Sarmila/GeoWiki-Features huggingface dataset:
Paulina Lake. Paulina Lake is one of the twin crater lakes in Newberry Crater, central Oregon, United States (the other being East Lake). It is located above sea level in the Newberry National Volcanic Monument near La Pine. The lake's primary inflow is seepage from East Lake, snow melt, and hot springs, and its outflow is Paulina Creek, a tributary of the Little Deschutes River.

Geographic entities mentioned:
surface_form: paulina lake
instance_of: Lake
countries: United States
coordinates: lat: 43.7198736
lon: -121.2583009
The lake is classified as mesotrophic, with a transparency of approximately. It is about lower and one mile west of its twin, East Lake. Paulina Lake sits within the Newberry Crater, formed from over 500,000 years of volcanic activity. The lake bears the name of Paulina, a Northern Paiute leader. Recreational Activities.

Geographic entities mentioned:
surface_form: paulina lake
instance_of: Lake
countries: United States
coordinates: lat: 43.7198736
lon: -121.2583009
The lake bears the name of Paulina, a Northern Paiute leader. Recreational Activities. Paulina Lake supports a number of recreational activities, including camping, hiking, fishing, kayaking, canoeing and paddle-boarding. A 10 mph speed limit on the lake prohibits motorized high speed watersports such as waterskiing and jet skis, which protects the lake as a popular fishing destination.

Geographic entities mentioned:
surface_form: paulina lake
instance_of: Lake
countries: United States
coordinates: lat: 43.7198736
lon: -121.2583009
New York State Route 104. New York State Route 104 (NY 104) is a east–west state highway in Upstate New York in the United States. It spans six counties and enters the vicinity of four cities—Niagara Falls, Lockport, Rochester, and Oswego—as it follows a routing largely parallel to the southern shoreline of Lake Ontario, along a ridge of the old shoreline of Glacial Lake Iroquois.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Past I-190, NY 104 begins to deviate from the Niagara River. It heads through a small neighborhood situated between the Moses Parkway and NY 104 and intersects the northern end of NY 265. North of this junction, NY 104 curves northeast to descend the Niagara Escarpment. As it heads downward in elevation, it intersects the western terminus of NY 18 by way of an interchange.

Geographic entities mentioned:
surface_form: Niagara Escarpment
instance_of: Mountain
countries: Canada
coordinates: lat: 43.8334
lon: -79.99966
Orleans and Monroe counties. The route heads northeast through the town of Ridgeway to the hamlet of the same name, where NY 104 meets NY 63. NY 63 joins NY 104 east along Ridge Road for about before continuing north toward Lake Ontario. NY 104, meanwhile, continues through the rural towns of Ridgeway and Gaines to a junction with NY 279 north of Albion.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Strada Statale 36 del Lago di Como e dello Spluga (designated SS 36) is an Italian state highway approximately long, located entirely within the Lombardy region of Italy. It is a major highway and one of the primary north-south routes in Lombardy, providing the main access to the Valtellina valley and the Swiss canton of Grisons via the Splügen Pass (Italian: &quot;Passo dello Spluga&quot;).

Geographic entities mentioned:
surface_form: Valtellina
instance_of: Valley
countries: Italy
coordinates: lat: 46.166666666667
lon: 9.8666666666667
At Giussano, the highway reduces to four lanes and shifts eastward towards Lecco. Beyond Civate (the highway's former northern terminus until 2000), the SS 36 continues towards Lecco via tunnels under Monte Barro and through the city centre. The Lecco city tunnel features stacked roadways, with northbound and southbound traffic on separate levels.

Geographic entities mentioned:
surface_form: Monte Barro
instance_of: Mountain
countries: Italy
coordinates: lat: 45.8325
lon: 9.37916667
History. The name &quot;Nuova Valassina&quot; (New Valassina) stems from an earlier plan to create a modern highway connecting Erba with southern Brianza and Milan, generally following the Valassina valley and crossing the Lambro river. While the current SS 36 deviates from parts of this original plan, the name persists for the high-capacity section through Brianza.

Geographic entities mentioned:
surface_form: Valassina
instance_of: Valley
countries: Italy
coordinates: lat: 45.88333
lon: 9.26667
He left Zurich and transferred its collection to Cologny, just outside Geneva, on the shores of Lake Geneva.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
Indigo Lake (Ohio). Indigo Lake is a small, roughly triangular lake in Summit County, Ohio, in the United States. It is not a natural lake, having been created by the park service in Cuyahoga Valley National Park. It is a popular fishing location, with several species present including the Largemouth bass. National Park.

Geographic entities mentioned:
surface_form: indigo lake (ohio)
instance_of: Lake
countries: United States
coordinates: lat: 41.193
lon: -81.5817
Lake Rawa Pening. Rawa Pening (literally meaning 'Clear Swamp', from the Javanese &quot;Bening&quot;) is a lake in the Ambarawa Basin in Central Java, Indonesia. It serves as a source of power, irrigation, and flood control, and is used for fishing. Location and description. Rawa Pening is located in the volcanic Ambarawa Basin in Central Java,
between Ambarawa and Salatiga.

