Sarmila/GeoWiki-Features huggingface dataset:
It was also a refuge site for the Shilshole people when they experienced slave raids coming from the far north, in what is now Alaska and northern British Columbia. It is a glacial lake with its basin having been dug 15,000 years ago by the Puget Lobe of the Cordilleran Ice Sheet, which also created Lake Washington, Union, Green, and Haller Lakes.

Geographic entities mentioned:
surface_form: Lake Washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: Union
instance_of: Lake
countries: United States
coordinates: lat: 47.6392
lon: -122.3337
surface_form: Haller Lakes
instance_of: Lake
countries: United States
coordinates: lat: 47.719619
lon: -122.334688
surface_form: lake washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: lake washington
instance_of: Lake
countries: United States
coordinates: lat: 28.1528
lon: -80.7428
surface_form: lake washington
instance_of: Lake
countries: United States
coordinates: lat: 45.06972222
lon: -94.36166667
surface_form: lake washington
instance_of: Lake
countries: United States
coordinates: lat: 41.9162
lon: -71.757
surface_form: lake washington
instance_of: Lake
countries: United States
coordinates: lat: 41.491
lon: -74.068
surface_form: lake washington
instance_of: Lake
countries: United States
coordinates: lat: 44.243333333333
lon: -93.8725
surface_form: lake washington
instance_of: Lake
countries: United States
coordinates: lat: 38.56499
lon: -121.5536
The lake is situated between Greenwood Avenue North to the west, Linden Avenue North to the east, North 137th Street to the north, and North 130th Street to the south. Bitter Lake drains through a piped outlet at its southeast end that eventually flows into Lake Union.

Geographic entities mentioned:
surface_form: Lake Union
instance_of: Lake
countries: United States
coordinates: lat: 47.6392
lon: -122.3337
surface_form: lake union
instance_of: Lake
countries: United States
coordinates: lat: 47.6392
lon: -122.3337
Bitter Lake (Seattle). Bitter Lake () is a small lake in northwest Seattle, Washington, USA. The lake covers, with a mean depth of and a maximum depth of. Until 1913, a sawmill was located at its southwest corner. Tannic acid from logs dumped into the lake gave its water a bitter taste and the lake itself a name in English.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: bitter lake
instance_of: Lake
countries: United States
coordinates: lat: 43.915227
lon: -97.7117073
surface_form: bitter lake
instance_of: Lake
countries: United States
coordinates: lat: 45.2726302
lon: -97.3246646
surface_form: bitter lake
instance_of: Lake
countries: United States
coordinates: lat: 47.726666666667
lon: -122.35222222222
Bitter Lake (Seattle). Bitter Lake () is a small lake in northwest Seattle, Washington, USA. The lake covers, with a mean depth of and a maximum depth of. Until 1913, a sawmill was located at its southwest corner. Tannic acid from logs dumped into the lake gave its water a bitter taste and the lake itself a name in English.

Geographic entities mentioned:
surface_form: bitter lake
instance_of: Lake
countries: United States
coordinates: lat: 43.915227
lon: -97.7117073
surface_form: bitter lake
instance_of: Lake
countries: United States
coordinates: lat: 45.2726302
lon: -97.3246646
surface_form: bitter lake
instance_of: Lake
countries: United States
coordinates: lat: 47.726666666667
lon: -122.35222222222
It is a glacial lake with its basin having been dug 15,000 years ago by the Puget Lobe of the Cordilleran Ice Sheet, which also created Lake Washington, Union, Green, and Haller Lakes. The Seattle-to-Everett Interurban streetcar reached the lake in 1906, and the Bitter Lake neighborhood was annexed by Seattle in 1954.

Geographic entities mentioned:
surface_form: bitter lake
instance_of: Lake
countries: United States
coordinates: lat: 43.915227
lon: -97.7117073
surface_form: bitter lake
instance_of: Lake
countries: United States
coordinates: lat: 45.2726302
lon: -97.3246646
surface_form: bitter lake
instance_of: Lake
countries: United States
coordinates: lat: 47.726666666667
lon: -122.35222222222
10 oz pistol is elaborately decorated; the pistol's cherry wood stock is inlaid with ivory and staghorn, its metalwork is engraved and sheaved in gold, while the gun's grip is intricately carved. The bodywork of the gun is stamped with a double headed eagle (Charles' symbol as Holy Roman Emperor) and an image of the Pillars of Hercules, a symbol of the Crown of Spain.

Geographic entities mentioned:
surface_form: Pillars of Hercules
instance_of: Landform
countries: Morocco
Spain
Gibraltar
coordinates: lat: 36
lon: -5.35
stutzeri&quot;, &quot;P. mendocina&quot; and &quot;P. putida)&quot; were shown to be isolated from the Lingshui River in China, and could be further used in bioaugmentation to clear contaminated water. In addition to Pseudomonas, &quot;Acinetobacter sp.&quot; SYF26 was isolated from the Heihe reservoir in China.

