Sarmila/GeoWiki-Features huggingface dataset:
SR-92 then bends to the south (with a short bend that extends briefly into Wasatch County) to connect with the west end of the Cascade Scenic Byway (Forest Road 114). After passing the east side of Mount Timpanogos and then the Sundance Resort, the road links up with US-189 in Provo Canyon at Wildwood, just west of the Utah-Wasatch county line and east of the Provo Canyon Tunnels.

Geographic entities mentioned:
surface_form: Mount Timpanogos
instance_of: Mountain
countries: United States
coordinates: lat: 40.390836111111
lon: -111.64594444444
History. The Jiu Valley miners left again for Bucharest, unhappy with the government's reduction of subsidies, which would result in the closing of the mines.Together with the miners who left for Bucharest, there were also members of PUNR, PRM, PDSR and PS.

Geographic entities mentioned:
surface_form: Jiu Valley
instance_of: Valley
countries: Romania
coordinates: lat: 43.77805556
lon: 23.81333333
Marcello Rodriguez Pons has represented Argentina eight times in Sailing World Championships in different classes of windsurfing and sailing boats; he was among the World Top 10 on four occasions: Buenos Aires 1990, Puerto Sherry 2006, Puerto de Santa Maria 2009 and Mar Chiquita 2014.

Geographic entities mentioned:
surface_form: Mar Chiquita
instance_of: Lake
countries: Argentina
coordinates: lat: -37.6247
lon: -57.3044
Bruce Peninsula National Park. Bruce Peninsula National Park is a national park on the Bruce Peninsula in Ontario, Canada. Located on a part of the Niagara Escarpment, the park comprises 156 square kilometres and is one of the largest protected areas in southern Ontario, forming the core of UNESCO's Niagara Escarpment World Biosphere Reserve.

Geographic entities mentioned:
surface_form: Niagara Escarpment
instance_of: Mountain
countries: Canada
coordinates: lat: 43.8334
lon: -79.99966
The station was launched in the mid-1990s. Geology. The Niagara Escarpment runs from near Rochester, New York, to Tobermory, then on to Manitoulin, St. Joseph Island and other islands located in northern Lake Huron where it turns westwards into the Upper Peninsula of northern Michigan, south of Sault Ste. Marie.

Geographic entities mentioned:
surface_form: Niagara Escarpment
instance_of: Mountain
countries: Canada
coordinates: lat: 43.8334
lon: -79.99966
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
Marie. The escarpment then extends southwards into Wisconsin following the Door Peninsula and then more inland from the western coast of Lake Michigan and Milwaukee ending northwest of Chicago near the Wisconsin-Illinois border. It forms the backbone of the Bruce Peninsula and shapes the northern boundary of most of the park and provides the park with some of its most spectacular scenery.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Climate. The park has a typical climate for lakeside Northern Ontario, though the surrounding bodies of Lake Huron moderate the temperates. The park has a humid continental climate (&quot;Dfb&quot;), with warm to hot summers and cool winters. In the coastal northern parts of the peninsula, the climate is among the most temperate in Ontario.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
In the coastal northern parts of the peninsula, the climate is among the most temperate in Ontario. The climate of the park is influenced by both Georgian Bay and Lake Huron, which significantly moderate temperatures. As a result, they tend to prolong milder temperatures in the fall and cooler temperatures in spring.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
Punta del Pollo. Punta del Pollo is a mountain of Catalonia, Spain. It has an elevation of 693 metres above sea level.

Geographic entities mentioned:
surface_form: punta del pollo
instance_of: Mountain
countries: Spain
coordinates: lat: 40.92588889
lon: 0.60884444
Middletown, Staten Island. Middletown was a town in Richmond County, New York. It was incorporated in 1860 from parts of Southfield and Castleton. At the time, it included the most populous part of the village of Edgewater and the hilly ridges of the interior, Grymes Hill and Todt Hill among others. It was dissolved in 1898 upon consolidation into the City of New York.

Geographic entities mentioned:
surface_form: Todt Hill
instance_of: Mountain
countries: United States
coordinates: lat: 40.602222222222
lon: -74.112222222222
He was born in New Jersey, the son of Thomas Millidge, a United Empire Loyalist who served with the New Jersey Volunteers, and Mercy Berker. Millidge came to Nova Scotia with his parents in 1783. He moved to a location on the Kennebecasis River in New Brunswick where he established himself as a shipbuilder. A community known as Millidgeville, which later became part of Saint John, developed there.

Geographic entities mentioned:
surface_form: Kennebecasis River
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.31666667
lon: -66.13333333
Bad Freienwalde. Bad Freienwalde () is a spa town in the Märkisch-Oderland district in Brandenburg, in north-eastern Germany. Geography. The town is situated on the Alte Oder, an old branch of the Oder River at the northwestern rim of the Oderbruch basin and the steep rise of the Barnim Plateau. It is located east of Eberswalde, and northeast of Berlin, near the border with Poland.

Geographic entities mentioned:
surface_form: Barnim Plateau
instance_of: Plateau
countries: Germany
coordinates: lat: 52.6667
lon: 14.25
2nd Burma Brigade, which had marched independently along a poor bullock-track to the west, covering in 14 days, made contact with the Chin Hills Battalion near Kalemyo on 12 May and was evacuated to Tamu by motor transport supplied by IV Corps. 17th Indian Division marched up the Kabaw Valley through the rains and reached Tamu on 17 May. The final rearguard, 63rd Indian Bde, marched in on 19 May.

