Template:Transclude linked excerpt/testcases
 | This is the template test cases page for the sandbox of Template:Transclude linked excerpt. to update the examples. If there are many examples of a complicated template, later ones may break due to limits in MediaWiki; see the HTML comment "NewPP limit report" in the rendered page. You can also use Special:ExpandTemplates to examine the results of template uses. You can test how this page looks in the different skins and parsers with these links: |
Errors
[edit]| {{Transclude linked excerpt}} | {{Transclude linked excerpt/sandbox}} |
|---|---|
| {{Transclude linked excerpt}} | {{Transclude linked excerpt/sandbox}} |
|---|---|
| {{Transclude linked excerpt}} | {{Transclude linked excerpt/sandbox}} |
|---|---|
| {{Transclude linked excerpt}} | {{Transclude linked excerpt/sandbox}} |
|---|---|
| Untitled was an outdoor mural created in 1972 by architect Peter Mayer located at 430 Massachusetts Avenue in downtown Indianapolis, Indiana. The mural, which featured a large ear of corn with the word "HOOSIER" spelled out in the center in yellow on a white background, occupied the southern wall of the six-story apartment building. The mural was part of the renovation of the apartment complex, which opened on 11 December 1972. (Full article...) | Untitled was an outdoor mural created in 1972 by architect Peter Mayer located at 430 Massachusetts Avenue in downtown Indianapolis, Indiana. The mural, which featured a large ear of corn with the word "HOOSIER" spelled out in the center in yellow on a white background, occupied the southern wall of the six-story apartment building. The mural was part of the renovation of the apartment complex, which opened on 11 December 1972. (Full article...) |
Basic
[edit]Select from anywhere
| {{Transclude linked excerpt}} | {{Transclude linked excerpt/sandbox}} |
|---|---|
| Christopher Frank Rendall Potter OBE (9 September 1939 – 2023) was an English schoolmaster who served for twenty-three years as headmaster of Old Swinford Hospital, the seventeenth-century state boarding school in Stourbridge, from 1978 until 2001. Under his leadership the school recovered from a long decline, became one of the first grant-maintained schools in England in 1989, and by the mid-1990s was repeatedly placed at or near the top of the national examination league tables for non-selective schools, being ranked the best-performing comprehensive in the country in successive years. Earlier in his career, as a classics master at Ardingly College, Potter had been among the first schoolmasters in Britain to teach archaeology at A-level, and his pupils included several future professional archaeologists. He was appointed OBE for services to education at the end of his career. (Full article...) | Christopher Frank Rendall Potter OBE (9 September 1939 – 2023) was an English schoolmaster who served for twenty-three years as headmaster of Old Swinford Hospital, the seventeenth-century state boarding school in Stourbridge, from 1978 until 2001. Under his leadership the school recovered from a long decline, became one of the first grant-maintained schools in England in 1989, and by the mid-1990s was repeatedly placed at or near the top of the national examination league tables for non-selective schools, being ranked the best-performing comprehensive in the country in successive years. Earlier in his career, as a classics master at Ardingly College, Potter had been among the first schoolmasters in Britain to teach archaeology at A-level, and his pupils included several future professional archaeologists. He was appointed OBE for services to education at the end of his career. (Full article...) |
Section
[edit]Select from section
| {{Transclude linked excerpt}} | {{Transclude linked excerpt/sandbox}} |
|---|---|
|
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...) |
Subsection
[edit]Select from subsection
| {{Transclude linked excerpt}} | {{Transclude linked excerpt/sandbox}} |
|---|---|
|
Knap Hill lies on the northern rim of the Vale of Pewsey, in northern Wiltshire, England, about a mile (1.6 km) north of the village of Alton Priors. At the top of the hill is a causewayed enclosure, a form of Neolithic earthwork that was constructed in England from about 3700 BC onwards, characterized by the full or partial enclosure of an area with ditches that are interrupted by gaps, or causeways. Their purpose is not known: they may have been settlements, or meeting places, or ritual sites of some kind. The site has been scheduled as an ancient monument. Knap Hill is notable as the first causewayed enclosure to be excavated and identified. In 1908 and 1909, Benjamin and Maud Cunnington spent two summers investigating the site, and Maud published two reports of their