Sarmila/GeoWiki-Features huggingface dataset:
There have been upgrades to the stations from 2015 to 2017, leading to a capacity increase from 450 to 800 parking spaces. In 2023, Kathmandu Metropolitan City enforced all long-distance busses from Kathmandu to destinations outside the Kathmandu Valley to be operated from Gongabu Bus Park. For this, 56 new ticket stalls were added to the bus park. Controversies.

Geographic entities mentioned:
surface_form: Kathmandu Valley
instance_of: Valley
countries: Nepal
coordinates: lat: 27.703944444444
lon: 85.308583333333
The lake is fed by bayous in the Barataria Basin including Grand Bayou and Bayou Chevreuil. Its waters flow southeast into Bayou des Allemands, then into Lake Salvador and eventually the Gulf of Mexico. Lac des Allemands is surrounded by cypress swamp and the bayous and canals offer a habitat for catfish, bass, bream, crappie and panfish.

Geographic entities mentioned:
surface_form: Lake Salvador
instance_of: Lake
countries: United States
coordinates: lat: 29.7238
lon: -90.2462
surface_form: lake salvador
instance_of: Lake
countries: United States
coordinates: lat: 29.7238
lon: -90.2462
St. Charles Parish and St. John the Baptist Parish are part of a region called the German Coast. Lac des Allemands is a shallow lake, with a maximum depth of and an average depth of about. It is mostly located at sea level and measures about long and wide. The lake is fed by bayous in the Barataria Basin including Grand Bayou and Bayou Chevreuil.

Geographic entities mentioned:
surface_form: shallow lake
instance_of: Lake
countries: United States
coordinates: lat: 43.49
lon: -74.444
Lac des Allemands. Lac des Allemands is a lake located about southwest of New Orleans, Louisiana, in Lafourche, St. Charles, and St. John the Baptist Parishes. The lake name is French for &quot;Lake of the Germans&quot;, referring to the early settlers who inhabited that part of Louisiana. St. Charles Parish and St. John the Baptist Parish are part of a region called the German Coast.

Geographic entities mentioned:
surface_form: lac des allemands
instance_of: Lake
countries: United States
coordinates: lat: 29.923611
lon: -90.577778
Cliftonville Golf Club. Cliftonville Golf Club is located on Westland Road in north Belfast. It consists of a 9-hole course with an eighteen-hole par of 70. The club was founded in 1911. The course lies underneath the shadow of Cavehill. The first hole has been nominated twice in BBC NI's toughest Par 3.

Geographic entities mentioned:
surface_form: Cavehill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.647
lon: -5.951
Tsagkarada. Tsagkarada () is a village and a community in the municipal unit of Mouresi in the eastern part of Magnesia, Greece. It was the seat of the former municipality Mouresi. It is situated at 408 m elevation, on the eastern slope of the forested Pelion mountains. The community includes the village Mylopotamos.

Geographic entities mentioned:
surface_form: Pelion
instance_of: Mountain
countries: Greece
coordinates: lat: 39.433333333333
lon: 23.05
The valley is long, oriented east-north-east to west-south-west. From the north it is bounded by a low-lying (300–400m) ridge − part of the Kangaamiut dike swarm − separating it from large glacial lakes of Aajuitsup Tasia and Sanningasoq. On the southern side the boundary is formed by an exposed, barren, and flattened ridge of Akuliarusiarsuk.

Geographic entities mentioned:
surface_form: Aajuitsup Tasia
instance_of: Lake
countries: Greenland
coordinates: lat: 67.0833
lon: -50.3833
surface_form: Sanningasoq
instance_of: Lake
countries: Greenland
coordinates: lat: 67.0792
lon: -50.6
Summit Lake (Kabinakagami River). Summit Lake is a lake in the James Bay drainage basin in the Unorganized North Part of Algoma District in northeastern Ontario, Canada. It is the source of the Kabinakagami River, which flows via the Kenogami River and Albany River to James Bay. The lake is about long and wide, lies at an elevation of, and there are no significant inflows.

Geographic entities mentioned:
surface_form: summit lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.1081
lon: -84.6292
surface_form: summit lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.0422
lon: -93.7006
surface_form: summit lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.2736
lon: -79.7622
surface_form: summit lake (kabinakagami river)
instance_of: Lake
countries: Canada
coordinates: lat: 48.4753
lon: -84.8669
surface_form: summit lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.0464
lon: -76.8425
surface_form: summit lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.15006
lon: -104.73377
surface_form: summit lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.2636
lon: -84.5308
surface_form: summit lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.49
lon: -84.3683
surface_form: summit lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.4256
lon: -87.7375
surface_form: summit lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.25
lon: -124.683
surface_form: summit lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.28861111111111
lon: -122.65972222222223
surface_form: summit lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.4831
lon: -92.6544
surface_form: summit lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.42638888888889
lon: -82.72083333333333
surface_form: summit lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.0072
lon: -114.026
Summit Lake (Kabinakagami River). Summit Lake is a lake in the James Bay drainage basin in the Unorganized North Part of Algoma District in northeastern Ontario, Canada. It is the source of the Kabinakagami River, which flows via the Kenogami River and Albany River to James Bay. The lake is about long and wide, lies at an elevation of, and there are no significant inflows.

