OpenLLM-France/wikimedia huggingface dataset:
# Taylor Mountain (Sonoma County, California)

Taylor Mountain is a summit at the northern extreme of the Sonoma Mountains in California. The mountain lies in the Laguna de Santa Rosa drainage basin; its east flank drains to Matanzas Creek, a northwestward flowing stream running the length of Bennett Valley, and its west flank drains to Five Creek. The mountain is named after California Gold Rush pioneer John Shackleford Taylor, who settled on the mountain slopes in 1853 to raise dairy cows and plant a vineyard.
North of Taylor Mountain, Taylor Ridge descends toward the city of Santa Rosa. Some of Santa Rosa's urban expansion is taking place to the east of this ridge.
Taylor Mountain is readily visible from Sonoma Mountain, Bennett Valley, the Santa Rosa Plain and from as far north as the Alexander Valley.
The peak of Taylor Mountain defines (in part) the boundary between the Sonoma Coast AVA and the Sonoma Valley AVA, two federally designated grape-growing regions. Wines made from grapes grown on its western slopes would qualify for the Sonoma Coast appellation, whereas those made from grapes grown on its eastern slopes would qualify for the Sonoma Valley appellation.

## Taylor Mountain Regional Park

The Taylor Mountain Open Space Preserve encompasses over 1,100 acres (450 ha) of Taylor Mountain. The land was purchased for public use between 1995 and 2011 by the Sonoma County Agricultural Preservation and Open Space District. A Landpaths permit program allowed public access in 2010. The park was opened to the general public on February 23, 2013 with four miles of dirt trails for hikers. A second entrance and trailhead opened along Petaluma Hill Road, south of Yolanda Avenue, on June 13, 2015. The new entrance includes amenities such as picnic tables and parking for horse trailers. From this entrance, you can take a 1.2-mile (1.9 km) trail which connects to the other side of the park. Licensed dogs are allowed on leashes no longer than 6 feet. The flanks of the 1,400 feet (430 m) peak provide panoramic views of the Santa Rosa Plains to the west with Bennett Valley and Annadel State Park to the north. Trail access is from a parking lot near the eastern end of Kawana Terrace off Kawana Springs Road east of Santa Rosa Avenue and Petaluma Hill Road. There is a $7 fee per vehicle for day use. The park is open from 8 AM to sunset.
# Teanaway Peak

Teanaway Peak is a 6,779-foot (2,066-metre) mountain summit located in the Wenatchee Mountains, on the shared border of Kittitas County with Chelan County in Washington state. It is situated on the boundary of the Alpine Lakes Wilderness, on land managed by Wenatchee National Forest. Its nearest higher neighbor is Bills Peak, 0.72 mi (1.16 km) to the east. Precipitation runoff from the peak drains south into tributaries of the Teanaway River, or north into Turnpike Creek which is part of the Wenatchee River drainage basin. The view from the summit of this peak showcases the impressive Mount Stuart and Stuart Range for those who climb it. This peak also goes by the name "Genes Peak", which is for Gene Prater (1929–1993), the younger brother of Bill Prater, for whom Bills Peak was named. Gene was co-inventor of the modern aluminum snowshoe, and author of the seminal book, "Snowshoeing: From Novice to Master." Gene is also credited with first ascents of Sherpa Peak, Colchuck Balanced Rock, and the east summit of Ingalls Peak.

## Climate

Lying east of the Cascade crest, the area around Teanaway Peak is a bit drier than areas to the west. Summers can bring warm temperatures and occasional thunderstorms. Most weather fronts originate in the Pacific Ocean, and travel east toward the Cascade Mountains. As fronts approach, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the eastern slopes of the Cascades experience lower precipitation than the western slopes. 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 Alpine Lakes Wilderness features some of the most rugged topography in the Cascade Range with craggy peaks and ridges, deep glacial valleys, and granite walls spotted with over 700 mountain lakes. Geological events occurring many years ago created the diverse topography and drastic elevation changes over the Cascade Range leading to the various climate differences.
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 and shaped the landscape. The last glacial retreat in the Alpine Lakes area began about 14,000 years ago and was north of the Canada–US border by 10,000 years ago. The U-shaped cross section of the river valleys is a result of that 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 Alpine Lakes Wilderness area.
# Carisbrook railway station

Carisbrook railway station is a closed railway station on the Moolort railway line at Carisbrook, Victoria. The station was opened on Tuesday, 7 July 1874.
Although no longer in use Carisbrook retains a bricks station building, platform and goods shed.

