Sarmila/GeoWiki-Features huggingface dataset:
Collaterally, due to the expropriation and planting of pine trees to prevent the siltation of the reservoir, the following upstream towns were affected: Larrosa, Villanovilla, Bescós de Garcipollera, Bergosa, Acín, and, Yosa de Garcipollera in the Garcipollera valley, now belonging to the municipality of Jaca and Cenarbe in Villanúa.

Geographic entities mentioned:
surface_form: Garcipollera valley
instance_of: Valley
countries: Spain
coordinates: lat: 42.62
lon: -0.4855555555555556
This complex would generate an irrigated area of 30 000 ha in several towns of Navarre and Zaragoza. The reservoirs would be located as follows: Yesa, where the current one is located; Foz de Biniés in the waters of the Veral river; Salvatierra, on the Ezka River, Usún would be located in the Salazar Valley, 6 km from Lumbier.

Geographic entities mentioned:
surface_form: Salazar Valley
instance_of: Valley
countries: Spain
coordinates: lat: 42.89261884
lon: -1.086191576
A collateral effect was the purchase by the Patrimonio Forestal del Estado of the valley of La Garcipollera, which leads to Castiello de Jaca, by means of a decree of forced repopulation to plant laricio pine to prevent erosion and silting of the reservoir.

Geographic entities mentioned:
surface_form: valley of La Garcipollera
instance_of: Valley
countries: Spain
coordinates: lat: 42.62
lon: -0.4855555555555556
Vileshchay. The Vileshchay (,) is a river of Azerbaijan. It is one of the larger rivers of the country, flowing into the Caspian Sea in southeastern Azerbaijan. Overview. The Vilesh is a part of Gizil-Agach State Reserve, an ecological haven for migratory birds, created in 1929. The river is long, with the basin size of. It starts at the Guludash Peak of Talysh Mountains.

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
Overview. The Vilesh is a part of Gizil-Agach State Reserve, an ecological haven for migratory birds, created in 1929. The river is long, with the basin size of. It starts at the Guludash Peak of Talysh Mountains. Along its path, it additionally branches off to Şərətük river on its right (29 km long) and Mətəli river on the left (21 km long).

Geographic entities mentioned:
surface_form: Guludash Peak
instance_of: Mountain
countries: Azerbaijan
It is located in the Marcapata District, Quispicanchi Province in the Cusco Region. Ccolcce lies north to northwest of Yanajasa and Kiswarniyuq. It is situated between the rivers Sayapata and Cajamayu (possibly from Quechua for &quot;rock river&quot;). They flow to the Arasa River &quot;(Araza)&quot; in the north.

Geographic entities mentioned:
surface_form: Yanajasa
instance_of: Mountain
countries: Peru
coordinates: lat: -13.7611
lon: -70.895
surface_form: kiswarniyuq
instance_of: Mountain
countries: Peru
coordinates: lat: -13.7353
lon: -70.8944
surface_form: kiswarniyuq
instance_of: Mountain
countries: Peru
coordinates: lat: -14.8294
lon: -73.7333
surface_form: yanajasa
instance_of: Mountain
countries: Peru
coordinates: lat: -13.7611
lon: -70.895
Ccolcce (Cusco). Ccolcce (possibly from Aymara and Quechua for silver, money) or Jolje Cruz (Spanish &quot;cruz&quot; cross, &quot;silver cross&quot;) is a mountain in the Vilcanota mountain range in the Andes of Peru, about high. It is located in the Marcapata District, Quispicanchi Province in the Cusco Region. Ccolcce lies north to northwest of Yanajasa and Kiswarniyuq.

Geographic entities mentioned:
surface_form: ccolcce
instance_of: Mountain
countries: Peru
coordinates: lat: -13.7139
lon: -70.905
History. Altwis is first mentioned in 1113 as &quot;Altwise&quot;. Geography. Altwis is located in the Seetal valley, at the western foot of the Lindenberg mountain, between Lake Hallwil and Lake Baldegg. The former municipality consists of the village of Altwis. It had an area of. Of this area, 63.8% is used for agricultural purposes, while 29% is forested.

Geographic entities mentioned:
surface_form: Seetal valley
instance_of: Valley
countries: Switzerland
coordinates: lat: 47.23166667
lon: 8.24361111
surface_form: Lake Hallwil
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.284166666666664
lon: 8.216111111111111
surface_form: Lake Baldegg
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.198611111111
lon: 8.2605555555556
Schiedea adamantis. &quot;Schiedea adamantis&quot;, commonly known as Diamond Head schiedea'&quot;, is a species of flowering plant in the family Caryophyllaceae, that is endemic to the island of Oahu in Hawaii. It inhabits low shrublands on steep slopes along the northwest rim of Diamond Head Crater. Associated plants include nehe (&quot;Lipochaeta lobata&quot; var.

Geographic entities mentioned:
surface_form: Diamond Head Crater
instance_of: Mountain
countries: United States
coordinates: lat: 21.259722222222
lon: -157.81175
Diet and hunting. Like other mustelids, this species is a predatory animal, and lizards make up most of its diet. An individual from Wadi El Natrun in Egypt captured in 1903 reportedly had a preference for eating these reptiles over all other food. It also feeds on eggs, birds, insects and small mammals, with rodents of the genus &quot;Gerbillus&quot; being the most commonly taken mammalian prey.

Geographic entities mentioned:
surface_form: Wadi El Natrun
instance_of: Valley
countries: Egypt
coordinates: lat: 30.416666666667
lon: 30.333333333333
Kara-Suu Lake. Kara-Suu Lake () is a rock-dammed lake in Toktogul District of Jalal-Abad Province of Kyrgyzstan. It is located at the altitude of 2022 m in riverbed of Kara-Suu, right tributary of Naryn River.

