Sarmila/GeoWiki-Features huggingface dataset:
Overview. An Riabhachan reaches a height of 1129 metres (3704 feet) and is one of the highest Munros north of the Great Glen. The mountain's name originates from the Gaelic language and translates as “The Brindled One” which is believed to refer to the flecked effect given by the stone studded turf on the hill. Geography. An Riabhachan is a mainly grassy mountain.

Geographic entities mentioned:
surface_form: Great Glen
instance_of: Valley
countries: United Kingdom
coordinates: lat: 57.3
lon: -4.45
surface_form: the great glen
instance_of: Valley
countries: United Kingdom
coordinates: lat: 57.3
lon: -4.45
surface_form: an riabhachan
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.362438
lon: -5.104728
Ascents. The mountain is usually climbed together with two or three of the other Munros on the north side of Loch Mullardoch. The most convenient ascent of all four Munros starts at the Mullardoch dam in Glen Cannich (grid reference) and proceeds 9 km along the loch's northern shore before climbing An Socach, continuing to An Riabhachan and returning via Sgurr na Lapaich and Càrn nan Gobhar.

Geographic entities mentioned:
surface_form: càrn nan gobhar
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.363304
lon: -5.024544
surface_form: càrn nan gobhar
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.452331
lon: -4.879935
surface_form: glen cannich
instance_of: Valley
countries: United Kingdom
coordinates: lat: 57.34000015
lon: -4.94999981
surface_form: sgurr na lapaich
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.369311
lon: -5.059726
surface_form: an socach
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.902295
lon: -3.513165
surface_form: an riabhachan
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.362438
lon: -5.104728
surface_form: an socach
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.350229
lon: -5.158603
From the power station a stalkers' path leads to the Bealach Toll an Lochain between An Riabhachan and Sgurr na Lapaich, from where there is a further climb west of over 300 metres to reach the summit. A return to the power station can be made over Sgurr na Lapaich and Càrn nan Gobhar.

Geographic entities mentioned:
surface_form: càrn nan gobhar
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.363304
lon: -5.024544
surface_form: càrn nan gobhar
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.452331
lon: -4.879935
surface_form: sgurr na lapaich
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.369311
lon: -5.059726
Geography. An Riabhachan is a mainly grassy mountain. The only rocky area is at the north-east end of the summit ridge, above the fine craggy coire of Coire Gnada containing the lochans of Loch Mòr and Loch Beag. The east ridge links to the adjacent Munro of Sgurr na Lapaich and follows the steep edge above Coire Gnada.

Geographic entities mentioned:
surface_form: sgurr na lapaich
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.369311
lon: -5.059726
From the power station a stalkers' path leads to the Bealach Toll an Lochain between An Riabhachan and Sgurr na Lapaich, from where there is a further climb west of over 300 metres to reach the summit. A return to the power station can be made over Sgurr na Lapaich and Càrn nan Gobhar.

Geographic entities mentioned:
surface_form: sgurr na lapaich
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.369311
lon: -5.059726
surface_form: an riabhachan
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.362438
lon: -5.104728
With the demise of the NE Top, An Riabhachan has been left with just two subsidiary Tops. The West Top with a height of 1040 metres stands at the western end of the summit ridge, before descending to the Bealach Bholla and reascending to the adjoining Munro of An Socach. The South West Top lies 700m SE of the West Top and has a height of 1086 metres.

Geographic entities mentioned:
surface_form: an socach
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.902295
lon: -3.513165
surface_form: an socach
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.350229
lon: -5.158603
The long walk along the shore can be bypassed by hiring a boat, currently available between 1 April and 1 August. The walk can be shortened by omitting An Socach, but it is better to include it if you can as there is no easier access to this remote Munro.

Geographic entities mentioned:
surface_form: an socach
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.902295
lon: -3.513165
surface_form: an socach
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.350229
lon: -5.158603
The South West Top lies 700m SE of the West Top and has a height of 1086 metres. The summit ridge falls away on both sides over grassy slopes to Loch Mullardoch to the south and to the upper part of Glen Strathfarrar to the north. Ascents. The mountain is usually climbed together with two or three of the other Munros on the north side of Loch Mullardoch.

Geographic entities mentioned:
surface_form: glen strathfarrar
instance_of: Valley
countries: United Kingdom
coordinates: lat: 57.414166666667
lon: -4.8391666666667
The alternative route starts in Glen Strathfarrar to the north at the hydroelectric power station in Gleann Innis (grid reference), reached by a 17-mile drive from Struy along a private road; the locked gate at the entrance to this road is opened at specified times to give access to vehicles.

Geographic entities mentioned:
surface_form: glen strathfarrar
instance_of: Valley
countries: United Kingdom
coordinates: lat: 57.414166666667
lon: -4.8391666666667
An Riabhachan. An Riabhachan is a Scottish mountain in the Skye and Lochalsh district of the Highland council area. It is situated 35 kilometres east of Kyle of Lochalsh standing in an isolated position at the western end of Loch Mullardoch, ten kilometres from any public road. Overview.

Geographic entities mentioned:
surface_form: an riabhachan
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.362438
lon: -5.104728
The mountain's name originates from the Gaelic language and translates as “The Brindled One” which is believed to refer to the flecked effect given by the stone studded turf on the hill. Geography. An Riabhachan is a mainly grassy mountain. The only rocky area is at the north-east end of the summit ridge, above the fine craggy coire of Coire Gnada containing the lochans of Loch Mòr and Loch Beag.