Geographic entities mentioned:
surface_form: lake rawa pening
instance_of: Lake
countries: Indonesia
coordinates: lat: -7.28333333
lon: 110.43333333
surface_form: rawa pening
instance_of: Lake
countries: Indonesia
coordinates: lat: -7.28333333
lon: 110.43333333
Lake Rawa Pening. Rawa Pening (literally meaning 'Clear Swamp', from the Javanese &quot;Bening&quot;) is a lake in the Ambarawa Basin in Central Java, Indonesia. It serves as a source of power, irrigation, and flood control, and is used for fishing. Location and description. Rawa Pening is located in the volcanic Ambarawa Basin in Central Java,
between Ambarawa and Salatiga.

Geographic entities mentioned:
surface_form: rawa pening
instance_of: Lake
countries: Indonesia
coordinates: lat: -7.28333333
lon: 110.43333333
It reached its largest size from 11,000 to 9,000 BC but shrank until it reached its current size around 6,000 BC. To protect Rawa Pening, the local government has enacted a green belt policy. Several establishments, such as the tourist attraction Kampoeng Rawa, were controversial owing to their construction within this belt. Role.

Geographic entities mentioned:
surface_form: rawa pening
instance_of: Lake
countries: Indonesia
coordinates: lat: -7.28333333
lon: 110.43333333
Several establishments, such as the tourist attraction Kampoeng Rawa, were controversial owing to their construction within this belt. Role. One of the major roles of Rawa Pening is as a source of hydroelectricity, with a power station located on the Tuntang River near the lake. Fishing is common as a source of supplementary income, and the water from the lake irrigates nearby rice fields.

Geographic entities mentioned:
surface_form: rawa pening
instance_of: Lake
countries: Indonesia
coordinates: lat: -7.28333333
lon: 110.43333333
It has also been cited as being used for flood control. Plant infestation. Numerous species of aquatic plants live in Rawa Pening, including &quot;Panicum repens&quot;, &quot;Eichhornia crassipes&quot;, &quot;Salvinia cucullata&quot;, and &quot;Hydrilla verticillata&quot;. Estimates of the total number of species vary, from 20 in 1949 to 19 aquatic and 71 semi-aquatic species in 1972.

Geographic entities mentioned:
surface_form: rawa pening
instance_of: Lake
countries: Indonesia
coordinates: lat: -7.28333333
lon: 110.43333333
The area is identical to the former municipality named Sandsvær. Sandsvær is situated in the valley of Lågendalen on the Numedalslågen river, and is bordered by Kongsberg town in the north, and the county border to Vestfold and Telemark counties in the south. Historically, Sandsvær as a part of &quot;Sandsvær og Numedal fogderi&quot; had belonged to Akershus &quot;amt&quot; from 7 February 1685.

Geographic entities mentioned:
surface_form: Lågendalen
instance_of: Valley
countries: Norway
Initially, the municipality had 821 residents. During the 1960s, there were many municipal mergers across Norway due to the work of the Schei Committee. On 1 January 1964, the middle part of the Eksingedalen valley (population: 151) was transferred from Modalen to the municipality of Vaksdal.

Geographic entities mentioned:
surface_form: Eksingedalen
instance_of: Valley
countries: Norway
coordinates: lat: 60.78128889
lon: 5.87511111
Both roads were constructed fairly recently, before that time, the municipality was only accessible by boat or crossing mountains on foot. The Modalen Tunnel was built in 1976 and it connects this valley to the Eksingedalen valley to the south. The other road was finished in 1996, and it follows the fjord heading west to Lindås. The Modalen valley centers around the river Moelva.

Geographic entities mentioned:
surface_form: Eksingedalen
instance_of: Valley
countries: Norway
coordinates: lat: 60.78128889
lon: 5.87511111
The other road was finished in 1996, and it follows the fjord heading west to Lindås. The Modalen valley centers around the river Moelva. The lake Steinslandsvatnet, in the central part of the municipality, is the headwaters of the river. The high mountains that surround the valley provide many sources of hydroelectric power such as the lake Skjerjavatnet.

Geographic entities mentioned:
surface_form: Steinslandsvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 60.893888888889
lon: 5.9772222222222
The lake Steinslandsvatnet, in the central part of the municipality, is the headwaters of the river. The high mountains that surround the valley provide many sources of hydroelectric power such as the lake Skjerjavatnet. Modalen borders the municipality of Høyanger to the north and the municipality of Vik to the east, Vaksdal to the south, and Alver and Masfjorden to the west. The Modalen project.

Geographic entities mentioned:
surface_form: Skjerjavatnet
instance_of: Lake
countries: Norway
coordinates: lat: 60.870833333333
lon: 6.1077777777778
Moxotó River. The Moxotó River is a tributary of the São Francisco River in northeastern Brazil. The Moxotó originates on the Borborema Plateau in Pernambuco state, and flows southwest to join the São Francisco. The lower portion of the river forms the border between Pernambuco state to the west and Alagoas state to the east.

Geographic entities mentioned:
surface_form: Borborema Plateau
instance_of: Plateau
countries: Brazil
coordinates: lat: -7
lon: -37
Lake Superior National Marine Conservation Area. Lake Superior National Marine Conservation Area () is a National Marine Conservation Area (NMCA) on the north shore of Lake Superior in Ontario, and is a unit of the national park system. Established on September 1, 2015, it is the largest freshwater marine protected area in the world.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
They arrived in Dar es Salaam in August 1928 by steamer after a voyage through the Red Sea and down the east coast of Africa. On July 26, 1929, in a mountainous area at the northern end of Lake Tanganyika, Moses was the first to find and shoot a Grauer's broadbill.

