Sarmila/GeoWiki-Features huggingface dataset:
Composition. The composition of Hualca Hualca's rocks ranges from andesite-trachyandesite to dacite-trachydacite, and define a potassium-rich calc-alkaline rock suite similar to that of the other volcanoes in the Ampato volcanic complex. Phenocrysts consist of amphibole, biotite, plagioclase and pyroxene.

Geographic entities mentioned:
surface_form: hualca hualca
instance_of: Mountain
countries: Peru
coordinates: lat: -15.816666666667
lon: -71.883333333333
Phenocrysts consist of amphibole, biotite, plagioclase and pyroxene. The magmas that built Hualca Hualca formed when the mantle wedge, metasomatised during subduction, melted; the magmas underwent fractional crystallization before erupting at the surface. Minor geochemical differences between the rocks of the three Ampato complex volcanoes may reflect differences in magma generation processes.

Geographic entities mentioned:
surface_form: hualca hualca
instance_of: Mountain
countries: Peru
coordinates: lat: -15.816666666667
lon: -71.883333333333
Annual precipitation is about, decreasing at lower elevations. During December–March, the Intertropical Convergence Zone reaches the mountain and draws moisture from the Amazon, as part of the South American Summer Monsoon (Pacific Ocean-derived moisture is trapped beneath a temperature inversion at an elevation of and cannot reach Hualca Hualca).

Geographic entities mentioned:
surface_form: hualca hualca
instance_of: Mountain
countries: Peru
coordinates: lat: -15.816666666667
lon: -71.883333333333
This is the wet season, during which most of the annual precipitation falls. April to November is the dry season. The mountain is snow-covered year-round. Precipitation on Hualca Hualca may constitute a source of groundwater and recharge the hydrothermal system. El Niño-Southern Oscillation events cause temperatures to increase and precipitation to decrease.

Geographic entities mentioned:
surface_form: hualca hualca
instance_of: Mountain
countries: Peru
coordinates: lat: -15.816666666667
lon: -71.883333333333
Above that altitude, cushion plants such as &quot;Azorella compacta&quot; replace the herbs until elevation, where most vegetation disappears except for lichens and mosses. Peat bogs grow in valleys on the southern side of Hualca Hualca in places where precipitation water and meltwater accumulate. They are classified as &quot;bofedales&quot;.

Geographic entities mentioned:
surface_form: hualca hualca
instance_of: Mountain
countries: Peru
coordinates: lat: -15.816666666667
lon: -71.883333333333
The advances produced several generations of moraines, and eroded older moraines. Cosmogenic isotope dating has yielded ages of 17,000–16,000 and 12,000 years ago for glacial advances at Hualca Hualca, implying that glacier retreat at Hualca Hualca occurred later than at other Central Andean volcanoes.

Geographic entities mentioned:
surface_form: hualca hualca
instance_of: Mountain
countries: Peru
coordinates: lat: -15.816666666667
lon: -71.883333333333
surface_form: hualca hualca
instance_of: Mountain
countries: Peru
coordinates: lat: -15.816666666667
lon: -71.883333333333
The active geyser is known as &quot;Pinchollo&quot;. Other geothermal manifestations are a solfatara, gas venting at Paclla, and hot springs in the amphitheatre such as Puye Puye, where there are mud pools. Some of these geothermal manifestations may reflect local tectonic features rather than being part of Hualca Hualca's volcanic system.

Geographic entities mentioned:
surface_form: hualca hualca
instance_of: Mountain
countries: Peru
coordinates: lat: -15.816666666667
lon: -71.883333333333
surface_form: hualca hualca
instance_of: Mountain
countries: Peru
coordinates: lat: -15.816666666667
lon: -71.883333333333
Some of these geothermal manifestations may reflect local tectonic features rather than being part of Hualca Hualca's volcanic system. A hydrothermal system underlies the Ampato volcanic complex, including Hualca Hualca, where it feeds the hot springs and geysers, perhaps with water pooled in one of the buried calderas and heated by the magma under Hualca Hualca.

Geographic entities mentioned:
surface_form: hualca hualca
instance_of: Mountain
countries: Peru
coordinates: lat: -15.816666666667
lon: -71.883333333333
The magmatic system experiences the entry of new mafic magmas, that in turn drives activity in the shallow magmatic system and eruptions at Sabancaya, while explaining the low correlation between deformation and activity at Sabancaya. Hualca Hualca is also impacted on the surface by activity at Sabancaya, recent eruptions have deposited volcanic ash on Hualca Hualca.

Geographic entities mentioned:
surface_form: hualca hualca
instance_of: Mountain
countries: Peru
coordinates: lat: -15.816666666667
lon: -71.883333333333
Hualca Hualca is also impacted on the surface by activity at Sabancaya, recent eruptions have deposited volcanic ash on Hualca Hualca. The volcano is within the hazard zone of Sabancaya; ash falls from the latter volcano can melt the ice on Hualca Hualca to form lahars, threatening agricultural land and infrastructure such as the regionally important Majes-Siguas canal.

Geographic entities mentioned:
surface_form: hualca hualca
instance_of: Mountain
countries: Peru
coordinates: lat: -15.816666666667
lon: -71.883333333333
Volcanic fallout from Sabancaya is frequent. Name, religious and cultural importance. During Inca times, Hualca Hualca was regarded as an &quot;apu&quot;, a mountain deity. During eruptions of Sabancaya, the Inca rulers offered sacrifices, such as the mummy Juanita at Ampato, to the &quot;apus&quot; of the region including Hualca Hualca.