## Calls for Reopening

A movement for the re-opening of the railway line has been gaining momentum over the past 2 years. On Sunday 8 December 2013 a Community Rally calling for the reopening of the railway station and the railway line will take place. A discussion on the rally and the Group Rally for the return of rail services can be found on Railpage
# Tenaya Peak

Tenaya Peak is a mountain in the Yosemite high country, rising above Tenaya Lake. Tenaya Peak is named after Chief Tenaya, who met the Mariposa Battalion near the shores of the Tenaya lake. In 1851, the Mariposa Battalion under Captain John Boling expelled Chief Tenaya and his people from what was to become Yosemite National Park.

## Recreation

Tenaya Peak is a popular rock climbing destination, with multiple climbing ascents. There is also some class 2 and class 3 hikes to the summit.
# Thatchtop

Thatchtop is a 12,668-foot-elevation (3,861-meter) mountain summit in Larimer County, Colorado, United States.

## Description

Thatchtop is set one mile east of the Continental Divide in the Front Range of the Rocky Mountains. The mountain is situated within Rocky Mountain National Park, approximately 10.5 miles (16.9 km) southwest of Estes Park. Precipitation runoff from the mountain drains into tributaries of Glacier Creek which in turn is a tributary of the Big Thompson River. Topographic relief is significant with the summit rising 2,670 feet (810 meters) above Glacier Gorge in 0.75 mile (1.21 km).

## Etymology

The mountain's descriptive name refers to the matted groundcover of the roof-shaped mountain. The landforms's toponym was officially adopted in 1932 by the United States Board on Geographic Names, although it appeared in publications as early as 1911 if not earlier. The Arapaho called the mountain "Buffalo Climb."

## Climate

According to the Köppen climate classification system, Thatchtop is located in an alpine subarctic climate zone with cold, snowy winters, and cool to warm summers. Due to its altitude, it receives precipitation all year, as snow in winter, and as thunderstorms in summer, with a dry period in late spring.
# Antrustion

An antrustion (Latin: antrustio, plural antrustiones) was a member of the bodyguard or military household of the Merovingian kings of the Franks. The bodyguard itself is called the trustis (French: truste), a Frankish word with a Latin ending, possibly signifying comfort, aid, fidelity, trust (compare Old High German trost). An alternative etymology relates it to proto-Germanic *druhtiz, warband, whence old high German truht and perhaps Slavonic druzhina.
Information about the antrustions is derived from one of the formulae of Marculfus and from various provisions of the Salic law. Anyone desiring to enter the antrustions had to present himself armed at the royal palace, and there, with his hands in those of the king, take a special oath or trustis and fidelitas, in addition to the oath of fidelity sworn by every subject at the king's accession. This done, he was considered to be in truste dominica and bound to provide the services this involved. In return for these, the antrustion enjoyed certain advantages, entitled to royal assistance and protection; his wergeld was three times that of an ordinary Frank; the slayer of a Frank was paid compensation of 200 solidi, that of an antrustion had to find 600. The antrustion was always of Frankish descent, and only in certain exceptional cases were Gallo-Romans admitted into the group. These Gallo-Romans then took the name of convivae regis, and the wergeld of 300 solidi was three times that of a homo romanus. The antrustions, belonging as they did to one body, had strictly defined responsibilities towards one another; e.g., one antrustion was forbidden to bear witness against another under penalty of 15 solidi compensation.
The antrustions seem to have played an important part at the time of Clovis. Apparently they formed the army that conquered the land, an army composed chiefly of Franks, with a few Gallo-Romans who had taken the side of Clovis. After the conquest, the role of the antrustions became less important. For each expedition, the king raised an army of citizens in which the Gallo-Romans mingled more and more with the Franks; they only kept one small permanent body which acted as their bodyguard (trustis dominica). Some members were assigned other tasks, such as that of forming garrisons in frontier towns. The institution seems to have disappeared during the anarchy with which the 8th century opened.
It has wrongly been held to be the origin of vassalage. Only the king had antrustions; while every lord could have vassals. The antrustions were a military institution; vassalage was a social institution with complicated origins.
# The Bulge