Geographic entities mentioned:
surface_form: Lingshui River
instance_of: Watercourse
countries: People's Republic of China
coordinates: lat: 18.493055555556
lon: 110.06888888889
While travelling in Kashmir, he recorded and produced a brief history on account of the geography, the culture of the people and the tyrannic Dogra rule over Kashmir. During his brief visit to Kashmir Valley, he authored the first recorded complete encyclopaedia of Kashmir, &quot;The Valley of Kashmir&quot;. In 1896, Lawrence left the Indian Civil Service.

Geographic entities mentioned:
surface_form: Kashmir Valley
instance_of: Valley
countries: India
coordinates: lat: 34.0333
lon: 74.6667
It was made in the Zurich Pottery and Porcelain Factory, which was founded in 1763 by decorator Salomon Gessner. The factory was based in Kilchberg-Schooren on Lake Zurich and produced a mixture of faience (tin-glazed pottery) and &quot;faience fine&quot; (lead-glazed earthenware) alongside the more traditional Zurich ware.

Geographic entities mentioned:
surface_form: Lake Zurich
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.2475
lon: 8.6775
The village lies in a secluded east–west valley between two ridges of the Purbeck Hills. To the north is the main ridge with Povington Hill () and its highest point, Ridgeway Hill (). To the south is the ridge above Gad Cliff that runs from the headland of Worbarrow Tout in the west to the knoll of Tyneham Cap () in the east. Access.

Geographic entities mentioned:
surface_form: Povington Hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 50.6297
lon: -2.1597
Montagne del Morrone. The Montagne del Morrone are a mountain group in Abruzzo, central Italy, part of the Apennines. Overlooking the town of Sulmona, they are bounded by the Valle Peligna, the river Aterno and the Majella massif. They are included into the Majella National Park. The range is composed of limestone, and have their highest peak in the Monte Morrone (2,061 m).

Geographic entities mentioned:
surface_form: Valle Peligna
instance_of: Valley
countries: Italy
coordinates: lat: 42.0803
lon: 13.8878
Montagne del Morrone. The Montagne del Morrone are a mountain group in Abruzzo, central Italy, part of the Apennines. Overlooking the town of Sulmona, they are bounded by the Valle Peligna, the river Aterno and the Majella massif. They are included into the Majella National Park. The range is composed of limestone, and have their highest peak in the Monte Morrone (2,061 m).

Geographic entities mentioned:
surface_form: montagne del morrone
instance_of: Mountain
countries: Italy
coordinates: lat: 42.118675
lon: 13.965736111111111
Haardt. The Haardt () is a range of wooded, sandstone hills in the state of Rhineland-Palatinate in southwestern Germany. The range is some long and lies within the Palatinate Forest (&quot;Pfälzerwald&quot;). Its highest point is the Kalmit, near Maikammer, which stands above sea level.

Geographic entities mentioned:
surface_form: Kalmit
instance_of: Mountain
countries: Germany
coordinates: lat: 49.318888888889
lon: 8.0827777777778
It was listed on the National Register of Historic Places in 1979. Description and history. The Center Meetinghouse occupies a prominent site in the center of Newbury's main village, overlooking the southern end of Lake Sunapee at the eastern corner of the junction of New Hampshire Routes 103 and 103A. It is a single-story wood-frame structure, with a gabled roof and clapboarded exterior.

Geographic entities mentioned:
surface_form: Lake Sunapee
instance_of: Lake
countries: United States
coordinates: lat: 43.375833333333
lon: -72.056388888889
Ganzepoot. The Ganzepoot (Dutch for &quot;goose foot&quot;) is a series of locks and spillways in the inner port of Nieuwpoort, Belgium which connect one river, three water channels and two canals with the mouth of the Yser River and the maritime port. The spillways control the level of the two channels and the drainage of the polders.

Geographic entities mentioned:
surface_form: ganzepoot
instance_of: Lake
countries: Belgium
coordinates: lat: 51.134722
lon: 2.756389
Veslekletten Peak. Veslekletten Peak () is a small mountain about 1 nautical mile (1.9 km) south of Storkletten Peak on the Ahlmann Ridge in Queen Maud Land. It was mapped by Norwegian cartographers from surveys and air photos by the Norwegian-British-Swedish Antarctic Expedition (NBSAE) (1949–52) and named Veslekletten, meaning &quot;the little mountain.&quot;

Geographic entities mentioned:
surface_form: Storkletten Peak
instance_of: Mountain
coordinates: lat: -72.05
lon: -3.41667
surface_form: small
instance_of: Mountain
coordinates: lat: -70.5
lon: 64.7
surface_form: veslekletten peak
instance_of: Mountain
coordinates: lat: -72.0833
lon: -3.43333
Veslekletten Peak. Veslekletten Peak () is a small mountain about 1 nautical mile (1.9 km) south of Storkletten Peak on the Ahlmann Ridge in Queen Maud Land. It was mapped by Norwegian cartographers from surveys and air photos by the Norwegian-British-Swedish Antarctic Expedition (NBSAE) (1949–52) and named Veslekletten, meaning &quot;the little mountain.&quot;

Geographic entities mentioned:
surface_form: veslekletten
instance_of: Mountain
coordinates: lat: -72.0833
lon: -3.43333
It is east of the larger Stickley Lake and is surrounded by a forest of mature jack pine. The lake's outflow is a short stream that flows west into Stickley Lake, which in turn flows south into Upper Fishing Lake. Upper Fishing Lake is along the course of Caribou Creek, which flows into Lower Fishing Lake and eventually on to the Saskatchewan River via Stewart Creek and Torch River. Recreation.

