Sarmila/GeoWiki-Features huggingface dataset:
Although sulfur was found, the amount of the ore that was able to be mined in a season was only enough to make up the cost of getting it off the mountain and was not enough to be competitive. Part of this stemmed from Dean's desire that if operations were expanded, an ore as well as passenger transport system was needed, and his desire that Adams not be significantly scarred by the operation.

Geographic entities mentioned:
surface_form: adams
instance_of: Mountain
countries: United States
coordinates: lat: 46.202411111111
lon: -121.49089444444
surface_form: adams
instance_of: Mountain
countries: United States
coordinates: lat: 46.202411111111
lon: -121.49089444444
This is more than any other mountain in the Pacific Northwest. The first extensive list of flora from the area around Mount Adams was published in 1896 by William Suksdorf and Thomas Howell and listed 480 species. Suksdorf had taken it upon himself to catalogue as many species around Adams as he could and the list was the result of his extraordinary collection efforts.

Geographic entities mentioned:
surface_form: adams
instance_of: Mountain
countries: United States
coordinates: lat: 46.202411111111
lon: -121.49089444444
Adams is home to many rare plants including tall bugbane, Suksdorf's monkeyflower, northern microseris (&quot;Microceris borealis&quot;), Brewer's potentilla (&quot;Potentilla breweri&quot;), and mountain blue-eyed grass. The plant diversity is most evident in the many meadows and wetlands on the flanks of Adams.

Geographic entities mentioned:
surface_form: adams
instance_of: Mountain
countries: United States
coordinates: lat: 46.202411111111
lon: -121.49089444444
All the lakes in the High Lakes Area are periodically replanted with varying species of trout. Bull trout can be found in the upper reaches of the Klickitat and Lewis Rivers. Westslope cutthroat trout can be found the Klickitat and cutthroat trout are found in the Lewis River and upper reaches of the Cispus River. Whitefish can be found in the Klickitat, Lewis, and Cispus Rivers.

Geographic entities mentioned:
surface_form: klickitat
instance_of: Mountain
countries: United States
coordinates: lat: 46.202411111111
lon: -121.49089444444
The last known lava flow was approximately 1,000 years ago. The volcano has the potential for future hazards, including lahars, pyroclastic flows, and ashfall. Its deeply eroded flanks drain into major regional rivers like the Cispus, Klickitat and Lewis Rivers.

Geographic entities mentioned:
surface_form: klickitat
instance_of: Mountain
countries: United States
coordinates: lat: 46.202411111111
lon: -121.49089444444
To the south is the Upper Chinook language. An early-20th century mountaineer, William Denison Lyman recorded a Wasco-dialect name for the mountain, &quot;Kakon,&quot; which he stated can refer to any high mountain. One Oregon history magazine stated that the Native American name for the mountain was &quot;Klick-i-lat&quot; Lyman sometimes called it &quot;Klickitat&quot; in his writings.

Geographic entities mentioned:
surface_form: klickitat
instance_of: Mountain
countries: United States
coordinates: lat: 46.202411111111
lon: -121.49089444444
surface_form: klickitat
instance_of: Mountain
countries: United States
coordinates: lat: 46.202411111111
lon: -121.49089444444
This created the Ridge of Wonders between the two. Of the four glaciers on the east side, the Mazama Glacier is the farthest south and begins between the Suksdorf Ridge and Ridge of Wonders at about. Near its terminus, it straddles the Ridge of Wonders and a small portion feeds into the Klickitat Glacier.

Geographic entities mentioned:
surface_form: klickitat
instance_of: Mountain
countries: United States
coordinates: lat: 46.202411111111
lon: -121.49089444444
Klickitat Glacier on the volcano's eastern flank originates in a wide cirque and is fed by two smaller glaciers from the summit ice cap. It terminates around, where it becomes the source of Big Muddy Creek, a tributary of the Klickitat River. The Rusk Glacier does not start from the summit ice cap but starts at below the Roosevelt Cliff and is fed by avalanching snow and ice from the summit cap.

Geographic entities mentioned:
surface_form: klickitat
instance_of: Mountain
countries: United States
coordinates: lat: 46.202411111111
lon: -121.49089444444
It is also fed by an arm of the Lyman Glacier as it flows down from the summit ice cap. The Wilson Glacier terminates at where it is the source of Little Muddy Creek, another tributary of the Klickitat. The north side is distinguished by two major glaciers, the Lyman and Lava Glaciers.

Geographic entities mentioned:
surface_form: klickitat
instance_of: Mountain
countries: United States
coordinates: lat: 46.202411111111
lon: -121.49089444444
Surrounding area. Mount Adams is surrounded by a variety of other volcanic features and volcanoes. It stands near the center of a north–south trending volcanic field that is about wide and long, from just south of the Goat Rocks to Guler Mountain, the vent farthest south in the field. This field includes over 120 vents; about 25 of these are considered flank volcanoes of Mount Adams.

Geographic entities mentioned:
surface_form: goat rocks
instance_of: Mountain
countries: United States
The original goal of the feed materials program in 1942 was to acquire approximately of triuranium octoxide () (black oxide). By the time of the dissolution of the Manhattan District on 1 January 1947, it had acquired about, of which came from the Belgian Congo, from the Colorado Plateau, and from Canada.

