Sarmila/GeoWiki-Features huggingface dataset:
Geography. Furnes Municipality was located in the Hedmarken district to the northeast of the large lake Mjøsa. Åmot Municipality was located to the north, Vang Municipality was located to the east, Hamar Municipality was located to the south, Nes Municipality was located to the southwest, and Ringsaker Municipality was located to the west.

Geographic entities mentioned:
surface_form: Mjøsa
instance_of: Lake
countries: Norway
coordinates: lat: 60.666666666667
lon: 11
Lucifer Crags surmount the lake on the southwest. The area was visited by early 19th century sealers. The feature is named after Acheron River in Greek underworld. Location. Acheron Lake is centred south of Point Smellie, west-northwest of Wasp Hill and northeast of Devils Point and north-northeast of Point Smellie. Detailed Spanish mapping in 1992, and Bulgarian mapping in 2009 and 2017.

Geographic entities mentioned:
surface_form: Wasp Hill
instance_of: Mountain
coordinates: lat: -62.6644
lon: -61.1311
surface_form: acheron lake
instance_of: Lake
coordinates: lat: -62.66222222
lon: -61.15111111
Acheron Lake. Acheron Lake (,) is the B-shaped long in southwest-northeast direction and wide lake on President Beaches, Byers Peninsula on Livingston Island in the South Shetland Islands, Antarctica. It has a surface area of, and is separated from Osogovo Bay waters by a wide strip of land. Lucifer Crags surmount the lake on the southwest. The area was visited by early 19th century sealers.

Geographic entities mentioned:
surface_form: acheron lake
instance_of: Lake
coordinates: lat: -62.66222222
lon: -61.15111111
Schmidt (volcano). Schmidt (, &quot;Vulkan Schmidta&quot;) is a shield volcano located in the southeastern part of Kamchatka Peninsula, Russia.

Geographic entities mentioned:
surface_form: schmidt (volcano)
instance_of: Mountain
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 54.92
lon: 160.63
Schmidt (volcano). Schmidt (, &quot;Vulkan Schmidta&quot;) is a shield volcano located in the southeastern part of Kamchatka Peninsula, Russia.

Geographic entities mentioned:
surface_form: schmidt
instance_of: Mountain
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 54.92
lon: 160.63
The entire area south of downtown is widely called South Minneapolis. The westerly portion surrounding the city's Chain of Lakes is loosely labeled Southwest Minneapolis, bounded on the east by I-35W and on the north by 36th St W, which extends west from Bde Maka Ska to the city limits. Common conceptions of Minneapolis neighborhoods do not always align with official city maps.

Geographic entities mentioned:
surface_form: Bde Maka Ska
instance_of: Lake
countries: United States
coordinates: lat: 44.941944444444
lon: -93.312222222222
The seven cultural districts are 38th Street, Cedar Avenue South, Central Avenue, East Lake Street, Franklin Avenue East, West Broadway, and Lowry Avenue North. Bde Maka Ska-Isles. Calhoun-Isles is in western Minneapolis. It is named after Lake Calhoun (the former name of Bde Maka Ska) and Lake of the Isles. It includes the city's Uptown area. Camden. Camden is in far northwest Minneapolis.

Geographic entities mentioned:
surface_form: Bde Maka Ska
instance_of: Lake
countries: United States
coordinates: lat: 44.941944444444
lon: -93.312222222222
surface_form: Lake of the Isles
instance_of: Lake
countries: United States
coordinates: lat: 44.954722
lon: -93.3075
Near North is northwest of downtown Minneapolis. Along with Camden, the two communities comprise north Minneapolis. Nokomis. The Nokomis community is in south Minneapolis. It takes its name from Lake Nokomis. It includes Nokomis East, which refers to the four neighborhoods of Keewaydin, Minnehaha, Morris Park, and Wenonah that are represented by one neighborhood organization. Northeast.

Geographic entities mentioned:
surface_form: Lake Nokomis
instance_of: Lake
countries: United States
coordinates: lat: 44.909444444444
lon: -93.242222222222
Name. In Tibet, the river is called &quot;Bum-chu&quot;, also transliterated &quot;Phung-Chu&quot; or from Chinese as &quot;Peng Qu&quot; or &quot;Pumqu&quot;. The &quot;Men Qu&quot; or &quot;Moinqu&quot; is an upper tributary draining glaciers from Shishapangma. In Nepal, the river's name changes to &quot;Arun&quot;. Tibet.

Geographic entities mentioned:
surface_form: Shishapangma
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 28.352222222222
lon: 85.779722222222
Another river that meets Bum-chu is Trakar-chu. The river flows past the town of Kharda, gateway to the Khangzhung east face of Mount Everest. The force of its accumulated waters carves its way, south of Drengtrang, through the main chain of the Himalayas directly between the mountain massifs of Makalu and Kangchenjunga into Nepal.

Geographic entities mentioned:
surface_form: Kharda
instance_of: Valley
countries: People's Republic of China
coordinates: lat: 28.1
lon: 87.1667
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
Another river that meets Bum-chu is Trakar-chu. The river flows past the town of Kharda, gateway to the Khangzhung east face of Mount Everest. The force of its accumulated waters carves its way, south of Drengtrang, through the main chain of the Himalayas directly between the mountain massifs of Makalu and Kangchenjunga into Nepal.

