Sarmila/GeoWiki-Features huggingface dataset:
It is situated in the La Paz Department, Sud Yungas Province, Irupana Municipality. Wisk'achani lies west of the Illimani massif, northeast of Link'u Link'u.

Geographic entities mentioned:
surface_form: Illimani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.633333333333
lon: -67.790833333333
surface_form: Link'u Link'u
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.6636
lon: -67.7367
surface_form: link'u link'u
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.6636
lon: -67.7367
Wisk'achani (Sud Yungas). Wisk'achani (Aymara &quot;wisk'acha&quot; a rodent, &quot;-ni&quot; a suffix to indicate ownership, &quot;the one with the viscacha (or viscachas)&quot;, Hispanicized spelling &quot;Viscachani&quot;) is a mountain in the eastern extensions of the Cordillera Real in the Andes of Bolivia. It is situated in the La Paz Department, Sud Yungas Province, Irupana Municipality.

Geographic entities mentioned:
surface_form: wisk'achani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.0397
lon: -67.3411
surface_form: wisk'achani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.24444444
lon: -67.69694444
surface_form: wisk'achani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.28833333
lon: -66.52972222
surface_form: wisk'achani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.6408
lon: -67.7108
surface_form: wisk'achani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.2631
lon: -66.8253
surface_form: wisk'achani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.09388889
lon: -67.69277778
surface_form: wisk'achani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.48055556
lon: -66.41166667
Bottoms Reservoir (Derbyshire). Bottoms Reservoir is a man-made lake in Longdendale in north Derbyshire, England. It was constructed between 1865 and 1877, by John Frederick Bateman as part of the Longdendale Chain of reservoirs to supply water from the River Etherow to the urban areas of Greater Manchester.

Geographic entities mentioned:
surface_form: Longdendale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.471666666666664
lon: -1.9505555555555554
Bottoms Reservoir (Derbyshire). Bottoms Reservoir is a man-made lake in Longdendale in north Derbyshire, England. It was constructed between 1865 and 1877, by John Frederick Bateman as part of the Longdendale Chain of reservoirs to supply water from the River Etherow to the urban areas of Greater Manchester.

Geographic entities mentioned:
surface_form: Longdendale Chain
instance_of: Group of lakes
countries: United Kingdom
coordinates: lat: 53.483333333333
lon: -1.9
The Bluff Point Stoneworks. The Bluff Point Stoneworks are a prehistoric structure located in the town of Jerusalem, New York, at the crux of Keuka Lake in the Finger Lakes region of western New York State. Though they were studied many times throughout the 20th century, the structure has been mostly destroyed, and it is still uncertain who built the structure.

Geographic entities mentioned:
surface_form: Keuka Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.496388888889
lon: -77.146111111111
surface_form: Finger Lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 42.666666666667
lon: -76.833333333333
Laghi del Gorzente. Laghi del Gorzente is a group of three lakes in north-west Italy which straddles the provinces of Genoa (in Liguria) and Alessandria (in Piedmont). Geography. The lowest lake is named &quot;Lago Bruno&quot; (647 m), while &quot;Lago Lungo&quot; is at 684 m and &quot;Lago Badana&quot; at 717 m. Nature conservation.

Geographic entities mentioned:
surface_form: lago lungo
instance_of: Lake
countries: Italy
coordinates: lat: 44.550555555556
lon: 8.8216666666667
surface_form: lago bruno
instance_of: Lake
countries: Italy
coordinates: lat: 44.550555555556
lon: 8.8216666666667
surface_form: lago badana
instance_of: Lake
countries: Italy
coordinates: lat: 44.550555555556
lon: 8.8216666666667
Laghi del Gorzente. Laghi del Gorzente is a group of three lakes in north-west Italy which straddles the provinces of Genoa (in Liguria) and Alessandria (in Piedmont). Geography. The lowest lake is named &quot;Lago Bruno&quot; (647 m), while &quot;Lago Lungo&quot; is at 684 m and &quot;Lago Badana&quot; at 717 m. Nature conservation.

Geographic entities mentioned:
surface_form: laghi del gorzente
instance_of: Lake
countries: Italy
coordinates: lat: 44.550555555556
lon: 8.8216666666667
Melaleuca wonganensis. &quot;Melaleuca wonganensis&quot; is an erect shrub in the myrtle family Myrtaceae and is endemic to the south-west of Western Australia. It is a shrub with narrow leaves and purple to deep mauve flowers and is restricted in its distribution to the Wongan Hills district. Description. &quot;Melaleuca wonganensis&quot; grows to a height of.

Geographic entities mentioned:
surface_form: Wongan Hills
instance_of: Mountain
countries: Australia
coordinates: lat: -30.8
lon: 116.617
It is part of Nyenchen Tanglha Shan, although it is sometimes included in Namcha Barwa Himal of the Himalayas. Gyala Peri lies just north of the Great Bend of the Yarlung Tsangpo River, the main river of southeastern Tibet, which becomes the Brahmaputra in India. It is NNW of the higher Namcha Barwa. Notable features.

Geographic entities mentioned:
surface_form: Namcha Barwa
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 29.630555555556
lon: 95.055277777778
surface_form: namcha barwa
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 29.630555555556
lon: 95.055277777778
Gyala Peri. Gyala Peri (Chinese: 加拉白垒, Pinyin: &quot;Jiālābáilěi&quot;) is a peak just beyond the eastern end of the Himalayas at the entrance to Tsangpo gorge. It is part of Nyenchen Tanglha Shan, although it is sometimes included in Namcha Barwa Himal of the Himalayas.

