Sarmila/GeoWiki-Features huggingface dataset:
Davis Valley and other, adjacent ice-free valleys, forms one of the most southerly ‘dry valley’ systems on the continent and has exceptional scientific value for the interpretation of past glacial events and climate in this part of Antarctica. With Forlidas Pond some away, the site is protected under the Antarctic Treaty System as Antarctic Specially Protected Area (ASPA) No.119. Preslik Spur.

Geographic entities mentioned:
surface_form: Forlidas Pond
instance_of: Lake
coordinates: lat: -82.45
lon: -51.35
surface_form: pond
instance_of: Mountain
coordinates: lat: -62.95
lon: -60.55
Preslik Spur. An ice-free spur lying south of Clemons Spur and Forlidas Ridge. Named by US-ACAN, at the suggestion of USGS party leader Arthur B. Ford, after Private First Class Joseph W. Preslik, a member of the United States Army Aviation Detachment with the USGS Pensacola Mountains survey, 1965-66. Kistler Valley. A mostly ice-filled valley in the east-central part of the Dufek Massif.

Geographic entities mentioned:
surface_form: arthur
instance_of: Mountain
coordinates: lat: -67.65
lon: 49.86667
Clemons Spur. A bare rock spur next south of Forlidas Ridge. Named at the suggestion of party leader Arthur B. Ford, USGS, after Samuel D. Clemons, steward, United States Navy Squadron VXE-6, with the USGS Pensacola Mountains survey, 1965-66. Forlidas Ridge. A rock ridge that forms the west side of Davis Valley. Mapped by USGS from surveys and United States Navy air photos, 1956-66.

Geographic entities mentioned:
surface_form: arthur
instance_of: Mountain
coordinates: lat: -67.65
lon: 49.86667
The only pond in the northern Pensacola Mountains, it is of much interest to biologists. The pond was discovered and briefly investigated in December 1957 by a US-IGY party from Ellsworth Station. The name is in association with Forlidas Ridge and was suggested by Arthur B. Ford of USGS following geological work in the area, 1978-79. Wujek Ridge.

Geographic entities mentioned:
surface_form: arthur
instance_of: Mountain
coordinates: lat: -67.65
lon: 49.86667
Location. David Valley is towards the northeast of the Dufek Massif, between Jaeger Table to the southwest and Boyd Escarpment to the northeast. The Ford Ice Piedmont is to the north and the Sallee Snowfield is to the south. Features include Preslik Spur, Clemons Spur, Edge Glacier, Forlidas Ridge, Forlidas Pond and Wujeck Ridge. Antarctic Specially Protected Area.

Geographic entities mentioned:
surface_form: pond
instance_of: Mountain
coordinates: lat: -62.95
lon: -60.55
surface_form: forlidas pond
instance_of: Lake
coordinates: lat: -82.45
lon: -51.35
Mapped by USGS from surveys and United States Navy air photos, 1956-66. Named by US-ACAN after Charles W. Forlidas, radioman, Ellsworth Station winter party, 1957. Forlidas Pond. A round frozen pond, in diameter, lying in a morainal valley east of the north end of Forlidas Ridge. The only pond in the northern Pensacola Mountains, it is of much interest to biologists.

Geographic entities mentioned:
surface_form: pond
instance_of: Mountain
coordinates: lat: -62.95
lon: -60.55
surface_form: forlidas pond
instance_of: Lake
coordinates: lat: -82.45
lon: -51.35
Forlidas, radioman, Ellsworth Station winter party, 1957. Forlidas Pond. A round frozen pond, in diameter, lying in a morainal valley east of the north end of Forlidas Ridge. The only pond in the northern Pensacola Mountains, it is of much interest to biologists. The pond was discovered and briefly investigated in December 1957 by a US-IGY party from Ellsworth Station.

Geographic entities mentioned:
surface_form: pond
instance_of: Mountain
coordinates: lat: -62.95
lon: -60.55
Forlidas Pond. A round frozen pond, in diameter, lying in a morainal valley east of the north end of Forlidas Ridge. The only pond in the northern Pensacola Mountains, it is of much interest to biologists. The pond was discovered and briefly investigated in December 1957 by a US-IGY party from Ellsworth Station. The name is in association with Forlidas Ridge and was suggested by Arthur B.

Geographic entities mentioned:
surface_form: pond
instance_of: Mountain
coordinates: lat: -62.95
lon: -60.55
Davis Valley. Davis Valley () is an ice-free valley just east of Floridas Ridge in north-east Dufek Massif, in the Pensacola Mountains, Antarctica. Mapping and name. Davis Valley was mapped by the United States Geological Survey (USGS) from surveys and United States Navy air photos in 1956–66. It was named by the United States Advisory Committee on Antarctic Names (US-ACAN) for Edward H.

Geographic entities mentioned:
surface_form: davis valley
instance_of: Valley
coordinates: lat: -82.4667
lon: -51.15
surface_form: davis
instance_of: Mountain
coordinates: lat: -78.1
lon: -86.25
Features include Preslik Spur, Clemons Spur, Edge Glacier, Forlidas Ridge, Forlidas Pond and Wujeck Ridge. Antarctic Specially Protected Area. Davis Valley and other, adjacent ice-free valleys, forms one of the most southerly ‘dry valley’ systems on the continent and has exceptional scientific value for the interpretation of past glacial events and climate in this part of Antarctica.

