Sarmila/GeoWiki-Features huggingface dataset:
The region is noted for numerous lakes, waterfalls, and dense coniferous forests interspersed with alpine meadows. Major sites in the immediate vicinity that can be accessed by trails include Lake Josephine, Grinnell Lake, the Grinnell Glacier, Cracker Lake, Granite Park Chalet, the Iceberg Cirque, and the Ptarmigan Tunnel, a hiking tunnel carved through the mountainside during the 1930s.

Geographic entities mentioned:
surface_form: Grinnell Lake
instance_of: Lake
countries: United States
coordinates: lat: 48.766111111111
lon: -113.70416666667
surface_form: Cracker Lake
instance_of: Lake
countries: United States
coordinates: lat: 48.7444
lon: -113.643
The Saint Mary together with the Belly River and Waterton River drain a small portion of Montana, in the United States, to the Hudson Bay watershed in Canada. The river rises as a stream on Gunsight Mountain in Glacier National Park and flows into Gunsight Lake, then into Saint Mary Lake, exits the park and flows on into Lower St. Mary Lake in the Blackfeet Indian Reservation.

Geographic entities mentioned:
surface_form: Gunsight Lake
instance_of: Lake
countries: United States
coordinates: lat: 48.6233
lon: -113.72
surface_form: Saint Mary Lake
instance_of: Lake
countries: United States
coordinates: lat: 48.682777777778
lon: -113.54555555556
Chief Mountain. Nínaiistáko is located northwest of Babb on the border of Glacier National Park and the Blackfeet Indian Reservation. The mountain is one of the most prominent peaks and rock formations along the Rocky Mountain Front, a overthrust fault, known as the Lewis Overthrust, which extends from central Montana into southern Alberta.

Geographic entities mentioned:
surface_form: Nínaiistáko
instance_of: Mountain
countries: United States
coordinates: lat: 48.933833
lon: -113.610047
Location. The peak is located at, which is northwest of Mount Bowles (, summit of Bowles Ridge), north-northwest of Rayna Knyaginya Peak, north-northeast of Chirpan Peak, northeast of Rezen Knoll, m east by north of Aleko Point, and south by east of the summit of Gleaner Heights () (Rough British mapping in 1968, Bulgarian mapping from a 1995-96 ground survey).

Geographic entities mentioned:
surface_form: Mount Bowles
instance_of: Mountain
coordinates: lat: -62.616666666667
lon: -60.202222222222
surface_form: Rayna Knyaginya Peak
instance_of: Mountain
coordinates: lat: -62.6125
lon: -60.213611111111
surface_form: Rezen Knoll
instance_of: Mountain
coordinates: lat: -62.6253
lon: -60.2769
surface_form: Gleaner Heights
instance_of: Landform
Mountain
coordinates: lat: -62.5736
lon: -60.2331
surface_form: bowles
instance_of: Mountain
coordinates: lat: -61.283333333333
lon: -54.133333333333
surface_form: bowles
instance_of: Mountain
coordinates: lat: -61.283333333333
lon: -54.133333333333
surface_form: bowles
instance_of: Mountain
coordinates: lat: -62.616666666667
lon: -60.202222222222
surface_form: bowles
instance_of: Mountain
coordinates: lat: -62.616666666667
lon: -60.202222222222
The feature is breast-shaped, long in east-west direction and wide, and overlooks Kaliakra Glacier to the northeast and Perunika Glacier to the southwest. Hemus is an ancient name of Stara Planina (Balkan Mountains), the central mountain range separating northern from southern Bulgaria. Location.

Geographic entities mentioned:
surface_form: southern
instance_of: Mountain
coordinates: lat: -74.2
lon: -76.4667
Hemus Peak. Hemus Peak (,) is an ice-covered peak rising to off the northwest extremity of Bowles Ridge in eastern Livingston Island. The feature is breast-shaped, long in east-west direction and wide, and overlooks Kaliakra Glacier to the northeast and Perunika Glacier to the southwest.

Geographic entities mentioned:
surface_form: bowles
instance_of: Mountain
coordinates: lat: -61.283333333333
lon: -54.133333333333
surface_form: hemus peak
instance_of: Mountain
coordinates: lat: -62.606111111111
lon: -60.220555555556
surface_form: bowles
instance_of: Mountain
coordinates: lat: -62.616666666667
lon: -60.202222222222
Hemus Peak. Hemus Peak (,) is an ice-covered peak rising to off the northwest extremity of Bowles Ridge in eastern Livingston Island. The feature is breast-shaped, long in east-west direction and wide, and overlooks Kaliakra Glacier to the northeast and Perunika Glacier to the southwest.

Geographic entities mentioned:
surface_form: hemus peak
instance_of: Mountain
coordinates: lat: -62.606111111111
lon: -60.220555555556
The tall mountain is located in the Jotunheimen mountains, about north of the village of Vang i Valdres. The mountain is surrounded by several other notable mountains including Rasletinden and Kalvehøgde to the northeast, Nørdre Kalvehølotinden to the east, Galdeberget and Oksedalshøi to the west, and Langedalstinden to the northwest.