Geographic entities mentioned:
surface_form: summit lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.1081
lon: -84.6292
surface_form: summit lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.0422
lon: -93.7006
surface_form: summit lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.2736
lon: -79.7622
surface_form: summit lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.4753
lon: -84.8669
surface_form: summit lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.0464
lon: -76.8425
surface_form: summit lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.15006
lon: -104.73377
surface_form: summit lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.2636
lon: -84.5308
surface_form: summit lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.49
lon: -84.3683
surface_form: summit lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.4256
lon: -87.7375
surface_form: summit lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.25
lon: -124.683
surface_form: summit lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.28861111111111
lon: -122.65972222222223
surface_form: summit lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.4831
lon: -92.6544
surface_form: summit lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.42638888888889
lon: -82.72083333333333
surface_form: summit lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.0072
lon: -114.026
The lake is about long and wide, lies at an elevation of, and there are no significant inflows. The Canadian Pacific Railway transcontinental main line (used at this point by the Via Rail Sudbury – White River train service) runs along the entire south shore; the lake lies between the railway points of Amyot to the west and Girdwood to the east.

Geographic entities mentioned:
surface_form: white river
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.93055556
lon: -74.10138889
surface_form: white river
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.99639
lon: -71.46167
The Canadian Pacific Railway transcontinental main line (used at this point by the Via Rail Sudbury – White River train service) runs along the entire south shore; the lake lies between the railway points of Amyot to the west and Girdwood to the east. As well, it is about southeast of the community of White River and northeast of Dubreuilville.

Geographic entities mentioned:
surface_form: white river
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.93055556
lon: -74.10138889
surface_form: white river
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.99639
lon: -71.46167
Rugby career. Although born in Scotland, Ramsey moved to the Rhondda Valley in Wales where he became a collier during the industrial growth of the area in the late Victorian period. Ramsey joined local team Treorchy in the early 1890s and in the 1892/93 season was made team captain, holding the captaincy the next season too.

Geographic entities mentioned:
surface_form: Rhondda Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.615938888889
lon: -3.4175222222222
Lake Puhau. Lake Puhau is a lake in the Northland Region of New Zealand.

Geographic entities mentioned:
surface_form: lake puhau
instance_of: Lake
countries: New Zealand
coordinates: lat: -35.477292
lon: 173.365634
His first reaction to the score being the music he wrote should use instruments common to the region—violin, guitar, fiddle, banjo, mandolin. However, he did not want the music to be a pastiche of the Ozark style and from the offset he wanted the score to be played in a different way.

Geographic entities mentioned:
surface_form: Ozark
instance_of: Plateau
countries: United States
coordinates: lat: 37.1822
lon: -92.5159
It flows west-southwest for a short distance before turning southwest for several tenths of a mile, receiving an unnamed tributary from the right and entering Harford Township. Here, the creek flows south-southwest for more than a mile, receiving another unnamed tributary from the right before turning south and passing through a wetland and Beaver Meadow Pond.

Geographic entities mentioned:
surface_form: Beaver Meadow Pond
instance_of: Lake
countries: United States
coordinates: lat: 42.0306908
lon: -75.2049686
Kvernaland. The larger Kvernaland area is an amalgamation of villages in Rogaland county, Norway. The village is located along the north end of the lake Frøylandsvatnet. The village is located in both the municipalities of Klepp and Time (and a very small part extends into Sandnes municipality as well).

Geographic entities mentioned:
surface_form: Frøylandsvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 58.749722222222
lon: 5.6758333333333
Background. As assembled by Bugliosi, the evidence of the vision indicated that Manson had been predicting racial conflict for some time before he used the term &quot;Helter Skelter&quot;. According to Paul Watkins, he first used the term at a gathering of the Family on New Year's Eve 1968 at Myers Ranch, near California's Death Valley.

Geographic entities mentioned:
surface_form: Death Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.45693888888889
lon: -116.86528055555556
Sevier, Snake Valley, and Emery gray also occur in painted varieties. A unique and beautiful painted bowl form, Ivie Creek black-on-white, is found along either side of the southern Wasatch Plateau.

Geographic entities mentioned:
surface_form: Wasatch Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 39.311666666667
lon: -111.33694444444
Poison Pond. Poison Pond is a small freshwater lake in the Temagami region of Northeastern Ontario, Canada, located near Pecours Bay of Snake Island Lake. Poison Pond is in the White Bear Forest and is typically approached from the Peregrine Trail, which adjoins the Red Fox Trail to the west. Its eastern portion adjoins the Otter Trail.

Geographic entities mentioned:
surface_form: Snake Island Lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.0642
lon: -79.7617
surface_form: island lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.8464
lon: -113.532
surface_form: island lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
surface_form: island lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.9819
lon: -107.7276
surface_form: poison pond
instance_of: Lake
countries: Canada
coordinates: lat: 47.0543
lon: -79.7445
Its eastern portion adjoins the Otter Trail. Poison Pond is the location of a few locally rare plants, including wild mint, striped maple, spikenard and water parsnip, which are not typically found in the White Bear Forest. It is also home to beavers and moose. The lake gets its name from the abundant poison ivy found along its shoreline.

