Sarmila/GeoWiki-Features huggingface dataset:
Border disputes. When the city of Toledo was incorporated in 1833, it was part of Monroe County instead of the state of Ohio. The small strip of land surrounding the mouth of the Maumee River was under the jurisdiction of the Michigan Territory, because the borders originally drawn up for the Northwest Ordinance of 1787 set a territorial boundary as the southernmost edge of Lake Michigan.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Monroe County's boundary remained unchanged from 1837 to 1973, when a final unresolved dispute from the Toledo War was resolved, 136 years after the conflict. Ownership over the very small, uninhabited Turtle Island in a remote portion of Lake Erie was disputed for decades after the island's lighthouse was shut down. The island was long controlled by Michigan but still disputed by Ohio.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
This would later evolve into the worldwide La-Z-Boy Incorporated, and their world headquarters are located on North Telegraph Road in Monroe. In 1957, the Enrico Fermi Nuclear Generating Station first opened in Frenchtown Charter Township near Lake Erie. Today, the plant is operated by Detroit Edison but is entirely owned by parent company DTE Energy.

Geographic entities mentioned:
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 (19%) is water. Monroe is Michigan's only county on Lake Erie. The River Raisin and Sandy Creek flow through the county. Sterling State Park is the county's only state park and the only of Michigan's 98 state parks located on Lake Erie.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Severe weather events are very rare. Monroe County has experienced a total approximately 30 tornadoes since 1950. Infrequent waterspouts can also be seen out on Lake Erie. Many tornadoes have been a part of major outbreaks, and none have directly affected the heavily populated areas. Three separate F4 tornadoes killed 13 people during the 1965 Palm Sunday tornado outbreak on April 11, 1965.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
During this period of his life, he specialized in hydroelectricity and electromagnetism. Private sector Greece. By 1919, Paul moved to Athens, Greece, and continued working as a hydroelectric engineer for the Greek government. He studied the Edessa Waterfalls, Lake Vegoritida, and Agra Pella. He continued in this position until 1921. He worked in the private sector from 1921 until 1930.

Geographic entities mentioned:
surface_form: Lake Vegoritida
instance_of: Lake
countries: Greece
coordinates: lat: 40.760555555556
lon: 21.789166666667
Mount Abraham (Maine). Mount Abraham is a mountain located in Franklin County, Maine. One of Maine's &quot;4,000 footers&quot;, it is flanked to the north by Spaulding Mountain. Watersheds. The northeast side of Mt. Abraham is drained by Rapid Stream, then into the West Branch of the Carrabassett River, the Kennebec River, and into the Gulf of Maine.

Geographic entities mentioned:
surface_form: Spaulding Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.003
lon: -70.3335
surface_form: spaulding mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.003
lon: -70.3335
The two-man crew of No.57-376 ejected with minor injuries and the second aircraft made an emergency landing at Dow AFB. Access. The Appalachian Trail (AT), a National Scenic Trail from Georgia to Maine, runs between Saddleback Junior and Spaulding, passing northwest of the summit of Abraham. The summit of Mount Abraham can be reached from the AT via the blue-blazed Mount Abraham Side Trail.

Geographic entities mentioned:
surface_form: Saddleback Junior
instance_of: Mountain
countries: United States
coordinates: lat: 44.95815
lon: -70.457783333333
surface_form: saddleback junior
instance_of: Mountain
countries: United States
coordinates: lat: 44.95815
lon: -70.457783333333
Mount Abraham (Maine). Mount Abraham is a mountain located in Franklin County, Maine. One of Maine's &quot;4,000 footers&quot;, it is flanked to the north by Spaulding Mountain. Watersheds. The northeast side of Mt. Abraham is drained by Rapid Stream, then into the West Branch of the Carrabassett River, the Kennebec River, and into the Gulf of Maine.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: mount abraham
instance_of: Mountain
countries: United States
coordinates: lat: 44.973
lon: -70.3265
surface_form: mount abraham
instance_of: Mountain
countries: United States
coordinates: lat: 44.1204
lon: -72.9362
One of Maine's &quot;4,000 footers&quot;, it is flanked to the north by Spaulding Mountain. Watersheds. The northeast side of Mt. Abraham is drained by Rapid Stream, then into the West Branch of the Carrabassett River, the Kennebec River, and into the Gulf of Maine. The southern half of the southwest side drains into Quick Stream, then into the West Branch.

Geographic entities mentioned:
surface_form: west branch
instance_of: Watercourse
countries: United States
coordinates: lat: 45.3333
lon: -69.9697
surface_form: mt. abraham
instance_of: Mountain
countries: United States
coordinates: lat: 44.973
lon: -70.3265
surface_form: mt. abraham
instance_of: Mountain
countries: United States
coordinates: lat: 44.1204
lon: -72.9362
The northeast side of Mt. Abraham is drained by Rapid Stream, then into the West Branch of the Carrabassett River, the Kennebec River, and into the Gulf of Maine. The southern half of the southwest side drains into Quick Stream, then into the West Branch. The northern half drains into Perham Stream, then into Orbeton Stream, and the Sandy River, another tributary of the Kennebec. History.

