Sarmila/GeoWiki-Features huggingface dataset:
Flint Hills. The Flint Hills, historically known as Bluestem Pastures or Blue Stem Hills, are a region of hills and prairies that lie mostly in eastern Kansas. It is named for the abundant residual flint eroded from the bedrock that lies near or at the surface.

Geographic entities mentioned:
surface_form: flint hills
instance_of: Landform
countries: United States
coordinates: lat: 37.2833
lon: -96.6753
These ranches rely on annual controlled burns conducted by ranchers every spring to renew the prairie grasses for cattle to graze. The Flint Hills Discovery Center, a science and history museum focusing on the Flint Hills, opened in Manhattan, Kansas, in April 2012. Description.

Geographic entities mentioned:
surface_form: flint hills
instance_of: Landform
countries: United States
coordinates: lat: 37.2833
lon: -96.6753
The Flint Hills Discovery Center, a science and history museum focusing on the Flint Hills, opened in Manhattan, Kansas, in April 2012. Description. Explorer Zebulon Pike first coined the name the Flint Hills in 1806 when he entered into his journal, &quot;passed very ruff flint hills&quot;. The underlying bedrock of the hills is a flinty limestone.

Geographic entities mentioned:
surface_form: flint hills
instance_of: Landform
countries: United States
coordinates: lat: 37.2833
lon: -96.6753
surface_form: flint hills
instance_of: Landform
countries: United States
coordinates: lat: 37.2833
lon: -96.6753
Description. Explorer Zebulon Pike first coined the name the Flint Hills in 1806 when he entered into his journal, &quot;passed very ruff flint hills&quot;. The underlying bedrock of the hills is a flinty limestone. The largest town in the area is Manhattan, Kansas, and the hills can be accessed from the Flint Hills Scenic Byway, which passes through the region. Geology.

Geographic entities mentioned:
surface_form: flint hills
instance_of: Landform
countries: United States
coordinates: lat: 37.2833
lon: -96.6753
The largest town in the area is Manhattan, Kansas, and the hills can be accessed from the Flint Hills Scenic Byway, which passes through the region. Geology. The rocks exposed in the Flint Hills were laid down about 250 million years ago during the Permian Period. During this time, much of the Midwest, including Kansas and Oklahoma, was covered with shallow seas.

Geographic entities mentioned:
surface_form: flint hills
instance_of: Landform
countries: United States
coordinates: lat: 37.2833
lon: -96.6753
During this time, much of the Midwest, including Kansas and Oklahoma, was covered with shallow seas. As a result, much of the Flint Hills is composed of limestone and shale, with plentiful fossils of prehistoric sea creatures. The most notable layer of chert-bearing limestone is the Florence Limestone Member, which is approximately.

Geographic entities mentioned:
surface_form: flint hills
instance_of: Landform
countries: United States
coordinates: lat: 37.2833
lon: -96.6753
Numerous roadcuts of the Florence Member are prominent along Interstate 70 in Riley County, Kansas. Unlike the Pennsylvanian limestones to the east, however, many of the limestones in the Flint Hills contain several bands of chert or flint. Because chert is much less soluble than the limestone surrounding it, the weathering of the limestone has left behind a clay soil with abundant chert gravel.

Geographic entities mentioned:
surface_form: flint hills
instance_of: Landform
countries: United States
coordinates: lat: 37.2833
lon: -96.6753
For this reason, cattle ranching became the main agricultural activity in the region. Never having been ploughed over and sparsely developed, the Flint Hills represent the last expanse of intact tallgrass prairie in the nation. They present the best opportunity for sustained preservation of this unique habitat that once covered the vast Great Plains.

Geographic entities mentioned:
surface_form: flint hills
instance_of: Landform
countries: United States
coordinates: lat: 37.2833
lon: -96.6753
They present the best opportunity for sustained preservation of this unique habitat that once covered the vast Great Plains. Most of the plains, such as the Central tall grasslands to the north, have better soil than the Flint Hills and a richer plant cover, but have almost entirely been converted to farmland.

Geographic entities mentioned:
surface_form: flint hills
instance_of: Landform
countries: United States
coordinates: lat: 37.2833
lon: -96.6753
The elk that once roamed the region are gone. The United States Environmental Protection Agency and the World Wildlife Fund have designated the Flint Hills as an ecoregion, distinct from other grasslands of the Great Plains. Four tallgrass prairie preserves are located in the Flint Hills.

Geographic entities mentioned:
surface_form: flint hills
instance_of: Landform
countries: United States
coordinates: lat: 37.2833
lon: -96.6753
The other preserves in Kansas, are the Tallgrass Prairie National Preserve in northern Chase County near Strong City, the Flint Hills Tallgrass Prairie Preserve east of Cassoday, &quot;the Prairie Chicken Capital of the World&quot;, and the Konza Prairie, which is managed as a tallgrass prairie biological research station by Kansas State University and is located near Manhattan.

Geographic entities mentioned:
surface_form: flint hills
instance_of: Landform
countries: United States
coordinates: lat: 37.2833
lon: -96.6753
Filmed in locations within the Adelaide Hills and Barossa Valley regions of South Australia, the series starred Lorraine Bayly, Max Cullen, Catherine Wilkin and Liddy Clark in the role of Verity &quot;Birdie&quot; Birdwood. Clark's &quot;Birdie&quot; was notably different in both appearance (Clark had short, blonde hair) and manner (Clark portrayed a more extroverted, outwardly confident Birdie).

