Sarmila/GeoWiki-Features huggingface dataset:
Virginia has 226 species of freshwater fish from 25 families, a diversity attributable to the area's varied and humid climate, topography, interconnected river system, and lack of Pleistocene glaciers. Common examples on the Cumberland Plateau and higher-elevation regions include Eastern blacknose dace, sculpin, smallmouth bass, redhorse sucker, Kanawha darter, and brook trout, the state fish.

Geographic entities mentioned:
surface_form: Cumberland Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 36
lon: -85
Immigrants from Britain and Ireland settled throughout the Commonwealth during the colonial period, when roughly three-fourths of immigrants came as indentured servants. The Appalachian mountains and Shenandoah Valley have many settlements that were populated by German and Scotch-Irish immigrants in the 18th and 19th centuries, often following the Great Wagon Road.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
The closest approach to the mountain is from Kinlochleven to the south, however the mountain is often approached along its north eastern or eastern ridges as part of the highly rated “Ring of Steall” ridge walk which starts and finishes in Glen Nevis and climbs the other Munros of An Gearanach, Stob Coire a' Chàirn and Sgurr a' Mhàim.

Geographic entities mentioned:
surface_form: An Gearanach
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.759146
lon: -4.966211
surface_form: Stob Coire a' Chàirn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.750747
lon: -4.969017
surface_form: sgurr a' mhàim
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.75592
lon: -5.00369
Am Bodach translates from the Gaelic as “The Old Man”, this name was often given to a conspicuous hill overlooking a community and it was probably named by settlers at the head of Loch Leven which the mountain overlooks. The mountain should not be confused with another Am Bodach at the eastern end of the Aonach Eagach ridge in Glen Coe. Geography.

Geographic entities mentioned:
surface_form: Aonach Eagach
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.679497
lon: -5.012554
surface_form: am bodach
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.741729
lon: -4.983387
The view from the summit takes in Ben Nevis to the north and Loch Leven and the mountains surrounding Glen Coe to the south, with Bidean nam Bian looking especially fine.

Geographic entities mentioned:
surface_form: Ben Nevis
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.796891
lon: -5.003675
surface_form: Bidean nam Bian
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.642768
lon: -5.029335
surface_form: bidean nam bian
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.642768
lon: -5.029335
surface_form: loch leven
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.194444444444
lon: -3.375
surface_form: ben nevis
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.796891
lon: -5.003675
Am Bodach translates from the Gaelic as “The Old Man”, this name was often given to a conspicuous hill overlooking a community and it was probably named by settlers at the head of Loch Leven which the mountain overlooks. The mountain should not be confused with another Am Bodach at the eastern end of the Aonach Eagach ridge in Glen Coe. Geography.

Geographic entities mentioned:
surface_form: loch leven
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.194444444444
lon: -3.375
surface_form: am bodach
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.741729
lon: -4.983387
Am Bodach has three ridges radiating from its summit, the western one connects to the former Munro of Sgurr an Iubhair (downgraded to a &quot;Top&quot; in the 1997 revisions) while the north eastern ridge, which is steep and rocky, connects to the Munro of Stob Coire a' Chàirn, it is along these two ridges that walkers undertaking the Ring of Steall walk will arrive and leave the mountain.

Geographic entities mentioned:
surface_form: stob coire a' chàirn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.750747
lon: -4.969017
surface_form: am bodach
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.741729
lon: -4.983387
It can also be approached via a stalker's path up Coire na Bà which reaches the main Mamores ridge east of Stob Coire a' Chàirn; this summit is then traversed, joining the Ring of Steall, before continuing south westwards to reach the north east ridge of Am Bodach.

Geographic entities mentioned:
surface_form: stob coire a' chàirn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.750747
lon: -4.969017
surface_form: am bodach
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.741729
lon: -4.983387
Am Bodach. Am Bodach is a Scottish mountain which lies in the Mamores range, four kilometres north of Kinlochleven in the Highland council area. Overview. Am Bodach is a Munro which reaches a height of 1032 metres (3386 feet) making it the 100th highest mountain in that classification, it is situated on the main ridge of the Mamores in a central position and is the most accessible of the group.

Geographic entities mentioned:
surface_form: am bodach
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.741729
lon: -4.983387
The mountain should not be confused with another Am Bodach at the eastern end of the Aonach Eagach ridge in Glen Coe. Geography. Am Bodach is a fine looking mountain with a sharp peak formed by its three steep and rocky faces, the eastern face above the Coire na Ba is especially precipitous and craggy and holds patches of snow well into summer.

Geographic entities mentioned:
surface_form: am bodach
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.741729
lon: -4.983387
Ascents. The ascent of Am Bodach starts at sea level at Kinlochleven; various routes, including the path initially followed by the West Highland Way from the western end of the village, can be followed to reach the old military road to Fort William built by General Caulfield, which the West Highland Way then follows; all routes from the south involve initially reaching this track.

Geographic entities mentioned:
surface_form: am bodach
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.741729
lon: -4.983387
Oakley Down Barrow Cemetery. Oakley Down Barrow Cemetery is a group of Bronze Age round barrows on Cranborne Chase, about east of the village of Sixpenny Handley in Dorset, England. It is a scheduled monument. Description. There are many prehistoric remains on Cranborne Chase from the Neolithic and Early Bronze Age.

