Sarmila/GeoWiki-Features huggingface dataset:
Topography. Binsey stands on the otherwise low-level watershed separating the catchments of the Ellen to the north and the Derwent to the south. A slight ridge connects it to Great Cockup in the main massif of the Northern Fells, two miles to the south east. Binsey itself has a rounded form, but somehow manages to impress the eye more than the similar Great Mell Fell and Little Mell Fell.

Geographic entities mentioned:
surface_form: Great Cockup
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.6895
lon: -3.12931
Topography. Binsey stands on the otherwise low-level watershed separating the catchments of the Ellen to the north and the Derwent to the south. A slight ridge connects it to Great Cockup in the main massif of the Northern Fells, two miles to the south east. Binsey itself has a rounded form, but somehow manages to impress the eye more than the similar Great Mell Fell and Little Mell Fell.

Geographic entities mentioned:
surface_form: Great Mell Fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.62
lon: -2.933
surface_form: Little Mell Fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.60785
lon: -2.8948194444444
A computer-generated summit panorama can be seen here. The furthest point visible on a clear day is the top of Slieve Donard, the highest mountain in Northern Ireland, in Mourne, 115 miles (185 km) away. Geology. The hill is formed from volcanic rocks, namely various sub-units of the Eycott Volcanic Group, which consists of basaltic andesite, andesite and rhyolitic lavas.

Geographic entities mentioned:
surface_form: Slieve Donard
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.180277777778
lon: -5.9208333333333
Tobaru. Mount Tobaru or Mount Lolodai is located in the northern part of Halmahera island, west of Dukono volcano. Little is known about this volcano because of its remote location.

Geographic entities mentioned:
surface_form: Dukono
instance_of: Mountain
countries: Indonesia
coordinates: lat: 1.699505
lon: 127.878105
surface_form: mount tobaru
instance_of: Mountain
countries: Indonesia
coordinates: lat: 1.63
lon: 127.67
surface_form: lolodai
instance_of: Mountain
countries: Indonesia
coordinates: lat: 1.63
lon: 127.67
surface_form: tobaru
instance_of: Mountain
countries: Indonesia
coordinates: lat: 1.63
lon: 127.67
Tobaru. Mount Tobaru or Mount Lolodai is located in the northern part of Halmahera island, west of Dukono volcano. Little is known about this volcano because of its remote location.

Geographic entities mentioned:
surface_form: tobaru
instance_of: Mountain
countries: Indonesia
coordinates: lat: 1.63
lon: 127.67
(There is even a unique species of aloe, the Table Mountain Aloe, which is also endemic to Table Mountain's Peninsula Sandstone Fynbos.)
The variety of tall Protea species are particularly striking and noticeable and are especially common growing in the rough sands of wetter spots.

Geographic entities mentioned:
surface_form: Table Mountain
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
In areas which are protected from seasonal fires, such as river valleys, the Fynbos is replaced by dense, indigenous Afrotemperate forest. Natural distribution. This is the predominant vegetation type of the higher parts of the Cape Peninsula, from the face of Table Mountain in the north, southwards as far as Cape Point.

Geographic entities mentioned:
surface_form: Table Mountain
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
Insect paleobiota of Burmese amber. Burmese amber is fossil resin dating to the early Late Cretaceous Cenomanian age recovered from deposits in the Hukawng Valley of northern Myanmar. It is known for being one of the most diverse Cretaceous age amber paleobiotas, containing rich arthropod fossils, along with uncommon vertebrate fossils and even rare marine inclusions.

Geographic entities mentioned:
surface_form: Hukawng Valley
instance_of: Valley
countries: Myanmar
coordinates: lat: 26.438333333333
lon: 96.558888888889
Biography. Nairi Zarian was born on December 31, 1900, in the village of Karagündüz (called Kharakonis by its Armenian inhabitants), near Lake Erçek, in the Van Vilayet of the Ottoman Empire. His parents, Yeghiazar and Hourig Yeghiazaryan, were farmers. Zarian received his early education at the local parish school, Saint Theodoros.

Geographic entities mentioned:
surface_form: Lake Erçek
instance_of: Lake
countries: Turkey
coordinates: lat: 38.6717
lon: 43.5783
Port Essington, British Columbia. Port Essington was a cannery town on the south bank of the Skeena River estuary in northwestern British Columbia, Canada, between Prince Rupert and Terrace, and at the confluence of the Skeena and Ecstall Rivers.

Geographic entities mentioned:
surface_form: Ecstall
instance_of: Watercourse
countries: Canada
coordinates: lat: 54.15836
lon: -129.94543
History. In 1871, at the height of the Omineca Gold Rush, one route to the new goldfields led up the Skeena River to Hazelton, overland to Babine Lake and on to the Omineca River. The Provincial Government granted Robert Cunningham and Thomas Hankin the right to build a toll road from Hazelton to Babine Lake, while William Moore was placed in charge of the running pack mules on the trail.