Geographic entities mentioned:
surface_form: Colorado Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37
lon: -110
It occurs in various ores, including pitchblende, torbernite, carnotite, and autunite. In the early 19th century it was recovered as a byproduct of mining other ores. Mining of uranium as the principal product began in Joachimsthal in Bohemia in about 1850, at the South Terras mine in Cornwall in 1873, and in Paradox Valley in Colorado in 1898.

Geographic entities mentioned:
surface_form: Paradox Valley
instance_of: Landform
countries: United States
coordinates: lat: 38.3167
lon: -108.85
By 1 January 1947, of sludge was stored there, and had been returned to African Metals. Eldorado mine. After the Belgian Congo, the next most important source of uranium ore was Canada. Canadian ore came from the Eldorado Mine in the Great Bear Lake area, not far south of the Arctic Circle. In May 1930, Gilbert LaBine went prospecting in the area.

Geographic entities mentioned:
surface_form: Great Bear Lake
instance_of: Lake
countries: Canada
coordinates: lat: 66
lon: -121
By 1 January 1947, the Manhattan District had contracted from Eldorado for of ore concentrates to be delivered as of black oxide at a cost of approximately USD$5,082,300 (). United States. In the United States, carnotite ores were mined on the Colorado plateau for their vanadium content. The ores contained roughly 1.75% vanadium pentoxide () and 0.25% uranium dioxide ().

Geographic entities mentioned:
surface_form: Colorado plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37
lon: -110
Black oxide. Eldorado's Port Hope refinery was located on the shores of Lake Ontario in buildings originally built in 1847 as part of a grain terminal. When production started in January 1933, there were just 25 employees; this rose to 287 in 1943.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Soon after Foucault published his results, Bravais was inspired to experimentally test and to mathematically investigate the conical system, leading to the publication &quot;Memoir on the influence exerted by the rotation of the Earth on the oscillatory motions of a conical pendulum&quot;, in 1854. The mountain Bravaisberget, in Svalbard, is named after Bravais.

Geographic entities mentioned:
surface_form: Bravaisberget
instance_of: Mountain
countries: Norway
coordinates: lat: 77.6256
lon: 14.9743
He was then promoted to leading aircraftman. Leaving South Africa, he sailed from Durban to Suez on the &quot;Nieuw Amsterdam&quot;. After &quot;killing time&quot; at RAF Kasfareet near the Great Bitter Lake in the Suez Canal Zone in 1942, he resumed intelligence work in the city of Ismaïlia. He was then attached to No.

Geographic entities mentioned:
surface_form: Great Bitter Lake
instance_of: Lake
countries: Egypt
coordinates: lat: 30.3225
lon: 32.3825
After the Allied invasion of Italy, the squadron was based in Foggia and Termoli during the winter of 1943, where Lee was then seconded to the Army during an officers' swap scheme. During most of the Battle of Monte Cassino he was attached to the Gurkhas of the 8th Indian Infantry Division. While spending some time on leave in Naples, Lee climbed Mount Vesuvius, which erupted three days later.

Geographic entities mentioned:
surface_form: Mount Vesuvius
instance_of: Mountain
countries: Italy
coordinates: lat: 40.821388888889
lon: 14.425555555556
Valle Anzasca. Valle Anzasca (Anzasca Valley) is a valley of the Alps, situated in the Pennine range. The valley is drained by the Anza, a tributary of the Toce at Piedimulera. It is situated to the south of the Valle Antrona. The valley is located in the Province of Verbano-Cusio-Ossola, in the Piedmont region of Italy.

Geographic entities mentioned:
surface_form: Valle Antrona
instance_of: Valley
countries: Italy
coordinates: lat: 46.067
lon: 8.117
The highest mountain in the valley is the Monte Rosa Massif. The highest peak of the massif, amongst several peaks of over, is the Dufourspitze (), the second highest mountain in the Alps and western Europe, after Mont Blanc. The eastern face of the Monte Rosa towards the Valle Anzasca, at Macugnaga has a height of about and is the highest mountain face of the Alps.

Geographic entities mentioned:
surface_form: Dufourspitze
instance_of: Mountain
countries: Switzerland
coordinates: lat: 45.936666666667
lon: 7.8666666666667
surface_form: Mont Blanc
instance_of: Mountain
countries: France
Italy
coordinates: lat: 45.83277777777778
lon: 6.865
The valley is drained by the Anza, a tributary of the Toce at Piedimulera. It is situated to the south of the Valle Antrona. The valley is located in the Province of Verbano-Cusio-Ossola, in the Piedmont region of Italy. It is politically divided into six municipalities: Piedimulera, Calasca-Castiglione, Macugnaga, Bannio Anzino, Vanzone con San Carlo en Ceppo Morelli.

