Sarmila/GeoWiki-Features huggingface dataset:
The lake is named for Sebring's developer, George Sebring. It is a shallow muck lake with max depth of. A public boat ramp, on the lake's southwest, is just off Memorial Drive. Canals connect the lake to Little Red Water Lake, to the northeast, and to Lake Jackson, to the south. Canals indirectly connect a number of area lakes to Lake Sebring. Fishing is allowed.

Geographic entities mentioned:
surface_form: Little Red Water Lake
instance_of: Lake
countries: United States
coordinates: lat: 27.5411
lon: -81.472
surface_form: lake jackson
instance_of: Lake
countries: United States
coordinates: lat: 33.368
lon: -83.8555
Lake Sebring. Lake Sebring is a natural freshwater lake in Highlands County, Florida, and located north of Sebring, Florida, and Lake Jackson. The lake is somewhat oval shaped and has a surface area. The lake is named for Sebring's developer, George Sebring. It is a shallow muck lake with max depth of. A public boat ramp, on the lake's southwest, is just off Memorial Drive.

Geographic entities mentioned:
surface_form: lake sebring
instance_of: Lake
countries: United States
coordinates: lat: 27.5286
lon: -81.484
Lake Sebring. Lake Sebring is a natural freshwater lake in Highlands County, Florida, and located north of Sebring, Florida, and Lake Jackson. The lake is somewhat oval shaped and has a surface area. The lake is named for Sebring's developer, George Sebring. It is a shallow muck lake with max depth of. A public boat ramp, on the lake's southwest, is just off Memorial Drive.

Geographic entities mentioned:
surface_form: lake sebring
instance_of: Lake
countries: United States
coordinates: lat: 27.5286
lon: -81.484
surface_form: lake jackson
instance_of: Lake
countries: United States
coordinates: lat: 33.368
lon: -83.8555
It is a shallow muck lake with max depth of. A public boat ramp, on the lake's southwest, is just off Memorial Drive. Canals connect the lake to Little Red Water Lake, to the northeast, and to Lake Jackson, to the south. Canals indirectly connect a number of area lakes to Lake Sebring. Fishing is allowed. The lake has largemouth bass, Florida gar, bowfin, Florida crappie and two types of catfish.

Geographic entities mentioned:
surface_form: lake sebring
instance_of: Lake
countries: United States
coordinates: lat: 27.5286
lon: -81.484
Canals connect the lake to Little Red Water Lake, to the northeast, and to Lake Jackson, to the south. Canals indirectly connect a number of area lakes to Lake Sebring. Fishing is allowed. The lake has largemouth bass, Florida gar, bowfin, Florida crappie and two types of catfish. No public swimming beaches are on Lake Sebring's shore.

Geographic entities mentioned:
surface_form: lake sebring
instance_of: Lake
countries: United States
coordinates: lat: 27.5286
lon: -81.484
It extends from west Phillipsburg northeast approximately to Allamuchy Township, New Jersey. The ridge continues on north past Washington as Upper Pohatcong Mountain. It is located in eastern Warren County, and extends northeast of Washington approximately 6 mi (10 km) to the vicinity of Hackettstown.

Geographic entities mentioned:
surface_form: Upper Pohatcong Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.8437
lon: -74.8576
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: pohatcong mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.7303
lon: -75.0175
The ridge continues on north past Washington as Upper Pohatcong Mountain. It is located in eastern Warren County, and extends northeast of Washington approximately 6 mi (10 km) to the vicinity of Hackettstown. The ridge has an average height of approximately 800 ft (240 m) and reaches a maximum summit of 1235 ft (374 m).

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Pohatcong Mountain. Pohatcong Mountain is a ridge, approximately 6 mi (10 km) long, in the Appalachian Mountains of northwestern New Jersey in the United States. It extends from west Phillipsburg northeast approximately to Allamuchy Township, New Jersey. The ridge continues on north past Washington as Upper Pohatcong Mountain.

Geographic entities mentioned:
surface_form: pohatcong mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.7303
lon: -75.0175
The ridge has an average height of approximately 800 ft (240 m) and reaches a maximum summit of 1235 ft (374 m). The term &quot;Pohatcong Mountain&quot; is sometimes taken to include both Pohatcong and Upper Pohatcong Mountain. The ridge is approximately 800 ft (244 m) high along much of its length.

Geographic entities mentioned:
surface_form: pohatcong mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.7303
lon: -75.0175
surface_form: pohatcong mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.7303
lon: -75.0175
Taxonomy. The deepwater sculpin was first described in 1851 by Charles Frédéric Girard under the name &quot;Triglopsis thompsonii&quot;. The description was based on specimens obtained by Spencer Fullerton Baird for the Smithsonian Institution from the stomachs of burbot (&quot;Lota lota&quot;) caught by anglers on Lake Ontario.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Age estimation with otoliths suggests that deepwater sculpin can live up to nine years. Distribution and habitat. The deepwater sculpin is found from the Gatineau through the Laurentian Great Lakes, Manitoba, and Saskatchewan to the Great Slave and Great Bear Lakes. It is also found in Waterton Lake within Waterton Lakes National Park and Glacier National Park.

