Sarmila/GeoWiki-Features huggingface dataset:
The thickness of ice is from to. In most severe winters it may become up to. The period of freeze-up is from 150 to 170 days. The Rivers. Inflow rivers are the Sapshanka () in the south and the Sapsha () in the west. The outflow river is the Sapsha in the east. The Sapsha connects Lake Sapsho and Lake Petrakovskoye (). Both lakes have similar surface elevation. The area of Lake Petrakovskoye is.

Geographic entities mentioned:
surface_form: lake sapsho
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 55.495555555556
lon: 31.845277777778
surface_form: sapsho
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 55.495555555556
lon: 31.845277777778
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
The Sapsha connects Lake Sapsho and Lake Petrakovskoye (). Both lakes have similar surface elevation. The area of Lake Petrakovskoye is. During the period of melting snow in spring and heavy showers in summer Lake Petrakovskoye fills with water faster than Lake Sapsho. Therefore, the Sapsha changes its flow. Usually changing of flow of the Sapsha happens several times a year. The Islands.

Geographic entities mentioned:
surface_form: lake sapsho
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 55.495555555556
lon: 31.845277777778
surface_form: sapsho
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 55.495555555556
lon: 31.845277777778
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
Lake Sapsho. Lake Sapsho () is a glacial lake in Demidovsky District of Smolensk Oblast, Russia. It is the largest lake (3,04 km2) of the Smolenskoye Poozerye National Park. It is situated northeast of Demidov in the northwestern part of the oblast, near the settlement of Przhevalskoye. Famous 19th century Russian traveller Nikolay Przhevalsky compared the lake with Lake Baikal in miniature.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
It is situated northeast of Demidov in the northwestern part of the oblast, near the settlement of Przhevalskoye. Famous 19th century Russian traveller Nikolay Przhevalsky compared the lake with Lake Baikal in miniature. The lake is a natural monument. It is connected with the Baltic Sea by the Sapsha, Vasilyevka, Yelsha, and Daugava rivers. There are 4 big and 2 small islands on the lake.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
Famous 19th century Russian traveller Nikolay Przhevalsky compared the lake with Lake Baikal in miniature. The lake is a natural monument. It is connected with the Baltic Sea by the Sapsha, Vasilyevka, Yelsha, and Daugava rivers. There are 4 big and 2 small islands on the lake. There are a lot of tumuli of the Tushumlin culture by Lake Sapsho. The flora and fauna of the lake are very diverse.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
It is connected with the Baltic Sea by the Sapsha, Vasilyevka, Yelsha, and Daugava rivers. There are 4 big and 2 small islands on the lake. There are a lot of tumuli of the Tushumlin culture by Lake Sapsho. The flora and fauna of the lake are very diverse. Yet in the beginning of the 20th century there was the industrial fishery. Though now any industry is prohibited here.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
The flora and fauna of the lake are very diverse. Yet in the beginning of the 20th century there was the industrial fishery. Though now any industry is prohibited here. A lot of species of the flora and fauna of the lake are in the Red Book. The Lake. Lake Sapsho is situated in the north-west of Smolensk Oblast, to the north of Smolensk.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
Yet in the beginning of the 20th century there was the industrial fishery. Though now any industry is prohibited here. A lot of species of the flora and fauna of the lake are in the Red Book. The Lake. Lake Sapsho is situated in the north-west of Smolensk Oblast, to the north of Smolensk. It is on the Sloboda Upland () that is a part of Smolensk–Moscow Upland ().

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
The Lake. Lake Sapsho is situated in the north-west of Smolensk Oblast, to the north of Smolensk. It is on the Sloboda Upland () that is a part of Smolensk–Moscow Upland (). It is the largest lake in Smolenskoye Poozerye National Park. There are two eskers. One of them is partly destroyed by glacial flows. It caused the arising of five of six islands.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
There are two eskers. One of them is partly destroyed by glacial flows. It caused the arising of five of six islands. Lake Sapsho is divided into deep northern and shallow southern parts. The other esker forms the western border of the lake. The northern side is also abrupt. On the contrary, the eastern and southern sides are gentle. The bottom of the lake here is also not steep.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
Lake Sapsho is divided into deep northern and shallow southern parts. The other esker forms the western border of the lake. The northern side is also abrupt. On the contrary, the eastern and southern sides are gentle. The bottom of the lake here is also not steep. The northern basin is divided into western and eastern parts by a long underwater spit. The depth here is less than.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
Lake Sapsho drains into the rivers of the Western Dvina () basin. In spring, usually by the middle or end of April, water volume increases because of melting snow. The melting of ice on the lake usually takes from 10 to 15 days more, and ends in the late April or early May. The swimming season opens in late June or early July, and finishes in late July or early August.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
Inflow rivers are the Sapshanka () in the south and the Sapsha () in the west. The outflow river is the Sapsha in the east. The Sapsha connects Lake Sapsho and Lake Petrakovskoye (). Both lakes have similar surface elevation. The area of Lake Petrakovskoye is. During the period of melting snow in spring and heavy showers in summer Lake Petrakovskoye fills with water faster than Lake Sapsho.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
Therefore, the Sapsha changes its flow. Usually changing of flow of the Sapsha happens several times a year. The Islands. There 6 islands on the lake. Four of them are large: Chernetsky / Monk Island (), Raspashnoy / Border Island (), Bagryany / Crimson Island (), Dlinny / Long Island (). Two of them are small: Dubovy / Oak Island () and Lyubvi / Island of Love ().

