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The untitled fourth studio album by the English rock band Led Zeppelin, commonly known as Led Zeppelin IV, was released on 8 November 1971, by Atlantic Records. It was produced by the band's guitarist, Jimmy Page, and recorded between December 1970 and February 1971, mostly in the country house Headley Grange. The album contains one of the band's most well-known recordings, the eight-minute-long "Stairway to Heaven".

The informal recording environment inspired the band, allowing them to try different arrangements of material and create songs in various styles. After the previous album Led Zeppelin III (1970) received lukewarm reviews from critics, they decided their fourth album would officially be untitled and represented instead by four symbols – one chosen by each band member – without featuring the name or any other details on the cover. Unlike the prior two albums, the band was joined by guest musicians: singer Sandy Denny on "The Battle of Evermore", and pianist Ian Stewart on "Rock and Roll". As with prior albums, most of the material was written by the band, though there was one cover song, a hard rock re-interpretation of the Memphis Minnie blues song "When the Levee Breaks".

The untitled fourth studio album by the English rock band Led Zeppelin, commonly known as Led Zeppelin IV, was released on 8 November 1971, by Atlantic Records. It was produced by the band's guitarist, Jimmy Page, and recorded between December 1970 and February 1971, mostly in the country house Headley Grange. The album contains one of the band's most well-known recordings, the eight-minute-long "Stairway to Heaven".

The informal recording environment inspired the band, allowing them to try different arrangements of material and create songs in various styles. After the previous album Led Zeppelin III (1970) received lukewarm reviews from critics, they decided their fourth album would officially be untitled and represented instead by four symbols – one chosen by each band member – without featuring the name or any other details on the cover. Unlike the prior two albums, the band was joined by guest musicians: singer Sandy Denny on "The Battle of Evermore", and pianist Ian Stewart on "Rock and Roll". As with prior albums, most of the material was written by the band, though there was one cover song, a hard rock re-interpretation of the Memphis Minnie blues song "When the Levee Breaks".

Stanley Casson FSA (1889 – 17 April 1944) was an English classical archaeologist. He published widely on the history, culture, art and archaeology of Greece, and conducted excavations in Greece and in Constantinople. He served as a staff officer during the First World War and in military intelligence during the Second World War.

Educated at Ipswich School and at Merchant Taylors' School in Hertfordshire, Casson attended Lincoln College, Oxford, on an exhibition, where he studied both archaeology and anthropology. He continued his studies at St John's College, Oxford, and the British School at Athens (BSA), where he pursued a then-unusual interest in modern Greek historical anthropology. During the First World War, he served as an officer in the East Lancashire Regiment, and was wounded on the Western Front in 1915. He subsequently transferred as a staff officer to the Macedonian front under George Milne, where he undertook archaeological excavations at Chauchitza and helped to establish the rules and procedures for heritage protection in the area during wartime. He also served in Turkestan, was one of the first Allied officers to enter Constantinople after the Ottoman surrender of November 1918, and was mentioned in despatches.

Following his demobilisation, Casson became the assistant director of the BSA from 1919 until 1922, took a fellowship in 1920 at New College, Oxford, and lectured widely in person and on BBC radio on archaeological matters. During the inter-war period, he carried out excavations on behalf of the British Academy in the Hippodrome of Constantinople, and held temporary posts at the University of Bristol and at Bowdoin College in the United States. He returned to military service shortly before the outbreak of the Second World War in September 1939, joining the Intelligence Corps as an officer and instructor. He was almost captured during the German invasion of the Netherlands in May 1940, and was subsequently posted to Greece as the chief intelligence officer of No. 27 Military Mission, the British reporting mission to the country. In Greece, he served on the staff of Henry Maitland Wilson and was again almost captured during the Battle of Crete in May 1941. He subsequently joined the Special Operations Executive (SOE), and was serving as the SOE's liaison officer in Greece when he was killed in an aircraft crash on 17 April 1944.

Stanley Casson FSA (1889 – 17 April 1944) was an English classical archaeologist. He published widely on the history, culture, art and archaeology of Greece, and conducted excavations in Greece and in Constantinople. He served as a staff officer during the First World War and in military intelligence during the Second World War.

Educated at Ipswich School and at Merchant Taylors' School in Hertfordshire, Casson attended Lincoln College, Oxford, on an exhibition, where he studied both archaeology and anthropology. He continued his studies at St John's College, Oxford, and the British School at Athens (BSA), where he pursued a then-unusual interest in modern Greek historical anthropology. During the First World War, he served as an officer in the East Lancashire Regiment, and was wounded on the Western Front in 1915. He subsequently transferred as a staff officer to the Macedonian front under George Milne, where he undertook archaeological excavations at Chauchitza and helped to establish the rules and procedures for heritage protection in the area during wartime. He also served in Turkestan, was one of the first Allied officers to enter Constantinople after the Ottoman surrender of November 1918, and was mentioned in despatches.

Following his demobilisation, Casson became the assistant director of the BSA from 1919 until 1922, took a fellowship in 1920 at New College, Oxford, and lectured widely in person and on BBC radio on archaeological matters. During the inter-war period, he carried out excavations on behalf of the British Academy in the Hippodrome of Constantinople, and held temporary posts at the University of Bristol and at Bowdoin College in the United States. He returned to military service shortly before the outbreak of the Second World War in September 1939, joining the Intelligence Corps as an officer and instructor. He was almost captured during the German invasion of the Netherlands in May 1940, and was subsequently posted to Greece as the chief intelligence officer of No. 27 Military Mission, the British reporting mission to the country. In Greece, he served on the staff of Henry Maitland Wilson and was again almost captured during the Battle of Crete in May 1941. He subsequently joined the Special Operations Executive (SOE), and was serving as the SOE's liaison officer in Greece when he was killed in an aircraft crash on 17 April 1944.

