Sarmila/GeoWiki-Features huggingface dataset:
This irked Ahmad Shah and he attacked Sorath. Ahmad Shah won pitched battle at Vanthali in 1413. Later he imposed siege of Junagadh in 1414. Meliga retired to the hill fortress of Girnar. Ahmad Shah, though unable to capture the hill, gained the fortified citadel of Junagaḍh. Finding further resistance vain, the chief tendered his submission, and Junagaḍh was admitted among the tributary states.

Geographic entities mentioned:
surface_form: Girnar
instance_of: Mountain
countries: India
coordinates: lat: 21.516962
lon: 70.53154
state of Michigan. The population was 1,370 at the 2020 census. The village of Three Oaks is located in the southwest corner of Michigan, just 5 miles from the shores of Lake Michigan and within 2 miles of the Indiana border along US 12. History. The village was first settled by Henry Chamberlain in 1850 and became a village in 1867.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
General information. Historically, the district was the location of the temple complex of Pachacámac. The district was created on January 2, 1857, and since then it has been an agricultural district as it is located in the center of the Lurín River valley.

Geographic entities mentioned:
surface_form: Lurín River
instance_of: Watercourse
countries: Peru
coordinates: lat: -12.272369
lon: -76.904984
Soldiers Farewell Hill. Soldiers Farewell Hill, a summit at an elevation of 6135 feet, in the Big Burro Mountains, in Grant County, New Mexico. History. Soldiers Farewell Hill lies south of the Burro Cienega.

Geographic entities mentioned:
surface_form: soldiers farewell hill
instance_of: Mountain
countries: United States
coordinates: lat: 32.356388888889
lon: -108.33
Soldiers Farewell Hill, a summit at an elevation of 6135 feet, in the Big Burro Mountains, in Grant County, New Mexico. History. Soldiers Farewell Hill lies south of the Burro Cienega. It marked the site of Ojo Ynez, a watering place nearby the old road between Janos, Chihuahua and the Santa Rita copper mines, later used by Cooke's Wagon Road and the San Antonio-San Diego Mail Line.

Geographic entities mentioned:
surface_form: soldiers farewell hill
instance_of: Mountain
countries: United States
coordinates: lat: 32.356388888889
lon: -108.33
Settlements in Utah, south of the Wasatch Front, stretched from St. George in the southwest to Nephi in the northeast, including the Sevier River valley. The corridor is roughly congruent with the area between present-day Interstate 15 and U.S. Route 89. Outside of the Wasatch Front, and Utah's Cache Valley, most of the population of the state resides in this corridor. History.

Geographic entities mentioned:
surface_form: Cache Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.816666666667
lon: -111.93416666667
Arrington asserted that within ten years of the LDS arrival in the Salt Lake Valley, &quot;...nearly 100 colonies had been planted; by 1867, more than 200; and by the time of (Young's) death in 1877, nearly 400 colonies.&quot; These colonies had four distinct purposes: &quot;...first, settlements intended to be temporary places of gathering and recruitment, such as Carson Valley in Nevada; second, colonies to serve as centers for production, such as iron at Cedar City, cotton at St.

Geographic entities mentioned:
surface_form: Salt Lake Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.6839
lon: -111.978
Interior Minister 1993–1996. In 1988, Babar was a Special Assistant to the Prime Minister, Benazir Bhutto and successfully ran the election for Begum Nusrat Bhutto from Chitral during the preceding elections.

Geographic entities mentioned:
surface_form: Chitral
instance_of: Valley
countries: Pakistan
coordinates: lat: 35.85111111111111
lon: 71.78888888888889
La Barranca de San Jerónimo. La Barranca de San Jerónimo, also known simply as La Barranca, is a cliff situated 1 mile northwest of the town of San Jerónimo, Jalisco, Mexico. Although the town adjacent to the cliff is located in the municipality of San Martín de Hidalgo, the Barranca lies within the neighboring municipality of Ameca.

Geographic entities mentioned:
surface_form: la barranca de san jerónimo
instance_of: Mountain
countries: Mexico
Geography. According to the United States Census Bureau, the town has a total area of, of which, of it is land and of it (16.31%) is water. The south town line borders Schuyler County, New York, to the southwest and Tompkins County to the southeast and the east town line is defined by Cayuga Lake, one of the Finger Lakes. The town of Lodi is to the west and the town of Ovid is to the north.

Geographic entities mentioned:
surface_form: Cayuga Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.68805555555556
lon: -76.70222222222222
surface_form: Finger Lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 42.666666666667
lon: -76.833333333333
In 1889 members of the Balsam Lake Club built the Catskills' first fire tower on the summit of Balsam Lake Mountain; twenty years later, after the fires two drought-plagued summers had taken a heavy toll on the forests, the state's Forest, Fish and Game Commission (FFGC) took it over as part of a new strategy, proven successful in Maine.

Geographic entities mentioned:
surface_form: Balsam Lake Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.0457
lon: -74.5945
The cab is equipped with paper cutouts identifying the mountains and other landmarks visible within the area of the tower on clear days. This 360-degree panorama is dominated by Peekamoose and Table mountains, southernmost of the Catskill High Peaks, and other features of the Slide Mountain Wilderness Area to the north.

