Sarmila/GeoWiki-Features huggingface dataset:
She developed an affectionate, although sometimes strained, friendship with Robert F. Kennedy, perhaps because of his relatively thin skin. When Alice privately made fun of his scaling the newly named Mount Kennedy in Canada, he was not amused. She admitted to voting for President Lyndon Johnson over Senator Barry Goldwater in 1964 because she believed Goldwater was too mean.

Geographic entities mentioned:
surface_form: Mount Kennedy
instance_of: Mountain
countries: Canada
coordinates: lat: 60.341166666667
lon: -138.96633333333
It is the largest tributary on the left side of Yarlung Tsangpo. Its source is the Arza Gongla Glacier, at an elevation of 4900m. It first flows north into Ngagung Tso, then turn northwest to Rakwa Tso. It joins Yarlung Tsangpo near Bomê. The total length of Parlung Tsangpo is 266 km, and the drop of elevation is 3360m. The drainage basin covers an area of 23,800 square kilometers.

Geographic entities mentioned:
surface_form: Rakwa Tso
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 29.45
lon: 96.8
Assam. The Barak Valley comprising the present districts of Cachar, Karimganj and Hailakandi is contiguous to Sylhet (Bengal plains), where the Bengali Hindus, according to historian J.B. Bhattacharjee, had settled well before the colonial period, influencing the culture of Dimasa Kacaharis.

Geographic entities mentioned:
surface_form: Barak Valley
instance_of: Valley
countries: India
coordinates: lat: 24.833333333333332
lon: 92.8
Migrations to Cachar increased after the British annexation of the region. The Bengali Hindus settled in Brahmaputra Valley largely during the colonial period as professionals. After the Partition and especially after the genocide of 1950, Bengali Hindus of Sylhet immigrated to the Barak Valley. Later on during the 1971 Bangladesh genocide, thousands of Bengali Hindus took refuge in Assam.

Geographic entities mentioned:
surface_form: Brahmaputra Valley
instance_of: Valley
countries: India
coordinates: lat: 26.5983
lon: 92.4506
Tossal de Mirapallars i Urgell. Tossal de Mirapallars i Urgell is a mountain of Catalonia, Spain. It has an elevation of 1,672 metres above sea level.

Geographic entities mentioned:
surface_form: tossal de mirapallars
instance_of: Mountain
countries: Spain
coordinates: lat: 42.0210727556
lon: 0.959033353518
Chapman Snowfield. A large snowfield lying west of the central ridge in the Churchill Mountains. It is bounded to the north by Elder Peak and the massif surmounted by Mount Wharton, to the south by Soza Icefalls, Black Icefalls and the head of Starshot Glacier, and to the west by the Wallabies Nunataks and the All-Blacks Nunataks. Soza Icefalls.

Geographic entities mentioned:
surface_form: Elder Peak
instance_of: Mountain
coordinates: lat: -81.1167
lon: 157.333
surface_form: Mount Wharton
instance_of: Mountain
coordinates: lat: -81.04916667
lon: 157.79250333
surface_form: All-Blacks Nunataks
instance_of: Mountain
coordinates: lat: -81.4833
lon: 155.75
Soza Icefalls. A line of icefalls nearly high at the southern margin of Chapman Snowfield. The icefalls extend southwest for from Mount Massam, ending near the head of Starshot Glacier. They were named after Ezekiel R. Soza, a United States Geological Survey topographic engineer with the Topo North - Topo South survey expedition in these mountains, 1961–62. Black Icefalls.

Geographic entities mentioned:
surface_form: Mount Massam
instance_of: Mountain
coordinates: lat: -81.7333
lon: 158.2
Black Icefalls. A line of icefalls at the south margin of Chapman Snowfield. The icefalls extend southwest from Mount Massam to Vance Bluff, and were named in honor of A. W. Black, a member of the 1959 Cape Hallett winter-over team, working as a technician on the geomagnetic project. Ahern Glacier.

Geographic entities mentioned:
surface_form: Mount Massam
instance_of: Mountain
coordinates: lat: -81.7333
lon: 158.2
Named by US-ACAN for Cdr. Edward W. Donnally, USN, officer in charge of Naval support personnel at McMurdo Station, winter 1962. Flynn Glacier. A glacier about long, draining eastward from Mount Nares in the Churchill Mountains and entering Starshot Glacier south of Kelly Plateau. Named by US-ACAN for Cdr. William F.

Geographic entities mentioned:
surface_form: Mount Nares
instance_of: Mountain
coordinates: lat: -81.45
lon: 158.1666667
surface_form: Kelly Plateau
instance_of: Plateau
coordinates: lat: -81.4
lon: 159.5
Mansergh, geologist with the party. Sivjee Glacier. A glacier 10 nautical miles (18 km) long which drains the northeast slopes of Hunt Mountain. It flows north along the west side of Stark Ridge to enter Starshot Glacier south of Mount Hoskins. Named by Advisory Committee on Antarctic Names (US-ACAN) after Gulamabas G.

Geographic entities mentioned:
surface_form: Hunt Mountain
instance_of: Mountain
coordinates: lat: -82.08333333
lon: 159.26666667
Mansergh, geologist with the party. Sivjee Glacier. A glacier 10 nautical miles (18 km) long which drains the northeast slopes of Hunt Mountain. It flows north along the west side of Stark Ridge to enter Starshot Glacier south of Mount Hoskins. Named by Advisory Committee on Antarctic Names (US-ACAN) after Gulamabas G.

