Grave Circle A is a 16th-century BC royal cemetery situated to the south of the Lion Gate, the main entrance of the Bronze Age citadel of Mycenae in southern Greece. This burial complex was initially constructed outside the walls of Mycenae and ultimately enclosed in the acropolis when the fortification was extended during the 13th century BC. Grave Circle A and Grave Circle B, the latter found outside the walls of Mycenae, represents one of the significant characteristics of the early phase of the Mycenaean civilization.

The site circle has a diameter of 27.5 m (90ft) and contains six shaft graves. The largest of the shaft graves measures about 6.5 m (21 ft 3 in) in length and about 4.1 m (13 ft 6 in) in width. A total of nineteen bodies of men, women, and children buried here, with two to five bodies per shaft. It has been suggested that a mound was constructed over each grave, and funeral stelae were erected. Among the funerary gifts found were a series of gold death masks, full sets of weapons, ornate staffs, gold jewelry, as well as gold and silver cups. The funerary gifts found here are more precious than that of those at Grave Circle B. It has been estimated that Circle A contained about 15 kilos of gold in total (not all of high purity); a considerable quantity, but a good deal less than in just the inner coffin of Tutankhamun.

The site was excavated by the archaeologist Heinrich Schliemann and Panagiotis Stamatakis in 1876–77, following the descriptions of Homer and Pausanias. One of the five gold death masks he unearthed became known as "The Death Mask of Agamemnon", ruler of Mycenae, of Greek mythology. However, it has been proven that the burials are dated approximately three centuries earlier before Agamemnon is supposed to have lived.

Grave Circle A is a 16th-century BC royal cemetery situated to the south of the Lion Gate, the main entrance of the Bronze Age citadel of Mycenae in southern Greece. This burial complex was initially constructed outside the walls of Mycenae and ultimately enclosed in the acropolis when the fortification was extended during the 13th century BC. Grave Circle A and Grave Circle B, the latter found outside the walls of Mycenae, represents one of the significant characteristics of the early phase of the Mycenaean civilization.

The site circle has a diameter of 27.5 m (90ft) and contains six shaft graves. The largest of the shaft graves measures about 6.5 m (21 ft 3 in) in length and about 4.1 m (13 ft 6 in) in width. A total of nineteen bodies of men, women, and children buried here, with two to five bodies per shaft. It has been suggested that a mound was constructed over each grave, and funeral stelae were erected. Among the funerary gifts found were a series of gold death masks, full sets of weapons, ornate staffs, gold jewelry, as well as gold and silver cups. The funerary gifts found here are more precious than that of those at Grave Circle B. It has been estimated that Circle A contained about 15 kilos of gold in total (not all of high purity); a considerable quantity, but a good deal less than in just the inner coffin of Tutankhamun.

The site was excavated by the archaeologist Heinrich Schliemann and Panagiotis Stamatakis in 1876–77, following the descriptions of Homer and Pausanias. One of the five gold death masks he unearthed became known as "The Death Mask of Agamemnon", ruler of Mycenae, of Greek mythology. However, it has been proven that the burials are dated approximately three centuries earlier before Agamemnon is supposed to have lived.

Rempstone Stone Circle (grid reference SY994820) is a stone circle located near to Corfe Castle on the Isle of Purbeck in the south-western English county of Dorset. Archaeologists believe that it was likely erected during the Bronze Age. The Rempstone ring is part of a tradition of stone circle construction that spread throughout much of Britain, Ireland, and Brittany during the Late Neolithic and Early Bronze Age, over a period between 3,300 and 900 BC. The purpose of such monuments is unknown, although archaeologists speculate that they were likely religious sites, with the stones perhaps having supernatural associations for those who built the circles. Local folklore holds that the stones arrived in their position after being thrown at Corfe Castle by the Devil.

Rempstone Stone Circle (grid reference SY994820) is a stone circle located near to Corfe Castle on the Isle of Purbeck in the south-western English county of Dorset. Archaeologists believe that it was likely erected during the Bronze Age. The Rempstone ring is part of a tradition of stone circle construction that spread throughout much of Britain, Ireland, and Brittany during the Late Neolithic and Early Bronze Age, over a period between 3,300 and 900 BC. The purpose of such monuments is unknown, although archaeologists speculate that they were likely religious sites, with the stones perhaps having supernatural associations for those who built the circles. Local folklore holds that the stones arrived in their position after being thrown at Corfe Castle by the Devil.

Norton Priory is a historic site in Norton, Runcorn, Cheshire, England, comprising the remains of an abbey complex dating from the 12th to 16th centuries, and an 18th-century country house; it is now a museum. The remains are a scheduled ancient monument and are recorded in the National Heritage List for England as a designated Grade I listed building. They are considered to be the most important monastic remains in Cheshire.

The priory was established as an Augustinian foundation in the 12th century, and was raised to the status of an abbey in 1391. The abbey was closed in 1536, as part of the dissolution of the monasteries. Nine years later the surviving structures, together with the manor of Norton, were purchased by Sir Richard Brooke, who built a Tudor house on the site, incorporating part of the abbey. This was replaced in the 18th century by a Georgian house. The Brooke family left the house in 1921, and it was partially demolished in 1928. In 1966 the site was given in trust for the use of the general public.

Excavation of the site began in 1971, and became the largest to be carried out by modern methods on any European monastic site. It revealed the foundations and lower parts of the walls of the monastery buildings and the abbey church. Important finds included: a Norman doorway; a finely carved arcade; a floor of mosaic tiles, the largest floor area of this type to be found in any modern excavation; the remains of the kiln where the tiles were fired; a bell casting pit used for casting the bell; and a large medieval statue of Saint Christopher.

Norton Priory is a historic site in Norton, Runcorn, Cheshire, England, comprising the remains of an abbey complex dating from the 12th to 16th centuries, and an 18th-century country house; it is now a museum. The remains are a scheduled ancient monument and are recorded in the National Heritage List for England as a designated Grade I listed building. They are considered to be the most important monastic remains in Cheshire.

The priory was established as an Augustinian foundation in the 12th century, and was raised to the status of an abbey in 1391. The abbey was closed in 1536, as part of the dissolution of the monasteries. Nine years later the surviving structures, together with the manor of Norton, were purchased by Sir Richard Brooke, who built a Tudor house on the site, incorporating part of the abbey. This was replaced in the 18th century by a Georgian house. The Brooke family left the house in 1921, and it was partially demolished in 1928. In 1966 the site was given in trust for the use of the general public.

Excavation of the site began in 1971, and became the largest to be carried out by modern methods on any European monastic site. It revealed the foundations and lower parts of the walls of the monastery buildings and the abbey church. Important finds included: a Norman doorway; a finely carved arcade; a floor of mosaic tiles, the largest floor area of this type to be found in any modern excavation; the remains of the kiln where the tiles were fired; a bell casting pit used for casting the bell; and a large medieval statue of Saint Christopher.

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 northwest, 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 southwest, providing relief from the hot northeasterly 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 southwest 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.

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 northwest, 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 southwest, providing relief from the hot northeasterly 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 southwest 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.