Sarmila/GeoWiki-Features huggingface dataset:
Kullu Valley. Kullu Valley is a broad open valley in Himachal Pradesh, India, formed by the Beas River between Manali and Larji. This valley is famous for its temples, beauty and its majestic hills covered with pine and deodar forest and sprawling apple orchards.

Geographic entities mentioned:
surface_form: hills
instance_of: Mountain
countries: India
coordinates: lat: 23.166666666667
lon: 92.833333333333
Kullu Valley. Kullu Valley is a broad open valley in Himachal Pradesh, India, formed by the Beas River between Manali and Larji. This valley is famous for its temples, beauty and its majestic hills covered with pine and deodar forest and sprawling apple orchards.

Geographic entities mentioned:
surface_form: kullu valley
instance_of: Valley
countries: India
coordinates: lat: 31.957777777778
lon: 77.109444444444
The course of the Beas river presents a succession of magnificent, clad with forests of deodar, towering above trees of pine on the lower rocky ridges. Kullu valley is sandwiched between the Pir Panjal, Lower Himalayan and Great Himalayan Ranges. Ski touring is a sport growing in popularity in the Himilayan peaks surrounding the valley. Economy.

Geographic entities mentioned:
surface_form: kullu valley
instance_of: Valley
countries: India
coordinates: lat: 31.957777777778
lon: 77.109444444444
Ski touring is a sport growing in popularity in the Himilayan peaks surrounding the valley. Economy. &quot;See Economy section in Kullu district.&quot;
Tourism. &quot;For places of interest, festivals, and outdoor sports in the Kullu valley, see Attractions section in Kullu district.&quot;
Further reading. &quot;See Further reading section in Kullu district.&quot;

Geographic entities mentioned:
surface_form: kullu valley
instance_of: Valley
countries: India
coordinates: lat: 31.957777777778
lon: 77.109444444444
Background. Mount Meager, located north of Vancouver, is a peak of the Mount Meager massif. This is a group of coalescent stratovolcanoes and the largest volcanic centre in the Garibaldi Volcanic Belt. It comprises about of eruptive rocks that were deposited during four distinct eruptive periods, the first beginning 2.2 million years ago.

Geographic entities mentioned:
surface_form: Garibaldi Volcanic Belt
instance_of: Mountain
countries: Canada
coordinates: lat: 51.5283
lon: -126.113
Between July 1840 and June 1842 Fallmerayer embarked on his second major journey, setting out from Regensburg and travelling along the Danube and across the Black Sea to Trapezunt. After long stays in Trapezunt, Constantinople, Athos&ndash;Chalkidiki and the rest of Macedonia, and Athens, he returned to Munich via Trieste and Venice.

Geographic entities mentioned:
surface_form: Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
A new bishop was ordained while Paul was still alive. He was banished to Paleostrovsky monastery, on an island in Lake Onega, moving to Khutyn Monastery in 1656. The cause of his death is unknown but he is believed to have been murdered on April 16, 1656. He is regarded as a martyr by the Old Believers.

Geographic entities mentioned:
surface_form: Lake Onega
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 61.690555555556
lon: 35.655555555556
Øyrlandet. Øyrlandet is a coastal plain and peninsula in Sørkapp Land at Spitsbergen, Svalbard. The plain extends from Kistefjellet and St. Nikolausfjellet to the east, Belopol'skijbreen to the northeast, and Olsokbreen, Olsokneset and Stormbukta to the north. At the southeastern side of Øyrlandet is the bay of Sommerfeldtbukta, and the southernmost tip is the headland Øyrlandsodden.

Geographic entities mentioned:
surface_form: Kistefjellet
instance_of: Mountain
countries: Norway
coordinates: lat: 76.6054
lon: 16.6597
surface_form: St. Nikolausfjellet
instance_of: Mountain
countries: Norway
coordinates: lat: 76.6367
lon: 16.6729
The source of the river is in the Town of Port Wing within the Moquah Barrens Research Natural Area. The river then flows through the Town of Orienta and back into the Town of Port Wing. From there, it goes past the census-designated place of Port Wing and empties into Lake Superior. The Flag River State Wildlife Area is directly east of the river.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
The species was described in 2021 by the Indonesian ornithologist Mohammed Irham and his colleagues based on genetic, morphological, and vocal differences from other &quot;Zosterops&quot; white-eyes. It is endemic to the Meratus Mountains of Indonesian Borneo, where it has been observed on Mount Besar and Mount Karokangen.

Geographic entities mentioned:
surface_form: Meratus Mountains
instance_of: Mountain
countries: Indonesia
coordinates: lat: -2.75
lon: 115.66666666667
According to tradition, she rejected many suitors when younger, and in each town she conquered would behead a man after spending the night with them. Expansion north was blocked by Kano and Katsina, and east by the Jos Plateau; therefore Amina campaigned to the southeast and southwest. She conquered large tracts of land as far as Kwararafa and Nupe, including Bauchi and Yauri.

