Sarmila/GeoWiki-Features huggingface dataset:
Toqui Hill. Toqui Hill is the 82 m summit of the small (2.6 km by 1.6 km) ice-free promontory forming the north extremity of Ioannes Paulus II Peninsula, western Livingston Island in the South Shetland Islands, Antarctica and ending up in Cape Shirreff. It surmounts Mansa Cove to the northeast, Yamana Beach to the west and Shirreff Cove to the west and southwest.

Geographic entities mentioned:
surface_form: small
instance_of: Mountain
coordinates: lat: -70.5
lon: 64.7
surface_form: toqui hill
instance_of: Mountain
coordinates: lat: -62.4678
lon: -60.7915
surface_form: paulus
instance_of: Mountain
coordinates: lat: -72.6167
lon: 31
Toqui Hill. Toqui Hill is the 82 m summit of the small (2.6 km by 1.6 km) ice-free promontory forming the north extremity of Ioannes Paulus II Peninsula, western Livingston Island in the South Shetland Islands, Antarctica and ending up in Cape Shirreff. It surmounts Mansa Cove to the northeast, Yamana Beach to the west and Shirreff Cove to the west and southwest.

Geographic entities mentioned:
surface_form: toqui hill
instance_of: Mountain
coordinates: lat: -62.4678
lon: -60.7915
History. &quot;Ya Po Ah&quot; means &quot;very high place&quot; in the language of the Kalapuya Indians who inhabited the Willamette Valley prior to the arrival of the Euro-American settlers. Ya Po Ah was the name used by the tribe for what is now called Skinner Butte, in honor of Eugene Franklin Skinner, the founder of Eugene City.

Geographic entities mentioned:
surface_form: Willamette Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.9
lon: -123.1
History. &quot;Ya Po Ah&quot; means &quot;very high place&quot; in the language of the Kalapuya Indians who inhabited the Willamette Valley prior to the arrival of the Euro-American settlers. Ya Po Ah was the name used by the tribe for what is now called Skinner Butte, in honor of Eugene Franklin Skinner, the founder of Eugene City.

Geographic entities mentioned:
surface_form: Skinner Butte
instance_of: Landform
countries: United States
coordinates: lat: 44.0586
lon: -123.093
Gößnitzkopf. Gößnitzkopf is a mountain in the Schober Group of the Hohe Tauern range. It is located in Austria, along the border of East Tyrol and Carinthia. The elevation at its peak is. The nearest municipalities are Nußdorf-Debant, Tyrol to the west and Heiligenblut, Carinthia to the east.

Geographic entities mentioned:
surface_form: gößnitzkopf
instance_of: Mountain
countries: Austria
coordinates: lat: 46.967183
lon: 12.743782
Casablanca (volcano). Casablanca () is a Holocene stratovolcano in the Andes of Los Lagos Region, Chile. It is located about 90 km east of the city of Osorno and host on its slopes the Antillanca ski resort. The complex erupted lavas with composition between basalt and andesite and has no recorded historical eruptions. Several scoria cones formed after the last ice age.

Geographic entities mentioned:
surface_form: casablanca
instance_of: Mountain
countries: Chile
coordinates: lat: -40.77138889
lon: -72
Casablanca (volcano). Casablanca () is a Holocene stratovolcano in the Andes of Los Lagos Region, Chile. It is located about 90 km east of the city of Osorno and host on its slopes the Antillanca ski resort. The complex erupted lavas with composition between basalt and andesite and has no recorded historical eruptions. Several scoria cones formed after the last ice age.

Geographic entities mentioned:
surface_form: osorno
instance_of: Mountain
countries: Chile
coordinates: lat: -41.1
lon: -72.493055555556
Monte Fasce. Monte Fasce is a mountain in Liguria, northern Italy, part of the Ligurian Apennines. It is located in the province of Genoa. It lies at an altitude of 834 metres. Nature conservation. The mountain and its surrounding area are included in a SIC &quot;(Site of Community Importance)&quot; called &quot;Monte Fasce&quot; (code:IT1331718).

Geographic entities mentioned:
surface_form: monte fasce
instance_of: Mountain
countries: Italy
coordinates: lat: 44.409444444444
lon: 9.0344444444444
Overton County straddles the Eastern Highland Rim, and generally consists of low, rolling hills divided by narrow creek valleys. The backwaters of Dale Hollow Lake, namely the Mitchell Creek and Big Eagle Creek sections, spill over into the northern part of the county. The county is located on the Cumberland Plateau. 2020 census.

Geographic entities mentioned:
surface_form: Cumberland Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 36
lon: -85
Balmoral, British Columbia. Balmoral is an unincorporated settlement in the Shuswap Country region of the Southern Interior of British Columbia, Canada. It is located to the south of Blind Bay on Shuswap Lake and is administered by the Columbia-Shuswap Regional District.

Geographic entities mentioned:
surface_form: Shuswap Lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.000693
lon: -119.01263
This had a 'salutary effect' in the political atmosphere in the state witnessing its first 'free and fair' election. The revival of the National Conference was greeted with great enthusiasm in the Kashmir Valley. In the words of Kashmiri, &quot;the entire valley was red with N. C. flags. Every house and every market stood decorated with bunting.&quot;
Results.