Geographic entities mentioned:
surface_form: west branch
instance_of: Watercourse
countries: United States
coordinates: lat: 45.3333
lon: -69.9697
Mount Abraham (Maine). Mount Abraham is a mountain located in Franklin County, Maine. One of Maine's &quot;4,000 footers&quot;, it is flanked to the north by Spaulding Mountain. Watersheds. The northeast side of Mt. Abraham is drained by Rapid Stream, then into the West Branch of the Carrabassett River, the Kennebec River, and into the Gulf of Maine.

Geographic entities mentioned:
surface_form: mount abraham
instance_of: Mountain
countries: United States
coordinates: lat: 44.973
lon: -70.3265
surface_form: mount abraham
instance_of: Mountain
countries: United States
coordinates: lat: 44.1204
lon: -72.9362
The two-man crew of No.57-376 ejected with minor injuries and the second aircraft made an emergency landing at Dow AFB. Access. The Appalachian Trail (AT), a National Scenic Trail from Georgia to Maine, runs between Saddleback Junior and Spaulding, passing northwest of the summit of Abraham. The summit of Mount Abraham can be reached from the AT via the blue-blazed Mount Abraham Side Trail.

Geographic entities mentioned:
surface_form: mount abraham
instance_of: Mountain
countries: United States
coordinates: lat: 44.973
lon: -70.3265
surface_form: mount abraham
instance_of: Mountain
countries: United States
coordinates: lat: 44.973
lon: -70.3265
surface_form: mount abraham
instance_of: Mountain
countries: United States
coordinates: lat: 44.1204
lon: -72.9362
surface_form: mount abraham
instance_of: Mountain
countries: United States
coordinates: lat: 44.1204
lon: -72.9362
He succeeded his father as Duke of Mecklenburg-Strelitz on 12 May 1708. In 1712 the ducal family’s castle and the town of Strelitz burnt down. Because of this Adolphus Frederick and his family were forced to live in their hunting lodges. In 1726 Adolphus ordered a construction of a new residence, at Lake Zierke. The construction was finished in 1733.

Geographic entities mentioned:
surface_form: Lake Zierke
instance_of: Lake
countries: Germany
coordinates: lat: 53.361513888889
lon: 13.035963888889
and, when that country entered the conflict in 1917, was seized and converted to a troop transport, becoming USS &quot;Huron&quot; (ID-1408). Originally commissioned as USS &quot;Fredrick Der Grosse&quot;, the ship was renamed &quot;Huron&quot; – after Lake Huron, the center lake of the Great Lakes – while undergoing repairs and conversion at a U.S. Navy yard.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
The ship, Commander S. H. R. Doyle in command, was renamed &quot;Huron&quot; on 1 September 1917 after the center lake of the Great Lakes. &quot;Huron&quot; acted as a troop transport during the remaining years of the war. During the beginning of one voyage to France. &quot;Huron&quot;, in convoy, departed Hoboken on 23 April 1918.

Geographic entities mentioned:
surface_form: center lake
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
This name, expanded by the possessive suffix &quot;*-jь&quot; (&quot;*Radogostjь&quot;), formed many toponyms throughout Slavdom, cf. Polish villages &quot;Radogoszcz&quot;, Czech mountain &quot;Radhošť&quot;, Serbo-Croatian toponym, Russian, and Russian hydronyms and and others, as well as the town of &quot;Radogošč&quot;, which belonged to the Redarii tribe.

Geographic entities mentioned:
surface_form: Radhošť
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 49.491838888889
lon: 18.222786111111
Legend of Radhošť. In the Czech Republic, there is a local legend associated with Saints Cyril and Methodius, according to which Radegast was worshipped on Radhošť. According to this legend, Cyril and Methodius decided to go on a Christianizing mission to the mountain. They set out to Radhošť from Velehrad through Zašová, where they baptized people.

Geographic entities mentioned:
surface_form: Radhošť
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 49.491838888889
lon: 18.222786111111
Hidden Lake is located in Glacier National Park, in the U.S. state of Montana. The lake is surrounded by several peaks, including Bearhat Mountain to the southwest, Dragons Tail to the south, Clements Mountain to the north, and Reynolds Mountain to the east. It is a popular destination for hikers, with the Hidden Lake Overlook Trail leading to the lake. Location and Features.

Geographic entities mentioned:
surface_form: Bearhat Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.6670102
lon: -113.7638424
surface_form: Clements Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.6931
lon: -113.74
surface_form: Reynolds Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.6719
lon: -113.723
Hidden Lake (Flathead County, Montana). Hidden Lake is located in Glacier National Park, in the U.S. state of Montana. The lake is surrounded by several peaks, including Bearhat Mountain to the southwest, Dragons Tail to the south, Clements Mountain to the north, and Reynolds Mountain to the east. It is a popular destination for hikers, with the Hidden Lake Overlook Trail leading to the lake.

Geographic entities mentioned:
surface_form: hidden lake
instance_of: Lake
countries: United States
coordinates: lat: 60.485
lon: -150.2625
surface_form: hidden lake
instance_of: Lake
countries: United States
coordinates: lat: 45.2624
lon: -111.172
surface_form: hidden lake (flathead county, montana)
instance_of: Lake
countries: United States
coordinates: lat: 48.6764
lon: -113.741
surface_form: hidden lake
instance_of: Lake
countries: United States
coordinates: lat: 48.4956
lon: -121.189
Hidden Lake (Flathead County, Montana). Hidden Lake is located in Glacier National Park, in the U.S. state of Montana. The lake is surrounded by several peaks, including Bearhat Mountain to the southwest, Dragons Tail to the south, Clements Mountain to the north, and Reynolds Mountain to the east. It is a popular destination for hikers, with the Hidden Lake Overlook Trail leading to the lake.