Geographic entities mentioned:
surface_form: Mount Hoskins
instance_of: Mountain
coordinates: lat: -81.8333
lon: 159.05
The music was written by Geddy Lee and Alex Lifeson, and the lyrics were written by Neil Peart. Background. The &quot;Lakeside Park&quot; mentioned in this song is on the shore of Port Dalhousie, a suburb of St. Catharines, Ontario, on the south shore of Lake Ontario in Canada. Peart lived very close to Lakeside Park, and spent summers as a youth working and playing there.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Cruach nam Mult. Cruach nam Mult is a mountain in the Arrochar Alps, Argyll, Scotland which lies to the southern side of Hell's Glen. The mountain is near Loch Fyne and GlenGoil and is part of the northern side of the area of the Arrochar Alps that follow south to Loch Goil.

Geographic entities mentioned:
surface_form: hell
instance_of: Landform
countries: United Kingdom
coordinates: lat: 19.37935
lon: -81.40678
surface_form: cruach nam mult
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.207777777778
lon: -4.9525
surface_form: hell's glen
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.217
lon: -4.946
Cruach nam Mult. Cruach nam Mult is a mountain in the Arrochar Alps, Argyll, Scotland which lies to the southern side of Hell's Glen. The mountain is near Loch Fyne and GlenGoil and is part of the northern side of the area of the Arrochar Alps that follow south to Loch Goil.

Geographic entities mentioned:
surface_form: cruach nam mult
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.207777777778
lon: -4.9525
Isola Peak. Isola Peak is a summit in Alberta, Canada. Isola Peak was so named on account of its isolated location.

Geographic entities mentioned:
surface_form: isola peak
instance_of: Mountain
countries: Canada
coordinates: lat: 50.1284
lon: -114.4987
2022 ICF Canoe Sprint World Championships – Women's K-1 200 metres. The women's K-1 200 metres competition at the 2022 ICF Canoe Sprint World Championships in Dartmouth took place on Lake Banook. Heats. The fastest boat in each heat advanced to the A final. The next six fastest boats in each heat advanced to the semifinals. Semifinal.

Geographic entities mentioned:
surface_form: Lake Banook
instance_of: Lake
countries: Canada
coordinates: lat: 44.6809
lon: -63.5569
Svarthornkammen Ridge. Svarthornkammen Ridge () is a high rock ridge extending north for 5 nautical miles (9 km) from Svarthorna Peaks in the Mittlere Petermann Range, Wohlthat Mountains. Discovered and plotted from air photos by German Antarctic Expedition, 1938–39. Replotted from air photos and surveys by Norwegian Antarctic Expedition, 1956–60, and named Svarthornkammen (the black peak ridge).

Geographic entities mentioned:
surface_form: Svarthorna Peaks
instance_of: Mountain
coordinates: lat: -71.5833
lon: 12.6167
surface_form: svarthornkammen
instance_of: Mountain
coordinates: lat: -71.5167
lon: 12.5167
Svarthornkammen Ridge. Svarthornkammen Ridge () is a high rock ridge extending north for 5 nautical miles (9 km) from Svarthorna Peaks in the Mittlere Petermann Range, Wohlthat Mountains. Discovered and plotted from air photos by German Antarctic Expedition, 1938–39. Replotted from air photos and surveys by Norwegian Antarctic Expedition, 1956–60, and named Svarthornkammen (the black peak ridge).

Geographic entities mentioned:
surface_form: svarthornkammen ridge
instance_of: Mountain
coordinates: lat: -71.5167
lon: 12.5167
Svarthornkammen Ridge. Svarthornkammen Ridge () is a high rock ridge extending north for 5 nautical miles (9 km) from Svarthorna Peaks in the Mittlere Petermann Range, Wohlthat Mountains. Discovered and plotted from air photos by German Antarctic Expedition, 1938–39. Replotted from air photos and surveys by Norwegian Antarctic Expedition, 1956–60, and named Svarthornkammen (the black peak ridge).

Geographic entities mentioned:
surface_form: svarthornkammen
instance_of: Mountain
coordinates: lat: -71.5167
lon: 12.5167
surface_form: black peak
instance_of: Mountain
coordinates: lat: -44.58388888888889
lon: 168.83138888888888
Pinto Mountain. Pinto Mountain is a summit, north of Round Valley, within the Mojave National Preserve, in San Bernardino County, California. Its summit rises to an elevation of.

Geographic entities mentioned:
surface_form: pinto mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.1808
lon: -115.3705
Pinto Mountain. Pinto Mountain is a summit, north of Round Valley, within the Mojave National Preserve, in San Bernardino County, California. Its summit rises to an elevation of.

Geographic entities mentioned:
surface_form: pinto mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.1808
lon: -115.3705
surface_form: round valley
instance_of: Valley
countries: United States
coordinates: lat: 35.15166667
lon: -115.36194444
Lehigh Gap. The Lehigh Gap or Lehigh Water Gap is a water gap located in the townships of Lehigh, Washington, Lower Towamensing, and East Penn in the Lehigh Valley and Coal Region regions of eastern Pennsylvania. It was formed by the Lehigh River, where it cuts through the Blue Mountain in Pennsylvania.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
Hanksite is normally found in crystal form as evaporite deposits. Hanksite crystals are large but not complex in structure. It is often found in Searles Lake, Soda Lake, Mono Lake, and in Death Valley. At its deposits in San Bernardino County, California hanksite is commonly found beneath the surface embedded in mud or in drill cores (Palache et al., 1960).

