Sarmila/GeoWiki-Features huggingface dataset:
Mittelallalin. The Mittelallalin () is a minor summit below the Allalinhorn situated above Saas Fee. This place is well known for the revolving restaurant which is the highest in the world and a glacier cave. Access. Mittelallalin can be reached easily by cable car from Saas Fee to the Felskinn intermediate station and finally to the top with the Metro Alpin, the highest funicular in the world.

Geographic entities mentioned:
surface_form: Allalinhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.046138888889
lon: 7.8948055555556
surface_form: mittelallalin
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.057672222222
lon: 7.9049666666667
Access. Mittelallalin can be reached easily by cable car from Saas Fee to the Felskinn intermediate station and finally to the top with the Metro Alpin, the highest funicular in the world. Ski and mountain-climbing. The Mittelallalin is also an all year round ski area (between in winter, Fee Glacier in summer). From there the ascent of Allalinhorn is very popular and can be done in just two hours.

Geographic entities mentioned:
surface_form: Allalinhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.046138888889
lon: 7.8948055555556
Mittelallalin. The Mittelallalin () is a minor summit below the Allalinhorn situated above Saas Fee. This place is well known for the revolving restaurant which is the highest in the world and a glacier cave. Access. Mittelallalin can be reached easily by cable car from Saas Fee to the Felskinn intermediate station and finally to the top with the Metro Alpin, the highest funicular in the world.

Geographic entities mentioned:
surface_form: mittelallalin
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.057672222222
lon: 7.9049666666667
This place is well known for the revolving restaurant which is the highest in the world and a glacier cave. Access. Mittelallalin can be reached easily by cable car from Saas Fee to the Felskinn intermediate station and finally to the top with the Metro Alpin, the highest funicular in the world. Ski and mountain-climbing.

Geographic entities mentioned:
surface_form: mittelallalin
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.057672222222
lon: 7.9049666666667
Access. Mittelallalin can be reached easily by cable car from Saas Fee to the Felskinn intermediate station and finally to the top with the Metro Alpin, the highest funicular in the world. Ski and mountain-climbing. The Mittelallalin is also an all year round ski area (between in winter, Fee Glacier in summer). From there the ascent of Allalinhorn is very popular and can be done in just two hours.

Geographic entities mentioned:
surface_form: mittelallalin
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.057672222222
lon: 7.9049666666667
It is a small Arts and Crafts-style stone building constructed in the 1920s with a donation from Charles E. Rushmore, a local resident for whom Mount Rushmore is also named. It served as the Town of Woodbury public library until the mid-1980s, when a larger modern library was built. Today it is the headquarters of the town historical society.

Geographic entities mentioned:
surface_form: Mount Rushmore
instance_of: Mountain
countries: United States
coordinates: lat: 43.878947222222
lon: -103.459825
Its current leaders include Leopoldo Puchi, Felipe Mújica and Carlos Tablante. In the period since 1989, when state governors have been directly elected, the party has won state governorships in Delta Amacuro, Lara, Portuguesa, Sucre (Ramón Martínez) and Zulia. Some of his past members included: Pompeyo Márquez, Rafael Guerra Ramos and Carlos Tablante. Presidential candidates supported.

Geographic entities mentioned:
surface_form: Delta Amacuro
instance_of: Body of water
countries: Venezuela
coordinates: lat: 8.7
lon: -61.15
The whole island was formerly occupied by Fort Hughes, a U.S. defense fortification before World War II. It was heavily bombed during the war. Geological history. Caballo and Corregidor Islands are believed to be the rims of the Corregidor Caldera. The gap between the two islands is only about 1/4 mile with a depth of and is never used for large vessel navigation.

Geographic entities mentioned:
surface_form: Corregidor Caldera
instance_of: Mountain
countries: Philippines
coordinates: lat: 14.38333333
lon: 120.575
At that time, Taekkyon was practised as a martial art and a folk game by people in the vicinity of Seoul. Song learnt in a glade located on the flanks of the Inwangsan mountain near the Archery center called Hwanghakjeong (). At the time, the High-village or Widaepae () designated those who lived inside of Seoul town walls and Araedaepae or Low-village (), those who lived outside.

Geographic entities mentioned:
surface_form: Inwangsan
instance_of: Mountain
countries: South Korea
coordinates: lat: 37.58472222
lon: 126.95861111
Career. Dickinson was renowned for his work in plate tectonics, sedimentary geology and Pacific Oceana geology and was considered one of the foremost experts on the geology of the Colorado Plateau. Dickinson was one of the founders of the Gazzi-Dickinson Method and its primary application, QFL diagrams and their use in sandstone provenance.

Geographic entities mentioned:
surface_form: Colorado Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37
lon: -110
It traces its rise from an early hill fort and later royal residence to the bustling city and capital of Scotland that it is today. 1st millennium. Pre-1st century AD: Late Bronze Age (c.600 BC) weapons were found in Duddingston Loch in 1778. Traces of four Iron Age forts have been identified at Arthur's Seat, Dunsapie Crag, Salisbury Crags and Samson's Ribs.