Geographic entities mentioned:
surface_form: Barossa Valley
instance_of: Valley
countries: Australia
coordinates: lat: -34.533333333333
lon: 138.95
As the hurricane tracked inland, it passed over the Everglades, producing winds of at Everglades City. Along the southern shore of Lake Okeechobee, winds gusted to; barometric pressure there fell to. Storm surge in the region triggered foot-deep flooding of some streets in local towns. Docks and fishing equipment suffered extensive damage in the region.

Geographic entities mentioned:
surface_form: Lake Okeechobee
instance_of: Lake
countries: United States
coordinates: lat: 26.933333333333
lon: -80.8
Teams. All eighteen UCI WorldTeams, four UCI ProTeams, and the Canadian national team made up the twenty-three teams that participated in the race. Course. The race used a hilly circuit around Mount Royal, with the longest climb being Côte Camilien-Houde (1.8 km long and 8% average grade). 18 laps of the circuit made the race in length, with of cumulative climbing during the race.

Geographic entities mentioned:
surface_form: Mount Royal
instance_of: Mountain
countries: Canada
coordinates: lat: 45.506388888889
lon: -73.588888888889
According to the 2011 census, the village residents numbered 293. It is located by the southeastern edge of Kėdainiai city, by the confluence of the Obelis and Nevėžis rivers, next to the crossroad of the Jonava-Šeduva (KK144) and Kėdainiai-Babtai roads. The Šerkšnys river passes through the village. History. In the beginning of the 20th century, Paobelys was a small &quot;falwark&quot;.

Geographic entities mentioned:
surface_form: Šerkšnys
instance_of: Watercourse
countries: Lithuania
coordinates: lat: 55.257734
lon: 23.953286
It also includes ranges to the east in Kelantan, Terengganu, and Pahang states. The highest peak in the Titiwangsa Mountains is Mount Korbu at 2,183 meters elevation. Other peaks include Mount Tahan (2,188 m), the highest peak in peninsular Malaysia, and Mount Benum (2,130 m). The ecoregion is surrounded at lower elevations by the ecologically-distinct Peninsular Malaysian rain forests. Flora.

Geographic entities mentioned:
surface_form: Mount Korbu
instance_of: Mountain
countries: Malaysia
coordinates: lat: 4.6833333333333
lon: 101.3
It also includes ranges to the east in Kelantan, Terengganu, and Pahang states. The highest peak in the Titiwangsa Mountains is Mount Korbu at 2,183 meters elevation. Other peaks include Mount Tahan (2,188 m), the highest peak in peninsular Malaysia, and Mount Benum (2,130 m). The ecoregion is surrounded at lower elevations by the ecologically-distinct Peninsular Malaysian rain forests. Flora.

Geographic entities mentioned:
surface_form: Mount Tahan
instance_of: Mountain
countries: Malaysia
coordinates: lat: 4.6311111111111
lon: 102.23444444444
surface_form: Mount Benum
instance_of: Mountain
countries: Malaysia
coordinates: lat: 3.82333
lon: 102.094
It meets the Doubs a second time further upstream, at. From here, it follows the winding course of the river as far as the Lac des Brenets, north of Le Locle, at. After passing the Col des Roches at, the border runs in a south-westerly direction, generally following the Jura ridge, reaching an altitude of (&quot;Le Meix Musy&quot;).

Geographic entities mentioned:
surface_form: Lac des Brenets
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 47.069166666667
lon: 6.6977777777778
After passing the Col des Roches at, the border runs in a south-westerly direction, generally following the Jura ridge, reaching an altitude of (&quot;Le Meix Musy&quot;). It turns towards the south to include Pontarlier in France and again to the southwest to include Vallorbe and the Lac de Joux in Switzerland.

Geographic entities mentioned:
surface_form: Lac de Joux
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.639444444444
lon: 6.2858333333333
It turns towards the south to include Pontarlier in France and again to the southwest to include Vallorbe and the Lac de Joux in Switzerland. Here it reaches an altitude of, before crossing the Orbe river upstream of Bois-d'Amont. South of Les Rousses it turns to the south and then southeast, running towards Lake Geneva, rising to at, passing south of La Dôle peak.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
surface_form: La Dôle
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.425
lon: 6.0994444444444
From Grand Perrond (), the border descends to, crossing the road from Martigny to Chamonix, before ascending to Les Grandes Otanes (), the Aiguille du Tour (), the Aiguille d'Argentière (), Tour Noir () and finally to the tripoint with the French–Italian and Swiss–Italian borders, at a point just west of Mont Dolent, and at altitude. Border checks.

Geographic entities mentioned:
surface_form: Les Grandes Otanes
instance_of: Mountain
countries: Switzerland
France
coordinates: lat: 46.019444444444
lon: 6.9813888888889
surface_form: Aiguille du Tour
instance_of: Mountain
countries: Switzerland
France
coordinates: lat: 45.994416666667
lon: 7.0098333333333
surface_form: Aiguille d'Argentière
instance_of: Mountain
countries: Switzerland
France
coordinates: lat: 45.959761111111
lon: 7.0203194444444
surface_form: Tour Noir
instance_of: Mountain
countries: Switzerland
coordinates: lat: 45.950305555556
lon: 7.03675
surface_form: Mont Dolent
instance_of: Mountain
countries: Switzerland
Italy
France
coordinates: lat: 45.9225
lon: 7.0461111111111
Utoy Creek. Utoy Creek is a stream in the U.S. state of Georgia. It is a tributary to the Chattahoochee River. Utoy Creek most likely was named for the Utoy Indians. The Battle of Utoy Creek was fought here in 1864.