Geographic entities mentioned:
surface_form: namcha barwa
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 29.630555555556
lon: 95.055277777778
surface_form: nyenchen tanglha
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 30.38886944
lon: 90.56030278
It is NNW of the higher Namcha Barwa. Notable features. Gyala Peri has great vertical relief above the Tsangpo gorge and is the highest peak of the Nyenchen Tanglha Shan. Climbing history. The first ascent of Gyala Peri was in 1986, by a Japanese expedition, via the South Ridge. The group spent about 1 months on the mountain. The U.K. Alpine Club's Himalayan Index lists no other ascents.

Geographic entities mentioned:
surface_form: nyenchen tanglha
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 30.38886944
lon: 90.56030278
Gyala Peri. Gyala Peri (Chinese: 加拉白垒, Pinyin: &quot;Jiālābáilěi&quot;) is a peak just beyond the eastern end of the Himalayas at the entrance to Tsangpo gorge. It is part of Nyenchen Tanglha Shan, although it is sometimes included in Namcha Barwa Himal of the Himalayas.

Geographic entities mentioned:
surface_form: gyala peri
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 29.814166666667
lon: 94.968333333333
It is NNW of the higher Namcha Barwa. Notable features. Gyala Peri has great vertical relief above the Tsangpo gorge and is the highest peak of the Nyenchen Tanglha Shan. Climbing history. The first ascent of Gyala Peri was in 1986, by a Japanese expedition, via the South Ridge. The group spent about 1 months on the mountain. The U.K. Alpine Club's Himalayan Index lists no other ascents.

Geographic entities mentioned:
surface_form: gyala peri
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 29.814166666667
lon: 94.968333333333
The name is also spelled. The mountain is also called Nevado Coropuna; &quot;Nevado&quot; is the Spanish word for &quot;snowy&quot;. There is another volcano in the Andahua volcanic field which has the same name, but is completely separate. Geography and geomorphology. Coropuna lies in the Andes of Peru, on the border between the Castilla and Condesuyos Provinces of the Arequipa Department.

Geographic entities mentioned:
surface_form: Andahua volcanic field
instance_of: Mountain
countries: Peru
coordinates: lat: -15.257
lon: -72.483
Coropuna is in the Central Volcanic Zone of the Andes, which contains 44 stratovolcanoesincluding many of the world's highestand several glaciated volcanoes. Besides Coropuna, some of the latter are Sara Sara, Solimana, Mismi, Ampato, Hualca Hualca, Sabancaya, Chachani, Misti, Ubinas, Huaynaputina, Tutupaca, Yucamane and Casiri. Also found nearby are Neogene-age calderas.

Geographic entities mentioned:
surface_form: Sara Sara
instance_of: Mountain
countries: Peru
coordinates: lat: -15.323527777778
lon: -73.449361111111
surface_form: Mismi
instance_of: Mountain
countries: Peru
coordinates: lat: -15.525277777778
lon: -71.690833333333
surface_form: Ampato
instance_of: Mountain
countries: Peru
coordinates: lat: -15.820555555555556
lon: -71.88
surface_form: Hualca Hualca
instance_of: Mountain
countries: Peru
coordinates: lat: -15.816666666667
lon: -71.883333333333
surface_form: Chachani
instance_of: Mountain
countries: Peru
coordinates: lat: -16.194166666667
lon: -71.531666666667
surface_form: Misti
instance_of: Mountain
countries: Peru
coordinates: lat: -16.296388888888888
lon: -71.41055555555556
surface_form: Ubinas
instance_of: Mountain
countries: Peru
coordinates: lat: -16.34861111111111
lon: -70.90222222222222
surface_form: Huaynaputina
instance_of: Mountain
countries: Peru
coordinates: lat: -16.615555555555556
lon: -70.84972222222223
surface_form: Tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.02638889
lon: -70.37166667
surface_form: Yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
Ice cover makes discerning its structure difficult, but about six separate peaks as well as six not readily recognisable summit craters have been counted. Additional lava domes form a southeastward trending line on the southwestern side of the volcano and dikes crop out close to Lake Pallarcocha. Coropuna overlies the margin of a buried caldera.

Geographic entities mentioned:
surface_form: Pallarcocha
instance_of: Lake
countries: Peru
coordinates: lat: -15.57611111
lon: -72.72222222
A sector collapse took place on the southwestern flank and formed a landslide deposit as well as a horseshoe-shaped valley that was later filled by glaciers. Also on the southern side, mud-water flow deposits have been found in the Capiza River valley and appear to relate to Coropuna; at least eight such debris flows have been identified. Lahars (mudflows) have reached the Colca River valley.

Geographic entities mentioned:
surface_form: Colca River
instance_of: Watercourse
countries: Peru
coordinates: lat: -16.63206
lon: -72.76484
The volcano is situated on a drainage divide. Most of Coropuna drains to the Rio Arma west of the volcano, a tributary of the Ocoña River, while to the east, the Colca River is part of the Majes River watershed. An endorheic area that receives meltwater from the volcano also exists northeast from Coropuna, on Pampa Pucaylla where the lake of the same name lies.