Geographic entities mentioned:
surface_form: ossola
instance_of: Valley
countries: Italy
coordinates: lat: 46.283333333333
lon: 8.35
surface_form: cusio
instance_of: Lake
countries: Italy
coordinates: lat: 45.8098
lon: 8.3963
Valle Anzasca. Valle Anzasca (Anzasca Valley) is a valley of the Alps, situated in the Pennine range. The valley is drained by the Anza, a tributary of the Toce at Piedimulera. It is situated to the south of the Valle Antrona. The valley is located in the Province of Verbano-Cusio-Ossola, in the Piedmont region of Italy.

Geographic entities mentioned:
surface_form: valle anzasca
instance_of: Valley
countries: Italy
coordinates: lat: 45.9667
lon: 7.96667
The highest mountain in the valley is the Monte Rosa Massif. The highest peak of the massif, amongst several peaks of over, is the Dufourspitze (), the second highest mountain in the Alps and western Europe, after Mont Blanc. The eastern face of the Monte Rosa towards the Valle Anzasca, at Macugnaga has a height of about and is the highest mountain face of the Alps.

Geographic entities mentioned:
surface_form: valle anzasca
instance_of: Valley
countries: Italy
coordinates: lat: 45.9667
lon: 7.96667
At only, it does not rank as an Arderin, or a Vandeleur-Lynam; however, it has the prominence to rank as a Marilyn. Diamond Hill lies just west of Knockbrack and the small massif of Benbrack, and looks into the Polladirk valley, around which several major Bens are located.

Geographic entities mentioned:
surface_form: Benbrack
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.533333333333
lon: -9.8666666666667
surface_form: diamond hill
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.55
lon: -9.9166666666667
Geography. Diamond Hill is an isolated peak of the Twelve Bens, which lies in the north-west corner of the range. Immediately east of Diamond Hill is the minor peak of Knockbrack at, which is part of the small massif of Benbrack, one of the core &quot;Twelve Bens&quot;.

Geographic entities mentioned:
surface_form: Benbrack
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.533333333333
lon: -9.8666666666667
surface_form: benbrack
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.533333333333
lon: -9.8666666666667
surface_form: diamond hill
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.55
lon: -9.9166666666667
Immediately east of Diamond Hill is the minor peak of Knockbrack at, which is part of the small massif of Benbrack, one of the core &quot;Twelve Bens&quot;. To the north of Diamond Hill is Kylemore Lough (and Kylemore Abbey), and across the Lough is the massif of Garraun, which is part of the wider Twelve Bens/Garraun Complex Special Area of Conservation.

Geographic entities mentioned:
surface_form: Kylemore Lough
instance_of: Lake
countries: Ireland
coordinates: lat: 53.56027778
lon: -9.85444444
surface_form: garraun
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.584444444444
lon: -9.8605555555556
surface_form: garraun
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.584444444444
lon: -9.8605555555556
surface_form: diamond hill
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.55
lon: -9.9166666666667
To the southeast is the scenic valley of Polladirk, around which several major Bens are located, including Benbrack, Benfree (and Benbaun at, the tallest Ben in the range just behind Benfree), Muckanaght, and Bencullagh. Hill walking.

Geographic entities mentioned:
surface_form: Benbaun
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.521111111111
lon: -9.8311111111111
surface_form: benbaun
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.521111111111
lon: -9.8311111111111
surface_form: benbrack
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.533333333333
lon: -9.8666666666667
Hill walking. Diamond Hill is popular for its accessibility and panoramic views, only ranking behind Croagh Patrick for footfall, and attracts both Irish walkers and foreign tourists. The mountain was closed to climbing in 2002 due to severe erosion but was re-opened in December 2005 after the completion of a Euro 1.4 million wooden boardwalk and stone path trail that would limit further erosion.

Geographic entities mentioned:
surface_form: Croagh Patrick
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.7595
lon: -9.6584
Diamond Hill (Ireland). Diamond Hill or Bengooria () is an isolated peak overlooking the village of Letterfrack, in the northwest corner of the Twelve Bens in Connemara National Park in County Galway, Ireland. At only, it does not rank as an Arderin, or a Vandeleur-Lynam; however, it has the prominence to rank as a Marilyn.

Geographic entities mentioned:
surface_form: arderin
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.03805556
lon: -7.65388889
Diamond Hill (Ireland). Diamond Hill or Bengooria () is an isolated peak overlooking the village of Letterfrack, in the northwest corner of the Twelve Bens in Connemara National Park in County Galway, Ireland. At only, it does not rank as an Arderin, or a Vandeleur-Lynam; however, it has the prominence to rank as a Marilyn.

Geographic entities mentioned:
surface_form: diamond hill
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.55
lon: -9.9166666666667
B. Yeats’ play, &quot;The King’s Threshold&quot;. He is also associated with Dunguaire Castle, near the village of Kinvara. Tempan also notes that Diamond Hill is also known as &quot;Bengooria&quot;, being an anglicised version of its Irish name, as well as &quot;Benhoowirra&quot;, an alternative anglicisation.

Geographic entities mentioned:
surface_form: benhoowirra
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.55
lon: -9.9166666666667
surface_form: bengooria
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.55
lon: -9.9166666666667
Diamond Hill (Ireland). Diamond Hill or Bengooria () is an isolated peak overlooking the village of Letterfrack, in the northwest corner of the Twelve Bens in Connemara National Park in County Galway, Ireland. At only, it does not rank as an Arderin, or a Vandeleur-Lynam; however, it has the prominence to rank as a Marilyn.