Geographic entities mentioned:
surface_form: hidden lake
instance_of: Lake
countries: United States
coordinates: lat: 60.485
lon: -150.2625
surface_form: hidden lake
instance_of: Lake
countries: United States
coordinates: lat: 45.2624
lon: -111.172
surface_form: hidden lake
instance_of: Lake
countries: United States
coordinates: lat: 48.6764
lon: -113.741
surface_form: hidden lake
instance_of: Lake
countries: United States
coordinates: lat: 48.4956
lon: -121.189
state of Montana. The lake is surrounded by several peaks, including Bearhat Mountain to the southwest, Dragons Tail to the south, Clements Mountain to the north, and Reynolds Mountain to the east. It is a popular destination for hikers, with the Hidden Lake Overlook Trail leading to the lake. Location and Features. Hidden Lake is situated in Glacier National Park, Flathead County, Montana, US.

Geographic entities mentioned:
surface_form: hidden lake
instance_of: Lake
countries: United States
coordinates: lat: 60.485
lon: -150.2625
surface_form: hidden lake
instance_of: Lake
countries: United States
coordinates: lat: 45.2624
lon: -111.172
surface_form: hidden lake
instance_of: Lake
countries: United States
coordinates: lat: 48.6764
lon: -113.741
surface_form: hidden lake
instance_of: Lake
countries: United States
coordinates: lat: 48.4956
lon: -121.189
It is a popular destination for hikers, with the Hidden Lake Overlook Trail leading to the lake. Location and Features. Hidden Lake is situated in Glacier National Park, Flathead County, Montana, US. The lake is 1.4 miles (2.25 km) long and 0.40 miles (0.64 km) wide, with a surface elevation of 6,375 feet (1,943 m). The primary outflow from the lake is Hidden Creek. Hidden Lake Overlook Trail.

Geographic entities mentioned:
surface_form: hidden lake
instance_of: Lake
countries: United States
coordinates: lat: 60.485
lon: -150.2625
surface_form: hidden lake
instance_of: Lake
countries: United States
coordinates: lat: 45.2624
lon: -111.172
surface_form: hidden lake
instance_of: Lake
countries: United States
coordinates: lat: 48.6764
lon: -113.741
surface_form: hidden lake
instance_of: Lake
countries: United States
coordinates: lat: 48.4956
lon: -121.189
The lake is 1.4 miles (2.25 km) long and 0.40 miles (0.64 km) wide, with a surface elevation of 6,375 feet (1,943 m). The primary outflow from the lake is Hidden Creek. Hidden Lake Overlook Trail. The Hidden Lake Overlook Trail is a 2.7-mile out-and-back trail that provides visitors an opportunity to experience the beauty of Hidden Lake.

Geographic entities mentioned:
surface_form: hidden lake
instance_of: Lake
countries: United States
coordinates: lat: 60.485
lon: -150.2625
surface_form: hidden lake
instance_of: Lake
countries: United States
coordinates: lat: 45.2624
lon: -111.172
surface_form: hidden lake
instance_of: Lake
countries: United States
coordinates: lat: 48.6764
lon: -113.741
surface_form: hidden lake
instance_of: Lake
countries: United States
coordinates: lat: 48.4956
lon: -121.189
The primary outflow from the lake is Hidden Creek. Hidden Lake Overlook Trail. The Hidden Lake Overlook Trail is a 2.7-mile out-and-back trail that provides visitors an opportunity to experience the beauty of Hidden Lake. The trail starts at the Logan Pass Visitor Center and is suitable for individuals of all fitness levels.

Geographic entities mentioned:
surface_form: hidden lake
instance_of: Lake
countries: United States
coordinates: lat: 60.485
lon: -150.2625
surface_form: hidden lake
instance_of: Lake
countries: United States
coordinates: lat: 60.485
lon: -150.2625
surface_form: hidden lake
instance_of: Lake
countries: United States
coordinates: lat: 45.2624
lon: -111.172
surface_form: hidden lake
instance_of: Lake
countries: United States
coordinates: lat: 45.2624
lon: -111.172
surface_form: hidden lake
instance_of: Lake
countries: United States
coordinates: lat: 48.6764
lon: -113.741
surface_form: hidden lake
instance_of: Lake
countries: United States
coordinates: lat: 48.6764
lon: -113.741
surface_form: hidden lake
instance_of: Lake
countries: United States
coordinates: lat: 48.4956
lon: -121.189
surface_form: hidden lake
instance_of: Lake
countries: United States
coordinates: lat: 48.4956
lon: -121.189
As the trail ascends in elevation, hikers are treated to mesmerizing views of the landscape, including a meadow known as the Hanging Gardens where wildflowers bloom and wildlife is abundant. Wildlife. Hidden Lake Overlook Trail offers a diverse range of wildlife. The trail serves as a migration route for several wild creatures. Mountain goats and bighorn sheep are commonly spotted along the trail.