Geographic entities mentioned:
surface_form: Ocoña River
instance_of: Watercourse
countries: Peru
coordinates: lat: -16.4525
lon: -73.111944444444
The region is characterised by high plateaus separated by deep canyons, including some of the world's deepest gorges that reach depths of. Apart from river erosion, giant landslides have affected the Altiplano below Coropuna, such as the Chuquibamba landslide, which took place over the last 120,000years in the form of multiple collapse events within a fault-controlled basin.

Geographic entities mentioned:
surface_form: Altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
Geomorphologically, Coropuna lies at the edge of the Altiplano high plateau on the Western Cordillera mountain range; in the Central Andes this mountain chain is split into two rangesthe western and the eastern Cordilleraseparated by the Altiplano. The Pucuncho Basin and Firura volcano lie north of Coropuna, while Solimana volcano is northwest from Coropuna.

Geographic entities mentioned:
surface_form: Firura
instance_of: Mountain
countries: Peru
coordinates: lat: -15.23608
lon: -72.64069
In 1910 it was believed that the volcano was over high and thus the highest mountain in South America, ahead of Aconcagua, although a North American expedition during the preceding year had determined that Coropuna was not the highest, as they only found an elevation of, and Huascaran is higher than this. Varying snow elevations might also lead to varying height estimates.

Geographic entities mentioned:
surface_form: Aconcagua
instance_of: Mountain
countries: Argentina
coordinates: lat: -32.653055555555554
lon: -70.01166666666667
Over longer timespans, precipitation in the region increases whenever iceberg discharge and cooling occur in the North Atlantic. This was the case during the Heinrich events and the Younger Dryas when lakes formed on the Bolivian Altiplano: The Sajsi formed about 25,000–19,000years ago, Tauca about 18,000–14,000 and Coipasa 13,000–11,000years ago.

Geographic entities mentioned:
surface_form: Tauca
instance_of: Lake
countries: Peru
coordinates: lat: -20
lon: -68
On the way on to the mountain, the souls are judged for their treatment of domestic animals and kitchen utensils. In Huaquira District mythology, the exhalations of the souls yield underground lakes, which return water to the living. In different mythologies Coropuna is instead the starting point for the deceased on a journey to Surimana. Coropuna and Solimana are often paired.

Geographic entities mentioned:
surface_form: Surimana
instance_of: Mountain
countries: Peru
coordinates: lat: -14.7717
lon: -72.4494
Line 1 is located in the northernmost borough of Gustavo A. Madero. It runs from the area serving the Indios Verdes STC Metro station to the Campos Revolución STC Metro station, where the line divides into two cables for transfer, one toward Cuautepec station and the other toward Tlalpexco station, in the Cerro del Chiquihuite. The ropeway installation for Line 1 was built by Doppelmayr Mexico.

Geographic entities mentioned:
surface_form: Cerro del Chiquihuite
instance_of: Mountain
countries: Mexico
coordinates: lat: 19.5328
lon: -99.1306
Atherton Tableland. The Atherton Tableland is a fertile plateau, which is part of the Great Dividing Range in Queensland, Australia. It has very deep, rich basaltic soils and the main industry is agriculture. The principal river flowing across the plateau is the Barron River, which was dammed to form the irrigation reservoir named Lake Tinaroo.

Geographic entities mentioned:
surface_form: atherton tableland
instance_of: Plateau
countries: Australia
coordinates: lat: -17.16666667
lon: 145.53333333
Since that time, the uplifted western portion has been slowly eroding westwards, creating the abrupt Great Escarpment, which separates the coastal plain to the east from the uplifted tablelands to the west. Between 4 million to less than 10,000 years ago, a series of volcanic eruptions occurred over the Atherton Tableland.

Geographic entities mentioned:
surface_form: atherton tableland
instance_of: Plateau
countries: Australia
coordinates: lat: -17.16666667
lon: 145.53333333
History. The Atherton Tableland has a long history of Indigenous occupation. Aspects of traditional Aboriginal land use and culture have been documented from the period of first contact to present.

Geographic entities mentioned:
surface_form: atherton tableland
instance_of: Plateau
countries: Australia
coordinates: lat: -17.16666667
lon: 145.53333333
&quot;Yidinji&quot; (also known as &quot;Yidinj&quot;, &quot;Yidiny&quot;, and &quot;Idindji&quot;) is a local Australian Aboriginal language. Its traditional region is within the local government areas of Cairns Region and Tablelands Region, in such localities as Cairns, Gordonvale, and the Mulgrave River, and the southern part of the Atherton Tableland including Atherton and Kairi.

Geographic entities mentioned:
surface_form: atherton tableland
instance_of: Plateau
countries: Australia
coordinates: lat: -17.16666667
lon: 145.53333333
Tree species used for the timber industry include red cedar, kauri, maple, black bean, walnut, white beech and red tulip oak. As part of the mining and timber booms a large population of Chinese-Australians moved into the Atherton Tableland region. In addition to mining and timber, the Chinese population took up agriculture.

Geographic entities mentioned:
surface_form: atherton tableland
instance_of: Plateau
countries: Australia
coordinates: lat: -17.16666667
lon: 145.53333333
Dyirbal (also known as Djirbal) is a language of Far North Queensland, particularly the area around Tully and Tully River Catchment extending to the Atherton Tablelands. The Dyirbal language region includes the landscape within the local government boundaries of Cassowary Coast Regional Council and Tablelands Regional Council.