Geographic entities mentioned:
surface_form: Kalvehøgde
instance_of: Mountain
countries: Norway
coordinates: lat: 61.393055555556
lon: 8.6194444444444
surface_form: Nørdre Kalvehølotinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.37111111
lon: 8.63055556
surface_form: Galdeberget
instance_of: Mountain
countries: Norway
coordinates: lat: 61.38055556
lon: 8.44222222
surface_form: Oksedalshøi
instance_of: Mountain
countries: Norway
coordinates: lat: 61.38787
lon: 8.40451
surface_form: Langedalstinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.400833333333
lon: 8.5233333333333
It is situated on the northern shore of lake Bygdin on the western side of the Svartdalen Valley and is the southernmost and most prominent summit on a rather long ridge containing twelve more 2000 m peaks. Torfinnstindene has three main summits: Øystre Torfinnstind, Midtre Torfinnstind, and Vestre Torfinnstind (Eastern, Middle and Western).

Geographic entities mentioned:
surface_form: Bygdin
instance_of: Lake
countries: Norway
coordinates: lat: 61.348475
lon: 8.518661
The name is also found in the valley due west of the summits, the small glacier covering parts of the extremely steep north wall, the sharp ridge pointing northwards from the Western summit and the tourist lodge situated on lake Bygdin south of the mountain. The summits are the southernmost peaks in Norway, except for one other peak further south.

Geographic entities mentioned:
surface_form: Bygdin
instance_of: Lake
countries: Norway
coordinates: lat: 61.348475
lon: 8.518661
The climb up the lowest, western summit, is quite easy, but many would prefer to use a rope on a short part of the climb. From the western summit, a sharp edge leads down to the long ridge turning northwards towards lake Gjende. The rest of the descent is long talus slopes.

Geographic entities mentioned:
surface_form: Gjende
instance_of: Lake
countries: Norway
coordinates: lat: 61.489444444444
lon: 8.68
surface_form: gjende
instance_of: Lake
countries: Norway
coordinates: lat: 61.489444444444
lon: 8.68
Torfinnstindene. Torfinnstindene is a mountain in Vang Municipality in Innlandet county, Norway. The tall mountain is located in the Jotunheimen mountains, about north of the village of Vang i Valdres.

Geographic entities mentioned:
surface_form: valdres
instance_of: Valley
countries: Norway
coordinates: lat: 60.916666666667
lon: 9.1666666666667
Torfinnstindene. Torfinnstindene is a mountain in Vang Municipality in Innlandet county, Norway. The tall mountain is located in the Jotunheimen mountains, about north of the village of Vang i Valdres.

Geographic entities mentioned:
surface_form: torfinnstindene
instance_of: Mountain
countries: Norway
coordinates: lat: 61.372222222222
lon: 8.5805555555556
It is situated on the northern shore of lake Bygdin on the western side of the Svartdalen Valley and is the southernmost and most prominent summit on a rather long ridge containing twelve more 2000 m peaks. Torfinnstindene has three main summits: Øystre Torfinnstind, Midtre Torfinnstind, and Vestre Torfinnstind (Eastern, Middle and Western).

Geographic entities mentioned:
surface_form: torfinnstindene
instance_of: Mountain
countries: Norway
coordinates: lat: 61.372222222222
lon: 8.5805555555556
The summits are the southernmost peaks in Norway, except for one other peak further south. The mountain is made of the extremely hard gabbro rock. The gabbro in Torfinnstindene is partly of the normal &quot;gray-with-black-specs&quot; variety, but parts of the eastern summit are of a red variety. The view from the summits, particularly the Eastern, is one of the best in southern Norway.

Geographic entities mentioned:
surface_form: torfinnstindene
instance_of: Mountain
countries: Norway
coordinates: lat: 61.372222222222
lon: 8.5805555555556
Under the overall leadership of the Austrian commander in chief Joseph Nikolaus De Vins, Montferrat launched an offensive in mid-August 1793 to recapture the Duchy of Savoy from the French. Because the French were preoccupied with the Siege of Lyon, the Piedmontese recovered most of the Maurienne and Tarentaise Valleys, but they were stopped just short of Albertville and the reconquest of Savoy.

Geographic entities mentioned:
surface_form: Maurienne
instance_of: Valley
countries: France
coordinates: lat: 45.2
lon: 6.6666666666667
The army's left (north) flank was south of Geneva in the Arve river valley, also called the Faucigny. Going south, the army defended the Isère river valley and its upper reaches, called the Tarentaise Valley; the Arc river valley, also called the Maurienne; the Durance river; and the Ubaye river. The right (south) flank was anchored by the fortified Camp de Tournoux.

Geographic entities mentioned:
surface_form: Maurienne
instance_of: Valley
countries: France
coordinates: lat: 45.2
lon: 6.6666666666667
While this raid rattled Toirdelbach, he demonstrated that he was not weak by attacking the Conmaicne and Breifne, with mixed fortunes; he defeated the former at Mag Na, but his army was defeated by the men of Breifne at Mag Brenair. He attacked the Northern Uí Néill the next year in 1111, plundering Termonn Dabeoc in Tír Chonaill and ravaging modern County Fermanagh as far as Lough Erne.

Geographic entities mentioned:
surface_form: Lough Erne
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.48262
lon: -7.80622
Over Water. Over Water is a small lake or tarn in the north of the English Lake District, southwest of the hamlet of Longlands. Binsey, Great Cockup and Longlands Fell overlook the lake. Over Water was a small natural waterbody which was dammed in 1904 to increase its size. It served as a reservoir supplying drinking water to the town of Wigton until October 2022.

Geographic entities mentioned:
surface_form: Great Cockup
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.6895
lon: -3.12931
surface_form: Longlands Fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.7075
lon: -3.12671
The lake is owned by the National Trust, while the shore is privately owned by a number of different landowners. It is notable for being a feeding place for the Ospreys which breed beside Bassenthwaite Lake. Ospreys are still extremely rare breeding birds in England. There is an official Osprey viewpoint at Dodd Wood in the locality.