Geographic entities mentioned:
surface_form: hidden lake
instance_of: Lake
countries: United States
coordinates: lat: 60.485
lon: -150.2625
surface_form: hidden lake
instance_of: Lake
countries: United States
coordinates: lat: 45.2624
lon: -111.172
surface_form: hidden lake
instance_of: Lake
countries: United States
coordinates: lat: 48.6764
lon: -113.741
surface_form: hidden lake
instance_of: Lake
countries: United States
coordinates: lat: 48.4956
lon: -121.189
His work includes decades of research, field studies, and policy advocacy. He has served in various governmental roles, including being the Deputy Commissioner in Assam and as Secretary in the state government, and ultimately retiring as the Divisional Commissioner of Barak Valley in August 2019.

Geographic entities mentioned:
surface_form: Barak Valley
instance_of: Valley
countries: India
coordinates: lat: 24.833333333333332
lon: 92.8
Overview. &quot;Miho no Matsubara&quot; is renowned as a seashore with green pine trees and sand spanning over seven kilometers. It has a great scenic view of Mount Fuji and the Izu Peninsula across Suruga Bay. Due to its natural environment, it is designated as one of along with its three pine groves.

Geographic entities mentioned:
surface_form: Mount Fuji
instance_of: Mountain
countries: Japan
coordinates: lat: 35.36055555555556
lon: 138.7275
The Battle of Cedar Creek was fought near Middletown, Virginia on October 19, 1864. The battle was the decisive engagement of Major General Philip Sheridan’s Valley Campaigns of 1864 and was the largest battle fought in the Shenandoah Valley. Twelve Union Army enlisted men and nine officers were awarded the Medal of Honor for gallantry during the battle.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
It is an extant taxon. It is a scrambling tree which grows from 4 to 15 meters tall. It is likely pollinated by insects, and its fruit and seeds dispersed by birds. It is known from the area of Mount Suckling, Mount Dayman, and Mount Simpson area in the eastern New Guinea Highlands, at the border area of Milne Bay, Oro (Northern), and Central provinces.

Geographic entities mentioned:
surface_form: Mount Suckling
instance_of: Mountain
countries: Papua New Guinea
coordinates: lat: -9.6691666666667
lon: 149.01083333333
John Bird Burnham. an4m827u258hh2pk4qc1qe9qmpzcd" xml:space="preserve">John Bird Burnham (March 16, 1869-1939) was a conservationist and entrepreneur who founded the Crater Club off of Whallons Bay on Lake Champlain in 1899. Born in Newcastle, Delaware, he worked in New York City as editor of Forest and Stream from 1881 to 1887, where he wrote many articles advocating for game protection.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
Steske. Steske () is a small settlement in western Slovenia in the Municipality of Nova Gorica. It is located near the village of Branik in the Branik Valley, part of Vipava Valley. Geography. The main part of Steske lies along the Branica River, a tributary of the Vipava River. The hamlet of Pekel lies to the northwest along the Vipava.

Geographic entities mentioned:
surface_form: Vipava Valley
instance_of: Valley
countries: Slovenia
coordinates: lat: 45.876147222222
lon: 13.907319444444
Drainage. Tippecanoe is drained by the Tippecanoe River which flows generally south to the Wabash River. The river ends near Battle Ground, Indiana, in Tippecanoe county. Two reservoirs, Lake Shafer and Lake Freeman, are fed by the Tippecanoe River. The reservoirs both have dams controlling inflow from the Tippecanoe River. Notable residents. A notable resident was Chris Schenkel.

Geographic entities mentioned:
surface_form: Lake Shafer
instance_of: Lake
countries: United States
coordinates: lat: 40.8297
lon: -86.7983
Aside from golf, T.L.C.C. also provides tennis, swimming and boating, and is an excellent location to watch the fireworks display for the 4 July. Marinas. Patona Bay Marina is located on the west shore of Lake Tippecanoe. The marina is a dealership complemented by a full-service parts and service department. The marina also offers boat and kayak rentals, daily or weekly.

Geographic entities mentioned:
surface_form: lake tippecanoe
instance_of: Lake
countries: United States
coordinates: lat: 41.327777777778
lon: -85.759722222222
Tippecanoe Lake. Tippecanoe Lake () is a large, glacially created lake in Leesburg, Kosciusko County, Indiana and, at deep, is the deepest natural lake in the state. Location. Tippecanoe Lake is about two miles west of the town of North Webster, Indiana, and Webster Lake with the small unincorporated area of Oswego (now located in Leesburg, Indiana) located near its west-northwestern shore.

Geographic entities mentioned:
surface_form: tippecanoe lake
instance_of: Lake
countries: United States
coordinates: lat: 41.327777777778
lon: -85.759722222222
Tippecanoe Lake () is a large, glacially created lake in Leesburg, Kosciusko County, Indiana and, at deep, is the deepest natural lake in the state. Location. Tippecanoe Lake is about two miles west of the town of North Webster, Indiana, and Webster Lake with the small unincorporated area of Oswego (now located in Leesburg, Indiana) located near its west-northwestern shore. Recreation.

Geographic entities mentioned:
surface_form: tippecanoe lake
instance_of: Lake
countries: United States
coordinates: lat: 41.327777777778
lon: -85.759722222222
Recreation. Tippecanoe Lake is used mostly for recreational purposes such as fishing, boating and skiing, and is surrounded mostly by residential housing. A prominent historical location is on the southwest shore of the lake: Tippy Dance Hall.

