Sarmila/GeoWiki-Features huggingface dataset:
displayed constant hostility toward the Golaniad protests in Bucharest, which ranged for much of early 1990, and expressed praise for the Mineriad of June 13–15, 1990. During the latter, miners from the Jiu Valley, instigated by some of the officials, entered Bucharest and quashed the opposition's sit-in.

Geographic entities mentioned:
surface_form: Jiu Valley
instance_of: Valley
countries: Romania
coordinates: lat: 43.77805556
lon: 23.81333333
Location and habitat. The mines comprise one of a series of Sites of Special Scientific Interest within the Forest of Dean and Wye Valley (Gloucestershire and Monmouthshire). These sites support (between them) important breeding and hibernation roosts for lesser and greater horseshoe bats. This is of European importance.

Geographic entities mentioned:
surface_form: Wye Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.69255
lon: -2.66283
several years later. Tournaments. The first Pebble Beach Championship for Women was played February 9–12, 1923, with Marion Hollins as champion over Doreen Kavanaugh. Pebble Beach hosted the first California Women's Amateur Championship in 1967 as well as subsequent tournaments until it was moved to Quail Lodge & Golf Club in Carmel Valley in 1987.

Geographic entities mentioned:
surface_form: Carmel Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.4748315
lon: -121.7205075
The descent at the southern end leads into a karst landscape of deep gorges and pitted slopes where water penetrating the rock has carved a series of caves. Location. The massif is bordered in the west by the Dâmbovița River, which separates it from the Iezer–Păpușa Massif. In the north-west, the Bârsa River and the Curmătura Foii gorge separate it from the Făgăraș Mountains.

Geographic entities mentioned:
surface_form: Iezer–Păpușa Massif
instance_of: Mountain
countries: Romania
coordinates: lat: 45.4762
lon: 24.95414
Samarasimha had at least two sons and a daughter. His daughter Lila-devi married the Chaulukya monarch Bhima II. This is attested by the 1206 Kadi inscription of Bhima II. His two sons were Manavasimha and Udayasimha. The elder son Manavasimha was an ancestor of the founders of the Chauhan principalities of Chandravati and Abu. Udayasimha succeeded Samarasimha on the throne of Jalore.

Geographic entities mentioned:
surface_form: Abu
instance_of: Mountain
countries: India
coordinates: lat: 24.5925
lon: 72.708333333333
New York State Route 39 crosses the center of the town. Adjacent towns and areas. On the north, the town borders Lake Erie, and on the northeast, Cattaraugus Creek, which is the boundary of the Cattaraugus Reservation in Erie County. The east town line borders the town of Perrysburg and the portion of the Cattaraugus Reservation in Cattaraugus County.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Mount Stevens (Alaska). Mount Stevens is a mountain located in Matanuska-Susitna Borough, Alaska. Mount Stevens is flanked to the northwest by Mount Hunter, and is about south of Denali. The mountain was named in 2010, after Ted Stevens (1923–2010), who had represented Alaska in the U.S. Senate from 1968 to 2009.

Geographic entities mentioned:
surface_form: Denali
instance_of: Mountain
countries: United States
coordinates: lat: 63.06916666666667
lon: -151.0063888888889
surface_form: mount hunter
instance_of: Mountain
countries: United States
coordinates: lat: 62.9508
lon: -151.089
surface_form: mount stevens
instance_of: Mountain
countries: United States
coordinates: lat: 62.9205
lon: -151.067
Mount Stevens (Alaska). Mount Stevens is a mountain located in Matanuska-Susitna Borough, Alaska. Mount Stevens is flanked to the northwest by Mount Hunter, and is about south of Denali. The mountain was named in 2010, after Ted Stevens (1923–2010), who had represented Alaska in the U.S. Senate from 1968 to 2009.

Geographic entities mentioned:
surface_form: mount stevens (alaska)
instance_of: Mountain
countries: United States
coordinates: lat: 62.9205
lon: -151.067
Mount Stevens (Alaska). Mount Stevens is a mountain located in Matanuska-Susitna Borough, Alaska. Mount Stevens is flanked to the northwest by Mount Hunter, and is about south of Denali. The mountain was named in 2010, after Ted Stevens (1923–2010), who had represented Alaska in the U.S. Senate from 1968 to 2009.

Geographic entities mentioned:
surface_form: mount stevens
instance_of: Mountain
countries: United States
coordinates: lat: 62.9205
lon: -151.067
Senate from 1968 to 2009. It had been the highest unnamed peak in Alaska, though unofficially called South Hunter Peak. Mount Stevens stands within the watershed of the Susitna River, which drains into Cook Inlet. The east sides of Mount Stevens drain into the Tokositna Glacier, thence into the Tokositna River, Chulitna River, and the Susitna.

Geographic entities mentioned:
surface_form: mount stevens
instance_of: Mountain
countries: United States
coordinates: lat: 62.9205
lon: -151.067
Mount Stevens stands within the watershed of the Susitna River, which drains into Cook Inlet. The east sides of Mount Stevens drain into the Tokositna Glacier, thence into the Tokositna River, Chulitna River, and the Susitna. The west sides of Stevens drain into Kahiltna Glacier, thence into Kahiltna River and the Susitna.

Geographic entities mentioned:
surface_form: mount stevens
instance_of: Mountain
countries: United States
coordinates: lat: 62.9205
lon: -151.067
The mountain was named in 2010, after Ted Stevens (1923–2010), who had represented Alaska in the U.S. Senate from 1968 to 2009. It had been the highest unnamed peak in Alaska, though unofficially called South Hunter Peak. Mount Stevens stands within the watershed of the Susitna River, which drains into Cook Inlet.

