Sarmila/GeoWiki-Features huggingface dataset:
The park is open from 7 am to dusk. In May 2025, Swimmer's itch was reported at the lake, prompting Thurston County to issue a public advisory to avoid swimming there. Lake Management District. Since 1987, Long Lake property owners have authorized Lake Management District No. 19 to oversee the management of the lake. The District was authorized for January 1, 2011 to December 31, 2015.

Geographic entities mentioned:
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 34.78779
lon: -111.210939
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 43.9728
lon: -74.4211
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 44.718
lon: -85.748
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 44.1086787
lon: -75.1564925
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 44.1657291
lon: -98.7168782
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 43.9334172
lon: -97.0073724
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 45.9496317
lon: -95.9225667
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 45.8456754
lon: -99.2676497
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 45.127777777778
lon: -83.973055555556
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 46.235907
lon: -89.49916
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 44.9348621
lon: -97.3996461
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 45.20461
lon: -83.47775
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 43.5597393
lon: -75.1515847
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 45.248184
lon: -85.075807
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 41.615555555556
lon: -87.210555555556
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 45.7281765
lon: -97.3795798
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 47.483055555556
lon: -122.58972222222
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 43.971666666667
lon: -70.611666666667
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 45.8387529
lon: -88.6755297
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 47.0191485
lon: -122.7747634
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 44.572222222222
lon: -85.298888888889
19 to oversee the management of the lake. The District was authorized for January 1, 2011 to December 31, 2015. Boating safety rules. Thurston County establishes regulations regarding boating operations and water safety on Long Lake. Polar Bear Plunge. Each year on New Year's Day, Long Lake Park hosts the Polar Bear Plunge where hundreds ring in the new year by jumping into the lake.

Geographic entities mentioned:
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 34.78779
lon: -111.210939
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 43.9728
lon: -74.4211
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 44.718
lon: -85.748
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 44.1086787
lon: -75.1564925
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 44.1657291
lon: -98.7168782
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 43.9334172
lon: -97.0073724
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 45.9496317
lon: -95.9225667
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 45.8456754
lon: -99.2676497
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 45.127777777778
lon: -83.973055555556
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 46.235907
lon: -89.49916
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 44.9348621
lon: -97.3996461
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 45.20461
lon: -83.47775
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 43.5597393
lon: -75.1515847
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 45.248184
lon: -85.075807
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 41.615555555556
lon: -87.210555555556
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 45.7281765
lon: -97.3795798
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 47.483055555556
lon: -122.58972222222
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 43.971666666667
lon: -70.611666666667
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 45.8387529
lon: -88.6755297
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 47.0191485
lon: -122.7747634
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 44.572222222222
lon: -85.298888888889
Long Lake is fed by Pattison Lake and drains via Himes/Woodland Creek and Lois Lake to Henderson Inlet. Long Lake was given its descriptive name in 1853. Boat launch. The lake can be accessed via a Washington State Department of Fish and Wildlife (WDFW) boat launch. The launch is open during fishing season and requires a WDFW vehicle use permit. Long Lake Park.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Cedar Lake (Martin County, Minnesota). Cedar Lake is a lake in Martin County, in the U.S. state of Minnesota. Cedar Lake was named for the red cedar trees near the lake.

Geographic entities mentioned:
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 47.3869
lon: -121.7
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 29.1925638
lon: -95.082994
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3743
lon: -74.3212
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 46.221
lon: -93.404
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 44.97777778
lon: -94.46138889
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 45.5275
lon: -68.801111111111
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 44.960277777778
lon: -93.321111111111
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 43.78972222
lon: -94.73388889
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 45.2144
lon: -92.571
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 40.9111048
lon: -74.4729616
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 44.59
lon: -93.523333333333
1899 famine in central Kenya. The famine in central Kenya in 1899 is regarded as a devastating catastrophe in Kenyan history. It spread rapidly from 1898 in the central region of the country around Mount Kenya after several consecutive years of low rainfall.

Geographic entities mentioned:
surface_form: Mount Kenya
instance_of: Mountain
countries: Kenya
coordinates: lat: -0.1
lon: 37.2
Social organisation. By the end of the 19th century, Central Kenya was already a densely populated region due to its fertile soils and the rainy climate, especially in the highlands. In addition to the area around Lake Victoria, this region was the most populous in British East Africa, with an estimated population of approximately one million individuals.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
In addition to the area around Lake Victoria, this region was the most populous in British East Africa, with an estimated population of approximately one million individuals. The high-lying area between Mount Kenya and the Ngong Hills was predominantly populated by Kikuyu, Embu, Meru, Mbeere and Ogiek communities.

Geographic entities mentioned:
surface_form: Mount Kenya
instance_of: Mountain
countries: Kenya
coordinates: lat: -0.1
lon: 37.2
Heralds of colonial power. The initial endeavours of the British colonial power to establish a foothold in Kenya were a significant contributing factor to the subsequent disasters. From 1889, the Imperial British East Africa Company established several administrative posts along the existing trade route from the harbour town of Mombasa to Lake Victoria.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
This resulted in the creation of a further cohort of refugees, who subsequently relocated to new regions, thereby causing food scarcity in those areas as well. The highlands between Mount Kenya and the Nyandarua Mountains, which are known for their high rainfall, were not affected by the famine.

