Sarmila/GeoWiki-Features huggingface dataset:
state of Oregon. Little Blitzen River rises on the west flank of Steens Mountain about southeast of Frenchglen and about south of Burns in Harney County. Flowing west in a steep-walled canyon, it joins the South Fork Donner und Blitzen River at to form the Donner und Blitzen main stem, which continues north about another to its mouth at in Malheur Lake.

Geographic entities mentioned:
surface_form: Malheur Lake
instance_of: Lake
countries: United States
coordinates: lat: 43.332777777778
lon: -118.79305555556
It is a sub-prefecture of the Nord department. It is situated 14 km from the Belgian border, and 18 km south of Maubeuge, the nearest larger town. The river Helpe Majeure, a tributary of the Sambre, flows through the town. Upstream of Avesnes on the river there is the Lac du Val-Joly, an artificial lake. History. Avesnes was founded in the 11th century.

Geographic entities mentioned:
surface_form: Lac du Val-Joly
instance_of: Lake
countries: France
coordinates: lat: 50.11528
lon: 4.13222
Eteobalea serratella. &quot;Eteobalea serratella&quot; is a moth in the family Cosmopterigidae. It is found in most of Europe, except the Benelux, Great Britain, Ireland, Iceland, Fennoscandia and the Baltic states. It was approved for release in the United States in 1995 for the biological control of toadflax.

Geographic entities mentioned:
surface_form: Fennoscandia
instance_of: Landform
countries: Norway
Sweden
Finland
Russia
Russian Empire
Soviet Union
coordinates: lat: 63
lon: 17
Coleophora amellivora. &quot;Coleophora amellivora&quot; is a moth of the family Coleophoridae. It is found from Fennoscandia to the Pyrenees, Italy and Romania and from France to Poland. The larvae feed on &quot;Aster alpinus&quot;, &quot;Aster amellus&quot;, &quot;Aster linosyris&quot; and &quot;Aster salignus&quot;. Larvae can be found from September to May.

Geographic entities mentioned:
surface_form: Fennoscandia
instance_of: Landform
countries: Norway
Sweden
Finland
Russia
Russian Empire
Soviet Union
coordinates: lat: 63
lon: 17
History. Ada was laid out in 1874 and incorporated on February 9, 1881. It was named in honor of a daughter of William H. Fisher (the namesake of Fisher, Minnesota), of St. Paul, then attorney and superintendent of the St. Paul and Pacific Railroad, under whose superintendency this line of the Red River Valley was constructed. A post office has been in operation at Ada since 1876.

Geographic entities mentioned:
surface_form: Red River Valley
instance_of: Valley
countries: Canada
United States
coordinates: lat: 49
lon: -97.5
The range is named after Cathedral Peak, which resembles a cathedral spire. Geography. The range includes Cathedral Peak, Unicorn Peak, Eichorn Pinnacle, Echo Peaks, Echo Ridge, Matthes Crest, Rafferty Peak, Vogelsang Peak, Fletcher Peak and Cockscomb. The highest point in the range is Mount Florence, one of the most prominent peaks in the Yosemite high country.

Geographic entities mentioned:
surface_form: Rafferty Peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.81493
lon: -119.35571
surface_form: Vogelsang Peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.7775
lon: -119.348
surface_form: Fletcher Peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.7917821
lon: -119.3357502
The highest point in the range is Mount Florence, one of the most prominent peaks in the Yosemite high country. The highest peak in Tuolumne Meadows is Johnson Peak. The range runs beside the two Cathedral Lakes, just one mile southwest of Cathedral Peak. Hikers can access the lakes and Cathedral range by the John Muir trail from the trailhead in Tuolumne Meadows. Geology.

Geographic entities mentioned:
surface_form: Cathedral Lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 37.844994
lon: -119.423954
Eastern Turkic Khaganate. The Eastern Turkic Khaganate () was a Turkic khaganate formed as a result of the internecine wars in the beginning of the 7th century (AD 581–603) after the First Turkic Khaganate (founded in the 6th century in the Mongolian Plateau by the Ashina clan) had splintered into two polities – one in the east and the other in the west.

Geographic entities mentioned:
surface_form: Mongolian Plateau
instance_of: Plateau
countries: Mongolia
People's Republic of China
Russia
Russian Empire
Soviet Union
coordinates: lat: 45
lon: 107
Finally, the Eastern Turkic Khaganate was defeated and absorbed by the Tang dynasty, and Xueyantuo occupied the territory of the former Turkic Khaganate. Outline. In 552–555 the Göktürks replaced the Rouran Khaganate as the dominant power on the Mongolian Plateau, forming the First Turkic Khaganate (552–630). They quickly spread west to the Caspian Sea.

Geographic entities mentioned:
surface_form: Mongolian Plateau
instance_of: Plateau
countries: Mongolia
People's Republic of China
Russia
Russian Empire
Soviet Union
coordinates: lat: 45
lon: 107
This was a period of significant expansion of the geographical territory occupied by Germanic tribes, and consequently of the number of German speakers. Whereas during the Old High German period the Germanic tribes extended only as far east as the Elbe and Saale rivers, the MHG period saw a number of these tribes expanding beyond this eastern boundary into Slavic territory (known as the ').

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Oceania. In Australia, the state of South Australia experienced a pronounced wave of Prussian immigration in the 1840s (particularly from Silesia region). With the prolonged isolation from other German speakers and contact with Australian English, a unique dialect known as Barossa German developed, spoken predominantly in the Barossa Valley near Adelaide.