Geographic entities mentioned:
surface_form: hunter peak
instance_of: Mountain
countries: United States
coordinates: lat: 31.91345
lon: -104.83023
The main trail is more than long and there are over of associated side trails. The trail mostly follows the edge of the Niagara Escarpment, one of the nineteen UNESCO World Biosphere Reserves in Canada. The land the trail traverses is owned by the Government of Ontario, local municipalities, local conservation authorities, private landowners, and the Bruce Trail Conservancy (BTC).

Geographic entities mentioned:
surface_form: Niagara Escarpment
instance_of: Mountain
countries: Canada
coordinates: lat: 43.8334
lon: -79.99966
It passes through parks operated by various levels of government, including Woodend Conservation Area in Niagara-on-the-Lake, Battlefield Park in Stoney Creek, Dundas Valley Conservation Area in Dundas, the Hamilton-Brantford Rail Trail, Mount Nemo Conservation Area, Rattlesnake Point Conservation Area, Crawford Lake Conservation Area, Mono Cliffs Provincial Park, and the Bruce Peninsula National Park, which is located between Georgian Bay and Lake Huron near the northern tip of Bruce Peninsula.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
Ballantyne Lake. Ballantyne Lake is a lake in Blue Earth County, Minnesota, in the United States. Ballantyne Lake was named for James Ballantyne, an early settler.

Geographic entities mentioned:
surface_form: ballantyne lake
instance_of: Lake
countries: United States
coordinates: lat: 44.211944444444
lon: -93.835555555556
Adults are on the wing from January to April. Taxonomy. This species was first described by Edward Meyrick in 1882 using specimens collected by Richard William Fereday near Lake Guyon in March. Meyrick went on to give a fuller description of the species in 1883. In 1909 Meyrick placed this species in the genus &quot;Epichorista&quot;. This species is the type species of that genus.

Geographic entities mentioned:
surface_form: Lake Guyon
instance_of: Lake
countries: New Zealand
coordinates: lat: -42.2898
lon: 172.648
These populations are not thought to be related to the Central European populations, rather storröding from Lake Sommen and Lake Vättern are closely related to the char of Lake Ladoga in Russia.

Geographic entities mentioned:
surface_form: Lake Vättern
instance_of: Lake
countries: Sweden
coordinates: lat: 58.4
lon: 14.6
surface_form: Lake Ladoga
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.842777777777776
lon: 31.459722222222222
It is situated west of the suburb Hervanta. It has a small beach where people can sunbathe or swim during the summer. There are also two trails which bound the lake. The name derives from Finnish &quot;suoli&quot; (intestine) and &quot;järvi&quot; (lake). This is probably due to the curved shape of the lake. Suolijärvi is also a village near Puolanka in the Northern Finland east of Oulu.

Geographic entities mentioned:
surface_form: oulu
instance_of: Lake
countries: Finland
coordinates: lat: 64.333333333333
lon: 27.25
Suolijärvi. Suolijärvi is a small lake in Tampere, Finland. It is situated west of the suburb Hervanta. It has a small beach where people can sunbathe or swim during the summer. There are also two trails which bound the lake. The name derives from Finnish &quot;suoli&quot; (intestine) and &quot;järvi&quot; (lake). This is probably due to the curved shape of the lake.

Geographic entities mentioned:
surface_form: suolijärvi
instance_of: Lake
countries: Finland
coordinates: lat: 61.441111111111
lon: 23.828333333333
Barnes Butte. Barnes Butte is a rhyolite dome of volcanic rock in Crook County, Oregon, United States located partly within the city of Prineville. Barnes Butte is composed of welded tuff and is a part of the Crooked River caldera. It was the site of a 1940s mercury mine.

Geographic entities mentioned:
surface_form: Crooked River caldera
instance_of: Mountain
countries: United States
coordinates: lat: 44.3
lon: -120.9
surface_form: barnes butte
instance_of: Mountain
countries: United States
coordinates: lat: 44.31861111
lon: -120.81055556
Barnes Butte. Barnes Butte is a rhyolite dome of volcanic rock in Crook County, Oregon, United States located partly within the city of Prineville. Barnes Butte is composed of welded tuff and is a part of the Crooked River caldera. It was the site of a 1940s mercury mine.

Geographic entities mentioned:
surface_form: barnes butte
instance_of: Mountain
countries: United States
coordinates: lat: 44.31861111
lon: -120.81055556
It was the site of a 1940s mercury mine. In 2015, a BLM cleanup of mercury was done to reduce the health risk to residents of nearby IronHorse neighborhood and the Barnes Butte Elementary School. The butte is a recreational area and includes the Barnes Butte hiking trail, a loop that includes a 2.6-mile (4.2 km) hike to the summit.

Geographic entities mentioned:
surface_form: barnes butte
instance_of: Mountain
countries: United States
coordinates: lat: 44.31861111
lon: -120.81055556
The butte is a recreational area and includes the Barnes Butte hiking trail, a loop that includes a 2.6-mile (4.2 km) hike to the summit. A concept plan, &quot;Echo of the Butte,&quot; was developed by the Barnes Butte Focus Committee to establish a visitor's center, amphitheater, and pond around the Happy Hour Plateau.