Geographic entities mentioned:
surface_form: Bassenthwaite Lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.652
lon: -3.215
surface_form: bassenthwaite lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.652
lon: -3.215
Over Water. Over Water is a small lake or tarn in the north of the English Lake District, southwest of the hamlet of Longlands. Binsey, Great Cockup and Longlands Fell overlook the lake. Over Water was a small natural waterbody which was dammed in 1904 to increase its size. It served as a reservoir supplying drinking water to the town of Wigton until October 2022.

Geographic entities mentioned:
surface_form: over water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.704722222222
lon: -3.1625
Binsey, Great Cockup and Longlands Fell overlook the lake. Over Water was a small natural waterbody which was dammed in 1904 to increase its size. It served as a reservoir supplying drinking water to the town of Wigton until October 2022. Over Water supports a range of flora including water lilies and water lobelia. The name of the tarn has changed over time.

Geographic entities mentioned:
surface_form: over water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.704722222222
lon: -3.1625
Today. The town is located near the San Diego River, just north of the Cleveland National Forest at the junction of Highway 78 and Highway 79. Other notable sights of the small town include the famous Dudley's Bakery and the Julian Apple Pie factory. The town serves as a gateway to the mountain areas of San Diego County, including the Laguna Mountains, Julian, and Palomar Mountain. Climate.

Geographic entities mentioned:
surface_form: Palomar Mountain
instance_of: Mountain
countries: United States
Mexico
coordinates: lat: 33.363483333333
lon: -116.83639444444
The archaeologist Frans de Liagre Böhl has highlighted that the word &quot;Mashu&quot; in Sumerian means &quot;twins&quot;. Jensen and Zimmern thought it to be the geographic location between Mount Lebanon and Mount Hermon in the Anti-Lebanon mountains. Edward Lipiński and P. Kyle McCarter Jr.

Geographic entities mentioned:
surface_form: Mount Hermon
instance_of: Mountain
countries: Lebanon
Israel
Syria
coordinates: lat: 33.4
lon: 35.85
Geography. Hagerman is located in south-central Chaves County approximately west of the Pecos River. New Mexico State Road 2 passes through the town, leading northwest to Roswell, the county seat, and south to Artesia. NM 249 leads east from the center of town to the top of the Mescalero Ridge. According to the United States Census Bureau, the town has a total area of, all land. Demographics.

Geographic entities mentioned:
surface_form: Mescalero Ridge
instance_of: Mountain
countries: United States
coordinates: lat: 33.0431
lon: -103.854
Most of the country has an elevation of less than 200 m. Although Hungary has several moderately high ranges of mountains, those reaching heights of 300 m or more cover less than 2% of the country. The highest point in the country is Kékes (1,014 m) in the Mátra Mountains northeast of Budapest. The lowest spot is 77.6 m above sea level, located in the south of Hungary, near Szeged.

Geographic entities mentioned:
surface_form: Kékes
instance_of: Mountain
countries: Hungary
coordinates: lat: 47.87222222222222
lon: 20.012777777777778
The Tisza River is navigable for 444 km in the country. Less important rivers include the Drava along the Croatian border, the Rába, the Szamos, the Sió, and the Ipoly along the Slovakian border. Hungary has three major lakes. Lake Balaton, the largest, is 78 km long and from 3 to 14 km wide, with an area of 600 square km. Hungarians often refer to it as the &quot;Hungarian Sea&quot;.

Geographic entities mentioned:
surface_form: Lake Balaton
instance_of: Lake
countries: Hungary
coordinates: lat: 46.85
lon: 17.72
It is Central Europe's largest freshwater lake and an important recreation area. Its shallow waters offer good summer swimming, and in winter its frozen surface provides excellent opportunities for winter sports. Smaller bodies of water are Lake Velence (26 square km) in Fejér County and Lake Fertő (Neusiedler See—about 82 square km within Hungary), and the artificial Lake Tisza.

Geographic entities mentioned:
surface_form: Lake Velence
instance_of: Lake
countries: Hungary
coordinates: lat: 47.208333333333
lon: 18.6
Alpokalja (literally &quot;the foothills of the Alps&quot;) is located along the Austrian border; its highest point is Írott-kő with an elevation of 882 metres. The Transdanubian Mountains stretch from the west part of Lake Balaton to the Danube Bend near Budapest, where it meets the North Hungarian Mountains. Its tallest peak is the 757 m high Pilis.

Geographic entities mentioned:
surface_form: Lake Balaton
instance_of: Lake
countries: Hungary
coordinates: lat: 46.85
lon: 17.72
Its tallest peak is the 757 m high Pilis. Mecsek is the southernmost Hungarian mountain range, located north from Pécs - Its highest point is the Zengő with 682 metres. The North Hungarian Mountains lie north of Budapest and run in a northeasterly direction south of the border with Slovakia. The higher ridges, which are mostly forested, have rich coal and iron deposits.

Geographic entities mentioned:
surface_form: Zengő
instance_of: Mountain
countries: Hungary
coordinates: lat: 46.183333333333
lon: 18.383333333333
Minerals are a major resource of the area and have long been the basis of the industrial economies of cities in the region. Viticulture is also important, producing the famous Tokaji wine. The highest peak of it is the Kékes, located in the Mátra mountain range. Climate. Hungary has a mainly continental climate with the rest of the Pannonian Plain, with cold winters and warm to hot summers.