Geographic entities mentioned:
surface_form: Peekamoose
instance_of: Mountain
countries: United States
coordinates: lat: 41.953
lon: -74.3982
This 360-degree panorama is dominated by Peekamoose and Table mountains, southernmost of the Catskill High Peaks, and other features of the Slide Mountain Wilderness Area to the north. To the southeast the view takes in the Shawangunk Ridge and the Hudson Valley beyond. It is possible to see the river itself, as well as New Jersey's highest mountain, High Point, when visibility is at its maximum.

Geographic entities mentioned:
surface_form: Hudson Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.9209
lon: -73.9613
West Paradise. West Paradise is a community in the Canadian province of Nova Scotia, located in Annapolis County. It is located in the Annapolis Valley along Nova Scotia Route 201 across the Annapolis River from Paradise. The Evergreen United Baptist Church is a municipally designated heritage building.

Geographic entities mentioned:
surface_form: Annapolis Valley
instance_of: Valley
countries: Canada
coordinates: lat: 44.979166666666664
lon: -64.89222222222222
When Fanny died in Santa Barbara, California, Field described her as &quot;the only woman in the world worth dying for.&quot; Soon after, he married her daughter Isobel Osbourne. In 1915, Fanny's ashes were taken by her daughter to Samoa where they were interred next to Stevenson on top of Mount Vaea. The bronze plaque for Fanny bears her Samoan name 'Aolele' (&quot;Flying Cloud&quot; in Samoan).

Geographic entities mentioned:
surface_form: Mount Vaea
instance_of: Mountain
countries: Samoa
coordinates: lat: -13.86666667
lon: -171.76666667
The Tanggula settlement, also known as Marquwo, Tuotuoheyan, or Togtogquwo, is located at above sea level in the central part of Tanggula Mountains, as the town's name indicates. The town's area includes the Geladaindong Peak, a mountain which stands at in elevation.

Geographic entities mentioned:
surface_form: Geladaindong Peak
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 33.495833333333
lon: 91.1675
Accident. The aircraft was on a flight from AFB Waterkloof to Mthatha Airport when it crashed near Giant's Castle in the Drakensberg, killing all eleven people on board. Shortly before the crash at 09:45 hours South African Standard Time (07:45 UTC), the crew reported that they were flying on instruments at in instrument meteorological conditions.

Geographic entities mentioned:
surface_form: Giant's Castle
instance_of: Mountain
countries: South Africa
coordinates: lat: -29.34608
lon: 29.48364
Geography. Tatasi is located on the Bolivian Altiplano, in the northern foothills of the Cordillera de Lípez. The climate of the region is arid and has a clear time of day, in which the average daily temperature fluctuations are stronger than the temperature fluctuations over the course of the year. The terrain around Tatasi is mainly hilly, but to the northeast it is flat.

Geographic entities mentioned:
surface_form: Altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
List of Northern Cordilleran volcanoes. The geography of northwestern British Columbia and Yukon, Canada is dominated by volcanoes of the Northern Cordilleran Volcanic Province formed due to continental rifting of the North American Plate. It is the most active volcanic region in Canada.

Geographic entities mentioned:
surface_form: Northern Cordilleran Volcanic Province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
Some of the volcanoes are notable for their eruptions, for instance, Tseax Cone for its catastrophic eruption estimated to have occurred in the 18th century which was responsible for the death of at least 2,000 Nisga'a people from poisonous volcanic gases, the Mount Edziza volcanic complex for at least 20 eruptions throughout the past 10,000 years, and The Volcano (also known as Lava Fork volcano) for the most recent eruption in Canada during 1904.

Geographic entities mentioned:
surface_form: Tseax Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 55.1108
lon: -128.899
surface_form: Mount Edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
Yukon. The central portion of the Northern Cordilleran Volcanic Province extends through Yukon where very few Northern Cordilleran volcanoes exist. Near the junction of the Yukon and Pelly rivers in central Yukon lies the Fort Selkirk Volcanic Field. It is the northernmost Holocene age volcanic field in Canada, consisting of a sequence of valley-filling basalt and basanite lava flows.

Geographic entities mentioned:
surface_form: Fort Selkirk Volcanic Field
instance_of: Mountain
countries: Canada
coordinates: lat: 62.93
lon: -137.38
British Columbia. Over half of the Northern Cordilleran volcanoes are located in northwestern British Columbia. This portion is where the most recent eruptions in Canada and of the Northern Cordilleran Volcanic Province have occurred, including the catastrophic 18th century eruption of Tseax Cone and the 1904 eruption of The Volcano.

Geographic entities mentioned:
surface_form: Tseax Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 55.1108
lon: -128.899
Assembly plants were transferred to underground factories that had been built in a massive hollow cave complex in the Harz mountains in Germany. The research, development, and design (codenamed &quot;Project Cement&quot;) were handled by secret offices in Ebensee, near the banks of Lake Traunsee in Austria.

Geographic entities mentioned:
surface_form: Lake Traunsee
instance_of: Lake
countries: Austria
coordinates: lat: 47.866666666667
lon: 13.8
The play was performed by &quot;Theatro Erevnas&quot; of Dimitris Potamitis at the Mount Lycabettus theatre in Athens and later broadcast by the Greek national television ERT on 12 November 1979.

