Sarmila/GeoWiki-Features huggingface dataset:
Established in 1993, it is one of the 23 National Biodiversity Conservation Areas of Laos. Dong Ampham is home to &quot;some of the last intact areas of lowland and tropical forests remaining in mainland Southeast Asia.&quot; Topographical features include the Xe Kaman and Xe Xou Rivers, and the volcanic lake Nong Fa Lake. Tigers and Clouded leopard have been recorded here.

Geographic entities mentioned:
surface_form: Nong Fa Lake
instance_of: Lake
countries: Laos
coordinates: lat: 15.1075
lon: 107.42444444
Saskatchewan Highway 910. Highway 910 is a provincial highway in the north-west region of the Canadian province of Saskatchewan. It runs from Highway 165 until it transitions into the access road at Besnard Lake for Besnard Lake Recreation Site. Highway 910 was completed in 1973 and is about long.

Geographic entities mentioned:
surface_form: Besnard Lake
instance_of: Lake
countries: Canada
coordinates: lat: 55.41673
lon: -106.0005
She died of stomach cancer on September 2, 2016. Personal life. A native of Appenzell, Switzerland, Margrit Kellenberger was raised in her family home overlooking Lake Maggiore, in the canton of Ticino. By the end of World War II, Margrit met Capt. Philip Biever, a United States Army captain.

Geographic entities mentioned:
surface_form: Lake Maggiore
instance_of: Lake
countries: Switzerland
Italy
coordinates: lat: 46.098055555555554
lon: 8.714722222222223
Vijayalaya Chola. Vijayalaya Chola (;) founded the Imperial Chola Empire. He ruled over the region to the north of the river Kaveri. He is one of the descendants of the famous Sangam age Chola king, Karikala Chola. Vijayalaya was succeeded by his son Aditya Chola I who laid the foundation of the Imperial Chola Empire. Dark age of Chola.

Geographic entities mentioned:
surface_form: Kaveri
instance_of: Watercourse
countries: India
coordinates: lat: 11.370345
lon: 79.828105
It is considered by some to straddle the southern edge of the Cariboo country of British Columbia, although others consider Ashcroft-Cache Creek, Lillooet, Savona, Kamloops and even Lytton and Spences Bridge to be in the Cariboo. Clinton, however, does sit immediately below the southern edge of the Cariboo Plateau.

Geographic entities mentioned:
surface_form: Cariboo Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 50.81652
lon: -118.81904
Highway 97 runs through the village north-south, meeting just south of downtown with the Pavilion Mountain Road, which connects from Pavilion and Kelly Lake and is the route of the Old Cariboo Road and follows what is known as Cut-Off Valley from the foot of the road over Pavilion Mountain, which is also the route used by the British Columbia Railway although that route does not traverse Pavilion Mountain but comes via the Fraser Canyon via Moran and Arden Forest.

Geographic entities mentioned:
surface_form: Pavilion Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.9833
lon: -121.683
Also diverging from Highway 97 at Clinton is the route of the original Cariboo Road, which climbs a gentler grade up the side of the Bonaparte River valley up to the Cariboo Plateau, via Chasm and the associated provincial park and the community of Lone Butte.

Geographic entities mentioned:
surface_form: Cariboo Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 50.81652
lon: -118.81904
Machia Biological Park. Machia Biological Park (also known as Machia Safari Park) is a zoological garden and wildlife conservation facility located near Kaylana Lake, approximately 7–8 km west of Jodhpur in Rajasthan, India. Established on 41 hectares of protected forest land, the park opened to the public on 20 January 2016.

Geographic entities mentioned:
surface_form: Kaylana Lake
instance_of: Lake
countries: India
coordinates: lat: 26.2975
lon: 72.97111111111111
Mark died of natural causes on 7 October and was buried in the catacomb of Balbina. In 1048, his remains were removed to the town of Velletri, and in 1145 were relocated to the Basilica of San Marco in Rome, where they are kept in an urn under the altar. His feast day is celebrated on 7 October. He is particularly venerated at the Abbadia San Salvatore at Monte Amiata.

Geographic entities mentioned:
surface_form: Monte Amiata
instance_of: Mountain
countries: Italy
coordinates: lat: 42.88775
lon: 11.624369444444
In 1917 the regiment operated in the Val Posina until it was transferred in July to the Banjšice plateau where the regiment fought in August 1917 in the Eleventh Battle of the Isonzo in the area of Kal nad Kanalom. In October 1917 the regiment fought in the Battle of Caporetto.

Geographic entities mentioned:
surface_form: Banjšice plateau
instance_of: Plateau
countries: Slovenia
coordinates: lat: 46.04905
lon: 13.69995
In October 1917 the regiment fought in the Battle of Caporetto. In June 1918 the Brigade &quot;Roma&quot; fought in the Second Battle of the Piave River at Monastier and in October the brigade was deployed on Monte Grappa, where it fought in the decisive Battle of Vittorio Veneto.

Geographic entities mentioned:
surface_form: Monte Grappa
instance_of: Mountain
countries: Italy
coordinates: lat: 45.873333333333
lon: 11.799166666667
Redondo Peak (Tewa: &quot;Tsiku'mup'in&quot;) is a conspicuous summit in the Jemez Mountains of New Mexico, in the southwestern United States. It is located entirely within the Valles Caldera National Preserve. It is the second highest summit in the Jemez after Chicoma Mountain. It is the most visually prominent peak in the range when viewed from the south, for example, from Albuquerque.