Geographic entities mentioned:
surface_form: Kabaw Valley
instance_of: Valley
countries: Myanmar
coordinates: lat: 24.333333333333
lon: 94.416666666667
Pasimoni River. The Pasimoni River () is a river in the state of Amazonas, Venezuela. It is a tributary of the Casiquiare canal, in turn a tributary of the Rio Negro. The Pasimoni forms on the northern slope of the Cerro de la Neblina and flows northward to Casiquiare canal. It surrounded by low, poorly drained country.

Geographic entities mentioned:
surface_form: Cerro de la Neblina
instance_of: Mountain
countries: Brazil
Venezuela
coordinates: lat: 0.88638889
lon: -65.98944444
surface_form: pasimoni
instance_of: Watercourse
countries: Venezuela
coordinates: lat: 1.917097
lon: -66.599434
Pasimoni River. The Pasimoni River () is a river in the state of Amazonas, Venezuela. It is a tributary of the Casiquiare canal, in turn a tributary of the Rio Negro. The Pasimoni forms on the northern slope of the Cerro de la Neblina and flows northward to Casiquiare canal. It surrounded by low, poorly drained country.

Geographic entities mentioned:
surface_form: pasimoni river
instance_of: Watercourse
countries: Venezuela
coordinates: lat: 1.917097
lon: -66.599434
Nickajack Creek. Nickajack Creek is a stream in Cobb and Fulton counties in the U.S. state of Georgia. It is a tributary to the Chattahoochee River. Groundwater serves as the water source, with the creek beginning in Marietta, Georgia. The creek runs through the city of Smyrna and terminates at the Chattahoochee River in the town of Mableton. History and notable landmarks.

Geographic entities mentioned:
surface_form: Chattahoochee River
instance_of: Watercourse
countries: United States
coordinates: lat: 30.7088028
lon: -84.8638097
It contained high busts of the presidents of the United States from George Washington to George W. Bush. The statues were sculpted by Houston artist David Adickes, who was inspired as he drove past Mount Rushmore when returning from a trip to Canada. The park was opened in March 2004 by local visitor attraction entrepreneur Everette H.

Geographic entities mentioned:
surface_form: Mount Rushmore
instance_of: Mountain
countries: United States
coordinates: lat: 43.878947222222
lon: -103.459825
Walhallow shares a boundary to the north with Mallapunyah Station, to the south and east with Cresswell Downs, and to the south and west with Anthony Lagoon. Description. Occupying an area of of open plains, mitchell grass downs, coolabah woodland and spinifex desert situated on the Barkly Tableland. The station has a carrying capacity of 50,000 head of Brahman cattle.

Geographic entities mentioned:
surface_form: Barkly Tableland
instance_of: Plateau
countries: Australia
coordinates: lat: -19
lon: 138
The station has a carrying capacity of 50,000 head of Brahman cattle. The neighbouring property to the south is Anthony Lagoon. History. The first Europeans to explore the area, which was Kotandji land, were Ernest Favenc and Nathaniel Buchanan who conducted expeditions around the Barkly Tableland area in 1878. The property was first settled by John Bassett and William Christian in 1881.

Geographic entities mentioned:
surface_form: Barkly Tableland
instance_of: Plateau
countries: Australia
coordinates: lat: -19
lon: 138
Camp 15 Peak. Camp 15 Peak is a mountain in the borough of Juneau, Alaska, United States. It is part of the Boundary Ranges of the Coast Mountains in western North America. On the divide east of Battle Glacier, it is located 3 miles southwest of The Tusk and 28 miles north-northwest of the city of Juneau.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: camp 15 peak
instance_of: Mountain
countries: United States
coordinates: lat: 58.6933
lon: -134.563
It is part of the Boundary Ranges of the Coast Mountains in western North America. On the divide east of Battle Glacier, it is located 3 miles southwest of The Tusk and 28 miles north-northwest of the city of Juneau. The Juneau Icefield Research Program (JIRP) included Camp 15 Peak in its 2001 survey of conditions throughout parts of the Juneau Icefield.

Geographic entities mentioned:
surface_form: battle
instance_of: Watercourse
countries: United States
coordinates: lat: 44.9266
lon: -93.0291
Camp 15 Peak. Camp 15 Peak is a mountain in the borough of Juneau, Alaska, United States. It is part of the Boundary Ranges of the Coast Mountains in western North America. On the divide east of Battle Glacier, it is located 3 miles southwest of The Tusk and 28 miles north-northwest of the city of Juneau.

Geographic entities mentioned:
surface_form: camp 15 peak
instance_of: Mountain
countries: United States
coordinates: lat: 58.6933
lon: -134.563
It is part of the Boundary Ranges of the Coast Mountains in western North America. On the divide east of Battle Glacier, it is located 3 miles southwest of The Tusk and 28 miles north-northwest of the city of Juneau. The Juneau Icefield Research Program (JIRP) included Camp 15 Peak in its 2001 survey of conditions throughout parts of the Juneau Icefield.

Geographic entities mentioned:
surface_form: camp 15 peak
instance_of: Mountain
countries: United States
coordinates: lat: 58.6933
lon: -134.563
Administration. The Presidency was divided into four Commisserates and twenty-four districts with Bombay city as the capital. The four divisions were Sind, the northern or Gujarat, the central or Deccan and the southern or Carnatic. The government of Bombay was administered by a Governor-in-Council, consisting of the Governor as president and two ordinary members.

Geographic entities mentioned:
surface_form: Deccan
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
Young people who were about to get married would go and ask for his blessing. At the Chapel Island Mission boats would stop if he was crossing.&quot;
Traditionally, the Grand Council met on a small island, &quot;Mniku&quot;, on the Bras d'Or Lake in Cape Breton. In the early 21st century, this site is now within the reserve known as Chapel Island or &quot;Potlotek&quot;.