Geographic entities mentioned:
surface_form: Mount Lycabettus
instance_of: Mountain
countries: Greece
coordinates: lat: 37.981944444444
lon: 23.743055555556
Xiao arrives at Nana's home and awkwardly meets Haofeng, then offers to show him around again. The three visit a bookstore, where Haofeng gets intrigued by depictions of the Changbai Mountains and Heaven Lake, while Nana lingers on a book about figure skating. Later at a nightclub, Haofeng tells Xiao and Nana to go dance as he stays in his seat and cries alone.

Geographic entities mentioned:
surface_form: Heaven Lake
instance_of: Lake
countries: People's Republic of China
North Korea
coordinates: lat: 42.006
lon: 128.057
Completed in May, 2003, the wave is constructed using 650 unique pieces of antique Chinese granite laid on a substrate of closed-cell foam and mortar. At once echoing the surging of waves and the volcanic core of Mount Rainier, the sculpture presents a zone of visual serenity among the museum's galleries.

Geographic entities mentioned:
surface_form: Mount Rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
Pipe Peak. Pipe Peak () is a sharp peak on a ridge, 1,720 m, rising 1.5 nautical miles (2.8 km) north of Matney Peak in the Founders Peaks, Heritage Range. It was named so by members of the University of Minnesota Geological Party of 1963–64 because a pipe was left here after a visit to the area.

Geographic entities mentioned:
surface_form: Matney Peak
instance_of: Mountain
coordinates: lat: -79.166666666667
lon: -86.233333333333
surface_form: Founders Peaks
instance_of: Mountain
coordinates: lat: -79.1667
lon: -86.25
surface_form: pipe peak
instance_of: Mountain
coordinates: lat: -79.15
lon: -86.25
Pipe Peak. Pipe Peak () is a sharp peak on a ridge, 1,720 m, rising 1.5 nautical miles (2.8 km) north of Matney Peak in the Founders Peaks, Heritage Range. It was named so by members of the University of Minnesota Geological Party of 1963–64 because a pipe was left here after a visit to the area.

Geographic entities mentioned:
surface_form: pipe peak
instance_of: Mountain
coordinates: lat: -79.15
lon: -86.25
According to the 2020 census, it has a population of 28,023 people. Etymology. Bayang is one the 15 original royal sultanates of Lanao, most documented royal sultanate of West Unayan, founded by Imam Diwan of Unayan, when he chose lakeside for the religious purposes and called it &quot;Bayang&quot;, a Malay term which means &quot;shadow&quot;, Bayang is a reflection of his image as religious man.

Geographic entities mentioned:
surface_form: lakeside
instance_of: Lake
countries: Philippines
coordinates: lat: 7.88
lon: 124.2525
The American troops, three infantry battalions and a battery of artillery total to some 1200 men, were led to Bayang by colonel Frank Baldwin to demand the extradition of the Moros responsible for the ambushing and killing of two American soldiers at the construction of a road from Iligan to Lake Lanao, two months earlier.

Geographic entities mentioned:
surface_form: Lake Lanao
instance_of: Lake
countries: Philippines
coordinates: lat: 7.88
lon: 124.2525
The Municipality of Bayang is located about 61 km. south of Marawi City. It has an area of 7,850 hectares. It lays 124’15’00 and about ‘45’00 latitude. It is bounded on the north and east by Lake Lanao, on the west by the municipality of Binidayan and on the south by the municipality of Lumbatan. Topography. The topography of the municipality is generally
characterized by moderately sloping lands.

Geographic entities mentioned:
surface_form: Lake Lanao
instance_of: Lake
countries: Philippines
coordinates: lat: 7.88
lon: 124.2525
Two accounts of his death are incompatible. One report has him being injured in the war and killed in the San Joaquin Valley in April 1863. This seems unlikely since it was prior to the McLaughlin Campaign, when Joaquin Jim was still leading a band in the upper valley.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
He was the first chairman and CEO of the new Norfolk Southern, and is credited with locating the headquarters of the Fortune 500 company in Norfolk, Virginia, within sight of the massive coal pier at Lambert's Point on the Elizabeth River at Hampton Roads. Robert B.

Geographic entities mentioned:
surface_form: Lambert's Point
instance_of: Landform
countries: United States
coordinates: lat: 36.87468
lon: -76.32348
Igopogo. In Canadian folklore, the Igopogo is a mythical creature said to dwell in Lake Simcoe, Ontario. The creature's name is ostensibly based on the Ogopogo, of Lake Okanagan, British Columbia, and also the title of the 1952 book &quot;I Go Pogo&quot;, a slogan often mentioned in the comic.

Geographic entities mentioned:
surface_form: Lake Simcoe
instance_of: Lake
countries: Canada
coordinates: lat: 44.436666666667
lon: -79.339166666667
Route. At its northern end New England Highway connects to D'Aguilar Highway, and at its southern end it connects to Pacific Highway. It traverses the Darling Downs, New England, and Hunter Valley regions. During the winter months, some parts of the New England Highway are subject to frost and snowfall, with the 350 km section from the Moonbi Ranges to Stanthorpe located at high altitudes.