Geographic entities mentioned:
surface_form: Death Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.45693888888889
lon: -116.86528055555556
Lake Onega. Lake Onega (; also known as Onego;,;; Livvi: &quot;Oniegujärvi&quot;;) is a lake in northwestern Russia, on the territory of the Republic of Karelia, Leningrad Oblast and Vologda Oblast. It belongs to the basin of the Baltic Sea, and is the second-largest lake in Europe after Lake Ladoga, slightly smaller than Lebanon. The lake is fed by about 50 rivers and is drained by the Svir.

Geographic entities mentioned:
surface_form: Lake Ladoga
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.842777777777776
lon: 31.459722222222222
In the bays, the visibility may decrease to about a meter. The water is fresh, with a salinity of 35 mg/L. This is relatively low for a lake and is about times lower than in the other large lake of the area, Lake Ladoga. The maximum surface water temperature is on the open lake and in the bays. The deep waters are much colder, from in winter to in summer.

Geographic entities mentioned:
surface_form: Lake Ladoga
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.842777777777776
lon: 31.459722222222222
Basin and islands. The catchment area of drains into the lake via 58 rivers and more than 110 tributaries, including the Shuya, Suna, Vodla, Vytegra and Andoma. The only outgoing Svir, which marks the southern boundary of Karelia, runs from the southwestern shore of Lake Onega to Lake Ladoga and continues as the Neva to the Gulf of Finland.

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: lake onega
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 61.690555555556
lon: 35.655555555556
surface_form: onega
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 61.690555555556
lon: 35.655555555556
The White Sea–Baltic Canal runs through the lake from the White Sea to the Baltic Sea. The Volga–Baltic Waterway connects Onega Lake with the Volga, Caspian Sea and Black Sea. The Onega Canal, which follows the southern banks of the lake, was built in 1818–1820 and 1845–1852 between Vytegra in the east and Svir in the west.

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
surface_form: onega lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 61.690555555556
lon: 35.655555555556
surface_form: onega
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 61.690555555556
lon: 35.655555555556
The associated with the plant Verkhnesvirsk Reservoir has an area of and volume of, i.e. almost the same as those of Onega Lake. Its construction raised the water level of the lake by. The lake contains a well-developed navigation system which is part of the Volga–Baltic Waterway and White Sea – Baltic Canal, connecting the basins of Baltic, Caspian and the northern seas.

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
Lake Onega. Lake Onega (; also known as Onego;,;; Livvi: &quot;Oniegujärvi&quot;;) is a lake in northwestern Russia, on the territory of the Republic of Karelia, Leningrad Oblast and Vologda Oblast. It belongs to the basin of the Baltic Sea, and is the second-largest lake in Europe after Lake Ladoga, slightly smaller than Lebanon. The lake is fed by about 50 rivers and is drained by the Svir.

Geographic entities mentioned:
surface_form: lake onega
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 61.690555555556
lon: 35.655555555556
surface_form: onega
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 61.690555555556
lon: 35.655555555556
Lake Onega. Lake Onega (; also known as Onego;,;; Livvi: &quot;Oniegujärvi&quot;;) is a lake in northwestern Russia, on the territory of the Republic of Karelia, Leningrad Oblast and Vologda Oblast. It belongs to the basin of the Baltic Sea, and is the second-largest lake in Europe after Lake Ladoga, slightly smaller than Lebanon. The lake is fed by about 50 rivers and is drained by the Svir.

Geographic entities mentioned:
surface_form: lake onega
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 61.690555555556
lon: 35.655555555556
surface_form: oniegujärvi
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 61.690555555556
lon: 35.655555555556
surface_form: onego
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 61.690555555556
lon: 35.655555555556
surface_form: onega
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 61.690555555556
lon: 35.655555555556
These canals allow water transport of goods from the lake to the countries from Germany to Iran; most traffic goes to Finland, Sweden, Germany and Denmark. The Onega Canal running along the southern shore of the lake there is not used at present. Cargo on Lake Onega amounts to 10–12 million tonnes per year with about 10,300 ship voyages.

Geographic entities mentioned:
surface_form: onega
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 61.690555555556
lon: 35.655555555556
To the west of them lies the deep (deeper than) Greater Onega () area containing the Kondopozhskaya (, depth up to), Ilem-Gorskaya (), Lizhemskoy () and Unitskoy () bays. To the southwest of Greater Onega lies Petrozavodskoye Onego () containing the large Petrozavodsk and small Yalguba and Pinguba bays.

Geographic entities mentioned:
surface_form: onego
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 61.690555555556
lon: 35.655555555556
surface_form: onega
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 61.690555555556
lon: 35.655555555556
They contain numerous elongated bays resulting in the lake's outline appearing similar to a giant crayfish. In the northern part lies a large Zaonezhye Peninsula (); south of it, is the Big Klimenetsky () island. To the west of them lies the deep (deeper than) Greater Onega () area containing the Kondopozhskaya (, depth up to), Ilem-Gorskaya (), Lizhemskoy () and Unitskoy () bays.

Geographic entities mentioned:
surface_form: onega
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 61.690555555556
lon: 35.655555555556
To the east of Zaonezhye there is a bay, northern part of which is called Povenetsky Bay and the southern part is Zaonezhsky Bay. There, deep sections alternate with banks and islands which split the bay into several parts. The southernmost part of them, Lesser Onega, is deep. All the shores there are rocky. The average depth of the lake is, and the deepest spot of is located in the northern part.

Geographic entities mentioned:
surface_form: onega
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 61.690555555556
lon: 35.655555555556
The pogost was included in the list of UNESCO World Heritage sites in 1990. In the summer, there are daily boat connections to the island from Petrozavodsk. Onega petroglyphs. Another attraction of the lake are the Onega petroglyphs (rock engravings). They are located on the eastern coast of the lake and date back to between the 4th and 2nd millennia BC.

