Sarmila/GeoWiki-Features huggingface dataset:
One hypothesized explanation for oceanic island basalt in the Earth's upper mantle under the Northern Cordilleran Volcanic Province is the existence of a slab window. However, not much of a noticeable evidence linking the production of magma in the upper mantle to a possible tectonic system has been stated.

Geographic entities mentioned:
surface_form: northern cordilleran volcanic province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
But these faults were in a matter of dispute in 1997 by geologists, stating these faults were last active between 20 and five million years ago. In 1999, a sequence of north-trending faults were mapped that seem to represent young rifting events parallel with the southwestern boundary of the Northern Cordilleran Volcanic Province.

Geographic entities mentioned:
surface_form: northern cordilleran volcanic province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
These rift-related faults might have been active as recently as five million years ago and they might have connections with adjacent Miocene and younger volcanic activity in the southern part of the Northern Cordilleran Volcanic Province.

Geographic entities mentioned:
surface_form: northern cordilleran volcanic province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
In addition, brittle faults with similar north-trending directions might enlarge as far north as the fault next to the western flank of the Mount Edziza volcanic complex. These tectonic events might have helped form the structure the Northern Cordilleran Volcanic Province. Subduction beside the northern portion of the Western Cordillera deceased between 43 and 40 million years ago.

Geographic entities mentioned:
surface_form: northern cordilleran volcanic province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
Although extensive rifting has not yet been recognized in the Northern Cordilleran Volcanic Province, volcanism throughout the past 1.6 million years is possibly due to repetitive upper mantle upwelling and adjacent transtension throughout the Queen Charlotte Fault, accommodated partly by numerous east–west trending fault zones that extend all through the Northern Cordilleran Volcanic Province.

Geographic entities mentioned:
surface_form: northern cordilleran volcanic province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
surface_form: northern cordilleran volcanic province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
The volcanics comprising the Northern Cordilleran Volcanic Province are consistent with the rifting environment. Alkaline basalt, lesser hawaiite and basanite magmas from effusive eruptions create the massive shield volcanoes and small cinder cones throughout the volcanic province, several of which comprise lherzolite magma.

Geographic entities mentioned:
surface_form: northern cordilleran volcanic province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
These felsic volcanics are understood to have been created by fractionation of mainly alkali basalt magma in crustal reservoirs. An area of continental rifting, such as the Northern Cordilleran Volcanic Province, would aid the formation of high-level reservoirs of capable size and thermal activity to maintain long-lived fractionation. Lithosphere thickness.

Geographic entities mentioned:
surface_form: northern cordilleran volcanic province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
Lithosphere thickness. The variety of different temperature ranges from xenoliths throughout the Northern Cordilleran Volcanic Province indicate that a narrow lithosphere lies under the northern portion of the volcanic province and a more dense lithosphere lies under the southern portion of the volcanic province.

Geographic entities mentioned:
surface_form: northern cordilleran volcanic province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
This indication is further provided if the geothermal gradient inside the lithosphere under the northern portion of the Northern Cordilleran Volcanic Province is greater than that in the southern portion of the province.

Geographic entities mentioned:
surface_form: northern cordilleran volcanic province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
Further evidence that indicate lithospheric thickening beneath the middle portion of Stikinia include the increased profusion of cognate inclusion and plagioclase megacrysts in volcanic rocks from the southern portion of the volcanic province, which might be evidence of magma ponding and magma crystallization in the lithosphere before a volcanic eruption, and the restricted existence of petrologically evolved rock types in the southern half of the Northern Cordilleran Volcanic Province.

Geographic entities mentioned:
surface_form: northern cordilleran volcanic province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
If the developed magmas originated from fractionation of mafic magmas, fractionation associated with lithospheric contamination, or entirely from melting of the associated lithosphere, their existence suggests more dense lithosphere lies under the southern portion of the Northern Cordilleran Volcanic Province.

Geographic entities mentioned:
surface_form: northern cordilleran volcanic province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
Analysis of recent data related to earthquakes in the southwestern portion of the volcanic province indicates that the crust under Stikinia, which comprises the bedrock underlying a large number of volcanoes in the southern portion of the Northern Cordilleran Volcanic Province, is also more dense than the crust under the nearby Coast Plutonic Complex, which consists of a broad belt of granitic and dioritic intrusive rocks that collectively represent more than 140 million years of nearly continuous subduction-related magmatism.

Geographic entities mentioned:
surface_form: northern cordilleran volcanic province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
Geological features. Hot springs are present throughout the Northern Cordilleran Volcanic Province, indicating magmatic heat is present under the Northern Cordilleran Volcanic Province. They are formed if water percolates deeply through the crust and heats up from the primal magmatic heat under the surface.

Geographic entities mentioned:
surface_form: northern cordilleran volcanic province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
surface_form: northern cordilleran volcanic province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
After the groundwater is heated, the heated groundwater rises to the surface as a hot spring. In some cases, the heated groundwater may rise along extensional faults related to rifting in the Northern Cordilleran Volcanic Province. The Lakelse Hot Springs near Lakelse Lake Provincial Park in northern British Columbia is interpreted to be one such example.