Geographic entities mentioned:
surface_form: hualca hualca
instance_of: Mountain
countries: Peru
coordinates: lat: -15.816666666667
lon: -71.883333333333
During eruptions of Sabancaya, the Inca rulers offered sacrifices, such as the mummy Juanita at Ampato, to the &quot;apus&quot; of the region including Hualca Hualca. The veneration is attested since the 16th century, but probably pre-dates Inca rule, and remains of the offerings have been found at an elevation of at Hualca Hualca.

Geographic entities mentioned:
surface_form: hualca hualca
instance_of: Mountain
countries: Peru
coordinates: lat: -15.816666666667
lon: -71.883333333333
surface_form: hualca hualca
instance_of: Mountain
countries: Peru
coordinates: lat: -15.816666666667
lon: -71.883333333333
Despite initial resistance to the Majes canal project and disputes about its supply, the town eventually began to use it and the water rituals involving Hualca Hualca largely (but not entirely) stopped.

Geographic entities mentioned:
surface_form: hualca hualca
instance_of: Mountain
countries: Peru
coordinates: lat: -15.816666666667
lon: -71.883333333333
Martin Schippert. Martin &quot;Tino&quot; Schippert (1 May 1946 – 1981) was a Swiss &quot;Halbstarker&quot; (member of a youth subculture similar to Beatniks or Yobbo), Rocker, a so-called &quot;68er&quot; and is considered to be founder of the Hells Angels in Switzerland. Schippert grew up in an upper-class environment, at the Zürichberg. He suffered from various illnesses.

Geographic entities mentioned:
surface_form: Zürichberg
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.3856
lon: 8.56694
The Großer Auersberg is covered by dense deciduous forest and lies within the Wildflecken Training Area, established in 1938. The entire terrain is a military out-of-bounds area, which civilians may not enter. A good two kilometres to the west-southwest rises the slightly less high Kleiner Auersberg. Neither should be confused with the Auersberg near Hilders in the Hessian part of the Rhön.

Geographic entities mentioned:
surface_form: Kleiner Auersberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.3605
lon: 9.84135
surface_form: auersberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.455555555556
lon: 12.648055555556
surface_form: auersberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.5972
lon: 10.0095
Großer Auersberg. The Großer Auersberg is a mountain, in the Bavarian part of the Rhön mountains. It is located in an unparished area, 4.68 km² in area, in the county of Bad Kissingen, three kilometres southwest of the village centre of Wildflecken. The Großer Auersberg is covered by dense deciduous forest and lies within the Wildflecken Training Area, established in 1938.

Geographic entities mentioned:
surface_form: auersberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.455555555556
lon: 12.648055555556
surface_form: auersberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.5972
lon: 10.0095
surface_form: großer auersberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.367472222222
lon: 9.8717305555556
It is located in an unparished area, 4.68 km² in area, in the county of Bad Kissingen, three kilometres southwest of the village centre of Wildflecken. The Großer Auersberg is covered by dense deciduous forest and lies within the Wildflecken Training Area, established in 1938. The entire terrain is a military out-of-bounds area, which civilians may not enter.

Geographic entities mentioned:
surface_form: auersberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.455555555556
lon: 12.648055555556
surface_form: auersberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.5972
lon: 10.0095
surface_form: großer auersberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.367472222222
lon: 9.8717305555556
The Großer Auersberg is covered by dense deciduous forest and lies within the Wildflecken Training Area, established in 1938. The entire terrain is a military out-of-bounds area, which civilians may not enter. A good two kilometres to the west-southwest rises the slightly less high Kleiner Auersberg. Neither should be confused with the Auersberg near Hilders in the Hessian part of the Rhön.

Geographic entities mentioned:
surface_form: auersberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.455555555556
lon: 12.648055555556
surface_form: auersberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.5972
lon: 10.0095
Dearne & District F.C.. Dearne & District Football Club is an English football club representing the Dearne Valley area of South Yorkshire. They currently play in the. History. The club was founded in 1982 as a youth team for the Rotherham area. In 2018 an adult side was formed and joined Division One of the Doncaster Senior League.

Geographic entities mentioned:
surface_form: Dearne Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.5
lon: -1.2166666666667
On January 10 at 6:00 p.m., evacuation warnings extended northeast, with the warnings changing to orders within the hour for the area enclosed by Sunset Boulevard to the south, Encino Reservoir to the north, Interstate 405 to the east, and Mandeville Canyon to the west. Communities in this area include parts of Tarzana and Encino in the San Fernando Valley.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Annagh Hill. Annagh Hill () is a hill in the north of County Wexford, Ireland. Geography. Annagh Hill is separated from Croghan Mountain to the north by the &quot;Wicklow Gap&quot;, not to be confused with the Wicklow Gap in County Wicklow. Except for the southeastern face (see photo) it is covered in coniferous forest.

Geographic entities mentioned:
surface_form: Croghan Mountain
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.8
lon: -6.3166666666667
surface_form: annagh hill
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.75
lon: -6.3666666666667
Annagh Hill. Annagh Hill () is a hill in the north of County Wexford, Ireland. Geography. Annagh Hill is separated from Croghan Mountain to the north by the &quot;Wicklow Gap&quot;, not to be confused with the Wicklow Gap in County Wicklow. Except for the southeastern face (see photo) it is covered in coniferous forest.