The Bulge is a mountain located in Coos County, New Hampshire. The mountain is part of the Pilot Range of the White Mountains.
The Bulge is flanked to the northeast by The Horn, and to the southwest by Mount Cabot.
The Bulge stands within the watershed of the Connecticut River, which drains into Long Island Sound in Connecticut. The southeast face of The Bulge drains into the headwaters of the West Branch of the Upper Ammonoosuc River, a tributary of the Connecticut River. The north face of The Bulge drains north, thence into the West Branch of Mill Brook, and into the Upper Ammonoosuc. The west face of The Bulge drains into Fox Brook, thence into Whipple Brook, Burnside Brook, Otter Brook, and the Israel River, another tributary of the Connecticut.
# The Citadel (Sierra Nevada)

The Citadel is an 11,738-foot-elevation (3,578-meter) mountain summit located in the Sierra Nevada mountain range, in Fresno County of central California, United States. It is situated in northern Kings Canyon National Park, 20 miles (32 km) west-southwest of the community of Big Pine, and 2.4 miles (3.9 km) south of Langille Peak. Topographic relief is significant as it rises 3,400 feet (1,000 meters) above Le Conte Canyon in approximately one mile. The long approach to this remote peak is made via the John Muir Trail. The Northeast Arête, also known as Edge of Time Arête, is considered one of the classic climbing routes in the Sierra Nevada.

## Climate

According to the Köppen climate classification system, The Citadel is located in an alpine climate zone. Most weather fronts originate in the Pacific Ocean, and travel east toward the Sierra Nevada mountains. As fronts approach, they are forced upward by the peaks, causing them to drop their moisture in the form of rain or snowfall onto the range (orographic lift). Precipitation runoff from this mountain drains into the Middle Fork Kings River.

## Climbing

Non-technical routes:
* West Ridge – class 2 – First ascent June 24, 1951, by Richard Searle, William Wirt
* Northeast Face – class 4 – FA by Donald Goodrich, Robert Means also on June 24, 1951
* North Wall – class 4 – FA by Locker, Albright, G. Hufbauer, and K. Hufbauer
Established rock climbing routes:
* North Face – class 5.7 A3 – FA 1968 by T. M. Herbert, Don Lauria, Dennis Hennick
* Edge of Time Arête – class 5.10+ – 14 pitches – FA 1991 by Dave Nettle and Jim Howle
* Quality Time – class 5.10b – 9 pitches – FA 2003 by Urmas Franosch, Peter Mayfield
* Wild Kingdom – class 5.11- – 16 pitches – FA 2019 by Katie Lambert, Ben Ditto

## Gallery

* The Citadel with cascade
* The Citadel (centered) and Wheel Mountain (behind, left)
# The Incredible Hulk (California)

The Incredible Hulk, or Incredible Hulk, is a granitic summit with an elevation of 11,300 feet (3,444 m) located in the Sierra Nevada mountain range, in Mono County of northern California, United States. The summit is set in Little Slide Canyon of the Hoover Wilderness, on land managed by Humboldt–Toiyabe National Forest, and is one mile outside the boundary of Yosemite National Park. The peak is situated approximately three miles southwest of Twin Lakes, three-quarters mile east of Kettle Peak, and 2.5 miles northwest of Matterhorn Peak. The nearest town is Bridgeport, 14 miles to the northeast. Topographic relief is significant as the summit rises 3,700 feet (1,100 meters) above Robinson Creek in one mile (1.6 km). Incredible Hulk is the unofficial name of this landform, and will remain unofficial as long as the USGS policy of not adopting new toponyms in designated wilderness areas remains in effect.