Geographic entities mentioned:
surface_form: Kashmir Valley
instance_of: Valley
countries: India
coordinates: lat: 34.0333
lon: 74.6667
The National Conference won the majority in the Assembly with 47 of the 76 seats. Whereas it won 40 of the 42 seats in the Kashmir Valley, it was able to win only 7 seats out of 32 in the Jammu province. The Indian National Congress (former National Conference, which had been in power since the State's accession) was reduced to third place, winning 11 seats in Jammu and none in the Valley.

Geographic entities mentioned:
surface_form: Kashmir Valley
instance_of: Valley
countries: India
coordinates: lat: 34.0333
lon: 74.6667
Lac de la Cavayère. Lac de la Cavayère is an artificial lake in the Occitanie &quot;région&quot; of France, close to the medieval town of Carcassonne. The lake, also known as &quot;Carcassonne Plage&quot; (in English, &quot;Carcassonne Beach&quot;), was created by the building of a 23 metre high dam in 1988 after severe forest fires affected the area in 1985.

Geographic entities mentioned:
surface_form: lac de la cavayère
instance_of: Lake
countries: France
coordinates: lat: 43.185277777778
lon: 2.4194444444444
surface_form: cavayère
instance_of: Lake
countries: France
coordinates: lat: 43.185277777778
lon: 2.4194444444444
The headquarters of Southwest Airlines are located at 2702 Love Field Drive, adjacent to the airport. Several other large manufacturing plants are in the neighborhood. Geography. The only body of water within Love Field is Bachman Lake. It lies between Northwest Highway and Dallas Love Field. The Trinity River has several runoffs. Public schools.

Geographic entities mentioned:
surface_form: Bachman Lake
instance_of: Lake
countries: United States
coordinates: lat: 32.848888888889
lon: -96.871111111111
The island in Loch Morar known as Eilean Bàn was briefly the location first of a Mass stone and then of an illegal and clandestine Catholic minor seminary founded by Bishop James Gordon, until the Jacobite rising of 1715 forced its closure and eventual reopening at Scalan in Glenlivet. Even long afterwards, Eilean Bàn remained a secret chapel and library for Bishop Gordon's successors. Legacy.

Geographic entities mentioned:
surface_form: Loch Morar
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.95
lon: -5.6722222222222
surface_form: Glenlivet
instance_of: Valley
countries: United Kingdom
coordinates: lat: 57.349166666667
lon: -3.3319444444444
At the Christian pilgrimage shrine to 'Our Lady of the Highlands', within the grounds of Immaculate Conception Roman Catholic Church near Loch Ness, a new outdoor Mass stone was consecrated by Bishop Hugh Gilbert of the Roman Catholic Diocese of Aberdeen in March 2017. Wales. The ruins of an Iron Age hill fort and a mediæval chapel, dedicated to St.

Geographic entities mentioned:
surface_form: Loch Ness
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.3
lon: -4.45
According to a book on the history and folklore of Mass rocks by Tony Nugent, a Catholic priest named Fr. Mac Aidghalle was murdered while saying Mass at a mass rock still known in Ulster Irish as &quot;Cloch na hAltorach&quot; that stands atop Slieve Gullion, County Armagh. The perpetrators were a company of redcoats under the command of a priest hunter named Turner.

Geographic entities mentioned:
surface_form: Slieve Gullion
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.133333333333
lon: -6.4333333333333
In addition, invests in the North Indian Ocean cyclone basin are also labelled by the JTWC, and are suffixed with &quot;A&quot; if they form in the Arabian Sea and with &quot;B&quot; if they form in the Bay of Bengal.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Sailing. A South Korean sailor secured a quota place in the following events through the 2024 Semaine Olympique Française (Last Chance Regatta) in Hyères, France. Shooting. South Korean shooters achieved quota places for the following events based on their results at the 2022 and 2023 ISSF World Championships, 2023 and 2024 Asian Championships, and 2024 ISSF World Olympic Qualification Tournament.

Geographic entities mentioned:
surface_form: Hyères
instance_of: Mountain
countries: France
coordinates: lat: 43.118888888889
lon: 6.1286111111111
Hindscarth. Hindscarth is a mountain between the valleys of Buttermere and Newlands, in the north-western part of the English Lake District. The fell's name is derived from two words from the Old Norse language, &quot;Hind&quot; and &quot;Skarth&quot;, and means the pass used by the red deer. Topography.

Geographic entities mentioned:
surface_form: Buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
surface_form: Newlands
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.573011111111
lon: -3.1848694444444
surface_form: hindscarth
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.537661111111
lon: -3.2147611111111
Two roads cross from east to west, dividing the fells into three convenient groups. Hindscarth stands in the southern sector. The principal ridge in this group of fells runs east from Buttermere, climbing over Robinson, Hindscarth and Dale Head. It then turns north, descending gradually toward Derwentwater, the main tops being High Spy, Maiden Moor and Catbells.

Geographic entities mentioned:
surface_form: Dale Head
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.527
lon: -3.2020805555556
surface_form: dale head
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.527
lon: -3.2020805555556
surface_form: buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
surface_form: robinson
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.54
lon: -3.236
surface_form: hindscarth
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.537661111111
lon: -3.2147611111111
The principal ridge in this group of fells runs east from Buttermere, climbing over Robinson, Hindscarth and Dale Head. It then turns north, descending gradually toward Derwentwater, the main tops being High Spy, Maiden Moor and Catbells. The ridge from Robinson to Dale Head forms the heads of Little Dale and Newlands, bypassing the intervening summit of Hindscarth.