Geographic entities mentioned:
surface_form: naryn
instance_of: Mountain
countries: Kyrgyzstan
coordinates: lat: 41.359415
lon: 76.471226
Kara-Suu Lake. Kara-Suu Lake () is a rock-dammed lake in Toktogul District of Jalal-Abad Province of Kyrgyzstan. It is located at the altitude of 2022 m in riverbed of Kara-Suu, right tributary of Naryn River.

Geographic entities mentioned:
surface_form: kara-suu lake
instance_of: Lake
countries: Kyrgyzstan
coordinates: lat: 41.55777778
lon: 73.25833333
Suárez lake. zc7tz97qpe1zkdwmalrpzrz20usu" xml:space="preserve">#REDIRECT Suárez Lake

Geographic entities mentioned:
surface_form: suárez lake
instance_of: Lake
countries: Bolivia
coordinates: lat: -14.884908333333
lon: -64.873338888889
Telikol. Telikol (;) is a lake in the Kyzylorda Region, Kazakhstan. The area of the lake lies in the Syrdariya and Shieli districts. The Telikol lake zone includes a Important Bird Area. Geography. Telikol is a cluster of small lakes that lies close to the western edge of the Ashchykol Depression and east of the Daryalyktakyr plain (Дарьялыктакыр). The lakeshores are flat and wide.

Geographic entities mentioned:
surface_form: ashchykol
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 45.13828
lon: 67.28035
surface_form: telikol
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 45.2
lon: 66.56666666666666
surface_form: ashchykol
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 43.5
lon: 70.6
The lakeshores are flat and wide. In years of abundant spring floods, the Sarysu river flows into the Ashchykol Depression from the north, bends westwards, and reaches the Telikol from the east. In such years the water level rises in the whole area, connecting the lakes. The lake bottom is smooth, made up of clay and silt.

Geographic entities mentioned:
surface_form: ashchykol
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 45.13828
lon: 67.28035
surface_form: telikol
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 45.2
lon: 66.56666666666666
surface_form: ashchykol
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 43.5
lon: 70.6
Telikol. Telikol (;) is a lake in the Kyzylorda Region, Kazakhstan. The area of the lake lies in the Syrdariya and Shieli districts. The Telikol lake zone includes a Important Bird Area. Geography. Telikol is a cluster of small lakes that lies close to the western edge of the Ashchykol Depression and east of the Daryalyktakyr plain (Дарьялыктакыр). The lakeshores are flat and wide.

Geographic entities mentioned:
surface_form: telikol
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 45.2
lon: 66.56666666666666
In such years the water level rises in the whole area, connecting the lakes. The lake bottom is smooth, made up of clay and silt. The long Shieli-Telikol Canal was built for irrigation, connecting the lacustrine basin with the Syr Darya river to the south near Shieli. Flora. The Telikol lake area has sparse vegetation made up mainly of saltwort and wormwood, as well as saxaul and tamarisk.

Geographic entities mentioned:
surface_form: telikol
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 45.2
lon: 66.56666666666666
The lake bottom is smooth, made up of clay and silt. The long Shieli-Telikol Canal was built for irrigation, connecting the lacustrine basin with the Syr Darya river to the south near Shieli. Flora. The Telikol lake area has sparse vegetation made up mainly of saltwort and wormwood, as well as saxaul and tamarisk. The western stretches of the lakeshores are covered with reeds.

Geographic entities mentioned:
surface_form: telikol
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 45.2
lon: 66.56666666666666
It was pillaged several times between 814 and 819 by the Normans. The monks built a new abbey at Déas, on the shores of Lac de Grand-Lieu, after obtaining authorization from Louis the Pious, now Emperor, to divert the Boulogne river in 819. Noirmoutier was again sacked by the Vikings in 824, 830 and 835, and the abbey was finally burnt down in 846.

Geographic entities mentioned:
surface_form: Lac de Grand-Lieu
instance_of: Lake
countries: France
coordinates: lat: 47.083333333333
lon: -1.6666666666667
Qum Island. Qum Island or Peschanniy (; 'Sandy Island'), Azeri: Qum adası) is an island in the Bay of Baku, in the Caspian Sea. Geography. Qum Island is in length with a maximum width of. It is a part of the Surakhany raion, located south of Baku, Azerbaijan.

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
Rogue River Wars. The Rogue River Wars were an armed conflict in 1855&ndash;1856 between the U.S. Army, local militias and volunteers, and the Native American tribes commonly grouped under the designation of Rogue River Indians, in the Rogue Valley area of what today is southern Oregon.

Geographic entities mentioned:
surface_form: Rogue Valley
instance_of: Valley
countries: United States
coordinates: lat: 42.440122222222
lon: -122.92615277778
Four of the eight European-Americans were killed; William J. Bailey and George Gay were two survivors. In 1837, as part of the Willamette Cattle Company, Bailey, Gay and others were herding cattle north to the Willamette Valley when Gay shot and killed a native boy in revenge for earlier attacks against whites. The local Indians raided the cattle drive, but killed or drove off only a few cattle.

Geographic entities mentioned:
surface_form: Willamette Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.9
lon: -123.1
Tunnell, a lawyer from Georgetown, Delaware. In the 72nd Congress, he was chairman of the Committee to Audit and Control the Contingent Expenses. He was also a member of the Mount Rushmore National Memorial Commission in 1939 and 1940. Death and legacy. Townsend died at age 92 in Philadelphia, and is buried in the Red Men's Cemetery at Selbyville.