Geographic entities mentioned:
surface_form: Duddingston Loch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 55.94
lon: -3.15
1st millennium. Pre-1st century AD: Late Bronze Age (c.600 BC) weapons were found in Duddingston Loch in 1778. Traces of four Iron Age forts have been identified at Arthur's Seat, Dunsapie Crag, Salisbury Crags and Samson's Ribs. 2nd century AD: Roman forts were built and manned at Cramond and Inveresk on the western and eastern margins of the present-day city.

Geographic entities mentioned:
surface_form: Arthur's Seat
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.944166666667
lon: -3.1619444444444
1702: Advocates Library moved from Faculty of Advocates to Parliament House
1706: Framework knitters from Haddington are working in Edinburgh
1707: Act of Union passed by the Parliament of Scotland
1711: David Hume, philosopher, is born
1713: The main radial roads into Edinburgh are turnpiked
1715: Jacobites occupy Leith Citadel, but make no attempt to enter Edinburgh
1718: &quot;Edinburgh Evening Courant&quot; newspaper is launched; damasks are woven at Drumsheugh
1720s: Daniel Defoe praises the High Street, decries Old Tolbooth, notes sales of woollens, linens, drapery and &quot;mercery&quot;
1722: Signet Library is founded
1725: Barony of Calton (including Calton Hill) purchased by the city
1726: The poet Allan Ramsay establishes Britain's first circulating library; Edinburgh Medical School founded at the town's college; James Hutton, geologist, is born
1727: Royal Bank of Scotland established
1729: The city's first infirmary is opened
1733: Alexander Monro Secundus, discoverer of lymphatic and nervous systems, is born
1735: Golf is played on Bruntsfield Links; also the traditional date for the founding of the Royal Burgess Golfing Society
1736: The Royal Infirmary is given a Royal charter; Porteous Riots shake the city
1737: The Lord provost is debarred from office following the riots
1738: Edinburgh is described as the &quot;world's leading medical centre&quot;; George Watson's College is founded
1739: &quot;The Scots Magazine&quot; is first published in the city
1740: There are four printing firms in Edinburgh; the biographer James Boswell is born
1741: Royal Infirmary designed by William Adam opens in, what became, Infirmary Street
1744: The first premises at Fountainbridge are built, with more than five looms; first known rules of golf drawn up in Edinburgh for the Gentlemen Golfers of Edinburgh for a competition at Leith Links
1745: Charles Edward Stuart enters the city and proclaims his father James VIII and III; in the &quot;Canter of Coltbrigg&quot;, dragoons flee Jacobites
1746: The British Linen Company is formed
1747: A theatre is established at Playhouse Close in the Canongate
1748: Moral philosopher and political economist Adam Smith delivers his first series of public lectures at the University of Edinburgh
1749: A stagecoach service opens between Edinburgh and Glasgow
1750: Birth of the poet Robert Fergusson
1751: A survey shows a severe state of dilapidation in the Old Town
1752: Convention of Royal Burghs publishes proposals for new public buildings, the draining of the Nor Loch and the city's expansion, which are accepted and implemented by the town council
1753: Stagecoach services are introduced to London (taking two weeks)
1754: Building of the Royal Exchange (later Edinburgh City Chambers) in the High Street begins; the Select Society is founded; Mons Meg removed from the castle to the Tower of London
1755: Dr.

Geographic entities mentioned:
surface_form: Calton Hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.955278
lon: -3.182222
xxi) establishes police commissioners with responsibility for policing the city (and also cleansing and lighting)
1807-15: Nelson Monument erected on Calton Hill
1810: Construction of Signet Library building by Robert Reid begins (interior by William Stark, 1812–13)
1811–1812: Tron riot, 68 youths were arrested
1813: Royal Edinburgh Hospital, originally called the Edinburgh Lunatic Asylum, opens in Morningside
1814: Waverley, the first of the Waverley Novels, written by Sir Walter Scott, is published; a protest meeting against West Indian slavery is held; two coaches a day run to Stirling
1815: Scottish Widows Fund and Life Assurance Society established
1816–1819: Regent Bridge is built
1817: First copy of &quot;The Scotsman&quot; newspaper is published in January; Blackwood's Magazine first published; the Old Tolbooth and the remaining Luckenbooth in the High Street are demolished; new County Buildings are erected on the west side of Parliament Square
1818: The Union Canal is begun; new Calton Hill observatory is founded by the Edinburgh Astronomical Institution; the Scottish regalia are found in Edinburgh Castle; Cambridge geologist and antiquarian Edward Daniel Clarke likens Edinburgh topographically to Athens, a view echoed in 1820 by landscape painter Hugh William Williams who coins the terms &quot;Modern Athens&quot; and &quot;Athens of the North&quot;; gas lighting makes its first appearance
1819: Five coaches a day run between Edinburgh and Glasgow, taking 12 hours for the journey of
1820: Remaining western end of the Nor Loch drained; Charlotte Square completed; there are protests at George IV's treatment of Queen Caroline; the Royal Botanic Garden begins its move from Leith Walk to Inverleith; the Radical Road built along base of Salisbury Crags
1821: The official government census gives the population of Edinburgh and Leith as 138,235 with Leith as approx.