Geographic entities mentioned:
surface_form: Great Slave
instance_of: Lake
countries: Canada
coordinates: lat: 61.666666666667
lon: -114
surface_form: Great Bear Lake
instance_of: Lake
countries: Canada
coordinates: lat: 66
lon: -121
The deepwater sculpin is found from the Gatineau through the Laurentian Great Lakes, Manitoba, and Saskatchewan to the Great Slave and Great Bear Lakes. It is also found in Waterton Lake within Waterton Lakes National Park and Glacier National Park. Within its range, it is limited to deep, well-oxygenated lakes with ties to former Wisconsinan glacial lakes or the Champlain Sea.

Geographic entities mentioned:
surface_form: Waterton Lake
instance_of: Lake
countries: Canada
United States
coordinates: lat: 49
lon: -113.9
They will also take chironomid larvae. Zooplankton are likely prey at the larval stage. Reproduction. Spawning of deepwater sculpin is poorly described, but evaluations of gonadal development suggests that spawning consists of a singular event over a prolonged period in Lake Ontario. Deepwater sculpin eggs hatch from November to August, peaking in March.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Most of these trails have been built along the abandoned rail grades that run along the river (see Rail trail). The Ohio to Erie Trail project, under construction, aims to link these trails to other trails statewide to create a single bike trail from Lake Erie to the Ohio River. The Little Miami is also popular among canoers and anglers.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Route 202. A network of suburban streets climb the southern slopes of the mountain, and a number of communications towers sprout from the summit peaks. The Metacomet Ridge extends north from Talcott Mountain as Hatchet Hill and south as Farmington Mountain. The north and west sides of the mountain drain into the Farmington River, thence into the Connecticut River and Long Island Sound.

Geographic entities mentioned:
surface_form: Farmington Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.713433333333
lon: -72.815652777778
surface_form: hatchet hill
instance_of: Mountain
countries: United States
coordinates: lat: 41.9281
lon: -72.7475
surface_form: farmington mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.713433333333
lon: -72.815652777778
The north and west sides of the mountain drain into the Farmington River, thence into the Connecticut River and Long Island Sound. The Farmington River runs along the west base of the mountain, cutting through the Metacomet Ridge between Talcott Mountain and Hatchet Hill at the Tarriffville Gorge.

Geographic entities mentioned:
surface_form: hatchet hill
instance_of: Mountain
countries: United States
coordinates: lat: 41.9281
lon: -72.7475
surface_form: talcott mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.825
lon: -72.798
Notable peaks on the ridge include the high point, on which stands the historic Heublein Tower,; &quot;Ely Mound,&quot;, a conical peak south of the main summit overlooking Ely Pond; &quot;Kilkenny Rocks,&quot;, an exposed ledge near the southern end of the mountain; &quot;King Phillip Mountain,&quot;, just north of the main summit; &quot;Burnt Hill&quot;, a summit located on the southeast side of the mountain; and &quot;The Pinnacle&quot; (not to be confused with Pinnacle Rock of Plainville, Connecticut, also part of the Metacomet Ridge to the south), in Penwood State Park, just north of the centerpoint of the mountain.

Geographic entities mentioned:
surface_form: burnt hill
instance_of: Mountain
countries: United States
coordinates: lat: 42.258888888889
lon: -74.685555555556
surface_form: the pinnacle
instance_of: Mountain
countries: United States
coordinates: lat: 35.207816666667
lon: -81.312627777778
surface_form: high point
instance_of: Mountain
countries: United States
coordinates: lat: 41.924722222222
lon: -74.288055555556
surface_form: pinnacle rock
instance_of: Mountain
countries: United States
coordinates: lat: 41.6897
lon: -72.8328
surface_form: high point
instance_of: Mountain
countries: United States
coordinates: lat: 41.3209
lon: -74.6616
surface_form: the pinnacle
instance_of: Mountain
countries: United States
coordinates: lat: 40.6128
lon: -75.9114
Talcott Mountain. Talcott Mountain of central Connecticut, with a high point of, is a long trap rock mountain ridge located west of the city of Hartford. The ridge, a prominent landscape feature, forms a continuous line of exposed western cliffs visible across the Farmington River valley from Farmington to Simsbury.

Geographic entities mentioned:
surface_form: high point
instance_of: Mountain
countries: United States
coordinates: lat: 41.924722222222
lon: -74.288055555556
surface_form: talcott mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.825
lon: -72.798
surface_form: high point
instance_of: Mountain
countries: United States
coordinates: lat: 41.3209
lon: -74.6616
surface_form: rock mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.799444444444
lon: -120.97444444444
The Farmington River runs along the west base of the mountain, cutting through the Metacomet Ridge between Talcott Mountain and Hatchet Hill at the Tarriffville Gorge. The east side of the mountain drains into the Park River, thence into the Connecticut River and Long Island Sound. Geology.

Geographic entities mentioned:
surface_form: long island
instance_of: Landform
countries: United States
coordinates: lat: 46.7269
lon: -90.785
Talcott Mountain. Talcott Mountain of central Connecticut, with a high point of, is a long trap rock mountain ridge located west of the city of Hartford. The ridge, a prominent landscape feature, forms a continuous line of exposed western cliffs visible across the Farmington River valley from Farmington to Simsbury.

