Sarmila/GeoWiki-Features huggingface dataset:
History. The original homeland of Proto-South-Cushitic was in southwestern Ethiopia. South Cushitic speakers then migrated south to Lake Turkana in northern Kenya by 3000 BC and further south, entering northern Tanzania in 2000 BC. The speakers of South Cushitic were likely the first peoples to introduce agriculture and pastoralism in the lands east of Lake Victoria.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
Alavaipatti. Alavaipatti is a village panchayat located in the Namakkal district of Tamil Nadu state, India. Alavaimalai. Alavaiptti name is derived from Alavaimalai A temple to lord Murugan is located halfway up the hill, so the hill name is arai (half) vazhi (way) malai (hill), or Alavaimalai. Geography.

Geographic entities mentioned:
surface_form: Alavaimalai
instance_of: Mountain
countries: India
coordinates: lat: 11.46963889
lon: 78.11952778
Territory. Carantania's capital was most likely Karnburg () in the Zollfeld Field (), north of modern-day town of Klagenfurt (). The principality was centered in the area of modern Carinthia, and included territories of modern Styria, most of today's East Tyrol and of the Puster Valley, the Lungau and Ennspongau regions of Salzburg, and parts of southern Upper Austria and Lower Austria.

Geographic entities mentioned:
surface_form: Puster Valley
instance_of: Valley
countries: Italy
Austria
coordinates: lat: 46.7405
lon: 12.369555555555555
Course. The Ekwan drainage basin lies between and is enveloped by the larger ones of neighbouring rivers, the Winisk River on the north and the Attawapiskat River on the south. The source of the river is Zumar Lake at an elevation of, just northeast of part of the North Channel outlet from Attawapiskat Lake, the source of the Attawapiskat River.

Geographic entities mentioned:
surface_form: Zumar Lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.3417
lon: -87.2042
surface_form: Attawapiskat Lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.2375
lon: -87.87638888888888
Carapace Nunatak. Carapace Nunatak () is a prominent isolated nunatak, the most westerly near the head of Mackay Glacier in Victoria Land, standing southwest of Mount Brooke where it is visible for a considerable distance from many directions.

Geographic entities mentioned:
surface_form: Mount Brooke
instance_of: Mountain
coordinates: lat: -76.8167
lon: 159.9
surface_form: carapace nunatak
instance_of: Mountain
coordinates: lat: -76.8833
lon: 159.4
Associated macrofossils include notostracan branchiopods, ostracodes, insect nymphs and wings, and plant leaves. Macroscopic trace fossils are extremely rare. The lake cherts from the upper part of Carapace Sandstone contain an abundance of fusainized plant material and animal remains. This fine-grained Magadi-type chert preserves abundant plant fossils.

Geographic entities mentioned:
surface_form: Magadi-type chert
instance_of: Lake
countries: Kenya
coordinates: lat: -1.8666666666667
lon: 36.266666666667
The base of the Carapace Sandstone is not exposed. The Carapace Nunatak is the type locality for the Carapace Sandstone. Conformably overlying the Carapace Sandstone is of Kirkpatrick Basalt. The basalt lava flows include a thick layer of hyaloclastite breccia with beds of pillow lava at its base. About above its base, a thick layer of volcanic breccia lies sandwiched between basaltic lava flows.

Geographic entities mentioned:
surface_form: kirkpatrick
instance_of: Mountain
coordinates: lat: -84.333333333333
lon: 166.41666666667
About above its base, a thick layer of volcanic breccia lies sandwiched between basaltic lava flows. The lava flows exhibit columnar jointing and, at the base of the Kirkpatrick Basalt, contain with very large (up to thick) xenoliths (&quot;rafts&quot;) of fossiliferous, laminated siltstone and chert. The upper surface of the Kirkpatrick Basalt has been long since removed by erosion. Fossils.

Geographic entities mentioned:
surface_form: kirkpatrick
instance_of: Mountain
coordinates: lat: -84.333333333333
lon: 166.41666666667
It was so named by the New Zealand party of the Commonwealth Trans-Antarctic Expedition (1956–1958) because of the fossil carapaces of small crustaceans found in the exposed rocks. Geology. The Carapace Nunatak is an erosional outlier of Jurassic strata, which consists of about of the Ferrar Group.

Geographic entities mentioned:
surface_form: small
instance_of: Mountain
coordinates: lat: -70.5
lon: 64.7
In the laminated, and silicified, fine-grained lake deposits of Carapace Sandstone, fossil conchostracans (clam shrimp) are the most important in terms of number of individuals and distribution. They consist of small, bivalved spinicaudatan arthropods. They are most typical of ephemeral, alkaline ponds.

Geographic entities mentioned:
surface_form: small
instance_of: Mountain
coordinates: lat: -70.5
lon: 64.7
Carapace Nunatak. Carapace Nunatak () is a prominent isolated nunatak, the most westerly near the head of Mackay Glacier in Victoria Land, standing southwest of Mount Brooke where it is visible for a considerable distance from many directions.

Geographic entities mentioned:
surface_form: carapace nunatak
instance_of: Mountain
coordinates: lat: -76.8833
lon: 159.4
Geology. The Carapace Nunatak is an erosional outlier of Jurassic strata, which consists of about of the Ferrar Group. The exact thickness is unknown because the strata is broken up by faults and discontinuous glacial moraines conceal the underlying Jurassic strata. At the base of Carapace Nunatak, about of cross-bedded sandstones and fine lithic conglomerates of the Carapace Sandstone outcrops.