Geographic entities mentioned:
surface_form: northern cordilleran volcanic province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
Hot springs are also present in Iskut River Hot Springs Provincial Park and Choquette Hot Springs Provincial Park in northwestern British Columbia. Xenoliths, rock fragments that become enveloped in a larger igneous rock, are widespread in the Northern Cordilleran Volcanic Province. Xenoliths that originated in the Earth's crust include rich metamorphic rocks and felsic intrusive rocks.

Geographic entities mentioned:
surface_form: northern cordilleran volcanic province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
More than 14 volcanic zones throughout the Northern Cordilleran Volcanic Province comprise xenoliths that originated from the Earth's mantle and are located mainly at the Yukon–Tanana terrane, the Cache Creek terrane and at volcanoes occupying the Paleozoic and Mesozoic Stikinia terrane. They consist of lherzolite, harzburgite, wehrlite, dunite, websterite and garnet composed pyroxenite.

Geographic entities mentioned:
surface_form: northern cordilleran volcanic province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
At Castle Rock in northern British Columbia, mantle xenoliths record the maximum temperature of, as well as the maximum temperature range from. The minimum xenolith temperatures indicate that the boundary between the Earth's crust and mantle is shallowest beneath the northern portion of the Northern Cordilleran Volcanic Province.

Geographic entities mentioned:
surface_form: northern cordilleran volcanic province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
Therefore, the temperature ranges for the northernmost xenolith series is about one-half the temperature range found in xenoliths at the southern portion of the volcanic province. Megacrysts, crystals or grains that are considerably larger than the encircling matrix, are commonly found in lava flows throughout the Northern Cordilleran Volcanic Province.

Geographic entities mentioned:
surface_form: northern cordilleran volcanic province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
Megacrysts made of kaersutite are known to be found mainly at Llangorse Mountain in northern British Columbia. Black glassy clinopyroxene megacrysts are widespread throughout the Northern Cordilleran Volcanic Province, suggesting their creation is independent of lithosphere structure.

Geographic entities mentioned:
surface_form: northern cordilleran volcanic province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
Black glassy clinopyroxene megacrysts are widespread throughout the Northern Cordilleran Volcanic Province, suggesting their creation is independent of lithosphere structure. In contrast, clear glassy plagioclase megacrysts are found largely at the southern end of the Northern Cordilleran Volcanic Province and largely within the boundaries of the Stikinia terrane.

Geographic entities mentioned:
surface_form: northern cordilleran volcanic province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
Megacrysts made of plagioclase and clinopyroxene regionally show significant evidence of reaction with the associated magma, including sieve-textured cores and random, resorbed and embayed outer margins wherever they are located. Lava tubes are widespread in the Northern Cordilleran Volcanic Province, and are typically basaltic in composition. At Level Mountain, lava tubes reach diameters of to.

Geographic entities mentioned:
surface_form: northern cordilleran volcanic province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
Sections of these collapsed lava tubes now form volcanic pits. Extensive areas of nearly flat-lying lava flows throughout the Northern Cordilleran Volcanic Province can cover areas of at least and are generally composed of highly-fluid basaltic lava.

Geographic entities mentioned:
surface_form: northern cordilleran volcanic province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
For example, lava beds at least a million years old in central Yukon contain unconsolidated glacial deposits that were deposited when glacial ice rode on top of the lava flows comprising the lava beds. Subvolcanic intrusions in the Northern Cordilleran Volcanic Province are exposed in areas of high relief.

Geographic entities mentioned:
surface_form: northern cordilleran volcanic province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
Terranes and boundaries. The bedrock of the Northern Cordilleran Volcanic Province consists of four large terranes, known as Stikinia, Cache Creek, Yukon–Tanana and Cassiar. Stikinia is a sequence of late Paleozoic and Mesozoic aged volcanic, plutonic and sedimentary rocks interpreted to have been created in an island arc environment that were later placed along a pre-existing continental margin.

Geographic entities mentioned:
surface_form: northern cordilleran volcanic province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
The Yukon–Tanana and Cassiar terranes consist of shifted sedimentary and metamorphic rocks that were derived from the North American continent. The southern boundary of the Northern Cordilleran Volcanic Province is parallel with southwestern Stikinia and is characterized by separate volcanic vents and erosional remains of lavas south of the small community of Stewart.

Geographic entities mentioned:
surface_form: northern cordilleran volcanic province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
The southern boundary of the Northern Cordilleran Volcanic Province also parallels with a gap in modern volcanism and the supposed northern boundary of the Cascadia subduction zone, defined by the eastward extension of the northern edge of the subducting Juan de Fuca Plate.

Geographic entities mentioned:
surface_form: northern cordilleran volcanic province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
Tintina and Denali fault zones. The Tintina and Denali faults are the largest fault zones associated with the Northern Cordilleran Volcanic Province rift zone, with all volcanism occurring west of the Tintina Fault and east of the Denali Fault.

Geographic entities mentioned:
surface_form: northern cordilleran volcanic province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
Since the Cretaceous, the Tintina Fault has offset of the surface, although some evidence suggest as much as of offset. The offset caused the Northern Cordilleran Volcanic Province and the terrains of which the volcanic province occupies to move northwards.

