Sarmila/GeoWiki-Features huggingface dataset:
East of the saddle rise the Reither Spitze () and the Seefeld Spitze () to its north. To the west is the Gschwandtkopf (). Watershed. The Seefeld Saddle is located on the watershed between the Inn and Isar rivers.

Geographic entities mentioned:
surface_form: Gschwandtkopf
instance_of: Mountain
countries: Austria
coordinates: lat: 47.31388888888889
lon: 11.178888888888888
It approaches from the southeast from Zirl in the Inn valley (with a junction at Innsbruck with the A12 or B 171) over the south and east flanks of the Zirler Berg (with a gradient of up to 16%) through Reith and Seefeld and then heads northeast to the village of Scharnitz on the River Isar by the Austro-German border, crossing the Scharnitz Pass, from where it continues in Germany as the B 2 running past Mittenwald via Garmisch-Partenkirchen as far as Gartz (Oder).

Geographic entities mentioned:
surface_form: Zirler Berg
instance_of: Mountain
countries: Austria
coordinates: lat: 47.2853
lon: 11.2247
The Plants are massive and rapidly out-compete terrestrial flora, forming a monoculture. They appear unwholesome to the native fauna, and the extinction of all Earthly life seems inevitable. The novel opens with a small rural community struggling for survival on the border of Lake Superior, a few years after the coming of the Plants and the collapse of civilization.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
Geography. The fjord is oriented in a roughly NE/SW direction, to the southwest the Southern Sermilik Fjord opens into the Labrador Sea of the North Atlantic Ocean. It separates two long mountainous peninsulas, the mountains on the northwestern side of the fjord rising steeply from the shore to heights of over, and the 1,590 m high Napasorsuaq peak rising in the peninsula to the east of the fjord.

Geographic entities mentioned:
surface_form: Napasorsuaq
instance_of: Mountain
countries: Greenland
coordinates: lat: 60.35
lon: -44.733333333333
Tabular Hills. The Tabular Hills form an east–west line along the southern bounds of the North York Moors, between Scarborough in the east and Black Hambleton in the west. The name refers to their flat summits composed of hard Corallian limestone, known locally as &quot;nabs&quot;. They form the northern boundary of the Vale of Pickering. Description.

Geographic entities mentioned:
surface_form: Vale of Pickering
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.2
lon: -0.7
Striking among the river valleys are Newton Dale and Forge Valley – deep channels formed when an exit to the North Sea for glacial meltwater was denied by the North Sea ice-sheet, pouring over the lowest points in the local landscape during the last ice age and cutting steeply sided channels. The Hole of Horcum is a scallop-shaped valley formed by the action of a line of springs.

Geographic entities mentioned:
surface_form: Newton Dale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.35472222222222
lon: -0.7105555555555555
surface_form: Forge Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.2699
lon: -0.489654
Swaledale cheese. Swaledale is a full fat hard cheese produced in the town of Richmond in Swaledale, North Yorkshire, England. The cheese is produced from cows’ milk, Swaledale sheep's milk and goats’ milk. Description. The cheeses are round in shape with an average weight for the cheese wheel of and are made with unpasteurised milk.

Geographic entities mentioned:
surface_form: Swaledale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.361
lon: -1.838
Description. The cheeses are round in shape with an average weight for the cheese wheel of and are made with unpasteurised milk. The animals whose milk is used to make Swaledale cheese, all graze on land in Swaledale which makes their milk characteristic of the area as a particular mixture of herbs and grasses grow there due to its soil and climate and this give the cheese distinctive properties.

Geographic entities mentioned:
surface_form: Swaledale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.361
lon: -1.838
It is named for the Trinity River of Texas. A stratigraphic column at the Mount Bonnell Fault location starts with the Lower Cretaceous Trinity Group overlain by the Edwards Group. Upper Cretaceous formations follow, starting with the Del Rio Clay, Buda Limestone, and then the Eagle Ford Group.

Geographic entities mentioned:
surface_form: Mount Bonnell
instance_of: Mountain
countries: United States
coordinates: lat: 30.321084
lon: -97.773566
Zaachila District. Zaachila District is located in the west of the Valles Centrales Region of the State of Oaxaca, Mexico. The district includes the municipalities of San Antonio Huitepec, San Miguel Peras, San Pablo Cuatro Venados, Santa Inés del Monte, Trinidad Zaachila and Villa de Zaachila.

Geographic entities mentioned:
surface_form: Valles Centrales Region
instance_of: Valley
countries: Mexico
coordinates: lat: 17.0833
lon: -96.75
Dutch ownership. The fort was built on the shores of Pulicat Lake, which provides access to the Bay of Bengal and the Coromandel Coast, an important area for trade and a scene of rivalry between the colonial powers of the Dutch, the Portuguese, and the British.

Geographic entities mentioned:
surface_form: Pulicat Lake
instance_of: Lake
countries: India
coordinates: lat: 13.565833333333
lon: 80.174722222222
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Sprinkling Tarn. Sprinkling Tarn is a body of water at the foot of Great End, in the Southern Fells in Lake District, from Seathwaite, Cumbria, England. It is noted for its trout and an introduced rare fish, vendace. Formerly known also as Sparkling Tarn. It is known as the wettest place of England with an annual precipitation of over.

