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Untitled is an abstract 1990 sculpture by Joel Shapiro. Bronze edition 4/4 is installed in the Lillie and Hugh Roy Cullen Sculpture Garden, as part of the collection of the Museum of Fine Arts, Houston. Another bronze copy is installed on the Seattle University campus.

(Full article...)

Untitled is an abstract 1990 sculpture by Joel Shapiro. Bronze edition 4/4 is installed in the Lillie and Hugh Roy Cullen Sculpture Garden, as part of the collection of the Museum of Fine Arts, Houston. Another bronze copy is installed on the Seattle University campus.

(Full article...)

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The cord is a unit of measure of dry volume used to measure firewood and pulpwood in the United States and Canada.

A cord is the amount of wood that, when "racked and well stowed" (arranged so pieces are aligned, parallel, touching, and compact), occupies a volume of 128 cubic feet (3.62 m3). This corresponds to a well-stacked woodpile 4 feet (122 cm) high, 8 feet (244 cm) wide, and 4 feet (122 cm) deep; or any other arrangement of linear measurements that yields the same volume.

The name cord probably comes from the use of a cord or string to measure it.

The face cord is a unit of volume for stacked firewood, 8 feet long, 4 feet wide, and 16 inches high—equal to 1/3 of a cord. The symbol for the unit is fc - cd. (Full article...)

The cord is a unit of measure of dry volume used to measure firewood and pulpwood in the United States and Canada.

A cord is the amount of wood that, when "racked and well stowed" (arranged so pieces are aligned, parallel, touching, and compact), occupies a volume of 128 cubic feet (3.62 m3). This corresponds to a well-stacked woodpile 4 feet (122 cm) high, 8 feet (244 cm) wide, and 4 feet (122 cm) deep; or any other arrangement of linear measurements that yields the same volume.

The name cord probably comes from the use of a cord or string to measure it.

The face cord is a unit of volume for stacked firewood, 8 feet long, 4 feet wide, and 16 inches high—equal to 1/3 of a cord. The symbol for the unit is fc - cd. (Full article...)
{{Transclude list item excerpt|List of sharks}}
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The striped smooth-hound (Mustelus fasciatus) is a houndshark of the family Triakidae, found on the continental shelves of the subtropical southwest Atlantic from southern Brazil to northern Argentina between latitudes 30° S and 47° S, from the surface to 250 m (820 ft). It can grow up to a length of 1.77 m (5 ft 10 in). The reproduction of this shark is Ovoviviparous, with the length at birth up to 39 cm (15 in). (Full article...) The striped smooth-hound (Mustelus fasciatus) is a houndshark of the family Triakidae, found on the continental shelves of the subtropical southwest Atlantic from southern Brazil to northern Argentina between latitudes 30° S and 47° S, from the surface to 250 m (820 ft). It can grow up to a length of 1.77 m (5 ft 10 in). The reproduction of this shark is Ovoviviparous, with the length at birth up to 39 cm (15 in). (Full article...)
{{Transclude list item excerpt|List of dams and reservoirs}}
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The Koman Hydroelectric Power Station is a large hydroelectric power station (HPP), for which a dam on the Drin River was built. The dam is near the settlement of Koman, northern Albania. It is the second of three dams of the Drin River cascade; the Fierza Hydroelectric Power Station upstream, and the Vau i Dejës Hydroelectric Power Station downstream. The dam, 130m tall, was completed in 1985 and the reservoir was filled with water at full capacity in 1986.

Completed in 1986, the power station consists of four turbines of French origin with a nominal capacity of 150 MW each, totalling the installed capacity to 600 MW.

(Full article...)

The Koman Hydroelectric Power Station is a large hydroelectric power station (HPP), for which a dam on the Drin River was built. The dam is near the settlement of Koman, northern Albania. It is the second of three dams of the Drin River cascade; the Fierza Hydroelectric Power Station upstream, and the Vau i Dejës Hydroelectric Power Station downstream. The dam, 130m tall, was completed in 1985 and the reservoir was filled with water at full capacity in 1986.

Completed in 1986, the power station consists of four turbines of French origin with a nominal capacity of 150 MW each, totalling the installed capacity to 600 MW.

(Full article...)