Geographic entities mentioned:
surface_form: bengooria
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.55
lon: -9.9166666666667
surface_form: diamond hill
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.55
lon: -9.9166666666667
Despite its moderate size and isolation, compared to the nearby Twelve Bens, Diamond Hill is a popular peak due to its paths and boarded mountain trail, and relative ease of access, together with views of the core Twelve Bens range, and western Connemara. Naming.

Geographic entities mentioned:
surface_form: diamond hill
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.55
lon: -9.9166666666667
Geography. Diamond Hill is an isolated peak of the Twelve Bens, which lies in the north-west corner of the range. Immediately east of Diamond Hill is the minor peak of Knockbrack at, which is part of the small massif of Benbrack, one of the core &quot;Twelve Bens&quot;.

Geographic entities mentioned:
surface_form: diamond hill
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.55
lon: -9.9166666666667
McCall Glacier is located in the Goat Rocks region in the U.S. state of Washington. The glacier is near to the Pacific Crest National Scenic Trail and in the Goat Rocks Wilderness of Snoqualmie National Forest, southeast of Old Snowy Mountain. Packwood Glacier is to the west. Consisting of numerous small bodies of ice, the largest section of McCall Glacier is immediately east of Ives Peak ().

Geographic entities mentioned:
surface_form: Old Snowy Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 46.5119
lon: -121.454
McCall Glacier is located in the Goat Rocks region in the U.S. state of Washington. The glacier is near to the Pacific Crest National Scenic Trail and in the Goat Rocks Wilderness of Snoqualmie National Forest, southeast of Old Snowy Mountain. Packwood Glacier is to the west. Consisting of numerous small bodies of ice, the largest section of McCall Glacier is immediately east of Ives Peak ().

Geographic entities mentioned:
surface_form: Ives Peak
instance_of: Mountain
countries: United States
coordinates: lat: 46.5031
lon: -121.447
In the middle is a water basin and a richly decorated base. The four figures lying at the foot of Athena are allegorical representations of the four most important rivers of the Austro-Hungarian Empire. They represent at the front the Danube and Inn, in the back the Elbe and Vltava (German: Moldau) rivers. On the sides, little cupids ride dolphins.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
The state cabinet, consisting of seven ministers and three advisors, was approved by the state's members of parliament in March 2016. Resources. Tonj State has two major rivers: the Jur River in the northern part of the state and the Tonj River in the southern and eastern parts of the state. Much of the land is considered suitable for agrarian activities.

Geographic entities mentioned:
surface_form: Tonj River
instance_of: Watercourse
countries: South Sudan
coordinates: lat: 8.25493111111111
lon: 29.502146944444444
The thirteener is located east by south (bearing 102°) of the Town of Crestone in Saguache County, Colorado, United States. The Crestones are a cluster of high summits in the Sangre de Cristo Range, comprising Crestone Peak, Crestone Needle, Kit Carson Peak, Challenger Point, Humboldt Peak, and Columbia Point. Columbia Point is subpeak of Kit Carson Mountain.

Geographic entities mentioned:
surface_form: Crestone Peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.9667
lon: -105.585
surface_form: Crestone Needle
instance_of: Mountain
countries: United States
coordinates: lat: 37.964722222222
lon: -105.57666666667
surface_form: Kit Carson Peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.979722222222
lon: -105.6025
surface_form: Challenger Point
instance_of: Mountain
countries: United States
coordinates: lat: 37.980277777778
lon: -105.60666666667
surface_form: humboldt peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.9013
lon: -115.12
surface_form: columbia point
instance_of: Mountain
countries: United States
coordinates: lat: 37.9789
lon: -105.598
Columbia Point. Columbia Point is a high mountain summit of the Crestones in the Sangre de Cristo Range of the Rocky Mountains of North America. The thirteener is located east by south (bearing 102°) of the Town of Crestone in Saguache County, Colorado, United States.

Geographic entities mentioned:
surface_form: columbia point
instance_of: Mountain
countries: United States
coordinates: lat: 37.9789
lon: -105.598
The thirteener is located east by south (bearing 102°) of the Town of Crestone in Saguache County, Colorado, United States. The Crestones are a cluster of high summits in the Sangre de Cristo Range, comprising Crestone Peak, Crestone Needle, Kit Carson Peak, Challenger Point, Humboldt Peak, and Columbia Point. Columbia Point is subpeak of Kit Carson Mountain.

Geographic entities mentioned:
surface_form: columbia point
instance_of: Mountain
countries: United States
coordinates: lat: 37.9789
lon: -105.598
Columbia Point is subpeak of Kit Carson Mountain. It was known informally as Kat Carson, but was officially named Columbia Point in 2003 to honor the seven astronauts who died when the Space Shuttle Columbia disintegrated during re-entry on February 1, 2003. With a topographic prominence over, it qualifies as a separate summit under the standard cutoff, but it is not a well-known peak.