Geographic entities mentioned:
surface_form: Cranborne Chase
instance_of: Plateau
countries: United Kingdom
coordinates: lat: 50.961419444444
lon: -2.0440888888889
Table Mountain Aerial Cableway. The Table Mountain Aerial Cableway is a cable car transportation system offering visitors a five-minute ride to the top of Table Mountain in Cape Town, South Africa. It is one of Cape Town's most popular tourist attractions with approximately one million people a year using the Cableway. In January 2019, the Cableway welcomed its 28 millionth visitor.

Geographic entities mentioned:
surface_form: Table Mountain
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
Specifications. The &quot;Rotair&quot; cableway was installed by Garaventa (Doppelmayr Garaventa Group) from Switzerland in 1997, the design being based on the Titlis Rotair cableway in Engelberg, Switzerland. Each car carries 65 passengers (compared to 25 for the old cars), and runs on a double cable making them more stable in high winds, giving a faster journey of 4–5 minutes to the summit.

Geographic entities mentioned:
surface_form: Titlis Rotair
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.771944444444
lon: 8.4377777777778
Georgia's Tallulah Gorge State Park protects much of the gorge and its waterfalls. The Tallulah Gorge has been dubbed one of the &quot;Seven Natural Wonders of Georgia&quot;. Tallulah Falls Lake lies just above the gorge. It was created in 1913 by a hydroelectric dam built by Georgia Railway and Power (now Georgia Power) in order to run Atlanta's city streetcars.

Geographic entities mentioned:
surface_form: Tallulah Falls Lake
instance_of: Lake
countries: United States
coordinates: lat: 34.7387
lon: -83.3961
Tallulah Gorge. The Tallulah Gorge is a canyon in the southern Appalachian Mountains of the U.S. state of Georgia. Located near the town of Tallulah Falls in the northeastern part of the state, the gorge was formed by the Tallulah River as it cut through the Tallulah Dome rock formation. It measures approximately long and almost deep.

Geographic entities mentioned:
surface_form: tallulah gorge
instance_of: Valley
countries: United States
coordinates: lat: 34.725
lon: -83.370277777778
Located near the town of Tallulah Falls in the northeastern part of the state, the gorge was formed by the Tallulah River as it cut through the Tallulah Dome rock formation. It measures approximately long and almost deep. Georgia's Tallulah Gorge State Park protects much of the gorge and its waterfalls. The Tallulah Gorge has been dubbed one of the &quot;Seven Natural Wonders of Georgia&quot;.

Geographic entities mentioned:
surface_form: tallulah gorge
instance_of: Valley
countries: United States
coordinates: lat: 34.725
lon: -83.370277777778
It measures approximately long and almost deep. Georgia's Tallulah Gorge State Park protects much of the gorge and its waterfalls. The Tallulah Gorge has been dubbed one of the &quot;Seven Natural Wonders of Georgia&quot;. Tallulah Falls Lake lies just above the gorge.

Geographic entities mentioned:
surface_form: tallulah gorge
instance_of: Valley
countries: United States
coordinates: lat: 34.725
lon: -83.370277777778
History. Since the early 19th century, Tallulah Gorge and its waterfalls have been a tourist attraction. In 1882, Tallulah Falls Railway was built, increasing the accessibility of the area to visitors from Atlanta and elsewhere in Georgia, and the gorge became North Georgia's leading tourist attraction.

Geographic entities mentioned:
surface_form: tallulah gorge
instance_of: Valley
countries: United States
coordinates: lat: 34.725
lon: -83.370277777778
The area was cleared and then flooded to become Lake Burton in 1919. Many nearby residents opposed the dams, including Helen Dortch Longstreet, widow of Confederate general James Longstreet, who led an unsuccessful campaign in 1911 to have Tallulah Gorge protected by the state. The Georgia Assembly was unable to raise the $1 million required to purchase the gorge, but Mrs.

Geographic entities mentioned:
surface_form: tallulah gorge
instance_of: Valley
countries: United States
coordinates: lat: 34.725
lon: -83.370277777778
Tallulah Gorge. The Tallulah Gorge is a canyon in the southern Appalachian Mountains of the U.S. state of Georgia. Located near the town of Tallulah Falls in the northeastern part of the state, the gorge was formed by the Tallulah River as it cut through the Tallulah Dome rock formation. It measures approximately long and almost deep.

Geographic entities mentioned:
surface_form: tallulah dome
instance_of: Valley
countries: United States
coordinates: lat: 34.725
lon: -83.370277777778
surface_form: dome rock
instance_of: Mountain
countries: United States
coordinates: lat: 44.7525
lon: -122.20861111111
The town of Burton, Georgia was purchased and its residents relocated. The area was cleared and then flooded to become Lake Burton in 1919. Many nearby residents opposed the dams, including Helen Dortch Longstreet, widow of Confederate general James Longstreet, who led an unsuccessful campaign in 1911 to have Tallulah Gorge protected by the state.

Geographic entities mentioned:
surface_form: lake burton
instance_of: Lake
countries: United States
coordinates: lat: 34.8269
lon: -83.5551
Resort hotels and bars sprang up to serve the tourist trade, which, after the addition of the railway, swelled to as many as 2,000 people on any given Sunday. In 1883, tightrope walker Professor Bachman crossed the gorge as part of a publicity stunt for a local hotel. On July 18, 1970, Karl Wallenda became the second man to walk across the gorge on a tightrope.