Geographic entities mentioned:
surface_form: northern cordilleran volcanic province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
As more mapping and dating of volcanic deposits was completed in the Western Cordillera, the Stikine Volcanic Belt was expanded to include volcanic deposits further and further from the geographic area associated with the name Stikine. In part for this reason, scientists Ben Edwards and James Russell redefined this area of volcanism as the Northern Cordilleran Volcanic Province.

Geographic entities mentioned:
surface_form: northern cordilleran volcanic province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
A switch in relative plate motions at the Queen Charlotte Fault 10 million years ago produced consequent strain throughout the northern portion of the Western Cordillera, resulting in crustal thinning and decompression melting of oceanic island basalt-like mantle to create alkaline volcanism.

Geographic entities mentioned:
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
Terranes and boundaries. The bedrock of the Northern Cordilleran Volcanic Province consists of four large terranes, known as Stikinia, Cache Creek, Yukon–Tanana and Cassiar. Stikinia is a sequence of late Paleozoic and Mesozoic aged volcanic, plutonic and sedimentary rocks interpreted to have been created in an island arc environment that were later placed along a pre-existing continental margin.

Geographic entities mentioned:
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
This includes volcanic plugs found at the Mount Edziza volcanic complex, Level Mountain, Hoodoo Mountain and in the Atlin and Maitland areas. Volcanic plugs in the Atlin and Maitland areas consist of olivine nephelinite and basanite magmas. Minor plugs made of gabbroic and granitic magma are associated with volcanic stratigraphy at the Mount Edziza volcanic complex and Level Mountain.

Geographic entities mentioned:
surface_form: atlin
instance_of: Lake
countries: Canada
coordinates: lat: 60.0133333
lon: -133.8308333
At least four large volcanoes are grouped with the Northern Cordilleran Volcanic Province, including Hoodoo Mountain in the Boundary Ranges, the Mount Edziza volcanic complex on the Tahltan Highland, and Level Mountain and Heart Peaks on the Nahlin Plateau. These four volcanoes have volumes of more than, the largest and oldest which is Level Mountain with an area of and a volume of more than.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Lava tubes are widespread in the Northern Cordilleran Volcanic Province, and are typically basaltic in composition. At Level Mountain, lava tubes reach diameters of to. These owed their origin to highly fluid lavas with temperatures of at least.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The highest and lowest temperatures recorded by mantle xenoliths increase to the south and decrease to the north. Mantle xenoliths at Prindle Volcano in easternmost Alaska record the minimum temperature of and mantle xenoliths from the Fort Selkirk Volcanic Field in central Yukon record the minimum temperature range from.

Geographic entities mentioned:
surface_form: fort selkirk volcanic field
instance_of: Mountain
countries: Canada
coordinates: lat: 62.93
lon: -137.38
Gravel Island (Wisconsin). Gravel Island is an island in Lake Michigan. It is located in Ellison Bay, in the town of Liberty Grove, Wisconsin. The Gravel Island National Wildlife Refuge is made up of Gravel Island, and nearby Spider Island. The island is uninhabited, and a botanist who visited in 1999 was unable to find any vascular plants on the island.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Upon his return in the autumn of that year, de Queylus embarked on an ambitious program of missionary activity by the Sulpicians of the colony. He sent two priests to establish a mission among the Onondagas on Lake Ontario, aided the following year by François-Saturnin Lascaris d'Urfé. By 1670 there were three separate missions on the shores of the lake.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
He sent two priests to establish a mission among the Onondagas on Lake Ontario, aided the following year by François-Saturnin Lascaris d'Urfé. By 1670 there were three separate missions on the shores of the lake. At the same time, he sent two Sulpicians to evangelize the Odawa people in the Mississippi Valley. They traveled as far as Lake Erie, which they claimed in the name of France.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
The film is Khan's 249th film. The film grossed against a budget of. The filming wrapped up on March 1, 2024 with a climax scene featuring Shakib Khan and Mahiya Mahi in Sajek Valley, Rangamati. The film was theatrically released on 11 April 2024, coinciding with Eid al-Fitr, which was met with mixed to positive and didn’t perform well as expectations. Synopsis.

Geographic entities mentioned:
surface_form: Sajek Valley
instance_of: Valley
countries: Bangladesh
After a day's rest, the entire unit started shooting on February 5. On February 28, Shakib Khan and other crew members of the film returned to the country after filming for eighteen consecutive days in the United States. On the same day, he went to Sajek Valley, Rangamati to participate final lot of the filming, where some post-production work will be done, including patch work.

Geographic entities mentioned:
surface_form: Sajek Valley
instance_of: Valley
countries: Bangladesh
It was built over a period of nearly 400 years, with contributions from several rulers of the Mewar dynasty. Its construction began in 1553, started by Maharana Udai Singh II of the Sisodia Rajput family as he shifted his capital from the erstwhile Chittor to the newfound city of Udaipur. The palace is located on the east bank of Lake Pichola and has several palaces built within its complex.

Geographic entities mentioned:
surface_form: Lake Pichola
instance_of: Lake
countries: India
coordinates: lat: 24.572
lon: 73.679
Ajamaru Lakes rainbowfish. The Ajamaru Lakes rainbowfish (&quot;Melanotaenia ajamaruensis&quot;) is a species of rainbowfish in the Melanotaeniinae subfamily. It is endemic to the Ayamaru Lakes in West Papua, Indonesia.

