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[untitled] is the fourth EP by American indie rock band mewithoutYou. The record was produced by Will Yip. On August 13, 2018, mewithoutYou released the first single off of the not-yet-announced [Untitled], "Julia (or, 'Holy to the LORD' on the Bells of Horses)." At the same time of the single's release, the band tweeted a link to a page on their website containing only a countdown timer. The timer finished at 12:00 am Eastern time (05:00 UTC) on August 17, 2018 and the band announced they would be releasing their seventh studio album, [Untitled], on October 5, 2018. In addition to the full length album announcement, mewithoutYou digitally released a "partner" EP named [untitled]. (Full article...)

[untitled] is the fourth EP by American indie rock band mewithoutYou. The record was produced by Will Yip. On August 13, 2018, mewithoutYou released the first single off of the not-yet-announced [Untitled], "Julia (or, 'Holy to the LORD' on the Bells of Horses)." At the same time of the single's release, the band tweeted a link to a page on their website containing only a countdown timer. The timer finished at 12:00 am Eastern time (05:00 UTC) on August 17, 2018 and the band announced they would be releasing their seventh studio album, [Untitled], on October 5, 2018. In addition to the full length album announcement, mewithoutYou digitally released a "partner" EP named [untitled]. (Full article...)

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Panagiotis Kavvadias or Cawadias (Greek: Παναγιώτης Καββαδίας; 14 May [O.S. 2 May] 1850 – 20 July 1928) was a Greek archaeologist. He was responsible for the excavation of ancient sites in Greece, including Epidaurus in Argolis and the Acropolis of Athens, as well as archaeological discoveries on his native island of Kephallonia. As Ephor General (the head of the Greek Archaeological Service) from 1885 until 1909, Kavvadias oversaw the expansion of the Archaeological Service and the introduction of Law 2646 of 1899, which increased the state's powers to address the illegal excavation and smuggling of antiquities. Kavvadias's work had a particular impact on the Acropolis of Athens, and has been credited with completing its "transformation [...] from castle to monument". Between 1885 and 1890, he removed almost all of the Acropolis's remaining medieval and modern structures, uncovering many ancient monuments in the process. He also played a role in the extensive reconstruction of the site by the architect and engineer Nikolaos Balanos. Though praised initially, the work caused considerable damage to several monuments and was almost completely deconstructed and rebuilt during the later 20th and early 21st centuries. Kavvadias oversaw the opening of the National Archaeological Museum in Athens, organised its first collections, and wrote some of its first catalogues. As an administrator, Kavvadias was regarded as energetic, centralising and autocratic. His career saw significant modernisation in the practice of archaeology in Greece, and he reformed and professionalised the Archaeological Service. His patronage of Athens's foreign archaeological schools was credited with promoting the development of Greek archaeology, but was also criticised by native Greek archaeologists. He created further discontent among the Archaeological Society of Athens by reducing its role in favour of the governmental Archaeological Service. After the Goudi coup of 1909, dissatisfaction in the Greek press and among his subordinates in the Archaeological Service led to his removal from office, from the Archaeological Society and from his professorship at the University of Athens, though he was able to return to public and academic life from 1912, and remained active in Greek archaeology until his death in 1928. (Full article...)