Geographic entities mentioned:
surface_form: annagh hill
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.75
lon: -6.3666666666667
When the Army was reorganized in 1821, he became a Second Lieutenant in the First Artillery. From 1821 to 1822, Whistler was an Assistant Professor of Drawing at West Point. Whistler was reassigned back to artillery corps duty as a topographical engineer in 1822, his first assignment was supporting the Commission tracing the international boundary between Lake Superior and Lake of the Woods.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
surface_form: Lake of the Woods
instance_of: Lake
countries: Canada
United States
coordinates: lat: 49.09027777777778
lon: -95.2388888888889
Fortingall. Fortingall () (lit. &quot;Escarpment Church&quot;—i.e. &quot;church at the foot of an escarpment or steep slope&quot;) is a small village in Glen Lyon, Perthshire, Scotland. Its nearest sizable neighbours are Aberfeldy and Kenmore.

Geographic entities mentioned:
surface_form: Glen Lyon
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.59864
lon: -4.25283
KMVU-DT. KMVU-DT (channel 26) is a television station in Medford, Oregon, United States, affiliated with the Fox network. It is owned by Marquee Broadcasting alongside low-power dual MyNetworkTV/Telemundo affiliate KFBI-LD (channel 48). The two stations share studios on Crater Lake Avenue in Medford; KMVU-DT's transmitter is located atop Mount Baldy, near Phoenix, Oregon. History.

Geographic entities mentioned:
surface_form: Crater Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.943611111111
lon: -122.10666666667
The new (7 National Network) was positioned as targeting the working class and rural areas, while, based from XHDF, targeted a more middle- and upper-class audience. The insertion of a channel 7 into Mexico City required a shuffle of frequencies in neighboring areas, with stations in Mexico City, Toluca and on Altzomoni moving to accommodate the last VHF station in the nation's capital.

Geographic entities mentioned:
surface_form: Altzomoni
instance_of: Mountain
countries: Mexico
coordinates: lat: 19.12
lon: -98.654
The Baw Baw Plateau provides an abundance of easy touring terrain. Mount Baw Baw downhill ski village is approximately 9 km away across the Baw Baw plateau to the south-west and trails link the resorts. Mount St Gwinear was named by the Geologist William Baragwanath after Saint Gwinear of Cornwall. He also name the nearby Mt St Phillack.

Geographic entities mentioned:
surface_form: Mount Baw Baw
instance_of: Mountain
countries: Australia
coordinates: lat: -37.833333333333
lon: 146.26666666667
Mount St Gwinear. Mount St Gwinear is a mountain in Victoria, Australia, located at the north-east end of the Baw Baw National Park in the Gippsland high country. It is popular with families looking for a cheap and accessible snow-play/tobogganing destination and cross-country skiers. The Baw Baw Plateau provides an abundance of easy touring terrain.

Geographic entities mentioned:
surface_form: mount st gwinear
instance_of: Mountain
countries: Australia
coordinates: lat: -37.833333333333
lon: 146.31666666667
The Baw Baw Plateau provides an abundance of easy touring terrain. Mount Baw Baw downhill ski village is approximately 9 km away across the Baw Baw plateau to the south-west and trails link the resorts. Mount St Gwinear was named by the Geologist William Baragwanath after Saint Gwinear of Cornwall. He also name the nearby Mt St Phillack.

Geographic entities mentioned:
surface_form: mount st gwinear
instance_of: Mountain
countries: Australia
coordinates: lat: -37.833333333333
lon: 146.31666666667
In the 1879 session, he was chairman of the Committee on Improved Sewage that built part of the sewer under South Bay. In the 1881 session, he introduced an order to take water from Lake Winnipiseogee in New Hampshire and use it to increase the Boston water supply at a cost of fifty million dollars. He served in the Massachusetts House of Representatives in 1880 and from 1891 to 1894.

Geographic entities mentioned:
surface_form: Lake Winnipiseogee
instance_of: Lake
countries: United States
coordinates: lat: 43.598888888889
lon: -71.323055555556
Betty Kuntiwa Pumani is an Aboriginal Australian artist from Anangu Pitjantjatjara Yankunytjatjara in South Australia. Her paintings have won several awards, including the National Aboriginal & Torres Strait Islander Art Award and the 2017 Wynne Prize for landscape art. Pumani is one of the traditional owners of the Indigenous Protected Area of Antara, which is located south of the Everard Ranges.

Geographic entities mentioned:
surface_form: Everard Ranges
instance_of: Mountain
countries: Australia
coordinates: lat: -27.1128
lon: 132.529
San Antonio Creek (San Bernardino County). San Antonio Creek is a major stream in Los Angeles County and San Bernardino County, California, draining southwards from Mount San Antonio in the San Gabriel Mountains into Chino Creek, a tributary of the Santa Ana River.

Geographic entities mentioned:
surface_form: Mount San Antonio
instance_of: Mountain
countries: United States
coordinates: lat: 34.2889
lon: -117.647
Upon leaving San Antonio Canyon and entering the broad alluvial plain of the Pomona Valley, it is known as the San Antonio Wash or the San Antonio Creek Channel, the former referring to the creek's seasonal dry nature below the mouth of San Antonio Canyon. Geography. The creek is long and has a drainage basin of about. Course.

Geographic entities mentioned:
surface_form: Pomona Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.076
lon: -117.657
Geography. The creek is long and has a drainage basin of about. Course. San Antonio Creek rises on the southeast flank of Mount San Antonio (Mount Baldy), the highest peak in the San Gabriel Mountains range. The stream flows southwest through San Antonio Canyon and past Mount Baldy Village, then south, winding through the Angeles National Forest.