Geographic entities mentioned:
surface_form: barnes butte
instance_of: Mountain
countries: United States
coordinates: lat: 44.31861111
lon: -120.81055556
It is bordered on the south by South Wollo, on the west by South Gondar, on the north by Wag Hemra, on the northeast by Tigray Region, and on the east by Afar Region; part of its southern border is defined by the Mille River. Its highest point is Mount Abuna Yosef. Its towns include Lasta Lalibela (known for its rock-cut churches) and Weldiya (also spelled Woldia).

Geographic entities mentioned:
surface_form: Mount Abuna Yosef
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 12.140833333333
lon: 39.181666666667
It weighs approximately. Distribution and habitat. James' sportive lemur is found in southeastern Madagascar, where it is known from the Manombo Special Reserve and the Manombo Classified Forest. The exact boundaries of its range are unknown, but the Manampatrana River and the Mananara River have been suggested as potential northern and southern limits.

Geographic entities mentioned:
surface_form: Manampatrana River
instance_of: Watercourse
countries: Madagascar
coordinates: lat: -22.81944444
lon: 47.81666667
Uchuck Lake. Uchuck Lake is a lake located on Vancouver Island north west of head of Uchucklesit Inlet on the north side of lower Alberni Inlet.

Geographic entities mentioned:
surface_form: uchuck lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.0369
lon: -125.106
Geography. The creek drains portions of Clarksburg, Germantown, and Boyds. It rises south of Damascus and flows southward about to Little Seneca Lake, a reservoir created by construction of a dam on the creek. The reservoir empties to the lower portion of the creek, which flows south about to Seneca Creek, which drains to the Potomac River and the Chesapeake Bay.

Geographic entities mentioned:
surface_form: Little Seneca Lake
instance_of: Lake
countries: United States
coordinates: lat: 39.188
lon: -77.3067
This became the basis for a new treaty. An Indenture (a revision) of the deal was made on August 1, 1805. Both the 1787 Purchase and its 1805 Indenture were registered as Crown Treaty No. 13. For this revision, the Mississaugas of New Credit First Nation also claimed the Toronto Islands, which was not part of the purchase as the agreement only went to the Lake Ontario shoreline. 2010 settlement.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Her brother Hamish has severe cerebral palsy and requires around-the-clock care. Jenny used to be a swimmer and taught her three daughters to swim, in the pool at the family's home. Cate also recalls swimming near Hippopotami in Lake Malawi as a small child. Lake Malawi is the second deepest lake in Africa. It was in this lake that her father, Eric, would go sailing on weekends.

Geographic entities mentioned:
surface_form: Lake Malawi
instance_of: Lake
countries: Malawi
Mozambique
Tanzania
coordinates: lat: -12.183333333333
lon: 34.366666666667
Dents du Midi. The Dents du Midi (; French: &quot;teeth of midday&quot;) are a three-kilometre-long mountain range in the Chablais Alps in the canton of Valais, Switzerland. Overlooking the Val d'Illiez and the Rhône valley to the south, they face the Lac de Salanfe, an artificial reservoir, and are part of the geological ensemble of the Giffre massif.

Geographic entities mentioned:
surface_form: Val d'Illiez
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.2409
lon: 6.8922
A fourth, the (the lazy ones' pass), is situated below the Haute Cime (). The Dents du Midi are linked to the Tour Sallière by a ridge to the south. It is on this ridge that the (Susanfe pass) is located, which allows one to pass from the valley of Susanfe to that of Salanfe. Geology.

Geographic entities mentioned:
surface_form: Tour Sallière
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.126666666667
lon: 6.9245
The collision caused folds in the tectonic plate, which caused the Dents du Midi to protrude from the surface. They represent the frontal hinge of the Morcles nappe, which extends to the south-west and includes Mont Joly and the Aravis mountain range in Savoie and Haute-Savoie. When they were formed, the Dents du Midi were connected with the Dent de Morcles.

Geographic entities mentioned:
surface_form: Mont Joly
instance_of: Mountain
countries: France
coordinates: lat: 45.82583333
lon: 6.69277778
They represent the frontal hinge of the Morcles nappe, which extends to the south-west and includes Mont Joly and the Aravis mountain range in Savoie and Haute-Savoie. When they were formed, the Dents du Midi were connected with the Dent de Morcles. The current shape of the Dents du Midi appeared during the Würm glaciation, the last of the great glaciations, which began 100,000 years ago.

Geographic entities mentioned:
surface_form: Dent de Morcles
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.198888888889
lon: 7.0758333333333
These areas of each were classified in 2017 with the aim of protecting Switzerland's dry meadows and pastures from agricultural use, almost 95% of which have disappeared since 1900. Culture. The Dents du Midi are represented in painting by many artists, most often as a backdrop for paintings of villages, Lake Geneva or Chillon Castle, but also alone.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
The everyday lives of the Aztecs are also shown in detail: artisans weaving and making pottery, mothers carrying babies, painting on scrolls, and calligraphy. Religious practices such as dances to the Sun God and the worship of snakes and jaguars are also shown. Rivera also included geographical features such as the volcanoes around the Valley of Mexico, as well corn and other crops. West wall.

Geographic entities mentioned:
surface_form: Valley of Mexico
instance_of: Valley
countries: Mexico
coordinates: lat: 19.66666667
lon: -98.86666667
Catharines, and Port Colborne. It has been traditionally known as the place &quot;where rails and water meet&quot;, referring to the railways from Buffalo to Toronto and Southwestern Ontario, and the waterways of Welland Canal and Welland River, which played a great role in the city's development.