Geographic entities mentioned:
surface_form: Great End
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.464
lon: -3.194
surface_form: sprinkling tarn
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.4716
lon: -3.1928
Sprinkling Tarn. Sprinkling Tarn is a body of water at the foot of Great End, in the Southern Fells in Lake District, from Seathwaite, Cumbria, England. It is noted for its trout and an introduced rare fish, vendace. Formerly known also as Sparkling Tarn. It is known as the wettest place of England with an annual precipitation of over.

Geographic entities mentioned:
surface_form: sprinkling tarn
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.4716
lon: -3.1928
Formerly known also as Sparkling Tarn. It is known as the wettest place of England with an annual precipitation of over. Sprinkling tarn has aquatic plants including intermediate water-starwort, quillwort, shoreweed, floating bur-reed and awlwort and this lake is within the Site of Special Scientific Interest called &quot;Scafell Pikes&quot; (see Scafells).

Geographic entities mentioned:
surface_form: sprinkling tarn
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.4716
lon: -3.1928
surface_form: scafell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.448
lon: -3.225
The surface of Nordkrone is plateau-like with ridges attaining high elevations and an ice cap out of which flow many glaciers. Its slopes are intersected by deep ravines with steep sides. With a height of, Mt Wistar is the highest elevation of Peary Land to the south of Frederick E. Hyde Fjord. It rises at the northwestern end, west of the Balder Glacier.

Geographic entities mentioned:
surface_form: Mt Wistar
instance_of: Mountain
countries: Greenland
coordinates: lat: 82.88333
lon: -32.5
Nordkrone. Nordkrone (, meaning &quot;Northern Crown&quot;) is a mountainous area in Peary Land, Northern Greenland. Administratively it is part of the Northeast Greenland National Park. Fossils dating back to the Silurian have been found in the area of the range. They belong to the Nordkronen Formation of the Peary Land Group. Geography.

Geographic entities mentioned:
surface_form: nordkrone
instance_of: Plateau
countries: Greenland
coordinates: lat: 82.75
lon: -31
Geography. Nordkrone is located in central Peary Land, to the south of Frederick E. Hyde Fjord, describing an arc to the east and northwest of the head of the Freja Fjord, around the Balder Glacier flowing from the south. The Børglum River &quot;(Børglum Elv)&quot; flows southward from Nordkrone to Brønlund Fjord. Nordkrone is variously described as a plateau and as a ridge.

Geographic entities mentioned:
surface_form: nordkrone
instance_of: Plateau
countries: Greenland
coordinates: lat: 82.75
lon: -31
surface_form: nordkrone
instance_of: Plateau
countries: Greenland
coordinates: lat: 82.75
lon: -31
The Børglum River &quot;(Børglum Elv)&quot; flows southward from Nordkrone to Brønlund Fjord. Nordkrone is variously described as a plateau and as a ridge. The surface of Nordkrone is plateau-like with ridges attaining high elevations and an ice cap out of which flow many glaciers. Its slopes are intersected by deep ravines with steep sides.

Geographic entities mentioned:
surface_form: nordkrone
instance_of: Plateau
countries: Greenland
coordinates: lat: 82.75
lon: -31
Its slopes are intersected by deep ravines with steep sides. With a height of, Mt Wistar is the highest elevation of Peary Land to the south of Frederick E. Hyde Fjord. It rises at the northwestern end, west of the Balder Glacier. Other elevations within Nordkrone range from about to more than.

Geographic entities mentioned:
surface_form: nordkrone
instance_of: Plateau
countries: Greenland
coordinates: lat: 82.75
lon: -31
Balatonőszöd. Balatonőszöd is a village in Somogy county, Hungary, located on the shores of Lake Balaton. It is notable primarily for the speech that Hungarian Prime Minister Ferenc Gyurcsány delivered to members of the Hungarian Socialist Party (MSZP) in 2006. The settlement is part of the Balatonboglár wine region.

Geographic entities mentioned:
surface_form: Lake Balaton
instance_of: Lake
countries: Hungary
coordinates: lat: 46.85
lon: 17.72
Haplochromis apogonoides. &quot;Haplochromis apogonoides&quot; is a species of cichlid endemic to Lake Victoria, but has not been seen since 1983. It may be extinct, but is maintained as Critically Endangered by the IUCN in the small chance that a tiny –but currently unknown– population survives. This species can reach a length of SL.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
An unpasteurized version is sold as &quot;Tsingtao Draft Beer&quot;. Tsingtao Beer was long advertized as being &quot;brewed with mineral water from the Laoshan Spring&quot;, which contributed to its characteristic flavor, but that now applies only to beer produced in Qingdao, and not to those produced in the company's other breweries.

Geographic entities mentioned:
surface_form: Lao
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 36.191666666667
lon: 120.59166666667
According to the company's financial figures from 2010, Tsingtao saw a 6.6% year-on-year revenue increase from sales to Hong Kong and other overseas markets. National marketing. Before the 1949 takeover by the new PRC government, the brewery had used imported raw material and water from the Laoshan mountain.