Geographic entities mentioned:
surface_form: Derwentwater
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.583333333333
lon: -3.15
surface_form: High Spy
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.534
lon: -3.185
surface_form: Maiden Moor
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5532
lon: -3.18275
surface_form: catbells
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5686
lon: -3.17083
surface_form: derwentwater
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.583333333333
lon: -3.15
surface_form: high spy
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.534
lon: -3.185
surface_form: maiden moor
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5532
lon: -3.18275
Due to their proximity, Hindscarth and Robinson are often combined into a single walk starting from Newlands. The fell is also part of a longer walk including Catbells, High Spy, Dale Head and along the &quot;Littledale Edge&quot; ridge to Robinson — the Newlands horseshoe. Geology.

Geographic entities mentioned:
surface_form: High Spy
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.534
lon: -3.185
surface_form: Dale Head
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.527
lon: -3.2020805555556
surface_form: catbells
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5686
lon: -3.17083
surface_form: dale head
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.527
lon: -3.2020805555556
surface_form: high spy
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.534
lon: -3.185
surface_form: robinson
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.54
lon: -3.236
Summit. The summit carries an untidy cairn amid some embedded rocks. Elsewhere there are patches of grass and gravel. A hundred yards south is a larger cairn, marked as a Shelter on Ordnance Survey maps. The view north into the Newlands Valley is excellent, backed by Skiddaw. All of the major fell groups with the exception of High Street can be seen.

Geographic entities mentioned:
surface_form: Skiddaw
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.651388888889
lon: -3.1477777777778
surface_form: skiddaw
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.651388888889
lon: -3.1477777777778
Mining. The northern ridge of Hindscarth which falls away to the Newlands valley has at its foot (at Scope End) one of the most famous former mines in the Lake District. The Goldscope mine has been designated as a major national important site by English Heritage who have stated that it should receive priority treatment for its protection and preservation.

Geographic entities mentioned:
surface_form: newlands valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.573011111111
lon: -3.1848694444444
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
It then turns north, descending gradually toward Derwentwater, the main tops being High Spy, Maiden Moor and Catbells. The ridge from Robinson to Dale Head forms the heads of Little Dale and Newlands, bypassing the intervening summit of Hindscarth. This stands off to the north, forming the dividing wall between the two valleys.

Geographic entities mentioned:
surface_form: dale head
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.527
lon: -3.2020805555556
surface_form: hindscarth
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.537661111111
lon: -3.2147611111111
The fell is also part of a longer walk including Catbells, High Spy, Dale Head and along the &quot;Littledale Edge&quot; ridge to Robinson — the Newlands horseshoe. Geology. Hindscarth is an example of the Buttermere Formation, an olistostrome of disrupted, sheared and folded mudstone, siltstone and sandstone. Mining.

Geographic entities mentioned:
surface_form: buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
Summit. The summit carries an untidy cairn amid some embedded rocks. Elsewhere there are patches of grass and gravel. A hundred yards south is a larger cairn, marked as a Shelter on Ordnance Survey maps. The view north into the Newlands Valley is excellent, backed by Skiddaw. All of the major fell groups with the exception of High Street can be seen.

Geographic entities mentioned:
surface_form: high street
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.492
lon: -2.865
The southern face of Hindscarth looks down over Honister Pass. Ascents. A popular ascent starts from a parking area nearby Newlands Church and passes over the Scope End ridge before continuing up crags to the summit. Due to their proximity, Hindscarth and Robinson are often combined into a single walk starting from Newlands.

Geographic entities mentioned:
surface_form: robinson
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.54
lon: -3.236
surface_form: hindscarth
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.537661111111
lon: -3.2147611111111
Hindscarth. Hindscarth is a mountain between the valleys of Buttermere and Newlands, in the north-western part of the English Lake District. The fell's name is derived from two words from the Old Norse language, &quot;Hind&quot; and &quot;Skarth&quot;, and means the pass used by the red deer. Topography.

Geographic entities mentioned:
surface_form: hindscarth
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.537661111111
lon: -3.2147611111111
The ridge from Robinson to Dale Head forms the heads of Little Dale and Newlands, bypassing the intervening summit of Hindscarth. This stands off to the north, forming the dividing wall between the two valleys. The long north-west ridge steps down over several tiers of crag to the confluence of its bordering streams. The southern face of Hindscarth looks down over Honister Pass. Ascents.