Geographic entities mentioned:
surface_form: atherton tablelands
instance_of: Plateau
countries: Australia
coordinates: lat: -17.16666667
lon: 145.53333333
The deregulation of the dairy industry in 2000 is blamed for the decline. Tourism. Tourism is the second largest economic driver of the Atherton Tablelands economy, with Tinaroo Dam and extensive trail network being the focal point. Towns. Atherton and Mareeba are the largest towns in the area.

Geographic entities mentioned:
surface_form: atherton tablelands
instance_of: Plateau
countries: Australia
coordinates: lat: -17.16666667
lon: 145.53333333
Towns. Atherton and Mareeba are the largest towns in the area. Herberton, Kairi, Kuranda, Malanda, Millaa Millaa, Tinaroo, Tolga, Yungaburra, Chillagoe, Walkamin and Ravenshoe are also located on the Atherton Tablelands. Environment. The tableland contains several small remnants of the rainforest which once covered it, many of which are now protected in national parks.

Geographic entities mentioned:
surface_form: atherton tablelands
instance_of: Plateau
countries: Australia
coordinates: lat: -17.16666667
lon: 145.53333333
The municipality existed from 1869 until 1964. It included the land just north of the town of Steinkjer in what is now Steinkjer Municipality in Trøndelag county. The small municipality was south of the lake Snåsavatnet, west of the lake Fossemvatnet, and east of Beitstad Municipality. The main church for the municipality was Egge Church, just north of the town of Steinkjer.

Geographic entities mentioned:
surface_form: Snåsavatnet
instance_of: Lake
countries: Norway
coordinates: lat: 64.1874
lon: 12.0249
surface_form: Fossemvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 64.0626
lon: 11.6227
The reserve is home to over 1,300 plant species, including 112 species of trees and shrubs. Mountains and glaciers. The highest point is Talgar peak () within the Talgar massif, which is a powerful center of glaciation. Peaks-giants stand out with a special harsh beauty: Bogatyr (N-4626), Corp (N-4631), Aktau (N-4686), Metallurg (N-4600).

Geographic entities mentioned:
surface_form: Talgar peak
instance_of: Mountain
countries: Kazakhstan
Russian Empire
Soviet Union
coordinates: lat: 43.117838888889
lon: 77.341333333333
Steep Rock Lake. Steep Rock Lake is a body of water near the township of Atikokan, northern Ontario, Canada. It was originally fed by the Seine River. Geography. Steep Rock Lake and the surrounding region was carved out by retreating glaciers. The lake was carved out as a sprawling &quot;M&quot; shape and is 14 miles long with a surface area of 7 square miles.

Geographic entities mentioned:
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.4597
lon: -118.263
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.833333333333336
lon: -78.66666666666667
surface_form: steep rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.79
lon: -91.67
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.16916667
lon: -99.24694444
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.77775
lon: -94.41457
It was originally fed by the Seine River. Geography. Steep Rock Lake and the surrounding region was carved out by retreating glaciers. The lake was carved out as a sprawling &quot;M&quot; shape and is 14 miles long with a surface area of 7 square miles. The lake lies 6–7 km (4 miles) north of Atikokan and 215–225 km (135–140 miles) west of Thunder Bay.

Geographic entities mentioned:
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.4597
lon: -118.263
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.833333333333336
lon: -78.66666666666667
surface_form: steep rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.79
lon: -91.67
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.16916667
lon: -99.24694444
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.77775
lon: -94.41457
The ridges around the water rose 25 meters in places, often with visible outcrops of iron. The area straddles two major fault systems: The Quetico Fault and the Steep Rock Lake Fault systems. Active speculation about mining the area began as early as 1885, when land deposits were bought by the McKellar and Graham families.

Geographic entities mentioned:
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.4597
lon: -118.263
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.833333333333336
lon: -78.66666666666667
surface_form: steep rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.79
lon: -91.67
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.16916667
lon: -99.24694444
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.77775
lon: -94.41457
However, a patchwork terrain of deep soil, swamp land, and boulders hindered exploitation. Julian Cross, a mining prospector, later came to the area in 1926 and in 1937 through exploratory drilling located a major orebody under Steep Rock Lake. During World War II, a program was implemented to drain the lake.

Geographic entities mentioned:
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.4597
lon: -118.263
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.833333333333336
lon: -78.66666666666667
surface_form: steep rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.79
lon: -91.67
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.16916667
lon: -99.24694444
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.77775
lon: -94.41457
One result of this was a revival of iron-ore mining in Ontario, with one of the most difficult and spectacular mining projects ever undertaken in this country-and perhaps in any other. The first speculation of iron ore being under Steep Rock Lake was in 1891, when Professor Henry L. Smyth, of Harvard University, came across boulders containing iron ore on the south shore of the lake.

Geographic entities mentioned:
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.4597
lon: -118.263
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.833333333333336
lon: -78.66666666666667
surface_form: steep rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.79
lon: -91.67
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.16916667
lon: -99.24694444
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.77775
lon: -94.41457
Exploration and development would not occur until 1938. On January 6, 1938, Julian Cross and W.S. Morlock founded the Steerola Expedition Company Limited to finance a drilling project on Steep Rock Lake led by Julian Cross. In March of the same year, Cross discovered a body of iron ore under Steep Rock Lake after 6 test holes were drilled. The find confirmed what has previously been suspected.

