Sarmila/GeoWiki-Features huggingface dataset:
Thor Peak (Washington). Thor Peak is a mountain summit in Chelan County, Washington, United States. Description. Thor Peak is part of the Wenatchee Mountains which are a subrange of the Cascade Range. It is situated south of Stevens Pass and one mile east of the Cascade crest. Thor Peak is in the Alpine Lakes Wilderness on land managed by the Okanogan–Wenatchee National Forest.

Geographic entities mentioned:
surface_form: thor peak
instance_of: Mountain
coordinates: lat: 47.658391
lon: -121.107591
It is situated south of Stevens Pass and one mile east of the Cascade crest. Thor Peak is in the Alpine Lakes Wilderness on land managed by the Okanogan–Wenatchee National Forest. Precipitation runoff from the peak drains into Trapper and Prospect creeks which are tributaries of Icicle Creek, which in turn is a tributary of the Wenatchee River.

Geographic entities mentioned:
surface_form: thor peak
instance_of: Mountain
coordinates: lat: 47.658391
lon: -121.107591
The Nicarao settled throughout western Nicaragua, inhabiting Rivas, Jinotega, Chinandega, Nueva Segovia, Masaya, Carazo, Madriz, Matagalpa, Esteli, Leon, Granada and Managua. In addition the Nicarao controlled Tiger Lagoon, Lake Managua, Lake Cocibolca, and the islands of Ometepe and Zapatera. Lake Ometepe and Isla Zapatera in Lake Nicaragua were also sacred to the Nicarao.

Geographic entities mentioned:
surface_form: Lake Managua
instance_of: Lake
countries: Nicaragua
coordinates: lat: 12.333333333333
lon: -86.416666666667
The Nicarao settled throughout western Nicaragua, inhabiting Rivas, Jinotega, Chinandega, Nueva Segovia, Masaya, Carazo, Madriz, Matagalpa, Esteli, Leon, Granada and Managua. In addition the Nicarao controlled Tiger Lagoon, Lake Managua, Lake Cocibolca, and the islands of Ometepe and Zapatera. Lake Ometepe and Isla Zapatera in Lake Nicaragua were also sacred to the Nicarao.

Geographic entities mentioned:
surface_form: Lake Nicaragua
instance_of: Lake
countries: Nicaragua
coordinates: lat: 11.5742
lon: -85.3563
The dating of Nicarao arrival in what is now Nicaragua has also been linked to the Classic Maya collapse, with the cessation of Maya influence in the region, and the rise of cultural traits originating in the Valley of Mexico. The Nicarao had a sizeable population concentrated in nucleated villages all over western Nicaragua and what is now northwestern Costa Rica.

Geographic entities mentioned:
surface_form: Valley of Mexico
instance_of: Valley
countries: Mexico
coordinates: lat: 19.66666667
lon: -98.86666667
They displaced both the Chorotega and the Cacaopera that had previously settled the region; evidence shows some of their culture was integrated into their own. The Nicarao appear to have seized control of the most productive land around the western portions of Lake Nicaragua, Ometepe, and the Gulf of Fonseca.

Geographic entities mentioned:
surface_form: Lake Nicaragua
instance_of: Lake
countries: Nicaragua
coordinates: lat: 11.5742
lon: -85.3563
Renton, West Dunbartonshire. Renton (;) is a village in West Dunbartonshire, in the west Central Lowlands of Scotland. In the 2001 National Census it had a population of 2,138. Renton is particularly famous for the village's association football side.

Geographic entities mentioned:
surface_form: Central Lowlands
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.408
lon: -4.044
The only known population to be found protected within a nature conservation area is at the Yacyretá Dam Island Reserve at Parque Nacional Lago Ypacarai in Itapua, Paraguay, with three known localities here.

Geographic entities mentioned:
surface_form: Parque Nacional Lago Ypacarai
instance_of: Lake
countries: Paraguay
coordinates: lat: -25.3
lon: -57.35
Anvil Peak. Anvil Peak is a cone volcano located in Aleutian Islands, Alaska, United States. Etymology. The volcano was originally named in 1951, on a map by the United States Geological Survey. Its name was taken after a plateau located on the northern side of the volcano's main summit, taking the appearance of an anvil. Location.

Geographic entities mentioned:
surface_form: anvil peak
instance_of: Mountain
countries: United States
coordinates: lat: 51.9856
lon: 179.6011
Its name was taken after a plateau located on the northern side of the volcano's main summit, taking the appearance of an anvil. Location. Anvil Peak is located on Semisopochnoi Island, in the Rat Islands of the western Aleutian Islands. It is one of the seven hills with a summit crater on the island. It is the highest point on the island as well as the highest point on all of the Rat Islands.

Geographic entities mentioned:
surface_form: anvil peak
instance_of: Mountain
countries: United States
coordinates: lat: 51.9856
lon: 179.6011
The volcano is located away from Atka, from Shemya, and from Attu. Geology. Anvil Peak has two summits, which are both volcanic cones. The larger main summit is tall, making it the highest point on the island. This summit is surrounded by ravines, which contain snow at certain times of the year.

Geographic entities mentioned:
surface_form: anvil peak
instance_of: Mountain
countries: United States
coordinates: lat: 51.9856
lon: 179.6011
The other summit is located southwest of the main summit, and is slightly shorter. It is not known exactly when Anvil Peak first formed, but it is believed to have formed after Mount Cerberus. According to the Global Volcanism Program of the Smithsonian Institution, its formation occurred during the late Pleistocene epoch.