Geographic entities mentioned:
surface_form: Chattahoochee River
instance_of: Watercourse
countries: United States
coordinates: lat: 30.7088028
lon: -84.8638097
Shrub encroachment has led to the decline of soil quality of up to 40% in Northwest China. In the Tibetan Plateau, woody encroachment is found to be one of the main grassland disturbance factors. Among the encroaching species is &quot;Potentilla fruticose.&quot; Encroachment has a significant influence on the water balance of the plateau.

Geographic entities mentioned:
surface_form: Tibetan Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
The neighborhood is part of the district Midtbyen (the town center) and borders the neighborhoods of Frederiksbjerg and Marselisborg to the East and the district of Viby to the South. Langenæs is delimited by the streets &quot;Søndre Ringgade&quot;, &quot;Skanderborgvej&quot;, &quot;Marselis Boulevard&quot; and the valley of Brabrand Ådal.

Geographic entities mentioned:
surface_form: Brabrand Ådal
instance_of: Lake
countries: Denmark
coordinates: lat: 56.1458
lon: 10.1125
As of 1984 it had been collected in the Alay Mountains (&quot;Archa-bakhi&quot;); in the Zaalaisk Mountains at the Kyzylart Pass in Kyrgyzstan on the border between Gorno-Badakshan province in Tajikistan and Osh Province, Kyrgyzstan; in the Pamir Mountain proper at a place called &quot;Kara-kuzun&quot; and at Beyik Pass, at 4200m elevation, in far eastern Gorno-Badakshan, leading to the Taghdumbash Pamir region of Xinjiang; and in the Hindu Kush.

Geographic entities mentioned:
surface_form: Taghdumbash Pamir
instance_of: Valley
countries: People's Republic of China
coordinates: lat: 37.2
lon: 75.4
Paragon Peak. Paragon Peak is located at the southern end of Mount Robson Provincial Park on the border of Alberta and British Columbia in Canada. It was named in 1921 by Howard Palmer.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mount robson
instance_of: Mountain
countries: Canada
coordinates: lat: 53.11055555555556
lon: -119.15666666666667
surface_form: paragon peak
instance_of: Mountain
countries: Canada
coordinates: lat: 52.675
lon: -118.288
Paragon Peak. Paragon Peak is located at the southern end of Mount Robson Provincial Park on the border of Alberta and British Columbia in Canada. It was named in 1921 by Howard Palmer.

Geographic entities mentioned:
surface_form: paragon peak
instance_of: Mountain
countries: Canada
coordinates: lat: 52.675
lon: -118.288
The river takes its source from Pirin's largest and deepest glacial lake, Popovo, at an altitude of 2,234 m. At an altitude of 2,174 m near the Fish Popovi Lakes it is joined by two mountain streams — one from the north sloping down the summit of Polezhan (2,851 m), and one from the west coming from the Polezhanski Lakes.

Geographic entities mentioned:
surface_form: Polezhanski Lakes
instance_of: Group of lakes
countries: Bulgaria
coordinates: lat: 41.718611111111
lon: 23.499444444444
At an altitude of 2,174 m near the Fish Popovi Lakes it is joined by two mountain streams — one from the north sloping down the summit of Polezhan (2,851 m), and one from the west coming from the Polezhanski Lakes. Further downstream another stream coming from the Kremenski Lakes flows into the Retizhe. It then flows in north-eastern direction in a deep valley, forming rapids and small waterfalls.

Geographic entities mentioned:
surface_form: Kremenski Lakes
instance_of: Group of lakes
countries: Bulgaria
coordinates: lat: 41.6969
lon: 23.5186
Ronald Ridge. Ronald Ridge () is a narrow ridge, 5 nautical miles (9 km) long, located 1 nautical mile (1.9 km) west of Donald Ridge, which it resembles, in the Pioneer Heights, Heritage Range, Antarctica. Mapped by United States Geological Survey (USGS) from surveys and U.S. Navy air photos, 1961–66. Named by Advisory Committee on Antarctic Names (US-ACAN) for Ronald C.

Geographic entities mentioned:
surface_form: Donald Ridge
instance_of: Mountain
coordinates: lat: -79.6167
lon: -83.1667
After the war, Zancanaro produced different types of works in various genres and traveled around Europe, particularly in Paris and Eastern Europe. He produced works of social realism in the 1950s, documenting women workers in the rice fields in northern Italy's Po Valley using photos and sketches he completed in the field in Roncoferraro in the 1950s (&quot;Mondine di Roncoferraro&quot;, 1953).

Geographic entities mentioned:
surface_form: Po Valley
instance_of: Valley
countries: Italy
coordinates: lat: 45.330277777778
lon: 9.7988888888889
At this time Fairbrother was replaced by another pākehā officer, Major Russell Young, who was promoted to lieutenant colonel and subsequently led the battalion until July 1944. As part of the Fifth Army's advance up the Liri valley, the Māori Battalion's next major engagement came in early 1944 when they took part in the fighting around Monte Cassino.