Section

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{{Transclude list item excerpt|List of mountain ranges|section=Mountain ranges on planet Earth}}
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{{Transclude list item excerpt|List of dams and reservoirs|section=Oceania |sectiononly=yes}}
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The Yaté Dam is an arch dam on the Yaté River in Yaté commune of New Caledonia, France. The primary purpose of the dam is hydroelectric power generation and it supports a 68 MW power station. Plans for the project began in the early 1950s and the dam was designed by Coyne et Bellier. The owner and operator of the project, New Caledonian Society Energy (ENERCAL), was established on 27 August 1955 to implement the project. Construction began that year and the power station was commissioned in 1958. The dam and entire scheme was inaugurated by Jacques Soustelle, then Minister of State in charge of Overseas Departments, on 21 September 1959. It is the tallest dam and creates the largest reservoir in New Caledonia.

While the main retaining portion of the dam is an arch design, it also has a concrete gravity section and an earthen and rock-fill section. The arch dam has a height of 60 m (200 ft) and length of 200 m (660 ft). On its left side adjoins the gravity section which serves as a spillway and is 61 m (200 ft) tall. It is 100 m (330 ft) long. The embankment section located direct the northwest of the gravity portion is 280 m (920 ft) long. Water from the dam is diverted through the hillsides via two 2,600 m (8,500 ft) long penstocks to the power station downstream along the Yaté River in the town of Yaté. The difference in elevation between the dam and power station affords a hydraulic head (water drop) of 157 m (515 ft). Within the power station lies four 17 MW Francis turbine-generates which produce an average of 307 GWh annually. (Full article...)

The Yaté Dam is an arch dam on the Yaté River in Yaté commune of New Caledonia, France. The primary purpose of the dam is hydroelectric power generation and it supports a 68 MW power station. Plans for the project began in the early 1950s and the dam was designed by Coyne et Bellier. The owner and operator of the project, New Caledonian Society Energy (ENERCAL), was established on 27 August 1955 to implement the project. Construction began that year and the power station was commissioned in 1958. The dam and entire scheme was inaugurated by Jacques Soustelle, then Minister of State in charge of Overseas Departments, on 21 September 1959. It is the tallest dam and creates the largest reservoir in New Caledonia.

While the main retaining portion of the dam is an arch design, it also has a concrete gravity section and an earthen and rock-fill section. The arch dam has a height of 60 m (200 ft) and length of 200 m (660 ft). On its left side adjoins the gravity section which serves as a spillway and is 61 m (200 ft) tall. It is 100 m (330 ft) long. The embankment section located direct the northwest of the gravity portion is 280 m (920 ft) long. Water from the dam is diverted through the hillsides via two 2,600 m (8,500 ft) long penstocks to the power station downstream along the Yaté River in the town of Yaté. The difference in elevation between the dam and power station affords a hydraulic head (water drop) of 157 m (515 ft). Within the power station lies four 17 MW Francis turbine-generates which produce an average of 307 GWh annually. (Full article...)

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The lycophytes, when broadly circumscribed, are a group of vascular plants that include the clubmosses. They are sometimes placed in a division Lycopodiophyta or Lycophyta or in a subdivision Lycopodiophytina. They are one of the oldest lineages of extant (living) vascular plants; the group contains extinct plants that have been dated from the Silurian (ca. 425 million years ago). Lycophytes were some of the dominating plant species of the Carboniferous period, and included the tree-like Lepidodendrales, some of which grew over 40 metres (130 ft) in height, although extant lycophytes are relatively small plants.

The scientific names and the informal English names used for this group of plants are ambiguous. For example, "Lycopodiophyta" and the shorter "Lycophyta" as well as the informal "lycophyte" may be used to include the extinct zosterophylls or to exclude them. (Full article...)

The lycophytes, when broadly circumscribed, are a group of vascular plants that include the clubmosses. They are sometimes placed in a division Lycopodiophyta or Lycophyta or in a subdivision Lycopodiophytina. They are one of the oldest lineages of extant (living) vascular plants; the group contains extinct plants that have been dated from the Silurian (ca. 425 million years ago). Lycophytes were some of the dominating plant species of the Carboniferous period, and included the tree-like Lepidodendrales, some of which grew over 40 metres (130 ft) in height, although extant lycophytes are relatively small plants.

The scientific names and the informal English names used for this group of plants are ambiguous. For example, "Lycopodiophyta" and the shorter "Lycophyta" as well as the informal "lycophyte" may be used to include the extinct zosterophylls or to exclude them. (Full article...)
|more= (an empty value)
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The lycophytes, when broadly circumscribed, are a group of vascular plants that include the clubmosses. They are sometimes placed in a division Lycopodiophyta or Lycophyta or in a subdivision Lycopodiophytina. They are one of the oldest lineages of extant (living) vascular plants; the group contains extinct plants that have been dated from the Silurian (ca. 425 million years ago). Lycophytes were some of the dominating plant species of the Carboniferous period, and included the tree-like Lepidodendrales, some of which grew over 40 metres (130 ft) in height, although extant lycophytes are relatively small plants.