Geographic entities mentioned:
surface_form: an riabhachan
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.362438
lon: -5.104728
It was deleted from the list of Munro Tops in 1997. With the demise of the NE Top, An Riabhachan has been left with just two subsidiary Tops. The West Top with a height of 1040 metres stands at the western end of the summit ridge, before descending to the Bealach Bholla and reascending to the adjoining Munro of An Socach.

Geographic entities mentioned:
surface_form: an riabhachan
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.362438
lon: -5.104728
Penetangore River. The Penetangore River is a river in Kincardine, Bruce County in Southwestern Ontario, Canada. It is in the Great Lakes Basin and empties into Lake Huron. A boardwalk, a harbour, and the Kincardine lighthouse are located on the bank of this river near its mouth.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
Location. Garsdale lies on the western slopes of the Pennines, between Baugh Fell to the north and Rise Hill to the south. It is within the Yorkshire Dales National Park. The dale is the valley of the Clough River, which rises on the north eastern slopes of Baugh Fell and flows through Grisedale, the &quot;Dale that Died&quot;, as Grisedale Beck until it becomes the Clough River at Garsdale Head.

Geographic entities mentioned:
surface_form: Grisedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.333333333333
lon: -2.35
surface_form: grisedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.333333333333
lon: -2.35
surface_form: garsdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.301
lon: -2.391
The largest settlement, known as &quot;The Street&quot;, lies east of Sedbergh and west of Hawes. The other hamlet in Garsdale is Garsdale Head, also called &quot;Hawes Junction&quot;, the old name for Garsdale station, after the former Wensleydale branch on the Settle to Carlisle railway.

Geographic entities mentioned:
surface_form: Wensleydale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.3056
lon: -2.16667
surface_form: garsdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.301
lon: -2.391
surface_form: garsdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.301
lon: -2.391
surface_form: garsdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.301
lon: -2.391
surface_form: wensleydale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.3056
lon: -2.16667
Garsdale. Garsdale is a dale in the south-east of Cumbria, England. It lies within the Westmorland and Furness local government district and in the Yorkshire Dales National Park for planning purposes; it was historically a part of the West Riding of Yorkshire. In the 2001 census, the parish had a population of 202, decreasing to 191 in 2011. History.

Geographic entities mentioned:
surface_form: garsdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.301
lon: -2.391
In the 2001 census, the parish had a population of 202, decreasing to 191 in 2011. History. Historically, Garsdale was a chapelry in the ancient parish of Sedbergh in the Ewecross wapentake, in the West Riding of Yorkshire. In 1866, it became a separate civil parish. From 1894 to 1974, it was part of Sedbergh Rural District; it became part of the new county of Cumbria in 1974. Location.

Geographic entities mentioned:
surface_form: garsdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.301
lon: -2.391
In 1866, it became a separate civil parish. From 1894 to 1974, it was part of Sedbergh Rural District; it became part of the new county of Cumbria in 1974. Location. Garsdale lies on the western slopes of the Pennines, between Baugh Fell to the north and Rise Hill to the south. It is within the Yorkshire Dales National Park.

Geographic entities mentioned:
surface_form: garsdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.301
lon: -2.391
The dale forms the civil parish of Garsdale, although the last mile and a half of the course of the Clough river, before its confluence with the Rawthey, is part of the parish of Sedbergh. Small settlements lie along the main Northallerton to Kendal road (the A684) which runs through the dale for, with frequent bridges in the upper part of the dale.

Geographic entities mentioned:
surface_form: garsdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.301
lon: -2.391
The Sedgwick Trail, named after the well-known geologist Adam Sedgwick runs along the Clough from Danny Bridge and highlights rock features along the Dent Fault. Garsdale is host to the charity which aims at enhancing the land for nature, restoring the peat bog and providing young people an opportunity to gain experience in conservation work. Governance.

Geographic entities mentioned:
surface_form: dent
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5023
lon: -3.48242
The Sedgwick Trail, named after the well-known geologist Adam Sedgwick runs along the Clough from Danny Bridge and highlights rock features along the Dent Fault. Garsdale is host to the charity which aims at enhancing the land for nature, restoring the peat bog and providing young people an opportunity to gain experience in conservation work. Governance.

Geographic entities mentioned:
surface_form: garsdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.301
lon: -2.391
Governance. Garsdale is part of the Westmorland and Lonsdale parliamentary constituency, of which Tim Farron is the current MP representing the Liberal Democrats. Garsdale has its own parish council: &quot;Garsdale Parish Council&quot;. Churches.

Geographic entities mentioned:
surface_form: garsdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.301
lon: -2.391
surface_form: garsdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.301
lon: -2.391
Churches. The Anglican Church of St John the Baptist, built in 1861 next to the original medieval church, lies from Sedbergh, between The Street and Garsdale Hall, which was once an inn but is now used as a farm store. There are also three Methodist chapels: Low Smithy and Garsdale Street, both in regular use, and Hawes Junction which has occasional special events. Farming.

Geographic entities mentioned:
surface_form: garsdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.301
lon: -2.391
surface_form: garsdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.301
lon: -2.391
Churches. The Anglican Church of St John the Baptist, built in 1861 next to the original medieval church, lies from Sedbergh, between The Street and Garsdale Hall, which was once an inn but is now used as a farm store. There are also three Methodist chapels: Low Smithy and Garsdale Street, both in regular use, and Hawes Junction which has occasional special events. Farming.