Geographic entities mentioned:
surface_form: Chicoma Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.007336111111
lon: -106.38455277778
surface_form: chicoma mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.007336111111
lon: -106.38455277778
It is the most visually prominent peak in the range when viewed from the south, for example, from Albuquerque. From many other directions it is less prominent or not visible, due to its location in the center of the Valles Caldera, well away from the caldera's rim. Redondo Peak is an example of the volcanic feature known as a resurgent dome.

Geographic entities mentioned:
surface_form: Valles Caldera
instance_of: Mountain
countries: United States
coordinates: lat: 35.866666666667
lon: -106.56666666667
surface_form: valles caldera
instance_of: Mountain
countries: United States
coordinates: lat: 35.866666666667
lon: -106.56666666667
Redondo Peak. Redondo Peak (Tewa: &quot;Tsiku'mup'in&quot;) is a conspicuous summit in the Jemez Mountains of New Mexico, in the southwestern United States. It is located entirely within the Valles Caldera National Preserve. It is the second highest summit in the Jemez after Chicoma Mountain.

Geographic entities mentioned:
surface_form: redondo peak
instance_of: Mountain
countries: United States
coordinates: lat: 35.871963888889
lon: -106.56057777778
Redondo Peak. Redondo Peak (Tewa: &quot;Tsiku'mup'in&quot;) is a conspicuous summit in the Jemez Mountains of New Mexico, in the southwestern United States. It is located entirely within the Valles Caldera National Preserve. It is the second highest summit in the Jemez after Chicoma Mountain.

Geographic entities mentioned:
surface_form: valles caldera
instance_of: Mountain
countries: United States
coordinates: lat: 35.866666666667
lon: -106.56666666667
Cullaby Lake. Cullaby Lake is a lake near Warrenton, Oregon, United States. It is the central feature of Cullaby Lake County Park, and one of the major lakes of Clatsop Plains. Cullaby Lake's main water inflow is Cullaby Creek which flows in from the south and drains the coastal hills to the east of Clatsop Plains, Gearhart and Seaside.

Geographic entities mentioned:
surface_form: cullaby lake
instance_of: Lake
countries: United States
coordinates: lat: 46.084
lon: -123.903
Geological studies have been conducted at the volcano since at least the 1960s, but its very remote location has impeded detailed fieldwork. As a result, the eruptive history of the caldera is poorly known and its affinity to the Garibaldi Volcanic Belt remains unclear.

Geographic entities mentioned:
surface_form: Garibaldi Volcanic Belt
instance_of: Mountain
countries: Canada
coordinates: lat: 51.5283
lon: -126.113
It lies in a rugged, ice-dominated portion of the Pacific Ranges which are the southernmost subdivision of the Coast Mountains. The surrounding mountains are the highest in British Columbia south of the Saint Elias Mountains; Mount Waddington northeast of the head of Knight Inlet has an elevation of and is the highest mountain entirely within British Columbia.

Geographic entities mentioned:
surface_form: Mount Waddington
instance_of: Mountain
countries: Canada
coordinates: lat: 51.373611111111
lon: -125.26333333333
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
Charnaud Creek originates from a valley-filling lava flow adjacent to the southeastern boundary of the caldera and flows southwest into the Kingcome River. At the terminus of Pashleth Glacier in the northern part of the caldera is Pashleth Creek; it flows northwest into the Machmell River which flows west into Owikeno Lake at the head of Rivers Inlet.

Geographic entities mentioned:
surface_form: Owikeno Lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.683333333333
lon: -126.91666666667
The relationship of the Silverthrone Caldera to other volcanoes in southwestern British Columbia remains unclear due to there having been very little geological studies conducted at the caldera. It has been considered to be part of the Garibaldi Volcanic Belt, but it lies west-northwest of the main portion of this volcanic zone, making its connection to the Garibaldi Volcanic Belt questionable.

Geographic entities mentioned:
surface_form: Garibaldi Volcanic Belt
instance_of: Mountain
countries: Canada
coordinates: lat: 51.5283
lon: -126.113
It has been considered to be part of the Garibaldi Volcanic Belt, but it lies west-northwest of the main portion of this volcanic zone, making its connection to the Garibaldi Volcanic Belt questionable. The volcano has also been included as part of the much older Pemberton Volcanic Belt, which overlaps with the trend of the Garibaldi Volcanic Belt near Meager Creek to the southeast.

Geographic entities mentioned:
surface_form: Pemberton Volcanic Belt
instance_of: Mountain
countries: Canada
coordinates: lat: 50.58051944
lon: -122.93235278
Likewise, the lifespan of the caldera is comparable to most of the large evolved eruptive centres in the Cascade Volcanic Arc, which have lifespans ranging from 100,000 to 1,000,000 years. Silverthrone and its closest prominent neighbour, the Franklin Glacier Complex about to the east-southeast, are sometimes excluded from the Garibaldi Volcanic Belt due to their ambiguous affinity.

