OpenLLM-France/wikimedia huggingface dataset:
# Ford, Gloucestershire

Ford is a hamlet in Gloucestershire, England.
Ford lies on the B4077 road where it crosses the upper reaches of the River Windrush between Tewkesbury and Stow-on-the-Wold. The nearest village is Cutsdean a mile to its north.
# Perry Street Historic District (Helena–West Helena, Arkansas)

The Perry Street Historic District encompasses a fine collection of early-20th century architecture in Helena–West Helena, Arkansas. It includes fifteen buildings, arrayed on the single city blocks stretching south and west from the junction of Perry and Pecan Streets. The buildings on these blocks represent a cross-section of private and public architecture spanning 1880–1930, including two churches, the only synagogue in Phillips County (the 1913 Temple Bethel), and the county's oldest public building, the 1879 Helena Library and Museum. Most of the residences in the district were built between 1900 and the 1920s. Although most of the residential architecture is Arts and Crafts in style, it includes two fine Queen Anne Victorians: the Moore House at 608 Perry (built 1900) and the William Nicholas Straub House at 531 Perry (also built 1900).
The district was listed on the National Register of Historic Places (NRHP) in 1986.
# Going to Bed Under Difficulties

Le Déshabillage impossible, released in the United States as Going to Bed Under Difficulties and in the United Kingdom as An Increasing Wardrobe, is a 1900 French short silent comedy trick film, directed by Georges Méliès. In the film, a man attempts to undress so he can go to sleep.

## Plot

A man in a hotel room wants to sleep for the night. He takes off his suit (placing it on a clothing rack) and his trousers (placing them on a chair), but then finds himself wearing a coat and hat that have appeared magically. The man removes them, but a new hat and a plaid pair of trousers appear in their places. He removes these clothes as well; this process repeats, with the man undoing each addition of clothing with more and more agitation.
The end of the film is lost; according to a contemporary catalogue description, the man's attempt to undress ends with him rolling about on the floor and on the bed, and finally collapsing in an epileptic seizure.

## Production and release

Méliès plays the man in the film. An editing effect called the substitution splice was used for the magically appearing clothes. An American catalogue mentions that the end of the film also uses fast motion photography as a special effect; if so, it is the only known Méliès film to do so. (It is difficult to verify whether fast motion was used at the end, since the last few seconds appear to be missing from the surviving print.)
The film was released by Méliès's Star Film Company and numbered 312–313 in its catalogues.

## Historical significance

Going to Bed Under Difficulties marks the second use of the sight gag by Méliès in which a character, trying to undress, is foiled by magically appearing clothes; the first being Up-To-Date Spiritualism (1900). The gag was frequently recycled by rival studios over the following few years in a series of close imitations of the Méliès film, with titles such as Undressing Impossible (1901), Clothes Enchanted (1901), Undressing Extraordinary (1901), and The Inexhaustible Wardrobe (1902).
The broader concept on which the film is founded, that of clothes on revolt, had previously appeared in Méliès's film The Bewitched Inn. The film historian Paolo Cherchi Usai notes that the film evokes the concept of a split personality, a constantly recurring theme in Méliès's work:
   Méliès, constantly torn between unabashed playfulness and sheer perfectionism, was obsessed by the idea of multiple identity. He was so aware of his multiplicitous personality that he staged a revealing and somehow disturbing parody of himself in Going to Bed under Difficulties (1900), in which he tries to undress and sleep while different clothes in various styles systematically appear, at increasing speed, upon his body.
# A Perfect Crime (TV series)

A Perfect Crime (German: Rohwedder: Einigkeit und Mord und Freiheit) is a 2020 German docuseries released on Netflix on September 25, 2020. It centers on German politician Detlev Karsten Rohwedder, head of the Treuhandanstalt, who was assassinated at his home in Düsseldorf on April 1, 1991.

## Story

A Perfect Crime is a story described as Germany’s version of the assassination of JFK. In 1991, Detlev Karsten Rohwedder, the man given the unenviable task of privatizing state-run businesses in the former East Germany, was assassinated in his home in an affluent Dusseldorf neighborhood. The case was never solved, and this four-part series examines the story and tries to uncover the mystery.