Geographic entities mentioned:
surface_form: Mount Kenya
instance_of: Mountain
countries: Kenya
coordinates: lat: -0.1
lon: 37.2
Migration. The rainy central highlands, the northern Kikuyu region and the area around Mount Kenya had no shortage of food, which attracted thousands of migrants from neighbouring regions. Many of these migrants died on the way or shortly after their arrival. The survivors attempted to overcome the famine by working as labourers in the fields of the still fertile areas.

Geographic entities mentioned:
surface_form: Mount Kenya
instance_of: Mountain
countries: Kenya
coordinates: lat: -0.1
lon: 37.2
She was launched on 24 January 1943, sponsored by Mrs. C. C. West, and commissioned on 13 July 1943. July–October 1943. Following training in Lake Michigan, &quot;Raton&quot; moved to Coco Solo in the Panama Canal Zone for additional training. She was off Coco Solo on 11 August 1943 when the merchant ship ′s United States Navy Armed Guard mistakenly opened fire on her, firing one and two rounds.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Rowing at the 1992 Summer Olympics – Women's coxless four. Women's coxless fours competition at the 1992 Summer Olympics in Barcelona was held between 27 July and 1 August at Lake of Banyoles. The event was an open-style, individual rowing event conducted as part of the Rowing at the 1992 Summer Olympics program. Heats. First team of each heat qualify to the final, remainder goes to the repechage.

Geographic entities mentioned:
surface_form: Lake of Banyoles
instance_of: Lake
countries: Spain
coordinates: lat: 42.125277777778
lon: 2.7552777777778
Talayarde River. The rivière Talayarde is a tributary of the Sainte-Anne river flowing in the unorganized territory of Lac-Blanc and in the town of Saint-Raymond, in the MRC Portneuf Regional County Municipality, in the administrative region of Capitale-Nationale, at Quebec, in Canada.

Geographic entities mentioned:
surface_form: rivière talayarde
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.994444
lon: -71.746388
The surveyor Ignace P.-Déry designated this river under the name Talleyarde, in 1862. The surveyor NJE Lefrançois used the current form Rivière Talayarde in his report of 1888. The toponym &quot;Talayarde River&quot; was formalized on December 5, 1968, at the Place Names Bank of the Commission de toponymie du Québec.

Geographic entities mentioned:
surface_form: rivière talayarde
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.994444
lon: -71.746388
Talayarde River. The rivière Talayarde is a tributary of the Sainte-Anne river flowing in the unorganized territory of Lac-Blanc and in the town of Saint-Raymond, in the MRC Portneuf Regional County Municipality, in the administrative region of Capitale-Nationale, at Quebec, in Canada.

Geographic entities mentioned:
surface_form: talayarde river
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.994444
lon: -71.746388
The rivière Talayarde is a tributary of the Sainte-Anne river flowing in the unorganized territory of Lac-Blanc and in the town of Saint-Raymond, in the MRC Portneuf Regional County Municipality, in the administrative region of Capitale-Nationale, at Quebec, in Canada. The Talayarde river valley is mainly served by the forest road R0300 which goes up north passing on the east side of the valley.

Geographic entities mentioned:
surface_form: talayarde river
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.994444
lon: -71.746388
The main economic activities in the sector are forestry and recreational tourism activities. The surface of the Talayarde River (except the rapids areas) is generally frozen from the beginning of December to the end of March, but the safe circulation on the ice is generally made from the end of December to the beginning of March.

Geographic entities mentioned:
surface_form: talayarde river
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.994444
lon: -71.746388
The surveyor Ignace P.-Déry designated this river under the name Talleyarde, in 1862. The surveyor NJE Lefrançois used the current form Rivière Talayarde in his report of 1888. The toponym &quot;Talayarde River&quot; was formalized on December 5, 1968, at the Place Names Bank of the Commission de toponymie du Québec.

Geographic entities mentioned:
surface_form: talayarde river
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.994444
lon: -71.746388
Awkin. Awkin (Quechua &quot;awki&quot; prince; a mythical figure of the Andean culture; grandfather, &quot;-n&quot; a suffix, Hispanicized spelling &quot;Auquin&quot;) is a mountain in the Andes of Peru. It is located in the Lima Region, Cajatambo Province, on the border of the districts of Cajatambo and Gorgor, and in the Oyón Province, Oyón District.

Geographic entities mentioned:
surface_form: awkin
instance_of: Mountain
countries: Peru
coordinates: lat: -10.5844
lon: -76.8656
Mont Limon. Mont Limon is the highest point on the Mauritian island of Rodrigues. It is located roughly in the center of the eastern part of the island and has a height of. Some sources give a higher elevation of. It is located approximately four kilometres south-east of the island's capital, Port Mathurin.

Geographic entities mentioned:
surface_form: mont limon
instance_of: Mountain
countries: Mauritius
coordinates: lat: -19.7
lon: 63.433333333333
Crystal Peak (Box Elder County, Utah). Crystal Peak, at, is a peak in the Raft River Mountains of Utah. The peak is located in Box Elder County and the area designated as Sawtooth National Forest, but the U.S. Forest Service does not own or manage the land on and around the peak. It is located east of Bull Mountain. No roads or trails go to the summit. The summit took its name from Crystal Spring.