Geographic entities mentioned:
surface_form: Franklin Glacier Complex
instance_of: Mountain
countries: Canada
coordinates: lat: 51.3333
lon: -125.4
The tectonic settings of the Silverthrone and Franklin Glacier complexes appear to differ from other volcanoes in the Garibaldi Volcanic Belt. The main portion of this volcanic belt, which extends from the Salal Glacier volcanic complex in the north to the Watts Point volcanic centre in the south, is the result of subduction of the Juan de Fuca Plate beneath the North American Plate.

Geographic entities mentioned:
surface_form: Salal Glacier volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 50.79
lon: -123.38
surface_form: Watts Point volcanic centre
instance_of: Mountain
countries: Canada
coordinates: lat: 49.65
lon: -123.21
surface_form: watts point volcanic centre
instance_of: Mountain
countries: Canada
coordinates: lat: 49.65
lon: -123.21
The lack of detailed geothermal analysis for the Silverthrone Caldera is due to its very remote location and the lack of electrical development at the volcano. As a result, geothermal exploration at the volcano is less favourable than elsewhere in British Columbia such as at Mount Cayley, Mount Garibaldi and Mount Meager.

Geographic entities mentioned:
surface_form: Mount Garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
Based on the volume of the silicious volcanic rocks found at Silverthrone, its geothermal power potential is 2,000 megawatts, which is comparable to that for the Mount Edziza region but greater than those for Mount Cayley and Meager Creek combined.

Geographic entities mentioned:
surface_form: Mount Edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
This makes the caldera one of several volcanoes in British Columbia with known obsidian source material often found at archaeological sites throughout the province; others include Mount Garibaldi, Anahim Peak, the Ilgachuz Range and the Mount Edziza volcanic complex.

Geographic entities mentioned:
surface_form: Anahim Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 52.7578
lon: -125.625
surface_form: Mount Edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
surface_form: mount edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
The youngest lava flows occupying the local valleys were said to be probably no older than Early Pleistocene age. The other eruptive centres visited by Jack Souther in 1967 were the Mount Edziza volcanic complex in the Northern Cordilleran Volcanic Province and the Rainbow, Ilgachuz and Itcha ranges in the Anahim Volcanic Belt.

Geographic entities mentioned:
surface_form: Northern Cordilleran Volcanic Province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
surface_form: Anahim Volcanic Belt
instance_of: Mountain
countries: Canada
coordinates: lat: 52.666666666666664
lon: -125.83333333333333
surface_form: mount edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
The flying times from Tatlayoko Lake and Campbell River are about one and two hours, respectively. A much more difficult way to access Silverthrone is to traverse one of the several intermontane valleys on foot, which can be reached from the British Columbia Coast or the Interior Plateau. The icefields of the Silverthrone area can be trekked on foot from the adjoining valleys.

Geographic entities mentioned:
surface_form: Interior Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 52
lon: -123
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
Silverthrone Caldera. The Silverthrone Caldera is a potentially active volcano in Range 2 Coast Land District of southwestern British Columbia, Canada. It lies within the Pacific Ranges of the Coast Mountains and reaches an elevation of, although some sources give the elevation as high as. The caldera is about wide and has been deeply eroded, resulting in the formation of rugged topography.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: silverthrone caldera
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4333
lon: -126.3
Location and climate. The volcano is north of Kingcome Inlet and northwest of Knight Inlet in southwestern British Columbia, Canada. It lies in a rugged, ice-dominated portion of the Pacific Ranges which are the southernmost subdivision of the Coast Mountains.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
Moist air originating from the Pacific Ocean ascends over Queen Charlotte Sound, Queen Charlotte Strait or the Vancouver Island Ranges before reaching the Pacific Ranges. While ascending the Pacific Ranges, this air comes in contact with cold air from the British Columbia Interior and drops significant precipitation in the form of heavy rains or snow.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
Tectonic setting. The relationship of the Silverthrone Caldera to other volcanoes in southwestern British Columbia remains unclear due to there having been very little geological studies conducted at the caldera.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: silverthrone caldera
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4333
lon: -126.3
Their extreme explosivity is caused by silica-rich magma which cools on the land surface in the form of volcanic rocks such as dacite and rhyolite. Reconnaissance mapping of volcanic rocks associated with the Silverthrone Caldera prior to 1980 indicates it is one of the largest centres of Quaternary felsic volcanism in British Columbia.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: silverthrone caldera
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4333
lon: -126.3
Artifacts made of Kingcome obsidian have been found at archaeological sites in the Sunshine Coast region, which was the location of trading between indigenous peoples about 5,000–2,000 years ago. Obsidian from Mount Garibaldi occurs with the Kingcome obsidian in this part of British Columbia, as does obsidian from Whitewater Ridge and Gregory Creek in the U.S. state of Oregon.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
A report of the British Columbia Prospectors Assistance Program listed copper and gemstones as commodities in the breccia pipe. Conservation. Part of Silverthrone lies in the Catto Creek Conservancy, a conservation area in Range 2 Coast Land District established on August 23, 1973, under the Protected Areas of British Columbia Act.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
The review noted that although the volcano scores highly for primary volcanic hazard factors, it has a relatively low exposure score due to its very remote location. Therefore, the review gave Silverthrone a lower hazard rating than for Mount Edziza, Mount Price, Mount Cayley, Mount Meager and Mount Garibaldi, which were rated as &quot;high&quot; and &quot;very high&quot; threat volcanoes.

