Sarmila/GeoWiki-Features huggingface dataset:
Geology and history. The heart of these &quot;kuppen&quot;, that were called the Hessian Skittles thanks to their similar shape and number, consists mainly of hexagonal basalt columns (see also under Stoppelsberg), that were formed as the lava cooled off. According to legend, the giants had a skittle alley here, using the Stoppelsberg as the bowling ball. Mountains and hills.

Geographic entities mentioned:
surface_form: Stoppelsberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.751388888889
lon: 9.7016666666667
Mountains and hills. The Gehilfersberg (456 m) is not, however one of the skittles, even though it could have been considered due to its location. The sentence is used to remember the names of the various hills that all end in &quot;-berg&quot;: the Wissels-, Rückers-, Appels-, Stoppels-, Klein-, Mors-, Stall-, Licht- and Soisberg as the nine peaks in the game of skittles.

Geographic entities mentioned:
surface_form: Gehilfersberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.725277777778
lon: 9.885
In the historical records, Tartessos () appears as a semi-mythical or legendary harbor city and the surrounding culture on the south coast of the Iberian Peninsula (in modern Andalusia, Spain), at the mouth of the Guadalquivir. It appears in sources from Greece and the Near East starting during the first millennium BC. Herodotus, for example, describes it as beyond the Pillars of Hercules.

Geographic entities mentioned:
surface_form: Pillars of Hercules
instance_of: Landform
countries: Morocco
Spain
Gibraltar
coordinates: lat: 36
lon: -5.35
Kanga (garment). The kanga (in some areas known as leso) is a colourful fabric similar to kitenge, but lighter, worn by women and occasionally by men throughout the African Great Lakes region.

Geographic entities mentioned:
surface_form: African Great Lakes
instance_of: Group of lakes
countries: Burundi
Zambia
Kenya
Democratic Republic of the Congo
Malawi
Mozambique
Rwanda
Tanzania
Uganda
Ethiopia
coordinates: lat: -8
lon: 35
At age 17, he jumped off a bridge over the Drina to save a drowning 11-year-old. Two years later, he rescued a mother and daughter from a car that had crashed into a ravine in Ivan planina while he was on leave from military duty. Four years later, he saved a mother and her two children who were trapped in a burning vehicle while he was in Zurich.

Geographic entities mentioned:
surface_form: Ivan planina
instance_of: Mountain
countries: Bosnia and Herzegovina
coordinates: lat: 43.79198
lon: 18.0092
In the recent past, Kashmir has been portrayed in many films for the unrest in the region, however in this film there is no violence and the movie depicts the beauty and chastity of Kashmir and Kashmiris. The movie portrays how even today Muslims and Pandit's stay in harmony in the Kashmir Valley. The film travels through many beautiful locations in Kashmir.

Geographic entities mentioned:
surface_form: Kashmir Valley
instance_of: Valley
countries: India
coordinates: lat: 34.0333
lon: 74.6667
Caughnawaga, New York. Caughnawaga is a former town in then Tryon County, later Montgomery County, New York, United States. Its former site lies near Fultonville, New York, ten miles west of Amsterdam in the Mohawk Valley west of Albany. Caughnawaga is believed to be a Mohawk language word meaning &quot;at the rapids&quot;, referring to the site along the Mohawk River.

Geographic entities mentioned:
surface_form: Mohawk Valley
instance_of: Valley
countries: United States
In the following years, he competed many times in the finals of the Polish Youth Chess Championships in various age groups, winning two medals: gold (Kołobrzeg 2004) and bronze (Wisła 2003), both in the U10 age group. In 2007, he took third place in the open chess championships Podhale held in Rabka-Zdrój.

Geographic entities mentioned:
surface_form: Podhale
instance_of: Valley
countries: Poland
coordinates: lat: 49.4793
lon: 20.0291
The peak lies above the Shyamvarn Glacier. The elevation of Shyamvarn is and its prominence is. It is 150th highest located entirely within the Uttrakhand. Nanda Devi, is the highest mountain in this category. It lies 3.3 km east of Sudarshan Parbat. Saife lies 2.5 km WSW and it is 3 km ESE of Shwetvarna. It lies 2.8 km South of Yogeshwar. Climbing history.

Geographic entities mentioned:
surface_form: Nanda Devi
instance_of: Mountain
countries: India
coordinates: lat: 30.37388888888889
lon: 79.97083333333333
The peak lies above the Shyamvarn Glacier. The elevation of Shyamvarn is and its prominence is. It is 150th highest located entirely within the Uttrakhand. Nanda Devi, is the highest mountain in this category. It lies 3.3 km east of Sudarshan Parbat. Saife lies 2.5 km WSW and it is 3 km ESE of Shwetvarna. It lies 2.8 km South of Yogeshwar. Climbing history.

Geographic entities mentioned:
surface_form: Sudarshan Parbat
instance_of: Mountain
countries: India
coordinates: lat: 30.976944444444445
lon: 79.09333333333333
The elevation of Shyamvarn is and its prominence is. It is 150th highest located entirely within the Uttrakhand. Nanda Devi, is the highest mountain in this category. It lies 3.3 km east of Sudarshan Parbat. Saife lies 2.5 km WSW and it is 3 km ESE of Shwetvarna. It lies 2.8 km South of Yogeshwar. Climbing history. The first ascent of Shyamvarn ends with a tragedy.

Geographic entities mentioned:
surface_form: Saife
instance_of: Mountain
countries: India
coordinates: lat: 30.964444444444446
lon: 79.09972222222223
surface_form: Shwetvarna
instance_of: Mountain
countries: India
Shyamvarna. Shyamvarn is a mountain of the Garhwal Himalaya in Uttarakhand India. The peak lies above the Shyamvarn Glacier. The elevation of Shyamvarn is and its prominence is. It is 150th highest located entirely within the Uttrakhand. Nanda Devi, is the highest mountain in this category. It lies 3.3 km east of Sudarshan Parbat. Saife lies 2.5 km WSW and it is 3 km ESE of Shwetvarna.