Geographic entities mentioned:
surface_form: Bras d'Or Lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.860277777778
lon: -60.778888888889
The Halifax Treaties (1760–1761), marked the end of warfare between the Mi'kmaq and the British. The 1752 Peace and Friendship Treaty Between His Majesty the King and Jean-Baptiste Cope, on behalf of the Shubenacadie Mi'kmaq has been cited in the Supreme Court of Canada's 1985 decision in &quot;R v Simon&quot;.

Geographic entities mentioned:
surface_form: Shubenacadie
instance_of: Valley
countries: Canada
coordinates: lat: 45.0864
lon: -63.408
The people attempt to survive the flood by traveling in bark canoes, but only a single old man and woman survive to populate the earth. Spiritual sites. One spiritual capital of the Mi'kmaq Nation is Mniku, Unama'ki, the gathering place of the Mi'kmaq Grand Council or Sante' Mawio'mi, Chapel Island in Bras d'Or Lake of Nova Scotia. The island is also the site of the St.

Geographic entities mentioned:
surface_form: Bras d'Or Lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.860277777778
lon: -60.778888888889
Then the numbers grew slightly again, before becoming apparently stable during the 19th century. During the 20th century, the population was on the rise again. The average growth from 1965 to 1970 was about 2.5%. Commemorations. The Mi'kmaq people have been commemorated in numerous ways, including HMCS Mi'kmaq (R10), and place names such as Lake Mi'kmaq, and the Mic Mac Mall.

Geographic entities mentioned:
surface_form: Lake Mi'kmaq
instance_of: Lake
countries: Canada
coordinates: lat: 44.6932
lon: -63.5534
Lake Ospedaletto. Lake Ospedaletto (in Friulian &quot;Lât di Ospedalét&quot;), also known as Lake Minisini, is a small prealpine water body of periglacial origin located near the hamlet of in the municipality of Gemona del Friuli, Province of Udine, in Friuli-Venezia Giulia, Italy. Etymology. The lake takes its name from the nearby settlement of Ospedaletto.

Geographic entities mentioned:
surface_form: lake ospedaletto
instance_of: Lake
countries: Italy
coordinates: lat: 46.297789
lon: 13.124285
The importance of the biotope is recognized and protected at the European level as a special area of conservation (Natura 2000 Site IT3320013 Lago Minisini and Rivoli Bianchi). The Lake Ospedaletto is included in the list of geosites of the Friuli-Venezia Giulia region as it &quot;represents one of the last examples of a periglacial lake in Friuli&quot;. History and economy.

Geographic entities mentioned:
surface_form: lago minisini
instance_of: Lake
countries: Italy
coordinates: lat: 46.297789
lon: 13.124285
Desert Spring, California. Desert Spring is a former settlement in Kern County, California in the Fremont Valley, south of Red Rock Canyon State Park. It was located northeast of Cantil. The place, with natural springs, was important as a source of freshwater to the Native Americans, explorers, prospectors, and others in the Mojave Desert. Visitors included Joseph R. Walker in 1834, John C.

Geographic entities mentioned:
surface_form: Fremont Valley
instance_of: Valley
countries: United States
coordinates: lat: 35.1083
lon: -118.047
There is no firm evidence that members of King Leopold expedition actually reached the lake. Lago Leopoldo was first seen from the air as a landmark near the Cerro Autana tepui during the 1950s. The lake was first visited by helicopter in March 1973 by the Spanish naturalist Félix Rodríguez de la Fuente.

Geographic entities mentioned:
surface_form: Cerro Autana
instance_of: Mountain
Landform
countries: Venezuela
coordinates: lat: 4.855029
lon: -67.449737
surface_form: lago leopoldo
instance_of: Lake
countries: Venezuela
coordinates: lat: 4.9657
lon: -67.4855
surface_form: autana
instance_of: Mountain
Landform
countries: Venezuela
coordinates: lat: 4.855029
lon: -67.449737
The lake is likely the result of the collapse of sandstones in a process similar to the formation of the caves of Cerro Autana. The bottom of the lake is composed mostly of sand and small quantities of mud. Sand composition is largely quartz arenite and a small percentage of monomineralic components dominated by quartz and some accessory minerals (zircon, feldspar, hematite, and rutile).

Geographic entities mentioned:
surface_form: Cerro Autana
instance_of: Mountain
Landform
countries: Venezuela
coordinates: lat: 4.855029
lon: -67.449737
surface_form: autana
instance_of: Mountain
Landform
countries: Venezuela
coordinates: lat: 4.855029
lon: -67.449737
surface_form: cerro autana
instance_of: Mountain
Landform
countries: Venezuela
coordinates: lat: 4.855029
lon: -67.449737
Lake Leopoldo. Lago Leopoldo (Lake Leopold) is a body of water located in the Venezuelan Amazon in the westernmost range of the Guiana Shield. It measures about by and and up to deep. The water level was documented at above sea level but may have diminished in recent years.

Geographic entities mentioned:
surface_form: lago leopoldo
instance_of: Lake
countries: Venezuela
coordinates: lat: 4.9657
lon: -67.4855
The following April, the terrestrial route from the original King Leopold III camp was established by a Venezuelan expedition which reached the shores of the lake on April 18, 1973. Lago Leopoldo figures prominently in the oral history and lore of the native Piaroans where it is referred as &quot;Paraka-Wachoe&quot; or the lake in the mountains.

