Sarmila/GeoWiki-Features huggingface dataset:
Sex Noir. The Sex Noir (2,731 m) is a mountain of the Bernese Alps, located north of Anzère in the canton of Valais. It belongs to the massif of the Wildhorn and lies approximately halfway between the summit of the Wildhorn and the Prabé, on the range separating the valley of La Morge from the valley of La Sionne. Both rivers end in the Rhone.

Geographic entities mentioned:
surface_form: Wildhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.354583333333
lon: 7.3608611111111
surface_form: Prabé
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.284111111111
lon: 7.3498888888889
surface_form: sionne
instance_of: Watercourse
countries: Switzerland
coordinates: lat: 46.31927
lon: 7.38493
surface_form: wildhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.354583333333
lon: 7.3608611111111
Sex Noir. The Sex Noir (2,731 m) is a mountain of the Bernese Alps, located north of Anzère in the canton of Valais. It belongs to the massif of the Wildhorn and lies approximately halfway between the summit of the Wildhorn and the Prabé, on the range separating the valley of La Morge from the valley of La Sionne. Both rivers end in the Rhone.

Geographic entities mentioned:
surface_form: sex noir
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.31775
lon: 7.3573333333333
He served as a French translator to the government from 1909. In 1918 a refusal to drink to the health of King George V at a party held in Horsleykonda on 24 May (Empire Day) resulted in his being sidelined and a formal inquiry was held by a committee headed by Sir William Ayling. Galletti published a book on &quot;The Dutch in Malabar&quot; in 1911. He retired from the civil service in 1934.

Geographic entities mentioned:
surface_form: Horsleykonda
instance_of: Mountain
countries: India
coordinates: lat: 13.6508702
lon: 78.3965255
With the North American Plate overriding the Pacific Plate, episodes of volcanic igneous activity persisted. Glacier Peak, a stratovolcano that is west of Chilly Peak, began forming in the mid-Pleistocene. During the Pleistocene period dating back over two million years ago, glaciation advancing and retreating repeatedly scoured the landscape leaving deposits of rock debris.

Geographic entities mentioned:
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: chilly peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.098098
lon: -120.776815
Chilly Peak is a mountain summit located in the Entiat Mountains, a sub-range of the North Cascades, in Chelan County of Washington state. It ranks as 194th of Washington's highest 200 peaks. The nearest higher neighbor is Ice Box, to the northwest, and Spectacle Buttes are set to the north-northeast. Chilly Peak is situated south of Ice Lakes in the Okanogan–Wenatchee National Forest.

Geographic entities mentioned:
surface_form: ice box
instance_of: Mountain
countries: United States
coordinates: lat: 48.112143
lon: -120.79555
Chilly Peak. Chilly Peak is a mountain summit located in the Entiat Mountains, a sub-range of the North Cascades, in Chelan County of Washington state. It ranks as 194th of Washington's highest 200 peaks. The nearest higher neighbor is Ice Box, to the northwest, and Spectacle Buttes are set to the north-northeast.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: chelan
instance_of: Lake
countries: United States
coordinates: lat: 47.841111111111
lon: -120.04638888889
surface_form: chilly peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.098098
lon: -120.776815
Chilly Peak. Chilly Peak is a mountain summit located in the Entiat Mountains, a sub-range of the North Cascades, in Chelan County of Washington state. It ranks as 194th of Washington's highest 200 peaks. The nearest higher neighbor is Ice Box, to the northwest, and Spectacle Buttes are set to the north-northeast.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Chilly Peak. Chilly Peak is a mountain summit located in the Entiat Mountains, a sub-range of the North Cascades, in Chelan County of Washington state. It ranks as 194th of Washington's highest 200 peaks. The nearest higher neighbor is Ice Box, to the northwest, and Spectacle Buttes are set to the north-northeast.

Geographic entities mentioned:
surface_form: chilly peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.098098
lon: -120.776815
The nearest higher neighbor is Ice Box, to the northwest, and Spectacle Buttes are set to the north-northeast. Chilly Peak is situated south of Ice Lakes in the Okanogan–Wenatchee National Forest. Precipitation runoff from the mountain drains east into Ice Creek which is a tributary of the Entiat River, and west into Rock Creek, a tributary of the Chiwawa River. Climate.

Geographic entities mentioned:
surface_form: chilly peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.098098
lon: -120.776815
Precipitation runoff from the mountain drains east into Ice Creek which is a tributary of the Entiat River, and west into Rock Creek, a tributary of the Chiwawa River. Climate. Lying east of the Cascade crest, the area around Chilly Peak is a bit drier than areas to the west. Summers can bring warm temperatures and occasional thunderstorms.

Geographic entities mentioned:
surface_form: chilly peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.098098
lon: -120.776815
As a result, the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. With its impressive height, Chilly Peak can have snow on it in late-spring and early-fall, and it can be very cold in the winter. Geology. The North Cascades features some of the most rugged topography in the Cascade Range with craggy peaks, ridges, and deep glacial valleys.

Geographic entities mentioned:
surface_form: chilly peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.098098
lon: -120.776815
During the Middle Ages, Trebević was known as &quot;Zlatni Do&quot;. During the 1984 Winter Olympics Trebević, like the other Sarajevo mountains, was used for several Olympic events, such as bobsledding. Trebević today is important as a tourist destination for citizens of Sarajevo as Igman or Bjelašnica. Most of the land mines are now cleared from heavy fighting that took place in the early 1990s.