Geographic entities mentioned:
surface_form: Calton Hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.955278
lon: -3.182222
Madrean Sky Islands region. The valley lies in a region of southeast Arizona and southwest New Mexico called the Madrean Sky Islands; the valley is a northeast drainage to the San Simon Valley, but only in the Whitlock Valley southern region, and the neighboring mountains east and west. The south of the valley forms a water divide to the northeast region of San Simon Creek.

Geographic entities mentioned:
surface_form: San Simon Valley
instance_of: Valley
countries: United States
coordinates: lat: 32.8017
lon: -109.633
surface_form: san simon valley
instance_of: Valley
countries: United States
coordinates: lat: 32.8017
lon: -109.633
surface_form: whitlock valley
instance_of: Valley
countries: United States
coordinates: lat: 32.5528
lon: -109.335
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
The valley is endorheic, with a small dry lake called Parks Lake, and merges southwest into the north of the San Simon Valley, where the San Simon River has its origins in the flatlands, and surrounding perimeter mountains. The valley was named after Captain James H. Whitlock who commanded during the Battle of Mount Gray in 1864 which was fought near the valley. Regional endorheic valley.

Geographic entities mentioned:
surface_form: dry lake
instance_of: Lake
countries: United States
coordinates: lat: 44.6282988
lon: -97.0561783
surface_form: dry lake
instance_of: Lake
countries: United States
coordinates: lat: 38.3360373
lon: -117.7898285
surface_form: dry lake
instance_of: Lake
countries: United States
coordinates: lat: 45.0425
lon: -97.31972222
surface_form: san simon valley
instance_of: Valley
countries: United States
coordinates: lat: 32.8017
lon: -109.633
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
The valley is endorheic, with a small dry lake called Parks Lake, and merges southwest into the north of the San Simon Valley, where the San Simon River has its origins in the flatlands, and surrounding perimeter mountains. The valley was named after Captain James H. Whitlock who commanded during the Battle of Mount Gray in 1864 which was fought near the valley. Regional endorheic valley.

Geographic entities mentioned:
surface_form: battle
instance_of: Watercourse
countries: United States
coordinates: lat: 44.9266
lon: -93.0291
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
A water divide creates Parks Lake at the south of the Whitlock Valley. Whitlock Valley. Whitlock Valley is a mostly north–south 22-mile (35 km) long valley, bordered on the west by the small north–south Whitlock Mountains. The east of the valley is bordered by the north region of the Peloncillo Mountains (Cochise County), a north–south stretch, only about 8 mi wide.

Geographic entities mentioned:
surface_form: long valley
instance_of: Landform
countries: United States
coordinates: lat: 37.716666666667
lon: -118.88416666667
surface_form: long valley
instance_of: Valley
countries: United States
coordinates: lat: 39.6833
lon: -115.722
surface_form: whitlock valley
instance_of: Valley
countries: United States
coordinates: lat: 32.5528
lon: -109.335
surface_form: long valley
instance_of: Valley
countries: United States
coordinates: lat: 37.3789
lon: -112.573
Regional endorheic valley. The west-flowing Gila River is forced into a NW-West-SW excursion by the small range of the Black Hills (Greenlee County). The Whitlock Valley drains south from the range, and merges into the north of the San Simon Valley, where the San Simon River forms a playa, flatland region, then continues northwest to the Gila River.

Geographic entities mentioned:
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 46.99
lon: -123.14
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 43.1693
lon: -120.68
The west-flowing Gila River is forced into a NW-West-SW excursion by the small range of the Black Hills (Greenlee County). The Whitlock Valley drains south from the range, and merges into the north of the San Simon Valley, where the San Simon River forms a playa, flatland region, then continues northwest to the Gila River. A water divide creates Parks Lake at the south of the Whitlock Valley.

Geographic entities mentioned:
surface_form: san simon valley
instance_of: Valley
countries: United States
coordinates: lat: 32.8017
lon: -109.633
surface_form: whitlock valley
instance_of: Valley
countries: United States
coordinates: lat: 32.5528
lon: -109.335
Whitlock Valley. The Whitlock Valley is a small valley in southeast Graham County, Arizona, southwestern United States, lying between three mountain ranges.

Geographic entities mentioned:
surface_form: whitlock valley
instance_of: Valley
countries: United States
coordinates: lat: 32.5528
lon: -109.335
The Whitlock Valley drains south from the range, and merges into the north of the San Simon Valley, where the San Simon River forms a playa, flatland region, then continues northwest to the Gila River. A water divide creates Parks Lake at the south of the Whitlock Valley. Whitlock Valley.

Geographic entities mentioned:
surface_form: whitlock valley
instance_of: Valley
countries: United States
coordinates: lat: 32.5528
lon: -109.335
A water divide creates Parks Lake at the south of the Whitlock Valley. Whitlock Valley. Whitlock Valley is a mostly north–south 22-mile (35 km) long valley, bordered on the west by the small north–south Whitlock Mountains. The east of the valley is bordered by the north region of the Peloncillo Mountains (Cochise County), a north–south stretch, only about 8 mi wide.