Geographic entities mentioned:
surface_form: davis valley
instance_of: Valley
coordinates: lat: -82.4667
lon: -51.15
surface_form: davis
instance_of: Mountain
coordinates: lat: -78.1
lon: -86.25
Ford, USGS, after Samuel D. Clemons, steward, United States Navy Squadron VXE-6, with the USGS Pensacola Mountains survey, 1965-66. Forlidas Ridge. A rock ridge that forms the west side of Davis Valley. Mapped by USGS from surveys and United States Navy air photos, 1956-66. Named by US-ACAN after Charles W. Forlidas, radioman, Ellsworth Station winter party, 1957. Forlidas Pond.

Geographic entities mentioned:
surface_form: davis valley
instance_of: Valley
coordinates: lat: -82.4667
lon: -51.15
surface_form: davis
instance_of: Mountain
coordinates: lat: -78.1
lon: -86.25
Ford of USGS following geological work in the area, 1978-79. Wujek Ridge. A rock ridge trending north–south and marking the east extent of Davis Valley. Named by US-ACAN in 1979 after CWO Stanley J. Wujek, United States Army, helicopter pilot of the Army Aviation Detachment which supported the USGS Pensacola Mountains survey, 1965-66.

Geographic entities mentioned:
surface_form: davis valley
instance_of: Valley
coordinates: lat: -82.4667
lon: -51.15
surface_form: davis
instance_of: Mountain
coordinates: lat: -78.1
lon: -86.25
Forlidas Ridge. A rock ridge that forms the west side of Davis Valley. Mapped by USGS from surveys and United States Navy air photos, 1956-66. Named by US-ACAN after Charles W. Forlidas, radioman, Ellsworth Station winter party, 1957. Forlidas Pond. A round frozen pond, in diameter, lying in a morainal valley east of the north end of Forlidas Ridge.

Geographic entities mentioned:
surface_form: charles
instance_of: Mountain
coordinates: lat: -67.38333
lon: 50
Mapping and name. Davis Valley was mapped by the United States Geological Survey (USGS) from surveys and United States Navy air photos in 1956–66. It was named by the United States Advisory Committee on Antarctic Names (US-ACAN) for Edward H. Davis, a construction mechanic with the Ellsworth Station winter party in 1957. Location.

Geographic entities mentioned:
surface_form: davis
instance_of: Mountain
coordinates: lat: -78.1
lon: -86.25
It is a right tributary of the river Rhume and long. Geography. The Söse rises on the plateau of &quot;Auf dem Acker&quot; in the district of Göttingen in the southwestern part of the Harz Mountains in Germany. From there it flows initially westwards; and is then impounded at a pre-dam and then by the Söse Dam between the Osterode village of Riefensbeek and the town of Osterode itself.

Geographic entities mentioned:
surface_form: Auf dem Acker
instance_of: Mountain
countries: Germany
coordinates: lat: 51.7488
lon: 10.4453
River Cladagh. The Cladagh River () is a small river in County Fermanagh, formed from three rivers and a number of streams draining off the northern slopes of Cuilcagh mountain, which combine underground in the Marble Arch Cave system.

Geographic entities mentioned:
surface_form: Cuilcagh
instance_of: Mountain
countries: United Kingdom
Ireland
coordinates: lat: 54.2
lon: -7.811
Camille D'Arcy. Camille D'Arcy (1879 – September 26, 1916) was an American stage and silent film actress. In film she played matronly or character roles; all of her film appearances were with the Essanay Company of Chicago. In private life she was married to Dr. Loren Wilder. In the fall of 1916 she went swimming in Lake Michigan, caught an infection and died at age 37 in Chicago.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Hills Ferry, California. Hills Ferry was a small unincorporated community of the northern San Joaquin Valley in Stanislaus County, California. Hills Ferry was located at, on the southern border of Stanislaus County with Merced County, northeast of the city of Newman. Hills Ferry is just west of the river mouth of the Merced River, at its confluence with the San Joaquin River. History.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
Although he was a lieutenant in the infantry reserve upon the outbreak of World War II, he was not called up because of his civil-service role. In October 1940, he was dismissed by the Vichy régime which suspected him of anti-Vichy feelings (&quot;mal penser&quot;) and returned to the &quot;Conseil d'État&quot; now in the Puy de Dôme.

Geographic entities mentioned:
surface_form: Puy de Dôme
instance_of: Mountain
countries: France
coordinates: lat: 45.772
lon: 2.9624
Big Silver Creek. oc8gghavqty52wu5ptix99d3p8zvy" xml:space="preserve">The Silver River, aka the Big Silver River and Big Silver Creek, or zácta in the St'at'imcets language of the In-SHUCK-ch people, is the second-largest stream entering Harrison Lake in the Lower Mainland of British Columbia, Canada (the largest is the 209-km long Lillooet River, at the head of the lake).

Geographic entities mentioned:
surface_form: Harrison Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.55
lon: -121.83333333333
There are number of tracks that run up from the Edburton Road, including the Edburton bostal, Perching bostal and Fulking bostal. Devil's Dyke and surrounding woodland. Devil's Dyke (area eight) itself is also in unfavourable but recovering condition, but is geologically important as an example of Pleistocene erosion of a dry chalk valley. The adjacent two areas are categorised as woodland.

Geographic entities mentioned:
surface_form: Devil's Dyke
instance_of: Valley
countries: United Kingdom
coordinates: lat: 50.885
lon: -0.205
Caspian tadpole goby. The Caspian tadpole goby (&quot;Benthophilus macrocephalus&quot;) is a species of goby which is widespread in the basin of the Caspian Sea, specifically in the near-estuary zone of the rivers and in small bays. It is a common species in the Volga River delta near Astrakhan, occurred in the deltas of rivers Terek, Ural, Samur.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
Lūšna. Lūšna is a lake in Northwest Lithuania, Rokiškis District Municipality, about south-east of Rokiškis. It is the origin of Nemunėlis River.