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
Army officer, eventually rising to become a Brevet Brigadier General. He saw service in Florida and became a notable artillery specialist and the first commander of Fort Monroe, located at the entrance to the harbor of Hampton Roads in Virginia. In Florida, Lake Eustis and the city of Eustis were each named in his honor. Camp Abraham Eustis, a World War I-era U.S.

Geographic entities mentioned:
surface_form: Lake Eustis
instance_of: Lake
countries: United States
coordinates: lat: 28.8489
lon: -81.7253
According to the wuthors, resolving the phylogenetic positions of &quot;Gualicho, Aoniraptor, Deltadromeus&quot; and megaraptorans is a critical issue facing theropod systematics. &quot;Deltadromeus&quot; was also considered a noasaurid in a 2020 review of the Kem Kem Group geology and fauna.

Geographic entities mentioned:
surface_form: Kem Kem Group
instance_of: Mountain
countries: Morocco
coordinates: lat: 30.9
lon: -4
Saint-Bruno-de-Guigues. Saint-Bruno-de-Guigues (), often shortened to Guigues, is a municipality in northwestern Quebec, Canada, in the Témiscamingue Regional County Municipality. In addition to the main namesake population centre, the municipality also includes the hamlet of Pointe-Piché, located on the shores of Lake Timiskaming. History.

Geographic entities mentioned:
surface_form: Lake Timiskaming
instance_of: Lake
countries: Canada
coordinates: lat: 47.333333333333
lon: -79.5
The winery was shut down by the Prohibition era. Inhibited by the lack of water, Vista grew slowly through the early 1910s to less than 1,000 people. With a 1923, however, the Vista Irrigation District had the necessary funding to construct a new water supply from Lake Henshaw. Agriculture began to flourish in the area, including citrus fruits, tomatoes, celery, and most prominently avocados.

Geographic entities mentioned:
surface_form: Lake Henshaw
instance_of: Lake
countries: United States
coordinates: lat: 33.236703
lon: -116.7454423
A new station southwest of the former Western Pacific station site opened with the start of the Altamont Commuter Express service on October 19, 1998. Bus connections. WHEELS local routes 53 and 54 service the station, plus the County Connection express route 92X which provides access to ACE from the San Ramon Valley to the north. The 8 and 10R WHEELS routes connect to the Pleasanton BART station.

Geographic entities mentioned:
surface_form: San Ramon Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.75
lon: -121.95
As a result, water is constantly collecting and flowing into the lake. Location. Lake Churat is situated 10 kilometers from the village of Churat in Sari county, which serves as the center of Mazandaran province and offers a view of the Caspian Sea. The Iranian capital, Tehran, is situated approximately two hours drive from Mazandaran province. Geography and topography.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
WRAY-TV. WRAY-TV (channel 30) is a religious television station licensed to Wake Forest, North Carolina, United States, serving the Research Triangle region as an owned-and-operated station of Tri-State Christian Television (TCT). The station's transmitter is located on Terrells Mountain near Chapel Hill.

Geographic entities mentioned:
surface_form: Terrells Mountain
instance_of: Landform
Mountain
countries: United States
coordinates: lat: 35.8665
lon: -79.1672
Xixiang Chi. Xixiang Chi (), also known as Tianhua Chanyuan (), is one of the most important Buddhist temples and monasteries on Mount Emei in Emeishan City, Sichuan, China. The temple is located more than 2,000 metres above sea level. The monastery was founded in the Ming dynasty and was expanded during the reign of the Kangxi Emperor in the Qing dynasty.

Geographic entities mentioned:
surface_form: Mount Emei
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 29.519722222222
lon: 103.3325
In April 2019, IS activity indicated that the terrorist organization was in control of Jebel Bishri, a mountain near the intersection of the borders of the Raqqa, Deir ez-Zor, and Homs Governorates, as well as the surrounding area between the Al-Sukhnah and Deir ez-Zor countrysides.