Geographic entities mentioned:
surface_form: talcott mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.825
lon: -72.798
The ridge, a prominent landscape feature, forms a continuous line of exposed western cliffs visible across the Farmington River valley from Farmington to Simsbury. Talcott Mountain is part of the narrow, linear Metacomet Ridge that extends from Long Island Sound near New Haven, Connecticut, north through the Connecticut River Valley of Massachusetts to the Vermont border.

Geographic entities mentioned:
surface_form: talcott mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.825
lon: -72.798
surface_form: long island
instance_of: Landform
countries: United States
coordinates: lat: 46.7269
lon: -90.785
surface_form: river valley
instance_of: Valley
countries: United States
coordinates: lat: 35.36
lon: -93.37
A popular outdoor recreation resource, Talcott Mountain is known for its microclimate ecosystems, rare plant communities, and expansive views from cliffs that tower up to above the surrounding landscape. Talcott Mountain encompasses two state parks, several municipal recreation areas and reservoirs, a science center and school, a demonstration forest, and the historic Heublein Tower.

Geographic entities mentioned:
surface_form: talcott mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.825
lon: -72.798
The Metacomet Trail traverses the ridge. Geography. The Talcott Mountain ridgeline, located in Farmington, West Hartford, Avon, Bloomfield, and Simsbury, Connecticut, is composed of a tiered series of west facing cliffs punctuated by knobs and peaks. Two of the ridge tiers are distinct along most of the mountain's length; additional tiers manifest themselves over shorter sections of the mountain.

Geographic entities mentioned:
surface_form: talcott mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.825
lon: -72.798
Geography. The Talcott Mountain ridgeline, located in Farmington, West Hartford, Avon, Bloomfield, and Simsbury, Connecticut, is composed of a tiered series of west facing cliffs punctuated by knobs and peaks. Two of the ridge tiers are distinct along most of the mountain's length; additional tiers manifest themselves over shorter sections of the mountain. Talcott Mountain is at its widest point.

Geographic entities mentioned:
surface_form: talcott mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.825
lon: -72.798
Talcott Mountain is an important aquifer serving metropolitan Hartford and several other communities. Notable reservoirs and other bodies of water on the mountain include: Wash Brook Pond; Lake Louise, a glacial kettle pond with a swamp boardwalk, observation platform, and waterfall; Hartford Reservoirs #'s 1, 2, 3, 5, and 6; Hoe Pond; Ely Pond; Dyke Pond; and Woodridge Lake.

Geographic entities mentioned:
surface_form: lake louise
instance_of: Lake
countries: United States
coordinates: lat: 45.92916667
lon: -95.41888889
Basalt frequently breaks into octagonal and pentagonal columns, creating a unique &quot;postpile&quot; appearance. Huge slopes made of fractured basalt scree are visible beneath many of the ledges of Talcott Mountain; they are particularly evident along the base of the lower tier of cliffs west of Heublein Tower.

Geographic entities mentioned:
surface_form: talcott mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.825
lon: -72.798
Because the trap rock ridges generate such varied terrain, they are the home of several plant and animal species that are state-listed or globally rare. Infestation by an invasive species, the Hemlock Woolly Adelgid, resulted in the death of large stands of mature eastern hemlock in Penwood State Park on Talcott Mountain.

Geographic entities mentioned:
surface_form: talcott mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.825
lon: -72.798
surface_form: hemlock
instance_of: Lake
countries: United States
coordinates: lat: 42.718611111111
lon: -77.608888888889
The infestation and subsequent tree removal dramatically impacted the character of the forests on that part of the mountain. The massive Pinchot Sycamore, a champion tree candidate with a trunk in diameter, is located at the foot of the mountain next to the Farmington River in Simsbury. Talcott Mountain is also an important seasonal raptor migration path. Recreation.

Geographic entities mentioned:
surface_form: talcott mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.825
lon: -72.798
The Metropolitan District Commission of Connecticut (MDC), a non-profit municipal corporation chartered by the state of Connecticut, manages more than on Talcott Mountain as public water supply, watershed, and open space. Besides providing drinking water, the MDC manages hiking trails and dirt roads (non-motorized use only) and practices silvaculture in the property's forests.

Geographic entities mentioned:
surface_form: talcott mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.825
lon: -72.798
In 2000, Talcott Mountain was included in a study by the National Park Service for the designation of a new National Scenic Trail now tentatively called the New England National Scenic Trail, which would include the Metacomet-Monadnock Trail in Massachusetts, and the Mattabesett Trail and Metacomet Trail in Connecticut.

Geographic entities mentioned:
surface_form: talcott mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.825
lon: -72.798
A number of regional and local non-profit organizations are active in conserving the landscape and ecosystems of Talcott Mountain, most notably the Connecticut Forest and Park Association, Simsbury Land Trust, Avon Land Trust and the Farmington Land Trust.