Geographic entities mentioned:
surface_form: garsdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.301
lon: -2.391
Ammianus Marcellinus referred to &quot;Mogontiacum&quot; as &quot;municipium Mogontiacum&quot; in 355. Provincial capital Mogontiacum of the province of Germania superior. After Tiberius renounced the permanent occupation of &quot;Magna Germania&quot; with the desired Elbe border, the organisation of the areas on the left bank of the Rhine remained in a provisional administrative stage.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Eureka Peak. Eureka Peak is a 7,447-foot granite peak in the Northern Sierra Nevada in Plumas County, California in the United States. Formerly known as Gold Mountain, it is located within the Plumas Eureka State Park. Prospectors in search of the mystical Gold Lake discovered gold in a quartz outcrop on May 23, 1851, and gold mining continued until 1942.

Geographic entities mentioned:
surface_form: eureka peak
instance_of: Mountain
countries: United States
coordinates: lat: 34.0325
lon: -116.35
surface_form: eureka peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.749166666667
lon: -120.72111111111
Eureka Peak. Eureka Peak is a 7,447-foot granite peak in the Northern Sierra Nevada in Plumas County, California in the United States. Formerly known as Gold Mountain, it is located within the Plumas Eureka State Park. Prospectors in search of the mystical Gold Lake discovered gold in a quartz outcrop on May 23, 1851, and gold mining continued until 1942.

Geographic entities mentioned:
surface_form: eureka peak
instance_of: Mountain
countries: United States
coordinates: lat: 34.0325
lon: -116.35
surface_form: granite peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.9101
lon: -122.872
surface_form: granite peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.163416666667
lon: -109.80744444444
surface_form: granite peak
instance_of: Mountain
countries: United States
coordinates: lat: 41.6681
lon: -117.589
surface_form: eureka peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.749166666667
lon: -120.72111111111
surface_form: granite peak
instance_of: Mountain
countries: United States
coordinates: lat: 61.7972
lon: -148.8858
Eureka Peak. Eureka Peak is a 7,447-foot granite peak in the Northern Sierra Nevada in Plumas County, California in the United States. Formerly known as Gold Mountain, it is located within the Plumas Eureka State Park. Prospectors in search of the mystical Gold Lake discovered gold in a quartz outcrop on May 23, 1851, and gold mining continued until 1942.

Geographic entities mentioned:
surface_form: gold mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.5489
lon: -122.787
Formerly known as Gold Mountain, it is located within the Plumas Eureka State Park. Prospectors in search of the mystical Gold Lake discovered gold in a quartz outcrop on May 23, 1851, and gold mining continued until 1942. The mine's tramway may have served as the world's first ski lift.

Geographic entities mentioned:
surface_form: gold lake
instance_of: Lake
countries: United States
coordinates: lat: 47.55
lon: -121.34388888889
Precolonial period. The traditional origins of the town are attributed to ten Bornean datus who sailed northward on board balangays and ended in Silang through Taal Lake. Its first settlers were Gat Hingiw, his wife Gat Kaliwanag, and their seven children, who later moved to different parts of the town and established their respective barangays.

Geographic entities mentioned:
surface_form: Taal Lake
instance_of: Lake
countries: Philippines
coordinates: lat: 13.986944
lon: 121.012222
Mybster. Mybster is a small village, in Caithness, Scottish Highlands, and is in the Scottish council area of Highland. Mybster lies northwest of the Loch of Toftingall, with the village of Watten lying directly to the east, and Thurso located north along the A9 road.

Geographic entities mentioned:
surface_form: Loch of Toftingall
instance_of: Lake
countries: United Kingdom
coordinates: lat: 58.45
lon: -3.3833333333333
Sila National Park. Sila National Park () is an Italian national park in Calabria, located on the Sila Plateau. It was established in 1997 and covers about. Its highest mountains are Mt. Botte Donato (1,928 m), in Sila Grande, and Mt. Gariglione (1,764 m) in Sila Piccola. The park was established with the Regional Decree of 14 November 2002 and includes its own management agency.

Geographic entities mentioned:
surface_form: Botte Donato
instance_of: Mountain
countries: Italy
coordinates: lat: 39.2847
lon: 16.4472
Noohalk Mountain. Noohalk Mountain 2099 m (6886 feet) is a mountain in the northernmost Pacific Ranges of the Coast Mountains in British Columbia, Canada. It is located on the south side of the Bella Coola Valley between Hagensborg and Bella Coola. Name origin.

Geographic entities mentioned:
surface_form: Bella Coola Valley
instance_of: Valley
countries: Canada
Noohalk Mountain. Noohalk Mountain 2099 m (6886 feet) is a mountain in the northernmost Pacific Ranges of the Coast Mountains in British Columbia, Canada. It is located on the south side of the Bella Coola Valley between Hagensborg and Bella Coola. Name origin.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: noohalk mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 52.333330555556
lon: -126.62916944444
Name origin. &quot;Noohalk&quot; is an older transliteration of the local native name for the valley and the river, which has been adopted as the modern name of that people, the Nuxalk, who once had villages all through the adjoining inlets and islands of North and South Bentinck Arms, Dean Channel, Burke Channel and on King Island.

Geographic entities mentioned:
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
Noohalk Mountain. Noohalk Mountain 2099 m (6886 feet) is a mountain in the northernmost Pacific Ranges of the Coast Mountains in British Columbia, Canada. It is located on the south side of the Bella Coola Valley between Hagensborg and Bella Coola. Name origin.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: noohalk mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 52.333330555556
lon: -126.62916944444
Geography. The Cavée river has its source at Rieutard Lake (length:; altitude:, located in the unorganized territory of Lac-Jacques-Cartier, in the La Côte-de-Beaupré Regional County Municipality This lake receives water from the eastern side of the discharge of a set of lakes (Mérillon, Dugas, de la Rocaille, Hardy, Joug and Dan).