Geographic entities mentioned:
surface_form: Mount Rushmore
instance_of: Mountain
countries: United States
coordinates: lat: 43.878947222222
lon: -103.459825
Mount Craddock. Mount Craddock is a large, bold mountain forming the south extremity of Craddock Massif in Sentinel Range, the ninth highest mountain in Antarctica. It is linked by Karnare Col to Mount Strybing in the southern Sentinel Range. The ninth-highest mountain in Antarctica was first climbed in January 1992.

Geographic entities mentioned:
surface_form: Mount Strybing
instance_of: Mountain
coordinates: lat: -78.683333333333
lon: -85.066666666667
surface_form: southern
instance_of: Mountain
coordinates: lat: -74.2
lon: -76.4667
surface_form: strybing
instance_of: Mountain
coordinates: lat: -78.683333333333
lon: -85.066666666667
During 1960–61, Craddock led a Minnesota geological expedition in examining the Jones Mountains. Mount Craddock is the second-highest point of the Craddock Massif which includes Mount Rutford (highest point), Rada Peak, and Bugueño Pinnacle. Rutford was named for R. H. Rutford, Antarctic geologist and colleague of Craddock.

Geographic entities mentioned:
surface_form: Mount Rutford
instance_of: Mountain
coordinates: lat: -78.6
lon: -85.3
surface_form: rada peak
instance_of: Mountain
coordinates: lat: -78.61666667
lon: -85.21666667
surface_form: craddock
instance_of: Mountain
coordinates: lat: -78.633333333333
lon: -85.2
surface_form: craddock
instance_of: Mountain
coordinates: lat: -78.633333333333
lon: -85.2
surface_form: mount craddock
instance_of: Mountain
coordinates: lat: -78.633333333333
lon: -85.2
surface_form: bugueño pinnacle
instance_of: Mountain
coordinates: lat: -78.61666667
lon: -85.25
surface_form: rutford
instance_of: Mountain
coordinates: lat: -78.6
lon: -85.3
Mount Craddock is the second-highest point of the Craddock Massif which includes Mount Rutford (highest point), Rada Peak, and Bugueño Pinnacle. Rutford was named for R. H. Rutford, Antarctic geologist and colleague of Craddock. Rada Peak and Bugueño Pinnacle were named for Camilo Rada and Manuel Bugueño, climbing partners of Damien Gildea, a leading Antarctic researcher and climber.

Geographic entities mentioned:
surface_form: rada peak
instance_of: Mountain
coordinates: lat: -78.61666667
lon: -85.21666667
surface_form: bugueño pinnacle
instance_of: Mountain
coordinates: lat: -78.61666667
lon: -85.25
The mountain was named by US-ACAN for J. Campbell Craddock (1930–2006), leader of a University of Minnesota expedition (1962–63) that made geological investigations and cartographic surveys in the Sentinel and Heritage Ranges of the Ellsworth Mountains. During 1960–61, Craddock led a Minnesota geological expedition in examining the Jones Mountains.

Geographic entities mentioned:
surface_form: campbell
instance_of: Mountain
coordinates: lat: -84.91667
lon: -174
surface_form: craddock
instance_of: Mountain
coordinates: lat: -78.633333333333
lon: -85.2
Mount Craddock. Mount Craddock is a large, bold mountain forming the south extremity of Craddock Massif in Sentinel Range, the ninth highest mountain in Antarctica. It is linked by Karnare Col to Mount Strybing in the southern Sentinel Range. The ninth-highest mountain in Antarctica was first climbed in January 1992.

Geographic entities mentioned:
surface_form: craddock
instance_of: Mountain
coordinates: lat: -78.633333333333
lon: -85.2
surface_form: mount craddock
instance_of: Mountain
coordinates: lat: -78.633333333333
lon: -85.2
Mount Craddock. Mount Craddock is a large, bold mountain forming the south extremity of Craddock Massif in Sentinel Range, the ninth highest mountain in Antarctica. It is linked by Karnare Col to Mount Strybing in the southern Sentinel Range. The ninth-highest mountain in Antarctica was first climbed in January 1992.

Geographic entities mentioned:
surface_form: craddock
instance_of: Mountain
coordinates: lat: -78.633333333333
lon: -85.2
surface_form: craddock
instance_of: Mountain
coordinates: lat: -78.633333333333
lon: -85.2
surface_form: mount craddock
instance_of: Mountain
coordinates: lat: -78.633333333333
lon: -85.2
The ninth-highest mountain in Antarctica was first climbed in January 1992. The name Mount Craddock was originally recommended by the Advisory Committee on Antarctic Names (US-ACAN) in 1965 for the present-day Craddock Massif but subsequent maps limited Mount Craddock to the massif's southernmost peak, a position that became established over years.

Geographic entities mentioned:
surface_form: craddock
instance_of: Mountain
coordinates: lat: -78.633333333333
lon: -85.2
surface_form: craddock
instance_of: Mountain
coordinates: lat: -78.633333333333
lon: -85.2
surface_form: craddock
instance_of: Mountain
coordinates: lat: -78.633333333333
lon: -85.2
surface_form: mount craddock
instance_of: Mountain
coordinates: lat: -78.633333333333
lon: -85.2
surface_form: mount craddock
instance_of: Mountain
coordinates: lat: -78.633333333333
lon: -85.2
To avoid confusion and to fix the position of the name, US-ACAN redefined Mount Craddock in 2006 to apply to the southernmost peak described above. The mountain was named by US-ACAN for J.

Geographic entities mentioned:
surface_form: craddock
instance_of: Mountain
coordinates: lat: -78.633333333333
lon: -85.2
surface_form: mount craddock
instance_of: Mountain
coordinates: lat: -78.633333333333
lon: -85.2
The mountain was named by US-ACAN for J. Campbell Craddock (1930–2006), leader of a University of Minnesota expedition (1962–63) that made geological investigations and cartographic surveys in the Sentinel and Heritage Ranges of the Ellsworth Mountains. During 1960–61, Craddock led a Minnesota geological expedition in examining the Jones Mountains.