Geographic entities mentioned:
surface_form: shyamvarna
instance_of: Mountain
countries: India
coordinates: lat: 30.976111111111113
lon: 79.12777777777778
Shyamvarna. Shyamvarn is a mountain of the Garhwal Himalaya in Uttarakhand India. The peak lies above the Shyamvarn Glacier. The elevation of Shyamvarn is and its prominence is. It is 150th highest located entirely within the Uttrakhand. Nanda Devi, is the highest mountain in this category. It lies 3.3 km east of Sudarshan Parbat. Saife lies 2.5 km WSW and it is 3 km ESE of Shwetvarna.

Geographic entities mentioned:
surface_form: shyamvarn
instance_of: Mountain
countries: India
coordinates: lat: 30.976111111111113
lon: 79.12777777777778
Saife lies 2.5 km WSW and it is 3 km ESE of Shwetvarna. It lies 2.8 km South of Yogeshwar. Climbing history. The first ascent of Shyamvarn ends with a tragedy. An Indian eight member team led by climber Asit Kumar Moitra Climbed Shyamvarn on 26 September 1985. On the way back from the summit, the leader Asit Kumar Moitra slipped and fell 2000 feet to his death.

Geographic entities mentioned:
surface_form: shyamvarn
instance_of: Mountain
countries: India
coordinates: lat: 30.976111111111113
lon: 79.12777777777778
The team consisted of Samir Bhattacharya, Manas Bardhan, Nabagopal Basak, Ramjan Bose, Krishna Ganguli, Asish Roy and Sanjoy Roy. An Indian team from Bombay was led by Ramakant Mahadik. On 20 June 1989 seven member climbed Shyamvarn this is the second ascent of this peak. Glaciers and rivers. Swetvarn Bamak on the western side.

Geographic entities mentioned:
surface_form: shyamvarn
instance_of: Mountain
countries: India
coordinates: lat: 30.976111111111113
lon: 79.12777777777778
On 20 June 1989 seven member climbed Shyamvarn this is the second ascent of this peak. Glaciers and rivers. Swetvarn Bamak on the western side. Shyamvarn bamak on the eastern side both these Glaciers are tributaries of Raktvarn Bamak which drain itself at Gangotri Glacier. From the snout of Gangotri Glacier which was called Gomukh emerges Bhagirathi river.

Geographic entities mentioned:
surface_form: shyamvarn
instance_of: Mountain
countries: India
coordinates: lat: 30.976111111111113
lon: 79.12777777777778
Dessau. Dessau is a district of the independent city of Dessau-Roßlau in Saxony-Anhalt at the confluence of the rivers Mulde and Elbe, in the &quot;Bundesland&quot; (Federal State) of Saxony-Anhalt. Until 1 July 2007, it was an independent city. The population of Dessau is 67,747 (Dec. 2020). Geography. Dessau is situated on a floodplain where the Mulde flows into the Elbe.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Until 1 July 2007, it was an independent city. The population of Dessau is 67,747 (Dec. 2020). Geography. Dessau is situated on a floodplain where the Mulde flows into the Elbe. This causes yearly floods. The worst flood took place in the year 2002, when the Waldersee district was nearly completely flooded. The south of Dessau touches a well-wooded area called Mosigkauer Heide.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Plover Islands. The uninhabited Plover Islands are an archipelago, members of the Arctic Archipelago and the Ungava Bay Archipelago, in the Qikiqtaaluk Region of Nunavut, Canada. They are located in western Ungava Bay, just northeast of the Arnaud River and the community of Kangirsuk on Quebec's Ungava Peninsula. Geography. The islands have a hard granitic gneiss and a thin layer of soil.

Geographic entities mentioned:
surface_form: Arnaud River
instance_of: Watercourse
countries: Canada
coordinates: lat: 59.98166666666667
lon: -69.75944444444444
Miller Woods is also the only part of the National Park that also adjoins the Grand Calumet River. The northern part of Miller Woods adjoins Lake Michigan, and includes foredunes and high dunes, as well as blowouts and pannes. The southern and larger part of Miller Woods consists of rolling ridge and swale, with beach ridges dominated by oak savanna.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
This river flows on the north bank of the Grand Touradi River which flows northeast to the south bank of the Rimouski River; the latter flows west, then north, to the south shore of the St. Lawrence River where it pours into the heart of the city of Rimouski. Geography.

Geographic entities mentioned:
surface_form: Rimouski River
instance_of: Watercourse
countries: Canada
coordinates: lat: 48.445277777777775
lon: -68.54083333333334
Sidi Ghrib. Sidi Ghrib is a Tunisian archaeological site about southwest of Carthage and from Borj El Amri, known for its beautiful Roman mosaics. Archaeology. The site was searched in 1975. The study by Abdelmajid Ennabli showed that the site was a Roman villa of the late 4th or early 5th century. The thermal baths at the site formed part of the villa and were therefore private.

Geographic entities mentioned:
surface_form: sidi ghrib
instance_of: Mountain
countries: Morocco
Xinovrysi. Xinovrysi (, before 1927: Μπεστίνικα - &quot;Bestinika&quot;) is a village in the Pelion area in Magnesia, Greece. It is part of the municipal unit of Argalasti. Xinovrysi is 3.5 km northeast of Argalasti, 7 km north of Promyri and 30 km southeast of Volos. The community includes the village Potistika. History.

Geographic entities mentioned:
surface_form: Pelion
instance_of: Mountain
countries: Greece
coordinates: lat: 39.433333333333
lon: 23.05
Itinerary items in Antarctica include Zodiac boat landings and cruises to Paulet Island and the Argentine Esperanza Base; Deception Island, a dormant volcano inhabited by chinstrap penguins; Koerner Rock, Neko Harbour and Ukraine's Vernadsky Station, a scientific research base in Antarctica; Petermann Island, home of gentoo penguin and Adélie penguin colonies, Pleneau Island, Danco Island, and Goudier Island, and the rocky Wauwermans Islands.