Geographic entities mentioned:
surface_form: Mount San Antonio (Mount Baldy)
instance_of: Mountain
countries: United States
coordinates: lat: 34.2889
lon: -117.647
At the end of the canyon it reaches the San Antonio Dam, but after passing through the dam, the stream is usually dry. It flows south through a concrete flood control channel, passing through the several cities of the Pomona Valley, including Claremont, Montclair, and Chino. The creek joins Chino Creek in northwestern Chino, upstream from the larger stream's mouth at the Santa Ana River. History.

Geographic entities mentioned:
surface_form: Pomona Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.076
lon: -117.657
One of the large warships built under the direction of Commodore Isaac Chauncey for service against the British on Lake Ontario, &quot;Mohawk&quot; departed Sackets Harbor on 31 July 1814 in Chauncey’s squadron to challenge the British squadron of Captain Sir James Yeo, Royal Navy, for control of the lake during the crucial Niagara campaign of 1814.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Lake Valets flows to the bottom of a bay to the northeast in the Capousacataca River. Toponymy. The name &quot;Lac Valets&quot; was officialized on December 5, 1968 by the Commission de toponymie du Québec when it was created.

Geographic entities mentioned:
surface_form: lac valets
instance_of: Lake
countries: Canada
coordinates: lat: 48.54306
lon: -76.48806
Valets Lake. Valets Lake is a freshwater body that straddles Valets and Girouard Townships in Senneterre in La Vallée-de-l'Or Regional County Municipality (RCM), in the administrative region of Abitibi-Témiscamingue, in province of Quebec, in Canada. Forestry is the main economic activity of the sector; recreational tourism activities come second.

Geographic entities mentioned:
surface_form: valets lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.54306
lon: -76.48806
Valets Lake. Valets Lake is a freshwater body that straddles Valets and Girouard Townships in Senneterre in La Vallée-de-l'Or Regional County Municipality (RCM), in the administrative region of Abitibi-Témiscamingue, in province of Quebec, in Canada. Forestry is the main economic activity of the sector; recreational tourism activities come second.

Geographic entities mentioned:
surface_form: valets lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.54306
lon: -76.48806
surface_form: témiscamingue
instance_of: Lake
countries: Canada
coordinates: lat: 47.333333333333
lon: -79.5
surface_form: abitibi
instance_of: Lake
countries: Canada
coordinates: lat: 48.666666666666664
lon: -79.75
The mouth of this lake is located at the bottom of a northeastern bay north of the confluence of the Capousacataca River with the Mégiscane River; at north-east of the confluence of the Mégiscane River with Parent Lake (Abitibi); to north of the Canadian National Railway's Paradise Station and northeast of Senneterre.

Geographic entities mentioned:
surface_form: parent lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.6522
lon: -77.0636
surface_form: abitibi
instance_of: Lake
countries: Canada
coordinates: lat: 48.666666666666664
lon: -79.75
The pond's outlet is at its south end, where Willard Pond Brook flows south into Carpenter Marsh and Moose Brook. Moose Brook flows southeast to Norway Pond in the center of Hancock, then flows east to the Contoocook River in Powder Mill Pond. The Contoocook flows northeast to the Merrimack River, which flows south, then east, to the Atlantic Ocean in Newburyport, Massachusetts. Wildlife.

Geographic entities mentioned:
surface_form: Powder Mill Pond
instance_of: Lake
countries: United States
coordinates: lat: 42.969444444444
lon: -71.9325
surface_form: mill pond
instance_of: Lake
countries: United States
coordinates: lat: 41.7708
lon: -70.6719
surface_form: mill pond
instance_of: Lake
countries: United States
coordinates: lat: 42.0181
lon: -70.7125
Because the pond and the land around it are part of the sanctuary, the shore is unable to be developed. Therefore, there are no buildings around the pond and there won't be any in the foreseeable future. Willard is instead surrounded by extensive amounts of wilderness and hiking trails that lead around the pond and to the summits of Bald Mountain and Goodhue Hill.

Geographic entities mentioned:
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.655
lon: -114.409
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 46.8827026
lon: -88.0390147
New Hampshire Audubon keeps track of the loons and sends out workers to count the number and inspect the area frequently. Hiking. There are hiking trails near Willard that lead hikers up Bald Mountain as well as through the surrounding woods. They are well-maintained and can be hiked in any season. Bald Mountain Trail. This leads hikers up Bald Mountain.

Geographic entities mentioned:
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.655
lon: -114.409
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 46.8827026
lon: -88.0390147
They are well-maintained and can be hiked in any season. Bald Mountain Trail. This leads hikers up Bald Mountain. Glacial boulders can be seen at the beginning of the trail, which goes part way around the pond before turning up the mountain. It is a rather steep trail and has great views at the top. Tudor Trail.

Geographic entities mentioned:
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.655
lon: -114.409
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 46.8827026
lon: -88.0390147
It is a rather steep trail and has great views at the top. Tudor Trail. This trail goes halfway around the pond and offers opportunities to view the beautiful wildlife along the water's edge. Halfway along the trail hikers can go left to the Bald Mountain Trail or continue to the point on the opposite side of the pond where the trail stops. Mill Pond Trail.

Geographic entities mentioned:
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.655
lon: -114.409
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 46.8827026
lon: -88.0390147
The mountain is named as such because of a fire that left the summit without vegetation. Immediately south of Willard is Mill Pond, which is extremely small but offers opportunities to see animals such as beavers and otters. Willard's parking lot is located a short walk from the actual boat launch, and there is a caretaker's house between the parking lot and the pond.