Geographic entities mentioned:
surface_form: lūšna
instance_of: Lake
countries: Lithuania
coordinates: lat: 55.9108
lon: 25.6022
Yanacucho. Yanacucho (Quechua &quot;yana&quot; black, &quot;k'uchu&quot; corner, &quot;black corner&quot;) is a mountain in the Vilcanota mountain range in the Andes of Peru, about high. It is situated in the Cusco Region, Canchis Province, Pitumarca District. Yanacucho lies southwest of the mountain named Comercocha and northwest of Cóndor Tuco.

Geographic entities mentioned:
surface_form: Cóndor Tuco
instance_of: Mountain
countries: Peru
coordinates: lat: -13.84916667
lon: -71.13527778
surface_form: tuco
instance_of: Mountain
countries: Peru
coordinates: lat: -10.008888888889
lon: -77.176111111111
surface_form: comercocha
instance_of: Mountain
countries: Peru
coordinates: lat: -14.03027778
lon: -70.91638889
surface_form: cóndor tuco
instance_of: Mountain
countries: Peru
coordinates: lat: -13.84916667
lon: -71.13527778
Yanacucho. Yanacucho (Quechua &quot;yana&quot; black, &quot;k'uchu&quot; corner, &quot;black corner&quot;) is a mountain in the Vilcanota mountain range in the Andes of Peru, about high. It is situated in the Cusco Region, Canchis Province, Pitumarca District. Yanacucho lies southwest of the mountain named Comercocha and northwest of Cóndor Tuco.

Geographic entities mentioned:
surface_form: yanacucho
instance_of: Mountain
countries: Peru
coordinates: lat: -13.82777778
lon: -71.15416667
In both inscriptions, Veraudunus is invoked along with Inciona. On the large stone slab from Mensdorf on the Widdebierg, pictured at right, the god Veraudunus (DEO VERAVDVNO) and Inciona are invoked in honour of the imperial family in fulfilment of a vow made by Marcus Pl(autius?) Restitutus' mother Alpinia Lucana.

Geographic entities mentioned:
surface_form: Widdebierg
instance_of: Mountain
countries: Luxembourg
coordinates: lat: 49.662
lon: 6.315
It was located to the northwest of Derbent, a little inland from the Caspian Sea coast, and was founded in order to provide for a secure base against constant raids during his difficult campaign in Dagestan. According to the modern historian Michael Axworthy, Nader's bitter decision to name the camp &quot;Ruin of Iran&quot; was &quot;hardly encouraging for his troops&quot;.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
Copper smelting is also documented at this site at about the same time period (soon after 6000 BC). However, the use of lead seems to precede copper smelting. Early metallurgy is also documented at the nearby site of Tell Maghzaliyah, which seems to be dated even earlier, and completely lacks pottery. The Timna Valley contains evidence of copper mining in 7000–5000 BC.

Geographic entities mentioned:
surface_form: Timna Valley
instance_of: Valley
countries: Israel
coordinates: lat: 29.78777778
lon: 34.98888889
The largest of the resorts was The Lyndale, which opened in 1883 but was destroyed by fire in 1885. Even before its destruction, The Lyndale had struggled to compete with resorts on Lake Minnetonka, and it was not rebuilt. Over time, the railway lost money and was sold to the Minneapolis Street Railway in 1887.

Geographic entities mentioned:
surface_form: Lake Minnetonka
instance_of: Lake
countries: United States
coordinates: lat: 44.933333333333
lon: -93.566666666667
surface_form: lake minnetonka
instance_of: Lake
countries: United States
coordinates: lat: 44.933333333333
lon: -93.566666666667
Lake and surrounding area. Bde Maka Ska is part of the Grand Rounds National Scenic Byway, connecting with Lake of the Isles on the northeast, Cedar Lake and Brownie Lake on the northwest, and Lake Harriet on the south. The Minneapolis Park and Recreation Board trail system has a trail around the lake for bicyclists and skaters and a trail around it for pedestrians.

Geographic entities mentioned:
surface_form: Lake of the Isles
instance_of: Lake
countries: United States
coordinates: lat: 44.954722
lon: -93.3075
surface_form: Brownie Lake
instance_of: Body of water
countries: United States
coordinates: lat: 44.9675
lon: -93.32444444444444
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: brownie lake
instance_of: Body of water
countries: United States
coordinates: lat: 44.9675
lon: -93.32444444444444
surface_form: lake of the isles
instance_of: Lake
countries: United States
coordinates: lat: 44.954722
lon: -93.3075
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3743
lon: -74.3212
surface_form: lake harriet
instance_of: Lake
countries: United States
coordinates: lat: 44.921388888889
lon: -93.305277777778
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
This public sentiment led the Minneapolis Park and Recreation Board to dredge the Chain of Lakes, including Bde Maka Ska. This dredging formed much of the landscape around Bde Maka Ska today. In 1906, the MPRB began connecting Cedar Lake, Lake of the Isles, and Bde Maka Ska with channels. When the project was completed in 1911, over 100,000 people celebrated its opening.

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: lake of the isles
instance_of: Lake
countries: United States
coordinates: lat: 44.954722
lon: -93.3075
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3743
lon: -74.3212
surface_form: bde maka ska
instance_of: Lake
countries: United States
coordinates: lat: 44.941944444444
lon: -93.312222222222
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
Bde Maka Ska. Bde Maka Ska (, previously named Lake Calhoun) is the largest lake in Minneapolis, Minnesota, United States, and part of the city's Chain of Lakes. Surrounded by city park land and circled by bike and walking trails, it is popular for many outdoor activities. The lake has an area of and a maximum depth of. Geology.