Geographic entities mentioned:
surface_form: Lao
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 36.191666666667
lon: 120.59166666667
Pildra. &quot;Pildra&quot; is an extinct genus of Pseudocheiridae from the Oligocene–Miocene of Australia. Specimens have been collected from the Tirari Desert and Frome Basin in northern South Australia and the Oligo-Miocene freshwater limestone deposits of the Riversleigh World Heritage Area in northwestern Queensland. It is estimated to have weighed between.

Geographic entities mentioned:
surface_form: Frome Basin
instance_of: Lake
countries: Australia
coordinates: lat: -30.616666666667
lon: 139.86666666667
In July 1862 &quot;Arago&quot;, with the schooner &quot;Caswell&quot; and steamer &quot;Bibb&quot; returned to New York. Resumption of regular service. &quot;Arago&quot; was again in South Carolina in May, 1863 surveying passages between St. Helena and Port Royal Sounds to assist naval communications between Port Royal and Savannah, Georgia.

Geographic entities mentioned:
surface_form: St. Helena
instance_of: Landform
countries: United States
coordinates: lat: 32.45472222
lon: -80.44027778
The eastern trails converged with the southern trails out of Maryland and headed northwest ultimately to New York, Lake Erie, and Canada, and south-west to the convergence of the Ohio, Monongahela, and Allegheny Rivers where Fort Duquesne was eventually erected on the site of the future city of Pittsburgh.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Upper Canada included all of modern-day Southern Ontario and all those areas of Northern Ontario in the which had formed part of New France, essentially the watersheds of the Ottawa River or Lakes Huron and Superior, excluding any lands within the watershed of Hudson Bay.

Geographic entities mentioned:
surface_form: Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
surface_form: Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
As a result, few of these poor settlers had any hope of starting their own farm, although many tried. Huron Tract. The Huron Tract lies in the counties of Huron, Perth, Middlesex and present-day Lambton County, Ontario, bordering on Lake Huron to the west and Lake Erie to the east. The tract was purchased by the Canada Company for resale to settlers.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
The first wave of settlement in the Detroit/Windsor area came in the 18th century during the French regime. A second wave came in the 19th and early 20th centuries to the areas of Eastern Ontario and Northeastern Ontario. In the Ottawa Valley, in particular, some families have moved back and forth across the Ottawa River for generations (the river is the border between Ontario and Quebec).

Geographic entities mentioned:
surface_form: Ottawa Valley
instance_of: Valley
countries: Canada
coordinates: lat: 45.91682
lon: -77.13276
The timber trade was Upper and Lower Canada's major industry in terms of employment and value of the product. The largest supplier of square red and white pine to the British market was the Ottawa River and the Ottawa Valley. They had &quot;rich red and white pine forests.&quot; Bytown (later called Ottawa), was a major lumber and sawmill centre of Canada. Canal system.

Geographic entities mentioned:
surface_form: Ottawa Valley
instance_of: Valley
countries: Canada
coordinates: lat: 45.91682
lon: -77.13276
Desjardins Canal. The Desjardins Canal, named after its promoter Pierre Desjardins, was built to give Dundas, Ontario, easier access to Burlington Bay and Lake Ontario. Access to Lake Ontario from Dundas was made difficult by the topography of the area, which included a natural sand and gravel barrier, across Burlington Bay which allowed only boats with a shallow draft through.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
While &quot;Frontenac&quot; was launched first, &quot;Ontario&quot; began active service first. The first steamboat on the upper Great Lakes was the passenger-carrying &quot;Walk-In-The-Water&quot;, built in 1818 to navigate Lake Erie. In the years between 1809 and 1837 just over 100 steamboats were launched by Upper and Lower Canadians for the St.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
It was first roughly surveyed in 1909 by the French Antarctic Expedition under Jean-Baptiste Charcot, who named it for the French city of Calais. The mountain was resurveyed in 1948 by the Falkland Islands Dependencies Survey. Mount Calais is the eighth-highest point of Alexander Island while Mount Stephenson remains the highest of all the peaks.

Geographic entities mentioned:
surface_form: Mount Stephenson
instance_of: Mountain
coordinates: lat: -69.816666666667
lon: -69.716666666667
surface_form: calais
instance_of: Mountain
coordinates: lat: -69.1833
lon: -70.25
surface_form: mount calais
instance_of: Mountain
coordinates: lat: -69.1833
lon: -70.25
surface_form: alexander
instance_of: Mountain
coordinates: lat: -63.3039
lon: -55.80564
Mount Calais. Mount Calais () is a massive mountain, high, at the northwest side of Schokalsky Bay in the northeast part of Alexander Island, Antarctica. It was first roughly surveyed in 1909 by the French Antarctic Expedition under Jean-Baptiste Charcot, who named it for the French city of Calais. The mountain was resurveyed in 1948 by the Falkland Islands Dependencies Survey.

Geographic entities mentioned:
surface_form: calais
instance_of: Mountain
coordinates: lat: -69.1833
lon: -70.25
surface_form: mount calais
instance_of: Mountain
coordinates: lat: -69.1833
lon: -70.25
Mount Calais. Mount Calais () is a massive mountain, high, at the northwest side of Schokalsky Bay in the northeast part of Alexander Island, Antarctica. It was first roughly surveyed in 1909 by the French Antarctic Expedition under Jean-Baptiste Charcot, who named it for the French city of Calais. The mountain was resurveyed in 1948 by the Falkland Islands Dependencies Survey.