The scientific names and the informal English names used for this group of plants are ambiguous. For example, "Lycopodiophyta" and the shorter "Lycophyta" as well as the informal "lycophyte" may be used to include the extinct zosterophylls or to exclude them. (Full article...)

The lycophytes, when broadly circumscribed, are a group of vascular plants that include the clubmosses. They are sometimes placed in a division Lycopodiophyta or Lycophyta or in a subdivision Lycopodiophytina. They are one of the oldest lineages of extant (living) vascular plants; the group contains extinct plants that have been dated from the Silurian (ca. 425 million years ago). Lycophytes were some of the dominating plant species of the Carboniferous period, and included the tree-like Lepidodendrales, some of which grew over 40 metres (130 ft) in height, although extant lycophytes are relatively small plants.

The scientific names and the informal English names used for this group of plants are ambiguous. For example, "Lycopodiophyta" and the shorter "Lycophyta" as well as the informal "lycophyte" may be used to include the extinct zosterophylls or to exclude them. (Full article...)
|more=Foobar
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The lycophytes, when broadly circumscribed, are a group of vascular plants that include the clubmosses. They are sometimes placed in a division Lycopodiophyta or Lycophyta or in a subdivision Lycopodiophytina. They are one of the oldest lineages of extant (living) vascular plants; the group contains extinct plants that have been dated from the Silurian (ca. 425 million years ago). Lycophytes were some of the dominating plant species of the Carboniferous period, and included the tree-like Lepidodendrales, some of which grew over 40 metres (130 ft) in height, although extant lycophytes are relatively small plants.

The scientific names and the informal English names used for this group of plants are ambiguous. For example, "Lycopodiophyta" and the shorter "Lycophyta" as well as the informal "lycophyte" may be used to include the extinct zosterophylls or to exclude them. (Foobar)

The lycophytes, when broadly circumscribed, are a group of vascular plants that include the clubmosses. They are sometimes placed in a division Lycopodiophyta or Lycophyta or in a subdivision Lycopodiophytina. They are one of the oldest lineages of extant (living) vascular plants; the group contains extinct plants that have been dated from the Silurian (ca. 425 million years ago). Lycophytes were some of the dominating plant species of the Carboniferous period, and included the tree-like Lepidodendrales, some of which grew over 40 metres (130 ft) in height, although extant lycophytes are relatively small plants.

The scientific names and the informal English names used for this group of plants are ambiguous. For example, "Lycopodiophyta" and the shorter "Lycophyta" as well as the informal "lycophyte" may be used to include the extinct zosterophylls or to exclude them. (Foobar)
|more=false
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{{Transclude list item excerpt}}{{Transclude list item excerpt/sandbox}}

The lycophytes, when broadly circumscribed, are a group of vascular plants that include the clubmosses. They are sometimes placed in a division Lycopodiophyta or Lycophyta or in a subdivision Lycopodiophytina. They are one of the oldest lineages of extant (living) vascular plants; the group contains extinct plants that have been dated from the Silurian (ca. 425 million years ago). Lycophytes were some of the dominating plant species of the Carboniferous period, and included the tree-like Lepidodendrales, some of which grew over 40 metres (130 ft) in height, although extant lycophytes are relatively small plants.

The scientific names and the informal English names used for this group of plants are ambiguous. For example, "Lycopodiophyta" and the shorter "Lycophyta" as well as the informal "lycophyte" may be used to include the extinct zosterophylls or to exclude them.

The lycophytes, when broadly circumscribed, are a group of vascular plants that include the clubmosses. They are sometimes placed in a division Lycopodiophyta or Lycophyta or in a subdivision Lycopodiophytina. They are one of the oldest lineages of extant (living) vascular plants; the group contains extinct plants that have been dated from the Silurian (ca. 425 million years ago). Lycophytes were some of the dominating plant species of the Carboniferous period, and included the tree-like Lepidodendrales, some of which grew over 40 metres (130 ft) in height, although extant lycophytes are relatively small plants.

The scientific names and the informal English names used for this group of plants are ambiguous. For example, "Lycopodiophyta" and the shorter "Lycophyta" as well as the informal "lycophyte" may be used to include the extinct zosterophylls or to exclude them.

References

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