Geographic entities mentioned:
surface_form: Monte Cassino
instance_of: Mountain
countries: Italy
coordinates: lat: 41.49
lon: 13.813888888889
The specific name comes from Zhongyuan, an ancient name for the geographic area of the province. &quot;Yubaatar&quot; is the first known and southernmost Late Cretaceous multituberculate outside of the Mongolian plateau (most multituberculate specimens mainly consist only of teeth and jaws, and are rarely found in eastern Asia).

Geographic entities mentioned:
surface_form: Mongolian plateau
instance_of: Plateau
countries: Mongolia
People's Republic of China
Russia
Russian Empire
Soviet Union
coordinates: lat: 45
lon: 107
Mount Franklin (Australian Capital Territory). Mount Franklin is a mountain with an elevation of in the Brindabella Ranges that is located on the border between the Australian Capital Territory and New South Wales, Australia. The summit of the mountain is located in the Australian Capital Territory. The mountain is located in the Bimberi Nature Reserve and the Namadgi National Park.

Geographic entities mentioned:
surface_form: mount franklin
instance_of: Mountain
countries: Australia
coordinates: lat: -37.2651
lon: 144.15
surface_form: mount franklin (australian capital territory)
instance_of: Mountain
countries: Australia
coordinates: lat: -35.4872
lon: 148.774
Mount Franklin (Australian Capital Territory). Mount Franklin is a mountain with an elevation of in the Brindabella Ranges that is located on the border between the Australian Capital Territory and New South Wales, Australia. The summit of the mountain is located in the Australian Capital Territory. The mountain is located in the Bimberi Nature Reserve and the Namadgi National Park.

Geographic entities mentioned:
surface_form: mount franklin
instance_of: Mountain
countries: Australia
coordinates: lat: -37.2651
lon: 144.15
surface_form: mount franklin
instance_of: Mountain
countries: Australia
coordinates: lat: -35.4872
lon: 148.774
The summit of the mountain is located in the Australian Capital Territory. The mountain is located in the Bimberi Nature Reserve and the Namadgi National Park. A marked walking trail to the summit can be reached via Mount Franklin Road. The summit is accessible by bush walking trails and requires no specialised climbing skills.

Geographic entities mentioned:
surface_form: mount franklin
instance_of: Mountain
countries: Australia
coordinates: lat: -37.2651
lon: 144.15
surface_form: mount franklin
instance_of: Mountain
countries: Australia
coordinates: lat: -35.4872
lon: 148.774
It is located close to Brindabella Station where the Australian author Miles Franklin once lived and the mountain is named after her family. The mountain is often covered in snow in winter and Australian ski pioneers based themselves at Mount Franklin from the 1930s. Nowadays, cross country skiing is possible in the area during winter, when conditions allow. Skiing on Mount Franklin.

Geographic entities mentioned:
surface_form: mount franklin
instance_of: Mountain
countries: Australia
coordinates: lat: -37.2651
lon: 144.15
surface_form: mount franklin
instance_of: Mountain
countries: Australia
coordinates: lat: -35.4872
lon: 148.774
The mountain is often covered in snow in winter and Australian ski pioneers based themselves at Mount Franklin from the 1930s. Nowadays, cross country skiing is possible in the area during winter, when conditions allow. Skiing on Mount Franklin. A ski chalet was constructed at Mount Franklin in 1938 to service the Canberra Alpine Club. Ski runs were cleared and ski tows were improvised.

Geographic entities mentioned:
surface_form: mount franklin
instance_of: Mountain
countries: Australia
coordinates: lat: -37.2651
lon: 144.15
surface_form: mount franklin
instance_of: Mountain
countries: Australia
coordinates: lat: -35.4872
lon: 148.774
Nowadays, cross country skiing is possible in the area during winter, when conditions allow. Skiing on Mount Franklin. A ski chalet was constructed at Mount Franklin in 1938 to service the Canberra Alpine Club. Ski runs were cleared and ski tows were improvised. The chalet later operated as a museum before being destroyed in the 2003 Canberra bushfires.

Geographic entities mentioned:
surface_form: mount franklin
instance_of: Mountain
countries: Australia
coordinates: lat: -37.2651
lon: 144.15
surface_form: mount franklin
instance_of: Mountain
countries: Australia
coordinates: lat: -35.4872
lon: 148.774
It serves as an interpretive centre and can provide park managers and emergency services personnel with a base to conduct search and rescue operations in the event of future bushfires. The ACT/NSW boundary passes through the Franklin Chalet ruin area. Nowadays, cross country skiing is possible at Mount Franklin and surrounding peaks in winter, if conditions allow.

Geographic entities mentioned:
surface_form: mount franklin
instance_of: Mountain
countries: Australia
coordinates: lat: -37.2651
lon: 144.15
surface_form: mount franklin
instance_of: Mountain
countries: Australia
coordinates: lat: -35.4872
lon: 148.774
Fawnskin is an unincorporated community in San Bernardino County, California, United States. It is located on the northwest side of Big Bear Valley, in the heart of the San Bernardino Mountains, at an altitude of 6,827 feet (2,081 m). The tiny community has a &quot;permanent&quot; population of 380, and many vacation homes that range from multi-million dollar mansions to decaying log cabins.