Geographic entities mentioned:
surface_form: Makalu
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.889166666667
lon: 87.088611111111
surface_form: Kangchenjunga
instance_of: Mountain
countries: India
Nepal
coordinates: lat: 27.7
lon: 88.133333
The main rivers forming the Koshi system are – the Sun Koshi, the Indravati River, the Bhoté Koshi, the Dudh Koshi, the Arun River, Barun River, and Tamur River. The combined river flows through the Chatra Gorge in a southerly direction to emerge from the hills. The Sun Koshi contributes 44 per cent of the total water in the Sapta Koshi, the Arun 37 per cent and the Tamur 19 per cent. Nepal.

Geographic entities mentioned:
surface_form: Chatra Gorge
instance_of: Valley
countries: Nepal
coordinates: lat: 26.86856
lon: 87.15185
Wielki Staw. Wielki Staw (, Polish for &quot;The Big Pond&quot;, &quot;Grosser Teich&quot; in German) - post glacial natural lake in the Krkonoše mountains, in western Poland. It is situated in the Karkonosze National Park at the bottom of the cirque, on the southern slope of the Smogornia mountain. With its area of 8.3 hectares, it is the biggest glacial lake in the whole range.

Geographic entities mentioned:
surface_form: Smogornia
instance_of: Mountain
countries: Czech Republic
Poland
coordinates: lat: 50.755
lon: 15.676388888889
Wielki Staw. Wielki Staw (, Polish for &quot;The Big Pond&quot;, &quot;Grosser Teich&quot; in German) - post glacial natural lake in the Krkonoše mountains, in western Poland. It is situated in the Karkonosze National Park at the bottom of the cirque, on the southern slope of the Smogornia mountain. With its area of 8.3 hectares, it is the biggest glacial lake in the whole range.

Geographic entities mentioned:
surface_form: wielki staw
instance_of: Lake
countries: Poland
coordinates: lat: 50.7583
lon: 15.6936
It is the highest peak of the Ban massif, a group of peaks higher than 2,800 meters (also including Monte Immel, Punta Morasco, Punta del Ghiacciaio di Ban, Gemelli di Ban, Punta Lebendum, Punta dei Camosci, Pizzo del Costone, Pizzo del Vallone, Punta della Sabbia) located between Lake Morasco and Lake Sabbione, in the upper Val Formazza. Corno di Ban is the only three-thousander in the massif.

Geographic entities mentioned:
surface_form: Val Formazza
instance_of: Valley
countries: Italy
coordinates: lat: 46.383
lon: 8.433
Church Lake. Church Lake is a lake in Grant County, in the U.S. state of Minnesota. Church Lake took its name from a church which stood near its shore.

Geographic entities mentioned:
surface_form: church lake
instance_of: Lake
countries: United States
coordinates: lat: 45.879444444444
lon: -95.798888888889
When the US entered World War II he tried to join the Army Air Corps but, because he was too light for his height, he did not pass the Army's physical exam. He then spent nine months at a Jackson Hole dude ranch, working to increase his weight and then passed his physical exam on the second try in October 1942.

Geographic entities mentioned:
surface_form: Jackson Hole
instance_of: Valley
countries: United States
coordinates: lat: 43.516666666667
lon: -110.83333333333
Uzlomac. uqgkagacyg5klthbur4et4eidhn6l" xml:space="preserve">Uzlomac is a long mountain in Bosnia and Herzegovina (Bosnia), east from line direction Maslovare – Vrbanjci – Kotor Varoš – Čelinac. It stretches from the southeast to the northwest through the mountainous area, from Kruševica River (west of Borja mountains) to Jošavka. Its maximum altitude is.

Geographic entities mentioned:
surface_form: uzlomac
instance_of: Mountain
countries: Bosnia and Herzegovina
coordinates: lat: 44.59
lon: 17.04
Its maximum altitude is. The mountain is very rich in mixed forests resources and hunting wildlife, including Bosnian endemic quarry mammals. Its forest wealth is diverse: deciduous oak and deciduous beech. It also is rich in water resources: springs, streams and rivers. On Uzlomac many tributaries of Vrbanja river, Usora and Ukrina rise, i.e. tributaries of Vrbas and Bosna confluences.

Geographic entities mentioned:
surface_form: uzlomac
instance_of: Mountain
countries: Bosnia and Herzegovina
coordinates: lat: 44.59
lon: 17.04
The most prominent peaks in the municipality of Vintl include the Niederer Weißzint (3,263 m) and the Grabspitze () near the Pfunderer Joch, the highest peak on the ridge between the Pfitscher valley and Weitenberger Kar, the Wurmaulspitze (), the highest summit west of the Weitenberger Alm, the Napfspitze () south of the Eisbruggjoch col, the Hochgrubbachspitze (2,819 m), the highest point in the eastern Pfunderer and, in front of it, the Eidechsspitze (), the &quot;Hausberg&quot; of Vintl.

Geographic entities mentioned:
surface_form: Grabspitze
instance_of: Mountain
countries: Italy
coordinates: lat: 46.93834
lon: 11.6146
surface_form: Wurmaulspitze
instance_of: Mountain
countries: Italy
coordinates: lat: 46.914444444444
lon: 11.636944444444
The conquest was publicly celebrated in the panegyric court poetry of Theocritus and by the erection of a long list of Nubian districts at the Temple of Isis at Philae, near Syene. The conquered territory included the rich gold mines at Wadi Allaqi, where Ptolemy founded a city called Berenice Panchrysus and instituted a large-scale mining programme.

