Sarmila/GeoWiki-Features huggingface dataset:
Tributary rivers form valleys where villages lie and whose economy is based on agriculture, livestock, and artisan production. The savanna is bordered to the east by the Eastern Hills that run north-south and contain the Guadalupe and Monserrate hills. The western city limit is formed by the Bogotá River.

Geographic entities mentioned:
surface_form: Guadalupe
instance_of: Mountain
countries: Colombia
coordinates: lat: 4.59194
lon: -74.0544
surface_form: Monserrate
instance_of: Mountain
countries: Colombia
coordinates: lat: 4.605833
lon: -74.056389
There currently remains approximately 700,000 people in the metropolitan area and 75,000 in other nearby municipalities that are without water services. Drainage. The Bogotá drainage system consists of three main sub-catchments: the Salitre, Fucha and Tunjuelo Rivers. Each one flows from east to west. The drainage system is a combination of a combined and separated system.

Geographic entities mentioned:
surface_form: Tunjuelo River
instance_of: Watercourse
countries: Colombia
coordinates: lat: 4.30708333
lon: -74.13061111
The plan also calls for the construction of a larger primary plant with a treatment capacity to be located downstream of Bogotá. This larger WWTP called Canoas will treat wastewater from the Fucha, Tunjuelo and Soacha basins.

Geographic entities mentioned:
surface_form: Tunjuelo
instance_of: Watercourse
countries: Colombia
coordinates: lat: 4.30708333
lon: -74.13061111
surface_form: Soacha basins
instance_of: Watercourse
countries: Colombia
coordinates: lat: 4.53675
lon: -74.17313889
These planned expansions to the wastewater treatment capacity are meant to address one of the biggest environmental problems facing Bogotá and that is untreated wastewater entering the Bogota River as it flows through the middle basin. In this section, Bogotá City discharges all of its wastewater into the river through three main urban tributaries: Salitre, Fucha, and Tunjuelo Rivers.

Geographic entities mentioned:
surface_form: Tunjuelo River
instance_of: Watercourse
countries: Colombia
coordinates: lat: 4.30708333
lon: -74.13061111
It is notable that the airport is publicly owned but private-use only. The airport was previously known as Isle Municipal Airport. Isle is the only city on Mille Lacs Lake with a functioning airport. Pilots flying into the Isle Private Airport must be members of the Isle Airport Association, formerly known as the Isle Flying Club, or have permission from a current member.

Geographic entities mentioned:
surface_form: Mille Lacs Lake
instance_of: Lake
countries: United States
coordinates: lat: 46.2381
lon: -93.6434
On Thursday, November 20, 1980, the drill assembly of a Texaco contracted oil rig, just offshore of the salt dome-caused Jefferson Island (itself in the east southeast section of Lake Peigneur), pierced an inactive third level of the Diamond Crystal Salt Company salt mine.

Geographic entities mentioned:
surface_form: jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 44.6743006
lon: -121.799573611
surface_form: peigneur
instance_of: Lake
countries: United States
coordinates: lat: 29.9808
lon: -91.9833
surface_form: lake peigneur
instance_of: Lake
countries: United States
coordinates: lat: 29.9808
lon: -91.9833
Pillars of salt had been left in place to support the ceiling at each level. The pillars were dissolved by the encroaching fresh water and caused the mine tunnels to collapse. The resultant sinkhole swallowed the drilling platform, eleven barges holding supplies for the drilling operation, a tugboat, many trees, and of the surrounding terrain, including much of Jefferson Island.

Geographic entities mentioned:
surface_form: jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 44.6743006
lon: -121.799573611
Lake Peigneur. Lake Peigneur is a brackish lake in the U.S. state of Louisiana, north of Delcambre and west of New Iberia, near the northernmost tip of Vermilion Bay. With a maximum depth of, it is the deepest lake in Louisiana.

Geographic entities mentioned:
surface_form: vermilion
instance_of: Lake
countries: United States
coordinates: lat: 47.857908333333
lon: -92.299611111111
surface_form: peigneur
instance_of: Lake
countries: United States
coordinates: lat: 29.9808
lon: -91.9833
surface_form: lake peigneur
instance_of: Lake
countries: United States
coordinates: lat: 29.9808
lon: -91.9833
So much water drained into the caverns that the flow of the Delcambre Canal that usually empties the lake into Vermilion Bay was reversed, causing salt water from the Gulf of Mexico to flow into what was now a dry lakebed. This backflow created for a few days the tallest waterfall ever in the state of Louisiana, at, as the lake refilled with salty water from the Delcambre Canal and Vermilion Bay.

Geographic entities mentioned:
surface_form: vermilion
instance_of: Lake
countries: United States
coordinates: lat: 47.857908333333
lon: -92.299611111111
Lake Peigneur. Lake Peigneur is a brackish lake in the U.S. state of Louisiana, north of Delcambre and west of New Iberia, near the northernmost tip of Vermilion Bay. With a maximum depth of, it is the deepest lake in Louisiana.

Geographic entities mentioned:
surface_form: peigneur
instance_of: Lake
countries: United States
coordinates: lat: 29.9808
lon: -91.9833
surface_form: lake peigneur
instance_of: Lake
countries: United States
coordinates: lat: 29.9808
lon: -91.9833
With a maximum depth of, it is the deepest lake in Louisiana. Its name comes from the French word &quot;peigneur&quot;, meaning &quot;one who combs.&quot;
Previously, it had been a freshwater lake, popular for recreation, until human activity caused an unusual disaster on November 20, 1980, that changed its structure and the surrounding land. Drilling disaster.