Geographic entities mentioned:
surface_form: moose
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.91444444444444
lon: -118.80638888888889
Poison Pond. Poison Pond is a small freshwater lake in the Temagami region of Northeastern Ontario, Canada, located near Pecours Bay of Snake Island Lake. Poison Pond is in the White Bear Forest and is typically approached from the Peregrine Trail, which adjoins the Red Fox Trail to the west. Its eastern portion adjoins the Otter Trail.

Geographic entities mentioned:
surface_form: bear
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.2833
lon: -126.967
surface_form: poison pond
instance_of: Lake
countries: Canada
coordinates: lat: 47.0543
lon: -79.7445
Poison Pond is in the White Bear Forest and is typically approached from the Peregrine Trail, which adjoins the Red Fox Trail to the west. Its eastern portion adjoins the Otter Trail. Poison Pond is the location of a few locally rare plants, including wild mint, striped maple, spikenard and water parsnip, which are not typically found in the White Bear Forest. It is also home to beavers and moose.

Geographic entities mentioned:
surface_form: bear
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.2833
lon: -126.967
surface_form: poison pond
instance_of: Lake
countries: Canada
coordinates: lat: 47.0543
lon: -79.7445
Poison Pond. Poison Pond is a small freshwater lake in the Temagami region of Northeastern Ontario, Canada, located near Pecours Bay of Snake Island Lake. Poison Pond is in the White Bear Forest and is typically approached from the Peregrine Trail, which adjoins the Red Fox Trail to the west. Its eastern portion adjoins the Otter Trail.

Geographic entities mentioned:
surface_form: poison pond
instance_of: Lake
countries: Canada
coordinates: lat: 47.0543
lon: -79.7445
Akzhar. Akzhar (;) is a salt lake group in the Zhambyl and Turkistan regions, Kazakhstan. The lakes lie northwest of Saudakent town and northeast of Kumkent. The Akzhar lake zone includes a Important Bird Area. Geography. The cluster of lakes is located in an arid, sandy sector of the Muyunkum Desert to the north of the northern slopes of the Karatau Mountains.

Geographic entities mentioned:
surface_form: zhambyl
instance_of: Mountain
countries: Kazakhstan
coordinates: lat: 44.809444444444445
lon: 73.01972222222223
surface_form: akzhar
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 44
lon: 69.75
The Akzhar lake zone includes a Important Bird Area. Geography. The cluster of lakes is located in an arid, sandy sector of the Muyunkum Desert to the north of the northern slopes of the Karatau Mountains. The border between the Sozak District of Turkestan Region and Sarysu District of Zhambyl Region runs from the SSW to NNE across the lakes.

Geographic entities mentioned:
surface_form: zhambyl
instance_of: Mountain
countries: Kazakhstan
coordinates: lat: 44.809444444444445
lon: 73.01972222222223
Akzhar. Akzhar (;) is a salt lake group in the Zhambyl and Turkistan regions, Kazakhstan. The lakes lie northwest of Saudakent town and northeast of Kumkent. The Akzhar lake zone includes a Important Bird Area. Geography. The cluster of lakes is located in an arid, sandy sector of the Muyunkum Desert to the north of the northern slopes of the Karatau Mountains.

Geographic entities mentioned:
surface_form: akzhar
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 44
lon: 69.75
The lakes are scattered over a large area. They are numerous, but all are small. Akzhar, the largest individual lake, lies in the southwestern end, and lake Zhylkybay (Жылқыбай) close to the eastern edge, north of Igilik village. The Talas river reaches the northern end from the east and sinks in the sands.

Geographic entities mentioned:
surface_form: akzhar
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 44
lon: 69.75
Flora and fauna. Most lakes have bare, barren-looking, shores. Tamarisk and, less frequently, saxaul may be found in some stretches. Festuca and saltwort may grow sparsely in the land areas in between. The Akzhar lakes are an important place for the breeding, migrating and wintering of a number of bird species.

Geographic entities mentioned:
surface_form: akzhar
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 44
lon: 69.75
The Department of Public Lands approved this request in an order that allowed the irrigation district to inundate lakeshores on the lake. The dams on Upper and Lower Snow Lakes as well as neighboring Nada Lake were completed in 1940 and later expanded in 1941 by the United States Bureau of Reclamation authorizing 25 cfs, 1,000 acre-feet per year for irrigation of 7,000 acres of lands.

Geographic entities mentioned:
surface_form: Nada Lake
instance_of: Lake
countries: United States
coordinates: lat: 47.4960919
lon: -120.738793
surface_form: snow lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 47.483116
lon: -120.7586572
Snow Lakes. Snow Lakes are a system of freshwater reservoir lakes made by Upper Snow Lake and Lower Snow Lake, approximately a mile long. They are located on the eastern slope of The Enchantments, in Chelan County, Washington. The Snow Lakes are one of the most heavily used destination in the Forest Service wildernesses in Oregon and Washington.

Geographic entities mentioned:
surface_form: snow lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 47.483116
lon: -120.7586572
They are located on the eastern slope of The Enchantments, in Chelan County, Washington. The Snow Lakes are one of the most heavily used destination in the Forest Service wildernesses in Oregon and Washington. Self-issued Alpine Lakes Wilderness permits are required for transit within the Snow Lakes area. History.