Geographic entities mentioned:
surface_form: hindscarth
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.537661111111
lon: -3.2147611111111
Zyuratkul. Zyuratkul (;) is a freshwater lake in Satkinsky District, Chelyabinsk Oblast, Russia. The name &quot;Zyuratkul&quot; comes from the Bashkir &quot;yöräk/kul&quot; (йөрәк/күл), meaning &quot;heart/lake&quot;. In 1993 the Zyuratkul National Park, a protected area, was established in the lake and its surroundings. Geography.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: zyuratkul
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 54.916666666667
lon: 59.2
Zyuratkul. Zyuratkul (;) is a freshwater lake in Satkinsky District, Chelyabinsk Oblast, Russia. The name &quot;Zyuratkul&quot; comes from the Bashkir &quot;yöräk/kul&quot; (йөрәк/күл), meaning &quot;heart/lake&quot;. In 1993 the Zyuratkul National Park, a protected area, was established in the lake and its surroundings. Geography.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: zyuratkul
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 54.916666666667
lon: 59.2
surface_form: zyuratkul
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 54.916666666667
lon: 59.2
Zyuratkul. Zyuratkul (;) is a freshwater lake in Satkinsky District, Chelyabinsk Oblast, Russia. The name &quot;Zyuratkul&quot; comes from the Bashkir &quot;yöräk/kul&quot; (йөрәк/күл), meaning &quot;heart/lake&quot;. In 1993 the Zyuratkul National Park, a protected area, was established in the lake and its surroundings. Geography.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
It is located about to the south of the small mountain range named after it. Its southern shore stretches at the feet of the northern slopes of the larger Nurgush range. Previously, in its natural state, the lake was smaller and surrounded by swamps. After WWII a dam was built and the new reservoir doubled the surface area of the ancient lake.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
Its southern shore stretches at the feet of the northern slopes of the larger Nurgush range. Previously, in its natural state, the lake was smaller and surrounded by swamps. After WWII a dam was built and the new reservoir doubled the surface area of the ancient lake. The water of Zyuratkul is not as clear as is normal in high-altitude lakes.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
Previously, in its natural state, the lake was smaller and surrounded by swamps. After WWII a dam was built and the new reservoir doubled the surface area of the ancient lake. The water of Zyuratkul is not as clear as is normal in high-altitude lakes. The reason is that the inflowing watercourses originate in swamps. The Bolshaya Satka, a left hand tributary of the Ay, is the outflow of the lake.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
Zyuratkul. Zyuratkul (;) is a freshwater lake in Satkinsky District, Chelyabinsk Oblast, Russia. The name &quot;Zyuratkul&quot; comes from the Bashkir &quot;yöräk/kul&quot; (йөрәк/күл), meaning &quot;heart/lake&quot;. In 1993 the Zyuratkul National Park, a protected area, was established in the lake and its surroundings. Geography.

Geographic entities mentioned:
surface_form: zyuratkul
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 54.916666666667
lon: 59.2
Geography. The Klastline River originates in a valley on the Klastline Plateau between Tsazia Mountain and Mount Poelzer. From its source the Klastline River flows about north to the southern base of an unnamed circular, flat-topped mountain. It then flows generally west for about to the northeastern side of the Big Raven Plateau.

Geographic entities mentioned:
surface_form: Klastline Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.95
lon: -130.083
Geography. The Klastline River originates in a valley on the Klastline Plateau between Tsazia Mountain and Mount Poelzer. From its source the Klastline River flows about north to the southern base of an unnamed circular, flat-topped mountain. It then flows generally west for about to the northeastern side of the Big Raven Plateau.

Geographic entities mentioned:
surface_form: Big Raven Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.7167
lon: -130.75
It then flows generally west for about to the northeastern side of the Big Raven Plateau. From there, the Klastline River flows generally northwest for about along the northern end of the Big Raven Plateau through the Tahltan Highland to the western end of the Grand Canyon of the Stikine where it joins the Stikine River. The Klastline River contains six named right tributaries.

Geographic entities mentioned:
surface_form: Grand Canyon of the Stikine
instance_of: Valley
countries: Canada
coordinates: lat: 58.08222222222222
lon: -130.735
Only three left tributaries of the Klastline River are named. The first one is Tsazia Creek which flows north into the Klastline River. Kakiddi Creek, the second named left tributary, flows north into the Klastline River. The third named left tributary is Buckley Creek which flows northeast into the Klastline River east of Telegraph Creek.

Geographic entities mentioned:
surface_form: Kakiddi Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.872778
lon: -130.425556
Geology. The Klastline River has been repeatedly blocked by lava flows from the adjacent Mount Edziza volcanic complex. In the Pleistocene, massive basalt flows from at least three eruptive centres on the northern side of the volcanic complex entered the narrow valley of the Klastline River from Kakiddi Valley, temporarily blocking it to form a large shallow lake upstream.

Geographic entities mentioned:
surface_form: Mount Edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
The Klastline River was forced to establish a new route along the northern valley wall where it still flows to this day. Williams Cone produced a more than lava flow into Klastline Valley where its distal lobe formed a temporary dam across the Klastline River. All three cinder cones and associated lava flows are assigned to the Big Raven Formation.

Geographic entities mentioned:
surface_form: Williams Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.78
lon: -130.599
The biggest city in the region is Lahti. Päijät-Häme boasts a landscape shaped by two key features. Finland's second-largest, Lake Päijänne, dominates the region, offering a vast freshwater expanse and a vital transportation route. The Häme Ridge, a glacial remnant, adds a touch of elevation and scenic variation. Beyond these, Päijät-Häme features extensive coniferous forests.