Geographic entities mentioned:
surface_form: columbia point
instance_of: Mountain
countries: United States
coordinates: lat: 37.9789
lon: -105.598
With a topographic prominence over, it qualifies as a separate summit under the standard cutoff, but it is not a well-known peak. The Memorial. The USGS Board of Geographic Names approved the name of Columbia Point in June, 2003. On the weekend of August 7, 2003, a group consisting of family members, astronauts, friends and climbers installed a memorial plaque on the summit.

Geographic entities mentioned:
surface_form: columbia point
instance_of: Mountain
countries: United States
coordinates: lat: 37.9789
lon: -105.598
Brock Mountain. Brock Mountain is a mountain located in the Catskill Mountains of New York southeast of Downsville, New York. Sugarloaf Mountain is located northwest of Brock Mountain and Mary Smith Hill is located east.

Geographic entities mentioned:
surface_form: Mary Smith Hill
instance_of: Mountain
countries: United States
coordinates: lat: 42.0437
lon: -74.83377
surface_form: sugarloaf mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.0748
lon: -123.807
surface_form: sugarloaf mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.6781
lon: -113.051
surface_form: sugarloaf mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.068611111111
lon: -74.926944444444
surface_form: sugarloaf mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.2194
lon: -83.53
surface_form: brock mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.0525
lon: -74.903333333333
surface_form: sugarloaf mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.458333333333
lon: -73.975
surface_form: sugarloaf mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.588055555556
lon: -80.119166666667
surface_form: sugarloaf mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.8875
lon: -74.497777777778
surface_form: sugarloaf mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.0314
lon: -70.3131
surface_form: sugarloaf mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.491111111111
lon: -91.985833333333
surface_form: sugarloaf mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.303333333333
lon: -74.404722222222
surface_form: sugarloaf mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.4728
lon: -72.5975
surface_form: smith hill
instance_of: Mountain
countries: United States
coordinates: lat: 43.144722222222
lon: -75.176388888889
surface_form: sugarloaf mountain
instance_of: Mountain
countries: United States
coordinates: lat: 28.6494
lon: -81.7331
surface_form: sugarloaf mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.198888888889
lon: -116.81444444444
surface_form: sugarloaf mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.9933
lon: -117.322
surface_form: sugarloaf
instance_of: Mountain
countries: United States
coordinates: lat: 43.832777777778
lon: -74.822222222222
surface_form: sugarloaf mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.1313
lon: -74.1502
surface_form: sugarloaf mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.738888888889
lon: -74.931666666667
Brock Mountain. Brock Mountain is a mountain located in the Catskill Mountains of New York southeast of Downsville, New York. Sugarloaf Mountain is located northwest of Brock Mountain and Mary Smith Hill is located east.

Geographic entities mentioned:
surface_form: brock mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.0525
lon: -74.903333333333
Brock Mountain. Brock Mountain is a mountain located in the Catskill Mountains of New York southeast of Downsville, New York. Sugarloaf Mountain is located northwest of Brock Mountain and Mary Smith Hill is located east.

Geographic entities mentioned:
surface_form: brock mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.0525
lon: -74.903333333333
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
Europe shares the landmass of Eurasia with Asia, and of Afro-Eurasia with both Africa and Asia. Europe is commonly considered to be separated from Asia by the watershed of the Ural Mountains, the Ural River, the Caspian Sea, the Greater Caucasus, the Black Sea, and the Turkish straits.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
Europe is taken to be bounded by large bodies of water to the north, west and south; Europe's limits to the east and north-east are usually taken to be the Ural Mountains, the Ural River, and the Caspian Sea; to the south-east, the Caucasus Mountains, the Black Sea, and the waterways connecting the Black Sea to the Mediterranean Sea.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
Europe's eastern frontier was defined in the 1st century by geographer Strabo at the River Don. The &quot;Book of Jubilees&quot; described the continents as the lands given by Noah to his three sons; Europe was defined as stretching from the Pillars of Hercules at the Strait of Gibraltar, separating it from Northwest Africa, to the Don, separating it from Asia.

Geographic entities mentioned:
surface_form: Pillars of Hercules
instance_of: Landform
countries: Morocco
Spain
Gibraltar
coordinates: lat: 36
lon: -5.35
To the south, the Kuma–Manych Depression was identified by a German naturalist, Peter Simon Pallas, as a valley that once connected the Black Sea and the Caspian Sea, and subsequently was proposed as a natural boundary between continents.

Geographic entities mentioned:
surface_form: Kuma–Manych Depression
instance_of: Valley
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 45.715
lon: 44.105
Flora. Having lived side by side with agricultural peoples for millennia, Europe's animals and plants have been profoundly affected by the presence and activities of humans. With the exception of Fennoscandia and northern Russia, few areas of untouched wilderness are currently found in Europe, except for various national parks. The main natural vegetation cover in Europe is mixed forest.

Geographic entities mentioned:
surface_form: Fennoscandia
instance_of: Landform
countries: Norway
Sweden
Finland
Russia
Russian Empire
Soviet Union
coordinates: lat: 63
lon: 17
The Arkansas River was given its name to indicate that it
was the river of the Arkansas (Indians); therefore the &quot;Arkansas River.&quot; The mountains in the vicinity of the Arkansas River were also given that
name to mean also the mountains of the Arkansas (Indians); therefore the
The growing of grapes is well suited to the climate and soils of the Ozarks.