Geographic entities mentioned:
surface_form: Babine Lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.75
lon: -126
Background. After the Chilean occupation of Calama, in March 1879, and other Bolivian villages in the Atacama Desert, by the military contingents, the so-called “Loa Line” was established; with the objective of preventing a Bolivian offensive from the Altiplano and controlling the Litoral Department.

Geographic entities mentioned:
surface_form: Altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
Caldwell died on December 10, 1967, aged 18, of a plane crash in Lake Monona with Redding and three other band members (Phalon Jones, Carl Cunningham and Jimmie King), their valet Matthew Kelly and the pilot Richard Fraser while on their way to a performance in Madison, Wisconsin. Caldwell is interred in the Memorial Park Cemetery in Memphis.

Geographic entities mentioned:
surface_form: Lake Monona
instance_of: Lake
countries: United States
coordinates: lat: 43.069166666667
lon: -89.359444444444
The museum and its collection was added to as a National Monument (&quot;Monument Istoric&quot;) in 2004 with an LMI code of CS-II-a-A-10905. In 2013, the &quot;Resicza&quot; lost out to the Danube Gorge to become the regional symbol of the Romanian Banat for European Cooperation Day, which is yearly on September 21. &quot;RESICZA&quot; – Romania's first locomotive.

Geographic entities mentioned:
surface_form: Danube Gorge
instance_of: Valley
countries: Serbia
Romania
coordinates: lat: 44.671111111111
lon: 22.529722222222
More than 30,000 Buddhist statues from the time of this dynasty have been found in the caves. Many of these sculptures were two-faced. At the same time, the Shaolin Temple was also built by the Emperor to accommodate an Indian monk on the Mount Song right next to Luoyang City. The Yongning Temple (), the tallest pagoda in China, was also built in Luoyang.

Geographic entities mentioned:
surface_form: Mount Song
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 34.484722222222
lon: 112.96027777778
Savić commanded the Garda Panteri (), which was later incorporated as a special unit in the armed forces of the Republika Srpska. The unit, initially called the &quot;Serbian National Guard of SAO Semberija and Majevica,&quot; was renamed to the &quot;Garda Panteri&quot; by Savić in honor of the commander preceding him, Branko Pantelić, who was killed in action in September 1992.

Geographic entities mentioned:
surface_form: Semberija
instance_of: Landform
countries: Bosnia and Herzegovina
coordinates: lat: 44.80083333
lon: 19.21361111
There are many islands on the lake with total area of 186 km2. Among the rivers that flow into lake Pyaozero is the river Oulankajoki that begins in Finland, where one of its tributaries is the river Kitkanjoki that begins from lake Kitkajärvi in Finland. From south also the waters of Lake Topozero in the Republic of Karelia flow into the Lake Pyaozero.

Geographic entities mentioned:
surface_form: Kitkajärvi
instance_of: Lake
countries: Finland
coordinates: lat: 66.1283503
lon: 28.587218
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: pyaozero
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 66.083333333333
lon: 30.966666666667
surface_form: lake pyaozero
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 66.083333333333
lon: 30.966666666667
There are many islands on the lake with total area of 186 km2. Among the rivers that flow into lake Pyaozero is the river Oulankajoki that begins in Finland, where one of its tributaries is the river Kitkanjoki that begins from lake Kitkajärvi in Finland. From south also the waters of Lake Topozero in the Republic of Karelia flow into the Lake Pyaozero.

Geographic entities mentioned:
surface_form: Lake Topozero
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 65.65
lon: 32
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: topozero
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 65.65
lon: 32
surface_form: pyaozero
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 66.083333333333
lon: 30.966666666667
surface_form: lake pyaozero
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 66.083333333333
lon: 30.966666666667
Lake Pyaozero. Lake Pyaozero (,) is a large freshwater lake in the Republic of Karelia, northwestern part of Russia. It has an area of 659 km2, and it is drained by the river Kovda. There are many islands on the lake with total area of 186 km2.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: pyaozero
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 66.083333333333
lon: 30.966666666667
surface_form: lake pyaozero
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 66.083333333333
lon: 30.966666666667
Lake Pyaozero. Lake Pyaozero (,) is a large freshwater lake in the Republic of Karelia, northwestern part of Russia. It has an area of 659 km2, and it is drained by the river Kovda. There are many islands on the lake with total area of 186 km2.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: pyaozero
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 66.083333333333
lon: 30.966666666667
surface_form: lake pyaozero
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 66.083333333333
lon: 30.966666666667
It has an area of 659 km2, and it is drained by the river Kovda. There are many islands on the lake with total area of 186 km2. Among the rivers that flow into lake Pyaozero is the river Oulankajoki that begins in Finland, where one of its tributaries is the river Kitkanjoki that begins from lake Kitkajärvi in Finland.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
Eisberg (Eastern Upper Lusatia). Eisberg () is a mountain of Saxony, southeastern Germany.

