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 (stylized as 「untitled」) is the sixteenth studio album by the Japanese idol group Arashi. The album was released on October 18, 2017 under their record label J Storm in two editions: a first press/limited edition and a regular edition. With more than 750,000 copies sold, the album was certified Triple Platinum by the Recording Industry Association of Japan (RIAJ). It was released digitally on February 7, 2020. (Full article...) | Untitled (stylized as 「untitled」) is the sixteenth studio album by the Japanese idol group Arashi. The album was released on October 18, 2017 under their record label J Storm in two editions: a first press/limited edition and a regular edition. With more than 750,000 copies sold, the album was certified Triple Platinum by the Recording Industry Association of Japan (RIAJ). It was released digitally on February 7, 2020. (Full article...) |
Basic
[edit]Select from anywhere
| {{Transclude linked excerpt}} | {{Transclude linked excerpt/sandbox}} |
|---|---|
|
Porlock Stone Circle is a stone circle located on Exmoor, near the village of Porlock in the south-western English county of Somerset. The Porlock 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 3300 and 900 BCE. The purpose of such monuments is unknown, although archaeologists speculate that the stones represented supernatural entities for the circles' builders. Although Exmoor witnessed the construction of many monuments during the Bronze Age, only two stone circles survive in this area, the other being Withypool Stone Circle. The Porlock circle is about 24 metres (79 feet) in diameter and contains thirteen green micaceous sandstone rocks; there may originally have been more. Directly to the north-east of the circle is a cairn connected to a linear stone row. No evidence has been found that allows for absolute dating of the monument's construction, although archaeologists have suggested that the cairn dates from the Early Bronze Age, the circle being a Middle Bronze Age addition. A small lead wheel found inside Porlock Stone Circle suggests that the site was visited during the Romano-British period. The site was rediscovered in the 1920s and since then a variety of stones have been added to it; its current appearance is a composite of prehistoric and modern elements. In 1928 the site was surveyed and excavated by the archaeologist Harold St George Gray. A second excavation took place under the leadership of Mark Gillings in 2013. (Full article...) |
Porlock Stone Circle is a stone circle located on Exmoor, near the village of Porlock in the south-western English county of Somerset. The Porlock 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 3300 and 900 BCE. The purpose of such monuments is unknown, although archaeologists speculate that the stones represented supernatural entities for the circles' builders. Although Exmoor witnessed the construction of many monuments during the Bronze Age, only two stone circles survive in this area, the other being Withypool Stone Circle. The Porlock circle is about 24 metres (79 feet) in diameter and contains thirteen green micaceous sandstone rocks; there may originally have been more. Directly to the north-east of the circle is a cairn connected to a linear stone row. No evidence has been found that allows for absolute dating of the monument's construction, although archaeologists have suggested that the cairn dates from the Early Bronze Age, the circle being a Middle Bronze Age addition. A small lead wheel found inside Porlock Stone Circle suggests that the site was visited during the Romano-British period. The site was rediscovered in the 1920s and since then a variety of stones have been added to it; its current appearance is a composite of prehistoric and modern elements. In 1928 the site was surveyed and excavated by the archaeologist Harold St George Gray. A second excavation took place under the leadership of Mark Gillings in 2013. (Full article...) |
Section
[edit]Select from section
| {{Transclude linked excerpt}} | {{Transclude linked excerpt/sandbox}} |
|---|---|
|
Walter Abel Heurtley OBE FSA (24 October 1882 – 2 January 1955) was a British classical archaeologist. The son of a Church of England vicar, he was educated at Uppingham School and read classics at Gonville and Caius College, Cambridge, on a scholarship. Upon leaving Cambridge, he worked as a teacher at The Oratory School, and became a reserve officer in the Royal Engineers. He served in the East Lancashire Regiment during the First World War, where he was mentioned in dispatches three times and acted as deputy governor of the British military prison at Salonika in Greece. After the war, Heurtley studied classical archaeology at Oriel College, Oxford, under Percy Gardner and with Stanley Casson, the assistant director of the British School at Athens (BSA). Heurtley followed Casson to the BSA, excavating in 1921 with him in Macedonia, and with the school's director, Alan Wace, at Mycenae. In 1923, Heurtley succeeded Casson as the BSA's assistant director, and also assumed the role of its librarian; he held both posts until his dismissal, on financial grounds, in 1932. He subsequently became the librarian of the Department of Antiquities of the Mandate for Palestine, a position he held until 1939, and ended his career as bursar of The Oratory School. Heurtley was elected as a fellow of the Society of Antiquaries in 1936. He excavated widely in northern Greece during the 1920s and 1930s, and published his monograph, Prehistoric Macedonia, in 1939. He also excavated on the island of Ithaca between 1930 and 1932, and spent a season at Troy under Carl Blegen in 1932. He was often accompanied on his excavations by his wife, Eileen, who cooked for his excavators. He retired to her ancestral home in County Kerry in 1945, and died of cancer in 1955. (Full article...) |