Geographic entities mentioned:
surface_form: Igman
instance_of: Plateau
countries: Bosnia and Herzegovina
coordinates: lat: 43.783333333333
lon: 18.25
surface_form: igman
instance_of: Plateau
countries: Bosnia and Herzegovina
coordinates: lat: 43.783333333333
lon: 18.25
Trebević. Trebević () is a mountain in central Bosnia and Herzegovina, located in the territories of Republika Srpska, Sarajevo and Istočno Sarajevo, bordering Jahorina mountain. Trebević is tall, making it the second shortest of the Sarajevo mountains. During the Middle Ages, Trebević was known as &quot;Zlatni Do&quot;.

Geographic entities mentioned:
surface_form: trebević
instance_of: Mountain
countries: Bosnia and Herzegovina
coordinates: lat: 43.823333333333
lon: 18.448888888889
Trebević is tall, making it the second shortest of the Sarajevo mountains. During the Middle Ages, Trebević was known as &quot;Zlatni Do&quot;. During the 1984 Winter Olympics Trebević, like the other Sarajevo mountains, was used for several Olympic events, such as bobsledding. Trebević today is important as a tourist destination for citizens of Sarajevo as Igman or Bjelašnica.

Geographic entities mentioned:
surface_form: trebević
instance_of: Mountain
countries: Bosnia and Herzegovina
coordinates: lat: 43.823333333333
lon: 18.448888888889
Trebević is tall, making it the second shortest of the Sarajevo mountains. During the Middle Ages, Trebević was known as &quot;Zlatni Do&quot;. During the 1984 Winter Olympics Trebević, like the other Sarajevo mountains, was used for several Olympic events, such as bobsledding. Trebević today is important as a tourist destination for citizens of Sarajevo as Igman or Bjelašnica.

Geographic entities mentioned:
surface_form: trebević
instance_of: Mountain
countries: Bosnia and Herzegovina
coordinates: lat: 43.823333333333
lon: 18.448888888889
surface_form: trebević
instance_of: Mountain
countries: Bosnia and Herzegovina
coordinates: lat: 43.823333333333
lon: 18.448888888889
Most of the land mines are now cleared from heavy fighting that took place in the early 1990s. There are a few hotels, mountaineering homes, and other such structures on Trebević and the immediate area. The mountain is very popular for family picnics, hiking, climbing, mountain biking and it has a downhill track for local and international skiing competitions.

Geographic entities mentioned:
surface_form: trebević
instance_of: Mountain
countries: Bosnia and Herzegovina
coordinates: lat: 43.823333333333
lon: 18.448888888889
The biological diversity is among the highest and it is extraordinary to find such a phenomenon near the heart of the big city. On 9 April 2014, Sarajevo Canton Assembly declared Trebević a protected area, in order to conserve and improve each element of the geographical and biological diversity.

Geographic entities mentioned:
surface_form: trebević
instance_of: Mountain
countries: Bosnia and Herzegovina
coordinates: lat: 43.823333333333
lon: 18.448888888889
surface_form: trebević
instance_of: Mountain
countries: Bosnia and Herzegovina
coordinates: lat: 43.823333333333
lon: 18.448888888889
On 9 April 2014, Sarajevo Canton Assembly declared Trebević a protected area, in order to conserve and improve each element of the geographical and biological diversity. Trebević can be reached from Sarajevo by the Trebević Cable Car, which starts from the neighbourhood of Bistrik. Mineral and crystal deposits.

Geographic entities mentioned:
surface_form: trebević
instance_of: Mountain
countries: Bosnia and Herzegovina
coordinates: lat: 43.823333333333
lon: 18.448888888889
The Frænfjorden cuts into the middle of the municipality. The coastal areas are low and marshy while the interior of the municipality is mountainous. The highest point in the municipality is the tall mountain Snøtinden on the border with Gjemnes Municipality. Other notable mountains include Jendemsfjellet Høgheitinden, and Lågheia. The Bjørnsund islands lie off the northwestern coast.

Geographic entities mentioned:
surface_form: Jendemsfjellet
instance_of: Mountain
countries: Norway
coordinates: lat: 62.800833333333
lon: 7.0436111111111
surface_form: Høgheitinden
instance_of: Mountain
countries: Norway
coordinates: lat: 62.8737
lon: 7.216
1995–1996. Peterka made his World Cup debut on 4 January 1996. Due to the poor performance of Slovenian competitors at the time, Peterka was brought in as a replacement for the Four Hills Tournament event in Innsbruck, where he finished eighth. Peterka continued his good form, winning the competitions in Zakopane and Falun, and finished the season tenth overall.

Geographic entities mentioned:
surface_form: Innsbruck
instance_of: Mountain
countries: Austria
coordinates: lat: 47.246666666667
lon: 11.399722222222
The area of the park is. Geology. The park is located at the southern edge of the Ukrainian crystalline shield in the spurs of the Podolian and Near-Dnipro Uplands. On the territory of the park the Southern Buh cuts into the crystalline massif (array) of the Ukrainian shield the outcome of which produced many rapids in the river.

Geographic entities mentioned:
surface_form: Podolian
instance_of: Plateau
countries: Ukraine
Moldova
coordinates: lat: 49.0275
lon: 27.85619444
Cugnot Ice Piedmont. Cugnot Ice Piedmont () is an ice piedmont in Trinity Peninsula, Antarctica. It is about long and between wide, extending from Russell East Glacier to Eyrie Bay and bounded on the landward side by Louis Philippe Plateau. Location. Cugnot Ice Piedmont is in Graham Land in the center of the south coast of the Trinity Peninsula, which forms the tip of the Antarctic Peninsula.

Geographic entities mentioned:
surface_form: Louis Philippe Plateau
instance_of: Landform
coordinates: lat: -63.6
lon: -58.35
Location. Cugnot Ice Piedmont is in Graham Land in the center of the south coast of the Trinity Peninsula, which forms the tip of the Antarctic Peninsula. It is on the coast of the Prince Gustav Channel to the south of the Louis Philippe Plateau and Broad Valley. Eyre Bay is to the northeast and Russell East Glacier is to the southwest.

