Template:Transclude linked excerpt/testcases

Errors

{{Transclude linked excerpt}}

Side by side comparison

{{Transclude linked excerpt}}	{{Transclude linked excerpt/sandbox}}

{{Transclude linked excerpt|}}

Side by side comparison

{{Transclude linked excerpt}}	{{Transclude linked excerpt/sandbox}}

{{Transclude linked excerpt| }}

Side by side comparison

{{Transclude linked excerpt}}	{{Transclude linked excerpt/sandbox}}

{{Transclude linked excerpt|No title}}

Side by side comparison

{{Transclude linked excerpt}}	{{Transclude linked excerpt/sandbox}}

Basic

Select from anywhere

{{Transclude linked excerpt|Wikipedia:WikiProject Archaeology/Monitoring}}

Side by side comparison

{{Transclude linked excerpt}}	{{Transclude linked excerpt/sandbox}}
(Full article...)	(Full article...)

Section

Select from section

{{Transclude linked excerpt|Wikipedia:WikiProject Archaeology/Monitoring |section=Recognised content}}

Side by side comparison

{{Transclude linked excerpt}}

{{Transclude linked excerpt/sandbox}}

Borobudur, also transcribed Barabudur (Indonesian: Candi Borobudur, Javanese: ꦕꦤ꧀ꦝꦶꦧꦫꦧꦸꦝꦸꦂ, romanized: Candhi Barabudhur), is a 9th-century Mahayana Buddhist temple in Magelang Regency, near the city of Magelang and the town of Muntilan, in Central Java, Indonesia. Constructed of gray andesite-like stone, the temple consists of nine stacked platforms, six square and three circular, topped by a central dome. It is decorated with 2,672 relief panels and originally 504 Buddha statues. The central dome is surrounded by 72 Buddha statues, each seated inside a perforated stupa. The monument guides pilgrims through an extensive system of stairways and corridors with 1,460 narrative relief panels on the walls and the balustrades. Borobudur has one of the world's most extensive collections of Buddhist reliefs. Built during the reign of the Sailendra Dynasty, the temple design follows Javanese Buddhist architecture, which blends the Indonesian indigenous tradition of ancestor worship and the Buddhist concept of attaining nirvāṇa. The monument is a shrine to the Buddha and a place for Buddhist pilgrimage. Evidence suggests that Borobudur was constructed in the 8th century and subsequently abandoned following the 14th-century decline of Hindu kingdoms in Java and the Javanese conversion to Islam. Worldwide knowledge of its existence was sparked in 1814 by Sir Thomas Stamford Raffles, then the British ruler of Java, who was advised of its location by native Indonesians. Borobudur has since been preserved through several restorations. The largest restoration project was completed at 1983 by the Indonesian government and UNESCO, followed by the monument's listing as a UNESCO World Heritage Site. Borobudur is the largest Buddhist temple in the world, and ranks with Bagan in Myanmar and Angkor Wat in Cambodia as one of the great archeological sites of Southeast Asia. Borobudur remains popular for pilgrimage, with Buddhists in Indonesia celebrating Vesak Day at the monument. Among Indonesia's tourist attractions, Borobudur is the most-visited monument. (Full article...)

Akkadian or Mesopotamian royal titulary refers to the royal titles and epithets (and the style they were presented in) assumed by monarchs in Ancient Mesopotamia from the Akkadian period to the fall of the Neo-Babylonian Empire (roughly 2334 to 539 BC), with some scant usage in the later Achaemenid and Seleucid periods. The titles and the order they were presented in varied from king to king, with similarities between kings usually being because of a king's explicit choice to align himself with a predecessor. Some titles, like the Akkadian šar kibrāt erbetti ("king of the Four Corners of the World") and šar kiššatim ("king of the Universe") and the Neo-Sumerian šar māt Šumeri u Akkadi ("king of Sumer and Akkad") would remain in use for more than a thousand years through several different empires and others were only used by a single king. In the Akkadian-speaking kingdoms of Assyria and Babylonia, distinct styles of Akkadian titulature would develop, retaining titles and elements of earlier kings but applying new royal traditions. In Assyrian royal titulary, emphasis would typically be placed on the strength and power of the king whilst Babylonian royal titulary would usually focus on the protective role and the piety of the king. Monarchs who controlled both Assyria and Babylon (such as some of the Neo-Assyrian kings) often used "hybrid" titularies combining aspects of both. Such hybrid titularies are also recorded for the only known examples of Akkadian titularies beyond the fall of the Neo-Babylonian Empire, employed by Cyrus the Great (r. 559–530 BC) of the Achaemenid Empire and Antiochus I (r. 281–261 BC) of the Seleucid Empire, who also introduced some aspects of their own royal ideologies. (Full article...)

Subsection

Select from subsection

{{Transclude linked excerpt|Wikipedia:WikiProject Archaeology/Monitoring |section=Featured articles}}

Side by side comparison

{{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...)

List with sections

Select section in each list item

{{Transclude linked excerpt|Template:Transclude linked excerpt/testcases/list}}

Side by side comparison

{{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

This section contains references and notes. It should be empty.