Geographic entities mentioned:
surface_form: Upper Fishing Lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.0567
lon: -104.6603
surface_form: fishing lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.8466
lon: -103.532
It is east of the larger Stickley Lake and is surrounded by a forest of mature jack pine. The lake's outflow is a short stream that flows west into Stickley Lake, which in turn flows south into Upper Fishing Lake. Upper Fishing Lake is along the course of Caribou Creek, which flows into Lower Fishing Lake and eventually on to the Saskatchewan River via Stewart Creek and Torch River. Recreation.

Geographic entities mentioned:
surface_form: Lower Fishing Lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.0334
lon: -104.6337
surface_form: fishing lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.8466
lon: -103.532
surface_form: fishing lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.8466
lon: -103.532
surface_form: stewart creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.31657
lon: -117.2355
surface_form: upper fishing lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.0567
lon: -104.6603
At the campground, there's access to the lake, a boat launch, picnic tables, a fishing cleaning station, and fire pits. It is one of four campgrounds in the Narrow Hills Provincial Park that are RV accessible. The other three are located at Lower Fishing Lake, Zeden Lake, and Ispuchaw Lake. Fish species.

Geographic entities mentioned:
surface_form: Lower Fishing Lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.0334
lon: -104.6337
surface_form: Zeden Lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.98339
lon: -104.6671
surface_form: Ispuchaw Lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.00006
lon: -104.68377
surface_form: fishing lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.8466
lon: -103.532
Baldy Lake. Baldy Lake is a lake in the east-central part of the Canadian province of Saskatchewan in Narrow Hills Provincial Park. It is situated in the Cub Hills and the boreal forest ecozone of Canada. Baldy Lake is accessed from a secondary road that branches off from the Hanson Lake Road. It is east of the larger Stickley Lake and is surrounded by a forest of mature jack pine.

Geographic entities mentioned:
surface_form: baldy lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.10006
lon: -104.63377
Baldy Lake. Baldy Lake is a lake in the east-central part of the Canadian province of Saskatchewan in Narrow Hills Provincial Park. It is situated in the Cub Hills and the boreal forest ecozone of Canada. Baldy Lake is accessed from a secondary road that branches off from the Hanson Lake Road. It is east of the larger Stickley Lake and is surrounded by a forest of mature jack pine.

Geographic entities mentioned:
surface_form: baldy lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.10006
lon: -104.63377
surface_form: hanson lake
instance_of: Lake
countries: Canada
Recreation. Baldy Lake Campground is a small campground located at the northern end of the lake that is RV accessible with 12 non-electric campsites. At the campground, there's access to the lake, a boat launch, picnic tables, a fishing cleaning station, and fire pits. It is one of four campgrounds in the Narrow Hills Provincial Park that are RV accessible.

Geographic entities mentioned:
surface_form: baldy lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.10006
lon: -104.63377
It is one of four campgrounds in the Narrow Hills Provincial Park that are RV accessible. The other three are located at Lower Fishing Lake, Zeden Lake, and Ispuchaw Lake. Fish species. Fish commonly found in Baldy Lake include walleye, yellow perch, white sucker, and northern pike. The lake is periodically stocked with walleye fry.

Geographic entities mentioned:
surface_form: baldy lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.10006
lon: -104.63377
Early on 26 February, the Syrian Army made more advances, recapturing three villages. The advances nearly besieged ISIL forces in a pocket of villages southwest of Lake Jabbul. Later in the day, the Army captured the remaining four villages that ISIL held, thus clearing the road to Aleppo. However, elsewhere, ISIL took control of a village near al-Hamam Mountain, that overlooks the supply road.

Geographic entities mentioned:
surface_form: Lake Jabbul
instance_of: Lake
countries: Syria
coordinates: lat: 36.06666667
lon: 37.5
Aftermath. Between 9 and 10 March, government forces captured 13 villages previously held by ISIL, near the southern bank of Lake Jabbūl, forcing ISIL to set up a new defensive line east of the lake. On 14 April, ISIL launched another offensive on Khanasir, and by the following day they captured hills near the town, the Duraham Oil Field and 10 villages.

Geographic entities mentioned:
surface_form: Lake Jabbūl
instance_of: Lake
countries: Syria
coordinates: lat: 36.06666667
lon: 37.5
The ridge is 2.2 km long in the east-west direction, featuring Sliven Peak and Etropole Peak, with the summit Melnik Peak forming its west extremity. It has partly snow-free southern slopes. The ridge was first surveyed by Lyubomir Ivanov and Doychin Vasilev from Camp Academia on 28 December 2004, as part of 05 topographic survey. Melnik is the name of a town in south-western Bulgaria. Location.