Geographic entities mentioned:
surface_form: bull mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.9117
lon: -113.365
surface_form: bull
instance_of: Watercourse
countries: United States
coordinates: lat: 49.46663
lon: -115.45205
surface_form: bull mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.140277777778
lon: -110.73222222222
Crystal Peak (Box Elder County, Utah). Crystal Peak, at, is a peak in the Raft River Mountains of Utah. The peak is located in Box Elder County and the area designated as Sawtooth National Forest, but the U.S. Forest Service does not own or manage the land on and around the peak. It is located east of Bull Mountain. No roads or trails go to the summit. The summit took its name from Crystal Spring.

Geographic entities mentioned:
surface_form: crystal peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.113333333333
lon: -121.83583333333
surface_form: crystal peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.4344
lon: -106.114
surface_form: crystal peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.557777777778
lon: -120.08833333333
surface_form: crystal peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.942222222222
lon: -120.125
surface_form: crystal peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.964722222222
lon: -106.79972222222
surface_form: crystal peak
instance_of: Mountain
countries: United States
coordinates: lat: 46.906247
lon: -121.519048
surface_form: crystal peak
instance_of: Mountain
countries: United States
coordinates: lat: 41.9185
lon: -113.227
There is also a legend that, when practicing archery at Mount Nasu in 1180, Suketaka met Yoshitsune who came to Nasu Onsen-jinja Shrine to pray for certain victory and exchanged an agreement with his older brother Juro Tametaka to let Yoichi join the Minamoto clan. In addition, there are several temples and shrines which Yoichi founded.

Geographic entities mentioned:
surface_form: Mount Nasu
instance_of: Mountain
countries: Japan
coordinates: lat: 37.15
lon: 139.95
List of castles and palaces in Jelenia Góra valley. This is a list of castles, palaces and manors in Jelenia Góra valley and the surrounding area.

Geographic entities mentioned:
surface_form: Jelenia Góra valley
instance_of: Valley
countries: Prussia
coordinates: lat: 50.916666666667
lon: 15.75
Arrival of the Viceroy. On July 3, 1522, the Viceroy's artillery assembled at the Taconera field in Pamplona. Two days later, after bolstering their forces with Castilian and Beamontese troops, they marched toward Baztán, led by the Viceroy, Count of Miranda. On the 5th of July, they arrived in Lantz despite the difficult road conditions.

Geographic entities mentioned:
surface_form: Baztán
instance_of: Valley
countries: Spain
coordinates: lat: 43.146787
lon: -1.5171681
Letters from King Henry II of Navarre. There is even a letter dated 26 March 1522 from King Henry II of Navarre to Jaime Vélaz de Medrano, regarding the oath of fidelity of the inhabitants of Cinco Villas, Baztán and Tierra de Lerín and to request an end to mistreatment.

Geographic entities mentioned:
surface_form: Baztán
instance_of: Valley
countries: Spain
coordinates: lat: 43.146787
lon: -1.5171681
Fossil ornithopod tracks have been reported from the formation. A stratigraphic column at the Mount Bonnell Fault location reveals the following sequence: the Lower Cretaceous Trinity Group is overlain by the Edwards Group. This is followed by Upper Cretaceous formations, starting with the Del Rio Clay, then the Buda Limestone, and finally the Eagle Ford Group.

Geographic entities mentioned:
surface_form: Mount Bonnell
instance_of: Mountain
countries: United States
coordinates: lat: 30.321084
lon: -97.773566
Spion Kop (mountain). Spion Kop (,; “Lookout Mountain”,) is a mountain in the province of KwaZulu-Natal, South Africa. It is located near the town of Ladysmith, 27 km to the WSW and about 2.5 km to the north of the Spioenkop Dam, a reservoir for the waters of the Tugela River. History. This mountain has historical significance.

Geographic entities mentioned:
surface_form: spion kop
instance_of: Mountain
countries: South Africa
coordinates: lat: -28.65
lon: 29.51638889
History. This mountain has historical significance. Its hilltop was the site of the Battle of Spion Kop (one of the most important battles of the Boer Wars) from 23 to 24 January 1900. near the Tugela River, Natal in South Africa
Spion Kop Nature Reserve is located beneath the southern side of this mountain.

Geographic entities mentioned:
surface_form: spion kop
instance_of: Mountain
countries: South Africa
coordinates: lat: -28.65
lon: 29.51638889
Spion Kop (mountain). Spion Kop (,; “Lookout Mountain”,) is a mountain in the province of KwaZulu-Natal, South Africa. It is located near the town of Ladysmith, 27 km to the WSW and about 2.5 km to the north of the Spioenkop Dam, a reservoir for the waters of the Tugela River. History. This mountain has historical significance.

Geographic entities mentioned:
surface_form: spioenkop
instance_of: Mountain
countries: South Africa
coordinates: lat: -28.65
lon: 29.51638889
According to the 2011 census, 5,512 ethnic Macedonians lived in Albania. In the 1989 census, 4,697 people had declared themselves Macedonian. The condition of the Macedonian population living in the Prespa area is described in positive terms, and particular praise is given since all the villages of the area are allowed schooling in their mother tongue.