Geographic entities mentioned:
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.4597
lon: -118.263
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.833333333333336
lon: -78.66666666666667
surface_form: steep rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.79
lon: -91.67
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.16916667
lon: -99.24694444
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.77775
lon: -94.41457
In March of the same year, Cross discovered a body of iron ore under Steep Rock Lake after 6 test holes were drilled. The find confirmed what has previously been suspected. In the summer of 1938, the sent a geological party to survey and map the Steep Rock Lake geology using an to outline the ore bodies.

Geographic entities mentioned:
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.4597
lon: -118.263
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.833333333333336
lon: -78.66666666666667
surface_form: steep rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.79
lon: -91.67
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.16916667
lon: -99.24694444
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.77775
lon: -94.41457
Morlock and R.D. Bradshaw were brought in during this period to be Directors of the company. Early Mining Efforts. In the early days of mining Steep Rock Lake, plans were made to sink a small shaft 1,400 ft. below the lake level and drill into the orebody to test the quality of the ore. July 1939 saw the of the No.1 shaft with Morson Scarth (Pop) Fotheringham, then a mining engineer, in charge.

Geographic entities mentioned:
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.4597
lon: -118.263
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.833333333333336
lon: -78.66666666666667
surface_form: steep rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.79
lon: -91.67
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.16916667
lon: -99.24694444
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.77775
lon: -94.41457
Donald Hogarth then stepped into the presidential role at Steep Rock Iron Mines. The Seine River Diversion. In March 1941, negotiations with the Ontario Government for the rights to dam off Steep Rock Lake were underway. The negotiations involved Steep Rock Iron Mines Limited, Ontario Hydro and Ontario-Minnesota Pulp and Paper Company.

Geographic entities mentioned:
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.4597
lon: -118.263
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.833333333333336
lon: -78.66666666666667
surface_form: steep rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.79
lon: -91.67
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.16916667
lon: -99.24694444
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.77775
lon: -94.41457
On July 23, 1943, a plug is blown at the bottom of Finlayson Lake which leads into a tunnel connecting to the Seine River to lower the water level in Finlayson. Through the fall of 1943, three dams were constructed and the first pumps were put into action in the middle arm of Steep Rock Lake to dewater that section. By May the water level had dropped 75 ft.

Geographic entities mentioned:
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.4597
lon: -118.263
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.833333333333336
lon: -78.66666666666667
surface_form: steep rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.79
lon: -91.67
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.16916667
lon: -99.24694444
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.77775
lon: -94.41457
By the new year, Both Raft and Finlayson Lakes had been drained to the required levels, dams were built-including the dam between Marmion Lake and Raft Lake known as the - and the cuts and canals had been completed. On January 28, 1944, the Raft Lake and Finlayson Diversion cuts were blown, which rerouted the water flow away from Steep Rock Lake.

Geographic entities mentioned:
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.4597
lon: -118.263
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.833333333333336
lon: -78.66666666666667
surface_form: steep rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.79
lon: -91.67
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.16916667
lon: -99.24694444
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.77775
lon: -94.41457
The lake was finally an isolated body of water and the job of pumping and mining the lake bottom could begin. &quot;B&quot; Ore Zone (Errington Mine). The spring and summer of 1944 saw the pumping of Steep Rock Lake to expose the lake bottom. To dredge the silt from the lake bottom to expose the ore body, a was modified with a suction dredge on it so that the dredging could begin.

Geographic entities mentioned:
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.4597
lon: -118.263
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.833333333333336
lon: -78.66666666666667
surface_form: steep rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.79
lon: -91.67
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.16916667
lon: -99.24694444
surface_form: rock lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.77775
lon: -94.41457
By May the water level had dropped 75 ft. Raft Lake (situated between Finlayson and Marmion Lake) was also lowered to connect the two larger lakes together to complete the diversion plan. All through the summer and winter of 1943, millions of tons of rock, gravel and earth were moved. More than a million cubic yards of rock had to be removed to create the canal between Raft Lake and Finlayson.

Geographic entities mentioned:
surface_form: marmion lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.873
lon: -91.53
When completed, it was six hundred yards long, a hundred feet wide, and as much as ninety feet deep in places. By the new year, Both Raft and Finlayson Lakes had been drained to the required levels, dams were built-including the dam between Marmion Lake and Raft Lake known as the - and the cuts and canals had been completed.

Geographic entities mentioned:
surface_form: marmion lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.873
lon: -91.53
The remnant of this giant mountain is now a ridge. Bandung basin. The Bandung basin is an ellipse-formed geological basin measuring 60 kilometres east-west, and 40 kilometres north-south, spanning from Padalarang in the west to Nagreg in the east, from Mount Tangkuban Perahu in the north to Mount Malabar in the south.

Geographic entities mentioned:
surface_form: Tangkuban Perahu
instance_of: Mountain
countries: Indonesia
coordinates: lat: -6.77
lon: 107.6
surface_form: Mount Malabar
instance_of: Mountain
countries: Indonesia
coordinates: lat: -7.13
lon: 107.65
The Lake is estimated to stretch from Cicalengka to Padalarang, as well as from Dago to the border of Soreang and Ciwidey, so that the area of this ancient lake is estimated to reach almost 3 times the area of DKI Jakarta Province, with the average depth of the lake estimated to be around 20-30 metres. The formation of the lake went further through the eruption of Mount Sunda.