Geographic entities mentioned:
surface_form: carapace nunatak
instance_of: Mountain
coordinates: lat: -76.8833
lon: 159.4
The exact thickness is unknown because the strata is broken up by faults and discontinuous glacial moraines conceal the underlying Jurassic strata. At the base of Carapace Nunatak, about of cross-bedded sandstones and fine lithic conglomerates of the Carapace Sandstone outcrops. The gravel fraction of the fine conglomerates consists of pebbles of coal, granite, greywacke, and weathered basalt.

Geographic entities mentioned:
surface_form: carapace nunatak
instance_of: Mountain
coordinates: lat: -76.8833
lon: 159.4
The uppermost contains beds of laminated and fossiliferous beds of mudstone, siltstone, and chert. The base of the Carapace Sandstone is not exposed. The Carapace Nunatak is the type locality for the Carapace Sandstone. Conformably overlying the Carapace Sandstone is of Kirkpatrick Basalt. The basalt lava flows include a thick layer of hyaloclastite breccia with beds of pillow lava at its base.

Geographic entities mentioned:
surface_form: carapace nunatak
instance_of: Mountain
coordinates: lat: -76.8833
lon: 159.4
Fossils. The fossiliferous horizons of the Ferrar Group at Carapace Nunatak contain one of the richest and most diverse freshwater Jurassic paleobiota known from Antarctica. Not only are these fossils diverse, except for poorly preserved petrified wood, the fossils found at Carapace Nunatak are remarkably well preserved to the extent that their source is referred to as a Lagerstätten.

Geographic entities mentioned:
surface_form: carapace nunatak
instance_of: Mountain
coordinates: lat: -76.8833
lon: 159.4
At the base of Carapace Nunatak, about of cross-bedded sandstones and fine lithic conglomerates of the Carapace Sandstone outcrops. The gravel fraction of the fine conglomerates consists of pebbles of coal, granite, greywacke, and weathered basalt. Some beds contain volcanic debris. The uppermost contains beds of laminated and fossiliferous beds of mudstone, siltstone, and chert.

Geographic entities mentioned:
surface_form: coal
instance_of: Mountain
coordinates: lat: -72.1167
lon: -68.5333
Pallavaram Lake. Pallavaram Lake, also known as Periya aeri (Big lake) or Pallavaram aeri, is situated along Pallavaram Thuraipakkam Radial Road. It used to be a large lake, but it dried up and was polluted by industrial wastewater and garbage. A burial site remains and is used for burial rites. Ecological impact.

Geographic entities mentioned:
surface_form: pallavaram lake
instance_of: Lake
countries: India
coordinates: lat: 12.95853611
lon: 80.15158333
The village has 33 homes, including eight riverfront homes. The residential streets are: Third Street, Aspinwall Avenue, Gannet Plaza Avenue, Friendship Place, Ernest Sand Road, 2nd Street, Turner Road, and Byham Road. Rotary Park at Suntree. A community river park is situated at the junction of Suntree Boulevard and U.S. Route 1, on the shore of the Indian River Lagoon.

Geographic entities mentioned:
surface_form: Indian River Lagoon
instance_of: Body of water
countries: United States
coordinates: lat: 28.05527778
lon: -80.57611111
Route numbering controversy. After the acquisition of CTB by Chow Tai Fook, NWFB's mother company, the rearrangement of bus services lead to a proposal of merger of the route with 5A, which ran between Happy Valley (Lower) and Felix Villas. Such a amalgamation was mooted as early as 1986 when the routes were still operated by CMB, but had never been approved well until 2004.

Geographic entities mentioned:
surface_form: Felix Villas
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.277
lon: 114.125
He did not arrive in time for the main address, but is recorded as saying that he &quot;had never known a man whose talents and position were so freely and distinctly sacrificed for the public good&quot;. He is also said to have remained physically fit into old age, climbing Snaefell at the age of eighty-five and dying the following year after a short illness.

Geographic entities mentioned:
surface_form: Snaefell
instance_of: Mountain
countries: Isle of Man
coordinates: lat: 54.263288
lon: -4.461618
Tables are arranged end-to-end to resemble a single long table, curved to match the features of the local landscape. Denevan sometimes also creates a site-specific piece of ephemeral art near the tables. In addition to farms, Outstanding in the Field events have been held in places including Jackson Hole, Chicago, and Coachella Valley Music and Arts Festival. Experience.

Geographic entities mentioned:
surface_form: Jackson Hole
instance_of: Valley
countries: United States
coordinates: lat: 43.516666666667
lon: -110.83333333333
Mountaineering. In addition to being a footballer, Pember was a keen outdoorsman. He successfully climbed Mont Blanc in August 1863, and would go on to describe his experience on the mountain in public lectures. Journalist. In 1868, Pember emigrated with his wife and two sons to New York, where he started a new career as a journalist.