Geographic entities mentioned:
surface_form: talcott mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.825
lon: -72.798
Eastern red cedar, a dry-loving species, clings to the barren edges of cliffs. Cooler east-facing backslopes tend to support extensive stands of eastern hemlock interspersed with the oak-hickory forest species more common in the surrounding lowlands. Narrow ravines crowded with hemlock block sunlight, creating damp, cooler growing conditions with associated cooler climate plant species.

Geographic entities mentioned:
surface_form: hemlock
instance_of: Lake
countries: United States
coordinates: lat: 42.718611111111
lon: -77.608888888889
surface_form: hemlock
instance_of: Lake
countries: United States
coordinates: lat: 42.718611111111
lon: -77.608888888889
Infestation by an invasive species, the Hemlock Woolly Adelgid, resulted in the death of large stands of mature eastern hemlock in Penwood State Park on Talcott Mountain. The Connecticut Department of Environmental Protection began a program of removal of dead trees and contaminated living trees in 2000.

Geographic entities mentioned:
surface_form: dead
instance_of: Watercourse
countries: United States
coordinates: lat: 45.3333
lon: -69.9697
Route 202. A network of suburban streets climb the southern slopes of the mountain, and a number of communications towers sprout from the summit peaks. The Metacomet Ridge extends north from Talcott Mountain as Hatchet Hill and south as Farmington Mountain. The north and west sides of the mountain drain into the Farmington River, thence into the Connecticut River and Long Island Sound.

Geographic entities mentioned:
surface_form: long island
instance_of: Landform
countries: United States
coordinates: lat: 46.7269
lon: -90.785
Talcott Mountain. Talcott Mountain of central Connecticut, with a high point of, is a long trap rock mountain ridge located west of the city of Hartford. The ridge, a prominent landscape feature, forms a continuous line of exposed western cliffs visible across the Farmington River valley from Farmington to Simsbury.

Geographic entities mentioned:
surface_form: river valley
instance_of: Valley
countries: United States
coordinates: lat: 35.36
lon: -93.37
Veeder, an industrialist, inventor, and outdoorsperson. Veeder wished the property to &quot;be kept in a natural state so that those who love nature may enjoy this property as I have enjoyed it.&quot; He blazed many of the original trails in the park; Lake Louise, a scenic kettle pond atop the ridge, also called Gale Pond, was named after his wife.

Geographic entities mentioned:
surface_form: lake louise
instance_of: Lake
countries: United States
coordinates: lat: 45.92916667
lon: -95.41888889
The population are predominantly of indigenous descent. Geography. Pathibhara is located in the Himalayas in the northeast of the country. Pathibhara borders Pawakhola to the east, Num to the south, Makalu to the west and Hatiya to the north. It lies in proximity to Makalu (8,485 m), the world's fifth highest peak. It is located near the Makalu Barun National Park.

Geographic entities mentioned:
surface_form: Makalu
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.889166666667
lon: 87.088611111111
Max Burghardt. Max Burghardt (November 27, 1893 – January 22, 1977) was a German actor, director, and president of the Cultural Association of the GDR. Life. Burghardt was born in Wickendorf, Schwerin, where his maternal grandfather owned a small estate near Lake Schwerin. He lived there for about three to four years and then moved with his family to Berlin-Moabit.

Geographic entities mentioned:
surface_form: Lake Schwerin
instance_of: Lake
countries: Germany
coordinates: lat: 53.716666666667
lon: 11.466666666667
Blackwater Creek (Lake County, Florida). Blackwater Creek is an approximately 19 mile riverine feature in Florida. The creek flows from Lake Norris and has a confluence with the Wekiva River near where it in turn flows into the St. Johns River. The upper sections of Black Creek are traversed by kayak and canoe. Other sections a difficult to navigate due to snags.

Geographic entities mentioned:
surface_form: Lake Norris
instance_of: Lake
countries: United States
coordinates: lat: 28.9377
lon: -81.5349
Allium feinbergii. &quot;Allium feinbergii&quot; is a species of onions found on Mount Hermon, near where the three nations of Israel, Syria, and Lebanon meet. It is a bulb-forming perennial producing an umbel of flowers. Flowers are reddish-purple, narrowly urn-shaped, on long peduncles so that most of them are drooping.

Geographic entities mentioned:
surface_form: Mount Hermon
instance_of: Mountain
countries: Lebanon
Israel
Syria
coordinates: lat: 33.4
lon: 35.85
Price Glacier (Mount Shuksan). Price Glacier is in North Cascades National Park in the U.S. state of Washington, on the northeast slopes of Mount Shuksan, below the subpeak known as Nooksack Tower. Price Glacier descends from and is the steepest and most heavily crevasseed glacier on Mount Shuksan. The disconnected lowest portions of Price Glacier calve small icebergs into Price Lake.

Geographic entities mentioned:
surface_form: Mount Shuksan
instance_of: Mountain
countries: United States
coordinates: lat: 48.8316
lon: -121.603
surface_form: Nooksack Tower
instance_of: Mountain
countries: United States
coordinates: lat: 48.8364
lon: -121.587
Upstream from the gorges, its name is the Niari River and it flows through the Niari Valley. The river combines with the Louessé, the Loudima and the Bouenza River and eventually flows into the Atlantic Ocean. It covers about 560 km from its origin in the Batéké Plateau of the Congo to its mouth at the coast.