Geographic entities mentioned:
surface_form: Rieutard Lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.702777777778
lon: -71.434722222222
Upper course of the Cavée river (segment of)
Lower course of the Cavée river (segment of)
From the confluence of the Cuvée river, the current follows the course of the Rivière Jacques-Cartier Nord-Ouest on, the course of the Jacques-Cartier River on to the south the northeast bank of the Saint Lawrence River. Toponymy.

Geographic entities mentioned:
surface_form: Jacques-Cartier River
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.671388888889
lon: -71.747222222222
Queen Victoria Rock is a pillar in Grand County, Utah, United States. Description. Queen Victoria Rock is located within Arches National Park and like many of the rock formations in the park, it is composed of Entrada Sandstone, specifically the Slick Rock Member overlaying the Dewey Bridge Member. Topographic relief is significant as the summit rises above the Park Avenue Trail in laterally.

Geographic entities mentioned:
surface_form: park
instance_of: Mountain
coordinates: lat: -67.2333
lon: 51
surface_form: park
instance_of: Mountain
coordinates: lat: -67.2333
lon: 51
surface_form: queen victoria rock
instance_of: Mountain
coordinates: lat: 38.6275
lon: -109.599
surface_form: dewey
instance_of: Mountain
coordinates: lat: -65.9
lon: -64.3167
Queen Victoria Rock is a pillar in Grand County, Utah, United States. Description. Queen Victoria Rock is located within Arches National Park and like many of the rock formations in the park, it is composed of Entrada Sandstone, specifically the Slick Rock Member overlaying the Dewey Bridge Member. Topographic relief is significant as the summit rises above the Park Avenue Trail in laterally.

Geographic entities mentioned:
surface_form: park
instance_of: Mountain
coordinates: lat: -67.2333
lon: 51
surface_form: trail
instance_of: Mountain
coordinates: lat: -67.2
lon: 50.85
Climate. According to the Köppen climate classification system, Queen Victoria Rock is located in a cold semi-arid climate zone with cold winters and hot summers. Spring and fall are the most favorable seasons to experience Arches National Park, when highs average and lows average. Summer temperatures often exceed. Winters are cold, with highs averaging, and lows averaging.

Geographic entities mentioned:
surface_form: park
instance_of: Mountain
coordinates: lat: -67.2333
lon: 51
Queen Victoria Rock. Queen Victoria Rock is a pillar in Grand County, Utah, United States. Description. Queen Victoria Rock is located within Arches National Park and like many of the rock formations in the park, it is composed of Entrada Sandstone, specifically the Slick Rock Member overlaying the Dewey Bridge Member.

Geographic entities mentioned:
surface_form: queen victoria rock
instance_of: Mountain
coordinates: lat: 38.6275
lon: -109.599
Topographic relief is significant as the summit rises above the Park Avenue Trail in laterally. Precipitation runoff from Queen Victoria Rock drains to the nearby Colorado River via Courthouse Wash.

Geographic entities mentioned:
surface_form: queen victoria rock
instance_of: Mountain
coordinates: lat: 38.6275
lon: -109.599
Charlie Fowler and Alison Sheets also climbed the route, &quot;Queen For A Day&quot;, rated (I, A-2). Climate. According to the Köppen climate classification system, Queen Victoria Rock is located in a cold semi-arid climate zone with cold winters and hot summers. Spring and fall are the most favorable seasons to experience Arches National Park, when highs average and lows average.

Geographic entities mentioned:
surface_form: queen victoria rock
instance_of: Mountain
coordinates: lat: 38.6275
lon: -109.599
He was a trusted member of King Richard III's council, and, by reason of his position, judge of the Duchy court that sat at Westminster. Thomas Metcalfe built Nappa Hall in Wensleydale, North Yorkshire in the 1470s. He married Elizabeth Hartlington of Hartlington, in Craven, Yorkshire, heiress of an ancient family of Clifford tenants who had been bailiffs of Kettlewelldale.

Geographic entities mentioned:
surface_form: Wensleydale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.3056
lon: -2.16667
Norway. In 1957, the director of the secret service NIS, Vilhelm Evang, protested strongly against the pro-active intelligence activities at AFNORTH, as described by the chairman of CPC: &quot;[NIS] was extremely worried about activities carried out by officers at Kolsås. This concerned SB, Psywar and Counter Intelligence.&quot; These activities supposedly included the blacklisting of Norwegians.

Geographic entities mentioned:
surface_form: Kolsås
instance_of: Mountain
countries: Norway
coordinates: lat: 59.933333333333
lon: 10.516666666667
It was founded by Sardar Abdur Rab Nishtar in 1951, and named after the Quaid-e-Azam (the founder of Pakistan). It has famous Warcha salt mine. It has road links to the sandy agricultural area of Thal and with the mountain of Soon Valley. It is part of National Assembly constituency NA-94 and Provincial Assembly of Punjab constituency PP-82. History.