Geographic entities mentioned:
surface_form: Ayamaru Lakes
instance_of: Group of lakes
countries: Indonesia
coordinates: lat: -1.26666667
lon: 132.2
Svitavsko Lake. Svitavsko Lake () is semi-artificial lake in Bosnia and Herzegovina, between village Svitava and Neretva river. The lake is a part of Hutovo Blato complex of marshes, lakes, underground karstic wellsprings and rivers, that form the &quot;Hutovo Blato&quot; Nature Park.

Geographic entities mentioned:
surface_form: svitavsko lake
instance_of: Lake
countries: Bosnia and Herzegovina
coordinates: lat: 43.024126
lon: 17.784023
Upper Truckee River. The Upper Truckee River is a stream that flows northward from the western slope of Red Lake Peak in Alpine County, California to Lake Tahoe via the Truckee Marsh in South Lake Tahoe, California. The river flows northeasterly and is long. It is Lake Tahoe's largest tributary. History.

Geographic entities mentioned:
surface_form: Red Lake Peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.7141
lon: -119.987
Tributaries include Angora, Echo, Grass Lake, and Big Meadow Creeks, and Upper and Lower Echo, Round, and Dardanelles Lakes. Major lakes include and smaller lakes include Dardanelles, Round, Showers, Elbert, Tamarack, Ralston, and Angora Lakes. The stretch between Meyers and South Lake Tahoe is known as Lake Valley.

Geographic entities mentioned:
surface_form: Angora Lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 38.864166666667
lon: -120.06666666667
A shamanic background is perceptible in several ancient myths featuring a horse, notably that of Pegasus (whose background is Asian), which symbolizes sublimated instinct and the wise man initiated through the ascent of Olympus, and that of Sleipnir.

Geographic entities mentioned:
surface_form: Olympus
instance_of: Mountain
countries: Greece
coordinates: lat: 40.083333333333336
lon: 22.35
Shasta County comprises the Redding, California metropolitan statistical area. The county occupies the northern reaches of the Sacramento Valley, with portions extending into the southern reaches of the Cascade Range. Points of interest in Shasta County include Shasta Lake, Lassen Peak, and the Sundial Bridge. Mount Shasta is in adjacent Siskiyou County to the north. History.

Geographic entities mentioned:
surface_form: Sacramento Valley
instance_of: Valley
countries: United States
coordinates: lat: 39
lon: -121.5
Shasta County comprises the Redding, California metropolitan statistical area. The county occupies the northern reaches of the Sacramento Valley, with portions extending into the southern reaches of the Cascade Range. Points of interest in Shasta County include Shasta Lake, Lassen Peak, and the Sundial Bridge. Mount Shasta is in adjacent Siskiyou County to the north. History.

Geographic entities mentioned:
surface_form: Lassen Peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.488055555555555
lon: -121.505
Shasta County comprises the Redding, California metropolitan statistical area. The county occupies the northern reaches of the Sacramento Valley, with portions extending into the southern reaches of the Cascade Range. Points of interest in Shasta County include Shasta Lake, Lassen Peak, and the Sundial Bridge. Mount Shasta is in adjacent Siskiyou County to the north. History.

Geographic entities mentioned:
surface_form: Mount Shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
History. Shasta County was one of the original counties of California, created in 1850 at the time of statehood. The county was named after Mount Shasta; the name is derived from the English equivalent for the Shasta people. Their population declined in the 1850s due to disease, low birth rates, starvation, killings, and massacres, as White settlers moved in.

Geographic entities mentioned:
surface_form: Mount Shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
One route operates to Burney via State Route 299. Amtrak's &quot;Coast Starlight&quot; serves Redding Station once a day in each direction. Amtrak Thruway provides twice daily service from Redding to/from Stockton or Sacramento for connections to the &quot;San Joaquins&quot;, which serve the San Francisco Bay Area, San Joaquin Valley and the Los Angeles area via rail and bus connections. Airports.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
Story. In 1964, the Czechoslovak State Security publicly claimed to have discovered Nazi-era intelligence files hidden beneath the surface of Černé jezero, a Czech Republic lake in the Šumava, on the border with West Germany. The four chests containing the papers were supposedly discovered during the making of a documentary in the presence of members of the Western press.

Geographic entities mentioned:
surface_form: Černé jezero
instance_of: Lake
countries: Czech Republic
coordinates: lat: 49.179166666667
lon: 13.1825
Kalousi. Kalousi () is a village in the municipality of Erymanthos, Achaea, Greece. It is located in a mountainous area of inland of north Peloponnese peninsula, north-northwest of mount Erymanthos. The village is 9 km south of Chalandritsa and 15 km by road.

Geographic entities mentioned:
surface_form: Erymanthos
instance_of: Mountain
countries: Greece
coordinates: lat: 37.852777777778
lon: 21.8225
Overview. The region of Apapa lies near the mouth of Lagos Lagoon, and contains ports and terminals for various commodities such as containers and bulk cargo, houses, offices and a small old disused railway station (Apapa North). It is the site of a major container terminal which was owned and operated by the Federal government of Nigeria until March 2005, and now is operated by the Danish firm A.