Geographic entities mentioned:
surface_form: Paulet Island
instance_of: Mountain
coordinates: lat: -63.583333333333
lon: -55.783333333333
Prehistoric pile dwellings around Lake Zurich. Prehistoric pile dwellings around Lake Zurich are pile dwelling sites located around Lake Zurich in the cantons of Schwyz, St. Gallen and Zurich. The article focuses on the 9 Lake Zurich sites that are among the 111 sites included in the UNESCO World Heritage Prehistoric pile dwellings around the Alps established in 2011.

Geographic entities mentioned:
surface_form: Lake Zurich
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.2475
lon: 8.6775
56 of the 111 UNESCO World Heritage pile dwelling sites are located in Switzerland and 9 thereof are located on the Lake Zurich seashore. The article also includes one UNESCO World Heritage site at the nearby Greifensee and one UNESCO World Heritage site at the Pfäffikersee.

Geographic entities mentioned:
surface_form: Pfäffikersee
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.352222222222
lon: 8.78
Geography. The 11 prehistoric pile-dwelling (or stilt house) sites are concentrated within an area of about, on Lake Zurich, specifically &quot;Obersee&quot; lakeshore in the cantons of Schwyz, St. Gallen and Zurich. Characteristics. The pile-dwelling sites were built from around 5000 BC to 500 BC.

Geographic entities mentioned:
surface_form: Lake Zurich
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.2475
lon: 8.6775
Most of the settlements were inhabited for some decades and then re-erected at a quite different location. A notable exception is the settlement Robenhausen at the Pfäffikersee, discovered and researched by Jakob Messikommer at the end of the 19th century, which was continuously inhabited for thousands of years.

Geographic entities mentioned:
surface_form: Pfäffikersee
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.352222222222
lon: 8.78
The following nine Lake Zurich sites are among the 111 sites included in the UNESCO World Heritage Prehistoric pile dwellings around the Alps. Greifensee. The Greifensee is located at a distance of appromimately 7km to the northeast of Lake Zurich. Pfäffikersee. The Pfäffikersee is located at a distance of appromimately 6km to the east of the Greifensee. Protection.

Geographic entities mentioned:
surface_form: Pfäffikersee
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.352222222222
lon: 8.78
Booth was born in 1924 in Farnham, Surrey. His father Lionel Booth is credited as the inventor of the telephoto lens. He was brought up in Wensleydale, Yorkshire and attended Sedbergh school. He served as a frogman in the Royal Navy from 1942. A Navy doctor encouraged him to study medicine, so he enrolled at the Bute Medical School of the University of St.

Geographic entities mentioned:
surface_form: Wensleydale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.3056
lon: -2.16667
It lies south of the lakes Tipiqucha and Huch'uy Tipiqucha, and northeast of the lakes Yanaqucha (&quot;black lake&quot;) and Kunturqucha.

Geographic entities mentioned:
surface_form: Huch'uy Tipiqucha
instance_of: Lake
countries: Peru
coordinates: lat: -14.9094
lon: -73.1497
surface_form: Kunturqucha
instance_of: Lake
countries: Peru
coordinates: lat: -14.935
lon: -73.1639
surface_form: yanaqucha
instance_of: Lake
countries: Peru
coordinates: lat: -12.8997
lon: -74.1439
surface_form: yanaqucha
instance_of: Lake
countries: Peru
coordinates: lat: -10.8611
lon: -75.9903
surface_form: yanaqucha
instance_of: Lake
countries: Peru
coordinates: lat: -10.04233333
lon: -77.20836111
surface_form: yanaqucha
instance_of: Mountain
countries: Peru
coordinates: lat: -10.5658
lon: -75.9417
surface_form: kunturqucha
instance_of: Lake
countries: Peru
coordinates: lat: -14.935
lon: -73.1639
surface_form: yanaqucha
instance_of: Lake
countries: Peru
coordinates: lat: -9.5275
lon: -77.2306
surface_form: yanaqucha
instance_of: Lake
countries: Peru
coordinates: lat: -12.9525
lon: -74.1194
surface_form: yanaqucha
instance_of: Mountain
countries: Peru
coordinates: lat: -14.4561
lon: -70.9019
surface_form: yanaqucha
instance_of: Mountain
countries: Peru
coordinates: lat: -13.97694444
lon: -70.90138889
surface_form: yanaqucha
instance_of: Mountain
countries: Peru
coordinates: lat: -13.64861111
lon: -70.73361111
surface_form: yanaqucha
instance_of: Mountain
countries: Peru
coordinates: lat: -9.69777778
lon: -77.08888889
surface_form: yanaqucha
instance_of: Lake
countries: Peru
coordinates: lat: -10.1069
lon: -76.0678
surface_form: yanaqucha
instance_of: Mountain
countries: Peru
coordinates: lat: -13.38444444
lon: -72.32555556
Hatun Tipiqucha. Hatun Tipiqucha (Quechua &quot;hatun&quot; big, &quot;tipi&quot; &quot;Pennisetum clandestinum&quot; (a grass species), &quot;tipiy&quot; to husk maize, to snap, to break, &quot;qucha&quot; lake, Hispanicized spelling &quot;Ccatuntipicocha&quot;) is a lake in Peru located in the Ayacucho Region, Paucar del Sara Sara Province, Oyolo District.

Geographic entities mentioned:
surface_form: tipiqucha
instance_of: Lake
countries: Peru
coordinates: lat: -11.745
lon: -75.220277777778
surface_form: tipiqucha
instance_of: Lake
countries: Peru
coordinates: lat: -12.795
lon: -75.21444444
surface_form: hatun tipiqucha
instance_of: Lake
countries: Peru
coordinates: lat: -14.9206
lon: -73.1447
Hatun Tipiqucha. Hatun Tipiqucha (Quechua &quot;hatun&quot; big, &quot;tipi&quot; &quot;Pennisetum clandestinum&quot; (a grass species), &quot;tipiy&quot; to husk maize, to snap, to break, &quot;qucha&quot; lake, Hispanicized spelling &quot;Ccatuntipicocha&quot;) is a lake in Peru located in the Ayacucho Region, Paucar del Sara Sara Province, Oyolo District.