Geographic entities mentioned:
surface_form: Wadi Allaqi
instance_of: Valley
countries: Egypt
coordinates: lat: 22.5
lon: 34
Colonisation of the Red Sea. Ptolemy revived earlier Egyptian programmes to access the Red Sea. A canal from the Nile near Bubastis to the Gulf of Suez – via Pithom, Lake Timsah and the Bitter Lakes – had been dug by Darius I in the sixth century BC. However, by Ptolemy's time it had silted up.

Geographic entities mentioned:
surface_form: Lake Timsah
instance_of: Lake
countries: Egypt
coordinates: lat: 30.577777777778
lon: 32.288888888889
surface_form: Bitter Lakes
instance_of: Group of lakes
countries: Egypt
coordinates: lat: 30.268611111111
lon: 32.447222222222
After the war was over, in July 253 BC Ptolemy travelled to Memphis. There he rewarded his soldiers by distributing large plots of land that had been reclaimed from Lake Moeris in the Fayyum to them as estates (&quot;kleroi&quot;). The area was established as a new nome, named the Arsinoite nome, in honour of the long-dead Arsinoe II. Later reign and death (252–246 BC).

Geographic entities mentioned:
surface_form: Lake Moeris
instance_of: Lake
countries: Egypt
coordinates: lat: 29.472222222222
lon: 30.614166666667
Efforts were made to increase the amount of arable land in Egypt, particularly by reclaiming large amounts of land from Lake Moeris in the Fayyum. Ptolemy distributed this land to the Ptolemaic soldiers as agricultural estates in 253 BC.

Geographic entities mentioned:
surface_form: Lake Moeris
instance_of: Lake
countries: Egypt
coordinates: lat: 29.472222222222
lon: 30.614166666667
Geography. Přerov nad Labem is located about west of Nymburk and east of Prague. It lies in the Central Elbe Table within the Polabí region. The highest point is the hill Přerovská hůra at above sea level. The municipality is situated on the left bank of the Elbe River, which forms the northern municipal border. History. The first written mention of Přerov nad Labem is from 993.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Muskegon, Michigan. Muskegon () is a city in and the county seat of Muskegon County, Michigan, United States. Situated around a harbor of Lake Michigan, Muskegon is known for fishing, sailing regattas, and boating. It is the most populous city along Lake Michigan's eastern shore. At the 2020 census, the city's population was 38,318.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Between 1790 and 1800, a French-Canadian trader named Joseph La Framboise established a fur-trading post at the mouth of Duck Lake. Between 1810 and 1820, several French-Canadian fur traders, including Lamar Andie, Jean Baptiste Recollect, and Pierre Constant, had established fur-trading posts around Muskegon Lake.

Geographic entities mentioned:
surface_form: Muskegon Lake
instance_of: Lake
countries: United States
coordinates: lat: 43.236849
lon: -86.290199
Bluffton was founded as a lumbering village in 1862 in Laketon Township. It had its own post office from 1868 until 1892. Muskegon annexed it in 1889. Geography. Muskegon is in western Muskegon County, on the south side of Muskegon Lake, a harbor of Lake Michigan. The city is bordered to the north, across Muskegon Lake, by the city of North Muskegon and Laketon Township.

Geographic entities mentioned:
surface_form: Muskegon Lake
instance_of: Lake
countries: United States
coordinates: lat: 43.236849
lon: -86.290199
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Climate. Muskegon has a humid continental climate (&quot;Dfa&quot;) with hot summers and cold winters. Precipitation is consistent year-round. Muskegon receives heavy lake-effect snow from Lake Michigan during winter. 2010 census. As of the census of 2010, 38,401 people, 13,967 households, and 7,895 families resided in the city. The population density was.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
The Seaway Run is run every year in late June. It features a 15k race, 5k race, 5k walk for fun, 15k wheelchair race. Parks and recreation. Pere Marquette Beach is the largest free public beach on the eastern shore of Lake Michigan. Windsurfing, kite boarding competitions, and professional volleyball tournaments are held there. Its quartz sand beach is expansive and bordered by large sand dunes.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
McKinney Creek. nthg9me9y8hg3qghd93jh384ujpg" xml:space="preserve">McKinney Creek is located in the Boundary Country region of British Columbia. The creek is one of the main tributaries of Rock Creek. McKinney Creek flows into Rock Creek from the west. The creek has been mined by Europeans and Chinese miners.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mckinney creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.06647
lon: -119.21905
McKinney Creek. nthg9me9y8hg3qghd93jh384ujpg" xml:space="preserve">McKinney Creek is located in the Boundary Country region of British Columbia. The creek is one of the main tributaries of Rock Creek. McKinney Creek flows into Rock Creek from the west. The creek has been mined by Europeans and Chinese miners.

Geographic entities mentioned:
surface_form: mckinney creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.06647
lon: -119.21905
28 April 1988 — Alcalá del Río to Badajoz,
Stage 5. 29 April 1988 — Badajoz to Béjar,
Stage 6. 30 April 1988 — Béjar to Valladolid,
Stage 7. 1 May 1988 — Valladolid to León,
Stage 8. 2 May 1988 — León to,
Stage 9. 3 May 1988 — Oviedo to Monte Naranco, (ITT)
Stage 10. 4 May 1988 — Oviedo to Santander,
Stage 11. 5 May 1988 — Santander to Valdezcaray,

Geographic entities mentioned:
surface_form: Monte Naranco
instance_of: Mountain
countries: Spain
coordinates: lat: 43.38333333
lon: -5.86666667
The tall mountain lies in the eastern part of the municipality of Luster in Vestland county, Norway. The mountain lies in between Nordre Skagastølstind, Vetle Skagastølstind, and Store Skagastølstind. The mountains Store Styggedalstinden, Jervvasstind, and Sentraltind all lie about to the east of this mountain. The village of Skjolden lies about to the west. Name.