Geographic entities mentioned:
surface_form: Mont Blanc
instance_of: Mountain
countries: France
Italy
coordinates: lat: 45.83277777777778
lon: 6.865
The daughter was also known as Pero. The island of Mykonos was also said to have been the location of the &quot;Gigantomachy&quot;, the great battle between Zeus and Giants and where Hercules killed the invincible giants having lured them from the protection of Mount Olympus. According to myth, the large rocks all over the island are said to be the petrified corpses of the giants.

Geographic entities mentioned:
surface_form: Mount Olympus
instance_of: Mountain
countries: Greece
coordinates: lat: 40.083333333333336
lon: 22.35
Terry Peak is a mountain and ski area in the west central United States, in the Black Hills of South Dakota outside of Lead. With an elevation of above sea level, it is the most prominent peak in the Northern Black Hills area, and the sixth highest summit in the range; the tallest is Black Elk Peak (formerly Harney Peak) at. The mountain was named for Alfred Howe Terry, who had explored the area.

Geographic entities mentioned:
surface_form: Black Elk Peak
instance_of: Mountain
countries: United States
coordinates: lat: 43.871666666667
lon: -103.53166666667
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 46.99
lon: -123.14
surface_form: elk peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.0243
lon: -115.037
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 43.1693
lon: -120.68
surface_form: harney peak
instance_of: Mountain
countries: United States
coordinates: lat: 43.871666666667
lon: -103.53166666667
The mountain was named for Alfred Howe Terry, who had explored the area. It was first used as a ski area in 1936 by the Bald Mountain Ski Club when a rope tow was installed. The first chair lift was installed in 1952 and began operation in 1954. The ski area has since seen many upgrades in chair lifts, trails, and accommodations.

Geographic entities mentioned:
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.655
lon: -114.409
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 46.8827026
lon: -88.0390147
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.8822
lon: -123.866
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.6611024
lon: -107.4103338
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.4291
lon: -75.7503
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.6988
lon: -110.902
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.021388888889
lon: -75.190833333333
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.5344
lon: -119.115
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.423611111111
lon: -74.593888888889
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.1209
lon: -74.2001
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.902777777778
lon: -74.724444444444
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.4439
lon: -105.969
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.7386
lon: -74.9129
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.294722222222
lon: -74.387777777778
Terry Peak. Terry Peak is a mountain and ski area in the west central United States, in the Black Hills of South Dakota outside of Lead. With an elevation of above sea level, it is the most prominent peak in the Northern Black Hills area, and the sixth highest summit in the range; the tallest is Black Elk Peak (formerly Harney Peak) at.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 46.99
lon: -123.14
surface_form: terry peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.329
lon: -103.835
surface_form: black hills
instance_of: Landform
countries: United States
coordinates: lat: 43.1693
lon: -120.68
Terry Peak. Terry Peak is a mountain and ski area in the west central United States, in the Black Hills of South Dakota outside of Lead. With an elevation of above sea level, it is the most prominent peak in the Northern Black Hills area, and the sixth highest summit in the range; the tallest is Black Elk Peak (formerly Harney Peak) at.

Geographic entities mentioned:
surface_form: terry peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.329
lon: -103.835
Grovatnet. Grovatnet is a lake that lies in Sørfold Municipality in Nordland county, Norway. The lake is located northeast of the Sagfjorden, about southwest of the village of Mørsvikbotn.

Geographic entities mentioned:
surface_form: grovatnet
instance_of: Lake
countries: Norway
coordinates: lat: 67.6162
lon: 15.5042
Lake Wood (Philippines). Lake Wood (Subanen: Danaw) is a large lake located in the province of Zamboanga del Sur in Mindanao, Philippines. The lake is the largest in the province, and is situated at the foot of Mt. Serongan. On its shores are the municipalities of Lakewood and Kumalarang. History.

Geographic entities mentioned:
surface_form: lake wood (philippines)
instance_of: Lake
countries: Philippines
coordinates: lat: 7.8444444
lon: 123.165
Lake Wood (Philippines). Lake Wood (Subanen: Danaw) is a large lake located in the province of Zamboanga del Sur in Mindanao, Philippines. The lake is the largest in the province, and is situated at the foot of Mt. Serongan. On its shores are the municipalities of Lakewood and Kumalarang. History.

Geographic entities mentioned:
surface_form: lake wood
instance_of: Lake
countries: Philippines
coordinates: lat: 7.8444444
lon: 123.165
Smith of the 14th Cavalry Regiment of the United States Army discovered Lake Danaw and proceeded to report it to the American Administration. Captain Smith then renamed the lake as &quot;Lake Leonard Wood&quot;, after the Governor-General of the time, Governor Leonard Wood. Over time, the lake's name changed to &quot;Lake Wood&quot;. Physical characteristics.

Geographic entities mentioned:
surface_form: lake wood
instance_of: Lake
countries: Philippines
coordinates: lat: 7.8444444
lon: 123.165
surface_form: lake wood
instance_of: Lake
countries: Philippines
coordinates: lat: 7.8444444
lon: 123.165
On the southeast side is the Biswangan River, the lake's only outlet, which flows into Dumanquilas Bay. Biodiversity. Because of the limited information about Lake Wood, not much is known about the flora and fauna of the lake. There is only one known species of endemic fish that resides in the lake, that is the &quot;Rasbora philippina&quot;, locally known as &quot;Porang&quot;. Legends.

