OpenLLM-France/wikimedia huggingface dataset:
# Wayne Hearn

Wayne Hearn (born August 5, 1962) is an American former professional tennis player.
Born in Charlotte, North Carolina, Hearn won the North Carolina state championship in 1980 at South Mecklenburg High School. He played two seasons of collegiate tennis for the University of North Carolina. He won an ACC championship in 1984 at No. 2 singles and was ACC Player of the Year in 1985.
Hearn competed on the professional tour in the late 1980s and had a best world ranking of 247. He qualified for the main draw of the 1987 US Open and upset world number 33 Ulf Stenlund in the first round, then fell in the second round to Jimmy Connors.
# Muhammad Anwar (politician)

Muhammad Anwar is a Pakistani politician who has been a member of the Gilgit Baltistan Assembly since November 2020.

## Political career

Anwar contested the 2020 Gilgit-Baltistan Assembly election on 15 November 2020 from GBA-16 (Diamer-II) on the ticket from Pakistan Muslim League (N). He won the election by the margin of 669 votes over the Independent runner up Attaullah. He garnered 6415 votes while Attaullah received 5746 votes.
# Zawady, Sieradz County

Zawady is a village in the administrative district of Gmina Błaszki, within Sieradz County, Łódź Voivodeship, in central Poland. It lies approximately 4 kilometres (2 mi) east of Błaszki, 20 km (12 mi) west of Sieradz, and 70 km (43 mi) west of the regional capital Łódź.
# Zawodzie, Radomsko County

Zawodzie is a village in the administrative district of Gmina Wielgomłyny, within Radomsko County, Łódź Voivodeship, in central Poland. It lies approximately 5 kilometres (3 mi) north-west of Wielgomłyny, 20 km (12 mi) east of Radomsko, and 84 km (52 mi) south of the regional capital Łódź.
# Zbęk

Zbęk is a village in the administrative district of Gmina Skomlin, within Wieluń County, Łódź Voivodeship, in south-central Poland. It lies approximately 3 kilometres (2 mi) east of Skomlin, 13 km (8 mi) south-west of Wieluń, and 100 km (62 mi) south-west of the regional capital Łódź.

## History

During the German occupation of Poland (World War II), in 1940, the German gendarmerie carried out expulsions of Poles, who were either enslaved as forced labour in the region or deported to the General Government in the more eastern part of German-occupied Poland. Houses and farms of expelled Poles were handed over to German colonists as part of the Lebensraum policy.
# Zduny, Łowicz County

Zduny is a village in Łowicz County, Łódź Voivodeship, in central Poland. It is the seat of the gmina (administrative district) called Gmina Zduny. It lies approximately 10 kilometres (6 mi) north-west of Łowicz and 47 km (29 mi) north-east of the regional capital Łódź.
# Zdziechów Nowy

Zdziechów Nowy is a village in the administrative district of Gmina Lutomiersk, within Pabianice County, Łódź Voivodeship, in central Poland. It lies approximately 5 kilometres (3 mi) north of Lutomiersk, 21 km (13 mi) north-west of Pabianice, and 19 km (12 mi) west of the regional capital Łódź.
From 1975 to 1998, the town belonged administratively to the Sieradz Voivodship.
# Dytikosicula

Dytikosicula is a genus of Cambrian arthropod from the Marjum Formation of Utah. It contains one species, Dytikosicula desmatae. The taxon may be synonymous with Dicranocaris, however this is uncertain.

## Description

Dytikosicula's affinity is unclear, although it may be allied with the megacheirans like its apparent relative Dicranocaris. Unusually its head is not preserved aside from a head shield, meaning the possible "great appendages" common to megacheirans cannot be seen. In addition, no appendages of any kind are preserved, further complicating matters. Dytikosicula differs from Dicranocaris by having a pleural extension on its first trunk segment, alongside a somewhat more circular head. The two also differ due to the latter being conspicuously larger. Due to this, material formerly assigned to Dicranocaris from the Wheeler Formation may belong to this genus instead. These specimens, despite being poorly preserved, may show evidence of a pleuron on the first trunk segment. This genus also shares similarities with Serracaris from the Kinzers Formation, namely an elongate trunk with large pleurae. However, in Serracaris these tergal extensions seem to be doubled, alongside a posterior segment having relatively larger extensions.