Geographic entities mentioned:
surface_form: Ozarks
instance_of: Plateau
countries: United States
coordinates: lat: 37.1822
lon: -92.5159
The state is coterminous with the eponymous region of Zulia. Zulia is located in northwestern Venezuela, bordering Lake Maracaibo, the largest body of its kind in Latin America. The lake's basin holds some of the largest oil and gas reserves in the Western Hemisphere.

Geographic entities mentioned:
surface_form: Lake Maracaibo
instance_of: Lake
countries: Venezuela
coordinates: lat: 9.8158333333333
lon: -71.556666666667
Its economy is primarily based on oil and natural gas. Oil activity has been conducted intensively since 1912, both on land and in Lake Maracaibo, generating income that extends beyond the regional scope, as it serves as a major pillar of the national economy. Zulia contributes a large share of the country's oil and hydrocarbon production.

Geographic entities mentioned:
surface_form: Lake Maracaibo
instance_of: Lake
countries: Venezuela
coordinates: lat: 9.8158333333333
lon: -71.556666666667
Devarmalai. Kathir Narasinga Perumal temple in Devar Mala or Devarmalai is a five-centuries-old Hindu shrine. This temple is famous for its legend, which goes back to Hiranya Samhara. After Hiranya Samharam, the ferocious Narasimha, came to the forest area of Devar Malai, where he was intercepted by the Devas who had congregated in large numbers.

Geographic entities mentioned:
surface_form: Devar Mala
instance_of: Mountain
countries: India
coordinates: lat: 9.189438888888889
lon: 77.24586944444445
This temple is famous for its legend, which goes back to Hiranya Samhara. After Hiranya Samharam, the ferocious Narasimha, came to the forest area of Devar Malai, where he was intercepted by the Devas who had congregated in large numbers. In an effort to calm him down, the Devas brought sacred water and performed abishekam for Narasimha.

Geographic entities mentioned:
surface_form: Devar Mala
instance_of: Mountain
countries: India
coordinates: lat: 9.189438888888889
lon: 77.24586944444445
Takusa. Takusa (Amharic: ጣቁሳ) is a woreda in Amhara Region, Ethiopia. Part of the Semien Gondar Zone, Takusa is bordered on the south by Alefa, on the west by Qwara, on the northwest by the Metemma, on the north by Chilga, on the northeast by Dembiya, and on the east by Lake Tana. Towns in Takusa include Delgi. Takusa was part of Alefa woreda. Demographics.

Geographic entities mentioned:
surface_form: Lake Tana
instance_of: Lake
countries: Ethiopia
coordinates: lat: 12
lon: 37.25
Location. The hill located at which is 690 m southwest of Xenia Hill, 1.03 km north by west of La Morenita Hill, 10.43 km east by north of Sliven Peak, Livingston Island, 8.1 km east by south of Sindel Point, Livingston Island and 6.81 km southeast of Edinburgh Hill, Livingston Island (Bulgarian mapping in 2005 and 2009).

Geographic entities mentioned:
surface_form: Sliven Peak
instance_of: Mountain
coordinates: lat: -62.600972222222
lon: -60.128333333333
surface_form: Edinburgh Hill
instance_of: Mountain
coordinates: lat: -62.5425
lon: -60.0169
In 1417 he acquired the rights over the city of Feldkirch and in 1424 added Rheineck and Altstätten. Following his successful invasion of Appenzell, in 1428 at the end of the Appenzell Wars, he had acquired almost all the Austrian possessions from Rheineck to Montafon as well as the county of Werdenburg from Sargans to the upper regions of Lake Zurich.

Geographic entities mentioned:
surface_form: Montafon
instance_of: Valley
countries: Austria
coordinates: lat: 47.08
lon: 9.9
surface_form: Lake Zurich
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.2475
lon: 8.6775
Design. The train is -long and painted in royal blue. It gets its name from the Deccan Plateau which is located in Maharashtra. The design is meant to emulate the luxuries enjoyed by 16th century Maharajas. The train has 21 coaches, each named after places in Maharashtra and can accommodate up to 88 passengers. Amenities.

Geographic entities mentioned:
surface_form: Deccan Plateau
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
All Cachar Karimganj Hailakandi Students Association. All Cachar Karimganj Hailakandi Students Association (ACKHSA) was established in 1983 by Pradip Dutta Roy. The movement resulted in the establishment of Assam University. Dutta Roy's started a mass movement in 1983 towards the educational development of Barak Valley.

Geographic entities mentioned:
surface_form: Barak Valley
instance_of: Valley
countries: India
coordinates: lat: 24.833333333333332
lon: 92.8
Medicine Lake (South Dakota). Medicine Lake is a natural lake in South Dakota, in the United States. The lake's name comes from the Sioux Indians of the area, who believed the waters of Medicine Lake held medicinal qualities.

Geographic entities mentioned:
surface_form: medicine lake
instance_of: Lake
countries: United States
coordinates: lat: 45.00644
lon: -93.41997
surface_form: medicine lake (south dakota)
instance_of: Lake
countries: United States
coordinates: lat: 44.9841655
lon: -97.3519987
Medicine Lake (South Dakota). Medicine Lake is a natural lake in South Dakota, in the United States. The lake's name comes from the Sioux Indians of the area, who believed the waters of Medicine Lake held medicinal qualities.