Geographic entities mentioned:
surface_form: Kékes
instance_of: Mountain
countries: Hungary
coordinates: lat: 47.87222222222222
lon: 20.012777777777778
Roland T. Dempster. Roland Tombekai Dempster (1910–1965) was a Liberian writer and literary figure. He was born in Tosoh (on the banks of Lake Piso), Grand Cape Mount County in the Republic of Liberia. He wrote &quot;The Mystic Reformation of Gondolia&quot; in 1953. On January 4, 1960, he wrote &quot;A Song Out of Midnight: Souvenir of the Tubman-Tolbert Inauguration&quot;.

Geographic entities mentioned:
surface_form: Lake Piso
instance_of: Lake
countries: Liberia
coordinates: lat: 6.7352777777778
lon: -11.251111111111
Challhuani. Challhuani (possibly from Aymara &quot;challwa&quot; fish, &quot;-ni&quot; a suffix, &quot;the one with fish&quot;) is mountain in the Carabaya mountain range in the Andes of Peru, about high. It is located in the Puno Region, Carabaya Province, Ajoyani District. Challhuani lies southeast of Queroni.

Geographic entities mentioned:
surface_form: Queroni
instance_of: Mountain
countries: Peru
coordinates: lat: -14.0844
lon: -70.2608
Challhuani. Challhuani (possibly from Aymara &quot;challwa&quot; fish, &quot;-ni&quot; a suffix, &quot;the one with fish&quot;) is mountain in the Carabaya mountain range in the Andes of Peru, about high. It is located in the Puno Region, Carabaya Province, Ajoyani District. Challhuani lies southeast of Queroni.

Geographic entities mentioned:
surface_form: challhuani
instance_of: Mountain
countries: Peru
coordinates: lat: -14.10861111
lon: -70.22333333
The now-dry valley of the original stream is known as a wind gap. Glacier retreat. The Slims River was previously fed by meltwater from the Kaskawulsh Glacier in the Saint Elias Mountains in the Yukon and its waters flowed into Kluane Lake and on to the Bering Sea. Because of climate change, the glacier has rapidly receded and the meltwater no longer feeds the Slims.

Geographic entities mentioned:
surface_form: Kluane Lake
instance_of: Lake
countries: Canada
coordinates: lat: 61.263888888888886
lon: -138.74444444444444
Second Debsconeag Lake. The second lake is the fourth-largest of the chain, but twice as large as the fifth lake. In addition to discharge from the upstream lakes of the Debsconeag chain, the west end of the second lake receives drainage from Big and Little Beaver Ponds, Big and Little Minister Ponds, and Moose Pond. The east end of the second lake overflows into the first lake to the east.

Geographic entities mentioned:
surface_form: fifth lake
instance_of: Lake
countries: United States
coordinates: lat: 43.7480012
lon: -74.7919972
surface_form: second lake
instance_of: Lake
countries: United States
coordinates: lat: 43.722567
lon: -74.9126731
Fourth Debsconeag Lake. The fourth lake is the third-largest of the chain, and holds more water than the combined total of the three smaller lakes. Drainage from the fifth lake enters the north side of the lake, while the east end of the lake overflows into the third lake to the east. This unusually clear lake supports a few brook trout, but is a more favorable habitat for lake trout.

Geographic entities mentioned:
surface_form: fifth lake
instance_of: Lake
countries: United States
coordinates: lat: 43.7480012
lon: -74.7919972
surface_form: third lake
instance_of: Lake
countries: United States
coordinates: lat: 43.7295112
lon: -74.9001732
This unusually clear lake supports a few brook trout, but is a more favorable habitat for lake trout. Fifth Debsconeag Lake. The fifth lake is the second-smallest of the chain. It is three times as large as the smallest sixth lake. Drainage from the upstream ponds enters the west end of the lake, while the east end of the lake overflows into the fourth lake to the southeast.

Geographic entities mentioned:
surface_form: fifth lake
instance_of: Lake
countries: United States
coordinates: lat: 43.7480012
lon: -74.7919972
The sixth lake (sometimes called the sixth &quot;pond&quot;) is the smallest of the chain. The lake supports a population of native brook trout. The east end of the lake overflows into the fifth lake. Debsconeag Ponds. The Eighth Debsconeag Pond at drains through the Seventh Debsconeag Pond at into the chain of lakes downstream of the sixth lake and upstream of the fifth lake.

Geographic entities mentioned:
surface_form: fifth lake
instance_of: Lake
countries: United States
coordinates: lat: 43.7480012
lon: -74.7919972
The lake supports a population of native brook trout. The east end of the lake overflows into the fifth lake. Debsconeag Ponds. The Eighth Debsconeag Pond at drains through the Seventh Debsconeag Pond at into the chain of lakes downstream of the sixth lake and upstream of the fifth lake. These ponds are much smaller than any of the six lakes.

Geographic entities mentioned:
surface_form: fifth lake
instance_of: Lake
countries: United States
coordinates: lat: 43.7480012
lon: -74.7919972
surface_form: sixth lake
instance_of: Lake
countries: United States
coordinates: lat: 43.7492321
lon: -74.7732258
surface_form: chain of lakes
instance_of: Group of lakes
Lake
countries: United States
coordinates: lat: 44.982536
lon: -97.2713448
Third Debsconeag Lake. The third lake is larger than the combined total of all the other lakes in the chain. Drainage from the fourth lake enters the end of the western arm of the lake, while the northwestern arm of the lake overflows into the second lake to the north. This unusually clear lake supports a native population of brook trout and lake trout. Fourth Debsconeag Lake.