Geographic entities mentioned:
surface_form: mill pond
instance_of: Lake
countries: United States
coordinates: lat: 41.7708
lon: -70.6719
surface_form: mill pond
instance_of: Lake
countries: United States
coordinates: lat: 42.0181
lon: -70.7125
Halfway along the trail hikers can go left to the Bald Mountain Trail or continue to the point on the opposite side of the pond where the trail stops. Mill Pond Trail. Looping around the Hatch Mill Pond, this trail takes hikers to the Goodhue Hill Trail, which starts about halfway around the pond. Hatch Mill Pond is historic because it was once dammed to supply waterpower for the Hatch Sawmill.

Geographic entities mentioned:
surface_form: mill pond
instance_of: Lake
countries: United States
coordinates: lat: 41.7708
lon: -70.6719
surface_form: mill pond
instance_of: Lake
countries: United States
coordinates: lat: 41.7708
lon: -70.6719
surface_form: mill pond
instance_of: Lake
countries: United States
coordinates: lat: 42.0181
lon: -70.7125
surface_form: mill pond
instance_of: Lake
countries: United States
coordinates: lat: 42.0181
lon: -70.7125
Goodhue Hill Trail. This brings hikers to the top of Goodhue Hill, which lies adjacent to Willard. While going through the woods hikers will come across many stone walls which were once used to separate sheep pastures. This trail can be veered off of to continue on the Mill Pond trail on the way back down.

Geographic entities mentioned:
surface_form: mill pond
instance_of: Lake
countries: United States
coordinates: lat: 41.7708
lon: -70.6719
surface_form: mill pond
instance_of: Lake
countries: United States
coordinates: lat: 42.0181
lon: -70.7125
Willard Pond. Willard Pond is a small, protected lake in Antrim, New Hampshire, United States. The lake, located in southwestern New Hampshire, is about in size with an average depth of and a maximum depth of. No petroleum motors are allowed, and fly fishing is the only form of fishing allowed. It is part of the dePierrefeu Wildlife Sanctuary, which is owned by the New Hampshire Audubon Society.

Geographic entities mentioned:
surface_form: willard pond
instance_of: Lake
countries: United States
coordinates: lat: 43.0214
lon: -72.0161
Willard is a popular fishing, boating and hiking destination, and it has become more popular with its mention in numerous magazines and newspapers. History. In 1967, Elsa Tudor dePierrefeu first created the Audubon Sanctuary at Willard Pond. Elsa had lost her husband in World War I and had a strong vision for a sanctuary with wildlife at the forefront of her vision.

Geographic entities mentioned:
surface_form: willard pond
instance_of: Lake
countries: United States
coordinates: lat: 43.0214
lon: -72.0161
Many boulders can be accessed by hiking or by boating. The pond is part of the Merrimack River watershed. The pond's outlet is at its south end, where Willard Pond Brook flows south into Carpenter Marsh and Moose Brook. Moose Brook flows southeast to Norway Pond in the center of Hancock, then flows east to the Contoocook River in Powder Mill Pond.

Geographic entities mentioned:
surface_form: willard pond
instance_of: Lake
countries: United States
coordinates: lat: 43.0214
lon: -72.0161
Reintaler See. Reintaler See is a lake of Tyrol, Austria. Reintaler See is located at the southern foot of the Voldöppberg in the Brandenberg Alps. The lake is divided into three basins, the maximum depth of the eastern basin is 10.30 m, the north basin 9.90 m and the west basin 7.60 m. The lake is essentially fed by groundwater and drained from the western basin to Krummsee.

Geographic entities mentioned:
surface_form: krummsee
instance_of: Lake
countries: Austria
coordinates: lat: 47.4573
lon: 11.8847
Reintaler See. Reintaler See is a lake of Tyrol, Austria. Reintaler See is located at the southern foot of the Voldöppberg in the Brandenberg Alps. The lake is divided into three basins, the maximum depth of the eastern basin is 10.30 m, the north basin 9.90 m and the west basin 7.60 m. The lake is essentially fed by groundwater and drained from the western basin to Krummsee.

Geographic entities mentioned:
surface_form: reintaler see
instance_of: Lake
countries: Austria
coordinates: lat: 47.4606
lon: 11.8955
The name can also be transliterated as Uzi. It may be a nickname for Uzzah, Uzziah, and Uzziel. According to Samaritan tradition, Uzzi hid the tent sanctuary of the desert wandering (Mishkan) in a cave on Mount Gerizim when the Israelites introduced the cult in Shiloh, which was illegitimate from the Samaritan point of view.

Geographic entities mentioned:
surface_form: Mount Gerizim
instance_of: Mountain
countries: State of Palestine
coordinates: lat: 32.199444444444
lon: 35.272777777778
They were one of the eight teams that competed in the 2020 Indian Premier League. The Kings XI Punjab's catchment areas are Kashmir, Jammu, Himachal Pradesh, Punjab and Haryana—evident from the letter sequence &quot;K J H P H&quot; in the banner of the team's logo. Kings XI Punjab finished the tournament in 6th position with 6 wins and 8 losses, failing to qualify for the playoffs.

Geographic entities mentioned:
surface_form: Kashmir
instance_of: Valley
countries: India
coordinates: lat: 34.0333
lon: 74.6667
Alvdal Municipality. Alvdal is a municipality in Innlandet county, Norway. It is located in the traditional district of Østerdalen. The administrative centre of the municipality is the village of Alvdal. Other villages include Barkald, Plassmoen, and Strømmen.

