Sarmila/GeoWiki-Features huggingface dataset:
The first building at the lake was La Casa de Miguel Ortiz, an adobe built by Miguel Ortiz, a muleteer, on land given him by his employer, wealthy landowner Edward Fitzgerald Beale. Southwest of the Ortiz Adobe was the Andrada Stage Station adobe, sited where the old Fort Tejon Road entered San Francisquito Canyon. Circa 1915, there were hot springs in Elizabeth Lake Canyon. A U.S.

Geographic entities mentioned:
surface_form: elizabeth lake
instance_of: Lake
countries: United States
coordinates: lat: 34.6658
lon: -118.403
surface_form: lake canyon
instance_of: Lake
countries: United States
coordinates: lat: 27.9926
lon: -81.9433
The lake was dry between 2013 and 2023 because of a drought. Education. In 1869, the Los Angeles County Board of Supervisors designated the Elizabeth Lake School District to serve the area, which had the only established school between Los Angeles and Bakersfield. Land for the school was donated by Samuel and Almeda Frakes from their ranch lands.

Geographic entities mentioned:
surface_form: elizabeth lake
instance_of: Lake
countries: United States
coordinates: lat: 34.6658
lon: -118.403
Education. In 1869, the Los Angeles County Board of Supervisors designated the Elizabeth Lake School District to serve the area, which had the only established school between Los Angeles and Bakersfield. Land for the school was donated by Samuel and Almeda Frakes from their ranch lands. Children from the Lake Hughes, Elizabeth Lake, and Green Valley areas are still served by this school district.

Geographic entities mentioned:
surface_form: elizabeth lake
instance_of: Lake
countries: United States
coordinates: lat: 34.6658
lon: -118.403
Children from the Lake Hughes, Elizabeth Lake, and Green Valley areas are still served by this school district. The 1869 wooden schoolhouse lasted until it was replaced by an adobe structure in the early 1930s, located on the east side of Elizabeth Lake Road, ¼ mile north of Andrada Corner at the intersection of San Francisquito and Elizabeth Lake Roads.

Geographic entities mentioned:
surface_form: elizabeth lake
instance_of: Lake
countries: United States
coordinates: lat: 34.6658
lon: -118.403
surface_form: elizabeth lake
instance_of: Lake
countries: United States
coordinates: lat: 34.6658
lon: -118.403
Geography. The lake, at in elevation, is within the Angeles National Forest. It is a natural perennial lake, but may dry up entirely during drought years. It is south of the western Antelope Valley. Elizabeth Lake is one of a series of sag ponds created by the motion of the Earth's tectonic plates along the San Andreas Fault in the area, with others including Hughes Lake and the Munz Lakes.

Geographic entities mentioned:
surface_form: antelope valley
instance_of: Valley
countries: United States
coordinates: lat: 39.8858
lon: -117.328
Mount Erebus disaster. On 28 November 1979 Air New Zealand flight 901, a scheduled sightseeing flight over Antarctica, crashed into Mount Erebus. The Douglas DC-10-30 disintegrated on impact killing all 237 passengers aboard as well as the 20 crewmembers. This remains New Zealand's deadliest disaster. 1980s.

Geographic entities mentioned:
surface_form: Mount Erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
El Centro, California. El Centro (Spanish for &quot;The Center&quot;) is a city in and the county seat of Imperial County, California, United States. El Centro is the most populous city in the Imperial Valley, the east anchor of the Southern California Border Region, and the core urban area and principal city of the El Centro metropolitan area which encompasses all of Imperial County.

Geographic entities mentioned:
surface_form: Imperial Valley
instance_of: Valley
countries: United States
coordinates: lat: 33.1
lon: -115.5
Geography. According to the United States Census Bureau, the city has a total area of, of which over 99% is land. El Centro is located in the Imperial Valley (considered locally as synonymous with Imperial County). The city is below sea level and the largest city in the United States below sea level. The Imperial Valley is in the Colorado Desert, an extension of the larger Sonoran Desert.

Geographic entities mentioned:
surface_form: Imperial Valley
instance_of: Valley
countries: United States
coordinates: lat: 33.1
lon: -115.5
Interstate 8 connects San Diego to the west and Yuma, Arizona to the east. State Route 86 and State Route 111 parallel each other as they go north to Brawley before running along the west and east shores of the Salton Sea, respectively, on their way to the Coachella Valley. Going south from El Centro, State Route 86 terminates at State Route 111, which runs to Calexico and Mexicali, Mexico.

Geographic entities mentioned:
surface_form: Coachella Valley
instance_of: Valley
countries: United States
coordinates: lat: 33.72
lon: -116.2
Ahwahnechee. The Ahwahnechee, Awani, or Awalache were an Indigenous people of California who historically lived in the Yosemite Valley. They were a band of Mono and Miwok People. The Awani people's heritage can be found all over Yosemite National Park. Name. The name &quot;Awani&quot; was also the name of their primary village.

Geographic entities mentioned:
surface_form: Yosemite Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
G. & J. Salter. After giving up seafaring, Salter went into business with his brother George in Saint John. The firm of G. & J. Salter, with their knowledge of foreign business contacts, operated as ship brokers for local shipbuilders. On October 24, 1846, George purchased the former Stephen Binney shipyard on the banks of the Petitcodiac River at &quot;The Bend&quot;, now known as Moncton.