Geographic entities mentioned:
surface_form: craddock
instance_of: Mountain
coordinates: lat: -78.633333333333
lon: -85.2
Mount Craddock is the second-highest point of the Craddock Massif which includes Mount Rutford (highest point), Rada Peak, and Bugueño Pinnacle. Rutford was named for R. H. Rutford, Antarctic geologist and colleague of Craddock. Rada Peak and Bugueño Pinnacle were named for Camilo Rada and Manuel Bugueño, climbing partners of Damien Gildea, a leading Antarctic researcher and climber.

Geographic entities mentioned:
surface_form: craddock
instance_of: Mountain
coordinates: lat: -78.633333333333
lon: -85.2
surface_form: rutford
instance_of: Mountain
coordinates: lat: -78.6
lon: -85.3
During 1960–61, Craddock led a Minnesota geological expedition in examining the Jones Mountains. Mount Craddock is the second-highest point of the Craddock Massif which includes Mount Rutford (highest point), Rada Peak, and Bugueño Pinnacle. Rutford was named for R. H. Rutford, Antarctic geologist and colleague of Craddock.

Geographic entities mentioned:
surface_form: rutford
instance_of: Mountain
coordinates: lat: -78.6
lon: -85.3
The river fulfills demands for agricultural irrigation in Danishpet village. The Sarabanga flows through the towns of Danishpet, Omalur, Thoppur, Tharamangalam, Dhadhapuram, Idappadi, Chettipatti, Peramachipalayam, and Thevur, and joins the Kaveri River near Kaniyalampatti, before flowing into the Bay of Bengal. Annamar Kovil, a Hindu temple, stands near the confluence of the two rivers.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
The river then runs through Danishpet, Kadayampatti, Pannapatti before joining the Periyaaru at Omalur. From Omalur, the Sarabanga river flows south-westwards, passing through K.R. Thoppur, Chinnapampatti, Dhadhapuram, Edappadi, Thevur, while feeding number of lakes. The Sarabanga river joins the Kaveri river in Pullagoundampatti, Salem near Annamar Kovil. See also. List of rivers of Tamil Nadu

Geographic entities mentioned:
surface_form: Kaveri
instance_of: Watercourse
countries: India
coordinates: lat: 11.370345
lon: 79.828105
On the north it borders the comarca of Los Montes on the southern border of the Cordillera Subbética; on the north west are the Sierra de Loja and El Hacho; on the southwest the Sierra Gorda; in the south the Sierra de la Almijara; and in the east the aforementioned Sierra Nevada. It is one of the series of valleys forming the Surco Intrabético.

Geographic entities mentioned:
surface_form: Surco Intrabético
instance_of: Valley
countries: Spain
coordinates: lat: 37.3
lon: -3.18333
On the north it borders the comarca of Los Montes on the southern border of the Cordillera Subbética; on the north west are the Sierra de Loja and El Hacho; on the southwest the Sierra Gorda; in the south the Sierra de la Almijara; and in the east the aforementioned Sierra Nevada. It is one of the series of valleys forming the Surco Intrabético.

Geographic entities mentioned:
surface_form: hacho
instance_of: Mountain
countries: Spain
coordinates: lat: 35.8969252
lon: -5.2867421
It is one of the series of valleys forming the Surco Intrabético. The two easiest points of communication with the outside world are the threshold between the Sierra Nevada and the Sierra de la Almijara (the Lecrin Valley) and the gorge of the River Genil in the Infiernos de Loja, which separates El Hacho from the Sierra Gorda.

Geographic entities mentioned:
surface_form: hacho
instance_of: Mountain
countries: Spain
coordinates: lat: 35.8969252
lon: -5.2867421
Granada Basin. The Granada Basin, Depression of Granada or Granada Depression () is a totally enclosed valley in Andalusia, Spain. The river Genil runs through the valley upon exiting from the Sierra Nevada until it passes through the Infiernos de Loja.

Geographic entities mentioned:
surface_form: granada basin
instance_of: Valley
countries: Spain
coordinates: lat: 37.1
lon: -3.83333333
Granada Basin. The Granada Basin, Depression of Granada or Granada Depression () is a totally enclosed valley in Andalusia, Spain. The river Genil runs through the valley upon exiting from the Sierra Nevada until it passes through the Infiernos de Loja.

Geographic entities mentioned:
surface_form: granada basin
instance_of: Valley
countries: Spain
coordinates: lat: 37.1
lon: -3.83333333
surface_form: depression of granada
instance_of: Valley
countries: Spain
coordinates: lat: 37.1
lon: -3.83333333
The river and its tributaries were carved out, and after the Quaternary climate crisis, river terraces formed. The River Genil has two well-defined terraces. The deepening of the Depression of Granada at the foot of the Sierra Nevada led to the formation of a flooded area between Santa Fe and Granada.

Geographic entities mentioned:
surface_form: depression of granada
instance_of: Valley
countries: Spain
coordinates: lat: 37.1
lon: -3.83333333
The Quaternary also produced a diapiric uprising of a mass of gypsum clay to the height of the town of Láchar, which made area from Láchar to Granada more easily flooded, and broke the original depression into two units the Depression of Granada and the &quot;Pasillo&quot; or Depression of Loja.

Geographic entities mentioned:
surface_form: depression of granada
instance_of: Valley
countries: Spain
coordinates: lat: 37.1
lon: -3.83333333
Qian's face also replaced the faces of Jake Gyllenhaal on a &quot;Brokeback Mountain&quot; poster and Tom Hanks on a &quot;The Da Vinci Code&quot; poster, and his face had also replaced one of the faces on an image of Mount Rushmore in the United States. In one photograph Qian's face appeared on a man next to President of the United States George W. Bush.