Geographic entities mentioned:
surface_form: onega
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 61.690555555556
lon: 35.655555555556
The company was incorporated in 1936 to organize the ownership of a large tract of land that was consolidated from four Mexican land grants acquired in the 1850s and 1860s by ranch founder Edward Fitzgerald Beale. The company owns over 270,000 acres (1,093 km2) in the southern San Joaquin Valley, Tehachapi Mountains, and Antelope Valley.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
Beale's son, Truxtun Beale, sold the Tejon Ranch in 1912 to a syndicate of investors headed by &quot;Los Angeles Times&quot; publisher Harry Chandler and land developer Moses Sherman. Both also had extensive holdings in the San Fernando Valley. In 1917, some surviving Kitanemuk Indians lived on Tejon Ranch.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Both also had extensive holdings in the San Fernando Valley. In 1917, some surviving Kitanemuk Indians lived on Tejon Ranch. In 1936, the Tejon Ranch Company became a public company, with the Chandler–Sherman group retaining a controlling interest. The Chandlers' Times Mirror Company sold its stake in 1997.

Geographic entities mentioned:
surface_form: Kitanemuk
instance_of: Valley
countries: United States
Col du Lein. Col du Lein (el. 1623 m.) is a high mountain pass in the Alps in the canton of Valais in Switzerland. It connects Saxon in the valley of the Rhône with Vollèges in the Val de Bagnes.

Geographic entities mentioned:
surface_form: Val de Bagnes
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.05
lon: 7.267
Winters lived the rest of his life in Miami, where he founded an export firm. He died there October 30, 1984 and his ashes were buried in the Alliance International Cemetery in Jerusalem's &quot;German Colony,&quot; next to Jerusalem's German Templar cemetery as well as scattered from Mount Tabor. Pardon.

Geographic entities mentioned:
surface_form: Mount Tabor
instance_of: Mountain
countries: Israel
coordinates: lat: 32.68625
lon: 35.392916666667
Present condition. At present, six columns remain standing along its south side with their entablature. Their capitals remain nearly perfect on the south side, while the Beqaa's winter winds have worn the northern faces almost bare. The remaining architrave and frieze blocks weigh as much as, with one corner block weighing over, all of them raised to a height of above the ground.

Geographic entities mentioned:
surface_form: Beqaa
instance_of: Valley
countries: Lebanon
coordinates: lat: 34.008888888889
lon: 36.145277777778
Rouge River East. The Rivière Rouge East is a tributary of the east bank of the Rouge River. This stream flows in the municipality of Château-Richer, in the La Jacques-Cartier Regional County Municipality, in the administrative region of Capitale-Nationale, in the province from Quebec, to Canada.

Geographic entities mentioned:
surface_form: rivière rouge
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.099721
lon: -71.109722
Toponymy. The toponyms &quot;Rivière Rouge&quot; and &quot;Rivière Rouge Est&quot; are linked. The toponym &quot;Rivière Rouge Est&quot; was officialized 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
surface_form: rivière rouge
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.099721
lon: -71.109722
surface_form: rivière rouge
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.099721
lon: -71.109722
surface_form: rivière rouge est
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.096666
lon: -71.106111
surface_form: rivière rouge est
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.096666
lon: -71.106111
The Rivière Rouge East is a tributary of the east bank of the Rouge River. This stream flows in the municipality of Château-Richer, in the La Jacques-Cartier Regional County Municipality, in the administrative region of Capitale-Nationale, in the province from Quebec, to Canada. The upper part of this forest valley surrounded by mountains is served by a forest road from the south.

Geographic entities mentioned:
surface_form: jacques-cartier
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.671388888889
lon: -71.747222222222
Rouge River East. The Rivière Rouge East is a tributary of the east bank of the Rouge River. This stream flows in the municipality of Château-Richer, in the La Jacques-Cartier Regional County Municipality, in the administrative region of Capitale-Nationale, in the province from Quebec, to Canada.

Geographic entities mentioned:
surface_form: rouge river east
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.096666
lon: -71.106111
Geography. The Rouge River East flows on the East bank of the Rouge river. From this confluence of the Rouge River East, the current descends on towards the northwest by following the course of the Rouge River, then descends on generally towards the south by the course of the Montmorency River, up to the northwest bank of the Saint Lawrence River. Toponymy.

Geographic entities mentioned:
surface_form: rouge river east
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.096666
lon: -71.106111
Forestry is the main economic activity in this valley; second, recreational tourism. Because of its altitude, the surface of the upper part of the Rouge East River is generally frozen from the end of November to the beginning of April; however, safe circulation on the ice is generally done from mid-December to the end of March.

Geographic entities mentioned:
surface_form: east river
instance_of: Watercourse
countries: Canada
coordinates: lat: 44.5529
lon: -62.3032
This brig took a member of a United States presidential expedition to survey land and the inhabitants of the area in the 1830s. The ship then transported members of the Willamette Cattle Company from Oregon Country to California in an effort to increase livestock in the Willamette Valley settlements. Early years.

Geographic entities mentioned:
surface_form: Willamette Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.9
lon: -123.1
The population was 412 as of 2013. There are 4 streets. Geography. Mirabilit lies in the Kulunda Steppe, near lake Maloye Shklo, and to the SSW of lake Bolshoye Shklo. It is located 8 km east of Kulunda (the district's administrative centre) by road. Kulunda is the nearest rural locality.