Geographic entities mentioned:
surface_form: Lagos Lagoon
instance_of: Lake
countries: Nigeria
coordinates: lat: 6.5015814
lon: 3.5224915
Middle Island gained an influx of Estonian refugees during the 1940s and 1950s mainly around the Pine Lake area. Geography. According to the United States Census Bureau, the CDP has a total area of, of which is land and, or 0.71%, is water. Middle Island has several lakes including Artist Lake, Pine Lake, and Spring Lake.

Geographic entities mentioned:
surface_form: Artist Lake
instance_of: Lake
countries: United States
coordinates: lat: 40.883888888889
lon: -72.931388888889
Azcapotzalco (altepetl). Azcapotzalco was a pre-Columbian Nahua &quot;altepetl&quot; (state), capital of the Tepanec empire, in the Valley of Mexico, on the western shore of Lake Texcoco. The name &quot;Azcapotzalco&quot; means &quot;at the anthill&quot; in Nahuatl. Its inhabitants were called &quot;Azcapotzalca&quot;.

Geographic entities mentioned:
surface_form: Valley of Mexico
instance_of: Valley
countries: Mexico
coordinates: lat: 19.66666667
lon: -98.86666667
surface_form: Lake Texcoco
instance_of: Lake
countries: Mexico
coordinates: lat: 19.5
lon: -98.99
The most famous ruler (&quot;tlatoani&quot;) of Azcapotzalco was Tezozomoctli. History. According to chronicler Fernando Alva Ixtlilxóchitl, the Tepanecs were a Chichimec group that settled in 1012 in the region west of Lake Texcoco. Their lineage began when their Acolhua leader (or Acolnahuacatl) married Xolotl's daughter Cuetlaxochitzin.

Geographic entities mentioned:
surface_form: Lake Texcoco
instance_of: Lake
countries: Mexico
coordinates: lat: 19.5
lon: -98.99
El Pilar de la Mola. El Pilar de la Mola is a village in Formentera, Balearic Islands, Spain. It lies on the La Mola peninsula, the highest point on the island, and has a good view of Formentera.

Geographic entities mentioned:
surface_form: La Mola
instance_of: Plateau
countries: Spain
coordinates: lat: 38.666666666666664
lon: 1.55
Pioneer Creek. Pioneer Creek is a tributary of Baker Creek in the U.S. state of Alaska. Other Baker tributaries in the vicinity include Eureka, Thanksgiving, and Gold Run. Geography. Pioneer Creek heads against the Baker-Minook divide, flows around the head of the Eureka, and then, at a distance of, flows parallel to the main course of that creek.

Geographic entities mentioned:
surface_form: Eureka
instance_of: Landform
countries: United States
coordinates: lat: 65.0922
lon: -150.285
The most well-known is probably the Mountain King, which is mentioned in the play &quot;Peer Gynt&quot; and its music by Edvard Grieg. The Norwegian name for Mountain King, &quot;Dovregubbe&quot;, is a compound word whose first part is used in the name for the mountain range Dovrefjell where the characters meet the final troll.

Geographic entities mentioned:
surface_form: Dovrefjell
instance_of: Mountain
countries: Norway
coordinates: lat: 62.1
lon: 9.41666667
Thorius boreas. &quot;Thorius boreas&quot;, commonly known as the boreal thorius, is a species of salamander in the family Plethodontidae. It is endemic to Oaxaca, Mexico, and only known from the Sierra Juárez. Its natural habitats are pine-oak and fir forests, often at forest edges.

Geographic entities mentioned:
surface_form: Sierra Juárez
instance_of: Mountain
countries: Mexico
coordinates: lat: 17.58333333
lon: -96.66666667
Black Rock Desert volcanic field. The Black Rock Desert volcanic field in Millard County, Utah, is a cluster of several volcanic features of the Great Basin including Pahvant Butte, The Cinders, and Tabernacle Hill. The field's Ice Springs event was an explosive eruption followed by lava flows that were Utah's most recent volcanic activity (1140–1440 AD).

Geographic entities mentioned:
surface_form: Tabernacle Hill
instance_of: Mountain
countries: United States
coordinates: lat: 38.91
lon: -112.53027777778
Gulf of Roses. The Gulf of Roses () is the most northeastern bay on the Catalan coast of Spain. The bay is wide and is formed by the valley of the Fluvià river but also contains the estuaries of the Manol and the Muga rivers. These rivers drain the southern flanks of the eastern end of the Pyrenees and Alberes. The area is often affected by the severe Tramuntana wind.

Geographic entities mentioned:
surface_form: Fluvià
instance_of: Watercourse
countries: Spain
coordinates: lat: 42.0934
lon: 2.4591
Lebanon is located in northwest Oregon, southeast of Salem. The population was 19,690 at the 2020 census. Lebanon sits beside the South Santiam River on the eastern edge of the Willamette Valley, close to the Cascade Range and a 25-minute drive to either of the larger cities of Corvallis and Albany. Lebanon is known for its foot-and-bike trails and its small-town character. 2010 census.

Geographic entities mentioned:
surface_form: Willamette Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.9
lon: -123.1
Its seat of administration was in the town Chalandritsa. Farres is situated in the centre of Achaea, on the upper courses of the rivers Peiros and Parapeiros. Towards the southeast (Mount Erymanthos) and northeast (Panachaiko) the terrain is increasingly mountainous. It is located about 15 km south of Patras and 30 km west of Kalavryta.