Geographic entities mentioned:
surface_form: Prespa
instance_of: Lake
countries: North Macedonia
Albania
Greece
coordinates: lat: 40.9
lon: 21.05
As a result, the Slavic minority in Albania was recognized in 1945 as Macedonian. The former Prime Minister Aleksander Meksi openly admitted the presence of ethnic Bulgarians near the Lake Prespa in 1993. After the fall of communism, in 1998, many Macedonians from Mala Prespa and Golo Brdo illegally crossed to the Republic of Macedonia.

Geographic entities mentioned:
surface_form: Lake Prespa
instance_of: Lake
countries: North Macedonia
Albania
Greece
coordinates: lat: 40.9
lon: 21.05
Some, however, have moved to larger cities like Tirana, where roughly 500 ethnic Macedonians live as of the 2011 census. Pustec Municipality (Mala Prespa). Macedonians are only officially recognised as a minority population in Municipality of Pustec, on the shores of Lake Prespa. Devoll. Macedonians also inhabit the region to the south of Lake Prespa, within the Devoll municipality.

Geographic entities mentioned:
surface_form: Lake Prespa
instance_of: Lake
countries: North Macedonia
Albania
Greece
coordinates: lat: 40.9
lon: 21.05
Enfield, Nova Scotia. Enfield is an unincorporated community in the Canadian province of Nova Scotia, located in both East Hants Municipality and Halifax Regional Municipality. Enfield is situated along the Shubenacadie River and its source at Grand Lake, and is directly adjacent to the community of Elmsdale.

Geographic entities mentioned:
surface_form: Grand Lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.9183
lon: -63.5944
Enfield experienced a period of growth during the mid-19th century as a shipping hub for the nearby gold mining area of Renfrew. During this time a system of locks on the Shubenacadie River was constructed to assist small vessels in navigating from the Bay of Fundy to nearby Grand Lake as part of the Shubenacadie Canal.

Geographic entities mentioned:
surface_form: Grand Lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.9183
lon: -63.5944
surface_form: Shubenacadie Canal
instance_of: Watercourse
countries: Canada
coordinates: lat: 44.7018
lon: -63.5543
Horne had spent a number of years traveling the United States and Canada before discovering the site of the Noranda Mines in Quebec. After finding success in Quebec he eventually returned to his hometown of Enfield and established his estate, Monte Vista Farm, on Grand Lake. At his estate Horne raised prize winning cattle and established himself as an integral part of the community.

Geographic entities mentioned:
surface_form: Grand Lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.9183
lon: -63.5944
Geography. Enfield lies in the Shubenacadie Valley, on the northwestern and eastern side of Grand Lake, situated along the meanders of the Shubenacadie River. The community is situated north of Halifax Stanfield International Airport on the border of Hants County and Halifax County. Enfield exists in both the East Hants Municipality and Halifax Regional Municipality. Climate.

Geographic entities mentioned:
surface_form: Shubenacadie Valley
instance_of: Valley
countries: Canada
coordinates: lat: 45.0864
lon: -63.408
surface_form: Grand Lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.9183
lon: -63.5944
Lake Tharthar. Lake Tharthar (also Therthar), and known in Iraq as Buhayrat ath-Tharthar (), is an artificial lake created in 1956, situated 100 kilometers (62 mi) northwest of Baghdad between the Tigris and the Euphrates rivers. History. In 1956, the southern part of the Tharthar depression was turned into an artificial reservoir to collect floodwaters of the Tigris River.

Geographic entities mentioned:
surface_form: lake tharthar
instance_of: Lake
countries: Iraq
coordinates: lat: 33.966666666667
lon: 43.183333333333
surface_form: tharthar
instance_of: Lake
countries: Iraq
coordinates: lat: 33.966666666667
lon: 43.183333333333
Lake Tharthar. Lake Tharthar (also Therthar), and known in Iraq as Buhayrat ath-Tharthar (), is an artificial lake created in 1956, situated 100 kilometers (62 mi) northwest of Baghdad between the Tigris and the Euphrates rivers. History. In 1956, the southern part of the Tharthar depression was turned into an artificial reservoir to collect floodwaters of the Tigris River.

Geographic entities mentioned:
surface_form: lake tharthar
instance_of: Lake
countries: Iraq
coordinates: lat: 33.966666666667
lon: 43.183333333333
surface_form: tharthar
instance_of: Lake
countries: Iraq
coordinates: lat: 33.966666666667
lon: 43.183333333333
surface_form: tharthar
instance_of: Lake
countries: Iraq
coordinates: lat: 33.966666666667
lon: 43.183333333333
Lake Tharthar was the site of a joint American-Iraqi raid in 2005 against an insurgent training base in the region. On October 11, 2007, 19 terrorists and 15 civilians were killed by U.S. forces in Lake Tharthar region during an operation targeting senior leaders of Al-Qaeda in Iraq. Description.

Geographic entities mentioned:
surface_form: lake tharthar
instance_of: Lake
countries: Iraq
coordinates: lat: 33.966666666667
lon: 43.183333333333
surface_form: tharthar
instance_of: Lake
countries: Iraq
coordinates: lat: 33.966666666667
lon: 43.183333333333
History. In 1956, the southern part of the Tharthar depression was turned into an artificial reservoir to collect floodwaters of the Tigris River. The water flows via an artificial inlet canal, named Tharthar Canal. The canal diverts the excess water, by means of a regulator, Samarra Barrage. It merges with the lake in its southeastern bank.