Geographic entities mentioned:
surface_form: snow lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 47.483116
lon: -120.7586572
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
They are located on the eastern slope of The Enchantments, in Chelan County, Washington. The Snow Lakes are one of the most heavily used destination in the Forest Service wildernesses in Oregon and Washington. Self-issued Alpine Lakes Wilderness permits are required for transit within the Snow Lakes area. History.

Geographic entities mentioned:
surface_form: snow lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 47.483116
lon: -120.7586572
History. Archaeological surveying in the area of the Snow Lakes shows evidence that the occupation of indigenous groups dated to at least 12,000 years before the present era. The lakes are within the traditional territory of the Wenatchi People, one of the Confederated Tribes of the Colville Reservation and within the ceded lands of the Yakama Nation.

Geographic entities mentioned:
surface_form: snow lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 47.483116
lon: -120.7586572
Urban Grassi, a Catholic Priest was the first to use irrigation in the Valley. The Icicle Irrigation District applied in 1930 for the right to appropriate water from the Snow Lakes for seasonal irrigation purposes. The State Supervisor of Hydraulics had issued Permit Number 828 in January 1927 for the appropriation of surrounding lakes.

Geographic entities mentioned:
surface_form: snow lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 47.483116
lon: -120.7586572
The Snow Lakes also have water right certificate for 16,000 acre-feet per year to supplement the water supply for the Leavenworth National Fish Hatchery and holding ponds. The Snow Lakes system is owned and operated by United States Fish and Wildlife Service. In 1939, the Bureau of Reclamation acquired an easement on portions adjacent to Snow and Nada Lakes from the IPID.

Geographic entities mentioned:
surface_form: snow lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 47.483116
lon: -120.7586572
The Snow Lakes system is owned and operated by United States Fish and Wildlife Service. In 1939, the Bureau of Reclamation acquired an easement on portions adjacent to Snow and Nada Lakes from the IPID. That easement was transferred to the U.S.

Geographic entities mentioned:
surface_form: snow lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 47.483116
lon: -120.7586572
This infrastructure allows for controlled releases of stored water to supplement flows into Icicle Creek through its outflowing tributaries and increase the water supply available during low flow periods, which typically occur during the late summer. Between 1994 and 2005, the total average usable storage volume from Snow Lakes is 8,600 acre-feet.

Geographic entities mentioned:
surface_form: snow lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 47.483116
lon: -120.7586572
Between 1994 and 2005, the total average usable storage volume from Snow Lakes is 8,600 acre-feet. Due to the reliability of recharge in the Upper and Lower Snow Lakes basin the storage volume isn't always persistent, however between the Alpine Lakes managed by the IPID the usable storage volume is approximately 20,015 acre-feet.

Geographic entities mentioned:
surface_form: snow lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 47.483116
lon: -120.7586572
The Leavenworth National Fish Hatchery receives Water supply from a combination of Icicle Creek flows and groundwater wells with reservoir storage from Snow Lakes and Nada Lake. The hatchery serves as mitigation for fish losses resulting from the construction of Grand Coulee Dam and the creation of the Columbia Basin Project.

Geographic entities mentioned:
surface_form: snow lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 47.483116
lon: -120.7586572
The year-round water supply to the hatchery ensures current production goals of 1.2 million fish annually. Recreation. Most visitors to Snow Lakes are day hikers although the lakes are provided with campsites. The majority of visitors remain in the Southeast shore where the trail system approaches Upper Snow Lake.

Geographic entities mentioned:
surface_form: snow lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 47.483116
lon: -120.7586572
The trail will lead first to Nada Lake, approximately 5.5 miles from the trailhead. The trail has a second lap towards the Snow Lakes that starts on the Southeast shore of Nada Lake. Lower Snow Lake is 1.75 miles, Lake Viviane is another mile through an unmaintained trail, then Leprechaun Lake a short climb past Lake Viviane.

Geographic entities mentioned:
surface_form: snow lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 47.483116
lon: -120.7586572
Lower Snow Lake is 1.75 miles, Lake Viviane is another mile through an unmaintained trail, then Leprechaun Lake a short climb past Lake Viviane. Further up the trail leads to Sprite Pond and around the east side of Perfection Lake where the trail then becomes Colchuck Lake Trail #1599.1. Self-issued Alpine Lake Wilderness permit is required for transit within the Snow Lakes area.

Geographic entities mentioned:
surface_form: snow lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 47.483116
lon: -120.7586572
Snow Lakes. Snow Lakes are a system of freshwater reservoir lakes made by Upper Snow Lake and Lower Snow Lake, approximately a mile long. They are located on the eastern slope of The Enchantments, in Chelan County, Washington. The Snow Lakes are one of the most heavily used destination in the Forest Service wildernesses in Oregon and Washington.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Background. Aberfan is situated toward the bottom of the western valley slope of the Taff Valley, on the eastern slope of Mynydd Merthyr, approximately south of Merthyr Tydfil. When the Merthyr Vale Colliery was sunk on 23 August 1869 by John Nixon and partners, Aberfan consisted of two cottages and an inn frequented by local farmers and bargemen.

Geographic entities mentioned:
surface_form: Mynydd Merthyr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 51.705
lon: -3.37306
He was awarded the MBE in 1974 for services to sport. In late 1989, Morris and his wife retired to the town of Cessnock in the Hunter Region, north of Sydney. He continued to play tennis into his late seventies and enjoyed watching Test cricket although he refused to watch one-day cricket, introduced after his playing days, due to his preference for tradition.