Geographic entities mentioned:
surface_form: bachman
instance_of: Lake
countries: United States
coordinates: lat: 32.848888888889
lon: -96.871111111111
Isteren. Isteren is a lake in Engerdal Municipality in Innlandet county, Norway. The lake lies to the southwest of the large lake Femunden and about northwest of the village of Drevsjø. Isteren is a lake with a large diversity of species. It is a popular fishing area, and the chances for the good catch is certainly present.

Geographic entities mentioned:
surface_form: Femunden
instance_of: Lake
countries: Norway
coordinates: lat: 62.183333333333
lon: 11.9
It is also rich in whitefish, pike, perch, grayling, burbot and herring. Around the lake there are two fish mounds and some single cabins. The river Sømåa, originating from lake Langsjøen, flows into Isteren from the north. It is a river with a rich bird life, especially in the spring. Here one can observe rare species of migrating birds.

Geographic entities mentioned:
surface_form: langsjøen
instance_of: Lake
countries: Norway
coordinates: lat: 62.166666666667
lon: 11.5875
surface_form: isteren
instance_of: Lake
countries: Norway
coordinates: lat: 62.01777778
lon: 11.77055556
Isteren. Isteren is a lake in Engerdal Municipality in Innlandet county, Norway. The lake lies to the southwest of the large lake Femunden and about northwest of the village of Drevsjø. Isteren is a lake with a large diversity of species. It is a popular fishing area, and the chances for the good catch is certainly present.

Geographic entities mentioned:
surface_form: isteren
instance_of: Lake
countries: Norway
coordinates: lat: 62.01777778
lon: 11.77055556
Isteren is a lake in Engerdal Municipality in Innlandet county, Norway. The lake lies to the southwest of the large lake Femunden and about northwest of the village of Drevsjø. Isteren is a lake with a large diversity of species. It is a popular fishing area, and the chances for the good catch is certainly present. In the summer of 2006, a trout weighing was caught with a rod from a small boat.

Geographic entities mentioned:
surface_form: isteren
instance_of: Lake
countries: Norway
coordinates: lat: 62.01777778
lon: 11.77055556
Battery Street Historic District. The Battery Street Historic District encompasses one of the oldest developed areas of Burlington, Vermont. With a history dating to 1790, this area, south of downtown Burlington and initially bounded roughly by Main, St.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
Nyanga people. The Nyanga (also &quot;Banianga&quot;, &quot;Banyanga&quot;, &quot;Kinyanga&quot;, &quot;Nianga&quot; or &quot;Nyangas&quot;) are a Bantu people in the African Great Lakes region. Today they live predominantly in the Kivu region of the Democratic Republic of the Congo, near the frontier with Rwanda and Uganda.

Geographic entities mentioned:
surface_form: African Great Lakes
instance_of: Group of lakes
countries: Burundi
Zambia
Kenya
Democratic Republic of the Congo
Malawi
Mozambique
Rwanda
Tanzania
Uganda
Ethiopia
coordinates: lat: -8
lon: 35
Lake Wylie. Lake Wylie is a reservoir or man-made lake in the U.S. states of South Carolina and North Carolina. The lake has a surface area of and features of shoreline. History. The man-made lake was first formed when the Catawba Power Company built the Catawba Dam and Power Plant near India Hook, South Carolina in 1904.

Geographic entities mentioned:
surface_form: lake wylie
instance_of: Lake
countries: United States
coordinates: lat: 35.085805555556
lon: -81.058583333333
The Southern Power Company was merged with Duke Power Company in 1927. In October 1960, the power station was renamed the Wylie Hydroelectric Station, and the lake was renamed Lake Wylie in honor of W. Gil Wylie, one of the founders of the original Catawba Power Company that had created the lake and become Duke Power. Other information.

Geographic entities mentioned:
surface_form: lake wylie
instance_of: Lake
countries: United States
coordinates: lat: 35.085805555556
lon: -81.058583333333
Gil Wylie, one of the founders of the original Catawba Power Company that had created the lake and become Duke Power. Other information. Lake Wylie's location on both the South Carolina and North Carolina borders makes it a common recreational destination for residents of nearby cities including Charlotte, Fort Mill, and Rock Hill. Duke Power manages six public boat access areas on the lake.

Geographic entities mentioned:
surface_form: lake wylie
instance_of: Lake
countries: United States
coordinates: lat: 35.085805555556
lon: -81.058583333333
Duke Power manages six public boat access areas on the lake. There are also two towns that are located on Lake Wylie, including Tega Cay and Lake Wylie. Lake Wylie is one of 11 lakes on the Catawba River and is the oldest lake in the Catawba River basin, with water being moved around each lake on the chain system through Duke Power.

Geographic entities mentioned:
surface_form: lake wylie
instance_of: Lake
countries: United States
coordinates: lat: 35.085805555556
lon: -81.058583333333
surface_form: lake wylie
instance_of: Lake
countries: United States
coordinates: lat: 35.085805555556
lon: -81.058583333333
Duke Power manages six public boat access areas on the lake. There are also two towns that are located on Lake Wylie, including Tega Cay and Lake Wylie. Lake Wylie is one of 11 lakes on the Catawba River and is the oldest lake in the Catawba River basin, with water being moved around each lake on the chain system through Duke Power.