Geographic entities mentioned:
surface_form: Hunter Valley
instance_of: Valley
countries: Australia
coordinates: lat: -32.56
lon: 151.17083333333332
Operations. In Dec 2016 INS &quot;Bangaram&quot; was operationally deployed in the rescue of 800 tourist alongside, and LCU 38 from the Havelock Island and ferried them to Port Blair as a result of severe cyclonic storm in the Bay of Bengal. In Mar 2017 the warship alongside INS Karmuk (P64) visited Yangon in Myanmar to take part in the 5th Indo-Myanmar coordinated patrol CORPAT.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Three of these pools: Fens Pool, Middle Pool and Grove Pool are grouped together in the north eastern part of the reserve. These pools form the Fens Pools site of Special Scientific Interest. The other large pool in the reserve, Foot's Hole, lies to the south west of this group, separated by the Dell Stadium (a sports ground owned by Dudley Council).

Geographic entities mentioned:
surface_form: Fens Pools site of Special Scientific Interest
instance_of: Group of lakes
countries: United Kingdom
coordinates: lat: 52.4953
lon: -2.11926
Fords Hill. Fords Hill is a mountain located in the Catskill Mountains of New York southeast of Bovina Center. Fords Hill is located south of Mount Pisgah.

Geographic entities mentioned:
surface_form: mount pisgah
instance_of: Mountain
countries: United States
coordinates: lat: 44.306111111111
lon: -70.023888888889
surface_form: mount pisgah
instance_of: Mountain
countries: United States
coordinates: lat: 42.377222222222
lon: -74.245
surface_form: mount pisgah
instance_of: Mountain
countries: United States
coordinates: lat: 42.3653
lon: -71.6578
surface_form: mount pisgah
instance_of: Mountain
countries: United States
coordinates: lat: 44.7297
lon: -72.0308
surface_form: fords hill
instance_of: Mountain
countries: United States
coordinates: lat: 42.17425
lon: -74.74294
surface_form: mount pisgah
instance_of: Mountain
countries: United States
coordinates: lat: 41.8098
lon: -76.7159
surface_form: mount pisgah
instance_of: Mountain
countries: United States
coordinates: lat: 35.4255
lon: -82.7569
surface_form: mount pisgah
instance_of: Mountain
countries: United States
coordinates: lat: 40.86944444444445
lon: -75.74972222222222
surface_form: mount pisgah
instance_of: Mountain
countries: United States
coordinates: lat: 44.340833333333
lon: -74.128055555556
surface_form: mount pisgah
instance_of: Mountain
countries: United States
coordinates: lat: 39.996388888889
lon: -76.548888888889
surface_form: mount pisgah
instance_of: Mountain
countries: United States
coordinates: lat: 42.221111111111
lon: -74.735833333333
Fords Hill. Fords Hill is a mountain located in the Catskill Mountains of New York southeast of Bovina Center. Fords Hill is located south of Mount Pisgah.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: fords hill
instance_of: Mountain
countries: United States
coordinates: lat: 42.17425
lon: -74.74294
Fords Hill. Fords Hill is a mountain located in the Catskill Mountains of New York southeast of Bovina Center. Fords Hill is located south of Mount Pisgah.

Geographic entities mentioned:
surface_form: fords hill
instance_of: Mountain
countries: United States
coordinates: lat: 42.17425
lon: -74.74294
It depicts a number of real historical events such as the Peterloo Massacre. Plot. An orphaned child is rescued by a tanner and his daughter from the River Irk during a storm. Simon, the tanner learns that the child's family did not survive the flood and Bess, his daughter, decides to foster the child herself.

Geographic entities mentioned:
surface_form: River Irk
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 53.4869
lon: -2.24504
Mount Grosvenor. Mount Grosvenor is a elevation glaciated summit located west of Valdez in the Chugach Mountains of the U.S. state of Alaska, on land managed by Chugach National Forest. Although modest in elevation, relief is significant since the mountain rises from tidewater at Unakwik Inlet of Prince William Sound in approximately three miles.

Geographic entities mentioned:
surface_form: mount grosvenor
instance_of: Mountain
countries: United States
coordinates: lat: 62.886944444444445
lon: -150.70638888888888
surface_form: mount grosvenor
instance_of: Mountain
countries: United States
coordinates: lat: 61.1836
lon: -147.43
Climate. Based on the Köppen climate classification, Mount Grosvenor 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: mount grosvenor
instance_of: Mountain
countries: United States
coordinates: lat: 62.886944444444445
lon: -150.70638888888888
surface_form: mount grosvenor
instance_of: Mountain
countries: United States
coordinates: lat: 61.1836
lon: -147.43
Since that date, the western edge of North America has grown westward as a succession of island arcs and assorted ocean-floor rocks have been added along the continental margin. There are at least five geologic provinces in the area: the Cascade Volcanoes, the Columbia Plateau, the North Cascades, the Coast Mountains, and the Insular Mountains.

Geographic entities mentioned:
surface_form: Columbia Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 45.999444444444
lon: -119.00138888889
Within this region, nearly 20 major volcanic centers lie in sequence. Although the largest volcanoes like Mount St. Helens get the most attention, the Cascade Volcanic Arc includes a band of thousands of very small, short-lived volcanoes that have built a platform of lava and volcanic debris. Rising above this volcanic platform are a few strikingly large volcanoes that dominate the landscape.