Geographic entities mentioned:
surface_form: Bouenza River
instance_of: Watercourse
countries: Republic of the Congo
coordinates: lat: -4.1855555555556
lon: 13.820277777778
The river combines with the Louessé, the Loudima and the Bouenza River and eventually flows into the Atlantic Ocean. It covers about 560 km from its origin in the Batéké Plateau of the Congo to its mouth at the coast. The lower Kouilou basin has been designated an Important Bird Area (IBA) by BirdLife International because it supports significant populations of many bird species. Hydrology.

Geographic entities mentioned:
surface_form: Batéké Plateau
instance_of: Plateau
countries: Gabon
Republic of the Congo
coordinates: lat: -3.51
lon: 15.76
Mount Race. Mount Race, is a mountain in Berkshire County, Massachusetts. It shares many characteristics with the slightly higher Mount Everett about a mile to the north. Part of the Taconic Mountains, Race is known for its waterfalls, an eastern escarpment of nearly 2,000 feet, and expansive views.

Geographic entities mentioned:
surface_form: Mount Everett
instance_of: Mountain
countries: United States
coordinates: lat: 42.1019
lon: -73.4325
The peak bears the surname of William Race, a local resident killed in 1755 by agents of Livingston Manor in a colonial border dispute concerning ownership and farm tenancy. Western slopes are in the town of Mount Washington, and the east slopes are in Sheffield, Massachusetts. Much of the mountain is part of Mount Washington State Forest; other parcels are privately held.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: mount washington
instance_of: Mountain
countries: United States
coordinates: lat: 47.5311964
lon: -123.2459807
Mount Race. Mount Race, is a mountain in Berkshire County, Massachusetts. It shares many characteristics with the slightly higher Mount Everett about a mile to the north. Part of the Taconic Mountains, Race is known for its waterfalls, an eastern escarpment of nearly 2,000 feet, and expansive views.

Geographic entities mentioned:
surface_form: mount race
instance_of: Mountain
countries: United States
coordinates: lat: 42.0825
lon: -73.4322
Details. Both Race Brook Falls and Bear Rock Falls spill from the steep eastern slopes of Mount Race, the summit of which is part of a divide between the Hudson and Housatonic rivers. The peak bears the surname of William Race, a local resident killed in 1755 by agents of Livingston Manor in a colonial border dispute concerning ownership and farm tenancy.

Geographic entities mentioned:
surface_form: mount race
instance_of: Mountain
countries: United States
coordinates: lat: 42.0825
lon: -73.4322
Balsam Beartown Mountain. Balsam Beartown Mountain is a mountain located in Tazewell County, Virginia, in the United States. The mountain is the sixth-highest mountain in Virginia by elevation, sixth in the state by prominence, as well as sixth in the state by isolation.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: balsam beartown mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.081416
lon: -81.413675
surface_form: beartown mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.9362
lon: -81.8865
Balsam Beartown Mountain. Balsam Beartown Mountain is a mountain located in Tazewell County, Virginia, in the United States. The mountain is the sixth-highest mountain in Virginia by elevation, sixth in the state by prominence, as well as sixth in the state by isolation.

Geographic entities mentioned:
surface_form: balsam beartown mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.081416
lon: -81.413675
surface_form: beartown mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.9362
lon: -81.8865
Even though this evidence comes from the Middle East, it has been suggested that the 'cradle' of schistosomes lies in the region of the African Great Lakes, an area in which both the parasites and their intermediate hosts are in an active state of evolution.

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
Lütschental became a part of the Bernese bailiwick of Interlaken. Beginning in the late 19th century, the population of the village dropped as residents moved to the cities of the Swiss Plateau or emigrated in search of jobs. The construction of a power plant for the Jungfrau railway, in 1908, provided more jobs but was unable to stop the population decline.

Geographic entities mentioned:
surface_form: Swiss Plateau
instance_of: Plateau
countries: Switzerland
coordinates: lat: 47.1167
lon: 7.36667
He joined the Academic Flying League and started to construct gliders, as production and operation of powered aircraft in Germany had been restricted under the provisions of the 1919 Treaty of Versailles. Baade also learned to fly and participated in the annual glider competitions at the Wasserkuppe.

Geographic entities mentioned:
surface_form: Wasserkuppe
instance_of: Mountain
countries: Germany
coordinates: lat: 50.498055555556
lon: 9.9377777777778
The elevation at the summit is. Geography. Unlike surrounding mountains, Roundtop Hill is not part of an extended ridge system, and is only about in length. It is located just under from the crest of Tonoloway Ridge, about southwest of Hancock. Its presence causes a large bend in the Potomac River, which curves around its eastern slope.