Panagiotis Kavvadias or Cawadias (Greek: Παναγιώτης Καββαδίας; 14 May [O.S. 2 May] 1850 – 20 July 1928) was a Greek archaeologist. He was responsible for the excavation of ancient sites in Greece, including Epidaurus in Argolis and the Acropolis of Athens, as well as archaeological discoveries on his native island of Kephallonia. As Ephor General (the head of the Greek Archaeological Service) from 1885 until 1909, Kavvadias oversaw the expansion of the Archaeological Service and the introduction of Law 2646 of 1899, which increased the state's powers to address the illegal excavation and smuggling of antiquities. Kavvadias's work had a particular impact on the Acropolis of Athens, and has been credited with completing its "transformation [...] from castle to monument". Between 1885 and 1890, he removed almost all of the Acropolis's remaining medieval and modern structures, uncovering many ancient monuments in the process. He also played a role in the extensive reconstruction of the site by the architect and engineer Nikolaos Balanos. Though praised initially, the work caused considerable damage to several monuments and was almost completely deconstructed and rebuilt during the later 20th and early 21st centuries. Kavvadias oversaw the opening of the National Archaeological Museum in Athens, organised its first collections, and wrote some of its first catalogues. As an administrator, Kavvadias was regarded as energetic, centralising and autocratic. His career saw significant modernisation in the practice of archaeology in Greece, and he reformed and professionalised the Archaeological Service. His patronage of Athens's foreign archaeological schools was credited with promoting the development of Greek archaeology, but was also criticised by native Greek archaeologists. He created further discontent among the Archaeological Society of Athens by reducing its role in favour of the governmental Archaeological Service. After the Goudi coup of 1909, dissatisfaction in the Greek press and among his subordinates in the Archaeological Service led to his removal from office, from the Archaeological Society and from his professorship at the University of Athens, though he was able to return to public and academic life from 1912, and remained active in Greek archaeology until his death in 1928. (Full article...)

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Krak des Chevaliers (French: [kʁak de ʃ(ə)valje]; Arabic: قلعة الحصن, romanized: Qalʿat al-Ḥiṣn, Arabic: [ˈqalʕat alˈħisˤn]; Old French: Crac des Chevaliers or Crac de l'Ospital, lit. 'karak [fortress] of the hospital'; from Classical Syriac: ܟܪܟܐ, romanized: karəḵā, lit. 'walled city') is a medieval castle in Syria and one of the most important preserved medieval castles in the world. The site was first inhabited in the 11th century by Kurdish troops garrisoned there by the Mirdasids. In 1142 it was given by Raymond II, Count of Tripoli, to the order of the Knights Hospitaller. It remained occupied by them until it was reconquered by the Muslims in 1271. The Hospitallers began rebuilding the castle in the 1140s and were finished by 1170 when an earthquake damaged the castle. The order controlled castles along the border of the County of Tripoli, a state founded after the First Crusade. Krak des Chevaliers was among the most important and acted as a center of administration as well as a military base. After a second phase of building was undertaken in the 13th century, Krak des Chevaliers became a concentric castle. This phase created the outer wall and gave the castle its current appearance. The first half of the century has been described as Krak des Chevaliers' "golden age". At its peak, Krak des Chevaliers housed a garrison of around 2,000. Such a large garrison allowed the Hospitallers to exact tribute from a wide area. From the 1250s the fortunes of the Knights Hospitaller took a turn for the worse and in 1271 the Mamluk Sultanate captured Krak des Chevaliers after a siege lasting 36 days, supposedly by way of a forged letter purportedly from the Hospitallers' Grand Master that caused the knights to surrender. Renewed interest in Crusader castles in the 19th century led to the investigation of Krak des Chevaliers, and architectural plans were drawn up. In the late 19th or early 20th century a settlement had been created within the castle, causing damage to its fabric. The 500 inhabitants were moved in 1933 and the castle was given over to the French Alawite State, which carried out a program of clearing and restoration. When Syria declared independence in 1946, it assumed control. Today, the village of al-Husn exists around the castle and has a population of nearly 9,000. Krak des Chevaliers is approximately 40 kilometres (25 mi) west of the city of Homs, close to the border of Lebanon, and is administratively part of the Homs Governorate. Since 2006, the castles of Krak des Chevaliers and Qal'at Salah El-Din have been recognised by UNESCO as World Heritage Sites. It was partially damaged in the Syrian civil war from shelling and recaptured by the Syrian government forces in 2014. Since then, reconstruction and conservation work on the site had begun. Reports by UNESCO and the Syrian government on the state of the site are produced yearly. (Full article...)