Geographic entities mentioned:
surface_form: Louis Philippe Plateau
instance_of: Landform
coordinates: lat: -63.6
lon: -58.35
surface_form: Broad Valley
instance_of: Valley
coordinates: lat: -63.3667
lon: -57.9167
Features of the west part of the ice piedmont include, from west to east,
Chochoveni Nunatak. A rocky hill rising to high in the southwest part of Cugnot Ice Piedmont. Situated south by east of Smin Peak, northwest of Kolobar Nunatak, northeast of Coburg Peak and east of Drenta Bluff. Named after the settlements of Golyamo Chochoveni and Malko Chochoveni in Southeastern Bulgaria. Kolobar Nunatak.

Geographic entities mentioned:
surface_form: Smin Peak
instance_of: Mountain
coordinates: lat: -63.6381
lon: -58.3147
Named after the settlement of Gornik in Northern Bulgaria. McCalman Peak. The high summit of an east–west trending ridge north of Crystal Hill. Named by UK-APC for Donald McCalman, FIDS surveyor at Hope Bay, 1958-59. Crystal Hill. Ice-free hill, high, forming the summit of a headland between Bald Head and Camp Hill on the south side of Trinity Peninsula.

Geographic entities mentioned:
surface_form: donald
instance_of: Mountain
coordinates: lat: -65.0833
lon: -60.1
surface_form: hope
instance_of: Lake
coordinates: lat: -63.4167
lon: -57.0167
Shelter Cove. A small coastal indentation on the north shore of Prince Gustav Channel, between Chapel Hill and Church Point. The name, given by UK-APC, is descriptive of the only part of this coast which is sufficiently sheltered from the prevailing southwest winds to afford a reliable camp site. Chernopeev Peak.

Geographic entities mentioned:
surface_form: small
instance_of: Mountain
coordinates: lat: -70.5
lon: 64.7
surface_form: chapel hill
instance_of: Mountain
coordinates: lat: -63.68496
lon: -57.97586
A point west of Camp Hill. The feature was sighted by Swedish Antarctic Expedition (SwedAE) in 1903. It was surveyed by FIDS in 1945 and so named because the point rises to a rock peak high, the sides of which resemble a church steeple. Striped Hill. A small ice-free hill, high, standing near the south shore of Trinity Peninsula, east-northeast of Church Point. Charted and named by the FIDS, 1946.

Geographic entities mentioned:
surface_form: small
instance_of: Mountain
coordinates: lat: -70.5
lon: 64.7
Striped Hill. A small ice-free hill, high, standing near the south shore of Trinity Peninsula, east-northeast of Church Point. Charted and named by the FIDS, 1946. The descriptive name is derived from the stratifications on a small cliff on the seaward side of the hill. Botany Bay. A small bay between Church Point and Camp Hill on the south coast of Trinity Peninsula.

Geographic entities mentioned:
surface_form: small
instance_of: Mountain
coordinates: lat: -70.5
lon: 64.7
Charted and named by the FIDS, 1946. The descriptive name is derived from the stratifications on a small cliff on the seaward side of the hill. Botany Bay. A small bay between Church Point and Camp Hill on the south coast of Trinity Peninsula. Surveyed by FIDS, December 1946, and named by UK-APC from the fossil plants collected there. Camp Hill.

Geographic entities mentioned:
surface_form: small
instance_of: Mountain
coordinates: lat: -70.5
lon: 64.7
Botany Bay. A small bay between Church Point and Camp Hill on the south coast of Trinity Peninsula. Surveyed by FIDS, December 1946, and named by UK-APC from the fossil plants collected there. Camp Hill. Small ice-free hill, high, which lies east of Church Point. Charted in 1946 by the FIDS, who so named it because a geological camp was established at the foot of the hill. Kribul Hill.

Geographic entities mentioned:
surface_form: small
instance_of: Mountain
coordinates: lat: -70.5
lon: 64.7
Eyre Bay is to the northeast and Russell East Glacier is to the southwest. Features, from west to east, include Benz Pass, Panhard Nunatak, Levassor Nunatak, Chapel Hill, Shelter Cove, Church Point, Striped Hill, Camp Hill, McCalman Peak, Crystal Hill, Bald Head and Jade Point. Exploration and name.

Geographic entities mentioned:
surface_form: chapel hill
instance_of: Mountain
coordinates: lat: -63.68496
lon: -57.97586
surface_form: mccalman peak
instance_of: Mountain
coordinates: lat: -63.6167
lon: -57.7833
surface_form: levassor nunatak
instance_of: Mountain
coordinates: lat: -63.6667
lon: -58.1167
surface_form: panhard nunatak
instance_of: Mountain
coordinates: lat: -63.7
lon: -58.28333333
Named after the town of Bratsigovo in Southern Bulgaria. Central features. Features around Church Point include, from west to east,
Chapel Hill. A hill, high, forming the summit of a headland west-southwest of Church Point. Charted by the Falkland Islands Dependencies Survey (FIDS) in 1946, who so named it because of its proximity to Church Point. Shelter Cove.

Geographic entities mentioned:
surface_form: chapel hill
instance_of: Mountain
coordinates: lat: -63.68496
lon: -57.97586
Bratsigovo Hills. A chain of rocky hills rising to high and extending from the coast of Prince Gustav Channel northwards. Situated on the southeast side of Cugnot Ice Piedmont, west of Chernopeev Peak and east-northeast of Levassor Nunatak. Named after the town of Bratsigovo in Southern Bulgaria. Central features. Features around Church Point include, from west to east,
Chapel Hill.

