OpenLLM-France/wikimedia huggingface dataset:
# Symphonaire Infernus et Spera Empyrium

Symphonaire Infernus et Spera Empyrium is the first EP by English doom metal band My Dying Bride. "Symphonaire" was made only a few months after signing to the Peaceville Records label. The song was also released as a vinyl record and an audio tape. The artwork was designed and created by Dave McKean, who also designed some of the band's other sleeves including "As the Flower Withers".
The EP was the band's first release as a 5-piece, following the introduction of bassist Adrian Jackson. The title track was originally recorded for the band's first demo, "Towards the Sinister". This version can be found on the compilation album "Meisterwerk 1". "God Is Alone" was originally recorded as a single that also includes "De Sade Soliloquay". These versions have not been re-released since their original appearance.
The EP was also released as part of the limited box-set, "The Stories", alongside the band's other singles, "The Thrash of Naked Limbs" and "I Am the Bloody Earth". All three were released on one disc on the compilation "Trinity" in 1995.
The song's video, available on "For Darkest Eyes" features bizarre imagery and slow-motion footage of the band members walking through the wilderness. The video version of the song is the edited version that appears as "Act 1" on the vinyl release of the EP. "Act 2" is the section of the songs which begins at 5:15 in the full-length version.
Live versions of the title track are available on "The Voice of the Wretched" and in the bonus features of the DVD version of "For Darkest Eyes".

## Track listing
### CD

* "Symphonaire Infernus et Spera Empyrium" – 11:39
* "God Is Alone" – 4:51
* "De Sade Soliloquay" – 3:42

### Vinyl

* "Symphonaire Infernus et Spera Empyrium Act 1"
* "Symphonaire Infernus et Spera Empyrium Act 2"

### Audio tape

* "Symphonaire Infernus et Spera Empyrium" – 11:39
* "God Is Alone" – 4:51
* "De Sade Soliloquay" – 3:42

## Personnel

* Aaron Stainthorpe - vocals
* Andrew Craighan - guitar
* Calvin Robertshaw - guitar
* Adrian Jackson - bass
* Rick Miah - drums

### Additional personnel

* Martin Powell - session violin
* Dave McKean - album artwork
# Westmill, Hitchin

Westmill is a residential area of Hitchin, in the North Hertfordshire district, in the county of Hertfordshire, England. It was originally built as a council housing estate in the 1920s. There is a primary school, Oughton Junior, Infant and Nursery School. It forms part of Oughton ward for local government purposes.
It is close to the Oughtonhead Common, a Local Nature Reserve, and Oughtonhead Lane, a geological Site of Special Scientific Interest.
# Dohoin Usu Formation

The Dohoin Usu Formation is a Late Cretaceous (Campanian) geologic formation in Mongolia. Dinosaur remains are among the fossils that have been recovered from the formation, although none have yet been referred to a specific genus.

## Fossil content

The formation has provided the following fossils:

### Reptiles

* Goniopholididae indet.
* Hadrosauridae indet.
* Nanhsiungchelyidae indet.

### Gastropods

* Gastropoda indet.
# Dovžan Gorge Formation

The Dovžan Gorge Formation (Slovene: dovžanovosoteška formacija) is a geologic formation in Slovenia. It preserves fossils dating back to the Permian period. The formation is named after the Dovžan Gorge.

## Fossil content

The following fossils have been reported from the formation:

### Trilobites

* Ditomopyge aff. kumpani
* Paraphillipsia aff. taurica
* Pseudophillipsia (Carniphillipsia) aff. caruancensis
* Neoproetus sp.
* Pseudophillipsia sp.

### Brachiopods

* Capillomesolobus heritschi
# Dukamaje Formation

The Dukamaje Formation is a geological formation in Niger and Nigeria whose strata date back to the Late Cretaceous. Dinosaur remains are among the fossils that have been recovered from the formation. A wealth of Mosasaur fossils have also been recovered from this formation, particularly from the area around Mt. Igdaman.