Geographic entities mentioned:
surface_form: Mount Rushmore
instance_of: Mountain
countries: United States
coordinates: lat: 43.878947222222
lon: -103.459825
Monte Nero (Picentini). Monte Nero is a mountain of Campania, Italy.

Geographic entities mentioned:
surface_form: picentini
instance_of: Mountain
countries: Italy
coordinates: lat: 40.75
lon: 15
surface_form: monte nero
instance_of: Mountain
countries: Italy
coordinates: lat: 40.41444444
lon: 15.10083333
Monte Nero (Picentini). Monte Nero is a mountain of Campania, Italy.

Geographic entities mentioned:
surface_form: monte nero
instance_of: Mountain
countries: Italy
coordinates: lat: 40.41444444
lon: 15.10083333
Monte Mutria. The Monte Mutria is a mountain in the Matese mountain range, part of the central-southern Apennines, southern Italy. Having an altitude of 1,822 m, it is located in the eastern part of the massif, on the boundary between Molise and Campania.

Geographic entities mentioned:
surface_form: monte mutria
instance_of: Mountain
countries: Italy
coordinates: lat: 41.385
lon: 14.523333333333
surface_form: mutria
instance_of: Mountain
countries: Italy
coordinates: lat: 41.385
lon: 14.523333333333
The mountain sits about southwest of the village of Fossbergom and about northeast of the village of Øvre Årdal. The mountain is surrounded by several other notable mountains including Loftet and Veslfjelltinden to the north; Skagsnebb to the northeast; Galdhøpiggen and Sauhøi to the east; Storbreahøe, Storbreatinden, and Rundhøe to the southeast; and Store Smørstabbtinden and Kniven to the south.

Geographic entities mentioned:
surface_form: Loftet
instance_of: Mountain
countries: Norway
coordinates: lat: 61.62305556
lon: 8.12611111
surface_form: Veslfjelltinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.6103
lon: 8.11361
surface_form: Skagsnebb
instance_of: Mountain
countries: Norway
coordinates: lat: 61.607781
lon: 8.151181
surface_form: Galdhøpiggen
instance_of: Mountain
countries: Norway
coordinates: lat: 61.633333333333
lon: 8.3
surface_form: Sauhøi
instance_of: Mountain
countries: Norway
coordinates: lat: 61.60122
lon: 8.20591
surface_form: Storbreahøe
instance_of: Mountain
countries: Norway
coordinates: lat: 61.58944444
lon: 8.14472222
surface_form: Storbreatinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.5872
lon: 8.12611
surface_form: Store Smørstabbtinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.571666666667
lon: 8.1191666666667
surface_form: Kniven
instance_of: Mountain
countries: Norway
coordinates: lat: 61.568055555556
lon: 8.125
surface_form: rundhøe
instance_of: Mountain
countries: Norway
coordinates: lat: 61.57456
lon: 8.17869
surface_form: smørstabbtinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.57001
lon: 8.12111
surface_form: smørstabbtinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.571666666667
lon: 8.1191666666667
Veslbreatinden. Veslbreatinden is a mountain in Lom Municipality in Innlandet county, Norway. The tall mountain is located in the Jotunheimen mountains just to the north of Jotunheimen National Park. The mountain sits about southwest of the village of Fossbergom and about northeast of the village of Øvre Årdal.

Geographic entities mentioned:
surface_form: veslbreatinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.5936
lon: 8.11167
BN-350 reactor. The BN-350 was a sodium-cooled, fast reactor located at the &quot;Mangyshlak Nuclear Power Plant&quot; (or &quot;Mangyshlak Atomic Energy Combine&quot;), located in Aktau (formerly known as Shevchenko), Kazakhstan, on the shore of the Caspian Sea. Construction of the BN-350 fast breeder reactor began in 1964, and the plant first produced electricity in 1973.

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
Westport, Ontario. Westport is a village in the United Counties of Leeds and Grenville, Eastern Ontario, Canada. It lies at the west end of Upper Rideau Lake, at the head of the navigable Rideau Canal system, southwest of Ottawa. The village of Westport was incorporated as an independent municipality in 1904. It is an enclave within the Township of Rideau Lakes. History.

Geographic entities mentioned:
surface_form: Upper Rideau Lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.682
lon: -76.336
Yellow perch, smallmouth bass, pickerel, and Northern pike populate the waters. Foley Mountain Conservation Area, the highest conservation area in the Rideau Valley, is a picturesque park overlooking Westport. It features a variety of wildlife in 308 hectares (2.4 km2) of woods and fields. The area also has a sandy beach with changing facilities.

Geographic entities mentioned:
surface_form: Rideau Valley
instance_of: Valley
countries: Canada
Isle Royale Queen IV. &quot;Isle Royale Queen IV&quot; is a passenger ferry operating on Lake Superior between Copper Harbor, Michigan, and Isle Royale National Park, the largest island on Lake Superior and the State of Michigan's only national park. The ferry operates from mid-May to the end of September each year. In the months of June, July, and August the ferry operates nearly every day.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
Cultural and religious life. To move from the Sihl Valley to Dürnten was &quot;perfect&quot; – among other things, the building is furthermore located in a valley and on a stream, as for the temple festival the flowing water is of particular importance. Every Friday evening between 100 and 150 people attend the &quot;Pooja&quot;, and on other weekdays 10 to 20 attend.