Geographic entities mentioned:
surface_form: Sliven Peak
instance_of: Mountain
coordinates: lat: -62.600972222222
lon: -60.128333333333
surface_form: Etropole Peak
instance_of: Mountain
coordinates: lat: -62.601944444444
lon: -60.140277777778
surface_form: Melnik Peak
instance_of: Mountain
coordinates: lat: -62.601777777778
lon: -60.153111111111
A neighbour city across the Russian border is Kostomuksha. Vartius, one of the border crossing points between Finland and Russia, is located in northern Kuhmo. Kuhmo's eastern border is located at a drainage divider, and the town area is within the drainage basin of Oulujärvi. The municipality is unilingually Finnish. History.

Geographic entities mentioned:
surface_form: Oulujärvi
instance_of: Lake
countries: Finland
coordinates: lat: 64.333333333333
lon: 27.25
The municipality is unilingually Finnish. History. The first inhabitants arrived in Kuhmo after the last ice-age, around 8000 BCE. Proof of Stone Age habitation has been found around Ontojärvi and Lammasjärvi. Sami people inhabited Kuhmo area until migration from Karelia and Savonia pushed Sami people up north. The influence of Sami culture is still found in the placenames.

Geographic entities mentioned:
surface_form: Ontojärvi
instance_of: Lake
countries: Finland
coordinates: lat: 64.1303194
lon: 29.2002292
surface_form: Lammasjärvi
instance_of: Lake
countries: Finland
coordinates: lat: 64.0860875
lon: 29.716875
Akseli Gallen-Kallela, who is considered one of the founders of Karelianism, spent his honeymoon in Kuhmo. During their stay Gallen-Kallela painted some of his works at Lapinsalmi, lake Lentua. Scenery to lake Lentua based the background of the middle picture in his work Aino triptych. During the 19th century burn-beating was still essential in agriculture but in decline.

Geographic entities mentioned:
surface_form: Lentua
instance_of: Lake
countries: Finland
coordinates: lat: 64.23333333
lon: 29.6
Tar was shipped from Kuhmo to Oulu by rowboats. Largest boats could carry 25 – 27 barrels, 125 litres each. Remains of tar pits, where tar was distilled from pine, can be found everywhere in the Kuhmo area. The village of Jonkeri and its surroundings near Lake Jonkeri were transferred from Nurmeksen maalaiskunta to Kuhmo in 1903. The Winter War was an important event in the history of Kuhmo.

Geographic entities mentioned:
surface_form: Lake Jonkeri
instance_of: Lake
countries: Finland
coordinates: lat: 63.84676
lon: 29.90769
Overlook Film Festival. The Overlook Film Festival is an annual film festival that takes place each May, showcasing horror films and live performances. The inaugural event took place at the Timberline Lodge in Mount Hood, Oregon in 2017. Since 2018, the festival has been held in New Orleans, Louisiana. History. The Overlook Film Festival takes place each year in late May.

Geographic entities mentioned:
surface_form: Mount Hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
The Stanley Film Festival went on hiatus in 2016, leading to the creation of the Overlook Film Festival. The 1st annual Overlook Film Festival took place at the Timberline Lodge in Mount Hood, Oregon, which served as the exterior of the Overlook Hotel in the 1980 film &quot;The Shining&quot;.

Geographic entities mentioned:
surface_form: Mount Hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
US has 30 World Cup wins since 1994. Lake Placid, New York hosted the World Luge Congress in 2016 and 2024. Luge facilities are in Lake Placid, Park City, Utah, Muskegon, Michigan, and Negaunee, Michigan. Sled dog racing. Iditarod Trail Sled Dog Race is an annual long-distance sled dog race run in early March from Anchorage to Nome, entirely in the state of Alaska.

Geographic entities mentioned:
surface_form: Lake Placid
instance_of: Mountain
countries: United States
coordinates: lat: 44.21
lon: -73.9293
When working with villagers in the Jimi Valley, Pharoah ran a clinical trial whereby he injected iodised oil into women who were of child-bearing age and found out that cretinism (as congenital iodine deficiency syndrome was known at the time) was caused by iodine deficiency during pregnancy; this led to iodised salt being the only salt imported and thus the disease was eradicated.

Geographic entities mentioned:
surface_form: Jimi Valley
instance_of: Valley
countries: Papua New Guinea
Oasis, Mono County, California. Oasis is an unincorporated community in Mono County, California. It is located in Fish Lake Valley east-southeast of Mount Bancroft. Oasis is at the junction of California State Route 266 and California State Route 168. The 2000 Census reports that Oasis had a population of 22. A post office operated at Oasis from 1873 to 1942.

Geographic entities mentioned:
surface_form: Fish Lake Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.6947
lon: -118.078
surface_form: Mount Bancroft
instance_of: Mountain
countries: United States
coordinates: lat: 39.8416539
lon: -105.7005598
&quot;Chief Commissioner&quot; was a Hudson's Bay Company propeller driven steamship intended for operation on the Saskatchewan River. She was launched in May, 1872, in Fort Garry. However, her draft was too deep, and for her three years of operation, she provided service on Lake Winnipeg. She was retired in 1875, with her components cannibalized and used in other vessels.