Geographic entities mentioned:
surface_form: tharthar
instance_of: Lake
countries: Iraq
coordinates: lat: 33.966666666667
lon: 43.183333333333
It merges with the lake in its southeastern bank. The lake has an artificial outlet called Taksim Tharthar Canal, which drains to the Euphrates River directly. The canal, after 28 km (17.4 mi) from its outlet, bifurcates to another canal called &quot;Dhira'a Dijla&quot; (Arm of Tigris) that returns water back to the Tigris River.

Geographic entities mentioned:
surface_form: tharthar
instance_of: Lake
countries: Iraq
coordinates: lat: 33.966666666667
lon: 43.183333333333
Description. The Tharthar depression was formed during the Holocene age, mainly by karstification, due to dissolving of gypsum rocks of the Fatha Formation nearby. Tharthar covers roughly and flows from the central and eastern parts of the Sinjar Mountains and adjacent hills, with a floor of –3m above sea level. The maximum length and width of the depression are 120 and 48 km, respectively.

Geographic entities mentioned:
surface_form: tharthar
instance_of: Lake
countries: Iraq
coordinates: lat: 33.966666666667
lon: 43.183333333333
The eastern rim of the depression is higher than the western one; the heights of both rims are and, respectively. The main purpose of the Tharthar Lake is to collect excess water of the Tigris River during flood seasons and to recharge water to the Tigris and Euphrates Rivers during dry seasons, when there is shortage of water in both rivers.

Geographic entities mentioned:
surface_form: tharthar
instance_of: Lake
countries: Iraq
coordinates: lat: 33.966666666667
lon: 43.183333333333
The area harbors many species of animals and vegetation. Birds. Tharthar Lake is considered the main wintering grounds for many threatened species of migrant birds such as saker falcon, MacQueen's bustard, and sociable lapwing. 54 bird species were seen in Tharthar lake including: pallid harrier, European roller, and black-tailed godwit.

Geographic entities mentioned:
surface_form: tharthar
instance_of: Lake
countries: Iraq
coordinates: lat: 33.966666666667
lon: 43.183333333333
Jim Bridwell. Jim Bridwell (July 29, 1944 – February 16, 2018) was an American rock climber and mountaineer, active from 1965 in Yosemite Valley, but later in Patagonia and Alaska. He was noted for pushing the standards of both aid climbing and big wall climbing, and later alpine climbing. He wrote numerous articles on climbing and developed several important pieces of aid climbing equipment.

Geographic entities mentioned:
surface_form: Yosemite Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
Climbing career. Bridwell is credited with over 100 first ascents (FA) in Yosemite Valley, in addition to conducting the first one-day ascent of &quot;The Nose&quot; on El Capitan on May 26, 1975, with John Long and Billy Westbay. He founded Yosemite National Park's Search and Rescue Team (YOSAR), spearheading many rescues.

Geographic entities mentioned:
surface_form: Yosemite Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
Schmidt Glacier (Heard Island and McDonald Islands). Schmidt Glacier () is a glacier, 0.7 nautical miles (1.3 km) long, flowing west from Baudissin Glacier between Mount Drygalski and North West Cornice, on the west side of Heard Island in the southern Indian Ocean.

Geographic entities mentioned:
surface_form: Mount Drygalski
instance_of: Mountain
countries: Australia
coordinates: lat: -53.03333333333333
lon: 73.38333333333334
Tonlé Sap. Tonlé Sap (;,; or commonly translated as <nowiki/>'Great Lake<nowiki/>') is a lake in the northwest of Cambodia. Belonging to the Mekong River system, Tonlé Sap is the largest freshwater lake in Southeast Asia and one of the most diverse and productive ecosystems in the world. It was designated as a Biosphere Reserve by UNESCO in 1997 due to its high biodiversity.

Geographic entities mentioned:
surface_form: tonlé sap
instance_of: Lake
countries: Cambodia
coordinates: lat: 12.883333333333
lon: 104.06666666667
Geography. Tonlé Sap Lake is located in the northwest of the lower Mekong plain, formed by the collision and collapse of the Indian Plate and the Eurasian Plate. The lower Mekong plain used to be a bay, and the sea level rose rapidly at the end of the last glacial period.

Geographic entities mentioned:
surface_form: tonlé sap
instance_of: Lake
countries: Cambodia
coordinates: lat: 12.883333333333
lon: 104.06666666667
The current river morphology of the Mekong Delta was developed over the past 6,000 years, while the remaining waters in the northwest corner of the lower Mekong plain formed the Tonlé Sap. Hydrology. The Tonlé Sap drainage basin is bordered to the southwest by the Cardamom Mountains, with heights of more than, and to the north are the Piandan Mountains with an average height of.

Geographic entities mentioned:
surface_form: tonlé sap
instance_of: Lake
countries: Cambodia
coordinates: lat: 12.883333333333
lon: 104.06666666667
Hydrology. The Tonlé Sap drainage basin is bordered to the southwest by the Cardamom Mountains, with heights of more than, and to the north are the Piandan Mountains with an average height of. The basin covers an area of. The -long Tonlé Sap River connects the Tonlé Sap Lake with the Mekong River and contributes 9% of the flow of the Mekong River.