Geographic entities mentioned:
surface_form: whitlock valley
instance_of: Valley
countries: United States
coordinates: lat: 32.5528
lon: -109.335
The north Peloncillos form the border between Graham County, northwest, and Greenlee County to the east, (extreme southeast county). Parks Lake and Whitlock Cienega. Parks Lake is the low point of Whitlock Valley in the south. The southern Whitlock Mountains are to the west, and on the southeast foothills of the Whitlocks lie Whitlock Cienega, at.

Geographic entities mentioned:
surface_form: whitlock valley
instance_of: Valley
countries: United States
coordinates: lat: 32.5528
lon: -109.335
The Whitlock Valley is a small valley in southeast Graham County, Arizona, southwestern United States, lying between three mountain ranges. The valley lies on the south perimeter region of the White Mountains in eastern Arizona, and lies south of the west-flowing Gila River, and the region transitions south into Cochise County and three large valleys, with some scattered dry lakes.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
The valley is endorheic, with a small dry lake called Parks Lake, and merges southwest into the north of the San Simon Valley, where the San Simon River has its origins in the flatlands, and surrounding perimeter mountains. The valley was named after Captain James H. Whitlock who commanded during the Battle of Mount Gray in 1864 which was fought near the valley. Regional endorheic valley.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
A water divide creates Parks Lake at the south of the Whitlock Valley. Whitlock Valley. Whitlock Valley is a mostly north–south 22-mile (35 km) long valley, bordered on the west by the small north–south Whitlock Mountains. The east of the valley is bordered by the north region of the Peloncillo Mountains (Cochise County), a north–south stretch, only about 8 mi wide.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
She achieved her first World Cup victory on 18 January 2015 in Zaō, Japan. At the Nordic World Ski Championships 2013 in Val di Fiemme, she won the bronze medal in the mixed normal hill competition together with Ulrike Gräßler, Richard Freitag, and Severin Freund. At the Nordic World Ski Championships 2015 in Falun, she won the gold medal in the individual normal hill competition.

Geographic entities mentioned:
surface_form: Val di Fiemme
instance_of: Valley
countries: Italy
coordinates: lat: 46.2833
lon: 11.5667
Craddock Crags. Craddock Crags () are steep, rugged rock summits that rise to about just east of Beitzel Peak in the Marble Hills, Heritage Range, Ellsworth Mountains. They were named by the Advisory Committee on Antarctic Names (2004) after John P. Craddock, a geologist who was a member of a United States Antarctic Research Program 1979–80 Ellsworth Mountains expedition.

Geographic entities mentioned:
surface_form: Beitzel Peak
instance_of: Mountain
coordinates: lat: -80.283333333333
lon: -82.3
Bernard Pierre. Bernard Pierre (1920–1997) was a French mountaineer, notable as a climber and an expedition leader. Biography. Born in Chelles, Pierre was trained as a lawyer and ran his family's textile business, and was a mountaineer on the side. He made a number of notable ascents in the Alps, including of the north face of the Aiguille du Dru and the northwest face of La Civetta.

Geographic entities mentioned:
surface_form: Aiguille du Dru
instance_of: Mountain
countries: France
coordinates: lat: 45.932777777778
lon: 6.9563888888889
He made a number of notable ascents in the Alps, including of the north face of the Aiguille du Dru and the northwest face of La Civetta. He made the second ascent of the Piz Badile's northeast face, and was a lead climber on the first ascents of a route on the Aiguille des Aigles and the face of the Aiguille de la Brenva.

Geographic entities mentioned:
surface_form: Piz Badile
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.294722
lon: 9.586111
surface_form: Aiguille de la Brenva
instance_of: Mountain
countries: Italy
coordinates: lat: 45.8342
lon: 6.91786
He made the second ascent of the Piz Badile's northeast face, and was a lead climber on the first ascents of a route on the Aiguille des Aigles and the face of the Aiguille de la Brenva. In 1951 he climbed in the Hoggar Mountains in southern Algeria, making a number of first ascents—he returned to the mountain range in 1961.

Geographic entities mentioned:
surface_form: Hoggar Mountains
instance_of: Plateau
countries: Algeria
France
coordinates: lat: 23.288611
lon: 5.534167
In 1951 he climbed in the Hoggar Mountains in southern Algeria, making a number of first ascents—he returned to the mountain range in 1961. In 1952, he led a French-American expedition including Claude Kogan to the Andes, and made the first ascent of Salcantay. Pierre also led the team which made the first ascent of Nun in India.

Geographic entities mentioned:
surface_form: Salcantay
instance_of: Mountain
countries: Peru
coordinates: lat: -13.333611111111
lon: -72.544444444444
Later that same day Claude Kogan and Pierre Vittoz reached the summit. He led a French-Iranian expedition to Mount Damavand for its first ascent in 1954, an expedition to the Rwenzori Mountains in 1955–1956, and to the Caucasus in 1958.

Geographic entities mentioned:
surface_form: Mount Damavand
instance_of: Mountain
countries: Iran
coordinates: lat: 35.955277777778
lon: 52.109166666667
In April and May 1945, the remaining reserves of the Reichsbank – gold (730 bars), cash (6 large sacks), and precious stones and metals such as platinum (25 sealed boxes) – were dispatched by Walther Funk to be buried on the Klausenhof Mountain at Einsiedl in Bavaria, where the final German resistance was to be concentrated.