Geographic entities mentioned:
surface_form: calais
instance_of: Mountain
coordinates: lat: -69.1833
lon: -70.25
surface_form: mount calais
instance_of: Mountain
coordinates: lat: -69.1833
lon: -70.25
surface_form: alexander
instance_of: Mountain
coordinates: lat: -63.3039
lon: -55.80564
Mount Calais. Mount Calais () is a massive mountain, high, at the northwest side of Schokalsky Bay in the northeast part of Alexander Island, Antarctica. It was first roughly surveyed in 1909 by the French Antarctic Expedition under Jean-Baptiste Charcot, who named it for the French city of Calais. The mountain was resurveyed in 1948 by the Falkland Islands Dependencies Survey.

Geographic entities mentioned:
surface_form: calais
instance_of: Mountain
coordinates: lat: -69.1833
lon: -70.25
The relations between various members of this house are assumed mostly from Javanese traditions, oral or written in &quot;babads&quot; or other forms of writings. Economy. Demak derived its income from trade, importing spices and exporting rice to Malacca and the Maluku Islands. It was a busy port located at the end of a then navigable channel separating Java and Muria Island.

Geographic entities mentioned:
surface_form: Muria Island
instance_of: Mountain
countries: Indonesia
coordinates: lat: -6.61666667
lon: 110.88333333
Taxonomy and naming. &quot;Eucalyptus ordiana&quot; was first formally described in 1992 by Clyde Dunlop and Christopher Done in the journal &quot;Nuytsia&quot; from material collected near Lake Kununurra in the Kimberley. The specific epithet &quot;ordiana&quot; refers to the Ord River with a Latin ending meaning &quot;belonging to&quot;. Distribution and habitat.

Geographic entities mentioned:
surface_form: Lake Kununurra
instance_of: Lake
countries: Australia
coordinates: lat: -15.8
lon: 128.733
Christine Jensen Burke. Chris Jensen Burke (born 2 July 1968) is a New Zealand–Australian mountain climber who was the first New Zealand or Australian woman to reach the summit of K2. Since climbing Mount Everest on 20 May 2011, Burke has climbed nine other eight-thousanders, including K2 on 26 July 2014 and Kanchenjunga on 17 May 2018.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
Climbing career. Burke commenced the Seven Summits endeavor by successfully reaching the summit of Kilimanjaro on 6 August 2010, and completed the last of the Seven Summits ('Bass' list) with her successful climb of Mount Elbrus in Russia on 25 July 2012. She completed the 'Messner' list on 15 January 2013, on successful completion of her Carstensz Pyramid climb.

Geographic entities mentioned:
surface_form: Mount Elbrus
instance_of: Mountain
countries: Russia
Soviet Union
Russian Empire
coordinates: lat: 43.35254
lon: 42.437875
She completed the 'Messner' list on 15 January 2013, on successful completion of her Carstensz Pyramid climb. She reached the summit of Mount Everest on 20 May 2011. Personal life. Burke has engaged in numerous private charitable initiatives in Nepal, including fundraising for and supporting disadvantaged and trafficked women and girls.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
Another variant, the &quot;Citronella&quot; morph from the vicinity of Kasikasima, Suriname, is primarily deep yellow with some black blotches on the back and head, and royal blue legs and underparts with tiny black spots. Despite the large variation in appearance, the genetic differences between the different populations of the dyeing poison dart frog are very marginal. Poison.

Geographic entities mentioned:
surface_form: Kasikasima
instance_of: Mountain
countries: Suriname
coordinates: lat: 2.979722222222222
lon: -55.410833333333336
Lake Kariba. Lake Kariba is the world's largest artificial lake and reservoir by volume. It lies upstream from the mouth of the Zambezi river on the Indian Ocean, along the border between Zambia and Zimbabwe. Lake Kariba was filled between 1958 and 1963 following the completion of the Kariba Dam at its northeastern end, flooding the Kariba Gorge on the Zambezi River.

Geographic entities mentioned:
surface_form: Kariba Gorge
instance_of: Landform
countries: Zimbabwe
Zambia
coordinates: lat: -16.503888888889
lon: 28.795555555556
As a result, the ecology of Lake Kariba is vibrant. A number of fish species have been introduced to the lake, notably the sardine-like kapenta (transported from Lake Tanganyika), which now supports a thriving commercial fishery. Other inhabitants of Lake Kariba include Nile crocodiles and hippopotamuses.

Geographic entities mentioned:
surface_form: Lake Tanganyika
instance_of: Lake
countries: Tanzania
Democratic Republic of the Congo
Burundi
Zambia
coordinates: lat: -6.1
lon: 29.5
John D. Long Lake. John D. Long Lake is an manmade lake in Union County, South Carolina. It is used for fishing, with largemouth bass, bluegill, shellcracker (redear sunfish), and catfish in the lake. There is a boat ramp and a fishing pier. Location and geography. The lake is located about west of Lockhart, the nearest town, and about northeast of Union, the nearest city.