Geographic entities mentioned:
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 43.1256
lon: -93.4247
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 44.75388889
lon: -96.6575
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 46.8675
lon: -122.76666666667
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 28.5219
lon: -81.4103
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 39.0616
lon: -122.8272
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 44.3606
lon: -121.993
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 44.1622
lon: -75.4947
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 46.823611111111
lon: -122.47388888889
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 29.5594
lon: -95.05632
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 45.274722222222
lon: -94.445277777778
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 44.7668323
lon: -97.1762718
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 43.7612743
lon: -97.0121224
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 41.8325
lon: -86.421388888889
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 43.6437495
lon: -124.1824432
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 45.1805262
lon: -121.7089251
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 45.69361111
lon: -97.35944444
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 43.988333333333
lon: -74.920555555556
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 43.900277777778
lon: -95.076944444444
The fourth lake is the third-largest of the chain, and holds more water than the combined total of the three smaller lakes. Drainage from the fifth lake enters the north side of the lake, while the east end of the lake overflows into the third lake to the east. This unusually clear lake supports a few brook trout, but is a more favorable habitat for lake trout. Fifth Debsconeag Lake.

Geographic entities mentioned:
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 43.1256
lon: -93.4247
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 44.75388889
lon: -96.6575
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 46.8675
lon: -122.76666666667
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 28.5219
lon: -81.4103
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 39.0616
lon: -122.8272
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 44.3606
lon: -121.993
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 44.1622
lon: -75.4947
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 46.823611111111
lon: -122.47388888889
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 29.5594
lon: -95.05632
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 45.274722222222
lon: -94.445277777778
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 44.7668323
lon: -97.1762718
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 43.7612743
lon: -97.0121224
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 41.8325
lon: -86.421388888889
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 43.6437495
lon: -124.1824432
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 45.1805262
lon: -121.7089251
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 45.69361111
lon: -97.35944444
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 43.988333333333
lon: -74.920555555556
surface_form: clear lake
instance_of: Lake
countries: United States
coordinates: lat: 43.900277777778
lon: -95.076944444444
The population of native brook trout fare poorly in competition with pumpkinseed and yellow perch. Third Debsconeag Lake. The third lake is larger than the combined total of all the other lakes in the chain. Drainage from the fourth lake enters the end of the western arm of the lake, while the northwestern arm of the lake overflows into the second lake to the north.

Geographic entities mentioned:
surface_form: third lake
instance_of: Lake
countries: United States
coordinates: lat: 43.7295112
lon: -74.9001732
Second Debsconeag Lake. The second lake is the fourth-largest of the chain, but twice as large as the fifth lake. In addition to discharge from the upstream lakes of the Debsconeag chain, the west end of the second lake receives drainage from Big and Little Beaver Ponds, Big and Little Minister Ponds, and Moose Pond. The east end of the second lake overflows into the first lake to the east.

Geographic entities mentioned:
surface_form: moose pond
instance_of: Lake
countries: United States
coordinates: lat: 44.0636663
lon: -70.8121557
surface_form: second lake
instance_of: Lake
countries: United States
coordinates: lat: 43.722567
lon: -74.9126731
In addition to discharge from the upstream lakes of the Debsconeag chain, the west end of the second lake receives drainage from Big and Little Beaver Ponds, Big and Little Minister Ponds, and Moose Pond. The east end of the second lake overflows into the first lake to the east. The population of native brook trout fare poorly in competition with pumpkinseed and yellow perch.

Geographic entities mentioned:
surface_form: second lake
instance_of: Lake
countries: United States
coordinates: lat: 43.722567
lon: -74.9126731
surface_form: first lake
instance_of: Lake
countries: United States
coordinates: lat: 43.7178449
lon: -74.9251732
Third Debsconeag Lake. The third lake is larger than the combined total of all the other lakes in the chain. Drainage from the fourth lake enters the end of the western arm of the lake, while the northwestern arm of the lake overflows into the second lake to the north. This unusually clear lake supports a native population of brook trout and lake trout. Fourth Debsconeag Lake.

Geographic entities mentioned:
surface_form: second lake
instance_of: Lake
countries: United States
coordinates: lat: 43.722567
lon: -74.9126731
surface_form: fourth lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3576716
lon: -73.8246423
surface_form: fourth lake
instance_of: Lake
countries: United States
coordinates: lat: 43.7492331
lon: -74.8729512
First Debsconeag Lake. The first lake is the second-largest of the chain, and holds more water than the combined total of the four smaller lakes. The west end of the first lake receives discharge from the upstream lakes of the Debsconeag chain, while the eastern end overflows into the Debsconeag Deadwater on the West Branch at about the same level as the first lake.

Geographic entities mentioned:
surface_form: first lake
instance_of: Lake
countries: United States
coordinates: lat: 43.7178449
lon: -74.9251732
First Debsconeag Lake. The first lake is the second-largest of the chain, and holds more water than the combined total of the four smaller lakes. The west end of the first lake receives discharge from the upstream lakes of the Debsconeag chain, while the eastern end overflows into the Debsconeag Deadwater on the West Branch at about the same level as the first lake.

Geographic entities mentioned:
surface_form: first lake
instance_of: Lake
countries: United States
coordinates: lat: 43.7178449
lon: -74.9251732
surface_form: first lake
instance_of: Lake
countries: United States
coordinates: lat: 43.7178449
lon: -74.9251732
surface_form: west branch
instance_of: Watercourse
countries: United States
coordinates: lat: 45.3333
lon: -69.9697
The west end of the first lake receives discharge from the upstream lakes of the Debsconeag chain, while the eastern end overflows into the Debsconeag Deadwater on the West Branch at about the same level as the first lake. The first lake supports a population of lake trout and land-locked Atlantic salmon. Second Debsconeag Lake.