Geographic entities mentioned:
surface_form: lago leopoldo
instance_of: Lake
countries: Venezuela
coordinates: lat: 4.9657
lon: -67.4855
surface_form: lago leopoldo
instance_of: Lake
countries: Venezuela
coordinates: lat: 4.9657
lon: -67.4855
Lake Leopoldo. Lago Leopoldo (Lake Leopold) is a body of water located in the Venezuelan Amazon in the westernmost range of the Guiana Shield. It measures about by and and up to deep. The water level was documented at above sea level but may have diminished in recent years.

Geographic entities mentioned:
surface_form: lake leopoldo
instance_of: Lake
countries: Venezuela
coordinates: lat: 4.9657
lon: -67.4855
In March 1973, the Spanish naturalist Félix Rodríguez de la Fuente reached the surface of the lake by helicopter and obtained film footage. The first expedition that established the terrestrial route to Lake Leopoldo started in the Rio Sipapo and travelled up the Sipapo, Autana and Umaj-Aje rivers. A camp was established in the same site of King Leopold's camp 20 years earlier.

Geographic entities mentioned:
surface_form: lake leopoldo
instance_of: Lake
countries: Venezuela
coordinates: lat: 4.9657
lon: -67.4855
surface_form: autana
instance_of: Mountain
Landform
countries: Venezuela
coordinates: lat: 4.855029
lon: -67.449737
Berrizbeitia, three times 1990–1996) and possibly others. The land route to Lake Leopoldo has been established using a base camp at the Elata rapid and a second camp at the base of the mountain that harbors the lake. There are no Piaroan dwellings in the area and the Indians seldom visit the area for which there are no trails other than animal paths that follow the edge of the rivers. Mythology.

Geographic entities mentioned:
surface_form: lake leopoldo
instance_of: Lake
countries: Venezuela
coordinates: lat: 4.9657
lon: -67.4855
Mythology. Lake Leopoldo lies in the same area of Cerro Autana which has a distinct role in the ancestral and creation myths of the Piaroa Indians. Nonetheless, specific references to Lake Leopoldo in Piaroan mythology are rare. The lake is known to them as &quot;Paraka-Wachoe&quot; or the lake in the mountain.

Geographic entities mentioned:
surface_form: lake leopoldo
instance_of: Lake
countries: Venezuela
coordinates: lat: 4.9657
lon: -67.4855
The water level was documented at above sea level but may have diminished in recent years. Its name derives from the expedition that King Leopold III of Belgium made in 1952 which motored up the Sipapo, Autana and Umaj-Ajé rivers and set camp several miles from the lake. There is no firm evidence that members of King Leopold expedition actually reached the lake.

Geographic entities mentioned:
surface_form: autana
instance_of: Mountain
Landform
countries: Venezuela
coordinates: lat: 4.855029
lon: -67.449737
Lago Leopoldo figures prominently in the oral history and lore of the native Piaroans where it is referred as &quot;Paraka-Wachoe&quot; or the lake in the mountains. Lago Leopoldo now renamed Lago Autana has been included as a natural monument within a protected area which includes the Cerro Autana and adjacent lands. Description.

Geographic entities mentioned:
surface_form: autana
instance_of: Mountain
Landform
countries: Venezuela
coordinates: lat: 4.855029
lon: -67.449737
surface_form: autana
instance_of: Mountain
Landform
countries: Venezuela
coordinates: lat: 4.855029
lon: -67.449737
surface_form: cerro autana
instance_of: Mountain
Landform
countries: Venezuela
coordinates: lat: 4.855029
lon: -67.449737
Description. Lago Leopoldo is located in the westernmost section of the Cuao-Sipapo Massif which constitutes the western edge of the Guiana Shield, east of the Sipapo and Orinoco Rivers. It lies between the hydrological basins of the rivers Cuao to the north and Autana to the south.

Geographic entities mentioned:
surface_form: autana
instance_of: Mountain
Landform
countries: Venezuela
coordinates: lat: 4.855029
lon: -67.449737
Its water collects from rain accumulation; drainage is by a subterranean stream which emerges at a distance from the lake's edge in the south. This stream drains into an affluent of the Umaj-Ajé River which drains into the Autana. The edge consists of nutrient-poor sandy soils originating from the erosion of the surrounding sandstone.

Geographic entities mentioned:
surface_form: autana
instance_of: Mountain
Landform
countries: Venezuela
coordinates: lat: 4.855029
lon: -67.449737
There are no Piaroan dwellings in the area and the Indians seldom visit the area for which there are no trails other than animal paths that follow the edge of the rivers. Mythology. Lake Leopoldo lies in the same area of Cerro Autana which has a distinct role in the ancestral and creation myths of the Piaroa Indians. Nonetheless, specific references to Lake Leopoldo in Piaroan mythology are rare.

Geographic entities mentioned:
surface_form: autana
instance_of: Mountain
Landform
countries: Venezuela
coordinates: lat: 4.855029
lon: -67.449737
surface_form: cerro autana
instance_of: Mountain
Landform
countries: Venezuela
coordinates: lat: 4.855029
lon: -67.449737
Haplochromis argens. &quot;Haplochromis argens&quot; is a species of haplochromine cichlid endemic to Lake Victoria where it is only known from the Tanzanian portion. This species reaches a length of SL. It feeds on zooplankton, primarily copepods and cladocerans, reflecting its dietary specialization as a zooplanktivore.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
Fort Kaministiquia. Fort Kaministiquia (former spellings include Fort Camanistigoyan, Fort Kanastigoya, Fort Kamanastigoya and others), was a French fort in North America. It was located on the north shore of Lake Superior at the mouth of the Kaministiquia River, in modern-day Thunder Bay, Ontario, Canada.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
Details of the route can be found under Kaministiquia River. In 1685 Daniel Greysolon, Sieur du Lhut built a post nearby. In 1688 Jacques de Noyon went from Kaministiquia as far as Rainy Lake. In 1696 the post was abandoned along with many western posts when the system of fur trade permits (congés) was abolished due to a surplus of beaver.