Geographic entities mentioned:
surface_form: mount price
instance_of: Mountain
countries: Canada
coordinates: lat: 49.9175
lon: -123.03555555555556
Silverthrone Caldera. The Silverthrone Caldera is a potentially active volcano in Range 2 Coast Land District of southwestern British Columbia, Canada. It lies within the Pacific Ranges of the Coast Mountains and reaches an elevation of, although some sources give the elevation as high as. The caldera is about wide and has been deeply eroded, resulting in the formation of rugged topography.

Geographic entities mentioned:
surface_form: silverthrone caldera
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4333
lon: -126.3
Several glacial meltwater streams originating from the caldera flow through valleys in the Pacific Ranges; among these streams are the Pashleth, Selman and Catto creeks and the Kingcome and Wakeman rivers. Volcanic rocks deposited by eruptions of the Silverthrone Caldera and associated vents include rhyolites, dacites, andesites and basaltic andesites.

Geographic entities mentioned:
surface_form: silverthrone caldera
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4333
lon: -126.3
The caldera mainly poses a threat to air traffic from renewed explosive eruptions, but lahars or debris flows could also be produced from the melting of glacial ice. The Silverthrone Caldera was a source of obsidian for indigenous peoples during the pre-contact era and was studied in the 1970s as a potential source of geothermal energy.

Geographic entities mentioned:
surface_form: silverthrone caldera
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4333
lon: -126.3
Names and etymology. The Silverthrone Caldera has also been described as the Silverthrone Caldera Complex and the Silverthrone Depression. Other terms, such as the Silverthrone volcanic complex and the Silverthrone volcanic field, refer to the caldera and associated volcanic rocks.

Geographic entities mentioned:
surface_form: silverthrone caldera
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4333
lon: -126.3
surface_form: silverthrone caldera
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4333
lon: -126.3
In addition to Silverthrone Mountain, the Silverthrone Caldera also shares its name with Silverthrone Glacier, an outlet glacier of the local Ha-Iltzuk Icefield which covers approximately of the southern Coast Mountains.

Geographic entities mentioned:
surface_form: silverthrone caldera
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4333
lon: -126.3
Alpine vegetation is restricted to a narrow band between the subalpine forests and the higher icefields. There are no settlements near the Silverthrone Caldera, although summer sport fishing recreation camps and logging operations have been in the area. Drainage.

Geographic entities mentioned:
surface_form: silverthrone caldera
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4333
lon: -126.3
Drainage. From Kingcome Glacier in the southern part of the caldera, the Kingcome River flows south into the head of Kingcome Inlet northeast of Broughton Island. Trudel Creek, a tributary of the Kingcome River, originates from the head of Trudel Glacier and flows southwest along the inferred southeastern boundary of the Silverthrone Caldera.

Geographic entities mentioned:
surface_form: silverthrone caldera
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4333
lon: -126.3
At the terminus of Pashleth Glacier in the northern part of the caldera is Pashleth Creek; it flows northwest into the Machmell River which flows west into Owikeno Lake at the head of Rivers Inlet. Selman Creek, a tributary of Pashleth Creek, flows to the northeast from Selman Lake at the northwestern end of the Silverthrone Caldera.

Geographic entities mentioned:
surface_form: silverthrone caldera
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4333
lon: -126.3
Both volcanic belts were formed by subduction zone volcanism along the continental margin of western North America in the last 29 million years and are part of the Cascade Volcanic Arc. The types of volcanic rocks at the Silverthrone Caldera are comparable to those found in continental arcs; they belong to the calc-alkaline magma series.

Geographic entities mentioned:
surface_form: silverthrone caldera
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4333
lon: -126.3
Further studies of the magmatic products of the Silverthrone and Franklin Glacier complexes are required to provide additional insights on mantle and slab processes. The Smithsonian Institution's Global Volcanism Program lists the tectonic setting of the Silverthrone Caldera as a subduction zone and the underlying continental crust more than thick.

Geographic entities mentioned:
surface_form: silverthrone caldera
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4333
lon: -126.3
Reconnaissance mapping of volcanic rocks associated with the Silverthrone Caldera prior to 1980 indicates it is one of the largest centres of Quaternary felsic volcanism in British Columbia. The inferred boundaries of the Silverthrone Caldera are exposed to the south and west whereas the northern and eastern boundaries are buried under volcanic deposits and glacial ice, respectively.

Geographic entities mentioned:
surface_form: silverthrone caldera
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4333
lon: -126.3
Unlike the neighbouring Franklin Glacier Complex whose volcanic rocks have been mostly eroded away to expose underlying subvolcanic intrusions, the Silverthrone Caldera still possesses mainly volcanic rocks. The main volcanic rocks at the caldera are rhyolites, dacites, andesites and basaltic andesites which comprise breccias, lava domes, lava flows and volcanic cones.

Geographic entities mentioned:
surface_form: silverthrone caldera
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4333
lon: -126.3
The volcanic deposits extend over a distance of more than and vary in elevation from near sea level to or. They have a volume of at least twice as much as that of the Mount Meager complex, which consists of of volcanic rocks. Underlying the eruptive products of the Silverthrone Caldera are older rocks of the Coast Plutonic Complex.