Geographic entities mentioned:
surface_form: Welland River
instance_of: Watercourse
countries: Canada
coordinates: lat: 43.0377
lon: -79.1798
Cook's Mills was the second to last engagement of the War of 1812 on Canadian soil. The First Welland Canal was extended in 1833 to reach Lake Erie and has influenced development of this city ever since. A wooden aqueduct was built to carry the Welland Canal over the Welland River at what is now downtown Welland, and the area became known as simply Aqueduct.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
The island was created when the alignment of the First Welland Canal was constructed basically parallel to the Welland River and since the abandonment of the old canal has been established as Merritt Park, featuring a popular four kilometre-long paved trail. Climate.

Geographic entities mentioned:
surface_form: Welland River
instance_of: Watercourse
countries: Canada
coordinates: lat: 43.0377
lon: -79.1798
Welland Canal trails. The Welland Canal Parkway Trail is a paved recreational path beginning in the City of St. Catharines at Lake Ontario and ending at Lake Erie in Port Colborne. The sections of the trail located within Welland are paved. The trail follows alongside the Welland ship and Recreational Canals, and passes through downtown Welland. Welland Canal.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
The sections of the trail located within Welland are paved. The trail follows alongside the Welland ship and Recreational Canals, and passes through downtown Welland. Welland Canal. The Welland Canal, linking Lake Ontario with Lake Erie, is the transportation mode that Welland is best known for. Until 1972, the canal passed through downtown Welland.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Catharines. The proponents argue that an adequate rail line is already in place and using the Trillium's track through the Townline Tunnel would allow for uninterrupted train traffic to Niagara Falls. They also point out that a station in Welland would fit in the Niagara Region's &quot;Grow South&quot; policy of expanding the infrastructure south of the Niagara Escarpment. Air.

Geographic entities mentioned:
surface_form: Niagara Escarpment
instance_of: Mountain
countries: Canada
coordinates: lat: 43.8334
lon: -79.99966
Fokker FG-2. The Fokker FG-2 was built by Anthony Fokker for the 1922 Rhön gliding competition, after visiting the Wasserkuppe during the 1921 competition. Design and development. After Fokker's visit to the Wasserkuppe during the 1921 contest, he set about designing and building a two-seat biplane glider to fly at the 1922 competition.

Geographic entities mentioned:
surface_form: Wasserkuppe
instance_of: Mountain
countries: Germany
coordinates: lat: 50.498055555556
lon: 9.9377777777778
Allen after Saint Piran, the Patron Saint of Cornwall. The mountain can be climbed from the eastern side via a hiking trail that branches North off the trail to the Little Beehive. Alternatively, the mountain can be climbed on the SW side from slopes below the SE face of Mount Niblock. Going up one side and down the other completes a loop on the northern side of Lake Agnes.

Geographic entities mentioned:
surface_form: Mount Niblock
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4175
lon: -116.271
Mount St. Piran. Mount St. Piran is a mountain in Banff National Park near Lake Louise, Alberta, Canada. Located in the Bow River Valley southeast of the Minewakun Lake Valley; northwest of Lake Agnes; between Lake Louise Valley and lower Bath Creek. It was named in 1894 by Samuel E.S. Allen after Saint Piran, the Patron Saint of Cornwall.

Geographic entities mentioned:
surface_form: mount st. piran
instance_of: Mountain
countries: Canada
coordinates: lat: 51.42138888888889
lon: -116.25277777777778
The Old Elm was voted European Tree of the Year 2014. The city also served as an important strategic centre for the Bulgarian Army, with the headquarters of the Bulgarian Third Army located in the centre of the city, being situated relatively near to the sensitive Turkish border. Sliven Peak on Livingston Island in the South Shetland Islands, Antarctica is named after Sliven. Etymology.

Geographic entities mentioned:
surface_form: Sliven Peak
instance_of: Mountain
coordinates: lat: -62.600972222222
lon: -60.128333333333
Napo River. The Napo River () is a tributary to the Amazon River that rises in Ecuador on the flanks of the east Andean volcanoes of Antisana, Sincholagua and Cotopaxi. The total length is. The river drains an area of ca 103,000 km2. The mean annual discharge at Mazán. Geography.

Geographic entities mentioned:
surface_form: Antisana
instance_of: Mountain
countries: Ecuador
coordinates: lat: -0.48138888888889
lon: -78.140833333333
surface_form: Cotopaxi
instance_of: Mountain
countries: Ecuador
coordinates: lat: -0.68055555555556
lon: -78.437777777778
Location. Knole is located at the southern end of Sevenoaks, in the Weald of west Kent. To the north, the land slopes down to the Darenth valley and the narrow fertile &quot;pays&quot; of Holmesdale, at the foot of the North Downs. The land around Sevenoaks itself has sandy soils, with woodland that was used in the Middle Ages in the traditional Wealden way, for pannage, rough pasture and timber.

Geographic entities mentioned:
surface_form: Holmesdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.233333333333
lon: -0.33333333333333
The Dumbell summit is slightly higher than the northeast subpeak (8,408 ft) which is unofficially called &quot;Greenwood Mountain&quot;. The nearest higher neighbor is Chiwawa Mountain, to the east-southeast. Precipitation runoff from Dumbell Mountain drains into tributaries of the Chelan River and the Wenatchee River.