Geographic entities mentioned:
surface_form: Vetle Skagastølstind
instance_of: Mountain
countries: Norway
coordinates: lat: 61.464444444444
lon: 7.8741666666667
surface_form: Store Skagastølstind
instance_of: Mountain
countries: Norway
coordinates: lat: 61.461388888889
lon: 7.8713888888889
The tall mountain lies in the eastern part of the municipality of Luster in Vestland county, Norway. The mountain lies in between Nordre Skagastølstind, Vetle Skagastølstind, and Store Skagastølstind. The mountains Store Styggedalstinden, Jervvasstind, and Sentraltind all lie about to the east of this mountain. The village of Skjolden lies about to the west. Name.

Geographic entities mentioned:
surface_form: Store Styggedalstinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.464444444444
lon: 7.9013888888889
surface_form: Jervvasstind
instance_of: Mountain
countries: Norway
coordinates: lat: 61.464722222222
lon: 7.9111111111111
surface_form: Sentraltind
instance_of: Mountain
countries: Norway
coordinates: lat: 61.463611111111
lon: 7.8825
Midtre Skagastølstind. Midtre Skagastølstind is one of the peaks constituting Skagastølstindane (&quot;Skagastøl peaks&quot;) in the Hurrungane mountain range. The tall mountain lies in the eastern part of the municipality of Luster in Vestland county, Norway. The mountain lies in between Nordre Skagastølstind, Vetle Skagastølstind, and Store Skagastølstind.

Geographic entities mentioned:
surface_form: midtre skagastølstind
instance_of: Mountain
countries: Norway
coordinates: lat: 61.468055555556
lon: 7.8688888888889
Distribution. The plant is endemic to California, where it grows in the Sacramento Valley and adjacent foothills of the California Coast Ranges to the west, and of the Sierra Nevada to the east. It can grow in oak woodland and grassland habitats below, sometimes on serpentine soils. Description.

Geographic entities mentioned:
surface_form: Sacramento Valley
instance_of: Valley
countries: United States
coordinates: lat: 39
lon: -121.5
Tordera (river). The Tordera (;) is a river of Catalonia (Spain). It flows through the town of Tordera. Course. The river is long. Its source is in the Montseny Massif, and it discharges in the Mediterranean Sea. The river's average discharge is. Its main tributaries are the Riera de Gualba, Riera de Arbúcies, Riera de Santa Coloma and the Riera de Valmanya.

Geographic entities mentioned:
surface_form: montseny
instance_of: Mountain
countries: Spain
coordinates: lat: 42.4901106285
lon: 1.02442265779
The river's average discharge is. Its main tributaries are the Riera de Gualba, Riera de Arbúcies, Riera de Santa Coloma and the Riera de Valmanya. The river runs through the protected areas of the Parc Natural del Montseny and the Parc Natural del Montnegre i el Corredor. The last stretch of the Tordera is a wide sandy bed subject to seasonal flow.

Geographic entities mentioned:
surface_form: montseny
instance_of: Mountain
countries: Spain
coordinates: lat: 42.4901106285
lon: 1.02442265779
In the last week of January 1939 the 77th Division of the Spanish Republican Army, together with the 242nd Mixed Brigade —which had not been ascribed to any division—, tried to establish a planned defensive line along the course of the Tordera River in order to halt the massive rebel offensive. The units took position along the course of the river east of the Montseny Massif on 27 January.

Geographic entities mentioned:
surface_form: montseny
instance_of: Mountain
countries: Spain
coordinates: lat: 42.4901106285
lon: 1.02442265779
Tordera (river). The Tordera (;) is a river of Catalonia (Spain). It flows through the town of Tordera. Course. The river is long. Its source is in the Montseny Massif, and it discharges in the Mediterranean Sea. The river's average discharge is. Its main tributaries are the Riera de Gualba, Riera de Arbúcies, Riera de Santa Coloma and the Riera de Valmanya.

Geographic entities mentioned:
surface_form: tordera
instance_of: Watercourse
countries: Spain
coordinates: lat: 41.803521
lon: 2.418014
The river runs through the protected areas of the Parc Natural del Montseny and the Parc Natural del Montnegre i el Corredor. The last stretch of the Tordera is a wide sandy bed subject to seasonal flow. The brackish lagoon in its final delta area is an important area for migratory birds. History.

Geographic entities mentioned:
surface_form: tordera
instance_of: Watercourse
countries: Spain
coordinates: lat: 41.803521
lon: 2.418014
The brackish lagoon in its final delta area is an important area for migratory birds. History. In the last week of January 1939 the 77th Division of the Spanish Republican Army, together with the 242nd Mixed Brigade —which had not been ascribed to any division—, tried to establish a planned defensive line along the course of the Tordera River in order to halt the massive rebel offensive.

Geographic entities mentioned:
surface_form: tordera
instance_of: Watercourse
countries: Spain
coordinates: lat: 41.803521
lon: 2.418014
In the face of the powerful and steady enemy advance the 77th Division abandoned the defensive line along the Tordera and withdrew to the town of Vic, which it lost on 1 February.