Geographic entities mentioned:
surface_form: tonlé sap
instance_of: Lake
countries: Cambodia
coordinates: lat: 12.883333333333
lon: 104.06666666667
The basin covers an area of. The -long Tonlé Sap River connects the Tonlé Sap Lake with the Mekong River and contributes 9% of the flow of the Mekong River. The size and water volume of the lake varies greatly throughout the year, with a minimum area of about and a volume of about in the dry season, and the water body expands in the rainy season, increasing the depth to.

Geographic entities mentioned:
surface_form: tonlé sap
instance_of: Lake
countries: Cambodia
coordinates: lat: 12.883333333333
lon: 104.06666666667
surface_form: tonlé sap
instance_of: Lake
countries: Cambodia
coordinates: lat: 12.883333333333
lon: 104.06666666667
The maximum area is, and the volume is about. About 34% of the water in the Tonlé Sap comes from the rivers that enter the lake, about 53.5% from the Mekong River, and 12.5% from precipitation. May to October is the rainy season in the lower Mekong plain, and November to March is the dry season. The annual rainfall is. Almost all the precipitation is in the rainy season.

Geographic entities mentioned:
surface_form: tonlé sap
instance_of: Lake
countries: Cambodia
coordinates: lat: 12.883333333333
lon: 104.06666666667
May to October is the rainy season in the lower Mekong plain, and November to March is the dry season. The annual rainfall is. Almost all the precipitation is in the rainy season. At the end of the dry season, the Tonlé Sap Lake has a typical depth of. As the monsoon rain begins, the water level of the river begins to rise, eventually reversing the flow of the river.

Geographic entities mentioned:
surface_form: tonlé sap
instance_of: Lake
countries: Cambodia
coordinates: lat: 12.883333333333
lon: 104.06666666667
As the monsoon rain begins, the water level of the river begins to rise, eventually reversing the flow of the river. The water level of the Tonlé Sap increases by about, the flow of the Mekong gradually decreases at the end of the rainy season, and the flow of the Tonlé Sap then reverses and begins to replenish the flow of the Mekong.

Geographic entities mentioned:
surface_form: tonlé sap
instance_of: Lake
countries: Cambodia
coordinates: lat: 12.883333333333
lon: 104.06666666667
surface_form: tonlé sap
instance_of: Lake
countries: Cambodia
coordinates: lat: 12.883333333333
lon: 104.06666666667
The extreme hydrodynamic complexity of the Tonlé Sap Lake, both in time and space, makes it impossible to measure specific flow, and water level rather than velocity and volume determines the movement of water as it shapes the landscape. 72% of the modern sediments deposited in the Tonlé Sap come from the Mekong River, while only 28% come from the catchments upstream of the lake.

Geographic entities mentioned:
surface_form: tonlé sap
instance_of: Lake
countries: Cambodia
coordinates: lat: 12.883333333333
lon: 104.06666666667
Ecology. The land cover of the Tonlé Sap Basin is 55% forest and 45% agricultural land. The lake is surrounded by freshwater mangroves known as &quot;flood forests&quot;, accounting for 3% of the basin area, and the floodplain is surrounded by low hills and covered with evergreen or deciduous seasonal tropical plants.

Geographic entities mentioned:
surface_form: tonlé sap
instance_of: Lake
countries: Cambodia
coordinates: lat: 12.883333333333
lon: 104.06666666667
The Mekong giant catfish, which lives in the Tonlé Sap Lake, is one of the largest freshwater fish in the world. A fisherman caught a Mekong giant catfish weighing nearly 648 pounds in May 2004, but its population has been declining since the mid-1970s. It is currently illegal for fishermen to catch and retain Mekong giant catfish, and only a few are used for scientific research.

Geographic entities mentioned:
surface_form: tonlé sap
instance_of: Lake
countries: Cambodia
coordinates: lat: 12.883333333333
lon: 104.06666666667
It is currently illegal for fishermen to catch and retain Mekong giant catfish, and only a few are used for scientific research. As a natural flood reservoir for the entire Mekong River system, Tonlé Sap Lake regulates floods in the lower reaches of Phnom Penh during the rainy season, and is also an important supplement to the dry season flow of the Mekong Delta.

Geographic entities mentioned:
surface_form: tonlé sap
instance_of: Lake
countries: Cambodia
coordinates: lat: 12.883333333333
lon: 104.06666666667
In 1997, UNESCO designated the Tonle Sap as a biosphere reserve, but scientists have been concerned that high dams built in southern China and Laos will affect the strength and flow of countercurrents into the Tonlé Sap, reducing the number of fish in the lake.

Geographic entities mentioned:
surface_form: tonlé sap
instance_of: Lake
countries: Cambodia
coordinates: lat: 12.883333333333
lon: 104.06666666667
surface_form: tonle sap
instance_of: Lake
countries: Cambodia
coordinates: lat: 12.883333333333
lon: 104.06666666667
surface_form: tonle sap
instance_of: Lake
countries: Cambodia
coordinates: lat: 12.883333333333
lon: 104.06666666667
The approximately 1.2 million people who live in the Tonlé Sap Lake area, which accounts for about 60% of Cambodia's annual freshwater catch of over 400,000 tons, account for 60% of the country's population's protein intake. Most fish are eaten fresh, and savory and fermented fish paste Prahoc is usually marinated from the least popular fish or leftover fish that cannot be sold fresh.