The tomb of Tutankhamun (reigned c. 1332–1323 BC), a pharaoh of the Eighteenth Dynasty of ancient Egypt, is located in the Valley of the Kings. The tomb, also known by its tomb number KV62, consists of four chambers and an entrance staircase and corridor. It is smaller and less extensively decorated than other Egyptian royal tombs of its time, and it probably originated as a tomb for a non-royal individual that was adapted for Tutankhamun's use after his premature death. Like other pharaohs, Tutankhamun was buried with a wide variety of funerary objects and personal possessions, such as coffins, furniture, clothing and jewelry, though in the unusually limited space these goods had to be densely packed. Robbers entered the tomb twice in the years immediately following the burial, but Tutankhamun's mummy and most of the burial goods remained intact. The tomb's low position, dug into the floor of the valley, allowed its entrance to be hidden by debris deposited by flooding and tomb construction. Thus, unlike other tombs in the valley, it was not stripped of its valuables during the Third Intermediate Period (c. 1070–664 BC).

Tutankhamun's tomb was discovered in 1922 by excavators led by George Herbert, 5th Earl of Carnarvon and Howard Carter. As a result of the quantity and spectacular appearance of the burial goods, the tomb attracted a media frenzy and became the most famous find in the history of Egyptology. The discovery produced only limited evidence about the history of Tutankhamun's reign and the Amarna Period that preceded it, but it provided insight into the material culture of wealthy ancient Egyptians as well as patterns of ancient tomb robbery. Tutankhamun became one of the best-known pharaohs, and some artefacts from his tomb, such as his golden funerary mask, are among the best-known artworks from ancient Egypt.

The tomb of Tutankhamun (reigned c. 1332–1323 BC), a pharaoh of the Eighteenth Dynasty of ancient Egypt, is located in the Valley of the Kings. The tomb, also known by its tomb number KV62, consists of four chambers and an entrance staircase and corridor. It is smaller and less extensively decorated than other Egyptian royal tombs of its time, and it probably originated as a tomb for a non-royal individual that was adapted for Tutankhamun's use after his premature death. Like other pharaohs, Tutankhamun was buried with a wide variety of funerary objects and personal possessions, such as coffins, furniture, clothing and jewelry, though in the unusually limited space these goods had to be densely packed. Robbers entered the tomb twice in the years immediately following the burial, but Tutankhamun's mummy and most of the burial goods remained intact. The tomb's low position, dug into the floor of the valley, allowed its entrance to be hidden by debris deposited by flooding and tomb construction. Thus, unlike other tombs in the valley, it was not stripped of its valuables during the Third Intermediate Period (c. 1070–664 BC).

Tutankhamun's tomb was discovered in 1922 by excavators led by George Herbert, 5th Earl of Carnarvon and Howard Carter. As a result of the quantity and spectacular appearance of the burial goods, the tomb attracted a media frenzy and became the most famous find in the history of Egyptology. The discovery produced only limited evidence about the history of Tutankhamun's reign and the Amarna Period that preceded it, but it provided insight into the material culture of wealthy ancient Egyptians as well as patterns of ancient tomb robbery. Tutankhamun became one of the best-known pharaohs, and some artefacts from his tomb, such as his golden funerary mask, are among the best-known artworks from ancient Egypt.

Kronan, also called Stora Kronan, was a Swedish warship that served as the flagship of the Swedish Navy in the Baltic Sea in the 1670s. When built, she was one of the largest seagoing vessels in the world. The construction of Kronan lasted from 1668 to 1672 and was delayed by difficulties with financing and conflicts between the shipwright Francis Sheldon and the Swedish admiralty. After four years of service, the ship sank in rough weather at the Battle of Öland on 1 June 1676: while making a sharp turn under too much sail she capsized, and the gunpowder magazine ignited and blew off most of the bow. Kronan sank quickly, taking about 800 men and more than 100 guns with her, along with valuable military equipment, weapons, personal items, and large quantities of silver and gold coins.

The loss of Kronan was a heavy blow for Sweden during the Scanian War. Besides being the largest and most heavily armed ship in the Swedish Navy, she had been an important status symbol for the monarchy of the young Charles XI. Along with Kronan, the navy lost a sizeable proportion of its best manpower, acting supreme commander Lorentz Creutz, numerous high-ranking fleet officers, and the chief of the navy medical staff. A commission was set up to investigate whether any individuals could be held responsible for the defeat at the Battle of Öland and other major defeats during the war.

Kronan, also called Stora Kronan, was a Swedish warship that served as the flagship of the Swedish Navy in the Baltic Sea in the 1670s. When built, she was one of the largest seagoing vessels in the world. The construction of Kronan lasted from 1668 to 1672 and was delayed by difficulties with financing and conflicts between the shipwright Francis Sheldon and the Swedish admiralty. After four years of service, the ship sank in rough weather at the Battle of Öland on 1 June 1676: while making a sharp turn under too much sail she capsized, and the gunpowder magazine ignited and blew off most of the bow. Kronan sank quickly, taking about 800 men and more than 100 guns with her, along with valuable military equipment, weapons, personal items, and large quantities of silver and gold coins.

The loss of Kronan was a heavy blow for Sweden during the Scanian War. Besides being the largest and most heavily armed ship in the Swedish Navy, she had been an important status symbol for the monarchy of the young Charles XI. Along with Kronan, the navy lost a sizeable proportion of its best manpower, acting supreme commander Lorentz Creutz, numerous high-ranking fleet officers, and the chief of the navy medical staff. A commission was set up to investigate whether any individuals could be held responsible for the defeat at the Battle of Öland and other major defeats during the war.

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.