Geographic entities mentioned:
surface_form: southern
instance_of: Mountain
coordinates: lat: -74.2
lon: -76.4667
Chernopeev Peak. A rocky peak rising to high on the southeast side of Cugnot Ice Piedmont, north of Church Point, east-northeast of Levassor Nunatak, south-southwest of Kribul Hill and southwest of McCalman Peak. Named after Hristo Chernopeev (1868-1915), a leader of the Bulgarian liberation movement in Macedonia. Church Point. A point west of Camp Hill.

Geographic entities mentioned:
surface_form: mccalman peak
instance_of: Mountain
coordinates: lat: -63.6167
lon: -57.7833
surface_form: levassor nunatak
instance_of: Mountain
coordinates: lat: -63.6667
lon: -58.1167
surface_form: cugnot ice piedmont
instance_of: Landform
coordinates: lat: -63.6333
lon: -58.1667
Named after the settlement of Kribul in Southwestern Bulgaria. Gornik Knoll. A rocky hill rising to high on Trinity Peninsula. Situated on the southeast side of Cugnot Ice Piedmont, west-southwest of McCalman Peak, east-northeast of Kribul Hill and south-southeast of Marten Crag. Named after the settlement of Gornik in Northern Bulgaria. McCalman Peak.

Geographic entities mentioned:
surface_form: mccalman peak
instance_of: Mountain
coordinates: lat: -63.6167
lon: -57.7833
surface_form: cugnot ice piedmont
instance_of: Landform
coordinates: lat: -63.6333
lon: -58.1667
Situated on the southeast side of Cugnot Ice Piedmont, west-southwest of McCalman Peak, east-northeast of Kribul Hill and south-southeast of Marten Crag. Named after the settlement of Gornik in Northern Bulgaria. McCalman Peak. The high summit of an east–west trending ridge north of Crystal Hill. Named by UK-APC for Donald McCalman, FIDS surveyor at Hope Bay, 1958-59. Crystal Hill.

Geographic entities mentioned:
surface_form: mccalman peak
instance_of: Mountain
coordinates: lat: -63.6167
lon: -57.7833
Zaldapa Ridge. A predominantly ice-free ridge extending in an east–west direction and wide on Yatrus Promontory. The ridge's twin rocky summits rise to and high respectively, with the higher western one situated east-northeast of McCalman Peak and west by south of Jade Point. Named after the ancient Thracian and Roman town of Zaldapa in Northeastern Bulgaria. Bald Head.

Geographic entities mentioned:
surface_form: mccalman peak
instance_of: Mountain
coordinates: lat: -63.6167
lon: -57.7833
Named after the settlements of Golyamo Chochoveni and Malko Chochoveni in Southeastern Bulgaria. Kolobar Nunatak. A rocky hill rising to high in the southwest part of Cugnot Ice Piedmont. Situated northeast of Panhard Nunatak, southeast of Chochoveni Nunatak and southwest of Levassor Nunatak. Named after the settlement of Kolobar in Northeastern Bulgaria. Levassor Nunatak.

Geographic entities mentioned:
surface_form: levassor nunatak
instance_of: Mountain
coordinates: lat: -63.6667
lon: -58.1167
surface_form: panhard nunatak
instance_of: Mountain
coordinates: lat: -63.7
lon: -58.28333333
A rocky hill rising to high in the southwest part of Cugnot Ice Piedmont. Situated northeast of Panhard Nunatak, southeast of Chochoveni Nunatak and southwest of Levassor Nunatak. Named after the settlement of Kolobar in Northeastern Bulgaria. Levassor Nunatak. A conspicuous horseshoe-shaped nunatak inland in the middle of Cugnot Ice Piedmont. Mapped from surveys by FIDS (1960-61).

Geographic entities mentioned:
surface_form: levassor nunatak
instance_of: Mountain
coordinates: lat: -63.6667
lon: -58.1167
Bratsigovo Hills. A chain of rocky hills rising to high and extending from the coast of Prince Gustav Channel northwards. Situated on the southeast side of Cugnot Ice Piedmont, west of Chernopeev Peak and east-northeast of Levassor Nunatak. Named after the town of Bratsigovo in Southern Bulgaria. Central features. Features around Church Point include, from west to east,
Chapel Hill.

Geographic entities mentioned:
surface_form: levassor nunatak
instance_of: Mountain
coordinates: lat: -63.6667
lon: -58.1167
surface_form: cugnot ice piedmont
instance_of: Landform
coordinates: lat: -63.6333
lon: -58.1667
Cugnot Ice Piedmont. Cugnot Ice Piedmont () is an ice piedmont in Trinity Peninsula, Antarctica. It is about long and between wide, extending from Russell East Glacier to Eyrie Bay and bounded on the landward side by Louis Philippe Plateau. Location. Cugnot Ice Piedmont is in Graham Land in the center of the south coast of the Trinity Peninsula, which forms the tip of the Antarctic Peninsula.

Geographic entities mentioned:
surface_form: cugnot ice piedmont
instance_of: Landform
coordinates: lat: -63.6333
lon: -58.1667
Location. Cugnot Ice Piedmont is in Graham Land in the center of the south coast of the Trinity Peninsula, which forms the tip of the Antarctic Peninsula. It is on the coast of the Prince Gustav Channel to the south of the Louis Philippe Plateau and Broad Valley. Eyre Bay is to the northeast and Russell East Glacier is to the southwest.