Geographic entities mentioned:
surface_form: lake calhoun
instance_of: Lake
countries: United States
coordinates: lat: 45.27305556
lon: -94.8325
surface_form: bde maka ska
instance_of: Lake
countries: United States
coordinates: lat: 44.941944444444
lon: -93.312222222222
surface_form: lake calhoun
instance_of: Lake
countries: United States
coordinates: lat: 44.941944444444
lon: -93.312222222222
surface_form: chain of lakes
instance_of: Group of lakes
Lake
countries: United States
coordinates: lat: 44.982536
lon: -97.2713448
Another Dakota name for the lake may have been, the name initially adopted by settlers, either as &quot;Lake Medoza&quot; or in translation as &quot;Loon Lake&quot;. The Dakota also described it as, meaning &quot;the set back lake&quot;. Calhoun naming. United States Secretary of War John C. Calhoun sent the Army to survey the area surrounding Fort Snelling in 1817.

Geographic entities mentioned:
surface_form: loon lake
instance_of: Lake
countries: United States
coordinates: lat: 42.681175
lon: -83.358048
surface_form: loon lake
instance_of: Lake
countries: United States
coordinates: lat: 42.492777777778
lon: -77.566944444444
surface_form: loon lake
instance_of: Lake
countries: United States
coordinates: lat: 43.6794
lon: -73.8581
surface_form: lake medoza
instance_of: Lake
countries: United States
coordinates: lat: 44.941944444444
lon: -93.312222222222
surface_form: loon lake
instance_of: Lake
countries: United States
coordinates: lat: 43.5958
lon: -123.844
surface_form: loon lake
instance_of: Lake
countries: United States
coordinates: lat: 48.0476
lon: -117.624
surface_form: loon lake
instance_of: Lake
countries: United States
coordinates: lat: 46.2
lon: -89.3
surface_form: loon lake
instance_of: Lake
countries: United States
coordinates: lat: 48.076
lon: -90.689
surface_form: loon lake
instance_of: Lake
countries: United States
coordinates: lat: 47.096111111111
lon: -93.870833333333
The Minneapolis Park and Recreation Board trail system has a trail around the lake for bicyclists and skaters and a trail around it for pedestrians. Both trails connect to the larger trail system via connections to Lake of the Isles and Lake Harriet. In addition, the Midtown Greenway Trail is just north of the lake and Lake Street.

Geographic entities mentioned:
surface_form: lake of the isles
instance_of: Lake
countries: United States
coordinates: lat: 44.954722
lon: -93.3075
surface_form: lake harriet
instance_of: Lake
countries: United States
coordinates: lat: 44.921388888889
lon: -93.305277777778
Bde Maka Ska. Bde Maka Ska (, previously named Lake Calhoun) is the largest lake in Minneapolis, Minnesota, United States, and part of the city's Chain of Lakes. Surrounded by city park land and circled by bike and walking trails, it is popular for many outdoor activities. The lake has an area of and a maximum depth of. Geology.

Geographic entities mentioned:
surface_form: bde maka ska
instance_of: Lake
countries: United States
coordinates: lat: 44.941944444444
lon: -93.312222222222
The lake has an area of and a maximum depth of. Geology. Bde Maka Ska and other lakes in the Chain of Lakes were formed by glacial activity 10,000 to 12,000 years ago. Long before Bde Maka Ska took shape, interglacial rivers created valleys in the Twin Cities region potentially 100 to 250 meters deep, which were gradually filled in by glacial movement. According Myrbo et.

Geographic entities mentioned:
surface_form: bde maka ska
instance_of: Lake
countries: United States
coordinates: lat: 44.941944444444
lon: -93.312222222222
surface_form: chain of lakes
instance_of: Group of lakes
Lake
countries: United States
coordinates: lat: 44.982536
lon: -97.2713448
The lake has an area of and a maximum depth of. Geology. Bde Maka Ska and other lakes in the Chain of Lakes were formed by glacial activity 10,000 to 12,000 years ago. Long before Bde Maka Ska took shape, interglacial rivers created valleys in the Twin Cities region potentially 100 to 250 meters deep, which were gradually filled in by glacial movement. According Myrbo et.

Geographic entities mentioned:
surface_form: bde maka ska
instance_of: Lake
countries: United States
coordinates: lat: 44.941944444444
lon: -93.312222222222
According Myrbo et. al, some of these valleys &quot;overprinted on the deeper [Mississippi] river paleochannels.&quot; The final recession of the Laurentide ice sheet, mainly the Superior lobe, deposited sediment and glacial ice blocks in these valleys, eventually forming kettle lakes like Bde Maka Ska. Bde Maka Ska is the deepest member of the Chain of Lakes and Minneapolis lakes as a whole.

Geographic entities mentioned:
surface_form: bde maka ska
instance_of: Lake
countries: United States
coordinates: lat: 44.941944444444
lon: -93.312222222222
surface_form: bde maka ska
instance_of: Lake
countries: United States
coordinates: lat: 44.941944444444
lon: -93.312222222222
Bde Maka Ska is the deepest member of the Chain of Lakes and Minneapolis lakes as a whole. Before human settlement, Bde Maka Ska and the Chain of Lakes were mostly surrounded by bogs and marshes that slowly grew in the depressions left behind by glacial movement. Between 1911 and 1924, Bde Maka Ska was dredged and these wetlands were filled in.