Geographic entities mentioned:
surface_form: Einsiedl
instance_of: Lake
countries: Germany
coordinates: lat: 47.593888888889
lon: 11.346111111111
These bacterial communities contain both hydrogen- or sulfur- consuming autotrophs and heterotrophs and appear to be capable of long-range propagation, considering that relatives of the species found are known from Vulcano in Italy. Aside from hyperthermophiles, craniids, corals, polynoids and sponges have been found in the summit area of Macdonald.

Geographic entities mentioned:
surface_form: Vulcano
instance_of: Mountain
countries: Italy
coordinates: lat: 38.4042
lon: 14.9658
Lake of the Woods Provincial Park. Lake of the Woods Provincial Park is a provincial park in northwestern Ontario, Canada. It protects several islands in Lake of the Woods, in both Kenora and Rainy River Districts. It was established in 1967 and expanded with in 1985. It provides backcountry camping opportunities. Description.

Geographic entities mentioned:
surface_form: Lake of the Woods
instance_of: Lake
countries: Canada
United States
coordinates: lat: 49.09027777777778
lon: -95.2388888888889
Arrowhead Mountain (Flathead County, Montana). Arrowhead Mountain is a mountain in Flathead County, Montana, United States.

Geographic entities mentioned:
surface_form: arrowhead mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.274166666667
lon: -122.40027777778
surface_form: arrowhead mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.670555555556
lon: -73.12
surface_form: arrowhead mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.578333333333
lon: -111.66
surface_form: arrowhead mountain (flathead county, montana)
instance_of: Mountain
countries: United States
coordinates: lat: 48.1075
lon: -113.18361111111
surface_form: arrowhead mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.75761
lon: -120.96538
surface_form: arrowhead mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.8825
lon: -111.4665
surface_form: arrowhead mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.513055555556
lon: -105.69138888889
Arrowhead Mountain (Flathead County, Montana). Arrowhead Mountain is a mountain in Flathead County, Montana, United States.

Geographic entities mentioned:
surface_form: arrowhead mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.274166666667
lon: -122.40027777778
surface_form: arrowhead mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.670555555556
lon: -73.12
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: arrowhead mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.578333333333
lon: -111.66
surface_form: arrowhead mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.1075
lon: -113.18361111111
surface_form: arrowhead mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.75761
lon: -120.96538
surface_form: arrowhead mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.8825
lon: -111.4665
surface_form: arrowhead mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.513055555556
lon: -105.69138888889
Mount Nebo (Oregon). Mount Nebo is a mountain in the Eagle Cap Wilderness of Oregon, in the United States. Named after the biblical Mount Nebo overlooking Israel, which is said to be the place of Moses' death. It is the centerpiece of the Imnaha Divide, inside the Wallowa–Whitman National Forest. Mount Nebo is one of the important areas where sheep and cattle graze throughout Eagle Cap Wilderness.

Geographic entities mentioned:
surface_form: mount nebo
instance_of: Mountain
countries: United States
coordinates: lat: 35.2159
lon: -93.2535
surface_form: mount nebo
instance_of: Mountain
countries: United States
coordinates: lat: 39.8214
lon: -111.76
surface_form: mount nebo
instance_of: Mountain
countries: United States
coordinates: lat: 45.161111111111
lon: -117.1375
surface_form: mount nebo
instance_of: Landform
countries: United States
coordinates: lat: 46.3561
lon: -95.1072
surface_form: mount nebo
instance_of: Mountain
countries: United States
coordinates: lat: 42.365833333333
lon: -74.221944444444
Mount Nebo (Oregon). Mount Nebo is a mountain in the Eagle Cap Wilderness of Oregon, in the United States. Named after the biblical Mount Nebo overlooking Israel, which is said to be the place of Moses' death. It is the centerpiece of the Imnaha Divide, inside the Wallowa–Whitman National Forest. Mount Nebo is one of the important areas where sheep and cattle graze throughout Eagle Cap Wilderness.

Geographic entities mentioned:
surface_form: mount nebo
instance_of: Mountain
countries: United States
coordinates: lat: 35.2159
lon: -93.2535
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: eagle cap
instance_of: Mountain
countries: United States
coordinates: lat: 45.1636
lon: -117.302
surface_form: mount nebo
instance_of: Mountain
countries: United States
coordinates: lat: 39.8214
lon: -111.76
surface_form: mount nebo
instance_of: Mountain
countries: United States
coordinates: lat: 45.161111111111
lon: -117.1375
surface_form: mount nebo
instance_of: Landform
countries: United States
coordinates: lat: 46.3561
lon: -95.1072
surface_form: mount nebo
instance_of: Mountain
countries: United States
coordinates: lat: 42.365833333333
lon: -74.221944444444
Mount Nebo is a mountain in the Eagle Cap Wilderness of Oregon, in the United States. Named after the biblical Mount Nebo overlooking Israel, which is said to be the place of Moses' death. It is the centerpiece of the Imnaha Divide, inside the Wallowa–Whitman National Forest. Mount Nebo is one of the important areas where sheep and cattle graze throughout Eagle Cap Wilderness. Location.