Geographic entities mentioned:
surface_form: Mount St. Helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
As long as subduction continues, new Cascade volcanoes will continue to rise. Volcanism outside the Cascades. The Garibaldi Volcanic Belt in southwestern British Columbia is the northern extension of the Cascade Volcanic Arc in the United States and contains the most explosive young volcanoes in Canada. Like the rest of the arc, it has its origins in the Cascadia subduction zone.

Geographic entities mentioned:
surface_form: Garibaldi Volcanic Belt
instance_of: Mountain
countries: Canada
coordinates: lat: 51.5283
lon: -126.113
Helens. Ash from this eruption can be traced eastward to western Alberta. It is also the most unstable volcanic massif in Canada, which has dumped clay and rock several meters (yards) deep into the Pemberton Valley at least three times during the past 7,300 years. Hot springs near the Mount Cayley and Mount Meager massifs suggest that magmatic heat is still present.

Geographic entities mentioned:
surface_form: Pemberton Valley
instance_of: Valley
countries: Canada
coordinates: lat: 50.5
lon: -123
A few isolated volcanic centers northwest of the Mount Meager massif such as the Franklin Glacier Complex and the Silverthrone Caldera, which lie in the Pemberton Volcanic Belt, may also be the product of Cascadia subduction, but geologic investigations have been very limited in this remote region.

Geographic entities mentioned:
surface_form: Franklin Glacier Complex
instance_of: Mountain
countries: Canada
coordinates: lat: 51.3333
lon: -125.4
surface_form: Silverthrone Caldera
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4333
lon: -126.3
surface_form: Pemberton Volcanic Belt
instance_of: Mountain
countries: Canada
coordinates: lat: 50.58051944
lon: -122.93235278
However, the Pemberton Volcanic Belt is usually merged with the Garibaldi Volcanic Belt, making Mount Silverthrone the northernmost, but an uncertain Cascadia subduction-related volcano. The most active volcanic region of the northern Pacific Northwest is called the Northern Cordilleran Volcanic Province (sometimes called the Stikine Volcanic Belt).

Geographic entities mentioned:
surface_form: Northern Cordilleran Volcanic Province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
The broad dissected summit region consists of trachytic and rhyolitic lava domes and was considered to be dotted with several minor basaltic vents of postglacial age, although considered Holocene activity to be uncertain. The Mount Edziza volcanic complex is perhaps the most spectacular volcanic edifice in British Columbia.

Geographic entities mentioned:
surface_form: Mount Edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
The Mount Edziza volcanic complex is perhaps the most spectacular volcanic edifice in British Columbia. It is the second largest persistent eruptive center within the Northern Cordilleran Volcanic Province and is flanked with numerous young satellite cones, including the young, well-preserved Eve Cone.

Geographic entities mentioned:
surface_form: Eve Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.81305555555556
lon: -130.67555555555555
There are some indications that Level Mountain and Mount Edziza volcanic complex may be between 11 and 9 million years old. The Anahim Volcanic Belt is a volcanic belt that stretches from just north of Vancouver Island to near Quesnel.

Geographic entities mentioned:
surface_form: Anahim Volcanic Belt
instance_of: Mountain
countries: Canada
coordinates: lat: 52.666666666666664
lon: -125.83333333333333
The Anahim Volcanic Belt is a volcanic belt that stretches from just north of Vancouver Island to near Quesnel. It is thought to have formed as a result of the North American Plate moving over a stationary hotspot, similar to the hotspot feeding the Hawaiian Islands, called the Anahim hotspot. The youngest volcano within the volcanic belt is Nazko Cone.

Geographic entities mentioned:
surface_form: Nazko Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 52.9272
lon: -123.734
It is within the Wells Gray Provincial Park, which also includes the -high Helmcken Falls. The origin of the volcanism is unknown, but is probably related to crustal thinning. Some of the lava flows in the field are similar to those that erupted at Volcano Mountain in the Yukon, where olivine nephelinite occurs. The last eruption in the field was about 400 years ago at Kostal Cone.

Geographic entities mentioned:
surface_form: Volcano Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 62.93
lon: -137.38
The origin of the volcanism is unknown, but is probably related to crustal thinning. Some of the lava flows in the field are similar to those that erupted at Volcano Mountain in the Yukon, where olivine nephelinite occurs. The last eruption in the field was about 400 years ago at Kostal Cone. Numerous seamounts lie off British Columbia's coast and are related to hotspot volcanism.

Geographic entities mentioned:
surface_form: Kostal Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1667
lon: -119.95
The Bowie Seamount is also the youngest seamount in the Kodiak-Bowie Seamount chain. Volcanic disasters. The last eruption of the Tseax Cone around the years 1750 or 1775 is Canada's worst known geophysical disaster. The eruption produced a long lava flow, destroying the Nisga'a villages and the death of at least 2000 Nisga'a people by volcanic gases and poisonous smoke.

Geographic entities mentioned:
surface_form: Tseax Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 55.1108
lon: -128.899
In addition, eleven volcanoes in Canada have had seismic activity since 1975, including: the Silverthrone Caldera, Mount Meager massif, Wells Gray-Clearwater volcanic field, Mount Garibaldi, Mount Cayley, Castle Rock, The Volcano, Mount Edziza volcanic complex, Hoodoo Mountain, Crow Lagoon and Nazko Cone. Columbia Plateau.