Geographic entities mentioned:
surface_form: Sihl Valley
instance_of: Valley
countries: Switzerland
coordinates: lat: 47.266666666667
lon: 8.5666666666667
Upon the deaths of her aunts Mara and Kantakouzene in 1487 and 1490 respectively, Maria inherited their possessions in accordance with the Islamic Sharia law. She immediately launched a claim to icons left by Mara to the Christian monastery of Great Lavra on Mount Athos.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
The first possible alignment (approximately 4.5 km) would be a parallel link several hundred metres directly to the east of the existing bridge, while the second alignment (approximately 6.5 km) would start in the same general environs in the North Shore, but travel diagonally southeastwards to link up with the motorway at Grafton Gully, east of the Auckland CBD.

Geographic entities mentioned:
surface_form: Grafton Gully
instance_of: Valley
countries: New Zealand
coordinates: lat: -36.858711111111
lon: 174.76667777778
In medieval Bosnia, Vitovlje was in the Parish of Mel (Župa Mel). Through the settlement the Dedića potok (Dedići's stream) flows through the settlement, a tributary of the Ugar, south of the Korićani's Rocks. The Pougarje stretches from Vitovlje, along the Ugar, between the mountains of Ranča and Ugarske stijene (Ugar's Rocks).

Geographic entities mentioned:
surface_form: Korićani's Rocks
instance_of: Landform
countries: Bosnia and Herzegovina
coordinates: lat: 44.28333333333333
lon: 17.666666666666668
Through the settlement the Dedića potok (Dedići's stream) flows through the settlement, a tributary of the Ugar, south of the Korićani's Rocks. The Pougarje stretches from Vitovlje, along the Ugar, between the mountains of Ranča and Ugarske stijene (Ugar's Rocks). At the last census in 1991, before the collapse of Yugoslavia, Vitovlje had 708 inhabitants.

Geographic entities mentioned:
surface_form: Ranča
instance_of: Mountain
countries: Bosnia and Herzegovina
coordinates: lat: 44.36277778
lon: 17.40972222
Charles Borromeo Church (North Hollywood). St. Charles Borromeo Church is a Catholic church and elementary school in North Hollywood, Los Angeles, California. It is one of the oldest parishes in the San Fernando Valley, dating back to 1921. It has long been a parish with celebrity members and was the site of funerals for Bob Hope, Dorothy Lamour, and Robert Urich, among other notables. Beginnings.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
For example, in 1907 there were eight brush and brushwood factories in Ramberg. The raw materials, especially wood and Common Broom, were obtained &quot;inter alia&quot; from the Holpertal valley, which begins just northeast of Ramberg. The Ramberg brush merchants sold their wares not just across the whole of Germany, but also in other European countries. Museum.

Geographic entities mentioned:
surface_form: Holpertal
instance_of: Valley
countries: Germany
coordinates: lat: 49.2708
lon: 8.01484
The Green Bowl. The Green Bowl is a gorge just southeast of Kinuseo Falls at the north end of Monkman Provincial Park in the Northern Rockies of British Columbia, Canada, northeast of the city of Prince George and south of the community of Tumbler Ridge. &quot;The Green Bowl was a place of serenity and beauty.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: the green bowl
instance_of: Valley
countries: Canada
coordinates: lat: 54.7528
lon: -121.174
The Green Bowl. The Green Bowl is a gorge just southeast of Kinuseo Falls at the north end of Monkman Provincial Park in the Northern Rockies of British Columbia, Canada, northeast of the city of Prince George and south of the community of Tumbler Ridge. &quot;The Green Bowl was a place of serenity and beauty.

Geographic entities mentioned:
surface_form: the green bowl
instance_of: Valley
countries: Canada
coordinates: lat: 54.7528
lon: -121.174
The Green Bowl is a gorge just southeast of Kinuseo Falls at the north end of Monkman Provincial Park in the Northern Rockies of British Columbia, Canada, northeast of the city of Prince George and south of the community of Tumbler Ridge. &quot;The Green Bowl was a place of serenity and beauty. Each end narrowed to a rock cleft which could be sealed off by poles to prevent the horses wandering.

Geographic entities mentioned:
surface_form: the green bowl
instance_of: Valley
countries: Canada
coordinates: lat: 54.7528
lon: -121.174
Classification. Lombardic is classified as part of the Upper German group of West Germanic languages, descended from Elbe Germanic, and most closely related to its geographical neighbours Alemannic and Bavarian. This is consistent with the accounts of classical historians, and indeed with the archaeological evidence of Langobardic settlement along the river Elbe.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
&quot;The Fearway&quot; is a 2023 American horror film directed by Robert Gajic and starring Shannon Dalonzo, Eileen Dietz, Simon Phillips, and Jessica Gray. Plot. A young couple is traveling in their car along the famous Highway 66, which runs through Death Valley. Suddenly, they notice a strange pursuer behind them. This trip turns into a real repeated nightmare in a time loop for them.

Geographic entities mentioned:
surface_form: Death Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.45693888888889
lon: -116.86528055555556
In the 1920s, the area was popular with industrialists who erected villas and mountain hostels in the town. In 1927, mountain shelters on Mount Klimczok and Sampolska Pass were built. In 1933, the popular shelter on Skrzyczne was opened. Following the 1939 Invasion of Poland, which started World War II, Szczyrk was occupied by Nazi Germany and annexed to the German Province of Upper Silesia.

Geographic entities mentioned:
surface_form: Skrzyczne
instance_of: Mountain
countries: Poland
coordinates: lat: 49.684444444444
lon: 19.030277777778
After World War II, the town experienced a tourist boom. Thanks to its picturesque location and Silesian Beskids mountains, it became a popular and well-known resort town and a winter sports center. In 1959, a chairlift leading to Mount Skrzyczne was opened becoming one of the top tourist attractions of the town. In 1973, Szczyrk was granted city rights. Tourism and geography.