Geographic entities mentioned:
surface_form: Østerdalen
instance_of: Valley
countries: Norway
coordinates: lat: 61.575916666666664
lon: 11.087111111111112
Geography. Alvdal is bordered by Tynset Municipality to the north, Rendalen Municipality to the east and south, Stor-Elvdal Municipality to the south, and Folldal Municipality to the west. The highest point in the municipality is the tall mountain Storsølnkletten. Another notable mountain in the municipality is Tronfjell. The lake Savalen is partially located in Alvdal.

Geographic entities mentioned:
surface_form: Storsølnkletten
instance_of: Mountain
countries: Norway
coordinates: lat: 61.98
lon: 10.292222222222
Geography. Alvdal is bordered by Tynset Municipality to the north, Rendalen Municipality to the east and south, Stor-Elvdal Municipality to the south, and Folldal Municipality to the west. The highest point in the municipality is the tall mountain Storsølnkletten. Another notable mountain in the municipality is Tronfjell. The lake Savalen is partially located in Alvdal.

Geographic entities mentioned:
surface_form: Tronfjell
instance_of: Mountain
countries: Norway
coordinates: lat: 62.174741666667
lon: 10.693797222222
The highest point in the municipality is the tall mountain Storsølnkletten. Another notable mountain in the municipality is Tronfjell. The lake Savalen is partially located in Alvdal. The rivers Sivilla and Glåma both flow through the municipality. The Jutulhogget canyon is located in this municipality as well. Economy.

Geographic entities mentioned:
surface_form: Savalen
instance_of: Lake
countries: Norway
coordinates: lat: 62.241111111111
lon: 10.482222222222
It is located west of Bralorne on the northeastern flank of the Mount Meager massif. With an elevation of, it lies on the steep northern face of Plinth Peak, a high volcanic peak comprising the northern portion of Meager. The vent rises above the western shoulder of the Pemberton Valley and represents the northernmost volcanic feature of the Mount Meager massif.

Geographic entities mentioned:
surface_form: Plinth Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 50.6452
lon: -123.511
With an elevation of, it lies on the steep northern face of Plinth Peak, a high volcanic peak comprising the northern portion of Meager. The vent rises above the western shoulder of the Pemberton Valley and represents the northernmost volcanic feature of the Mount Meager massif. At least eight volcanic vents compose the Meager massif, with the Bridge River Vent being the most recent to form.

Geographic entities mentioned:
surface_form: Pemberton Valley
instance_of: Valley
countries: Canada
coordinates: lat: 50.5
lon: -123
surface_form: mount meager
instance_of: Mountain
countries: Canada
coordinates: lat: 50.63166667
lon: -123.50416667
At least eight volcanic vents compose the Meager massif, with the Bridge River Vent being the most recent to form. It is the only vent of the massif to exhibit volcanic activity in the past 10,000 years and one of the several vents in the Garibaldi Volcanic Belt to erupt since the end of the last glacial period.

Geographic entities mentioned:
surface_form: Garibaldi Volcanic Belt
instance_of: Mountain
countries: Canada
coordinates: lat: 51.5283
lon: -126.113
Substantially, the Bridge River event was explosive in nature, ranging from Plinian to Peléan activity. This is one of the most recent eruptions in the Garibaldi Volcanic Belt and the largest known explosive eruption in Canada in the past 10,000 years. It had similarities to the 1980 eruption of Mount St. Helens in the U.S.

Geographic entities mentioned:
surface_form: Soufrière Hills
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 16.716666666667
lon: -62.183333333333
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
Strong high-altitude winds carried material east-northeasterly from the Plinian column to as far as Alberta, away from the vent to produce a large volcanic ash deposit. This widespread ash deposit, known as the Bridge River Ash, overlies older ash deposits from other large explosive eruptions in the Cascade Volcanic Arc, such as the 3,400-year-old Yn Ash from Mount St.

Geographic entities mentioned:
surface_form: Mount St. Helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
surface_form: Mount Mazama
instance_of: Mountain
countries: United States
coordinates: lat: 42.9165186
lon: -122.0844711
However, the eruption column was likely higher than the estimated data indicates because it does not include the highest portions of the column. During this time of the eruption, tephra spread into the stratosphere and parts of the mushroom-shaped ash column collapsed, devastating nearby areas with heavy pyroclastic fall which deposited tephra on Meager's steep flanks.

Geographic entities mentioned:
surface_form: mushroom
instance_of: Mountain
countries: Canada
coordinates: lat: 62.8
lon: -137.45
Bridge River Vent. The Bridge River Vent is a volcanic crater in the Pacific Ranges of the Coast Mountains in southwestern British Columbia, Canada. It is located west of Bralorne on the northeastern flank of the Mount Meager massif. With an elevation of, it lies on the steep northern face of Plinth Peak, a high volcanic peak comprising the northern portion of Meager.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: bridge river vent
instance_of: Mountain
countries: Canada
coordinates: lat: 50.6563
lon: -123.502
Background. Volcanic activity of the Mount Meager massif is caused by subduction of the Juan de Fuca Plate under the North American Plate at the Cascadia subduction zone. This is a long fault zone running off the Pacific Northwest from Northern California to southwestern British Columbia. The plates move at a relative rate of over per year at an oblique angle to the subduction zone.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
The crater constitutes a bowl-shaped depression overlain by glacial ice and volcanic debris that were deposited during volcanic activity. Its breached northern rim has been a pathway for lava and ash flows that have traveled throughout the nearby Pemberton Valley. Background.