## Climbing

The first ascent of the summit was made September 6, 1936, by Bestor Robinson, Florence Robinson, Don Woods, and Carl Jensen.
Established rock climbing routes on the 1,200-foot-high walls of Incredible Hulk:
* The Donaldson Route – class 5.8 – First Ascent 1970 by Greg Donaldson, Joe Kiskis, Bob Grow
* Mountaineers Route (Southwest Couloir) – class 4-5 – FA 1971 by Bob Grow, Joe Kiskis
* Fallen Leaf – class 5.9 – FA 1970s by Mike Farrell, partner
* Red Dihedral – class 5.10 – FA 1975 by Dale Bard, Mike Farrell, Bob Locke
* Polish Route – class 5.10 – FA 1976 by Bob Harrington, Rick Wheeler
* Positive Vibrations – class 5.11b – FA 1981 by Bob Harrington, Alan Bartlett
* Astrohulk – class 5.11 – FA 1996 by Dave Nettle, Mike Davis
* Escape from Poland – class 5.10 – FA 1998 by Dave Nettle, John Fehrman
* Sun Spot Dihedral – class 5.11b – FA 1999 by Dave Nettle, Jimmy Haden
* Airstream – class 5.13 – FA 2004 by Peter Croft, Dave Nettle, Greg Epperson
* The Venturi Effect – class 5.13 – FA 2004 by Peter Croft, Dave Nettle
* Blowhard – class 5.12 – FA 2005 by Peter Croft, Andrew Stevens
* Solar Flare – class 5.12 – FA 2007 by Peter Croft, Conrad Anker
* Eye of the Storm – class 5.12 – FA 2007 by Nils Davis, Brent Obinger
* Sun Burn – class 5.12 – FA 2008 by Peter Croft, Dave Nettle
* Wind Shear – class 5.12 – FA 2016 by Peter Croft, Dave Nettle, Andy Puhvel
* Lenticular Gyrations – class 5.12 – FA 2016 by Aaron Cassebeer, Jeff Gicklhorn, Patrick O'Donnell
Red Dihedral (originally named "Yggdrasil") and Positive Vibrations are considered classic climbing routes in the Sierra Nevada.

## Climate

According to the Köppen climate classification system, The Incredible Hulk is located in an alpine climate zone. Most weather fronts originate in the Pacific Ocean, and travel east toward the Sierra Nevada mountains. As fronts approach, they are forced upward by the peaks (orographic lift), causing moisture in the form of rain or snowfall to drop onto the range. Precipitation runoff from this rock feature drains to Robinson Creek which is a tributary of the Walker River.
# Thunder Mountain (Amador County, California)

Thunder Mountain in the Sierra Nevada of California is located east of Silver Lake and west of Kirkwood Mountain Resort in the Eldorado National Forest. The mountain has two peaks, the 9,414-foot (2,869 m) main peak and a 9,412-foot (2,869 m) sub-peak west of the main peak. The main summit is the highest point in Amador County. Due to the high elevation, most precipitation that falls on Thunder Mountain consists of snow.
The peak was named by United States Forest Service personnel because "thunderstorms appear to build up in that area."

## Climate

According to the Köppen climate classification system, Thunder Mountain is located in an alpine climate zone. Most weather fronts originate in the Pacific Ocean and travel east toward the Sierra Nevada mountains. As fronts approach, they are forced upward by the peaks (orographic lift), causing them to drop their moisture in the form of rain or snowfall onto the range.
# Northside Village Historic District

The Northside Village Historic District encompasses a rural village center on Stafford Road in northern Charlton, Massachusetts. Located at the junction of Stafford Road with Northside and Cemetery Roads is a small cluster of residential buildings, developed beginning in 1735 around a small tanning business, and later as a stagecoach stop. The district was listed on the National Register of Historic Places in 1977.

## Description and history

Charlton was settled in 1735 as part of Oxford, and was separately incorporated in 1775. One of its first settlers was Jonothan Wheelock, whose house built that year still stands near the eastern end of the district. Wheelock established a tannery and distillery on a nearby brook, of which only archaeological remnants survive on their sites. In 1796 his house was purchased by John Haven, who is credited with building a number of the surviving buildings in the village. The Rider Tavern, built in 1797, became a stop on the stagecoach route between Worcester and Hartford, Connecticut, including among its visitors the Marquis de Lafayette. The tavern is now a museum operated by the local historical society.
The historic district is centered on the two junctions of Stafford Road, the historic stage route, with Northside Road, extending south to the town center, and Cemetery Road, running north. There are thirteen buildings in the district, most of which were built before 1850. In addition to the Rider Tavern and Wheelock House, notable buildings include the Waters-Morton House, which was home both to a prominent local politician, and was the childhood home of Dr. William T. G. Morton, a dentist who introduced the use of ether as an anesthetic. The only non-residential building in the district is the former 1848 Northside District School.
# Tinker Hill

Tinker Hill is a summit in Putnam County, in the U.S. state of New York. It has an elevation of 935 feet (285 m).
The hill was named for the fact that a jack of all trades, or a "tinkering" man, settled there ca. 1800.
# Tlingit Peak

Tlingit Peak is a 3,274-foot (998 m) mountain summit in the US state of Alaska.