Geographic entities mentioned:
surface_form: Barossa Valley
instance_of: Valley
countries: Australia
coordinates: lat: -34.533333333333
lon: 138.95
Alemannic dialects are spoken in Switzerland (High Alemannic in the densely populated Swiss Plateau including Zürich and Bern, in the south also Highest Alemannic, and Low Alemannic in Basel), Baden-Württemberg (Swabian and Low Alemannic, in the southwest also High Alemannic), Bavarian Swabia (Swabian, in the southwesternmost part also Low Alemannic), Vorarlberg/Austria (Low, High, and Highest Alemannic), Alsace/France (Low Alemannic, in the southernmost part also High Alemannic), Liechtenstein (High and Highest Alemannic), and in the district of Reutte in Tyrol, Austria (Swabian).

Geographic entities mentioned:
surface_form: Swiss Plateau
instance_of: Plateau
countries: Switzerland
coordinates: lat: 47.1167
lon: 7.36667
She arrived in Calcutta, India, in April 1945. She left Calcutta on a hospital ship that crossed the Bay of Bengal and sailed through the Strait of Malacca toward Singapore. Her convoy slowly made its way single-file through mine-invested waters and Fletcher did not arrive in Singapore until September 2.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Contact Peak. Contact Peak () is a prominent rock peak, high, which is the southeasternmost peak on Pourquoi Pas Island, off the west coast of Graham Land. It was first sighted and roughly charted in 1909 by the French Antarctic Expedition under Jean-Baptiste Charcot. It was surveyed in 1936 by the British Graham Land Expedition and in 1948 by the Falkland Islands Dependencies Survey (FIDS).

Geographic entities mentioned:
surface_form: contact peak
instance_of: Mountain
coordinates: lat: -67.7667
lon: -67.4833
Kirk Lake (New York). Kirk Lake is a controlled lake in the hamlet of Mahopac in the town of Carmel in Putnam County, New York. First impounded in 1871, with a substantially larger dam placed in 1881, it lies due west and sharply below considerably larger Lake Mahopac. It is one of three controlled lakes in the New York City water supply system's Croton Watershed.

Geographic entities mentioned:
surface_form: kirk lake (new york)
instance_of: Lake
countries: United States
coordinates: lat: 41.386111111111
lon: -73.751944444444
surface_form: kirk lake
instance_of: Lake
countries: United States
coordinates: lat: 47.15666667
lon: -95.25333333
Kirk Lake (New York). Kirk Lake is a controlled lake in the hamlet of Mahopac in the town of Carmel in Putnam County, New York. First impounded in 1871, with a substantially larger dam placed in 1881, it lies due west and sharply below considerably larger Lake Mahopac. It is one of three controlled lakes in the New York City water supply system's Croton Watershed.

Geographic entities mentioned:
surface_form: kirk lake
instance_of: Lake
countries: United States
coordinates: lat: 41.386111111111
lon: -73.751944444444
surface_form: kirk lake
instance_of: Lake
countries: United States
coordinates: lat: 47.15666667
lon: -95.25333333
It is one of three controlled lakes in the New York City water supply system's Croton Watershed. The outfall of Kirk Lake is a tributary of the Muscoot River, which flows into the Croton River that drains the Croton River watershed. Waters from Kirk lake join the Muscoot approximately one mile below its northernmost headwaters to the west.

Geographic entities mentioned:
surface_form: kirk lake
instance_of: Lake
countries: United States
coordinates: lat: 41.386111111111
lon: -73.751944444444
surface_form: kirk lake
instance_of: Lake
countries: United States
coordinates: lat: 47.15666667
lon: -95.25333333
History. Kirk Lake was originally much smaller than today. An initial dam was built in 1871, and substantially altered into a 220 foot wide, 28 foot high structure in 1881, dramatically enlarging its empoundment area. It is unclear whether there would be any natural empoundment at all if it were removed. The dam is a stone masonry-earth buttress.

Geographic entities mentioned:
surface_form: kirk lake
instance_of: Lake
countries: United States
coordinates: lat: 41.386111111111
lon: -73.751944444444
surface_form: kirk lake
instance_of: Lake
countries: United States
coordinates: lat: 47.15666667
lon: -95.25333333
Maximum reservoir capacity is 1822 acre-feet, or. Kirk Lake is owned by the New York City Department of Environmental Protection (which absorbed the New York City Bureau of Water Supply). Its drainage area is 2.95 square miles, and maximum discharge of its spillway and 36&quot; overflow pipe 440 cubic feet of water per second.

Geographic entities mentioned:
surface_form: kirk lake
instance_of: Lake
countries: United States
coordinates: lat: 41.386111111111
lon: -73.751944444444
surface_form: kirk lake
instance_of: Lake
countries: United States
coordinates: lat: 47.15666667
lon: -95.25333333
A 1981 report by the New York District Corps of Engineers determined that the dam possessed structural deficiencies that would require attention to mitigate flood risks. This work was completed in September 2000. The normal length of Kirk Lake's pool is 0.8 miles, with a total surface area of 122 acres. Its maximum depth is and mean is. Maximum pool size is 220 acres.