Geographic entities mentioned:
surface_form: Lake Päijänne
instance_of: Lake
countries: Finland
coordinates: lat: 61.583333333333
lon: 25.5
Landscape architect Jens Jensen designed the estate's grounds, which he also used as a studio; these became the modern park after the home's removal. The park includes a beach on Lake Michigan, the North Shore Sanitary District Tower (closed), an empty stone pool and artificial stream, and a walking path that leads to a bridge over a ravine.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Pinehouse Lake Airport. Pinehouse Lake Airport is located adjacent to Pinehouse Lake and serves Pinehouse, Saskatchewan, Canada.

Geographic entities mentioned:
surface_form: Pinehouse Lake
instance_of: Lake
countries: Canada
coordinates: lat: 55.5333
lon: -106.583
Geography. According to the U.S. Census Bureau, the township has a total area of, of which is land and (2.32%) is water. The Au Sable River runs through the northeast boundary and has its river mouth at Lake Huron within the township. Demographics. As of the census of 2000, there were 2,230 people, 956 households, and 636 families residing in the township. The population density was.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
For instance, he had a total of 60 wives. While keeping his administration small, mainly composed of a council, it was his personality which built a coalition with the neighboring leaders. His domain extended from Lake Buluan to Sarangani Bay.

Geographic entities mentioned:
surface_form: Lake Buluan
instance_of: Lake
countries: Philippines
coordinates: lat: 6.6405555555556
lon: 124.825
This prompted Federico Roldan, Governor of Cotabato, to attack Buayan. In 1886, two Spanish corps under General Serina razed Bakat to make way for the construction of a new fort and a railway from Iligan to Lake Lanao. The project was abandoned as Uto's forces harassed the Spaniards, gathering the metal used in construction to produce krises.

Geographic entities mentioned:
surface_form: Lake Lanao
instance_of: Lake
countries: Philippines
coordinates: lat: 7.88
lon: 124.2525
History. Basin Recreation was established in 1986 by the Summit County Board of Commissioners as an agency to provide public recreational services to the Snyderville Basin. In the early 1990s, the Snyderville Basin area was growing rapidly, with Basin Recreation having few resources to deal with the increased demand.

Geographic entities mentioned:
surface_form: Snyderville Basin
instance_of: Valley
countries: United States
coordinates: lat: 40.7261
lon: -111.509
Frick was appointed prime minister in 1945 following the resignation of Josef Hoop. His first years in office included domestic challenges, particularly that of pressure to repatriate the soldiers of the First Russian National Army and to cede the Ellhorn mountain to Switzerland.

Geographic entities mentioned:
surface_form: Ellhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.05243
lon: 9.4788
He also attempted to join the European Free Trade Association but was unsuccessful, instead being represented by Switzerland. In 1949, he oversaw Liechtenstein ceding the Ellhorn mountain to Switzerland as a result of Swiss demands and threats to, among other things, cease end the customs union between the two countries.

Geographic entities mentioned:
surface_form: Ellhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.05243
lon: 9.4788
It contains eleven major independent summits, each over in height. It is named after Mont Blanc (), the highest point in western Europe and the European Union. Because of its considerable overall altitude, a large proportion of the massif is covered by glaciers, which include the Mer de Glace and the Miage Glacierthe longest glaciers in France and Italy, respectively.

Geographic entities mentioned:
surface_form: Mont Blanc
instance_of: Mountain
countries: France
Italy
coordinates: lat: 45.83277777777778
lon: 6.865
Its watercourse, la Dranse de Ferret, flows northwards to join the Rhône at Martigny. The west side of the northern end of the massif is drained by the Trient, also joining the Rhône near Martigny. The borders of all three countries converge at a tripoint near the summit of Mont Dolent at an altitude of.

Geographic entities mentioned:
surface_form: Mont Dolent
instance_of: Mountain
countries: Switzerland
Italy
France
coordinates: lat: 45.9225
lon: 7.0461111111111
From here the French – Italian border runs southwestwards along a ridge of high summits on the southern side of the massif, many of which are over in height, including the Grandes Jorasses, Rochefort Ridge, Dent du Géant, Mont Maudit, Mont Blanc and its western satellite, the Aiguille de Bionnassay.

Geographic entities mentioned:
surface_form: Grandes Jorasses
instance_of: Mountain
countries: Italy
France
coordinates: lat: 45.866666666667
lon: 6.9833333333333
surface_form: Rochefort Ridge
instance_of: Mountain
countries: France
Italy
coordinates: lat: 45.86194444
lon: 6.95944444
surface_form: Dent du Géant
instance_of: Mountain
countries: France
Italy
coordinates: lat: 45.861944444444
lon: 6.9516666666667
surface_form: Mont Maudit
instance_of: Mountain
countries: Italy
France
coordinates: lat: 45.847777777778
lon: 6.8758333333333
surface_form: Mont Blanc
instance_of: Mountain
countries: France
Italy
coordinates: lat: 45.83277777777778
lon: 6.865
surface_form: Aiguille de Bionnassay
instance_of: Mountain
countries: France
Italy
coordinates: lat: 45.835833333333
lon: 6.8180555555556
From here the border turns southwards over the Dômes de Miage and Aiguille de Tré la Tête before dropping down to the Col de la Seigne.

