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The United Nations Educational, Scientific and Cultural Organization (UNESCO) World Heritage Sites are places of importance to cultural or natural heritage as described in the UNESCO World Heritage Convention, established in 1972. Vietnam accepted the convention on 19 October 1987, making its natural and cultural sites eligible for inclusion on the list. As of 2023, there are eight World Heritage Sites in Vietnam, including five cultural sites, two natural sites, and one mixed. Vietnam holds the second-highest number of World Heritage Sites in Southeast Asia, after Indonesia with ten sites. The Complex of Huế Monuments was the first site in Vietnam to be inscribed on the list at the 17th session of the World Heritage Committee held in Colombia in 1993. Two cultural sites from Quảng Nam were listed in 1999: Hội An Ancient Town and Mỹ Sơn Sanctuary. Hạ Long Bay and Phong Nha – Kẻ Bàng National Park were listed as natural sites in 1994 and 2003, respectively, before receiving the extension on the criteria for exceptional geological and geomorphologic values by the World Heritage Committee in 2000 and 2015. The Central Sector of Imperial Citadel of Thăng Long was inscribed in 2010, coinciding with the Millennial Anniversary of the Thăng Long capital. The most recent site added was Tràng An Scenic Landscape Complex in 2016, the first mixed site in Southeast Asia. After being recognized, the sites became popular tourist attractions. They are also considered to be driving forces behind the growth of tourism in the country. According to the Ministry of Culture, Sports and Tourism, Tràng An was the most popular World Heritage Site in Vietnam, attracted more than 6 million visitors and raised 867.5 million VND in 2019 alone. In addition to its World Heritage Sites, Vietnam also maintains seven properties on its tentative list. (Full article...) |
The United Nations Educational, Scientific and Cultural Organization (UNESCO) World Heritage Sites are places of importance to cultural or natural heritage as described in the UNESCO World Heritage Convention, established in 1972. Vietnam accepted the convention on 19 October 1987, making its natural and cultural sites eligible for inclusion on the list. As of 2023, there are eight World Heritage Sites in Vietnam, including five cultural sites, two natural sites, and one mixed. Vietnam holds the second-highest number of World Heritage Sites in Southeast Asia, after Indonesia with ten sites. The Complex of Huế Monuments was the first site in Vietnam to be inscribed on the list at the 17th session of the World Heritage Committee held in Colombia in 1993. Two cultural sites from Quảng Nam were listed in 1999: Hội An Ancient Town and Mỹ Sơn Sanctuary. Hạ Long Bay and Phong Nha – Kẻ Bàng National Park were listed as natural sites in 1994 and 2003, respectively, before receiving the extension on the criteria for exceptional geological and geomorphologic values by the World Heritage Committee in 2000 and 2015. The Central Sector of Imperial Citadel of Thăng Long was inscribed in 2010, coinciding with the Millennial Anniversary of the Thăng Long capital. The most recent site added was Tràng An Scenic Landscape Complex in 2016, the first mixed site in Southeast Asia. After being recognized, the sites became popular tourist attractions. They are also considered to be driving forces behind the growth of tourism in the country. According to the Ministry of Culture, Sports and Tourism, Tràng An was the most popular World Heritage Site in Vietnam, attracted more than 6 million visitors and raised 867.5 million VND in 2019 alone. In addition to its World Heritage Sites, Vietnam also maintains seven properties on its tentative list. (Full article...) |
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Kingston Russell Stone Circle, also known as the Gorwell Circle, is a stone circle located between the villages of Abbotsbury and Littlebredy in the south-western English county of Dorset. Archaeologists believe that it was likely erected during the Bronze Age. The Kingston Russell 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 BCE. 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. A number of these circles were built in the area around modern Dorset, typically being constructed from sarsen stone and being smaller than those found elsewhere. The Kingston Russell ring is the largest of those in Dorset, measuring 24 by 27 metres (79 feet by 89 feet) in diameter and containing eighteen sarsen stones arranged in an oval shape. The site has not been excavated or been subject to in-depth archaeological investigation. (Full article...) |
Kingston Russell Stone Circle, also known as the Gorwell Circle, is a stone circle located between the villages of Abbotsbury and Littlebredy in the south-western English county of Dorset. Archaeologists believe that it was likely erected during the Bronze Age. The Kingston Russell 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 BCE. 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. A number of these circles were built in the area around modern Dorset, typically being constructed from sarsen stone and being smaller than those found elsewhere. The Kingston Russell ring is the largest of those in Dorset, measuring 24 by 27 metres (79 feet by 89 feet) in diameter and containing eighteen sarsen stones arranged in an oval shape. The site has not been excavated or been subject to in-depth archaeological investigation. (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 foundered 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 foundered 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 south central Victorian standards, are nonetheless drizzly and overcast. The lack of winter rainfall is owed to 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 and/or the land mass, particularly in spring and autumn; this can set up a "bay effect", similar to the "lake effect" seen in colder climates, 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 predominately 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...) |
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. 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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