Geographic entities mentioned:
surface_form: silverthrone caldera
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4333
lon: -126.3
No flow rates for the local springs have been reported and the heat exchange potential remains unknown. At least one spring with a recorded temperature of possibly occurs along a ring fault associated with the collapse of the Silverthrone Caldera. As of 2016, the only geothermal exploration conducted at Silverthrone has been geological mapping.

Geographic entities mentioned:
surface_form: silverthrone caldera
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4333
lon: -126.3
As of 2016, the only geothermal exploration conducted at Silverthrone has been geological mapping. The lack of detailed geothermal analysis for the Silverthrone Caldera is due to its very remote location and the lack of electrical development at the volcano.

Geographic entities mentioned:
surface_form: silverthrone caldera
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4333
lon: -126.3
Eruptive history. The eruptive history of the Silverthrone Caldera is poorly known due to limited geological studies but it is probably similar in age to those of other volcanoes in the Garibaldi Volcanic Belt. Three stages of volcanic activity have been identified at the caldera, each of which have been radiometrically dated.

Geographic entities mentioned:
surface_form: silverthrone caldera
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4333
lon: -126.3
Three stages of volcanic activity have been identified at the caldera, each of which have been radiometrically dated. Most of the volcanic deposits inside the Silverthrone Caldera appear to have been erupted between 100,000 and 900,000 years ago during the Pleistocene epoch.

Geographic entities mentioned:
surface_form: silverthrone caldera
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4333
lon: -126.3
According to the Smithsonian Institution's Global Volcanism Program, the last eruption of the Silverthrone Caldera is unknown, but there is credible evidence for the caldera having been active during the current Holocene epoch, which began about 11,700 years ago.

Geographic entities mentioned:
surface_form: silverthrone caldera
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4333
lon: -126.3
Small magnitude, shallow earthquakes have been recorded near Silverthrone since 1980, but because this seismicity is not demonstrably magmatic in origin, the volcano was given a score of 0.5 on a scale of 0 to 1 for observed seismic unrest. Nevertheless, the presence of seismicity suggests the Silverthrone Caldera is potentially active and its volcanic hazards may be significant.

Geographic entities mentioned:
surface_form: silverthrone caldera
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4333
lon: -126.3
It may sense an increase in seismic activity if the Silverthrone Caldera becomes highly restless, but this may only provide a warning for a large eruption; the system might detect activity only once the volcano has started erupting. If the Silverthrone Caldera were to erupt, mechanisms exist to orchestrate relief efforts.

Geographic entities mentioned:
surface_form: silverthrone caldera
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4333
lon: -126.3
Mejia &quot;et al.&quot; (2002) sampled basaltic andesite flows from Silverthrone and obtained 16 potassium–argon dates. Most of these dates indicated the lava flows were extruded sometime in the last 120,000 years, but two of the potassium–argon dates gave ages as old as 400,000 years. As of 2023, the remoteness of the Silverthrone Caldera has impeded detailed fieldwork. Mineral exploration.

Geographic entities mentioned:
surface_form: silverthrone caldera
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4333
lon: -126.3
Lackawanna was a center of steel manufacture throughout most of the 20th century. In 1899, the Lackawanna Steel Company, based in Scranton, Pennsylvania since its founding, purchased all the land along the West Seneca shore of Lake Erie. Construction was started in 1900 and the Lackawanna Steel Company relocated to the area in 1902. The plant began operations in 1903.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Geography. The city has an area of, of which, or 0.75%, is water. Lackawanna sits on Lake Erie, although the Bethlehem Steel facility's remnants occupy the waterfront. Smokes Creek (named after Seneca Indian Chief Sayenqueraghta who was nicknamed &quot;Old Smoke&quot;) runs through the city before it discharges into Lake Erie. Abbott Road is a major road that runs north–south through the city.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
In 1907 he moved to the University of Vienna where he succeeded Gustav Tschermak. He worked there until his retirement in 1922. Doelter's work involved travel in the early years and was involved in a survey of the Pontine Islands (1874), Monte Ferro and Cape Verde (1880-1881), and he described his observations and experiences in his 1884 travelogue.

Geographic entities mentioned:
surface_form: Monte Ferro
instance_of: Mountain
countries: Italy
coordinates: lat: 46.583889
lon: 12.669167
This rig was called the Grand Haven Rig or (Jack Ass Rig)...&quot; It was said to have been the result of a serendipity, when the master of a three-masted schooner had its mainmast removed due to rot, and found how well the ship sailed. There &quot;were at least a dozen craft with this rig many of them in Lake Michigan.&quot; Similar rigs might be called a &quot;jackass schooner.&quot;

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Mughal conquest of Golconda. With death of Shivaji in 1680, Maratha power in the Deccan began to decline and the Mughal Emperor Aurangzeb lead a huge expedition to the South to recover lost territories. In 1686, Aurangazeb's son Muazzam launched an invasion of Golconda culminating in the siege and the eventual conquest of the capital in September 1687.

Geographic entities mentioned:
surface_form: Deccan
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
Connecting Slough. Connecting Slough, the former slough between Kern Lake and Buena Vista Lake in the southeastern San Joaquin Valley, in Kern County, California. It was part of the Tulare Lake Basin and Kern River system, before agricultural diversions by the Central Valley Project. It was a tributary of the San Joaquin River until the latter 19th century.