Geographic entities mentioned:
surface_form: pemberton valley
instance_of: Valley
countries: Canada
coordinates: lat: 50.5
lon: -123
This lake continued to fill when the third block-and-ash flow was erupted, eventually reaching a maximum elevation of and a depth of at least. As the lake continued to rise from inflow of the Lillooet River, the variably welded, poorly indurated pyroclastic dam failed catastrophically, releasing lake water down the Pemberton Valley to produce an outburst flood.

Geographic entities mentioned:
surface_form: pemberton valley
instance_of: Valley
countries: Canada
coordinates: lat: 50.5
lon: -123
Bridge River Vent. The Bridge River Vent is a volcanic crater in the Pacific Ranges of the Coast Mountains in southwestern British Columbia, Canada. It is located west of Bralorne on the northeastern flank of the Mount Meager massif. With an elevation of, it lies on the steep northern face of Plinth Peak, a high volcanic peak comprising the northern portion of Meager.

Geographic entities mentioned:
surface_form: mount meager
instance_of: Mountain
countries: Canada
coordinates: lat: 50.63166667
lon: -123.50416667
Background. Volcanic activity of the Mount Meager massif is caused by subduction of the Juan de Fuca Plate under the North American Plate at the Cascadia subduction zone. This is a long fault zone running off the Pacific Northwest from Northern California to southwestern British Columbia. The plates move at a relative rate of over per year at an oblique angle to the subduction zone.

Geographic entities mentioned:
surface_form: mount meager
instance_of: Mountain
countries: Canada
coordinates: lat: 50.63166667
lon: -123.50416667
When the plate finally slips, the 500 years of stored energy are released in a massive earthquake. Bridge River eruption. The Bridge River Vent was formed during an onset of eruptive activity about 2,350 years ago that ended a long period of dormancy at the Mount Meager massif. Substantially, the Bridge River event was explosive in nature, ranging from Plinian to Peléan activity.

Geographic entities mentioned:
surface_form: mount meager
instance_of: Mountain
countries: Canada
coordinates: lat: 50.63166667
lon: -123.50416667
surface_form: bridge river vent
instance_of: Mountain
countries: Canada
coordinates: lat: 50.6563
lon: -123.502
Substantially, the Bridge River event was explosive in nature, ranging from Plinian to Peléan activity. This is one of the most recent eruptions in the Garibaldi Volcanic Belt and the largest known explosive eruption in Canada in the past 10,000 years. It had similarities to the 1980 eruption of Mount St. Helens in the U.S.

Geographic entities mentioned:
surface_form: garibaldi volcanic belt
instance_of: Mountain
countries: Canada
coordinates: lat: 51.5283
lon: -126.113
About 1–5% of the pumice grains contain white to dark grey bands. About 1–2% of the grains comprising the thick pyroclastic fall deposit were derived from the older Plinth Assemblage as the energetic Plinian column blasted the surrounding rock of Plinth Peak. These clasts are relatively minor to the abundant pumice grains.

Geographic entities mentioned:
surface_form: plinth peak
instance_of: Mountain
countries: Canada
coordinates: lat: 50.6452
lon: -123.511
Bridge River Vent. The Bridge River Vent is a volcanic crater in the Pacific Ranges of the Coast Mountains in southwestern British Columbia, Canada. It is located west of Bralorne on the northeastern flank of the Mount Meager massif. With an elevation of, it lies on the steep northern face of Plinth Peak, a high volcanic peak comprising the northern portion of Meager.

Geographic entities mentioned:
surface_form: bridge river vent
instance_of: Mountain
countries: Canada
coordinates: lat: 50.6563
lon: -123.502
With an elevation of, it lies on the steep northern face of Plinth Peak, a high volcanic peak comprising the northern portion of Meager. The vent rises above the western shoulder of the Pemberton Valley and represents the northernmost volcanic feature of the Mount Meager massif. At least eight volcanic vents compose the Meager massif, with the Bridge River Vent being the most recent to form.

Geographic entities mentioned:
surface_form: bridge river vent
instance_of: Mountain
countries: Canada
coordinates: lat: 50.6563
lon: -123.502
Plinian phase. At the start of the eruption, a large Plinian column rose above the Bridge River Vent, creating its bowl-shaped volcanic crater. This explosive eruption might have been followed by the collapse of a former lava dome based on the existence of a thick cover of welded vitrophyric breccia. The Plinian column is estimated to have had a height of to.

Geographic entities mentioned:
surface_form: bridge river vent
instance_of: Mountain
countries: Canada
coordinates: lat: 50.6563
lon: -123.502
The pyroclastic flow burnt and buried Meager's forested slopes in place. Remnants of this catastrophe are exposed south and east of the Bridge River Vent along the Lillooet River. At the vent area, the thickness of this pyroclastic flow ranges from to. Peléan phase. After the first major pyroclastic flow, a hot block and ash flow was erupted off the face of an advancing lava dome.

Geographic entities mentioned:
surface_form: bridge river vent
instance_of: Mountain
countries: Canada
coordinates: lat: 50.6563
lon: -123.502
Later eruptions. In 1977, J. A. Westgate of the University of Toronto suggested that a smaller eruption may have occurred at the Bridge River Vent after the eruption 2,350 years ago, sending tephra to the southeast. A tephra deposit overlying the Bridge River Ash at Otter Creek shows strong genetic relationships with the Bridge River Ash, differing only by its absence of biotite.