Geographic entities mentioned:
surface_form: cugnot ice piedmont
instance_of: Landform
coordinates: lat: -63.6333
lon: -58.1667
Exploration and name. Cugnot Ice Piedmont was mapped from surveys by the Falkland Islands Dependencies Survey (FIDS; 1960–61), and was named by the UK Antarctic Place-Names Committee (UK-APC) for Nicolas-Joseph Cugnot (1725-1804), a French military engineer who designed and built the first full-sized vehicle propelled by its own engine (steam), in 1769. Western features.

Geographic entities mentioned:
surface_form: cugnot ice piedmont
instance_of: Landform
coordinates: lat: -63.6333
lon: -58.1667
Western features. Features of the west part of the ice piedmont include, from west to east,
Chochoveni Nunatak. A rocky hill rising to high in the southwest part of Cugnot Ice Piedmont. Situated south by east of Smin Peak, northwest of Kolobar Nunatak, northeast of Coburg Peak and east of Drenta Bluff. Named after the settlements of Golyamo Chochoveni and Malko Chochoveni in Southeastern Bulgaria.

Geographic entities mentioned:
surface_form: cugnot ice piedmont
instance_of: Landform
coordinates: lat: -63.6333
lon: -58.1667
Named after the settlements of Golyamo Chochoveni and Malko Chochoveni in Southeastern Bulgaria. Kolobar Nunatak. A rocky hill rising to high in the southwest part of Cugnot Ice Piedmont. Situated northeast of Panhard Nunatak, southeast of Chochoveni Nunatak and southwest of Levassor Nunatak. Named after the settlement of Kolobar in Northeastern Bulgaria. Levassor Nunatak.

Geographic entities mentioned:
surface_form: cugnot ice piedmont
instance_of: Landform
coordinates: lat: -63.6333
lon: -58.1667
A rocky hill rising to high in the southwest part of Cugnot Ice Piedmont. Situated northeast of Panhard Nunatak, southeast of Chochoveni Nunatak and southwest of Levassor Nunatak. Named after the settlement of Kolobar in Northeastern Bulgaria. Levassor Nunatak. A conspicuous horseshoe-shaped nunatak inland in the middle of Cugnot Ice Piedmont. Mapped from surveys by FIDS (1960-61).

Geographic entities mentioned:
surface_form: cugnot ice piedmont
instance_of: Landform
coordinates: lat: -63.6333
lon: -58.1667
Charted in 1946 by the FIDS, who so named it because a geological camp was established at the foot of the hill. Kribul Hill. A rocky hill rising to high on Trinity Peninsula. Situated on the southeast side of Cugnot Ice Piedmont, west-southwest of Gornik Knoll, north of Church Point and south by west of Marten Crag. Named after the settlement of Kribul in Southwestern Bulgaria. Gornik Knoll.

Geographic entities mentioned:
surface_form: cugnot ice piedmont
instance_of: Landform
coordinates: lat: -63.6333
lon: -58.1667
Church Point. A point west of Camp Hill. The feature was sighted by Swedish Antarctic Expedition (SwedAE) in 1903. It was surveyed by FIDS in 1945 and so named because the point rises to a rock peak high, the sides of which resemble a church steeple. Striped Hill. A small ice-free hill, high, standing near the south shore of Trinity Peninsula, east-northeast of Church Point.

Geographic entities mentioned:
surface_form: steeple
instance_of: Mountain
coordinates: lat: -63.4333
lon: -57.05
Ammaiyar Image in Cambodia. Banteay Srei or Banteay Srey () is a 10th-century Cambodian temple dedicated to the Hindu god Shiva. Located in the area of Angkor, it lies near the hill of Phnom Dei, north-east of the main group of temples that once belonged to the medieval capitals of Yasodharapura and Angkor Thom. The second enclosure.

Geographic entities mentioned:
surface_form: Phnom Dei
instance_of: Mountain
countries: Cambodia
coordinates: lat: 13.59583333
lon: 103.98361111
It was incorporated as Ridgeley on November 28, 1914, named for the former owners of the land upon which the town was built. Geography. Ridgeley is located along the North Branch of the Potomac River, opposite Cumberland, Maryland. According to the United States Census Bureau, the town has a total area of, of which is land and is water. Transportation.

Geographic entities mentioned:
surface_form: North Branch of the Potomac River
instance_of: Watercourse
countries: United States
coordinates: lat: 39.5284255
lon: -78.5875141
Music. Bosnian roots music came from Middle Bosnia, Posavina, the Drina valley and Kalesija. It is usually performed by singers with two violinists and a šargija player. These bands first appeared around World War I and became popular in the 1960s. This is the third oldest music following after the sevdalinka and ilahija.

Geographic entities mentioned:
surface_form: Posavina
instance_of: Valley
countries: Croatia
Bosnia and Herzegovina
Serbia
coordinates: lat: 45.16667
lon: 17.33333
Abkhazian villages are concentrated around the cities of Adapazarı, Düzce, Sinop, Hendek and Samsun in the northern part, and in the west around cities such as Bilecik, Inegöl and Eskişehir; they are mainly found in the provinces of Sakarya and Bolu in the western part, and near the Çoruh river in the north-east.

Geographic entities mentioned:
surface_form: Çoruh
instance_of: Watercourse
countries: Turkey
Georgia
coordinates: lat: 40.3074
lon: 40.9997
Route description. VT 36 begins at an intersection with VT 78 in the village of Swanton, two blocks from VT 78's intersection with U.S. Route 7. VT 36 runs south along the eastern edge of Lake Champlain for approximately, then turns eastward towards the city of St. Albans.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
Viterra, the monopoly grain handler in South Australia, progressively closed most silos served by the Murraylands lines, resulting in rail haulage ending in the period 2002–2015. Viterra also moved to road transport on the Eyre Peninsula in 2019, resulting in the peninsula network becoming dormant except for the gypsum haulage line from Lake MacDonnell to the port of Thevenard near Ceduna.