Geographic entities mentioned:
surface_form: Dômes de Miage
instance_of: Mountain
countries: France
coordinates: lat: 45.8158
lon: 6.8
surface_form: Aiguille de Tré la Tête
instance_of: Mountain
countries: France
Italy
coordinates: lat: 45.79476
lon: 6.8141
North of Mont Dolent the border between France and Switzerland meanders roughly north-northwestwards along a ridge-line of slightly lower peaks, including the Aiguille d'Argentière, the Aiguille du Chardonnet and the Aiguille du Tour, before dropping down to the Col de Balme. The Swiss – Italian border runs southwest from Mont Dolent, down to the twin passes of Col Ferret.

Geographic entities mentioned:
surface_form: Aiguille d'Argentière
instance_of: Mountain
countries: Switzerland
France
coordinates: lat: 45.959761111111
lon: 7.0203194444444
surface_form: Aiguille du Chardonnet
instance_of: Mountain
countries: France
coordinates: lat: 45.968986111111
lon: 7.0014277777778
surface_form: Aiguille du Tour
instance_of: Mountain
countries: Switzerland
France
coordinates: lat: 45.994416666667
lon: 7.0098333333333
In 2014, a group of climbers found a body on the Glacier du Talèfre, close to the Couvercle Hut. It was identified as that of a young Chamonix guide who had been caught in a winter storm during a solo ascent of the Nant Blanc face of the Aiguille Verte in 1982 and was assumed to have fallen into a crevasse. In 2013, a box of valuable gemstones was found by a climber on the Bossons Glacier.

Geographic entities mentioned:
surface_form: Aiguille Verte
instance_of: Mountain
countries: France
coordinates: lat: 45.934722222222
lon: 6.97
The central granites make up Mont Blanc, the steep slopes of the Drus, the Grandes Jorasses and the Dent du Géant, and at the highest points are topped by schists, which are visible in places such as Grands Montets and near Mont Blanc's summit. The granite mountains around Chamonix have been eroded into steep needle-shaped peaks (known as).

Geographic entities mentioned:
surface_form: Drus
instance_of: Mountain
countries: France
coordinates: lat: 45.932777777778
lon: 6.9563888888889
Some farmers in the valley of Chamonix joined their counterparts from the neighbouring valleys of Maurienne, Beaufortain and Tarentaise and crossed the Alps into southern Germany, Austria and northern Italy to sell their products and bring back goods for sale in local markets. Tourist beginnings.

Geographic entities mentioned:
surface_form: Maurienne
instance_of: Valley
countries: France
coordinates: lat: 45.2
lon: 6.6666666666667
surface_form: Beaufortain
instance_of: Valley
countries: France
coordinates: lat: 45.73333333
lon: 6.55
The Aiguille du Midi Cable Car in Chamonix attracts 500,000 people each year and gives views over much of the massif, and up towards Mont Blanc itself. From Chamonix it rises to the summit of the Aiguille du Midi at, and holds the world record for the highest vertical ascent of any cable car ().

Geographic entities mentioned:
surface_form: Aiguille du Midi
instance_of: Mountain
countries: France
coordinates: lat: 45.878888888889
lon: 6.8875
In 1820, an ill-fated expedition led by Dr Hamel included pigeons intended for release at varying altitudes to measure the impact of reduced air density on their ability to fly. In 1890, Joseph Vallot built a small meteorological observatory at approximately between the Dôme du Goûter and Mont Blanc's summit from where numerous measurements and scientific experiments were conducted.

Geographic entities mentioned:
surface_form: Dôme du Goûter
instance_of: Mountain
countries: France
Italy
coordinates: lat: 45.841666666667
lon: 6.8433333333333
Trains running on the line are called &quot;Mont Blanc Express&quot;. Elsewhere in the massif, the Montenvers Railway connects Chamonix to Montenvers near the foot of the Mer de Glace, whilst the Téléphérique du Lognan connects Argentière with Aiguille des Grands Montets, where Les Grand Montets is an important winter skiing area in the region.

Geographic entities mentioned:
surface_form: Aiguille des Grands Montets
instance_of: Mountain
countries: France
coordinates: lat: 45.948280555556
lon: 6.9605222222222
At, the summit station also provides relatively easy access for climbers to the northeastern peaks of the range, including short introductory rock scrambles and a simple ice-face route on the NW face of the Petite Aiguille Verte. The Mont Blanc Tramway takes tourists and hikers from Saint-Gervais to the Nid d'Aigle, near the Glacier de Bionnassay.

Geographic entities mentioned:
surface_form: Petite Aiguille Verte
instance_of: Mountain
countries: France
coordinates: lat: 45.94777778
lon: 6.95861111
Summit. The main summit bears a number of rock tors, protruding sharply from the heathery plateau. King's How has a steep sided domed top. Both bear cairns. The view from the top of the fell takes in Derwentwater with Skiddaw in the background, while Borrowdale and the high fells round its head show well in the opposite direction.

Geographic entities mentioned:
surface_form: Skiddaw
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.651388888889
lon: -3.1477777777778
surface_form: skiddaw
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.651388888889
lon: -3.1477777777778
surface_form: derwentwater
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.583333333333
lon: -3.15
surface_form: borrowdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.42
lon: -2.665
The fell has a summit plateau which consist of many heather-covered hummocks, drystone walls and clumps of trees. Well-known Lake District writer Alfred Wainwright credits Grange Fell as a single fell with three main summits, namely Brund Fell, King's How and Ether Knott. The lesser known Ether Knott is now identified as the highest point at a height of and is less frequently visited by walkers.