Geographic entities mentioned:
surface_form: kirk lake
instance_of: Lake
countries: United States
coordinates: lat: 41.386111111111
lon: -73.751944444444
surface_form: kirk lake
instance_of: Lake
countries: United States
coordinates: lat: 47.15666667
lon: -95.25333333
From then on Glenoglehead functioned as a private halt for railway servants and as a crossing place. A branch to Ballachulish. The West Highland Railway opened to Fort William in 1894, and interest was aroused in opening up other areas of the region. Railways along the Great Glen were proposed, and attention also turned to the tract of remote terrain between Oban and Fort William.

Geographic entities mentioned:
surface_form: Great Glen
instance_of: Valley
countries: United Kingdom
coordinates: lat: 57.3
lon: -4.45
Only Glenoglehead station building still stands, now in use as a private house. Most of the underbridges have been removed or destroyed, but the impressive Glen Ogle viaduct still survives. Parts of the trackbed between Killin Junction and Crianlarich have been obliterated by improvements to the A85 road.

Geographic entities mentioned:
surface_form: Glen Ogle viaduct
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.408333333333
lon: -4.3125
Ráby. Ráby () is a municipality and village in Pardubice District in the Pardubice Region of the Czech Republic. It has about 600 inhabitants. The Kunětická hora mountain with the Kunětická hora Castle lies in the municipality.

Geographic entities mentioned:
surface_form: Kunětická hora
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.08
lon: 15.812777777778
Early Logging Operations. By the 1890s, lumbermen, including Frederick Weyerhaeuser, had begun timbering the vast pine forests north of Lake Superior. Initially, the massive pine logs were floated down the entire length of the often frozen and perilous Cloquet River to the City of Cloquet, Minnesota via the Saint Louis River.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
Alden Lake. Alden Lake (aka Big Alden Lake) is a freshwater 180-acre lake with 159 (88%) acres of littoral area and a maximum depth of 29 feet located in northern Minnesota 14 miles northeast of Duluth off St. Louis County Highway #44. Alden does not have a developed public access along the shoreline but can be accessed by canoe through the Cloquet River.

Geographic entities mentioned:
surface_form: alden lake
instance_of: Lake
countries: United States
coordinates: lat: 47.06111111
lon: -92.03277778
Alden Lake. Alden Lake (aka Big Alden Lake) is a freshwater 180-acre lake with 159 (88%) acres of littoral area and a maximum depth of 29 feet located in northern Minnesota 14 miles northeast of Duluth off St. Louis County Highway #44. Alden does not have a developed public access along the shoreline but can be accessed by canoe through the Cloquet River.

Geographic entities mentioned:
surface_form: alden lake
instance_of: Lake
countries: United States
coordinates: lat: 47.06111111
lon: -92.03277778
surface_form: alden lake
instance_of: Lake
countries: United States
coordinates: lat: 47.06111111
lon: -92.03277778
This means of transporting the timber was obviously less than ideal, and in 1901, M. Joseph Scanlon and Lester Brooks formed the Brooks-Scanlon Lumber Company and planned to improve the transport of the large timber stands they controlled along the Cloquet River by building a sorting works and rail operation at Alden Lake. Construction of Railway and Sorting Works.

Geographic entities mentioned:
surface_form: alden lake
instance_of: Lake
countries: United States
coordinates: lat: 47.06111111
lon: -92.03277778
Construction of Railway and Sorting Works. Cloquet lumbermen under Weyerhaeuser's direction objected to this plan, however, claiming that the Alden Lake sorting works would interfere with the floating of their logs beyond it to Cloquet. Brooks-Scanlon argued that the additional expense and extended delivery time of water transport made rail shipment imperative.

Geographic entities mentioned:
surface_form: alden lake
instance_of: Lake
countries: United States
coordinates: lat: 47.06111111
lon: -92.03277778
In partnership with the Minnesota and North Wisconsin Railroad (1898-1912), a main rail line was constructed from Brooks-Scanlon's mill in Scanlon, Minnesota to Carolon, 44.5 miles to the northeast. In 1904, a 3.5-mile branch of this line was built from Alden Junction to Alden Lake, to which logs were floated from upstream.

Geographic entities mentioned:
surface_form: alden lake
instance_of: Lake
countries: United States
coordinates: lat: 47.06111111
lon: -92.03277778
In 1904, a 3.5-mile branch of this line was built from Alden Junction to Alden Lake, to which logs were floated from upstream. At Alden Lake, a logging dam was constructed and a hoist was erected to load logs onto rail cars. At the peak of its operation, Brooks-Scanlon employed approximately 1500 men and harvested a record-breaking amount of board feet of pine.

Geographic entities mentioned:
surface_form: alden lake
instance_of: Lake
countries: United States
coordinates: lat: 47.06111111
lon: -92.03277778
By the time it reaches Baltonsborough it is only some above sea level and the surrounding countryside is drained into it by way of numerous rhynes. It passes Glastonbury, where it acts as a natural boundary with nearby village of Street, before flowing in a largely artificial channel across the Somerset Levels and into the River Parrett at Burnham-on-Sea.

Geographic entities mentioned:
surface_form: River Parrett
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 51.2292
lon: -3.00861
The Glastonbury Canal used the course of the River Brue from Highbridge to Cripp's Bridge, and part of the South Drain to Ashcott Corner. The Glastonbury Canal ran for just over through two locks from Glastonbury to Highbridge, where it entered the River Parrett and from there the Bristol Channel. The canal was authorised by Parliament in 1827 and opened in 1834.

