 | 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
editSelect from anywhere
| {{Transclude linked excerpt}} | {{Transclude linked excerpt/sandbox}} |
|---|---|
| (Full article...) | (Full article...) |
Section
editSelect from section
| {{Transclude linked excerpt}} | {{Transclude linked excerpt/sandbox}} |
|---|---|
|
Agriculture encompasses crop and livestock production, aquaculture, and forestry for food and non-food products. Agriculture was the key development in the rise of sedentary human civilization, whereby farming of domesticated species created food surpluses that enabled people to live in cities. While humans started gathering grains at least 105,000 years ago, nascent farmers only began planting them around 11,500 years ago. Sheep, goats, pigs, and cattle were domesticated around 10,000 years ago. Plants were independently cultivated in at least 11 regions of the world. In the 20th century, industrial agriculture based on large-scale monocultures came to dominate agricultural output. , small farms produce about one-third of the world's food, but large farms are prevalent. The largest 1% of farms in the world are greater than 50 hectares (120 acres) and operate more than 70% of the world's farmland. Nearly 40% of agricultural land is found on farms larger than 1,000 hectares (2,500 acres). However, five of every six farms in the world consist of fewer than 2 hectares (4.9 acres), and take up only around 12% of all agricultural land. Farms and farming greatly influence rural economics and greatly shape rural society, effecting both the direct agricultural workforce and broader businesses that support the farms and farming populations. The major agricultural products can be broadly grouped into foods, fibers, fuels, and raw materials (such as rubber). Food classes include cereals (grains), vegetables, fruits, cooking oils, meat, milk, eggs, and fungi. Global agricultural production amounts to approximately 11 billion tonnes of food, 32 million tonnes of natural fibres and 4 billion m3 of wood. However, around 14% of the world's food is lost from production before reaching the retail level. Modern agronomy, plant breeding, agrochemicals such as pesticides and fertilizers, and technological developments have sharply increased crop yields, but also contributed to ecological and environmental damage. Selective breeding and modern practices in animal husbandry have similarly increased the output of meat, but have raised concerns about animal welfare and environmental damage. Environmental issues include contributions to climate change, depletion of aquifers, deforestation, antibiotic resistance, and other agricultural pollution. Agriculture is both a cause of and sensitive to environmental degradation, such as biodiversity loss, desertification, soil degradation, and climate change, all of which can cause decreases in crop yield. Genetically modified organisms are widely used, although some countries ban them. (Full article...) |
Agriculture encompasses crop and livestock production, aquaculture, and forestry for food and non-food products. Agriculture was the key development in the rise of sedentary human civilization, whereby farming of domesticated species created food surpluses that enabled people to live in cities. While humans started gathering grains at least 105,000 years ago, nascent farmers only began planting them around 11,500 years ago. Sheep, goats, pigs, and cattle were domesticated around 10,000 years ago. Plants were independently cultivated in at least 11 regions of the world. In the 20th century, industrial agriculture based on large-scale monocultures came to dominate agricultural output. , small farms produce about one-third of the world's food, but large farms are prevalent. The largest 1% of farms in the world are greater than 50 hectares (120 acres) and operate more than 70% of the world's farmland. Nearly 40% of agricultural land is found on farms larger than 1,000 hectares (2,500 acres). However, five of every six farms in the world consist of fewer than 2 hectares (4.9 acres), and take up only around 12% of all agricultural land. Farms and farming greatly influence rural economics and greatly shape rural society, effecting both the direct agricultural workforce and broader businesses that support the farms and farming populations. The major agricultural products can be broadly grouped into foods, fibers, fuels, and raw materials (such as rubber). Food classes include cereals (grains), vegetables, fruits, cooking oils, meat, milk, eggs, and fungi. Global agricultural production amounts to approximately 11 billion tonnes of food, 32 million tonnes of natural fibres and 4 billion m3 of wood. However, around 14% of the world's food is lost from production before reaching the retail level. Modern agronomy, plant breeding, agrochemicals such as pesticides and fertilizers, and technological developments have sharply increased crop yields, but also contributed to ecological and environmental damage. Selective breeding and modern practices in animal husbandry have similarly increased the output of meat, but have raised concerns about animal welfare and environmental damage. Environmental issues include contributions to climate change, depletion of aquifers, deforestation, antibiotic resistance, and other agricultural pollution. Agriculture is both a cause of and sensitive to environmental degradation, such as biodiversity loss, desertification, soil degradation, and climate change, all of which can cause decreases in crop yield. Genetically modified organisms are widely used, although some countries ban them. (Full article...) |