Geographic entities mentioned:
surface_form: bde maka ska
instance_of: Lake
countries: United States
coordinates: lat: 44.941944444444
lon: -93.312222222222
surface_form: chain of lakes
instance_of: Group of lakes
Lake
countries: United States
coordinates: lat: 44.982536
lon: -97.2713448
Before human settlement, Bde Maka Ska and the Chain of Lakes were mostly surrounded by bogs and marshes that slowly grew in the depressions left behind by glacial movement. Between 1911 and 1924, Bde Maka Ska was dredged and these wetlands were filled in. Since human settlement, the water quality of Bde Maka Ska and the Chain of Lakes has declined.

Geographic entities mentioned:
surface_form: bde maka ska
instance_of: Lake
countries: United States
coordinates: lat: 44.941944444444
lon: -93.312222222222
Between 1911 and 1924, Bde Maka Ska was dredged and these wetlands were filled in. Since human settlement, the water quality of Bde Maka Ska and the Chain of Lakes has declined. The Chain of Lakes watershed was polluted by 19th-century agricultural development and 20th-century storm sewer drainage systems. This increased phosphorus concentrations in the lake, leading to eutrophication.

Geographic entities mentioned:
surface_form: bde maka ska
instance_of: Lake
countries: United States
coordinates: lat: 44.941944444444
lon: -93.312222222222
surface_form: chain of lakes
instance_of: Group of lakes
Lake
countries: United States
coordinates: lat: 44.982536
lon: -97.2713448
surface_form: chain of lakes
instance_of: Group of lakes
Lake
countries: United States
coordinates: lat: 44.982536
lon: -97.2713448
This increased phosphorus concentrations in the lake, leading to eutrophication. In 1990, restoration efforts in the Chain of Lakes watershed began due to public pressure over poor water quality. Over the next decade, public awareness campaigns about stormwater runoff, regulations for phosphorus in fertilizer, and targeted sediment management improved the Chain of Lakes' water quality.

Geographic entities mentioned:
surface_form: chain of lakes
instance_of: Group of lakes
Lake
countries: United States
coordinates: lat: 44.982536
lon: -97.2713448
No permanent settlement was observed before 1828. Between 1829 and 1839, Bde Maka Ska was the site of the Bdewákhathuŋwaŋ Dakota agricultural village known as Ḣeyate Otuŋwe. This village began as an effort by Indian agent Lawrence Taliaferro to encourage Dakota living in the area to adopt European agricultural practices.

Geographic entities mentioned:
surface_form: bde maka ska
instance_of: Lake
countries: United States
coordinates: lat: 44.941944444444
lon: -93.312222222222
George Catlin painted the village in 1836. The Pond brothers soon built a cabin on the east side of Bde Maka Ska. Taliaferro hired them to oversee the village, work the land, and &quot;instruct them in the arts & habits of civilised life.&quot; Taliaferro also gave the Ponds supplies to continue growing crops.

Geographic entities mentioned:
surface_form: bde maka ska
instance_of: Lake
countries: United States
coordinates: lat: 44.941944444444
lon: -93.312222222222
By the late 1850s and 1860s, Minneapolis was increasing in population, with large swaths of land available for sale. The largest surges in development around Bde Maka Ska began when the Minneapolis, Lyndale, and Minnetonka Railway Company started operating in 1879. Bde Maka Ska was seen as an attractive tourist destination, and many people invested in resorts and property along the lake.

Geographic entities mentioned:
surface_form: bde maka ska
instance_of: Lake
countries: United States
coordinates: lat: 44.941944444444
lon: -93.312222222222
surface_form: bde maka ska
instance_of: Lake
countries: United States
coordinates: lat: 44.941944444444
lon: -93.312222222222
Over time, the railway lost money and was sold to the Minneapolis Street Railway in 1887. Despite plans for a resort community on Bde Maka Ska failing to materialize, residential neighborhoods began to arise around the lake. By 1883, a neighborhood known as Cottage City was built to provide small houses for middle-class residents looking to get away from the city.

Geographic entities mentioned:
surface_form: bde maka ska
instance_of: Lake
countries: United States
coordinates: lat: 44.941944444444
lon: -93.312222222222
Like much of the early urban development in Minneapolis, a stop on the streetcar line attracted residents. Over time, many of these homes were replaced by larger residences, now part of the Linden Hills neighborhood. East Bde Maka Ska follows parts of the aforementioned Minneapolis, Lyndale, and Minnetonka Railway, with luxurious homes being erected around the time of the railway's existence.

Geographic entities mentioned:
surface_form: bde maka ska
instance_of: Lake
countries: United States
coordinates: lat: 44.941944444444
lon: -93.312222222222
During the time Bde Maka Ska was becoming a residential tourist attraction, many saw the lakeshore, which largely existed as a swamp, as undesirable. This public sentiment led the Minneapolis Park and Recreation Board to dredge the Chain of Lakes, including Bde Maka Ska. This dredging formed much of the landscape around Bde Maka Ska today.

Geographic entities mentioned:
surface_form: bde maka ska
instance_of: Lake
countries: United States
coordinates: lat: 44.941944444444
lon: -93.312222222222
surface_form: chain of lakes
instance_of: Group of lakes
Lake
countries: United States
coordinates: lat: 44.982536
lon: -97.2713448
This public sentiment led the Minneapolis Park and Recreation Board to dredge the Chain of Lakes, including Bde Maka Ska. This dredging formed much of the landscape around Bde Maka Ska today. In 1906, the MPRB began connecting Cedar Lake, Lake of the Isles, and Bde Maka Ska with channels. When the project was completed in 1911, over 100,000 people celebrated its opening.

Geographic entities mentioned:
surface_form: bde maka ska
instance_of: Lake
countries: United States
coordinates: lat: 44.941944444444
lon: -93.312222222222
Even before the lake was dredged, the lake was commonly used for sports and recreation. By the late 1870s, boating clubs regularly hosted regattas on it. Sailing, a common activity on Bde Maka Ska today, was formally organized as early as 1901 by what was then called the Calhoun Yacht Club. Lake and surrounding area.