## Etymology

Dytikosicula derives from the Greek word for west, dytikos, and the word for a small dagger, sicula, in combined reference to the geological area where the fossils are from and the recurved paratergal extensions. The species name, desmatae, derives from the Greek word desmos meaning "chain", in reference to its proposed link to other Cambrian megacheirans.
# Lin Shu-fen

Lin Shu-fen (Chinese: 林淑芬; pinyin: Lín Shūfēn; Wade–Giles: Lin Shu-fen; born 17 January 1973) is a member of the Democratic Progressive Party who is in the Legislative Yuan in Taiwan.

## Education

Lin obtained her bachelor's degree in social development from Shih Hsin University.

## Political careers
### 2016 legislative election

Legislative Election 2016: New Taipei 2nd district :
| Party | Party | Candidate | Votes | % |
| | DPP | Lin Shu-fen | 123,299 | 68.75 |
| | Kuomintang | Chen Ming-yih | 56,057 | 31.25 |
| Majority | Majority | Majority | 67,242 | 37.50 |
| Total valid votes | Total valid votes | Total valid votes | 179,356 | 97.62 |
| Rejected ballots | Rejected ballots | Rejected ballots | 4,380 | 2.38 |
| | DPP hold | DPP hold | Swing | |
| Turnout | Turnout | Turnout | 183,736 | 66.88 |
| Registered electors | Registered electors | Registered electors | 274,711 | |
# Sugden Audio

Sugden Audio is a British engineering company that manufactures hi-fi and audio equipment. Founded by James Edward Sugden in Cleckheaton, West Yorkshire in 1967, the company is best known as the manufacturer of the Sugden A21 amplifier.
Sugden had been involved in the manufacture of scientific equipment since 1960 with his company Research Electronics. Sugden was keenly interested in hi-fi, in particular in overcoming the problem of crossover distortion common in Class B solid state amplifier designs at the time. He developed a Class-A amplifier, the Si 402, which avoided this, however it was extremely expensive, costing 100 Guineas (£105, equivalent to £2,400 in 2023) and few if any were sold. At the time, Sugden was the only company in the industry using Class A design in their Hi-Fi amplifiers.
The following year Sugden agreed to work with local loudspeaker manufacture Richard Allan, which would market Sugden's amplifiers under their brand name. In April 1968 the A21 amplifier was premiered at an audio fair in London. It would sell for a much more attractive £52 and received good reviews in the audio press.
Shortly after they set up a factory at Carr Street in Cleckheaton in West Yorkshire and started producing the A21 amplifier under their name. They subsequently expanded their range of products to include other amplifiers and tuners.
In 1981, they relocated to Valley Road in Heckmondwike where they remain.
# Hiding Place

The Hiding Place or Hiding Place may refer to:

## Film

* The Hiding Place (Playhouse 90), March 22, 1960 episode of American TV series; based on Robert Shaw's 1959 novel
* The Hiding Place (film), 1975 American drama based on the 1971 book by Corrie ten Boom
* The Hiding Place, 2000 American drama starring Kim Hunter and Timothy Bottoms, from the play by Mitch Giannunzio
* The Hiding Place, 2008 American drama by Jeff Whitty

## Literature

* The Hiding Place, 1959 British novel by Robert Shaw
* The Hiding Place (biography), 1971 memoir by Corrie ten Boom, who hid Dutch Jews during WWII
* Hiding Place (Wideman novel), 1981 middle volume of "Homewood Trilogy" by American John Edgar Wideman
* The Hiding Place (Azzopardi novel), 2000 Welsh Booker Prize shortlist
* The Hiding Place (Bell novel), 2012 American mystery

## Music

* Hiding Place (band), Scottish rock band, active from 2004 to 2007
* Hiding Place (Selah album), 2004
* Hiding Place (Don Moen album), 2006
* Hiding Place (Tori Kelly album), 2018
# Shichikenjaya Station

Shichikenjaya Station (七軒茶屋駅, Shichikenjaya-eki) is a JR West Kabe Line station located in Midorii, Asaminami-ku, Hiroshima, Hiroshima Prefecture, Japan.