Geographic entities mentioned:
surface_form: Jos Plateau
instance_of: Plateau
countries: Nigeria
coordinates: lat: 9.5667
lon: 9.0833
She conquered large tracts of land as far as Kwararafa and Nupe, including Bauchi and Yauri. Sokoto caliph Muhammad Bello claimed she reached what presumably was the confluence of the Niger and Benue rivers, and extracted tribute from Katsina and Kano, however contemporary historians dispute the latter claim.

Geographic entities mentioned:
surface_form: Benue
instance_of: Watercourse
countries: Cameroon
Nigeria
coordinates: lat: 7.783333
lon: 6.766667
The old Nord-Innherad prosti was headquartered at Steinkjer Church in the town of Steinkjer in Steinkjer Municipality. Stjørdal prosti== . This deanery () covers the traditional district of Stjørdalen in eastern Trøndelag county. The deanery includes the parishes in the municipalities of Stjørdal, Meråker, Malvik, Selbu, and Tydal.

Geographic entities mentioned:
surface_form: Stjørdalen
instance_of: Valley
countries: Norway
coordinates: lat: 63.4372
lon: 11.3444
In 1883–1884, she traveled for 13 months, spending a summer in Ireland, Wales, Scotland and England, also visiting Austria, Hungary, Southern Italy, Spain, and Morocco. In previous years, she had traveled to the Pacific Coast and Yosemite Valley. Woolson died in 1921.

Geographic entities mentioned:
surface_form: Yosemite Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
Disease. A survey conducted across 20172018 made the first detection of &quot;Xylella fastidiosa&quot; in the country. This was found on almond in the Hula Valley, which is in the northeast. Polymerase chain reaction (PCR) identified it as the &quot;Xylella fastidiosa&quot; subsp. &quot;fastidiosa&quot; (&quot;Xff&quot;) subspecies. Agritourism.

Geographic entities mentioned:
surface_form: Hula Valley
instance_of: Valley
countries: Israel
coordinates: lat: 33.103333333333
lon: 35.609166666667
Lecarrow Canal. The Lecarrow Canal () is a navigable canal in County Roscommon, Ireland, connecting the village of Lecarrow to Lough Ree. Constructed in the 1840s to carry limestone from a quarry to Athlone for construction projects by the Shannon Commissioners, it first fell into disuse after 17 years but was cleaned up in 1889 and was dredged in the 1960s by the Office of Public Works.

Geographic entities mentioned:
surface_form: Lough Ree
instance_of: Lake
countries: Ireland
coordinates: lat: 53.5
lon: -7.9666666666667
Coleophora gryphipennella. &quot;Coleophora gryphipennella&quot; is a moth of the family Coleophoridae. It is found in most of Europe, from Fennoscandia to the Iberian Peninsula and Italy and from Ireland to the Black Sea. The wingspan is. Head whitish-ochreous or greyish-ochreous. Antennae white, ringed with dark fuscous, basal joint whitish-ochreous.

Geographic entities mentioned:
surface_form: Fennoscandia
instance_of: Landform
countries: Norway
Sweden
Finland
Russia
Russian Empire
Soviet Union
coordinates: lat: 63
lon: 17
The city occupies an area of 127 square miles (330 km2), of which, is water. The Río Grande de Arecibo is the main river in the municipality, running through the middle of it. South of the municipality, in the karst region, it forms the Dos Bocas Lake, a primary source of water for northern Puerto Rico. Several rivers feed the Río Grande, including the Tanamá River.

Geographic entities mentioned:
surface_form: Dos Bocas Lake
instance_of: Lake
countries: United States
coordinates: lat: 18.335555555556
lon: -66.6675
Holden (Lierne). Holden is a lake in Lierne Municipality in Trøndelag county, Norway. The lake lies north of the lakes Lenglingen and Gusvatnet. The municipal center, Sandvika, is located about to the north of the lake.

Geographic entities mentioned:
surface_form: Lenglingen
instance_of: Lake
countries: Norway
coordinates: lat: 64.25
lon: 13.716666666667
surface_form: Gusvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 64.2825
lon: 13.4889
Holden (Lierne). Holden is a lake in Lierne Municipality in Trøndelag county, Norway. The lake lies north of the lakes Lenglingen and Gusvatnet. The municipal center, Sandvika, is located about to the north of the lake.

Geographic entities mentioned:
surface_form: holden
instance_of: Lake
countries: Norway
coordinates: lat: 64.0739
lon: 10.9445
surface_form: holden (lierne)
instance_of: Lake
countries: Norway
coordinates: lat: 64.3372
lon: 13.5385
Holden (Lierne). Holden is a lake in Lierne Municipality in Trøndelag county, Norway. The lake lies north of the lakes Lenglingen and Gusvatnet. The municipal center, Sandvika, is located about to the north of the lake.

Geographic entities mentioned:
surface_form: holden
instance_of: Lake
countries: Norway
coordinates: lat: 64.0739
lon: 10.9445
surface_form: holden
instance_of: Lake
countries: Norway
coordinates: lat: 64.3372
lon: 13.5385
Lake Winnipesaukee Sailing Association. d7cl0gd6mn4s1ip603q4at9qptkq3" xml:space="preserve">Lake Winnipesaukee Sailing Association (LWSA) is a non-profit educational institution focused on sailing education that was founded in 1988 in Gilford, New Hampshire on Lake Winnipesaukee in the Lakes Region. Since 1988, LWSA has educated over 2,500 young sailors. History.