Geographic entities mentioned:
surface_form: Mount Erymanthos
instance_of: Mountain
countries: Greece
coordinates: lat: 37.852777777778
lon: 21.8225
surface_form: Panachaiko
instance_of: Mountain
countries: Greece
coordinates: lat: 38.2025
lon: 21.868888888889
In the summer of 1872, Christen Christensen, shopkeeper P.C.Pedersen, shopkeeper G.Wierød and Christen Lorentz Sørensen d.y. from Nordby built a steam sawmill at &quot;Svines&quot; by the lake Gogsjo. This came into the ownership of sheriff Bjørndal and Ole and Anders Skorges in the summer of 1916. This was named &quot;Gogsjø Dampsag&quot;.

Geographic entities mentioned:
surface_form: Gogsjo
instance_of: Lake
countries: Norway
coordinates: lat: 59.168055555556
lon: 10.1425
It is sometimes considered a suburb or small town within Panama City, northeast of the limits of the town of Balboa. Ancon Hill is also the name of a large hill that overlooks Panama City and once served as a form of protection from pirates and sea invasion. The township was originally located around this hill, and was created to house employees of the Panama Canal during its construction.

Geographic entities mentioned:
surface_form: Ancon Hill
instance_of: Mountain
countries: Panama
coordinates: lat: 8.9572777777778
lon: -79.549444444444
Sites of interest. The district of Ancón includes the Parque Natural Metropolitano, a vast jungle located a few minutes from the city, and its highest elevation, Ancon Hill. In its urban areas, you can visit several historical sites of the Panamanian capital, the building that houses the headquarters of the Panama Canal Authority, popularly known as the Administration Building.

Geographic entities mentioned:
surface_form: Ancon Hill
instance_of: Mountain
countries: Panama
coordinates: lat: 8.9572777777778
lon: -79.549444444444
Hill taught the Nimíipuu and later the neighboring Liksiyu about the loss of territorial sovereignty among Native Americans east of the Rocky Mountains to the expansionist United States of America. These stories incensed men from both Indigenous nations to mistrust ABCFM stations established on the Columbia Plateau. Henry H.

Geographic entities mentioned:
surface_form: Columbia Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 45.999444444444
lon: -119.00138888889
The state took over the maintenance of the road by the beginning of the 20th century. The former plank road and an extension south to Otisco Lake and southwest to Skaneateles Lake was first designated as Route 174 in the 1930 state highway renumbering. Since then, several minor realignments have been made in the areas of the villages of Marcellus and Camillus to accommodate newly built bypasses.

Geographic entities mentioned:
surface_form: Otisco Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.8652
lon: -76.2868
surface_form: Skaneateles Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.8625
lon: -76.372777777778
Route description. NY 174 begins its route through Onondaga County at an intersection with NY 41 in the hamlet of Borodino, on the shores of Skaneateles Lake. The road heads north, passing to the east of Hardscrabble Point, to an intersection with Eibert Road (County Route 131 or CR 131) where it turns east.

Geographic entities mentioned:
surface_form: Skaneateles Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.8625
lon: -76.372777777778
The road heads north, passing to the east of Hardscrabble Point, to an intersection with Eibert Road (County Route 131 or CR 131) where it turns east. The highway then heads eastward for about a mile (1.6 km) to a turn along the shore of Otisco Lake. It follows the shoreline of the lake northward into the town of Marcellus, soon entering the hamlet of Marietta.

Geographic entities mentioned:
surface_form: Otisco Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.8652
lon: -76.2868
The village of Marcellus was first settled in 1794 at the intersection of two transportation routes: an old Iroquois trail running east–west (later to become the Seneca Turnpike) and the north–south Nine Mile Creek. At the beginning of the 19th century, land travel along the Nine Mile Creek was very difficult and most travel between Marcellus and the settlements along Onondaga Lake was by water.

Geographic entities mentioned:
surface_form: Onondaga Lake
instance_of: Lake
countries: United States
coordinates: lat: 43.088888888889
lon: -76.208333333333
Gustavus Hamilton (c. 1739–16 December 1775) was an Irish miniature painter. Life and family. Gustavus Hamilton was born circa 1739. He was the son of Rev. Gustavus Hamilton, vicar of Errigal and rector of Gallon, County Meath and his wife Jane (née Cathcart). Hamilton was one of the couple's younger children. The Hamiltons claimed descent from the Hamiltons of Priestfield, Midlothian, Scotland.

Geographic entities mentioned:
surface_form: Errigal
instance_of: Mountain
countries: Ireland
coordinates: lat: 55.033
lon: -8.112
Sept Îles Lake (Saint-Raymond). The Lac Sept Îles (sometimes spelled &quot;Lac aux Sept-Isles&quot;) (English: Seven Islands Lake) is a body of water located in the township of Gosford, in the municipality of Saint-Raymond, in the Portneuf Regional County Municipality, in the administrative region of Capitale-Nationale, in Quebec, in Canada.