Geographic entities mentioned:
surface_form: peigneur
instance_of: Lake
countries: United States
coordinates: lat: 29.9808
lon: -91.9833
The mine was finally closed in December 1986. Since 1994, AGL Resources has used Lake Peigneur's underlying salt dome as a storage and hub facility for pressurized natural gas. There was concern from local residents in 2009 over the safety of storing the gas under the lake and nearby drilling operations.

Geographic entities mentioned:
surface_form: peigneur
instance_of: Lake
countries: United States
coordinates: lat: 29.9808
lon: -91.9833
surface_form: lake peigneur
instance_of: Lake
countries: United States
coordinates: lat: 29.9808
lon: -91.9833
Aftermath. In 1983, Texaco and the drilling contractor Wilson Brothers paid million (equivalent to $ million in) to Diamond Crystal, while Texaco, Wilson Brothers and Diamond Crystal also paid a total of $12.8million (equivalent to $ million in) to the Live Oak Gardens botanical garden and plant nursery, in out-of-court settlements to compensate for the damage caused.

Geographic entities mentioned:
surface_form: brothers
instance_of: Mountain
countries: United States
coordinates: lat: 47.6537193
lon: -123.140575
surface_form: brothers
instance_of: Mountain
countries: United States
coordinates: lat: 47.6537193
lon: -123.140575
Casa View, Dallas. Casa View is a residential neighborhood in Dallas, Texas, United States, located near White Rock Lake in the northeastern portion of the city. According to the Greater Casa View Alliance, the Greater Casa View area is bordered by Buckner Boulevard, Garland Road, I-635 and Oates to the city line of neighboring Mesquite.

Geographic entities mentioned:
surface_form: White Rock Lake
instance_of: Lake
countries: United States
coordinates: lat: 32.834166666667
lon: -96.722777777778
Østerdal Billag. Østerdal Billag is a Norwegian bus operator operating in Østerdalen in Innlandet. The company also operates in cooperates with Gauldal Billag on a NOR-WAY express bus between Trondheim and Oslo. The company has its headquarters in Tynset. The company was founded in 1973 as a merger between 23 local bus companies and is owned by Gauldal Billag.

Geographic entities mentioned:
surface_form: Østerdalen
instance_of: Valley
countries: Norway
coordinates: lat: 61.575916666666664
lon: 11.087111111111112
Cahilty Lake (British Columbia). Cahilty Lake is a lake in British Columbia, Canada.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: cahilty lake (british columbia)
instance_of: Lake
countries: Canada
coordinates: lat: 50.93222
lon: -119.88083
Cahilty Lake (British Columbia). Cahilty Lake is a lake in British Columbia, Canada.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: cahilty lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.93222
lon: -119.88083
It surmounts Barclay Bay to the east and northeast, and Diomedes Lake on the southeast
The feature is part of the Antarctic Specially Protected Area &quot;ASPA 126 Byers Peninsula&quot;, situated in one of its restricted zones.

Geographic entities mentioned:
surface_form: Diomedes Lake
instance_of: Lake
coordinates: lat: -62.60194444444444
lon: -61.111111111111114
The hill is named after the Jordi Enrique from Juan Carlos I Base who, together with Francesc Sàbat, made the first ascent of the island's summit Mount Friesland (1700 m) on 30 December 1991. Location. Enrique Hill is located at, which is 1.54 km east-northeast of Dulo Hill, 850 m east-southeast of Battenberg Hill and 1.4 km northwest of Penca Hill.

Geographic entities mentioned:
surface_form: Mount Friesland
instance_of: Mountain
coordinates: lat: -62.670805555556
lon: -60.186305555556
surface_form: mount friesland
instance_of: Mountain
coordinates: lat: -62.670805555556
lon: -60.186305555556
surface_form: enrique
instance_of: Mountain
coordinates: lat: -62.5987
lon: -61.127
Location. Enrique Hill is located at, which is 1.54 km east-northeast of Dulo Hill, 850 m east-southeast of Battenberg Hill and 1.4 km northwest of Penca Hill. Spanish mapping in 1992, and Bulgarian in 2009 and 2017.

Geographic entities mentioned:
surface_form: Dulo Hill
instance_of: Mountain
coordinates: lat: -62.5994
lon: -61.1578
surface_form: Penca Hill
instance_of: Mountain
coordinates: lat: -62.6014
lon: -61.1231
surface_form: penca hill
instance_of: Mountain
coordinates: lat: -62.6014
lon: -61.1231
surface_form: dulo hill
instance_of: Mountain
coordinates: lat: -62.5994
lon: -61.1578
Enrique Hill. Enrique Hill (, ‘Halm Enrique’ \'h&lm en-'ri-ke\) is the ice-free hill rising to 156 m in Dospey Heights on the Ray Promontory of Byers Peninsula, Livingston Island in the South Shetland Islands, Antarctica.

Geographic entities mentioned:
surface_form: enrique hill
instance_of: Mountain
coordinates: lat: -62.5987
lon: -61.127
Enrique Hill. Enrique Hill (, ‘Halm Enrique’ \'h&lm en-'ri-ke\) is the ice-free hill rising to 156 m in Dospey Heights on the Ray Promontory of Byers Peninsula, Livingston Island in the South Shetland Islands, Antarctica.