Geographic entities mentioned:
surface_form: anvil peak
instance_of: Mountain
countries: United States
coordinates: lat: 51.9856
lon: 179.6011
According to the Global Volcanism Program of the Smithsonian Institution, its formation occurred during the late Pleistocene epoch. It has not erupted in recent times; it is thought that its last activity was probably thousands of years ago. Anvil Peak has experienced deep erosion, more so than the other cones on the islands, which is partially due to its height.

Geographic entities mentioned:
surface_form: anvil peak
instance_of: Mountain
countries: United States
coordinates: lat: 51.9856
lon: 179.6011
Overview. Maoile Lunndaidh is a large and remote mountain, covering an area in excess of. Its location is almost equidistant from the valleys of Strathconon, Strathfarrar and Glen Carron, the nearest public road being over 10 km away. The mountain is listed in the current edition of Munro's Tables as in elevation. This height dates from the introduction of the 1:50k OS map series in the 1970s.

Geographic entities mentioned:
surface_form: Strathfarrar
instance_of: Valley
countries: United Kingdom
coordinates: lat: 57.414166666667
lon: -4.8391666666667
Maoile Lunndaidh. Maoile Lunndaidh or Maoil Lunndaidh is a Scottish mountain situated 13 km south of Achnasheen in the Ross and Cromarty district of the Highland council area. It is part of the high ground between Loch Monar and Gleann Fhiodhaig. Overview. Maoile Lunndaidh is a large and remote mountain, covering an area in excess of.

Geographic entities mentioned:
surface_form: loch monar
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.4171
lon: -5.0988
Between 1921 and 1981 Creag Toll a’ Choin was declared the Munro after its height changed to on the map. In 1981 the summit reverted to the original location when the 1007 m spot appeared on the new Landranger map, a decision not without some controversy as Creag Toll a’ Choin is the better viewpoint for Loch Monar. The latest 1:25000 map gives both points a spot height of 1005 metres.

Geographic entities mentioned:
surface_form: loch monar
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.4171
lon: -5.0988
Fuar Tholl Mòr has several small lochans nestling within it. On the eastern flanks of the mountain are the larger bodies of water of Loch a’ Chlaidheimh and Loch nam Breac Dearga. The southern slopes of the mountain descend to the former site of Strathmore Lodge on Loch Monar, made famous by Iain Thomson in his book “Isolation Shepherd”.

Geographic entities mentioned:
surface_form: loch monar
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.4171
lon: -5.0988
surface_form: strathmore
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.717
lon: -3.549
surface_form: strathmore
instance_of: Valley
countries: United Kingdom
coordinates: lat: 58.376388888889
lon: -4.64
From there the mountain can be climbed by following the west edge of the Fuar Tholl Mòr corrie. The approach from Strathglass is a 22 km round trip which starts at the Loch Monar dam (grid reference), a drive along a private road from the locked gate at Struy. Car access is permitted at certain times, but there is a quota on the number of vehicles entering the glen.

Geographic entities mentioned:
surface_form: loch monar
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.4171
lon: -5.0988
Maoile Lunndaidh. Maoile Lunndaidh or Maoil Lunndaidh is a Scottish mountain situated 13 km south of Achnasheen in the Ross and Cromarty district of the Highland council area. It is part of the high ground between Loch Monar and Gleann Fhiodhaig. Overview. Maoile Lunndaidh is a large and remote mountain, covering an area in excess of.

Geographic entities mentioned:
surface_form: maoile lunndaidh
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.464477
lon: -5.111002
It is part of the high ground between Loch Monar and Gleann Fhiodhaig. Overview. Maoile Lunndaidh is a large and remote mountain, covering an area in excess of. Its location is almost equidistant from the valleys of Strathconon, Strathfarrar and Glen Carron, the nearest public road being over 10 km away. The mountain is listed in the current edition of Munro's Tables as in elevation.

Geographic entities mentioned:
surface_form: maoile lunndaidh
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.464477
lon: -5.111002
However the current 1:25000 map shows a spot height of, in better agreement with the trigonometric height of on old 6-inch maps (equivalent to 1004.1 metres after conversion to the Newlyn datum). Maoile Lunndaidh has been described as &quot;the flattest of bulks&quot;. Its extensive level summit plateau is reminiscent of the Cairngorm and seems out of place amongst the west coast peaks.

Geographic entities mentioned:
surface_form: maoile lunndaidh
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.464477
lon: -5.111002
The latest 1:25000 map gives both points a spot height of 1005 metres. A 2014 survey clarified Creag Toll a’ Choin was taller than Maoile Lunndaidh, and Maoile Lunndaidh's official prominence was reduced from 400 m to 10.5m. At the western end of the summit ridge stands Càrn nan Fiaclan (Cairn of the teeth) with a height of 993 metres on the 1:25000 map.

Geographic entities mentioned:
surface_form: maoile lunndaidh
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.464477
lon: -5.111002
surface_form: maoile lunndaidh
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.464477
lon: -5.111002
Other mountain writers (Ralph Storer and Robin Howie) recommend the approach from Glen Strathfarrar because of the scenery. The approach from Craig starts on the A890 road at grid reference. A forestry track leads 10 km to the remote Glenuaig Lodge at the foot of Maoile Lunndaidh. From there the mountain can be climbed by following the west edge of the Fuar Tholl Mòr corrie.

Geographic entities mentioned:
surface_form: maoile lunndaidh
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.464477
lon: -5.111002
Maoile Lunndaidh has been described as &quot;the flattest of bulks&quot;. Its extensive level summit plateau is reminiscent of the Cairngorm and seems out of place amongst the west coast peaks. The mountain has two impressive corries which cut deeply into the mountain on its NW and SE sides and are its most impressive geographical features.