Geographic entities mentioned:
surface_form: Lake Winnipesaukee
instance_of: Lake
countries: United States
coordinates: lat: 43.598888888889
lon: -71.323055555556
Research and career. Mackay was appointed a lecturer at University College London in 2000 and promoted to Professor in 2013. They have extensively investigated the impact of pollution on Lake Baikal, as well as the Aral Sea and Okavango Delta. They have reconstructed the climate history of Lake Baikal for the past 800,000 years.

Geographic entities mentioned:
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
surface_form: Aral Sea
instance_of: Lake
countries: Kazakhstan
Uzbekistan
Russian Empire
Soviet Union
coordinates: lat: 45
lon: 60
surface_form: Okavango Delta
instance_of: Body of water
Watercourse
countries: Botswana
coordinates: lat: -19.4
lon: 22.9
They have extensively investigated the impact of pollution on Lake Baikal, as well as the Aral Sea and Okavango Delta. They have reconstructed the climate history of Lake Baikal for the past 800,000 years. Lake Baikal is the world's deepest and oldest lake, and is home to one fifth of the world's fresh water. Over 75% of the species exist nowhere else in the world.

Geographic entities mentioned:
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
Over 75% of the species exist nowhere else in the world. Mackay has studied the numbers of the microalgae diatoms in Lake Baikal, and showed that they have declined as the lake gets warmer. Some diatoms are more sensitive than others, which lets Mackay and colleagues look at the impact of pollution in the past.

Geographic entities mentioned:
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
They have two sons, István (b. 1950) and András (b. 1953). After teaching she became a pensioner, and started her painting as an individual artist. She worked all around her village and neighborhood, after in Hungary, at Lake Balaton for example, and also in some beautiful places of Europe, from Italy to Norway, and from Germany to Croatia. She had numerous expositions in her Country.

Geographic entities mentioned:
surface_form: Lake Balaton
instance_of: Lake
countries: Hungary
coordinates: lat: 46.85
lon: 17.72
In 1801 the Reverend Luke Yarker employed several people as musicians and singers in the church. The musicians were supplanted in 1865 by a harmonium, which was replaced in 1894 by an organ that had previously been in Constable Burton Hall. The church is next to Leeming Beck (named Bedale Beck further down the valley) and was formerly in an Anglo-Saxon village.

Geographic entities mentioned:
surface_form: Bedale Beck
instance_of: Watercourse
countries: United Kingdom
Boryeonsan. Boryeonsan () is a mountain in Chungju, South Korea. It has an elevation of.

Geographic entities mentioned:
surface_form: boryeonsan
instance_of: Mountain
countries: South Korea
coordinates: lat: 37.0667
lon: 127.783
History. The tower was built in 1966 as part of the now-demolished Divis Flats complex, which comprised twelve eight-storey blocks of terraces and flats, named after the nearby Divis Mountain. The tower, a vertical complex of 96 flats housing approximately 110 residents, was designed by architect Frank Robertson for the Northern Ireland Housing Trust.

Geographic entities mentioned:
surface_form: Divis Mountain
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.6075
lon: -6.0094444444444
The river drains a watershed of and is formed by the confluence of the Fontas River flowing from the east, and the Sikanni Chief River flowing from the south. These, along with the Sahtaneh and Muskwa Rivers, constitute the major tributaries. The source of the Sikanni Chief, on the eastern slope of the Rocky Mountains, is ultimately the headwater of the Fort Nelson River.

Geographic entities mentioned:
surface_form: Sahtaneh
instance_of: Watercourse
countries: Canada
coordinates: lat: 59.03306
lon: -122.45297
It turns north again near Fort Nelson, where the Muskwa River flows into it. Further north it receives the McConachie Creek, Cridland Creek and Sahtaneh River, which also carries waters from the Snake River. It then turns north-west and west, where it receives the Shush Creek, Onion Creek, Tsimeh Creek, Stanolind Creek and Kiwigana River.

Geographic entities mentioned:
surface_form: Sahtaneh River
instance_of: Watercourse
countries: Canada
coordinates: lat: 59.03306
lon: -122.45297
It is located in the La Paz Department, Ingavi Province, on the border of the municipalities of Guaqui and Jesús de Machaca. Achachi Qala lies south of Wiñaymarka Lake, the southern branch of Lake Titicaca, northwest of Wanq'uni and southwest of Quta Willk'i.

Geographic entities mentioned:
surface_form: Wiñaymarka
instance_of: Lake
countries: Bolivia
Peru
coordinates: lat: -16.333333333333332
lon: -68.83333333333333
surface_form: Titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
surface_form: Quta Willk'i
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.6411
lon: -68.8058
surface_form: wanq'uni
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.6547
lon: -68.7931
surface_form: quta willk'i
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.6411
lon: -68.8058
surface_form: willk'i
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.39861111
lon: -69.02222222
surface_form: wanq'uni
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.78277778
lon: -65.67194444
Achachi Qala (Ingavi). Achachi Qala (Aymara for &quot;gigantic stone&quot;, also spelled &quot;Achachicala&quot;) is a mountain in the Chilla-Kimsa Chata mountain range in the Andes of Bolivia which reaches a height of approximately. It is located in the La Paz Department, Ingavi Province, on the border of the municipalities of Guaqui and Jesús de Machaca.