Geographic entities mentioned:
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 34.78779
lon: -111.210939
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 43.9728
lon: -74.4211
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 44.718
lon: -85.748
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 44.1086787
lon: -75.1564925
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 44.1657291
lon: -98.7168782
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 43.9334172
lon: -97.0073724
surface_form: john d. long lake
instance_of: Lake
countries: United States
coordinates: lat: 34.775
lon: -81.51233333
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 45.9496317
lon: -95.9225667
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 45.8456754
lon: -99.2676497
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 45.127777777778
lon: -83.973055555556
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 46.235907
lon: -89.49916
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 44.9348621
lon: -97.3996461
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 45.20461
lon: -83.47775
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 43.5597393
lon: -75.1515847
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 45.248184
lon: -85.075807
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 41.615555555556
lon: -87.210555555556
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 45.7281765
lon: -97.3795798
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 47.483055555556
lon: -122.58972222222
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 43.971666666667
lon: -70.611666666667
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 45.8387529
lon: -88.6755297
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 47.0191485
lon: -122.7747634
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 44.572222222222
lon: -85.298888888889
Access to the western end of the lake, where the fishing pier and boat ramp is located, is via Black Bottom Road which connects to Highway 9. Access to the eastern end is from John D. Long Lake Road which connects to Highway 49. This gives out on a small parkland near the dam, where the boat ramp was formerly located. History.

Geographic entities mentioned:
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 34.78779
lon: -111.210939
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 43.9728
lon: -74.4211
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 44.718
lon: -85.748
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 44.1086787
lon: -75.1564925
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 44.1657291
lon: -98.7168782
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 43.9334172
lon: -97.0073724
surface_form: john d. long lake
instance_of: Lake
countries: United States
coordinates: lat: 34.775
lon: -81.51233333
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 45.9496317
lon: -95.9225667
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 45.8456754
lon: -99.2676497
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 45.127777777778
lon: -83.973055555556
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 46.235907
lon: -89.49916
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 44.9348621
lon: -97.3996461
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 45.20461
lon: -83.47775
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 43.5597393
lon: -75.1515847
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 45.248184
lon: -85.075807
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 41.615555555556
lon: -87.210555555556
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 45.7281765
lon: -97.3795798
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 47.483055555556
lon: -122.58972222222
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 43.971666666667
lon: -70.611666666667
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 45.8387529
lon: -88.6755297
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 47.0191485
lon: -122.7747634
surface_form: long lake
instance_of: Lake
countries: United States
coordinates: lat: 44.572222222222
lon: -85.298888888889
From the state line, they found a &quot;dim trail&quot; leading to the summit. Thornborough concludes her report by saying, &quot;if it is wilderness you want, then go to Guyot.&quot;
Access. The Appalachian Trail and the Balsam Mountain Trail intersect just south of Guyot
at Tricorner Knob. They are the only maintained trails to traverse the mountain.

Geographic entities mentioned:
surface_form: Tricorner Knob
instance_of: Mountain
countries: United States
coordinates: lat: 35.695561111111
lon: -83.254169444444
surface_form: tricorner knob
instance_of: Mountain
countries: United States
coordinates: lat: 35.695561111111
lon: -83.254169444444
From this
intersection, it is approximately to Guyot Spring, on Mt. Guyot's west slope. A section of the Appalachian Trail stretches from Newfound Gap to Tricorner Knob, near Guyot's south slope. The Appalachian-Balsam Trail intersection is approximately from Balsam Mountain Road, a gravel road that begins near Cherokee, North Carolina.

Geographic entities mentioned:
surface_form: Tricorner Knob
instance_of: Mountain
countries: United States
coordinates: lat: 35.695561111111
lon: -83.254169444444
surface_form: tricorner knob
instance_of: Mountain
countries: United States
coordinates: lat: 35.695561111111
lon: -83.254169444444
Mount Guyot (Great Smoky Mountains). Mount Guyot is a mountain in the Great Smoky Mountains, located in the southeastern United States. At in elevation, Guyot is the fourth-highest summit in the Eastern U.S., and the second-highest in the Great Smoky Mountains National Park. While the mountain is remote, the Appalachian Trail crosses its south slope, passing to within of the summit.

Geographic entities mentioned:
surface_form: mount guyot
instance_of: Mountain
countries: United States
coordinates: lat: 39.4587
lon: -105.938
surface_form: mount guyot
instance_of: Mountain
countries: United States
coordinates: lat: 44.1681
lon: -71.534
surface_form: mount guyot
instance_of: Mountain
countries: United States
coordinates: lat: 35.705
lon: -83.2575
Mount Guyot (Great Smoky Mountains). Mount Guyot is a mountain in the Great Smoky Mountains, located in the southeastern United States. At in elevation, Guyot is the fourth-highest summit in the Eastern U.S., and the second-highest in the Great Smoky Mountains National Park. While the mountain is remote, the Appalachian Trail crosses its south slope, passing to within of the summit.