Geographic entities mentioned:
surface_form: Mount Skrzyczne
instance_of: Mountain
countries: Poland
coordinates: lat: 49.684444444444
lon: 19.030277777778
Poland's Winter Olympics athletes train in Szczyrk for events such as skiing and ski jumping. The two mountain ranges that surround the valley are dominated by the peaks of Skrzyczne at and Klimczok, both of significant interest to tourists since they have commanding views from either peak. Moreover, both peaks are accessible to most people in one day's hike via the tourist routes.

Geographic entities mentioned:
surface_form: Skrzyczne
instance_of: Mountain
countries: Poland
coordinates: lat: 49.684444444444
lon: 19.030277777778
Skrzyczne is also accessible via a chairlift. To the west of Szczyrk is Wisła, a town where the source of the Vistula (Wisła) river can be found (around the Barania Góra mountain). The town is home Mercure Szczyrk Resort, Europe's longest hotel, which opened in 2024 and measures 330 meters (1,082 ft) in length.

Geographic entities mentioned:
surface_form: Barania Góra
instance_of: Mountain
countries: Poland
coordinates: lat: 49.611388888889
lon: 19.010555555556
It was named after HMS &quot;Britannia&quot;, a vessel utilized as the Britannia Royal Naval College in England, which had been attended by several officers of Scott's expedition. Location. The Britannia Range is east of the Antarctic Plateau. It is south of the Darwin Mountains and the Cook Mountains, which are north of the Hatherton Glacier and the Darwin Glacier.

Geographic entities mentioned:
surface_form: Antarctic Plateau
instance_of: Plateau
coordinates: lat: -90
lon: 0
Others have been found across the country, including near Bishoftu and Wondo Genet. The spider thrives in grasslands, particularly near water. It has been collected on grass on a rock face near Lake Ziway at an altitude of above sea level. Another specimen was found near Hawassa in lush grass near a stream at a height of above sea level.

Geographic entities mentioned:
surface_form: Lake Ziway
instance_of: Lake
countries: Ethiopia
coordinates: lat: 8
lon: 38.83
Other parts of the duchies were ruled by the Dukes of Schleswig-Holstein-Gottorp. The territories of Holstein-Glückstadt are located in present-day Denmark and Germany. The main centre of administration was Segeberg and from 1648 Glückstadt (founded in 1617) on the River Elbe. History.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
He was defeated by Dacke's constantly growing army of peasants. Other attempts to defeat Dacke militarily also failed. Dacke and his army reached as far north as Mjölby at the fringes of the Östergötland plains () and enjoyed widespread support around Sommen and Ydre. Local aristocrat Måns Johansson (Natt och Dag) sided with the king despite having a troublesome relation to him.

Geographic entities mentioned:
surface_form: Sommen
instance_of: Lake
countries: Sweden
coordinates: lat: 58.015833333333
lon: 15.176944444444
Petite rivière à l'Ours - West. The Petite rivière à l'Ours - West (&quot;English: &quot;Little Bear River&quot; - West&quot;) is a tributary of rivière à l'Ours, flowing in the municipality of Saint-Félicien, in the Le Domaine-du-Roy Regional County Municipality, in the administrative region of Saguenay–Lac-Saint-Jean, in the province of Quebec, in Canada.

Geographic entities mentioned:
surface_form: saint-jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
surface_form: petite rivière à l'ours
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.22810277777778
lon: -77.91514166666667
surface_form: rivière à l'ours
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.24194
lon: -77.9625
surface_form: rivière à l'ours
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.24194
lon: -77.9625
surface_form: rivière à l'ours
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.29833305555555
lon: -63.058055
surface_form: rivière à l'ours
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.29833305555555
lon: -63.058055
surface_form: petite rivière
instance_of: Watercourse
countries: Canada
coordinates: lat: 44.226597
lon: -64.434607
surface_form: petite rivière à l'ours - west
instance_of: Watercourse
countries: Canada
coordinates: lat: 48.616769444444444
lon: -72.44908055555555
surface_form: bear river
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.2833
lon: -126.967
surface_form: rivière à l'ours
instance_of: Watercourse
countries: Canada
coordinates: lat: 48.646666666667
lon: -72.390555555556
surface_form: rivière à l'ours
instance_of: Watercourse
countries: Canada
coordinates: lat: 48.646666666667
lon: -72.390555555556
Geography. From the mouth of the Little Bear River, the current successively descends the course of the rivière à l'Ours] over east, then northeast; the Ashuapmushuan River towards the south-east on; then crosses lake Saint-Jean east on (ie its full length), follows the course of the Saguenay River via the Petite Décharge on east to Tadoussac where it merges with the Saint Lawrence Estuary.

Geographic entities mentioned:
surface_form: saint-jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
surface_form: rivière à l'ours
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.24194
lon: -77.9625
surface_form: rivière à l'ours
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.24194
lon: -77.9625
surface_form: rivière à l'ours
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.29833305555555
lon: -63.058055
surface_form: rivière à l'ours
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.29833305555555
lon: -63.058055
surface_form: bear river
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.2833
lon: -126.967
surface_form: rivière à l'ours
instance_of: Watercourse
countries: Canada
coordinates: lat: 48.646666666667
lon: -72.390555555556
surface_form: rivière à l'ours
instance_of: Watercourse
countries: Canada
coordinates: lat: 48.646666666667
lon: -72.390555555556
Petite rivière à l'Ours - West. The Petite rivière à l'Ours - West (&quot;English: &quot;Little Bear River&quot; - West&quot;) is a tributary of rivière à l'Ours, flowing in the municipality of Saint-Félicien, in the Le Domaine-du-Roy Regional County Municipality, in the administrative region of Saguenay–Lac-Saint-Jean, in the province of Quebec, in Canada.