Walter Abel Heurtley OBE FSA (24 October 1882 – 2 January 1955) was a British classical archaeologist. The son of a Church of England vicar, he was educated at Uppingham School and read classics at Gonville and Caius College, Cambridge, on a scholarship. Upon leaving Cambridge, he worked as a teacher at The Oratory School, and became a reserve officer in the Royal Engineers. He served in the East Lancashire Regiment during the First World War, where he was mentioned in dispatches three times and acted as deputy governor of the British military prison at Salonika in Greece. After the war, Heurtley studied classical archaeology at Oriel College, Oxford, under Percy Gardner and with Stanley Casson, the assistant director of the British School at Athens (BSA). Heurtley followed Casson to the BSA, excavating in 1921 with him in Macedonia, and with the school's director, Alan Wace, at Mycenae. In 1923, Heurtley succeeded Casson as the BSA's assistant director, and also assumed the role of its librarian; he held both posts until his dismissal, on financial grounds, in 1932. He subsequently became the librarian of the Department of Antiquities of the Mandate for Palestine, a position he held until 1939, and ended his career as bursar of The Oratory School. Heurtley was elected as a fellow of the Society of Antiquaries in 1936. He excavated widely in northern Greece during the 1920s and 1930s, and published his monograph, Prehistoric Macedonia, in 1939. He also excavated on the island of Ithaca between 1930 and 1932, and spent a season at Troy under Carl Blegen in 1932. He was often accompanied on his excavations by his wife, Eileen, who cooked for his excavators. He retired to her ancestral home in County Kerry in 1945, and died of cancer in 1955. (Full article...) |
Subsection
[edit]Select from subsection
| {{Transclude linked excerpt}} | {{Transclude linked excerpt/sandbox}} |
|---|---|
|
The Horncastle boar's head is an early seventh-century Anglo-Saxon ornament depicting a boar that probably was once part of the crest of a helmet. It was discovered in 2002 by a metal detectorist searching in the town of Horncastle, Lincolnshire. It was reported as found treasure and acquired for £15,000 by the Lincoln City and County Museum—now Lincoln Museum—where it is on permanent display. The fragment is 40 mm (1.6 in) long and made of silver. Its elongated head is semi-naturalistic, depicting a crouching quadruped on either side of the skull, divided by a mane along the centre. The boar's eyes are formed from garnet, and its eyebrows, skull, mouth, tusks, and snout are gilded. Its head is hollow; in the space underneath, which was filled with soil and plant matter when found, are three rivets that would have attached it to a larger object, probably a helmet. The fragment would probably have formed the crest terminal of one of the "crested helmets" used in Northern Europe during the sixth through eleventh centuries. The boar's head terminal is one of several representations of the animal on contemporaneous helmets. Boars surmount the Benty Grange and Wollaston helmets, and form the ends of the eyebrows of the Sutton Hoo and perhaps York helmets. These evidence a thousand-years-long tradition in Germanic paganism associating boars with both deities and protection. The Roman historian Tacitus suggested that the Baltic Aesti wore boar symbols in battle to invoke the protection of a mother goddess, and in the Anglo-Saxon epic Beowulf, the poet writes that boar symbols on helmets kept watch over the warriors wearing them. (Full article...) |
The Horncastle boar's head is an early seventh-century Anglo-Saxon ornament depicting a boar that probably was once part of the crest of a helmet. It was discovered in 2002 by a metal detectorist searching in the town of Horncastle, Lincolnshire. It was reported as found treasure and acquired for £15,000 by the Lincoln City and County Museum—now Lincoln Museum—where it is on permanent display. The fragment is 40 mm (1.6 in) long and made of silver. Its elongated head is semi-naturalistic, depicting a crouching quadruped on either side of the skull, divided by a mane along the centre. The boar's eyes are formed from garnet, and its eyebrows, skull, mouth, tusks, and snout are gilded. Its head is hollow; in the space underneath, which was filled with soil and plant matter when found, are three rivets that would have attached it to a larger object, probably a helmet. The fragment would probably have formed the crest terminal of one of the "crested helmets" used in Northern Europe during the sixth through eleventh centuries. The boar's head terminal is one of several representations of the animal on contemporaneous helmets. Boars surmount the Benty Grange and Wollaston helmets, and form the ends of the eyebrows of the Sutton Hoo and perhaps York helmets. These evidence a thousand-years-long tradition in Germanic paganism associating boars with both deities and protection. The Roman historian Tacitus suggested that the Baltic Aesti wore boar symbols in battle to invoke the protection of a mother goddess, and in the Anglo-Saxon epic Beowulf, the poet writes that boar symbols on helmets kept watch over the warriors wearing them. (Full article...) |
List with sections
[edit]Select section in each list item
| {{Transclude linked excerpt}} | {{Transclude linked excerpt/sandbox}} |
|---|---|
|
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...) |
References
[edit]This section contains references and notes. It should be empty.