Geographic entities mentioned:
surface_form: Lake Tanganyika
instance_of: Lake
countries: Tanzania
Democratic Republic of the Congo
Burundi
Zambia
coordinates: lat: -6.1
lon: 29.5
Fionn Loch is a remote deep freshwater loch. It is oriented roughly NNW–SSE and is about 7 km long and around 1 km wide. It lies four miles north-east of, and roughly parallel to, Loch Maree, 4.5 miles south-east of Aultbea and 6 miles east of Poolewe in Wester Ross. Dubh Loch. At the southern end of Fionn Loch is Dubh Loch (&quot;White Loch&quot; and &quot;Black Loch&quot;).

Geographic entities mentioned:
surface_form: Loch Maree
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.689722222222
lon: -5.4575
surface_form: maree
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.689722222222
lon: -5.4575
Dubh Loch. At the southern end of Fionn Loch is Dubh Loch (&quot;White Loch&quot; and &quot;Black Loch&quot;). This is a small loch that is separated from Fionn Loch by a shallow bar about 100 yards long, which is now used by a causeway to connect the two sides.

Geographic entities mentioned:
surface_form: black loch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 55.4196
lon: -4.22822
surface_form: white loch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.5707
lon: -3.3525
surface_form: fionn loch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 58.1068
lon: -5.1747
surface_form: dubh loch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.929375
lon: -3.253024
surface_form: black loch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.5691
lon: -3.3433
surface_form: black loch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 55.909444444444
lon: -3.8230555555556
surface_form: fionn loch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.75602
lon: -5.453
Fionn Loch (Fisherfield Forest, Wester Ross). Fionn Loch is a remote deep freshwater loch. It is oriented roughly NNW–SSE and is about 7 km long and around 1 km wide. It lies four miles north-east of, and roughly parallel to, Loch Maree, 4.5 miles south-east of Aultbea and 6 miles east of Poolewe in Wester Ross. Dubh Loch.

Geographic entities mentioned:
surface_form: fionn loch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 58.1068
lon: -5.1747
surface_form: fionn loch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.75602
lon: -5.453
Dubh Loch. At the southern end of Fionn Loch is Dubh Loch (&quot;White Loch&quot; and &quot;Black Loch&quot;). This is a small loch that is separated from Fionn Loch by a shallow bar about 100 yards long, which is now used by a causeway to connect the two sides.

Geographic entities mentioned:
surface_form: fionn loch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 58.1068
lon: -5.1747
surface_form: fionn loch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.75602
lon: -5.453
This is a small loch that is separated from Fionn Loch by a shallow bar about 100 yards long, which is now used by a causeway to connect the two sides. In its 1876–77 session, the Outer House of the Court of Session decided that Dubh Loch was part of Fionn Loch, in an action brought by a fisherman who wanted to fish both lochs under the original fishing agreement without paying more.

Geographic entities mentioned:
surface_form: fionn loch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 58.1068
lon: -5.1747
surface_form: dubh loch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.929375
lon: -3.253024
surface_form: fionn loch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.75602
lon: -5.453
Fionn Loch is a remote deep freshwater loch. It is oriented roughly NNW–SSE and is about 7 km long and around 1 km wide. It lies four miles north-east of, and roughly parallel to, Loch Maree, 4.5 miles south-east of Aultbea and 6 miles east of Poolewe in Wester Ross. Dubh Loch. At the southern end of Fionn Loch is Dubh Loch (&quot;White Loch&quot; and &quot;Black Loch&quot;).

Geographic entities mentioned:
surface_form: dubh loch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.929375
lon: -3.253024
Wind power in New Hampshire. Wind power in New Hampshire began in 1980, with the installation of the world's first wind farm at Crotched Mountain, consisting of 20 30 kW wind turbines, although it closed decades ago.

Geographic entities mentioned:
surface_form: Crotched Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.998294444444
lon: -71.873711111111
The primary reason for the rejection was stated as the visual and aesthetic impact the proposed turbines would have had on the Audubon Society of New Hampshire's Willard Pond Sanctuary and the region in general. The project was eventually approved with 9 turbines, one fewer than originally proposed. New Hampshire is a net power producer, generating more than is consumed.

Geographic entities mentioned:
surface_form: Willard Pond
instance_of: Lake
countries: United States
coordinates: lat: 43.0214
lon: -72.0161
Development. The form and location of the monument were not initially settled and Hope first successfully applied to the town council for a site at the north east edge of Calton Hill. A correspondent in the &quot;Caledonian Mercury&quot; opposed the Calton Hill site, instead proposing the monument could be built on Arthur's Seat.

Geographic entities mentioned:
surface_form: Calton Hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.955278
lon: -3.182222
The form and location of the monument were not initially settled and Hope first successfully applied to the town council for a site at the north east edge of Calton Hill. A correspondent in the &quot;Caledonian Mercury&quot; opposed the Calton Hill site, instead proposing the monument could be built on Arthur's Seat. Further suggestions included Picardy Place or, nearby, the top of Leith Walk.

Geographic entities mentioned:
surface_form: Arthur's Seat
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.944166666667
lon: -3.1619444444444
He moved to Chilliwack at the age of 12 from Mission, British Columbia, and graduated from Chilliwack Senior Secondary School in 1978. In the early 1980s he started a bus charter company which made ski trips to Mount Baker. He also bought a houseboat and ran charters on Cultus Lake. In 1987, he raised money to build the Cultus Lake Kids Park and started the Cultus Lake Beach Party.

