England; more than one site can be included in a single entry. While a scheduled monument can also be recognised as a listed building, Historic England's aim is to set the most appropriate form of protection in place for the building or site. Applications to deschedule a site are administered Historic England, who will carry out an assessment and make a recommendation to the Secretary of State. The metropolitan county of Greater Manchester is composed of 10 metropolitan boroughs: Bolton, Bury, Manchester, Oldham, Rochdale, Salford, Stockport, Tameside, Trafford and Wigan. Rochdale has no scheduled monuments; those in the other boroughs are listed separately. They range from prehistoric structures – the oldest of which date from the Bronze Age – to more modern structures such as the Astley Green Colliery, from 1908. Greater Manchester has seven prehistoric monuments (i.e. Bronze or Iron Age), found in Bury, Oldham, Salford, Stockport, and Tameside. The Bronze Age sites are mainly cairns and barrows, and both the Iron Age sites are military in nature, promontory forts. The trend of military sites continues from the Iron Age into the Roman period; two Roman forts in Greater Manchester are scheduled monuments and were the two main areas of Roman activity in the county. Of the nine castles in Greater Manchester, four are scheduled monuments: Buckton Castle, Watch Hill Castle, Bury Castle, and Radcliffe Tower. The last two are fortified manor houses, and although defined as castles were not exclusively military in nature; they probably acted as the administrative centre of the manors they were in. There are several other manor houses and country houses – some with moats – in the county that are protected as scheduled monuments. The Astley Green Colliery, the Marple Aqueduct, Oldknows Limekilns, and the Worsley Delph are scheduled relics of Greater Manchester's industrial history. (Full article...)

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Monte Testaccio (Italian pronunciation: [ˈmonte teˈstattʃo]) or Monte Testaceo, also known as Monte dei Cocci, is an artificial mound in Rome composed almost entirely of testae (Italian: cocci), fragments of broken ancient Roman pottery, nearly all discarded amphorae dating from the time of the Roman Empire, some of which were labelled with tituli picti. It is one of the largest spoil heaps found anywhere in the ancient world, covering an area of 2 hectares (4.9 acres) at its base and with a volume of approximately 580,000 cubic metres (760,000 cu yd), containing the remains of an estimated 53 million amphorae. It has a circumference of nearly a kilometre (0.6 mi) and stands 35 metres (115 ft) high, though it was probably considerably higher in ancient times. It stands a short distance away from the east bank of the River Tiber, near the Horrea Galbae where the state-controlled reserve of olive oil was stored in the late 2nd century AD. The mound later had both religious and military significance. (Full article...)

Monte Testaccio (Italian pronunciation: [ˈmonte teˈstattʃo]) or Monte Testaceo, also known as Monte dei Cocci, is an artificial mound in Rome composed almost entirely of testae (Italian: cocci), fragments of broken ancient Roman pottery, nearly all discarded amphorae dating from the time of the Roman Empire, some of which were labelled with tituli picti. It is one of the largest spoil heaps found anywhere in the ancient world, covering an area of 2 hectares (4.9 acres) at its base and with a volume of approximately 580,000 cubic metres (760,000 cu yd), containing the remains of an estimated 53 million amphorae. It has a circumference of nearly a kilometre (0.6 mi) and stands 35 metres (115 ft) high, though it was probably considerably higher in ancient times. It stands a short distance away from the east bank of the River Tiber, near the Horrea Galbae where the state-controlled reserve of olive oil was stored in the late 2nd century AD. The mound later had both religious and military significance. (Full article...)

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The Mary Rose was a carrack in the English Tudor navy of King Henry VIII. She was launched in 1511 and served for 34 years in several wars against France, Scotland, and Brittany. After being substantially rebuilt in 1536, she saw her last action on 19 July 1545. She led the attack on the galleys of a French invasion fleet, but sank off Spithead in the Solent, the strait north of the Isle of Wight. The wreck of the Mary Rose was located in 1971 and was raised on 11 October 1982 by the Mary Rose Trust in one of the most complex and expensive maritime salvage projects in history. The surviving section of the ship and thousands of recovered artefacts are of great value as a Tudor period time capsule. The excavation and raising of the Mary Rose was a milestone in the field of maritime archaeology, comparable in complexity and cost to the raising of the 17th-century Swedish warship Vasa in 1961. The Mary Rose site is designated under the Protection of Wrecks Act 1973 by statutory instrument 1974/55. The wreck is a Protected Wreck managed by Historic England. The finds include weapons, sailing equipment, naval supplies, and a wide array of objects used by the crew. Many of the artefacts are unique to the Mary Rose and have provided insights into topics ranging from naval warfare to the history of musical instruments. The remains of the hull have been on display at the Portsmouth Historic Dockyard since the mid-1980s while undergoing restoration. An extensive collection of well-preserved artefacts is on display at the Mary Rose Museum, built to display the remains of the ship and her artefacts. Mary Rose was one of the largest ships in the English navy through more than three decades of intermittent war, and she was one of the earliest examples of a purpose-built sailing warship. She was armed with new types of heavy guns that could fire through the recently invented gun-ports. She was substantially rebuilt in 1536 and was also one of the earliest ships that could fire a broadside, although the line of battle tactics had not yet been developed. Several theories have sought to explain the demise of the Mary Rose, based on historical records, knowledge of 16th-century shipbuilding, and modern experiments. The precise cause of her sinking is subject to conflicting testimonies and a lack of conclusive evidence. (Full article...)

The Mary Rose was a carrack in the English Tudor navy of King Henry VIII. She was launched in 1511 and served for 34 years in several wars against France, Scotland, and Brittany. After being substantially rebuilt in 1536, she saw her last action on 19 July 1545. She led the attack on the galleys of a French invasion fleet, but sank off Spithead in the Solent, the strait north of the Isle of Wight. The wreck of the Mary Rose was located in 1971 and was raised on 11 October 1982 by the Mary Rose Trust in one of the most complex and expensive maritime salvage projects in history. The surviving section of the ship and thousands of recovered artefacts are of great value as a Tudor period time capsule. The excavation and raising of the Mary Rose was a milestone in the field of maritime archaeology, comparable in complexity and cost to the raising of the 17th-century Swedish warship Vasa in 1961. The Mary Rose site is designated under the Protection of Wrecks Act 1973 by statutory instrument 1974/55. The wreck is a Protected Wreck managed by Historic England. The finds include weapons, sailing equipment, naval supplies, and a wide array of objects used by the crew. Many of the artefacts are unique to the Mary Rose and have provided insights into topics ranging from naval warfare to the history of musical instruments. The remains of the hull have been on display at the Portsmouth Historic Dockyard since the mid-1980s while undergoing restoration. An extensive collection of well-preserved artefacts is on display at the Mary Rose Museum, built to display the remains of the ship and her artefacts. Mary Rose was one of the largest ships in the English navy through more than three decades of intermittent war, and she was one of the earliest examples of a purpose-built sailing warship. She was armed with new types of heavy guns that could fire through the recently invented gun-ports. She was substantially rebuilt in 1536 and was also one of the earliest ships that could fire a broadside, although the line of battle tactics had not yet been developed. Several theories have sought to explain the demise of the Mary Rose, based on historical records, knowledge of 16th-century shipbuilding, and modern experiments. The precise cause of her sinking is subject to conflicting testimonies and a lack of conclusive evidence. (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 north-west, 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 south-west, providing relief from the hot north-easterly 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 south-west 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 north-west, 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 south-west, providing relief from the hot north-easterly 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 south-west 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...)

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