Geographic entities mentioned:
surface_form: Jebel Bishri
instance_of: Mountain
countries: Syria
coordinates: lat: 35.28972222
lon: 39.21888889
Kvam Municipality (Nord-Trøndelag). Kvam is a former municipality in what was Nord-Trøndelag county in Norway. The municipality existed from 1909 until its dissolution in 1964. The municipality encompassed the areas north and west of the lake Snåsavatnet in what is now Steinkjer Municipality in Trøndelag county. The administrative centre was the village of Kvam on the shore of the lake.

Geographic entities mentioned:
surface_form: Snåsavatnet
instance_of: Lake
countries: Norway
coordinates: lat: 64.1874
lon: 12.0249
Location. The municipality lies in the western Hunsrück on the &quot;Hunsrückhöhenstraße&quot; (“Hunsrück Heights Road”, a scenic road across the Hunsrück built originally as a military road on Hermann Göring’s orders), some 7 km northwest of the Erbeskopf. Thalfang lies roughly 25 km southeast of Wittlich and 25 km east of Trier. Through the municipality flows the Thalfanger Bach.

Geographic entities mentioned:
surface_form: Erbeskopf
instance_of: Mountain
countries: Germany
coordinates: lat: 49.72944
lon: 7.08889
Transport. Thalfang lies on the &quot;Hunsrückhöhenstraße&quot; between Hermeskeil and Morbach. Tourism. The idyllic location and the proximity to tourist destinations such as the Moselle, Trier and the Erbeskopf, as well as the relatively short distance to Luxembourg and France, make Thalfang a popular holiday destination. Sons and daughters of the town.

Geographic entities mentioned:
surface_form: Erbeskopf
instance_of: Mountain
countries: Germany
coordinates: lat: 49.72944
lon: 7.08889
The Cosquín River is a small river in the province of Córdoba, Argentina. It is located in the area of the Punilla Valley and is part of the upper drainage basin of the Suquía River. The Cosquín receives the waters of several other minor rivers and streams and flows southwards into and across the Punilla Valley, passing by the city of Cosquín and then taking the name of Santa María River.

Geographic entities mentioned:
surface_form: Punilla Valley
instance_of: Valley
countries: Argentina
coordinates: lat: -31.033333333333
lon: -64.5
Cosquín River. The Cosquín River is a small river in the province of Córdoba, Argentina. It is located in the area of the Punilla Valley and is part of the upper drainage basin of the Suquía River.

Geographic entities mentioned:
surface_form: cosquín river
instance_of: Watercourse
countries: Argentina
coordinates: lat: -31.216666666667
lon: -64.483333333333
It is situated south of the mountain Wayna Potosí and north-east of Milluni Lake at a height of about 4,664 metres (15,302 ft). The little lake north-east of Janq'u Quta is named Pata Quta &quot;(Pata Khota)&quot;. There is a smaller lake of the same name east of Janq'u Quta in the La Paz Municipality.

Geographic entities mentioned:
surface_form: Wayna Potosí
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.261944444444
lon: -68.148888888889
surface_form: Milluni
instance_of: Lake
countries: Bolivia
coordinates: lat: -16.358333333333334
lon: -68.16666666666667
Janq'u Quta (El Alto). __NOTOC__
Janq'u Quta (Aymara &quot;janq'u&quot; white, &quot;quta&quot; lake, &quot;white lake&quot;, Hispanicized spelling &quot;Jankho Khota, Jankho Kkota, Janko Khota, Janko Kota&quot;) is a lake in Bolivia located in the La Paz Department, Pedro Domingo Murillo Province, El Alto Municipality.

Geographic entities mentioned:
surface_form: janq'u quta
instance_of: Lake
countries: Bolivia
coordinates: lat: -16.3
lon: -68.13333333
Janq'u Quta (El Alto). __NOTOC__
Janq'u Quta (Aymara &quot;janq'u&quot; white, &quot;quta&quot; lake, &quot;white lake&quot;, Hispanicized spelling &quot;Jankho Khota, Jankho Kkota, Janko Khota, Janko Kota&quot;) is a lake in Bolivia located in the La Paz Department, Pedro Domingo Murillo Province, El Alto Municipality.

Geographic entities mentioned:
surface_form: janq'u quta (el alto)
instance_of: Lake
countries: Bolivia
coordinates: lat: -16.3
lon: -68.13333333
The boundary between the geological platform made of greywacke hornfels and the underlying fine-grained granite from Brocken runs by the Hohe Klippen. Religion. The population of Sankt Andreasberg is mostly Protestant. Sport. As a result of their elevation, Sankt Andreasberg () and Sonnenberg () still have fairly guaranteed snow.