Geographic entities mentioned:
surface_form: Lake Winnipeg
instance_of: Lake
countries: Canada
coordinates: lat: 52.116666666667
lon: -97.25
Layton Kor. Layton Kor (June 11, 1938 &ndash; April 21, 2013) was an American rock climber active in the 1960s, whose first ascents and drive for climbing are well known in the climbing world. His routes included many climbs in Eldorado Canyon, near Boulder, Colorado, The Diamond on Longs Peak, towers in the desert southwest, and Yosemite National Park, among other locations.

Geographic entities mentioned:
surface_form: Longs Peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.255013888889
lon: -105.61511388889
Notable among his first ascents is the Kor-Ingalls Route on Castleton Tower and The Finger of Fate Route up the Fisher Towers' Titan; both routes are recognized in the historic climbing text &quot;Fifty Classic Climbs of North America&quot;. Kor also authored the book &quot;Beyond the Vertical&quot;.

Geographic entities mentioned:
surface_form: Castleton Tower
instance_of: Mountain
countries: United States
coordinates: lat: 38.6514
lon: -109.3686
surface_form: Fisher Towers
instance_of: Mountain
countries: United States
coordinates: lat: 38.724
lon: -109.308
In October 2017, the New York City Police Department (NYPD), London's Metropolitan Police Service (MPS) and the Los Angeles Police Department (LAPD) were reviewing allegations against Weinstein following reports about his conduct. The London investigation&mdash;dubbed &quot;Operation Kaguyak&quot;&mdash;reportedly investigated fifteen alleged sexual assaults by Weinstein, dating back to the 1990s.

Geographic entities mentioned:
surface_form: Kaguyak
instance_of: Mountain
countries: United States
coordinates: lat: 58.608
lon: -154.028
Production. Working titles for the film were &quot;Dantley & Vanessa: A Fiberglass Romance&quot;, &quot;Stingray&quot; and &quot;The Hot One&quot;. Scenes of Kenny's high school were filmed at Burbank High School (Burbank, California) in the San Fernando Valley, and Verdugo Hills High School in Tujunga. The novelization of &quot;Corvette Summer&quot; was written by Wayland Drew.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
The Santa Rita Mountains are across the Santa Cruz Valley to the east. The broad Altar Valley lies to the west with the Baboquivari Mountains beyond. Arivaca Road, which connects Arivaca Junction on the east with Arivaca to the southwest at the south end of the Las Guijas Mountains, runs through the valley on the southeast of the Cerro Colorados. Cerro Colorado mine.

Geographic entities mentioned:
surface_form: Altar Valley
instance_of: Valley
countries: United States
coordinates: lat: 31.82
lon: -111.4
In April 1851, the convict ship &quot;Pyrenees&quot; arrived, which forced Governor Charles Fitzgerald to establish depots in country areas. For the Toodyay valley, Michael Clarkson became the Superintendent of the Toodyay Convict Hiring Depot. At first the convicts were housed at the Toodyay Barracks in the Toodyay townsite.

Geographic entities mentioned:
surface_form: Toodyay valley
instance_of: Valley
countries: Australia
coordinates: lat: -31.70198
lon: 115.9620439
East Kill. East Kill, a tributary of Schoharie Creek, flows across the town of Jewett, New York, United States, from its source on Stoppel Point. Ultimately its waters reach the Hudson River via the Mohawk. Since it drains into the Schoharie upstream of Schoharie Reservoir, it is part of the New York City water supply system.

Geographic entities mentioned:
surface_form: Stoppel Point
instance_of: Mountain
countries: United States
coordinates: lat: 42.22509
lon: -74.06514
surface_form: east kill
instance_of: Watercourse
countries: United States
coordinates: lat: 42.23638889
lon: -74.31888889
Ultimately its waters reach the Hudson River via the Mohawk. Since it drains into the Schoharie upstream of Schoharie Reservoir, it is part of the New York City water supply system. East Kill drains the southern slopes of the Blackhead Mountains, which include Thomas Cole Mountain, Black Dome, and Blackhead Mountain, the fourth-, third-, and fifth-highest peaks in the Catskills, respectively.

Geographic entities mentioned:
surface_form: Thomas Cole Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.2708
lon: -74.1362
surface_form: black dome
instance_of: Mountain
countries: United States
coordinates: lat: 42.2701
lon: -74.1226
surface_form: blackhead
instance_of: Mountain
countries: United States
coordinates: lat: 42.2679
lon: -74.1046
surface_form: blackhead
instance_of: Mountain
countries: United States
coordinates: lat: 42.2679
lon: -74.1046
surface_form: east kill
instance_of: Watercourse
countries: United States
coordinates: lat: 42.23638889
lon: -74.31888889
The remainder of the creek drops to an average slope of per mile until it reaches its confluence with Schoharie Creek. East Kill begins on the northwestern slopes of Stoppel Point and begins flowing northwestward, then soon curves to the west. It continues west for a short distance, then flows into Colgate Lake, a lake.