## Fossil content

Dinosaurs of the Dukamaje Formation :
| Taxa | Presence | Description | Images |
| Genus:  ?Bahariasaurus  ?B. ingens. | Geographically present in Département De Tahoua, Niger. | | |
Mosasaurs of the Dukamaje Formation :
| Taxa | Presence | Description | Images |
| Genus: Igdamanosaurus I. aegyptiacus | Geographically present on Mt. Igdaman, near the village of Igdaman (or In Daman). | Mid-sized globidensine mosasaur. Originally described as a plioplatecarpine. Durophagous. | Goronyosaurus and juvenile elasmosaurs |
| Genus: Goronyosaurus G. nigeriensis G. sp. | Type locality unknown. From the portion of the Dukamaje Formation located in Nigeria. Geographically present on Mt. Igdaman. From the portion of the Dukamaje Formation located in Niger. | Large mosasaur of uncertain affiliations. High number of foramina on the snout and small eyes indicate a murky-water hunter. | Goronyosaurus and juvenile elasmosaurs |
| Genus:  ?Angolasaurus  ?A. sp. | Geographically present on Mt. Igdaman. | Represented here by four vertebrae, one from a juvenile. Fragmentary state makes identification difficult. | Goronyosaurus and juvenile elasmosaurs |
| Genus: Halisaurus H. sp. | Geographically present on Mt. Igdaman. | Mid-sized mosasaur. Represented here by four vertebrae. | Goronyosaurus and juvenile elasmosaurs |
| Genus: Plioplatecarpus P. sp. | Geographically present on Mt. Igdaman. | Mid-sized plioplatecarpine mosasaur. Represented here by several vertebrae. | Goronyosaurus and juvenile elasmosaurs |
| Genus: Platecarpus P. sp. | Geographically present on Mt. Igdaman. | Mid-sized plioplatecarpine mosasaur. Represented here by a single fragmentary vertebrae. | Goronyosaurus and juvenile elasmosaurs |
| Genus: Mosasaurus cf. M. hoffmannii | Geographically present on Mt. Igdaman. | Massive mosasaurine mosasaur. Represented here by a fragmentary tooth crown. The first example of Mosasaurus from Niger and Nigeria. | Goronyosaurus and juvenile elasmosaurs |

### Other reptiles

* Sokotosuchus ianwilsoni
* Palaeophis sp.
* Podocnemis sp.
* Trematochampsa taqueti
* Libycosuchus sp.

### Fishes

* Asteracanthus aegyptiacus
* Igdabatis sigmodon
* Lamna nigeriana
* Schizorhiza stromeri
* Stephanodus lybicus
* Stratodus apicalis
* Ischyrhiza nigeriensis
* Ceratodus sp.
* Ginglymostoma sp.
* Pycnodus sp.
# El Salto Formation, Nicaragua

The El Salto Formation is a geologic formation in Nicaragua. It preserves fossils dating back to the Pliocene period.

## Fossil content

* Mysticeti indet.
# Etjo Sandstone

The Etjo Sandstone is an Early Jurassic geologic formation in northern Namibia. The formation overlies the Omingonde Formation in the Waterberg Basin and the Doros and Gai-As Formations in the Huab Basin and has a total thickness of 140 metres (460 ft). Fossil theropod tracks of Prosauropoda indet., Theropoda indet., Tetrapodium elmenhorsti, Saurichnium anserinum, S. damarense, S. parallelum and S. tetractis have been reported from the formation, deposited in an aeolian environment.
# Pin Oak, West Virginia

Pin Oak is an unincorporated community in Hampshire County in the U.S. state of West Virginia. Pin Oak is located along West Virginia Route 29 between Paw Paw and Forks of Cacapon. Pin Oak is roughly centered at the intersection of Pin Oak Road (West Virginia Secondary Route 29/3) and Cabin Run Road (West Virginia Secondary Route 29/4) with West Virginia Route 29. The old Pinoak School lies north of this intersection.