Geographic entities mentioned:
surface_form: Soon Valley
instance_of: Valley
countries: Pakistan
coordinates: lat: 32.58
lon: 72.15
Southwick Beach State Park. Southwick Beach State Park is a New York State park that lies along an unusual stretch of sandy beach on the eastern shore of Lake Ontario. The park is in size with a length of beach, and is visited annually by about 100,000 people. Immediately to the south is the Lakeview Wildlife Management Area (), which extends the publicly accessible beach by several miles.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
The improvement in beachgrass growth has been documented by a &quot;photomonitoring project&quot; from 1995-2005. Until the 20th Century, the beachgrass in this region would have been the type now known as &quot;Champlain beachgrass&quot;, which is found only along eastern Lake Ontario and along Lake Champlain.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
Phutunqu. Phutunqu (Aymara for a small vessel or a hole, pit, crater, also spelled &quot;Phutunkhu&quot;) is a mountain in the Bolivian Andes. It is located in the Chuquisaca Department, Azurduy Province, Tarvita Municipality. It lies west of the San Antonio River which is a left tributary of the Pillku Mayu (Quechua for &quot;red river&quot;).

Geographic entities mentioned:
surface_form: phutunqu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.93
lon: -64.59277778
Ein Harod (Ihud). Ein Harod (Ihud) () is a kibbutz in northern Israel. Located in the Jezreel Valley near Mount Gilboa, it falls under the jurisdiction of Gilboa Regional Council. In it had a population of. Etymology. The kibbutz is named after the biblical spring of En Harod, which has become associated with the spring known in Hebrew as Ma'ayan Harod and in Arabic as Ain Jalut.

Geographic entities mentioned:
surface_form: Jezreel Valley
instance_of: Valley
countries: Israel
coordinates: lat: 32.596388888889
lon: 35.241944444444
Iseltwald. Iseltwald is a village and municipality on the southern shore of Lake Brienz in the Bernese Oberland region of Switzerland. Politically, the municipality is located in the Interlaken-Oberhasli administrative district of the canton of Bern. History. Iseltwald is first mentioned in 1146 as &quot;Iseltwalt&quot;.

Geographic entities mentioned:
surface_form: Lake Brienz
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.716667
lon: 7.95
Course. Mink Run begins about southeast of Lake Nockamixon at an elevation of and runs about where it turns south-southeast and picks up two tributaries, one on either side, after flowing another mile it shares its mouth with Deer Run at an elevation of. Its average slope is Wolf Run meets the Tohickon only a couple hundred feet downstream of Mink Run's confluence. Geology.

Geographic entities mentioned:
surface_form: Lake Nockamixon
instance_of: Lake
countries: United States
coordinates: lat: 40.465488888889
lon: -75.220988888889
In this &quot;battle&quot;, the contribution of the &quot;Regia Aeronautica&quot; was decisive as it decimated the Ethiopian troops on the shores of Lake Ashenge, effectively breaking apart the last army of the northern front. Background in Maychew. After the defeat of &quot;Ras&quot; Immrù in the Battle of Shire, Hailé Selassié gathered his imperial guard and moved north to meet the Italian army.

Geographic entities mentioned:
surface_form: Lake Ashenge
instance_of: Lake
countries: Ethiopia
coordinates: lat: 12.580555555556
lon: 39.5
However, due to the lack of supplies and the heavy defeats suffered, the army began to dissolve and the men ended up no longer obeying the orders of their leaders, advancing without any guide on the steep mountain paths that sloped down to the dangerously exposed basin of Lake Ashenge due to the lack of vegetation. Pietro Badoglio's &quot;trap&quot;.

Geographic entities mentioned:
surface_form: Lake Ashenge
instance_of: Lake
countries: Ethiopia
coordinates: lat: 12.580555555556
lon: 39.5
On April 4, 150 Italian planes surprised the retreating army near the shores of Lake Ashenge at first light.

Geographic entities mentioned:
surface_form: Lake Ashenge
instance_of: Lake
countries: Ethiopia
coordinates: lat: 12.580555555556
lon: 39.5
One group of deserters attempted to break through the British and French lines and escape but was forced back to the forts by rifle fire. Another group took horses and rode past the Allied lines to the Benue River which was flooded at the time. While attempting to swim across the river, many of the native soldiers drowned.

Geographic entities mentioned:
surface_form: Benue River
instance_of: Watercourse
countries: Cameroon
Nigeria
coordinates: lat: 7.783333
lon: 6.766667
Personal life. Ringier was married to the late law graduate Ellen Ringier (born Lüthy; who died in 2025) and has two adopted daughters. Ringier is considered a proven art collector with a collection of more than 4,000 works of contemporary art and lives in a modern villa on Lake Zurich. He likes to spend his holidays in his holiday home in Engadin.

Geographic entities mentioned:
surface_form: Lake Zurich
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.2475
lon: 8.6775
Ringier was married to the late law graduate Ellen Ringier (born Lüthy; who died in 2025) and has two adopted daughters. Ringier is considered a proven art collector with a collection of more than 4,000 works of contemporary art and lives in a modern villa on Lake Zurich. He likes to spend his holidays in his holiday home in Engadin. Ringier likes to jog and is a passionate tennis and golf player.

Geographic entities mentioned:
surface_form: Engadin
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.5497
lon: 9.8959
A substantial Samoyed city grew up at Mangazeya in the 16th century as a trade city, but was destroyed at the beginning of the 17th century. The Southern Samoyedic languages, of which only the Selkup language has survived to the present day, historically ranged across a wide territory in central Siberia, extending from the basin of the Ob River in the west to the Sayan-Baikal uplands in the east.

Geographic entities mentioned:
surface_form: Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
Burney Mountain. Burney Mountain is a lava dome complex located in the Cascade Range of eastern Shasta County, California, next to the slightly larger Crater Peak and slightly smaller Magee Peak. It stands at 2,397 m (7,854 ft) and is around 8.9 km (5.5 mi) south-southeast of Burney, California. Burney Mountain last erupted about 230,000 years ago during the Pleistocene epoch.