## Cast

* Alfred Hartung as Günther Classen
* Tobias Kasimirowicz as Gerd Korinthenberg
* Beate Malkus as Birgit Hogefeld

## Notable interviewees

* Peter Bachsleitner, Rohwedder's chief of staff
* Hero Brahms, vice-president of the Treuhandanstalt
* Günther Classen, crime reporter, Düsseldorfer Express
* Peter-Michael Diestel, deputy Prime Minister and Minister of the Interior, GDR (April–October 1990)
* Willi Fundermann, spokesman for the German Federal Criminal Police Office (Bundeskriminalamt, BKA)
* Rainer Hofmeyer, head of the counter-terrorism section, BKA
* Christian "Flake" Lorenz, member of Neue Deutsche Härte band Rammstein, native of East Berlin
* Christa Luft, deputy Prime Minister and Minister of Economics, GDR (November 1989–March 1990)
* Winfried Ridder, expert on the Red Army Faction (RAF), Federal Office for the Protection of the Constitution
* Silke Maier-Witt, former member of the RAF, involved in kidnapping and murder of Hanns Martin Schleyer in 1977
* Thilo Sarrazin, economist, Ministry of Finance, West Germany/unified Germany
* Lutz Taufer, former member of the RAF, involved in West German Embassy siege in Stockholm in 1975
* Theo Waigel, Minister of Finance, West Germany/unified Germany (1989–98)

## Episodes

| No. | Title | Original release date |
| 1 | "Märtyrer (Martyr)" | September 25, 2020 (2020-09-25) |
| The murder of Detlev Rohwedder, shot as he stood by a window in his Düsseldorf home, shakes the nation. But insiders understood the danger he was in. |||
| 2 | "Kapitalist (Capitalist)" | September 25, 2020 (2020-09-25) |
| In a letter left at the scene of the crime the RAF claims responsibility for the assassination of Rohwedder; however, a lack of evidence and motivation shadow this in doubt. |||
| 3 | "Besatzer (Occupier)" | September 25, 2020 (2020-09-25) |
| Questions arise about the motivation behind the assassination of Rohwedder and whether or not it was the RAF or former Stasi officers. |||
| 4 | "Opfer (Victim)" | September 25, 2020 (2020-09-25) |
| Political tensions heat up after German reunification and East Germany's transition from socialism to capitalism. The police botch an operation to capture an RAF member and suspect in the assassination of Rohwedder. |||
# Higashi-Kuyakusho-Mae Station

Higashi-Kuyakusho-Mae Station (東区役所前駅) is a Sapporo Municipal Subway in Higashi-ku, Sapporo, Hokkaido, Japan. The station number is H05.

## Platforms

| 1 | ■ Tōhō Line | for Fukuzumi |
| 2 | ■ Tōhō Line | for Sakaemachi |

## History

The station opened on 2 December 1988 coinciding with the opening of the Toho Line from Sakaemachi Station to Hōsui-Susukino Station.

## Surrounding area

* Sapporo Beer Museum
* Sapporo Ōtani University
* Sapporo Otani Junior College
# Gakuen-Mae Station (Hokkaido)

Gakuen-Mae Station (学園前駅, Gakuen-Mae-eki) is a subway station on the Sapporo Municipal Subway Tōhō Line in Toyohira-ku, Sapporo, Hokkaido, Japan. It is numbered "H10".

## Platforms

| 1 | ■ Tōhō Line | for Fukuzumi |
| 2 | ■ Tōhō Line | for Sakaemachi |

## History

The station opened on 14 October 1994 coinciding with the opening of the Toho Line extension from Hōsui-Susukino Station to Fukuzumi Station.

## Surrounding area

* National Route 453, (to Date)
* National Route 36, (to Muroran)
* Hokkai Gakuen University
* Hokkai School of Commerce
# Standing Peachtree

Standing Peachtree was a Muscogee village and the closest Indian settlement to what is now the Buckhead area of Atlanta, Georgia. It was located where Peachtree Creek flows into the Chattahoochee River, in today's Paces neighborhood. It was located in the borderlands of the Cherokee and Muscogee nations. It is referred to in several documents dating as far back as 1782.

## Etymology

Standing Peachtree's name is an accurate preservation of its native Muscogee Indian name, Pakanahuili.
Some sources claim that "peachtree" is a corruption of "pitch tree", a supposed reference to pine trees from which pitch could be obtained. However, there is no evidence for the "pitch tree" name from before the 20th century, while "Standing Peachtree" can be traced back to the 18th century.