Geographic entities mentioned:
surface_form: lake wylie
instance_of: Lake
countries: United States
coordinates: lat: 35.085805555556
lon: -81.058583333333
The Catawba Nuclear Generating Station is located on the south-western part of the lake, and draws its cooling water from the lake. Allen Steam Station located on the northern part of the lake (west of Charlotte) also draws its cooling water from the lake. The South Fork River and Catawba River confluence is now submerged under Lake Wylie near the North Carolina/South Carolina state line.

Geographic entities mentioned:
surface_form: lake wylie
instance_of: Lake
countries: United States
coordinates: lat: 35.085805555556
lon: -81.058583333333
This debris disk is constrained to a diameter of 12.2 AU. By 2001, the &quot;Long Wavelength Spectrometer&quot; at the Keck Observatory on Mauna Kea, Hawaii, was used more accurately to constrain the radius of the dust. It was found to lie within a 5.4 AU radius. The temperature of the dust was estimated as about 340 K.

Geographic entities mentioned:
surface_form: Mauna Kea
instance_of: Mountain
countries: United States
coordinates: lat: 19.820555555555554
lon: -155.46805555555557
A few years earlier, the Mughal Emperor had been forced to relinquish to the Marathas the right to collect &quot;Chauth&quot; taxes in Malwa and Gujarat. This levy was financially beneficial to the Maratha caste, as both the king Shahu and his Peshwa, Bajirao, were in large amounts of debt at the time. Agriculture in the Deccan depended heavily on the timeliness and duration of the monsoons.

Geographic entities mentioned:
surface_form: Deccan
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
Mount Ritchie. Mount Ritchie () is a mountain rising over 1600 m in the southeast part of Warren Range, Antarctica. The feature is northeast of Wise Peak on the west side of Deception Glacier.

Geographic entities mentioned:
surface_form: Wise Peak
instance_of: Mountain
coordinates: lat: -78.5833
lon: 158.3
Mount Ritchie. Mount Ritchie () is a mountain rising over 1600 m in the southeast part of Warren Range, Antarctica. The feature is northeast of Wise Peak on the west side of Deception Glacier.

Geographic entities mentioned:
surface_form: ritchie
instance_of: Mountain
coordinates: lat: -78.5333
lon: 158.417
surface_form: mount ritchie
instance_of: Mountain
coordinates: lat: -78.5333
lon: 158.417
The feature is northeast of Wise Peak on the west side of Deception Glacier. It was named by the Victoria University of Wellington Antarctic Expedition (VUWAE), 1970–71, after Alex Ritchie, curator of fossils at the Australian Museum, Sydney, a member of the VUWAE party that discovered important sites of fossil fish in this Skelton Neve area. Geology.

Geographic entities mentioned:
surface_form: ritchie
instance_of: Mountain
coordinates: lat: -78.5333
lon: 158.417
Geology. Mount Ritchie consists of a thick sequence of well-exposed, sedimentary strata of the Beacon Supergroup capped by a summit composed of an erosional remnant of a dolerite sill belonging to the Ferrar Dolerite sills. The dolerite summit of Mount Ritchie is underlain by of the Weller Coal Measures. It is composed of fossiliferous interbedded Permian sandstone, siltstone, shale, and coal.

Geographic entities mentioned:
surface_form: ritchie
instance_of: Mountain
coordinates: lat: -78.5333
lon: 158.417
surface_form: mount ritchie
instance_of: Mountain
coordinates: lat: -78.5333
lon: 158.417
These thrust sheets were caused by the north-eastward advance of grounded ice into a glaciomarine setting during a Late Paleozoic icehouse glacial epoch. Underlying the Metschel Tillite and forming the base of Mount Ritchie is over of late Devonian Aztec Siltstone.

Geographic entities mentioned:
surface_form: ritchie
instance_of: Mountain
coordinates: lat: -78.5333
lon: 158.417
surface_form: mount ritchie
instance_of: Mountain
coordinates: lat: -78.5333
lon: 158.417
Fossils. Mount Ritchie is an important late Devonian vertebrate fossil site in Antarctica. On Mount Ritchie, the Aztec Siltstone has yielded a varied fauna of fossil vertebrates and conchostracans.

Geographic entities mentioned:
surface_form: ritchie
instance_of: Mountain
coordinates: lat: -78.5333
lon: 158.417
surface_form: mount ritchie
instance_of: Mountain
coordinates: lat: -78.5333
lon: 158.417
Associated with these fossil fish were palynomorphs including &quot;Geminospora lemurata&quot;. Among the researchers who have collected and studied fossil vertebrates from Mount Ritchie include the eponymous A. Ritchie. The Wellner Coal Measures at Mount Ritchie contain abundant Permian leaf, root, petrified wood, and other plant fossils.

Geographic entities mentioned:
surface_form: ritchie
instance_of: Mountain
coordinates: lat: -78.5333
lon: 158.417
surface_form: ritchie
instance_of: Mountain
coordinates: lat: -78.5333
lon: 158.417
surface_form: ritchie
instance_of: Mountain
coordinates: lat: -78.5333
lon: 158.417
surface_form: mount ritchie
instance_of: Mountain
coordinates: lat: -78.5333
lon: 158.417
surface_form: mount ritchie
instance_of: Mountain
coordinates: lat: -78.5333
lon: 158.417
Very important on this route is the Lower Volta Bridge across the lower Volta River. Also, closer to the Lower Volta Bridge are the Holy Trinity Spa and Health Farm and the South Tongu District Assembly Office Complex. It is about 169.1 km(2 hours and 54 minutes drive via the Ho-Adidome road) from the famous Mount Afadja.