Geographic entities mentioned:
surface_form: Big Bear Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.276381
lon: -116.824737
History. This small community was once an artists' colony, which attracted artisans, musicians, composers and actors from the Los Angeles area. Mountain travelers in the 19th century came to the Big Bear Valley through Fawnskin on the rough road by stagecoach and later motorcars.

Geographic entities mentioned:
surface_form: Big Bear Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.276381
lon: -116.824737
Several hundred homes are located along the north shore of Big Bear Lake and in the forested mountainside adjacent to the San Bernardino National Forest. Gold miners, loggers, and hunters were drawn to the adjacent Holcomb Valley during the 19th century. The Native American legend about how the town got its name has been turned into the urban legend.

Geographic entities mentioned:
surface_form: Holcomb Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.307222222222
lon: -116.9275
Several writers live there full-time, including William Sarabande. Jordan Romero, who as a 13-year-old boy conquered Mount Everest, is also known as one of the &quot;Fawnskin Folks.&quot;
Actress/singer Shirley Jones and her husband actor/comedian Marty Ingels also own a home in Fawnskin. Marty Ingels and Shirley Jones bought a piece of property in 2001 and created Fawn Park in downtown Fawnskin.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
It is part of the Saint Lawrence River drainage basin, and is about southwest of the community of Kenabeek. The lake has one unnamed inflow, at the southwest. The primary outflow is an unnamed creek at the northeast which flows to McKenzie Lake and onward, flowing subsequently via Spray Creek, Spring Creek, the Montreal River and the Ottawa River to the Saint Lawrence River.

Geographic entities mentioned:
surface_form: mckenzie lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.55694444444445
lon: -80.22166666666666
surface_form: montreal river
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.2389
lon: -84.6458
surface_form: mckenzie lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.45944444444444
lon: -91.055
surface_form: mckenzie lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.36416666666667
lon: -78.02277777777778
surface_form: mckenzie lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.68638888888889
lon: -82.44777777777777
surface_form: mckenzie lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.316944444444445
lon: -81.08472222222223
surface_form: montreal
instance_of: Lake
countries: Canada
coordinates: lat: 54.3333
lon: -105.667
Harebell Lake. Harebell Lake () is a lake in geographic Speight Township in the Unorganized West Part of Timiskaming District in Northeastern Ontario, Canada. It is part of the Saint Lawrence River drainage basin, and is about southwest of the community of Kenabeek. The lake has one unnamed inflow, at the southwest.

Geographic entities mentioned:
surface_form: harebell lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.54611111111111
lon: -80.235
It was bounded to the north by Pierrefonds—Senneville, to the southeast by Saint-Laurent, to the south by Dorval–L'Île-Dorval, to the southwest by Pointe-Claire, and to the west by Kirkland. The northern part of Roxboro had two salients that reach the bank of the Rivière des Prairies, exclaving two sections of Pierrefonds—Senneville. The borough had an area of 17,30 km2 and a population of 53,848.

Geographic entities mentioned:
surface_form: Rivière des Prairies
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.708333333333
lon: -73.479166666667
Exhibits. The main permanent exhibit on the first floor offers an extensive display of the natural history of the region, particularly as it relates to Lake Superior. A smaller exhibit space on the second floor is home to a periodically changing exhibit, which usually relates more to regional human history, rather than natural history.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
The Robert Frost Trail is a long footpath that passes through the eastern Connecticut River Valley of Massachusetts. The trail runs from the Connecticut River in South Hadley, Massachusetts to Ruggles Pond in Wendell State Forest, through both Hampshire and Franklin County and includes a number of scenic features such as the Holyoke Range, Mount Orient, Puffer's Pond, and Mount Toby.

Geographic entities mentioned:
surface_form: Mount Orient
instance_of: Mountain
countries: United States
coordinates: lat: 42.393333333333
lon: -72.461388888889
surface_form: Mount Toby
instance_of: Mountain
countries: United States
coordinates: lat: 42.487777777778
lon: -72.5375
It follows the northern slopes of the range from Mount Holyoke to Taylor Notch, along the ridge line, descending south to Lithia Springs Reservoir, before climbing again to the ridgeline, where it goes north of Mount Hitchcock and Bare Mountain, then crosses to the north slope of the range before summiting Rattlesnake Knob (the eastern peak of Mount Norwottuck), and Long Mountain.

Geographic entities mentioned:
surface_form: Mount Holyoke
instance_of: Mountain
countries: United States
coordinates: lat: 42.300833333333
lon: -72.586944444444
surface_form: Mount Norwottuck
instance_of: Mountain
countries: United States
coordinates: lat: 42.305555555556
lon: -72.51
The middle section of the Robert Frost Trail traverses the Connecticut River Valley in the vicinity of eastern Amherst, south Leverett, and abutting towns. Highlights along the way include the Lawrence Swamp, Pomroy Pond, Harkness Brook Ravine, Amethyst Brook, the Mount Orient ledges, Atkins Reservoir, Cushman Brook Ravine, Puffer's Pond, and the Leverett Knobs.