Geographic entities mentioned:
surface_form: eisberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.9916
lon: 14.7833
surface_form: eisberg
instance_of: Mountain
countries: Germany
coordinates: lat: 49.5405
lon: 12.4029
surface_form: eisberg
instance_of: Mountain
countries: Germany
coordinates: lat: 47.6259
lon: 12.8473
surface_form: eisberg
instance_of: Mountain
countries: Germany
coordinates: lat: 51.1464
lon: 9.77528
Serbia is mountainous, with complex geology and parts of several mountain ranges: Dinaric Alps in the southwest, the northwestern corner of the Rila-Rhodope Mountains in the southeast of the country, Carpathian Mountains in the northeast, and Balkan Mountains and the easternmost section of Srednogorie mountain chain system in the east, separated by a group of dome mountains along the Morava river valley.

Geographic entities mentioned:
surface_form: easternmost section
instance_of: Mountain
countries: Serbia
coordinates: lat: 42.9867
lon: 22.5878
surface_form: dome mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 58.4535
lon: -129.63516666667
Aeaea was later identified by classical Roman writers with Mount Circeo on Cape Circeo (Cape Circaeum) on the western coast of Italy – about 100 kilometers south of Rome – which at that time may have looked like an island owing to the marshes and sea surrounding its base, but which now is a small peninsula. Dionysius of Halicarnassus wrote that it was already a peninsula in his time.

Geographic entities mentioned:
surface_form: Mount Circeo
instance_of: Mountain
countries: Italy
coordinates: lat: 41.23109
lon: 13.05553
For its conduct at Jamiano and Flondar the 7th Bersaglieri Regiment was awarded a Silver Medal of Military Valor, which was affixed to the regiment's flag and added to the regiment's coat of arms. In October 1917 the brigade fought in the Battle of Caporetto on Monte Piana and on Mauria Pass.

Geographic entities mentioned:
surface_form: Monte Piana
instance_of: Mountain
countries: Italy
coordinates: lat: 46.61527778
lon: 12.23944444
priscus&quot;, named in 1830 and described in 2020. The holotype of &quot;Aeolodon priscus&quot; was found in the Mörnsheim Formation of Daiting, Bavaria, Germany, in the same quarry that produced the &quot;Geosaurus giganteus&quot; holotype and the assigned specimen was discovered in the Canjuers conservation Lagerstätte of Var, France.

Geographic entities mentioned:
surface_form: Canjuers
instance_of: Plateau
countries: France
coordinates: lat: 43.70833333
lon: 6.30833333
Edwards Plateau. The Edwards Plateau is a geographic region forming the crossroads of Central, South and West Texas, United States. It is named in honor of Haden Edwards. It is bounded by the Balcones Fault to the south and east; the Llano Uplift and the Llano Estacado to the north; and the Pecos River and Chihuahuan Desert to the west.

Geographic entities mentioned:
surface_form: edwards plateau
instance_of: Plateau
countries: United States
coordinates: lat: 30.3
lon: -99.6
The Balcones Fault zone which runs along the southern and eastern edge of the plateau is an ecological demarcation for the ranges of a number of species. Fauna. Caves of the Edwards Plateau are important habitats for wildlife and for many endemic species. The area is home to some of the largest colonies of bats in the world, including millions of Mexican free-tailed bats.

Geographic entities mentioned:
surface_form: edwards plateau
instance_of: Plateau
countries: United States
coordinates: lat: 30.3
lon: -99.6
The Edwards Plateau is home to at least 14 endemic freshwater fishes, including two subterranean species of catfish and 13 fish species considered to be spring-associated. Mechanisms for spring association of fishes is not fully understood, but thought to mediated by water temperature.

Geographic entities mentioned:
surface_form: edwards plateau
instance_of: Plateau
countries: United States
coordinates: lat: 30.3
lon: -99.6
After the expulsion of the Apachean groups from the Plains by the Comanche, this area was dominated by the Penateka band of the Southern Comanche. Counties in the Edwards Plateau. A map showing the counties is provided by Texas Parks and Wildlife Department for the Edwards Plateau Ecoregion.

Geographic entities mentioned:
surface_form: edwards plateau
instance_of: Plateau
countries: United States
coordinates: lat: 30.3
lon: -99.6
The ecoregion is somewhat larger than the geographic region, as the map from Texas Parks And Wildlife includes additional counties that are listed by the Texas Water Development Board, notably the isolated area of Edwards Plateau in Taylor, Runnels, and Nolan Counties that is separated from the main region.

Geographic entities mentioned:
surface_form: edwards plateau
instance_of: Plateau
countries: United States
coordinates: lat: 30.3
lon: -99.6
Llyn Bedydd. Llyn Bedydd is a small lake in Wrexham County Borough, in northeastern Wales, near the border with England. It is south west of Whitchurch. The lake and the surrounding woodland are designated as a Site of Special Scientific Interest. Description. Llyn Bedydd means the &quot;lake of Beda&quot;, the identity of Beda is however not known.

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
The thin fringing strip of fen supports other interesting plants, especially sedges. The fen creates a tussocky species rich floating mat at the southern end of the lake while on the land in the southeastern corner of the SSSI there is a small area of fen pasture which grades into a bog.