Geographic entities mentioned:
surface_form: River Parrett
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 51.2292
lon: -3.00861
Hart Fell is gently sloping on three sides of the hill, however the east ridge is steep and craggy and features a deep corrie known as Blackhope. The normal route is from the southern ridge, passing over Swatte Fell and can be extended to include a full loop of Blackhope, finishing on Saddle Yoke, known as the Hart Fell Horseshoe.

Geographic entities mentioned:
surface_form: yoke
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.451
lon: -2.869
surface_form: hart fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.4
lon: -3.4
Hart Fell. Hart Fell is a hill in the Moffat Hills range, part of the Southern Uplands of Scotland. It lies north of the town of Moffat on the border with the Scottish Borders and Dumfries and Galloway. A broad, rolling hill, is visible from the M74 motorway in the west, parts of Dumfries and ranges to the east.

Geographic entities mentioned:
surface_form: hart fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.4
lon: -3.4
It lies north of the town of Moffat on the border with the Scottish Borders and Dumfries and Galloway. A broad, rolling hill, is visible from the M74 motorway in the west, parts of Dumfries and ranges to the east. Hart Fell is gently sloping on three sides of the hill, however the east ridge is steep and craggy and features a deep corrie known as Blackhope.

Geographic entities mentioned:
surface_form: hart fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.4
lon: -3.4
Knowes of Trotty is one of the earliest group of burial mounds in Orkney and one of the largest Bronze Age cemeteries in the United Kingdom. The site. The Knowes of Trotty Bronze Age burial site is located east of the Loch of Harray, in Mainland, Orkney. Twelve burial mounds are situated at the bottom of the western slopes of the Ward of Redland.

Geographic entities mentioned:
surface_form: Loch of Harray
instance_of: Lake
countries: United Kingdom
coordinates: lat: 59.02408
lon: -3.22996
Tischer Creek. Tischer Creek is a stream in the U.S. state of Minnesota. It empties into Lake Superior in the city of Duluth on the grounds of the Glensheen Historic Estate. Its waters supply a 60,000 gallon reservoir and are used to maintain the grounds of the estate. Tischer Creek was named after Urs and Elizabeth Tischer, pioneers who settled the area in the 1850s.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
The Wayilwan clan were on their southeastern flank, the Wangaaypuwan clan southwest while the Gamilaraay were to the northeast and the Paakantyi to their west and northwest. Mount Grenfell, some northwest of Cobar, is an important site for the Ngiyampaa people, who were barred from accessing it until the 1970s. Group classifications.

Geographic entities mentioned:
surface_form: Mount Grenfell
instance_of: Mountain
countries: Australia
coordinates: lat: -31.301111111111112
lon: 145.30944444444444
In 1926, the plans included an educational center, an idea originally made by the previous owner of the property, state senator David Hume Baker. The land was acquired by C. Edgar Wood a capitalist from Baltimore with the aim to develop it and the area around Lake Okahumpka and Lake Deaton. State senator Baker lived in Orange Home and his historic Baker House remains there.

Geographic entities mentioned:
surface_form: Lake Okahumpka
instance_of: Lake
countries: United States
coordinates: lat: 28.825833333333
lon: -82.005555555556
surface_form: Lake Deaton
instance_of: Lake
countries: United States
coordinates: lat: 28.834722222222222
lon: -81.98194444444445
Dent du Bourgo. The Dent du Bourgo (1,909 m) is a mountain of the Swiss Prealps, located east of Gruyères in the canton of Fribourg. It lies on the range north of the Vanil Noir, between the valleys of the Sarine and the Motélon.

Geographic entities mentioned:
surface_form: Vanil Noir
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.528472222222
lon: 7.1483611111111
Dent du Bourgo. The Dent du Bourgo (1,909 m) is a mountain of the Swiss Prealps, located east of Gruyères in the canton of Fribourg. It lies on the range north of the Vanil Noir, between the valleys of the Sarine and the Motélon.

Geographic entities mentioned:
surface_form: dent du bourgo
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.57555556
lon: 7.13972222
Borgu Game Reserve. The Borgu Game Reserve is a section of the Kainji National Park, in the Borgu Local Government Area of Niger State and Baruten Local
Government Area of Kwara State, Nigeria. It is bordered on the east by Kainji Lake and reaches almost to the border with Benin to the west, covering. It was amalgamated with the Zugurma Game Reserve in 1975 to form the Kainji Lake National Park.

Geographic entities mentioned:
surface_form: Kainji Lake
instance_of: Lake
countries: Nigeria
coordinates: lat: 10.406111111111
lon: 4.5644444444444
Gruner received &quot;emeritus&quot; status in 1969, but held lectures at the Dresden University of Technology until 1978. He died in Dresden and his grave is located in the cemetery &quot;Waldfriedhof Weißer Hirsch&quot; in the eastern borough of Loschwitz above the right bank of the Elbe. Awards.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Research. Levesque uses both observations and modeling in her work. In the ultraviolet portion of the spectrum, she uses the Hubble Space Telescope to obtain spectra of star-forming galaxies. In the optical, she uses the Gemini and Keck observatories on Mauna Kea and the Las Campanas Observatories in Chile to study red supergiants in the Milky Way and in the Magellanic Clouds.