Geographic entities mentioned:
surface_form: Brocken
instance_of: Mountain
countries: Germany
Kingdom of Prussia
coordinates: lat: 51.800555555556
lon: 10.617222222222
The Innominate. The Innominate () is a mountain peak located in the Bighorn Mountains in the U.S. state of Wyoming. Situated along a knife-like ridge known as an arête, the summit is located in the Cloud Peak Wilderness of Bighorn National Forest. The slightly taller Mount Woolsey is to the northwest. A small glacier lies below the arête to the east. The first recorded ascent was made by W. B.

Geographic entities mentioned:
surface_form: Mount Woolsey
instance_of: Mountain
countries: United States
coordinates: lat: 44.4011
lon: -107.177
The Innominate. The Innominate () is a mountain peak located in the Bighorn Mountains in the U.S. state of Wyoming. Situated along a knife-like ridge known as an arête, the summit is located in the Cloud Peak Wilderness of Bighorn National Forest. The slightly taller Mount Woolsey is to the northwest. A small glacier lies below the arête to the east. The first recorded ascent was made by W. B.

Geographic entities mentioned:
surface_form: cloud peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.382138888889
lon: -107.17391388889
The Innominate. The Innominate () is a mountain peak located in the Bighorn Mountains in the U.S. state of Wyoming. Situated along a knife-like ridge known as an arête, the summit is located in the Cloud Peak Wilderness of Bighorn National Forest. The slightly taller Mount Woolsey is to the northwest. A small glacier lies below the arête to the east. The first recorded ascent was made by W. B.

Geographic entities mentioned:
surface_form: the innominate
instance_of: Mountain
countries: United States
coordinates: lat: 44.3983
lon: -107.174
The Innominate. The Innominate () is a mountain peak located in the Bighorn Mountains in the U.S. state of Wyoming. Situated along a knife-like ridge known as an arête, the summit is located in the Cloud Peak Wilderness of Bighorn National Forest. The slightly taller Mount Woolsey is to the northwest. A small glacier lies below the arête to the east. The first recorded ascent was made by W. B.

Geographic entities mentioned:
surface_form: the innominate
instance_of: Mountain
countries: United States
coordinates: lat: 44.3983
lon: -107.174
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
h. hercegovinensis&quot; populates the coasts of Bosnia and Herzegovina, Croatia, and Montenegro. The oldest known evidence for &quot;T. hermanni&quot; on Sardinia is a fossil from the early Pleistocene of Monte Tuttavista. However, molecular evidence suggests extant populations of both this species and &quot;Emys orbicularis&quot; on Sardinia were actually introduced in recent times.

Geographic entities mentioned:
surface_form: Monte Tuttavista
instance_of: Mountain
countries: Italy
coordinates: lat: 40.38111111111111
lon: 9.638333333333334
The district's operations are supported by Educational Service District 121. In November 2015, the district had a total enrollment of 3,985 students. The Port Angeles School District stretches from McDonald Creek in the east to Lake Crescent in the west, and from the northern coastline of the Straits of Juan de Fuca to the foothills of Olympic National Park in the south.

Geographic entities mentioned:
surface_form: Lake Crescent
instance_of: Lake
countries: United States
coordinates: lat: 48.0595755
lon: -123.8291037
Monte Prado. Monte Prado (or Prato) is a mountain in the northern Apennines, located in the trait between the Pradarena and, with an altitude of. Geography. Monte Prado is right on the boundary between the province of Reggio Emilia and that of Lucca. Environment protection. The mountain is part of the National Park of the Appennino Tosco-Emiliano.

Geographic entities mentioned:
surface_form: monte prado
instance_of: Mountain
countries: Italy
coordinates: lat: 44.25
lon: 10.4075
Graioceli. The Graioceli were a small Gallic tribe dwelling in the valley of Maurienne, in the modern region of Savoie, during the Iron Age. Name. They are mentioned as &quot;Graioceli&quot; (var. &quot;graiocaeli, gaioceli&quot;) by Caesar (mid-1st c. BC). The etymology of the ethnonym &quot;Graioceli&quot; remains unclear.

Geographic entities mentioned:
surface_form: Maurienne
instance_of: Valley
countries: France
coordinates: lat: 45.2
lon: 6.6666666666667
Mount Meek. Mount Meek () is located in the Teton Range, on the border of Caribou-Targhee National Forest and Grand Teton National Park, U.S. state of Wyoming. Mount Meek is west of Mount Meek Pass and about ENE of Mount Jedediah Smith.