Geographic entities mentioned:
surface_form: Petitcodiac River
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.926944444444
lon: -65.188888888889
Robert H. Milroy, a former U.S. Congressman and Indiana militia general, was commissioned colonel. The regiment contained approximately 950 men in Companies A through K. Early service and Antietam. Ordered east to join the Army of the Potomac, the 27th camped near Washington, D.C., into late 1861. In February 1862 it advanced into Virginia's Shenandoah Valley under Maj. Gen. Nathaniel P. Banks.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
They continued in the campaign with an assault on Kennesaw Mountain (June 27), and saw action at Ruff's Station (July 4), Chattahoochee River (July 5–17), and the Battle of Peachtree Creek (July 19–20). The regiment remained engaged during the Siege of Atlanta (July 25–August 25), and participated in the operations at Chattahoochee River Bridge (August 26–September 2).

Geographic entities mentioned:
surface_form: Chattahoochee River
instance_of: Watercourse
countries: United States
coordinates: lat: 30.7088028
lon: -84.8638097
Fahnestock moved into Fairseat, but the home burned down leaving only the stucco carriage house and garden intact. In 1940, Fahnestock sold it to Leroy Grumman. Geography. According to the United States Census Bureau, the village has a total area of, of which is land and, or 13.56%, is water – including Leeds Pond in the northeastern part of the village. Topography.

Geographic entities mentioned:
surface_form: Leeds Pond
instance_of: Lake
countries: United States
coordinates: lat: 40.8131752
lon: -73.7009529
The Bury line ran northward from the junction, crossing the Irwell Valley on the Clifton Viaduct (known locally as the &quot;13 arches&quot;), to run on the opposite side of the valley from the Bolton line. A station at the junction, with two platforms for each route (Bolton or Bury), opened in June 1847, and was named &quot;Clifton Junction&quot;.

Geographic entities mentioned:
surface_form: Irwell Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.66
lon: -2.31
Winters, California. Winters is a city in rural Yolo County, and the western Sacramento Valley, in northern California, United States. Winters has a 2024 population of 7,860. Winters is currently growing at a rate of 2.16% annually and its population has increased by 9.24% since the most recent census, which recorded a population of 7,195 in 2020.

Geographic entities mentioned:
surface_form: Sacramento Valley
instance_of: Valley
countries: United States
coordinates: lat: 39
lon: -121.5
The median age in Winters is 37.9 years: 38.1 years for males, and 37.9 years for females. Geography. Winters is a small city located on Putah Creek in the western Sacramento Valley, near the California Coastal Range. It is situated along Interstate 505, from Vacaville. Winters is nearly from Sacramento and about from San Francisco, California. It is located at.

Geographic entities mentioned:
surface_form: Sacramento Valley
instance_of: Valley
countries: United States
coordinates: lat: 39
lon: -121.5
These Mesozoic covers correspond mainly to limestone deposits from a shallow epicontinental sea separating the European foreland from the northern passive margin of the Alpine Tethys. They are overlain, particularly in the south, by the Cenozoic molasse of the North Alpine foreland basin, also known as the Swiss Molasse Basin.

Geographic entities mentioned:
surface_form: Swiss Molasse Basin
instance_of: Plateau
countries: Switzerland
coordinates: lat: 47.1167
lon: 7.36667
It extends mainly along the Franco-Swiss border, forming an arc that shifts from a west-east axis in the north to a north-south axis in the south. Strictly speaking, the massif extends from the summit of Lägern (Zurich canton) in Switzerland to the / anticline plateau in the Isère department, France.

Geographic entities mentioned:
surface_form: Lägern
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.481666666667
lon: 8.3947222222222
The massif spans over 340 km in its inner arc and over 400 km in its outer arc, with a maximum width of 65 km between Besançon and Neuchâtel. Although geographically not part of the Jura Massif, the Salève, Mandallaz Mountain, and ridges all belong to the same geological unit as the Jura. The Jura Massif defines the outer boundary of the Alpine system.

Geographic entities mentioned:
surface_form: Salève
instance_of: Mountain
countries: France
coordinates: lat: 46.09417
lon: 6.14028
surface_form: Mandallaz Mountain
instance_of: Mountain
countries: France
coordinates: lat: 45.976267
lon: 6.079928
The shoulders of the Rhine Graben (the Vosges Massif to the west and the Black Forest to the east), as well as the, act as barriers against which the Jura Massif abuts. Finally, its inner boundary is marked by the Swiss Molasse Basin, or more broadly, the North Alpine foreland basin, which largely corresponds to the Swiss Plateau.

Geographic entities mentioned:
surface_form: Swiss Plateau
instance_of: Plateau
countries: Switzerland
coordinates: lat: 47.1167
lon: 7.36667
The second project was supervised by the University of Lausanne (Urs Eichenberger) and the Swiss Geophysics Commission (François Marillier). Nearly 4,500 km of seismic lines and thirty well data points were used to reconstruct the Swiss Molasse Basin from Lake Geneva to Lake Constance.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
The layers located in a more internal position, beneath the Swiss Molasse Basin, exhibit very little deformation (a few detachment folds with amplitudes below 500 m and multi-kilometer wavelengths), except for the Salève Ridge, the Mandallaz Mountain, and the, which accommodate 5 to 6 km of shortening.

Geographic entities mentioned:
surface_form: Salève
instance_of: Mountain
countries: France
coordinates: lat: 46.09417
lon: 6.14028
surface_form: Mandallaz Mountain
instance_of: Mountain
countries: France
coordinates: lat: 45.976267
lon: 6.079928
A new revision has been recognized by the Swiss Stratigraphy Committee but has not yet been applied in the southern Jura (Salève and Vuache) due to a lack of biostratigraphic data and relevant correlations. Debates also concern the age of deposition, particularly of the White Urgonian. Some authors attribute it to the late Hauterivian, while others argue for a late Barremian age.