Geographic entities mentioned:
surface_form: Rainy Lake
instance_of: Lake
countries: Canada
United States
coordinates: lat: 48.636944444444
lon: -93.031388888889
From 1919 it was one of the &quot;postes du nord&quot; which included a post on the Nipigon River and one at Michipicoten. La Vérendrye took over the postes du nord in 1728 and in 1731–1743 he pushed trade and exploration west beyond Lake Winnipeg, mainly via Grand Portage using Kaministiquia as a base. It was abandoned in 1758 or 1760 with the fall of New France.

Geographic entities mentioned:
surface_form: Lake Winnipeg
instance_of: Lake
countries: Canada
coordinates: lat: 52.116666666667
lon: -97.25
Kliment Ohridski base during the 1998/99 and subsequent seasons. Location. The ridge is located at, which is 10.24 km south by east of Mount Wilbye, 8.7 km southwest of Mount Kliment Ohridski in Sofia University Mountains, 8.77 km west of Rachenitsa Nunatak, 2.7 km north by west of Moriseni Peak and 9.5 km east by north of Faulkner Nunatak. British mapping in 1971.

Geographic entities mentioned:
surface_form: Mount Wilbye
instance_of: Mountain
coordinates: lat: -69.5
lon: -71.5333
surface_form: Mount Kliment Ohridski
instance_of: Mountain
coordinates: lat: -69.517777777778
lon: -71.391666666667
surface_form: Moriseni Peak
instance_of: Mountain
coordinates: lat: -69.609166666667
lon: -71.470833333333
surface_form: Faulkner Nunatak
instance_of: Mountain
coordinates: lat: -69.6
lon: -71.7
Northern Ireland. At the time of partition, English had become the first language of the vast majority in Northern Ireland. It had small elderly Irish-speaking populations in the Sperrin Mountains as well as in the northern Glens of Antrim and Rathlin Island. There were also pockets of Irish speakers in the southernmost part of County Armagh.

Geographic entities mentioned:
surface_form: Glens of Antrim
instance_of: Valley
countries: United Kingdom
coordinates: lat: 55.16
lon: -6.1
It is North America’s only Tilt Coaster. The ride will be Cedar Point's third roller coaster installation in as many years, after Wild Mouse (2023) and Top Thrill 2 (2024). Siren's Curse's theme is tied to the park's presence on Lake Erie and the old Lake Erie Shipping Co, making reference to Greek mythology, where &quot;sirens&quot; were female beings who sent sailors to their demise via songs.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Riders must be at least tall to ride. The ride's trains feature an integrated audio and lighting system to tie into the theme of &quot;sirens&quot; on Lake Erie. For safety, riders can not bring loose items onto the ride, and metal detectors are installed at the beginning of the queue. Track. The steel tubular track is long and the lift is approximately high.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Ibi-Sekigahara-Yōrō Quasi-National Park. is a Quasi-National Park in southwest Gifu Prefecture, Japan. The park was established in 1970. Attractions. , Ibi River, Mount Ikeda, Mount Yōrō, Sekigahara Battlefield, Tōkai Nature Trail, Yōrō Falls
Related municipalities. Ibigawa, Ikeda, Kaizu, Motosu, Ōgaki, Sekigahara, Tarui, Yōrō

Geographic entities mentioned:
surface_form: Mount Ikeda
instance_of: Mountain
countries: Japan
coordinates: lat: 35.441111111111
lon: 136.51694444444
surface_form: Mount Yōrō
instance_of: Mountain
countries: Japan
coordinates: lat: 35.263055555556
lon: 136.52333333333
Elevations. The Podolian Upland (270–370 meters above sea-level) occupies the central area of the Khmelnytskyi Oblast. The northwestern areas of the oblast are part of the Volyn highland (highest point — 329 m above sea-level), while to the north, the oblast claims a part of the historic region of Polissia (highest point — 200–250 m above sea-level).

Geographic entities mentioned:
surface_form: Podolian Upland
instance_of: Plateau
countries: Ukraine
Moldova
coordinates: lat: 49.0275
lon: 27.85619444
From these bases, French fur traders planned to move eastward to incorporate regional tribes, especially the Creek, into their business enterprise. In 1718, they built Fort Toulouse at the forks of the Coosa and Tallapoosa rivers, in the heart of Creek country. This settlement, designed to take business from Carolina traders, was close to the Creek capital of Coweta.

Geographic entities mentioned:
surface_form: Coosa
instance_of: Watercourse
countries: United States
coordinates: lat: 32.4862464
lon: -86.2777475
Tsing Yi Tong. Tsing Yi Lagoon, or Tsing Yi Tong, was a lagoon on the east shore of Tsing Yi Island in Hong Kong. Its water came from a stream in the nearby valley of Liu To and its outlet was at Tsing Yi Bay. It acted as the shelter for nearby boat people, especially after large-scale land reclamation in Tsuen Wan and Kwai Chung. Once their boats moved into the lagoon, they never moved out.