Geographic entities mentioned:
surface_form: Mount Jedediah Smith
instance_of: Mountain
countries: United States
coordinates: lat: 43.6822
lon: -110.892
surface_form: mount meek
instance_of: Mountain
countries: United States
coordinates: lat: 43.6858
lon: -110.882
surface_form: mount meek
instance_of: Mountain
countries: United States
coordinates: lat: 43.6858
lon: -110.882
Mount Meek. Mount Meek () is located in the Teton Range, on the border of Caribou-Targhee National Forest and Grand Teton National Park, U.S. state of Wyoming. Mount Meek is west of Mount Meek Pass and about ENE of Mount Jedediah Smith.

Geographic entities mentioned:
surface_form: grand teton
instance_of: Mountain
countries: United States
coordinates: lat: 43.7412
lon: -110.802
surface_form: mount meek
instance_of: Mountain
countries: United States
coordinates: lat: 43.6858
lon: -110.882
Mount Meek. Mount Meek () is located in the Teton Range, on the border of Caribou-Targhee National Forest and Grand Teton National Park, U.S. state of Wyoming. Mount Meek is west of Mount Meek Pass and about ENE of Mount Jedediah Smith.

Geographic entities mentioned:
surface_form: mount meek
instance_of: Mountain
countries: United States
coordinates: lat: 43.6858
lon: -110.882
Lealholm. Lealholm is a small village in the Glaisdale civil parish, in the county of North Yorkshire, England. It is sited at a crossing point of the River Esk, in Eskdale which is within the North York Moors National Park. It is by road from the nearest town of Whitby, and approximately from both Middlesbrough and Scarborough.

Geographic entities mentioned:
surface_form: Eskdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.478
lon: -0.786
The remains of the fording point are still visible next to the arched bridge used today, which dates back to the 17th century. Three roads lead from the centre of the village, one follows the river up the valley towards Danby; the second heads north past the hamlet of Lealholmside and across the moors towards Whitby; and the third leads south, towards Fryup and Rosedale.

Geographic entities mentioned:
surface_form: Rosedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.35
lon: -0.88333333333333
Corno Bianco. Corno Bianco (&quot;Weisshorn&quot; in German) is a mountain of the Pennine Alps. It's a popular climbing destination of Valsesia. Etymology. The literal English translation of &quot;Corno Bianco&quot; is &quot;White Horn&quot;. Geography. The mountain is located around 500 m east from the Dora Baltea/Sesia water divide and is totally included in Valsesia (VC, Italy).

Geographic entities mentioned:
surface_form: Valsesia
instance_of: Valley
countries: Italy
coordinates: lat: 45.816666666667
lon: 8.1333333333333
surface_form: valsesia
instance_of: Valley
countries: Italy
coordinates: lat: 45.816666666667
lon: 8.1333333333333
It's a popular climbing destination of Valsesia. Etymology. The literal English translation of &quot;Corno Bianco&quot; is &quot;White Horn&quot;. Geography. The mountain is located around 500 m east from the Dora Baltea/Sesia water divide and is totally included in Valsesia (VC, Italy). Administratively it belongs to the comunes of Alagna Valsesia and Riva Valdobbia. Access to the summit.

Geographic entities mentioned:
surface_form: Valsesia
instance_of: Valley
countries: Italy
coordinates: lat: 45.816666666667
lon: 8.1333333333333
surface_form: valsesia
instance_of: Valley
countries: Italy
coordinates: lat: 45.816666666667
lon: 8.1333333333333
Administratively it belongs to the comunes of Alagna Valsesia and Riva Valdobbia. Access to the summit. The easiest route for the summit starts from rifugio Abate Carestia (a CAI mountain hut) and follows the southern face and ridge of the mountain passing by Lago Bianco and Lago Nero. It requires some climbing skills.

Geographic entities mentioned:
surface_form: lago nero
instance_of: Lake
countries: Italy
coordinates: lat: 45.504843
lon: 7.873332
surface_form: lago bianco
instance_of: Lake
countries: Italy
coordinates: lat: 45.80833333
lon: 7.87888889
surface_form: lago nero
instance_of: Lake
countries: Italy
coordinates: lat: 45.998497
lon: 9.873984
surface_form: lago nero
instance_of: Lake
countries: Italy
coordinates: lat: 44.562
lon: 9.502
surface_form: lago nero
instance_of: Lake
countries: Italy
coordinates: lat: 44.90108
lon: 6.79467
surface_form: lago nero
instance_of: Lake
countries: Italy
coordinates: lat: 44.115555555556
lon: 10.636944444444
surface_form: lago nero
instance_of: Lake
countries: Italy
coordinates: lat: 45.81638889
lon: 7.87361111
Corno Bianco. Corno Bianco (&quot;Weisshorn&quot; in German) is a mountain of the Pennine Alps. It's a popular climbing destination of Valsesia. Etymology. The literal English translation of &quot;Corno Bianco&quot; is &quot;White Horn&quot;. Geography. The mountain is located around 500 m east from the Dora Baltea/Sesia water divide and is totally included in Valsesia (VC, Italy).