Geographic entities mentioned:
surface_form: bridge river vent
instance_of: Mountain
countries: Canada
coordinates: lat: 50.6563
lon: -123.502
Later eruptions. In 1977, J. A. Westgate of the University of Toronto suggested that a smaller eruption may have occurred at the Bridge River Vent after the eruption 2,350 years ago, sending tephra to the southeast. A tephra deposit overlying the Bridge River Ash at Otter Creek shows strong genetic relationships with the Bridge River Ash, differing only by its absence of biotite.

Geographic entities mentioned:
surface_form: otter creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 59.63274
lon: -133.40358
Matthew Turner was born in Geneva, Ohio on June 17, 1825, the fourth child of George Turner and Emily Atkins. George Turner owned a sawmill on the shores of Lake Erie and later launched his first ship, the sloop &quot;Geneva&quot;, in 1839, to ship lumber and building stone.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Coon Hollow (Washington County, Missouri). Coon Hollow is a valley in Washington County in the U.S. state of Missouri. Coon Hollow was so named on account of raccoons in the area.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: coon hollow
instance_of: Valley
countries: United States
coordinates: lat: 37.655598
lon: -92.4954486
surface_form: coon hollow
instance_of: Valley
countries: United States
coordinates: lat: 38.0969953
lon: -90.7648534
Coon Hollow (Washington County, Missouri). Coon Hollow is a valley in Washington County in the U.S. state of Missouri. Coon Hollow was so named on account of raccoons in the area.

Geographic entities mentioned:
surface_form: coon hollow
instance_of: Valley
countries: United States
coordinates: lat: 37.655598
lon: -92.4954486
surface_form: coon hollow
instance_of: Valley
countries: United States
coordinates: lat: 38.0969953
lon: -90.7648534
Fourmile Lake (Minnesota). Fourmile Lake is a lake in Grant County, in the U.S. state of Minnesota. Fourmile Lake was named from its distance, from Pomme de Terre station.

Geographic entities mentioned:
surface_form: fourmile lake
instance_of: Lake
countries: United States
coordinates: lat: 46.08111111
lon: -95.98527778
surface_form: fourmile lake
instance_of: Lake
countries: United States
coordinates: lat: 45.7228376
lon: -97.4879312
Fourmile Lake (Minnesota). Fourmile Lake is a lake in Grant County, in the U.S. state of Minnesota. Fourmile Lake was named from its distance, from Pomme de Terre station.

Geographic entities mentioned:
surface_form: fourmile lake
instance_of: Lake
countries: United States
coordinates: lat: 46.08111111
lon: -95.98527778
surface_form: pomme de terre
instance_of: Lake
countries: United States
coordinates: lat: 37.901666666667
lon: -93.320277777778
surface_form: fourmile lake
instance_of: Lake
countries: United States
coordinates: lat: 45.7228376
lon: -97.4879312
The Germans began to withdraw on 17 August, and on 19 August the Allies linked up in Chambois. German counter-attacks forced gaps in the Allied lines, the most significant of which was a corridor forced past the 1st Polish Armoured Division on Hill 262, a commanding position at the pocket mouth.

Geographic entities mentioned:
surface_form: Hill 262
instance_of: Mountain
countries: France
coordinates: lat: 48.84194444
lon: 0.15805556
After capturing Chambois, Polish troops moved northeast and occupied part of the strategic Hill 262 (Mont Ormel ridge), spending the night of 19 August digging in.On the morning of 20 August, Model ordered elements of the 2nd SS Panzer Division and 9th SS Panzer Division to attack from outside the pocket towards the Polish positions.

Geographic entities mentioned:
surface_form: Hill 262
instance_of: Mountain
countries: France
coordinates: lat: 48.84194444
lon: 0.15805556
Fort San, Saskatchewan. Fort San (2016 population:) is a resort village in the Canadian province of Saskatchewan within Census Division No. 6. It is on the shores of Echo Lake of the Fishing Lakes in the Rural Municipality of North Qu'Appelle No. 187. It is west of Fort Qu'Appelle and approximately northeast of Regina. Prior to becoming a resort village, Fort San was originally a sanatorium.

Geographic entities mentioned:
surface_form: Fishing Lakes
instance_of: Group of lakes
countries: Canada
coordinates: lat: 50.78333333333333
lon: -103.81666666666666
During the Civil War, the house was used as a landmark by Jubal Early's Confederate Army to mark their way to Belle Grove for the Battle of Cedar Creek as the house is clearly visible from Signal Knob on the top of Massanutten Mountain where Confederate Scouts had located a weakness in the Union Army's flank where Philip Sheridan was headquartered at Belle Grove.

Geographic entities mentioned:
surface_form: Massanutten Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.643
lon: -78.612
It stretches from northeast to southwest along the center of the peninsula and is made up of volcanoes, mostly shield volcanoes and stratovolcanoes. The highest peak of the range is Ichinsky, a stratovolcano some high. The Sredinny Range is separated from the north-south-running coastal Eastern Range &quot;(Vostochny)&quot; to the east, by the Central Kamchatka Depression.

Geographic entities mentioned:
surface_form: Ichinsky
instance_of: Mountain
countries: Russian Empire
Soviet Union
Russia
coordinates: lat: 55.677777777778
lon: 157.72166666667
Bell Bay Pulp Mill. The Bell Bay Pulp Mill, also known as the Tamar Valley Pulp Mill or Gunns Pulp Mill, was a proposed $2.3 billion pulp mill in which the former Gunns Limited was planning to build in the Tamar Valley, near Launceston, Tasmania.

Geographic entities mentioned:
surface_form: Tamar Valley
instance_of: Valley
countries: Australia