Geographic entities mentioned:
surface_form: tippecanoe lake
instance_of: Lake
countries: United States
coordinates: lat: 41.327777777778
lon: -85.759722222222
From the mid 1980s through 2016, Tippy Dance Hall was a teen dance club with Saturday night dances from Memorial Day until just after Labor day. Tippecanoe Lake Country Club. Tippecanoe Lake Country Club is a private club and one of the lake's largest attractions.

Geographic entities mentioned:
surface_form: tippecanoe lake
instance_of: Lake
countries: United States
coordinates: lat: 41.327777777778
lon: -85.759722222222
Tippecanoe Lake Country Club. Tippecanoe Lake Country Club is a private club and one of the lake's largest attractions. It is north of Kalorama Park at 7245 N Kalorama Road and accessed from Indiana State Road 13 via Kosciusko County Roads E650N and E800N. TLCC, a private club, was opened on April 15, 1926, with the clubhouse opening on June 11 of that year.

Geographic entities mentioned:
surface_form: tippecanoe lake
instance_of: Lake
countries: United States
coordinates: lat: 41.327777777778
lon: -85.759722222222
Previously uninhabitable due to mosquitoes carrying malaria, in Roman times armies marched as quickly as possible across it on the military road, the Via Appia. The marsh was bounded on one side by the sea and the other by mountains: the Monti Albani, the Monti Lepini, the Monti Ausoni, and further south the Monti Aurunci (where the allies had been brought to a halt before Monte Cassino).

Geographic entities mentioned:
surface_form: Monte Cassino
instance_of: Mountain
countries: Italy
coordinates: lat: 41.49
lon: 13.813888888889
In 1870-72 the township/chapelry had a population of 49. Topology. It is located at the head of the valley of Wasdale, and is surrounded by some of England's highest mountains: Scafell Pike, Sca Fell, Great Gable, Kirk Fell and Pillar. Climbing and walking. The hamlet was the centre of the early years of British rock climbing.

Geographic entities mentioned:
surface_form: Wasdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.425
lon: -3.35
surface_form: Scafell Pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.454166666667
lon: -3.2115277777778
surface_form: Great Gable
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.482
lon: -3.219
surface_form: Kirk Fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.483
lon: -3.242
There is a famous climber's hotel here, the Wasdale Head Inn, made popular in the Victorian period by Walter Parry Haskett Smith, Owen Glynne Jones and many other pioneers. Wasdale Head is a popular starting point for the ascent of Scafell Pike. On summer weekends, crowds of people can be found attempting this steep but straightforward walk.

Geographic entities mentioned:
surface_form: Scafell Pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.454166666667
lon: -3.2115277777778
Church. In the hamlet is St Olaf's Church, which is claimed as being the smallest church in England. The church has long been associated with British climbers. The south window has a small pane within it with an etching of Napes Needle on Great Gable, serving as a memorial to members of the Fell & Rock Climbing Club who lost their lives in the First World War. Will Ritson.

Geographic entities mentioned:
surface_form: Great Gable
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.482
lon: -3.219
Guavio Formation. The Guavio Formation (, Kicg) is a geological formation of the Altiplano Cundiboyacense, Eastern Ranges of the Colombian Andes. The formation consists of conglomerates, shales and limestones, dates to the Late Jurassic and Early Cretaceous periods; Tithonian to Berriasian epochs and has a maximum thickness of. Etymology.

Geographic entities mentioned:
surface_form: Altiplano Cundiboyacense
instance_of: Plateau
countries: Colombia
coordinates: lat: 5.532209
lon: -73.362877
The formation consists of conglomerates, shales and limestones, dates to the Late Jurassic and Early Cretaceous periods; Tithonian to Berriasian epochs and has a maximum thickness of. Etymology. The formation was defined and named in 1976 by Rodríguez and Ulloa after the Guavio River, Cundinamarca. Lithologies.

Geographic entities mentioned:
surface_form: Guavio River
instance_of: Watercourse
countries: Colombia
Chutu dynasty. The Chutu dynasty (IAST: Cuṭu) ruled parts of the Deccan region of South India between first and third centuries CE, with its capital at Banavasi in present-day Karnataka state. The Chutus probably rose to power as Satavahanas feudatories, and assumed sovereignty after the decline of the Satavahana power.

Geographic entities mentioned:
surface_form: Deccan
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
Dreischusterspitze. The Dreischusterspitze () is a mountain of the Dolomites in South Tyrol, Italy. It is the highest peak of the Sexten Dolomites and the most northerly 3,000m peak of the range. From the north it resembles a majestic pyramid, while from the east and west it resembles a jagged ridge. The mountain is located above the village of Sexten.

Geographic entities mentioned:
surface_form: dreischusterspitze
instance_of: Mountain
countries: Italy
coordinates: lat: 46.668611111111
lon: 12.318055555556
It was first climbed in 1869 by Paul Grohmann, Franz Innerkofler and Peter Salcher. Huts in the area are the Dreischusterhütte (Rifugio Tre Scarperi, 1653 m) in the Innerfeldtal as well as the Talschlusshütte (Rifugio al Fondo Valle, 1548 m) in the Fischlein Valley and the Dreizinnenhütte (Rifugio Locatelli, 2405 m) in the south of the Schusterplatte.