Geographic entities mentioned:
surface_form: mount guyot
instance_of: Mountain
countries: United States
coordinates: lat: 39.4587
lon: -105.938
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: mount guyot
instance_of: Mountain
countries: United States
coordinates: lat: 44.1681
lon: -71.534
surface_form: mount guyot
instance_of: Mountain
countries: United States
coordinates: lat: 35.705
lon: -83.2575
While the mountain is remote, the Appalachian Trail crosses its south slope, passing to within of the summit. Mount Guyot lies on the Tennessee-North Carolina border, between Sevier County and Haywood County. There are two peaks atop the mountain approximately one-half mile apart, with the southwestern peak in Tennessee being the true summit.

Geographic entities mentioned:
surface_form: mount guyot
instance_of: Mountain
countries: United States
coordinates: lat: 39.4587
lon: -105.938
surface_form: mount guyot
instance_of: Mountain
countries: United States
coordinates: lat: 44.1681
lon: -71.534
surface_form: mount guyot
instance_of: Mountain
countries: United States
coordinates: lat: 35.705
lon: -83.2575
without a trail. Geology. Mount Guyot is composed of Precambrian rocks of the Ocoee Supergroup, formed from ocean sediments approximately one billion years ago. The mountain is underlain by Thunderhead sandstone, which is common throughout the Smokies. The Thunderhead sandstone was thrust over Roaring Fork sandstone several hundred million years ago. Mt.

Geographic entities mentioned:
surface_form: mount guyot
instance_of: Mountain
countries: United States
coordinates: lat: 39.4587
lon: -105.938
surface_form: mount guyot
instance_of: Mountain
countries: United States
coordinates: lat: 44.1681
lon: -71.534
surface_form: mount guyot
instance_of: Mountain
countries: United States
coordinates: lat: 35.705
lon: -83.2575
Mt. Guyot itself was formed during the Appalachian orogeny over 200 million years ago, when the North American and African plates collided, thrusting the rock upward. History. Mount Guyot was named in honor of Swiss geographer Arnold Guyot by Guyot's friend, Samuel Buckley. Buckley was a naturalist who accompanied Thomas Lanier Clingman on a survey expedition to the crest of the Smokies in 1858.

Geographic entities mentioned:
surface_form: mount guyot
instance_of: Mountain
countries: United States
coordinates: lat: 39.4587
lon: -105.938
surface_form: mount guyot
instance_of: Mountain
countries: United States
coordinates: lat: 44.1681
lon: -71.534
surface_form: mount guyot
instance_of: Mountain
countries: United States
coordinates: lat: 35.705
lon: -83.2575
A faint manway rises from Guyot Spring to the northern summit, although the manway is heavily overgrown. Dead Fraser fir blowdowns and low visibility complicate navigation from any direction. The Appalachian Trail also passes by another Mount Guyot in New Hampshire approximately 1600 miles to the north.

Geographic entities mentioned:
surface_form: mount guyot
instance_of: Mountain
countries: United States
coordinates: lat: 39.4587
lon: -105.938
surface_form: mount guyot
instance_of: Mountain
countries: United States
coordinates: lat: 44.1681
lon: -71.534
surface_form: mount guyot
instance_of: Mountain
countries: United States
coordinates: lat: 35.705
lon: -83.2575
From this
intersection, it is approximately to Guyot Spring, on Mt. Guyot's west slope. A section of the Appalachian Trail stretches from Newfound Gap to Tricorner Knob, near Guyot's south slope. The Appalachian-Balsam Trail intersection is approximately from Balsam Mountain Road, a gravel road that begins near Cherokee, North Carolina.

Geographic entities mentioned:
surface_form: balsam mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.0908
lon: -74.488
surface_form: balsam mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.1837
lon: -74.38737
The mountain is underlain by Thunderhead sandstone, which is common throughout the Smokies. The Thunderhead sandstone was thrust over Roaring Fork sandstone several hundred million years ago. Mt. Guyot itself was formed during the Appalachian orogeny over 200 million years ago, when the North American and African plates collided, thrusting the rock upward. History.

Geographic entities mentioned:
surface_form: mt. guyot
instance_of: Mountain
countries: United States
coordinates: lat: 44.1681
lon: -71.534
surface_form: mt. guyot
instance_of: Mountain
countries: United States
coordinates: lat: 35.705
lon: -83.2575
While Buckley's measurements were often wildly inaccurate, Guyot conducted an expedition the following year, recording more accurate elevations and giving preliminary names to various peaks along the crest. Guyot measured the elevation of Mt. Guyot at, missing the modern measurement by just. Thornborough followed the route out of Greenbrier that ascends Guyot's western slope.

Geographic entities mentioned:
surface_form: mt. guyot
instance_of: Mountain
countries: United States
coordinates: lat: 44.1681
lon: -71.534
surface_form: mt. guyot
instance_of: Mountain
countries: United States
coordinates: lat: 35.705
lon: -83.2575
They are the only maintained trails to traverse the mountain. From the Cosby Campground (specifically behind Campsite B51), the Snake Den Ridge Trail
winds to its intersection with the Appalachian Trail at Inadu Knob. From this
intersection, it is approximately to Guyot Spring, on Mt. Guyot's west slope.