Geographic entities mentioned:
surface_form: Lake MacDonnell
instance_of: Lake
countries: Australia
coordinates: lat: -32.04138889
lon: 133.0025
Aitoliko Lagoon. The Aitoliko Lagoon (&quot;Limnothalassa Aitolikou&quot;) is a lagoon located in the south of Aetolia-Acarnania, Greece. It is separated from the larger Missolonghi Lagoon (a bay of the Gulf of Patras) to the south by the island of Aitoliko, but together they form the Missolonghi–Aitoliko Lagoons complex. Its maximum depth is 28 metres.

Geographic entities mentioned:
surface_form: Missolonghi Lagoon
instance_of: Lake
countries: Greece
coordinates: lat: 38.35
lon: 21.366666666667
surface_form: missolonghi lagoon
instance_of: Lake
countries: Greece
coordinates: lat: 38.35
lon: 21.366666666667
Aitoliko Lagoon. The Aitoliko Lagoon (&quot;Limnothalassa Aitolikou&quot;) is a lagoon located in the south of Aetolia-Acarnania, Greece. It is separated from the larger Missolonghi Lagoon (a bay of the Gulf of Patras) to the south by the island of Aitoliko, but together they form the Missolonghi–Aitoliko Lagoons complex. Its maximum depth is 28 metres.

Geographic entities mentioned:
surface_form: aitoliko lagoon
instance_of: Lake
countries: Greece
coordinates: lat: 38.4677
lon: 21.333
Its maximum depth is 28 metres. At a salinity of 19-28 PSU, its water is brackish. Oxygen depletion occurs in a large part of the lagoon, but has been reduced since 2002 by creating larger openings around Aitoliko island and dredging channels in Messolongi Lagoon. The main settlement on the lagoon is the town Aitoliko.

Geographic entities mentioned:
surface_form: messolongi lagoon
instance_of: Lake
countries: Greece
coordinates: lat: 38.35
lon: 21.366666666667
Among their children was Logan Fontenelle. Early in his career Fontenelle was involved in fur trading into the Rocky Mountains. However starting in the late 1820s he was in command at Fontenelle's Post in what would become Bellevue, Nebraska, along the Missouri River. In 1831 he led a trading expedition to the Cache Valley of Utah and Idaho with Andrew Drips. On their return to St.

Geographic entities mentioned:
surface_form: Cache Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.816666666667
lon: -111.93416666667
Early life. As a boy, Sepass accompanied his tribe north into the Fraser Canyon which was experiencing the Cariboo Gold Rush. His father built and operated a cedar log freight canoe to transport miners and supplies across Chilliwack Lake near the US/Canada border. His maternal grandfather was a chief from further north on the Thompson River.

Geographic entities mentioned:
surface_form: Chilliwack Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.05694444444445
lon: -121.41388888888889
The Mohawk, also known by their own name, (), are an Indigenous people of North America and the easternmost nation of the Haudenosaunee, or Iroquois Confederacy (also known as the Five Nations or later the Six Nations). Mohawk are an Iroquoian-speaking people with communities in southeastern Canada and northern New York State, primarily around Lake Ontario and the St. Lawrence River.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Brant continued as a political leader of the Mohawks for the rest of his life. This land extended 100 miles from the head of the Grand River to the head of Lake Erie where it discharges. Another Mohawk war chief, John Deseronto, led a group of Mohawk to the Bay of Quinte.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Also, in Eastern Christianity monastery libraries kept important manuscripts. The most important of them were the ones in the monasteries of Mount Athos for Orthodox Christians, and the library of the Saint Catherine's Monastery in the Sinai Peninsula, Egypt for the Coptic Church. A special case is constituted by the Jewish medieval libraries.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
Ramsjön, Haninge Municipality. Ramsjön is a lake in Stockholm County, Södermanland, Sweden.

Geographic entities mentioned:
surface_form: ramsjön, haninge municipality
instance_of: Lake
countries: Sweden
coordinates: lat: 59.183333333333
lon: 18.2
Ramsjön, Haninge Municipality. Ramsjön is a lake in Stockholm County, Södermanland, Sweden.

Geographic entities mentioned:
surface_form: ramsjön
instance_of: Lake
countries: Sweden
coordinates: lat: 59.183333333333
lon: 18.2
Pedra Furada (Santa Catarina). Pedra Furada (, literally &quot;Drilled Stone&quot;) is a naturally formed rock arch located in the municipality of Urubici, state of Santa Catarina, Southern Brazil. It can be spotted from the summit of a mountain named Morro da Igreja.

Geographic entities mentioned:
surface_form: Morro da Igreja
instance_of: Mountain
countries: Brazil
coordinates: lat: -28.125
lon: -49.474444444444
In July 2017, the Italian Alpine Club set a Guinness World Record for the world's longest &quot;static&quot; rope team when 2,846 climbers were connected to a single rope in Bergamo in Italy. In 2022, eighty female mountaineers set a record for the world's longest women's &quot;climbing&quot; rope team by summiting the Breithorn.

Geographic entities mentioned:
surface_form: Breithorn
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.941111111111
lon: 7.7472222222222
It is native primarily to high elevations in the Sierra Nevada from Nevada County to Tulare County, where it is a plant of the alpine climate. Additional populations occur on Lassen Peak in Lassen County, and also in Washoe County, Nevada. Description. &quot;Antennaria pulchella&quot; is a small, mat-forming perennial herb growing a patch of woolly grayish leaves dotted with purplish glands.