Geographic entities mentioned:
surface_form: enrique hill
instance_of: Mountain
coordinates: lat: -62.5987
lon: -61.127
surface_form: enrique
instance_of: Mountain
coordinates: lat: -62.5987
lon: -61.127
They proceeded up the North Branch of the Dead River, through the Chain of Ponds to Arnold Pond in Coburn Gore (T.2/3 R.6 WBKP), and across the height of land into the watershed of Quebec's Chaudière River. The logging industry is prominent in the area. Flagstaff Lake was formed by Long Falls Dam in 1950, to regulate the flow of the Dead River into the Kennebec River.

Geographic entities mentioned:
surface_form: Chaudière River
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.742777777777775
lon: -71.2786111111111
surface_form: dead
instance_of: Watercourse
countries: United States
coordinates: lat: 45.3333
lon: -69.9697
The Northern Forest Canoe Trail (NFCT) is a marked canoeing route extending from Old Forge, New York, to Fort Kent, Maine. From a four-mile portage between Wrangler on Wrangler Lake and Dallas Plantation on the South Branch, the trail runs about down the Dead River, to the mouth of Spencer Stream below Grand Falls.

Geographic entities mentioned:
surface_form: Wrangler Lake
instance_of: Lake
countries: United States
coordinates: lat: 44.683333333333
lon: -110.43472222222
surface_form: wrangler lake
instance_of: Lake
countries: United States
coordinates: lat: 44.683333333333
lon: -110.43472222222
surface_form: dead
instance_of: Watercourse
countries: United States
coordinates: lat: 45.3333
lon: -69.9697
Dead River (Kennebec River tributary). The Dead River, sometimes called the West Branch, is a river in central Maine in the United States. Its source is Flagstaff Lake, where its two main tributaries, South Branch Dead River and North Branch Dead River, join (). It flows generally east to join the Kennebec River at The Forks, Maine. The Dead River played a role in the American Revolution.

Geographic entities mentioned:
surface_form: dead river
instance_of: Watercourse
countries: United States
coordinates: lat: 45.3333
lon: -69.9697
Dead River (Kennebec River tributary). The Dead River, sometimes called the West Branch, is a river in central Maine in the United States. Its source is Flagstaff Lake, where its two main tributaries, South Branch Dead River and North Branch Dead River, join (). It flows generally east to join the Kennebec River at The Forks, Maine. The Dead River played a role in the American Revolution.

Geographic entities mentioned:
surface_form: dead river
instance_of: Watercourse
countries: United States
coordinates: lat: 45.3333
lon: -69.9697
surface_form: west branch
instance_of: Watercourse
countries: United States
coordinates: lat: 45.3333
lon: -69.9697
Dead River (Kennebec River tributary). The Dead River, sometimes called the West Branch, is a river in central Maine in the United States. Its source is Flagstaff Lake, where its two main tributaries, South Branch Dead River and North Branch Dead River, join (). It flows generally east to join the Kennebec River at The Forks, Maine. The Dead River played a role in the American Revolution.

Geographic entities mentioned:
surface_form: dead river
instance_of: Watercourse
countries: United States
coordinates: lat: 45.3333
lon: -69.9697
surface_form: dead river
instance_of: Watercourse
countries: United States
coordinates: lat: 45.3333
lon: -69.9697
surface_form: flagstaff lake
instance_of: Lake
countries: United States
coordinates: lat: 42.5825
lon: -119.80027777778
It flows generally east to join the Kennebec River at The Forks, Maine. The Dead River played a role in the American Revolution. In the fall of 1775 then newly commissioned Colonel Benedict Arnold led a force of over 1000 men on a grueling trip through Maine, as part of the invasion of Canada.

Geographic entities mentioned:
surface_form: dead river
instance_of: Watercourse
countries: United States
coordinates: lat: 45.3333
lon: -69.9697
Ascending the Kennebec in bateaux, they avoided the rapids of the lower Dead River via a portage of about at the &quot;Great Carrying Place&quot; (Carrying Place–Carrying Place Town, Maine Townships 1–2, Range 3, BKP WKR) to a position above Long Falls (now drowned in Flagstaff Lake).

Geographic entities mentioned:
surface_form: dead river
instance_of: Watercourse
countries: United States
coordinates: lat: 45.3333
lon: -69.9697
surface_form: flagstaff lake
instance_of: Lake
countries: United States
coordinates: lat: 42.5825
lon: -119.80027777778
The logging industry is prominent in the area. Flagstaff Lake was formed by Long Falls Dam in 1950, to regulate the flow of the Dead River into the Kennebec River. At the time, the river drive was still a primary means of delivering timber to the pulp mills downstream.

Geographic entities mentioned:
surface_form: dead river
instance_of: Watercourse
countries: United States
coordinates: lat: 45.3333
lon: -69.9697
Although improved highways and the trucking industry have replaced the river drive, water releases continue to serve hydroelectric power-generating plants downstream. Recreation. The majestic Bigelow Mountain Range looks down from Flagstaff Lake's southern shore, making the Dead River region a scenic favorite for outdoor enthusiasts. It is a popular river with whitewater boaters and rafters.

Geographic entities mentioned:
surface_form: dead river
instance_of: Watercourse
countries: United States
coordinates: lat: 45.3333
lon: -69.9697
surface_form: flagstaff lake
instance_of: Lake
countries: United States
coordinates: lat: 42.5825
lon: -119.80027777778
It is a popular river with whitewater boaters and rafters. The whitewater releases are controlled from Flagstaff Lake, which has been dammed and made into a reservoir, and range from 1200 to 7000 ft³/s (35–200 m³/s) and range in difficulty from easy class 2 to class 4+. The length of the run is from the put-in at Spencer Stream to the take-out at West Forks with no easy access by road.