Geographic entities mentioned:
surface_form: Chiwawa Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.163333333333
lon: -120.90722222222
surface_form: chiwawa mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.163333333333
lon: -120.90722222222
Subduction and tectonic activity in the area began during the late cretaceous period, about. Extensive volcanic activity began to take place in the oligocene, about. Glacier Peak, a stratovolcano that is southwest of Dumbell Mountain, began forming in the mid-Pleistocene. Climate. Dumbell Mountain is located in the marine west coast climate zone of western North America.

Geographic entities mentioned:
surface_form: Glacier Peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.11194444444445
lon: -121.11416666666666
surface_form: dumbell mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.179722222222
lon: -120.85888888889
Dumbell Mountain. Dumbell Mountain is an double summit massif located in the Glacier Peak Wilderness of the North Cascades, in Chelan County of Washington state. The Dumbell summit is slightly higher than the northeast subpeak (8,408 ft) which is unofficially called &quot;Greenwood Mountain&quot;. The nearest higher neighbor is Chiwawa Mountain, to the east-southeast.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.11194444444445
lon: -121.11416666666666
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.14972222
lon: -109.84944444
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.155013
lon: -117.293429
surface_form: chelan
instance_of: Lake
countries: United States
coordinates: lat: 47.841111111111
lon: -120.04638888889
surface_form: dumbell mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.179722222222
lon: -120.85888888889
The nearest higher neighbor is Chiwawa Mountain, to the east-southeast. Precipitation runoff from Dumbell Mountain drains into tributaries of the Chelan River and the Wenatchee River. The mountain's descriptive name was applied by Albert Hale Sylvester (1871–1944), pioneer surveyor, explorer, topographer, and forest supervisor in the Cascades. Geology.

Geographic entities mentioned:
surface_form: chelan
instance_of: Lake
countries: United States
coordinates: lat: 47.841111111111
lon: -120.04638888889
surface_form: dumbell mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.179722222222
lon: -120.85888888889
Dumbell Mountain. Dumbell Mountain is an double summit massif located in the Glacier Peak Wilderness of the North Cascades, in Chelan County of Washington state. The Dumbell summit is slightly higher than the northeast subpeak (8,408 ft) which is unofficially called &quot;Greenwood Mountain&quot;. The nearest higher neighbor is Chiwawa Mountain, to the east-southeast.

Geographic entities mentioned:
surface_form: greenwood mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.14176
lon: -74.3871
Dumbell Mountain. Dumbell Mountain is an double summit massif located in the Glacier Peak Wilderness of the North Cascades, in Chelan County of Washington state. The Dumbell summit is slightly higher than the northeast subpeak (8,408 ft) which is unofficially called &quot;Greenwood Mountain&quot;. The nearest higher neighbor is Chiwawa Mountain, to the east-southeast.

Geographic entities mentioned:
surface_form: dumbell mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.179722222222
lon: -120.85888888889
The opening theme is a new rendition of the opening in the original &quot;Tiger Mask,&quot; which was originally performed by Hideyo Morimoto. The show airs on TV Asahi's 26:45 (2:45 AM) time slot on Saturday, technically Sunday morning. Naoto Date's training facility on Mount Fuji and his dream about a children's land are original from the manga, but omitted in the first anime. Promotion.

Geographic entities mentioned:
surface_form: Mount Fuji
instance_of: Mountain
countries: Japan
coordinates: lat: 35.36055555555556
lon: 138.7275
Killagoola has locally derived place-names such as Mountview, Sruthan, Sceith and Baile Thiar to distinguish areas of the townland. The Lough Kip river runs from the lake, Lough Kip, through the townland towards Ballyquirke Lake, a feeder for the much larger Lough Corrib. Most of the land in the area is used as farmland, reclaimed from boggy or mountainous areas.

Geographic entities mentioned:
surface_form: Lough Corrib
instance_of: Lake
countries: Ireland
coordinates: lat: 53.466666666667
lon: -9.2833333333333
Piz da la Margna. Piz da la Margna (3,158 m) is a mountain in the Bernina Range of the Alps, overlooking Lake Sils in the Swiss canton of Graubünden. It lies to the south-east of the Maloja Pass at the south-western end of the Engadin valley. Ascents can be made from Maloja via the north ridge (F); a slightly easier route is via the Val Fedoz and the east flank.

Geographic entities mentioned:
surface_form: Lake Sils
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.416666666667
lon: 9.7333333333333
surface_form: sils
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.416666666667
lon: 9.7333333333333
surface_form: piz da la margna
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.381944444444
lon: 9.73
surface_form: bernina
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.382388888889
lon: 9.9081111111111
Piz da la Margna. Piz da la Margna (3,158 m) is a mountain in the Bernina Range of the Alps, overlooking Lake Sils in the Swiss canton of Graubünden. It lies to the south-east of the Maloja Pass at the south-western end of the Engadin valley. Ascents can be made from Maloja via the north ridge (F); a slightly easier route is via the Val Fedoz and the east flank.

Geographic entities mentioned:
surface_form: Engadin
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.5497
lon: 9.8959
It lies to the south-east of the Maloja Pass at the south-western end of the Engadin valley. Ascents can be made from Maloja via the north ridge (F); a slightly easier route is via the Val Fedoz and the east flank. The south-east ridge from the Fuorcla da la Margna (AD, IV) was first climbed by Hans Frick, Christian Zippert and Hans Casper on 14 August 1918.