## History

* December 25, 1910: Opened by extending the Japan Railway Hiroshima Branch Line (at that time) between Furuichibashi Station and Otagawa Bridge (current Kami-Yagi Station). Passenger station.
* March 11, 1919: The Hiroshima Branch Line of the Great Japan Railway is transferred to Kabe Railway, and becomes the company's station.
* May 1, 1926: Kabe Railway was merged with Hiroshima Electric and became the company's station.
* July 1, 1931: Hiroshima Electric Line is transferred to Hirohama Railway and becomes the company's station.
* September 1, 1936: Hirohama Railway nationalized.
* April 1, 1960: Japan Transport and Tourism Co., Ltd. entrusts station operations. Becomes a consignment station.
* May 1, 1973: National Railways (→JR) becomes a station in "Hiroshima City" in the specified metropolitan city system.
* April 1, 1987: West Japan Railway (JR West Japan) inherited by the division and privatization of the Japanese National Railways.
* October 2004: The business hours of the counter are changed and it will be open only on weekdays. In addition, the window will be closed during some hours during business hours.
* 2007:
** July 29: ICOCA-compatible simplified automatic ticket gate installed.
** September 1: IC card "ICOCA" will be available.
* March 15, 2008: Moved about 100m to Hiroshima, and the platform became compatible with 4-car trains. In addition, it will be an unmanned station.
* August 20, 2014: A landslide occurred in Hiroshima City due to heavy rain in August 2014. The operation between Midorii Station and Kabe Station was suspended until August 31.

## Around the station

The station building is located on the right bank (west bank) of the Furukawa River, a tributary of the Otagawa River. On the west side, there is a mountainous area from Mt. Gongen (397 m above sea level) to Mt. Abu (Hiroshima Prefecture) (586 m above sea level), and there are few plains around the station. Some of the residential areas on the west side of the station are lined up on slopes facing the mountains, and this slope is thought to be an alluvial fan formed by repeated accumulations of earth and sand from past debris flows. Prefectural highway and National highway run parallel to the Kabe line on the east side of the station. In particular, roadside stores are located along the national highway, making it a major commercial area.

## Station layout

Shichikenjaya Station features one side platform handling one bidirectional track. The station is unmanned, and contains an automatic ticket machine.

### Platforms

| 1 | ■ Kabe Line | for Hiroshima, Kabe, Aki-Kameyama |
# Willow Mountain

Willow Mountain is a 3,826-foot-elevation (1,166-meter) summit in Brewster County, Texas, United States.

## Description

Willow Mountain is set in the Christmas Mountains and the Chihuahuan Desert. The mountain is composed of 43-million-year-old volcanic rock which formed columnar jointing as displayed on the west face. Although modest in elevation, topographic relief is significant as the summit rises 1,000 feet (305 m) above Highway 118 in one-half mile (0.8 km). Based on the Köppen climate classification, Willow Mountain is located in a hot arid climate zone with hot summers and mild winters. Any scant precipitation runoff from the mountain's slopes drains to the Rio Grande via Bens Hole Creek and Terlingua Creek. The mountain's toponym has been officially adopted by the United States Board on Geographic Names, and has been listed in publications since at least 1904. The mountain may be named in association with Willow Spring at the south base of the mountain where the spring supports desert willows.

## Geology

Willow Mountain is the most spectacular display of rock joints in the southern Big Bend area. The mountain mass is an intrusive plug, which cooled below the surface and was subsequently uncovered by erosion. On cooling, the rock mass contracted and was uniformly jointed. After erosion uncovered this mass, weathering and erosion removed the soft areas to expose the joint pattern.
# Wolverine Peak

Wolverine Peak is a mountain in the Absaroka Range in the state of Montana, United States. It has a height of 10,479 feet (3,194 m) and is located in the Park County. The summit of Wolverine Peak is located at the triple border point between the Absaroka-Beartooth Wilderness, Custer National Forest and Yellowstone National Park.
# Wright Mountain (Texas)

Wright Mountain is a 6,031-foot-elevation (1,838-meter) summit in Brewster County, Texas, United States.

## Description

Wright Mountain is set within Big Bend National Park, the Chihuahuan Desert, and the Chisos Mountains. The mountain is composed of volcanic rock which formed during the Oligocene period. Although modest in elevation, topographic relief is significant as the summit rises 1,800 feet (549 m) above the surrounding terrain in one mile (1.6 km). Based on the Köppen climate classification, Wright Mountain is located in a hot arid climate zone with hot summers and mild winters. Any scant precipitation runoff from the mountain's slopes drains northeast to Tornillo Creek which is a tributary of the Rio Grande. The lower slopes of the peak are covered by juniper, oak, and piñon. The mountain's toponym was officially adopted in 1948 by the United States Board on Geographic Names to honor George Melendez Wright (1904–1936), an American biologist who conceived of, then conducted, the first scientific survey of fauna for the National Park Service between 1929 and 1933. He advanced quickly with the National Park Service, in 1933 becoming the first leader of the agency's new Wildlife Division. In 1936, Wright was part of an international commission to investigate the potential values of a protected area to straddle the Rio Grande area of Texas and Mexico. The report was enthusiastic and the commission endorsed the national park idea. Tragically, George Wright and Roger Toll were killed in a car accident on their return from Texas. Toll and Wright Mountains were named in their memory.
# Okukenu

Okukenu Sagbua (c. 1790–1862) was a Yoruba Egba chief. He was a founding member of the Ogboni of Egbaland, and also served as the first Alake of Egbaland.