Geographic entities mentioned:
surface_form: Buena Vista Lake
instance_of: Lake
countries: United States
coordinates: lat: 35.1919
lon: -119.295
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
Erynnis marloyi. &quot;Erynnis marloyi&quot;, commonly known as the inky skipper, is a species of butterfly in the family Hesperiidae. It is found in south-eastern Europe (Greece and the Balkans) across Asia Minor to Syria, Turkey, Lebanon, southern Iran and Chitral, Pakistan. The wingspan is 14–15 mm for males and 15–16 mm for females. Description in Seitz. &quot;Th. marloyi&quot; Bdv.

Geographic entities mentioned:
surface_form: Chitral
instance_of: Valley
countries: Pakistan
coordinates: lat: 35.85111111111111
lon: 71.78888888888889
Valery Tobias. Valery Tobias (born 24 September 2000) is an American middle-distance runner. She was runner-up at the 2025 USA Indoor Track and Field Championships over 800 metres. Early life. From Lower Rio Grande Valley in Texas, she attended Edinburg IDEA Quest. Career.

Geographic entities mentioned:
surface_form: Lower Rio Grande Valley
instance_of: Valley
countries: United States
Mexico
coordinates: lat: 26.22
lon: -98.12
Phou Pha Thi. Phou Pha Thi (Phathi) is a &quot;sacred mountain&quot; in Laos &quot;believed...inhabited by great &quot;phi&quot;, or spirits and used for the clandestine Lima Site 85 military installation during the Vietnam War. The lightly defended installation was destroyed by North Vietnamese attackers in the 10-11 March 1968 Battle of Lima Site 85.

Geographic entities mentioned:
surface_form: phou pha thi
instance_of: Mountain
countries: Laos
coordinates: lat: 20.468
lon: 103.7058
Deputy Mineral Surveyor in Nevada. Her artistic inspiration by the Santa Clara Valley ultimately contributed to that region becoming the technological hub known as Silicon Valley. After studying drawing and mathematics at Stanford University, she joined her father in Tonopah, Nevada, where the two established a mining engineering firm.

Geographic entities mentioned:
surface_form: Santa Clara Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.366944444444
lon: -121.98388888889
He would later theorize the semiconductor and become one of the co-inventors of the transistor while at Bell Labs, the latter leading to his winning the Nobel Prize in Physics. May Bradford Shockley was artistically inspired by the Santa Clara Valley, and she retired to Palo Alto after a period living in Hollywood following her husband's death.

Geographic entities mentioned:
surface_form: Santa Clara Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.366944444444
lon: -121.98388888889
Mitchell River silt jetties. The Mitchell River silt jetties are an unusually long, thin landform in the Gippsland Lakes region in Victoria, Australia. A type of digitate delta, they have been formed over thousands of years by sediment deposition from the Mitchell River during periods of low water flow and subsequent wash-through during periods of high water flow.

Geographic entities mentioned:
surface_form: Gippsland Lakes
instance_of: Group of lakes
countries: Australia
coordinates: lat: -38
lon: 147.65
Mount Liptak. Mount Liptak () is a mountain, high with twin summits, located southeast of Mount Craddock in the Sentinel Range of the Ellsworth Mountains in Antarctica. It surmounts Bolgrad Glacier to the west and Kornicker Glacier to the east. It was first mapped by the United States Geological Survey from surveys and U.S.

Geographic entities mentioned:
surface_form: Mount Craddock
instance_of: Mountain
coordinates: lat: -78.633333333333
lon: -85.2
surface_form: craddock
instance_of: Mountain
coordinates: lat: -78.633333333333
lon: -85.2
surface_form: liptak
instance_of: Mountain
coordinates: lat: -78.75
lon: -84.9
surface_form: mount liptak
instance_of: Mountain
coordinates: lat: -78.75
lon: -84.9
Navy air photos from 1957 to 1959, and was named by the Advisory Committee on Antarctic Names for L.H. Liptak, an aviation machinist mate in the U.S. Navy who served as plane captain on the first reconnaissance flights to this vicinity in January 1958. Mount Liptak was first successfully climbed on December 28, 2012, by Pachi Ibarra, Ralf Laier and Todd Passey.

Geographic entities mentioned:
surface_form: todd
instance_of: Mountain
coordinates: lat: -78.0942
lon: -85.8775
surface_form: liptak
instance_of: Mountain
coordinates: lat: -78.75
lon: -84.9
surface_form: mount liptak
instance_of: Mountain
coordinates: lat: -78.75
lon: -84.9
Mount Liptak. Mount Liptak () is a mountain, high with twin summits, located southeast of Mount Craddock in the Sentinel Range of the Ellsworth Mountains in Antarctica. It surmounts Bolgrad Glacier to the west and Kornicker Glacier to the east. It was first mapped by the United States Geological Survey from surveys and U.S.

Geographic entities mentioned:
surface_form: liptak
instance_of: Mountain
coordinates: lat: -78.75
lon: -84.9
surface_form: mount liptak
instance_of: Mountain
coordinates: lat: -78.75
lon: -84.9
It was first mapped by the United States Geological Survey from surveys and U.S. Navy air photos from 1957 to 1959, and was named by the Advisory Committee on Antarctic Names for L.H. Liptak, an aviation machinist mate in the U.S. Navy who served as plane captain on the first reconnaissance flights to this vicinity in January 1958.