Geographic entities mentioned:
surface_form: tordera
instance_of: Watercourse
countries: Spain
coordinates: lat: 41.803521
lon: 2.418014
It is currently governed by Archeparch Ibrahim M. Ibrahim, BS. Territory and statistics. The archeparchy includes most of the Beqaa Valley in Lebanon. Its archeparchial seat is the city of Zahleh, where is located the Cathedral of Our Lady of Deliverance, built in the 18th century. The territory is divided into 39 parishes and there were 150,000 Melkite Catholics in 2012. History.

Geographic entities mentioned:
surface_form: Beqaa Valley
instance_of: Valley
countries: Lebanon
coordinates: lat: 34.008888888889
lon: 36.145277777778
History. The Archeparchy of Zahle and Forzol is a Greco-Melchite archeparchy in the Beqaa Valley, Lebanon and has its origins in the 5th century. In the seventeenth, or perhaps in the 16th century, the diocese of Seleucia Pieria was for greater safety transferred by the Patriarch of Antioch to Maaloula in the Lebanon.

Geographic entities mentioned:
surface_form: Beqaa Valley
instance_of: Valley
countries: Lebanon
coordinates: lat: 34.008888888889
lon: 36.145277777778
Robert P. Oberhelman. president of Oberhellmann Vineyards, on behalf of local vintners, proposing a viticultural area in Gillespie County to be named &quot;Bell Mountain.&quot;
The AVA is on the northern rim of the Edwards Plateau, and north of its Peak is a region referred to as the &quot;Llano Uplift&quot;.

Geographic entities mentioned:
surface_form: Edwards Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 30.3
lon: -99.6
It was inaugurated in November 2018. Course. The Notora has its sources in the fringes of the Lena Plateau near Amga village, not far to the southeast from the Amga river valley. The river flows roughly eastwards all along its course. In its last stretch it enters the wide floodplain of the Aldan and makes a slight bend to the northeast.

Geographic entities mentioned:
surface_form: Lena Plateau
instance_of: Plateau
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.75
lon: 125
There are three unnamed secondary inflows: one at the east, and two at the southwest. The primary outflow, at the southeast, is also the Gull River, which flows to its mouth at Balsam Lake. Balsam Lake flows via the main Kawartha Lakes chain, the Otonabee River and the Trent River to the Bay of Quinte on Lake Ontario. Geology.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
surface_form: kawartha lakes
instance_of: Group of lakes
countries: Canada
coordinates: lat: 44.4994
lon: -78.441
surface_form: balsam lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.580555555556
lon: -78.841666666667
Silver Lake (Kawartha Lakes). Silver Lake is a small lake in the city of Kawartha Lakes in Central Ontario, Canada. Located near the community of Coboconk, it is the lowest lake on the Gull River, a drainage basin that supplies water at its mouth to Balsam Lake at the top of the Trent-Severn Waterway.

Geographic entities mentioned:
surface_form: kawartha
instance_of: Group of lakes
countries: Canada
coordinates: lat: 44.4994
lon: -78.441
surface_form: silver lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.8275
lon: -76.59944444444444
surface_form: silver lake
instance_of: Lake
countries: Canada
surface_form: silver lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.68416666666667
lon: -78.79916666666666
Geography. Silver Lake forms a portion of the boundary between the geographic townships of Somerville and Bexley. It is the southernmost lake in a chain of reservoirs feeding the Trent-Severn Waterway at its highest point. The primary inflow is the Gull River arriving at the north from Shadow Lake. There are three unnamed secondary inflows: one at the east, and two at the southwest.

Geographic entities mentioned:
surface_form: shadow lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.719444444444
lon: -78.793611111111
Located near the community of Coboconk, it is the lowest lake on the Gull River, a drainage basin that supplies water at its mouth to Balsam Lake at the top of the Trent-Severn Waterway. Like many other lakes in the Kawarthas, Silver Lake lies in a depression formed between the Precambrian granite to the north, and the Ordovician limestone to the south. Geography.

Geographic entities mentioned:
surface_form: silver lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.8275
lon: -76.59944444444444
surface_form: silver lake
instance_of: Lake
countries: Canada
surface_form: silver lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.68416666666667
lon: -78.79916666666666
Like many other lakes in the Kawarthas, Silver Lake lies in a depression formed between the Precambrian granite to the north, and the Ordovician limestone to the south. Geography. Silver Lake forms a portion of the boundary between the geographic townships of Somerville and Bexley. It is the southernmost lake in a chain of reservoirs feeding the Trent-Severn Waterway at its highest point.

Geographic entities mentioned:
surface_form: silver lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.8275
lon: -76.59944444444444
surface_form: silver lake
instance_of: Lake
countries: Canada
surface_form: silver lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.68416666666667
lon: -78.79916666666666
Geology. The lake sits atop the dividing line between the Precambrian granite Canadian Shield to the north, and the Paleozoic and Ordovician limestone to the south. Granite outcroppings can be seen beginning at the midpoint of the lake, including a small island in the north end of the lake with a cottage built upon it.

Geographic entities mentioned:
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
Silver Lake (Kawartha Lakes). Silver Lake is a small lake in the city of Kawartha Lakes in Central Ontario, Canada. Located near the community of Coboconk, it is the lowest lake on the Gull River, a drainage basin that supplies water at its mouth to Balsam Lake at the top of the Trent-Severn Waterway.