Geographic entities mentioned:
surface_form: Silverthrone Caldera
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4333
lon: -126.3
surface_form: Mount Garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
surface_form: Mount Edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
surface_form: Hoodoo Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 56.772222222222
lon: -131.29444444444
surface_form: Nazko Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 52.9272
lon: -123.734
The ice blocked the Clark Fork River, forming the huge Glacial Lake Missoula. The lake measured about and contained about, half the volume of Lake Michigan. Glacial Lake Missoula broke through the ice dam many times, allowing a tremendous volume of water to rush across northern Idaho and into eastern Washington.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Such catastrophic floods raced across the southward-dipping plateau a number of times, etching the coulees which characterize this region, now known as the channeled scablands. As the floods in this vicinity raced southward, two major cascades formed along their course. The larger cataract was that of the upper Grand Coulee, where the river roared over an waterfall.

Geographic entities mentioned:
surface_form: Grand Coulee
instance_of: Valley
countries: United States
coordinates: lat: 47.62
lon: -119.308
Volcanoes erupted to cover the older rocks with lava and ash. Large masses of molten rock invaded the older rocks from below. The volcanic arc is still active today, decorating the skyline with the cones of Mount Baker and Glacier Peak. The deep canyons and sharp peaks of today's North Cascades scene are products of profound erosion.

Geographic entities mentioned:
surface_form: Mount Baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: Glacier Peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.11194444444445
lon: -121.11416666666666
The plutonic complex is built on unusual island arc fragments, oceanic plateaus and continental margin assemblages accreted between the Triassic and the Cretaceous periods. In addition, the Garibaldi, Meager, Cayley and Silverthrone areas are of recent volcanic origin. The Coast Mountains consist of a single uplifted mass.

Geographic entities mentioned:
surface_form: Garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
surface_form: Silverthrone
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4333
lon: -126.3
The mountains flanking the Homathko River are the highest in the Coast Mountains, and include Mount Waddington west of the river in the Waddington Range and Mount Queen Bess east of the river, adjacent to the Homathko Icefield. The Pacific Ranges in southwestern British Columbia are the southernmost subdivision of the Coast Mountains.

Geographic entities mentioned:
surface_form: Mount Waddington
instance_of: Mountain
countries: Canada
coordinates: lat: 51.373611111111
lon: -125.26333333333
surface_form: Mount Queen Bess
instance_of: Mountain
countries: Canada
coordinates: lat: 51.2717
lon: -124.568
Mühlsee. The Mühlsee, or Lake Mills, is a lake in Lans, Tyrol. It had an inflow and outflow, but they were buried in 2005. Nowadays, the lake is without fresh water. In 1840, the lake was drained. It was allowed to refill after a fire in 1902. The lake is mainly used for fish breeding; bathing is prohibited due to the small size. Sometimes the lake is plagued by algae.

Geographic entities mentioned:
surface_form: mühlsee
instance_of: Lake
countries: Austria
coordinates: lat: 47.243055555556
lon: 11.428611111111
He was born in Stavanger to pharmacist Henrik Bernhard Pedersen and Tyri Josefine Pedersen. He graduated as a jurist in 1941 and was first assigned a position in Torridal. In January 1942 he was appointed acting district sheriff in Avaldsnes and mayor of Kopervik and Stangaland.

Geographic entities mentioned:
surface_form: Torridal
instance_of: Valley
countries: Norway
coordinates: lat: 58.204625
lon: 7.92921111
Georgia's main role in the world mineral supply was to serve as a transport route for oil and gas shipments out of the Caspian region to world markets. Three of the new large oil and gas export pipelines that had been or were being constructed in the Caspian region pass through Georgia.

Geographic entities mentioned:
surface_form: Caspian
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
Seat Sandal. Seat Sandal is a fell in the English Lake District, situated four kilometres (miles) north of the village of Grasmere from where it is very well seen. Nevertheless, it tends to be overshadowed by its higher neighbours in the Eastern Fells, Helvellyn and Fairfield. Topography.

Geographic entities mentioned:
surface_form: Helvellyn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.527230555556
lon: -3.0160527777778
surface_form: fairfield
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4969
lon: -2.99059
Seat Sandal is distinctive in that its drainage reaches the sea at more widely spread points than any other Lakeland Fell, with Raise Beck going through Thirlmere and Derwent Water to reach the Irish Sea at Workington, Tongue Beck going through the lakes of Grasmere and Windermere to reach Morecambe Bay and Grisedale Beck draining into Ullswater and then to the sea at the Solway Firth.

Geographic entities mentioned:
surface_form: Windermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.358333333333
lon: -2.9361111111111
surface_form: grisedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.333333333333
lon: -2.35
surface_form: derwent water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.583333333333
lon: -3.15
surface_form: grasmere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.449383
lon: -3.021239
surface_form: seat sandal
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.494561111111
lon: -3.01585
However, this is true only as a result of the diversion of Raise Beck north to feed Thirlmere Reservoir — before this (and still today when there is enough water in Raise Beck for it to flow both north and south), Dollywaggon Pike shared in this distinction — Birkside Gill feeding Thirlmere, Raise Beck feeding Grasmere, and Grisedale Beck feeding Ullswater.