Geographic entities mentioned:
surface_form: Hunter Region
instance_of: Valley
countries: Australia
coordinates: lat: -32.56
lon: 151.17083333333332
Brandywine Mountain. Brandywine Mountain, is a summit in the Powder Mountain Icefield of the Pacific Ranges of the Coast Mountains of southwestern British Columbia, Canada, about west of the resort town of Whistler. Its name is derived from that of Brandywine Falls, which was the result of a bet over the falls' height (with the wagers being a bottle of wine and a bottle of brandy).

Geographic entities mentioned:
surface_form: powder mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.1472
lon: -123.277
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: brandywine mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.114444444444
lon: -123.22111111111
Brandywine Mountain. Brandywine Mountain, is a summit in the Powder Mountain Icefield of the Pacific Ranges of the Coast Mountains of southwestern British Columbia, Canada, about west of the resort town of Whistler. Its name is derived from that of Brandywine Falls, which was the result of a bet over the falls' height (with the wagers being a bottle of wine and a bottle of brandy).

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: brandywine mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.114444444444
lon: -123.22111111111
The site covered 8 or 9 acres (32,000 to 36,000 m2). A tidal moat, up to wide in places, flowed about along the current streets of Fore Street and Castle Moat, and between Northgate and Chandos Street. The moat was filled from Durleigh brook, a tributary of the River Parrett. There is some evidence that there was a weir between the moat and the river.

Geographic entities mentioned:
surface_form: River Parrett
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 51.2292
lon: -3.00861
Vizcaíno's name stuck, and was later anglicized to today's version. Chumash beliefs. The Chumash people of the region have traditionally known Point Conception as the &quot;Western Gate&quot;, through which the souls of the dead could pass between the mortal world and the heavenly paradise of &quot;Similaqsa&quot;. It is called Humqaq (&quot;The Raven Comes&quot;) in the Chumashan languages.

Geographic entities mentioned:
surface_form: dead
instance_of: Watercourse
countries: United States
coordinates: lat: 45.3333
lon: -69.9697
Point Conception. Point Conception (Chumash: &quot;Humqaq&quot;; Spanish: &quot;Punta Concepción&quot;) is a headland along the Gaviota Coast in southwestern Santa Barbara County, California, United States.

Geographic entities mentioned:
surface_form: point conception
instance_of: Landform
countries: United States
coordinates: lat: 34.448113
lon: -120.471439
Point Conception. Point Conception (Chumash: &quot;Humqaq&quot;; Spanish: &quot;Punta Concepción&quot;) is a headland along the Gaviota Coast in southwestern Santa Barbara County, California, United States.

Geographic entities mentioned:
surface_form: point conception
instance_of: Landform
countries: United States
coordinates: lat: 34.448113
lon: -120.471439
surface_form: punta concepción
instance_of: Landform
countries: United States
coordinates: lat: 34.448113
lon: -120.471439
Point Conception Light is at its tip and the Jack and Laura Dangermond Preserve covers some of the surrounding land. Name. Point Conception was named &quot;Cabo de Galera&quot; (&quot;Galley Cape&quot;) by Spanish maritime explorer Juan Rodriguez Cabrillo in 1542.

Geographic entities mentioned:
surface_form: point conception
instance_of: Landform
countries: United States
coordinates: lat: 34.448113
lon: -120.471439
Career. Born in Paris, Moussard won seven titles at the French youth championships. He is the only player to have won a title in every age category, including the adult championship since his 2022 victory in finals against Étienne Bacrot. In 2002, he won his first title in the French under-8 championship in Hyères, in front of Jacques Netzer.

Geographic entities mentioned:
surface_form: Hyères
instance_of: Mountain
countries: France
coordinates: lat: 43.118888888889
lon: 6.1286111111111
Paley, to buy the struggling network. The Levy brothers were shareholders and directors at CBS for many years. Due to this long relationship, channel 10 signed on as CBS's third television affiliate. In the late 1950s, the Federal Communications Commission (FCC) collapsed northern Delaware, South Jersey, and the Lehigh Valley into the Philadelphia market.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
The eastern terminus of Route 1 is St. John's. From there, the highway crosses the island to Channel-Port aux Basques, its western terminus. From there, the Trans-Canada Highway is carried across the Cabot Strait by ferry to North Sydney, Nova Scotia. Route description. The following description details the highway from its eastern terminus to its western terminus.

Geographic entities mentioned:
surface_form: Cabot Strait
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.233333333333
lon: -59.716666666667
From Badger, Route 1 heads due north for 64 km to Springdale where the highway swings southwest for 137 km to Pasadena, passing through Deer Lake. At Pasadena, the highway transitions to a 4-lane expressway and continues southwest along the south shore of Deer Lake before following the Humber River through the narrow Humber Valley.

Geographic entities mentioned:
surface_form: Humber Valley
instance_of: Valley
countries: Canada
From the Confederation Drive interchange, Route 1 proceeds for 213 km in a southwest direction, bypassing Stephenville (accessible via Route 460 and Route 490) and passing through the Codroy Valley (where it is a 2-lane uncontrolled access highway) to Port aux Basques. It terminates southeast of the town at the Marine Atlantic ferry terminal. Outer Ring Road.