Geographic entities mentioned:
surface_form: Mauna Kea
instance_of: Mountain
countries: United States
coordinates: lat: 19.820555555555554
lon: -155.46805555555557
Course. Arroyo Trabuco begins in the Trabuco Ranger District of the Cleveland National Forest, just west of the Orange–Riverside County border, at an elevation of. The headwaters of the creek are in the large and deep Trabuco Canyon just north of Los Pinos Peak and south of Trabuco Peak.

Geographic entities mentioned:
surface_form: Los Pinos Peak
instance_of: Mountain
countries: United States
coordinates: lat: 33.6642
lon: -117.471
surface_form: Trabuco Peak
instance_of: Mountain
countries: United States
coordinates: lat: 33.7022
lon: -117.475
After entering the city limits of Rancho Santa Margarita, the creek flows southwest through the long, narrow wilderness preserve of O'Neill Regional Park. It crosses under California State Route 241, a toll road that follows the western foothills of the Santa Ana Mountains, and passes close to Lake Mission Viejo, a popular recreational lake in the city of Mission Viejo.

Geographic entities mentioned:
surface_form: Lake Mission Viejo
instance_of: Lake
countries: United States
coordinates: lat: 33.626666666667
lon: -117.64805555556
Although much of the Arroyo Trabuco watershed is bounded by the San Juan Creek basin it also borders on several other major Orange and Riverside County watersheds. Listed from east to west, the major San Juan Creek subwatersheds it bounds are Bell Canyon, Cañada Gobernadora, Cañada Chiquita and El Horno Creek.

Geographic entities mentioned:
surface_form: Bell Canyon
instance_of: Landform
countries: United States
coordinates: lat: 33.5342
lon: -117.555
Arroyo Trabuco's headwaters are actually not physically far from that of Bell Canyon and San Juan Creek, the first of which is the second longest tributary of San Juan Creek. On the west of the Arroyo Trabuco watershed is the Aliso Creek drainage basin, on the north the Santiago Creek, and on the northeast streams draining into the Lake Elsinore area.

Geographic entities mentioned:
surface_form: Lake Elsinore
instance_of: Lake
countries: United States
coordinates: lat: 33.660069444444
lon: -117.35183888889
The underlying rock of the Santa Ana foothills are Paleogene-age (66-2.59 MYA) sandstone. As the Santa Ana Mountains rose, Arroyo Trabuco first formed as a canyon cut into the southeastern part of the range. Many of the creeks draining the range—including Santiago Creek, San Diego Creek, Bell Canyon and San Juan Creek—first formed in the same way.

Geographic entities mentioned:
surface_form: Bell Canyon
instance_of: Landform
countries: United States
coordinates: lat: 33.5342
lon: -117.555
Hundålvatnet. Hundålvatnet is a lake that lies in Vefsn Municipality in Nordland county, Norway. The lake lies in the western part of the municipality, about west of the town of Mosjøen. It is located just north of the Lomsdal–Visten National Park. The lake flows into the Hundåla river which flows north into the Vefsnfjorden.

Geographic entities mentioned:
surface_form: hundålvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 65.815
lon: 12.938888888889
Bäderhorn. The Bäderhorn (2,009 m) is a mountain of the Bernese Alps, located north of the Jaun Pass in the canton of Bern. It lies on the range between the valleys of Jaun and Simmental.

Geographic entities mentioned:
surface_form: Simmental
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.55
lon: 7.36
Bäderhorn. The Bäderhorn (2,009 m) is a mountain of the Bernese Alps, located north of the Jaun Pass in the canton of Bern. It lies on the range between the valleys of Jaun and Simmental.

Geographic entities mentioned:
surface_form: bäderhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.61333333
lon: 7.3275
Rammuka, Pärnu County. Rammuka is a village in Pärnu urban municipality, Pärnu County, in southwestern Estonia. It has a population of 29 (as of 1 January 2011). Rammuka is bordered by Lake Ermistu to the east and Lake Tõhela to the northeast, Tõhela bog is located between the lakes.

Geographic entities mentioned:
surface_form: Lake Ermistu
instance_of: Lake
countries: Estonia
coordinates: lat: 58.36666667
lon: 23.975
surface_form: Lake Tõhela
instance_of: Lake
countries: Estonia
coordinates: lat: 58.41666667
lon: 23.99166667
The scene at Raisuli's headquarters was filmed at the castle of La Calahorra (Granada). The scene at Yellowstone National Park (where Roosevelt gives his famous grizzly bear speech) was filmed in the Meseta Central, north of Madrid. These latter two locations would each re-appear in Milius' 1982 film &quot;Conan the Barbarian&quot;.

Geographic entities mentioned:
surface_form: Meseta Central
instance_of: Plateau
countries: Spain
coordinates: lat: 40.5
lon: -3.5
Kima Rumi (Lima-Junín). Kima Rumi (Ancash Quechua &quot;kima&quot; three &quot;(kimsa)&quot;, Quechua &quot;rumi&quot; stone, &quot;three stones&quot;, also spelled &quot;Quimarumi&quot;) is a mountain in the Cordillera Central in the Andes of Peru which reaches a height of approximately.

Geographic entities mentioned:
surface_form: junín
instance_of: Lake
countries: Peru
coordinates: lat: -11.0201
lon: -76.1075
surface_form: kima rumi
instance_of: Mountain
countries: Peru
coordinates: lat: -12.02305556
lon: -75.82638889
Kima Rumi (Lima-Junín). Kima Rumi (Ancash Quechua &quot;kima&quot; three &quot;(kimsa)&quot;, Quechua &quot;rumi&quot; stone, &quot;three stones&quot;, also spelled &quot;Quimarumi&quot;) is a mountain in the Cordillera Central in the Andes of Peru which reaches a height of approximately.