Geographic entities mentioned:
surface_form: mt. guyot
instance_of: Mountain
countries: United States
coordinates: lat: 44.1681
lon: -71.534
surface_form: mt. guyot
instance_of: Mountain
countries: United States
coordinates: lat: 35.705
lon: -83.2575
There are two peaks atop the mountain approximately one-half mile apart, with the southwestern peak in Tennessee being the true summit. The mountain rises above its eastern base near Walnut Bottom and above its western base near Greenbrier Cove. Ramsey Cascades, one of the park's most spectacular waterfalls, spills down a sandstone cliff near the bottom of Guyot's western slope.

Geographic entities mentioned:
surface_form: greenbrier
instance_of: Valley
countries: United States
coordinates: lat: 35.7069
lon: -83.3831
Guyot at, missing the modern measurement by just. Thornborough followed the route out of Greenbrier that ascends Guyot's western slope. She recalls that &quot;there was no trail to Guyot, not even a dim one, but our guides knew the way.&quot; The party followed Ramsay Prong until it became &quot;a mere trickle of water,&quot; and emerged near modern-day Guyot Spring.

Geographic entities mentioned:
surface_form: greenbrier
instance_of: Valley
countries: United States
coordinates: lat: 35.7069
lon: -83.3831
without a trail. Geology. Mount Guyot is composed of Precambrian rocks of the Ocoee Supergroup, formed from ocean sediments approximately one billion years ago. The mountain is underlain by Thunderhead sandstone, which is common throughout the Smokies. The Thunderhead sandstone was thrust over Roaring Fork sandstone several hundred million years ago. Mt.

Geographic entities mentioned:
surface_form: roaring fork
instance_of: Watercourse
countries: United States
coordinates: lat: 35.716759
lon: -83.5118304
surface_form: thunderhead
instance_of: Mountain
countries: United States
coordinates: lat: 35.568611111111
lon: -83.706388888889
without a trail. Geology. Mount Guyot is composed of Precambrian rocks of the Ocoee Supergroup, formed from ocean sediments approximately one billion years ago. The mountain is underlain by Thunderhead sandstone, which is common throughout the Smokies. The Thunderhead sandstone was thrust over Roaring Fork sandstone several hundred million years ago. Mt.

Geographic entities mentioned:
surface_form: thunderhead
instance_of: Mountain
countries: United States
coordinates: lat: 35.568611111111
lon: -83.706388888889
Rancho Nacional. Rancho Nacional was a Mexican land grant in the Salinas Valley, in present day Monterey County, California given in 1839 by Governor Juan B. Alvarado to Vicente Cantua. The grant was between the Salinas River and present day Salinas. History.

Geographic entities mentioned:
surface_form: Salinas Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.7654
lon: -121.7918
This essentially ensured that territorial conflicts would persist after the treaty's authorization. The region between Lake Gokcha and Erivan remained one of the most disputable. Second war with Russia.

Geographic entities mentioned:
surface_form: Lake Gokcha
instance_of: Lake
countries: Armenia
coordinates: lat: 40.310555555556
lon: 45.349166666667
Geography. According to the U.S. Census Bureau, the county has a total area of, of which is land and (0.32%) is water. It is the fifth-smallest county in North Carolina by total area. The county's largest body of water is Lake Adger, located about north of Columbus. Lake Adger is a reservoir formed by the damming of the Green River, which flows from west to east across the county.

Geographic entities mentioned:
surface_form: Lake Adger
instance_of: Lake
countries: United States
coordinates: lat: 35.3346668
lon: -82.2234098
Songs of Earth. &quot;Songs of Earth&quot; () is a 2023 Norwegian documentary film written and directed by Margreth Olin. In the film, Olin follows her 85-year-old father through a year in the natural surroundings of Oldedalen in Vestland, where he grew up.

Geographic entities mentioned:
surface_form: Oldedalen
instance_of: Valley
countries: Norway
coordinates: lat: 61.69055556
lon: 6.81694444
Irwindale, California. Irwindale is a city in the San Gabriel Valley, in Los Angeles County, California. The population was 1,472 at the 2020 census, 1,422 at the 2010 census. The ZIP Codes serving the area are 91010, which is shared with Duarte, 91702, which is shared with Azusa, and 91706, which is shared with Baldwin Park.

Geographic entities mentioned:
surface_form: San Gabriel Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.101944444444
lon: -118.10277777778
Bujanovac. Bujanovac (,;) is a town and municipality located in the Pčinja District of southern Serbia. As of the 2022 census, the municipality has a population of 41,068. Situated in the South Morava basin, it is located in the geographical area known as Preševo Valley. It is also known for its source of mineral water and spa town &quot;Bujanovačka banja&quot;.

Geographic entities mentioned:
surface_form: Preševo Valley
instance_of: Valley
countries: Serbia
coordinates: lat: 42.3
lon: 21.633333333333
The II and III Corps were organised into the Army of the Isthmus which was located on the Karelian Isthmus, the likely location for the main Soviet attack. The IV Corps defended the area north of Lake Ladoga. The defence of the rest of the border up to Petsamo by the Arctic Ocean was given to the North Finland Group which consisted of a handful of independent battalions.

Geographic entities mentioned:
surface_form: Lake Ladoga
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.842777777777776
lon: 31.459722222222222
Sestola. Sestola (Sestolese:; Frignanese:) is a &quot;comune&quot; (municipality) in the province of Modena, in the Italian region of Emilia-Romagna, located about southwest of Bologna and about southwest of Modena. It is located near the Monte Cimone and other mountains of the northern Apennines separating Emilia and Tuscany.