Geographic entities mentioned:
surface_form: achachi qala
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.5233
lon: -67.9878
surface_form: achachi qala
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.13055556
lon: -67.70972222
surface_form: achachi qala
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.6525
lon: -68.80694444
surface_form: achachi qala
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.82833333
lon: -67.69222222
surface_form: achachi qala
instance_of: Mountain
countries: Bolivia
coordinates: lat: -15.66138889
lon: -68.57888889
Achachi Qala (Ingavi). Achachi Qala (Aymara for &quot;gigantic stone&quot;, also spelled &quot;Achachicala&quot;) is a mountain in the Chilla-Kimsa Chata mountain range in the Andes of Bolivia which reaches a height of approximately. It is located in the La Paz Department, Ingavi Province, on the border of the municipalities of Guaqui and Jesús de Machaca.

Geographic entities mentioned:
surface_form: achachi qala
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.5233
lon: -67.9878
surface_form: kimsa chata
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.1058
lon: -68.3858
surface_form: achachicala
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.13055556
lon: -67.70972222
surface_form: achachi qala
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.13055556
lon: -67.70972222
surface_form: kimsa chata
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.1214
lon: -68.3297
surface_form: kimsa chata
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.71666667
lon: -68.7
surface_form: achachicala
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.6525
lon: -68.80694444
surface_form: achachi qala
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.6525
lon: -68.80694444
surface_form: achachi qala
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.82833333
lon: -67.69222222
surface_form: kimsa chata
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.10972222
lon: -67.66222222
surface_form: achachicala
instance_of: Mountain
countries: Bolivia
coordinates: lat: -15.66138889
lon: -68.57888889
surface_form: achachi qala
instance_of: Mountain
countries: Bolivia
coordinates: lat: -15.66138889
lon: -68.57888889
surface_form: kimsa chata
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.88333333
lon: -68.85
The municipality covers an area of 11 km2. It is part of the Centro District in the Valles Centrales region. As of 2005, the municipality had a total population of 15,071.

Geographic entities mentioned:
surface_form: Valles Centrales region
instance_of: Valley
countries: Mexico
coordinates: lat: 17.0833
lon: -96.75
In the production of Townshend's masque, a young Thomas Killigrew, then a page to the King, appeared in the role of &quot;a Fugitive Favourite.&quot; In Townshend's version as in the French work, Circe is enraged at the escape of one of her captive lovers, who has run to the Vale of Tempe.

Geographic entities mentioned:
surface_form: Vale of Tempe
instance_of: Valley
countries: Greece
coordinates: lat: 39.872778
lon: 22.546667
Pakistan International Airlines Flight 661. Pakistan International Airlines Flight 661 was a Pakistani domestic passenger flight from Chitral to Islamabad, operated by Pakistan's flag carrier Pakistan International Airlines. On 7 December 2016, the aircraft serving the route, an ATR 42-500 twin-turboprop, crashed near Havelian following an engine failure.

Geographic entities mentioned:
surface_form: Chitral
instance_of: Valley
countries: Pakistan
coordinates: lat: 35.85111111111111
lon: 71.78888888888889
He fought off an attack by Shamil, a leader of anti-Russian insurgency in the North Caucasus, and scored a series of victories over the rebels in Tchar-Belakan in 1853, winning the rank of lieutenant general. In 1855, he was made commander of the pre-Caspian troops and promoted to adjutant general in 1857.

Geographic entities mentioned:
surface_form: Caspian
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
In 2005, he was the Swedish champion and won first prize in the Finnish National Championship. He was twelfth in the final rankings for Snowboard Cross at the 2006 Winter Olympics in Turin, Italy. He died in a snowboarding accident at Whiteface Mountain in Lake Placid, New York, five days after his 26th birthday. It was the last run he had planned for the day.

Geographic entities mentioned:
surface_form: Whiteface Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.3658
lon: -73.9028
Geography. Geologically Lake Komsomolskoye is part of the Lake Ladoga depression, a graben and syncline structure of Proterozoic age (Precambrian). Deglaciation following the Weichsel glaciation took place in the Lake Ladoga basin between 12,500 and 11,500 radiocarbon years BP.

Geographic entities mentioned:
surface_form: Lake Ladoga
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.842777777777776
lon: 31.459722222222222
surface_form: ladoga
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.842777777777776
lon: 31.459722222222222
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
surface_form: lake komsomolskoye
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.8
lon: 30.05
Geography. Geologically Lake Komsomolskoye is part of the Lake Ladoga depression, a graben and syncline structure of Proterozoic age (Precambrian). Deglaciation following the Weichsel glaciation took place in the Lake Ladoga basin between 12,500 and 11,500 radiocarbon years BP.