Geographic entities mentioned:
surface_form: Cultus Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.053333333333335
lon: -121.98694444444445
Tupungato River. The Tupungato River (in Spanish: &quot;Río Tupungato&quot;) is a river located in the western zone of the Mendoza Province called Uco Valley (in Spanish: &quot;Valle de Uco&quot;), flows in Luján de Cuyo and Tupungato departments, to the west of Argentina. It arises on the Del Plomo and Del Juncal glaciers in the north of the Tupungato Mountain and ends at the Mendoza River.

Geographic entities mentioned:
surface_form: Tupungato
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -33.358555555555554
lon: -69.77041666666666
surface_form: Mendoza River
instance_of: Watercourse
countries: Argentina
coordinates: lat: -32.35
lon: -68.3
surface_form: mendoza river
instance_of: Watercourse
countries: Argentina
coordinates: lat: -32.35
lon: -68.3
Tupungato River. The Tupungato River (in Spanish: &quot;Río Tupungato&quot;) is a river located in the western zone of the Mendoza Province called Uco Valley (in Spanish: &quot;Valle de Uco&quot;), flows in Luján de Cuyo and Tupungato departments, to the west of Argentina. It arises on the Del Plomo and Del Juncal glaciers in the north of the Tupungato Mountain and ends at the Mendoza River.

Geographic entities mentioned:
surface_form: río tupungato
instance_of: Watercourse
countries: Argentina
coordinates: lat: -33
lon: -70
surface_form: tupungato river
instance_of: Watercourse
countries: Argentina
coordinates: lat: -33
lon: -70
surface_form: mendoza
instance_of: Watercourse
countries: Argentina
coordinates: lat: -32.35
lon: -68.3
Tupungato River. The Tupungato River (in Spanish: &quot;Río Tupungato&quot;) is a river located in the western zone of the Mendoza Province called Uco Valley (in Spanish: &quot;Valle de Uco&quot;), flows in Luján de Cuyo and Tupungato departments, to the west of Argentina. It arises on the Del Plomo and Del Juncal glaciers in the north of the Tupungato Mountain and ends at the Mendoza River.

Geographic entities mentioned:
surface_form: tupungato river
instance_of: Watercourse
countries: Argentina
coordinates: lat: -33
lon: -70
When smaller fish approach and attempt to pick at the dead fish, &quot;P. friedrichsthalii&quot; ambush the smaller fish. Similar behaviour has also been observed in some species of Lake Malawi cichlids, particularly from the genus &quot;Nimbochromis&quot;. Description. Physically similar to other members of the genus, especially &quot;P. managuensis&quot; and &quot;P. motaguensis&quot;, &quot;P.

Geographic entities mentioned:
surface_form: Lake Malawi
instance_of: Lake
countries: Malawi
Mozambique
Tanzania
coordinates: lat: -12.183333333333
lon: 34.366666666667
Incumbent Marni von Wilpert ran unopposed for re-election and won the election outright in the primary on March 5, 2024. District 7. District 7 consists of the communities of Allied Gardens, Del Cerro, Grantville, Linda Vista, Mission Valley, San Carlos, Serra Mesa, and Tierrasanta. Incumbent Raul Campillo ran unopposed for re-election and won the election outright in the primary on March 5, 2024.

Geographic entities mentioned:
surface_form: Mission Valley
instance_of: Valley
countries: United States
coordinates: lat: 32.767261111111
lon: -117.14961666667
The film roused a public outcry. In 2008, she directed the full-length documentary &quot;The Cemetery Club&quot;, about s a group of elderly Holocaust survivors who immigrated to Israel from Poland and meet every week for the last 20 years in the cemetery on Mount Herzl, and hold a meeting there that includes discussions and reading their writings.

Geographic entities mentioned:
surface_form: Mount Herzl
instance_of: Mountain
countries: Israel
coordinates: lat: 31.774117
lon: 35.180567
Jenny Buttress. t37gsgjdvx85tnuna0a6lu2k64ams" xml:space="preserve">Jenny Buttress () is a rock buttress north of Melville Peak, overlooking Destruction Bay on the east side of King George Island, in the South Shetland Islands.

Geographic entities mentioned:
surface_form: Melville Peak
instance_of: Mountain
coordinates: lat: -62.0167
lon: -57.6833
Cameron's two European companions, Dr William Edward Dillon, surgeon in the Royal Navy, and Lieutenant Cecil Murphy of the Royal Artillery, turned back to join the task of returning Livingstone's body to the coast. Cameron continued his march and reached Ujiji, on Lake Tanganyika, in February 1874, where he found and sent to England Livingstone's papers.

Geographic entities mentioned:
surface_form: Lake Tanganyika
instance_of: Lake
countries: Tanzania
Democratic Republic of the Congo
Burundi
Zambia
coordinates: lat: -6.1
lon: 29.5
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. It lends its name to both a mountain to its south and a small town midway along its length. The West Kill's watershed accounts for 10 percent of the reservoir's basin.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.1679
lon: -74.2896
From there it turns to a more northerly course to the Schoharie at Lexington. Spruceton Valley. Two streams that later join rise in the cirque between Hunter and Southwest Hunter mountains, amidst the dense forests of the West Kill Wilderness Area, part of the Catskill Park. The source of the northern stream is at, the higher of the two.