Geographic entities mentioned:
surface_form: Stoppel Point
instance_of: Mountain
countries: United States
coordinates: lat: 42.22509
lon: -74.06514
surface_form: east kill
instance_of: Watercourse
countries: United States
coordinates: lat: 42.23638889
lon: -74.31888889
It exits the lake then passes by the East Kill Valley Church, as it continues along the road. It soon recei
ves Halsey Brook from the north, which drains the southwestern slopes of Black Dome and the southeastern slopes of Thomas Cole Mountain, the third and fourth of the Catskill High Peaks respectively. The creek then curves northward, passes through East Jewett, then curves back west.

Geographic entities mentioned:
surface_form: Thomas Cole Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.2708
lon: -74.1362
surface_form: black dome
instance_of: Mountain
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East Kill drains some of the highest slopes in the Catskills, including the Blackhead Mountains. The Blackhead Mountain range includes Thomas Cole Mountain, Black Dome, and Blackhead Mountain, the fourth-, third-, and fifth-highest peaks in the Catskills, respectively. The highest point in the East Kill watershed is at the summit of Black Dome Mountain in southeast Jewett.

Geographic entities mentioned:
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countries: United States
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The Blackhead Mountain range includes Thomas Cole Mountain, Black Dome, and Blackhead Mountain, the fourth-, third-, and fifth-highest peaks in the Catskills, respectively. The highest point in the East Kill watershed is at the summit of Black Dome Mountain in southeast Jewett. The average elevation of the watershed is approximately.

Geographic entities mentioned:
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On the lower stream, these include both sides of the creek from the mouth to Roaring Brook. Located along the kill within the Colgate Lake Wild Forest, is Colgate Lake. The lake is a popular year-round lake for trout, of which 750 brown trout from in length are stocked each year. The Lake is also popular for kayaking and has six campsites.

Geographic entities mentioned:
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coordinates: lat: 43.9344286
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coordinates: lat: 46.1508
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countries: United States
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The United States Geological Survey (USGS) maintains one stream gauge along East Kill. The station is located on Mill Hollow Road, northeast of Jewett Center, had a maximum discharge of per second on August 28, 2011, as Hurricane Irene passed through the area, and a minimum discharge of per second on August 13, 1997. Water quality.

Geographic entities mentioned:
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countries: United States
coordinates: lat: 37.035
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It then soon reaches Camp Beecher, where it curves north and begins to parallel State Route 296. After a short distance it curves back west and crosses under State Route 296. It soon receives Roaring Brook from the north, which drains part of the southern slope of Cave Mountain. East Kill then soon turns to the southwest, and soon converges with Schoharie Creek in Jewett Center. Watershed.

Geographic entities mentioned:
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instance_of: Mountain
countries: United States
coordinates: lat: 42.285833333333
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One wolf he tied up and tried to bring to the nearby town of Cairo, in order to get a larger bounty. The wolf died before Godsell was able to reach Cairo. From the late 1700s to early 1800s, the local economy thrived on the sale of hemlock bark, which was used to tan leather. The local industry later shifted to logging as lumber demands rose in the area.

Geographic entities mentioned:
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instance_of: Lake
countries: United States
coordinates: lat: 42.718611111111
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East Kill then soon turns to the southwest, and soon converges with Schoharie Creek in Jewett Center. Watershed. The East Kill's watershed, is mostly located within the town of Jewett, with a few small sections entering into the towns of Windham, Ashland, and Lexington. East Kill drains some of the highest slopes in the Catskills, including the Blackhead Mountains.

Geographic entities mentioned:
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instance_of: Mountain
countries: United States
coordinates: lat: 42.2679
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surface_form: east kill
instance_of: Watercourse
countries: United States
coordinates: lat: 42.23638889
lon: -74.31888889
East Kill. East Kill, a tributary of Schoharie Creek, flows across the town of Jewett, New York, United States, from its source on Stoppel Point. Ultimately its waters reach the Hudson River via the Mohawk. Since it drains into the Schoharie upstream of Schoharie Reservoir, it is part of the New York City water supply system.

Geographic entities mentioned:
surface_form: east kill
instance_of: Watercourse
countries: United States
coordinates: lat: 42.23638889
lon: -74.31888889
East Kill drains the southern slopes of the Blackhead Mountains, which include Thomas Cole Mountain, Black Dome, and Blackhead Mountain, the fourth-, third-, and fifth-highest peaks in the Catskills, respectively. The East Kill's watershed accounts for 3.9 percent of the Schoharie basin and is located near the southern end of that creek's watershed. Course.

Geographic entities mentioned:
surface_form: east kill
instance_of: Watercourse
countries: United States
coordinates: lat: 42.23638889
lon: -74.31888889
Course. East Kill begins as a mountainous stream dropping approximately in its first mile, then reduces in slope to dropping about over the next mile. The remainder of the creek drops to an average slope of per mile until it reaches its confluence with Schoharie Creek. East Kill begins on the northwestern slopes of Stoppel Point and begins flowing northwestward, then soon curves to the west.