Geographic entities mentioned:
surface_form: Magee Peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.6893
lon: -121.6194
surface_form: crater peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.0397
lon: -107.663
surface_form: burney mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.806666666667
lon: -121.62777777778
surface_form: shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
Burney Mountain. Burney Mountain is a lava dome complex located in the Cascade Range of eastern Shasta County, California, next to the slightly larger Crater Peak and slightly smaller Magee Peak. It stands at 2,397 m (7,854 ft) and is around 8.9 km (5.5 mi) south-southeast of Burney, California. Burney Mountain last erupted about 230,000 years ago during the Pleistocene epoch.

Geographic entities mentioned:
surface_form: burney mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.806666666667
lon: -121.62777777778
It stands at 2,397 m (7,854 ft) and is around 8.9 km (5.5 mi) south-southeast of Burney, California. Burney Mountain last erupted about 230,000 years ago during the Pleistocene epoch. It is composed of two craters, which open to the east. Burney Mountain is the largest Quaternary dome in the Cascade Volcanic Arc, containing a volume of about.

Geographic entities mentioned:
surface_form: burney mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.806666666667
lon: -121.62777777778
Burney Mountain last erupted about 230,000 years ago during the Pleistocene epoch. It is composed of two craters, which open to the east. Burney Mountain is the largest Quaternary dome in the Cascade Volcanic Arc, containing a volume of about. The eastern side of the mountain was burned in the Eiler Fire in 2014, ultimately destroying 21 structures and injuring 11 people, mostly in Hat Creek.

Geographic entities mentioned:
surface_form: burney mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.806666666667
lon: -121.62777777778
Named by US-ACAN for Ronald D. Brown, aviation structural mechanic at Ellsworth Station, winter 1957. Skidmore Cliff. An irregular east-facing cliff, long, located at the extremity of a spur trending eastward from Saratoga Table. Named by US-ACAN for Donald D. Skidmore, ionospheric scientist at Ellsworth Station, winter 1957. Vigen Cliffs. Cliffs rising to about high to the east of Gabbro Crest.

Geographic entities mentioned:
surface_form: donald
instance_of: Mountain
coordinates: lat: -65.0833
lon: -60.1
surface_form: skidmore
instance_of: Mountain
coordinates: lat: -80.3
lon: -28.9333
Named by US-ACAN in 1979 after Lieutenant Richard M. Hook, United States Navy, Medical Officer at South Pole Station, winter party 1969. Ronald Rock. A prominent rock, high, along the cliff next north of Skidmore Cliff, located east of Saratoga Table. Named by US-ACAN for Ronald D. Brown, aviation structural mechanic at Ellsworth Station, winter 1957. Skidmore Cliff.

Geographic entities mentioned:
surface_form: brown
instance_of: Mountain
coordinates: lat: -68.3
lon: 86.4167
Named by US-ACAN for Walter H. May, aerographer at Ellsworth Station, winter 1957. Kent Gap. An ice-filled gap connecting the heads of May Valley and Chambers Glacier and marking the divide between Lexington and Saratoga Tables. Named by US-ACAN for Kenneth K. Kent, electronics technician at Ellsworth Station, winter 1957. Sorna Bluff.

Geographic entities mentioned:
surface_form: the divide
instance_of: Body of water
coordinates: lat: -60.73333
lon: -45.16667
Saratoga Table. The Saratoga Table () is a high, flat, snow-covered plateau, long and wide, standing just south of Kent Gap and Lexington Table in the southern Forrestal Range, Pensacola Mountains, Antarctica. Discovery and name.

Geographic entities mentioned:
surface_form: southern
instance_of: Mountain
coordinates: lat: -74.2
lon: -76.4667
surface_form: saratoga table
instance_of: Mountain
coordinates: lat: -83.34517
lon: -50.59592
surface_form: lexington table
instance_of: Mountain
coordinates: lat: -83.11885
lon: -49.87252
Ford (1973–91) on the petrology of Antarctica and specifically on the Dufek intrusion of the northern Pensacola Mountains was critical for the understanding of the evolution of this major igneous complex. Haskill Nunatak. An elongate nunatak, high, standing west of Dyrdal Peak in southern Forrestal Range. Named by US-ACAN for Robert E. Haskill, radioman at Ellsworth Station, winter 1957.

Geographic entities mentioned:
surface_form: southern
instance_of: Mountain
coordinates: lat: -74.2
lon: -76.4667
An elongate nunatak, high, standing west of Dyrdal Peak in southern Forrestal Range. Named by US-ACAN for Robert E. Haskill, radioman at Ellsworth Station, winter 1957. Ray Nunatak. A nunatak, high, located just north of Beiszer Nunatak and southwest of Dyrdal Peak in southern Forrestal Range. Named by US-ACAN for James A. Ray, utilities man at Ellsworth Station, winter 1957. Beiszer Nunatak.

Geographic entities mentioned:
surface_form: southern
instance_of: Mountain
coordinates: lat: -74.2
lon: -76.4667
It is separated from the Lexington Table to the north by May Valley, Kent Gap and Chambers Glacier. Features, clockwise from the north, include Sorna Bluff, Mount Hummer, Mount Hook, Ronald Rock, Skidmore Cliff, Vigen Cliffs, Gabbro Crest, Sheriff Cliffs, Fierle Peak, Dyrdal Peak, Mount Stephens, Magnetite Bluff, Mathis Spur, Burmester Dome and Huie Cliffs.