Geographic entities mentioned:
surface_form: flagstaff lake
instance_of: Lake
countries: United States
coordinates: lat: 42.5825
lon: -119.80027777778
History. In 1985, Japan Air Lines Flight 123, a flight from Tokyo International Airport (informally called Haneda Airport) to Osaka International Airport (also known as Itami Airport), crashed into Mount Takamagahara. The accident was the deadliest involving a single aircraft.

Geographic entities mentioned:
surface_form: Mount Takamagahara
instance_of: Mountain
countries: Japan
coordinates: lat: 35.99194444444444
lon: 138.6886111111111
Putre. Putre is a Chilean town and commune, capital of the Parinacota Province in the Arica-Parinacota Region. It is located east of Arica, at an altitude of. The town is backdropped by Taapaca volcanic complex. Putre is on the edge of the Lauca National Park, and is popular with visitors to the National Park wishing to acclimatise to the altitude. There is a historical church in Putre.

Geographic entities mentioned:
surface_form: Taapaca
instance_of: Mountain
countries: Chile
coordinates: lat: -18.11277777777778
lon: -69.5075
Kidbrooke. Kidbrooke is an area of south-east London, England, in the Royal Borough of Greenwich south-east of Charing Cross and north west of Eltham. The district takes its name from the Kyd Brook, a watercourse which runs from Orpington to Lewisham, by which point it is part of the River Quaggy. It is a tributary to the River Ravensbourne. History.

Geographic entities mentioned:
surface_form: River Ravensbourne
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 51.482
lon: -0.017061111111111
Angami Naga Sign Language. Naga Hills Sign Language was a village sign language of Nagaland. Early in the 20th century, a high incidence of deafness was observed among communities of the Naga hills. A sign language was used by both deaf and hearing members of the community.

Geographic entities mentioned:
surface_form: Naga hills
instance_of: Mountain
countries: Myanmar
India
coordinates: lat: 26
lon: 95
The Poison Canyon Formation underlies the Cuchara Formation in the northern part of the Raton Basin. The formation derived its sediments from the San Luis uplift to the southwest and the Wet Mountains uplift to the north and northwest. Its age ranges from late Cretaceous (where the formation partially replaces the Raton Formation) to Paleocene. Fossils.

Geographic entities mentioned:
surface_form: San Luis
instance_of: Valley
countries: United States
coordinates: lat: 37.2
lon: -105.42
Less commonly observed mammals include porcupine, skunks, foxes and raccoons. Among the many types of avian species in the mountain, birders may view blue jays, cardinals, wood thrush, veery, and ruffed grouse. Reptiles on the mountain include brown snakes and garter snakes, while numerous types of amphibians, molluscs, and insects also occupy the space. Flora.

Geographic entities mentioned:
surface_form: blue
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.1
lon: -119.283
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Mont Bellevue. Mont Bellevue () is a peak standing, situated in Mont-Bellevue Park located in the borough of Mont-Bellevue in Sherbrooke, Quebec. The park also covers Mont Bellevue's parent peak, Mont John-S.-Bourque (elevation:), as well as of land, of trails, and several different types of ecosystems. Claiming 20% of the total park land, it is the largest park in Sherbrooke. Etymology.

Geographic entities mentioned:
surface_form: mont bellevue
instance_of: Mountain
countries: Canada
coordinates: lat: 45.3803
lon: -71.9142
The Université de Sherbrooke, built in 1954, originally used the land for sports, recreation, education, and research. In 1959, the City of Sherbrooke constructed the first ski lift on the mountain, signaling the beginning of the development of Mont Bellevue for public recreational purposes.

Geographic entities mentioned:
surface_form: mont bellevue
instance_of: Mountain
countries: Canada
coordinates: lat: 45.3803
lon: -71.9142
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
In 1976, the City of Sherbrooke undertook park management and maintenance. To this day, the City of Sherbrooke continues to improve the park with consideration for the environment through the &quot;Regroupement du Mont Bellevue&quot; organization. In August 2013, Mont Bellevue was one of the venues for the Canada Games.

Geographic entities mentioned:
surface_form: mont bellevue
instance_of: Mountain
countries: Canada
coordinates: lat: 45.3803
lon: -71.9142
surface_form: mont bellevue
instance_of: Mountain
countries: Canada
coordinates: lat: 45.3803
lon: -71.9142
In August 2013, Mont Bellevue was one of the venues for the Canada Games. In preparation for the event, the &quot;Club de vélo de montagne de Sherbrooke&quot; was granted CA $300,000 for the improvement of the park's mountain bike course. Recreation.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The black slug also has few natural predators in North America, meaning it is a threat to the stability of the ecosystems on the mountain. There is concern that the molluscs might spread to other parts of town via accidental transportation by automobiles that stay for long periods of time in the Mont Bellevue or university parking areas. Eradication efforts.