Geographic entities mentioned:
surface_form: Val Fedoz
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.395758
lon: 9.750399
Ascents can be made from Maloja via the north ridge (F); a slightly easier route is via the Val Fedoz and the east flank. The south-east ridge from the Fuorcla da la Margna (AD, IV) was first climbed by Hans Frick, Christian Zippert and Hans Casper on 14 August 1918. The first recorded ‘tourist’ ascent of the mountain was made by J. Caviezel, Krättli, Robbi and Zaun in June 1857.

Geographic entities mentioned:
surface_form: first
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.50486111
lon: 7.64305556
surface_form: first
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.6608
lon: 8.05469
Piz da la Margna. Piz da la Margna (3,158 m) is a mountain in the Bernina Range of the Alps, overlooking Lake Sils in the Swiss canton of Graubünden. It lies to the south-east of the Maloja Pass at the south-western end of the Engadin valley. Ascents can be made from Maloja via the north ridge (F); a slightly easier route is via the Val Fedoz and the east flank.

Geographic entities mentioned:
surface_form: piz da la margna
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.381944444444
lon: 9.73
Nero gave the V &quot;Macedonica&quot;, the X &quot;Fretensis&quot; and the XV &quot;Apollinaris&quot; to Titus Flavius Vespasianus to counter the revolt. In 67, in Galilee, the city of Sepphoris surrendered peacefully to the Roman army, and later the V &quot;Macedonica&quot; conquered Mount Gerizim, the chief sanctuary of the Samaritans.

Geographic entities mentioned:
surface_form: Mount Gerizim
instance_of: Mountain
countries: State of Palestine
coordinates: lat: 32.199444444444
lon: 35.272777777778
While returning from an attack on a suspected Austro-Hungarian submarine base in the Gulf of Drin by a mixed group of Italian, British and French cruisers and destroyers on 9 June, the British light cruiser was torpedoed by the submarine &quot;U-4&quot;. The close escort managed to drive the submarine away, and &quot;Dublin&quot; successfully reached Brindisi without further damage.

Geographic entities mentioned:
surface_form: Gulf of Drin
instance_of: Body of water
countries: Albania
coordinates: lat: 41.76666667
lon: 19.51666667
Strømsfoss. sb8e18qfdvneawj2neajng3tzkxl" xml:space="preserve">Strømsfoss is a village in Aremark municipality, Norway. Here, the Øymarksjøen-Rødenessjøen-Ara-Aspern-Femsjøen watershed meets the national road between Aremark and Rakkestad as well as the county road between Aremark and Ørje. Strømsfoss has a watermill museum, housed in an old mill built in 1897–98.

Geographic entities mentioned:
surface_form: Øymarksjøen
instance_of: Lake
countries: Norway
coordinates: lat: 59.372222222222
lon: 11.659722222222
surface_form: Rødenessjøen
instance_of: Lake
countries: Norway
coordinates: lat: 59.487777777778
lon: 11.645833333333
surface_form: Femsjøen
instance_of: Lake
countries: Norway
coordinates: lat: 59.134444444444
lon: 11.461388888889
Situated between the Alburni mountains and the borders of Campania with Basilicata, it is considered a geographical subregion of Cilento and is part of the Cilento and Vallo di Diano National Park, World Heritage Site of Italy from 1998. The greatest forestal park, mainly located in cilentan side, is Pruno. The area is composed by 17 municipalities, and the greatest one is Sala Consilina, with c.

Geographic entities mentioned:
surface_form: pruno
instance_of: Mountain
countries: Italy
coordinates: lat: 40.4118309
lon: 15.3628179
Vallo di Diano. The Vallo di Diano (also known as &quot;Valdiano&quot;) is an Italian valley of the south-eastern side of Campania, in the province of Salerno. Geography.

Geographic entities mentioned:
surface_form: vallo di diano
instance_of: Valley
countries: Italy
coordinates: lat: 40.4
lon: 15.566666666667
Vallo di Diano. The Vallo di Diano (also known as &quot;Valdiano&quot;) is an Italian valley of the south-eastern side of Campania, in the province of Salerno. Geography.

Geographic entities mentioned:
surface_form: vallo di diano
instance_of: Valley
countries: Italy
coordinates: lat: 40.4
lon: 15.566666666667
surface_form: valdiano
instance_of: Valley
countries: Italy
coordinates: lat: 40.4
lon: 15.566666666667
Geography. Situated between the Alburni mountains and the borders of Campania with Basilicata, it is considered a geographical subregion of Cilento and is part of the Cilento and Vallo di Diano National Park, World Heritage Site of Italy from 1998. The greatest forestal park, mainly located in cilentan side, is Pruno.

Geographic entities mentioned:
surface_form: vallo di diano
instance_of: Valley
countries: Italy
coordinates: lat: 40.4
lon: 15.566666666667
Beinn Udlamain. Beinn Udlamain is a Scottish mountain which stands just to the west of the summit of the Pass of Drumochter and east of Loch Ericht, some 30 km west-northwest of the village of Blair Atholl. The mountain’s summit stands on the border between the Highland and Perth and Kinross council areas. Overview.

Geographic entities mentioned:
surface_form: Loch Ericht
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.8323
lon: -4.3741
surface_form: beinn udlamain
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.835444
lon: -4.329976
Overview. At 1011 metres (3317 feet) Beinn Udlamain qualifies as a Munro, and with a high prominence, a Marilyn. It is the highest of the Drumochter hills, however it is not the most eye catching of the group, being flat topped and shielded from a clear view from the A9 road by the surrounding Munros of Sgairneach Mhòr and A' Mharconaich.

