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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.

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.

Château Gaillard (French pronunciation: [ʃɑto ɡajaʁ]) is a medieval castle ruin overlooking the River Seine above the commune of Les Andelys, in the French department of Eure, in Normandy. It is located some 95 kilometres (59 mi) north-west of Paris and 40 kilometres (25 mi) from Rouen. Construction began in 1196 under the auspices of Richard the Lionheart, who was simultaneously King of England and feudal Duke of Normandy. The castle was expensive to build, but the majority of the work was done in an unusually short period of time. It took just two years and, at the same time, the town of Petit Andely was constructed. Château Gaillard has a complex and advanced design, and uses early principles of concentric fortification; it was also one of the earliest European castles to use machicolations. The castle consists of three enclosures separated by dry moats, with a keep in the inner enclosure.

Château Gaillard (French pronunciation: [ʃɑto ɡajaʁ]) is a medieval castle ruin overlooking the River Seine above the commune of Les Andelys, in the French department of Eure, in Normandy. It is located some 95 kilometres (59 mi) north-west of Paris and 40 kilometres (25 mi) from Rouen. Construction began in 1196 under the auspices of Richard the Lionheart, who was simultaneously King of England and feudal Duke of Normandy. The castle was expensive to build, but the majority of the work was done in an unusually short period of time. It took just two years and, at the same time, the town of Petit Andely was constructed. Château Gaillard has a complex and advanced design, and uses early principles of concentric fortification; it was also one of the earliest European castles to use machicolations. The castle consists of three enclosures separated by dry moats, with a keep in the inner enclosure.

The Gevninge helmet fragment is the dexter eyepiece of a helmet from the Viking Age or end of the Nordic Iron Age. It was found in 2000 during the excavation of a Viking farmstead in Gevninge, near Lejre, Denmark. The fragment is moulded from bronze and gilded, and consists of a stylised eyebrow with eyelashes above an oval opening. There are three holes at the top and bottom of the fragment to affix the eyepiece to a helmet. The fragment is significant as rare evidence of contemporaneous helmets, and also for its discovery in Gevninge, an outpost that is possibly connected to the Anglo-Saxon epic Beowulf. It has been in the collection of the Lejre Museum since its discovery, and has been exhibited internationally as part of a travelling exhibition on Vikings.

The fragment is an ornate piece, but nothing else remains of the helmet; it might be the single remnant of a disintegrated helmet, or it might have been lost or discarded. It is one of two Scandinavian eyepieces discovered alone, giving rise to the suggestion that it was intentionally deposited in an invocation of the one-eyed god Odin. It would have been part of a decorated "crested helmet", the type of headgear that was common to England and Scandinavia from the sixth through eleventh centuries AD. These are particularly known from the examples found at Vendel, Valsgärde, and Sutton Hoo; the Tjele helmet fragment is the only other Danish example known.

The Gevninge helmet fragment is the dexter eyepiece of a helmet from the Viking Age or end of the Nordic Iron Age. It was found in 2000 during the excavation of a Viking farmstead in Gevninge, near Lejre, Denmark. The fragment is moulded from bronze and gilded, and consists of a stylised eyebrow with eyelashes above an oval opening. There are three holes at the top and bottom of the fragment to affix the eyepiece to a helmet. The fragment is significant as rare evidence of contemporaneous helmets, and also for its discovery in Gevninge, an outpost that is possibly connected to the Anglo-Saxon epic Beowulf. It has been in the collection of the Lejre Museum since its discovery, and has been exhibited internationally as part of a travelling exhibition on Vikings.

The fragment is an ornate piece, but nothing else remains of the helmet; it might be the single remnant of a disintegrated helmet, or it might have been lost or discarded. It is one of two Scandinavian eyepieces discovered alone, giving rise to the suggestion that it was intentionally deposited in an invocation of the one-eyed god Odin. It would have been part of a decorated "crested helmet", the type of headgear that was common to England and Scandinavia from the sixth through eleventh centuries AD. These are particularly known from the examples found at Vendel, Valsgärde, and Sutton Hoo; the Tjele helmet fragment is the only other Danish example known.

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.

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.