Geographic entities mentioned:
surface_form: Lassen Peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.488055555555555
lon: -121.505
On 1 October 1702 Dillon was promoted to brigadier. In 1703 Vendôme tried to effect a junction with the Bavarians, allied with the French against Austria, through the Tyrol and penetrated as far as Trent. Dillon took the town of Riva at the northern tip of Lake Garda. However, on 13 August 1704 Marlborough and Eugene beat the French and Bavarians at Blenheim.

Geographic entities mentioned:
surface_form: Lake Garda
instance_of: Lake
countries: Italy
coordinates: lat: 45.633333333333
lon: 10.666666666667
Doda Lake extends into the townships of Gradis, Machault, Du Guesglin and Royal. Forestry is the main economic activity of the sector. Recreational tourism activities come second with a navigable body of water of, including Father Lake (on southeast) and Françoise Lake (on north-west). The latter is formed by an enlargement of the Opawica River and has a dam built at its mouth.

Geographic entities mentioned:
surface_form: françoise lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.458888888889
lon: -75.305277777778
surface_form: father lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.311388888889
lon: -75.473888888889
The latter is formed by an enlargement of the Opawica River and has a dam built at its mouth. The Doda Lake hydrographic slope is accessible via the R1051 Forest Road from the North, then branches off to the east to serve the peninsula (extending eastward on the separating the Father Lake and Doda Lake.

Geographic entities mentioned:
surface_form: father lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.311388888889
lon: -75.473888888889
surface_form: doda lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.40111111
lon: -75.19444444
surface_form: doda lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.40111111
lon: -75.19444444
Toponymy. Father Lake and Doda Lake (area of) appear to be two twins, having been considered as one entity by explorers. In the past, a large forest camp has been set up on its shores, where a depot has already welcomed teams of loggers and log drivers. An outfitter is operating for recreational and tourism activities including hunting and fishing.

Geographic entities mentioned:
surface_form: father lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.311388888889
lon: -75.473888888889
surface_form: doda lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.40111111
lon: -75.19444444
Doda Lake. Doda Lake is a freshwater body of the southern part of Eeyou Istchee James Bay (municipality), in the administrative region of Nord-du-Québec, in the province of Quebec, in Canada. Doda Lake extends into the townships of Gradis, Machault, Du Guesglin and Royal. Forestry is the main economic activity of the sector.

Geographic entities mentioned:
surface_form: doda lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.40111111
lon: -75.19444444
The Doda Lake hydrographic slope is accessible via the R1051 Forest Road from the North, then branches off to the east to serve the peninsula (extending eastward on the separating the Father Lake and Doda Lake. The surface of Doda Lake is generally frozen from early December November to mid-May, however safe ice movement is generally from mid-November to mid-April. Toponymy.

Geographic entities mentioned:
surface_form: doda lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.40111111
lon: -75.19444444
Since December 2022, the Limmattal light rail line (route 20) terminates at &quot;Bahnhof Altstetten&quot; station. The light rail line has its own platforms, across the station plaza from platform two of the S-Bahn services. This service, operated by AVA, runs through the Limmat Valley region and connects to the Zürich tram network at Farbhof, just to the west of Altstetten station.

Geographic entities mentioned:
surface_form: Limmat Valley
instance_of: Valley
countries: Switzerland
coordinates: lat: 47.5
lon: 8.25
The 1969 La Paz Lloyd Aéreo Boliviano Douglas DC-6 crash, also known as the Viloco tragedy, was an accident involving a Douglas DC-6B of the Bolivian airline Lloyd Aéreo Boliviano that collided with Mount Choquetanga, 176 km (110 miles) southeast of La Paz, Bolivia, on 26 September 1969, killing all 74 people on board, including 17 members of a Bolivian association football team named The Strongest.

Geographic entities mentioned:
surface_form: Mount Choquetanga
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.30694444
lon: -67.96194444
The flight was under the command of Captain Teddy Scott Villa, age 39, First Officer Alberto Estrugo, 31, and Radio Operator Germán Guzmán, with flight attendants Carlos Fiorilo and Rosario Vergara in the cabin. Around 3.10pm while cruising at an altitude of
, the plane crashed into a slope of Mount Choquetanga, 176 km (110 miles) southeast of La Paz, Bolivia.

Geographic entities mentioned:
surface_form: Mount Choquetanga
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.30694444
lon: -67.96194444
The wider region extends into parts of northern Telangana, Andhra Pradesh, western Odisha and southern Uttar Pradesh. The region is part of the northern Deccan plateau, with an average height of about 600&ndash;700 metres. Geologically, it is mostly Precambrian rock, with some areas of Permian and Triassic age.

Geographic entities mentioned:
surface_form: Deccan plateau
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
This creates demand for building work and service industry. Less central to the economy, but still noteworthy is the spectacle manufacturing industry. Many employed by this commute to the Veneto region (particularly the Cadore area) where many of the world's major spectacle manufacturers are based.

Geographic entities mentioned:
surface_form: Cadore
instance_of: Valley
countries: Italy
coordinates: lat: 46.50916667
lon: 12.35722222
The river leaves the lake at the northeast over a dam and continues southeast, passes from Unorganized South Nipissing District into the geographic Dickens Township in the municipality of South Algonquin, passes through a series of rapids, takes in the left tributary Aylen River, turns southwest, and empties into Bark Lake on the Madawaska River, at the Ontario Highway 60 bridge and east of the community of Madawaska.

Geographic entities mentioned:
surface_form: Bark Lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.45
lon: -77.8333
Games venue. The main stadium was at Eden Park. Other venues were the Auckland Town Hall (boxing and wrestling), the Drill Hall (fencing), Western Springs (cycling and the closing ceremony) Lake Karapiro (rowing), and the Newmarket Olympic Pool (swimming). Accommodation was at the Ardmore Teachers' Training College, away at South Auckland.