Geographic entities mentioned:
surface_form: tipiqucha
instance_of: Lake
countries: Peru
coordinates: lat: -11.745
lon: -75.220277777778
surface_form: tipiqucha
instance_of: Lake
countries: Peru
coordinates: lat: -11.745
lon: -75.220277777778
surface_form: tipiqucha
instance_of: Lake
countries: Peru
coordinates: lat: -11.745
lon: -75.220277777778
surface_form: sara sara
instance_of: Mountain
countries: Peru
coordinates: lat: -15.323527777778
lon: -73.449361111111
surface_form: tipiqucha
instance_of: Lake
countries: Peru
coordinates: lat: -12.795
lon: -75.21444444
surface_form: tipiqucha
instance_of: Lake
countries: Peru
coordinates: lat: -12.795
lon: -75.21444444
surface_form: tipiqucha
instance_of: Lake
countries: Peru
coordinates: lat: -12.795
lon: -75.21444444
surface_form: sara sara
instance_of: Mountain
countries: Peru
coordinates: lat: -14.6381
lon: -72.7881
surface_form: hatun tipiqucha
instance_of: Lake
countries: Peru
coordinates: lat: -14.9206
lon: -73.1447
surface_form: ccatuntipicocha
instance_of: Lake
countries: Peru
coordinates: lat: -14.9206
lon: -73.1447
In the Himalayas and the Tibetan Plateau, there is evidence that glaciers advanced considerably, particularly between 47,000 and 27,000 BP, but the exact ages, as well as the formation of a single contiguous ice sheet on the Tibetan Plateau, is controversial. Other areas of the Northern Hemisphere did not bear extensive ice sheets, but local glaciers were widespread at high altitudes.

Geographic entities mentioned:
surface_form: Tibetan Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
Just south of the equator, an ice cap of several hundred square kilometers was present on the east African mountains in the Kilimanjaro massif, Mount Kenya, and the Rwenzori Mountains, which still bear relic glaciers today. Southern Hemisphere. Glaciation of the Southern Hemisphere was less extensive.

Geographic entities mentioned:
surface_form: Mount Kenya
instance_of: Mountain
countries: Kenya
coordinates: lat: -0.1
lon: 37.2
Antarctica was entirely glaciated, much like today, but unlike today the ice sheet left no uncovered area. In mainland Australia only a very small area in the vicinity of Mount Kosciuszko was glaciated, whereas in Tasmania glaciation was more widespread. An ice sheet formed in New Zealand, covering all of the Southern Alps, where at least three glacial advances can be distinguished.

Geographic entities mentioned:
surface_form: Mount Kosciuszko
instance_of: Mountain
countries: Australia
coordinates: lat: -36.4558303
lon: 148.2635105
The main areas of Papua New Guinea where glaciers developed during the LGP were the Central Cordillera, the Owen Stanley Range, and the Saruwaged Range. Mount Giluwe in the Central Cordillera had a &quot;more or less continuous ice cap covering about 188 km2 and extending down to 3200-3500 m&quot;.

Geographic entities mentioned:
surface_form: Mount Giluwe
instance_of: Mountain
countries: Papua New Guinea
coordinates: lat: -6.0388888888889
lon: 143.88611111111
Mount Giluwe in the Central Cordillera had a &quot;more or less continuous ice cap covering about 188 km2 and extending down to 3200-3500 m&quot;. In Western New Guinea, remnants of these glaciers are still preserved atop Puncak Jaya and Ngga Pilimsit. Small glaciers developed in a few favorable places in Southern Africa during the last glacial period.

Geographic entities mentioned:
surface_form: Puncak Jaya
instance_of: Mountain
countries: Indonesia
coordinates: lat: -4.0833333333333
lon: 137.18333333333
surface_form: Ngga Pilimsit
instance_of: Mountain
countries: Indonesia
coordinates: lat: -4.03555556
lon: 137.05916667
It radically altered the geography of North America north of the Ohio River. At the height of the Wisconsin episode glaciation, ice covered most of Canada, the Upper Midwest, and New England, as well as parts of Montana and Washington. On Kelleys Island in Lake Erie or in New York's Central Park, the grooves left by these glaciers can be easily observed.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
In its retreat, the Wisconsin episode glaciation left terminal moraines that form Long Island, Block Island, Cape Cod, Nomans Land, Martha's Vineyard, Nantucket, Sable Island, and the Oak Ridges Moraine in south-central Ontario, Canada. In Wisconsin itself, it left the Kettle Moraine. The drumlins and eskers formed at its melting edge are landmarks of the lower Connecticut River Valley.

Geographic entities mentioned:
surface_form: Oak Ridges Moraine
instance_of: Mountain
countries: Canada
coordinates: lat: 44.05
lon: -78.86666667
Around of the total glaciated area was in the Sierra Nevada de Mérida, and of that amount, the largest concentration, was in the areas of Pico Bolívar, Pico Humboldt, and Pico Bonpland. Radiocarbon dating indicates that the moraines are older than 10,000 BP, and probably older than 13,000 BP. The lower moraine level probably corresponds to the main Wisconsin glacial advance.

Geographic entities mentioned:
surface_form: Pico Bolívar
instance_of: Mountain
countries: Venezuela
coordinates: lat: 8.540861111111111
lon: -71.0465
surface_form: Pico Humboldt
instance_of: Mountain
countries: Venezuela
coordinates: lat: 8.5496611111111
lon: -70.996141666667
surface_form: Pico Bonpland
instance_of: Mountain
countries: Venezuela
coordinates: lat: 8.5425
lon: -71.00316666666667
The upper level probably represents the last glacial advance (Late Wisconsin). Llanquihue glaciation (Southern Andes). The Llanquihue glaciation takes its name from Llanquihue Lake in southern Chile, which is a fan-shaped piedmont glacial lake. On the lake's western shores, large moraine systems occur, of which the innermost belong to the LGP.

Geographic entities mentioned:
surface_form: Llanquihue Lake
instance_of: Lake
countries: Chile
coordinates: lat: -41.133333333333
lon: -72.783333333333
General Thomas Hills. The General Thomas Hills are a mountain range in Esmeralda County, Nevada.