work, noting that there were several gaps in the ditch and bank surrounding the enclosure. In the late 1920s, after the excavation of Windmill Hill and other sites, it became apparent that causewayed enclosures were a characteristic monument of the Neolithic period. About a thousand causewayed enclosures have now been found in Europe, including around seventy in Britain. This site was excavated again in 1961 by Graham Connah, who kept thorough stratigraphic documentation. In 2011, the Gathering Time project published an analysis of radiocarbon dates which included several new dates from Connah's finds. It concluded that there was a 91% chance that the Knap Hill enclosure was constructed between 3530 and 3375 BC. Two barrows lay within the Neolithic enclosure, and at least one more outside it. The hilltop also contains the remains of a Romano-British settlement on an adjoining smaller area called the plateau enclosure, along with some evidence of occupation in the 17th century. An Anglo-Saxon sword was found in the smaller enclosure, and there is evidence of an intense fire in the same area, which implies a violent end to the Romano-British occupation of the hilltop. (Full article...) |
Knap Hill lies on the northern rim of the Vale of Pewsey, in northern Wiltshire, England, about a mile (1.6 km) north of the village of Alton Priors. At the top of the hill is a causewayed enclosure, a form of Neolithic earthwork that was constructed in England from about 3700 BC onwards, characterized by the full or partial enclosure of an area with ditches that are interrupted by gaps, or causeways. Their purpose is not known: they may have been settlements, or meeting places, or ritual sites of some kind. The site has been scheduled as an ancient monument. Knap Hill is notable as the first causewayed enclosure to be excavated and identified. In 1908 and 1909, Benjamin and Maud Cunnington spent two summers investigating the site, and Maud published two reports of their work, noting that there were several gaps in the ditch and bank surrounding the enclosure. In the late 1920s, after the excavation of Windmill Hill and other sites, it became apparent that causewayed enclosures were a characteristic monument of the Neolithic period. About a thousand causewayed enclosures have now been found in Europe, including around seventy in Britain. This site was excavated again in 1961 by Graham Connah, who kept thorough stratigraphic documentation. In 2011, the Gathering Time project published an analysis of radiocarbon dates which included several new dates from Connah's finds. It concluded that there was a 91% chance that the Knap Hill enclosure was constructed between 3530 and 3375 BC. Two barrows lay within the Neolithic enclosure, and at least one more outside it. The hilltop also contains the remains of a Romano-British settlement on an adjoining smaller area called the plateau enclosure, along with some evidence of occupation in the 17th century. An Anglo-Saxon sword was found in the smaller enclosure, and there is evidence of an intense fire in the same area, which implies a violent end to the Romano-British occupation of the hilltop. (Full article...) |
List with sections
[edit]Select section in each list item
| {{Transclude linked excerpt}} | {{Transclude linked excerpt/sandbox}} |
|---|---|
|
Melbourne has, depending on the classification system used, a temperate oceanic (Köppen: Cfb) or humid subtropical (Trewartha: Cf) climate, 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 often cloudy. 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 about 425 millimetres (16.7 in) at Little River to 1,250 millimetres (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 rarely receives widespread or continuous rainfall (as experienced in other Australian cities, such as Sydney or Brisbane) and instead experiences precipitation through fleeting showers that can vary in intensity, Melbourne is particularly prone to these 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, depending on the classification system used, a temperate oceanic (Köppen: Cfb) or humid subtropical (Trewartha: Cf) climate, 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 often cloudy. 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 about 425 millimetres (16.7 in) at Little River to 1,250 millimetres (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 rarely receives widespread or continuous rainfall (as experienced in other Australian cities, such as Sydney or Brisbane) and instead experiences precipitation through fleeting showers that can vary in intensity, Melbourne is particularly prone to these 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...) |
References
[edit]This section contains references and notes. It should be empty.