Geographic entities mentioned:
surface_form: Southwest Hunter
instance_of: Mountain
countries: United States
coordinates: lat: 42.162666666667
lon: -74.243666666667
At Diamond Notch Falls, the Devil's Path merges briefly with the Diamond Notch Trail coming in from the west. The two cross the West Kill on a wooden bridge, the uppermost crossing of the stream. Just south of the stream, the trails again diverge, with the Devil's Path following the stream for a short distance on that side before beginning its ascent of West Kill Mountain to the southwest.

Geographic entities mentioned:
surface_form: West Kill Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.1679
lon: -74.2896
A half-mile further west, a short local street, Ad Van Road, crosses. Just below, at the former hamlet of Spruceton, Herdman Brook flows into the West Kill from the slopes of Evergreen Mountain to the north. Styles Brook follows shortly, draining the cirque below West Kill Mountain's summit, from the south, just west of where Baker Road crosses to provide access to several farms on that side.

Geographic entities mentioned:
surface_form: Evergreen Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.211666666667
lon: -74.308055555556
Schoolhouse Brook flows in from the north further west. Shoemaker Road, providing access to several properties on the stream's south side, crosses east of where Bennett Brook flows in from the south. Long Road crosses over the West Kill 0.6 mile (1 km) downstream, just above where Newton Brook flows down from a valley on the slopes of Mount Sherrill to the south.

Geographic entities mentioned:
surface_form: Mount Sherrill
instance_of: Mountain
countries: United States
coordinates: lat: 42.175833333333
lon: -74.372833333333
Immediately north of the bend, the West Kill crosses under Route 42, entering a section where both banks are shored up with riprap for the next as the stream and road again follow a north-northeasterly course. The natural banks return where Roarback Brook, the lowest tributary of the West Kill, flows in from slopes of Vly Mountain to the west.

Geographic entities mentioned:
surface_form: Vly Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.2458
lon: -74.4483
Ridgelines between the mountains on either side form the watershed's boundaries except for the area around its mouth at Lexington. On the north side Rusk Mountain and the peaks to its west form the boundary between the West Kill watershed and the Schoharie's.

Geographic entities mentioned:
surface_form: Rusk Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.2006
lon: -74.2769
South of the range from Southwest Hunter Mountain to Mount Sherrill drainage flows into Esopus Creek, another Hudson tributary in Ulster County. The unnamed peaks over in elevation between Halcott and Vly mountains on the southwestern boundary are part of the Catskill Divide, since the Vly Creek basin on the opposite side is part of the Delaware River watershed.

Geographic entities mentioned:
surface_form: Halcott
instance_of: Mountain
countries: United States
coordinates: lat: 42.1801
lon: -74.4379
That began in 1994 with a station one-eighth of a mile () above the stream's mouth; in 2002, a second station was established near the USGS stream gauge above Spruceton. Both have generally reported consistent high quality, better than the nearby subwatersheds of the East and Batavia kills. Metrics important to aquatic life habitat have remained above levels legally mandated or recommended.

Geographic entities mentioned:
surface_form: East
instance_of: Watercourse
countries: United States
coordinates: lat: 42.23638889
lon: -74.31888889
The Trinity Inlet (aka Smith Creek) is the northern boundary of the locality while Wrights Creek (the watercourse from which the locality takes its name) and Mackey Creek form parts of the eastern and western boundaries of the locality. Warner Road is the southern boundary. The northern part of the locality is undeveloped wetlands and the mountainous region is also undeveloped.

Geographic entities mentioned:
surface_form: Trinity Inlet
instance_of: Body of water
countries: Australia
coordinates: lat: -16.92
lon: 145.784
In the surrounding area there are important ranches. Mining is a possibility for economic development in the future; there are prospected deposits of platinum, gold, basalt, semiprecious stones, and decorative rocks nearby. In terms of tourism, there is fishing in the Pescado River, the Tecka River basin, and nearby lakes. There is also horseback riding and trekking. Demographics.

Geographic entities mentioned:
surface_form: Tecka River
instance_of: Watercourse
countries: Argentina
coordinates: lat: -43.05612
lon: -70.79048
He also directed the concluding scene: a political debate between strangers on a train about the world coffee market. The rest of the film was directed by Slatan Dudow. The film music was composed by Hanns Eisler. Kuhle Wampe itself was a tent camp on the Müggelsee in Berlin. &quot;Wampe&quot; is Berlin dialect for &quot;stomach&quot;, so the title could be rendered &quot;Empty Stomach&quot;.

Geographic entities mentioned:
surface_form: Müggelsee
instance_of: Lake
countries: Germany
coordinates: lat: 52.433333333333
lon: 13.65
Legiamayo River. Legiamayo or Lejiamayu (possibly from Quechua &quot;lliklla&quot; a rectangular shoulder cloth, &quot;mayu&quot; river) is a river in Peru located in the Ancash Region, Carhuaz Province, Marcará District. It originates in the Cordillera Blanca west of mount Copa, near Lake Lejiacocha. It is a tributary of the Marcará River, which in turn is a tributary of the Santa River.

Geographic entities mentioned:
surface_form: Lake Lejiacocha
instance_of: Lake
countries: Peru
coordinates: lat: -9.28583333
lon: -77.50555556
He traveled to the Pacific Coast in 1859, and three years later, joined the 2nd Regiment California Volunteer Cavalry. From 1874 through 1883, he worked as an editor and newspaper publisher in California mining camps, and founded ten newspapers, including the &quot;Panamint News&quot; (November 26, 1874), the first in the Death Valley area.