## Historic site

* Pin Oak Fountain, WV Route 29
# Hansa Pit

The Hansa Pit (German: Grube Hansa) was a mine on the territory of Harlingerode in the county of Wolfenbüttel in the Free State of Brunswick and later in Lower Saxony, West Germany. It was founded on the Langenberg south of Harlingerode; however, the only remainders are located on the north side.

## Geology

The Langenberg, internationally known for the discovery of Europasaurus and part of the Northern Harz Boundary Fault north of the Harz, consists of Korallenoolith with layers of chalky iron ore, containing up to 25% iron. On the northern part of the Hansa pit, limonite was more predominant and fossils of Orectolobiformes indet. were found.

## History
### 19th century

On behalf of consul Herrmann Henrich Meier, local geologist and director for mining administration Wilhelm Castendyck discovered the iron deposits beneath the Langenberg in the mid-19th century.

#### Hermann deposit

The earliest deposit, the Hermann deposit, was first mentioned in 1860 and established soon after that. It was located north of the Langenberg, where the remaining area around the opening hole is conserved nowadays. In order to reach the significant pyrolusite conglomerate beneath the Langenberg, a tunnel with a length of 187 metres was drilled. However, due to the strong mountain pressure and brittle rock, the tunnel needed further support and it was decided to extend the tunnel west- and eastwards instead. Due to unprofitability, the Hermann deposit was abandoned in 1867.

#### Hansa deposit

The relevant Hansa deposit was first documented in 1862. It was discovered as a characteristic Korallenoolith deposit in the Röseckenbach valley west of Göttingerode and southwest of the Langenberg. From here on, the seam was mined eastwards as far as to the outskirts of Schlewecke around 1.5 kilometres east.
A new area with the official name Hansa Pit was founded on June 3, 1865, west of where Göttingerode was founded later. Due to the very poor condition of roads at the location, the mine was temporarily closed in November 1865 until conditions improved.

### 20th century

The aftermath of the Great Depression caused the mine to be temporarily shut down on March 15, 1932. However, due to the German Nazi Party's plans to gain more autarky with their ressources, the mine was put back into operation on November 1, 1935. In order to provide sufficient living space for the necessary workers, the Göttingerode settlement was erected south of the Langenberg and next to the Hansa pit.
In 1938-39, a connection to the Oker–Bad Harzburg railway was established by erecting a chain conveyor to the Harlingerode station.
The Hansa pit was closed on August 23, 1960, due to lack of profitability.

## Links

* Regionalverband Harz: Hansa Mine (English), 2022
# Mount Lloyd George

Mount Lloyd George is a 2,938-metre (9,639 ft) peak in British Columbia, Canada, rising to a prominence of 1,208 metres (3,963 ft) above Lloyd George Pass. The mountain is located NE of Haworth Lake in Kwadacha Wilderness Provincial Park. Its line parent is Mount Sylvia, 37 kilometres (23 mi) away. It is part of the Northern Rocky Mountains.

## Geology

Lying in the Muskwa Ranges, Mount Lloyd George is a castellated limestone and quartzite peak. The diamictite sedimentary deposits of the mountain, several kilometers thick, date to the late Precambrian and probably have a glacial-marine origin. The age of the diamictite is not certain. It may be associated with either the Toby or the Vreeland formations of the North American Cordillera.

## Ice field

The Lloyd George Icefield in 1998 covered over 70 square kilometres (27 sq mi). There is a major concentration of glaciers around the mountain. The icefield is about 19 kilometres (12 mi) from north to south and 13 kilometres (8.1 mi) from east to west, bounded by the Warneford River and the Tuchodi River. The small Llanberis Glacier flows west from the icefield to Hawarth Lake. The larger Kwadacha and Lloyd George glaciers drain the icefield to the east.