Geographic entities mentioned:
surface_form: mont bellevue
instance_of: Mountain
countries: Canada
coordinates: lat: 45.3803
lon: -71.9142
Reptiles on the mountain include brown snakes and garter snakes, while numerous types of amphibians, molluscs, and insects also occupy the space. Flora. A variety of wildflowers, ferns, trees, edible plants, and fungus inhabit the mountain. Invasive species. Buckthorn, honeysuckle, and Japanese knotweed are among the invasive plants on the mountain. Black slug.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Flora. A variety of wildflowers, ferns, trees, edible plants, and fungus inhabit the mountain. Invasive species. Buckthorn, honeysuckle, and Japanese knotweed are among the invasive plants on the mountain. Black slug. The black slug (,) is an invasive pest native to Europe that was transported to the area during the construction of the Université de Sherbrooke in the 1950s.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
From there, they took to the Mont Bellevue Park, where the soil humidity is conducive to their locomotion, and where their massive size and lack of shell means they easily outcompete native species. The black slug also has few natural predators in North America, meaning it is a threat to the stability of the ecosystems on the mountain.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The area offers various recreational activities such as birdwatching, boating, and hiking. The striking backdrop of the Virunga Mountains, which include Muhabura, Mgahinga, and Sabinyo, further contributes to the aesthetic appeal of the region. Lake Mulehe often forms part of tours exploring the neighboring Bwindi Impenetrable National Park, which is renowned for its mountain gorilla population.

Geographic entities mentioned:
surface_form: Muhabura
instance_of: Mountain
countries: Rwanda
coordinates: lat: -1.3833333333333
lon: 29.666666666667
surface_form: Sabinyo
instance_of: Mountain
countries: Rwanda
Uganda
Democratic Republic of the Congo
coordinates: lat: -1.4
lon: 29.6
Lake Mulehe. Lake Mulehe is a crater lake situated in the Kisoro District of southwestern Uganda, close to the border with Rwanda. This lake is a part of the Albertine Rift, which is well known for its biological diversity and visually striking landscapes. Geography. Lake Mulehe is located around 1°13'05.0&quot;S 29°43'21.9&quot;E and an elevation of roughly 1,800 meters above sea level.

Geographic entities mentioned:
surface_form: lake mulehe
instance_of: Lake
countries: Uganda
coordinates: lat: -1.2180555555556
lon: 29.721388888889
Geography. Lake Mulehe is located around 1°13'05.0&quot;S 29°43'21.9&quot;E and an elevation of roughly 1,800 meters above sea level. Surrounded by verdant vegetation and terraced hills characteristic of the area's volcanic topography, it is relatively small, spanning approximately 4.11 square kilometers. Biodiversity.

Geographic entities mentioned:
surface_form: lake mulehe
instance_of: Lake
countries: Uganda
coordinates: lat: -1.2180555555556
lon: 29.721388888889
Cultural significance. The local communities surrounding Lake Mulehe possess a diverse cultural heritage, characterized by traditional practices and lifestyles that attract cultural tourism. Tourists often engage with these communities to gain insight into their customs, crafts, and way of life.

Geographic entities mentioned:
surface_form: lake mulehe
instance_of: Lake
countries: Uganda
coordinates: lat: -1.2180555555556
lon: 29.721388888889
Conservation efforts. As part of the Albertine Rift, various conservation efforts are in place to maintain the natural beauty and biodiversity of Lake Mulehe and its surrounding areas. These initiatives aim to promote sustainable tourism and protect the environment from the potential impacts of human activities.

Geographic entities mentioned:
surface_form: lake mulehe
instance_of: Lake
countries: Uganda
coordinates: lat: -1.2180555555556
lon: 29.721388888889
Phunchog Rai. Phunchog Rai (born 19 February 1944; also spelled as 'Phuntsok Rai<nowiki/>') is a politician from Himachal Pradesh, India, and a member of the Indian National Congress Party. Personal life and education. Rai hails from village Lari in the Spiti valley. He matriculated from the Government High School in Manali in 1965, and did graduation from Punjab University at Chandigarh.

Geographic entities mentioned:
surface_form: Spiti valley
instance_of: Valley
countries: India
Qing dynasty
coordinates: lat: 32.246944444444445
lon: 78.05222222222223
Barrett Creek (British Columbia). Barrett Creek is a creek in the Selkirk Mountains in the West Kootenay region of the Regional District of Central Kootenay in British Columbia, Canada. The creek flows east from Barrett Lake to the Salmo River in the community of Porto Rico a few kilometres north of Ymir.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: barrett creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.33318
lon: -117.23551
Barrett Creek (British Columbia). Barrett Creek is a creek in the Selkirk Mountains in the West Kootenay region of the Regional District of Central Kootenay in British Columbia, Canada. The creek flows east from Barrett Lake to the Salmo River in the community of Porto Rico a few kilometres north of Ymir.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: barrett creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.33318
lon: -117.23551
surface_form: kootenay
instance_of: Lake
countries: Canada
coordinates: lat: 49.3
lon: -116.75
surface_form: kootenay
instance_of: Lake
countries: Canada
coordinates: lat: 49.3
lon: -116.75
Barrett Creek is a creek in the Selkirk Mountains in the West Kootenay region of the Regional District of Central Kootenay in British Columbia, Canada. The creek flows east from Barrett Lake to the Salmo River in the community of Porto Rico a few kilometres north of Ymir. Porto Rico was the site of mines staked in 1896, and some early maps may refer to Barrett creek as Porto Rico creek.

Geographic entities mentioned:
surface_form: barrett creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.33318
lon: -117.23551
Barrett Creek is a creek in the Selkirk Mountains in the West Kootenay region of the Regional District of Central Kootenay in British Columbia, Canada. The creek flows east from Barrett Lake to the Salmo River in the community of Porto Rico a few kilometres north of Ymir. Porto Rico was the site of mines staked in 1896, and some early maps may refer to Barrett creek as Porto Rico creek.