Geographic entities mentioned:
surface_form: mount nebo
instance_of: Mountain
countries: United States
coordinates: lat: 35.2159
lon: -93.2535
surface_form: eagle cap
instance_of: Mountain
countries: United States
coordinates: lat: 45.1636
lon: -117.302
surface_form: mount nebo
instance_of: Mountain
countries: United States
coordinates: lat: 39.8214
lon: -111.76
surface_form: mount nebo
instance_of: Mountain
countries: United States
coordinates: lat: 45.161111111111
lon: -117.1375
surface_form: mount nebo
instance_of: Landform
countries: United States
coordinates: lat: 46.3561
lon: -95.1072
surface_form: mount nebo
instance_of: Mountain
countries: United States
coordinates: lat: 42.365833333333
lon: -74.221944444444
Mount Nebo is one of the important areas where sheep and cattle graze throughout Eagle Cap Wilderness. Location. Mount Nebo is located in the northern ridge of the Imnaha Divide, approximately 2 miles North of the confluence of the north and south forks of the Imnaha River. The slopes and meadows that surround Mount Nebo reach towards the Tenderfoot Wagon Road and Mine south of McCully Basin.

Geographic entities mentioned:
surface_form: mount nebo
instance_of: Mountain
countries: United States
coordinates: lat: 35.2159
lon: -93.2535
surface_form: mount nebo
instance_of: Mountain
countries: United States
coordinates: lat: 39.8214
lon: -111.76
surface_form: mount nebo
instance_of: Mountain
countries: United States
coordinates: lat: 45.161111111111
lon: -117.1375
surface_form: mount nebo
instance_of: Landform
countries: United States
coordinates: lat: 46.3561
lon: -95.1072
surface_form: mount nebo
instance_of: Mountain
countries: United States
coordinates: lat: 42.365833333333
lon: -74.221944444444
Location. Mount Nebo is located in the northern ridge of the Imnaha Divide, approximately 2 miles North of the confluence of the north and south forks of the Imnaha River. The slopes and meadows that surround Mount Nebo reach towards the Tenderfoot Wagon Road and Mine south of McCully Basin. Ecology. Mount Nebo has an open grassy south-facing slope.

Geographic entities mentioned:
surface_form: mount nebo
instance_of: Mountain
countries: United States
coordinates: lat: 35.2159
lon: -93.2535
surface_form: mount nebo
instance_of: Mountain
countries: United States
coordinates: lat: 39.8214
lon: -111.76
surface_form: mount nebo
instance_of: Mountain
countries: United States
coordinates: lat: 45.161111111111
lon: -117.1375
surface_form: mount nebo
instance_of: Landform
countries: United States
coordinates: lat: 46.3561
lon: -95.1072
surface_form: mount nebo
instance_of: Mountain
countries: United States
coordinates: lat: 42.365833333333
lon: -74.221944444444
The slopes and meadows that surround Mount Nebo reach towards the Tenderfoot Wagon Road and Mine south of McCully Basin. Ecology. Mount Nebo has an open grassy south-facing slope. It was a target of a significant fire in the early 1900s. Since then, mountain big sagebrush has invaded most of the open grassy slope.

Geographic entities mentioned:
surface_form: mount nebo
instance_of: Mountain
countries: United States
coordinates: lat: 35.2159
lon: -93.2535
surface_form: mount nebo
instance_of: Mountain
countries: United States
coordinates: lat: 39.8214
lon: -111.76
surface_form: mount nebo
instance_of: Mountain
countries: United States
coordinates: lat: 45.161111111111
lon: -117.1375
surface_form: mount nebo
instance_of: Landform
countries: United States
coordinates: lat: 46.3561
lon: -95.1072
surface_form: mount nebo
instance_of: Mountain
countries: United States
coordinates: lat: 42.365833333333
lon: -74.221944444444
Lookout tower. Several fire lookout towers were built in the early 1900s throughout the Wallowa–Whitman National Forest. Mount Nebo had a lookout tower and 10x10 cabin built in the 1920s. Maintenance and cabin occupation was reported through the 1950s. The tower and the cabin were removed in the 1970s.

Geographic entities mentioned:
surface_form: mount nebo
instance_of: Mountain
countries: United States
coordinates: lat: 35.2159
lon: -93.2535
surface_form: mount nebo
instance_of: Mountain
countries: United States
coordinates: lat: 39.8214
lon: -111.76
surface_form: mount nebo
instance_of: Mountain
countries: United States
coordinates: lat: 45.161111111111
lon: -117.1375
surface_form: mount nebo
instance_of: Landform
countries: United States
coordinates: lat: 46.3561
lon: -95.1072
surface_form: mount nebo
instance_of: Mountain
countries: United States
coordinates: lat: 42.365833333333
lon: -74.221944444444
Fish & Wildlife Service, Holyoke Boys & Girls Club. In recent years there has been discussion of reopening the property as a nature camp, or potentially as a special permit skiing area, not unlike Mount Snow, but while some have still used the remaining ski slopes in recent years, the area has been subject to vandalism and remains closed with no plans for reopening agreed on by its landholders.