Geographic entities mentioned:
surface_form: lake wood
instance_of: Lake
countries: Philippines
coordinates: lat: 7.8444444
lon: 123.165
In 1904, in an expedition from Misamis to Dumanquilas Bay, Captain Cornelius C. Smith of the 14th Cavalry Regiment of the United States Army discovered Lake Danaw and proceeded to report it to the American Administration. Captain Smith then renamed the lake as &quot;Lake Leonard Wood&quot;, after the Governor-General of the time, Governor Leonard Wood.

Geographic entities mentioned:
surface_form: smith
instance_of: Mountain
countries: Philippines
coordinates: lat: 19.536622222222
lon: 121.91284444444
It is bordered to the north by the municipalities of Peribán and Uruapan, to the east by Nuevo Parangaricutiro, to southeast by Parácuaro, to the south by Apatzingán, and to the southwest by Buenavista. A volcanic peak, Pico de Tancítaro or &quot;Volcán Tancítaro&quot;, is located in the municipality. At in elevation, it is the highest point in Michoacán state.

Geographic entities mentioned:
surface_form: Pico de Tancítaro
instance_of: Mountain
countries: Mexico
coordinates: lat: 19.416333333333
lon: -102.3195
S.I. Paul et al. (2021) isolated and biochemically characterized salt tolerant strains of &quot;Burkholderia cepacia&quot; from marine sponges of Saint Martin's Island of the Bay of Bengal, Bangladesh. Pathogenesis. BCC organisms are typically found in water and soil and can survive for prolonged periods in moist environments. They show a relatively poor virulence.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Modesto is located in the Central Valley region, south of Sacramento and north of Fresno. Distances from other places include: north of Merced, California, east of San Francisco, west of Yosemite National Park, and south of Stockton. The city, in the San Joaquin Valley, is surrounded by rich farmland. Stanislaus County ranks sixth among California counties in farm production.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
Mare d'Oursi. The Mare d'Oursi is a small, shallow lake in Oudalan Province in northern Burkina Faso, close to the town of Oursi. It is included in the List of Ramsar wetlands of international importance.

Geographic entities mentioned:
surface_form: mare d'oursi
instance_of: Lake
countries: Burkina Faso
coordinates: lat: 14.633333333333
lon: -0.5
Log home building and tourism are also an important part of the community. Tourism. 100 Mile House is a centre for outdoor activities and is becoming increasingly known for its richness of bird life. The surrounding area features hundreds of lakes for boating and fishing including 101 Mile Lake, 103 Mile Lake, Lac La Hache, Canim Lake, Horse Lake, Green Lake, Bridge Lake and Sheridan Lake.

Geographic entities mentioned:
surface_form: 101 Mile Lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.6677
lon: -121.2934
surface_form: 103 Mile Lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.685
lon: -121.299
Resen, North Macedonia. Resen () is a town in southwestern North Macedonia, with just under 9,000 inhabitants. Resen is approximately equidistant between Bitola and Ohrid. The town rises above sea level and is situated near Lake Prespa. Resen is the only town in the Prespa Lake area and is the seat of Resen Municipality. Name.

Geographic entities mentioned:
surface_form: Lake Prespa
instance_of: Lake
countries: North Macedonia
Albania
Greece
coordinates: lat: 40.9
lon: 21.05
During the Middle Ages, the Prespa area was part of the Bulgarian empire under Samuil. After the Battle of Klyuch, some of Samuil's soldiers, who were each blinded in one eye, settled in a village on the shore of Lake Prespa. The Byzantines called the village &quot;Asamati&quot;. The Byzantine meaning of this word is &quot;settlement of one-eyed people&quot;.

Geographic entities mentioned:
surface_form: Lake Prespa
instance_of: Lake
countries: North Macedonia
Albania
Greece
coordinates: lat: 40.9
lon: 21.05
Detainment. Significant numbers of Italian soldiers captured during the East African Campaign were interned in camps in Kenya, where they were used in civil infrastructure projects. Amongst those detained in Kenya was the Italian writer, Felice Benuzzi, who attempted to escape in 1943 by climbing Mount Kenya, though subsequently re-surrendered to the British.

Geographic entities mentioned:
surface_form: Mount Kenya
instance_of: Mountain
countries: Kenya
coordinates: lat: -0.1
lon: 37.2
Central Uplands. The Central Uplands () is one of the three major natural regions of Germany. It stretches east to west across the country. To the north lies the North German Plain or Northern Lowland; to the south, the Alps and the Alpine Foreland. Formation.

Geographic entities mentioned:
surface_form: Alpine Foreland
instance_of: Plateau
countries: Germany
coordinates: lat: 48
lon: 12
It comprises 180 acres of landscaped parkland which surround around 100 acres of water across two lakes. Both lakes are balancing lakes, designed to mitigate flooding from the River Ouzel. The southern lake offers a wide range of activities on and off the water, whilst the northern lake offers a more natural and tranquil setting, ideal for quiet walks and spotting wildlife.

Geographic entities mentioned:
surface_form: River Ouzel
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 51.882222222222
lon: -0.63555555555556
surface_form: ouzel
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 51.882222222222
lon: -0.63555555555556
There are large events held on the site throughout the year, including Comedy Central's FriendsFest
Operating. Since January 2010, Willen Lake has also been the location of the Milton Keynes parkrun, which currently starts just to the West of the lake, then follows the Grand Union canal to Great Holm, before making a complete loop of the South Lake and finishing by the Watersports Centre.