Geographic entities mentioned:
surface_form: tre scarperi
instance_of: Mountain
countries: Italy
coordinates: lat: 46.668611111111
lon: 12.318055555556
Dreischusterspitze. The Dreischusterspitze () is a mountain of the Dolomites in South Tyrol, Italy. It is the highest peak of the Sexten Dolomites and the most northerly 3,000m peak of the range. From the north it resembles a majestic pyramid, while from the east and west it resembles a jagged ridge. The mountain is located above the village of Sexten.

Geographic entities mentioned:
surface_form: sexten
instance_of: Valley
countries: Italy
coordinates: lat: 46.672777777778
lon: 12.376388888889
It is the highest peak of the Sexten Dolomites and the most northerly 3,000m peak of the range. From the north it resembles a majestic pyramid, while from the east and west it resembles a jagged ridge. The mountain is located above the village of Sexten. It was first climbed in 1869 by Paul Grohmann, Franz Innerkofler and Peter Salcher.

Geographic entities mentioned:
surface_form: sexten
instance_of: Valley
countries: Italy
coordinates: lat: 46.672777777778
lon: 12.376388888889
This watercourse dotted with falls and rapids has its source in the Lacs des Loups Marins (English: Lake of Sea Wolves) (length:; width:; altitude:; area:), one of the few freshwater bodies in the world where seals can be seen. The Nastapoka River Basin was originally part of the project to create the Lac-Guillaume-Delisle and Lac-à-l'Eau-claire National Park.

Geographic entities mentioned:
surface_form: Lacs des Loups Marins
instance_of: Group of lakes
countries: Canada
coordinates: lat: 56.5086
lon: -73.7494
Nastapoka River. The Nastapoka River is a tributary of Eastern shore of Hudson Bay, flowing in the administrative region of Nord-du-Québec, in Quebec, Canada. This river is one of the most important rivers of Nord-du-Québec, the 39th of Quebec because its watershed of. Geography.

Geographic entities mentioned:
surface_form: nastapoka river
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.91055556
lon: -76.54611111
This river is one of the most important rivers of Nord-du-Québec, the 39th of Quebec because its watershed of. Geography. The Nastapoka River flows into the Nastapoka Channel, on the eastern slope of Hudson Bay, almost at the center of the Nastapoka Islands archipelago, after a run of some, at north of the Inuit village of Umiujaq, Quebec and the immense Richmond Gulf.

Geographic entities mentioned:
surface_form: nastapoka river
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.91055556
lon: -76.54611111
surface_form: nastapoka
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.91055556
lon: -76.54611111
surface_form: nastapoka
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.91055556
lon: -76.54611111
surface_form: richmond gulf
instance_of: Lake
countries: Canada
coordinates: lat: 56.24944444444444
lon: -76.29416666666667
This watercourse dotted with falls and rapids has its source in the Lacs des Loups Marins (English: Lake of Sea Wolves) (length:; width:; altitude:; area:), one of the few freshwater bodies in the world where seals can be seen. The Nastapoka River Basin was originally part of the project to create the Lac-Guillaume-Delisle and Lac-à-l'Eau-claire National Park.

Geographic entities mentioned:
surface_form: nastapoka river
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.91055556
lon: -76.54611111
The Nastapoka River Basin was originally part of the project to create the Lac-Guillaume-Delisle and Lac-à-l'Eau-claire National Park. In its most recent version, the Nastapoka Basin was removed for reasons of potential hydroelectric development. Toponym.

Geographic entities mentioned:
surface_form: nastapoka
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.91055556
lon: -76.54611111
Toponym. The name &quot;Nastapoka&quot;, expression of the Cree language, means someone found there a caribou killed by the rapids, meaning that fits perfectly with the landscape data, because just before its mouth, the river reaches sea level with a crash down Nastapoka Falls and its steep vertical drop of. The falls are a popular destination for visitors to Tursujuq National Park.

Geographic entities mentioned:
surface_form: nastapoka
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.91055556
lon: -76.54611111
surface_form: nastapoka
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.91055556
lon: -76.54611111
The name Nastapoka River appears in the report of an exploration mission carried out in the sector in 1877 by the scientist Robert Bell. For its part, the name Rivière Nastapoka appears on the map of Quebec, leaflet north, published in 1914 by the Department of Lands and Forests. Its course, discontinuous, is approximate.

Geographic entities mentioned:
surface_form: nastapoka
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.91055556
lon: -76.54611111
surface_form: rivière nastapoka
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.91055556
lon: -76.54611111
The 1914 edition of the Dictionary of Rivers and Lakes of the Province of Quebec bears, probably by mistake, the Nastakopa form. It was in 1946 that the Quebec Geography Commission accepted the name Rivière Nastapoka. The official Quebec map of 1949 and the editions of 1969 of the Gazetteer and 1978 of the Toponymic Repertoire, among other documents, however, have the Nastapoca form.

Geographic entities mentioned:
surface_form: nastapoka
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.91055556
lon: -76.54611111
surface_form: rivière nastapoka
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.91055556
lon: -76.54611111
It was in 1946 that the Quebec Geography Commission accepted the name Rivière Nastapoka. The official Quebec map of 1949 and the editions of 1969 of the Gazetteer and 1978 of the Toponymic Repertoire, among other documents, however, have the Nastapoca form. The Commission de toponymie restored the Nastapoka script in 1986. &quot;

Geographic entities mentioned:
surface_form: nastapoka
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.91055556
lon: -76.54611111
The government tried to obtain the support of other African countries for her candidacy, and African Great Lakes nations pledged that they would support her; however, the government later withdrew her candidacy and backed Jean Ping of Gabon.