Geographic entities mentioned:
surface_form: Lake Karapiro
instance_of: Lake
countries: New Zealand
coordinates: lat: -37.943167
lon: 175.560833
Medals by country. At the 1950 British Empire Games all the teams won at least one medal. Rowing. All events were for men only. The events were held at Lake Karapiro, south of Auckland. Three special trains took 1500 people to Cambridge on 7 February 1950. Water polo. Water polo was contested by men's teams only, with New Zealand and Australia the only two teams entered.

Geographic entities mentioned:
surface_form: Lake Karapiro
instance_of: Lake
countries: New Zealand
coordinates: lat: -37.943167
lon: 175.560833
The current of the [Opawica River] flows through this lake on, almost its full length. Bras Coupé Lake has many bays, peninsulas and islands. The Opawica River crosses this set of water bodies, the main ones being &quot;Du Bras Coupé Lake&quot;, Bay Lake, Rane Lake, Lac des Vents, the Irene Lake, Caopatina Lake and its tributary, the Surprise Lake.

Geographic entities mentioned:
surface_form: Irene Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.541944444444
lon: -74.761388888889
surface_form: Caopatina Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.447777777778
lon: -74.765
surface_form: lac des vents
instance_of: Lake
countries: Canada
coordinates: lat: 49.476944444444
lon: -74.870555555556
surface_form: irene lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.541944444444
lon: -74.761388888889
surface_form: caopatina lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.447777777778
lon: -74.765
surface_form: bras coupé lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.561111111111
lon: -74.943888888889
surface_form: surprise lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.14528
lon: -125.56639
Toponymy. This hydronym was formalized in 1935 by the Quebec Geography Committee. This name reflects the particular shape of this river arm intersected by four large peninsulas downstream of the Lac des Vents. The toponym &quot;Lac Du Bras Coupé&quot; was formalized on December 5, 1968, by the Commission de toponymie du Québec, when it was created.

Geographic entities mentioned:
surface_form: lac des vents
instance_of: Lake
countries: Canada
coordinates: lat: 49.476944444444
lon: -74.870555555556
Lake Du Bras Coupé gets its supply on the north-west side by the Denning Lake outlet and Lescure Lake outlet; to the northeast by the Lac Gantier outlet and the Lac Sébastien outlet; to the south, by the outlet of Lake Bernard. Toponymy. This hydronym was formalized in 1935 by the Quebec Geography Committee.

Geographic entities mentioned:
surface_form: lake bernard
instance_of: Lake
countries: Canada
coordinates: lat: 45.7333
lon: -79.3833
Bras Coupé Lake. The Bras Coupé Lake (French: &quot;Lac du Bras Coupé&quot;) is a freshwater body of the southern part of Eeyou Istchee James Bay (municipality), in the administrative region of Nord-du-Québec, in the province of Quebec, in Canada.

Geographic entities mentioned:
surface_form: bras coupé lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.561111111111
lon: -74.943888888889
Bras Coupé Lake. The Bras Coupé Lake (French: &quot;Lac du Bras Coupé&quot;) is a freshwater body of the southern part of Eeyou Istchee James Bay (municipality), in the administrative region of Nord-du-Québec, in the province of Quebec, in Canada.

Geographic entities mentioned:
surface_form: bras coupé lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.561111111111
lon: -74.943888888889
surface_form: lac du bras coupé
instance_of: Lake
countries: Canada
coordinates: lat: 49.561111111111
lon: -74.943888888889
The area of Bras Coupé Lake extends entirely into the townships of Lescure, in the territory of the Eeyou Istchee James Bay (municipality) regional government, south of Chapais, Quebec. Forestry is the main economic activity of the sector. Recreational tourism activities come second, thanks to a navigable body of water with a length of (the full length of the lake).

Geographic entities mentioned:
surface_form: bras coupé lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.561111111111
lon: -74.943888888889
Geography. Formed by an enlargement of the Opawica River, the &quot;Bras Coupé Lake&quot; is shaped like a horseshoe open to the Southwest (the top of the inverted U is leaning eastward); this lake includes a peninsula attached to the south side of the lake and stretching on to the north-east.

Geographic entities mentioned:
surface_form: bras coupé lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.561111111111
lon: -74.943888888889
In parallel on the South-East side, a peninsula stretching out on the South-West bounds the eastern arm of the Lac du Bras Coupé and the Lac de la Baie. Another peninsula stretching south-west parallel to the previous peninsula on from the north-east delimits the Bay Lake and Rane.

Geographic entities mentioned:
surface_form: lac du bras coupé
instance_of: Lake
countries: Canada
coordinates: lat: 49.561111111111
lon: -74.943888888889
Downstream from the town of Provadia the river forms a large arch bulging south, then turns north and finally northeast, before emptying in Lake Beloslav some 2.6 km northeast of the village of Razdelna. The lake is connected to Lake Varna, which is itself linked with the Black Sea via a navigable channel.

Geographic entities mentioned:
surface_form: Lake Beloslav
instance_of: Lake
countries: Bulgaria
coordinates: lat: 43.18777778
lon: 27.7
Downstream from the town of Provadia the river forms a large arch bulging south, then turns north and finally northeast, before emptying in Lake Beloslav some 2.6 km northeast of the village of Razdelna. The lake is connected to Lake Varna, which is itself linked with the Black Sea via a navigable channel.

Geographic entities mentioned:
surface_form: Lake Varna
instance_of: Lake
countries: Bulgaria
coordinates: lat: 43.190277777778
lon: 27.825
Polabian Slavs. Polabian Slavs, also known as Elbe Slavs
and more broadly as Wends, is a collective term applied to a number of Lechitic (West Slavic) tribes who lived scattered along the Elbe river in what is today eastern Germany.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221