## Life

Okùkẹ́nù was born sometime in the 1790s to Ọ̀ṣọ́ of Igbein in Egba Ake and Matiku, who was herself from Imo, a town that was also in Egba Ake. His mother was a daughter of Adesomi, who was one of the daughters of Lukoye. Lukoye was a son of Laarun, an Alake of the Egba who ruled in the 18th century. His mother was also related to Deliyi, an early figure in Abeokuta history, who was the Balogun of the town of Ijemo.
Upon the exodus of the Egba refugees to the comparative safety of Olumo Rock in Abeokuta in the aftermath of their homeland's destruction during the Yoruba Civil Wars, the traditional councils of chiefs - otherwise known as the Ogboni - that had formerly governed them were reconstituted. Okukenu was co-opted into the civil council during this exercise, and so his erstwhile title - Sagbua - was recognized as a civil one thereafter, even though it had originally been a military rank as an Eso Ikoyi title.
Following the death of the Egba paramount chief Shodeke in 1845, Okukenu and a brace of other powerful chiefs ruled Abeokuta jointly for a time. The rivalry that existed between them led to an anarchy that was only exacerbated by the slave trade, which was then at its peak.
After the death of the Losi of Ake (hitherto a favourite to succeed Shodeke), Okukenu was chosen and crowned on 8 August 1854. Before his crowning, he unsuccessfully attempted to retrieve the head of the murdered Alake, Okikilu, who was the last paramount chief of the Egba people before the migration to Abeokuta.
Following his coronation, he became the first Alake to rule in the fortified city of Abeokuta. As an ex-civil chief, he had the support of the civil chiefs during his reign, but was opposed by both the war chiefs and the trade chiefs, who had both profited from the state of anarchy. Okukenu managed to maintain order in his kingdom despite their efforts, though his authority wasn't great. He was supported in this by Bashorun Apati, a former rival, who held office during his reign as the prime minister of Egbaland.
Okukenu died on August 31, 1862. During the subsequent interregnum, Bashorun Shomoye, a cousin of his, administered the kingdom.

## Marriage and family

Okukenu had many wives and children. One of his wives, Efunwunmi, was originally a wife to another high chief - the Baase of Igbein - and had a son by him by the name of Arikuola. Upon seeing Efunwunmi, Okukenu decreed that she must be his wife, and forcefully took her as such. Okukenu and Efunwunmi's son, Gbadebo (who was born in June 1854), later went on to become Gbadebo I, the Alake of Egbaland.

## Descendants

Okukenu's great-grandson, Adedotun Aremu Gbadebo III, is the current Alake of Egbaland.
# Altar of Sacrifice

Altar of Sacrifice is a 7,505-foot (2,288 m) Navajo Sandstone mountain in Zion National Park in Washington County, Utah, United States, that is part of the Towers of the Virgin.

## Description

Altar of Sacrifice is situated 2.5 mi (4.0 km) west-northwest of Zion's park headquarters, towering 3,500 feet (1,100 m) above the floor of Zion Canyon and the Virgin River which drains precipitation runoff from this mountain. Its nearest higher neighbor is The West Temple, one mile (1.6 km) to the south. Other neighbors include The Witch Head, Meridian Tower, Bee Hive, The Sentinel, Mount Spry, Bridge Mountain, and Mount Kinesava.

## Etymology and naming

Altar of Sacrifice, The Great White Throne, and Angels Landing were named by Methodist Minister Frederick Vining Fisher from Ogden during a visit to Zion Canyon in 1916. This feature's name gained its appropriateness from dark red stains caused by hematite (iron oxide) that appear on the face of the east wall, as though great quantities of blood had been spilled from the top. Altar of Sacrifice's name was officially adopted in 1934 by the U.S. Board on Geographic Names.

## Climate

Spring and fall are the most favorable seasons to visit Altar of Sacrifice. According to the Köppen climate classification system, it is located in a Cold semi-arid climate zone, which is defined by the coldest month having an average mean temperature below 32 °F (0 °C), and at least 50% of the total annual precipitation being received during the spring and summer. This desert climate receives less than 10 inches (250 millimeters) of annual rainfall, and snowfall is generally light during the winter.