Geographic entities mentioned:
surface_form: ladoga
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.842777777777776
lon: 31.459722222222222
surface_form: lake ladoga
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.842777777777776
lon: 31.459722222222222
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
Lake Komsomolskoye. Lake Komsomolskoye is a lake in the north of the Leningrad Region Priozersky District, in the middle of the Karelian Isthmus of north western Russia. Until 1948 it was called Kiimajärvi (Finnish Kiimajärvi). Description. Lake Komsomolskoye is long, miles wide, with a surface area of. The main inflow of Lake Komsomolskoye is from the Pionerka River.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: lake komsomolskoye
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.8
lon: 30.05
Lake Komsomolskoye. Lake Komsomolskoye is a lake in the north of the Leningrad Region Priozersky District, in the middle of the Karelian Isthmus of north western Russia. Until 1948 it was called Kiimajärvi (Finnish Kiimajärvi). Description. Lake Komsomolskoye is long, miles wide, with a surface area of. The main inflow of Lake Komsomolskoye is from the Pionerka River.

Geographic entities mentioned:
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
surface_form: lake komsomolskoye
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.8
lon: 30.05
Until 1948 it was called Kiimajärvi (Finnish Kiimajärvi). Description. Lake Komsomolskoye is long, miles wide, with a surface area of. The main inflow of Lake Komsomolskoye is from the Pionerka River. In the south, a small stream flows into Lake Komsomolskoye. At the northern end, Lake Komsomolskoye is drained by the Vesyolaya River which flows into the Vuoksi River near the village of Vasilyevo.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: lake komsomolskoye
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.8
lon: 30.05
Description. Lake Komsomolskoye is long, miles wide, with a surface area of. The main inflow of Lake Komsomolskoye is from the Pionerka River. In the south, a small stream flows into Lake Komsomolskoye. At the northern end, Lake Komsomolskoye is drained by the Vesyolaya River which flows into the Vuoksi River near the village of Vasilyevo. The lake is divided into three plains by two narrowings.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: lake komsomolskoye
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.8
lon: 30.05
The main inflow of Lake Komsomolskoye is from the Pionerka River. In the south, a small stream flows into Lake Komsomolskoye. At the northern end, Lake Komsomolskoye is drained by the Vesyolaya River which flows into the Vuoksi River near the village of Vasilyevo. The lake is divided into three plains by two narrowings. The North Pole occupies part of the basin with depths of 6 to 10 meters.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: lake komsomolskoye
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.8
lon: 30.05
In the south, a small stream flows into Lake Komsomolskoye. At the northern end, Lake Komsomolskoye is drained by the Vesyolaya River which flows into the Vuoksi River near the village of Vasilyevo. The lake is divided into three plains by two narrowings. The North Pole occupies part of the basin with depths of 6 to 10 meters. There is a small group of islands.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
The North Pole occupies part of the basin with depths of 6 to 10 meters. There is a small group of islands. Central reach is the deepest, with depressions up to 19.6 meters, the southern shallow, with gentle underwater slopes. The coastal shallows of the lake are covered with a mixture of sand and silt, the bottom in deep sections is covered with a thick layer of light brown mud.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
The coastal shallows of the lake are covered with a mixture of sand and silt, the bottom in deep sections is covered with a thick layer of light brown mud. With the exception of the bays, the lake is overgrown with little: the width of the green border near the coast is 10–20 meters. Geography.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
Deglaciation following the Weichsel glaciation took place in the Lake Ladoga basin between 12,500 and 11,500 radiocarbon years BP. During the existence of Lake Komsomolskoye there have been three sharp drops in the water level, so that the shore consists of small but distinctive terraces formed on the banks.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: lake komsomolskoye
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.8
lon: 30.05
During the existence of Lake Komsomolskoye there have been three sharp drops in the water level, so that the shore consists of small but distinctive terraces formed on the banks. The shores of the lake are indented with several bays and inlets, overgrown with sedges and reeds. On the south-eastern shore of the lake is the village of Solovyovka.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
The shores of the lake are indented with several bays and inlets, overgrown with sedges and reeds. On the south-eastern shore of the lake is the village of Solovyovka. At the northern extremity of the lake are the houses of the village of Torfyanoye. Notoriety. Part of the shore is fenced by the dacha cooperative Ozero, among the founders of which was Vladimir Putin.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
Lake Komsomolskoye. Lake Komsomolskoye is a lake in the north of the Leningrad Region Priozersky District, in the middle of the Karelian Isthmus of north western Russia. Until 1948 it was called Kiimajärvi (Finnish Kiimajärvi). Description. Lake Komsomolskoye is long, miles wide, with a surface area of. The main inflow of Lake Komsomolskoye is from the Pionerka River.

Geographic entities mentioned:
surface_form: kiimajärvi
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.8
lon: 30.05
surface_form: kiimajärvi
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.8
lon: 30.05
As of the 2020 census, the population was 11,539. The county seat is Del Norte. The county is named for the Rio Grande (Spanish language for &quot;Big River&quot;), which flows through the county. Description. The gateway to the San Juan Mountains, Rio Grande County is one of the highlights of the San Luis Valley. The county covers ranging from approximately on valley floor to several peaks.

