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}} |
|---|---|
|
The Coldrum Long Barrow, also known as the Coldrum Stones and the Adscombe Stones, is a chambered long barrow located near the village of Trottiscliffe in the south-eastern English county of Kent. Probably constructed in the fourth millennium BCE, during Britain's Early Neolithic period, today it survives only in a state of ruin. Archaeologists have established that the monument was built by pastoralist communities shortly after the introduction of agriculture to Britain from continental Europe. Part of an architectural tradition of long barrow building that was widespread across Neolithic Europe, the Coldrum Stones belong to a localised regional variant of barrows produced in the vicinity of the River Medway, now known as the Medway Megaliths. Of these, it is in the best surviving condition. It lies near to both Addington Long Barrow and Chestnuts Long Barrow on the western side of the river. Two further surviving long barrows, Kit's Coty House and Little Kit's Coty House, as well as possible survivals such as the Coffin Stone and White Horse Stone, are located on the Medway's eastern side. Built out of earth and around fifty local sarsen-stone megaliths, the long barrow consisted of a sub-rectangular earthen tumulus enclosed by kerb-stones. Within the eastern end of the tumulus was a stone chamber, into which human remains were deposited on at least two separate occasions during the Early Neolithic. Osteoarchaeological analysis of these remains has shown them to be those of at least seventeen individuals, a mixture of men, women, and children. At least one of the bodies had been dismembered before burial, potentially reflecting a funerary tradition of excarnation and secondary burial. As with other barrows, Coldrum has been interpreted as a tomb to house the remains of the dead, perhaps as part of a belief system involving ancestor veneration, although archaeologists have suggested that it may also have had further religious, ritual, and cultural connotations and uses. After the Early Neolithic, the long barrow fell into a state of ruined dilapidation, perhaps experiencing deliberate destruction in the Late Medieval period, either by Christian iconoclasts or treasure hunters. In local folklore, the site became associated with the burial of a prince and the countless stones motif. The ruin attracted the interest of antiquarians in the 19th century, while archaeological excavation took place in the early 20th. In 1926, ownership was transferred to heritage charity the National Trust. Open without charge to visitors all year around, the stones are the site of a rag tree, a May Day morris dance, and various modern Pagan rituals. (Full article...) |
The Coldrum Long Barrow, also known as the Coldrum Stones and the Adscombe Stones, is a chambered long barrow located near the village of Trottiscliffe in the south-eastern English county of Kent. Probably constructed in the fourth millennium BCE, during Britain's Early Neolithic period, today it survives only in a state of ruin. Archaeologists have established that the monument was built by pastoralist communities shortly after the introduction of agriculture to Britain from continental Europe. Part of an architectural tradition of long barrow building that was widespread across Neolithic Europe, the Coldrum Stones belong to a localised regional variant of barrows produced in the vicinity of the River Medway, now known as the Medway Megaliths. Of these, it is in the best surviving condition. It lies near to both Addington Long Barrow and Chestnuts Long Barrow on the western side of the river. Two further surviving long barrows, Kit's Coty House and Little Kit's Coty House, as well as possible survivals such as the Coffin Stone and White Horse Stone, are located on the Medway's eastern side. Built out of earth and around fifty local sarsen-stone megaliths, the long barrow consisted of a sub-rectangular earthen tumulus enclosed by kerb-stones. Within the eastern end of the tumulus was a stone chamber, into which human remains were deposited on at least two separate occasions during the Early Neolithic. Osteoarchaeological analysis of these remains has shown them to be those of at least seventeen individuals, a mixture of men, women, and children. At least one of the bodies had been dismembered before burial, potentially reflecting a funerary tradition of excarnation and secondary burial. As with other barrows, Coldrum has been interpreted as a tomb to house the remains of the dead, perhaps as part of a belief system involving ancestor veneration, although archaeologists have suggested that it may also have had further religious, ritual, and cultural connotations and uses. After the Early Neolithic, the long barrow fell into a state of ruined dilapidation, perhaps experiencing deliberate destruction in the Late Medieval period, either by Christian iconoclasts or treasure hunters. In local folklore, the site became associated with the burial of a prince and the countless stones motif. The ruin attracted the interest of antiquarians in the 19th century, while archaeological excavation took place in the early 20th. In 1926, ownership was transferred to heritage charity the National Trust. Open without charge to visitors all year around, the stones are the site of a rag tree, a May Day morris dance, and various modern Pagan rituals. (Full article...) |
Section
[edit]Select from section
| {{Transclude linked excerpt}} | {{Transclude linked excerpt/sandbox}} |
|---|---|
|
The Hellvi helmet eyebrow is a decorative eyebrow from a Vendel Period helmet. It comprises two fragments; the arch is made of iron decorated with strips of silver, and terminates in a bronze animal head that was cast on. The eyebrow was donated to the Statens historiska museum in November 1880 along with several other objects, all said to be from a grave find in Gotland, Sweden. The eyebrow dates to around 550 to 600 AD, and would have once adorned one of the "crested helmets" that appeared in England and Scandinavia around that time. Many of these also featured decorated eyebrows, such as the Sutton Hoo helmet and the Broe helmet; the Hellvi example is one of a number of decorated eyebrows that have been found without other traces of the original helmet, including the Lokrume helmet fragment in Gotland and the Gevninge helmet fragment in Denmark. (Full article...) |
The Hellvi helmet eyebrow is a decorative eyebrow from a Vendel Period helmet. It comprises two fragments; the arch is made of iron decorated with strips of silver, and terminates in a bronze animal head that was cast on. The eyebrow was donated to the Statens historiska museum in November 1880 along with several other objects, all said to be from a grave find in Gotland, Sweden. The eyebrow dates to around 550 to 600 AD, and would have once adorned one of the "crested helmets" that appeared in England and Scandinavia around that time. Many of these also featured decorated eyebrows, such as the Sutton Hoo helmet and the Broe helmet; the Hellvi example is one of a number of decorated eyebrows that have been found without other traces of the original helmet, including the Lokrume helmet fragment in Gotland and the Gevninge helmet fragment in Denmark. (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.