Geographic entities mentioned:
surface_form: Dollywaggon Pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.508069444444
lon: -3.0115611111111
surface_form: grisedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.333333333333
lon: -2.35
surface_form: grasmere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.449383
lon: -3.021239
The fell's main topographic attraction is Gavel Crag on its eastern side, which is connected to the main body of the fell by a fine rock arête. Dunmail Raise provides the topographical connection between the Eastern and Central Fells, Steel Fell rising on the other side of the pass. Geology.

Geographic entities mentioned:
surface_form: Steel Fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4915
lon: -3.05283
Topography. The fell's western flanks above Dunmail Raise are grassy and smooth while its eastern slopes are steep and craggy as they fall away towards Grisedale Hause which at contains Lakeland's highest substantial tarn, Grisedale Tarn. The fell reaches a height of and just scrapes into the list of Marilyns by being given prominence of ‘around’ 150 metres from the higher fell of Fairfield.

Geographic entities mentioned:
surface_form: grisedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.333333333333
lon: -2.35
surface_form: grisedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.333333333333
lon: -2.35
surface_form: grisedale tarn
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.5
lon: -3.0083333333333
The fell reaches a height of and just scrapes into the list of Marilyns by being given prominence of ‘around’ 150 metres from the higher fell of Fairfield. However, this must be regarded as a borderline case as there is no Ordnance Survey surveyed height for the top of Grisedale Hause.

Geographic entities mentioned:
surface_form: grisedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.333333333333
lon: -2.35
The Grasmere or Patterdale starts use the old packhorse route that links the two places; this is now part of Wainwright's Coast to Coast Walk. When Grisedale Hause is reached, it is a steep climb to the summit following a broken wall. The ascent from Dunmail Raise follows the bed of Raise Beck until it peters out at a height of; it is then a walk south up easy slopes to reach the summit.

Geographic entities mentioned:
surface_form: grisedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.333333333333
lon: -2.35
There is also a direct ascent up the western slopes starting at Mill Bridge. Summit. The view from the top is limited by the nearby Helvellyn and Fairfield ranges, although there is a good view of the fells to the west; the Solway Firth and Criffel are seen on a clear day, as is Morecambe Bay to the south.

Geographic entities mentioned:
surface_form: helvellyn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.527230555556
lon: -3.0160527777778
surface_form: fairfield
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4969
lon: -2.99059
Topography. The fell's western flanks above Dunmail Raise are grassy and smooth while its eastern slopes are steep and craggy as they fall away towards Grisedale Hause which at contains Lakeland's highest substantial tarn, Grisedale Tarn. The fell reaches a height of and just scrapes into the list of Marilyns by being given prominence of ‘around’ 150 metres from the higher fell of Fairfield.

Geographic entities mentioned:
surface_form: fairfield
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4969
lon: -2.99059
Seat Sandal. Seat Sandal is a fell in the English Lake District, situated four kilometres (miles) north of the village of Grasmere from where it is very well seen. Nevertheless, it tends to be overshadowed by its higher neighbours in the Eastern Fells, Helvellyn and Fairfield. Topography.

Geographic entities mentioned:
surface_form: grasmere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.449383
lon: -3.021239
surface_form: seat sandal
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.494561111111
lon: -3.01585
Geology. A hill of andesite lava forms the summit, the rocks beneath being the dacitic lapilli-tuffs of the Lincomb Tarns Formation. Ascents. The fell can be ascended from Grasmere or Dunmail Raise although a start from Patterdale is quite feasible. The Grasmere or Patterdale starts use the old packhorse route that links the two places; this is now part of Wainwright's Coast to Coast Walk.

Geographic entities mentioned:
surface_form: grasmere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.449383
lon: -3.021239
Ascents. The fell can be ascended from Grasmere or Dunmail Raise although a start from Patterdale is quite feasible. The Grasmere or Patterdale starts use the old packhorse route that links the two places; this is now part of Wainwright's Coast to Coast Walk. When Grisedale Hause is reached, it is a steep climb to the summit following a broken wall.

Geographic entities mentioned:
surface_form: grasmere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.449383
lon: -3.021239
Seat Sandal. Seat Sandal is a fell in the English Lake District, situated four kilometres (miles) north of the village of Grasmere from where it is very well seen. Nevertheless, it tends to be overshadowed by its higher neighbours in the Eastern Fells, Helvellyn and Fairfield. Topography.

Geographic entities mentioned:
surface_form: seat sandal
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.494561111111
lon: -3.01585
However, this must be regarded as a borderline case as there is no Ordnance Survey surveyed height for the top of Grisedale Hause. Alfred Wainwright gives it a height of giving Seat Sandal a topographic prominence of only 148 metres (two metres short of Marilyn qualification).

Geographic entities mentioned:
surface_form: seat sandal
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.494561111111
lon: -3.01585
Dong Ap Bia. Dong Ap Bia (, Ap Bia Mountain) is a mountain on the Laotian border of South Vietnam in Huế. Rising from the floor of the western A Shau Valley, it is a looming, solitary massif, unconnected to the ridges of the surrounding Annamite range. It dominates the northern valley, towering some 937 metres above sea level.