Geographic entities mentioned:
surface_form: east kill
instance_of: Watercourse
countries: United States
coordinates: lat: 42.23638889
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It continues west for a short distance, then flows into Colgate Lake, a lake. It exits the lake then passes by the East Kill Valley Church, as it continues along the road. It soon recei
ves Halsey Brook from the north, which drains the southwestern slopes of Black Dome and the southeastern slopes of Thomas Cole Mountain, the third and fourth of the Catskill High Peaks respectively.

Geographic entities mentioned:
surface_form: east kill
instance_of: Watercourse
countries: United States
coordinates: lat: 42.23638889
lon: -74.31888889
It then soon reaches Camp Beecher, where it curves north and begins to parallel State Route 296. After a short distance it curves back west and crosses under State Route 296. It soon receives Roaring Brook from the north, which drains part of the southern slope of Cave Mountain. East Kill then soon turns to the southwest, and soon converges with Schoharie Creek in Jewett Center. Watershed.

Geographic entities mentioned:
surface_form: east kill
instance_of: Watercourse
countries: United States
coordinates: lat: 42.23638889
lon: -74.31888889
East Kill then soon turns to the southwest, and soon converges with Schoharie Creek in Jewett Center. Watershed. The East Kill's watershed, is mostly located within the town of Jewett, with a few small sections entering into the towns of Windham, Ashland, and Lexington. East Kill drains some of the highest slopes in the Catskills, including the Blackhead Mountains.

Geographic entities mentioned:
surface_form: east kill
instance_of: Watercourse
countries: United States
coordinates: lat: 42.23638889
lon: -74.31888889
About 2.5 percent of the watershed is developed and the remaining 7.5 percent is shrubland. Water covers; the National Wetlands Inventory maintained by the U.S. Fish and Wildlife Service has identified 168 separate wetlands within the East Kill watershed, totaling, including all open water. About 84.5 percent of the total acreage is palustrine wetlands such as marshes and swamps. History.

Geographic entities mentioned:
surface_form: east kill
instance_of: Watercourse
countries: United States
coordinates: lat: 42.23638889
lon: -74.31888889
About 84.5 percent of the total acreage is palustrine wetlands such as marshes and swamps. History. When settlers first arrived in the East Kill Valley, they frequently encountered bears, wolves, and other dangerous wildlife. This caused many of the first settlers to only stay in the area for a short time.

Geographic entities mentioned:
surface_form: east kill
instance_of: Watercourse
countries: United States
coordinates: lat: 42.23638889
lon: -74.31888889
This caused many of the first settlers to only stay in the area for a short time. A man by the name of John Godsell, known as Uncle John by the locals, was an expert trapper along the creek, who killed between 40 and 50 wolves in the East Kill Valley. One wolf he tied up and tried to bring to the nearby town of Cairo, in order to get a larger bounty.

Geographic entities mentioned:
surface_form: east kill
instance_of: Watercourse
countries: United States
coordinates: lat: 42.23638889
lon: -74.31888889
The wolf died before Godsell was able to reach Cairo. From the late 1700s to early 1800s, the local economy thrived on the sale of hemlock bark, which was used to tan leather. The local industry later shifted to logging as lumber demands rose in the area. When the majority of the forests were cleared, dairy farms became the dominant economic revenue in the East Kill valley. Geology.

Geographic entities mentioned:
surface_form: east kill
instance_of: Watercourse
countries: United States
coordinates: lat: 42.23638889
lon: -74.31888889
Geology. While the Catskills originated during the Devonian period, around 375 million years ago, as a former river delta uplifted and became a dissected plateau, the East Kill's valley was formed during the recent effects of the Wisconsin glaciation, which ended about 12,000 years ago. Meltwater fed many streams, which eventually formed today's East Kill.

Geographic entities mentioned:
surface_form: east kill
instance_of: Watercourse
countries: United States
coordinates: lat: 42.23638889
lon: -74.31888889
Meltwater fed many streams, which eventually formed today's East Kill. Lodgement till, which is a very dense, clay-rich, and reddish brown deposit, is very frequent in the East Kill and upper Schoharie Creek watersheds. The extreme density is distinguished from the looser assemblage of mixed sediment that comprises melt-out till found in moraines and along mountain sides.

Geographic entities mentioned:
surface_form: east kill
instance_of: Watercourse
countries: United States
coordinates: lat: 42.23638889
lon: -74.31888889
The extreme density is distinguished from the looser assemblage of mixed sediment that comprises melt-out till found in moraines and along mountain sides. The presence of bedrock banks in the East Kill can represent natural limits to changes in the stream channel system. Examples of this are shown in the headwater waterfalls. Discharge.

Geographic entities mentioned:
surface_form: east kill
instance_of: Watercourse
countries: United States
coordinates: lat: 42.23638889
lon: -74.31888889
Examples of this are shown in the headwater waterfalls. Discharge. The East Kill's watershed receives an average of precipitation annually, making it one of the wettest areas of the Catskills. Most of the precipitation is concentrated in seasonal events such as summer thunderstorms, remnants of hurricanes later in the year, or rain-on-snow events in springtime.