Geographic entities mentioned:
surface_form: Mount Sunda
instance_of: Mountain
countries: Indonesia
coordinates: lat: -6.43
lon: 107.32
Legend. There is a Sundanese legend of Sangkuriang that mentions the existence of the lake, as well as the mythical origin on the lake's creation and Mount Tangkuban Perahu. This might suggest the collective native Sundanese memories about the lake's existence, transmitted through oral tradition in the Pantun Sunda through the ages.

Geographic entities mentioned:
surface_form: Tangkuban Perahu
instance_of: Mountain
countries: Indonesia
coordinates: lat: -6.77
lon: 107.6
Rào Cỏ Mountain. Rào Cỏ mountain (Vietnamese: &quot;Núi Rào Cỏ&quot;) is a mountain in Southeast Asia. It is one of the ultra prominent peaks of Southeast Asia. The mountain is 2,286 metres tall and sits on the international border between Laos and Vietnam.

Geographic entities mentioned:
surface_form: núi rào cỏ
instance_of: Mountain
countries: Vietnam
Laos
coordinates: lat: 18.15
lon: 105.58333333
surface_form: rào cỏ
instance_of: Mountain
countries: Vietnam
Laos
coordinates: lat: 18.15
lon: 105.58333333
surface_form: rào cỏ
instance_of: Mountain
countries: Vietnam
Laos
coordinates: lat: 18.15
lon: 105.58333333
Rào Cỏ Mountain. Rào Cỏ mountain (Vietnamese: &quot;Núi Rào Cỏ&quot;) is a mountain in Southeast Asia. It is one of the ultra prominent peaks of Southeast Asia. The mountain is 2,286 metres tall and sits on the international border between Laos and Vietnam.

Geographic entities mentioned:
surface_form: rào cỏ
instance_of: Mountain
countries: Vietnam
Laos
coordinates: lat: 18.15
lon: 105.58333333
Bagian received his Professional Engineers Certification in 1986 and was board-certified in aerospace medicine by the American College of Preventive Medicine in 1987. Since 1981, Bagian has been active in the mountain rescue community and has served as a member of the Denali Medical Research Project on Denali.

Geographic entities mentioned:
surface_form: Denali
instance_of: Mountain
countries: United States
coordinates: lat: 63.06916666666667
lon: -151.0063888888889
Since 1981, Bagian has been active in the mountain rescue community and has served as a member of the Denali Medical Research Project on Denali. He has been a snow-and-ice rescue techniques instructor on Mount Hood during this period. Bagian is a colonel in the U.S. Air Force Reserve and is the pararescue flight surgeon for the 939th Air Rescue Wing.

Geographic entities mentioned:
surface_form: Mount Hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
The river drains a broad valley south of the Alaska Range eponymously known as the Matanuska Valley. Course. Formed by the confluence of its east and south forks, the Matanuska River flows generally southwest to the Knik Arm of Cook Inlet. Downstream of its source, the river is joined by meltwater from Matanuska Glacier in the northern Chugach Mountains.

Geographic entities mentioned:
surface_form: Knik Arm
instance_of: Body of water
countries: United States
coordinates: lat: 61.2
lon: -150.217
From there it continues through the Matanuska Valley, between the Chugach Mountains to the south and the Talkeetna Mountains to the north. Population centers along its course include Chickaloon, Sutton, Palmer, and Butte. It enters the Knik Arm of Cook Inlet about southwest of Palmer and about northeast of Anchorage. The Glenn Highway runs roughly parallel to the river for much of its length.

Geographic entities mentioned:
surface_form: Knik Arm
instance_of: Body of water
countries: United States
coordinates: lat: 61.2
lon: -150.217
Lake Sidihoni. Lake Sidihoni is a lake located within Samosir Island which itself is an island within Lake Toba, in North Sumatra, Indonesia and is therefore notable for being a &quot;lake on an island in a lake on an island&quot;. It is approximately 11–12 km to the east of hot spring pools at Pangururan.

Geographic entities mentioned:
surface_form: lake sidihoni
instance_of: Lake
countries: Indonesia
coordinates: lat: 2.6014833333333
lon: 98.744763888889
&quot;Jutom-puszta&quot;, &quot;Csillag-puszta&quot;, &quot;Tomé-puszta&quot; and &quot;Kovászna&quot; are all parts of Nágocs. Geography. It lies in the middle of the &quot;Outer Somogy Hill Range&quot;, 25 km far from Lake Balaton and 35 km from Kaposvár. Its neighbors are Kapoly to the North, Andocs to the West, Somogyacsa to the South, Zics, Miklósi and Kára to the East.

Geographic entities mentioned:
surface_form: Lake Balaton
instance_of: Lake
countries: Hungary
coordinates: lat: 46.85
lon: 17.72
The general elevational range of the Vindhyas is between 450 and 600 m though a few points rise above 900 m. In contrast, the Satpuras are marked with higher elevation plateaus, the highest peak being Dhupgarh (1348 m). The Central Indian Highlands serve as a major watershed area for several rivers including the Narmada, Chambal, Betwa, Tons, Ken, Sone, Wainganga, Wardha, and Tapti rivers.