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
surface_form: willen lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 52.05101
lon: -0.71832
Geography. The lake is one of the largest purpose-built stormwater balancing lakes in the UK. The lake is designed to take surface run-off from Milton Keynes, the largest of a number designed to do so. The lake has capacity for an additional level increase of 1.3 metres, equivalent to a once in 200 years event.

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
The lake is designed to take surface run-off from Milton Keynes, the largest of a number designed to do so. The lake has capacity for an additional level increase of 1.3 metres, equivalent to a once in 200 years event. Unlike most of the rest of the UK, Milton Keynes has separate storm and foul sewers, so sewage pollution is not a significant problem.

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
The lake has capacity for an additional level increase of 1.3 metres, equivalent to a once in 200 years event. Unlike most of the rest of the UK, Milton Keynes has separate storm and foul sewers, so sewage pollution is not a significant problem. The lake is surrounded by a mixture of open parkland and woodland, which forms part of the wider Ouzel Valley Park.

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
surface_form: ouzel
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 51.882222222222
lon: -0.63555555555556
The lake is divided by an embankment and bridge carrying the A509 (H5 Portway), which runs between the east and west of the city, providing links to M1 Junction 14 (approximately to the north-east), and Central Milton Keynes and the A5 (approximately and to the south-west, respectively). Beside the North lake is the Peace Pagoda and Nipponzan-Myōhōji Buddhist temple.

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
Willen Lake. Willen Lake is a visitor attraction and public park in Milton Keynes, Buckinghamshire The site is owned by The Parks Trust, an independent, self-funded charity that cares for and maintains over 6,000 acres of green space across MK. Willen Lake is Milton Keynes's most popular park, attracting in excess of 750,000 visitors a year.

Geographic entities mentioned:
surface_form: willen lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 52.05101
lon: -0.71832
Frysjabreen. Frysjabreen is a glacier in Nathorst Land at Spitsbergen, Svalbard. It has a length of about six kilometers, and extends from the ridges of Breskarvet and Kjellmanberget down to the valley of Frysjadalen. The glacier is named after the river Frysja, which originates from Frysjabreen and flows through Frysjadalen until its outlet into Van Mijenfjorden.

Geographic entities mentioned:
surface_form: Breskarvet
instance_of: Mountain
countries: Norway
coordinates: lat: 77.657
lon: 15.645
On Sept. 18, yet another pilot reported a 300m-high ash plume. In early July 1996, a passing ship reported a 1-km high plume of &quot;ash and smoke&quot; (Neal and McGimsey, 1997). On August 28 Mt. Cleveland, 100 km to the northeast, was also active and winds were blowing towards Amukta. Composition.

Geographic entities mentioned:
surface_form: cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 52.822222222222
lon: -169.945
surface_form: mt. cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 52.822222222222
lon: -169.945
surface_form: mt. cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 48.9244858
lon: -113.848042
surface_form: amukta
instance_of: Mountain
countries: United States
coordinates: lat: 52.497777777778
lon: -171.25472222222
surface_form: mt. cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 44.046388888889
lon: -72.908055555556
No hot springs or fumaroles have been reported from Amukta. Sekora (1973, p. 29) reports the presence of a cinder cone near the northeastern shore of the island. Volcanic activity. Well documented reports of historical Amukta volcanism are sparse; activity was noted from 1786 to 1791, and again in 1876 (Coats, 1950).

Geographic entities mentioned:
surface_form: cinder cone
instance_of: Mountain
countries: United States
coordinates: lat: 40.547386111111
lon: -121.31997222222
In early July 1996, a passing ship reported a 1-km high plume of &quot;ash and smoke&quot; (Neal and McGimsey, 1997). On August 28 Mt. Cleveland, 100 km to the northeast, was also active and winds were blowing towards Amukta. Composition. Igneous rocks produced by this volcano range from granite to monzonite, however the most common rock found in/around Mt. Amukta is basalt. Sources. by T.P.

Geographic entities mentioned:
surface_form: mt. amukta
instance_of: Mountain
countries: United States
coordinates: lat: 52.497777777778
lon: -171.25472222222
surface_form: amukta
instance_of: Mountain
countries: United States
coordinates: lat: 52.497777777778
lon: -171.25472222222
Mount Amukta. The undissected stratovolcano of Amukta volcano makes up most of nearly circular, 7.7-km-wide Amukta Island (Amuux̂tax̂ in Aleut). It is the westernmost of the Islands of Four Mountains chain. The nearest islands to it are Yunaska and Seguam Island; it is separated from Seguam Island by Amukta Pass.

Geographic entities mentioned:
surface_form: amukta
instance_of: Mountain
countries: United States
coordinates: lat: 52.497777777778
lon: -171.25472222222
surface_form: amukta
instance_of: Mountain
countries: United States
coordinates: lat: 52.497777777778
lon: -171.25472222222
Persistent low clouds obscured the exact source of the lava, but the flow was seen to extend from the west side of the cone southwest into the sea at Traders Cove (Bulletin of Volcanic Eruptions, 1963). In late August and early September 1987, a commercial pilot observed a 10.5 km high eruption plume rising through cloud cover near Amukta Island.