Geographic entities mentioned:
surface_form: corno bianco
instance_of: Mountain
countries: Italy
coordinates: lat: 45.8225522
lon: 7.878678
surface_form: corno bianco
instance_of: Mountain
countries: Italy
coordinates: lat: 46.802777777778
lon: 11.397222222222
surface_form: corno bianco
instance_of: Mountain
countries: Italy
coordinates: lat: 46.354733
lon: 11.443291
It's a popular climbing destination of Valsesia. Etymology. The literal English translation of &quot;Corno Bianco&quot; is &quot;White Horn&quot;. Geography. The mountain is located around 500 m east from the Dora Baltea/Sesia water divide and is totally included in Valsesia (VC, Italy). Administratively it belongs to the comunes of Alagna Valsesia and Riva Valdobbia. Access to the summit.

Geographic entities mentioned:
surface_form: valsesia
instance_of: Valley
countries: Italy
coordinates: lat: 45.816666666667
lon: 8.1333333333333
Eaux-Bonnes is close to the small town of Laruns. It is situated at a height of at the entrance of a fine gorge, overlooking the confluence of two rivers. The village's waters were first documented in the middle of the 14th century. The Eaux-Chaudes spa is south-west of Eaux-Bonnes, and there is fine mountain scenery in the neighbourhood of both places, the Pic de Ger near Eaux-Bonnes.

Geographic entities mentioned:
surface_form: Pic de Ger
instance_of: Mountain
countries: France
coordinates: lat: 42.936439
lon: -0.354214
In 2005, FPL Group acquired Gexa Energy. In 2007, Florida's Public Service Commission rejected a plan by NextEra Energy to build a coal-burning power plant on in Moore Haven, Florida, near the Everglades National Park. The National Park Service raised concerns that the coal plant would contaminate Lake Okeechobee with mercury and harm the Everglades.

Geographic entities mentioned:
surface_form: Lake Okeechobee
instance_of: Lake
countries: United States
coordinates: lat: 26.933333333333
lon: -80.8
He was succeeded in 1808 by William Coulter as Lord Provost. His term of office saw various extensions agreed to the Second New Town including areas around Calton Hill such as Regent Terrace and Royal Terrace. In 1831 the bank merged with Thomas Kinnear & Son to form Kinnear, Smiths & Co.

Geographic entities mentioned:
surface_form: Calton Hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.955278
lon: -3.182222
Career. Giovanelli was appointed as a research fellow at the Commonwealth Solar Observatory (now known as Mount Stromlo Observatory) at Mount Stromlo, Canberra from 1937 to 1939, while he was completing his master's degree. His role as a research fellow at the observatory developed his interest in solar active regions and optical astronomy.

Geographic entities mentioned:
surface_form: Mount Stromlo, Canberra
instance_of: Mountain
countries: Australia
coordinates: lat: -35.316666666667
lon: 149.01666666667
Ritter. Donald Lawrence Ritter (born October 21, 1940) is a former Republican member of the U.S. House of Representatives from Pennsylvania. From 1979 to 1993, Ritter represented Pennsylvania's 15th congressional district, which then included the Lehigh Valley region of the state. Early life and education. Ritter was born in Washington Heights in New York City, the son of Frank and Ruth Ritter.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
Ritter represented the Lehigh Valley region of eastern Pennsylvania, which includes the cities of Allentown, Bethlehem, and Easton, and has hybrid economy of both heavy manufacturing companies and employees and a substantial university and college constituency. U.S. House Committees. In the U.S.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
Lehigh River. In his eastern Pennsylvania district, Ritter promoted the Lehigh River as a linear environmental center to the Lehigh Valley that was central to the leisure, recreation, and creative economic development needs of his constituents. Later, along with neighboring Pennsylvania Congressman Peter H.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
Personal life. Ritter was a resident of Coopersburg, Pennsylvania, in the Lehigh Valley for 25 years, prior to his divorce from his former wife Edith Duerksen Ritter, previously of Canada, with whom he has two children, a son, Jason Alexei, and a daughter, Kristina Larissa. Ritter resides in Washington, D.C., and Warrenton, Virginia, with his partner Victoria Stack.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
WVTF is a listener-supported station, holding periodic fundraisers on the air. The studios and offices are on Kingsbury Lane in Roanoke. WVTF has an effective radiated power (ERP) of 100,000 watts, the maximum for most FM radio stations in the U.S. The transmitter is on Poor Mountain, off Media Way in Bent Mountain, Virginia. WVTF broadcasts using HD Radio technology.