## Name

The mountain was named by Paul Leland Haworth after David Lloyd George, the British Prime Minister towards the end of World War I. In the words of Raymond M. Patterson,
   It has been said, and with some truth, that the Rockies are the worst named mountain system in the world... Haworth, in a fit of wartime enthusiasm, decided to suggest that one further alien name be added to the ill-assorted register: as soon as he got out he would propose to Ottawa that the high mountain he had seen that day, holding the Great Glacier in its lap, should be called Mount Lloyd George. With regrettable haste his suggestion was adopted. Time and the verdict of history have not added to the stature of the little Welsh politician.
# Hutton Sandstone

The Hutton Sandstone is a geological formation of the Surat Basin in Queensland, Australia. The ferruginous sandstones and coal were deposited in a floodplain environment and dates back to the Bajocian.
# Iquiri Formation

The Iquiri Formation is an Eifelian to Frasnian geologic formation of central Bolivia. The formation comprises black shales and sandstones.

## Fossil content

The formation has provided fossils of Proteolobus walli.
# Kabu Formation

The Kabu Formation is a Late Cretaceous geologic formation of Middle Cenomanian age and is part of the Mifune Group. Dinosaur remains are among the fossils that have been recovered from the formation, although none have yet been referred to a specific genus. The formation was named by N. & K. Wasada in 1979.

## Vertebrate paleofauna

| Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
| Megalosauridae? (nicknamed Mifune-ryu) | Indeterminate | Mifune-ryu, Kami-Umeki | | "Tooth (discovered in 1979)" | Could have been the same animal as Mifunesaurus | |
| Mifunesaurus | No species given | Mifune-ryu, Kami-Umeki | | "Tibia, a phalanx, a metatarsus and a single tooth (tooth catalogued as YNUGI 10003; rest of the skeleton catalogued as MDM 341)" | Informal species. Often referred to Tetanurae indet. | |
# Lipeón Formation

The Lipeón Formation is a Telychian to Pridoli geologic formation of southern Bolivia and northwestern Argentina. The formation comprises sandstones and siltstones. Plant fossils comprising rhyniophytes (specifically Aberlemnia, Steganotheca, Tarrantia, Hostinella and Cooksonia) are scattered throughout, with some abundant concentrations on micaceous bedding plains. The fossil flora is the oldest of South America. Also present were quite diverse small, irregularly branching fragments possibly the tips of algae such as Buthotrephis or Hungerfordia.

## Correlations

The Lipeón Formation is laterally equivalent to the Kirusillas Formation. The formation is a potential source rock for shale oil and shale gas.

## Fossil content

The formation has provided the following fossils:
* Ornatosinuitina reyesi
* Slimonia boliviana
* Styliolina sp.
* Lingulata indet.

### Flora

* Aberlemnia
* Cooksonia
* Hostinella
* Steganotheca
* Tarrantia
# List of fossiliferous stratigraphic units in Guyana

This is a list of fossiliferous stratigraphic units in Guyana.

## List of fossiliferous stratigraphic units

| Group | Formation | Period | Notes |
| Rewa Group | Takutu Formation | Late Jurassic | |
# Merchantville Formation

The Merchantville Formation is a geological formation in the northeastern United States whose strata date back to the Late Cretaceous, around the time of the Santonian and Campanian age. Dinosaur remains are among the fossils that have been recovered from the formation.

## Vertebrate fauna

* Tyrannosauroidea (Dryptosauridae) indet. (="Cryptotyrannus")
* Hadrosauridae indet. (="Atlantohadros")
* Hadrosaurus foulkii
* Bothremys cooki
* Mosasaurus sp.
* Ornithomimidae indet.
* Pteranodon. sp?
# Navatrasierra

Navatrasierra is a village that is part of the Villar del Pedroso municipality in the province of Cáceres, Extremadura, Spain. According to the 2014 census, the village has a population of 198 inhabitants.

## Geography

Navatrasierra is located in a mountainous area between the Sierra de Altamira in the northeast and the Sierra del Hospital del Obispo; the latter's highest peak is 1443 m high. These ranges are part of the Montes de Toledo system.
The Navatrasierra Shale Formation from the Ordovician period, is named after this town.

## Local celebrations

* Santo Tomás Apóstol, on 21 December
# Necromys

Necromys is a genus of South American sigmodontine rodents allied to Akodon. This genus has also been known as Cabreramys or more recently Bolomys, and the northern grass mouse (N. urichi) has recently been transferred from Akodon.