Geographic entities mentioned:
surface_form: kima rumi
instance_of: Mountain
countries: Peru
coordinates: lat: -12.02305556
lon: -75.82638889
surface_form: quimarumi
instance_of: Mountain
countries: Peru
coordinates: lat: -9.47611
lon: -77.3558
Iskanderkul. Iskanderkul (;) is a mountain lake of glacial origin in Tajikistan's Sughd Province. It lies at an altitude of on the northern slopes of the Gissar Range in the Fann Mountains. Triangular in shape, it has a surface area of and is up to deep.

Geographic entities mentioned:
surface_form: iskanderkul
instance_of: Lake
countries: Tajikistan
coordinates: lat: 39.074444444444
lon: 68.368333333333
Triangular in shape, it has a surface area of and is up to deep. Formed by a landslide that blocks the Saratogh river, the outflow of the lake is called the Iskander Darya, which joins the Yaghnob River to form the Fan Darya, a major left tributary of the Zeravshan River. 134 km from Dushanbe and 23 km from the Dushanbe—Khujand road, Iskanderkul is a popular tourist destination.

Geographic entities mentioned:
surface_form: iskanderkul
instance_of: Lake
countries: Tajikistan
coordinates: lat: 39.074444444444
lon: 68.368333333333
In the colonial city, the road began at the Old State House, the government center of the 18th-century city. Once called Cornhill, Orange, and Newbury Street, it's now modern-day Washington Street, running southwards off the Boston Neck towards the village of Roxbury. Middle Post Road. The Middle Post Road was the shortest, fastest, and youngest portion of the route.

Geographic entities mentioned:
surface_form: Boston Neck
instance_of: Landform
countries: United States
coordinates: lat: 42.34394444
lon: -71.06597222
It was designed with themes from the local native populations and for a 100-year-plus life span. Elizabeth II, Queen of Canada, with her consort, Prince Philip, Duke of Edinburgh, opened the legislative building on 21 August 1994. Sited directly on the shore of Frame Lake, the structure is nestled between outcroppings of the Canadian Shield, a natural peat bog, and large stands of existing trees.

Geographic entities mentioned:
surface_form: Frame Lake
instance_of: Lake
countries: Canada
coordinates: lat: 62.454
lon: -114.39
Hwangaksan. Hwangaksan is a mountain of South Korea. It has an elevation of 1,111 metres.

Geographic entities mentioned:
surface_form: hwangaksan
instance_of: Mountain
countries: South Korea
coordinates: lat: 36.11916667
lon: 127.96611111
Description. Tikishla Peak is located east of Anchorage in the western Chugach Mountains, on land belonging to Fort Richardson Military Reservation. Precipitation runoff from the mountain drains west to Cook Inlet via Ship Creek and Campbell Creek. Although modest in elevation, relief is significant as the summit rises approximately 2,300 feet (700 m) above Campbell Creek Canyon in.

Geographic entities mentioned:
surface_form: cook
instance_of: Mountain
coordinates: lat: -67.91667
lon: 56.46667
surface_form: campbell
instance_of: Mountain
coordinates: lat: -84.91667
lon: -174
Tikishla Peak. Tikishla Peak is a mountain summit in the U.S. state of Alaska. Description. Tikishla Peak is located east of Anchorage in the western Chugach Mountains, on land belonging to Fort Richardson Military Reservation. Precipitation runoff from the mountain drains west to Cook Inlet via Ship Creek and Campbell Creek.

Geographic entities mentioned:
surface_form: tikishla peak
instance_of: Mountain
coordinates: lat: 61.144444444444446
lon: -149.55611111111114
Climate. Based on the Köppen climate classification, Tikishla Peak is located in a subarctic climate zone with long, cold, snowy winters, and mild summers. Weather systems coming off the Gulf of Alaska are forced upwards by the Chugach Mountains (orographic lift), causing heavy precipitation in the form of rainfall and snowfall.

Geographic entities mentioned:
surface_form: tikishla peak
instance_of: Mountain
coordinates: lat: 61.144444444444446
lon: -149.55611111111114
An ascent of the summit involves hiking 15 miles (round-trip) with 5,200 feet of elevation gain. The months of May through September offer best conditions for climbing the peak. The peak's toponym &quot;Tikishla&quot;, meaning &quot;black bear&quot;, is derived from the Denaʼina language and was proposed in 1965 by the Mountaineering Club of Alaska. Climate.

Geographic entities mentioned:
surface_form: best
instance_of: Mountain
coordinates: lat: -66.8167
lon: 51.3833
Precipitation runoff from the mountain drains west to Cook Inlet via Ship Creek and Campbell Creek. Although modest in elevation, relief is significant as the summit rises approximately 2,300 feet (700 m) above Campbell Creek Canyon in. An ascent of the summit involves hiking 15 miles (round-trip) with 5,200 feet of elevation gain.

Geographic entities mentioned:
surface_form: campbell
instance_of: Mountain
coordinates: lat: -84.91667
lon: -174
Nowadays, the Grand Canal d'Alsace on the French side of the border runs parallel to the Altrhein. Extension of the urban area. The urban area runs along the Altrhein and lies mostly on a part of the Rhine Plain with the Rheinwald and the. The district of Steinenstadt also contains a vineyard as exclave in the between the towns of Auggen and Schliengen.