Geographic entities mentioned:
surface_form: Mount Orient
instance_of: Mountain
countries: United States
coordinates: lat: 42.393333333333
lon: -72.461388888889
Lawrence Swamp is a major local wildlife habitat and aquifer. The northern section of the Robert Frost Trail traverses the summit of Mount Toby, Stoddard Hill, and Dry Hill. Features along the route include the Mount Toby firetower, Cranberry Pond, the Pigpen, a historic sawmill and dam, and Ruggles Pond in Wendell State Forest.

Geographic entities mentioned:
surface_form: Mount Toby
instance_of: Mountain
countries: United States
coordinates: lat: 42.487777777778
lon: -72.5375
Features along the route include the Mount Toby firetower, Cranberry Pond, the Pigpen, a historic sawmill and dam, and Ruggles Pond in Wendell State Forest. Mount Toby, regarded as one of the most biologically diverse locations in New England, is a conglomerate rock massif unique in Massachusetts. The firetower on its summit provides panoramic views.

Geographic entities mentioned:
surface_form: Mount Toby
instance_of: Mountain
countries: United States
coordinates: lat: 42.487777777778
lon: -72.5375
History. The city was founded in 1938 by Flora Mae Statler. Statler was the daughter of another Arizona pioneer, Charles Gillett who helped found Glendale, specifically as a temperance community. Gillett owned much land in Glendale as well as the Verde Valley. Surprise officials previously thought the city was founded by Statler's husband, real estate developer and state legislator Homer C.

Geographic entities mentioned:
surface_form: Verde Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.753055555555555
lon: -112.02194444444444
He committed suicide shortly after committing his final murder. Early life. Albert Millet was born on 2 July 1929, in Hyères. He had a tumultuous childhood, as he was frequently beaten by his alcoholic father and was neglected by his mother, who preferred to spend time with her lover than with her family.

Geographic entities mentioned:
surface_form: Hyères
instance_of: Mountain
countries: France
coordinates: lat: 43.118888888889
lon: 6.1286111111111
The herds were considered inferior at first, but these pastures were good for stock, and the land which seemed a desert was actually good fattening country. In the 1860s and 1870s, German settlers from the Barossa Valley travelled upstream to settle in the eastern Riverina. Because of their religious distinctiveness as Lutherans, they preferred to form clustered German settlements.

Geographic entities mentioned:
surface_form: Barossa Valley
instance_of: Valley
countries: Australia
coordinates: lat: -34.533333333333
lon: 138.95
Pukaskwa National Park. Pukaskwa National Park () is a national park located south of the town of Marathon, Ontario in the Thunder Bay District of northern Ontario, Canada. Established in 1978, Pukaskwa is known for its vistas of Lake Superior and boreal forests. The park covers an area of, and protects a part of the longest undeveloped shoreline anywhere on the Great Lakes.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
Cougars may also be in the park, but numbers are not yet known. Climate. The park has a humid continental climate (&quot;Dfb&quot;) under the Köppen climate classification that is strongly influenced by Lake Superior. The Pic River enters Lake Superior just north of the park. The highest point in the park is the peak of Tip Top Mountain which rises to 641 meters / 2106 feet.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
The Pic River enters Lake Superior just north of the park. The highest point in the park is the peak of Tip Top Mountain which rises to 641 meters / 2106 feet. Thousand year old rock structures known as Pukaskwa Pits which were created by the original inhabitants of this area can be found on many of the park's cobblestone beaches.

Geographic entities mentioned:
surface_form: Tip Top Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 48.2667
lon: -86
Baintha Brakk. __NOTOC__
Baintha Brakk () or The Ogre is a steep, craggy mountain, high, in the Panmah Muztagh, a subrange of the Karakoram mountain range. It is located in Gilgit-Baltistan, Pakistan. It is famous for being one of the hardest peaks in the world to climb: twenty-four years elapsed between the first ascent in 1977 and the second in 2001. Location.

Geographic entities mentioned:
surface_form: muztagh
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.828333333333
lon: 76.360833333333
surface_form: the ogre
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.947777777778
lon: 75.753611111111
surface_form: ogre
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.947777777778
lon: 75.753611111111
surface_form: baintha brakk
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.947777777778
lon: 75.753611111111
surface_form: ogre
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.66361111111111
lon: 76.76138888888889
Notable features. Baintha Brakk is exceptional in its combination of altitude, height above local terrain, and steepness. It is a complex granite tower, steeper and rockier than most other Karakoram peaks, although similar to the Latok peaks next to it. For example, its South Face rises over above the Uzun Brakk Glacier in only of horizontal distance.

Geographic entities mentioned:
surface_form: latok
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.928611111111
lon: 75.823333333333
However, they were all able to reach base camp, where they had a long wait for assistance. The second ascent of Baintha Brakk was made by Urs Stöcker, Iwan Wolf, and Thomas Huber, on 21 July 2001, via the South Pillar route, following their first ascent of the subsidiary peak Ogre III (circa). They noted that there were more than 20 unsuccessful expeditions in the interim.

Geographic entities mentioned:
surface_form: ogre
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.947777777778
lon: 75.753611111111
surface_form: baintha brakk
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.947777777778
lon: 75.753611111111
surface_form: ogre
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.66361111111111
lon: 76.76138888888889
Baintha Brakk. __NOTOC__
Baintha Brakk () or The Ogre is a steep, craggy mountain, high, in the Panmah Muztagh, a subrange of the Karakoram mountain range. It is located in Gilgit-Baltistan, Pakistan. It is famous for being one of the hardest peaks in the world to climb: twenty-four years elapsed between the first ascent in 1977 and the second in 2001. Location.