Geographic entities mentioned:
surface_form: dong ap bia
instance_of: Mountain
countries: Vietnam
coordinates: lat: 16.25
lon: 107.18333333333
Local Montagnard tribesmen call Ap Bia &quot;the mountain of the crouching beast.&quot;
History. In May 1969, a ridge of Dong Ap Bia, &quot;Hill 937&quot; in contemporary US military terminology, was the site of the Battle of Hamburger Hill, a controversial battle of the Vietnam War fought by the United States and South Vietnam against North Vietnamese forces.

Geographic entities mentioned:
surface_form: dong ap bia
instance_of: Mountain
countries: Vietnam
coordinates: lat: 16.25
lon: 107.18333333333
Dong Ap Bia. Dong Ap Bia (, Ap Bia Mountain) is a mountain on the Laotian border of South Vietnam in Huế. Rising from the floor of the western A Shau Valley, it is a looming, solitary massif, unconnected to the ridges of the surrounding Annamite range. It dominates the northern valley, towering some 937 metres above sea level.

Geographic entities mentioned:
surface_form: a shau valley
instance_of: Valley
countries: Vietnam
coordinates: lat: 16.259305555556
lon: 107.2125
Saway-yanga, California. Saway-yanga is a former Tongva (Fernandeño) Native American settlement in Los Angeles County, California. It was located near Mission San Fernando Rey de España in the San Fernando Valley.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
However, it may also be the oldest volcano in the Clearwater Valley, dating to about 200,000 years ago when it was the source of the vast quantity of lava that comprises the Murtle Plateau. Viewed from Green Mountain, it looks like a low rounded dome, quite different from nearby Pyramid Mountain. The Wells Gray Loppet Trail, a popular cross-country ski route, goes over McLeod Hill.

Geographic entities mentioned:
surface_form: pyramid mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.9944
lon: -120.104
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: pyramid mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 52.9511
lon: -118.149
surface_form: pyramid mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 49.81916666666667
lon: -122.90444444444445
McLeod Hill. McLeod Hill is a tuya, located north of Clearwater in the Wells Gray-Clearwater volcanic field in Wells Gray Provincial Park, east-central British Columbia, Canada. McLeod Hill last erupted about 12,000 years ago when the Murtle Plateau was still covered by ice.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mcleod hill
instance_of: Mountain
countries: Canada
coordinates: lat: 52
lon: -120
It starts at the Murtle River near Dawson Falls and ends at Helmcken Falls Lodge, a distance of. The ski trail is tracked by B.C. Parks volunteers during most winters. Beyond the King Hut rest stop, the trail climbs steeply onto McLeod Hill, then there is a long descent into Hemp Creek Valley. In summer, the trail is one of Wells Gray Park's few mountain biking routes.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
McLeod Hill. McLeod Hill is a tuya, located north of Clearwater in the Wells Gray-Clearwater volcanic field in Wells Gray Provincial Park, east-central British Columbia, Canada. McLeod Hill last erupted about 12,000 years ago when the Murtle Plateau was still covered by ice.

Geographic entities mentioned:
surface_form: mcleod hill
instance_of: Mountain
countries: Canada
coordinates: lat: 52
lon: -120
Viewed from Green Mountain, it looks like a low rounded dome, quite different from nearby Pyramid Mountain. The Wells Gray Loppet Trail, a popular cross-country ski route, goes over McLeod Hill. It starts at the Murtle River near Dawson Falls and ends at Helmcken Falls Lodge, a distance of. The ski trail is tracked by B.C. Parks volunteers during most winters.

Geographic entities mentioned:
surface_form: mcleod hill
instance_of: Mountain
countries: Canada
coordinates: lat: 52
lon: -120
It starts at the Murtle River near Dawson Falls and ends at Helmcken Falls Lodge, a distance of. The ski trail is tracked by B.C. Parks volunteers during most winters. Beyond the King Hut rest stop, the trail climbs steeply onto McLeod Hill, then there is a long descent into Hemp Creek Valley. In summer, the trail is one of Wells Gray Park's few mountain biking routes.

Geographic entities mentioned:
surface_form: mcleod hill
instance_of: Mountain
countries: Canada
coordinates: lat: 52
lon: -120
Low Abbotside. Low Abbotside is a civil parish in the county of North Yorkshire, England. It is a rural parish on the north side of Wensleydale. There is no village in the parish. The population was estimated at 110 in 2012. Governance. The parish lies within the Richmond and Northallerton UK Parliament constituency.

Geographic entities mentioned:
surface_form: Wensleydale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.3056
lon: -2.16667
They are known as an &quot;early-run&quot; species, as they migrate to spawn in the early spring. Distribution. Currently skipjack herring are restricted to the Gulf of Mexico and its drainage, in the United States. The Gulf of Mexico drainage includes the Mobile River basin, the ACF basin (Apalachicola/Chattahoochee/Flint River), the Mississippi basin, and the Rio Grande basin.

Geographic entities mentioned:
surface_form: Chattahoochee
instance_of: Watercourse
countries: United States
coordinates: lat: 30.7088028
lon: -84.8638097