Geographic entities mentioned:
surface_form: balsam lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.580555555556
lon: -78.841666666667
The primary inflow is the Gull River arriving at the north from Shadow Lake. There are three unnamed secondary inflows: one at the east, and two at the southwest. The primary outflow, at the southeast, is also the Gull River, which flows to its mouth at Balsam Lake. Balsam Lake flows via the main Kawartha Lakes chain, the Otonabee River and the Trent River to the Bay of Quinte on Lake Ontario.

Geographic entities mentioned:
surface_form: balsam lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.580555555556
lon: -78.841666666667
Linnaeus Terrace. dlc8xonty51d0bpct5sgn2vkhxirc" xml:space="preserve">Linnaeus Terrace is a rock terrace on the north side of Oliver Peak in the Asgard Range of Victoria Land, Antarctica. It is protected under the Antarctic Treaty System as Antarctic Specially Protected Area No.138 because it is one of the richest known sites for the cryptoendolithic communities that colonise the Beacon Sandstone.

Geographic entities mentioned:
surface_form: Oliver Peak
instance_of: Mountain
coordinates: lat: -77.61666667
lon: 161.05
Chennakeshava Temple, Somanathapura. The Chennakesava Temple, also referred to as Chennakeshava Temple and Keshava Temple'&quot;, is a Vaishnava Hindu temple on the banks of River Kaveri at Somanathapura, Mysuru, Karnataka, India.The temple was consecrated in 1258 CE by Somanatha Dandanayaka, a general of the Hoysala King Narasimha III. It is located east of Mysuru city.

Geographic entities mentioned:
surface_form: Kaveri
instance_of: Watercourse
countries: India
coordinates: lat: 11.370345
lon: 79.828105
Weardale. Weardale is a dale, or valley, on the east side of the Pennines in County Durham, England. Large parts of Weardale fall within the North Pennines Area of Outstanding Natural Beauty (AONB) – the second-largest AONB in England and Wales. The upper dale is surrounded by high fells (up to O.D. at Burnhope Seat) and heather grouse moors.

Geographic entities mentioned:
surface_form: Burnhope Seat
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.732019444444
lon: -2.3353888888889
Weardale. Weardale is a dale, or valley, on the east side of the Pennines in County Durham, England. Large parts of Weardale fall within the North Pennines Area of Outstanding Natural Beauty (AONB) – the second-largest AONB in England and Wales. The upper dale is surrounded by high fells (up to O.D. at Burnhope Seat) and heather grouse moors.

Geographic entities mentioned:
surface_form: weardale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.716
lon: -1.925
at Burnhope Seat) and heather grouse moors. The River Wear flows through Weardale before reaching Bishop Auckland and then Durham, meeting the sea at Sunderland. The Wear Valley local government district covered the upper part of the dale, including Weardale, between 1974 and 2009, when it was abolished on County Durham's becoming a unitary authority.

Geographic entities mentioned:
surface_form: weardale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.716
lon: -1.925
The Wear Valley local government district covered the upper part of the dale, including Weardale, between 1974 and 2009, when it was abolished on County Durham's becoming a unitary authority. (From 1894 to 1974 there was a Weardale Rural District.) Upper Weardale is in the parliamentary constituency of North West Durham.

Geographic entities mentioned:
surface_form: weardale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.716
lon: -1.925
surface_form: weardale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.716
lon: -1.925
The dale's principal settlements include St John's Chapel and the towns of Crook, Stanhope and Wolsingham. Local climate. Weardale's winters are typically harsh and prolonged with regular snow, nowadays taken advantage of by skiers using a ski run at Swinhope Head. Wildlife and ecology. Wildlife includes an important population of black grouse, along with the more usual upland birds.

Geographic entities mentioned:
surface_form: weardale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.716
lon: -1.925
The Bishops of Durham owned the mineral rights and the Church retained them throughout the effective life of the lead industry, miners and companies being lessees. In 1327 Edward III led his first military campaign in Weardale. The so-called Weardale campaign against the Scots was a military failure but led to the politically important Treaty of Edinburgh–Northampton.

Geographic entities mentioned:
surface_form: weardale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.716
lon: -1.925
surface_form: weardale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.716
lon: -1.925
High House Chapel near Ireshopeburn has been claimed to be the Methodist chapel with the longest history of continuous use in the world and contains the Weardale Museum (not to be confused with the Lead Mining Museum at Killhope), which includes a room devoted to Methodist and Wesley memorabilia. As a youth between the world wars the poet W. H.

Geographic entities mentioned:
surface_form: weardale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.716
lon: -1.925
H. Auden walked amid the wild countryside and the relics of the lead-mining industry in and around Weardale and found them a lifelong source of inspiration. One place he visited, Rookhope, is also the setting of a border ballad, 'The Rookhope Ryde', which describes in some detail how in 1569 Weardale men drove out a party of cattle-raiders who had come down from the Roman wall area.

Geographic entities mentioned:
surface_form: weardale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.716
lon: -1.925
Weardale was historically important for lead mining and there is a lead-mining museum incorporating the preserved Park Level Mine at Killhope (pronounced &quot;Killup&quot;). The first documented evidence of mining in the Northern Pennines dates from the 12th century and records the presence of silver mines in the areas of what are now Alston Moor, just west of Weardale, and Northumberland.

Geographic entities mentioned:
surface_form: weardale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.716
lon: -1.925
surface_form: weardale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.716
lon: -1.925
at the Cornish Hush Mine. During the 1880s declining prices for lead forced both companies to give up their leases in the area, though the Weardale Lead Company continued lead mining and smelting until 1931. According to Dunham (1990) 28 separate lead-smelting operations were active in the region during the height of mining in the 19th century but by 1919 the last major commercial mine had closed.