Geographic entities mentioned:
surface_form: Salève
instance_of: Mountain
countries: France
coordinates: lat: 46.09417
lon: 6.14028
surface_form: Vuache
instance_of: Mountain
countries: France
coordinates: lat: 46.057777777778
lon: 5.94
However, their lateral extent is limited, as they are preferentially preserved in karsts, favoring the deposition of Oligocene molasses on Urgonian limestone. Their thickness increases from the Jura toward Salève along an NW-SE axis, with a growing proportion of sandstones at the expense of clayey intervals.

Geographic entities mentioned:
surface_form: Salève
instance_of: Mountain
countries: France
coordinates: lat: 46.09417
lon: 6.14028
In these depressions, lakes formed and gradually turned into peatlands as they filled in. Among the vegetation found in these peat bogs are sphagnum mosses, which can thrive in acidic environments. Peat and lake deposits have excellent preservation properties, allowing for the conservation of numerous artifacts along the shores of Lakes Clairvaux and Chalain.

Geographic entities mentioned:
surface_form: Clairvaux
instance_of: Group of lakes
countries: France
coordinates: lat: 46.565527777778
lon: 5.74925
surface_form: Chalain
instance_of: Lake
countries: France
coordinates: lat: 46.670727777778
lon: 5.7913055555556
Currently, active rockfalls can be identified by their lack of vegetation cover. Active rockfalls are rare in the Jura and are mainly found at the base of active cliffs with northern exposure, such as Creux du Van and Mont d’Or. The vast majority of rockfalls formed at the end of the last glaciation, during the glacier’s retreat. Marl can absorb water and become destabilized.

Geographic entities mentioned:
surface_form: Creux du Van
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.936666666667
lon: 6.7275
However, the weight and thickness of the molasse series in the North Alpine foreland basin (approximately 4 km thick) propagated mechanical stress outward, reaching what is now the Jura. Additionally, despite being located within the foreland basin, the Salève, Mandallaz, and Âge mountain ranges are also thought to have formed due to a decrease in molasse thickness toward the west.

Geographic entities mentioned:
surface_form: Salève
instance_of: Mountain
countries: France
coordinates: lat: 46.09417
lon: 6.14028
surface_form: Mandallaz
instance_of: Mountain
countries: France
coordinates: lat: 45.976267
lon: 6.079928
Thrust faults. Some anticlines in the Haute-Chaîne thrust over the synclines associated with them, creating faulted relief within the syncline. The Dent de Vaulion is a remnant of an eroded anticline, overturned westward, which thrusts over the terminus of the Joux syncline. This syncline disappears underground beneath the Dent de Vaulion, exposing Middle Jurassic limestones.

Geographic entities mentioned:
surface_form: Dent de Vaulion
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.68402
lon: 6.35132
Since then, it has been open to the public. Other smaller deposits were also exploited along the western shore of Lake Neuchâtel, particularly at Saint-Aubin and Sauges. The Saint-Aubin deposit contained three impregnated layers that were mined for about ten years in the 19th century for the manufacture of bitumen-coated cardboard pipes and asphalt mastic.

Geographic entities mentioned:
surface_form: Lake Neuchâtel
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.9
lon: 6.85
Further south, deposits have been identified in an area extending from the southernmost Jura (Chézery) to the banks of the Rhône north of Seyssel (Pyrimont and Challonges) and the (Lovagny and Chavanod). In addition to Urgonian limestones, asphalt has also been found in the red molasse (Lower Freshwater Molasse) around Geneva (Dardagny) and south of Lake Neuchâtel (Chavornay and Orbe). Iron.

Geographic entities mentioned:
surface_form: Lake Neuchâtel
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.9
lon: 6.85
Iron. Due to their high iron content, siderolithic sandstones have been extensively mined. On the Salève, these sandstones were locally exploited between the 5th and 13th centuries at the Rochers de Faverges for the production of iron and steel. Later, in the 19th and 20th centuries, mines were excavated in the Delémont Basin, though they failed to yield sufficient output.

Geographic entities mentioned:
surface_form: Salève
instance_of: Mountain
countries: France
coordinates: lat: 46.09417
lon: 6.14028
Coupled to this, &quot;The Ben&quot; was also having to contend with a headwind, blowing from the west. At 13:34 &quot;Ben-my-Chree&quot; arrived off Douglas Head and slowed for the last quarter of a mile as she approached her moorings at the Victoria Pier. &quot;Ben-my-Chree's&quot; exceptional service speed caused several stories to circulate about her.

Geographic entities mentioned:
surface_form: Douglas Head
instance_of: Landform
countries: Isle of Man
coordinates: lat: 54.14305556
lon: -4.46666667
It is improbable that the vessel approached 27 knots except in the most unusual conditions, and it is only known that she once achieved on a favourable tide. Going astern, she could travel at. In her first season between Liverpool and Douglas, her average time between the Bar Lightship and the Head was 2 hours 24 minutes. A year later she reduced this average by one minute.

Geographic entities mentioned:
surface_form: the Head
instance_of: Landform
countries: Isle of Man
coordinates: lat: 54.14305556
lon: -4.46666667
SS Widget. SS &quot;Widget&quot; was a diesel tugboat that operated on the Arrow Lakes in British Columbia, Canada. She was built by Ivan Horie in Vancouver, British Columbia in 1948. She was chartered by the Canadian Pacific Railway company to fill in until a replacement for SS &quot;Columbia&quot; (1920-1947), which had a damaged hull, could be acquired.