Geographic entities mentioned:
surface_form: general thomas hills
instance_of: Landform
countries: United States
coordinates: lat: 37.9616
lon: -117.405
In 937, the Dali Kingdom was founded by Duan Siping, a Bai man whose family had played a major role in the Nanzhao Kingdom, advocated for the &quot;relief of corvée&quot; () and joined 37 tribes in eastern Yunnan to instigate a rebellion. The Dali Kingdom persisted for about 300 years (937-1253), facilitating the Bai's establishment of internal cohesion centered around the Erhai Lake.

Geographic entities mentioned:
surface_form: Erhai Lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 25.763333333333
lon: 100.1875
Most Bai were subsistence rice farmers, but they also cultivated wheat, vegetables, and fruits. Unlike the Han and most other Chinese minority groups, the Bai ate cheese and made it from either cow or goat milk. The leftover whey from the process of cheese-making was fed to pigs. Those who lived around Erhai Lake fished. Bai fishermen have trained cormorants to fish since the 9th century.

Geographic entities mentioned:
surface_form: Erhai Lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 25.763333333333
lon: 100.1875
By mid-April 1992, Serb forces had effectively surrounded Konjic, setting up checkpoints at Bradina to the north, thus controlling the Mount Ivan saddle pass on the M17 road to Sarajevo and also blocking the highway to Mostar from the village of Donje Selo to the west.

Geographic entities mentioned:
surface_form: Mount Ivan
instance_of: Mountain
countries: Bosnia and Herzegovina
coordinates: lat: 43.79198
lon: 18.0092
While the name &quot;Chittenango&quot; is often thought by locals to mean &quot;river flowing north&quot; or &quot;where the waters divide and run north&quot;, a reference to the direction of water flow from the creek's point of origin to Oneida Lake, there is no derivation for these alternatives.

Geographic entities mentioned:
surface_form: Oneida Lake
instance_of: Lake
countries: United States
coordinates: lat: 43.2
lon: -75.9
Initial growth of the village is largely attributed to the construction of the Erie Canal, which officially opened in 1825, joining Buffalo on Lake Erie with Albany, the capital of New York, and the Hudson River. The Erie Canal passes just north of the village. The Chittenango Canal Company, incorporated in 1818, constructed a canal in length connecting Chittenango to the Erie Canal.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
State Routes 5 and 13 pass through the village center as Genesee Street. NY 5 leads east to Oneida and west to the center of Syracuse, while NY 13 follows NY 5 to the east as far as Canastota, then turns north toward Sylvan Beach on Oneida Lake. To the south, NY 13 leads to Cazenovia. NY 173 has its eastern terminus at Chittenango and leads southwest to Manlius. According to the U.S.

Geographic entities mentioned:
surface_form: Oneida Lake
instance_of: Lake
countries: United States
coordinates: lat: 43.2
lon: -75.9
Dammtorpssjön. Dammtorpssjön is a lake in Stockholm County, Södermanland, Sweden.

Geographic entities mentioned:
surface_form: dammtorpssjön
instance_of: Lake
countries: Sweden
coordinates: lat: 59.289
lon: 18.1475
Canal communities in Ontario. Conceived in the 1960s and built in the 1970s by Hungarian engineer Andrew Zsolt, Lagoon City on Lake Simcoe is the oldest and largest canal community in Ontario, Canada with 16 km of canals. Located in Brechin, Ontario, it is centered on the Trent–Severn Waterway with access to Lake Ontario.

Geographic entities mentioned:
surface_form: Lake Simcoe
instance_of: Lake
countries: Canada
coordinates: lat: 44.436666666667
lon: -79.339166666667
Conceived in the 1960s and built in the 1970s by Hungarian engineer Andrew Zsolt, Lagoon City on Lake Simcoe is the oldest and largest canal community in Ontario, Canada with 16 km of canals. Located in Brechin, Ontario, it is centered on the Trent–Severn Waterway with access to Lake Ontario. Further south, Young's Harbour is also situated on Lake Simcoe, in the Town of Georgina.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Since the highway followed a concession road, it was straight for almost its entire length, veering only at Browns Line (Highway 27), the Credit River, and at the Oakville border. At the time of construction, this route was surrounded by farmland, as most of the towns in the area at the time lay along Dundas or Lake Shore, to the north and south respectively.

Geographic entities mentioned:
surface_form: Credit River
instance_of: Watercourse
countries: Canada
coordinates: lat: 43.5478
lon: -79.5808
Taxonomy. It was first described by Alfred Jefferis Turner in 1917 from three specimens collected in November on Tamborine Mountain in Queensland, Australia. They were apparently all female. There are three syntypes, two are kept at Australian National Insect Collection, and one at the Natural History Museum, London, courtesy of Edward Meyrick.

Geographic entities mentioned:
surface_form: Tamborine Mountain
instance_of: Mountain
countries: Australia
coordinates: lat: -27.927513888889
lon: 153.19430555556
Ecology. The locality it was collected, Tamborine Mountain, has a cool subtropical highland climate, with the annual rainfall of about 1,550 mm. The imagoes (adult moths) are known to be active in November, based on when they were first collected, which is at the beginning of the warmer rainy season.

Geographic entities mentioned:
surface_form: Tamborine Mountain
instance_of: Mountain
countries: Australia
coordinates: lat: -27.927513888889
lon: 153.19430555556
Webers Peaks. Webers Peaks () is a line of peaks on a ridge bounded by Splettstoesser Glacier on the north, Balish Glacier on the east and Dobbratz and Fendorf Glaciers on the west, in the Heritage Range, Ellsworth Mountains. They were named by the University of Minnesota Ellsworth Mountains Party of 1962–63 for geologist Gerald F. Webers, a member of that party.