Geographic entities mentioned:
surface_form: amukta
instance_of: Mountain
countries: United States
coordinates: lat: 52.497777777778
lon: -171.25472222222
Mount Amukta. The undissected stratovolcano of Amukta volcano makes up most of nearly circular, 7.7-km-wide Amukta Island (Amuux̂tax̂ in Aleut). It is the westernmost of the Islands of Four Mountains chain. The nearest islands to it are Yunaska and Seguam Island; it is separated from Seguam Island by Amukta Pass.

Geographic entities mentioned:
surface_form: amukta
instance_of: Mountain
countries: United States
coordinates: lat: 52.497777777778
lon: -171.25472222222
surface_form: mount amukta
instance_of: Mountain
countries: United States
coordinates: lat: 52.497777777778
lon: -171.25472222222
It is the westernmost of the Islands of Four Mountains chain. The nearest islands to it are Yunaska and Seguam Island; it is separated from Seguam Island by Amukta Pass. The cone, about 5.8 km in basal diameter and topped by a 0.4 km wide summit crater, appears on synthetic-aperture radar imagery to be built upon a 300+ meter high, east-west trending arcuate ridge.

Geographic entities mentioned:
surface_form: amukta
instance_of: Mountain
countries: United States
coordinates: lat: 52.497777777778
lon: -171.25472222222
Extensions of that ridge on the southwest and east sides of the island indicate an older caldera approximately 6 km in diameter and open to the sea on the south side. No hot springs or fumaroles have been reported from Amukta. Sekora (1973, p. 29) reports the presence of a cinder cone near the northeastern shore of the island. Volcanic activity.

Geographic entities mentioned:
surface_form: amukta
instance_of: Mountain
countries: United States
coordinates: lat: 52.497777777778
lon: -171.25472222222
Volcanic activity. Well documented reports of historical Amukta volcanism are sparse; activity was noted from 1786 to 1791, and again in 1876 (Coats, 1950). Petroff (1884, citing Grewingk, 1850) lists activity at Amukhton in 1770, presumably the same volcano; conversely, Dall (1870, citing Grewingk, 1850) describes a cessation of activity at Amukta in 1770.

Geographic entities mentioned:
surface_form: amukta
instance_of: Mountain
countries: United States
coordinates: lat: 52.497777777778
lon: -171.25472222222
In late August and early September 1987, a commercial pilot observed a 10.5 km high eruption plume rising through cloud cover near Amukta Island. On September 4, another pilot observed a small dark ash plume issuing from the summit of Amukta (Smithsonian Institution, 1987). On Sept. 18, yet another pilot reported a 300m-high ash plume.

Geographic entities mentioned:
surface_form: amukta
instance_of: Mountain
countries: United States
coordinates: lat: 52.497777777778
lon: -171.25472222222
Pen y Brynfforchog. Pen y Brynfforchog is subsidiary summit of Glasgwm in North Wales forming part of the Aran range in southern Snowdonia. It is separated from Glasgwm by the pass, Bwlch y Fign. The summit is bare and marked by a few stones. The views to the Dyfi hills: include direct view of the Craig Portas ridge, with Maesglase and Cribin Fawr.

Geographic entities mentioned:
surface_form: Glasgwm
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.76
lon: -3.73
surface_form: pen y brynfforchog
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.7462
lon: -3.7529
Pen y Brynfforchog. Pen y Brynfforchog is subsidiary summit of Glasgwm in North Wales forming part of the Aran range in southern Snowdonia. It is separated from Glasgwm by the pass, Bwlch y Fign. The summit is bare and marked by a few stones. The views to the Dyfi hills: include direct view of the Craig Portas ridge, with Maesglase and Cribin Fawr.

Geographic entities mentioned:
surface_form: Maesglase
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.719996
lon: -3.752504
surface_form: Cribin Fawr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.721757
lon: -3.786277
Pen y Brynfforchog. Pen y Brynfforchog is subsidiary summit of Glasgwm in North Wales forming part of the Aran range in southern Snowdonia. It is separated from Glasgwm by the pass, Bwlch y Fign. The summit is bare and marked by a few stones. The views to the Dyfi hills: include direct view of the Craig Portas ridge, with Maesglase and Cribin Fawr.

Geographic entities mentioned:
surface_form: glasgwm
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.76
lon: -3.73
Pen y Brynfforchog. Pen y Brynfforchog is subsidiary summit of Glasgwm in North Wales forming part of the Aran range in southern Snowdonia. It is separated from Glasgwm by the pass, Bwlch y Fign. The summit is bare and marked by a few stones. The views to the Dyfi hills: include direct view of the Craig Portas ridge, with Maesglase and Cribin Fawr.

Geographic entities mentioned:
surface_form: pen y brynfforchog
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.7462
lon: -3.7529
Sangamas worshiped Virupaksha together with other pastoralist god Vitthal and worship of Vitthal is consistent with other pastoralist Deccan dynasties, of Kannadiga origin, that claimed Yadava lineage (Hoysalas and Seunas). Inscriptions on the temples constructed by Vijayanagara Emperors in Lepakshi indicate that Vitthal and Virupaksha were originally worshiped as Vitthal and Birappa.