Geographic entities mentioned:
surface_form: Arrow Lakes
instance_of: Group of lakes
countries: Canada
coordinates: lat: 50
lon: -118
1864 Valley Campaign. In June 1864, Ramseur and the rest of Early's corps was sent by Lee to the Shenandoah Valley to draw Union forces away from Petersburg, in the Valley Campaigns of 1864. They conducted a long and successful raid down the Valley, into Maryland, and reached the outskirts of Washington, D.C., before turning back. Maj. Gen.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
Cub Creek (South Hyco Creek tributary). Cub Creek is a long 1st order tributary to South Hyco Creek in Person County, North Carolina. Cub Creek joins South Hyco Creek within Hyco Lake. Course. Cub Creek rises about 1 mile southeast of Leasburg, North Carolina and then flows northeast to join South Hyco Creek about 1.5 miles south-southwest of Longs Store. Watershed.

Geographic entities mentioned:
surface_form: Hyco Lake
instance_of: Lake
countries: United States
coordinates: lat: 36.512777777778
lon: -79.046944444444
Soldiers were seen kicking and throwing the corpses of dead militants off a rooftop in the city. The al-Quds Brigades of PIJ targeted the Shaked settlement with gunfire. The al-Aqsa Martyrs' Brigades targeted an IDF checkpoint at Mount Ebal with gunfire. 21 September. The al-Aqsa Martyrs' Brigades targeted an IDF checkpoint at Mount Gerzim with gunfire. 25 September.

Geographic entities mentioned:
surface_form: Mount Ebal
instance_of: Mountain
countries: State of Palestine
coordinates: lat: 32.234
lon: 35.2733
The al-Quds Brigades of PIJ targeted the Shaked settlement with gunfire. The al-Aqsa Martyrs' Brigades targeted an IDF checkpoint at Mount Ebal with gunfire. 21 September. The al-Aqsa Martyrs' Brigades targeted an IDF checkpoint at Mount Gerzim with gunfire. 25 September. The IDF resumed operations inside Jenin. 26 September.

Geographic entities mentioned:
surface_form: Mount Gerzim
instance_of: Mountain
countries: State of Palestine
coordinates: lat: 32.199444444444
lon: 35.272777777778
Eriogonum truncatum. &quot;Eriogonum truncatum&quot;, the Mount Diablo buckwheat, is a small pink wildflower, believed to have been extinct since 1936 until its rediscovery in 2005. The species is only known to live on Mount Diablo in Contra Costa County, northern California. Habitat. It has been found on the edge of chaparral but may be a refugee there, squeezed out of more open areas by exotics.

Geographic entities mentioned:
surface_form: Mount Diablo
instance_of: Mountain
countries: United States
coordinates: lat: 37.881697781
lon: -121.914154997
Llandyrnog & District Summer League. The Llandyrnog & District Summer League is a football league in Wales, mostly covering rural areas in the Vale of Clwyd. The league is not part of the Welsh football league system and is not affiliated with the FAW. The league also plays the Bridson and Evans Memorial Shield, which was won by Llanrhaeadr in 2024. History. The league was founded in early 1927.

Geographic entities mentioned:
surface_form: Vale of Clwyd
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.21
lon: -3.38
Mount Hibok-Hibok. Mount Hibok-Hibok (also known as Catarman Volcano) is a stratovolcano on Camiguin Island in the Philippines. One of the active volcanoes in the country, it is part of the Pacific ring of fire. Description. Volcanologists classify Hibok-Hibok or Catarman Volcano as a stratovolcano and dome complex with an elevation of and a base diameter of.

Geographic entities mentioned:
surface_form: mount hibok-hibok
instance_of: Mountain
countries: Philippines
coordinates: lat: 9.2005555555556
lon: 124.66805555556
surface_form: hibok-hibok
instance_of: Mountain
countries: Philippines
coordinates: lat: 9.2005555555556
lon: 124.66805555556
Mount Hibok-Hibok. Mount Hibok-Hibok (also known as Catarman Volcano) is a stratovolcano on Camiguin Island in the Philippines. One of the active volcanoes in the country, it is part of the Pacific ring of fire. Description. Volcanologists classify Hibok-Hibok or Catarman Volcano as a stratovolcano and dome complex with an elevation of and a base diameter of.

Geographic entities mentioned:
surface_form: mount hibok-hibok
instance_of: Mountain
countries: Philippines
coordinates: lat: 9.2005555555556
lon: 124.66805555556
surface_form: catarman volcano
instance_of: Mountain
countries: Philippines
coordinates: lat: 9.2005555555556
lon: 124.66805555556
surface_form: hibok-hibok
instance_of: Mountain
countries: Philippines
coordinates: lat: 9.2005555555556
lon: 124.66805555556
Mount Timpoong and Hibok-Hibok form the two major landmarks within the Timpoong and Hibok-Hibok Natural Monument. The natural monument became an ASEAN Heritage Park in 2015. The indigenous Kamigin Manobo are believed to be the original inhabitants of Mount Hibok-Hibok. Eruptions. Hibok-Hibok has erupted four times in modern history.

Geographic entities mentioned:
surface_form: mount hibok-hibok
instance_of: Mountain
countries: Philippines
coordinates: lat: 9.2005555555556
lon: 124.66805555556
surface_form: hibok-hibok
instance_of: Mountain
countries: Philippines
coordinates: lat: 9.2005555555556
lon: 124.66805555556
One of the active volcanoes in the country, it is part of the Pacific ring of fire. Description. Volcanologists classify Hibok-Hibok or Catarman Volcano as a stratovolcano and dome complex with an elevation of and a base diameter of. It was described in a 1905 report as having &quot;suddenly risen from the plain a short distance from the town of Catarmin in 1872.