Geographic entities mentioned:
surface_form: Poor Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.1796
lon: -80.1628
It was used primarily to air college telecourses and give broadcasting students a chance to hone their skills. In 1975, WVWR-FM's transmitter was moved from Fishburn Hall on the VWCC campus to Poor Mountain, where most of Roanoke's major radio and television stations have their transmitters. The power also was increased from 4,100 watts to 100,000 watts.

Geographic entities mentioned:
surface_form: Poor Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.1796
lon: -80.1628
Hieronymus Pez. Hieronymus Pez (24 February 1685 &ndash; 14 October 1762) was an Austrian Benedictine librarian and historian. Life. Pez was born at Ybbs. In 1703 he entered the novitiate at Melk Abbey, and was ordained in 1711. He became assistant to his brother Bernhard Pez, after whose death he became librarian. He remained at Melk until his own death.

Geographic entities mentioned:
surface_form: Ybbs
instance_of: Watercourse
countries: Austria
coordinates: lat: 47.7603
lon: 15.2053
Ramachandi Temple. Ramachandi Temple is located at a spot on the banks of the Kusabhadra River where it flows into the Bay of Bengal. It is only 5 km away from Konark in the Puri District of Odisha, India. Goddess Ramachandi, the deity of Konark is thought by some to be the presiding deity of this temple, while others thought it to be the temple of Mayadevi, wife of Surya (Sun God). Location.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Description. The valley is in a region of dissected mountain ranges and valleys in the southern Wasatch Front, with the Wasatch Range on the northeast and the San Pitch Mountains on the southeast. The valley's north-northeast edge borders on the south of Utah Valley and another section of Utah Valley's southwest, the Goshen Valley.

Geographic entities mentioned:
surface_form: Goshen Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.093888888889
lon: -111.93
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Juab Valley is linear, mostly north-south trending, with the major city-center of Nephi adjacent north of the valley center. The extreme north of the valley is adjacent to Santaquin which is located between the three valleys of southwest Utah Valley, east Goshen Valley, and north Juab Valley.

Geographic entities mentioned:
surface_form: goshen valley
instance_of: Valley
countries: United States
coordinates: lat: 40.093888888889
lon: -111.93
surface_form: juab valley
instance_of: Valley
countries: United States
coordinates: lat: 39.5913
lon: -111.962
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
West of Levan it turns southwest then southerly into until it flows into the north end of the Chicken Creek Reservoir. The reservoir is located on the western edge of the valley, just north of the South Hills. The Chicken Creek flows out of the southwest corner of the reservoir and west out of the valley, by way of gap in the southern end of the West Hills.

Geographic entities mentioned:
surface_form: south hills
instance_of: Landform
countries: United States
coordinates: lat: 46.825
lon: -114.015
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
About south of Levan, Little Salt Creek flows west out of San Pitch Mountains and then northwest to the Chicken Creek Reservoir. The Chriss Creek also flows west out of the San Pitch Mountains, about south-southwest of Levan, and then flows southwest across and out of the valley, south of the South Hills, on its way to the Sevier River.

Geographic entities mentioned:
surface_form: south hills
instance_of: Landform
countries: United States
coordinates: lat: 46.825
lon: -114.015
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Juab Valley. The Juab Valley is a long valley located on the eastern edge of Juab County, Utah, United States. Description. The valley is in a region of dissected mountain ranges and valleys in the southern Wasatch Front, with the Wasatch Range on the northeast and the San Pitch Mountains on the southeast.

Geographic entities mentioned:
surface_form: juab valley
instance_of: Valley
countries: United States
coordinates: lat: 39.5913
lon: -111.962
Juab Valley. The Juab Valley is a long valley located on the eastern edge of Juab County, Utah, United States. Description. The valley is in a region of dissected mountain ranges and valleys in the southern Wasatch Front, with the Wasatch Range on the northeast and the San Pitch Mountains on the southeast.

Geographic entities mentioned:
surface_form: juab valley
instance_of: Valley
countries: United States
coordinates: lat: 39.5913
lon: -111.962
surface_form: long valley
instance_of: Landform
countries: United States
coordinates: lat: 37.716666666667
lon: -118.88416666667
surface_form: long valley
instance_of: Valley
countries: United States
coordinates: lat: 39.6833
lon: -115.722
surface_form: long valley
instance_of: Valley
countries: United States
coordinates: lat: 37.3789
lon: -112.573
The eastern end of the northern border of Juab County is on the valley's north; the eastern end of the southern county is on the valley's southeast. Juab Valley is linear, mostly north-south trending, with the major city-center of Nephi adjacent north of the valley center.

Geographic entities mentioned:
surface_form: juab valley
instance_of: Valley
countries: United States
coordinates: lat: 39.5913
lon: -111.962
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
The valley's extreme southwest borders a hilly region on the Sevier River's northeast riverbank-shoreline and Yuba State Park-(Sevier Bridge Reservoir), a stretch of the Sevier that flows north, then northwest to west. The Juab Valley north-south center is south of Nephi, in the region of Sharp.