## History

Most of the Brazilian members of the genus Necromys were first described in the second half of the nineteenth century, and the species from the Andes followed in the first decades of the twentieth century. Small rodents in South America were studied by the British zoologist Oldfield Thomas, curator at the Natural History Museum, London who erected the genus Bolomys in 1916.

## Characteristics

Members of the genus Necromys are spread out over a wide area of Central and South America. Morphologically, members of the genus are difficult to distinguish from two other genera found in the same region, the grass mice Akodon and the cane mice Zygodontomys. In 1987, the Argentine zoologist Osvaldo Reig listed the characteristics that distinguished the genus Bolomys from Akodon as; the braincase is broad and deep; the occipital region is short; the rostrum is fairly short; the rostrum tapers forwards when viewed from the side; the occiput is short and truncated; the zygomatic plate is broad, with the front edge straight or slightly concave; the upper incisors are orthodont or proodont; the molars are mesodont, broad and robust; the upper molars have transverse loops; and the lower molars have the lingual cusps slightly in front of the labial cusps.
There is very little variation in the karyotype of Necromys, where 2n=34 is the rule, with N. lactens and N. lasiurus having diploid numbers of 2n=36. This is in great contrast to the explosively radiating Akodon which has diploid numbers ranging from 2n=14 to 2n=52.

## Species

Species listed in Necromys include:
* N. amoenus Pleasant bolo mouse
* N. benefactus Argentine bolo mouse
* N. lactens Rufous-bellied bolo mouse
* N. lasiurus Hairy-tailed bolo mouse
* N. lenguarum Paraguayan bolo mouse
* N. lilloi
* N. obscurus Dark bolo mouse
* N. punctulatus Spotted bolo mouse
* N. temchuki Temchuk's bolo mouse
* N. urichi Northern grass mouse
* †N. bonapartei, Monte Hermoso Formation (Montehermosan)
# José Paulo Lanyi

José Paulo Lanyi (born April 10, 1970) is a Brazilian journalist, writer, producer, and filmmaker.
He is the author of the novel "Calixto – Azar de quem votou em mim" ("Calixto- Bad luck for whom voted for me", in free translation/Amazon) and of the 'scenic novel' "Deus me disse que não existe" ("God told me that he doesn't exist", in free translation/Chiado Books, Portugal)- 'scenic novel' is considered by Lanyi as a new literary genre that combines both novel and play (theatre).
Published by the Official Press of the State of São Paulo, his play "Quando dorme o vilarejo" ("When the village sleeps", in free translation), recognized in 2002 by the Brazilian Vladimir Herzog Award for Amnesty and Human Rights coverage, tells the story of a hamlet whose residents become happy when learn that they will be hanged by the community in which they live. Inspired by the surreal movies by Luis Buñuel, the play was staged with the United Nations support at the São Bento Theatre in São Paulo, on December 10, 2008.
Lanyi graduated in journalism from Faculdade Cásper Líbero in 1993. He has worked as a reporter for some of the major São Paulo television and radio networks, among them Globo TV, Rede Bandeirantes, Manchete TV, CBN Radio, Globo Radio, Radiobrás and CNT TV. He also collaborated with the literary magazine "Cult" and was a foreign correspondent in London (UK) in 1995.
He was a columnist for Observatório da Imprensa and Comunique-se media criticism websites and worked in São Paulo as a BBC freelance reporter and as a director of making of and as an executive producer for the 2017 film "Real- O Plano por trás da história" ("Real, The Plan Behind History").
In 2020 he published on Amazon his history play "Maquiavel, O Homem por Trás do Mal" ("Machiavelli, The Man Behind Evil").
Lanyi is a member of the São Paulo Association of Art Critics (Associação Paulista de Críticos de Arte) – APCA.