## Gallery

* The West Temple (left), The Sundial, The Witch Head, Altar of Sacrifice (right)
* The West Temple (left), Altar of Sacrifice (right)
* Towers of the Virgin. Left to rightː The Sundial, The Witch Head, Broken Tooth, Rotten Tooth, Altar of Sacrifice (upper right).
* Altar of Sacrifice (centered) seen from summit of The Watchman
* The Witch Head, Broken Tooth, Rotten Tooth, Altar of Sacrifice
# Balakai Mesa

Balakai Mesa is a summit in the U.S. state of Arizona.
Balakai Mesa is a name derived from the Navajo language meaning "place with reeds on it".
# Bee Hive (peak)

Bee Hive is a 6,904 feet (2,104 m) Navajo Sandstone mountain in Zion National Park in Washington County, Utah, United States, that is part of the Towers of the Virgin.

## Description

Bee Hive is located north of the park headquarters at the south entrance to Zion Canyon. The east face of Bee Hive, named The Streaked Wall, rises 2,900 feet (880 m) above the floor of Zion Canyon, and is a venue for big wall climbing. Neighbors include Altar of Sacrifice and Meridian Tower to the west, and The Sentinel to the northeast. The peak's descriptive name is for the beehive shape of the summit. This name was officially adopted in 1934 by the U.S. Board on Geographic Names. Precipitation runoff from the mountain drains into the North Fork Virgin River.

## Climate

Spring and fall are the most favorable seasons to see Bee Hive Peak. According to the Köppen climate classification system, it is located in a Cold semi-arid climate zone, which is defined by the coldest month having an average mean temperature below 32 °F (0 °C), and at least 50% of the total annual precipitation being received during the spring and summer. This desert climate receives less than 10 inches (250 millimeters) of annual rainfall, and snowfall is generally light during the winter.

## Climbing Regulations

A bivouac permit is required from the park visitor center for any climbs expected to last overnight.

## Gallery

* The West Temple behind Bee Hive at sunrise
* Bee Hive Peak (left) with The Streaked Wall featured. Note the white Navajo Sandstone of the beehive shaped summit. The peak to right is The Sentinel.
* Bee Hive Peak with The Streaked Wall
* Bee Hive Peak seen from museum
* The Streaked Wall
# Bull Mountain (Garfield County, Utah)

Bull Mountain is a 9,187-foot (2,800 m) elevation summit located in northern Garfield County of Utah, United States. Bull Mountain is part of the Henry Mountains which are set between Capitol Reef National Park to the west, and Glen Canyon National Recreation Area to the east. Mount Ellen is immediately southwest of Bull Mountain, and Burr Desert spreads out to the northeast. It is situated in a dry, rugged, and sparsely settled region, set on primitive land administered by the Bureau of Land Management. Precipitation runoff from this mountain drains into tributaries of the Colorado River. The nearest town is Hanksville, 17 miles to the north, and Robbers Roost is 20 miles to the northeast.

## Climate

Spring and fall are the most favorable seasons to visit Bull Mountain. According to the Köppen climate classification system, it is located in a Cold semi-arid climate zone, which is defined by the coldest month having an average mean temperature below 32 °F (0 °C), and at least 50% of the total annual precipitation being received during the spring and summer. This desert climate receives less than 10 inches (250 millimeters) of annual rainfall, and snowfall is generally light during the winter.

## Gallery

* South aspect
* Northeast aspect
* From the north
* North aspect
# Castle Dome (Zion National Park)

Castle Dome is a 7,054-foot (2,150 m) elevation Navajo Sandstone summit located in Zion National Park, in Washington County of southwest Utah, United States. Castle Dome is situated northwest of Zion Lodge, towering 2,800 feet (850 m) above the lodge and the floor of Zion Canyon. It is set on the west side of the North Fork Virgin River which drains precipitation runoff from this mountain. It is wedged between Behunin Canyon and Heaps Canyon, with the popular Emerald Pools set at the southeast foot of this mountain. Its neighbors include Mount Majestic, Cathedral Mountain, The Great White Throne, Red Arch Mountain, Mountain of the Sun, and Lady Mountain. This feature's name was officially adopted in 1934 by the U.S. Board on Geographic Names.

## Climate

Spring and fall are the most favorable seasons to visit Castle Dome. According to the Köppen climate classification system, it is located in a Cold semi-arid climate zone, which is defined by the coldest month having an average mean temperature below 32 °F (0 °C), and at least 50% of the total annual precipitation being received during the spring and summer. This desert climate receives less than 10 inches (250 millimeters) of annual rainfall, and snowfall is generally light during the winter.

## Gallery

* Castle Dome from Zion Lodge
* Castle Dome (left), The Spearhead (right)
* Castle Dome from Zion Lodge