Geographic entities mentioned:
surface_form: cairngorm
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.116714
lon: -3.644477
Most guide books recommend the route from Craig in Glen Carron because it is slightly shorter, and it is possible to use a bicycle as far as Glenuaig Lodge. Other mountain writers (Ralph Storer and Robin Howie) recommend the approach from Glen Strathfarrar because of the scenery. The approach from Craig starts on the A890 road at grid reference.

Geographic entities mentioned:
surface_form: glen strathfarrar
instance_of: Valley
countries: United Kingdom
coordinates: lat: 57.414166666667
lon: -4.8391666666667
A forestry track leads 10 km to the remote Glenuaig Lodge at the foot of Maoile Lunndaidh. From there the mountain can be climbed by following the west edge of the Fuar Tholl Mòr corrie. The approach from Strathglass is a 22 km round trip which starts at the Loch Monar dam (grid reference), a drive along a private road from the locked gate at Struy.

Geographic entities mentioned:
surface_form: fuar tholl
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.485376
lon: -5.379188
It is listed as a “top” in the Munros Tables despite having only about 10 metres of prominence. The summit ridge follows the rim of two massive corries, the Fuar Tholl Mòr (Big cold hollow) and the Toll a’ Choin (Boggy hollow), which cut into the mountain from the NW and SE respectively.

Geographic entities mentioned:
surface_form: fuar tholl
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.485376
lon: -5.379188
This took place from Cranfield, Bedfordshire. Bad weather prevented much flying and so the aircraft went back to Peak Sailplanes for a lengthening and lowering of the nose, giving it a slightly more pointed look. Serious testing resumed at Long Mynd that Easter and was ongoing in August. It received its BGA certificate of airworthiness no. &quot;BGA 1140&quot;. Operational history.

Geographic entities mentioned:
surface_form: Long Mynd
instance_of: Plateau
countries: United Kingdom
coordinates: lat: 52.5478
lon: -2.8389
Another member of the youthful artistic circle of the time was the painter-sculptor Hans von Matt (1899–1985) whom Annemarie Gunz married she was thirty, in 1935. Hans was from Stans, an ancient city in the hills to the south of the lake, and it was here that the couple made their home. Her new husband was a member of a long established Nidwalden family.

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.0194
lon: 8.4011
Chhanka. Chhanka (Quechua for cliff, hispanicized spelling &quot;Chanca&quot;) is a mountain in the Andes of Peru, about high. It is located in the Lima Region, Cajatambo Province, Cajatambo District. Chhanka lies southwest of Pishtaq. A little lake named Tuqtuqucha (&quot;hen lake&quot;) lies at its feet.

Geographic entities mentioned:
surface_form: chhanka
instance_of: Mountain
countries: Peru
coordinates: lat: -10.54444444
lon: -76.88055556
Chhanka. Chhanka (Quechua for cliff, hispanicized spelling &quot;Chanca&quot;) is a mountain in the Andes of Peru, about high. It is located in the Lima Region, Cajatambo Province, Cajatambo District. Chhanka lies southwest of Pishtaq. A little lake named Tuqtuqucha (&quot;hen lake&quot;) lies at its feet.

Geographic entities mentioned:
surface_form: pishtaq
instance_of: Mountain
countries: Peru
coordinates: lat: -10.54138889
lon: -76.87361111
Loki dialect. Loki (Boloki), or Ruki, is a Bantu language spoken in the Democratic Republic of the Congo. It is very close to Lingala. The Boloki (Baloki) people are named after the Ruki River; they live on either side of the Congo River where the Ruki joins it.

Geographic entities mentioned:
surface_form: Ruki River
instance_of: Watercourse
countries: Democratic Republic of the Congo
coordinates: lat: 0.0767
lon: 18.28104
Capital cities, elite precincts, and monumental architecture. Since the establishment of Goguryeo, its early history is well attested archaeologically: the first and second capital cities, Jolbon and Gungnae city, are located in and around today's Ji'an, Jilin. In 2004, the site was designated as a World Heritage Site by UNESCO.

Geographic entities mentioned:
surface_form: Jolbon
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 41.326666666667
lon: 125.41166666667
Mills Lake (Minnesota). Mills Lake is a lake in Blue Earth County, Minnesota, in the United States. Mills Lake was named for Titus Mills, an early settler whose farm was near this lake.

Geographic entities mentioned:
surface_form: mills lake
instance_of: Lake
countries: United States
coordinates: lat: 37.4027
lon: -118.7762
surface_form: mills lake (minnesota)
instance_of: Lake
countries: United States
coordinates: lat: 44.083333333333
lon: -94.1475
Mills Lake (Minnesota). Mills Lake is a lake in Blue Earth County, Minnesota, in the United States. Mills Lake was named for Titus Mills, an early settler whose farm was near this lake.

Geographic entities mentioned:
surface_form: mills lake
instance_of: Lake
countries: United States
coordinates: lat: 37.4027
lon: -118.7762
surface_form: mills lake
instance_of: Lake
countries: United States
coordinates: lat: 44.083333333333
lon: -94.1475
The county seat is the city of Poughkeepsie. The county was created in 1683, one of New York's first twelve counties, and later organized in 1713. Dutchess County is part of the Kiryas Joel–Poughkeepsie–Newburgh metropolitan area, which belongs to the larger New York–Newark–Bridgeport, NY-NJ-CT-PA Combined Statistical Area. The county is part of the Hudson Valley region of the state. History.