Geographic entities mentioned:
surface_form: Monte Cimone
instance_of: Mountain
countries: Italy
coordinates: lat: 44.193888888889
lon: 10.701388888889
It reaches. Scout Scar is the subject of a chapter of Wainwright's book &quot;The Outlying Fells of Lakeland&quot;, but the summit he describes is a lower summit at, 270m south of the highest point. Wainwright's anticlockwise recommended route also includes Cunswick Scar at.

Geographic entities mentioned:
surface_form: Cunswick Scar
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.3237
lon: -2.78716
It served with 21st Army Group during the campaign in North West Europe 1944–45. It built the first British bridges across the Rhine and the Elbe after the assault crossings in March and April 1945 and continued in British Army of the Rhine after the end of the war. Organisation.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Ó Flaithbheartaigh chronicled about a pool of water on the summit which turns the hair white of anyone who washes in it. Geography. Benlettery is the southernmost peak of the Twelve Bens and lies at its western edge. Benlettery is connected to the range by a high northerly ridge to the peak of Bengower; this ridge forms a fork which also connects neighboring Benglenisky to Bengower.

Geographic entities mentioned:
surface_form: Bengower
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.49244
lon: -9.83474
surface_form: Benglenisky
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.48759
lon: -9.85731
surface_form: bengower
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.49244
lon: -9.83474
surface_form: bengower
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.49244
lon: -9.83474
surface_form: benlettery
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.48294
lon: -9.84409
surface_form: benglenisky
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.48759
lon: -9.85731
Unlike most of the other main Bens, Benlettery is below 600-metres in elevation, however, its relative positioning at the southern end of the range, and its &quot;pyramidal&quot; summit (when viewed from the south), means that is often featured as a scenic backdrop to the Ballynahinch Castle and the Ballynahinch Lake. &quot;Ben Lettery Connemara Youth Hostel&quot;.

Geographic entities mentioned:
surface_form: Ballynahinch Lake
instance_of: Lake
countries: Ireland
coordinates: lat: 53.46722222
lon: -9.85833333
surface_form: ballynahinch lake
instance_of: Lake
countries: Ireland
coordinates: lat: 53.46722222
lon: -9.85833333
As with Derryclare, on the east side of the Glencoaghan Horseshoe, Benlettery's accessibility makes is a popular peak as a standalone 5-kilometre 2-3 hour climb (starting and ending at the Ben Lettery An Oige youth hostel); however, the high ridge Benlettery shares with the peaks of Bengower and Benglenisky, means that it is also climbed as part a 7-kilometre 3-4 hour horseshoe loop-walk with these peaks.

Geographic entities mentioned:
surface_form: Derryclare
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.49665
lon: -9.78599
surface_form: bengower
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.49244
lon: -9.83474
surface_form: benlettery
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.48294
lon: -9.84409
surface_form: benlettery
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.48294
lon: -9.84409
surface_form: ben lettery
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.48294
lon: -9.84409
surface_form: benglenisky
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.48759
lon: -9.85731
&quot;Ben Lettery Connemara Youth Hostel&quot;. On the southern slopes of Benlettery is the 40-bed &quot;Ben Lettery Connemara Youth Hostel&quot; (Benlettery spelt as two words), owned and operated by An Oige, the Irish YHA; it was ranked by &quot;Outside.ie&quot; as one of the ten best An Oige youth hostels in Ireland. Hill walking.

Geographic entities mentioned:
surface_form: benlettery
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.48294
lon: -9.84409
surface_form: benlettery
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.48294
lon: -9.84409
Benlettery. Benlettery () at, is the 259th–highest peak in Ireland on the Arderin scale. Benlettery is in the southernmost peak of the Twelve Bens mountain range in the Connemara National Park in County Galway, Ireland, and is the 11th-tallest of the core &quot;Twelve Bens&quot;. The Ben Lettery An Oige youth hostel is on the southern slopes of Benlettery, off the N59 road to Clifden. Naming.

Geographic entities mentioned:
surface_form: arderin
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.03805556
lon: -7.65388889
surface_form: benlettery
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.48294
lon: -9.84409
Benlettery. Benlettery () at, is the 259th–highest peak in Ireland on the Arderin scale. Benlettery is in the southernmost peak of the Twelve Bens mountain range in the Connemara National Park in County Galway, Ireland, and is the 11th-tallest of the core &quot;Twelve Bens&quot;. The Ben Lettery An Oige youth hostel is on the southern slopes of Benlettery, off the N59 road to Clifden. Naming.

Geographic entities mentioned:
surface_form: benlettery
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.48294
lon: -9.84409
Naming. According to Irish academic Paul Tempan, the townland of Lettery (, meaning &quot;wet hillsides&quot;) is on the south slope of Benlettery. Tempan notes an alternative name of Bindowglass or &quot;Bendouglas&quot; (, meaning &quot;peak of the black stream&quot;) was recorded as early as 1684 by Irish historian Ruaidhrí Ó Flaithbheartaigh.

Geographic entities mentioned:
surface_form: benlettery
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.48294
lon: -9.84409