Geographic entities mentioned:
surface_form: bde maka ska
instance_of: Lake
countries: United States
coordinates: lat: 44.941944444444
lon: -93.312222222222
There was also a proposal to rename the lake for Senator Paul Wellstone, who is buried in nearby Lakewood Cemetery. In 2017, the MPRB voted unanimously to recommend changing the lake's name to Bde Maka Ska, and the Hennepin County commissioners agreed. In January 2018, the Minnesota Department of Natural Resources (DNR) made Bde Maka Ska the official name in Minnesota.

Geographic entities mentioned:
surface_form: bde maka ska
instance_of: Lake
countries: United States
coordinates: lat: 44.941944444444
lon: -93.312222222222
On April 29, 2019, the Minnesota Court of Appeals reversed the DNR's decision, holding that a name that had been in use more than 40 years could be changed only by the legislature. The MPRB said it would continue to keep the signage of Bde Maka Ska at the lake and Minneapolis Mayor Jacob Frey said, &quot;I will continue to call Bde Maka Ska by its rightful name.

Geographic entities mentioned:
surface_form: bde maka ska
instance_of: Lake
countries: United States
coordinates: lat: 44.941944444444
lon: -93.312222222222
That was the lake's name before people who look like me renamed it to honor a slavery apologist and as far as I'm concerned that is still its name today&quot;. The DNR appealed the court decision, and released a statement confirming that the federal Board on Geographic Names (BGN) had adopted Bde Maka Ska as the lake's official name. Executive secretary of the U.S.

Geographic entities mentioned:
surface_form: bde maka ska
instance_of: Lake
countries: United States
coordinates: lat: 44.941944444444
lon: -93.312222222222
The Minnesota Court of Appeals decision was appealed to the Minnesota Supreme Court, which heard oral arguments on November 13, 2019. On May 13, 2020, the Minnesota Supreme Court ruled that the Minnesota Department of Natural Resources had the authority to rename the lake Bde Maka Ska, ruling that the law restricting renaming applied only to county boards, not to the DNR. Wildlife.

Geographic entities mentioned:
surface_form: bde maka ska
instance_of: Lake
countries: United States
coordinates: lat: 44.941944444444
lon: -93.312222222222
Taliaferro hired them to oversee the village, work the land, and &quot;instruct them in the arts & habits of civilised life.&quot; Taliaferro also gave the Ponds supplies to continue growing crops. In the summer of 1835, a competing mission on Lake Harriet formed, led by Reverend Jedediah D. Stevens and seeking to build a school that taught Dakota children.

Geographic entities mentioned:
surface_form: lake harriet
instance_of: Lake
countries: United States
coordinates: lat: 44.921388888889
lon: -93.305277777778
In July of that year, some members of Cloud Man's band retaliated by killing a member of Hole-in-the-Day's band. Tensions between the Bdewákhathuŋwaŋ Dakota and Ojibwe culminated in a June 1839 meeting at Fort Snelling, where after an apparent peace was reached, a surprise Ojibwe attack was launched near Lake Harriet, killing Cloud Man's son-in-law.

Geographic entities mentioned:
surface_form: lake harriet
instance_of: Lake
countries: United States
coordinates: lat: 44.921388888889
lon: -93.305277777778
This led to many battles between the Ojibwe and Dakota, putting Ḣeyate Otuŋwe under constant threat of attack. This instability led Stevens to abandon his mission on Lake Harriet, and after August 1839, Taliaferro resigned from his position as Indian agent, leaving Ḣeyate Otuŋwe with little support from Fort Snelling or local missionaries.

Geographic entities mentioned:
surface_form: lake harriet
instance_of: Lake
countries: United States
coordinates: lat: 44.921388888889
lon: -93.305277777778
On the west side is The Bakken, an old mansion with medicinal gardens and a library and museum devoted to medical electricity and the history of electromagnetism. The Como-Harriet Streetcar Line operates between the lake and Lake Harriet. Historic names.

Geographic entities mentioned:
surface_form: lake harriet
instance_of: Lake
countries: United States
coordinates: lat: 44.921388888889
lon: -93.305277777778
According Myrbo et. al, some of these valleys &quot;overprinted on the deeper [Mississippi] river paleochannels.&quot; The final recession of the Laurentide ice sheet, mainly the Superior lobe, deposited sediment and glacial ice blocks in these valleys, eventually forming kettle lakes like Bde Maka Ska. Bde Maka Ska is the deepest member of the Chain of Lakes and Minneapolis lakes as a whole.

Geographic entities mentioned:
surface_form: chain of lakes
instance_of: Group of lakes
Lake
countries: United States
coordinates: lat: 44.982536
lon: -97.2713448
Although this mountain is located south of the East African Rift, along with Mount Gugu to the north and Mount Kaka to the south, it is considered, geologically speaking, part of the Ethiopian Highlands.

Geographic entities mentioned:
surface_form: Mount Gugu
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 8.2
lon: 39.9667
surface_form: gugu
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 8.2
lon: 39.9667
surface_form: mount gugu
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 8.2
lon: 39.9667
Mount Chilalo. Mount Chilalo is an isolated, extinct silicic stratovolcano in southeastern Ethiopia. Its highest point (4036 m or 13,241 ft a.s.l.), in the Arsi Zone of the Oromia Region, is located in Arsi Mountains National Park on the border between the Hitosa and Tiyo woreda ().