Geographic entities mentioned:
surface_form: Sgairneach Mhòr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.828447
lon: -4.297792
surface_form: A' Mharconaich
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.857002
lon: -4.290668
From here the direct ascent goes up Coire Dhomhain to its head where the south ridge of the mountain can be followed to the summit. A complete round of all the peaks around Coire Dhomhain can be done from this starting point, including the two already mentioned Munros and the Corbett The Sow of Atholl. The summit of the mountain is marked by a large cairn and wind shelter.

Geographic entities mentioned:
surface_form: The Sow of Atholl
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.8371
lon: -4.2565
A complete round of all the peaks around Coire Dhomhain can be done from this starting point, including the two already mentioned Munros and the Corbett The Sow of Atholl. The summit of the mountain is marked by a large cairn and wind shelter. The highlight of the view from the summit is to the SW where there is a fine view of a long stretch of Loch Ericht with the Ben Alder massif behind.

Geographic entities mentioned:
surface_form: Ben Alder
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.813796
lon: -4.465089
surface_form: loch ericht
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.8323
lon: -4.3741
surface_form: ben alder
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.833498
lon: -4.529175
Beinn Udlamain. Beinn Udlamain is a Scottish mountain which stands just to the west of the summit of the Pass of Drumochter and east of Loch Ericht, some 30 km west-northwest of the village of Blair Atholl. The mountain’s summit stands on the border between the Highland and Perth and Kinross council areas. Overview.

Geographic entities mentioned:
surface_form: beinn udlamain
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.835444
lon: -4.329976
Overview. At 1011 metres (3317 feet) Beinn Udlamain qualifies as a Munro, and with a high prominence, a Marilyn. It is the highest of the Drumochter hills, however it is not the most eye catching of the group, being flat topped and shielded from a clear view from the A9 road by the surrounding Munros of Sgairneach Mhòr and A' Mharconaich.

Geographic entities mentioned:
surface_form: beinn udlamain
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.835444
lon: -4.329976
Other explanations of the name put forward by mountain writers are “hill of the unsteady place” and “hill of the shaking”. Geography. Beinn Udlamain has a long north-south orientated summit ridge which stays above the 970 metre contour for over 1.5 kilometres. This ridge continues to the south to a col with a height of 809 metres which links to the adjacent Munro of Sgairneach Mhòr.

Geographic entities mentioned:
surface_form: beinn udlamain
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.835444
lon: -4.329976
In the opposite direction this ridge swings NE to link to A' Mharconaich which lies three km distant. Beinn Udlamain’s slopes consist mostly of grass and heather with very little rock but they do drop steeply to the west towards Loch Ericht and to the east to the valley of the Allt Coire Dhomhain.

Geographic entities mentioned:
surface_form: beinn udlamain
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.835444
lon: -4.329976
surface_form: loch ericht
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.8323
lon: -4.3741
The mountain is crossed by an ancient line of iron fence posts which mark the old boundary between Perthshire and Invernesshire, this can be an aid to navigation in poor visibility. The rolling topography of Beinn Udlamain and its adjoining peaks make it ideal ski touring country.

Geographic entities mentioned:
surface_form: beinn udlamain
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.835444
lon: -4.329976
The rolling topography of Beinn Udlamain and its adjoining peaks make it ideal ski touring country. The ski circuit of A' Mharconaich, Beinn Udlamain and Sgairneach Mhor is a classic route made popular by the close accessibility of the A9 road and the fact that the hills hold snow very well.

Geographic entities mentioned:
surface_form: beinn udlamain
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.835444
lon: -4.329976
surface_form: a' mharconaich
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.857002
lon: -4.290668
surface_form: sgairneach mhor
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.828447
lon: -4.297792
The ski circuit of A' Mharconaich, Beinn Udlamain and Sgairneach Mhor is a classic route made popular by the close accessibility of the A9 road and the fact that the hills hold snow very well. Drainage from Beinn Udlamain goes to the east coast of Scotland either via Loch Ericht or the Allt Coire Dhomhain, both routes eventually join the River Tay. Ascents and view.

Geographic entities mentioned:
surface_form: beinn udlamain
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.835444
lon: -4.329976
surface_form: loch ericht
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.8323
lon: -4.3741
Ascents and view. Beinn Udlamain is invariably ascended from the A9 road from near the summit of the Drumochter Pass at grid reference, which gives a starting altitude of 462 metres. From here the direct ascent goes up Coire Dhomhain to its head where the south ridge of the mountain can be followed to the summit.

Geographic entities mentioned:
surface_form: beinn udlamain
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.835444
lon: -4.329976
Geography. Beinn Udlamain has a long north-south orientated summit ridge which stays above the 970 metre contour for over 1.5 kilometres. This ridge continues to the south to a col with a height of 809 metres which links to the adjacent Munro of Sgairneach Mhòr. In the opposite direction this ridge swings NE to link to A' Mharconaich which lies three km distant.

Geographic entities mentioned:
surface_form: a' mharconaich
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.857002
lon: -4.290668
Beinn Udlamain’s slopes consist mostly of grass and heather with very little rock but they do drop steeply to the west towards Loch Ericht and to the east to the valley of the Allt Coire Dhomhain. On the northern side of the mountain are two grassy corries, the Glas-choire and the Fraoch-choire, which both drain NW into Loch Ericht.

Geographic entities mentioned:
surface_form: loch ericht
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.8323
lon: -4.3741
Geography. Beinn Udlamain has a long north-south orientated summit ridge which stays above the 970 metre contour for over 1.5 kilometres. This ridge continues to the south to a col with a height of 809 metres which links to the adjacent Munro of Sgairneach Mhòr. In the opposite direction this ridge swings NE to link to A' Mharconaich which lies three km distant.