Geographic entities mentioned:
surface_form: sept îles lake (saint-raymond)
instance_of: Lake
countries: Canada
coordinates: lat: 46.933888888889
lon: -71.746666666667
Sept Îles Lake (Saint-Raymond). The Lac Sept Îles (sometimes spelled &quot;Lac aux Sept-Isles&quot;) (English: Seven Islands Lake) is a body of water located in the township of Gosford, in the municipality of Saint-Raymond, in the Portneuf Regional County Municipality, in the administrative region of Capitale-Nationale, in Quebec, in Canada.

Geographic entities mentioned:
surface_form: lac sept îles
instance_of: Lake
countries: Canada
coordinates: lat: 46.933888888889
lon: -71.746666666667
surface_form: lac sept îles
instance_of: Lake
countries: Canada
coordinates: lat: 46.8125
lon: -72.178333333333
During the 20th century, the perimeter of the lake was fitted out with numerous houses and chalets. The island of Genois, the largest and not accessible by road, has around twenty homes. The other islands contain some habitations. The toponym “Lac Sept Îles” was formalized on December 5, 1968, at the Bank of Place Names of the Commission de toponymie du Québec.

Geographic entities mentioned:
surface_form: lac sept îles
instance_of: Lake
countries: Canada
coordinates: lat: 46.933888888889
lon: -71.746666666667
surface_form: lac sept îles
instance_of: Lake
countries: Canada
coordinates: lat: 46.8125
lon: -72.178333333333
Thanks to its forest and mountain environment, its islands and bays, its proximity to Quebec city, and the Duchesnay tourist resort, the area around the lake is highly developed. A road completely surrounds the lake to serve residents and vacationers, an activity that dates to 1857–1858, compared to 1896 at Sergent Lake. Geography. The lake has several bays including Vachon Bay (to the southeast).

Geographic entities mentioned:
surface_form: sergent lake
instance_of: Lake
countries: Canada
coordinates: lat: 46.86555555555555
lon: -71.72222222222223
Thanks to its forest and mountain environment, its islands and bays, its proximity to Quebec city, and the Duchesnay tourist resort, the area around the lake is highly developed. A road completely surrounds the lake to serve residents and vacationers, an activity that dates to 1857–1858, compared to 1896 at Sergent Lake. Geography. The lake has several bays including Vachon Bay (to the southeast).

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Eriogonum prociduum. &quot;Eriogonum prociduum&quot; is a species of wild buckwheat known by the common name prostrate buckwheat. It is native to the western Great Basin of the United States in the region where Oregon meets California and Nevada, especially the Modoc Plateau, where it grows in exposed volcanic soils.

Geographic entities mentioned:
surface_form: Modoc Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 41.6
lon: -121.2
He invested in packet companies and steamboats that ran on the Mississippi River. In 1852, Dousman became a principal investor in the Madison & Prairie du Chien Railroad, a company formed to ensure that the larger Milwaukee & Mississippi Railroad would meet its goal of connecting Lake Michigan with the Mississippi River.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Arnold laid about 170 metres of track on his family property. The railway is in need of repair, and no longer in working condition. The locomotive and other equipment are stored on the island awaiting possible further use. There is a proposal to transfer the locomotive to the new narrow-gauge railway near Lake Wakatipu in New Zealand.

Geographic entities mentioned:
surface_form: Lake Wakatipu
instance_of: Lake
countries: New Zealand
coordinates: lat: -45.085
lon: 168.561
Oberreintalschrofen. Oberreintalschrofen (Upper Rhine Crag) is a mountain on the border of Bavaria, Germany and Tyrol, Austria. The first recorded ascent was by Hermann von Barth.

Geographic entities mentioned:
surface_form: oberreintalschrofen
instance_of: Mountain
countries: Germany
Austria
coordinates: lat: 47.395555555556
lon: 11.103888888889
Cut Hill. Cut Hill is a hill in North Dartmoor in the southwest English county of Devon. At 603 metres high, it is the joint third highest peak in Devon and Dartmoor, together with Hangingstone Hill, which lies around 4 kilometres to the northeast. The hill lies within the military training area on Dartmoor and is not accessible to the public except at certain times.

Geographic entities mentioned:
surface_form: cut hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 50.6275
lon: -3.9825
Stone row. In 2004, a stone row was discovered at Cut Hill dating to 3,500 BC and shedding new light on an area where there had hitherto been no evidence of prehistoric life. There are nine granite stones oriented in a northeast to southwest direction as at Stonehenge and they have been described by archaeologist, Dr Tom Greeves, as &quot;of worldwide significance.&quot;

Geographic entities mentioned:
surface_form: cut hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 50.6275
lon: -3.9825
With support from the Rwandan government, the Banyamulenge managed to fend off an attack by the Zairian Armed Forces. The rising tension between Rwanda and Zaire then led to an exchange of mortar fire over Lake Kivu between the two nations' armed forces. This violence involving the Banyamulenge in September–October 1996 is seen as the beginning of the First Congo War.

Geographic entities mentioned:
surface_form: Lake Kivu
instance_of: Lake
countries: Democratic Republic of the Congo
Rwanda
coordinates: lat: -1.8530555555556
lon: 29.135277777778
As each camp was destroyed, the refugees fled to the next, creating camps with massive populations. One camp at Mugungu, north of Lake Kivu, reached 500,000 inhabitants, which was completely unmanageable by humanitarian organizations. However, in fierce fighting in mid-November the Zairian government forces and RDR were either destroyed or forced out of the provinces of North and South Kivu.