## Peachtree Street

Standing Peachtree was the end of the Muscogee Peachtree Trail, which ran from near Toccoa to just south of what is now Piedmont Hospital in Buckhead. (A marker now stands there at the corner of Peachtree St. and Palisades Rd.) At this junction the path split. One branch went to Standing Peachtree (Pace's Ferry and Moore's Mill roads were built along this path). The other branch ran southwards towards what is now Five Points in Downtown Atlanta. Thus, much of Atlanta's main street, Peachtree Street follows the earlier Indian path.

## Fort Peachtree

Fort Peachtree was built here in 1812. Later known as Fort Gilmer, it was connected to Fort Daniel at Hog Mountain in what is now Gwinnett County, by a path which came to be known as Old Peachtree Road. The Muskogee ceded the land that is now Metro Atlanta in 1821 as part of a series of coerced treaties that systematically removed tribal nations from Georgia. Standing Peachtree thus ceased its role as tribal trading post. It was established as the first post office in the newly established DeKalb County, preceding Decatur (the area would later become part of Fulton County). Montgomery's Ferry (later DeFoor's Ferry) across the river opened at Standing Peachtree in 1837 and the area soon became better known by that name. The post office closed in 1842.
# EV-E301 series

The EV-E301 series (EV-E301系) is a two-car battery electric multiple unit (BEMU) train type operated by East Japan Railway Company (JR East) on the Karasuyama Line and Tohoku Main Line since 15 March 2014. The train goes by the nickname "Accum" (Akyumu).

## Overview

Developed from the experimental "Smart Denchi-kun" battery railcar tested on the Karasuyama Line in 2012, the two-car EV-E301 series train operates as an electric multiple unit (EMU) under the 1,500 V DC overhead wire of the Tohoku Main Line between Utsunomiya and Hōshakuji, and on battery power over the 20.4 km (12.7 mi) non-electrified Karasuyama Line. It can also be recharged via its pantographs at a recharging facility specially built at Karasuyama Station.
The two-car trainsets are equipped with 190 kWh lithium-ion storage batteries, and the train has a maximum design speed of 100 km/h (62 mph), although it normally runs at up to 65 km/h (40 mph) at service.
* Set V1 running under overhead wires on the Tohoku Line in March 2014
* Set V1 being recharged at Karasuyama Station in March 2014

## Formation

The two-car trains are formed as shown below, with car 1 at the Utsunomiya end.
| Car No. | 1 | 2 |
| Designation | Mc' | Mc |
| Type | EV-E300 | EV-E301 |
| Weight (t) | 37.7 | 40.2 |
| Passenger capacity (seated/total) | 48/133 | 48/133 |
The Mc car has two PS38 single-arm pantographs.

## Interior

Internally, the train uses LED lighting throughout. Seating accommodation consists of longitudinal bench seating. The train is not equipped with a toilet.
* View of the interior
* Priority seating
* Equipment room and free space
* Driver's cab
* LCD display

## Bogies

Each car is mounted on a TR255D non-powered trailer bogie at the outer end, and a DT79 motored bogie at the inner end.
* TR233D trailer bogie
* DT79 motor bogie

## History

The first set, V1, was delivered from the Japan Transport Engineering Company (J-TREC) factory in Yokohama on 21 January 2014. Test running commenced on 23 January, on the Utsunomiya Line, including running on battery power with the pantographs lowered. It entered revenue service on the Karasuyama Line from the start of the revised timetable on 15 March 2014.
In May 2015, the EV-E301 series was awarded the 2015 Laurel Prize, presented annually by the Japan Railfan Club. A presentation ceremony was held at Karasuyama Station on 26 September 2015.
A further three two-car EV-E301 series trainsets were delivered to Utsunomiya from the J-TREC factory in Yokohama in February 2017. These entered service from the start of the revised timetable on 4 March 2017, replacing the remaining diesel multiple-unit trains operating on the Karasuyama Line.
# Mount Fitzhenry

Mount Fitzhenry is a 6,050-foot (1,840-metre) mountain summit located within Olympic National Park in Clallam County of Washington state. Mt. Fitzhenry is in the Bailey Range, which is a subrange of the Olympic Mountains. The mountain can be seen from the visitor center at Hurricane Ridge in clear weather. Its nearest higher neighbor is Mount Fairchild, 1.57 mi (2.53 km) to the south. Precipitation runoff from the mountain drains into tributaries of the Elwha River. Mount Fitzhenry is situated at the head of Fitzhenry Creek, and both are named for Edward Allen Fitzhenry (1868–1937), Clallam County surveyor from 1892-1900. President Woodrow Wilson appointed Fitzhenry as Washington Surveyor General in 1913, and he later served as Deputy State Land Commissioner.