Geographic entities mentioned:
surface_form: Codroy Valley
instance_of: Valley
countries: Canada
John's City Hall, one must head geographically east for 1.5 km into the southeastern part of the city, continuing onto Duckworth Street (Route 60). Proceed north for 1 km on Cavendish Square and King's Bridge Road before turning east for 1.5 km along the north shore of Quidi Vidi Lake on The Boulevard, Or Turn Right Onto Forest Road And Continue To Quidi Vidi Village Road.

Geographic entities mentioned:
surface_form: Quidi Vidi Lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.5808
lon: -52.6889
Baviaanskloof River. The Baviaanskloof River is a river flowing through the Cape Fold Mountains of the Western Cape and eventually Eastern Cape provinces of South Africa. The river's origin is in the eastern extremity of the Little Karoo, and follows a valley between these mountains eastwards. It ends at a confluence with the Kouga River, some 80 km from its source.

Geographic entities mentioned:
surface_form: Cape Fold Mountains
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.4
lon: 22
Agricultural settlements along the river include Studtis and Sandvlakte. The valley is situated about 35 km north of the Langkloof, which is comparable though larger. The Kouga River, which rises in the Langkloof has the isolated Baviaanskloof River as its major tributary. The Baviaanskloof river is part of the Fish to Tsitsikama Water Management Area.

Geographic entities mentioned:
surface_form: Langkloof
instance_of: Valley
countries: South Africa
coordinates: lat: -33.825
lon: 23.857777777778
Maylandia barlowi. &quot;Maylandia barlowi&quot; is a species of cichlid endemic to Lake Malawi where it is only known from the area around the Maleri Islands where it prefers areas with soft substrates. This species can reach a length of SL. It is also found in the aquarium trade. The specific name of this species honours the ichthyologist George W. Barlow (1929–2007).

Geographic entities mentioned:
surface_form: Lake Malawi
instance_of: Lake
countries: Malawi
Mozambique
Tanzania
coordinates: lat: -12.183333333333
lon: 34.366666666667
Nadeau River. The Nadeau River (&quot;in French: rivière Nadeau&quot;) is a tributary of the west bank of the Chaudière River which flows northward to empty onto the south bank of the St. Lawrence River.

Geographic entities mentioned:
surface_form: Chaudière River
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.742777777777775
lon: -71.2786111111111
Geography. The Nadeau river has its source in the northern part of the municipality of Saint-Séverin, at north-west of the center of the village of Tring-Jonction, at north-west of the center of the village of Saint-Séverin and at west of the Chaudière River. The Nadeau river empties on the west bank of the Chaudière River, in Vallée-Jonction.

Geographic entities mentioned:
surface_form: Chaudière River
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.742777777777775
lon: -71.2786111111111
The tall mountain is located in the Rondane mountains within Rondane National Park. The mountain sits about northeast of the town of Otta. The mountain is surrounded by several other notable mountains including Bråkdalsbelgen, Sagtindan, and Indre Bråkdalshøe to the northwest; and Ljosåbelgen, Hoggbeitet, and Smiubelgen to the northeast.

Geographic entities mentioned:
surface_form: Bråkdalsbelgen
instance_of: Mountain
countries: Norway
coordinates: lat: 61.89090556
lon: 9.69989722
surface_form: Sagtindan
instance_of: Mountain
countries: Norway
coordinates: lat: 61.91297
lon: 9.66541
surface_form: Indre Bråkdalshøe
instance_of: Mountain
countries: Norway
coordinates: lat: 61.92027
lon: 9.63142
surface_form: Ljosåbelgen
instance_of: Mountain
countries: Norway
coordinates: lat: 61.89083333
lon: 9.69972222
surface_form: Hoggbeitet
instance_of: Mountain
countries: Norway
coordinates: lat: 61.8952
lon: 9.71251
Smiukampen. Smiukampen is a mountain in Sel Municipality in Innlandet county, Norway. The tall mountain is located in the Rondane mountains within Rondane National Park. The mountain sits about northeast of the town of Otta.

Geographic entities mentioned:
surface_form: smiukampen
instance_of: Mountain
countries: Norway
coordinates: lat: 61.882008
lon: 9.680436
Mussorgsky Peaks. Mussorgsky Peaks () are two rocky peaks rising to about 500 m lying northwest of Mount Grieg on the base of the Derocher Peninsula, a minor, ice-covered peninsula that protrudes out from the Beethoven Peninsula into the Wilkins Ice Shelf in the southwest portion of Alexander Island, Antarctica.

Geographic entities mentioned:
surface_form: Mount Grieg
instance_of: Mountain
coordinates: lat: -71.5667
lon: -73.1667
surface_form: mussorgsky peaks
instance_of: Mountain
coordinates: lat: -71.4833
lon: -73.3667
surface_form: grieg
instance_of: Mountain
coordinates: lat: -71.5667
lon: -73.1667
surface_form: alexander
instance_of: Mountain
coordinates: lat: -63.3039
lon: -55.80564
Mussorgsky Peaks. Mussorgsky Peaks () are two rocky peaks rising to about 500 m lying northwest of Mount Grieg on the base of the Derocher Peninsula, a minor, ice-covered peninsula that protrudes out from the Beethoven Peninsula into the Wilkins Ice Shelf in the southwest portion of Alexander Island, Antarctica.