Geographic entities mentioned:
surface_form: Bolshoye Shklo
instance_of: Lake
countries: Russia
Soviet Union
Russian Empire
coordinates: lat: 52.631944444444
lon: 79.068055555556
Tryvann. Tryvann is a small lake in Nordmarka, the forest area just north of Oslo city, near the Holmenkollen ski jump. By the water lies a cabin called Tryvannstua, in which there is a café open regularly during both summer and winter. On a hill above the lake looms the television tower Tryvannstårnet (&quot;The Tryvann tower&quot;), visible from most of Oslo.

Geographic entities mentioned:
surface_form: tryvann
instance_of: Lake
countries: Norway
coordinates: lat: 59.997222222222
lon: 10.668888888889
By the water lies a cabin called Tryvannstua, in which there is a café open regularly during both summer and winter. On a hill above the lake looms the television tower Tryvannstårnet (&quot;The Tryvann tower&quot;), visible from most of Oslo. Tryvann is the entry and beginning of Nordmarka. It is used all year around.

Geographic entities mentioned:
surface_form: tryvann
instance_of: Lake
countries: Norway
coordinates: lat: 59.997222222222
lon: 10.668888888889
surface_form: tryvann
instance_of: Lake
countries: Norway
coordinates: lat: 59.997222222222
lon: 10.668888888889
It is used all year around. The key purposes of this area in the winter are skiing and cross-country skiing, whereas in the summer it is more commonly used for walks in the forest and biking. When referring to Tryvann, it is mostly referred to as the Tryvann vinterpark. Facts and infrastructure. Tryvann vinterpark is an alpine ski resort in the area around Tryvann.

Geographic entities mentioned:
surface_form: tryvann
instance_of: Lake
countries: Norway
coordinates: lat: 59.997222222222
lon: 10.668888888889
surface_form: tryvann
instance_of: Lake
countries: Norway
coordinates: lat: 59.997222222222
lon: 10.668888888889
When referring to Tryvann, it is mostly referred to as the Tryvann vinterpark. Facts and infrastructure. Tryvann vinterpark is an alpine ski resort in the area around Tryvann. The first ski slope of Tryvann vinterpark, named &quot;Tryvannskleiva&quot;, was created in 1931. Since then an enormous expansion has occurred, and today Tryvann vinterpark consists of 18 slopes and 11 lifts.

Geographic entities mentioned:
surface_form: tryvann
instance_of: Lake
countries: Norway
coordinates: lat: 59.997222222222
lon: 10.668888888889
Facts and infrastructure. Tryvann vinterpark is an alpine ski resort in the area around Tryvann. The first ski slope of Tryvann vinterpark, named &quot;Tryvannskleiva&quot;, was created in 1931. Since then an enormous expansion has occurred, and today Tryvann vinterpark consists of 18 slopes and 11 lifts. The longest run (Wyllerløypa) is 1,400 metres, with a drop of 381 metres.

Geographic entities mentioned:
surface_form: tryvann
instance_of: Lake
countries: Norway
coordinates: lat: 59.997222222222
lon: 10.668888888889
Tryvann vinterpark is easily accessed by visitors with the metro system. The ride from Oslo city centre to the top of Tryvann takes approximately 25 minutes. This gives easy access and opportunities for over one million citizens in Oslo. Tryvann is Norway's fourth biggest ski resort in Norway, measured in ticket sales. In 2012 there were 205,000 visitors. History of Tryvannstua.

Geographic entities mentioned:
surface_form: tryvann
instance_of: Lake
countries: Norway
coordinates: lat: 59.997222222222
lon: 10.668888888889
The storm damaged a radius close to 7000 m3, bringing down 3000 trees. As a result, Tryvannstua was constructed with the purpose of serving food for people travelling in the woods, and that was the beginning of Tryvann vinterpark. Tryvannstua was renovated and expanded in 1965–66. This increased the seating capacity to 175 people, and a fireplace was built for freezing alpinists.

Geographic entities mentioned:
surface_form: tryvann
instance_of: Lake
countries: Norway
coordinates: lat: 59.997222222222
lon: 10.668888888889
Landscape. Griswold Scout Reservation is situated in the Lakes Region of New Hampshire. The property extends through the towns of Alton, Gilford, and Gilmanton and covers over of forest, lakes, and mountains. Griswold Scout Reservation is situated in the Belknap Mountain Range. Six mountain peaks are located on the property, Mt. Klem, Mt. Anna, Mt. Mack, Mt.

Geographic entities mentioned:
surface_form: Belknap Mountain Range
instance_of: Mountain
countries: United States
coordinates: lat: 43.51777778
lon: -71.36916667
Both Manning Lake and Sunset Lake are public bodies of water, while Lake Eileen is owned by Griswold Scout Reservation. GSR is surrounded by remote wilderness on most sides, with hiking trails leading to nearby Gunstock Mountain or Belknap Mountain State Forest. Several ponds, four swamps, caves, rock faces, and many hills are situated across the reservation.

Geographic entities mentioned:
surface_form: Gunstock Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.525633333333
lon: -71.378405555556
2013 Genting Highlands bus crash. The 2013 Genting Highlands bus crash was the deadliest road accident to occur in Malaysia. 37 passengers were killed, and 16 others were injured in the crash which took place near Chin Swee Temple, Genting Highlands, Pahang.