Subsection
editSelect from subsection
| {{Transclude linked excerpt}} | {{Transclude linked excerpt/sandbox}} |
|---|---|
|
The Corp Naomh ([kɔɾˠpˠ n̪ˠiːvˠ], KORP NEEV, English: Holy or Sacred Body) is an Irish bell shrine made in the 9th or 10th century to enclose a now-lost hand-bell, which probably dated to c. 600 to 900 AD and belonged to an early Irish saint. The shrine was rediscovered sometime before 1682 at Tristernagh Abbey, near Templecross, County Westmeath. The shrine is 23 cm (9.1 in) high and 12 cm (4.7 in) wide. It was heavily refurbished and added to during a second phase of embellishment in the 15th century, and now consists of cast and sheet bronze plates mounted on a wooden core decorated with silver, niello and rock crystal. It is severely damaged with extensive losses and wear across almost all of its parts, and when discovered a block of wood had been substituted for the bell itself. The remaining elements are considered of high historical and artistic value by archaeologists and art historians. Sections from its original, early Medieval phase include the cross on the reverse and the ornate semi-circular cap, which shows a bearded cleric holding a book. He is surrounded by horsemen above whom are large birds seemingly about to take flight. It was extensively refurbished in the 15th (and possibly 16th) centuries when the central bronze crucifix, the griffin and lion panel, the stamped border panels and the backing plate were added. The badly damaged crucifix and large enamel stud on the front date from at least the 15th century. The shrine's medieval provenance is incomplete. It was probably held by hereditary keepers after the dissolution of Tristernagh Abbey in 1536 until it passed into the possession of the Anglo-Irish owners of the site. The Corp Naomh was first exhibited in 1853 by the Royal Irish Academy (RIA) and was transferred to the National Museum of Ireland in 1887. (Full article...) |
The Corp Naomh ([kɔɾˠpˠ n̪ˠiːvˠ], KORP NEEV, English: Holy or Sacred Body) is an Irish bell shrine made in the 9th or 10th century to enclose a now-lost hand-bell, which probably dated to c. 600 to 900 AD and belonged to an early Irish saint. The shrine was rediscovered sometime before 1682 at Tristernagh Abbey, near Templecross, County Westmeath. The shrine is 23 cm (9.1 in) high and 12 cm (4.7 in) wide. It was heavily refurbished and added to during a second phase of embellishment in the 15th century, and now consists of cast and sheet bronze plates mounted on a wooden core decorated with silver, niello and rock crystal. It is severely damaged with extensive losses and wear across almost all of its parts, and when discovered a block of wood had been substituted for the bell itself. The remaining elements are considered of high historical and artistic value by archaeologists and art historians. Sections from its original, early Medieval phase include the cross on the reverse and the ornate semi-circular cap, which shows a bearded cleric holding a book. He is surrounded by horsemen above whom are large birds seemingly about to take flight. It was extensively refurbished in the 15th (and possibly 16th) centuries when the central bronze crucifix, the griffin and lion panel, the stamped border panels and the backing plate were added. The badly damaged crucifix and large enamel stud on the front date from at least the 15th century. The shrine's medieval provenance is incomplete. It was probably held by hereditary keepers after the dissolution of Tristernagh Abbey in 1536 until it passed into the possession of the Anglo-Irish owners of the site. The Corp Naomh was first exhibited in 1853 by the Royal Irish Academy (RIA) and was transferred to the National Museum of Ireland in 1887. (Full article...) |
List with sections
editSelect section in each list item
| {{Transclude linked excerpt}} | {{Transclude linked excerpt/sandbox}} |
|---|---|
|
Melbourne has a temperate oceanic climate (Köppen climate classification Cfb), bordering on a humid subtropical climate (Köppen climate classification Cfa), 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), bordering on a humid subtropical climate (Köppen climate classification Cfa), 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
editThis section contains references and notes. It should be empty.