Geographic entities mentioned:
surface_form: catarman volcano
instance_of: Mountain
countries: Philippines
coordinates: lat: 9.2005555555556
lon: 124.66805555556
surface_form: hibok-hibok
instance_of: Mountain
countries: Philippines
coordinates: lat: 9.2005555555556
lon: 124.66805555556
Eruptions. Hibok-Hibok has erupted four times in modern history. The first recorded eruption occurred in 1827 and a similar activity followed in 1862. Volcanic activity is currently monitored through solar-powered autonomous stations operated by the Hibok-Hibok Volcano Observatory under the Philippine Institute of Volcanology and Seismology. 1871 to 1875.

Geographic entities mentioned:
surface_form: hibok-hibok
instance_of: Mountain
countries: Philippines
coordinates: lat: 9.2005555555556
lon: 124.66805555556
1871 to 1875. On February 16, 1871, earthquakes and subterranean rumblings began to be felt on the island, which increased in severity until April 30 when a volcanic fissure opened up 400 yards southwest of the village of Catarman, on the northwest flank of Hibok-hibok Volcano. From the opening, lava was continuously ejected and poured into the sea for four years, destroying the town.

Geographic entities mentioned:
surface_form: hibok-hibok
instance_of: Mountain
countries: Philippines
coordinates: lat: 9.2005555555556
lon: 124.66805555556
Its adjacent volcanic edifices are: -high Mount Vulcan, northwest of Hibok-Hibok; -high Mount Mambajao, at the center of Camiguin; -high Mount Guinsiliban, southernmost Camiguin; -high Mount Butay; and Mount Uhay, north of Mount Guinsiliban. There are also domes and cones at Campana Hill, Minokol Hill, Tres Marias Hill, Mount Carling, Mount Tibane, and Piyakong Hill.

Geographic entities mentioned:
surface_form: hibok-hibok
instance_of: Mountain
countries: Philippines
coordinates: lat: 9.2005555555556
lon: 124.66805555556
There are also domes and cones at Campana Hill, Minokol Hill, Tres Marias Hill, Mount Carling, Mount Tibane, and Piyakong Hill. Mount Timpoong and Hibok-Hibok form the two major landmarks within the Timpoong and Hibok-Hibok Natural Monument. The natural monument became an ASEAN Heritage Park in 2015. The indigenous Kamigin Manobo are believed to be the original inhabitants of Mount Hibok-Hibok.

Geographic entities mentioned:
surface_form: hibok-hibok
instance_of: Mountain
countries: Philippines
coordinates: lat: 9.2005555555556
lon: 124.66805555556
surface_form: hibok-hibok
instance_of: Mountain
countries: Philippines
coordinates: lat: 9.2005555555556
lon: 124.66805555556
Solfataric activity continued up to 1902. In 1901, the volcano disappeared. 1948 to 1951. From 1948 to 1951, Mt. Hibok-Hibok constantly rumbled and smoked. There were also landslides and earthquakes followed by dome building and nuee ardente. The Peléan eruption in 1948 from the Kanangkaan crater caused little damage and loss of life.

Geographic entities mentioned:
surface_form: hibok-hibok
instance_of: Mountain
countries: Philippines
coordinates: lat: 9.2005555555556
lon: 124.66805555556
This time, however, it unleashed boiling lava, poisonous gases, and landslides enough to destroy nearly of land particularly in Mambajao. All in all, over 3,000 people were killed. Before the eruption of Mt. Hibok-Hibok in 1951, the population of Camiguin had reached 69,000. After the eruption, the population was reduced to about 34,000 due to massive emigration.

Geographic entities mentioned:
surface_form: hibok-hibok
instance_of: Mountain
countries: Philippines
coordinates: lat: 9.2005555555556
lon: 124.66805555556
Mont Bengoué. Mont Bengoué is the highest mountain in Gabon. Mont Bengoué is located in the Ogooué-Ivindo Province, at an elevation of 1,070 m (3,510 ft).

Geographic entities mentioned:
surface_form: mont bengoué
instance_of: Mountain
countries: Gabon
coordinates: lat: 0.95
lon: 13.683333333333
Horton in Ribblesdale. Horton in Ribblesdale is a small village and civil parish in Ribblesdale in the county of North Yorkshire, England. It is situated on the Settle&ndash;Carlisle Railway to the west of Pen-y-ghent. The parish extends from Helwith Bridge, south of the village, to a point north of the village.

Geographic entities mentioned:
surface_form: Ribblesdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.144333333333336
lon: -2.296333333333333
Horton in Ribblesdale. Horton in Ribblesdale is a small village and civil parish in Ribblesdale in the county of North Yorkshire, England. It is situated on the Settle&ndash;Carlisle Railway to the west of Pen-y-ghent. The parish extends from Helwith Bridge, south of the village, to a point north of the village.

Geographic entities mentioned:
surface_form: Pen-y-ghent
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.155277777778
lon: -2.2497222222222
The parish extends from Helwith Bridge, south of the village, to a point north of the village. It includes the summits of Pen-y-Ghent and Plover Hill on the east side of the dale, and the summit of Simon Fell to the west. In addition to the village of Horton the parish includes the hamlets of Selside, High Birkwith, Brackenbottom and Studfold.

Geographic entities mentioned:
surface_form: Plover Hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.172369444444
lon: -2.2328111111111
Visitor attractions. Horton in Ribblesdale is the traditional starting (and finishing) point for the Three Peaks walk. The Pennine Way and Ribble Way long-distance footpaths pass through the village. The region is also popular for caving and potholing, with Alum Pot and the Long Churn cave system just to the north of the village, and Hull Pot and Hunt Pot on the western side of Pen-y-ghent.