Geographic entities mentioned:
surface_form: Genting Highlands
instance_of: Mountain
countries: Malaysia
coordinates: lat: 3.42368
lon: 101.79335
Ilford Peak. Ilford Peak (Hasho Peak II) is a peak located on the watershed of the Nangmah, Khane and Lachit valleys, Pakistan. The mountain, located in the Karakoram mountain range, is 6080 meters high. It was first climbed on July 23, 2019 by the group of Russian climbers Markevich Konstantin, Sushko Denis and Anton Ivanov.

Geographic entities mentioned:
surface_form: ilford peak
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.34466666666667
lon: 76.48991666666667
Mohammad Panah. General Mohammad Panah was an Afghan military commander who was loyal to Ahmad Shah Massoud. Panah was famous for successfully fighting Soviet incursions in the Panjsher Valley and other northern areas of Afghanistan. Following the withdrawal of USSR forces from Afghanistan and the subsequent collapse of the Communist regime in Kabul, Panah fought Hezb-e-islami and the Taliban.

Geographic entities mentioned:
surface_form: Panjsher
instance_of: Valley
countries: Afghanistan
coordinates: lat: 35.266666666667
lon: 69.466666666667
Pics de la Font Sancte. The Pics de la Font Sancte is a mountain with two summits between the upper Ubaye Valley, Val Escreins and the Ceillac Valley, at the edge of the Queyras Regional Park. It is the highest peak of the &quot;Escreins Massif&quot; in the southern Cottian Alps in Hautes-Alpes, France. Its northern summit is high and its south summit.

Geographic entities mentioned:
surface_form: Ubaye Valley
instance_of: Valley
countries: France
coordinates: lat: 44.433780555556
lon: 6.6563416666667
surface_form: pics de la font sancte
instance_of: Mountain
countries: France
coordinates: lat: 44.60619
lon: 6.79912
It is the highest peak of the &quot;Escreins Massif&quot; in the southern Cottian Alps in Hautes-Alpes, France. Its northern summit is high and its south summit. They take their name from the Font Sancte, a source that springs from the rock in the valley at the foot of the peaks at 2,358 m. The northern peak is climbed mostly from the west.

Geographic entities mentioned:
surface_form: the rock
instance_of: Mountain
countries: France
coordinates: lat: 10.29236
lon: -109.20762983333333
Pics de la Font Sancte. The Pics de la Font Sancte is a mountain with two summits between the upper Ubaye Valley, Val Escreins and the Ceillac Valley, at the edge of the Queyras Regional Park. It is the highest peak of the &quot;Escreins Massif&quot; in the southern Cottian Alps in Hautes-Alpes, France. Its northern summit is high and its south summit.

Geographic entities mentioned:
surface_form: pics de la font sancte
instance_of: Mountain
countries: France
coordinates: lat: 44.60619
lon: 6.79912
This provides access from a sloping road crossed by a causeway over the moat. The fort has Hindu, Jain and Muslim architectural influence with temples and mosques within its limits, indicating cultural syncretism. The architectural styles seen in the mosques are of the Indo-Saracenic and Deccan type. The fort has been built with stones and mud. A wide moat runs round the fort. Jain temples.

Geographic entities mentioned:
surface_form: Deccan
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
Topography. The Molloy Deep is a roughly rectangular, seismically active, extensional, sea-floor basin that lies between the northwestern tip of the Molloy Fracture Zone (a right-lateral, strike-slip fault) and the Spitsbergen Fracture Zone (also a right-lateral, strike-slip fault).

Geographic entities mentioned:
surface_form: active
instance_of: Landform
Body of water
coordinates: lat: -63.4167
lon: -56.1667
surface_form: molloy deep
instance_of: Body of water
coordinates: lat: 79.137
lon: 2.817
Molloy Deep. The Molloy Deep (also known as the Molloy Hole) is a bathymetric feature in the Fram Strait, within the Greenland Sea east of Greenland and about west of Svalbard. It is the location of the deepest point in the Arctic Ocean. The Molloy Deep, Molloy Hole, Molloy Fracture Zone, and Molloy Ridge were named after Arthur E. Molloy, a U.S.

Geographic entities mentioned:
surface_form: arthur
instance_of: Mountain
coordinates: lat: -67.65
lon: 49.86667
surface_form: molloy deep
instance_of: Body of water
coordinates: lat: 79.137
lon: 2.817
Surveys. The Molloy Deep was discovered in September 1972 by the USNS Hayes (T-AGOR-16), the first of a new class of catamaran-hulled oceanographic research vessels. The Molloy Deep, Molloy Hole, Molloy Fracture Zone, and Molloy Ridge were named after Arthur E. Molloy, a U.S. Navy research scientist who worked in the North Atlantic, North Pacific and Arctic Oceans in the 1950s–1970s. Descents.

Geographic entities mentioned:
surface_form: arthur
instance_of: Mountain
coordinates: lat: -67.65
lon: 49.86667
surface_form: molloy deep
instance_of: Body of water
coordinates: lat: 79.137
lon: 2.817
Surveys. The Molloy Deep was discovered in September 1972 by the USNS Hayes (T-AGOR-16), the first of a new class of catamaran-hulled oceanographic research vessels. The Molloy Deep, Molloy Hole, Molloy Fracture Zone, and Molloy Ridge were named after Arthur E. Molloy, a U.S. Navy research scientist who worked in the North Atlantic, North Pacific and Arctic Oceans in the 1950s–1970s. Descents.