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
Llyn Bedydd. Llyn Bedydd is a small lake in Wrexham County Borough, in northeastern Wales, near the border with England. It is south west of Whitchurch. The lake and the surrounding woodland are designated as a Site of Special Scientific Interest. Description. Llyn Bedydd means the &quot;lake of Beda&quot;, the identity of Beda is however not known.

Geographic entities mentioned:
surface_form: llyn bedydd
instance_of: Lake
countries: United Kingdom
coordinates: lat: 52.946187
lon: -2.79003
The lake and the surrounding woodland are designated as a Site of Special Scientific Interest. Description. Llyn Bedydd means the &quot;lake of Beda&quot;, the identity of Beda is however not known. Llyn Bedydd is in area and is surrounded by carr woodland of willow and alder which merges into drier deciduous woodland dominated by downy birch and sycamore higher up the slope. Flora and fauna.

Geographic entities mentioned:
surface_form: llyn bedydd
instance_of: Lake
countries: United Kingdom
coordinates: lat: 52.946187
lon: -2.79003
surface_form: llyn bedydd
instance_of: Lake
countries: United Kingdom
coordinates: lat: 52.946187
lon: -2.79003
Flora and fauna. The wet carr around the Llyn Bedydd is notable for purple small reed and alder buckthorn which are very rare in Clwyd; tufted sedge and bay willow which are uncommon in Clwyd; and the nationally scarce cowbane. The thin fringing strip of fen supports other interesting plants, especially sedges.

Geographic entities mentioned:
surface_form: llyn bedydd
instance_of: Lake
countries: United Kingdom
coordinates: lat: 52.946187
lon: -2.79003
Llyn Beddyd is relatively shallow but it has steeply shelving banks which are shaded by the woodlands and these restrict the development of stands of emergent and marginal vegetation. Llyn Bedydd is supports a rich invertebrate fauna, species recorded include the nationally scarce variable damselfly and the local red-eyed damselfly.

Geographic entities mentioned:
surface_form: llyn bedydd
instance_of: Lake
countries: United Kingdom
coordinates: lat: 52.946187
lon: -2.79003
Llyn Bedydd is supports a rich invertebrate fauna, species recorded include the nationally scarce variable damselfly and the local red-eyed damselfly. Llyn Bedydd contains common bream, common rudd, common carp, European perch, tench and common roach. The fishing is run by Warners Fishing Club. Archaeology. In 1877 a logboat was found in the Llyn Bedydd.

Geographic entities mentioned:
surface_form: llyn bedydd
instance_of: Lake
countries: United Kingdom
coordinates: lat: 52.946187
lon: -2.79003
Elena Fanchini. Elena Fanchini (30 April 1985 – 8 February 2023) was an Italian World Cup alpine ski racer. Born in Val Camonica, she focused on the speed events of downhill and super-G. Her younger sisters Nadia and Sabrina also raced on the Italian team. Biography. Fanchini won two World Cup races in downhill 9 years apart and won a silver medal at the 2005 world championships.

Geographic entities mentioned:
surface_form: Val Camonica
instance_of: Valley
countries: Italy
coordinates: lat: 46.0075
lon: 10.3475
Lakes of Temagami. There are more than 200 named lakes located partially or entirely within the Municipality of Temagami, Northeastern Ontario, Canada. They are located in all 25 geographic townships comprising this municipality. The largest, by both area and volume, is Lake Temagami. It contains more than 1,200 islands and of shoreline.

Geographic entities mentioned:
surface_form: Lake Temagami
instance_of: Lake
countries: Canada
coordinates: lat: 46.95
lon: -80.0833
The largest, by both area and volume, is Lake Temagami. It contains more than 1,200 islands and of shoreline. Other significant lakes include Cross Lake, Gull Lake, Net Lake, Obabika Lake and Rabbit Lake. Temagami's lakes are situated in two watersheds. To the east, the Ottawa River basin drains lake water via the Matabitchuan River, which flows into Lake Timiskaming then enters the Ottawa River.

Geographic entities mentioned:
surface_form: Net Lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.113
lon: -79.804
Temagami's lakes are situated in two watersheds. To the east, the Ottawa River basin drains lake water via the Matabitchuan River, which flows into Lake Timiskaming then enters the Ottawa River. The Great Lakes Basin to the west drains lake water via the Sturgeon River which flows into Lake Nipissing then enters the French River, eventually reaching Georgian Bay of Lake Huron.

Geographic entities mentioned:
surface_form: Lake Timiskaming
instance_of: Lake
countries: Canada
coordinates: lat: 47.333333333333
lon: -79.5
Temagami's lakes are situated in two watersheds. To the east, the Ottawa River basin drains lake water via the Matabitchuan River, which flows into Lake Timiskaming then enters the Ottawa River. The Great Lakes Basin to the west drains lake water via the Sturgeon River which flows into Lake Nipissing then enters the French River, eventually reaching Georgian Bay of Lake Huron.