Geographic entities mentioned:
surface_form: Pen-y-ghent
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.155277777778
lon: -2.2497222222222
The Three Peaks walk is an endurance challenge of distance, including of ascent and descent of the mountains of Pen-y-ghent, Whernside and Ingleborough all to be completed in under 12 hours which attracts thousands of walkers each year.

Geographic entities mentioned:
surface_form: Whernside
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.227777777778
lon: -2.4033333333333
surface_form: Ingleborough
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.165833333333
lon: -2.3975
Kegan Lake. Kegan Lake is a lake in Dakota County, in the U.S. state of Minnesota. Kegan Lake was named for Andrew Keegan, a pioneer farmer.

Geographic entities mentioned:
surface_form: kegan lake
instance_of: Lake
countries: United States
coordinates: lat: 44.75833333
lon: -93.11638889
In the only creation of cardinals promoted by him, among the twelve raised to the purple, there were two monks of his order. He also visited personally the Benedictine monastery on Monte Cassino, where he persuaded the monks to accept his more rigorous rule. He sent fifty monks of his order to introduce it, who remained there, however, for only a few months.

Geographic entities mentioned:
surface_form: Monte Cassino
instance_of: Mountain
countries: Italy
coordinates: lat: 41.49
lon: 13.813888888889
The mountain is situated four km from the nearest public road but there are good stalkers paths within the deer forest which aid access to the foot of the mountain. An Ruadh-stac is closely associated with the adjoining Munro of Maol Cheann-dearg with which it is often climbed.

Geographic entities mentioned:
surface_form: Maol Cheann-dearg
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.491696
lon: -5.465565
surface_form: an ruadh-stac
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.4758
lon: -5.4678
It is possible to climb the mountain by a longer route from Glen Torridon starting from Annat at. The summit is littered with quartzite boulders, with the highest point marked by a cairn of rocks and gives a view which includes the Skye Cuillin to the SW, Upper Loch Torridon appears next to Beinn Damh to the NW while the Torridon hills are further round to the north.

Geographic entities mentioned:
surface_form: Beinn Damh
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.49335
lon: -5.51673
An Ruadh-stac. An Ruadh-stac is a Scottish mountain situated in the Wester Ross region of the Highland council area. It is located 26 km north east of Kyle of Lochalsh. Overview. An Ruadh-stac reaches a height of 890 metres (2926 feet) making it the 30th highest Corbett, it also qualifies as a Marilyn.

Geographic entities mentioned:
surface_form: an ruadh-stac
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.4758
lon: -5.4678
Overview. An Ruadh-stac reaches a height of 890 metres (2926 feet) making it the 30th highest Corbett, it also qualifies as a Marilyn. It is a distinguished looking mountain which is prominent in views because of its light grey coloured quartzite rocks, it stands in the ancient Coulin hunting forest, an area of rough mountainous country between Glen Carron and Glen Torridon.

Geographic entities mentioned:
surface_form: an ruadh-stac
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.4758
lon: -5.4678
The mountain's Gaelic name translates as the Red Stack or Red Conical Hill; this is slightly confusing and misleading, as it is invariably seen as a light-grey hill due to its quartzite rocks. Hamish Brown comments on the name thus: “An Ruadh-stac is a grey hill, sometimes touched white by the sun but never red like its ruddy, bald headed neighbour (Maol Cheann-dearg).”
Geography.

Geographic entities mentioned:
surface_form: an ruadh-stac
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.4758
lon: -5.4678
Hamish Brown comments on the name thus: “An Ruadh-stac is a grey hill, sometimes touched white by the sun but never red like its ruddy, bald headed neighbour (Maol Cheann-dearg).”
Geography. An Ruadh-stac has the classic triangular mountain shape formed by three steep ridges; the NE ridge is the least steep and the one usually used for ascent and descent by walkers.

Geographic entities mentioned:
surface_form: an ruadh-stac
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.4758
lon: -5.4678
Ascents and view. The summit of An Ruadh-stac is a long way from any road, but the closest starting point is on the A890 road at Coulags in Glen Carron at grid reference. This route follows the footpath north up the valley of the Fionn-abhainn before crossing the river and going west and climbing up to the Bealach a’ Choire Ghairbh.

Geographic entities mentioned:
surface_form: an ruadh-stac
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.4758
lon: -5.4678
The mountain's finest geographical feature is the north face, a precipitous rock wall which shows off the mountain's layered geology when viewed from a distance. These crags rise over 400 metres from the shore of Loch Coire an Ruaidh-staic and have received the attention of rock climbers, with Tom Patey and Chris Bonington pioneering a route in 1960.

Geographic entities mentioned:
surface_form: loch coire
instance_of: Lake
countries: United Kingdom
coordinates: lat: 58.216666666667
lon: -4.35
By exploring the summit plateau further it is possible to look 1000 feet down the cliffs of the north face to Loch Coire an Ruaidh-staic.

Geographic entities mentioned:
surface_form: loch coire
instance_of: Lake
countries: United Kingdom
coordinates: lat: 58.216666666667
lon: -4.35
In March 1930, Hoyt founded the International Desert Conservation League'&quot;. Throughout the 1930s she worked to encourage the state of California to create three parks: Joshua Tree, Death Valley, and Anza-Borrego Desert. Though initially thwarted, in 1936, she gained support by the administration of President Franklin D.

Geographic entities mentioned:
surface_form: Death Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.45693888888889
lon: -116.86528055555556
Kanyembo. veqs06ddkgd16bd4vgjg4acj324vp" xml:space="preserve">Kanyembo is the principal centre of the population on the Mofwe Lagoon, the largest of several lagoons in the Luapula River swamps south of Lake Mweru, in the Luapula Province of Zambia. It takes its name from its traditional ruler, Chief Kanyembo, one of the senior chiefs of the Kazembe-Lunda under Mwata Kazembe.