Geographic entities mentioned:
surface_form: Dhupgarh
instance_of: Mountain
countries: India
coordinates: lat: 22.44944444
lon: 78.37305556
Family. He was the eldest son and heir of Robert Lauder of the Bass and Margaret Sinclair. He is first mentioned in a feu renewal made by Andrew Forman, Archbishop of St Andrews, to his grandfather, Sir Robert Lauder of Bass, of the barony and lands of Tyninghame on 28 July 1517, when his name appears in the list of heirs and successors. He must have been an infant.

Geographic entities mentioned:
surface_form: Bass
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.08
lon: -2.64
Monte Chierico. Monte Chierico is a mountain of Lombardy, Italy. It is located within the Bergamo Alps.

Geographic entities mentioned:
surface_form: monte chierico
instance_of: Mountain
countries: Italy
coordinates: lat: 46.045
lon: 9.80861111
As of 2025, the university has approximately 1,800 undergraduate and graduate students. Karcher Mall opened in 1965, the first enclosed shopping mall in the Treasure Valley. It was &quot;the place to gather&quot; for several decades until the Boise Towne Square mall was built in Boise in 1988, drawing business away. Karcher Mall was renamed District 208 in 2022.

Geographic entities mentioned:
surface_form: Treasure Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.0403
lon: -116.933
She worked with hike organizer Caroline Hinman or mountain guide Christian Haesler Jr., and with the Alpine Club of Canada. She and British climber Kate Gardiner climbed Mount Bryce and Quéant Mountain in 1937; Polly Prescott and Marguerite Schnellbacher were other climbing companions. She climbed Mount Columbia in 1938.

Geographic entities mentioned:
surface_form: Mount Bryce
instance_of: Mountain
countries: Canada
coordinates: lat: 52.041111111111114
lon: -117.33027777777778
surface_form: Quéant Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 52.0083
lon: -117.24
Konnivesi. Konnivesi is a medium-sized lake of Finland in the Kymijoki main catchment area. It is located partly in region Päijänne Tavastia, near the town Heinola, partly in region Kymenlaakso. There is a waterway crossing the Heinola town and connecting the lake to another lake Ruotsalainen.

Geographic entities mentioned:
surface_form: ruotsalainen
instance_of: Lake
countries: Finland
coordinates: lat: 61.233333
lon: 25.916667
Konnivesi. Konnivesi is a medium-sized lake of Finland in the Kymijoki main catchment area. It is located partly in region Päijänne Tavastia, near the town Heinola, partly in region Kymenlaakso. There is a waterway crossing the Heinola town and connecting the lake to another lake Ruotsalainen.

Geographic entities mentioned:
surface_form: konnivesi
instance_of: Lake
countries: Finland
coordinates: lat: 61.166667
lon: 26.15
Biography. Pace Pasini was the son of Pietro, a descendant of a family originally from Valle Sabbia, who had moved to Schio and then to Vicenza, where he was ascribed to the Noble Council of the city. In the mid-seventeenth century - around the time of Pace's death - a member of the Pasini family from Vicenza figured among the merchants of silk and thick cloths.

Geographic entities mentioned:
surface_form: Valle Sabbia
instance_of: Valley
countries: Italy
coordinates: lat: 45.7158
lon: 10.4181
Kuruman can be found in the north-east and is known as a mission station. It is also well known for its artesian spring and Eye of Kuruman. The Orange River flows through the province, forming the borders with the Free State in the southeast and with Namibia to the northwest. The river is also used to irrigate the many vineyards in the arid region near Upington.

Geographic entities mentioned:
surface_form: Eye of Kuruman
instance_of: Lake
countries: South Africa
coordinates: lat: -27.4635
lon: 23.4363
Minorities speak the other official languages of South Africa and a few people speak indigenous languages such as Nama and Khwe. The provincial motto, &quot;Sa ǁa ǃaĩsi 'uĩsi&quot; (&quot;We go to a better life&quot;), is in the Nǀu language of the Nǁnǂe (ǂKhomani) people. It was given in 1997 by one of the language's last speakers, Ms. Elsie Vaalbooi of Rietfontein, who has since died.

Geographic entities mentioned:
surface_form: Rietfontein
instance_of: Mountain
countries: South Africa
coordinates: lat: -26.7333
lon: 20.0333
The Northern Cape is also the home of over 1,000 San who emigrated from Namibia following the independence of the country; they had served as trackers and scouts for the South African Defence Force during the South African Border War, and feared reprisals from their former foes. They were awarded a settlement in Platfontein in 1999 by the Mandela government.

Geographic entities mentioned:
surface_form: Platfontein
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.5167
lon: 24.0517
Lotru. The Lotru is a right tributary of the river Olt in Romania. Its source is in the Parâng Mountains. It feeds the reservoirs Vidra, Malaia and Brădișor. It flows into the Olt in Golotreni, near the town of Brezoi. It passes through the communes Voineasa, Malaia, and Brezoi. Its length is and its basin size is. Tributaries.

Geographic entities mentioned:
surface_form: Vidra
instance_of: Lake
countries: Romania
coordinates: lat: 45.430555555556
lon: 23.733333333333
Titusville is located in the northern half of Brevard County. According to the US Census Bureau, the city has a total area of. of it is land, and of it (14.26 percent) is water. Titusville is located on the Indian River Lagoon, part of the Atlantic Intracoastal Waterway. Flora. The city is the only place in the world where the endangered Dicerandra thinicola, or &quot;Titusville mint&quot; grows.