Geographic entities mentioned:
surface_form: Death Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.45693888888889
lon: -116.86528055555556
Although most of the Bantu peoples continued south, some remained and founded ethnic groups based on common ancestry. By 1500, the tribes had established several kingdoms such as the Maravi that reached from north of what became Nkhotakota to the Zambezi River and from Lake Malawi to the Luangwa River in what became Zambia and the Nkhamanga.

Geographic entities mentioned:
surface_form: Lake Malawi
instance_of: Lake
countries: Malawi
Mozambique
Tanzania
coordinates: lat: -12.183333333333
lon: 34.366666666667
Colonialisation (1859–1960). Missionary and explorer David Livingstone reached Lake Malawi (then Lake Nyasa) in 1859 and identified the Shire Highlands south of the lake as an area suitable for European settlement.

Geographic entities mentioned:
surface_form: Shire Highlands
instance_of: Plateau
countries: Malawi
coordinates: lat: -15.64684105
lon: 35.12557983
It lies between latitudes 9° and 18°S, and longitudes 32° and 36°E. The Great Rift Valley runs through the country from north to south, and to the east of the valley lies Lake Malawi (also called Lake Nyasa), making up over three-quarters of Malawi's eastern boundary. Lake Malawi is sometimes called the Calendar Lake as it is about long and wide.

Geographic entities mentioned:
surface_form: Lake Malawi
instance_of: Lake
countries: Malawi
Mozambique
Tanzania
coordinates: lat: -12.183333333333
lon: 34.366666666667
In the mountainous sections of Malawi surrounding the Rift Valley, plateaus rise generally above sea level, although some rise as high as in the north. To the south of Lake Malawi lies the Shire Highlands, gently rolling land at approximately above sea level. In this area, the Zomba and Mulanje mountain peaks rise to respective heights of.

Geographic entities mentioned:
surface_form: Shire Highlands
instance_of: Plateau
countries: Malawi
coordinates: lat: -15.64684105
lon: 35.12557983
Sugar, coffee, corn, potatoes, sorghum, cattle, and goats are also important components of the cuisine and economy. Lake Malawi is a source of fish, including chambo (similar to bream), usipa (similar to sardines), and mpasa (similar to salmon and kampango). Nsima is a food staple made from ground corn and typically served with side dishes of meat and vegetables.

Geographic entities mentioned:
surface_form: Lake Malawi
instance_of: Lake
countries: Malawi
Mozambique
Tanzania
coordinates: lat: -12.183333333333
lon: 34.366666666667
Geologists have recovered some peat buried by the lava and radiocarbon dating produced an age of 7560 years plus or minus 100 years. Flows from nearby Flourmill Cone, Kostal Cone and Spanish Lake Cones rest on glaciated bedrock without an intervening paleosol, suggesting an early Holocene age. Visits to Dragon Cone are very rare due to difficult access.

Geographic entities mentioned:
surface_form: Kostal Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1667
lon: -119.95
Flows from nearby Flourmill Cone, Kostal Cone and Spanish Lake Cones rest on glaciated bedrock without an intervening paleosol, suggesting an early Holocene age. Visits to Dragon Cone are very rare due to difficult access. The nearest trail is the overgrown Kostal Lake Trail, over to the south. Falls Creek is impassable for boats.

Geographic entities mentioned:
surface_form: Kostal Lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.164
lon: -119.976
Visits to Dragon Cone are very rare due to difficult access. The nearest trail is the overgrown Kostal Lake Trail, over to the south. Falls Creek is impassable for boats. The cone is best viewed from the air, but float plane landings on nearby Ray Lake are not permitted.

Geographic entities mentioned:
surface_form: Ray Lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.233333333333
lon: -120.06666666667
It is the source of a long lava flow, called Dragon's Tongue. This lava covered the floor of narrow Falls Creek Valley and terminated at the Clearwater River, damming it to a height of and raising the level of existing Clearwater Lake upstream. Geologists have recovered some peat buried by the lava and radiocarbon dating produced an age of 7560 years plus or minus 100 years.

Geographic entities mentioned:
surface_form: clearwater lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.203
lon: -79.233
surface_form: clearwater river
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.7481
lon: -111.384
surface_form: clearwater lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.2667
lon: -120.233
surface_form: clearwater lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.8734
lon: -107.9301
surface_form: clearwater lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.05
lon: -101.05
Dragon Cone. Dragon Cone is a monogenetic cinder cone located in Wells Gray Provincial Park in east-central British Columbia. It is the source of a long lava flow, called Dragon's Tongue. This lava covered the floor of narrow Falls Creek Valley and terminated at the Clearwater River, damming it to a height of and raising the level of existing Clearwater Lake upstream.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: dragon cone
instance_of: Mountain
countries: Canada
coordinates: lat: 52.25
lon: -120.05
surface_form: cinder cone
instance_of: Mountain
countries: Canada
coordinates: lat: 49.9717
lon: -123.007
Dragon Cone. Dragon Cone is a monogenetic cinder cone located in Wells Gray Provincial Park in east-central British Columbia. It is the source of a long lava flow, called Dragon's Tongue. This lava covered the floor of narrow Falls Creek Valley and terminated at the Clearwater River, damming it to a height of and raising the level of existing Clearwater Lake upstream.