Geographic entities mentioned:
surface_form: Lake Nipissing
instance_of: Lake
countries: Canada
coordinates: lat: 46.283333333333
lon: -80
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
Papaqucha (Lima). Papaqucha (Quechua &quot;papa&quot; potato, &quot;qucha&quot; lake, &quot;potato lake&quot;, hispanicized spelling &quot;Papacocha&quot;) is a lake in Peru located in the Lima Region, Yauyos Province, Huancaya District. It lies at the Cañete River, near the town of Vilca.

Geographic entities mentioned:
surface_form: papacocha
instance_of: Lake
countries: Peru
coordinates: lat: -12.7339
lon: -75.5233
surface_form: papaqucha
instance_of: Lake
countries: Peru
coordinates: lat: -12.7339
lon: -75.5233
Papaqucha (Lima). Papaqucha (Quechua &quot;papa&quot; potato, &quot;qucha&quot; lake, &quot;potato lake&quot;, hispanicized spelling &quot;Papacocha&quot;) is a lake in Peru located in the Lima Region, Yauyos Province, Huancaya District. It lies at the Cañete River, near the town of Vilca.

Geographic entities mentioned:
surface_form: papaqucha
instance_of: Lake
countries: Peru
coordinates: lat: -12.7339
lon: -75.5233
surface_form: papaqucha (lima)
instance_of: Lake
countries: Peru
coordinates: lat: -12.1083
lon: -75.8342
Paksong. Paksong is a city in Laos on the Bolaven Plateau. The city is known for its coffee exports. It is the capital of Paksong District.

Geographic entities mentioned:
surface_form: Bolaven Plateau
instance_of: Mountain
countries: Laos
coordinates: lat: 15.11
lon: 106.44
Geography. According to the United States Census Bureau, the town has a total area of, of which is land and (1.94%) is water. The northern town line is the border of Vermont. The Champlain Canal passes through the western section of the town. The South Bay of Lake Champlain forms part of the western town line. Conjoined U. S. Route 4 and NY Route 22 form a north–south highway through Whitehall.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
Bolthouse Farms. Bolthouse Farms, founded 1915 in Grant, Michigan, is a vertically integrated farm company specializing in refrigerated beverages, salad dressings, and baby carrots. It is located in the San Joaquin Valley of California and is headquartered in Bakersfield, California in Kern County. The company operates facilities in Prosser, Washington.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
The station was located in Gresham, Oregon just east of Portland and its transmitter (translator) antenna was located in the west hills of Portland, reaching most of the Portland-area Willamette Valley and to most of greater Vancouver, Washington and Clark County just across the Columbia River. Its former FM stereo broadcasting signal had 28 watts of power. KZME also streamed on the internet.

Geographic entities mentioned:
surface_form: Willamette Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.9
lon: -123.1
Different communities have developed their own variations, and rural areas still follow centuries-old cooking methods and recipes. Coastal Andhra. Coastal Andhra is dominated by the Krishna and Godavari river delta regions and is adjacent to the Bay of Bengal. This proximity to water has led to rice, lentils, and seafood becoming dietary staples in the region.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
The bottom lock is just above the junction, and Leys Junction is just above the top lock. From here, the Fens Branch is a short, navigable feeder from Fens Pools and the main canal continues for to Delph Locks, a flight at the start of the Dudley Canal, which originally consisted of nine locks, but was rebuilt as eight in 1858.

Geographic entities mentioned:
surface_form: Fens Pools
instance_of: Group of lakes
countries: United Kingdom
coordinates: lat: 52.4953
lon: -2.11926
Due to his civil engineering education, Ellis contracted out much of the work to Giddings. The next year, Giddings was contracted for twelve more surveys at the headwaters of the Rock River, in what is now northern Dodge County and western Fond du Lac County. He then surveyed all the land between Lake Winnebago and the Wolf River, comprising much of present-day Winnebago County.

Geographic entities mentioned:
surface_form: Lake Winnebago
instance_of: Lake
countries: United States
coordinates: lat: 44.0169756
lon: -88.4095327
In 1967 he became a vice-chairman of the Beijing Revolutionary Committee, and was elected member of the CCP Central Committee in 1969. As Mao Zedong clashed with Lin Biao and Chen Boda at the Central Committee plenum held in Lushan in 1970, Wu De advised him to act swiftly in order to avoid trouble within the People's Liberation Army. He said: &quot;The Chairman must act personally...

Geographic entities mentioned:
surface_form: Lushan
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 29.5725
lon: 115.97333333333
Marcahuasi. Marcahuasi () is a plateau in the Andes Mountains, located 60 km east of Lima, on the mountain range that rises to the right bank of the Rímac River. The site is located at above sea level and is known for its unusual geological formations; curious shapes of human faces and animals visible in granite rock. Research. The place was first investigated by Julio Tello in 1922.

Geographic entities mentioned:
surface_form: Rímac River
instance_of: Watercourse
countries: Peru
coordinates: lat: -12.032222222222
lon: -77.141111111111
surface_form: marcahuasi
instance_of: Plateau
countries: Peru
coordinates: lat: -11.7889
lon: -76.5736
Marcahuasi. Marcahuasi () is a plateau in the Andes Mountains, located 60 km east of Lima, on the mountain range that rises to the right bank of the Rímac River. The site is located at above sea level and is known for its unusual geological formations; curious shapes of human faces and animals visible in granite rock. Research. The place was first investigated by Julio Tello in 1922.