Geographic entities mentioned:
surface_form: medicine lake
instance_of: Lake
countries: United States
coordinates: lat: 45.00644
lon: -93.41997
surface_form: medicine lake
instance_of: Lake
countries: United States
coordinates: lat: 44.9841655
lon: -97.3519987
Sightings in the UK. They were first recorded in the Shin Valley in 1853. Two were found in 1996 on the top of Glas Maol in the Grampians with a further two found nearby. In June 2008 an adult Ethmia pyrausta moth was discovered in Easter Ross, by Andy Scott and Margaret Currie after finding it trapped in a spider web.

Geographic entities mentioned:
surface_form: Glas Maol
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.873059
lon: -3.368236
The area is located from Ballina town centre just off the N57. The Ramada Manor Court Hotel is metres away from the end of Rathnaconeen Road, as is Rehins school. The view from the top of Rathnaconeen hill takes in the railroad tracks and the mountain of Nephin. On the opposite view are the Ox Mountains.

Geographic entities mentioned:
surface_form: Nephin
instance_of: Mountain
countries: Ireland
coordinates: lat: 54.012
lon: -9.368
The Slettnes Lighthouse near the village of Gamvik is the northernmost lighthouse on the mainland of Europe. Nervei and Langfjordbotn are two very small villages in southern Gamvik that are only accessible by boat. Finnkongkeila is an abandoned village along the Tanafjorden. The municipality is the 65th largest by area out of the 357 municipalities in Norway.

Geographic entities mentioned:
surface_form: Finnkongkeila
instance_of: Valley
countries: Norway
coordinates: lat: 70.910555555556
lon: 28.453055555556
The &quot;Katastralgemeindes territory includes the two high valleys of Salzachursprung and Nadernachbach, and the area between the &quot;Ochsenkopf&quot; in the west, the Schwebenkopf and Kröndlhorn in the north and the Gernkogel to the east, up to the state border with Tyrol. It measures in area and about across at its widest point. History.

Geographic entities mentioned:
surface_form: Kröndlhorn
instance_of: Mountain
countries: Austria
coordinates: lat: 47.2983
lon: 12.1644
King Hollow. King Hollow is a valley in Hickman County, Tennessee in the United States. King Hollow was named for a pioneer named King who settled there in 1815.

Geographic entities mentioned:
surface_form: king hollow
instance_of: Valley
countries: United States
coordinates: lat: 35.672684
lon: -87.679554
They regrouped near Ombriano, aiming to ambush French foraging parties raiding nearby villages. Additional support arrived as a tax of one-and-a-half soldi funded the recruitment of Bergamasque infantry and Val Trompia arquebusiers. Two camps were established at Ombriano and, complete with wooden bridges over the Serio river to pressure the occupiers.

Geographic entities mentioned:
surface_form: Val Trompia
instance_of: Valley
countries: Italy
coordinates: lat: 45.691944444444
lon: 10.186388888889
Gisu people. The Gisu people, or &quot;Bamasaba&quot; people of Elgon, are a Bantu tribe and Bantu-speaking ethnic group of the Masaba people in eastern Uganda, closely related to the Bukusu people of Kenya. Bamasaba live mainly in the Mbale District of Uganda on the slopes of Mount Elgon.

Geographic entities mentioned:
surface_form: Mount Elgon
instance_of: Mountain
countries: Uganda
Kenya
coordinates: lat: 1.1185
lon: 34.5265
Genevieve. The community was also referred to as &quot;Establishment&quot; in the past due to its proximity to Establishment Creek and the adjacent Establishment Island in the Mississippi floodplain. A small stream in Staples Hollow joins Establishment Creek at the site. The current name is derived from the people who had a fishing club at the site.

Geographic entities mentioned:
surface_form: Staples Hollow
instance_of: Valley
countries: United States
coordinates: lat: 38.05777778
lon: -90.16638889
Drainage basin. Mount Cleveland stands within the watershed of Lake Champlain, which drains into the Richelieu River in Québec, the Saint Lawrence River, and then eventually into the Gulf of Saint Lawrence. The north side of Mount Cleveland drains into Stetson Brook, thence into the Mad River, the Winooski River, and into Lake Champlain.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
surface_form: cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 52.822222222222
lon: -169.945
surface_form: mount cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 52.822222222222
lon: -169.945
surface_form: mount cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 48.9244858
lon: -113.848042
surface_form: mount cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 44.046388888889
lon: -72.908055555556
Mount Cleveland (Vermont). Mount Cleveland is a mountain in the Green Mountains in the U.S. state of Vermont. Located in the Breadloaf Wilderness of the Green Mountain National Forest, its summit is in the town of Lincoln in Addison County. The mountain is named after Grover Cleveland, former president of the United States. Mount Cleveland is one of five peaks in Vermont's Presidential Range.