Geographic entities mentioned:
surface_form: first lake
instance_of: Lake
countries: United States
coordinates: lat: 43.7178449
lon: -74.9251732
Debsconeag Lakes. The chain of Debsconeag Lakes in the North Maine Woods is a tributary to the West Branch Penobscot River. The flow sequence is from the Sixth Debsconeag Lake through the Fifth, Fourth, Third, Second, and First into the Debsconeag Deadwater on the West Branch. First Debsconeag Lake.

Geographic entities mentioned:
surface_form: west branch
instance_of: Watercourse
countries: United States
coordinates: lat: 45.3333
lon: -69.9697
surface_form: debsconeag lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 45.77
lon: -69.04
Debsconeag Lakes. The chain of Debsconeag Lakes in the North Maine Woods is a tributary to the West Branch Penobscot River. The flow sequence is from the Sixth Debsconeag Lake through the Fifth, Fourth, Third, Second, and First into the Debsconeag Deadwater on the West Branch. First Debsconeag Lake.

Geographic entities mentioned:
surface_form: west branch
instance_of: Watercourse
countries: United States
coordinates: lat: 45.3333
lon: -69.9697
This unusually clear lake supports a native population of brook trout and lake trout. Fourth Debsconeag Lake. The fourth lake is the third-largest of the chain, and holds more water than the combined total of the three smaller lakes. Drainage from the fifth lake enters the north side of the lake, while the east end of the lake overflows into the third lake to the east.

Geographic entities mentioned:
surface_form: fourth lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3576716
lon: -73.8246423
surface_form: fourth lake
instance_of: Lake
countries: United States
coordinates: lat: 43.7492331
lon: -74.8729512
Fifth Debsconeag Lake. The fifth lake is the second-smallest of the chain. It is three times as large as the smallest sixth lake. Drainage from the upstream ponds enters the west end of the lake, while the east end of the lake overflows into the fourth lake to the southeast. The lake supports a population of native brook trout in competition with introduced yellow perch.

Geographic entities mentioned:
surface_form: fourth lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3576716
lon: -73.8246423
surface_form: fourth lake
instance_of: Lake
countries: United States
coordinates: lat: 43.7492331
lon: -74.8729512
Fifth Debsconeag Lake. The fifth lake is the second-smallest of the chain. It is three times as large as the smallest sixth lake. Drainage from the upstream ponds enters the west end of the lake, while the east end of the lake overflows into the fourth lake to the southeast. The lake supports a population of native brook trout in competition with introduced yellow perch.

Geographic entities mentioned:
surface_form: sixth lake
instance_of: Lake
countries: United States
coordinates: lat: 43.7492321
lon: -74.7732258
The lake supports a population of native brook trout in competition with introduced yellow perch. Falls below the lake prevent upstream migration into the lake. Sixth Debsconeag Lake. The sixth lake (sometimes called the sixth &quot;pond&quot;) is the smallest of the chain. The lake supports a population of native brook trout. The east end of the lake overflows into the fifth lake.

Geographic entities mentioned:
surface_form: sixth lake
instance_of: Lake
countries: United States
coordinates: lat: 43.7492321
lon: -74.7732258
Debsconeag Lakes. The chain of Debsconeag Lakes in the North Maine Woods is a tributary to the West Branch Penobscot River. The flow sequence is from the Sixth Debsconeag Lake through the Fifth, Fourth, Third, Second, and First into the Debsconeag Deadwater on the West Branch. First Debsconeag Lake.

Geographic entities mentioned:
surface_form: debsconeag lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 45.77
lon: -69.04
Bolton is flanked to the north by Mount Mayo. Bolton Mountain stands within the watershed of Lake Champlain, which drains into Canada's Richelieu River, the Saint Lawrence River, and into the Gulf of Saint Lawrence. The northeast slopes of Bolton Mountain drain into Miller Brook, thence into the Little River, the Winooski River, and into Lake Champlain.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
surface_form: bolton mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.4492
lon: -72.8396
Bolton Mountain (Vermont). Bolton Mountain is a mountain located in Chittenden County, Vermont. Bolton is flanked to the north by Mount Mayo. Bolton Mountain stands within the watershed of Lake Champlain, which drains into Canada's Richelieu River, the Saint Lawrence River, and into the Gulf of Saint Lawrence.

Geographic entities mentioned:
surface_form: bolton mountain (vermont)
instance_of: Mountain
countries: United States
coordinates: lat: 44.4492
lon: -72.8396
Bolton Mountain (Vermont). Bolton Mountain is a mountain located in Chittenden County, Vermont. Bolton is flanked to the north by Mount Mayo. Bolton Mountain stands within the watershed of Lake Champlain, which drains into Canada's Richelieu River, the Saint Lawrence River, and into the Gulf of Saint Lawrence.

Geographic entities mentioned:
surface_form: bolton mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.4492
lon: -72.8396
Bolton is flanked to the north by Mount Mayo. Bolton Mountain stands within the watershed of Lake Champlain, which drains into Canada's Richelieu River, the Saint Lawrence River, and into the Gulf of Saint Lawrence. The northeast slopes of Bolton Mountain drain into Miller Brook, thence into the Little River, the Winooski River, and into Lake Champlain.