Geographic entities mentioned:
surface_form: webers peaks
instance_of: Mountain
coordinates: lat: -79.4667
lon: -84.6667
Aravansay. The Aravansay (,) is a river in Kyrgyzstan and Uzbekistan. Its source is in the Kichi-Alay range, part of the Alay Range, and it discharges into the Shahrixonsoy, one of the canals of the Fergana Valley. The river is long, and the watershed covers. In its upper course, it is called the &quot;Gezart&quot;, and in its middle course the &quot;Chilisay&quot;.

Geographic entities mentioned:
surface_form: Fergana Valley
instance_of: Valley
countries: Kyrgyzstan
Uzbekistan
Tajikistan
coordinates: lat: 40.900833333333
lon: 71.757777777778
Chontacollo. Chontacollo (possibly from Aymara &quot;chunta&quot; prolonged, lengthened, &quot;qullu&quot; mountain, &quot;prolonged mountain&quot;) is a mountain in the north of the Barroso mountain range in the Andes of Peru, about high. It is situated in the Tacna Region, Tarata Province, Tarata District. Chontacollo lies northwest of the mountain Iñuma.

Geographic entities mentioned:
surface_form: Iñuma
instance_of: Mountain
countries: Peru
coordinates: lat: -17.4606
lon: -69.8383
surface_form: iñuma
instance_of: Mountain
countries: Peru
coordinates: lat: -17.4606
lon: -69.8383
Chontacollo. Chontacollo (possibly from Aymara &quot;chunta&quot; prolonged, lengthened, &quot;qullu&quot; mountain, &quot;prolonged mountain&quot;) is a mountain in the north of the Barroso mountain range in the Andes of Peru, about high. It is situated in the Tacna Region, Tarata Province, Tarata District. Chontacollo lies northwest of the mountain Iñuma.

Geographic entities mentioned:
surface_form: chunta
instance_of: Mountain
countries: Peru
coordinates: lat: -11.4964
lon: -76.3772
surface_form: barroso
instance_of: Mountain
countries: Peru
coordinates: lat: -17.556308
lon: -69.5954717
surface_form: chunta
instance_of: Mountain
countries: Peru
coordinates: lat: -14.7836
lon: -72.5717
surface_form: chunta
instance_of: Mountain
countries: Peru
coordinates: lat: -14.4222
lon: -73.8572
surface_form: chontacollo
instance_of: Mountain
countries: Peru
coordinates: lat: -17.4361
lon: -69.8533
Chontacollo. Chontacollo (possibly from Aymara &quot;chunta&quot; prolonged, lengthened, &quot;qullu&quot; mountain, &quot;prolonged mountain&quot;) is a mountain in the north of the Barroso mountain range in the Andes of Peru, about high. It is situated in the Tacna Region, Tarata Province, Tarata District. Chontacollo lies northwest of the mountain Iñuma.

Geographic entities mentioned:
surface_form: chontacollo
instance_of: Mountain
countries: Peru
coordinates: lat: -17.4361
lon: -69.8533
In the early hours of 30 May, &quot;I-21&quot;s floatplane conducted a reconnaissance flight over Sydney Harbour that confirmed the concentration of Allied shipping sighted by &quot;I-29&quot;s floatplane was still present and remained a worthwhile target. On the night of 31 May, three midget submarines were launched from the Japanese force outside the Sydney Heads.

Geographic entities mentioned:
surface_form: Sydney Heads
instance_of: Landform
countries: Australia
coordinates: lat: -33.8368
lon: 151.281
Billmore Hollow. Billmore Hollow is a valley in Oregon County in the U.S. state of Missouri. Billmore Hollow is an amalgamation of the name of William &quot;Bill&quot; Moore, a pioneer citizen who settled in the area after the Civil War. Billmore post office and Billmore school were established in the area.

Geographic entities mentioned:
surface_form: billmore hollow
instance_of: Valley
countries: United States
coordinates: lat: 36.57833333
lon: -91.20222222
The Pointers. The Pointers is a pair of rocks off the northwest coast of Rugged Island, lying between Eddystone Rocks and Start Point, Livingston Island in the South Shetland Islands, Antarctica. The rocks were known to 19th century sealers who named them descriptively as a navigational mark and hazard near the entrance to New Plymouth harbour. Location.

Geographic entities mentioned:
surface_form: plymouth
instance_of: Mountain
coordinates: lat: -62.462222222222
lon: -59.81625
The rocks were known to 19th century sealers who named them descriptively as a navigational mark and hazard near the entrance to New Plymouth harbour. Location. The rocks are centred at which is west of Start Point, Livingston Island, north-northwest of Cape Sheffield and east-northeast of Eddystone Rocks (British mapping in 1968, Chilean in 1971, Argentine in 1980, and Bulgarian in 2009).

Geographic entities mentioned:
surface_form: sheffield
instance_of: Mountain
coordinates: lat: -80.166666666667
lon: -25.7
surface_form: eddystone rocks
instance_of: Mountain
coordinates: lat: -62.59858333
lon: -61.38655556
The Pointers. The Pointers is a pair of rocks off the northwest coast of Rugged Island, lying between Eddystone Rocks and Start Point, Livingston Island in the South Shetland Islands, Antarctica. The rocks were known to 19th century sealers who named them descriptively as a navigational mark and hazard near the entrance to New Plymouth harbour. Location.

Geographic entities mentioned:
surface_form: the pointers
instance_of: Mountain
coordinates: lat: -62.589194
lon: -61.320917
surface_form: pointers
instance_of: Mountain
coordinates: lat: -62.589194
lon: -61.320917
The Pointers. The Pointers is a pair of rocks off the northwest coast of Rugged Island, lying between Eddystone Rocks and Start Point, Livingston Island in the South Shetland Islands, Antarctica. The rocks were known to 19th century sealers who named them descriptively as a navigational mark and hazard near the entrance to New Plymouth harbour. Location.