Geographic entities mentioned:
surface_form: Deccan
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
Pyramid Mountain (Alberta). Pyramid Mountain is a mountain in Jasper National Park, Alberta, Canada, named for its pyramid-like shape. James Hector named the mountain in 1859 due to its appearance from the Athabasca River valley on the eastern side of the peak. Part of the Victoria Cross Ranges in the Athabasca River Valley the mountain is in the major headwaters for the Athabasca River.

Geographic entities mentioned:
surface_form: pyramid mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.9944
lon: -120.104
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: pyramid mountain (alberta)
instance_of: Mountain
countries: Canada
coordinates: lat: 52.9511
lon: -118.149
surface_form: pyramid mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 49.81916666666667
lon: -122.90444444444445
Pyramid Mountain (Alberta). Pyramid Mountain is a mountain in Jasper National Park, Alberta, Canada, named for its pyramid-like shape. James Hector named the mountain in 1859 due to its appearance from the Athabasca River valley on the eastern side of the peak. Part of the Victoria Cross Ranges in the Athabasca River Valley the mountain is in the major headwaters for the Athabasca River.

Geographic entities mentioned:
surface_form: pyramid mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.9944
lon: -120.104
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: pyramid mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 52.9511
lon: -118.149
surface_form: pyramid mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 49.81916666666667
lon: -122.90444444444445
These slopes can be reached by following a steep fire road from the parking lot at Pyramid Lake, southeast of the peak. Based on the Köppen climate classification, Pyramid Mountain is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C.

Geographic entities mentioned:
surface_form: pyramid mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.9944
lon: -120.104
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: pyramid mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 52.9511
lon: -118.149
surface_form: pyramid mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 49.81916666666667
lon: -122.90444444444445
Pyramid Mountain (Alberta). Pyramid Mountain is a mountain in Jasper National Park, Alberta, Canada, named for its pyramid-like shape. James Hector named the mountain in 1859 due to its appearance from the Athabasca River valley on the eastern side of the peak. Part of the Victoria Cross Ranges in the Athabasca River Valley the mountain is in the major headwaters for the Athabasca River.

Geographic entities mentioned:
surface_form: athabasca
instance_of: Lake
countries: Canada
coordinates: lat: 59.266666666667
lon: -109.45
surface_form: athabasca
instance_of: Mountain
countries: Canada
coordinates: lat: 52.18055555555556
lon: -117.20166666666667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
James Hector named the mountain in 1859 due to its appearance from the Athabasca River valley on the eastern side of the peak. Part of the Victoria Cross Ranges in the Athabasca River Valley the mountain is in the major headwaters for the Athabasca River. The peak is just under north-west of the town of Jasper. The mountain is a relatively easy scramble on the eastern slopes.

Geographic entities mentioned:
surface_form: athabasca
instance_of: Lake
countries: Canada
coordinates: lat: 59.266666666667
lon: -109.45
surface_form: athabasca
instance_of: Lake
countries: Canada
coordinates: lat: 59.266666666667
lon: -109.45
surface_form: athabasca
instance_of: Mountain
countries: Canada
coordinates: lat: 52.18055555555556
lon: -117.20166666666667
surface_form: athabasca
instance_of: Mountain
countries: Canada
coordinates: lat: 52.18055555555556
lon: -117.20166666666667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The peak is just under north-west of the town of Jasper. The mountain is a relatively easy scramble on the eastern slopes. These slopes can be reached by following a steep fire road from the parking lot at Pyramid Lake, southeast of the peak. Based on the Köppen climate classification, Pyramid Mountain is located in a subarctic climate zone with cold, snowy winters, and mild summers.

Geographic entities mentioned:
surface_form: pyramid lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.9225
lon: -118.096
Part of the Victoria Cross Ranges in the Athabasca River Valley the mountain is in the major headwaters for the Athabasca River. The peak is just under north-west of the town of Jasper. The mountain is a relatively easy scramble on the eastern slopes. These slopes can be reached by following a steep fire road from the parking lot at Pyramid Lake, southeast of the peak.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Rueda-Otero obtained his DDS degree from the Facultad Dental de Cartagena in 1932 (this institution, now closed, had no connection with the University of Cartagena). Career and accomplishments. In his practice, Dr. Rueda met the dental needs of the people of Lorica, Cerete, San Pelayo, San Carlos, Garzones among all other southern and middles regions of the Sinú River.

Geographic entities mentioned:
surface_form: Sinú River
instance_of: Watercourse
countries: Colombia
coordinates: lat: 8.75825
lon: -75.88811111111112
Prominent among the belief is that an &quot;Amruthakalasha&quot; lies beneath the lotus feet of Goddess Lakshmi, which when invoked with devotion fulfills all desires. Nearby are the Shivanasamudra waterfalls, Shimsha, Cauvery Wildlife Sanctuary, Muthathi forest, Bheemeshwari Cauveri fishing camp near Halaguru., Galibore fishing camp and more

Geographic entities mentioned:
surface_form: Shimsha
instance_of: Watercourse
countries: India
coordinates: lat: 12.3
lon: 76.233
upstream of the valley is Vidra Lake, one of the largest dams and reservoirs in Romania, built between 1965 and 1972, and also the newly built Transalpina ski resort on lake's shore (Transalpina Resort is not on Transalpina Road but is connected to it by road).