Geographic entities mentioned:
surface_form: Hudson Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.9209
lon: -73.9613
The terrain of the county is mostly hilly, especially in the Hudson Highlands in the southwestern corner and the Taconic Mountains to the northeast. Some areas nearer the river are flatter. The highest point in the county is the summit of Brace Mountain, in the Taconics, at above sea level. The lowest point is sea level, along the Hudson River.

Geographic entities mentioned:
surface_form: Brace Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.044166666667
lon: -73.4925
The lowest point is sea level, along the Hudson River. The highest point of neighboring Fairfield County, Connecticut, is a point along the state line in Pawling. Wappinger Creek, at from its source at Thompson Pond in Pine Plains to where it drains into the Hudson at New Hamburg, is the longest stream in the county. Its watershed is likewise the largest in the county.

Geographic entities mentioned:
surface_form: Thompson Pond
instance_of: Lake
countries: United States
coordinates: lat: 41.961119444444
lon: -73.678736111111
To its south is the watershed of Dutchess County's second-longest stream, Fishkill Creek, part of which spills over into Putnam County. Within that watershed are the county's third-longest stream, Sprout Creek, and its largest, deepest and highest lakes: Whaley (), in the town of Pawling; Sylvan () in the town of Beekman and Beacon Reservoir, in the town of Fishkill, at respectively.

Geographic entities mentioned:
surface_form: Whaley
instance_of: Lake
countries: United States
coordinates: lat: 41.558333333333
lon: -73.6625
Exile from Rome. The pope was liberated, but after the Roman people became incensed by the excesses of his Norman allies, again withdrew to Monte Cassino, and later to the castle of Salerno by the sea, where he died on 25 May 1085. He was probably a prisoner of the Normans in Salerno.

Geographic entities mentioned:
surface_form: Monte Cassino
instance_of: Mountain
countries: Italy
coordinates: lat: 41.49
lon: 13.813888888889
Cobbs Lake Creek. Cobbs Lake Creek is a creek in Prescott and Russell County in eastern Ontario, Canada, which empties into the South Nation River. In the early 1900, the Cobb Lake Drainage Scheme reduced a large area covered by water to a tiny little creek.

Geographic entities mentioned:
surface_form: cobbs lake creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.4439
lon: -75.0503
Cathedral Crags. Cathedral Crags () is a rocky, ice-free hill with steeply cliffed sides, high, surmounting the peninsula between Neptune's Window and Fildes Point on the southeast side of Deception Island, in the South Shetland Islands.

Geographic entities mentioned:
surface_form: cathedral crags
instance_of: Mountain
coordinates: lat: -63
lon: -60.5667
Cathedral Crags. Cathedral Crags () is a rocky, ice-free hill with steeply cliffed sides, high, surmounting the peninsula between Neptune's Window and Fildes Point on the southeast side of Deception Island, in the South Shetland Islands.

Geographic entities mentioned:
surface_form: cathedral crags
instance_of: Mountain
coordinates: lat: -63
lon: -60.5667
surface_form: fildes
instance_of: Body of water
coordinates: lat: -62.2333
lon: -59
Although the feature was called The Convent or Weathercock Hill by the whalers operating from Deception Island in the period before 1930, these names have not been used recently. The name Cathedral Crags was reported in 1953 to have become well established in local use at the nearby Falkland Islands Dependencies Survey station.

Geographic entities mentioned:
surface_form: cathedral crags
instance_of: Mountain
coordinates: lat: -63
lon: -60.5667
Ñauña. Ñauña (possibly from Quechua for arête) is a mountain in the Andes of Peru, about high. It is located in the Cusco Region, Canchis Province, Pitumarca District, near the Vilcanota mountain range. Ñauña lies on a ridge between the rivers Chillcamayu and Yanamayu. It is situated northeast of the peak of Queullacocha and the lake of the same name.

Geographic entities mentioned:
surface_form: ñauña
instance_of: Mountain
countries: Peru
coordinates: lat: -13.9219
lon: -71.2106
Ñauña. Ñauña (possibly from Quechua for arête) is a mountain in the Andes of Peru, about high. It is located in the Cusco Region, Canchis Province, Pitumarca District, near the Vilcanota mountain range. Ñauña lies on a ridge between the rivers Chillcamayu and Yanamayu. It is situated northeast of the peak of Queullacocha and the lake of the same name.

Geographic entities mentioned:
surface_form: queullacocha
instance_of: Mountain
countries: Peru
coordinates: lat: -13.76527778
lon: -71.28361111
It is endemic to Spain. Distribution. This snail occurs in the eastern Basque Country and in northern Navarre. It can be found in the Aizkorri and Aralar Ranges and on Lindux Mountain. It lives under rocks in dry, open habitat types. The population is thought to be stable and there are few threats.

Geographic entities mentioned:
surface_form: Aizkorri
instance_of: Mountain
countries: Spain
coordinates: lat: 42.9513544
lon: -2.3253425
Bayuda Desert. The Bayuda Desert, located at, is in the eastern region of the Sahara Desert, spanning approximately 100,000 km2 of northeast Sudan north of Omdurman and south of Korti, embraced by the great bend of the Nile in the north, east, and south and limited by the Wadi Muqaddam in the west.

Geographic entities mentioned:
surface_form: Wadi Muqaddam
instance_of: Watercourse
Landform
countries: Sudan
coordinates: lat: 15.5091
lon: 31.880491
The north-to-south-aligned Wadi Abu Dom divides the Bayuda Desert into the eastern Bayuda Volcanic Field and the western ochre-colored sand-sheets scattered with rocky outcrop. Gold mining occurs today from October to March, as laborers work auriferous quartz found in wadis and shallow mines.