Geographic entities mentioned:
surface_form: weardale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.716
lon: -1.925
Of these, only a business at Tow Law persists (2009) as a going concern. Limestone quarrying continued into and beyond the 1960s, a relatively recent and large-scale development being the quarry serving the Blue Circle cement works near Eastgate, set up in the 1960s. This site has now been decommissioned and the major industry in Weardale is now cattle- and sheep-farming.

Geographic entities mentioned:
surface_form: weardale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.716
lon: -1.925
Weardale had a railway as far as Wearhead in three stages opened in 1847, 1862 and 1895, but the section of the line above Eastgate closed between 1961 and 1968 in another series of three closures owing to the decline of the lead industry. The remaining line was kept open by cement traffic and excursions until 1993, after which it was eventually taken over by the Weardale Railway.

Geographic entities mentioned:
surface_form: weardale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.716
lon: -1.925
Currently there is a regular Monday to Saturday bus service provided by Weardale Motor Services from Bishop Auckland and Crook to Cowshill at the head of the dale; it is possible at certain times of day to take the bus further on to the Killhope Lead Mining Museum and to return by bus from it at the times of the year when it is open.

Geographic entities mentioned:
surface_form: weardale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.716
lon: -1.925
People had forgotten &ndash; and now we have come to accept &ndash; that the Afghan war was going out of control. When I got to the Korangal Valley, and there was lots of fighting going on, it completely surprised me. I was gobsmacked. At the end of October 2007, 70 percent of American bombs being dropped were in that valley, and the casualty rate was at 25 percent wounded.

Geographic entities mentioned:
surface_form: Korangal Valley
instance_of: Valley
countries: Afghanistan
coordinates: lat: 34.881230555556
lon: 70.905161111111
By the early thirteenth century the lordships of the Guidi counts dotted the Apennines between Romagna and Tuscany, from the Mugello to the Casentino, and other lordships subject to them lay in the lower Valdarno west of Florence (Empoli and other castellanies), the upper Valdarno, the Pratomagno and the Val d'Ambra.

Geographic entities mentioned:
surface_form: Mugello
instance_of: Valley
countries: Italy
coordinates: lat: 43.95
lon: 11.3833
surface_form: Casentino
instance_of: Valley
countries: Italy
coordinates: lat: 43.7
lon: 11.816666666667
surface_form: lower Valdarno
instance_of: Valley
countries: Italy
coordinates: lat: 43.566666666667
lon: 11.533333333333
surface_form: upper Valdarno
instance_of: Valley
countries: Italy
coordinates: lat: 43.566666666667
lon: 11.533333333333
surface_form: Pratomagno
instance_of: Mountain
countries: Italy
coordinates: lat: 43.65
lon: 11.65
It is sometimes mistaken for Wheeler Peak, since it is along the standard route to Wheeler. Lake Fork Peak at lies just across Williams Lake and to the west of Wheeler Mountain. Taos Ski Valley lies to the northwest of Wheeler Peak, while both the town of Taos and Taos Pueblo are about to the southwest. Wheeler Peak is the focus of the Wheeler Peak Wilderness area in the Carson National Forest.

Geographic entities mentioned:
surface_form: Lake Fork Peak
instance_of: Mountain
countries: United States
coordinates: lat: 36.550277777778
lon: -105.44527777778
surface_form: williams lake
instance_of: Lake
countries: United States
coordinates: lat: 42.675699
lon: -83.423332
surface_form: wheeler mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.380555555556
lon: -106.13611111111
Another alternate route is to begin from the nearby ski resort of Red River. From the town of Red River drive 6.4 miles south on NM 578, then 1.3 miles on FR 58 to the trailhead parking area. From the parking area Wheeler peak is about 7 miles on Forest Trail 91. This route passes two alpine lakes, Lost Lake and Horseshoe Lake. Wheeler Peak has a summit register as do many major western peaks.

Geographic entities mentioned:
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 40.4725
lon: -121.336
surface_form: lost lake
instance_of: Lake
countries: United States
coordinates: lat: 42.5933
lon: -71.528
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 47.30912222222222
lon: -122.04138333333333
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 37.1489
lon: -89.355
surface_form: lost lake
instance_of: Lake
countries: United States
coordinates: lat: 43.9153
lon: -85.0356
surface_form: lost lake
instance_of: Lake
countries: United States
coordinates: lat: 44.4326
lon: -121.91
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 46.02805556
lon: -95.68916667
surface_form: lost lake
instance_of: Lake
countries: United States
coordinates: lat: 45.9651
lon: -89.4833
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 46.3087
lon: -121.569
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 45.59194444
lon: -93.05361111
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 37.6087742
lon: -119.0194324
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 47.40822
lon: -122.6643413
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 38.6994
lon: -90.085
surface_form: lost lake
instance_of: Lake
countries: United States
coordinates: lat: 45.489444444444
lon: -121.82166666667
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 46.119166666667
lon: -94.830277777778
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 47.4411
lon: -93.4733
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 45.459166666667
lon: -93.05
surface_form: lost lake
instance_of: Lake
countries: United States
coordinates: lat: 45.0305693
lon: -93.415597
surface_form: lost lake
instance_of: Lake
countries: United States
coordinates: lat: 43.6814
lon: -97.0581
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 44.131666666667
lon: -74.620833333333
surface_form: lost lake
instance_of: Lake
countries: United States
coordinates: lat: 38.8605
lon: -120.097
Wheeler Peak (New Mexico). Wheeler Peak is the highest natural point in the U.S. state of New Mexico. It is located northeast of Taos and south of Red River in the northern part of the state, and just southeast of the ski slopes of Taos Ski Valley. It lies in the Sangre de Cristo Mountains, the southernmost subrange of the Rocky Mountains. The peak's elevation is.