Geographic entities mentioned:
surface_form: bolton mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.4492
lon: -72.8396
The northeast slopes of Bolton Mountain drain into Miller Brook, thence into the Little River, the Winooski River, and into Lake Champlain. The southeast slopes of Bolton Mountain drain into Cotton Brook, thence into the Little River. The south end of Bolton drains into Joiner Brook, thence into the Winooski River. The west slopes of Bolton drain into Mill Brook, thence into the Winooski River.

Geographic entities mentioned:
surface_form: bolton mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.4492
lon: -72.8396
The west slopes of Bolton drain into Mill Brook, thence into the Winooski River. The northwest slopes of Bolton drain into Lee River, thence into Browns River, the Lamoille River, and into Lake Champlain. The Long Trail, a 272-mile (438-km) hiking trail running the length of Vermont, crosses the summit of Bolton Mountain.

Geographic entities mentioned:
surface_form: bolton mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.4492
lon: -72.8396
In 1987, Whittaker co-founded RedZone Robotics to develop and sell (or lease) robots that could operate in hazardous environments and situations too dangerous for humans. Whittaker has led teams that have created robots designed to search for fallen meteorites in the ice fields of Antarctica, climb into the craters of active volcanoes in Alaska and Antarctica, and explore the terrain of Mars.

Geographic entities mentioned:
surface_form: Alaska
instance_of: Mountain
countries: United States
coordinates: lat: 61.299722222222
lon: -152.25138888889
When Jan van Riebeek established a refreshment station for the VOC (Dutch East India Company), the Twelve Apostles were covered in forests with lion, leopard and antelope. In competition with the more recent settlers, the Gringqhaique lost their grazing lands on the south east slopes of Table Mountain and in 1657 were restricted to Camps Bay.

Geographic entities mentioned:
surface_form: Table Mountain
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
It is famous for the Ketef Hinnom scrolls, which are the oldest surviving texts from the Hebrew Bible currently known, dated to 600 BC. Ketef Hinnom is adjacent to St. Andrew's Church, now on the grounds of the Menachem Begin Heritage Center. It is located where the Valley of Rephaim and the Valley of Hinnom meet, on the old road from Jerusalem to Bethlehem. History. St.

Geographic entities mentioned:
surface_form: Valley of Rephaim
instance_of: Valley
countries: Israel
coordinates: lat: 31.763202777778
lon: 35.219122222222
The Renclusa refuge (Spanish: &quot;Refugio de la Renclusa&quot;) is a refuge located in the Spanish Pyrenees at the base of the massif de la Maladeta, at high, in the Ésera valley. It is the starting point for excursions to the summit of la Maladeta, of the monts Maudits and Aneto (highest point in the Pyrenees). It lies in the commune of Benasque, north-east of Huesca province, Aragon (Spain).

Geographic entities mentioned:
surface_form: Maladeta
instance_of: Mountain
countries: Spain
coordinates: lat: 42.64722222
lon: 0.63944444
surface_form: Aneto
instance_of: Mountain
countries: Spain
coordinates: lat: 42.63099166666667
lon: 0.6566861111111112
During the 1929 Palestine riots, when Afula was in danger of an attack from the residents of Jenin, women and children were gathered at Feingold House, either on the second floor or in the enclosed courtyard, until the danger passed. With the establishment of the State of Israel, Afula developed and expanded, with new neighborhoods such as Afula Illit and Givat Hamoreh being built.

Geographic entities mentioned:
surface_form: Givat Hamoreh
instance_of: Mountain
countries: Israel
coordinates: lat: 32.615833333333
lon: 35.363611111111
Feingold, Yehudit, and Margaret Palmer all lived in the hotel. The hotel, located at the corner of the streets of Ehad Ha'am and Bialik, also served as a cinema and became a focal point for residents of the Jordan Valley and Lower Galilee. Feingold failed in managing the hotel, and in 1930, he and Palmer declared bankruptcy, but they continued living in the hotel and managing it for others.

Geographic entities mentioned:
surface_form: Jordan Valley
instance_of: Valley
countries: Jordan
coordinates: lat: 32.317222
lon: 35.57
They live at the interface of the forest and the savannah, and their language is a dialect of Tikar, which is related to the Bantu languages. The Bedzan Pygmies also refer to themselves &quot;Tikar&quot;, a name inspired by the Tikar people of Bamenda Grassfields. The Bedzan may have been subjects of the Tikar fondom at one point in the past, which could explain why they speak a dialect of Tikar.

Geographic entities mentioned:
surface_form: Bamenda Grassfields
instance_of: Plateau
countries: Cameroon
coordinates: lat: 6.5
lon: 10.5
Ivano Marzola. Ivano Marzola (born 5 October 1963) is an Italian former alpine skier. Biography. Although Marzola was born in Trieste he is from Val Gardena. He is the brother of the other Italian skier Michaela Marzola.

Geographic entities mentioned:
surface_form: Val Gardena
instance_of: Valley
countries: Italy
coordinates: lat: 46.56
lon: 11.704722
Glenderaterra Beck. Glenderaterra Beck is a watercourse in the county of Cumbria, England. The length of the Glenderaterra, and its major tributary Whit Beck is, which have a total catchment area of. The beck runs from its source on Burnt Horse through the valley between Lonscale Fell and Blencathra to its confluence with the River Greta at Brundholme near Threlkeld.