Geographic entities mentioned:
surface_form: Lake Kivu
instance_of: Lake
countries: Democratic Republic of the Congo
Rwanda
coordinates: lat: -1.8530555555556
lon: 29.135277777778
In 1914, their next task would be to work on the construction for the Pacific Great Eastern Railway which was being built from Fort George south. Their new route would take them from Fort George to Soda Creek. The &quot;Operator&quot; and the &quot;Conveyor&quot; worked this route from May to August 1914, serving the new work camps and hauling supplies and equipment for rail construction.

Geographic entities mentioned:
surface_form: Soda Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.331944
lon: -122.280833
The main ranges are the Karakoram and the western Himalayas. The Pamir Mountains are to the north, and the Hindu Kush lies to the west. Amongst the highest mountains are K2 (Mount Godwin-Austen) and Nanga Parbat, the latter being one of the most feared mountains in the world. Known as the “Killer Mountain,” Nanga Parbat’s fatality rate is approximately 21 deaths per 100 successful summits.

Geographic entities mentioned:
surface_form: K2
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.881111111111
lon: 76.513333333333
surface_form: Nanga Parbat
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.239166666667
lon: 74.59
It is highest paved road in world is sometimes termed as the &quot;8th Wonder of World.&quot;
Major valleys. Gilgit Baltistan is home of world highest and beautiful valleys. These include Ghanche, Shiger, Astore Valley, Gilgit, Ghizer Valley, Hunza Valley, Skardu and Nagar Valley. Hunza Valley. Hunza Valley is considered one of the most beautiful valleys of Gilgit-Baltistan.

Geographic entities mentioned:
surface_form: Astore Valley
instance_of: Valley
countries: Pakistan
coordinates: lat: 35.03897222
lon: 75.11025278
surface_form: Ghizer Valley
instance_of: Valley
countries: Pakistan
coordinates: lat: 36.1573309
lon: 72.7381
surface_form: Hunza Valley
instance_of: Valley
countries: Pakistan
coordinates: lat: 36.31666667
lon: 74.65
surface_form: Nagar Valley
instance_of: Valley
countries: Pakistan
coordinates: lat: 35.4
lon: 73.8
These include Ghanche, Shiger, Astore Valley, Gilgit, Ghizer Valley, Hunza Valley, Skardu and Nagar Valley. Hunza Valley. Hunza Valley is considered one of the most beautiful valleys of Gilgit-Baltistan. It consists of Upper Hunza, Central Hunza, and Lower Hunza. Karimabad is the major city of the valley and has all facilities for mountaineers and tourists.

Geographic entities mentioned:
surface_form: Hunza Valley
instance_of: Valley
countries: Pakistan
coordinates: lat: 36.31666667
lon: 74.65
The popularity of the Hunza Valley and the amount of tourism there is due in part to its relative accessibility and proximity to the Karakoram Highway. Skardu Valley. Skardu Valley is located at confluence of Indus and Shiger rivers surrounded by the peaks of Karakoram. Eight-thousanders. Nanga Parbat
Gasherbrum l
Broad Peak
Gasherbrum ll
Seven-thousanders.

Geographic entities mentioned:
surface_form: Skardu Valley
instance_of: Valley
countries: Pakistan
coordinates: lat: 35.68
lon: 75.02694444
Skardu Valley. Skardu Valley is located at confluence of Indus and Shiger rivers surrounded by the peaks of Karakoram. Eight-thousanders. Nanga Parbat
Gasherbrum l
Broad Peak
Gasherbrum ll
Seven-thousanders. Gasherbrum lll
Gasherbrum lV
Saltoro Kangri (K10)

Geographic entities mentioned:
surface_form: Nanga Parbat
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.239166666667
lon: 74.59
surface_form: Gasherbrum l
instance_of: Mountain
countries: Pakistan
People's Republic of China
coordinates: lat: 35.724444444444
lon: 76.696388888889
surface_form: Broad Peak
instance_of: Mountain
countries: Pakistan
People's Republic of China
coordinates: lat: 35.810555555556
lon: 76.568055555556
surface_form: Gasherbrum ll
instance_of: Mountain
countries: Pakistan
People's Republic of China
coordinates: lat: 35.7575
lon: 76.652777777778
Skardu Valley. Skardu Valley is located at confluence of Indus and Shiger rivers surrounded by the peaks of Karakoram. Eight-thousanders. Nanga Parbat
Gasherbrum l
Broad Peak
Gasherbrum ll
Seven-thousanders. Gasherbrum lll
Gasherbrum lV
Saltoro Kangri (K10)

Geographic entities mentioned:
surface_form: Gasherbrum lll
instance_of: Mountain
countries: People's Republic of China
Pakistan
coordinates: lat: 35.759444444444
lon: 76.641944444444
surface_form: Gasherbrum lV
instance_of: Mountain
countries: People's Republic of China
Pakistan
coordinates: lat: 35.759166666667
lon: 76.615833333333
surface_form: Saltoro Kangri (K10)
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.399578333333
lon: 76.847516666667