Geographic entities mentioned:
surface_form: Vidra Lake
instance_of: Lake
countries: Romania
coordinates: lat: 45.430555555556
lon: 23.733333333333
The river is 246 kilometers away from Kazakhstan's capital, Astana. Geography. The river starts in the Kokshetau Massif, part of the Kokshetau Hills, in a birch forest on Semenov's Hill's western slope, flows west through Shchuchinsk, and bends north toward Frolovsky Pond before bending to the northwest. It crosses Bayanbai and passes two dams before it reaches Kenesary.

Geographic entities mentioned:
surface_form: Kokshetau Hills
instance_of: Mountain
countries: Kazakhstan
coordinates: lat: 53.080000000000005
lon: 70.18833333333333
It crosses Bayanbai and passes two dams before it reaches Kenesary. Finally it flows into Lake Kopa in Kokshetau at an altitude of above sea level, near the Zhaman-Karakalpak mountain. Lake Zhamantuz is part of the basin of the basin of the Kylshakty river.

Geographic entities mentioned:
surface_form: Lake Kopa
instance_of: Lake
countries: Kazakhstan
Russian Empire
Soviet Union
coordinates: lat: 53.3
lon: 69.35
Duffy's Peak. Duffy's Peak is a small hill or butte near the Salt Fork Brazos River in Garza County, Texas. Duffy's Peak extends less than above the river, yet despite its small size, it served as an important landmark for early surveyors of the region and is said to be named for a member of the original survey team who died and was buried nearby in the late 1870s.

Geographic entities mentioned:
surface_form: duffy's peak
instance_of: Mountain
countries: United States
coordinates: lat: 33.3581
lon: -101.342
Duffy's Peak extends less than above the river, yet despite its small size, it served as an important landmark for early surveyors of the region and is said to be named for a member of the original survey team who died and was buried nearby in the late 1870s. Duffy's Peak is located in the rolling plains to the south and east of the Caprock Escarpment of the Llano Estacado.

Geographic entities mentioned:
surface_form: duffy's peak
instance_of: Mountain
countries: United States
coordinates: lat: 33.3581
lon: -101.342
The erosionally resistant sandstones of the peak's cap have protected underlying soils that have remained intact, while surrounding sediments have eroded away. As a result of this process, Duffy's Peak now stands out as a small but relatively prominent landmark that can be seen from a significant distance.

Geographic entities mentioned:
surface_form: duffy's peak
instance_of: Mountain
countries: United States
coordinates: lat: 33.3581
lon: -101.342
As a result of this process, Duffy's Peak now stands out as a small but relatively prominent landmark that can be seen from a significant distance. In 1969, the Texas Historical Commission erected a historical marker for Duffy's Peak along Texas State Highway 207.

Geographic entities mentioned:
surface_form: duffy's peak
instance_of: Mountain
countries: United States
coordinates: lat: 33.3581
lon: -101.342
Duffy's Peak is located in the rolling plains to the south and east of the Caprock Escarpment of the Llano Estacado. The soils of the area are moderately deep silt loams that support mesquite, yucca, cacti, and grasses. The local terrain is eroded, cut by highly intermittent streams such as the Salt Fork Brazos River, and its tributaries, such as McDonald Creek and Lake Creek.

Geographic entities mentioned:
surface_form: yucca
instance_of: Mountain
countries: United States
coordinates: lat: 36.9402
lon: -116.485
The population was 16,871 at the 2020 census, up from 15,951 at the 2010 census. It is the county seat of Belknap County. Laconia, situated between Lake Winnipesaukee and Lake Winnisquam, includes the villages of Lakeport and Weirs Beach. Each June, the city hosts Laconia Motorcycle Week, also known as &quot;Bike Week,&quot; one of the country's largest motorcycle rallies. Name.

Geographic entities mentioned:
surface_form: Lake Winnipesaukee
instance_of: Lake
countries: United States
coordinates: lat: 43.598888888889
lon: -71.323055555556
surface_form: Lake Winnisquam
instance_of: Lake
countries: United States
coordinates: lat: 43.545
lon: -71.508888888889
History. A large Abenaki Indian settlement called Aquadoctan once existed at the point now known as The Weirs, named by colonists for fishing weirs discovered at the outlet of the Winnipesaukee River. Early explorers had hoped to follow the Piscataqua River north to Lake Champlain in search of the great lakes and rivers of Canada mentioned in Indian folklore.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
Laconia is located northwest of the geographic center of Belknap County. The city lies at the center of New Hampshire's Lakes Region, and all or part of four major bodies of water lie within its limits: Lake Winnipesaukee, Lake Winnisquam, Opechee Bay and Paugus Bay (sometimes counted as an arm of Winnipesaukee, but historically a separate body of water). Laconia contains three main villages.

Geographic entities mentioned:
surface_form: Lake Winnipesaukee
instance_of: Lake
countries: United States
coordinates: lat: 43.598888888889
lon: -71.323055555556
surface_form: Lake Winnisquam
instance_of: Lake
countries: United States
coordinates: lat: 43.545
lon: -71.508888888889
surface_form: Opechee Bay
instance_of: Lake
countries: United States
coordinates: lat: 43.546666666667
lon: -71.474722222222
surface_form: Paugus Bay
instance_of: Lake
countries: United States
coordinates: lat: 43.576111111111
lon: -71.459166666667