Geographic entities mentioned:
surface_form: Mount Snow
instance_of: Mountain
countries: United States
coordinates: lat: 42.95897
lon: -72.92371
Biography. Albin Moroder was the second born son of Otto Moroder and Anna Moroder, b. Knottner, as well as a grandson of the artist Josef Moroder Lusenber. Albin grew up in Schlitters in Zillertal, in 1927 the whole family moved to a house in Mayrhofen newly built by their father, where a lively tourism industry flourished and brought an economic boom to the then poor region.

Geographic entities mentioned:
surface_form: Zillertal
instance_of: Valley
countries: Austria
coordinates: lat: 47.333333333333
lon: 11.866666666667
Innsvatnet. Innsvatnet is a lake in Verdal Municipality in Trøndelag county, Norway. The lake lies in the eastern part of the municipality, just west of the border with Sweden. The lake is the headwaters for the river Inna, which later flows into the Verdalselva river. The lake sits at an elevation of above sea level.

Geographic entities mentioned:
surface_form: innsvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 63.6578
lon: 12.1994
Piz Surgonda. Piz Surgonda is a mountain of the Albula Alps, located north of the Julier Pass in the canton of Graubünden. It lies on the range surrounding the Val Bever, east of Piz d'Agnel. Piz Surgonda is composed of two summits of almost equal height: the western summit (3,193 m) and the eastern summit (3,196 m).

Geographic entities mentioned:
surface_form: Piz d'Agnel
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.511444444444
lon: 9.70225
Piz Surgonda. Piz Surgonda is a mountain of the Albula Alps, located north of the Julier Pass in the canton of Graubünden. It lies on the range surrounding the Val Bever, east of Piz d'Agnel. Piz Surgonda is composed of two summits of almost equal height: the western summit (3,193 m) and the eastern summit (3,196 m).

Geographic entities mentioned:
surface_form: piz surgonda
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.51
lon: 9.725
The Seri Saujana bridge, also called Bridge No 8, crosses Putrajaya Lake, an artificial lake made to provide natural cooling, and connects the Core Island (Precinct 4) to the Precinct 7 on Lebuh Sentosa highway.

Geographic entities mentioned:
surface_form: Putrajaya Lake
instance_of: Lake
countries: Malaysia
coordinates: lat: 2.9419416666667
lon: 101.68911111111
Càrn Gorm. Càrn Gorm is a mountain in the Breadalbane region of the Scottish Highlands, with a height of. It stands in a group of four Munro mountains known as the Càrn Mairg group or the Glen Lyon Horseshoe, on the north side of Glen Lyon, Perthshire. Overview. Càrn Gorm reaches a height of 1029 metres (3376 feet), it qualifies as a Munro and a Marilyn.

Geographic entities mentioned:
surface_form: Càrn Mairg
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.634635
lon: -4.145608
surface_form: Glen Lyon
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.59864
lon: -4.25283
surface_form: glen lyon
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.59864
lon: -4.25283
Overview. Càrn Gorm reaches a height of 1029 metres (3376 feet), it qualifies as a Munro and a Marilyn. It is often climbed as part of the circuit of the Càrn Mairg Munros which stand in a curving arc around the Invervar Burn. Càrn Gorm is the first of the hills climbed when the round is walked in a clockwise direction, it is then followed by Meall Garbh, Càrn Mairg and Meall nan Aighean.

Geographic entities mentioned:
surface_form: Càrn Mairg
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.634635
lon: -4.145608
surface_form: Meall nan Aighean
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.620618
lon: -4.12874
surface_form: meall garbh
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.566122
lon: -4.207714
surface_form: meall garbh
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.637381
lon: -4.207472
surface_form: càrn gorm
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.6221
lon: -4.2253
Geography. Càrn Gorm is mostly composed of grassy slopes with sporadic rocky outcrops, its attractive summit peak is formed by the meeting of four ridges of varying lengths. The NW ridge is the longest, running for eight km down to the shores of Loch Rannoch its lower slopes are clothed in the woodlands of the Carie and Cragganester Woods SSSI part of the ancient Black Wood of Rannoch.

Geographic entities mentioned:
surface_form: Loch Rannoch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.688299
lon: -4.30386
surface_form: loch rannoch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.688299
lon: -4.30386
In between the ridges there are steep slopes, especially to the east, north and SW. All drainage from Càrn Gorm feeds the River Tay with the majority going south via Glen Lyon although a small percentage goes north via Loch Rannoch. Ascents and summit.

Geographic entities mentioned:
surface_form: Loch Rannoch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.688299
lon: -4.30386
surface_form: loch rannoch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.688299
lon: -4.30386
surface_form: glen lyon
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.59864
lon: -4.25283
The summit has two high points, the true summit is marked by a small cairn while 80 metres to the NW is the site of the OS trig point which has been pushed over and is lying on its side, surrounded by a wind shelter. The best views from the summit are to the south, there being an aerial view of Glen Lyon and a good spectacle of the Ben Lawers range.

Geographic entities mentioned:
surface_form: Ben Lawers
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.544922
lon: -4.22086
surface_form: ben lawers
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.544922
lon: -4.22086
surface_form: glen lyon
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.59864
lon: -4.25283
The route goes north through the woodland for just over a kilometre until the open hillside is reached, the hill can then be climbed by its SE ridge. As an alternative to the Glen Lyon horseshoe walk, Càrn Gorm can climbed with the adjoining corbett of Beinn Dearg, which lies 2.5 km to the west across the steep sided Dubh Choirein starting at Camusvrachen (grid reference) at the foot of that glen.