## Description

Tlingit Peak is located in the Fairweather Range of the Saint Elias Mountains. It is set within Glacier Bay National Park and Preserve and is situated 2.14 miles (3.44 km) southwest of Marble Mountain. Precipitation runoff from the mountain drains into Geikie Inlet. Although modest in elevation, topographic relief is significant as the summit rises above tidewater of Tyndall Cove in one mile (1.6 km). The mountain's name was reported in 1951 by U.S. Geological Survey and the toponym has been officially adopted by the U.S. Board on Geographic Names. The peak is named after the Tlingit people. Other peaks within the park with the "Tlingit" name include Mount Tlingit and Mount Tlingit Ankawoo.

## Climate

Based on the Köppen climate classification, Tlingit Peak is located in a marine subpolar climate zone, with long, cold, snowy winters, and cool summers. Weather systems coming off the Gulf of Alaska are forced upwards by the Saint Elias Mountains (orographic lift), causing heavy precipitation in the form of rainfall and snowfall. Winter temperatures can drop below 0 °F with wind chill factors below −10 °F.
# Stansfield Hall, Todmorden

Stansfield Hall (/ˈstænsfiːld/ STANSS-feeld) is a privately owned historic and Grade II* listed building, in Stansfield, Todmorden, West Yorkshire, England, which was once the residence of the Yorkshire MP Joshua Fielden and is now divided into private residential apartments.

## History

Stansfield Hall was built in 1640 for James Stansfield, a descendant of the Stansfeld family of Stansfield and Sowerby, Yorkshire. The estate passed to John Pilling who later sold it, in 1675, to Joshua Horton (d.1679) of Sowerby. The Horton family sold it in 1696 to William Sutcliffe in whose family it remained for over a century until it was purchased by the MP Joshua Fielden (1827–87) who commissioned the architect John Gibson to add a large Gothic Revival style extension to the existing building in 1862.

## Architecture

The Hall's 17th century elements include a five-light chamfered mullioned window (lengthened with replaced mullions). The 1862 extension is an impressive range all with mullioned windows. Internally, there is a Tudor arched fireplace with Gothic decoration incorporating the initials J.F. and E.F.
# The Ghost Watcher

Dark Shadows: The Ghost Watcher is a Big Finish Productions original dramatic reading based on the long-running American horror soap opera series Dark Shadows.

## Plot

Maggie Evans has recovered from her ordeals and is ready to build a new life for herself, but then she meets the mysterious Ghost Watcher...

## Cast

* Maggie Evans – Kathryn Leigh Scott
* Nathan Hawkins – Alec Newman
# Rustam Abdulov

Rustam Rezoyevich Abdulov (Russian: Рустам Резоевич Абдулов; born 29 March 1973) is a former Russian football player.

## Club career

He made his Russian Premier League debut for FC Lokomotiv Nizhny Novgorod on 7 March 1993 in a game against FC Zhemchuzhina Sochi.
# Roger Guilhem

Roger Guilhem (1924–2009) was a French former professional rugby league footballer who represented France at the 1954 Rugby League World Cup, as a stand-off or loose forward. He was nicknamed La pieuvre (The octopus).

## Career

Guilhem, then playing for AS Carcassonne, was called up to represent France in the 1951 tour of Australia and New Zealand and the 1954 Rugby League World Cup played in France. He took part only in a match during the tournament and was in the bench during the final against Great Britain, the latter winning the tournament.

## Honours

* World Cup :
** Runner-up - 1954 (France).
* European Nations Cup :
** 2 times champion in 1949 and 1952 (France).
* French Championship :
** 4 times champion in 1946,1950, 1952 and 1953 (Carcassonne).
** 5 times finalist in 1947, 1948, 1949, 1955 and 1956 (Carcassonne).
* Lord Derby Cup :
** 4 times champion in1946 and 1947, 1951 and 1952 (Carcassonne).
** 1 time finalist in 1948 and 1949 (Carcassonne).