Geographic entities mentioned:
surface_form: mount chilalo
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 7.9166666666667
lon: 39.266666666667
surface_form: chilalo
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 7.9166666666667
lon: 39.266666666667
Chilalo rises with gentle slopes for more than 1500 meters from the top of the plateau. At the summit, there is a large, almost circular caldera about 6 kilometers in diameter, whose southern rim is considered to be the mountain's summit. Mount Chilalo last erupted in the Pleistocene. One authority identifies Mount Chilalo as a late Trap Series volcano.

Geographic entities mentioned:
surface_form: mount chilalo
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 7.9166666666667
lon: 39.266666666667
surface_form: chilalo
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 7.9166666666667
lon: 39.266666666667
Mount Chilalo last erupted in the Pleistocene. One authority identifies Mount Chilalo as a late Trap Series volcano. The geologist Erik Nilsson claimed to have identified traces of glaciation on Chilalo, as well as on its neighbor Mount Kaka down to about 3400 meters, which he dated to the &quot;Last Pluvial Period&quot;.

Geographic entities mentioned:
surface_form: mount chilalo
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 7.9166666666667
lon: 39.266666666667
surface_form: chilalo
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 7.9166666666667
lon: 39.266666666667
The mountain has an elliptical base (about 30 by 20 kilometers), whose major axis lies NNE-SSW or parallel to the predominant tectonic trend. Chilalo rises with gentle slopes for more than 1500 meters from the top of the plateau. At the summit, there is a large, almost circular caldera about 6 kilometers in diameter, whose southern rim is considered to be the mountain's summit.

Geographic entities mentioned:
surface_form: chilalo
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 7.9166666666667
lon: 39.266666666667
Mount Chilalo last erupted in the Pleistocene. One authority identifies Mount Chilalo as a late Trap Series volcano. The geologist Erik Nilsson claimed to have identified traces of glaciation on Chilalo, as well as on its neighbor Mount Kaka down to about 3400 meters, which he dated to the &quot;Last Pluvial Period&quot;.

Geographic entities mentioned:
surface_form: chilalo
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 7.9166666666667
lon: 39.266666666667
Niua Islands. Niua is a division of the Kingdom of Tonga, namely the northernmost group of islands. It consists of three islands (Niuafoʻou, Niuatoputapu and Tafahi) which together have an area of 71.69 km2 and a population of 1,150. The largest village is Hihifo on Niuatoputapu. Piu'o Tafahi is the highest point with an elevation of 560 m. Geography.

Geographic entities mentioned:
surface_form: Tafahi
instance_of: Mountain
countries: Tonga
coordinates: lat: -15.852777777777778
lon: -173.74583333333334
Niua Islands. Niua is a division of the Kingdom of Tonga, namely the northernmost group of islands. It consists of three islands (Niuafoʻou, Niuatoputapu and Tafahi) which together have an area of 71.69 km2 and a population of 1,150. The largest village is Hihifo on Niuatoputapu. Piu'o Tafahi is the highest point with an elevation of 560 m. Geography.

Geographic entities mentioned:
surface_form: Piu'o Tafahi
instance_of: Mountain
countries: Tonga
coordinates: lat: -15.852777777777778
lon: -173.74583333333334
Niuafoʻou lies at the center of the Niuafo'ou Plate and has erupted regularly since 1814. There are other volcanoes in this part of the Tofua chain which do not reach sea level, but form seamounts with between 1200 and 1500m of water above their peaks. This includes the Mata group, the Curacoa volcano, and the large submarine caldera Niuatahi. History.

Geographic entities mentioned:
surface_form: Curacoa volcano
instance_of: Mountain
countries: Tonga
coordinates: lat: -15.62
lon: -173.67
surface_form: Niuatahi
instance_of: Mountain
countries: Tonga
coordinates: lat: -15.37888888888889
lon: -174.00277777777777
Geography. According to the United States Census Bureau, the township has a total area of, of which is land and (35.08%) is water. Elmwood Township lies upon the West Arm of Grand Traverse Bay. Part of Lake Leelanau is located within the far northwest of Elmwood Township. Demographics. As of the census of 2000, there were 4,264 people, 1,697 households, and 1,259 families residing in the township.

Geographic entities mentioned:
surface_form: Lake Leelanau
instance_of: Lake
countries: United States
coordinates: lat: 44.85
lon: -85.73187
Sosnówka (lake). Sosnówka Lake is a retention reservoir and reservoir for drinking water located in the southern part of the Jelenia Góra Valley, Lower Silesian Voivodeship; in Poland. The reservoir has been in use since 2001.

Geographic entities mentioned:
surface_form: Jelenia Góra Valley
instance_of: Valley
countries: Prussia
coordinates: lat: 50.916666666667
lon: 15.75
Schlossberg von Tettelham. Schlossberg von Tettelham is a mountain of Bavaria, Germany.

Geographic entities mentioned:
surface_form: schlossberg
instance_of: Mountain
countries: Germany
coordinates: lat: 49.7583
lon: 11.5329
surface_form: schlossberg von tettelham
instance_of: Mountain
countries: Germany
coordinates: lat: 47.948055555556
lon: 12.678888888889
surface_form: schlossberg
instance_of: Mountain
countries: Germany
coordinates: lat: 47.99416667
lon: 7.85944444
Qixian Temple (Mount Wutai). Qixian Temple (), also known as Guanyin Cave (), is a Buddhist temple located on Mount Wutai of Taihuai Town, in Wutai County, Shanxi, China. History. The temple was originally built in the Kangxi era (1662&ndash;1722) of the Qing dynasty (1644&ndash;1911). Legend said that the 6th Dalai Lama once settled at the temple.