Geographic entities mentioned:
surface_form: dragon cone
instance_of: Mountain
countries: Canada
coordinates: lat: 52.25
lon: -120.05
Flows from nearby Flourmill Cone, Kostal Cone and Spanish Lake Cones rest on glaciated bedrock without an intervening paleosol, suggesting an early Holocene age. Visits to Dragon Cone are very rare due to difficult access. The nearest trail is the overgrown Kostal Lake Trail, over to the south. Falls Creek is impassable for boats.

Geographic entities mentioned:
surface_form: dragon cone
instance_of: Mountain
countries: Canada
coordinates: lat: 52.25
lon: -120.05
Further, some events regarded as supernatural kept his memory alive for many years among the French-Canadian people. The high point of Forbin-Janson's apostolate in Lower Canada was the raising of an immense cross on Mont Saint-Hilaire that was a counterpart to the one on Mont-Valérien which had been destroyed.

Geographic entities mentioned:
surface_form: Mont Saint-Hilaire
instance_of: Mountain
countries: Canada
coordinates: lat: 45.552222222222
lon: -73.163888888889
Issawiya. Al-Issawiya (, also spelled &quot;Isawiya&quot; or &quot;Isawiyah&quot;) is a Palestinian neighborhood in East Jerusalem. It is located on the eastern slopes of the Mount Scopus ridge.

Geographic entities mentioned:
surface_form: Mount Scopus
instance_of: Mountain
countries: Israel
coordinates: lat: 31.7925
lon: 35.244166666667
Geography. The district is mountainous and limited by the Morskoy, Khamar-Daban, Ulan-Burgas and Golondin ranges. It is bound on the northeast by the shores of Lake Baikal and by the left bank of the Selenga River in the southwestern part. The Turka and Itantsa are other important rivers of the area. History.

Geographic entities mentioned:
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
Pointe de Vouasson. The Pointe de Vouasson is a mountain of the Swiss Pennine Alps, overlooking Lac des Dix in the canton of Valais. It lies between the valleys of Hérémence (west) and Arolla (east), north of the Aiguilles Rouges d'Arolla. The east side of the mountain is covered by a glacier named &quot;Glacier de Vouasson&quot;.

Geographic entities mentioned:
surface_form: Aiguilles Rouges d'Arolla
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.055277777778
lon: 7.4338888888889
Pointe de Vouasson. The Pointe de Vouasson is a mountain of the Swiss Pennine Alps, overlooking Lac des Dix in the canton of Valais. It lies between the valleys of Hérémence (west) and Arolla (east), north of the Aiguilles Rouges d'Arolla. The east side of the mountain is covered by a glacier named &quot;Glacier de Vouasson&quot;.

Geographic entities mentioned:
surface_form: pointe de vouasson
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.072166666667
lon: 7.4252222222222
Chevrier Lake (Obatogamau River). The Chevrier Lake is a freshwater body integrated into a set of lakes designated &quot;Obatogamau Lakes&quot;, in the Eeyou Istchee James Bay (municipality) area, in the area of Nord-du-Québec, in the province of Quebec, Canada. This lake extends into the townships of Queylus, La Dauversière, Fancamp and Haüy. Forestry is the main economic activity of the sector.

Geographic entities mentioned:
surface_form: Obatogamau Lakes
instance_of: Group of lakes
countries: Canada
coordinates: lat: 49.593611111111
lon: -74.455555555556
surface_form: obatogamau lakes
instance_of: Group of lakes
countries: Canada
coordinates: lat: 49.593611111111
lon: -74.455555555556
The surface of Lake Chevrier is usually frozen from early November to mid-May, however safe ice circulation is generally mid-November to mid-April. Toponymy. In 1910, the Hudson's Bay Company built on the east shore of La Dauversière Lake a cabin which will become over the years a place of storage. Finally this cabin was deserted. Originally known as &quot;Dépôt-du-Lac-Chevrier&quot;.

Geographic entities mentioned:
surface_form: La Dauversière Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.566666666667
lon: -74.369444444444
surface_form: la dauversière lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.566666666667
lon: -74.369444444444
Chevrier Lake (Obatogamau River). The Chevrier Lake is a freshwater body integrated into a set of lakes designated &quot;Obatogamau Lakes&quot;, in the Eeyou Istchee James Bay (municipality) area, in the area of Nord-du-Québec, in the province of Quebec, Canada. This lake extends into the townships of Queylus, La Dauversière, Fancamp and Haüy. Forestry is the main economic activity of the sector.

Geographic entities mentioned:
surface_form: chevrier lake (obatogamau river)
instance_of: Lake
countries: Canada
coordinates: lat: 49.635555555556
lon: -74.463888888889
The Fonthill Park estate extends into the south of the parish. Landscaping which included the creation of Fonthill Lake was begun in 1740 by William Beckford (later Lord Mayor of London) and continued from c. 1793 by his son William Thomas Beckford, who built Fonthill Abbey, now almost completely demolished. The estate now belongs to Alastair Morrison, 3rd Baron Margadale.

Geographic entities mentioned:
surface_form: Fonthill Lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.086380555556
lon: -2.0970388888889
Popular recreational destinations, they are located within the Grand Staircase–Escalante National Monument. The headwaters of Fortymile and Willow Gulches have their origins along a 7-mile (11 km) segment of the Straight Cliffs, the eastern edge of the Kaiparowits Plateau.