Geographic entities mentioned:
surface_form: Bayuda Volcanic Field
instance_of: Mountain
countries: Sudan
coordinates: lat: 18.333333333333
lon: 32.75
In medieval times, Márcadópuszta existed within the village's territory, preserving the obligation to pay the March tithe in its name. The Rákóczi War of Independence began in 1703, leading to the presence of Kuruc hussars on the southern shore of Lake Balaton in the fall, marking the onset of military activities in Somogy County.

Geographic entities mentioned:
surface_form: Lake Balaton
instance_of: Lake
countries: Hungary
coordinates: lat: 46.85
lon: 17.72
Shackleton Valley. Shackleton Valley is a broad valley running west-northwest from Stromness Harbor, Stromness Bay, in South Georgia.

Geographic entities mentioned:
surface_form: shackleton valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: -54.15
lon: -36.716666666667
The long Kootenay section of Highway 3A begins at Castlegar, where it leaves Highway 3 and travels northeast to South Slocan, where Highway 6 merges onto Highway 3A. The two highways proceed east for to Nelson, where Highway 6 diverges south. northeast of Nelson, Highway 3A reaches Balfour, on the western shore of Kootenay Lake. A ferry takes Highway 3A across Kootenay Lake to Kootenay Bay.

Geographic entities mentioned:
surface_form: Kootenay Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.3
lon: -116.75
Geography. Kyōgoku is mountainous, with several peaks above. The town sits between Mount Yotei to the east, and Mount Muine (), Mount Nakadake, and Mount Kimobetsu () to the west. The Shiribetsu River (), which emerges from Lake Shikotsu to the south, runs through Kyōgoku between Mount Yotei and the western peaks in the town. The river eventually flows into the Sea of Japan. History.

Geographic entities mentioned:
surface_form: Lake Shikotsu
instance_of: Lake
countries: Japan
coordinates: lat: 42.75
lon: 141.33333333333
It is surrounded by Spring Township, a separate municipality. Pennsylvania Route 18 passes through the center of town, leading north to Albion and south to Conneautville. According to the United States Census Bureau, the borough has a total area of, all land. Conneaut Creek flows northward through the western side of the borough on its way to Lake Erie. Demographics.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Geography. Jutulsessen is a nunatak mountain with a peak above mean sea level. It is located north of Terningskarvet, also in the Gjelsvik Mountains of Queen Maud Land. Jutulsessen is located in the eastern part of Princess Martha Coast in Queen Maud Land, which Norway claims as a dependent territory. The main ice-free area of the Jutulsessen massif is about 10 km long by 5 km across.

Geographic entities mentioned:
surface_form: Terningskarvet
instance_of: Mountain
coordinates: lat: -72.1833
lon: 2.76667
The western arm is the location of Troll. The eastern arm is longer and consists of the narrow section of Jutulhogget and the wider Armlenet. Further north lies the isolated area of Stabben. Blåfallet is an ice-depression on the western side of Knokane, a ridge of Armlenet. Jutuldalen is a valley in Armlenet, with the ice-depression of Staupet to the west.

Geographic entities mentioned:
surface_form: Stabben
instance_of: Mountain
coordinates: lat: -71.95
lon: 2.8666666666667
surface_form: stabben
instance_of: Mountain
coordinates: lat: -67.483333333333
lon: 60.933333333333
The two arms of the area are located northwards. The western arm is the location of Troll. The eastern arm is longer and consists of the narrow section of Jutulhogget and the wider Armlenet. Further north lies the isolated area of Stabben. Blåfallet is an ice-depression on the western side of Knokane, a ridge of Armlenet.

Geographic entities mentioned:
surface_form: jutulhogget
instance_of: Mountain
coordinates: lat: -72.0333
lon: 2.85
Jutuldalen is a valley in Armlenet, with the ice-depression of Staupet to the west. Armlenet also features the glacier of Ringfingerbreen. Southeast of Sætet lies the broad valley of Brudgedalen, and to the southeast lies the ridge of Brudga. The three peaks closest to Troll are Trolltindane, the tallest of which is Trolltinden. The area has a cold and dry climate being located in a desert.

Geographic entities mentioned:
surface_form: broad valley
instance_of: Valley
coordinates: lat: -63.3667
lon: -57.9167
Jutulsessen. Jutulsessen is a nunatak in the Gjelsvik Mountains in Queen Maud Land, Antarctica. It is located in Princess Martha Coast, from the King Haakon VII Sea. Jutulsessen is the site of the Norwegian research station Troll and the affiliated Troll Satellite Station, which has two radomes on top of the mountain. Troll Airfield is located in the vicinity. Geography.

Geographic entities mentioned:
surface_form: jutulsessen
instance_of: Mountain
coordinates: lat: -72.0333
lon: 2.68333
Troll Airfield is located in the vicinity. Geography. Jutulsessen is a nunatak mountain with a peak above mean sea level. It is located north of Terningskarvet, also in the Gjelsvik Mountains of Queen Maud Land. Jutulsessen is located in the eastern part of Princess Martha Coast in Queen Maud Land, which Norway claims as a dependent territory.

Geographic entities mentioned:
surface_form: jutulsessen
instance_of: Mountain
coordinates: lat: -72.0333
lon: 2.68333
Geography. Jutulsessen is a nunatak mountain with a peak above mean sea level. It is located north of Terningskarvet, also in the Gjelsvik Mountains of Queen Maud Land. Jutulsessen is located in the eastern part of Princess Martha Coast in Queen Maud Land, which Norway claims as a dependent territory. The main ice-free area of the Jutulsessen massif is about 10 km long by 5 km across.

