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}} |
|---|---|
Basic[edit]
Select from anywhere
| {{Transclude linked excerpt}} | {{Transclude linked excerpt/sandbox}} |
|---|---|
| The Leekfrith torcs are four Iron Age gold torcs found by two hobby metal detectorists in December 2016 in a field in Leekfrith, north Staffordshire, England. The find consists of three neck torcs and a smaller bracelet, which were located in proximity to each other. They are believed to be the oldest Iron Age gold jewellery found in Britain. Subsequent archaeological examination of the area did not uncover further objects. (Full article...) | The Leekfrith torcs are four Iron Age gold torcs found by two hobby metal detectorists in December 2016 in a field in Leekfrith, north Staffordshire, England. The find consists of three neck torcs and a smaller bracelet, which were located in proximity to each other. They are believed to be the oldest Iron Age gold jewellery found in Britain. Subsequent archaeological examination of the area did not uncover further objects. (Full article...) |
Section[edit]
Select from section
| {{Transclude linked excerpt}} | {{Transclude linked excerpt/sandbox}} |
|---|---|
|
The Guilden Morden boar is a sixth- or seventh-century Anglo-Saxon copper alloy figure of a boar that may have once served as the crest of a helmet. It was found around 1864 or 1865 in a grave in Guilden Morden, a village in the eastern English county of Cambridgeshire. There the boar attended a skeleton with other objects, including a small earthenware bead with an incised pattern, although the boar is all that now remains. Herbert George Fordham, whose father originally discovered the boar, donated it to the British Museum in 1904; as of 2018 it was on view in room 41. The boar is simply designed, distinguished primarily by a prominent mane; eyes, eyebrows, nostrils and tusks are only faintly present. A pin and socket design formed by the front and hind legs suggests that the boar was mounted on another object, such as a helmet. Such is the case on one of the contemporary Torslunda plates found in Sweden, where boar-crested helmets are depicted similarly. Boar-crested helmets are a staple of Anglo-Saxon imagery, evidence of a Germanic tradition in which the boar invoked the protection of deities. The Guilden Morden boar is one of three—together with the helmets from Benty Grange and Wollaston—known to have survived to the present, and it has been exhibited both domestically and internationally. The Guilden Morden boar recalls a time when such decoration may have been common; in the Anglo-Saxon poem Beowulf, where boar-adorned helmets are mentioned five times, Hrothgar speaks of when "our boar-crests had to take a battering in the line of action." (Full article...) |
The Guilden Morden boar is a sixth- or seventh-century Anglo-Saxon copper alloy figure of a boar that may have once served as the crest of a helmet. It was found around 1864 or 1865 in a grave in Guilden Morden, a village in the eastern English county of Cambridgeshire. There the boar attended a skeleton with other objects, including a small earthenware bead with an incised pattern, although the boar is all that now remains. Herbert George Fordham, whose father originally discovered the boar, donated it to the British Museum in 1904; as of 2018 it was on view in room 41. The boar is simply designed, distinguished primarily by a prominent mane; eyes, eyebrows, nostrils and tusks are only faintly present. A pin and socket design formed by the front and hind legs suggests that the boar was mounted on another object, such as a helmet. Such is the case on one of the contemporary Torslunda plates found in Sweden, where boar-crested helmets are depicted similarly. Boar-crested helmets are a staple of Anglo-Saxon imagery, evidence of a Germanic tradition in which the boar invoked the protection of deities. The Guilden Morden boar is one of three—together with the helmets from Benty Grange and Wollaston—known to have survived to the present, and it has been exhibited both domestically and internationally. The Guilden Morden boar recalls a time when such decoration may have been common; in the Anglo-Saxon poem Beowulf, where boar-adorned helmets are mentioned five times, Hrothgar speaks of when "our boar-crests had to take a battering in the line of action." (Full article...) |
Subsection[edit]
Select from subsection
| {{Transclude linked excerpt}} | {{Transclude linked excerpt/sandbox}} |
|---|---|
|
The Benty Grange hanging bowl is a fragmentary Anglo-Saxon artifact from the seventh century AD. All that remains are parts of two escutcheons: bronze frames that are usually circular and elaborately decorated, and that sit along the outside of the rim or at the interior base of a hanging bowl. A third one disintegrated soon after excavation, and it no longer survives. The escutcheons were found in 1848 by the antiquary Thomas Bateman, while excavating a tumulus at the Benty Grange farm in western Derbyshire. They were presumably buried as part of an entire hanging bowl. The grave had probably been looted by the time of Bateman's excavation, but still contained high-status objects suggestive of a richly furnished burial, including the hanging bowl and the boar-crested Benty Grange helmet. The surviving escutcheons are made of enameled bronze and are 40 mm (1.6 in) in diameter. They show three dolphin-like creatures arranged in a circle, each biting the tail of the one ahead of it. Their bodies and the background are made of enamel, likely all yellow; the creatures' outlines and eyes are tinned or silvered, as are the borders of the escutcheons. Although three escutcheons from a hanging bowl at Faversham also contain dolphin-like creatures, the Benty Grange design is most closely paralleled by Insular manuscripts, particularly figures in the Durham Gospel Fragment and the Book of Durrow. Surviving illustrations of the third escutcheon show that it was of a different size and style, exhibiting a scroll-like pattern. It parallels the basal disc of a hanging bowl from Winchester and may have been originally placed at the bottom of the Benty Grange bowl. What remains of one escutcheon belongs to Museums Sheffield and as of 2023 was in the collection of the Weston Park Museum. The other is held by the Ashmolean Museum at the University of Oxford; as of 2023, it was not on display. (Full article...) |
The Benty Grange hanging bowl is a fragmentary Anglo-Saxon artifact from the seventh century AD. All that remains are parts of two escutcheons: bronze frames that are usually circular and elaborately decorated, and that sit along the outside of the rim or at the interior base of a hanging bowl. A third one disintegrated soon after excavation, and it no longer survives. The escutcheons were found in 1848 by the antiquary Thomas Bateman, while excavating a tumulus at the Benty Grange farm in western Derbyshire. They were presumably buried as part of an entire hanging bowl. The grave had probably been looted by the time of Bateman's excavation, but still contained high-status objects suggestive of a richly furnished burial, including the hanging bowl and the boar-crested Benty Grange helmet. The surviving escutcheons are made of enameled bronze and are 40 mm (1.6 in) in diameter. They show three dolphin-like creatures arranged in a circle, each biting the tail of the one ahead of it. Their bodies and the background are made of enamel, likely all yellow; the creatures' outlines and eyes are tinned or silvered, as are the borders of the escutcheons. Although three escutcheons from a hanging bowl at Faversham also contain dolphin-like creatures, the Benty Grange design is most closely paralleled by Insular manuscripts, particularly figures in the Durham Gospel Fragment and the Book of Durrow. Surviving illustrations of the third escutcheon show that it was of a different size and style, exhibiting a scroll-like pattern. It parallels the basal disc of a hanging bowl from Winchester and may have been originally placed at the bottom of the Benty Grange bowl. What remains of one escutcheon belongs to Museums Sheffield and as of 2023 was in the collection of the Weston Park Museum. The other is held by the Ashmolean Museum at the University of Oxford; as of 2023, it was not on display. (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 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...) |
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...) |
References[edit]
This section contains references and notes. It should be empty.