Krak des Chevaliers (French: [kʁak de ʃ(ə)valje]; Arabic: قلعة الحصن, romanized: Qalʿat al-Ḥiṣn, Arabic: [ˈqalʕat alˈħisˤn]; Old French: Crac des Chevaliers or Crac de l'Ospital, lit. 'karak [fortress] of the hospital'; from Classical Syriac: ܟܪܟܐ, romanized: karəḵā, lit. 'walled city') is a medieval castle in Syria and one of the most important preserved medieval castles in the world. The site was first inhabited in the 11th century by Kurdish troops garrisoned there by the Mirdasids. In 1142 it was given by Raymond II, Count of Tripoli, to the order of the Knights Hospitaller. It remained occupied by them until it was reconquered by the Muslims in 1271. The Hospitallers began rebuilding the castle in the 1140s and were finished by 1170 when an earthquake damaged the castle. The order controlled castles along the border of the County of Tripoli, a state founded after the First Crusade. Krak des Chevaliers was among the most important and acted as a center of administration as well as a military base. After a second phase of building was undertaken in the 13th century, Krak des Chevaliers became a concentric castle. This phase created the outer wall and gave the castle its current appearance. The first half of the century has been described as Krak des Chevaliers' "golden age". At its peak, Krak des Chevaliers housed a garrison of around 2,000. Such a large garrison allowed the Hospitallers to exact tribute from a wide area. From the 1250s the fortunes of the Knights Hospitaller took a turn for the worse and in 1271 the Mamluk Sultanate captured Krak des Chevaliers after a siege lasting 36 days, supposedly by way of a forged letter purportedly from the Hospitallers' Grand Master that caused the knights to surrender. Renewed interest in Crusader castles in the 19th century led to the investigation of Krak des Chevaliers, and architectural plans were drawn up. In the late 19th or early 20th century a settlement had been created within the castle, causing damage to its fabric. The 500 inhabitants were moved in 1933 and the castle was given over to the French Alawite State, which carried out a program of clearing and restoration. When Syria declared independence in 1946, it assumed control. Today, the village of al-Husn exists around the castle and has a population of nearly 9,000. Krak des Chevaliers is approximately 40 kilometres (25 mi) west of the city of Homs, close to the border of Lebanon, and is administratively part of the Homs Governorate. Since 2006, the castles of Krak des Chevaliers and Qal'at Salah El-Din have been recognised by UNESCO as World Heritage Sites. It was partially damaged in the Syrian civil war from shelling and recaptured by the Syrian government forces in 2014. Since then, reconstruction and conservation work on the site had begun. Reports by UNESCO and the Syrian government on the state of the site are produced yearly. (Full article...)

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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 hard 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. Most of the guns that sank with Kronan were salvaged in the 1680s, but eventually the wreck fell into obscurity. Its exact position was rediscovered in 1980 by the amateur researcher Anders Franzén, who had also located the 17th-century warship Vasa in the 1950s. Yearly diving operations have since surveyed and excavated the wreck site and salvaged artifacts, and Kronan has become the most widely publicized shipwreck in the Baltic after Vasa. More than 30,000 artifacts have been recovered, and many have been conserved and put on permanent public display at the Kalmar County Museum in Kalmar. The museum is responsible for the maritime archaeological operations and the permanent exhibitions on Kronan. (Full article...)

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 hard 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. Most of the guns that sank with Kronan were salvaged in the 1680s, but eventually the wreck fell into obscurity. Its exact position was rediscovered in 1980 by the amateur researcher Anders Franzén, who had also located the 17th-century warship Vasa in the 1950s. Yearly diving operations have since surveyed and excavated the wreck site and salvaged artifacts, and Kronan has become the most widely publicized shipwreck in the Baltic after Vasa. More than 30,000 artifacts have been recovered, and many have been conserved and put on permanent public display at the Kalmar County Museum in Kalmar. The museum is responsible for the maritime archaeological operations and the permanent exhibitions on Kronan. (Full article...)

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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. The sea temperature in Melbourne is warmer than the surrounding ocean during the summer months, and colder during the winter months. This is predominantly due to Port Phillip Bay being an enclosed and shallow bay that is largely protected from the ocean, resulting in greater temperature variation across seasons. (Full article...)

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. The sea temperature in Melbourne is warmer than the surrounding ocean during the summer months, and colder during the winter months. This is predominantly due to Port Phillip Bay being an enclosed and shallow bay that is largely protected from the ocean, resulting in greater temperature variation across seasons. (Full article...)

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