Geographic entities mentioned:
surface_form: barrett lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.3423
lon: -117.351
On the chapel's lunette, the Virgin Platytera enthroned, with angels seated on either side. Although the frescoes do not distinguish themselves with any innovations in fresco technique, they nonetheless remain prototypes of the 16th-century frescoes found in the Mount Athos. During the 17th century, frescoes became more and more popular in style and technique. The bath house.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
Großer Müllroser See. The Großer Müllroser See is a lake in Brandenburg, Germany. It is located in the district Oder-Spree between the town Müllrose in the north and the municipality Mixdorf in the south. The lake covers an area of 1,32 km². At an elevation of 41,6 m, its depth is maximal 8 m.

Geographic entities mentioned:
surface_form: großer müllroser see
instance_of: Lake
countries: Germany
coordinates: lat: 52.230833333333
lon: 14.418333333333
Petersburg Mountain. Petersburg Mountain is a mountain located in the Catskill Mountains of New York southeast of Cobleskill. Warnerville Hill is located northwest, and Donats Mountain is located northwest of Petersburg Mountain. In 1940, a steel fire lookout tower was built on the mountain.

Geographic entities mentioned:
surface_form: Warnerville Hill
instance_of: Mountain
countries: United States
coordinates: lat: 42.644166666667
lon: -74.474722222222
surface_form: Donats Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.66146
lon: -74.48375
surface_form: petersburg mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.63313
lon: -74.44903
Petersburg Mountain. Petersburg Mountain is a mountain located in the Catskill Mountains of New York southeast of Cobleskill. Warnerville Hill is located northwest, and Donats Mountain is located northwest of Petersburg Mountain. In 1940, a steel fire lookout tower was built on the mountain.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: petersburg mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.63313
lon: -74.44903
Petersburg Mountain. Petersburg Mountain is a mountain located in the Catskill Mountains of New York southeast of Cobleskill. Warnerville Hill is located northwest, and Donats Mountain is located northwest of Petersburg Mountain. In 1940, a steel fire lookout tower was built on the mountain.

Geographic entities mentioned:
surface_form: petersburg mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.63313
lon: -74.44903
Tracking generally west, the system steadily organized into a tropical storm, passing Vietnam to the south, before striking Thailand along the Malay Peninsula on November 15. Once over the Bay of Bengal, Forrest turned northward on November 17 and significantly intensified.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Conical Rock. vq1j519mevf1ufrtus4e9b3vymfh" xml:space="preserve">Conical Rock () is a rock lying in the eastern part of Morton Strait, south of the southwest tip of Livingston Island, in the South Shetland Islands. It was named by Discovery Investigations personnel on the &quot;Discovery II&quot;, who charted the area in 1930–31.

Geographic entities mentioned:
surface_form: Morton Strait
instance_of: Body of water
coordinates: lat: -62.6972
lon: -61.22
Amba Alagi. Imba Alaje is a mountain, or an amba, in northern Ethiopia. Located in the Debubawi Zone of the Tigray Region, Imba Alaje dominates the roadway that runs past it from the city of Mek'ele south to Maychew. Because of its strategic location, Emba Alaje has been the site of several battles.

Geographic entities mentioned:
surface_form: amba alagi
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 12.983333333333
lon: 39.55
On the northern flank at Addi Gura'i, the Mercy water bottling plant is located. Alagi Pass. Just three kilometers to the southeast of the top of Amba Alagi is the Alagi Pass. Here, the Ethiopian Highway 2 crosses the mountain ridge at an elevation of 3,090 meter above sea level. To the south, the road starts climbing from Ambalage at 2,450 meters. History.

Geographic entities mentioned:
surface_form: amba alagi
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 12.983333333333
lon: 39.55
The defenders, Italian troops under command of the Viceroy, the Duke of Aosta, thought themselves to be impregnable. The initial attacks on the approaches to Amba Alagi by British troops under Major-General Mayne from the north, commenced on May 4 with a pincer from the eastern and western sides. There was hard fighting in the jagged mountainous terrain.

Geographic entities mentioned:
surface_form: amba alagi
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 12.983333333333
lon: 39.55
A final assault was planned for the next day but a lucky strike by an artillery shell hit an Italian fuel dump, sending a stream of oil into their last remaining drinking water and forcing the garrison's surrender. The film &quot;La Pattuglia dell'Amba Alagi&quot;, shot in 1953 by Flavio Calzavara, glorifies the Italian defense against the British. Third Battle of Amba Alagi.

Geographic entities mentioned:
surface_form: amba alagi
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 12.983333333333
lon: 39.55
Signs on westbound I-70 prior to the MD 68 interchange remind motorists they should remain on I-70 to access I-68. I-70 continues east through Hagerstown Valley, where the highway crosses over Little Conococheague, Meadow Brook, and Conococheague creeks before reaching a diamond interchange with MD 63 (Greencastle Pike) south of Huyett.

Geographic entities mentioned:
surface_form: Hagerstown Valley
instance_of: Valley
countries: United States
coordinates: lat: 39.4397
lon: -77.7547
The westbound rest area is where the DC snipers, John Allen Muhammad and Lee Boyd Malvo, were apprehended by police in October 2002. I-70's eastbound climbing lane disappears and the Interstate has a westbound climbing lane from the top of the mountain southeast to a diamond interchange with MD 17 (Myersville Middletown Road) south of Myersville, where the freeway enters Middletown Valley.