Geographic entities mentioned:
surface_form: knott
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.686211111111
lon: -3.0935388888889
surface_form: grange fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5444
lon: -3.13253
Well-known Lake District writer Alfred Wainwright credits Grange Fell as a single fell with three main summits, namely Brund Fell, King's How and Ether Knott. The lesser known Ether Knott is now identified as the highest point at a height of and is less frequently visited by walkers. Brund Fell is at while King's How is the best viewpoint and has an altitude of.

Geographic entities mentioned:
surface_form: knott
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.686211111111
lon: -3.0935388888889
Shepherds Crag above the more famous rockface of that name, adjacent to the Lodore Falls and Hotel, and Grange Crags above Grange. Geology. The geology of the fell is complex with outcropping of various members of the Birker Fell Formation (andesite lavas), the Eagle Crag Member (siltstone and sandstone conglomerates), and intrusions of dolerite. Ascents.

Geographic entities mentioned:
surface_form: eagle crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.499
lon: -3.12097
Grange Fell. Grange Fell is a small fell in the English Lake District in the county of Cumbria, situated in the Borrowdale valley overlooking the villages of Grange in Borrowdale and Rosthwaite. Topography. The fell has a summit plateau which consist of many heather-covered hummocks, drystone walls and clumps of trees.

Geographic entities mentioned:
surface_form: borrowdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.42
lon: -2.665
surface_form: borrowdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.42
lon: -2.665
surface_form: grange fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5444
lon: -3.13253
Ascents. Ascents of Grange Fell can be started from Rosthwaite, Grange in Borrowdale or Watendlath. The Rosthwaite to Watendlath bridleway can be utilised to its highest point before striking northerly to the summit of Brund Fell following a high dry stone wall for much of the way.

Geographic entities mentioned:
surface_form: borrowdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.42
lon: -2.665
surface_form: grange fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5444
lon: -3.13253
Grange Fell. Grange Fell is a small fell in the English Lake District in the county of Cumbria, situated in the Borrowdale valley overlooking the villages of Grange in Borrowdale and Rosthwaite. Topography. The fell has a summit plateau which consist of many heather-covered hummocks, drystone walls and clumps of trees.

Geographic entities mentioned:
surface_form: grange fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5444
lon: -3.13253
The climb from Grange goes through the deciduous woodland at the foot of the fell and skirts round Greatend Crag before reaching King's How and is ranked as one of the &quot;loveliest short walks in the Lake District&quot;. The two principal summits of Brund Fell and King's How should both be climbed by any visitor to the fell and they are linked by an undulating path through the hillocks. Summit.

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
Molladavut, Karaçoban. Molladavut is a neighbourhood in the municipality and district of Karaçoban, Erzurum Province in Turkey. Its population is 578 (2022). Geography. Molladavut village is located on the Akdoğan Mountains and is very close to Lake Akdoğan.

Geographic entities mentioned:
surface_form: Lake Akdoğan
instance_of: Lake
countries: Turkey
coordinates: lat: 39.14006
lon: 41.74121
A descendant of the head of the Chichibu clan settled in the area and took the name, likely based on the name used for the place, and founded the Edo clan. Shigetsugu built a fortified residence, probably around the edge of the Musashino Terrace, that would become Edo castle.

Geographic entities mentioned:
surface_form: Musashino Terrace
instance_of: Plateau
countries: Japan
The building is the most architecturally sophisticated park pavilion in the city, and was listed on the National Register of Historic Places in 1980. Description. Green Hill Park is located in eastern Worcester, occupying about of uplands separating the Blackstone River valley from Lake Quinsigamond. Near the center of the park is Green Hill Pond, a artificial body of water.

Geographic entities mentioned:
surface_form: Lake Quinsigamond
instance_of: Lake
countries: United States
coordinates: lat: 42.270833333333
lon: -71.755
In 1976, only 720 Indian Wild ass were there, but due to the efforts it has been increasing steadily to 1,989 in 1983, 2,072 in 1990, 2,839 in 1999, 4,451 in 2014, 6,082 in 2020, and 7,672 in 2024. Of late, it has been spotted right outside Ahmedabad near Nal Sarovar Bird Sanctuary.

Geographic entities mentioned:
surface_form: Nal Sarovar Bird Sanctuary
instance_of: Lake
countries: India
coordinates: lat: 22.792569444444
lon: 72.023111111111
Coal and iron mines in the surrounding hills and mountains fueled the local economy, and by mid-century Danville was an important iron mill town. Many of the rails of the nation's expanding railroad system were made in Danville, an important contribution to a network which grew explosively for decades. By the 1890s there were 7-8 major railroads running into the Wyoming Valley for Anthracite.

Geographic entities mentioned:
surface_form: Wyoming Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.251
lon: -75.906
Djebel Bargou. Jebel Bargou (جبل برقو) is a mountain (Jebel) of Tunisia, which rises to 1266m altitude. Location. Located at information 36°03'36&quot;North, 9° 36'31&quot;East in north-central region of Tunisia, about twenty kilometers southeast of the town of Siliana, it gives its name to the town situated on its northern side, a few kilometers from its peak.