Geographic entities mentioned:
surface_form: mussorgsky peaks
instance_of: Mountain
coordinates: lat: -71.4833
lon: -73.3667
A number of peaks in this vicinity first appear on maps by the Ronne Antarctic Research Expedition (RARE), 1947–48. These peaks, apparently included within that group, were mapped from RARE air photos by Searle of the Falkland Islands Dependencies Survey (FIDS) in 1960. Named by the United Kingdom Antarctic Place-Names Committee (UK-APC) after Modeste Mussorgsky (1839–81), Russian composer.

Geographic entities mentioned:
surface_form: searle
instance_of: Mountain
coordinates: lat: -67.81666667
lon: -67.25
Karats. Karats () is a mountain lake in Norrbotten County, Lappland west of Jokkmokk that drains into Small Lule River by way of Pärl River.

Geographic entities mentioned:
surface_form: karats
instance_of: Lake
countries: Sweden
coordinates: lat: 66.716666666667
lon: 18.55
Maintop Mountain. Maintop Mountain is a mountain in Nelson County, Virginia. The mountain is a peak on a spur off the main Blue Ridge Mountains, about 2 miles (3 km) east of Elk Pond Mountain, and about 3.5 miles (5.5 km) west of The Priest. The mountain is located in the George Washington National Forest.

Geographic entities mentioned:
surface_form: Elk Pond Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.8127
lon: -79.1647
surface_form: the priest
instance_of: Mountain
countries: United States
coordinates: lat: 37.8198
lon: -79.0625
The mountain is located in the George Washington National Forest. Maintop Mountain stands within the watershed of the Tye River, which drains into the James River. The northwest side of Maintop Mountain drains into Mill Creek, thence into the South Fork of the Tye River. The northeast side of the mountain drains into the Maidenhead Branch of the South Fork.

Geographic entities mentioned:
surface_form: mill creek
instance_of: Watercourse
countries: United States
coordinates: lat: 44.4599675
lon: -89.6412311
surface_form: maintop mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.8308
lon: -79.1222
surface_form: mill creek
instance_of: Watercourse
countries: United States
coordinates: lat: 37.871442
lon: -90.093448
Maintop Mountain is a mountain in Nelson County, Virginia. The mountain is a peak on a spur off the main Blue Ridge Mountains, about 2 miles (3 km) east of Elk Pond Mountain, and about 3.5 miles (5.5 km) west of The Priest. The mountain is located in the George Washington National Forest. Maintop Mountain stands within the watershed of the Tye River, which drains into the James River.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Maintop Mountain. Maintop Mountain is a mountain in Nelson County, Virginia. The mountain is a peak on a spur off the main Blue Ridge Mountains, about 2 miles (3 km) east of Elk Pond Mountain, and about 3.5 miles (5.5 km) west of The Priest. The mountain is located in the George Washington National Forest.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: maintop mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.8308
lon: -79.1222
Maintop Mountain. Maintop Mountain is a mountain in Nelson County, Virginia. The mountain is a peak on a spur off the main Blue Ridge Mountains, about 2 miles (3 km) east of Elk Pond Mountain, and about 3.5 miles (5.5 km) west of The Priest. The mountain is located in the George Washington National Forest.

Geographic entities mentioned:
surface_form: maintop mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.8308
lon: -79.1222
The mountain is located in the George Washington National Forest. Maintop Mountain stands within the watershed of the Tye River, which drains into the James River. The northwest side of Maintop Mountain drains into Mill Creek, thence into the South Fork of the Tye River. The northeast side of the mountain drains into the Maidenhead Branch of the South Fork.

Geographic entities mentioned:
surface_form: maintop mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.8308
lon: -79.1222
The southwest side drains into the Louisa Spring Branch of the North Fork of the Piney River. The Appalachian Trail, a 2,170-mile (3,500-km) National Scenic Trail from Georgia to Maine, currently runs across the summit of Maintop Mountain. After a trail relocation scheduled to start in May 2009, the AT will follow a less steep route and pass below the summit.

Geographic entities mentioned:
surface_form: maintop mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.8308
lon: -79.1222
After a trail relocation scheduled to start in May 2009, the AT will follow a less steep route and pass below the summit. Maintop is a popular local destination because of the view from Spy Rock, a spur located about a quarter mile from the summit. Spy Rock can be reached by a steep mile and a half hike from a state fish hatchery in Montebello, Virginia

Geographic entities mentioned:
surface_form: spy rock
instance_of: Mountain
countries: United States
coordinates: lat: 30.8969
lon: -99.15
In 1968, the Shann Building was constructed between the Robertson Building and Arnold Hall and a new sports facility, the Cornell Gymnasium, was opened. At the beginning of the 1970s, Trinity purchased land beside Lake Eppalock, near Bendigo, opening the Leppitt Outdoor Education Centre in 1973, named after the headmaster.