Geographic entities mentioned:
surface_form: hayes
instance_of: Mountain
coordinates: lat: -66.83333333
lon: -64.16666667
surface_form: molloy deep
instance_of: Body of water
coordinates: lat: 79.137
lon: 2.817
Molloy Deep. The Molloy Deep (also known as the Molloy Hole) is a bathymetric feature in the Fram Strait, within the Greenland Sea east of Greenland and about west of Svalbard. It is the location of the deepest point in the Arctic Ocean. The Molloy Deep, Molloy Hole, Molloy Fracture Zone, and Molloy Ridge were named after Arthur E. Molloy, a U.S.

Geographic entities mentioned:
surface_form: molloy deep
instance_of: Body of water
coordinates: lat: 79.137
lon: 2.817
The outer rim of the trench is at a depth of and contains about inside the rim, descending to approximately at its greatest depth. The basin floor measures about and is the deepest point in the Arctic Ocean. The only person to have reached the bottom of the Molloy Deep is American explorer Victor Vescovo as part of his Five Deeps Expedition. Topography.

Geographic entities mentioned:
surface_form: molloy deep
instance_of: Body of water
coordinates: lat: 79.137
lon: 2.817
surface_form: victor
instance_of: Mountain
coordinates: lat: -72.6
lon: 31.26666667
Descents. The only person to reach the bottom of the Molloy Deep is Victor Vescovo on 24 August 2019. The Five Deeps Expedition leader and chief submersible pilot, Vescovo, descended into the Molloy Deep in the Deep-Submergence Vehicle &quot;Limiting Factor&quot; (a Triton 36000/2 model submersible) from the support ship, the Deep Submersible Support Vessel &quot;DSSV Pressure Drop&quot;.

Geographic entities mentioned:
surface_form: molloy deep
instance_of: Body of water
coordinates: lat: 79.137
lon: 2.817
surface_form: victor
instance_of: Mountain
coordinates: lat: -72.6
lon: 31.26666667
Descents. The only person to reach the bottom of the Molloy Deep is Victor Vescovo on 24 August 2019. The Five Deeps Expedition leader and chief submersible pilot, Vescovo, descended into the Molloy Deep in the Deep-Submergence Vehicle &quot;Limiting Factor&quot; (a Triton 36000/2 model submersible) from the support ship, the Deep Submersible Support Vessel &quot;DSSV Pressure Drop&quot;.

Geographic entities mentioned:
surface_form: molloy deep
instance_of: Body of water
coordinates: lat: 79.137
lon: 2.817
The Five Deeps Expedition leader and chief submersible pilot, Vescovo, descended into the Molloy Deep in the Deep-Submergence Vehicle &quot;Limiting Factor&quot; (a Triton 36000/2 model submersible) from the support ship, the Deep Submersible Support Vessel &quot;DSSV Pressure Drop&quot;. The Five Deeps Expedition established the depth of the Molloy Deep as ± by direct CTD pressure measurements.

Geographic entities mentioned:
surface_form: molloy deep
instance_of: Body of water
coordinates: lat: 79.137
lon: 2.817
Stage 1. 8 September 2001 — Salamanca to Salamanca, (ITT)
Stage 2. 9 September 2001 — Salamanca to Valladolid,
Stage 3. 10 September 2001 — Valladolid to León,
Stage 4. 11 September 2001 — León to Gijón,
Stage 5. 12 September 2001 — Gijón to Lagos de Covadonga,
Stage 6. 13 September 2001 — Cangas de Onís to Torrelavega,
Stage 7. 14 September 2001 — Torrelavega to Torrelavega, (ITT)
Stage 8.

Geographic entities mentioned:
surface_form: Lagos de Covadonga
instance_of: Group of lakes
countries: Spain
coordinates: lat: 43.26829288409789
lon: -4.985873734085007
(It was a part of the ancient region of Dahistan). Now a dry river channel and a center for archaeological excavations, the Uzboy flowed some, from a branch in the Amu Darya River via Sarykamysh Lake to the Caspian Sea.

Geographic entities mentioned:
surface_form: Sarykamysh Lake
instance_of: Lake
countries: Uzbekistan
Turkmenistan
coordinates: lat: 42
lon: 57.333333333333
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
They changed the course of the rivers, mainly the Amu Darya and its tributaries, which included the Uzboy. The Ustyurt Plateau protruded into the Aralo-Caspian lowland as a peninsula. It first separated the Caspian Sea from the Aral Sea near Bala-İşem, then the Uzboy Valley  and other natural connecting channels between the two lakes were formed.

Geographic entities mentioned:
surface_form: Ustyurt Plateau
instance_of: Plateau
countries: Uzbekistan
Kazakhstan
Russian Empire
Soviet Union
Turkmenistan
coordinates: lat: 43.283333333333
lon: 55.55
They changed the course of the rivers, mainly the Amu Darya and its tributaries, which included the Uzboy. The Ustyurt Plateau protruded into the Aralo-Caspian lowland as a peninsula. It first separated the Caspian Sea from the Aral Sea near Bala-İşem, then the Uzboy Valley  and other natural connecting channels between the two lakes were formed.

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
surface_form: Aral Sea
instance_of: Lake
countries: Kazakhstan
Uzbekistan
Russian Empire
Soviet Union
coordinates: lat: 45
lon: 60
It is possible that the main current shifted from the Aral to the Caspian, causing the Caspian to rise and the Aral to sink. There may have been a significant population along the Uzboy and farmland in what were later the marshes at the north end of the Oxus delta. It seems that about 1575 the east branch of the Oxus cut through some hills causing the main current to shift to the Aral Sea.