## Climate

Based on the Köppen climate classification, Mount Fitzhenry is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Olympic Mountains. As fronts approach, they are forced upward by the peaks of the Olympic Range, causing them to drop their moisture in the form of rain or snowfall (Orographic lift). As a result, the Olympics experience high precipitation, especially during the winter months. During winter, weather is usually cloudy, but, due to high-pressure systems over the Pacific Ocean that intensify during summer, there is often little or no cloud cover during the summer. In terms of favorable weather, the best months for viewing and climbing are July through September.

## Geology

The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and basaltic oceanic crust. The mountains were sculpted during the Pleistocene era by erosion and glaciers advancing and retreating multiple times.

## Gallery

* Mount Fitzhenry centered
* Mount Fitzhenry centered, Hurricane Ridge Visitor Center on the right
# Hoshikawa Station (Mie)

Hoshikawa Station (星川駅, Hoshikawa-eki) is a passenger railway station located in the city of Kuwana, Mie Prefecture, Japan, operated by the private railway operator Sangi Railway.

## Lines

Hoshikawa Station is served by the Hokusei Line, and is located 5.5 kilometres from the terminus of the line at Nishi-Kuwana Station.

## Layout

The station consists of a single side platform serving bi-directional traffic. The station is unattended.

### Platforms

| 1 | ■ Sangi Railway Hokusei Line | For Nishi-Kuwana For Ageki |

## Adjacent stations

| « | « | Service | » | » |
| Sangi Hokusei Line |||||
| Ariyoshi | Ariyoshi | Local | Nanawa | Nanawa |

## History

Hoshikawa Station was opened on April 5, 1914 as a station on the Hokusei Railway, but was closed on May 10, 1916. The station was reopened on September 8, 1927 for freight operations only, and passenger operations were resumed on November 1, 1932. The Hokusei Railway became the Hokusei Electric Railway on June 27, 1934. The station was again closed on July 1, 1944, and not reopened until February 1, 1964. Through a series of mergers, the line became part of the Kintetsu network by April 1, 1965. The station was closed for a third time on May 15, 1969. The Sangi Railway was spun out of Kintetsu as an independent company on April 1, 2003. Hoshikawa Station was reopened again on March 26, 2005 with a new station building, located some 500 meters towards Ageki from its original location.

## Passenger statistics

In fiscal 2019, the station was used by an average of 797 passengers daily (boarding passengers only).

## Surrounding area

* Tsuda Gakuen Junior and Senior High School
# Stetson University Campus Historic District

The Stetson University Campus Historic District in DeLand, Florida was listed on the National Register of Historic Places on March 14, 1991. The district is bounded by Michigan Avenue, North Florida Avenue, West University Avenue and a line South from North Hayden Avenue. It contains 10 historic buildings and one historic structure.
Elizabeth Hall is Stetson University's signature building, a stately building of patterned brick rising three stories, with a four-story central brick pavilion topped by a snowy white cupola. In the early days the tower contained a water tank, which supplied the campus with water until city water became available. In 1915 the Eloise bell chimes replaced the water tank, but they were moved in 1934. The first major building on campus built by Stetson's early benefactor, Philadelphia hat manufacturer John B. Stetson, it is named for his wife, Elizabeth. The south wing contains a 786-seat chapel, with a magnificent German-made Beckerath 2,700-pipe manual organ surrounded by stained glass windows. The chapel is dedicated to Stetson's son Ben, who died at the age of 6. Elizabeth Hall was the first campus building to be wired for electricity during construction. Total construction cost for the 1892 central portion and two 1897 wings was $125,000 - more than the combined cost of all other Florida higher education buildings to that date. The chapel remains Stetson's main concert hall, and is often used by lecturers as well. Those appearing on its stage have included: William Jennings Bryan, Basil Rathbone, Robert Frost, Jimmy Carter, Andres Segovia, Ralph Nader, Desmond Tutu, Julian Bond, and Buckminster Fuller. Stetson's School of Music also stages about 100 concerts on its stage each year, and brings a variety of visiting musicians as well, adding greatly to the cultural offerings of the community. Elizabeth Hall was renovated in 1991 and 2001, and is in excellent condition.
# Umedoi Station

Umedoi Station (梅戸井駅, Umedoi-eki) is a passenger railway station located in the city of Inabe, Mie Prefecture, Japan, operated by the private railway operator Sangi Railway.