Geographic entities mentioned:
surface_form: Lake Eppalock
instance_of: Lake
countries: Australia
coordinates: lat: -36.883333333333
lon: 144.56666666667
Outdoor education. The Outdoor Education program includes participation in bushwalking, sailing, canoeing, kayaking, cycling, first aid, navigation, cooking and rafting. The program is compulsory for students from Year 7 to Year 10. Camps are based around school properties at Lake Eppalock, Lake Nillahcootie and Licola. Trinity also offers The Duke of Edinburgh's Award. Sport.

Geographic entities mentioned:
surface_form: Lake Eppalock
instance_of: Lake
countries: Australia
coordinates: lat: -36.883333333333
lon: 144.56666666667
Among these rugged structures are natural arches formed by powerful wave action selectively eroding weaker strata of the rock formations. Approximately to the south is another major geological feature of the Northern California coast known as Bodega Head. Goat Beach lies below and slightly west of State Route 1.

Geographic entities mentioned:
surface_form: Bodega Head
instance_of: Mountain
countries: United States
coordinates: lat: 38.31111111111111
lon: -123.06583333333333
Mammoths are believed to have roamed here as recently as 40,000 years ago, and they are thought to have created these severe rubbing marks. Mammoth fossil remains have been found at Bodega Head at the south end of Sonoma Coast State Beach. The earliest known human settlement of this site was by the Native American Coast Miwok and Pomo tribes.

Geographic entities mentioned:
surface_form: Bodega Head
instance_of: Mountain
countries: United States
coordinates: lat: 38.31111111111111
lon: -123.06583333333333
In the first two years after his coronation, Ramesses VI stopped frequent raids by Libyan or Egyptian marauders in Upper Egypt and buried his predecessor in what is now an unknown tomb of the Theban necropolis. Ramesses VI usurped KV9, a tomb in the Valley of the Kings planned by and for Ramesses V, and had it enlarged and redecorated for himself.

Geographic entities mentioned:
surface_form: Valley of the Kings
instance_of: Valley
countries: Egypt
coordinates: lat: 25.74025
lon: 32.602358
The craftsmen's huts near the entrance of KV9 covered up the entrance to Tutankhamun's tomb, saving it from a wave of tomb robberies that occurred within 20 years of Ramesses VI's death. Ramesses VI may have planned and made six more tombs in the Valley of the Queens, none which are known today. Egypt lost control of its last strongholds in Canaan around the time of Ramesses VI's reign.

Geographic entities mentioned:
surface_form: Valley of the Queens
instance_of: Valley
countries: Egypt
coordinates: lat: 25.7275
lon: 32.593055555556
Such hypotheses have now been conclusively rejected and the relief is understood to mean exactly what it shows: that Ramesses VI was the son of Ramesses III. Ramesses VI's mother was probably Iset Ta-Hemdjert, Ramesses III's Great Royal Wife, as suggested by the presence of Ramesses VI's cartouches on a door-jamb of her tomb in the Valley of the Queens. Consort and children.

Geographic entities mentioned:
surface_form: Valley of the Queens
instance_of: Valley
countries: Egypt
coordinates: lat: 25.7275
lon: 32.593055555556
Tomb. Ramesses VI was buried in the Valley of the Kings, in a tomb now known as KV9. The tomb was first built for Ramesses V, who may have been buried in it for the short period of time necessary for another, likely undecorated tomb, to be cut for him somewhere else in the Valley of Kings and which remains to be discovered.

Geographic entities mentioned:
surface_form: Valley of the Kings
instance_of: Valley
countries: Egypt
coordinates: lat: 25.74025
lon: 32.602358
He is a faculty member at the Edge Performing Arts Center, Triple Threat Dance, and Intrigue Dance. He is represented by DDO Artists Agency. Beau Fournier. Beau Fournier (born July 1, 1983) is from the San Fernando Valley in Southern California. At the late age of 19, Beau started dance and it turned into a career. He is currently signed with DDO Artists Agency and Artist's International.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
History. The movement first started as an offshoot of the religion Baekdokyo (), itself an offshoot of Cheondoism. Baekdokyo was founded in 1899, with its official organization in 1912 and was led by leader Jeon Jeong-ye, an individual who claimed to have received a revelation on Mount Kumgang. Baekdogyo, despite its proselytization projects, was mostly run as a secret organization.

Geographic entities mentioned:
surface_form: Mount Kumgang
instance_of: Mountain
countries: North Korea
coordinates: lat: 38.656763888889
lon: 128.10490277778
Located south of Chennai and north of Kanyakumari, Tiruchirappalli sits almost at the geographic centre of Tamil Nadu. The Cauvery Delta begins west of the city where the Kaveri river splits into two, forming the island of Srirangam which is now incorporated into the Tiruchirappalli City Municipal Corporation. The city occupies an area of and had a population of 916,857 in 2011.

Geographic entities mentioned:
surface_form: Kaveri river
instance_of: Watercourse
countries: India
coordinates: lat: 11.370345
lon: 79.828105
Geography and climate. Tiruchirappalli is situated in central south-eastern India, almost at the geographic centre of the state of Tamil Nadu. The Cauvery Delta begins to form west of the city where the river divides into two streams—the Kaveri and the Kollidam—to form the island of Srirangam. By road it is south of Hyderabad, south-west of Chennai and south-east of Bangalore.

Geographic entities mentioned:
surface_form: Kaveri
instance_of: Watercourse
countries: India
coordinates: lat: 11.370345
lon: 79.828105