Geographic entities mentioned:
surface_form: jutulsessen
instance_of: Mountain
coordinates: lat: -72.0333
lon: 2.68333
Jutulsessen is located in the eastern part of Princess Martha Coast in Queen Maud Land, which Norway claims as a dependent territory. The main ice-free area of the Jutulsessen massif is about 10 km long by 5 km across. The base is located above mean sea level and is completely surrounded by the Antarctic ice sheet. Jutulsessen is from the coast of King Haakon VII Sea.

Geographic entities mentioned:
surface_form: jutulsessen
instance_of: Mountain
coordinates: lat: -72.0333
lon: 2.68333
The main ice-free area of the Jutulsessen massif is about 10 km long by 5 km across. The base is located above mean sea level and is completely surrounded by the Antarctic ice sheet. Jutulsessen is from the coast of King Haakon VII Sea. The mountain area is horseshoe-shaped with a glacier and cirque of Sætet to the north. The two arms of the area are located northwards.

Geographic entities mentioned:
surface_form: jutulsessen
instance_of: Mountain
coordinates: lat: -72.0333
lon: 2.68333
It was subsequently mapped by Norwegian cartographers from surveys and air photographs taken during the Norwegian–British–Swedish Antarctic Expedition in 1949–52 and the subsequent Norwegian expedition in 1958–59. It was given the Norwegian name Jutulsessen, which means &quot;the seat of the giant&quot;. Norway established the Antarctic polar station Maudheim in 1950.

Geographic entities mentioned:
surface_form: jutulsessen
instance_of: Mountain
coordinates: lat: -72.0333
lon: 2.68333
Personal life. After &quot;Huck Finn&quot; ended, Shea attended classes at Van Nuys High School in the San Fernando Valley where he lived with his family. Shea graduated from Van Nuys High School in 1971 and, after leaving show business in 1973, began working in a patio furniture shop in Studio City, Los Angeles. In 1979, Shea became a police officer with the Los Angeles Police Department.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
&quot;Hot Stuff&quot; had a scheduled refueling stop in Iceland but crashed into Mount Fagradalsfjall near the town of Grindavík, in bad weather on May 3, 1943. Fourteen of those on board were killed, including Andrews, Brigadier general Charles H. Barth Jr. and bishop Adna Wright Leonard; only the tail gunner, George Eisel, survived.

Geographic entities mentioned:
surface_form: Fagradalsfjall
instance_of: Mountain
Plateau
countries: Iceland
coordinates: lat: 63.905
lon: -22.2725
Darney. Darney () is a commune in the Vosges department in Grand Est in northeastern France. It is located in the Vôge Plateau, around the location of the source of the river Saône. Darney is known for its forest of oak and beech trees. History. Darney is built on a promontory dominating the valley of the Saône.

Geographic entities mentioned:
surface_form: Vôge Plateau
instance_of: Plateau
countries: France
coordinates: lat: 48.05
lon: 6.25
Route. The western end of the Greek National Road 30 is in Arta, where it is connected with GR-5. It runs northeast through the sparsely populated Athamanika mountains, until it reaches the town Pyli, where it enters the Thessalian Plain. At Trikala it connects with the GR-6, and turn southeast towards Karditsa, where it turns east.

Geographic entities mentioned:
surface_form: Athamanika
instance_of: Mountain
countries: Greece
coordinates: lat: 39.483333333333
lon: 21.2
McCallin became a regular on the Limerick county football team and played one game for Limerick in the Oireachtas Cup against Kilkenny. In 1987, McCallin returned to his native Antrim, choosing to live in Cushendall in the Glens of Antrim. He played hurling with Cushendall and football with Glenravel and went on to represent Antrim masters in 1999.

Geographic entities mentioned:
surface_form: Glens of Antrim
instance_of: Valley
countries: United Kingdom
coordinates: lat: 55.16
lon: -6.1
The species typically occurs in palustrine wetlands, swamps, small to medium blackwater rivers, on deep peat in pocosins, and in small seepages with organic soils. The species is only known to occur in the Atlantic Plain, Gulf Coastal Plain, and Mississippi Embayment, though it was earlier thought to exist in the Piedmont and Southern Appalachians as well.

Geographic entities mentioned:
surface_form: Mississippi Embayment
instance_of: Valley
countries: United States
coordinates: lat: 33.751
lon: -89.681
Shuswap Highland. The Shuswap Highland is a plateau-like hilly area of in British Columbia, Canada. It spans the upland area between the Bonaparte and Thompson Plateaus from the area of Mahood Lake, at the southeast corner of the Cariboo Plateau, southeast towards the lower Shuswap River east of Vernon in the Okanagan.

Geographic entities mentioned:
surface_form: Bonaparte
instance_of: Plateau
countries: Canada
coordinates: lat: 51.15
lon: -121.283
surface_form: Thompson Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 50.25
lon: -120.5
surface_form: Mahood Lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.910443
lon: -120.399196
surface_form: Cariboo Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 50.81652
lon: -118.81904
The highland is not a unified range, but a combination of small uplands broken up by the valleys of the Clearwater, North Thompson and Adams Rivers and also by the lowlands in the southwest flanking Shuswap Lake. In that area of the valley are the towns of Falkland, Westwold, and Monte Creek along Highway 97.

Geographic entities mentioned:
surface_form: Shuswap Lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.000693
lon: -119.01263
A son of the crown prince Abbas Mirza, Morad Mirza held various governorships throughout his career, including the Khorasan province five times. He first appears in historical sources as the governor of Qaradagh during the last years of his father's life. In 1837, he was sent by his brother and suzerain, Mohammad Shah Qajar (), to suppress an uprising in the Bakhtiari region.