Geographic entities mentioned:
surface_form: marcahuasi
instance_of: Plateau
countries: Peru
coordinates: lat: -11.7889
lon: -76.5736
It is about in area, and sits at an elevation of almost in Huarochirí Province, east of Lima, Peru. Marcahuasi is home to a unique set of huge granite rocks with curious shapes resembling human faces, animals, and religious symbols. There are many theories as to their origins, including the assertion that their unusual shapes formed naturally through erosion.

Geographic entities mentioned:
surface_form: marcahuasi
instance_of: Plateau
countries: Peru
coordinates: lat: -11.7889
lon: -76.5736
There were once 4,077 lakes. Global climate change is responsible for the reduction in flow of the (Huang He) Yellow River over the past several decades. The source of the Yellow River is the Qinghai-Xizang Tibetan plateau where the glaciers are receding sharply. In Hebei, which surrounds Beijing, the situation is much worse. Hebei is one of China's major wheat and corn growing provinces.

Geographic entities mentioned:
surface_form: Tibetan plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
Kazakhstan and Uzbekistan. The two rivers feeding the Aral Sea were dammed up and the water was diverted to irrigate the desert so that cotton could be produced. As a result, the Aral Sea's water has become much saltier and the sea's water level has decreased by over 60%. Drinking water is now contaminated with pesticides and other agricultural chemicals and contains bacteria and viruses.

Geographic entities mentioned:
surface_form: Aral Sea
instance_of: Lake
countries: Kazakhstan
Uzbekistan
Russian Empire
Soviet Union
coordinates: lat: 45
lon: 60
Mount Sir Sandford. Mount Sir Sandford is the highest mountain of the Sir Sandford Range and the highest mountain in the Selkirk Mountains of southeastern British Columbia, Canada. It is the 12th highest peak in the province. The mountain was named after Sir Sandford Fleming, a railway engineer for the Canadian Pacific Railway.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mount sir sandford
instance_of: Mountain
countries: Canada
coordinates: lat: 51.656666666667
lon: -117.8675
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
Mount Sir Sandford. Mount Sir Sandford is the highest mountain of the Sir Sandford Range and the highest mountain in the Selkirk Mountains of southeastern British Columbia, Canada. It is the 12th highest peak in the province. The mountain was named after Sir Sandford Fleming, a railway engineer for the Canadian Pacific Railway.

Geographic entities mentioned:
surface_form: mount sir sandford
instance_of: Mountain
countries: Canada
coordinates: lat: 51.656666666667
lon: -117.8675
It is the 12th highest peak in the province. The mountain was named after Sir Sandford Fleming, a railway engineer for the Canadian Pacific Railway. The mountain was first summited in 1912 after several attempts in prior years by a party of four, led by Edward W. D. Holway and including Howard Palmer, Edward Feuz Jr. and Rudolph Aemmer.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
cohenae&quot;), Smithers's horseshoe bat (&quot;R. smithersi&quot;), and the Mozambican horseshoe bat (&quot;R. mossambicus&quot;). The holotype for the Mount Mabu horseshoe bat had been collected on Mount Mabu in October 2008. Range and habitat. As of 2019, the species has only been documented at two sites in northern Mozambique: Mount Mabu and Mount Inago.

Geographic entities mentioned:
surface_form: Mount Mabu
instance_of: Mountain
countries: Mozambique
coordinates: lat: -16.298888888889
lon: 36.395555555556
mossambicus&quot;). The holotype for the Mount Mabu horseshoe bat had been collected on Mount Mabu in October 2008. Range and habitat. As of 2019, the species has only been documented at two sites in northern Mozambique: Mount Mabu and Mount Inago. All specimens collected as of 2012 were found in montane forests or submontane forests. Conservation.

Geographic entities mentioned:
surface_form: Mount Mabu
instance_of: Mountain
countries: Mozambique
coordinates: lat: -16.298888888889
lon: 36.395555555556
Wampar Rural LLG. Wampar Rural LLG is a local-level government (LLG) located in the Markham Valley of Morobe Province, Papua New Guinea. The Wampar language is spoken in the LLG, along with Labu, Yalu (Aribwaung), Watut, and other Markham languages.

Geographic entities mentioned:
surface_form: Markham Valley
instance_of: Valley
countries: Papua New Guinea
coordinates: lat: -6.7388888888889
lon: 146.96805555556
Spitzmauer. With its summit at above sea level, the Spitzmauer (lit. translatable as &quot;sharp/steep wall&quot;) is the second highest mountain of the Totes Gebirge mountain range in the south of Upper Austria. A Dachstein Formation, the mountain was first touristically climbed by Vienna botanist Karl Stoitzner, school teacher H.

Geographic entities mentioned:
surface_form: spitzmauer
instance_of: Mountain
countries: Austria
coordinates: lat: 47.695495
lon: 14.062151
During the 1950s, Mottar accompanied University of Arkansas folklorist Mary Celestia Parler undertaking the Folklore Research Project (1949–1965). The photographs feature Mary Celestia Parler and others active in collecting folklore, as well as the subjects of Ozark folklore studies. Overseas commissions.