Geographic entities mentioned:
surface_form: the pointers
instance_of: Mountain
coordinates: lat: -62.589194
lon: -61.320917
surface_form: pointers
instance_of: Mountain
coordinates: lat: -62.589194
lon: -61.320917
surface_form: eddystone rocks
instance_of: Mountain
coordinates: lat: -62.59858333
lon: -61.38655556
Battle on the Ice. The Battle on the Ice, also known as the Battle of Lake Peipus, took place on 5 April 1242. It was fought on the frozen Lake Peipus when the united forces of the Republic of Novgorod and Vladimir-Suzdal, led by Prince Alexander Nevsky, emerged victorious against the forces of the Livonian Order and Bishopric of Dorpat, led by Bishop Hermann of Dorpat.

Geographic entities mentioned:
surface_form: Lake Peipus
instance_of: Lake
countries: Estonia
Russia
Russian Empire
Soviet Union
coordinates: lat: 58.676666666667
lon: 27.491666666667
Alexander then continued into Estonian-German territory. In the spring of 1242, the Teutonic Knights defeated a detachment of the Novgorodian army about south of the fortress of Dorpat (now Tartu). As a result, Alexander set up a position at Lake Peipus, where the battle would take place on 5 April 1242. Accounts in primary sources.

Geographic entities mentioned:
surface_form: Lake Peipus
instance_of: Lake
countries: Estonia
Russia
Russian Empire
Soviet Union
coordinates: lat: 58.676666666667
lon: 27.491666666667
In 1958 and 1959, underwater investigations in the northern part of Lake Lämmi (which connects Lake Peipus with Lake Pikhva), where some Soviet researchers presumed the combat happened, failed to find any artefacts connected to the battle of 1242.

Geographic entities mentioned:
surface_form: Lake Lämmi
instance_of: Lake
countries: Estonia
Russia
Russian Empire
Soviet Union
coordinates: lat: 58.676666666667
lon: 27.491666666667
The Compagnie du chemin de fer du Congo (CFC) was given of land for every of line put into operation, as well as a strip wide along the railway. The CCCI and CFC lands were mostly grouped into the &quot;Bloc de la Busira-Momboyo&quot;, created in 1901, along the Busira and Momboyo rivers. This property of was exploited by the SAB.

Geographic entities mentioned:
surface_form: Busira
instance_of: Watercourse
countries: Democratic Republic of the Congo
coordinates: lat: -0.3497
lon: 20.7804
surface_form: Momboyo
instance_of: Watercourse
countries: Democratic Republic of the Congo
coordinates: lat: -0.34400000000000003
lon: 19.0093
Konowryggen. 6q2lw9l9gz5yighd7og6wdia8022" xml:space="preserve">Konowryggen is a mountain ridge in Oscar II Land at Spitsbergen, Svalbard. The ridge has a length of nine kilometers. On the eastern side is the glacier Konowbreen, and to the west is Gaffelbreen. The ridge is named after Wollert Konow.

Geographic entities mentioned:
surface_form: konowryggen
instance_of: Mountain
countries: Norway
coordinates: lat: 78.603
lon: 12.8569
Garden Peninsula. The Garden Peninsula is a peninsula of in length that extends southwestward into Lake Michigan from the mainland of Michigan's Upper Peninsula. The peninsula is bordered by Lake Michigan on the east, and by Big Bay de Noc on the west. The base of the peninsula is served by U.S. Highway 2, and the peninsula's west shore is reached by M-183.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Most of the peninsula is part of Delta County, although a small portion in the east is part of Schoolcraft County. Formation. The Garden Peninsula is part of the western sill of limestone bedrock of the Niagara Escarpment. The other surviving portion of the sill is now Wisconsin's Door Peninsula. Parts of the limestone sill between the Door and Garden peninsulas have been eroded away by glaciers.

Geographic entities mentioned:
surface_form: Niagara Escarpment
instance_of: Mountain
countries: Canada
coordinates: lat: 43.8334
lon: -79.99966
Fall Creek (New York). Fall Creek is a river located in Tompkins County, New York. It flows into Cayuga Lake by Ithaca, New York. Fall Creek makes its way through the campus of Cornell University in Ithaca, New York. Beebe Lake, Triphammer Falls, and Ithaca Falls are some of its notable features. It empties into Cayuga Lake at Stewart Park.

Geographic entities mentioned:
surface_form: Cayuga Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.68805555555556
lon: -76.70222222222222
Rotala andamanensis. &quot;Rotala andamanensis&quot; is a lesser-known endemic wetland plant species of the Andaman Islands in the Bay of Bengal belonging to the family Lythraceae. The type locality of this species is Wright Myo, the southern slope of the Mount Harriet Hill ranges. This is a rather rare species found to occur along the wetland area of the region.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Black Volcano. Black Volcano is an inactive volcano located near Albuquerque, New Mexico, and is part of the Albuquerque volcanic field. Black Volcano is located directly north of JA volcano. Black Volcano is the second of five volcanoes (traveling south to north) within the western boundary of Petroglyph National Monument. North of Black Volcano are Vulcan, Bond and Butte volcanoes.

Geographic entities mentioned:
surface_form: JA volcano
instance_of: Mountain
countries: United States
coordinates: lat: 35.1275
lon: -106.773
surface_form: black volcano
instance_of: Mountain
countries: United States
coordinates: lat: 56.5525
lon: -158.78472222222
surface_form: black volcano
instance_of: Mountain
countries: United States
coordinates: lat: 35.1325
lon: -106.773
Black Volcano is located directly north of JA volcano. Black Volcano is the second of five volcanoes (traveling south to north) within the western boundary of Petroglyph National Monument. North of Black Volcano are Vulcan, Bond and Butte volcanoes. JA, Black, and Vulcan Volcanoes are located along a single fissure through which the lava erupted.

Geographic entities mentioned:
surface_form: vulcan
instance_of: Mountain
countries: United States
coordinates: lat: 35.1414
lon: -106.772
surface_form: black volcano
instance_of: Mountain
countries: United States
coordinates: lat: 56.5525
lon: -158.78472222222
surface_form: black volcano
instance_of: Mountain
countries: United States
coordinates: lat: 35.1325
lon: -106.773
Black Volcano is the second of five volcanoes (traveling south to north) within the western boundary of Petroglyph National Monument. North of Black Volcano are Vulcan, Bond and Butte volcanoes. JA, Black, and Vulcan Volcanoes are located along a single fissure through which the lava erupted. The volcanoes are a rare example of a series of vents associated with a fissure eruption.