Geographic entities mentioned:
surface_form: Lonscale Fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.634838888889
lon: -3.1092111111111
surface_form: Blencathra
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.63985
lon: -3.0504611111111
It is longer than the stream in Sinen Gill which in turn is longer than the Burnt Horse contributor. On its southerly course, Glenderaterra Beck is joined by Sinen Gill and Roughten Gill, draining Blease Fell on Blencathra, and, lower down, Whit Beck, emanating from Jenkin Hill on Skiddaw. This river is used by Geography students for A Level and GCSE field studies.

Geographic entities mentioned:
surface_form: Skiddaw
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.651388888889
lon: -3.1477777777778
Hinterrhein (river). The Hinterrhein (;;;;;), or Posterior Rhine, is the right of the two initial tributaries of the Rhine (the other being the &quot;Vorderrhein&quot;). It is located in the canton of Grisons (), Switzerland. One of its upper tributaries is, which is the outflow of Lago di Lei located in Lombardy, Italy.

Geographic entities mentioned:
surface_form: Vorderrhein
instance_of: Watercourse
countries: Switzerland
coordinates: lat: 46.6325
lon: 8.6744444444444
It is located in the canton of Grisons (), Switzerland. One of its upper tributaries is, which is the outflow of Lago di Lei located in Lombardy, Italy. Although it is shorter in length, its volume is larger than that of the &quot;Vorderrhein&quot; at their confluence near Reichenau, after which the river is called the Alpine Rhine, which flows out into Lake Constance (). Course.

Geographic entities mentioned:
surface_form: Lago di Lei
instance_of: Lake
Valley
countries: Switzerland
Italy
coordinates: lat: 46.45205
lon: 9.44323611111111
It is located in the canton of Grisons (), Switzerland. One of its upper tributaries is, which is the outflow of Lago di Lei located in Lombardy, Italy. Although it is shorter in length, its volume is larger than that of the &quot;Vorderrhein&quot; at their confluence near Reichenau, after which the river is called the Alpine Rhine, which flows out into Lake Constance (). Course.

Geographic entities mentioned:
surface_form: Alpine Rhine
instance_of: Valley
countries: Switzerland
Austria
Liechtenstein
coordinates: lat: 47.07013888888889
lon: 9.483347222222223
Course. Flowing from the village Hinterrhein near the San Bernardino Pass through the Rheinwald valley, the river flows into a gorge called Rofla Gorge (). In this gorge, an equal-sized tributary, the Avers Rhine, adds waters from the deep Val Ferrera and the very remote alp of Avers and its side valley Valle di Lei, located on Italian territory.

Geographic entities mentioned:
surface_form: Rheinwald
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.551778
lon: 9.319788
Course. Flowing from the village Hinterrhein near the San Bernardino Pass through the Rheinwald valley, the river flows into a gorge called Rofla Gorge (). In this gorge, an equal-sized tributary, the Avers Rhine, adds waters from the deep Val Ferrera and the very remote alp of Avers and its side valley Valle di Lei, located on Italian territory.

Geographic entities mentioned:
surface_form: Val Ferrera
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.55
lon: 9.43333
surface_form: Valle di Lei
instance_of: Lake
Valley
countries: Switzerland
Italy
coordinates: lat: 46.45205
lon: 9.44323611111111
In this gorge, an equal-sized tributary, the Avers Rhine, adds waters from the deep Val Ferrera and the very remote alp of Avers and its side valley Valle di Lei, located on Italian territory. Below the Rofla Gorge, the valley widens into a section called Schams. The &quot;Hinterrhein&quot; then reaches Andeer, before passing through another gorge, the Viamala, before arriving at Thusis.

Geographic entities mentioned:
surface_form: Schams
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.612
lon: 9.426
It is assumed that Edward had learned photography from his uncle. In 1866, Sealy took his camera and other equipment to the upper Ashburton River and the Rangitata River, and the glaciers that feed these rivers. During the following year, he explored the whole length of the Mueller Glacier and took photos of Mount Cook from there.

Geographic entities mentioned:
surface_form: Mount Cook
instance_of: Mountain
countries: New Zealand
coordinates: lat: -43.595
lon: 170.14194444444445
Many of his photographs are held by the South Canterbury Museum and Canterbury Museum in Christchurch. Von Haast named a number of geographic features in the Southern Alps for him, including Mount Sealy and the Sealy Tarns in the Sealy Range. Sealy Glacier, which feeds Sealy Stream, located in South Westland, are probably also named for Sealy.

Geographic entities mentioned:
surface_form: Mount Sealy
instance_of: Mountain
countries: New Zealand
coordinates: lat: -43.765
lon: 170.045
His brother's house, which was accessed via the same driveway, still stands, is known as 'Craighead', and has given its name to the girls' school, Craighead Diocesan School, that is now occupying the land. When his granddaughter Audrey Barker died in February 1935, the Church of the Good Shepherd at Lake Tekapo was under construction.

Geographic entities mentioned:
surface_form: Lake Tekapo
instance_of: Lake
countries: New Zealand
coordinates: lat: -43.9
lon: 170.525
Petit Encantat. El Petit Encantat is a mountain peak of Catalonia, Spain. Located in the Pyrenees, it is the lower of the two peaks (the other being the Gran Encantat) of the Els Encantats mountain, with an altitude of 2,734 metres above sea level.

Geographic entities mentioned:
surface_form: Gran Encantat
instance_of: Mountain
countries: Spain
coordinates: lat: 42.568527
lon: 1.01466
surface_form: encantats
instance_of: Mountain
countries: Spain
coordinates: lat: 42.568527
lon: 1.01466
surface_form: els encantats
instance_of: Mountain
countries: Spain
coordinates: lat: 42.568527
lon: 1.01466