Geographic entities mentioned:
surface_form: liptak
instance_of: Mountain
coordinates: lat: -78.75
lon: -84.9
Kirtankhola. The Kirtankhola () is a river that starts at Sayeshtabad, in the district of Barisal, Bangladesh, and ends in Gajalia, near the Gabkhan canal. The total length of the river is about. Waste dumping, to the tune of 50 tons every day, by one account, has jeopardized the biodiversity of the river and its connected canals.

Geographic entities mentioned:
surface_form: kirtankhola
instance_of: Watercourse
countries: Bangladesh
coordinates: lat: 22.71
lon: 90.39
Harper Peak. Harper Peak () is a peak, high, standing east of Fortuna Peak and Fortuna Bay on the north coast of South Georgia. The name appears to be first used on a 1931 British Admiralty chart.

Geographic entities mentioned:
surface_form: Fortuna Peak
instance_of: Mountain
countries: United Kingdom
coordinates: lat: -54.1167
lon: -36.7833
surface_form: harper peak
instance_of: Mountain
countries: United Kingdom
coordinates: lat: -54.1167
lon: -36.75
Harper Peak. Harper Peak () is a peak, high, standing east of Fortuna Peak and Fortuna Bay on the north coast of South Georgia. The name appears to be first used on a 1931 British Admiralty chart.

Geographic entities mentioned:
surface_form: harper peak
instance_of: Mountain
countries: United Kingdom
coordinates: lat: -54.1167
lon: -36.75
Nine people died when the train derailed, and 28 others were injured, seven seriously. The landslide which reportedly derailed the train is believed to have been caused by a burst irrigation pipe, or by a valve inadvertently left open. The train was on a regional service, travelling between Mals and Merano, on the Vinschgau line, which reopened in 2005.

Geographic entities mentioned:
surface_form: Vinschgau
instance_of: Valley
countries: Italy
coordinates: lat: 46.615
lon: 10.705
Koncheto. Koncheto (,) is a name given to a knife-edge ridge in the Pirin Mountains in Bulgaria, at an elevation of approximately 2,810 metres, between the peaks Banski Suhodol (2,884 meters) and Kutelo (2,908 metres).

Geographic entities mentioned:
surface_form: koncheto
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 41.782152
lon: 23.393113
There is a steel cable stretched along the top of the ridge to help hikers across. It is said that some less experienced hikers go through Koncheto by saddling the ridge edge like a horse and slowly advancing, hence its name.

Geographic entities mentioned:
surface_form: koncheto
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 41.782152
lon: 23.393113
Oscar II Land. Oscar II Land is the land area between Isfjorden and Kongsfjorden on Spitsbergen, Svalbard. The long glacier Sveabreen divides Oscar II Land from James I Land. The area is named after Oscar II of Sweden. Older name variants are &quot;Oscar II's Land&quot; and &quot;Terre Oscar II&quot;. The Hofgaardtoppen mountain is the highest peak in Oscar II Land.

Geographic entities mentioned:
surface_form: Hofgaardtoppen
instance_of: Mountain
countries: Norway
coordinates: lat: 78.7332
lon: 12.5641
Mount Taimu. Mount Taimu () is a mountain in Ningde, Fujian, China. It is located 46km south of the county-level city of Fuding. Mythology. In Chinese mythology, the mountain was considered a gathering point for deities from the East China Sea. Tourism. Since 2013, it has been classified as a AAAAA scenic area by the China National Tourism Administration.

Geographic entities mentioned:
surface_form: mount taimu
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 27.1244
lon: 120.182
She also wrote an introduction to a 1980 edition of &quot;Azor and the Blue-Eyed Cow&quot; by Maude Crowley. Bohanon donated an easement on her land in New Hampshire to the Ausbon Sargent Land Preservation Trust, to protect the public view of Lake Sunapee. She also collected Indian art, and donated art to the Currier Museum of Art.

Geographic entities mentioned:
surface_form: Lake Sunapee
instance_of: Lake
countries: United States
coordinates: lat: 43.375833333333
lon: -72.056388888889
Avraamiev Monastery. Avraamiev Pokrovsky Gorodetsky Monastery () is a male monastery in the Galich Diocese of the Russian Orthodox Church in the village of Nozhkino, Kostroma Oblast, on the shore of Lake Chukhloma. The architectural ensemble is included in the list of monuments protected at the regional level. History.

Geographic entities mentioned:
surface_form: Lake Chukhloma
instance_of: Lake
countries: Russia
Soviet Union
Russian Empire
coordinates: lat: 58.783333333333
lon: 42.616666666667
History. This monastery was founded in the last third of the <abbr>14th century</abbr> by The Venerable Monk Abraham of Galich, disciple of Saint Sergius of Radonezh (after having founded a monastery on the shores of Lake Galich, dedicated to the Dormition of the Mother of God). Abraham built a wooden church dedicated to the Protection of the Mother of God where many local residents came to pray.

Geographic entities mentioned:
surface_form: Lake Galich
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 58.4065
lon: 42.2985
Disposition. In August 1880 the useful components of the steamer were stripped out and the vessel was converted to a barge. In March 1881, Col. William S. Button, of Roseburg, Oregon was supervising the removal of the machinery of the Fannie Patton so that it could be installed in the Lake Pend Oreille steamer &quot;Henry Villard&quot;.