Geographic entities mentioned:
surface_form: Tonoloway Ridge
instance_of: Mountain
countries: United States
coordinates: lat: 39.571666666667
lon: -78.325555555556
Roundtop Hill (Maryland). Roundtop Hill is a mountain in Washington County, Maryland, southwest of the town of Hancock. The elevation at the summit is. Geography. Unlike surrounding mountains, Roundtop Hill is not part of an extended ridge system, and is only about in length. It is located just under from the crest of Tonoloway Ridge, about southwest of Hancock.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: roundtop hill
instance_of: Mountain
countries: United States
coordinates: lat: 39.68
lon: -78.32
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: roundtop
instance_of: Mountain
countries: United States
coordinates: lat: 42.293888888889
lon: -74.490555555556
Roundtop Hill (Maryland). Roundtop Hill is a mountain in Washington County, Maryland, southwest of the town of Hancock. The elevation at the summit is. Geography. Unlike surrounding mountains, Roundtop Hill is not part of an extended ridge system, and is only about in length. It is located just under from the crest of Tonoloway Ridge, about southwest of Hancock.

Geographic entities mentioned:
surface_form: roundtop hill
instance_of: Mountain
countries: United States
coordinates: lat: 39.68
lon: -78.32
surface_form: roundtop
instance_of: Mountain
countries: United States
coordinates: lat: 42.293888888889
lon: -74.490555555556
The elevation at the summit is. Geography. Unlike surrounding mountains, Roundtop Hill is not part of an extended ridge system, and is only about in length. It is located just under from the crest of Tonoloway Ridge, about southwest of Hancock. Its presence causes a large bend in the Potomac River, which curves around its eastern slope.

Geographic entities mentioned:
surface_form: roundtop hill
instance_of: Mountain
countries: United States
coordinates: lat: 39.68
lon: -78.32
surface_form: roundtop
instance_of: Mountain
countries: United States
coordinates: lat: 42.293888888889
lon: -74.490555555556
Geology. Outstanding outcrops of the Silurian Wills Creek Formation and underlying Bloomsburg Formation are exposed along the old railroad grade at Roundtop Hill. Examples of folding, formation of cleavage, thrust faulting, and the deformation of bedded rocks are visible. About 500 feet of strata are exposed.

Geographic entities mentioned:
surface_form: roundtop hill
instance_of: Mountain
countries: United States
coordinates: lat: 39.68
lon: -78.32
surface_form: roundtop
instance_of: Mountain
countries: United States
coordinates: lat: 42.293888888889
lon: -74.490555555556
Peck Lake (Saskatchewan). Peck Lake (; French: &quot;lac Peck&quot;), a lake in the Canadian province of Saskatchewan, is located in the Bronson Forest Recreation Site in the Rural Municipality of Loon Lake No. 561, east of the Alberta border. Access to the lake and its amenities is from Highway 21. Geography.

Geographic entities mentioned:
surface_form: loon lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.10338388888889
lon: -121.25554305555555
surface_form: peck lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.9001
lon: -109.60077
surface_form: loon lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.25
lon: -124.7
Peck Lake (Saskatchewan). Peck Lake (; French: &quot;lac Peck&quot;), a lake in the Canadian province of Saskatchewan, is located in the Bronson Forest Recreation Site in the Rural Municipality of Loon Lake No. 561, east of the Alberta border. Access to the lake and its amenities is from Highway 21. Geography.

Geographic entities mentioned:
surface_form: peck lake (saskatchewan)
instance_of: Lake
countries: Canada
coordinates: lat: 53.9001
lon: -109.60077
561, east of the Alberta border. Access to the lake and its amenities is from Highway 21. Geography. Known for its bright turquoise-coloured water, unlike most other lakes in the region, Peck Lake is a popular spot for beachgoers, fishermen, and boaters. Peck Lake reaches a depth of. Water flows southward across the lake, entering Peck Lake from Galletly Lake and exiting into the Monnery River.

Geographic entities mentioned:
surface_form: peck lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.9001
lon: -109.60077
surface_form: peck lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.9001
lon: -109.60077
Geography. Known for its bright turquoise-coloured water, unlike most other lakes in the region, Peck Lake is a popular spot for beachgoers, fishermen, and boaters. Peck Lake reaches a depth of. Water flows southward across the lake, entering Peck Lake from Galletly Lake and exiting into the Monnery River. Monnery River is a tributary of the North Saskatchewan River.

Geographic entities mentioned:
surface_form: peck lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.9001
lon: -109.60077
Each campsite has a picnic table, firepit, electrical plug, and free access to firewood. Fish species. Sport fish commonly found in Peck Lake include walleye, northern pike, yellow perch, lake whitefish, and burbot. White sucker, spottail shiner, and brook stickleback also inhabit Peck Lake.

Geographic entities mentioned:
surface_form: peck lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.9001
lon: -109.60077
Tornagaleones River. Tornagaleones River (&quot;Spanish&quot;: Río Tornagaleones) is a river and eastuarine channel in Los Ríos Region, Chile. Together with Valdivia and Futa River it encloses the fluvial island of Isla del Rey. The fresh waters of Tornagaleones comes from Futa, Naguilán and Valdivia River. During high tide brackish waters from Corral Bay enters the channel.

Geographic entities mentioned:
surface_form: Futa River
instance_of: Watercourse
countries: Chile
coordinates: lat: -39.937222222222
lon: -73.221666666667
Ivenacker See. Ivenacker See is a lake in the Mecklenburgische Seenplatte district in Mecklenburg-Vorpommern, Germany. At an elevation of 39.5 m, its surface area is 0.97 km2.