Geographic entities mentioned:
surface_form: San Luis Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.2
lon: -105.42
Gaylor Peak. Gaylor Peak is an 11,004-foot (3,354-meter) mountain summit located on the crest of the Sierra Nevada mountain range in northern California, United States. The peak is positioned on the boundary between Yosemite National Park and the Inyo National Forest, and it also lies on the border between Mono County and Tuolumne County.

Geographic entities mentioned:
surface_form: yosemite
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
The mountain is listed on the Vagmarken Club's Sierra Crest List, recognizing notable summits in the region. The easiest route to the summit is a Class 2 hike on the Yosemite Decimal System scale, which indicates that the climb involves simple scrambling without the need for specialized climbing equipment. History.

Geographic entities mentioned:
surface_form: yosemite
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
History. The toponym of this mountain was officially adopted by the United States Board on Geographic Names to honor Andrew Jack Gaylor, one of the first rangers in Yosemite National Park. Gaylor died from a heart attack on April 19, 1921, while on patrol in the park, after serving 14 years with the National Park Service.

Geographic entities mentioned:
surface_form: yosemite
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
Gaylor Peak. Gaylor Peak is an 11,004-foot (3,354-meter) mountain summit located on the crest of the Sierra Nevada mountain range in northern California, United States. The peak is positioned on the boundary between Yosemite National Park and the Inyo National Forest, and it also lies on the border between Mono County and Tuolumne County.

Geographic entities mentioned:
surface_form: gaylor peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.91881
lon: -119.26571
The peak rises prominently above Tioga Pass and Tioga Lake, with a notable topographic relief, as the summit stands approximately above the lake within a distance of. Gaylor Peak is a popular hiking destination, particularly during the summer months, due to its accessibility.

Geographic entities mentioned:
surface_form: gaylor peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.91881
lon: -119.26571
Gaylor died from a heart attack on April 19, 1921, while on patrol in the park, after serving 14 years with the National Park Service. Prior to the official naming, early prospectors referred to the peak as &quot;Tioga Hill.&quot; The Great Sierra Mine Historic Site is located approximately one-half mile north of Gaylor Peak. Climate. Gaylor Peak is located in an alpine climate zone.

Geographic entities mentioned:
surface_form: gaylor peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.91881
lon: -119.26571
As these fronts approach, they are forced upward by the peaks through a process known as orographic lift, which causes the moisture to condense and fall as precipitation, either as rain or snow, depending on the season. Precipitation runoff from Gaylor Peak flows westward into Gaylor Lakes and then into the Dana Fork of the Tuolumne River.

Geographic entities mentioned:
surface_form: gaylor peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.91881
lon: -119.26571
Moostoos. Moostoos (meaning &quot;The Buffalo&quot;, also spelled Mostos; – November 19, 1918), also known as Louis Willier, was headman of the Sucker Creek First Nation. Personal life. Moostoos was born at the western end of Lesser Slave Lake, as the eldest of ten children of Masinigoneb and Marie Kowikkiu. He was a trapper, fisherman, and later, Chief and Headman of Sucker Creek First Nation.

Geographic entities mentioned:
surface_form: Lesser Slave Lake
instance_of: Lake
countries: Canada
coordinates: lat: 55.440556
lon: -115.488611
Moostos died on November 19, 1918, at the Sucker Creek Indian Reserve during that year's influenza pandemic. Participation in Treaty 8 Negotiations. During Treaty 8 negotiations, Moostoos and his younger brother Kinosew (Kinoosayo) spoke on behalf of the Cree at talks from June 20–22, 1899, at Willow Point, on Lesser Slave Lake. Moostoos' negotiation style is described as conciliatory.

Geographic entities mentioned:
surface_form: Lesser Slave Lake
instance_of: Lake
countries: Canada
coordinates: lat: 55.440556
lon: -115.488611
In 1900, along with other Cree Headmen, Moostoos requested land for a reserve east of the Driftpile River on Lesser Slave Lake. In 1910, reserve land was granted, but was not contiguous between Cree communities involved in the negotiations. Separate reserves were established for Driftpile first nation and Sucker Creek first nation.

Geographic entities mentioned:
surface_form: Lesser Slave Lake
instance_of: Lake
countries: Canada
coordinates: lat: 55.440556
lon: -115.488611
Canal Mauri. Canal Mauri is a canal in Peru and Chile. It transfers water from the Mauri River watershed and transfers it into the Caplina River for irrigation purposes. An earlier canal Canal Uchusuma was constructed in the early 19th century and was replaced by the Canal Mauri.

Geographic entities mentioned:
surface_form: Mauri River
instance_of: Watercourse
countries: Bolivia
Peru
coordinates: lat: -17.140278
lon: -70.015278
surface_form: Caplina River
instance_of: Watercourse
countries: Peru
coordinates: lat: -18.300327
lon: -70.443451
An earlier canal Canal Uchusuma was constructed in the early 19th century and was replaced by the Canal Mauri. This canal collects water from several tributaries of the Mauri River (notably the Uchusuma River) and diverts it through Chilean territory into the Quebrada Vilavilani, a tributary of the Caplina River; from there it is later diverted for irrigation purposes in the Tacna region.