Geographic entities mentioned:
surface_form: Indian River Lagoon
instance_of: Body of water
countries: United States
coordinates: lat: 28.05527778
lon: -80.57611111
Following the storm, there was a moratorium on clamming in the state's bays, due to contaminated waters. Along the Delmarva Peninsula and Virginia Beach, there was widespread water damage to homes, including ten affected houses in the Sandbridge Beach area of Virginia Beach, Virginia.

Geographic entities mentioned:
surface_form: Sandbridge Beach
instance_of: Landform
countries: United States
coordinates: lat: 36.746111111111
lon: -75.944166666667
The dialect belongs to the Lower Carniolan dialect group, and it evolved from the Lower Carniolan dialect base. Geographical distribution. The area where the Lower Carniolan dialect is spoken spans from the Javornik Hills and Snežnik Plateau in the west to Orehovec, Škocjan, and Polšnik in the east, and to the Sava River and Ljubljana Marsh in the north.

Geographic entities mentioned:
surface_form: Javornik Hills
instance_of: Plateau
countries: Slovenia
coordinates: lat: 45.73333333
lon: 14.28333333
As the Yellowstone river flows north from Yellowstone Lake, it leaves the Hayden Valley and plunges first over Upper Falls of the Yellowstone River and then downstream over Lower Falls of the Yellowstone River, at which point it then enters the Grand Canyon of the Yellowstone, which is up to deep. Upper Falls. The Upper Falls of the Yellowstone River () are high.

Geographic entities mentioned:
surface_form: Yellowstone Lake
instance_of: Lake
countries: United States
coordinates: lat: 44.466666666667
lon: -110.36666666667
surface_form: Hayden Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.6439
lon: -110.456
Iliamna bakeri. &quot;Iliamna bakeri&quot; is an uncommon species of flowering plant in the mallow family known by the common names Baker's globe mallow and Baker's wild hollyhock. It is endemic to northeastern California and southeastern Oregon. It grows in the Southern Cascade Range and Modoc Plateau forests and woodlands on volcanic soils. Description.

Geographic entities mentioned:
surface_form: Modoc Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 41.6
lon: -121.2
Built at a cost of, this facility consists of seven huge sheds, including one the size of an aircraft hangar, within which are housed artefacts as a section of the mast of, Nelson's flagship at the Battle of Trafalgar, and the spare wheel from &quot;Bluebird-Proteus CN7&quot;, the car Donald Campbell drove to break the world land speed record on Lake Eyre in the 1960s.

Geographic entities mentioned:
surface_form: Lake Eyre
instance_of: Lake
countries: Australia
coordinates: lat: -28.406
lon: 137.2963
The participants of the excursion, including Zamenhof and Bujwid, traveled by carriage to the after lunch. In the evening, they attended a reception hosted by the marshal of Nowy Targ County, Dr.. On Monday morning, the guests went to the Kościeliska Valley and then visited Dr. Kazimierz Dłuski's sanatorium.

Geographic entities mentioned:
surface_form: Kościeliska Valley
instance_of: Valley
countries: Poland
coordinates: lat: 49.2539
lon: 19.8669
In the evening, they attended a reception hosted by the marshal of Nowy Targ County, Dr.. On Monday morning, the guests went to the Kościeliska Valley and then visited Dr. Kazimierz Dłuski's sanatorium. After lunch at the Morskie Oko hotel, they visited the Tatra Museum, and the Jaworzynka Valley.

Geographic entities mentioned:
surface_form: Morskie Oko
instance_of: Lake
countries: Poland
coordinates: lat: 49.197222222222
lon: 20.070833333333
surface_form: Jaworzynka Valley
instance_of: Valley
countries: Poland
coordinates: lat: 49.2597
lon: 19.9883
WTAK-FM. WTAK-FM (106.1 MHz) is a classic rock-formatted radio station licensed to Hartselle, Alabama, and owned by San Antoniobased iHeartMedia, Inc. It serves Huntsville, Alabama, and the central Tennessee Valley area. Its broadcast tower is located on Brindlee Mountain in Morgan County, Alabama, near the Union Hill community, and its studios are located in Madison, Alabama.

Geographic entities mentioned:
surface_form: Tennessee Valley
instance_of: Valley
countries: United States
coordinates: lat: 35.959166666667
lon: -83.850277777778
The kings normally left the defeat of these enemies to their aristocratic vassals. The interior of the province from the Great Glen to Strathbogie was divided between six or more families, the greatest of which, at this time was the Clan Comyn lords of Badenoch and Lochaber. 1296 to 1346: Wars of Independence and creation of the earldom of Moray.

Geographic entities mentioned:
surface_form: Great Glen
instance_of: Valley
countries: United Kingdom
coordinates: lat: 57.3
lon: -4.45
A few may survive a second winter. Range and population level. Known only from Lake Waccamaw and the upper Waccamaw River in Columbus County, North Carolina, the silverside is found in the upper Waccamaw River only during periods of high water and is not a permanent resident.

Geographic entities mentioned:
surface_form: Lake Waccamaw
instance_of: Lake
countries: United States
coordinates: lat: 34.2867009
lon: -78.509745