Geographic entities mentioned:
surface_form: Mount Afadja
instance_of: Mountain
countries: Ghana
coordinates: lat: 7.1444444444444
lon: 0.355
While he was still an infant, his family moved to Albany. His father resigned from his commission and worked as vice president of the English Speaking Union in New York City starting in 1949. Treadwell grew up on a 385-acre family estate called Bessboro Farm in Westport, New York, overlooking Lake Champlain. There, his father raised Holstein cattle. Treadwell had one brother, Thomas Ord Treadwell.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
This trading post is the oldest continuously inhabited settlement in Saskatchewan. The lake's location gave westward access for fur traders to the Saskatchewan River, north-west access to the Sturgeon-Weir River and the Churchill River system (and Lake Athabasca via the Methye Portage), and the Grass River, which lead north-east towards York Factory on Hudson Bay. Description.

Geographic entities mentioned:
surface_form: Lake Athabasca
instance_of: Lake
countries: Canada
coordinates: lat: 59.266666666667
lon: -109.45
surface_form: athabasca
instance_of: Lake
countries: Canada
coordinates: lat: 59.266666666667
lon: -109.45
surface_form: athabasca
instance_of: Mountain
countries: Canada
coordinates: lat: 52.18055555555556
lon: -117.20166666666667
The southern portion of the lake is within this Important Bird Area. The Saskatchewan River and several of its channels flow into the west end of the lake. The Sturgeon-Weir River, which has its source to the north at Corneille Lake, works its way into the lake through Namew Lake, Whitey Narrows, and Cross Lake. Cross Lake flows directly into the east end of Cumberland Lake.

Geographic entities mentioned:
surface_form: Namew Lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.23681
lon: -101.93471
Cumberland Lake. Cumberland Lake (formally Pine Island Lake) is a glacial lake in the Canadian province of Saskatchewan. It is situated in the Saskatchewan River Delta in east-central Saskatchewan, about from the Manitoba border. Cumberland House and Cumberland House Provincial Historic Park are on the south shore of the lake on Cumberland Island.

Geographic entities mentioned:
surface_form: cumberland lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.05
lon: -102.3
Access to the lake and its amenities is from Highway 123 and Cumberland House Airport. The area around Cumberland Lake has been inhabited by humans for over 7,000 years, is the site of the oldest permanent settlement in Saskatchewan, and was the interior hub for three canoe routes travelled by Voyageurs during the fur trade era.

Geographic entities mentioned:
surface_form: cumberland lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.05
lon: -102.3
Lake (and delta) water levels have been dropping in recent years due to upstream damming, water usage, and water diversion. History. For over 7,000 years, Cumberland Lake and the surrounding delta has been inhabited by Indigenous peoples. In 1774, Samuel Hearne built the Hudson's Bay Company's first major inland trading post on Cumberland Island on the southern shore of the lake.

Geographic entities mentioned:
surface_form: cumberland lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.05
lon: -102.3
Description. Cumberland lake is a large, shallow lake in the Saskatchewan River Delta — also known as the Cumberland Marshes. The delta, at almost, is the largest inland delta in North America and Cumberland Lake, at in size, is the largest lake in the delta.

Geographic entities mentioned:
surface_form: cumberland lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.05
lon: -102.3
The Sturgeon-Weir River, which has its source to the north at Corneille Lake, works its way into the lake through Namew Lake, Whitey Narrows, and Cross Lake. Cross Lake flows directly into the east end of Cumberland Lake. The main outflows include a channel that connects it back to the Saskatchewan River and Tearing River (which also connects back to the Saskatchewan River).

Geographic entities mentioned:
surface_form: cumberland lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.05
lon: -102.3
It is bounded by Pine Island to the west and Spruce Island and Cumberland Island to the south. Lake water levels. Water levels in Cumberland Lake have been falling due to upstream damming and water usage. Several upstream dams have been constructed for reservoirs that provide water for consumption, irrigation, and hydroelectricity.

Geographic entities mentioned:
surface_form: cumberland lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.05
lon: -102.3
This disruption is problematic as it affects natural cycles and habitats of fish and animals. Reduced water flows into Cumberland Lake have reduced the lake's average depth to about from. During the winter — which typically lasts five to six months — the lake, due to being shallow, &quot;nearly freezes to the bottom, largely impacting fish populations&quot;.

Geographic entities mentioned:
surface_form: cumberland lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.05
lon: -102.3
During the winter — which typically lasts five to six months — the lake, due to being shallow, &quot;nearly freezes to the bottom, largely impacting fish populations&quot;. There are concerns that the $4 billion future irrigation project that will draw water from Lake Diefenbaker will further cause water shortages in Cumberland Lake and the Saskatchewan River Delta.

Geographic entities mentioned:
surface_form: cumberland lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.05
lon: -102.3
Barnett Hills. The Barnett Hills are a mountain range in Churchill County, Nevada.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: barnett hills
instance_of: Landform
countries: United States
coordinates: lat: 39.1421
lon: -118.555
Barnett Hills. The Barnett Hills are a mountain range in Churchill County, Nevada.