Geographic entities mentioned:
surface_form: beinn dearg
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.78635
lon: -4.929557
surface_form: beinn dearg
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.877346
lon: -3.883719
surface_form: beinn dearg
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.5888
lon: -5.52136
surface_form: glen lyon
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.59864
lon: -4.25283
surface_form: càrn gorm
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.6221
lon: -4.2253
The SE ridge descends to the glen of the Invervar Burn and is planted with coniferous woodland on its lower slopes. This eastern side of the mountain is part of the Càrn Gorm and Meall Garbh SSSI, a 1930 hectare area of sub-alpine mountain habitat, an example of natural and undisturbed territory within the UK with rare plant species.

Geographic entities mentioned:
surface_form: meall garbh
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.566122
lon: -4.207714
surface_form: meall garbh
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.637381
lon: -4.207472
surface_form: càrn gorm
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.6221
lon: -4.2253
Càrn Gorm's south ridge is short and steep with some crags and is best shunned as a walking route, it descends quickly to Glen Lyon near Camusvrachan. The north ridge is more significant connecting the mountain to the adjoining Munro of Meall Garbh, firstly going over the subsidiary top of An Sgorr (The Rocky Peak).

Geographic entities mentioned:
surface_form: meall garbh
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.566122
lon: -4.207714
surface_form: meall garbh
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.637381
lon: -4.207472
With a height of 924 metres An Sgorr is listed in the Munro Tables as a “Top” of Càrn Gorm. On the traverse between the two Munros, An Sgorr can be by-passed on its NW side, but most walkers will climb it and then drop to the col with a height of 845 metres before climbing to Meall Garbh. In between the ridges there are steep slopes, especially to the east, north and SW.

Geographic entities mentioned:
surface_form: meall garbh
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.566122
lon: -4.207714
surface_form: meall garbh
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.637381
lon: -4.207472
Lower down by the Invervar Burn are the remains of some old shielings from the time when cattle were brought up to summer pasture on these hills. Càrn Gorm's south ridge is short and steep with some crags and is best shunned as a walking route, it descends quickly to Glen Lyon near Camusvrachan.

Geographic entities mentioned:
surface_form: glen lyon
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.59864
lon: -4.25283
Ascents and summit. As mentioned, Càrn Gorm is invariably climbed as the first peak of the Glen Lyon horseshoe, the start is at Invervar in Glen Lyon (grid reference) where there is a small car park. The route goes north through the woodland for just over a kilometre until the open hillside is reached, the hill can then be climbed by its SE ridge.

Geographic entities mentioned:
surface_form: glen lyon
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.59864
lon: -4.25283
surface_form: glen lyon
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.59864
lon: -4.25283
Càrn Gorm. Càrn Gorm is a mountain in the Breadalbane region of the Scottish Highlands, with a height of. It stands in a group of four Munro mountains known as the Càrn Mairg group or the Glen Lyon Horseshoe, on the north side of Glen Lyon, Perthshire. Overview. Càrn Gorm reaches a height of 1029 metres (3376 feet), it qualifies as a Munro and a Marilyn.

Geographic entities mentioned:
surface_form: càrn gorm
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.6221
lon: -4.2253
It stands in a group of four Munro mountains known as the Càrn Mairg group or the Glen Lyon Horseshoe, on the north side of Glen Lyon, Perthshire. Overview. Càrn Gorm reaches a height of 1029 metres (3376 feet), it qualifies as a Munro and a Marilyn. It is often climbed as part of the circuit of the Càrn Mairg Munros which stand in a curving arc around the Invervar Burn.

Geographic entities mentioned:
surface_form: càrn gorm
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.6221
lon: -4.2253
Càrn Gorm is the first of the hills climbed when the round is walked in a clockwise direction, it is then followed by Meall Garbh, Càrn Mairg and Meall nan Aighean. Although not the highest of the group Càrn Gorm is often regarded as the finest looking with its summit shaped into a neat cone. The hill lies within the Chesthill estate, and large herds of deer are often seen on its slopes.

Geographic entities mentioned:
surface_form: càrn gorm
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.6221
lon: -4.2253
Càrn Gorm translates literally from the Gaelic as &quot;blue hill&quot;, but the word &quot;gorm&quot; is also used for the green of foliage, and probably comes from the dark tones of the grass on the hillside rather than the shady hues of the conifer plantation on its south east slopes which was planted well after the hill was named. Geography.

Geographic entities mentioned:
surface_form: càrn gorm
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.6221
lon: -4.2253
surface_form: càrn gorm
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.6221
lon: -4.2253
The north ridge is more significant connecting the mountain to the adjoining Munro of Meall Garbh, firstly going over the subsidiary top of An Sgorr (The Rocky Peak). With a height of 924 metres An Sgorr is listed in the Munro Tables as a “Top” of Càrn Gorm.

Geographic entities mentioned:
surface_form: càrn gorm
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.6221
lon: -4.2253