Geographic entities mentioned:
surface_form: Rheinwald
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.551778
lon: 9.319788
Nkhotakota. Nkhotakota (Un-kho-tah-kho-tuh) (formerly Kota Kota) (name derived from the Chichewa for &quot;Corner Corner&quot;) is a town and one of the districts in the Central Region of Malawi. It is on the shore of Lake Malawi (formerly Lake Nyasa) and is one of the main ports on Lake Malawi. As of 2018, Nkhotakota had a population estimated at 28,350. The district had a population of 301,000.

Geographic entities mentioned:
surface_form: Lake Malawi
instance_of: Lake
countries: Malawi
Mozambique
Tanzania
coordinates: lat: -12.183333333333
lon: 34.366666666667
Lake of No Return. Lake of No Return, also referred to as Naung Yang in Tai languages, is a body of water in Myanmar, lying in the area of the Pangsau Pass (3727') on the India–Myanmar border south of Pangsau (also called &quot;Pansaung&quot;) village. The lake is 1.4 km in length and 0.8 km in width at its widest part.

Geographic entities mentioned:
surface_form: lake of no return
instance_of: Lake
countries: Myanmar
coordinates: lat: 27.219166666667
lon: 96.143861111111
American sources repeat that account, for instance in the 2008 book by Brendan I. Koerner, ', about the life of Herman Perry, a U.S.

Geographic entities mentioned:
surface_form: lake of no return
instance_of: Lake
countries: Myanmar
coordinates: lat: 27.219166666667
lon: 96.143861111111
The second has it that a group of Japanese soldiers returning from battle lost their way and ended up at the lake. There, they were stricken by malaria and died and hence it is called the Lake of No Return. According to a third story, US Army soldiers, working on the Ledo Road, were sent to examine the lake and got trapped by the undergrowth and perished trying to escape.

Geographic entities mentioned:
surface_form: lake of no return
instance_of: Lake
countries: Myanmar
coordinates: lat: 27.219166666667
lon: 96.143861111111
A fourth story says this &quot;is the 'lake of no return' [because] retreating British troops in 1942 got lost in quicksand.&quot; Adding myth to legend, one author claims he has encountered the name on a document written by one of the Ten Lost Tribes of Israel, which he claims still hides out in the area.

Geographic entities mentioned:
surface_form: lake of no return
instance_of: Lake
countries: Myanmar
coordinates: lat: 27.219166666667
lon: 96.143861111111
The lake still maintains its reputation; the Indian newspaper &quot;The Telegraph&quot; reported, in a story on the possible reopening of the Ledo Road in 2007, that &quot;close by [Pansaung] is the Lake of No Return — the local Bermuda Triangle.

Geographic entities mentioned:
surface_form: lake of no return
instance_of: Lake
countries: Myanmar
coordinates: lat: 27.219166666667
lon: 96.143861111111
According to folklore, aircraft that fly over the lake never return.&quot; The lake's reputation is advertised in hopes of making the area more attractive to tourists: &quot;Who knows, the ‘Indian’ Bermuda Triangle might just turn out to be the next tourist-puller of the region.&quot;
In a recent article Joydeep Sircar has claimed to have solved the 'mystery' behind the Lake of No Return, which he visited in 2002.

Geographic entities mentioned:
surface_form: lake of no return
instance_of: Lake
countries: Myanmar
coordinates: lat: 27.219166666667
lon: 96.143861111111
Chakima Creek. Chakima Creek is a tributary of Shaman Creek and part of the Stikine River watershed in northwest part of the province of British Columbia, Canada.

Geographic entities mentioned:
surface_form: Shaman Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.61636
lon: -130.40395
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: chakima creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.59966
lon: -130.42066
From its source in the mountains south of Mount Edziza, near Cartoona Peak and Tadeda Peak, it flows generally east for roughly to empty into Shaman Creek, which flows to Kakiddi Creek, a tributary of the Klastline River, which in turn is a tributary of the Stikine River. Chakima Creek's mean annual discharge is estimated at. Its watershed covers, and is mostly within Mount Edziza Provincial Park.

Geographic entities mentioned:
surface_form: Mount Edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: Cartoona Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6067
lon: -130.615
surface_form: Tadeda Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5422
lon: -130.616
surface_form: Kakiddi Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.872778
lon: -130.425556
surface_form: shaman creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.61636
lon: -130.40395
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Geography. Chakima Creek originates in the high peaks south of Mount Edziza, north of Tadeda Peak and south of Cartoona Peak. From its source about south of the summit of Mount Edziza, Chakima Creek flows generally east for about. It is joined by numerous unnamed tributaries which drain various mountains such as Esja Peak and Hoyaa Peak.

Geographic entities mentioned:
surface_form: Mount Edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: tadeda peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5422
lon: -130.616
surface_form: cartoona peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6067
lon: -130.615
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
It flows through the northern end Mowchilla Lake, then continues northeast through wetlands to empty into Shaman Creek. Mowchilla Lake and the various unnamed creeks that empty into it are part of Chakima Creek's watershed. Chakima Creek's watershed is part of the Mount Edziza volcanic complex. It is mostly within Mount Edziza Provincial Park. Chakima Creek itself is entirely within the park.