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
Aytos Point. Aytos Point (Nos Aytos \'nos 'ay-tos\) is a point on the coast of Bransfield Strait, Livingston Island, Antarctica formed by an offshoot of Christoff Cliff. The point was named after the Bulgarian town of Aytos. Location. Aytos Point is located at which is 5.57 km east by north east of Samuel Point and 2.53 km southwest of M'Kean Point.

Geographic entities mentioned:
surface_form: Bransfield Strait
instance_of: Body of water
countries: Antarctica
coordinates: lat: -63
lon: -59
In the northeast, the territory extends into the Jizera Mountains and to the eponymous protected landscape area. In the west, the territory extends into the Ještěd–Kozákov Ridge and includes the highest point of Liberec and of the entire Ještěd–Kozákov Ridge, the mountain Ještěd at above sea level. Liberec is situated on the Lusatian Neisse River.

Geographic entities mentioned:
surface_form: Ještěd
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.732222222222
lon: 14.985277777778
The first tram was used in Liberec in 1897. Liberec shares the tramway line which connects it to its neighbouring Jablonec nad Nisou. There are also two city lines with. The first connects Horní Hanychov (next to the cable car to Ještěd) and Lidové Sady via Fügnerova. The second connects Dolní Hanychov and Lidové Sady via Fügnerova (only during workdays). There are also four historical trams.

Geographic entities mentioned:
surface_form: Ještěd
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.732222222222
lon: 14.985277777778
The team Start Gniezno Liberec race at the stadium. Sights. The main landmark and one of the symbols of the city is the Ještěd Tower on the Ještěd mountain,which is used as a transmitter, observation tower and hotel. It was built in 1966–1973 according to the design by the architect Karel Hubáček. It is the most important monument in the city, protected as a national cultural monument since 2006.

Geographic entities mentioned:
surface_form: Ještěd
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.732222222222
lon: 14.985277777778
It is bordered by the counties of Carlow, Laois, Meath, Offaly, South Dublin and Wicklow. As an inland county, Kildare is generally a lowland region. The county's highest points are the foothills of the Wicklow Mountains bordering to the east. The highest point in Kildare is Cupidstown Hill on the border with South Dublin, with the better-known Hill of Allen in central Kildare. Physical geography.

Geographic entities mentioned:
surface_form: Cupidstown Hill
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.22599167
lon: -6.49245556
surface_form: Hill of Allen
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.229497222222
lon: -6.8633111111111
Rhiana Griffith. Rhiana Jade Griffith (born April 16, 1985) is an Australian former actress and artist. Life and career. Griffith was born in the Hunter Region of New South Wales, Australia. She began modeling as a child, doing runway work and catalogue advertisements, and eventually progressed from there to television commercials.

Geographic entities mentioned:
surface_form: Hunter Region
instance_of: Valley
countries: Australia
coordinates: lat: -32.56
lon: 151.17083333333332
The north blockhouse resembles the south blockhouse, with greater attention to stonework. The north blockhouse houses seasonal park employees. The visitor center is set between and behind the blockhouses, with a view of Mount Rainier through large south-facing windows. The building was previously known as the &quot;campers' shelter&quot; and the Museum.

Geographic entities mentioned:
surface_form: Mount Rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
It is the longest river entirely in Washington state. Course. The river rises in the Cascade Range at an elevation of at Keechelus Dam on Keechelus Lake near Snoqualmie Pass, near Easton. The river flows through that town, skirts Ellensburg, passes the city of Yakima, and continues southeast to Richland, where it flows into the Columbia River creating the Yakima River Delta at an elevation of.

Geographic entities mentioned:
surface_form: Keechelus Lake
instance_of: Lake
countries: United States
coordinates: lat: 47.34777777777778
lon: -121.36888888888889
Badger Canyon was once a waterway of the Yakima River, this pre-existing channel led the Yakima River to make tribute to the Columbia River at the current location of the city of Kennewick. Beginning nearly 15,000 years ago the Columbia Plateau was transformed by the successive Missoula glacial outburst floods.

Geographic entities mentioned:
surface_form: Columbia Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 45.999444444444
lon: -119.00138888889
Yakima Valley. The Yakima River Basin consists of approximately located in south central Washington State. It is bounded by the Cascade Mountains on the west, the Wenatchee Mountains on the north, Rattlesnake Mountain and the Rattlesnake Hills on the east, and the Horse Heaven Hills to the south.

Geographic entities mentioned:
surface_form: Horse Heaven Hills
instance_of: Landform
countries: United States
coordinates: lat: 46.13
lon: -119.87
The Lingen Heights, the Damme Hills, the Kellenberg and the Brelinger Berg also belong to this push moraine, also called the &quot;Rehburg Phase&quot;, which can be dated to about 230,000 years ago. The Rehburg Hills by the lake of the Steinhuder Meer, are not, however, part of the moraine.