Geographic entities mentioned:
surface_form: barnett hills
instance_of: Landform
countries: United States
coordinates: lat: 39.1421
lon: -118.555
Many traditional Chinese houses tend to display images of the menshen (threshold guardian). Some buildings were built with a &quot;foundation stone&quot; (石敢當), based on the Mount Tai in Shandong, with the inscription &quot;tài shān zài cǐ&quot; (泰山在此, &quot;Mount Tai is here&quot;) or &quot;tài shān shí gǎn dāng&quot; (泰山石敢當, &quot;the stone of Mount Tai dares to resist&quot;).

Geographic entities mentioned:
surface_form: Mount Tai
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 36.266666666667
lon: 117.1
The area is bisected by the Eastern Continental Divide and has about of hiking trails, including of the Appalachian Trail. The area is part of the Ridge and Valley System of mountains. The intersection of Potts Mountain and Salt Pond Mountain create a plateau like area. Piney ridge runs along the northeast side of the wilderness and Little Mountain on the northwest.

Geographic entities mentioned:
surface_form: Salt Pond Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.4085
lon: -80.4945
The minimum rainfall needed for berebere, is 350 millimeters. The western area of the zone is dominated by the Chari and Logone rivers, which flow north from their sources in southern Chad and neighboring countries. The courses of these rivers, joining at N'Djamena to flow on to Lake Chad, create an ecological subregion.

Geographic entities mentioned:
surface_form: Logone
instance_of: Watercourse
countries: Cameroon
Central African Republic
Chad
coordinates: lat: 12.106111111111
lon: 15.035277777778
In the rest of the Sahel, the hardier varieties of millet, along with peanuts and dry beans, are grown. Crop yields are far lower than they are in the south or near rivers and lakes. Farmers take every advantage of seasonal flooding to grow recession crops before the waters dry away, a practice particularly popular around Lake Fitri. The Sahel is ideal for pasturage.

Geographic entities mentioned:
surface_form: Lake Fitri
instance_of: Lake
countries: Chad
coordinates: lat: 12.809166666667
lon: 17.5025
He won by eight minutes in 2h 35m 0s. In 1911. he finished third in the Anerley 12-hour time-trial. That qualified him to ride for Britain in the 1912 Olympic Games road race in Stockholm. The race was run over 200 miles around lake Mälaren. The organisation was chaotic, with riders bunching together instead of being separated, cars impeding the competitors and errors in time-keeping.

Geographic entities mentioned:
surface_form: Mälaren
instance_of: Lake
countries: Sweden
coordinates: lat: 59.5
lon: 17.2
In 1938, following the Anschluss, Walther's father lost his position at the University of Graz. As a result, Walther spent the war years with his family on the Wallersee, a lake near Salzburg. This was a time when he developed his interest in studying the local geology as he helped his father with scientific investigations.

Geographic entities mentioned:
surface_form: Wallersee
instance_of: Lake
countries: Austria
coordinates: lat: 47.91388888888889
lon: 13.175
Meina. Meina is a &quot;comune&quot; (municipality) in the Province of Novara in the Italian region of Piedmont, located about northwest of Milan, about northeast of Turin and about north of Novara, on the southern area of Lake Maggiore. Meina is often called the &quot;village of villas&quot; because of the many grand residences that dot the shoreline.

Geographic entities mentioned:
surface_form: Lake Maggiore
instance_of: Lake
countries: Switzerland
Italy
coordinates: lat: 46.098055555555554
lon: 8.714722222222223
Gallup Glacier runs along its north side. Features include Mount Black in the west and Matador Mountain in the east. Nearby features include Mount Rosenwald to the northwest, Mount Heekin to the north and Half Century Nunatak to the south. Mount Black.

Geographic entities mentioned:
surface_form: Half Century Nunatak
instance_of: Mountain
coordinates: lat: -85.3667
lon: -178.833
Named by F. Alton Wade, leader of the Texas Tech Shackleton Glacier Expedition (1962-63) because all three members of the party were affiliated with this college. &quot;Matador&quot; is the general name for the student body at Texas Technological College. Mount Rosenwald. A spectacular mountain, high, which forms a distinctive landmark between the heads of Gallup and Baldwin Glaciers.

Geographic entities mentioned:
surface_form: the general
instance_of: Mountain
coordinates: lat: 44.483387
lon: -114.802816
Bennett Platform. Bennett Platform () is a high, nearly flat, snow-free mesa of dark rock of Antarctica, about long and wide, located immediately east of Mount Black, on the west side of Shackleton Glacier. Discovery and naming. Bennett Platform was discovered and photographed by U.S.

Geographic entities mentioned:
surface_form: discovery
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: discovery
instance_of: Body of water
coordinates: lat: -64.5167
lon: -63.0167
Bennett Platform. Bennett Platform () is a high, nearly flat, snow-free mesa of dark rock of Antarctica, about long and wide, located immediately east of Mount Black, on the west side of Shackleton Glacier. Discovery and naming. Bennett Platform was discovered and photographed by U.S.