Geographic entities mentioned:
surface_form: wheeler peak
instance_of: Mountain
countries: United States
coordinates: lat: 36.5569
lon: -105.417
surface_form: wheeler peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.9861
lon: -114.313
Nearby peaks and features. Just north of Wheeler Peak is Mount Walter. At it is the second highest named summit in New Mexico, but it is not usually considered an independent peak as it has only about of topographic prominence. It is sometimes mistaken for Wheeler Peak, since it is along the standard route to Wheeler.

Geographic entities mentioned:
surface_form: wheeler peak
instance_of: Mountain
countries: United States
coordinates: lat: 36.5569
lon: -105.417
surface_form: mount walter
instance_of: Mountain
countries: United States
coordinates: lat: 36.5623
lon: -105.414
surface_form: wheeler peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.9861
lon: -114.313
Just north of Wheeler Peak is Mount Walter. At it is the second highest named summit in New Mexico, but it is not usually considered an independent peak as it has only about of topographic prominence. It is sometimes mistaken for Wheeler Peak, since it is along the standard route to Wheeler. Lake Fork Peak at lies just across Williams Lake and to the west of Wheeler Mountain.

Geographic entities mentioned:
surface_form: wheeler peak
instance_of: Mountain
countries: United States
coordinates: lat: 36.5569
lon: -105.417
surface_form: wheeler peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.9861
lon: -114.313
It is sometimes mistaken for Wheeler Peak, since it is along the standard route to Wheeler. Lake Fork Peak at lies just across Williams Lake and to the west of Wheeler Mountain. Taos Ski Valley lies to the northwest of Wheeler Peak, while both the town of Taos and Taos Pueblo are about to the southwest. Wheeler Peak is the focus of the Wheeler Peak Wilderness area in the Carson National Forest.

Geographic entities mentioned:
surface_form: wheeler peak
instance_of: Mountain
countries: United States
coordinates: lat: 36.5569
lon: -105.417
surface_form: wheeler peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.9861
lon: -114.313
Lake Fork Peak at lies just across Williams Lake and to the west of Wheeler Mountain. Taos Ski Valley lies to the northwest of Wheeler Peak, while both the town of Taos and Taos Pueblo are about to the southwest. Wheeler Peak is the focus of the Wheeler Peak Wilderness area in the Carson National Forest. Much of the mountain area just south of the peak is on Taos Pueblo land.

Geographic entities mentioned:
surface_form: wheeler peak
instance_of: Mountain
countries: United States
coordinates: lat: 36.5569
lon: -105.417
surface_form: wheeler peak
instance_of: Mountain
countries: United States
coordinates: lat: 36.5569
lon: -105.417
surface_form: wheeler peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.9861
lon: -114.313
surface_form: wheeler peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.9861
lon: -114.313
Much of the mountain area just south of the peak is on Taos Pueblo land. Some was returned to the pueblo from the Carson National Forest in 1970
Climbing. The standard route on Wheeler Peak is along the north ridge. The route starts at the parking lot for Taos Ski Valley, and proceeds east along an old road to a broad saddle at Bull-of-the-Woods Meadow.

Geographic entities mentioned:
surface_form: wheeler peak
instance_of: Mountain
countries: United States
coordinates: lat: 36.5569
lon: -105.417
surface_form: wheeler peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.9861
lon: -114.313
The route starts at the parking lot for Taos Ski Valley, and proceeds east along an old road to a broad saddle at Bull-of-the-Woods Meadow. It then turns south and winds its way among minor peaks and small valleys to gain Wheeler Peak from the north, going over the summit of Mount Walter along the way. This is a practical route, even in winter, due to low (but nonzero) avalanche exposure.

Geographic entities mentioned:
surface_form: wheeler peak
instance_of: Mountain
countries: United States
coordinates: lat: 36.5569
lon: -105.417
surface_form: mount walter
instance_of: Mountain
countries: United States
coordinates: lat: 36.5623
lon: -105.414
surface_form: wheeler peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.9861
lon: -114.313
Another alternate route is to begin from the nearby ski resort of Red River. From the town of Red River drive 6.4 miles south on NM 578, then 1.3 miles on FR 58 to the trailhead parking area. From the parking area Wheeler peak is about 7 miles on Forest Trail 91. This route passes two alpine lakes, Lost Lake and Horseshoe Lake. Wheeler Peak has a summit register as do many major western peaks.

Geographic entities mentioned:
surface_form: wheeler peak
instance_of: Mountain
countries: United States
coordinates: lat: 36.5569
lon: -105.417
surface_form: wheeler peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.9861
lon: -114.313
The standard route on Wheeler Peak is along the north ridge. The route starts at the parking lot for Taos Ski Valley, and proceeds east along an old road to a broad saddle at Bull-of-the-Woods Meadow. It then turns south and winds its way among minor peaks and small valleys to gain Wheeler Peak from the north, going over the summit of Mount Walter along the way.

Geographic entities mentioned:
surface_form: bull
instance_of: Watercourse
countries: United States
coordinates: lat: 49.46663
lon: -115.45205