## Awards

Esso Journalism Award (2005) – given to allTV in recognition of their journalistic work. Lanyi was part of the news team, as host, producer, editor and reporter.
Vladimir Herzog Award (2002) – for his play "Quando dorme o vilarejo".
IBest Award (2005/2006) given to Comunique-se web portal (where Lanyi worked as a columnist), for their journalistic activities.

## List of works

* 2020 -"Maquiavel, O Homem Por Trás do Mal" ("Machiavelli, The Man Behind Evil"; play).
* 2012–2013/2018 – Crítica de Jornalismo (Criticism of journalism; collection of media criticism, 5 volumes).
* 2012 – O Artista Joseval e Quando Dorme o Vilarejo (The artist Joseval and When the village sleeps; play).
* 2012 – Vida a três (Three-person relationship in free translation; screenplay).
* 2012 – Balbúrdia Literária (Literary Shambles; chronic, poetry, short stories).
* 2002 – Quando Dorme o Vilarejo (When the village sleeps; play).
* 2002/2018 – Deus Me Disse que Não Existe (God told me that He doesn't exist; scenic novel).
* 2000 – Calixto – Azar de quem votou em mim (Calixto- Bad luck for whom voted for me; novel).

## Title

* Member of the São Paulo Association of Art Critics (APCA).
# José Cibrián

José Cibrián (February 25, 1916 – December 28, 2002), nicknamed Pepe, was an Argentine actor. Born in Buenos Aires, where he also died, he has an extensive filmography, including well-received movies such as Pájaro loco and La Cigarra no es un bicho. He starred in over 45 films between 1940 and 1981.

## Filmography

* Amor de mis Amores (1940)
* Jesús de Nazareth (1942) ... Jesús
* Santa (1943) ... Hipolito
* El Hombre de La Mascara de Hierro (1943)
* El Globo de Cantoya (1943)
* Asi son Ellas (1944)
* La Trepadora (1944)
* The Daughter of the Regiment (1944)
* Tribunal de Justicia (1944)
* The Lieutenant Nun (1944)
* El Secreto de la solterona (1945)
* Soltera y con gemelos (1945)
* Su Gran Ilusión (1945)
* Como tu Ninguna (1946)
* Más allá del Amor (1946)
* Los Maridos Engañan de 7 a 9 (1946)
* El Desquite (1947)
* Don't Marry My Wife (1947)
* La Mujer que quiere a dos (1947)
* The Earring (1951)
# Siriusgnathus

Siriusgnathus is a traversodontid cynodont from the Carnian channel sandstones and mudstones of the Candelária Formation, belonging to the Santa Maria Supersequence of the Paraná Basin in southeastern Brazil. It includes one species, Siriusgnathus niemeyerorum and was described in 2018. The species epithet refers to the Niemeyer locality in Agudo, Rio Grande do Sul. It was found together with various archosauromorphs, dinosauromorphs and other cynodonts, such as Brasilitherium riograndensis, Brasilodon quadrangularis, Irajatherium hernandezi and Prozostrodon brasiliensis.
# Sousa Formation

The Sousa Formation is a Berriasian-Hauterivian geologic formation in Paraíba, Brazil. Fossil sauropod tracks have been reported from the formation.

## Ichnofossils

Among others, these ichnofossils have been reported from the formation:
* Carnosauria indet.
* Coelurosauria indet.
* Moraesichnium barbarenae
* Sousaichnium pricei
* Sousatitanosauripus robsoni.
* Staurichnium diogenis
# Therioherpeton

Therioherpeton is an extinct genus of small, carnivorous cynodonts belonging to the clade Prozostrodontia, which lived in what is now Brazil during the Late Triassic. Its type species is Therioherpeton cargnini. It was named in 1975 by the palaeontologists José Bonaparte and Mário Costa Barberena based on remains collected in the Hyperodapedon Assemblage Zone of the Santa Maria Formation in the Paraná Basin.
# Valle de Ángeles Group

The Valle de Ángeles Group is a geologic group in Honduras. It preserves fossils such as ornithopod and iguanodontid dinosaurs dating back to the Late Albian to Early Turonian stages of the Cretaceous period.