Geographic entities mentioned:
surface_form: Kaiparowits Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37.622
lon: -111.665
Florida Bay, lying between the Florida Keys and the mainland, is very shallow with depths between and. These shallow areas are subject to higher storm surges with smaller waves. Other shallow areas include much of the Gulf of Mexico coast, and the Bay of Bengal. The difference is due to how much flow area the storm surge can dissipate to.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Local topography, bay and river orientation, depth of the sea bottom, astronomical tides, as well as other physical features, are taken into account in a predefined grid referred to as a SLOSH basin. Overlapping SLOSH basins are defined for the southern and eastern coastline of the continental U.S.

Geographic entities mentioned:
surface_form: Lake Pontchartrain
instance_of: Lake
countries: United States
coordinates: lat: 30.188888888889
lon: -90.101388888889
This phenomenon is known as a reverse storm surge, or a negative storm surge. Historic storm surges. The deadliest storm surge on record was the 1970 Bhola cyclone, which killed up to 500,000 people in the area of the Bay of Bengal. The low-lying coast of the Bay of Bengal is particularly vulnerable to surges caused by tropical cyclones.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Penrhiwceiber. Penrhiwceiber is a village and community (and electoral ward) in the county borough of Rhondda Cynon Taf, Wales, that lies south of the town Aberpennar and north of the village of Tyntetown, and is one of many villages that lies within the Cynon Valley.

Geographic entities mentioned:
surface_form: Cynon Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.657
lon: -3.461
However, it is debatable if they are truly tropical in character. Tropical activity is also extremely rare in the Great Lakes. However, a storm system that appeared similar to a subtropical or tropical cyclone formed in September 1996 over Lake Huron. The system developed an eye-like structure in its center, and it may have briefly been a subtropical or tropical cyclone. Inland intensification.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
The village is strategically placed at the junction of the rivers Kent and Gowan, at the mouth of the Kentmere Valley. Three hills overlook the village; Reston Scar on the north side on which much of the village is built, Piked Howe to the northeast known to the locals as Craggy Wood and Lily Fell to the south in the direction of the village of Crook on the opposite side of the A591 bypass.

Geographic entities mentioned:
surface_form: Reston Scar
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.3818
lon: -2.8322
They have been converted for residential use. Education. Staveley CE Primary School was founded in 1755 and moved to its present position at Brow Lane on Reston Scar in 1840. A new building was built 30 years ago to house the infant classes. The school also caters for children from the nearby villages of Crook, Kentmere and Ings.

Geographic entities mentioned:
surface_form: Reston Scar
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.3818
lon: -2.8322
Mont Wyville Thomson. Mont Wyville Thomson is a mountain in the French Southern and Antarctic Lands. Located in the Ronarc'h Peninsula, Kerguelen, it rises to a height of above sea level. Mont Wyville Thomson is the highest point of the Ronarc'h Peninsula. It rises almost in the centre. History.

Geographic entities mentioned:
surface_form: mont wyville thomson
instance_of: Mountain
countries: France
coordinates: lat: -49.564444444444
lon: 70.160833333333
The Arctomys Formation is a stratigraphic unit of late Middle Cambrian age. It is present on the western edge of the Western Canada Sedimentary Basin in the Canadian Rockies of Alberta and British Columbia. It was named for Arctomys Peak near Mount Erasmus in Banff National Park by Charles Doolittle Walcott in 1920. Outcrops of the Arctomys can be seen in Banff and Jasper National Parks.

Geographic entities mentioned:
surface_form: Mount Erasmus
instance_of: Mountain
countries: Canada
coordinates: lat: 51.96
lon: -116.9206
Distribution and stratigraphic relationships. The Arctomys Formation is present in the Rocky Mountains of Alberta and British Columbia. It thickens northward from White Man Mountain to a maximum of 336 metres (1,100 ft) at Mount Robson. It is overlies the Pika Formation and is overlain by the Waterfowl Formation. Both contacts are gradational.

Geographic entities mentioned:
surface_form: White Man Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.755556
lon: -115.4825
surface_form: Mount Robson
instance_of: Mountain
countries: Canada
coordinates: lat: 53.11055555555556
lon: -119.15666666666667
To the north the Laguna Mountains are bounded by the Elsinore Fault Zone and to the south by Cameron Valley and Thing Valley. The highest point is Cuyapaipe Mountain at. The mountains are largely contained within Cleveland National Forest. Snow falls on the highest peaks several times a year. Mount Laguna is a village in the Laguna Mountains with a population of about 80.

Geographic entities mentioned:
surface_form: Cuyapaipe Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.8393
lon: -116.401
The remaining 12,000 were relocated to government internment camps in the BC interior or elsewhere in Canada. Judo played an important role in the life of many internees, and there were well-attended dojos at three camps: Tashme Internment Camp near Hope, British Columbia, Popoff Internment Camp in the Slocan Valley, British Columbia, and the Prisoner of War (POW) camp in Angler.

Geographic entities mentioned:
surface_form: Slocan Valley
instance_of: Valley
countries: Canada
coordinates: lat: 49.6834
lon: -117.5024
The lake is long and across and used to be home to a colony of flamingo until they were killed by foxes. The lake was originally fed from The Serpentine in Hyde Park, but is now sourced from a bore hole in the garden. The water is aerated by a waterfall, installed by Elizabeth II and Prince Philip, to replace a cascade constructed by the Queen's parents, George VI and Queen Elizabeth.

Geographic entities mentioned:
surface_form: The Serpentine
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.505277777778
lon: -0.16944444444444