## Lines

Umedoi Station is served by the Sangi Line, and is located 13.1 kilometres from the terminus of the line at Kintetsu-Tomida Station.

## Layout

The station consists of a single island platform connected to the station building by a level crossing.

### Platforms

| 1 | ■ Sangi Line | For Kintetsu-Tomida |
| 2 | ■ Sangi Line | For Nishi-Fujiwara |

## Adjacent stations

| « | « | Service | » | » |
| Sangi Railway Sangi Line |||||
| Hokusei Chuo Koenguchi | Hokusei Chuo Koenguchi | Local | Daian | Daian |

## History

Umedoi Station was opened on July 23, 1931.

## Passenger statistics

In fiscal 2019, the station was used by an average of 135 passengers daily (boarding passengers only).

## Surrounding area

* Umedoi Post Office
# Mount Hancock (New Hampshire)

Mount Hancock is a mountain in Grafton County, New Hampshire, named after John Hancock (1737–1793), one of the Founding Fathers of the United States.
The mountain is on the south side of the Pemigewasset Wilderness, the source of the Pemigewasset River in the heart of the White Mountains, between Franconia Notch and Crawford Notch. Mount Hancock is flanked to the northeast by Mount Carrigain, to the south by Mount Huntington, and to the west by Mount Hitchcock. Prior to the completion of the Kancamagus Highway, Mount Hancock was one of the most remote, inaccessible peaks in the White Mountains.
The Appalachian Mountain Club considers both Mount Hancock and the officially unnamed peak to its south to be "four-thousand footers", because the south peak rises more than 200 feet (61 m) above the col that adjoins it to the higher north peak.
# Mount Higgins

Mount Higgins is a 5,176-foot-elevation mountain summit located at the western edge of the North Cascades Range, in Skagit County, Washington. Mount Higgins has two subsidiary summits, Skadulgwas Peak (4,986 ft) which is the fin-shaped middle peak, and also Mount Higgins Lookout Site (4,849 ft), the western sub-summit. The mountain is set on land administered by the Mount Baker–Snoqualmie National Forest. Mount Higgins is situated along the north side of State Route 530, mid-way between the communities of Darrington and Oso, near the site of the 2014 Oso mudslide. The nearest higher neighbor is Round Mountain, 0.93 miles (1.50 km) to the north-northeast. This mountain is named for Oso homesteader Walter Higgins. The first ascent was made in 1888 by John Higgins, Frank Lawrence, and Al Baker. Precipitation runoff from Mount Higgins drains into tributaries of the Stillaguamish River. Topographic relief is significant as the south aspect rises 4,800 feet (1,500 m) above the Stillaguamish in two miles.

## Climate

Mount Higgins is located in the marine west coast climate zone of western North America. Most weather fronts coming off the Pacific Ocean travel northeast toward the Cascade Mountains. As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range (orographic lift), causing them to drop their moisture in the form of rain or snowfall onto the Cascades. As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer.

## Geology

The North Cascades features some of the most rugged topography in the Cascade Range with craggy peaks, ridges, and deep glacial valleys. Geological events occurring many years ago created the diverse topography and drastic elevation changes over the Cascade Range leading to the various climate differences. These climate differences lead to vegetation variety defining the ecoregions in this area.
The history of the formation of the Cascade Mountains dates back millions of years ago to the late Eocene Epoch. With the North American Plate overriding the Pacific Plate, episodes of volcanic igneous activity persisted. In addition, small fragments of the oceanic and continental lithosphere called terranes created the North Cascades about 50 million years ago.
During the Pleistocene period dating back over two million years ago, glaciation advancing and retreating repeatedly scoured the landscape leaving deposits of rock debris. The U-shaped cross section of the river valleys is a result of recent glaciation. Uplift and faulting in combination with glaciation have been the dominant processes which have created the tall peaks and deep valleys of the North Cascades area.