Geographic entities mentioned:
surface_form: east kill
instance_of: Watercourse
countries: United States
coordinates: lat: 42.23638889
lon: -74.31888889
The high average drainage density, steep slopes, and high precipitation causes flash floods during storm events. However, most of the watershed lies within forests that tend to mitigate this somewhat. The United States Geological Survey (USGS) maintains one stream gauge along East Kill.

Geographic entities mentioned:
surface_form: east kill
instance_of: Watercourse
countries: United States
coordinates: lat: 42.23638889
lon: -74.31888889
In the past, there has excessive stream bank erosion along the creek. However the East Kill does not seem to be as prone to sediment and turbidity problems like other Schoharie Creek tributaries in the area. However, sediment load from East Kill, along with West Kill and Batavia Kill, have been the principal contributors of sediment and turbidity in the Schoharie Reservoir.

Geographic entities mentioned:
surface_form: east kill
instance_of: Watercourse
countries: United States
coordinates: lat: 42.23638889
lon: -74.31888889
Flood control. In 2006, a combined effort of the Greene County Soil and Water Conservation District and the DEP resulted in a management plan for East Kill. The stream was subdivided into 11 sections from its source to the mouth and inventoried in great detail. Issues of concern for habitat and flood management were identified and recommendations made.

Geographic entities mentioned:
surface_form: east kill
instance_of: Watercourse
countries: United States
coordinates: lat: 42.23638889
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Lake Sebezhskoye. Sebezhskoye or Sebezh (Себежское озеро) is a freshwater lake in the southwest of Pskov Oblast in Russia, close to the borders with Latvia and Belarus. It has a surface area of. The lake takes its name from Sebezh, a town sitting on a low-lying promontory jutting out into the lake. The lake surface lies above sea level. Its maximum depth is.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: lake sebezhskoye
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 56.266666666667
lon: 28.5
Lake Sebezhskoye. Sebezhskoye or Sebezh (Себежское озеро) is a freshwater lake in the southwest of Pskov Oblast in Russia, close to the borders with Latvia and Belarus. It has a surface area of. The lake takes its name from Sebezh, a town sitting on a low-lying promontory jutting out into the lake. The lake surface lies above sea level. Its maximum depth is.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: себежское озеро
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 56.266666666667
lon: 28.5
Lake Sebezhskoye. Sebezhskoye or Sebezh (Себежское озеро) is a freshwater lake in the southwest of Pskov Oblast in Russia, close to the borders with Latvia and Belarus. It has a surface area of. The lake takes its name from Sebezh, a town sitting on a low-lying promontory jutting out into the lake. The lake surface lies above sea level. Its maximum depth is.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
It has a surface area of. The lake takes its name from Sebezh, a town sitting on a low-lying promontory jutting out into the lake. The lake surface lies above sea level. Its maximum depth is. In 1996, the lake basin with a cluster of similar lakes was designated the Sebezhsky National Park. The biggest tributary of the lake is the Cherneya River, which drains into Lake Sebezhskoye from the east.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
It has a surface area of. The lake takes its name from Sebezh, a town sitting on a low-lying promontory jutting out into the lake. The lake surface lies above sea level. Its maximum depth is. In 1996, the lake basin with a cluster of similar lakes was designated the Sebezhsky National Park. The biggest tributary of the lake is the Cherneya River, which drains into Lake Sebezhskoye from the east.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: lake sebezhskoye
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 56.266666666667
lon: 28.5
The biggest tributary of the lake is the Cherneya River, which drains into Lake Sebezhskoye from the east. The outflow of the lake is the Ugarinka River which flows to the west and crosses a narrow, several hundred meters wide, stretch of land separating Lake Sebezhskoye and Lake Orono, another big lake in the area. Both lakes belong to the drainage basin of the Daugava.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
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instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 56.266666666667
lon: 28.5
The name derives from a large species of ants, the &quot;Oecophylla smaragdina&quot; inhabiting the caves, where Handyong drove and buried alive the cunning serpents that disguised themselves as maidens. The epic also recounts that Mount Hantik, together with Mount Kulasi (now Colasi Peak) and Isarog, erupted around 4,500 years ago.

Geographic entities mentioned:
surface_form: Isarog
instance_of: Mountain
countries: Philippines
coordinates: lat: 13.659166666667
lon: 123.37333333333
Mount Bernacci. Mount Bernacci (locally known as Tangcong Vaca) is a mountain in Camarines Sur, Philippines, characterized by its mesa-like profile. It rises to above sea level. The mountain served as the base of operations for the during the Japanese occupation, taking name from the massif.

Geographic entities mentioned:
surface_form: tangcong vaca
instance_of: Mountain
countries: Philippines
coordinates: lat: 13.609166666667
lon: 122.97027777778
surface_form: mount bernacci
instance_of: Mountain
countries: Philippines
coordinates: lat: 13.609166666667
lon: 122.97027777778