Geographic entities mentioned:
surface_form: baintha brakk
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.947777777778
lon: 75.753611111111
It is famous for being one of the hardest peaks in the world to climb: twenty-four years elapsed between the first ascent in 1977 and the second in 2001. Location. Baintha Brakk rises above the north side of the Biafo Glacier, one of the major glaciers of the central Karakoram. It lies about north of Skardu, the major town of the region, and about north of the roadhead at Askole. Notable features.

Geographic entities mentioned:
surface_form: baintha brakk
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.947777777778
lon: 75.753611111111
It lies about north of Skardu, the major town of the region, and about north of the roadhead at Askole. Notable features. Baintha Brakk is exceptional in its combination of altitude, height above local terrain, and steepness. It is a complex granite tower, steeper and rockier than most other Karakoram peaks, although similar to the Latok peaks next to it.

Geographic entities mentioned:
surface_form: baintha brakk
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.947777777778
lon: 75.753611111111
For example, its South Face rises over above the Uzun Brakk Glacier in only of horizontal distance. It is because of this steep, rocky nature that Baintha Brakk has been both so difficult to climb and so attractive a target for extremely high-level mountaineers. Climbing history.

Geographic entities mentioned:
surface_form: baintha brakk
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.947777777778
lon: 75.753611111111
Swimming, canoeing, kayaking and fishing are also popular in the area. Four and half kilometres upstream from Colleges Crossing is the Mount Crosby Weir and Mount Crosby Pumping Station. Downstream from the crossing swimming is not recommended due to the presence of bull sharks and due to poor water quality. In 1960 2 shark attacks were reported in Sunday Mail 27/3/94, SMH 21/12/1960.

Geographic entities mentioned:
surface_form: Mount Crosby Weir
instance_of: Lake
countries: Australia
coordinates: lat: -27.5373
lon: 152.7979
The biggest of them are the Zhizhitsa River and the Usvyacha River. The two big lakes in the district, Lake Zhizhitskoye and Lake Dvinye-Velinskoye, which are two biggest lakes of Pskov Oblast after Lake Peipus, also belong to the basin of the Western Dvina. The western and the northern parts of the district belong to the Kunya River, a right tributary of the Lovat River, in the Neva river basin.

Geographic entities mentioned:
surface_form: Lake Zhizhitskoye
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 56.231534
lon: 31.251382
surface_form: Lake Peipus
instance_of: Lake
countries: Estonia
Russia
Russian Empire
Soviet Union
coordinates: lat: 58.676666666667
lon: 27.491666666667
Martha Poma Luque (born 19 November 1964) is a Bolivian politician, trade unionist, and textile artisan who served as senator for La Paz from 2010 to 2015. Born in highland Omasuyos Province, Poma spent her youth between the rural Altiplano and the migrant city of El Alto. A daughter of artisans, she worked in handicrafts, producing traditional indigenous textiles for much of her life.

Geographic entities mentioned:
surface_form: Altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
Poma spent her youth between the city and the countryside. Her family practiced agriculture and animal husbandry on the Altiplano; she was taught to work the fields, harvesting traditional Andean crops, primarily maize and potatoes.

Geographic entities mentioned:
surface_form: Altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
Montjuïc (disambiguation). y5hg19ylrrx6ez18r3yjf1wgmasi" xml:space="preserve">Montjuïc is a hill in Barcelona, Catalonia, Spain.

Geographic entities mentioned:
surface_form: Montjuïc
instance_of: Mountain
countries: Spain
coordinates: lat: 41.364166666667
lon: 2.1580555555556
Flowering occurs between October and February and the fruit is a spherical black drupe, long and wide. Taxonomy. &quot;Cryptocarya floydii&quot; was first formally described in 1979 by André Joseph Guillaume Henri Kostermans in the journal &quot;Brunonia&quot;, from specimens collected on Glenugie Peak near Grafton in 1959. Distribution and habitat.

Geographic entities mentioned:
surface_form: Glenugie Peak
instance_of: Mountain
countries: Australia
coordinates: lat: -29.8333
lon: 153.063
In November 2009, he wrote an endorsement for &quot;The King's Torah&quot;, a controversial book by Yitzhak Shapira. He later rescinded it, saying that the book includes statements that &quot;have no place in human intelligence.&quot;
Goldberg died on 20 August 2020 at Hadassah Medical Center in Ein Kerem, a week after collapsing in his home and was buried in Mount of Olives cemetery.

Geographic entities mentioned:
surface_form: Mount of Olives
instance_of: Mountain
countries: Israel
coordinates: lat: 31.777946
lon: 35.245686
Its design compares to a 3-inch ordnance rifle, which is 70 inches long and weighs about 800 pounds. Huffman solicited nearby New River Valley tradesmen for help and they were more than willing to assist. The companies donated materials and helped to make the new cannon, which became known as, &quot;Skipper II&quot;.