Geographic entities mentioned:
surface_form: Uchusuma River
instance_of: Watercourse
countries: Chile
Peru
Bolivia
coordinates: lat: -17.52379
lon: -69.24806
This has also resulted in damage to the wetlands that are located along the Uchusuma, as well as complaints by the Bolivian government. Path. Canal Mauri is a transbasin diversion that transports water from the Lake Titicaca watershed to the Pacific slope. The construction of the canals was facilitated by the gentle terrain of the Mauri River valley.

Geographic entities mentioned:
surface_form: Lake Titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
Another diversion on the Quebrada Queñuta collects its water separately in the Canal Queñuta and diverts it to the Uchusuma River. The canal proper starts at a diversion dam on the Uchusuma River and runs for (of it through Chilean territory) in a rectangular canal. The Patapujo I canal joins it soon afterwards, and there are two gauging stations there.

Geographic entities mentioned:
surface_form: Uchusuma River
instance_of: Watercourse
countries: Chile
Peru
Bolivia
coordinates: lat: -17.52379
lon: -69.24806
The Patapujo I canal joins it soon afterwards, and there are two gauging stations there. The path of the canal takes it through Chilean territory from Laguna Blanca along the Arica–La Paz railway southwestward between the mountains Tacora and Caracarani, close to the Canal Uchusuma.

Geographic entities mentioned:
surface_form: Tacora
instance_of: Mountain
countries: Chile
coordinates: lat: -17.716666666667
lon: -69.766666666667
The Canal Mauri has a capacity of. The Quebrada Vilavilani descends the Andes in southwestward direction, where it has several different names, and ends close to the city of Tacna into the Caplina River. There is a diversion on the Quebrada Vilavilani before it reaches the Caplina at Chuschuco, which gives rise to another canal also known as &quot;Canal Uchusuma&quot;.

Geographic entities mentioned:
surface_form: Caplina River
instance_of: Watercourse
countries: Peru
coordinates: lat: -18.300327
lon: -70.443451
History. Already during Spanish colonial time plans were developed to use the waters of the Uchusuma for irrigation. After Chile had occupied what is now its northern territory and Peru's Tacna Department during the War of the Pacific, it examined the possibility of transferring water from the Mauri River into Tacna to enable irrigated agriculture.

Geographic entities mentioned:
surface_form: Mauri River
instance_of: Watercourse
countries: Bolivia
Peru
coordinates: lat: -17.140278
lon: -70.015278
The plan projected that about of land could be irrigated at a capital cost of; the revenue from the irrigated land would be sufficient to offset the investment. The Canal Uchusuma already existed since 1820; it intercepted water from the Uchusuma River.

Geographic entities mentioned:
surface_form: Uchusuma River
instance_of: Watercourse
countries: Chile
Peru
Bolivia
coordinates: lat: -17.52379
lon: -69.24806
He spent more than twenty-five years researching in Tianjin. His expeditions spread across various parts of Northern and Central China (including the provinces of Shandong, Hebei, Shanxi, Henan, Shaanxi, Gansu, Inner Mongolia and eastern part of the Tibetan Plateau).

Geographic entities mentioned:
surface_form: Tibetan Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
Taxonomy. &quot;Cupaniopsis newmanii&quot; was first formally described in 1984 by Sally T. Reynolds in the journal &quot;Austrobaileya&quot; from specimens collected in the Numinbah Valley in 1978. The specific epithet (&quot;newmanii&quot;) honours John Newman (1931–1980), a cousin of Reynolds. Distribution and habitat.

Geographic entities mentioned:
surface_form: Numinbah Valley
instance_of: Valley
countries: Australia
coordinates: lat: -28.141127777778
lon: 153.22403055556
Lawrence River. Toponymy. In French Canadian toponymy, already in the 19th century, the term Hell was used to designate these entities as well as a mountain pierced by a deep crevasse, located southeast of Grand lac des Enfers. The stream has the same name as its head lake; these toponyms appear in the 1914 Dictionary of Rivers and Lakes of the Province of Quebec.

Geographic entities mentioned:
surface_form: grand lac
instance_of: Lake
countries: Canada
coordinates: lat: 48.866666666667
lon: -57.433333333333
surface_form: grand lac
instance_of: Lake
countries: Canada
coordinates: lat: 45.933611111111
lon: -66.032777777778
surface_form: grand lac des enfers
instance_of: Lake
countries: Canada
coordinates: lat: 47.71722111111111
lon: -71.00888805555556
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Lawrence River. Toponymy. In French Canadian toponymy, already in the 19th century, the term Hell was used to designate these entities as well as a mountain pierced by a deep crevasse, located southeast of Grand lac des Enfers. The stream has the same name as its head lake; these toponyms appear in the 1914 Dictionary of Rivers and Lakes of the Province of Quebec.

Geographic entities mentioned:
surface_form: head lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.0486
lon: -78.5161
surface_form: head lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.74027777777778
lon: -78.91277777777778
Rivière de l'Enfer. The Rivière de l'Enfer ('Hell's River') is a tributary of the eastern bank of the Malbaie River, flowing in the unorganized territory of Lac-Pikauba, in the regional county municipality (MRC) of Charlevoix Regional County Municipality, in the administrative region of Capitale-Nationale, in the province of Quebec, in Canada.