Geographic entities mentioned:
surface_form: petite rivière à l'ours
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.22810277777778
lon: -77.91514166666667
surface_form: rivière à l'ours
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.24194
lon: -77.9625
surface_form: rivière à l'ours
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.29833305555555
lon: -63.058055
surface_form: petite rivière
instance_of: Watercourse
countries: Canada
coordinates: lat: 44.226597
lon: -64.434607
surface_form: petite rivière à l'ours - west
instance_of: Watercourse
countries: Canada
coordinates: lat: 48.616769444444444
lon: -72.44908055555555
surface_form: rivière à l'ours
instance_of: Watercourse
countries: Canada
coordinates: lat: 48.646666666667
lon: -72.390555555556
The upper part of the Petite Rivière à l'Ours valley is served by forest roads. The lower part is served by chemin du rang Simple, chemin du rang Double and rue Notre-Dame. Forestry is the main economic activity in the upper part of this valley; agriculture, for the lower part.

Geographic entities mentioned:
surface_form: petite rivière à l'ours
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.22810277777778
lon: -77.91514166666667
surface_form: rivière à l'ours
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.24194
lon: -77.9625
surface_form: rivière à l'ours
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.29833305555555
lon: -63.058055
surface_form: petite rivière
instance_of: Watercourse
countries: Canada
coordinates: lat: 44.226597
lon: -64.434607
surface_form: petite rivière à l'ours
instance_of: Watercourse
countries: Canada
coordinates: lat: 48.616769444444444
lon: -72.44908055555555
surface_form: rivière à l'ours
instance_of: Watercourse
countries: Canada
coordinates: lat: 48.646666666667
lon: -72.390555555556
Forestry is the main economic activity in the upper part of this valley; agriculture, for the lower part. The surface of the Little Bear River is usually frozen from the beginning of December to the end of March, except the rapids areas; however, safe traffic on the ice is generally from mid-December to mid-March. Geography.

Geographic entities mentioned:
surface_form: bear river
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.2833
lon: -126.967
Toponymy. The rivière à l'Ours has two tributaries with the same toponymic designation: Little Bear River. The watercourse covered by this article constitutes the western branch. The toponym &quot;Little Bear River&quot; was formalized on December 5, 1968, at the Place Names Bank of the Commission de toponymie du Québec.

Geographic entities mentioned:
surface_form: bear river
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.2833
lon: -126.967
Hot Well Dunes. Hot Well Dunes is a hot spring in the San Simeon Valley of Arizona, located on BLM land southeast of the town of Safford. Description. Hot Well Dunes are a series of artesian hot spring wells that are surrounded by 2000 acres of open BLM land. Camping is permitted at the site for a maximum stay of two weeks.

Geographic entities mentioned:
surface_form: San Simeon Valley
instance_of: Valley
countries: United States
coordinates: lat: 32.8017
lon: -109.633
There are also more primitive soaking areas on-site surrounded by cattails that also provide habitat for wildlife and fish. Location. Hot Well Dunes are located on BLM land in a remote location the San Simon Valley, far away from any cities or towns. History. The hot springs were discovered in the late 1920s in this remote area as a during an oil exploration drilling operation.

Geographic entities mentioned:
surface_form: San Simon Valley
instance_of: Valley
countries: United States
coordinates: lat: 32.8017
lon: -109.633
Neermahal. Neermahal also known as Twijilikma Nuyung () is a former royal palace of Tripura Kingdom, built by Maharaja Bir Bikram Kishore Manikya bahadur in 1930. It is also the largest water palace in India. The palace is situated in the middle of Rudrasagar Lake (Twijilikma), in Melaghar 53 kilometers away from Agartala, the capital of Tripura. History.

Geographic entities mentioned:
surface_form: Rudrasagar Lake
instance_of: Lake
countries: India
coordinates: lat: 23.504
lon: 91.315
Maharaja Bir Bikram Kishore Manikya Debbarma, of the‘Manikya Dynasty’, which is supposed to be the second longest remaining dynasty in the world today, built this palace in 1921. In 1921, the Maharaja commissioned the British company, Martin and Burns to build a unique water palace in the middle of Lake Rudrasagar.

Geographic entities mentioned:
surface_form: Lake Rudrasagar
instance_of: Lake
countries: India
coordinates: lat: 23.504
lon: 91.315
Lundevatn. Lundevatn, or Lundevatnet, is a lake on the borders between the municipalities of Lund (in Rogaland county) and Flekkefjord (in Agder county) in Norway. The village of Moi lies at the northern end of the lake and the smaller village of Åna-Sira lies just south of the southern end of the lake.

Geographic entities mentioned:
surface_form: lundevatnet
instance_of: Lake
countries: Norway
coordinates: lat: 58.401666666667
lon: 6.6072222222222
surface_form: lundevatn
instance_of: Lake
countries: Norway
coordinates: lat: 58.401666666667
lon: 6.6072222222222
Lundevatn. Lundevatn, or Lundevatnet, is a lake on the borders between the municipalities of Lund (in Rogaland county) and Flekkefjord (in Agder county) in Norway. The village of Moi lies at the northern end of the lake and the smaller village of Åna-Sira lies just south of the southern end of the lake.

Geographic entities mentioned:
surface_form: lundevatn
instance_of: Lake
countries: Norway
coordinates: lat: 58.401666666667
lon: 6.6072222222222
It also may signify a less concentrated, more affordable, version of a popular perfume. History. The original &quot;Eau de Cologne&quot; is a spirit-citrus perfume launched in Cologne in 1709 by Giovanni Maria Farina (1685–1766), an Italian perfume maker from Santa Maria Maggiore, Valle Vigezzo.

Geographic entities mentioned:
surface_form: Valle Vigezzo
instance_of: Valley
countries: Italy
coordinates: lat: 46.1333
lon: 8.55