Geographic entities mentioned:
surface_form: crest
instance_of: Mountain
coordinates: lat: -63.40636
lon: -56.99204
surface_form: skidmore
instance_of: Mountain
coordinates: lat: -80.3
lon: -28.9333
Named by US-ACAN for Donald D. Skidmore, ionospheric scientist at Ellsworth Station, winter 1957. Vigen Cliffs. Cliffs rising to about high to the east of Gabbro Crest. Named by US-ACAN in 1979 for Oscar C. Vigen, Budget and Planning Officer, Division of Polar Programs, National Science Foundation, 1968–85. Gabbro Crest.

Geographic entities mentioned:
surface_form: crest
instance_of: Mountain
coordinates: lat: -63.40636
lon: -56.99204
Cliffs rising to about high to the east of Gabbro Crest. Named by US-ACAN in 1979 for Oscar C. Vigen, Budget and Planning Officer, Division of Polar Programs, National Science Foundation, 1968–85. Gabbro Crest. The crest about high of the mountain spur between Sheriff Cliffs and Vigen Cliffs on the southeast edge of Saratoga Table. So named in 1979 by US-ACAN, at the suggestion of Arthur B.

Geographic entities mentioned:
surface_form: crest
instance_of: Mountain
coordinates: lat: -63.40636
lon: -56.99204
So named in 1979 by US-ACAN, at the suggestion of Arthur B. Ford, USGS geologist, from the dominant rock type of the Forrestal Range. Sheriff Cliffs. Cliffs rising to about high to the west of Gabbro Crest. Named by US-ACAN in 1979 after Steven D. Sheriff, geologist, Western Washington State University, Bellingham, WA, who worked in this area, 1978–79. Fierle Peak.

Geographic entities mentioned:
surface_form: crest
instance_of: Mountain
coordinates: lat: -63.40636
lon: -56.99204
Saratoga Table. The Saratoga Table () is a high, flat, snow-covered plateau, long and wide, standing just south of Kent Gap and Lexington Table in the southern Forrestal Range, Pensacola Mountains, Antarctica. Discovery and name.

Geographic entities mentioned:
surface_form: discovery
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: discovery
instance_of: Body of water
coordinates: lat: -64.5167
lon: -63.0167
Vigen, Budget and Planning Officer, Division of Polar Programs, National Science Foundation, 1968–85. Gabbro Crest. The crest about high of the mountain spur between Sheriff Cliffs and Vigen Cliffs on the southeast edge of Saratoga Table. So named in 1979 by US-ACAN, at the suggestion of Arthur B. Ford, USGS geologist, from the dominant rock type of the Forrestal Range. Sheriff Cliffs.

Geographic entities mentioned:
surface_form: arthur
instance_of: Mountain
coordinates: lat: -67.65
lon: 49.86667
Magnetite Bluff. A bluff northeast of Mount Stephens on the west side of Saratoga Table. Named by US-ACAN, 1979, at the suggestion of Arthur B. Ford and following USGS geological work in the area, from the extensive occurrences of magnetite in the gabbro of this area which cause large magnetic anomalies over the Forrestal Range. Mathis Spur.

Geographic entities mentioned:
surface_form: arthur
instance_of: Mountain
coordinates: lat: -67.65
lon: 49.86667
Named by US-ACAN for Melvin Mathis, hospital corpsman at Ellsworth Station, winter 1957. Burmester Dome. An ice-capped dome rising to high in west-central Saratoga Table. At the suggestion of USGS party leader Arthur B. Ford, named by US-ACAN after Russell F. Burmester, geologist, Western Washington State University, Bellingham, WA, who worked in the Forrestal Range, 1978–79. Huie Cliffs.

Geographic entities mentioned:
surface_form: arthur
instance_of: Mountain
coordinates: lat: -67.65
lon: 49.86667
Saratoga Table. The Saratoga Table () is a high, flat, snow-covered plateau, long and wide, standing just south of Kent Gap and Lexington Table in the southern Forrestal Range, Pensacola Mountains, Antarctica. Discovery and name.

Geographic entities mentioned:
surface_form: saratoga table
instance_of: Mountain
coordinates: lat: -83.34517
lon: -50.59592
Discovery and name. The Saratoga Table was discovered and photographed on January 13, 1956 on a transcontinental nonstop flight by personnel of United States Navy Operation Deep Freeze I from McMurdo Sound to the vicinity of the Weddell Sea and return.

Geographic entities mentioned:
surface_form: saratoga table
instance_of: Mountain
coordinates: lat: -83.34517
lon: -50.59592
Named by US-ACAN for Kenneth K. Kent, electronics technician at Ellsworth Station, winter 1957. Sorna Bluff. A prominent rock bluff on the north side of Saratoga Table, overlooking the head of May Valley. Named by US-ACAN for Lieutenant Commander Ronald E. Sorna, United States Navy, pilot on photographic flights in the Pensacola Mountains. Mount Hummer.

Geographic entities mentioned:
surface_form: saratoga table
instance_of: Mountain
coordinates: lat: -83.34517
lon: -50.59592
Named by US-ACAN for Lieutenant Commander Ronald E. Sorna, United States Navy, pilot on photographic flights in the Pensacola Mountains. Mount Hummer. A snow-covered, bluff-type mountain on the southwest side of the head of Chambers Glacier, northeast Saratoga Table. Named by US-ACAN in 1979 after Doctor Michael G.