Geographic entities mentioned:
surface_form: New River Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.228888888889
lon: -80.382444444444
Wyldewood Surf Club. The Wyldewood Surf Club is a lake surfing club founded in 1965 in Port Colborne, Ontario, on the northeastern shore of Lake Erie by U.S. and Canadian surfers. It is recognized as the oldest surf club on the Great Lakes.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Original members. The first 17 Club members were local cottagers and surfers from the Hamilton area that learned to surf with very minimal equipment and boards. While a few of the original club members remain, over the years the club has grown to about 50 members, many of whom still surf Lake Erie as well as the hundreds of other breaks along the Great Lakes.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Addington volcanic field. The Addington volcanic field is a submerged volcanic field in the U.S. state of Alaska, located about offshore of Cape Addington on Prince of Wales Island in the Alexander Archipelago. It is southwest of Iphigenia Bay and may have been the source of Late Pleistocene pyroclastic fall distributed throughout the Alaskan Panhandle.

Geographic entities mentioned:
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
surface_form: addington volcanic field
instance_of: Mountain
coordinates: lat: 55.44
lon: -134.17
Addington volcanic field. The Addington volcanic field is a submerged volcanic field in the U.S. state of Alaska, located about offshore of Cape Addington on Prince of Wales Island in the Alexander Archipelago. It is southwest of Iphigenia Bay and may have been the source of Late Pleistocene pyroclastic fall distributed throughout the Alaskan Panhandle.

Geographic entities mentioned:
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
surface_form: addington volcanic field
instance_of: Mountain
coordinates: lat: 55.44
lon: -134.17
surface_form: alexander
instance_of: Mountain
coordinates: lat: -63.3039
lon: -55.80564
state of Alaska, located about offshore of Cape Addington on Prince of Wales Island in the Alexander Archipelago. It is southwest of Iphigenia Bay and may have been the source of Late Pleistocene pyroclastic fall distributed throughout the Alaskan Panhandle. The Addington volcanic field is not known to have been volcanically active since the Pleistocene.

Geographic entities mentioned:
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
surface_form: active
instance_of: Landform
Body of water
coordinates: lat: -63.4167
lon: -56.1667
surface_form: addington volcanic field
instance_of: Mountain
coordinates: lat: 55.44
lon: -134.17
Description. Adults of most populations have a brown forebody, gradually turning black towards the tail, often with spotting or mottling in the lighter parts. Adults from the Lake Victoria area and parts of the Congo Basin are entirely black dorsally.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
At this time, it was assigned to the 6th Military District. The brigade's constituent units were spread across various locations in Tasmania including Lyell, Zeehan, Burnie, Devonport, Deloraine, Beaconsfield, Launceston, Scottsdale, Hobart and Huon. The brigade consisted of four infantry battalions, numbered consecutively as the 90th, 91st, 92nd and 93rd.

Geographic entities mentioned:
surface_form: Huon
instance_of: Valley
countries: Australia
coordinates: lat: -43.12
lon: 146.43
The now-familiar endpapers of the Peter Rabbit series were introduced in the book. &quot;Squirrel Nutkin&quot; had its origins in a story and picture letter Potter sent Norah Moore, the daughter of her former governess, Annie Carter Moore. The background illustrations were modelled on Derwentwater and St. Herbert's Island in the Lake District.

Geographic entities mentioned:
surface_form: Derwentwater
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.583333333333
lon: -3.15
The Lumi, however, maintains its southerly direction, and may thus be said to represent the upper course of the Ruvu, one of tho two main sources of the Pangani River. It flows around the Lake Chala and the Taveta town in the west and empties into the Lake Jipe. The fish species &quot;Barbus&quot; sp.

Geographic entities mentioned:
surface_form: Lake Jipe
instance_of: Lake
countries: Tanzania
Kenya
coordinates: lat: -3.6069444444444
lon: 37.761666666667
Boundaries. The Arran ward was first created in 1974 by the Formation Electoral Arrangements for Cunninghame District Council from the previous Corrie and Brodick, Lamlash, Whiting Bay, Southend, Shedog and Lochranza electoral divisions of Bute County Council. The ward centres around the Isle of Arran and includes the Holy Isle and the uninhabited island of Pladda.

Geographic entities mentioned:
surface_form: Holy Isle
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.525
lon: -5.0722222222222
The bottom of the lake consists of silt and detritus and has abundant curly-leaf pondweed in the spring months before it dies back in July. The lake has a history of winterkill and there is fish migration from nearby Belle Lake. The lake has abundant common carp and black bullheads as well as moderate numbers of northern pike and black crappie.

Geographic entities mentioned:
surface_form: Belle Lake
instance_of: Lake
countries: United States
coordinates: lat: 44.98154
lon: -94.42687
Cedar Lake (McLeod and Meeker counties, Minnesota). Cedar Lake is a lake in McLeod and Meeker counties, in the U.S. state of Minnesota. Cedar Lake was named for the red cedar trees near the lake. Although Cedar Lake is a large lake (1,860 acres) it is also quite shallow lake reaching only 8 feet (2.4 m) deep.

Geographic entities mentioned:
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 47.3869
lon: -121.7
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 29.1925638
lon: -95.082994
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3743
lon: -74.3212
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 46.221
lon: -93.404
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 44.97777778
lon: -94.46138889
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 45.5275
lon: -68.801111111111
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 44.960277777778
lon: -93.321111111111
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 43.78972222
lon: -94.73388889
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 45.2144
lon: -92.571
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 40.9111048
lon: -74.4729616
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 44.59
lon: -93.523333333333