Geographic entities mentioned:
surface_form: Steinhuder Meer
instance_of: Lake
countries: Germany
coordinates: lat: 52.466666666667
lon: 9.3333333333333
Kejulik Volcano. Kejulik Volcano, also known as Mount Kejulik or the Kejulik Pinnacles, are highly eroded remnants of an andesitic stratovolcano located in the southwestern Kejulik Mountains within the Aleutian Range near Becharof Lake. The volcano lies on the border of Katmai National Park and Preserve and the Becharof National Wildlife Refuge, about 30 miles (48 km) southwest of Mount Katmai.

Geographic entities mentioned:
surface_form: Becharof Lake
instance_of: Lake
countries: United States
coordinates: lat: 57.952222222222
lon: -156.37611111111
Constituency. Lac-Saint-Jean is a Francophone riding in the Saguenay–Lac-Saint-Jean region of northeast Quebec, and takes its name from the lake of the same name. The largest town in the riding is Alma. Representation. The area was represented by Denis Lebel since 2007, who served as a minister in the Harper Cabinet.

Geographic entities mentioned:
surface_form: lake of the same name
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
Azas Plateau. Azas Plateau is a volcanic field in Russia. It is also known as East Tuva Plateau, Khamsara-Biykhem Plateau and Northeast Tuva Plateau. It covers a surface area of west of Lake Baikal. Volcanic activity in the area also occurred at the Oka Plateau and the Jom-Bolok volcanic field. The field is formed by a late Pliocene lava plateau.

Geographic entities mentioned:
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
Geography. The field is located in southern Siberia, between the East Sayan Mountains and the Todzha basin. There it covers a surface area of west of Lake Baikal, at an altitude of. Volcanic landforms include cones, lava fields, tuyas, and other volcanic structures including scoria cones, volcanic dykes, volcanic necks and volcanic vents.

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 baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
surface_form: baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
Ulug-Arginskii () is a cone that formed exposed in the air. The cone is accompanied by a maar with a lake to the south, and a lava flow from the cone reached in length. Shivit-Taiga with a length of over and a height of is among the biggest volcanoes in the world that formed beneath ice, but Derby-Taiga may be even larger depending on how the size is measured.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
Azas Plateau. Azas Plateau is a volcanic field in Russia. It is also known as East Tuva Plateau, Khamsara-Biykhem Plateau and Northeast Tuva Plateau. It covers a surface area of west of Lake Baikal. Volcanic activity in the area also occurred at the Oka Plateau and the Jom-Bolok volcanic field. The field is formed by a late Pliocene lava plateau.

Geographic entities mentioned:
surface_form: azas
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 52.397777777778
lon: 96.514722222222
surface_form: azas plateau
instance_of: Mountain
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 52.443508333333
lon: 98.387875
Activity in the rift zone started in the Oligocene and reached its maximum during the Miocene. Together with the Oka Plateau, the Azas Plateau forms the East Sayan province of the Baikal Rift Zone. Activity in the Azas Plateau has been influenced by a tectonic graben in the area. The Azas Plateau is the largest lava field in the Tuva volcanic province.

Geographic entities mentioned:
surface_form: azas
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 52.397777777778
lon: 96.514722222222
surface_form: baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
surface_form: azas plateau
instance_of: Mountain
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 52.443508333333
lon: 98.387875
Activity in the rift zone started in the Oligocene and reached its maximum during the Miocene. Together with the Oka Plateau, the Azas Plateau forms the East Sayan province of the Baikal Rift Zone. Activity in the Azas Plateau has been influenced by a tectonic graben in the area. The Azas Plateau is the largest lava field in the Tuva volcanic province.

Geographic entities mentioned:
surface_form: azas
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 52.397777777778
lon: 96.514722222222
surface_form: azas plateau
instance_of: Mountain
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 52.443508333333
lon: 98.387875
Together with the Oka Plateau, the Azas Plateau forms the East Sayan province of the Baikal Rift Zone. Activity in the Azas Plateau has been influenced by a tectonic graben in the area. The Azas Plateau is the largest lava field in the Tuva volcanic province. The Jom-Bolok volcanic field may be related to the Azas Plateau. Geomorphology.

Geographic entities mentioned:
surface_form: azas
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 52.397777777778
lon: 96.514722222222
surface_form: azas plateau
instance_of: Mountain
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 52.443508333333
lon: 98.387875
Activity in the Azas Plateau has been influenced by a tectonic graben in the area. The Azas Plateau is the largest lava field in the Tuva volcanic province. The Jom-Bolok volcanic field may be related to the Azas Plateau. Geomorphology. A large lava field with thicknesses of formed during the Late Pliocene, when the largest eruptions took place. These flows reached a thickness of approximately.

Geographic entities mentioned:
surface_form: azas
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 52.397777777778
lon: 96.514722222222
surface_form: azas plateau
instance_of: Mountain
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 52.443508333333
lon: 98.387875
Volcanism may be influenced by strike-slip faults associated with the Jom-Bolok fault. Individual volcanoes in the Azas Plateau volcanic field include the Derbi-Taiga tuya (), which is formed by several layers of hyaloclastite and lava flows and displays a prominent &quot;winged&quot; topography. The hyaloclastite layers were formerly considered to be tuffs and reach thicknesses of.

Geographic entities mentioned:
surface_form: azas
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 52.397777777778
lon: 96.514722222222
surface_form: azas plateau
instance_of: Mountain
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 52.443508333333
lon: 98.387875