Geographic entities mentioned:
surface_form: Liu To
instance_of: Valley
countries: People's Republic of China
coordinates: lat: 22.3528
lon: 114.097
Provenance and early life. Aldo Garòsci was born at Meana di Susa, a small mountain town overlooking the Susa Valley, roughly equidistant between Turin, to the east, and the mountain pass across into Savoy, to the west. Aldo was his father's third son. Antonio Garosci (1861-1941) was not originally from Piedmont. He had been born in San Remo down by the coast.

Geographic entities mentioned:
surface_form: Susa Valley
instance_of: Valley
countries: Italy
coordinates: lat: 45.133333333333
lon: 7.05
Baldwin Lake (Anoka County, Minnesota). Baldwin Lake is a lake on the Mississippi River in Anoka County, Minnesota.

Geographic entities mentioned:
surface_form: baldwin lake
instance_of: Lake
countries: United States
coordinates: lat: 34.1419
lon: -118.054
surface_form: baldwin lake
instance_of: Lake
countries: United States
coordinates: lat: 42.628836
lon: -83.401901
surface_form: baldwin lake
instance_of: Lake
countries: United States
coordinates: lat: 34.274444444444
lon: -116.81027777778
surface_form: baldwin lake
instance_of: Lake
countries: United States
coordinates: lat: 38.21
lon: -89.8767
surface_form: baldwin lake (anoka county, minnesota)
instance_of: Lake
countries: United States
coordinates: lat: 45.138611111111
lon: -93.135555555556
Baldwin Lake (Anoka County, Minnesota). Baldwin Lake is a lake on the Mississippi River in Anoka County, Minnesota.

Geographic entities mentioned:
surface_form: baldwin lake
instance_of: Lake
countries: United States
coordinates: lat: 34.1419
lon: -118.054
surface_form: baldwin lake
instance_of: Lake
countries: United States
coordinates: lat: 42.628836
lon: -83.401901
surface_form: baldwin lake
instance_of: Lake
countries: United States
coordinates: lat: 34.274444444444
lon: -116.81027777778
surface_form: baldwin lake
instance_of: Lake
countries: United States
coordinates: lat: 38.21
lon: -89.8767
surface_form: baldwin lake
instance_of: Lake
countries: United States
coordinates: lat: 45.138611111111
lon: -93.135555555556
Rio Grande Pyramid. Rio Grande Pyramid, elevation 13,827 feet, is a summit in the San Juan Mountains of southwest Colorado. The peak is in the Weminuche Wilderness of the San Juan National Forest northeast of Durango.

Geographic entities mentioned:
surface_form: pyramid
instance_of: Lake
countries: United States
coordinates: lat: 40.033333333333
lon: -119.56666666667
surface_form: rio grande pyramid
instance_of: Mountain
countries: United States
coordinates: lat: 37.679722222222
lon: -107.3925
Distance from Kachua to the district town is 16 km. Geography. Kachua is located at. It has 23,201 households and a total area of 131.62 km2. The Upazila is bordered by Chitalmari Upazila to the north, Nazirpur and Pirojpur Sadar Upazilas to the east, Bagerhat Sadar Upazila to the west and Morrelganj Upazila to the south. The main rivers are Baleshwar, Bhairab and Bishkhali. Demographics.

Geographic entities mentioned:
surface_form: Bhairab
instance_of: Watercourse
countries: Bangladesh
coordinates: lat: 22.85
lon: 89.56666667
KV49. Tomb KV49, located in the Valley of the Kings, in Egypt is a typical Eighteenth Dynasty corridor tomb. It was the first of a series of tombs discovered in 1906 by Edward R. Ayrton in the course of his excavations on behalf of Theodore M. Davis. The tomb was abandoned before it was completed, and the work was halted as the stairwell in the single chamber was being cut.

Geographic entities mentioned:
surface_form: Valley of the Kings
instance_of: Valley
countries: Egypt
coordinates: lat: 25.74025
lon: 32.602358
The Andean Plateau increases altitude sharply to the east, in the provinces of Otuzco and Santiago de Chuco. These two provinces comprise the Pacific hydrographic watershed, which give rise to the Moche and Virú rivers, to the south, and Chicama River to the north. Pacasmayo Province, located more to the north, is along the coast.

Geographic entities mentioned:
surface_form: Moche
instance_of: Watercourse
countries: Peru
coordinates: lat: -8.1611111111111
lon: -79.036388888889
Tramway. Located near the lake is an aerial cable gondola lift. It runs from the bottom of the valley to the top of Mount Howard, which is measured at. It was built in 1968 and opened to the public in 1970. From the tram car, passengers can view Wallowa Lake as well as the surrounding mountains.

Geographic entities mentioned:
surface_form: mount howard
instance_of: Mountain
countries: United States
coordinates: lat: 45.261
lon: -117.179
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: mount howard
instance_of: Mountain
countries: United States
coordinates: lat: 47.813888888889
lon: -120.95472222222
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
This led to the formation of many of the nearby towns that still exist today. After the surrender, Chief Joseph and the Nez Perce were banished from the area. Today many monuments and dedications are set up at the lake and its surrounding cities in remembrance of the Nez Perce tribe and the battle that took place. In 1880 the town nearest to Wallowa Lake, Joseph, was named after Chief Joseph.