Geographic entities mentioned:
surface_form: juab valley
instance_of: Valley
countries: United States
coordinates: lat: 39.5913
lon: -111.962
(Both basins are part of the Great Basin, a large endorheic watershed in the Western United States.)
South valley. While the southern part of the valley is part of the Sevier River basin, no streams flow directly into the Sevier River within the Juab Valley. Instead, they flow southwest out of the valley before emptying into the Sevier River.

Geographic entities mentioned:
surface_form: juab valley
instance_of: Valley
countries: United States
coordinates: lat: 39.5913
lon: -111.962
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
(In addition, Gardners Fork, Pigeon Creek, and Deep Creek, all flow west out of the San Pitch Mountains, but dissipate upon [or prior to] reaching the valley floor.)
North valley. The northern part of Juab Valley has Current Creek, which rises on the valley floor (rather than the adjacent mountains) and then flows north into the Mona Reservoir.

Geographic entities mentioned:
surface_form: juab valley
instance_of: Valley
countries: United States
coordinates: lat: 39.5913
lon: -111.962
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Roads. There is one Interstate Highway and four state highways in Juab Valley. Interstate 15 (I-15) enters the southwestern edge of the valley (just southwest of the Chicken Creek Reservoir) and runs north along the foothills on western edge of the valley.

Geographic entities mentioned:
surface_form: juab valley
instance_of: Valley
countries: United States
coordinates: lat: 39.5913
lon: -111.962
The Chriss Creek also flows west out of the San Pitch Mountains, about south-southwest of Levan, and then flows southwest across and out of the valley, south of the South Hills, on its way to the Sevier River. (In addition, Gardners Fork, Pigeon Creek, and Deep Creek, all flow west out of the San Pitch Mountains, but dissipate upon [or prior to] reaching the valley floor.)
North valley.

Geographic entities mentioned:
surface_form: deep creek
instance_of: Watercourse
countries: United States
coordinates: lat: 34.72138888888889
lon: -83.47777777777777
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Creeks and reservoirs. The valley has an east-west water divide, just north of Levan. The streams south of the divide are part of the Sevier River Basin and the streams north of the divide flow north out of the valley toward Utah Lake and are part of the basin of the Great Salt Lake. (Both basins are part of the Great Basin, a large endorheic watershed in the Western United States.)
South valley.

Geographic entities mentioned:
surface_form: salt lake
instance_of: Lake
countries: United States
coordinates: lat: 45.2767785
lon: -98.6946248
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: salt lake
instance_of: Lake
countries: United States
coordinates: lat: 44.965
lon: -96.443611111111
surface_form: salt lake
instance_of: Lake
countries: United States
coordinates: lat: 45.635555555556
lon: -99.9175
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Description. The valley is in a region of dissected mountain ranges and valleys in the southern Wasatch Front, with the Wasatch Range on the northeast and the San Pitch Mountains on the southeast. The valley's north-northeast edge borders on the south of Utah Valley and another section of Utah Valley's southwest, the Goshen Valley.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
The valley's north-northeast edge borders on the south of Utah Valley and another section of Utah Valley's southwest, the Goshen Valley. The eastern end of the northern border of Juab County is on the valley's north; the eastern end of the southern county is on the valley's southeast.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
The extreme north of the valley is adjacent to Santaquin which is located between the three valleys of southwest Utah Valley, east Goshen Valley, and north Juab Valley. The valley's extreme southwest borders a hilly region on the Sevier River's northeast riverbank-shoreline and Yuba State Park-(Sevier Bridge Reservoir), a stretch of the Sevier that flows north, then northwest to west.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
The Juab Valley north-south center is south of Nephi, in the region of Sharp. Sage Valley Pass is located on the west in the West Hills that border the east of a small mountain valley (Sage Valley). The valley was named after the local Native Americans (Uabs, Yuabs, or Yoabs) of the Piute tribe. Creeks and reservoirs. The valley has an east-west water divide, just north of Levan.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
The valley was named after the local Native Americans (Uabs, Yuabs, or Yoabs) of the Piute tribe. Creeks and reservoirs. The valley has an east-west water divide, just north of Levan. The streams south of the divide are part of the Sevier River Basin and the streams north of the divide flow north out of the valley toward Utah Lake and are part of the basin of the Great Salt Lake.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
While the southern part of the valley is part of the Sevier River basin, no streams flow directly into the Sevier River within the Juab Valley. Instead, they flow southwest out of the valley before emptying into the Sevier River. The Chicken Creek flows west out of the San Pitch Mountains (east of Levan).

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423