Geographic entities mentioned:
surface_form: vulcan
instance_of: Mountain
countries: United States
coordinates: lat: 35.1414
lon: -106.772
Black Volcano. Black Volcano is an inactive volcano located near Albuquerque, New Mexico, and is part of the Albuquerque volcanic field. Black Volcano is located directly north of JA volcano. Black Volcano is the second of five volcanoes (traveling south to north) within the western boundary of Petroglyph National Monument. North of Black Volcano are Vulcan, Bond and Butte volcanoes.

Geographic entities mentioned:
surface_form: black volcano
instance_of: Mountain
countries: United States
coordinates: lat: 56.5525
lon: -158.78472222222
surface_form: black volcano
instance_of: Mountain
countries: United States
coordinates: lat: 35.1325
lon: -106.773
Sahamaitso. Sahamaitso is a river in the region of Alaotra-Mangoro in eastern Madagascar. It is situated near the towns of Amboasary Gara, Tanifotsy and Ampangabe.

Geographic entities mentioned:
surface_form: mangoro
instance_of: Watercourse
countries: Madagascar
coordinates: lat: -20.004968
lon: 48.781672
surface_form: sahamaitso
instance_of: Watercourse
countries: Madagascar
coordinates: lat: -18.43538
lon: 48.24242
surface_form: alaotra
instance_of: Lake
countries: Madagascar
coordinates: lat: -17.5
lon: 48.5
Sahamaitso. Sahamaitso is a river in the region of Alaotra-Mangoro in eastern Madagascar. It is situated near the towns of Amboasary Gara, Tanifotsy and Ampangabe.

Geographic entities mentioned:
surface_form: sahamaitso
instance_of: Watercourse
countries: Madagascar
coordinates: lat: -18.43538
lon: 48.24242
Lake Manatee State Park. Lake Manatee State Park (Lake Manatee State Recreation Area) is a State Park in the U.S. state of Florida, located on the south shore of Lake Manatee. It is east of I-75 on State Road 64 in Bradenton. It is made up of pine flatwoods, Sand Pine scrub, marshes, and hardwood forests. Activities include canoeing and kayaking, camping, boating, picnicking, swimming.

Geographic entities mentioned:
surface_form: Lake Manatee
instance_of: Lake
countries: United States
coordinates: lat: 27.4836
lon: -82.3288
Phips gave the King's Troops the keys to the building, and after sunrise, they removed all of the gunpowder. Most of the regulars then returned to Boston the way they had come, but a small contingent marched to Cambridge, removed two field pieces, and took them to Boston by foot over the Great Bridge and up Boston Neck.

Geographic entities mentioned:
surface_form: Boston Neck
instance_of: Landform
countries: United States
coordinates: lat: 42.34394444
lon: -71.06597222
Also, some people living in the Codroy Valley, on the southwestern tip of Newfoundland, have ancestors who were francophone but represent Acadian settlers from Canada's Maritime Provinces. They arrived during the 19th century and have lost the French language as well. Indigenous. Most of the Indigenous influence within Newfoundland English has been assimilated and forgotten under colonialism.

Geographic entities mentioned:
surface_form: Codroy Valley
instance_of: Valley
countries: Canada
It is considered sacred by Hindus and its snow deposition pattern resembles the sacred 'Om' (ॐ). Near Om Parvat, Parvat Lake and &quot;Jonglingkong Lake&quot;. Jonglingkong Lake is sacred, as Lake Manasarovar, to the Hindus. Om Parvat yatra circuit. Om Parvat can be viewed on the route to the Kailash Manasarovar Yatra from the last camp (Nabhidhang Pass west of KMVN Huts) enroute Lipulekh Pass.

Geographic entities mentioned:
surface_form: Lake Manasarovar
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 30.666666666667
lon: 81.5
It has always been the sacred mountain for Hindus among all over the world. Many trekkers to Adi Kailash in Kuthi Valley often make a diversion at Gunji to view Om Parvat. Om Parvat is located east of Nabhi Dhang camp on Mount Kailash-Lake Manasarovar yatra route. Mount Kailash could be viewed from the Limpiyadhura Pass as well as the Old Lipulekh Pass (couple of kilometer west of Lipulekh Pass).

Geographic entities mentioned:
surface_form: Mount Kailash
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 31.066944444444
lon: 81.312777777778
surface_form: Lake Manasarovar
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 30.666666666667
lon: 81.5
The base camp of Adi Kailash is 17 km from the Kuthi (Kuti) village in Kuthi Valley at sacred Jolingkong Lake which has a Hindu Shiva temple on its bank. The Adi Kailash Yatra Circuit begins by going up the Darma Valley and then going to Kuthi Yankti Valley via the Sin La pass to join the Mount Kailash-Lake Manasarovar Tibetan pilgrimage route down the Sharda River.

Geographic entities mentioned:
surface_form: Darma Valley
instance_of: Valley
countries: India
surface_form: Kuthi Yankti Valley
instance_of: Valley
countries: India
coordinates: lat: 30.3064016
lon: 80.7557186
surface_form: Mount Kailash
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 31.066944444444
lon: 81.312777777778
surface_form: Lake Manasarovar
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 30.666666666667
lon: 81.5
Where as Nepal, claim it in Darchula District, Nepal. It has always been the sacred mountain for Hindus among all over the world. Many trekkers to Adi Kailash in Kuthi Valley often make a diversion at Gunji to view Om Parvat. Om Parvat is located east of Nabhi Dhang camp on Mount Kailash-Lake Manasarovar yatra route.

Geographic entities mentioned:
surface_form: kuthi valley
instance_of: Valley
countries: India
coordinates: lat: 30.3064016
lon: 80.7557186
surface_form: om parvat
instance_of: Mountain
countries: India
coordinates: lat: 30.1988
lon: 81.0347
surface_form: om parvat
instance_of: Mountain
countries: India
coordinates: lat: 30.1988
lon: 81.0347