Geographic entities mentioned:
surface_form: Qaradagh
instance_of: Mountain
countries: Iran
coordinates: lat: 38.74
lon: 46.7
Born in 1818, Morad Mirza was a member of the ruling Qajar dynasty of Iran and the thirteenth son of Abbas Mirza, who served as crown prince until his death from illness in 1832. He first appears in sources as the governor of Qaradagh during the last years of his father's life. In 1837, his brother and suzerain Mohammad Shah Qajar () sent him to suppress an uprising in the Bakhtiari region.

Geographic entities mentioned:
surface_form: Qaradagh
instance_of: Mountain
countries: Iran
coordinates: lat: 38.74
lon: 46.7
CFB Comox. Canadian Forces Base Comox, commonly referred to as CFB Comox or 19 Wing, is a Canadian Forces base on Vancouver Island in the Comox Valley, north northeast of Comox, British Columbia.

Geographic entities mentioned:
surface_form: Comox Valley
instance_of: Valley
countries: Canada
coordinates: lat: 49.6798337
lon: -124.9694395
The base hosts a biennial air show (although not held from 2005 to 2012, or 2015 to 2024) to celebrate Canadian Forces Day. The base is also home to the Comox Air Force Museum which features several aircraft and other historical exhibits. The base is a primary employer in the Comox Valley. Facilities. The Comox Airport has a number of facilities available.

Geographic entities mentioned:
surface_form: Comox Valley
instance_of: Valley
countries: Canada
coordinates: lat: 49.6798337
lon: -124.9694395
Lake Kanaw. Lake Kanaw is a lake in Ranya District, within Sulaymaniyah Governorate, in the Kurdistan Region of northern Iraq. It is located approximately 50 km from the center of Ranya District.

Geographic entities mentioned:
surface_form: lake kanaw
instance_of: Lake
countries: Iraq
coordinates: lat: 36.214311
lon: 44.938451
The entrance to Caprock Canyons State Park is located approximately three miles north of Quitaque on Farm to Market Road 1065, and the Caprock Canyons Trailway is located just south of the town. Kent Creek flows past north of the town and Quitaque Creek is about three miles south. According to the United States Census Bureau, the city has a total area of, all land. Climate.

Geographic entities mentioned:
surface_form: Quitaque Creek
instance_of: Watercourse
countries: United States
coordinates: lat: 34.2434007
lon: -100.8412486
Their water consumption is likely through their food. Habitat and distribution. The lizard is endemic to Coachella Valley, California. The lizard is restricted to habitats with fine, windblown sand deposits in the sandy plains of the Coachella Valley, Riverside County, California. Since the 1970s, estimates of this species' habitat has decreased by about 75% due to human activities.

Geographic entities mentioned:
surface_form: Coachella Valley
instance_of: Valley
countries: United States
coordinates: lat: 33.72
lon: -116.2
Arabeya Valley. Arabeya Valley, (also known as Wadi Arabiya or Wadi Thinia Bani Aisha), is a watercourse originating from the Khachna Mountains of Algeria. It flows through the Kabylia region, eventually draining into Isser River and then into the Mediterranean Sea, passing through the Boumerdès Governorate. Watercourse.

Geographic entities mentioned:
surface_form: Isser River
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 36.8391
lon: 3.6679
Arabeya Valley channel is characterized by the absence of schist and soil materials in its bed. This feature, shared by this watercourse along with Meraldene River, Boumerdès Valley, and Isser River, allows for the extraction of sand and gravel for use in mortar and concrete preparation. Wadi Arabiya is considered a true corridor, with its width ranging between 5 meters and 600 meters.

Geographic entities mentioned:
surface_form: Meraldene River
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 36.6981116
lon: 3.5435504
surface_form: Boumerdès Valley
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 36.7117798
lon: 3.5392878
surface_form: Isser River
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 36.8391
lon: 3.6679
Wadi Arabiya is considered a true corridor, with its width ranging between 5 meters and 600 meters. It gradually slopes from its intersection with Wadi Boumerdès at Mount Bouaârous in the west, heading towards its mouth in Isser River, east of the city of Thénia. The path. Arabeya Valley runs through one coastal Algerian province. Valleys.

Geographic entities mentioned:
surface_form: Boumerdès
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 36.7117798
lon: 3.5392878
surface_form: Isser River
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 36.8391
lon: 3.6679
Arabeya Valley. Arabeya Valley, (also known as Wadi Arabiya or Wadi Thinia Bani Aisha), is a watercourse originating from the Khachna Mountains of Algeria. It flows through the Kabylia region, eventually draining into Isser River and then into the Mediterranean Sea, passing through the Boumerdès Governorate. Watercourse.

Geographic entities mentioned:
surface_form: arabeya valley
instance_of: Watercourse
countries: Algeria
Watercourse. Arabeya Valley channel is characterized by the absence of schist and soil materials in its bed. This feature, shared by this watercourse along with Meraldene River, Boumerdès Valley, and Isser River, allows for the extraction of sand and gravel for use in mortar and concrete preparation.

Geographic entities mentioned:
surface_form: arabeya valley
instance_of: Watercourse
countries: Algeria
It gradually slopes from its intersection with Wadi Boumerdès at Mount Bouaârous in the west, heading towards its mouth in Isser River, east of the city of Thénia. The path. Arabeya Valley runs through one coastal Algerian province. Valleys. Arabeya Valley intersects with several other valleys in the Boumerdès along its course through the Khachna Mountains. Dams.