Geographic entities mentioned:
surface_form: Ozark
instance_of: Plateau
countries: United States
coordinates: lat: 37.1822
lon: -92.5159
Parkville is known for its antique shops, art galleries, and historic downtown. The city is home to Park University, English Landing Park, Platte Landing Park, and the National Golf Club of Kansas City. Large neighborhoods in Parkville include: Riss Lake, The National, Thousand Oaks, Creekside, Parkville Heights, River Hills, Riverchase, The Bluffs, Downtown, and Pinecrest. History.

Geographic entities mentioned:
surface_form: Riss Lake
instance_of: Lake
countries: United States
coordinates: lat: 39.199444444444
lon: -94.677222222222
Lago di San Casciano. Lago di San Casciano is a lake in the Province of Siena, Tuscany, Italy. At an elevation of 383 m, its surface area is 2 km2. Geography. The lake is located in south of the municipality of San Casciano dei Bagni, near the borders with Lazio and the village of Trevinano.

Geographic entities mentioned:
surface_form: lago di san casciano
instance_of: Lake
countries: Italy
coordinates: lat: 42.839771
lon: 11.849613
El Capitan. El Capitan (;) is a vertical rock formation in Yosemite National Park, on the north side of Yosemite Valley, near its western end. The granite monolith is about from base to summit along its tallest face and is a world-famous location for big wall climbing, including the disciplines of aid climbing, free climbing, and more recently for free solo climbing.

Geographic entities mentioned:
surface_form: Yosemite Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
The granite monolith is about from base to summit along its tallest face and is a world-famous location for big wall climbing, including the disciplines of aid climbing, free climbing, and more recently for free solo climbing. The top of El Capitan can be reached by hiking out of Yosemite Valley on the trail next to Yosemite Falls, then proceeding west.

Geographic entities mentioned:
surface_form: Yosemite Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
Geology. El Capitan is composed almost entirely of a pale, coarse-grained granite approximately 100 MYA (million years old). In addition to El Capitan, this granite forms most of the rock features of the western portions of Yosemite Valley. A separate intrusion of igneous rock, the Taft Granite, forms the uppermost portions of the cliff face.

Geographic entities mentioned:
surface_form: Yosemite Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
A separate intrusion of igneous rock, the Taft Granite, forms the uppermost portions of the cliff face. A third igneous rock, diorite, is present as dark-veined intrusions through both kinds of granite, especially prominent in the area known as the North America Wall. Along with most of the other rock formations of Yosemite Valley, El Capitan was carved by glacial action.

Geographic entities mentioned:
surface_form: Yosemite Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
Greenville Junction, Maine. Greenville Junction is an unincorporated village in the town of Greenville, Piscataquis County, Maine, United States. The community is located along Maine State Route 6 and the south shore of Moosehead Lake, northwest of Dover-Foxcroft. Greenville Junction has a post office, with ZIP code 04442.

Geographic entities mentioned:
surface_form: Moosehead Lake
instance_of: Lake
countries: United States
coordinates: lat: 45.633333333333
lon: -69.65
Easedale Tarn is a tarn in the centre of the English Lake District, about two miles west of the village of Grasmere. It lies in a hollow between Tarn Crag to the north and Blea Rigg to the south, about 910 feet or 280 metres above sea level. The hollow was formed by a small corrie glacier, and is believed to have filled with water around 11,000 years ago when the ice finished melting.

Geographic entities mentioned:
surface_form: Blea Rigg
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4608
lon: -3.07827
surface_form: tarn crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.463
lon: -2.787
surface_form: tarn crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.473
lon: -3.076
Easedale Tarn. Easedale Tarn is a tarn in the centre of the English Lake District, about two miles west of the village of Grasmere. It lies in a hollow between Tarn Crag to the north and Blea Rigg to the south, about 910 feet or 280 metres above sea level.

Geographic entities mentioned:
surface_form: grasmere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.449383
lon: -3.021239
surface_form: easedale tarn
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.4695
lon: -3.0696
Easedale Tarn is one of the larger tarns in the district, about long and wide. Its outflow is Sourmilk Gill, named after the milky white colour of its waterfalls, which runs east towards Grasmere. The gill displays impressive water scenery when seen from Grasmere, and from the path to the tarn. The tarn is a popular destination for walkers.

Geographic entities mentioned:
surface_form: grasmere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.449383
lon: -3.021239
The tarn is a popular destination for walkers. Many people climb the path from Grasmere which overlooks Sourmilk Gill. The ascent was popular during the Victorian period, and a refreshment hut was even established in the 19th century by Robert Hayton of Grasmere above the outlet of the tarn to service the thirsty visitors. The hut is long gone, and nettles now grow where the ruins used to be.