Geographic entities mentioned:
surface_form: ivenacker see
instance_of: Lake
countries: Germany
coordinates: lat: 53.707358333333
lon: 12.953927777778
There are no permanent settlements on the shores of the lake. The name of the lake in Chukot means &quot;a lake near a separate mountain.&quot;
Geography. Yanranaygytgyn is located in the Chukotka Mountains, to the south of Ervynaygytgyn. The lake has a roughly triangular shape and there are three islands in the middle. The southern shore is indented and the lake narrows towards its northern end.

Geographic entities mentioned:
surface_form: Ervynaygytgyn
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.275491
lon: 178.8097
surface_form: ervynaygytgyn
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.275491
lon: 178.8097
Yanranaygytgyn. Yanranaygytgyn (;) is a freshwater lake in Iultinsky District, Chukotka Autonomous Okrug, Russian Federation. It has an area of and a catchment area of. There are no permanent settlements on the shores of the lake. The name of the lake in Chukot means &quot;a lake near a separate mountain.&quot;
Geography.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: yanranaygytgyn
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 66.954264
lon: 178.310165
Yanranaygytgyn (;) is a freshwater lake in Iultinsky District, Chukotka Autonomous Okrug, Russian Federation. It has an area of and a catchment area of. There are no permanent settlements on the shores of the lake. The name of the lake in Chukot means &quot;a lake near a separate mountain.&quot;
Geography. Yanranaygytgyn is located in the Chukotka Mountains, to the south of Ervynaygytgyn.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
It has an area of and a catchment area of. There are no permanent settlements on the shores of the lake. The name of the lake in Chukot means &quot;a lake near a separate mountain.&quot;
Geography. Yanranaygytgyn is located in the Chukotka Mountains, to the south of Ervynaygytgyn. The lake has a roughly triangular shape and there are three islands in the middle.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
Yanranaygytgyn is located in the Chukotka Mountains, to the south of Ervynaygytgyn. The lake has a roughly triangular shape and there are three islands in the middle. The southern shore is indented and the lake narrows towards its northern end. Yanranaygytgyn lies in an area of lakes at the northern edge of the Amguema Valley.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
The southern shore is indented and the lake narrows towards its northern end. Yanranaygytgyn lies in an area of lakes at the northern edge of the Amguema Valley. It is the largest of the cluster, together with lake Kontalyagytgyn that lies to the southwest. An unnamed river, a small tributary of the Amguema, flows out of the lake from the northern end.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
Yanranaygytgyn lies in an area of lakes at the northern edge of the Amguema Valley. It is the largest of the cluster, together with lake Kontalyagytgyn that lies to the southwest. An unnamed river, a small tributary of the Amguema, flows out of the lake from the northern end. Yanranaygytgyn freezes in mid-September and stays under ice until June. Flora and fauna.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
It is the largest of the cluster, together with lake Kontalyagytgyn that lies to the southwest. An unnamed river, a small tributary of the Amguema, flows out of the lake from the northern end. Yanranaygytgyn freezes in mid-September and stays under ice until June. Flora and fauna. Yanranaygytgyn is surrounded by tundra. Arctic char is common in the waters of the lake.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
Yanranaygytgyn. Yanranaygytgyn (;) is a freshwater lake in Iultinsky District, Chukotka Autonomous Okrug, Russian Federation. It has an area of and a catchment area of. There are no permanent settlements on the shores of the lake. The name of the lake in Chukot means &quot;a lake near a separate mountain.&quot;
Geography.

Geographic entities mentioned:
surface_form: yanranaygytgyn
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 66.954264
lon: 178.310165
The trail was laid out in 1878 by Reverend Elkanah Lamb, long before the designation of the region as parkland. It was extended in 1910 by Enos Mills. The trail leads from the Tahosa Valley, running counterclockwise around Longs Peak and reaching the summit at 14,259 feet.

Geographic entities mentioned:
surface_form: Longs Peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.255013888889
lon: -105.61511388889
By proclamation of the Territorial Secretary and Acting Governor, Winthrop Sargent, on August 15, 1796, the boundaries of Wayne County were declared to begin at the mouth of the Cuyahoga River then west to Fort Wayne, then to the southernmost point of Lake Michigan and along the western shore north to the territorial boundary in Lake Superior and then along the territorial boundary through Lake Huron, Lake St.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
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
Geography. According to the U.S. Census Bureau, the county has a total area of, of which is land and (9.0%) is water. Its water area includes parts of the Detroit River and Lake St. Clair. Wayne County borders on Oakland County and Macomb County to the north, Washtenaw County to the west, Essex County, Ontario, Canada to the east, and Monroe County to the south.

Geographic entities mentioned:
surface_form: Lake St. Clair
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.450265
lon: -82.67572
Ferrara di Monte Baldo. Ferrara di Monte Baldo is a &quot;comune&quot; (municipality) in the Province of Verona in the Italian region Veneto, located in the Valle dell'Orsa about west of Venice and about northwest of Verona. The Monte Baldo is located nearby.