Geographic entities mentioned:
surface_form: arabeya valley
instance_of: Watercourse
countries: Algeria
The path. Arabeya Valley runs through one coastal Algerian province. Valleys. Arabeya Valley intersects with several other valleys in the Boumerdès along its course through the Khachna Mountains. Dams. Arabeya Valley passes through several dams in the Boumerdès along its course through the Khachna Mountains. National roads.

Geographic entities mentioned:
surface_form: arabeya valley
instance_of: Watercourse
countries: Algeria
Valleys. Arabeya Valley intersects with several other valleys in the Boumerdès along its course through the Khachna Mountains. Dams. Arabeya Valley passes through several dams in the Boumerdès along its course through the Khachna Mountains. National roads. Arabeya Valley intersects with several national roads as it crosses the Boumerdès in the Khachna Mountains.

Geographic entities mentioned:
surface_form: arabeya valley
instance_of: Watercourse
countries: Algeria
Washington State Route 10. State Route 10 (SR 10) is a state highway in the U.S. state of Washington. The highway is a remnant of U.S. Route 10 (US 10) in Kittitas County, traveling southeast along the Yakima River from SR 970 in Teanaway to US 97 northwest of Ellensburg. SR 10 was established in 1970 as the successor to US 10 after the completion of I-90 across the Snoqualmie Pass in 1968.

Geographic entities mentioned:
surface_form: Teanaway
instance_of: Landform
countries: United States
coordinates: lat: 47.1747
lon: -120.857
Route description. SR 10 begins at an intersection with SR 970 south of DeVere Field in the unincorporated community of Teanaway in Kittitas County, southeast of Cle Elum. The highway travels southeast, parallel to a portion of the Stampede Subdivision of the BNSF Railway through the Yakima River valley and crosses over the Teanaway River before its confluence with the Yakima River.

Geographic entities mentioned:
surface_form: Teanaway
instance_of: Landform
countries: United States
coordinates: lat: 47.1747
lon: -120.857
Lizard Lake (Juan de Fuca, Vancouver Island). Lizard Lake is a lake on Vancouver Island, in British Columbia, Canada near the town of Port Renfrew. It is located in the Capital Regional District (not to be confused with Lizard Lake (Vancouver Island), a lake located to the north near the city of Port Alberni). The lake is northeast of the junction of Harris Creek and the San Juan River.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: lizard lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.13944
lon: -124.67417
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
surface_form: lizard lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.60611111111111
lon: -124.22361111111111
Lizard Lake (Juan de Fuca, Vancouver Island). Lizard Lake is a lake on Vancouver Island, in British Columbia, Canada near the town of Port Renfrew. It is located in the Capital Regional District (not to be confused with Lizard Lake (Vancouver Island), a lake located to the north near the city of Port Alberni). The lake is northeast of the junction of Harris Creek and the San Juan River.

Geographic entities mentioned:
surface_form: lizard lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.13944
lon: -124.67417
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
surface_form: lizard lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.60611111111111
lon: -124.22361111111111
It is located in the Capital Regional District (not to be confused with Lizard Lake (Vancouver Island), a lake located to the north near the city of Port Alberni). The lake is northeast of the junction of Harris Creek and the San Juan River. Lizard Lake lies at an elevation of above sea level and has a surface area of. Its mean depth is with a maximum of.

Geographic entities mentioned:
surface_form: lizard lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.13944
lon: -124.67417
surface_form: lizard lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.60611111111111
lon: -124.22361111111111
Lizard Lake lies at an elevation of above sea level and has a surface area of. Its mean depth is with a maximum of. Lizard Lake is located along the Pacific Marine Circle Route to the east of Fairy Lake, and is a popular recreation site for swimming, canoeing and camping. In 2015 a large fire near the lake led to the closure of the highway and burned more than of forest.

Geographic entities mentioned:
surface_form: lizard lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.13944
lon: -124.67417
surface_form: lizard lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.60611111111111
lon: -124.22361111111111
Cloghernagh. Cloghernagh () at, does not have the prominence to qualify as an Arderin, but does have the prominence to be the 40th–highest peak on the Vandeleur-Lynam scale. Cloghernagh is situated in the southern sector of the Wicklow Mountains range, and is part of the large massif of Lugnaquilla, Wicklow's highest mountain.

Geographic entities mentioned:
surface_form: Lugnaquilla
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.966
lon: -6.463
surface_form: cloghernagh
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.967482
lon: -6.426189
Cloghernagh forms a &quot;horseshoe&quot; around the Fraughan Rock Glen with Lugnaquillia and Benleagh, and another &quot;horseshoe shape&quot; around the glen of the Carrawaystick River with Corrigasleggaun, and the corrie lake of Kelly's Lough.

Geographic entities mentioned:
surface_form: Benleagh
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.988606
lon: -6.454103
surface_form: Corrigasleggaun
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.960568
lon: -6.441736
surface_form: lugnaquillia
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.966
lon: -6.463
surface_form: corrigasleggaun
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.960568
lon: -6.441736
surface_form: benleagh
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.988606
lon: -6.454103
surface_form: cloghernagh
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.967482
lon: -6.426189
Cloghernagh. Cloghernagh () at, does not have the prominence to qualify as an Arderin, but does have the prominence to be the 40th–highest peak on the Vandeleur-Lynam scale. Cloghernagh is situated in the southern sector of the Wicklow Mountains range, and is part of the large massif of Lugnaquilla, Wicklow's highest mountain.

Geographic entities mentioned:
surface_form: arderin
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.03805556
lon: -7.65388889
surface_form: cloghernagh
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.967482
lon: -6.426189