Geographic entities mentioned:
surface_form: battle
instance_of: Watercourse
countries: United States
coordinates: lat: 44.9266
lon: -93.0291
surface_form: nez perce
instance_of: Mountain
countries: United States
coordinates: lat: 43.7194
lon: -110.797
These moraines begin well below the water's surface and climb to over above the lake. Before the glacial unit compounded enough to form the moraines that currently surround the lake, a large alluvial fan was present in the valley. This fan was created by the Wallowa River transporting debris into the valley.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Before the glacial unit compounded enough to form the moraines that currently surround the lake, a large alluvial fan was present in the valley. This fan was created by the Wallowa River transporting debris into the valley. The sediment left by the river was pushed by a series of glaciers that advanced north into the valley. As they pushed the debris, they also dug deep into the earth.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
As they pushed the debris, they also dug deep into the earth. Though the number of glaciers that formed the moraines is debated, the most accepted hypothesis is that eight or nine glaciers formed the walls that now dam the lake. The last glacier advanced into the valley about 17,000 years ago and is known as the Wallowa Glacier. Its moraines form much of the lake shore.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Occurring subsequent to the formation of Wallowa Lake, these did not reach the location of the lake. The earliest of these was 11,000&ndash;10,000 years before present. Gold rush and war with the Nez Perce. The Wallowa Lake area was inhabited by the Wallowa band of the Nez Perce tribe prior to the exploration of the area and the formation of the U.S. State of Oregon.

Geographic entities mentioned:
surface_form: nez perce
instance_of: Mountain
countries: United States
coordinates: lat: 43.7194
lon: -110.797
The earliest of these was 11,000&ndash;10,000 years before present. Gold rush and war with the Nez Perce. The Wallowa Lake area was inhabited by the Wallowa band of the Nez Perce tribe prior to the exploration of the area and the formation of the U.S. State of Oregon. The lake and its surrounding area was guaranteed to the Nez Perce as part of the Treaty of 1855.

Geographic entities mentioned:
surface_form: nez perce
instance_of: Mountain
countries: United States
coordinates: lat: 43.7194
lon: -110.797
Gold rush and war with the Nez Perce. The Wallowa Lake area was inhabited by the Wallowa band of the Nez Perce tribe prior to the exploration of the area and the formation of the U.S. State of Oregon. The lake and its surrounding area was guaranteed to the Nez Perce as part of the Treaty of 1855. This lasted until the discovery of gold in the area and the subsequent rush.

Geographic entities mentioned:
surface_form: nez perce
instance_of: Mountain
countries: United States
coordinates: lat: 43.7194
lon: -110.797
This lasted until the discovery of gold in the area and the subsequent rush. Conflict with miners and other trespassers resulted in new treaty negotiations in 1863, in which American agents aimed to shrink the reservation and exclude the Wallowa county from its boundaries. The Wallowa Nez Perce rejected the proposed treaty and refused to sign.

Geographic entities mentioned:
surface_form: nez perce
instance_of: Mountain
countries: United States
coordinates: lat: 43.7194
lon: -110.797
However, chiefs from bands unaffected by the new boundaries, from the areas that remained within the reservation, did sign, placing the Wallowa band outside the reservation. By 1877, pressures from non-Indian settlers provoked violence, including the murder of Nez Perce people in the Salmon River area by settlers, and subsequent revenge carried out by some young Nez Perce warriors.

Geographic entities mentioned:
surface_form: nez perce
instance_of: Mountain
countries: United States
coordinates: lat: 43.7194
lon: -110.797
surface_form: nez perce
instance_of: Mountain
countries: United States
coordinates: lat: 43.7194
lon: -110.797
After the war, the U.S. Government took the land and allowed it to be settled. This led to the formation of many of the nearby towns that still exist today. After the surrender, Chief Joseph and the Nez Perce were banished from the area. Today many monuments and dedications are set up at the lake and its surrounding cities in remembrance of the Nez Perce tribe and the battle that took place.

Geographic entities mentioned:
surface_form: nez perce
instance_of: Mountain
countries: United States
coordinates: lat: 43.7194
lon: -110.797
Wallowa Lake. Wallowa Lake is a ribbon lake south of Joseph, Oregon, United States, at an elevation of. Impounded by high moraines, it was formed by a series of Pleistocene glaciers. On the south end of the lake is a small community made up of vacation homes, lodging, restaurants, as well as other small businesses. Wallowa Lake has been used for recreation since at least 1880.

Geographic entities mentioned:
surface_form: wallowa lake
instance_of: Lake
countries: United States
coordinates: lat: 45.308888888889
lon: -117.21055555556
Impounded by high moraines, it was formed by a series of Pleistocene glaciers. On the south end of the lake is a small community made up of vacation homes, lodging, restaurants, as well as other small businesses. Wallowa Lake has been used for recreation since at least 1880. The Wallowa Lake State Park is at the southern tip of the lake. Geology and formation.

Geographic entities mentioned:
surface_form: wallowa lake
instance_of: Lake
countries: United States
coordinates: lat: 45.308888888889
lon: -117.21055555556
On the south end of the lake is a small community made up of vacation homes, lodging, restaurants, as well as other small businesses. Wallowa Lake has been used for recreation since at least 1880. The Wallowa Lake State Park is at the southern tip of the lake. Geology and formation. Wallowa Lake has been used in geology textbooks as an example of a lake dammed by moraines.

Geographic entities mentioned:
surface_form: wallowa lake
instance_of: Lake
countries: United States
coordinates: lat: 45.308888888889
lon: -117.21055555556
Wallowa Lake has been used for recreation since at least 1880. The Wallowa Lake State Park is at the southern tip of the lake. Geology and formation. Wallowa Lake has been used in geology textbooks as an example of a lake dammed by moraines. These moraines begin well below the water's surface and climb to over above the lake.