Geographic entities mentioned:
surface_form: tonlé sap
instance_of: Lake
countries: Cambodia
coordinates: lat: 12.883333333333
lon: 104.06666666667
After two days of racing all the canoes come together to celebrate the Naga, the water serpent, who supposedly spit out the lake into the sea at the end of the rainy season, while bringing fish into the Mekong through the Tonlé Sap River. The area is home to many Cambodians of Vietnamese origin who live in floating villages on boats by the lake.

Geographic entities mentioned:
surface_form: tonlé sap
instance_of: Lake
countries: Cambodia
coordinates: lat: 12.883333333333
lon: 104.06666666667
The area is home to many Cambodians of Vietnamese origin who live in floating villages on boats by the lake. Most of the fishermen of Tonlé Sap Lake are of Vietnamese origin. They have lived in Cambodia for a long time and are the main suppliers of the country's fishery market. They had to flee to Vietnam during the Khmer Rouge era from 1975 to 1979.

Geographic entities mentioned:
surface_form: tonlé sap
instance_of: Lake
countries: Cambodia
coordinates: lat: 12.883333333333
lon: 104.06666666667
Farther from the lake, the forest gradually turns into a thicket, and finally into a meadow. In areas with higher quality soils or higher altitudes, deciduous mixed forests and semi-evergreen forests occur. This diversity of vegetation types underlies the species diversity of the Tonle Sap ecosystem, with interlocking forests, grasslands and swamps providing refuge for local wildlife.

Geographic entities mentioned:
surface_form: tonle sap
instance_of: Lake
countries: Cambodia
coordinates: lat: 12.883333333333
lon: 104.06666666667
Tonle Sap habitat for nesting, breeding, spawning, and foraging in the floodplain, which will adversely affect fish productivity and overall biodiversity in the Tonle Sap.

Geographic entities mentioned:
surface_form: tonle sap
instance_of: Lake
countries: Cambodia
coordinates: lat: 12.883333333333
lon: 104.06666666667
In July 2020, under the influence of the El Niño phenomenon and the impoundment of dams in the tributaries of the Mekong River, the water level of the Tonle Sap Lake hit a record low for the same period in the past 60 years. Fishery.

Geographic entities mentioned:
surface_form: tonle sap
instance_of: Lake
countries: Cambodia
coordinates: lat: 12.883333333333
lon: 104.06666666667
Most of the fishermen of Tonlé Sap Lake are of Vietnamese origin. They have lived in Cambodia for a long time and are the main suppliers of the country's fishery market. They had to flee to Vietnam during the Khmer Rouge era from 1975 to 1979. After the downfall of the regime, they returned and continued to fish in the Tonle Sap.

Geographic entities mentioned:
surface_form: tonle sap
instance_of: Lake
countries: Cambodia
coordinates: lat: 12.883333333333
lon: 104.06666666667
Iso Lamujärvi. Iso Lamujärvi is a medium-sized lake in the Siikajoki main catchment area. It is located in the region Northern Ostrobothnia in Finland. There are eight islands in the lake.

Geographic entities mentioned:
surface_form: iso lamujärvi
instance_of: Lake
countries: Finland
coordinates: lat: 64.01184
lon: 26.27375
surface_form: lamujärvi
instance_of: Lake
countries: Finland
coordinates: lat: 64.01184
lon: 26.27375
It is a tributary of the East Fork Kaweah River. Course. Monarch Creek has its source in the high-elevation Monarch Lakes on Sawtooth Peak, at an elevation of 10,648 feet above sea level. It takes a steep descent of over 2,800 feet nearly due westward over a series of large cascades broken up by flat subalpine meadows. Its course is heavily defined by the glacial topography of the area.

Geographic entities mentioned:
surface_form: Sawtooth Peak
instance_of: Mountain
countries: United States
coordinates: lat: 36.455277777778
lon: -118.555
Kalusa, India. Kalusa or Kaloosa is a village in the Bandipore district of Jammu and Kashmir, India. About 72 families of Kashmiri Pandits lived in this village immediately before the mass forced-exodus from the valley in the early 1990s. Presently as of January 2009, only about 4 Kashmiri Pandit families live there. The rest of the population are Kashmiri Muslims.

Geographic entities mentioned:
surface_form: valley
instance_of: Valley
countries: India
coordinates: lat: 34.0333
lon: 74.6667
The waters of San Pablo Lakes provide a generous source of tilapia for Metro Manila and suburbs. Legend. The legend of Lake Mohicap is quite similar to those of Lakes Pandin and Yambo to the east. A couple once had a very sickly daughter named Munica, and frequently prayed to God for her health, vowing to do anything in return.

Geographic entities mentioned:
surface_form: Lakes Pandin and Yambo
instance_of: Group of lakes
countries: Philippines
Lake Muhikap. Lake Mohicap (also spelled as Mojicap) is one of the seven lakes of San Pablo City, in the province of Laguna, Philippines. The lake, located in Brgy. San Buenaventura, has an area of and is one of the main suppliers of water in the city. The waters of San Pablo Lakes provide a generous source of tilapia for Metro Manila and suburbs. Legend.

Geographic entities mentioned:
surface_form: laguna
instance_of: Mountain
countries: Philippines
coordinates: lat: 14.3236
lon: 121.253
Lake Muhikap. Lake Mohicap (also spelled as Mojicap) is one of the seven lakes of San Pablo City, in the province of Laguna, Philippines. The lake, located in Brgy. San Buenaventura, has an area of and is one of the main suppliers of water in the city. The waters of San Pablo Lakes provide a generous source of tilapia for Metro Manila and suburbs. Legend.