Geographic entities mentioned:
surface_form: sgairneach mhòr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.828447
lon: -4.297792
Skrino. Skrino () is a village in the municipality of Boboshevo, Kyustendil Province, western Bulgaria. As of 2013 it has 66 inhabitants. Geography. The village is located in the Ruen mountain, the northernmost part of the Vlahina mountain range. History. Skrino is known under the same name since the 9th century, when it was part of the Bulgarian Empire.

Geographic entities mentioned:
surface_form: Vlahina
instance_of: Mountain
countries: Bulgaria
North Macedonia
coordinates: lat: 41.856944444444
lon: 22.928888888889
Williams River (New South Wales). The Williams River is a perennial stream that is a tributary of the Hunter River, in the Hunter Region of New South Wales, Australia. Course and features.

Geographic entities mentioned:
surface_form: Hunter Region
instance_of: Valley
countries: Australia
coordinates: lat: -32.56
lon: 151.17083333333332
Course and features. The Williams River rises on the southern slopes of the Barrington Tops below Careys Peak within Barrington Tops National Park, and flows generally southeast and south, joined by ten tributaries including Chichester River, before reaching its confluence with the Hunter River at Raymond Terrace. The river descends over its course; through Dungog, Clarence Town and Seaham.

Geographic entities mentioned:
surface_form: Barrington Tops
instance_of: Landform
countries: Australia
coordinates: lat: -31.94998
lon: 151.52687
There they were completed and underwent builder's trials. When the Coast Guard accepted the ships, and ownership passed from Marinette Marine, they were placed &quot;in commission, special&quot; status. The crews were trained by Marinette personnel in Lake Michigan. They then sailed through the Great Lakes and out into the Atlantic to reach their new home ports. They made frequent stops.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Etymology. The name Cogua is derived from Chibcha and means &quot;Support of the hill&quot;. History. Cogua in the times before the Spanish conquest was inhabited by the Muisca who lived on the Altiplano Cundiboyacense and had established an advanced civilization. Cogua is located between two important sources of salt in the Muisca economy; Zipaquirá and Nemocón.

Geographic entities mentioned:
surface_form: Altiplano Cundiboyacense
instance_of: Plateau
countries: Colombia
coordinates: lat: 5.532209
lon: -73.362877
Its reservoir, known as the Andijan Reservoir in Uzbekistan and Kempir-Abad Reservoir in Kyrgyzstan, covers and stretches into the neighboring Osh Region of Kyrgyzstan. The dam serves several purposes including irrigation in the Fergana Valley and hydroelectric power production. Water released from the dam can enter a canal on either side of the river downstream.

Geographic entities mentioned:
surface_form: Fergana Valley
instance_of: Valley
countries: Kyrgyzstan
Uzbekistan
Tajikistan
coordinates: lat: 40.900833333333
lon: 71.757777777778
Lac Cabot, Mauricie. The Lac Cabot is a freshwater lake located in La Tuque, Mauricie, Quebec, Canada. It is situated near Lac Dale and Lac Eagle, at an average elevation of 454 meters above the sea level.

Geographic entities mentioned:
surface_form: lac eagle
instance_of: Lake
countries: Canada
coordinates: lat: 49.7
lon: -93.2167
Lac Cabot, Mauricie. The Lac Cabot is a freshwater lake located in La Tuque, Mauricie, Quebec, Canada. It is situated near Lac Dale and Lac Eagle, at an average elevation of 454 meters above the sea level.

Geographic entities mentioned:
surface_form: lac cabot
instance_of: Lake
countries: Canada
coordinates: lat: 47.685
lon: -73.56388888888888
In the 20th century, Canadian Molotschna Mennonites arrived in Mexico, and founded the Jagüeyes Colonies in Mexico. Phonological differences exist between the Plautdietsch of Catholics and Mennonites in Canada's Saskatchewan Valley. These include [iəә] for the phoneme /ea/ &quot;wea&quot; (was) and &quot;Pead&quot; (horses) for Mennonite speakers; Catholic speakers use [eəә], traced to Ukraine.

Geographic entities mentioned:
surface_form: Saskatchewan Valley
instance_of: Valley
countries: Canada
Nature reserve. Hoy and the surrounding Bay of Reutin (&quot;Reutiner Bucht&quot;) is designated as a nature reserve, the &quot;Bayerisches Bodenseeufer&quot;, with an area of 221 hectares. It is also part of the bird reserve, &quot;Bayerisches Bodensee&quot;. It has certain similarities with an artificial island in the lake of Chiemsee, the Schalch, which is also in Bavaria. History.

Geographic entities mentioned:
surface_form: Chiemsee
instance_of: Lake
countries: Germany
coordinates: lat: 47.89
lon: 12.47
Gif-sur-Yvette. Gif-sur-Yvette (, &quot;Gif-on-Yvette&quot;) is a commune in southwestern Île-de-France, France. It is located in the Vallée de Chevreuse, from the centre of Paris (at Notre-Dame), in the Essonne department on the departmental border with Yvelines. In 2021, it had a population of 22,352. Geography. The town is crossed by and named after the river Yvette.

Geographic entities mentioned:
surface_form: Vallée de Chevreuse
instance_of: Valley
countries: France
coordinates: lat: 48.7
lon: 2.0333333333333