Geographic entities mentioned:
surface_form: shackleton
instance_of: Mountain
coordinates: lat: -65.216666666667
lon: -63.933333333333
surface_form: bennett platform
instance_of: Plateau
coordinates: lat: -85.2167
lon: -177.833
Location. Bennett Platform is on the west side of Shackleton Glacier opposite the point where Logie Glacier joins it from the east through a gap in the Cumulus Hills. Gallup Glacier runs along its north side. Features include Mount Black in the west and Matador Mountain in the east.

Geographic entities mentioned:
surface_form: shackleton
instance_of: Mountain
coordinates: lat: -65.216666666667
lon: -63.933333333333
surface_form: bennett platform
instance_of: Plateau
coordinates: lat: -85.2167
lon: -177.833
Mount Black. A prominent mountain, high, with a gentle snow-covered slope on its southwest side and a steep rock face on its northwest side, forming a part of the polar escarpment just west of Bennett Platform and the upper reaches of Shackleton Glacier. Discovered and photographed by Rear Admiral Richard E.

Geographic entities mentioned:
surface_form: shackleton
instance_of: Mountain
coordinates: lat: -65.216666666667
lon: -63.933333333333
surface_form: bennett platform
instance_of: Plateau
coordinates: lat: -85.2167
lon: -177.833
Byrd on his return flight from the South Pole in November 1929, and named by him for Van Lear Black, American financier and contributor to ByrdAE of 1928-30 and 1933-35. Kitching Ridge. A prominent rock ridge on the west side of Shackleton Glacier, between Bennett Platform and Matador Mountain. Named by US-ACAN for South African vertebrate paleontologist James W.

Geographic entities mentioned:
surface_form: shackleton
instance_of: Mountain
coordinates: lat: -65.216666666667
lon: -63.933333333333
surface_form: bennett platform
instance_of: Plateau
coordinates: lat: -85.2167
lon: -177.833
Kitching who first found fossils here. Kitching was an exchange scientist with the Ohio State University Institute of Polar Studies 1970-71 geological party to the Queen Maud Mountains. Matador Mountain. A prominent, ice-free mountain, high, standing at the south side of the mouth of Gallup Glacier where the latter enters Shackleton Glacier. Named by F.

Geographic entities mentioned:
surface_form: shackleton
instance_of: Mountain
coordinates: lat: -65.216666666667
lon: -63.933333333333
A prominent, ice-free mountain, high, standing at the south side of the mouth of Gallup Glacier where the latter enters Shackleton Glacier. Named by F. Alton Wade, leader of the Texas Tech Shackleton Glacier Expedition (1962-63) because all three members of the party were affiliated with this college. &quot;Matador&quot; is the general name for the student body at Texas Technological College.

Geographic entities mentioned:
surface_form: shackleton
instance_of: Mountain
coordinates: lat: -65.216666666667
lon: -63.933333333333
Named by US-ACAN for John W. McDonough, USARP ionospheric physicist at the South Pole Station, 1962. Mount Heekin. A large, ice-free mountain overlooking the north side of the mouth of Baldwin Glacier where the latter enters Shackleton Glacier. Discovered and photographed by USN OpHjp (1946-47) on the flights of February 16, 1947, and named by US-ACAN for Lt. (j-g-) Robert P.

Geographic entities mentioned:
surface_form: shackleton
instance_of: Mountain
coordinates: lat: -65.216666666667
lon: -63.933333333333
surface_form: baldwin
instance_of: Mountain
coordinates: lat: -72.2575
lon: 163.28666667
&quot;Matador&quot; is the general name for the student body at Texas Technological College. Mount Rosenwald. A spectacular mountain, high, which forms a distinctive landmark between the heads of Gallup and Baldwin Glaciers. The mountain is entirely snow covered on the southwest side but has nearly vertical exposed-rock cliffs on the northeast side.

Geographic entities mentioned:
surface_form: baldwin
instance_of: Mountain
coordinates: lat: -72.2575
lon: 163.28666667
Bennett Platform. Bennett Platform () is a high, nearly flat, snow-free mesa of dark rock of Antarctica, about long and wide, located immediately east of Mount Black, on the west side of Shackleton Glacier. Discovery and naming. Bennett Platform was discovered and photographed by U.S.

Geographic entities mentioned:
surface_form: bennett platform
instance_of: Plateau
coordinates: lat: -85.2167
lon: -177.833
Discovery and naming. Bennett Platform was discovered and photographed by U.S. Navy Operation Highjump (1946–47), on the flights of February 16, 1947, and named by the United States Advisory Committee on Antarctic Names (US-ACAN) for Floyd Bennett, copilot on the Byrd North Pole Flight of May 1926. Location.

Geographic entities mentioned:
surface_form: bennett platform
instance_of: Plateau
coordinates: lat: -85.2167
lon: -177.833
As a result, HCE goes into hiding, where he is besieged at the closed gate of his pub by a visiting American looking for a drink after hours. HCE remains silent – not responding to the accusations or verbal abuse – dreams, is buried in a coffin at the bottom of Lough Neagh, and is finally brought to trial, under the name Festy King. He is eventually freed, and goes once more into hiding.

Geographic entities mentioned:
surface_form: Lough Neagh
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.618333333333
lon: -6.3952777777778
The municipal unit has an area of 54.447 km2. History. The traveler who will feel the need to visit the historical town of Ampelakia (nicknamed &quot;The jewel of Thessaly&quot;), has to go up the well made road that starts from the Tempe Valley. After just 5 kilometers is Ampelakia. As we get closer to the town the mansion of George Mavros (Schwartz) stands out.