Geographic entities mentioned:
surface_form: wallowa lake
instance_of: Lake
countries: United States
coordinates: lat: 45.308888888889
lon: -117.21055555556
Its moraines form much of the lake shore. Near Glacier Lake, high in the surrounding mountains, is evidence of several subsequent glacier advances. Occurring subsequent to the formation of Wallowa Lake, these did not reach the location of the lake. The earliest of these was 11,000&ndash;10,000 years before present. Gold rush and war with the Nez Perce.

Geographic entities mentioned:
surface_form: wallowa lake
instance_of: Lake
countries: United States
coordinates: lat: 45.308888888889
lon: -117.21055555556
After the surrender, Chief Joseph and the Nez Perce were banished from the area. Today many monuments and dedications are set up at the lake and its surrounding cities in remembrance of the Nez Perce tribe and the battle that took place. In 1880 the town nearest to Wallowa Lake, Joseph, was named after Chief Joseph. The war is remembered by historians as one of the last wars the U.S.

Geographic entities mentioned:
surface_form: wallowa lake
instance_of: Lake
countries: United States
coordinates: lat: 45.308888888889
lon: -117.21055555556
In 1880 the town nearest to Wallowa Lake, Joseph, was named after Chief Joseph. The war is remembered by historians as one of the last wars the U.S. forces had with Native Americans. Formation of Joseph and Wallowa Lake tourism. The first businesses near the lake were in the town of Joseph. In 1879, a man named Matthew Johnson who was the first postmaster for Joseph, ran the first store.

Geographic entities mentioned:
surface_form: wallowa lake
instance_of: Lake
countries: United States
coordinates: lat: 45.308888888889
lon: -117.21055555556
Wallowa Lake gained popularity among gold miners and soon began attracting guests from other areas. Seeing an emerging tourism market, entrepreneurs began building businesses at the lake. Among those built was the Wonderland Inn, now known as the Wallowa Lake Lodge. The Wonderland Inn was developed in 1923 as an amusement park at the south end of the lake.

Geographic entities mentioned:
surface_form: wallowa lake
instance_of: Lake
countries: United States
coordinates: lat: 45.308888888889
lon: -117.21055555556
The park contained a restaurant, store, bowling alley, dance hall, outdoor movie theater, horse drawn carousel and cabins for those wishing to stay overnight. An 18-passenger boat carried the guests who arrived in Joseph (which lies at the north end of the lake) down the entire four mile stretch of Wallowa Lake, finally arriving at the inn and amusement park.

Geographic entities mentioned:
surface_form: wallowa lake
instance_of: Lake
countries: United States
coordinates: lat: 45.308888888889
lon: -117.21055555556
The amusement park operated until 1940, when snowfall from an unusually harsh winter crushed most of the buildings and rendered the park inoperable. However, the inn survived the winter and still remains in operation, though renamed the Wallowa Lake Lodge. The area at the south end of the lake continued to be developed commercially.

Geographic entities mentioned:
surface_form: wallowa lake
instance_of: Lake
countries: United States
coordinates: lat: 45.308888888889
lon: -117.21055555556
Several more stores, lodges, restaurants, and rental cabins were built in the following years, turning the south end of the lake into a tourist community. The businesses at the south end of Wallowa Lake are members of a non-profit tourism association. This association maintains a website, supports tourism in the area and works to solve issues across the lake community.

Geographic entities mentioned:
surface_form: wallowa lake
instance_of: Lake
countries: United States
coordinates: lat: 45.308888888889
lon: -117.21055555556
This association maintains a website, supports tourism in the area and works to solve issues across the lake community. There are 2,000 to 3,000 people residing at the south end of Wallowa Lake in summer with all businesses open. However, from October through March there are less than 40 year-round residences at the south end of the lake, which is designated as a CDP by the U.S.

Geographic entities mentioned:
surface_form: wallowa lake
instance_of: Lake
countries: United States
coordinates: lat: 45.308888888889
lon: -117.21055555556
It runs from the bottom of the valley to the top of Mount Howard, which is measured at. It was built in 1968 and opened to the public in 1970. From the tram car, passengers can view Wallowa Lake as well as the surrounding mountains. In June 1992, a malfunction occurred in the operating system of the Tram and all passengers had to be evacuated by helicopter.

Geographic entities mentioned:
surface_form: wallowa lake
instance_of: Lake
countries: United States
coordinates: lat: 45.308888888889
lon: -117.21055555556
The last glacier advanced into the valley about 17,000 years ago and is known as the Wallowa Glacier. Its moraines form much of the lake shore. Near Glacier Lake, high in the surrounding mountains, is evidence of several subsequent glacier advances. Occurring subsequent to the formation of Wallowa Lake, these did not reach the location of the lake.

Geographic entities mentioned:
surface_form: glacier lake
instance_of: Lake
countries: United States
coordinates: lat: 47.4675
lon: -121.29611111111
However, the storm failed to intensify, and Bertha made landfall near Boothville, Louisiana as a minimal tropical storm early on August 5. It slowly weakened over the swampy portions of southeastern Louisiana, and degenerated to a tropical depression later on the 5th after crossing Lake Pontchartrain.

Geographic entities mentioned:
surface_form: Lake Pontchartrain
instance_of: Lake
countries: United States
coordinates: lat: 30.188888888889
lon: -90.101388888889
The oncoming flood would wipe out all animals and people not on the ship. After twelve days on the water, Uta-napishtim opened the hatch of his ship to look around and saw the slopes of Mount Nisir, where he rested his ship for seven days. On the seventh day, he sent a dove out to see if the water had receded, and the dove could find nothing but water, so it returned.

Geographic entities mentioned:
surface_form: Mount Nisir
instance_of: Mountain
countries: Iraq
coordinates: lat: 35.5
lon: 45.41666667