Geographic entities mentioned:
surface_form: Aral Sea
instance_of: Lake
countries: Kazakhstan
Uzbekistan
Russian Empire
Soviet Union
coordinates: lat: 45
lon: 60
Gigalitz. The Gigalitz is a mountain, on the Floitenkamm ridge of the Zillertal Alps between the bottoms of Floitengrund and Stillupgrund. It is the &quot;Hausberg&quot; of the Greizer Hut. Ascent. From the Greizer Hut the path runs up to the col of Lapenscharte (crossing to the Kasseler Hut) to a signed fork at a height of about 2,500 m.

Geographic entities mentioned:
surface_form: zillertal
instance_of: Valley
countries: Austria
coordinates: lat: 47.333333333333
lon: 11.866666666667
surface_form: gigalitz
instance_of: Mountain
countries: Austria
coordinates: lat: 47.0581
lon: 11.8908
Gigalitz. The Gigalitz is a mountain, on the Floitenkamm ridge of the Zillertal Alps between the bottoms of Floitengrund and Stillupgrund. It is the &quot;Hausberg&quot; of the Greizer Hut. Ascent. From the Greizer Hut the path runs up to the col of Lapenscharte (crossing to the Kasseler Hut) to a signed fork at a height of about 2,500 m.

Geographic entities mentioned:
surface_form: gigalitz
instance_of: Mountain
countries: Austria
coordinates: lat: 47.0581
lon: 11.8908
The Tartaro river contributed to the swamp; as the land dried up, some villages started to be set around its course: they were the first hamlets of Lendinara, Villanova del Ghebbo, Rovigo and Villadose. The Mincio river diverted to the south and has become a tributary of the Po river since then; it had been a waterway from the Adriatic Sea to the lake Garda until then.

Geographic entities mentioned:
surface_form: lake Garda
instance_of: Lake
countries: Italy
coordinates: lat: 45.633333333333
lon: 10.666666666667
I-90 begins at Washington State Route 519 in Seattle and crosses the Cascade Range in Washington and the Rocky Mountains in Montana. It then traverses the northern Great Plains and travels southeast through Wisconsin and the Chicago area by following the southern shore of Lake Michigan.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
It then traverses the northern Great Plains and travels southeast through Wisconsin and the Chicago area by following the southern shore of Lake Michigan. The freeway continues across Indiana and follows the shore of Lake Erie through Ohio and Pennsylvania to Buffalo.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Hadley Memorial Bridge, which carries westbound traffic and the future light rail line. The floating bridges cross Lake Washington to Mercer Island, where I-90 travels through a series of tunnels under of parkland, including Aubrey Davis Park. The freeway continues from the island and enters Bellevue, the largest city of the Eastside region, and intersects I-405 near Factoria.

Geographic entities mentioned:
surface_form: Lake Washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
The freeway continues from the island and enters Bellevue, the largest city of the Eastside region, and intersects I-405 near Factoria. I-90 then travels along Lake Sammamish and through Issaquah as it leaves the Seattle metropolitan area and ascends into the Cascade Range on the Mountains to Sound Greenway, a designated National Heritage Area and National Scenic Byway.

Geographic entities mentioned:
surface_form: Lake Sammamish
instance_of: Lake
countries: United States
coordinates: lat: 47.61638888888889
lon: -122.08944444444444
Route 97 (US 97). The highway crosses the Columbia River on the Vantage Bridge and turns northeast to climb the cliffs of the Columbia Plateau near George. After traveling east across Moses Lake and the surrounding agricultural region, I-90 begins a long concurrency with US 395 at Ritzville as the highways turn northeast towards Spokane.

Geographic entities mentioned:
surface_form: Columbia Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 45.999444444444
lon: -119.00138888889
I-90 then reaches Gillette, where it begins a concurrency with US 14 and US 16 to a three-way split in Moorcroft. The freeway continues into the Bear Lodge Mountains (part of the Black Hills) and is rejoined in Sundance by US 14, which looped north to serve the Devils Tower. I-90/US 14 then continues northeast to Beulah, where it enters South Dakota. South Dakota.

Geographic entities mentioned:
surface_form: Devils Tower
instance_of: Mountain
countries: United States
coordinates: lat: 44.590277777778
lon: -104.71527777778
I-90/US 14 then continues northeast to Beulah, where it enters South Dakota. South Dakota. I-90/US 14 enters South Dakota near Spearfish and travels east through prairie land, where it is briefly concurrent with US 85. Beyond Sturgis, the freeway turns south and follows the edge of the Black Hills to Rapid City, the gateway to Mount Rushmore.

Geographic entities mentioned:
surface_form: Mount Rushmore
instance_of: Mountain
countries: United States
coordinates: lat: 43.878947222222
lon: -103.459825
I-90 leaves Sioux Falls and crosses into Minnesota near Brandon. Minnesota. I-90 crosses the southern portion of Minnesota and carries unsigned Legislative Route 391 across the state. From the South Dakota border near Beaver Creek to Albert Lea, the freeway travels east across farmland and towns in the plains and rolling hills of the Buffalo Ridge.

Geographic entities mentioned:
surface_form: Buffalo Ridge
instance_of: Landform
countries: United States
coordinates: lat: 43.9802
lon: -96.0106
I-90 then crosses I-65 in eastern Gary and I-94 in Lake Station, where it begins a concurrency with I-80. I-94 travels northeast near the Lake Michigan shoreline from Lake Station to Michigan City, while the Indiana Toll Road (I-80/I-90) follows it to the south.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
I-80/I-90 then continues southeast across the Maumee River to Rossford on the southern outskirts of Toledo, where it intersects I-75. The turnpike travels southeast through a rural area near the southwest shore of Lake Erie, where it passes the cities of Fremont and Sandusky.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222