Geographic entities mentioned:
surface_form: cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 52.822222222222
lon: -169.945
surface_form: mount cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 52.822222222222
lon: -169.945
surface_form: mount cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 48.9244858
lon: -113.848042
surface_form: mount cleveland (vermont)
instance_of: Mountain
countries: United States
coordinates: lat: 44.046388888889
lon: -72.908055555556
Mount Cleveland (Vermont). Mount Cleveland is a mountain in the Green Mountains in the U.S. state of Vermont. Located in the Breadloaf Wilderness of the Green Mountain National Forest, its summit is in the town of Lincoln in Addison County. The mountain is named after Grover Cleveland, former president of the United States. Mount Cleveland is one of five peaks in Vermont's Presidential Range.

Geographic entities mentioned:
surface_form: cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 52.822222222222
lon: -169.945
surface_form: mount cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 52.822222222222
lon: -169.945
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: mount cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 48.9244858
lon: -113.848042
surface_form: mount cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 44.046388888889
lon: -72.908055555556
Mount Cleveland is a mountain in the Green Mountains in the U.S. state of Vermont. Located in the Breadloaf Wilderness of the Green Mountain National Forest, its summit is in the town of Lincoln in Addison County. The mountain is named after Grover Cleveland, former president of the United States. Mount Cleveland is one of five peaks in Vermont's Presidential Range. Drainage basin.

Geographic entities mentioned:
surface_form: cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 52.822222222222
lon: -169.945
Mount Cleveland is a mountain in the Green Mountains in the U.S. state of Vermont. Located in the Breadloaf Wilderness of the Green Mountain National Forest, its summit is in the town of Lincoln in Addison County. The mountain is named after Grover Cleveland, former president of the United States. Mount Cleveland is one of five peaks in Vermont's Presidential Range. Drainage basin.

Geographic entities mentioned:
surface_form: cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 52.822222222222
lon: -169.945
surface_form: mount cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 52.822222222222
lon: -169.945
surface_form: mount cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 48.9244858
lon: -113.848042
surface_form: mount cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 44.046388888889
lon: -72.908055555556
Drainage basin. Mount Cleveland stands within the watershed of Lake Champlain, which drains into the Richelieu River in Québec, the Saint Lawrence River, and then eventually into the Gulf of Saint Lawrence. The north side of Mount Cleveland drains into Stetson Brook, thence into the Mad River, the Winooski River, and into Lake Champlain.

Geographic entities mentioned:
surface_form: cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 52.822222222222
lon: -169.945
surface_form: mount cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 52.822222222222
lon: -169.945
surface_form: mount cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 48.9244858
lon: -113.848042
surface_form: mount cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 44.046388888889
lon: -72.908055555556
The north side of Mount Cleveland drains into Stetson Brook, thence into the Mad River, the Winooski River, and into Lake Champlain. The south and east sides of Mount Cleveland drain into Austin Brook and then into the Mad River. The west side of Mount Cleveland drains into the New Haven River, thence into Otter Creek, and into Lake Champlain. Hiking.

Geographic entities mentioned:
surface_form: cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 52.822222222222
lon: -169.945
surface_form: mount cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 52.822222222222
lon: -169.945
surface_form: mount cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 48.9244858
lon: -113.848042
surface_form: mount cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 44.046388888889
lon: -72.908055555556
The west side of Mount Cleveland drains into the New Haven River, thence into Otter Creek, and into Lake Champlain. Hiking. The Long Trail traverses the summit of Mount Cleveland at. The Cooley Glen Trail, whose trailhead is in the town of Lincoln, terminates at the Cooley Glen Shelter after. From the shelter, Mount Cleveland is south on the Long Trail.

Geographic entities mentioned:
surface_form: cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 52.822222222222
lon: -169.945
surface_form: mount cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 52.822222222222
lon: -169.945
surface_form: mount cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 48.9244858
lon: -113.848042
surface_form: mount cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 44.046388888889
lon: -72.908055555556
The Cooley Glen Trail, whose trailhead is in the town of Lincoln, terminates at the Cooley Glen Shelter after. From the shelter, Mount Cleveland is south on the Long Trail. The Emily Proctor Trail, whose trailhead coincides with the Cooley Glen Trailhead, terminates at the Emily Proctor Shelter, which is approximately south of Mount Cleveland on the Long Trail.

Geographic entities mentioned:
surface_form: cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 52.822222222222
lon: -169.945
surface_form: mount cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 52.822222222222
lon: -169.945
surface_form: mount cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 48.9244858
lon: -113.848042
surface_form: mount cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 44.046388888889
lon: -72.908055555556
From the shelter, Mount Cleveland is south on the Long Trail. The Emily Proctor Trail, whose trailhead coincides with the Cooley Glen Trailhead, terminates at the Emily Proctor Shelter, which is approximately south of Mount Cleveland on the Long Trail. A popular loop hike begins and ends at the Cooley Glen Trailhead (or the Emily Proctor Trailhead in a counterclockwise direction).

Geographic entities mentioned:
surface_form: cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 52.822222222222
lon: -169.945
surface_form: mount cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 52.822222222222
lon: -169.945
surface_form: mount cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 48.9244858
lon: -113.848042
surface_form: mount cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 44.046388888889
lon: -72.908055555556