Geographic entities mentioned:
surface_form: جبل برقو
instance_of: Mountain
countries: Tunisia
coordinates: lat: 36.0599
lon: 9.60861
surface_form: jebel bargou
instance_of: Mountain
countries: Tunisia
coordinates: lat: 36.0599
lon: 9.60861
Djebel Bargou. Jebel Bargou (جبل برقو) is a mountain (Jebel) of Tunisia, which rises to 1266m altitude. Location. Located at information 36°03'36&quot;North, 9° 36'31&quot;East in north-central region of Tunisia, about twenty kilometers southeast of the town of Siliana, it gives its name to the town situated on its northern side, a few kilometers from its peak.

Geographic entities mentioned:
surface_form: djebel bargou
instance_of: Mountain
countries: Tunisia
coordinates: lat: 36.0599
lon: 9.60861
Loveringite has also been generally found in areas of medium-grade metamorphism, reported from the Hoggar Mountains of Algeria; the
Hohe Tauern Mountains, Salzburg, Austria; the Koitelainen intrusion of Lappland, Finland; Bourg d’Oisans, Isere, France; Bracco, Liguria, Italy; the Kerguelen Islands; the Khibiny Massif in the Kola Peninsula of Russia; and at Makwiro on the Great Dyke in Zimbabwe.

Geographic entities mentioned:
surface_form: Hoggar Mountains
instance_of: Plateau
countries: Algeria
France
coordinates: lat: 23.288611
lon: 5.534167
Work began soon after his appointment, and by October 1794, the section from Woofferton near Tenbury to Marlbrook near Mamble was open for traffic. The following year saw most of the section from Leominster to Woofferton completed, while beyond Marlbrook the Southnet tunnel was finished and work started on an aqueduct over the River Lugg at Kingsland.

Geographic entities mentioned:
surface_form: River Lugg
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 52.0311
lon: -2.63611
Petersburg University in 1899, he became a &quot;privat-docent&quot; of the Chair of Armenian and Georgian Philology at his alma mater. From 1901 to 1902, he was a visiting scholar at the University of Berlin. In 1902, he accompanied his mentor, Academician Nikolai Marr, to Mount Sinai where they studied medieval Georgian manuscripts (such as the Georgian manuscripts of Saint Paul's letters).

Geographic entities mentioned:
surface_form: Mount Sinai
instance_of: Mountain
countries: Egypt
coordinates: lat: 28.5384
lon: 33.9752
Battleship Mountain. Battleship Mountain (is located in the Teton Range in the U.S. state of Wyoming. The peak is in the Jedediah Smith Wilderness of Caribou-Targhee National Forest and is west of Hurricane Pass.

Geographic entities mentioned:
surface_form: battleship mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.7233
lon: -110.869
Round Pond (Duxbury, Massachusetts). Round Pond is an reservoir in Duxbury, Massachusetts. The reservoir is located northeast of Pine Lake, northwest of Island Creek Pond, and southwest of North Hill Marsh Pond. An inlet provides the inflow for this reservoir from Pine Lake. The reservoir is associated hydro logically with an adjacent cranberry bog operation.

Geographic entities mentioned:
surface_form: Island Creek Pond
instance_of: Lake
countries: United States
coordinates: lat: 42.027777777778
lon: -70.711388888889
surface_form: North Hill Marsh Pond
instance_of: Lake
countries: United States
coordinates: lat: 42.041666666667
lon: -70.708333333333
surface_form: pine lake
instance_of: Lake
countries: United States
coordinates: lat: 43.197222222222
lon: -74.512777777778
surface_form: pine lake
instance_of: Lake
countries: United States
coordinates: lat: 37.736188888889
lon: -122.48882777778
surface_form: pine lake
instance_of: Lake
countries: United States
coordinates: lat: 43.5038
lon: -74.1526
surface_form: pine lake
instance_of: Lake
countries: United States
coordinates: lat: 44.232777777778
lon: -89.1625
surface_form: pine lake
instance_of: Lake
countries: United States
coordinates: lat: 47.5875
lon: -122.044
surface_form: pine lake
instance_of: Lake
countries: United States
coordinates: lat: 42.0319
lon: -70.7219
surface_form: pine lake
instance_of: Lake
countries: United States
coordinates: lat: 42.447222222222
lon: -74.928611111111
surface_form: pine lake
instance_of: Lake
countries: United States
coordinates: lat: 45.248184
lon: -85.075807
surface_form: pine lake
instance_of: Lake
countries: United States
coordinates: lat: 42.590359
lon: -83.34151
surface_form: pine lake
instance_of: Lake
countries: United States
coordinates: lat: 47.024722222222
lon: -94.383055555556
surface_form: pine lake
instance_of: Lake
countries: United States
coordinates: lat: 46.543055555556
lon: -95.778888888889
surface_form: pine lake
instance_of: Lake
countries: United States
coordinates: lat: 43.4206
lon: -75.0918
surface_form: pine lake
instance_of: Lake
countries: United States
coordinates: lat: 47.693611111111
lon: -95.526111111111
surface_form: pine lake
instance_of: Lake
countries: United States
coordinates: lat: 45.2924237
lon: -91.4589716