Geographic entities mentioned:
surface_form: Middletown Valley
instance_of: Valley
countries: United States
coordinates: lat: 39.43
lon: -77.53
Within the valley, the Interstate crosses Catoctin and Little Catoctin creeks. I-70 gains an eastbound climbing lane as it climbs Braddock Mountain, on top of which the freeway passes under a concrete arch bridge carrying Ridge Road. Westbound I-70 has a climbing lane as the highway descends Braddock Mountain and has partial interchanges with US 40 (National Pike) and US 40 Alt.

Geographic entities mentioned:
surface_form: Braddock Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.6478
lon: -77.4664
According to the press conference, Daniel garnered a massive 1.2 million out of 1.67 million votes (or about 68%) by the audience to win the finals (the voting time window was approximately 24 hours after the final show). The final show was on September 23, 2005, and the results show was on September 24, 2005, and held in Genting Highlands's Arena of Stars.

Geographic entities mentioned:
surface_form: Genting Highlands
instance_of: Mountain
countries: Malaysia
coordinates: lat: 3.42368
lon: 101.79335
Biography. Born in Charleston, March 12, 1788; Hayne was the son of William Hayne, a lowland planter, and his wife Elizabeth Peronneau. Hayne was of English and French Huguenot descent. He pursued classical studies, engaged in business, and served in the War of 1812 as a first lieutenant at Sackets Harbor on Lake Ontario, major of cavalry on the St. Lawrence, and inspector general in 1814.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
The Styx River is a river in the western portion of Central Queensland, Australia. The headwaters of the river rise on the Gilberton Plateau in the Einasleigh Uplands, part of the Atherton Tableland in the Great Dividing Range. The river flows generally south by southwest through the Blackbraes National Park before reaching its confluence with the Gilbert River below Conical Hill.

Geographic entities mentioned:
surface_form: Atherton Tableland
instance_of: Plateau
countries: Australia
coordinates: lat: -17.16666667
lon: 145.53333333
Geography. According to the U.S. Census Bureau, the county has a total area of, of which is land and (0.8%) is water. Chemung County is in the southwestern part of New York State, along the Pennsylvania border, in a part of New York called the Southern Tier and is also part of the Finger Lakes Region.

Geographic entities mentioned:
surface_form: Finger Lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 42.666666666667
lon: -76.833333333333
Choctella. &quot;Choctella&quot; is a genus of millipedes in the monotypic family Choctellidae. Its two species are native to the south-eastern United States. &quot;C. cumminsi&quot; Chamberlin, 1918, occurs on the Cumberland Plateau from central Tennessee to northern Alabama and &quot;C. hubrichti&quot; Hoffman, 1965, occurs in central Alabama.

Geographic entities mentioned:
surface_form: Cumberland Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 36
lon: -85
Deserts cover about 20% of the total land area. The largest is the Sahara, which covers nearly one-third of Africa. The elevation of the land surface of the Earth varies from the low point of −418 m (−1,371 ft) at the Dead Sea, to a 2005-estimated maximum altitude of 8,848 m (29,028 ft) at the top of Mount Everest. The mean height of land above sea level is 686 m (2,250 ft). Mars.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
Early town records show the name as &quot;Chabunagungamaug Pond&quot;, which was also the name of the local Nipmuc town (recorded in 1668 and 1674 with somewhat different spellings). This has been translated as &quot;boundary fishing place&quot;, but something close to &quot;fishing place at the boundary&quot; or &quot;that which is a divided island lake&quot; may be more accurate.

Geographic entities mentioned:
surface_form: island lake
instance_of: Lake
countries: United States
coordinates: lat: 44.38027778
lon: -96.00888889
surface_form: island lake
instance_of: Lake
countries: United States
coordinates: lat: 40.615
lon: -115.381
surface_form: island lake
instance_of: Lake
countries: United States
coordinates: lat: 46.73416667
lon: -93.19
surface_form: island lake
instance_of: Lake
countries: United States
coordinates: lat: 42.5181
lon: -122.238
surface_form: island lake
instance_of: Lake
countries: United States
coordinates: lat: 47.78027778
lon: -95.02888889
surface_form: island lake
instance_of: Lake
countries: United States
coordinates: lat: 47.6819019
lon: -122.6602552
Lake Chaubunagungamaug. Lake Chaubunagungamaug, also known as Webster Lake, is a lake in the town of Webster, Massachusetts. It is located near the state’s border with Connecticut and has a surface area of.

Geographic entities mentioned:
surface_form: webster
instance_of: Lake
countries: United States
coordinates: lat: 42.0425
lon: -71.843333333333
surface_form: chaubunagungamaug
instance_of: Lake
countries: United States
coordinates: lat: 42.0425
lon: -71.843333333333
surface_form: lake chaubunagungamaug
instance_of: Lake
countries: United States
coordinates: lat: 42.0425
lon: -71.843333333333
surface_form: webster
instance_of: Lake
countries: United States
coordinates: lat: 42.0425
lon: -71.843333333333
surface_form: webster lake
instance_of: Lake
countries: United States
coordinates: lat: 41.907018
lon: -86.301546
surface_form: webster lake
instance_of: Lake
countries: United States
coordinates: lat: 41.3247
lon: -85.6819
surface_form: webster lake
instance_of: Lake
countries: United States
coordinates: lat: 43.4694
lon: -71.6864
A more fitting translation is &quot;lake divided by islands&quot;, according to anthropologist Ives Goddard. The most memorable translation, however, is supposedly: &quot;You fish on your side; we fish on our side; nobody fish in the middle.&quot;
Today, &quot;Webster Lake&quot; may be the name most used, but some (including many residents of Webster) take pride in reeling off the longer versions.