Geographic entities mentioned:
surface_form: rivière de l'enfer
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.67527694444444
lon: -70.845555
The stream has the same name as its head lake; these toponyms appear in the 1914 Dictionary of Rivers and Lakes of the Province of Quebec. The toponymic designation &quot;Rivière de l'Enfer&quot; was first approved on April 3, 1959, by the Commission de géographie du Québec.

Geographic entities mentioned:
surface_form: rivière de l'enfer
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.67527694444444
lon: -70.845555
The toponymic designation &quot;Rivière de l'Enfer&quot; was first approved on April 3, 1959, by the Commission de géographie du Québec. The toponym &quot;Rivière de l'Enfer&quot; was formalized on December 5, 1968, at the Place Names Bank of the Commission de toponymie du Québec.

Geographic entities mentioned:
surface_form: rivière de l'enfer
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.67527694444444
lon: -70.845555
Cima de Nomnom. Cima de Nomnom is a mountain of the Lepontine Alps, overlooking Cauco in the Swiss canton of Graubünden. It lies on the range between the Val Calanca and the Val Mesolcina, north of Piz de Groven.

Geographic entities mentioned:
surface_form: Val Calanca
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.335833333333
lon: 9.1188888888889
surface_form: Piz de Groven
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.318277777778
lon: 9.1591666666667
surface_form: val mesolcina
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.385
lon: 9.235
surface_form: mesolcina
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.385
lon: 9.235
surface_form: val calanca
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.385
lon: 9.235
surface_form: calanca
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.335833333333
lon: 9.1188888888889
Cima de Nomnom. Cima de Nomnom is a mountain of the Lepontine Alps, overlooking Cauco in the Swiss canton of Graubünden. It lies on the range between the Val Calanca and the Val Mesolcina, north of Piz de Groven.

Geographic entities mentioned:
surface_form: cima de nomnom
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.34027778
lon: 9.15777778
Lake Kayumbu. Lake Kayumbu, also known as Lake Kayumba, is a lake in Kisoro District, South Western Uganda, north of the Rwanda border at an altitude of above sea level. The lake acts as a tourist destination which earns the country foreign exchange. The lake has a variety of fish species.

Geographic entities mentioned:
surface_form: lake kayumbu
instance_of: Lake
countries: Uganda
coordinates: lat: -1.3379
lon: 29.7875
Lake Kayumbu. Lake Kayumbu, also known as Lake Kayumba, is a lake in Kisoro District, South Western Uganda, north of the Rwanda border at an altitude of above sea level. The lake acts as a tourist destination which earns the country foreign exchange. The lake has a variety of fish species.

Geographic entities mentioned:
surface_form: lake kayumbu
instance_of: Lake
countries: Uganda
coordinates: lat: -1.3379
lon: 29.7875
surface_form: lake kayumba
instance_of: Lake
countries: Uganda
coordinates: lat: -1.3379
lon: 29.7875
Rouge River (Montmorency River tributary). This forest and mountain valley is served by a forest road passing on the east side of the river. Forestry is the main economic activity in this valley; second, recreational tourism.

Geographic entities mentioned:
surface_form: rouge river (montmorency river tributary)
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.099721
lon: -71.109722
Geography. The Rouge River flows into a bend on the east bank of the Montmorency River. From this confluence of the Rouge River, the current flows over generally south by the course of the Montmorency River, to the northwest shore of the St. Lawrence River. Toponymy. The toponym &quot;Rivière Rouge&quot; was formalized on December 13, 1996 at the Commission de toponymie du Québec.

Geographic entities mentioned:
surface_form: rivière rouge
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.099721
lon: -71.109722
Rouge River (Montmorency River tributary). This forest and mountain valley is served by a forest road passing on the east side of the river. Forestry is the main economic activity in this valley; second, recreational tourism.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Crooked Lake (Independence Township, Michigan). Crooked Lake is a 68-acre lake along the Clinton River. The lake, with a maximum depth of 65 feet, lies within Independence Township in Oakland County, Michigan. The lake is located west of Sashabaw Road and south of Shappie Road. Crooked Lake connects upstream to Upper Bushman Lake
Crooked Lake was formerly named Lower Bushman Lake. Fish.

Geographic entities mentioned:
surface_form: crooked lake
instance_of: Lake
countries: United States
coordinates: lat: 42.7875
lon: -76.15
surface_form: crooked lake
instance_of: Lake
countries: United States
coordinates: lat: 47.055833333333
lon: -123.10333333333
surface_form: crooked lake
instance_of: Lake
countries: United States
coordinates: lat: 42.496388888889
lon: -77.146111111111
surface_form: crooked lake
instance_of: Lake
countries: United States
coordinates: lat: 27.815555555556
lon: -81.566944444444
surface_form: michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
surface_form: crooked lake
instance_of: Lake
countries: United States
coordinates: lat: 42.776117
lon: -83.394695
surface_form: crooked lake
instance_of: Lake
countries: United States
coordinates: lat: 45.0184674
lon: -96.8536252
surface_form: crooked lake
instance_of: Lake
countries: United States
coordinates: lat: 45.411
lon: -84.828