Geographic entities mentioned:
surface_form: Mount Edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Its watershed covers, and is mostly within Mount Edziza Provincial Park. The watershed's land cover is classified as 45.7% conifer forest, 26.6% shrubland, 14.0% barren, 9.6% herbaceous, and small amounts of other cover. The mouth of Chakima Creek is located about southeast of Telegraph Creek, British Columbia, about north of Bob Quinn Lake, British Columbia, and about east of Juneau, Alaska.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: chakima creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.59966
lon: -130.42066
It flows through the northern end Mowchilla Lake, then continues northeast through wetlands to empty into Shaman Creek. Mowchilla Lake and the various unnamed creeks that empty into it are part of Chakima Creek's watershed. Chakima Creek's watershed is part of the Mount Edziza volcanic complex. It is mostly within Mount Edziza Provincial Park. Chakima Creek itself is entirely within the park.

Geographic entities mentioned:
surface_form: chakima creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.59966
lon: -130.42066
surface_form: chakima creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.59966
lon: -130.42066
Chakima Creek. Chakima Creek is a tributary of Shaman Creek and part of the Stikine River watershed in northwest part of the province of British Columbia, Canada.

Geographic entities mentioned:
surface_form: chakima creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.59966
lon: -130.42066
From its source in the mountains south of Mount Edziza, near Cartoona Peak and Tadeda Peak, it flows generally east for roughly to empty into Shaman Creek, which flows to Kakiddi Creek, a tributary of the Klastline River, which in turn is a tributary of the Stikine River. Chakima Creek's mean annual discharge is estimated at. Its watershed covers, and is mostly within Mount Edziza Provincial Park.

Geographic entities mentioned:
surface_form: chakima creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.59966
lon: -130.42066
The mouth of Chakima Creek is located about southeast of Telegraph Creek, British Columbia, about north of Bob Quinn Lake, British Columbia, and about east of Juneau, Alaska. Chakima Creek is in Mount Edziza Provincial Park, which lies within the traditional territory of the Tahltan First Nation, of the Tahltan people.

Geographic entities mentioned:
surface_form: chakima creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.59966
lon: -130.42066
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Chakima Creek is in Mount Edziza Provincial Park, which lies within the traditional territory of the Tahltan First Nation, of the Tahltan people. The name &quot;Chakima&quot; was created from the Talhtan words &quot;cha&quot; &quot;beaver&quot; and &quot;kima&quot; &quot;house&quot;, referring to the maze of beaver dams and ponds in the area where Chakima Creek joins Shaman Creek. Geography.

Geographic entities mentioned:
surface_form: chakima creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.59966
lon: -130.42066
surface_form: chakima creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.59966
lon: -130.42066
surface_form: shaman creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.61636
lon: -130.40395
Geography. Chakima Creek originates in the high peaks south of Mount Edziza, north of Tadeda Peak and south of Cartoona Peak. From its source about south of the summit of Mount Edziza, Chakima Creek flows generally east for about. It is joined by numerous unnamed tributaries which drain various mountains such as Esja Peak and Hoyaa Peak.

Geographic entities mentioned:
surface_form: chakima creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.59966
lon: -130.42066
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Chakima Creek's watershed is part of the Mount Edziza volcanic complex. It is mostly within Mount Edziza Provincial Park. Chakima Creek itself is entirely within the park. Chakima Creek flows through Mowchilla Lake, and some of that lake's unnamed tributaries, which are part of Chakima Creek's watershed, drain areas to the south and east of Mowchilla Lake, outside of Mount Edziza Provincial Park.

Geographic entities mentioned:
surface_form: chakima creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.59966
lon: -130.42066
Chakima Creek's watershed is part of the Mount Edziza volcanic complex. It is mostly within Mount Edziza Provincial Park. Chakima Creek itself is entirely within the park. Chakima Creek flows through Mowchilla Lake, and some of that lake's unnamed tributaries, which are part of Chakima Creek's watershed, drain areas to the south and east of Mowchilla Lake, outside of Mount Edziza Provincial Park.

Geographic entities mentioned:
surface_form: chakima creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.59966
lon: -130.42066
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
In its lower reaches it makes a southward curve, coming close to Mowdade Lake, then bending northward into a large wetland area. It flows through the northern end Mowchilla Lake, then continues northeast through wetlands to empty into Shaman Creek. Mowchilla Lake and the various unnamed creeks that empty into it are part of Chakima Creek's watershed.

Geographic entities mentioned:
surface_form: shaman creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.61636
lon: -130.40395
Chakima Creek's mean annual discharge is estimated at. Its watershed covers, and is mostly within Mount Edziza Provincial Park. The watershed's land cover is classified as 45.7% conifer forest, 26.6% shrubland, 14.0% barren, 9.6% herbaceous, and small amounts of other cover.

Geographic entities mentioned:
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Mynydd Tarw. Mynydd Tarw () is a subsidiary summit of Cadair Berwyn in north east Wales. It used to have a top: Rhos which has now been deleted as a Nuttall. The summit has a large shelter cairn. The views are extensive, with the lower; northern and western Berwyns visible, including Pen Bwlch Llandrillo. Cadair Berwyn, Godor, Moel yr Ewig and Foel Wen are also in view.

Geographic entities mentioned:
surface_form: Cadair Berwyn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.8806
lon: -3.38099
surface_form: mynydd tarw
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.8821
lon: -3.32005