Geographic entities mentioned:
surface_form: webster
instance_of: Lake
countries: United States
coordinates: lat: 42.0425
lon: -71.843333333333
surface_form: webster
instance_of: Lake
countries: United States
coordinates: lat: 42.0425
lon: -71.843333333333
surface_form: webster lake
instance_of: Lake
countries: United States
coordinates: lat: 41.907018
lon: -86.301546
surface_form: webster lake
instance_of: Lake
countries: United States
coordinates: lat: 41.3247
lon: -85.6819
surface_form: webster lake
instance_of: Lake
countries: United States
coordinates: lat: 43.4694
lon: -71.6864
Lake Chaubunagungamaug. Lake Chaubunagungamaug, also known as Webster Lake, is a lake in the town of Webster, Massachusetts. It is located near the state’s border with Connecticut and has a surface area of.

Geographic entities mentioned:
surface_form: chaubunagungamaug
instance_of: Lake
countries: United States
coordinates: lat: 42.0425
lon: -71.843333333333
surface_form: lake chaubunagungamaug
instance_of: Lake
countries: United States
coordinates: lat: 42.0425
lon: -71.843333333333
Many area residents and the official website of the town of Webster consider the longer version correct. The humorous translation is: &quot;You fish on your side, I'll fish on my side, and no one shall fish in the middle&quot;. Its humorous translation was perhaps invented by Laurence J. Daly, editor of &quot;The Webster Times&quot;.

Geographic entities mentioned:
surface_form: webster
instance_of: Lake
countries: United States
coordinates: lat: 42.0425
lon: -71.843333333333
In 1902 he wrote &quot;Across the Sub-Arctics of Canada: A Journey of 3,200 Miles by Canoe and Snow-shoe Through the Barren Lands&quot;, based on his expedition to map the land between Great Slave Lake and Hudson's Bay. He led a team of just 9 men. In 1905 Tyrrell conducted the first survey of the mouth of the Churchill River.

Geographic entities mentioned:
surface_form: Great Slave Lake
instance_of: Lake
countries: Canada
coordinates: lat: 61.666666666667
lon: -114
Atwell Peak. Atwell Peak is a dramatic pyramid-shaped volcanic peak located at the southern edge of Mount Garibaldi, British Columbia, Canada. Atwell Peak was the source of many pyroclastic flows during Garibaldi's development. Frequent landslides on its west face drops steeply into the Cheekye River.

Geographic entities mentioned:
surface_form: Mount Garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: atwell peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.8411
lon: -123.009
The two most visible routes are the north and south ridges. Atwell Peak is part of the Garibaldi Massif which is an eroded stratovolcano formed during the last ice age. The volcano is also part of the Garibaldi Volcanic Belt which is a segment of the Canadian Cascade Arc, but it is not within the geographic boundary of the Cascade Range. It is located in the Garibaldi Ranges of the Pacific Ranges.

Geographic entities mentioned:
surface_form: Garibaldi Volcanic Belt
instance_of: Mountain
countries: Canada
coordinates: lat: 51.5283
lon: -126.113
Atwell Peak. Atwell Peak is a dramatic pyramid-shaped volcanic peak located at the southern edge of Mount Garibaldi, British Columbia, Canada. Atwell Peak was the source of many pyroclastic flows during Garibaldi's development. Frequent landslides on its west face drops steeply into the Cheekye River.

Geographic entities mentioned:
surface_form: atwell peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.8411
lon: -123.009
Atwell Peak was the source of many pyroclastic flows during Garibaldi's development. Frequent landslides on its west face drops steeply into the Cheekye River. Atwell Peak is often mistakenly called Mount Garibaldi when viewed from Squamish, since the main peak is hidden. The peak is usually climbed during winter or early spring when the rock is frozen because it is very loose and rotten.

Geographic entities mentioned:
surface_form: atwell peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.8411
lon: -123.009
surface_form: mount garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
Atwell Peak is often mistakenly called Mount Garibaldi when viewed from Squamish, since the main peak is hidden. The peak is usually climbed during winter or early spring when the rock is frozen because it is very loose and rotten. Atwell Peak contains three ridges, the north, east, and south. The two most visible routes are the north and south ridges.

Geographic entities mentioned:
surface_form: atwell peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.8411
lon: -123.009
The two most visible routes are the north and south ridges. Atwell Peak is part of the Garibaldi Massif which is an eroded stratovolcano formed during the last ice age. The volcano is also part of the Garibaldi Volcanic Belt which is a segment of the Canadian Cascade Arc, but it is not within the geographic boundary of the Cascade Range. It is located in the Garibaldi Ranges of the Pacific Ranges.

Geographic entities mentioned:
surface_form: atwell peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.8411
lon: -123.009
It is located in the Garibaldi Ranges of the Pacific Ranges. Ridges. Atwell Peak consists of three ridges, the north, east, and south. The east ridge connects with the north ridge about 100 horizontal metres north of the summit. All ridges, with the possible exception of the upper east ridge, are sharp and heavily corniced in winter and spring. The north ridge is the shortest climbing route.

Geographic entities mentioned:
surface_form: atwell peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.8411
lon: -123.009
The northeast face is the shortest of the peak's faces but has many bergschrunds. Glaciers and icefield. To the east of Atwell Peak lies the Garibaldi Névé ice field, which is a popular objective with the ski touring crowd. Two pocket glaciers lie right below the east side of the peak, the Diamond Glacier to the southeast and the upper Bishop Glacier to the northeast.

Geographic entities mentioned:
surface_form: atwell peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.8411
lon: -123.009