Geographic entities mentioned:
surface_form: Lake Pend Oreille
instance_of: Lake
countries: United States
coordinates: lat: 48.166666666667
lon: -116.33333333333
Aarid Maql Saab. Aarid Maql Saab is a mountain located in northern Lebanon, specifically in the Akkar District of Mohafazat AakkârIt. t has an elevation of 1,462 meters (4,797 feet) above sea level. Geographic Significance. The mountain that is part of the Mount Lebanon range, which stretches along the western part of Lebanon.

Geographic entities mentioned:
surface_form: aarid maql saab
instance_of: Mountain
countries: Lebanon
coordinates: lat: 34.49138889
lon: 36.27583333
Geographic Significance. The mountain that is part of the Mount Lebanon range, which stretches along the western part of Lebanon. Aarid Maql Saab is the 17th highest peak out of 320 mountains in the Akkar District. Hiking. the mountain is a destination for hikers, as evidenced by the existence of hiking trails and routes to its summit.

Geographic entities mentioned:
surface_form: aarid maql saab
instance_of: Mountain
countries: Lebanon
coordinates: lat: 34.49138889
lon: 36.27583333
Owenmore River (County Cavan). The Owenmore River (, meaning &quot;Big River&quot;) rises in the Cuilcagh Mountains, in the townland of Dunmakeever, civil parish of Kinawley, Roman Catholic parish of Glangevlin, Barony of Tullyhaw, County Cavan. It then flows in a north-west direction and ends in the River Shannon in Gowlat townland. It has a fish population of brown trout.

Geographic entities mentioned:
surface_form: Cuilcagh
instance_of: Mountain
countries: United Kingdom
Ireland
coordinates: lat: 54.2
lon: -7.811
Schiers. Schiers () is a Swiss village in the Prättigau and a municipality in the political district Davos Region in the canton of Graubünden. The first concrete girder bridge ever built, Salginatobel Bridge, is located in Schiers.

Geographic entities mentioned:
surface_form: Prättigau
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.9165
lon: 9.8537194444444
Before 2017, the municipality was located in the Schiers sub-district of the Prättigau/Davos district on the border with Austria. The highest point is the Drusenfluh at. It is located in the lower Prättigau valley at the mouth of the Schraubach. It is the center of the middle and outer Prättigau valley.

Geographic entities mentioned:
surface_form: Prättigau
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.9165
lon: 9.8537194444444
Initially there were only twelve klaverns in the Association. In October 1945 the group conducted the first cross burning since the end of World War II atop Stone Mountain. At the time Green told the press that cross burning had been suspended during wartime because &quot;all factions had to unite to win the war&quot;. At the time of the cross burning the Association claimed 20,000 members.

Geographic entities mentioned:
surface_form: Stone Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.805944444444
lon: -84.145422222222
At the time of the cross burning the Association claimed 20,000 members. On March 21 the Klans attorney, Morgan Telser, filed a corporate registration with the Georgia Secretary of State for the &quot;Knights of the Ku Klux Klan, Inc&quot; and paid up the dues for the period 1943–6. On May 9, 1946, Green held the first large scale initiation ceremony on Stone Mountain.

Geographic entities mentioned:
surface_form: Stone Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.805944444444
lon: -84.145422222222
Biography. Guto is associated with the Ceiriog Valley, in the modern Wrexham county borough of north-east Wales, and many of his patrons lived in the same region, although he visited houses across Wales in the course of his journeys. His early life is obscure, but Glyn Ceiriog or Glyndyfrdwy have been suggested as his places of birth in the years between 1412 and 1420.

Geographic entities mentioned:
surface_form: Ceiriog Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 52.915
lon: -3.197
In 1860 he was in overall charge of the Royal Volunteer Review in Holyrood Park in Edinburgh for Queen Victoria. The 21,000 men on parade stood before a grandstamd holding 3000 spectators plus upward of 200,000 spectators on the northern slope of Arthur's Seat. Legacy. &quot;In Memory of General Sir George Augustus Wetherall, G.C.B., K.H., Colonel of the 84th Foot.

Geographic entities mentioned:
surface_form: Arthur's Seat
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.944166666667
lon: -3.1619444444444
The elevation at street level is approximately above sea level. In addition to sporting events, the Smith Spectrum is utilized for concerts, commencement ceremonies, and other special events central to the Cache Valley community. Originally known as the Assembly Center, the arena's first basketball game was on December 1, 1970, a 95–89 victory over Ohio State.

Geographic entities mentioned:
surface_form: Cache Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.816666666667
lon: -111.93416666667
The Debelt Glacier (,) on Varna Peninsula, Livingston Island in the South Shetland Islands, Antarctica is situated southeast of Rose Valley Glacier and northeast of Panega Glacier. It drains the southeastern slopes of Vidin Heights and flows into Moon Bay between Edinburgh Hill and Helis Nunatak. The glacier extends three km in an east-west direction, and 1.5 km in north-south direction.

Geographic entities mentioned:
surface_form: Edinburgh Hill
instance_of: Mountain
coordinates: lat: -62.5425
lon: -60.0169
surface_form: Helis Nunatak
instance_of: Mountain
coordinates: lat: -62.540277777778
lon: -60.077777777778