Geographic entities mentioned:
surface_form: Mofwe Lagoon
instance_of: Lake
countries: Zambia
coordinates: lat: -9.6166666666667
lon: 28.7
surface_form: Lake Mweru
instance_of: Lake
countries: Zambia
Democratic Republic of the Congo
coordinates: lat: -9.1666666666667
lon: 28.5
River Wheeler. The River Wheeler (Welsh: &quot;Afon Chwiler&quot;) is a tributary of the River Clwyd in north-east Wales. Rising on the east side of the Clwydian Range, it is a &quot;misfit stream&quot; occupying a deep valley cutting westwards through the range into the Vale of Clwyd.

Geographic entities mentioned:
surface_form: Vale of Clwyd
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.21
lon: -3.38
Alsea post office was established in 1871. In the early 1850s settlers moved from the Willamette Valley into the Alsea area to take up donation land claims. While logging was once the primary industry in Alsea, it is now known as a place for fishing on the Alsea River, particularly for steelhead, and a favorite stopping point on a well-traveled cycling loop. Climate.

Geographic entities mentioned:
surface_form: Willamette Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.9
lon: -123.1
Toponymy. In French, the word &quot;Cran&quot; means &quot;rock cap&quot;. This word is mainly use by people in the region of Lac Saint-Jean. The toponym &quot;Rivière du Cran&quot; was formalized on December 5, 1968, at the Place Names Bank of the Commission de toponymie du Québec.

Geographic entities mentioned:
surface_form: Lac Saint-Jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
surface_form: lac saint-jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
surface_form: saint-jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
Rivière du Cran. The Rivière du Cran (&quot;English: Cran River&quot;) is a tributary of Ashuapmushuan River, flowing in the unorganized territory of Lac-Ashuapmushuan and in the municipality of La Doré, in the Le Domaine-du-Roy Regional County Municipality, in the administrative region of Saguenay–Lac-Saint-Jean, in the province of Quebec, in Canada.

Geographic entities mentioned:
surface_form: saint-jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
surface_form: doré
instance_of: Lake
countries: Canada
coordinates: lat: 54.766666666667
lon: -107.3
surface_form: rivière du cran
instance_of: Watercourse
countries: Canada
coordinates: lat: 48.870277777778
lon: -72.837777777778
Lac des Jaseuers is encased between mountains in a forest area. From the mouth of the Cran river, the current descends the course of the Ashuapmushuan river on, then crosses Lake Saint-Jean east on (its full length), follows the course of the Saguenay river via the Petite Décharge on eastwards to Tadoussac where it merges with the estuary of Saint Lawrence. Toponymy.

Geographic entities mentioned:
surface_form: saint-jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
Rivière du Cran. The Rivière du Cran (&quot;English: Cran River&quot;) is a tributary of Ashuapmushuan River, flowing in the unorganized territory of Lac-Ashuapmushuan and in the municipality of La Doré, in the Le Domaine-du-Roy Regional County Municipality, in the administrative region of Saguenay–Lac-Saint-Jean, in the province of Quebec, in Canada.

Geographic entities mentioned:
surface_form: rivière du cran
instance_of: Watercourse
countries: Canada
coordinates: lat: 48.870277777778
lon: -72.837777777778
Tule Lake National Wildlife Refuge. The Tule Lake National Wildlife Refuge is a National Wildlife Refuge of the United States in northern California near the Oregon border. It covers in the Tule Lake basin. It is part of the Klamath Basin National Wildlife Refuge Complex, and is a crucial part of the Pacific Flyway corridor for migratory birds.

Geographic entities mentioned:
surface_form: Tule Lake
instance_of: Lake
countries: United States
coordinates: lat: 41.909322222222
lon: -121.53304722222
The town is on a small peninsula surrounded by Lake Washington, and is near the suburbs of Medina (to the southwest), Clyde Hill (to the south), Yarrow Point (on another peninsula to the east), and Kirkland (to the northeast), as well as the city of Bellevue (to the east). As of the 2020 census, the town had a total population of 457. History. Leigh S. J.

Geographic entities mentioned:
surface_form: Lake Washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Around 1900, the property was taken over by Puget Sound National Bank and sold to a group of Seattle men who used it as a family retreat for Sunday picnics and summer camping. Before the creation of the Evergreen Point Floating Bridge and Interstate 90 floating bridges across Lake Washington, residents commuted to Seattle via the &quot;Gazelle&quot;, one of several ferries on Lake Washington.

Geographic entities mentioned:
surface_form: Lake Washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
The first republican line, along the Deva River, was soon overrun, and the town of Llanes fell on 5 September 1937. However, the routes the Nationalists then had to take were commanded by the limestone walls of the Sierra de Cuera on the north of the front and the Deva Gorge to the south.

Geographic entities mentioned:
surface_form: Sierra de Cuera
instance_of: Mountain
countries: Spain
coordinates: lat: 43.35410278
lon: -4.76988333
Wacouta, Minnesota. Wacouta is an unincorporated community in Wacouta Township, Goodhue County, Minnesota, United States. The community is located southeast of Red Wing along Highways 61 and 63. Bullard Creek flows through the community, with the Mississippi River and Lake Pepin located nearby. Nearby places include Red Wing, Frontenac, Hay Creek, and Lake City. Transportation.