Geographic entities mentioned:
surface_form: saratoga table
instance_of: Mountain
coordinates: lat: -83.34517
lon: -50.59592
Hummer, M.D., Oklahoma Medical Research Foundation, a researcher in biomedicine and the physician at South Pole Station, winter party 1975. Mount Hook. A mountainous snow-covered projection from the east side of Saratoga Table, southeast of Sorna Bluff. Named by US-ACAN in 1979 after Lieutenant Richard M. Hook, United States Navy, Medical Officer at South Pole Station, winter party 1969.

Geographic entities mentioned:
surface_form: saratoga table
instance_of: Mountain
coordinates: lat: -83.34517
lon: -50.59592
Named by US-ACAN in 1979 after Lieutenant Richard M. Hook, United States Navy, Medical Officer at South Pole Station, winter party 1969. Ronald Rock. A prominent rock, high, along the cliff next north of Skidmore Cliff, located east of Saratoga Table. Named by US-ACAN for Ronald D. Brown, aviation structural mechanic at Ellsworth Station, winter 1957. Skidmore Cliff.

Geographic entities mentioned:
surface_form: saratoga table
instance_of: Mountain
coordinates: lat: -83.34517
lon: -50.59592
surface_form: skidmore
instance_of: Mountain
coordinates: lat: -80.3
lon: -28.9333
Named by US-ACAN for Ronald D. Brown, aviation structural mechanic at Ellsworth Station, winter 1957. Skidmore Cliff. An irregular east-facing cliff, long, located at the extremity of a spur trending eastward from Saratoga Table. Named by US-ACAN for Donald D. Skidmore, ionospheric scientist at Ellsworth Station, winter 1957. Vigen Cliffs. Cliffs rising to about high to the east of Gabbro Crest.

Geographic entities mentioned:
surface_form: saratoga table
instance_of: Mountain
coordinates: lat: -83.34517
lon: -50.59592
Vigen, Budget and Planning Officer, Division of Polar Programs, National Science Foundation, 1968–85. Gabbro Crest. The crest about high of the mountain spur between Sheriff Cliffs and Vigen Cliffs on the southeast edge of Saratoga Table. So named in 1979 by US-ACAN, at the suggestion of Arthur B. Ford, USGS geologist, from the dominant rock type of the Forrestal Range. Sheriff Cliffs.

Geographic entities mentioned:
surface_form: saratoga table
instance_of: Mountain
coordinates: lat: -83.34517
lon: -50.59592
Named by US-ACAN in 1979 after Steven D. Sheriff, geologist, Western Washington State University, Bellingham, WA, who worked in this area, 1978–79. Fierle Peak. A sharp peak, high, standing east-southeast of Dyrdal Peak at the south extremity of Saratoga Table. Named by US-ACAN for Gerard R. Fierle, meteorologist at Ellsworth Station, winter 1957. Dyrdal Peak.

Geographic entities mentioned:
surface_form: saratoga table
instance_of: Mountain
coordinates: lat: -83.34517
lon: -50.59592
Named by US-ACAN for Gerard R. Fierle, meteorologist at Ellsworth Station, winter 1957. Dyrdal Peak. A peak, high, standing at the southwest extremity of Saratoga Table, west-northwest of Fierle Peak. Named by US-ACAN for Frederick F. Dyrdal, aviation structural mechanic at Ellsworth Station, winter 1957. Mount Stephens. A prominent mountain, high, surmounting the west extremity of Saratoga Table.

Geographic entities mentioned:
surface_form: saratoga table
instance_of: Mountain
coordinates: lat: -83.34517
lon: -50.59592
Named by US-ACAN for Frederick F. Dyrdal, aviation structural mechanic at Ellsworth Station, winter 1957. Mount Stephens. A prominent mountain, high, surmounting the west extremity of Saratoga Table. Mapped by USGS from surveys and United States Navy air photos, 1956–66. Named by US-ACAN for Lieutenant Commander H.E.

Geographic entities mentioned:
surface_form: saratoga table
instance_of: Mountain
coordinates: lat: -83.34517
lon: -50.59592
Named by US-ACAN for Lieutenant Commander H.E. Stephens, United States Navy, leader of the unit from Mobile Construction Battalion One which constructed Ellsworth Station in January-February, 1957. Magnetite Bluff. A bluff northeast of Mount Stephens on the west side of Saratoga Table. Named by US-ACAN, 1979, at the suggestion of Arthur B.

Geographic entities mentioned:
surface_form: saratoga table
instance_of: Mountain
coordinates: lat: -83.34517
lon: -50.59592
Ford and following USGS geological work in the area, from the extensive occurrences of magnetite in the gabbro of this area which cause large magnetic anomalies over the Forrestal Range. Mathis Spur. A rock spur along the west side of Saratoga Table, north of Mount Stephens. Named by US-ACAN for Melvin Mathis, hospital corpsman at Ellsworth Station, winter 1957. Burmester Dome.

Geographic entities mentioned:
surface_form: saratoga table
instance_of: Mountain
coordinates: lat: -83.34517
lon: -50.59592
Mathis Spur. A rock spur along the west side of Saratoga Table, north of Mount Stephens. Named by US-ACAN for Melvin Mathis, hospital corpsman at Ellsworth Station, winter 1957. Burmester Dome. An ice-capped dome rising to high in west-central Saratoga Table. At the suggestion of USGS party leader Arthur B. Ford, named by US-ACAN after Russell F.

Geographic entities mentioned:
surface_form: saratoga table
instance_of: Mountain
coordinates: lat: -83.34517
lon: -50.59592