Geographic entities mentioned:
surface_form: Monte Baldo
instance_of: Mountain
countries: Italy
coordinates: lat: 45.733
lon: 10.833
Pilots flew individually against the clock and were required to complete tight turns through a slalom course consisting of inflatable pylons, known as &quot;Air Gates&quot;. The races were held mainly over water near cities, but were also held at airfields or natural wonders (such as Sugarloaf Mountain and Monument Valley).

Geographic entities mentioned:
surface_form: Sugarloaf Mountain
instance_of: Mountain
countries: Brazil
coordinates: lat: -22.949444444444445
lon: -43.156666666666666
Biography. Antonio Buttura was born in the town of Malcesine on the eastern shore of Lake Garda, during the final years of the Republic of Venice. A priest by training he became involved in literary work and translation during a period of growing Franco-Italian cultural exchange in the early 19th century.

Geographic entities mentioned:
surface_form: Lake Garda
instance_of: Lake
countries: Italy
coordinates: lat: 45.633333333333
lon: 10.666666666667
Lapara, Purulia. Lapara is a census town in the Kashipur CD block in the Raghunathpur subdivision of the Purulia district in the state of West Bengal, India. Area overview. Purulia district forms the lowest step of the Chota Nagpur Plateau. The general scenario is undulating land with scattered hills. Raghunathpur subdivision occupies the northern part of the district.

Geographic entities mentioned:
surface_form: Chota Nagpur Plateau
instance_of: Plateau
countries: India
coordinates: lat: 23
lon: 85
Borromeo first came from France to Bohemia in 1837 at the invitation of Alois Josef, Freiherr von Schrenk, Prince-Bishop of Prague. They established a hospital and nursing school on Petřín Hill below the Strahov Garden and soon became one of the most numerous and significant congregations in Bohemia. The Prague community was confirmed as a separate congregation in 1841.

Geographic entities mentioned:
surface_form: Petřín Hill
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.08166666666666
lon: 14.394444444444444
The principal agitators of the rebellion in Connacht were the MacWilliam Burke clan of County Mayo. Bingham entered their territory in March, taking Castlehag in Lough Mask, and agreed to withdraw his forces only if the men of the country prosecuted the rebels. In 1585 he took three young Burkes, Ulick, Richard and William aged fourteen, nine and seven.

Geographic entities mentioned:
surface_form: Lough Mask
instance_of: Lake
countries: Ireland
coordinates: lat: 53.621944444444
lon: -9.3822222222222
Walden Ridge. Walden Ridge (or Walden's Ridge) is a mountain ridge and escarpment located in Tennessee in the United States. It marks the eastern edge of the Cumberland Plateau and is generally considered part of it. Walden Ridge is about long, running generally north-south. Its highest point is at Hinch Mountain (near Crossville), which reaches above sea level.

Geographic entities mentioned:
surface_form: Cumberland Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 36
lon: -85
Sometimes Walden Ridge is called the Cumberland Escarpment. Geology. Sequatchie Valley, a long valley in the Cumberland Plateau, is located just west of the southern part of Walden Ridge. Being part of the Cumberland Plateau, Walden Ridge is also part of the Appalachian Plateau physiographic province. The Sequatchie River runs through the valley.

Geographic entities mentioned:
surface_form: Sequatchie Valley
instance_of: Valley
countries: United States
coordinates: lat: 35.125
lon: -85.5289
Geology. Sequatchie Valley, a long valley in the Cumberland Plateau, is located just west of the southern part of Walden Ridge. Being part of the Cumberland Plateau, Walden Ridge is also part of the Appalachian Plateau physiographic province. The Sequatchie River runs through the valley. To the east of Walden Ridge are the Ridge-and-valley Appalachians and the Tennessee River.

Geographic entities mentioned:
surface_form: Appalachian Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 40
lon: -78
The Sequatchie River runs through the valley. To the east of Walden Ridge are the Ridge-and-valley Appalachians and the Tennessee River. Walden Ridge is significantly higher than the Cumberland Plateau, and its eastern slope, descending over from the plateau to the Tennessee Valley, is steep and escarpment-like. Geologically, Walden Ridge continues south into Georgia and Alabama as Sand Mountain.

Geographic entities mentioned:
surface_form: Tennessee Valley
instance_of: Valley
countries: United States
coordinates: lat: 35.959166666667
lon: -83.850277777778
The height of the nearest key col is 5571 meters, leading to a topographic prominence of 479 meters. Peña Blanca is considered a Mountain according to the &quot;Dominance System&quot; and its dominance is 7.92%. Its parent peak is El Ermitaño and the Topographic isolation is 5.1 kilometers.

Geographic entities mentioned:
surface_form: El Ermitaño
instance_of: Mountain
countries: Chile
coordinates: lat: -26.786944444444
lon: -68.603333333333
Abtsrodaer Kuppe. Abtsrodaer Kuppe is a mountain in Hesse, Germany. It is close to the summit of Wasserkuppe and belongs to the Rhön Mountains. The mountain is characterized by its treeless summit formed from basalt rocks, making it a popular vantage point, especially when looking north. Location. The Abtsrodaer Kuppe rise is located in the High Rhön.

Geographic entities mentioned:
surface_form: Wasserkuppe
instance_of: Mountain
countries: Germany
coordinates: lat: 50.498055555556
lon: 9.9377777777778