Geographic entities mentioned:
surface_form: Lake Pepin
instance_of: Lake
countries: United States
coordinates: lat: 44.4982
lon: -92.3013
La Chute River. The La Chute River, also known as Ticonderoga Creek, is a short, fast-moving river, near the Vermont–New York border. It is now almost wholly contained within the municipality of Ticonderoga, New York, connecting the northern end and outlet of the long Lake George and the southern end of the long Lake Champlain through many falls and rapids.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
Lawrence River and then into the North Atlantic Ocean north of Nova Scotia. Geology and physiography. The Champlain Valley is among the northernmost valleys considered part of the Great Appalachian Valley, reaching from the province of Quebec, Canada somewhat northeast of Montreal at the outlet of the Richelieu River to Alabama.

Geographic entities mentioned:
surface_form: Great Appalachian Valley
instance_of: Valley
countries: United States
coordinates: lat: 39.5
lon: -77.83333333333333
Lake Champlain is situated in the Champlain Valley between the Green Mountains of Vermont and the Adirondack Mountains of New York, and Lake George is located in the Adirondack Park and mountain range north of the lower Berkshire Hills arrayed to the south and east, which give land routes through the region accessibility into the Hudson River and Connecticut River drainage basins.

Geographic entities mentioned:
surface_form: Champlain Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.45868
lon: -73.42617
Elected in 2020, she assumed office on January 19, 2021. Early life and education. Ortez was raised in farming community in the San Joaquin Valley. In 1989, she attended UC Davis' Young Scholars Program and went on to earn a Bachelor of Arts from Harvard University and a Master of Public Administration from the University of New Mexico. Career.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
Sirihuani. Sirihuani or Sirijuani is a mountain in the Urubamba mountain range in the Andes of Peru. It is located in the Cusco Region, Calca Province, in the districts of Calca and Lares. It is situated northwest of Sahuasiray and Canchacanchajasa mountains, and northeast of Chicón.

Geographic entities mentioned:
surface_form: Sahuasiray
instance_of: Mountain
countries: Peru
coordinates: lat: -13.21333333
lon: -71.99
surface_form: Canchacanchajasa
instance_of: Mountain
countries: Peru
coordinates: lat: -13.22
lon: -72.0089
surface_form: Chicón
instance_of: Mountain
countries: Peru
coordinates: lat: -13.23666667
lon: -72.05611111
Sirihuani. Sirihuani or Sirijuani is a mountain in the Urubamba mountain range in the Andes of Peru. It is located in the Cusco Region, Calca Province, in the districts of Calca and Lares. It is situated northwest of Sahuasiray and Canchacanchajasa mountains, and northeast of Chicón.

Geographic entities mentioned:
surface_form: urubamba
instance_of: Valley
countries: Peru
coordinates: lat: -13.333333333333
lon: -72.083333333333
surface_form: sirihuani
instance_of: Mountain
countries: Peru
coordinates: lat: -13.19916667
lon: -72.04416667
Sirihuani. Sirihuani or Sirijuani is a mountain in the Urubamba mountain range in the Andes of Peru. It is located in the Cusco Region, Calca Province, in the districts of Calca and Lares. It is situated northwest of Sahuasiray and Canchacanchajasa mountains, and northeast of Chicón.

Geographic entities mentioned:
surface_form: sirihuani
instance_of: Mountain
countries: Peru
coordinates: lat: -13.19916667
lon: -72.04416667
The raft was a propitiatory offering made within the historical context of the emerging muisca chiefdom of Pasca. According to some scholars, the piece probably refers to the gold offering ceremony described in the legend of &quot;El Dorado&quot;, which occasionally took place at Lake Guatavita.

Geographic entities mentioned:
surface_form: Lake Guatavita
instance_of: Lake
countries: Colombia
coordinates: lat: 4.9772222222222
lon: -73.775555555556
The piece is exhibited at the Gold Museum in Bogotá. Muisca people. The Muisca people, also known as the Chibcha, were situated at 9000 ft elevation in the eastern Andes of Colombia near modern day Bogotá, the town of Tunja, and Lake Guatavita. While most Muisca villages had a chief and priests, the Muisca were generally an egalitarian agricultural people.

Geographic entities mentioned:
surface_form: Lake Guatavita
instance_of: Lake
countries: Colombia
coordinates: lat: 4.9772222222222
lon: -73.775555555556
It was found together with another objet which represented a ruler seated on his litter, and was most likely a votive offering commissioned by the chief of Pasca. Traditionally, and notably at the Museo del Oro, it has been interpreted as representing the famous Guatavita ceremony associated with the myth of El Dorado.

Geographic entities mentioned:
surface_form: Guatavita
instance_of: Lake
countries: Colombia
coordinates: lat: 4.9772222222222
lon: -73.775555555556
Prillwitz. Prillwitz is a small village in Mecklenburg-Vorpommern (Mecklenburg-West Pomerania), on the shores of the lake Lieps, Germany. It is part of the municipality Hohenzieritz. It lies approximately 125 kilometres north of Berlin through the B96 or 205 kilometres through the A20. The town has a church and a small castle converted into a hotel and restaurant.

Geographic entities mentioned:
surface_form: Lieps
instance_of: Lake
countries: Germany
coordinates: lat: 53.451111111111
lon: 13.157222222222
Chinese Peak (Idaho). Chinese Peak is a summit in Bannock County, Idaho, in the United States. This peak is the highest point in the portion of the Portneuf Range called the Pocatello Range. With an elevation of, Chinese Peak is the 1069th highest summit in the state of Idaho. The peak is a fire lookout site and a road/bike trail leads to the top.

Geographic entities mentioned:
surface_form: chinese peak
instance_of: Mountain
countries: United States
coordinates: lat: 42.849
lon: -112.363
surface_form: chinese peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.2191
lon: -119.155