Geographic entities mentioned:
surface_form: Tempe Valley
instance_of: Valley
countries: Greece
coordinates: lat: 39.872778
lon: 22.546667
From other directions, it is less distinctive and harder to identify, such as from the road around the summit of Dlouhé stráně, where it appears to have a somewhat flattened ridge and is located between the peaks of Červená hora and. From the road encircling the summit of Praděd, it is difficult to recognize, as it is visible above. Slopes.

Geographic entities mentioned:
surface_form: Dlouhé stráně
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.07125
lon: 17.15675
surface_form: červená hora
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 49.7767
lon: 17.5411
surface_form: červená hora
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.14425
lon: 17.13597222222222
surface_form: dlouhé stráně
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.07125
lon: 17.15675
From other directions, it is less distinctive and harder to identify, such as from the road around the summit of Dlouhé stráně, where it appears to have a somewhat flattened ridge and is located between the peaks of Červená hora and. From the road encircling the summit of Praděd, it is difficult to recognize, as it is visible above. Slopes.

Geographic entities mentioned:
surface_form: Praděd
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.083194444444445
lon: 17.23086111111111
surface_form: praděd
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.083194444444445
lon: 17.23086111111111
The road includes nine road loops at elevations of 609, 620, 699, 770, 800, 832, 865, 897, and 922 m above sea level. The road is secured with guardrails along the mountain side, offering views towards many nearby peaks such as Dlouhé stráně, Medvědí hora, Suchá hora, and, at higher elevations, the tower on Praděd. Summit. Velký Klínovec is a mountain with a single summit.

Geographic entities mentioned:
surface_form: Dlouhé stráně
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.07125
lon: 17.15675
surface_form: Medvědí hora
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.08775
lon: 17.147166666666667
surface_form: praděd
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.083194444444445
lon: 17.23086111111111
surface_form: medvědí hora
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.08775
lon: 17.147166666666667
surface_form: dlouhé stráně
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.07125
lon: 17.15675
According to the publisher=State Administration of Land Surveying and Cadastre, the highest point of the mountain is the summit, with an elevation of 1,166.9 m above sea level and coordinates. Close to the summit's rocky outcrop is the starting area for the ski trails, providing perspectives on the peaks of the Keprník Mountains: Ucháč, Černá stráň,, Červená hora, and, and. Geology.

Geographic entities mentioned:
surface_form: Ucháč
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.093
lon: 17.048333333333332
surface_form: Černá stráň
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.12155555555555
lon: 17.077666666666666
surface_form: keprník
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.17086111111111
lon: 17.116444444444443
surface_form: červená hora
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 49.7767
lon: 17.5411
surface_form: ucháč
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.093
lon: 17.048333333333332
surface_form: červená hora
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.14425
lon: 17.13597222222222
surface_form: černá stráň
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.12155555555555
lon: 17.077666666666666
– Velký Klínovec – Hřebenová pass – – Sedlo pod Malým Jezerníkem pass – – – Sedlo Velký Jezerník pass – &quot;Švýcárna&quot; mountain hut – Praděd – pass – Petrovy kameny – – pass – Vysoká hole – Vysoká hole–JZ – – – pass – – Jelení studánka – Sedlo pod Jelení studánkou pass – – – Rýmařov
Červenohorské sedlo – Velký Klínovec – Výrovka Mountain – Malý Jezerník Mountain – &quot;Kamzík&quot;
Filipovice – – spring – – Velký Klínovec – Červenohorské sedlo – Kouty nad Desnou – Hučivá Desná valley – Sedlo pod Vřesovkou pass – Kamenne okno – Červená hora – &quot;Bílý sloup&quot;
Kouty nad Desnou – – – &quot;Kamzík&quot; – Velký Jezerník – Sedlo Velký Jezerník pass – &quot;Švýcárna&quot; mountain hut – Praděd – U Barborky pass – Petrovy kameny – Ovčárna – Karlova Studánka
Cycling routes.

Geographic entities mentioned:
surface_form: Praděd
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.083194444444445
lon: 17.23086111111111
surface_form: Vysoká hole
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.06263888888889
lon: 17.235611111111112
surface_form: praděd
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.083194444444445
lon: 17.23086111111111
surface_form: praděd
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.083194444444445
lon: 17.23086111111111
surface_form: desná
instance_of: Watercourse
countries: Czech Republic
coordinates: lat: 50.054632
lon: 17.222911
surface_form: klínovec
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.396111111111
lon: 12.967777777778
surface_form: klínovec
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.396111111111
lon: 12.967777777778
surface_form: klínovec
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.396111111111
lon: 12.967777777778
surface_form: červená hora
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 49.7767
lon: 17.5411
surface_form: červená hora
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.14425
lon: 17.13597222222222
surface_form: velký klínovec
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.11913888888889
lon: 17.162666666666667
surface_form: velký klínovec
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.11913888888889
lon: 17.162666666666667
surface_form: velký klínovec
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.11913888888889
lon: 17.162666666666667
surface_form: vysoká
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 49.4039
lon: 18.3611
surface_form: vysoká
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 49.4039
lon: 18.3611
surface_form: vysoká hole
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.06263888888889
lon: 17.235611111111112
surface_form: vysoká hole
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.06263888888889
lon: 17.235611111111112