Geographic entities mentioned:
surface_form: grasmere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.449383
lon: -3.021239
Easedale Tarn. Easedale Tarn is a tarn in the centre of the English Lake District, about two miles west of the village of Grasmere. It lies in a hollow between Tarn Crag to the north and Blea Rigg to the south, about 910 feet or 280 metres above sea level.

Geographic entities mentioned:
surface_form: easedale tarn
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.4695
lon: -3.0696
The hollow was formed by a small corrie glacier, and is believed to have filled with water around 11,000 years ago when the ice finished melting. Easedale Tarn is one of the larger tarns in the district, about long and wide. Its outflow is Sourmilk Gill, named after the milky white colour of its waterfalls, which runs east towards Grasmere.

Geographic entities mentioned:
surface_form: easedale tarn
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.4695
lon: -3.0696
With the construction of taimu international airport in future, fuding will be more and more open to the outside world. Taimu Mountain. The Taimu Mountain are one of the more famous tourist spots. Known as the &quot;wonderland on the sea&quot;, it sports many high and steep mountains, spectacular rock formations, secluded caves, a foggy climate, and additional rivers and parks. Dayushan Island.

Geographic entities mentioned:
surface_form: Taimu Mountain
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 27.1244
lon: 120.182
He married in 2001 and, as of 2007, lives in Canada. His work was exhibited at the Comox Valley Art Gallery in 1998, at the Alcheringa Gallery in 2001, and at the Washington State University's Department of Fine Arts in 2007. Lianga's art has also been featured on the cover of the autumn 2004 edition of &quot;The Contemporary Pacific&quot;.

Geographic entities mentioned:
surface_form: Comox Valley
instance_of: Valley
countries: Canada
coordinates: lat: 49.6798337
lon: -124.9694395
Black Dome Mountain. Black Dome Mountain is the northernmost summit of the Camelsfoot Range, which lies along the west side of the Fraser River, north of Lillooet, British Columbia, Canada. It is an ancient butte-like volcano located in the formation known as the Chilcotin Group, which lie between the Pacific Ranges of the Coast Mountains and the mid-Fraser River in British Columbia, Canada.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: black dome mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.3319
lon: -122.485
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: dome mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 58.4535
lon: -129.63516666667
Black Dome Mountain is the northernmost summit of the Camelsfoot Range, which lies along the west side of the Fraser River, north of Lillooet, British Columbia, Canada. It is an ancient butte-like volcano located in the formation known as the Chilcotin Group, which lie between the Pacific Ranges of the Coast Mountains and the mid-Fraser River in British Columbia, Canada. Location and terrain.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
The Churn Creek Protected Area adjoins the north and western flanks of the mountain, while the Fraser Canyon runs southward along its eastern flank. Geology. Like other volcanic landforms in British Columbia, Black Dome Mountain is part of the Pacific Ring of Fire which includes over 160 active volcanoes. There are obsidian deposits and other deposits around the volcano.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: black dome mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.3319
lon: -122.485
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: dome mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 58.4535
lon: -129.63516666667
Black Dome Mountain. Black Dome Mountain is the northernmost summit of the Camelsfoot Range, which lies along the west side of the Fraser River, north of Lillooet, British Columbia, Canada. It is an ancient butte-like volcano located in the formation known as the Chilcotin Group, which lie between the Pacific Ranges of the Coast Mountains and the mid-Fraser River in British Columbia, Canada.

Geographic entities mentioned:
surface_form: black dome mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.3319
lon: -122.485
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: dome mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 58.4535
lon: -129.63516666667
There are obsidian deposits and other deposits around the volcano. It has produced olivine basalt dykes, lavas, and agglomerate. Black Dome Mountain is thought to have formed as a result of extension of the crust behind the Cascadia subduction zone and last erupted during the Pliocene. History. During the early 1950s, Black Dome Mountain was the site of gold mining prospects by Bralorne Mines Inc.

Geographic entities mentioned:
surface_form: black dome mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.3319
lon: -122.485
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: dome mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 58.4535
lon: -129.63516666667
Black Dome Mountain is thought to have formed as a result of extension of the crust behind the Cascadia subduction zone and last erupted during the Pliocene. History. During the early 1950s, Black Dome Mountain was the site of gold mining prospects by Bralorne Mines Inc. and produced a bit of an excitement for people that lived near the mountain.

Geographic entities mentioned:
surface_form: black dome mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.3319
lon: -122.485
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: dome mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 58.4535
lon: -129.63516666667
Black Dome is located in the angle of Churn Creek and the Fraser Canyon, southwest of Dog Creek Bridge at Gang Ranch. It is the northernmost summit of the Camelsfoot Range, which lines the west bank of the Fraser north of Lillooet. The Churn Creek Protected Area adjoins the north and western flanks of the mountain, while the Fraser Canyon runs southward along its eastern flank. Geology.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: churn creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 51.5167
lon: -122.283
Black Dome Mountain is thought to have formed as a result of extension of the crust behind the Cascadia subduction zone and last erupted during the Pliocene. History. During the early 1950s, Black Dome Mountain was the site of gold mining prospects by Bralorne Mines Inc. and produced a bit of an excitement for people that lived near the mountain.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667