Geographic entities mentioned:
surface_form: lake muhikap
instance_of: Lake
countries: Philippines
coordinates: lat: 14.126
lon: 121.334
Schmitten im Taunus. Schmitten im Taunus (until 25 August 2021 &quot;Schmitten&quot;) is a municipality in the Hochtaunuskreis in Hessen, Germany. Geography. Schmitten is the highest community in the Taunus, approximately 24 km north of Frankfurt am Main, within which is the &quot;Großer Feldberg&quot; (881m). Neighbouring communities.

Geographic entities mentioned:
surface_form: Großer Feldberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.2325
lon: 8.4588888888889
Sidneys Knob is part of a bifurcated ridgeline as seen in the topographic map below. The mountain is seen on postcards, mainly viewed from the Pennsylvania Turnpike, as vehicles exit west out of the Tuscarora Mountain Tunnel northeast of the peak. Sometimes referred to as &quot;Pyramid Point&quot; or on early postcards as Henry's Knob, this landmark is one of the most noted on the turnpike.

Geographic entities mentioned:
surface_form: pyramid
instance_of: Lake
countries: United States
coordinates: lat: 40.033333333333
lon: -119.56666666667
surface_form: henry's knob
instance_of: Mountain
countries: United States
coordinates: lat: 35.130969444444
lon: -81.274244444444
Sidneys Knob. Sidneys Knob appears to be an atypical mountain for Pennsylvania when viewed from the northeast. Most of the mountains in the Commonwealth are long linear ridges or flatted topped plateau mountains. Sidneys Knob is part of a bifurcated ridgeline as seen in the topographic map below.

Geographic entities mentioned:
surface_form: sidneys knob
instance_of: Mountain
countries: United States
coordinates: lat: 40.061819444444
lon: -77.9054
Most of the mountains in the Commonwealth are long linear ridges or flatted topped plateau mountains. Sidneys Knob is part of a bifurcated ridgeline as seen in the topographic map below. The mountain is seen on postcards, mainly viewed from the Pennsylvania Turnpike, as vehicles exit west out of the Tuscarora Mountain Tunnel northeast of the peak.

Geographic entities mentioned:
surface_form: sidneys knob
instance_of: Mountain
countries: United States
coordinates: lat: 40.061819444444
lon: -77.9054
Sidneys Knob is part of a bifurcated ridgeline as seen in the topographic map below. The mountain is seen on postcards, mainly viewed from the Pennsylvania Turnpike, as vehicles exit west out of the Tuscarora Mountain Tunnel northeast of the peak. Sometimes referred to as &quot;Pyramid Point&quot; or on early postcards as Henry's Knob, this landmark is one of the most noted on the turnpike.

Geographic entities mentioned:
surface_form: tuscarora mountain
instance_of: Landform
countries: United States
coordinates: lat: 40.236666666667
lon: -77.738333333333
Carlin's Cairn. Carlin's Cairn is a hill in the Rhinns of Kells, a sub-range of the Galloway Hills range, part of the Southern Uplands of Scotland. It is located immediately north of Corserine, the highest summit of the range. The eighth highest hill in southern Scotland, the commonest ascent is from Forrest Lodge to the east but it is also climbed as part of a traverse along the entire ridge.

Geographic entities mentioned:
surface_form: Corserine
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.155082
lon: -4.359126
Sections. Geographically and hydrologically the Neretva is divided into three sections. Its source and headwaters gorge are situated deep in the Dinaric Alps at the base of the Zelengora and Lebršnik mountains, specifically under the Gredelj saddle. The river source is at 1,227 meters above sea level and consists of five small and distinct wellsprings.

Geographic entities mentioned:
surface_form: Zelengora
instance_of: Mountain
countries: Bosnia and Herzegovina
coordinates: lat: 43.4225
lon: 18.487777777778
surface_form: Lebršnik
instance_of: Mountain
countries: Bosnia and Herzegovina
coordinates: lat: 43.207273
lon: 18.650153
Right below Konjic, the Neretva again expands into a third and largest valley which provided fertile agricultural land before it was flooded by large artificial reservoir, Jablaničko Lake, formed after construction of a Jablanica Dam near town of Jablanica.

Geographic entities mentioned:
surface_form: Jablaničko Lake
instance_of: Lake
countries: Bosnia and Herzegovina
coordinates: lat: 43.692222222222
lon: 17.8275
From Jablanica, the Neretva enters third and the largest canyon on its course, running through the steep slopes mountains of Prenj, Čvrsnica and Čabulja reaching in depth. Three hydroelectric dams operate between Jablanica and Mostar. When the Neretva expands for the second and final time, it reaches its third section.

Geographic entities mentioned:
surface_form: Prenj
instance_of: Mountain
countries: Bosnia and Herzegovina
coordinates: lat: 43.53480621248335
lon: 17.90430346491326
surface_form: Čvrsnica
instance_of: Mountain
countries: Bosnia and Herzegovina
coordinates: lat: 43.616666666667
lon: 17.616666666667
surface_form: Čabulja
instance_of: Mountain
countries: Bosnia and Herzegovina
coordinates: lat: 43.4833
lon: 17.65