Geographic entities mentioned:
surface_form: Mount Wutai
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 39.081388888889
lon: 113.56694444444
Tony O. Wilt (born September 18, 1961) is an American politician. A Republican, he was elected to the Virginia House of Delegates in 2010. He the 34th district, made up of the city of Harrisonburg and part of Rockingham County in the Shenandoah Valley. Early life, education, business career. Born in Harrisonburg, Virginia, Wilt graduated from Broadway High School in 1979. He received an A.A.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
A Migratory Bird Sanctuary was established at the lake on March 9, 1925. This lake, in conjunction with Reed Lake and Chaplin Lake, forms a site of hemispheric importance in the Western Hemisphere Shorebird Reserve Network. It was designated in April 1997, and is &quot;one of the most important inland sites for migratory birds in North America&quot;.

Geographic entities mentioned:
surface_form: Reed Lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.40003
lon: -107.08397
surface_form: Chaplin Lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.4016
lon: -106.6004
According to some First Nations traditions, the spirits of the dead women continue to haunt a small island in the lake from which their voices can be heard at night. Some early accounts describing the region state that the name &quot;Old Wives Lake&quot; was originally applied to both the lake that currently bears that name and to nearby Chaplin Lake.

Geographic entities mentioned:
surface_form: Chaplin Lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.4016
lon: -106.6004
River slope is 1.1 m/km, annual drainage 0.26 km3. Lielā Jugla begins at the confluence of the Suda and Mergupe rivers in village Sidgunda. Lielā Jugla joins with Mazā Jugla thus forming the river Jugla shortly before its mouth into Jugla Lake at the Riga city eastern border with the municipality of Ropaži. The river is a water tourism site. The Ropaži hydroelectric plant is located on the river.

Geographic entities mentioned:
surface_form: Jugla Lake
instance_of: Lake
countries: Latvia
coordinates: lat: 56.978888888889
lon: 24.280277777778
The mine project, owned by Toro Energy Ltd, is located south of the mining town of Wiluna. The original proposal was to establish open cut mines at Lake Way and Centipede deposits. In 2013, the Wiluna project became the first uranium mine to receive all necessary approvals in the state of Western Australia since the ban on uranium mining was repealed there in 2008.

Geographic entities mentioned:
surface_form: Lake Way
instance_of: Lake
countries: Australia
coordinates: lat: -26.783333333333
lon: 120.33333333333
Mount Kuma. , or Mount Kumaga, is a stratovolcano located in the Daisetsuzan Volcanic Group of the Ishikari Mountains, Hokkaidō, Japan.

Geographic entities mentioned:
surface_form: mount kuma
instance_of: Mountain
countries: Japan
coordinates: lat: 43.670555555556
lon: 142.86194444444
Jordanshöhe. The Jordanshöhe is a mountain, roughly, in the Harz in central Germany. It lies north of the town of Sankt Andreasberg in the district of Goslar in Lower Saxony. To the west is the Kuppe. On the mountain there is the Jordanshöhe youth hostel and the Jordanshöhe nature trail (&quot;Gesteinskundlichen Lehrpfad Jordanshöhe&quot;).

Geographic entities mentioned:
surface_form: kuppe
instance_of: Mountain
countries: Germany
coordinates: lat: 51.7267
lon: 10.5086
Jordanshöhe. The Jordanshöhe is a mountain, roughly, in the Harz in central Germany. It lies north of the town of Sankt Andreasberg in the district of Goslar in Lower Saxony. To the west is the Kuppe. On the mountain there is the Jordanshöhe youth hostel and the Jordanshöhe nature trail (&quot;Gesteinskundlichen Lehrpfad Jordanshöhe&quot;).

Geographic entities mentioned:
surface_form: jordanshöhe
instance_of: Mountain
countries: Germany
coordinates: lat: 51.7228
lon: 10.5242
Jordanshöhe. The Jordanshöhe is a mountain, roughly, in the Harz in central Germany. It lies north of the town of Sankt Andreasberg in the district of Goslar in Lower Saxony. To the west is the Kuppe. On the mountain there is the Jordanshöhe youth hostel and the Jordanshöhe nature trail (&quot;Gesteinskundlichen Lehrpfad Jordanshöhe&quot;).

Geographic entities mentioned:
surface_form: jordanshöhe
instance_of: Mountain
countries: Germany
coordinates: lat: 51.7228
lon: 10.5242
surface_form: jordanshöhe
instance_of: Mountain
countries: Germany
coordinates: lat: 51.7228
lon: 10.5242
surface_form: jordanshöhe
instance_of: Mountain
countries: Germany
coordinates: lat: 51.7228
lon: 10.5242
Eagle Harbor Light. Eagle Harbor Light is an operational lighthouse at Eagle Harbor, in Keweenaw County in the state of Michigan. It sits on the rocky entrance to Eagle Harbor and is one of several light stations that guide mariners on Lake Superior across the northern edge of the Keweenaw Peninsula.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
The river flows from Sawyer County through Rusk, Chippewa, Eau Claire, Dunn, Pepin and Buffalo Counties, in Wisconsin, before emptying out into the Mississippi River. Sediment build-up at the river's mouth forms a delta that protrudes into the Mississippi, creating Lake Pepin in the process.

Geographic entities mentioned:
surface_form: Lake Pepin
instance_of: Lake
countries: United States
coordinates: lat: 44.4982
lon: -92.3013
The word &quot;Chippewa&quot; is a rendering of &quot;Ojibwe.&quot; The Ojibwe people controlled most of the upper Chippewa Valley and its tributaries until the Treaty of St. Peters in 1837. Of the pine forests in Wisconsin in the 1800s, the Chippewa River system held more than even the Wisconsin River.

Geographic entities mentioned:
surface_form: Chippewa Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.75
lon: -91.5