Sarmila/GeoWiki-Features huggingface dataset:
Austrarchaea woodae. &quot;Austrarchaea woodae&quot; is a species of spider in the family Archaeidae. It is commonly known as the Mount Bartle Frere Assassin Spider as the holotype male was found at Mount Bartle Frere in the Wooroonooran National Park. It was named to honour Hannah M. Wood and is endemic to Queensland, Australia.

Geographic entities mentioned:
surface_form: Mount Bartle Frere
instance_of: Mountain
countries: Australia
coordinates: lat: -17.383333333333
lon: 145.81666666667
Mohokos. The Mohokos is the highest peak of a hill range situated in Međimurje County, northern Croatia. The hill range extends for about 20 kilometres across the northwestern part of the County (so called &quot;Upper Međimurje&quot;) in northwest-southeast direction and represents the terminal easternmost slopes of the Alps.

Geographic entities mentioned:
surface_form: mohokos
instance_of: Mountain
countries: Croatia
coordinates: lat: 46.45388889
lon: 16.36361111
The hill range extends for about 20 kilometres across the northwestern part of the County (so called &quot;Upper Međimurje&quot;) in northwest-southeast direction and represents the terminal easternmost slopes of the Alps. As the highest elevation in the County, Mohokos lies exactly 344,4 metres above the sea level. There are meadows, vineyards, orchards and groves around it.

Geographic entities mentioned:
surface_form: mohokos
instance_of: Mountain
countries: Croatia
coordinates: lat: 46.45388889
lon: 16.36361111
There are meadows, vineyards, orchards and groves around it. On the top there is a stone landmark with a built-in polished plaque containing the following text: &quot;The highest geographical point in Međimurje – Mohokos 344,4 m – 26.IX.1999&quot;. Mohokos is a popular tourist destination, especially for many admirers of hiking, hillwalking or bicycle touring.

Geographic entities mentioned:
surface_form: mohokos
instance_of: Mountain
countries: Croatia
coordinates: lat: 46.45388889
lon: 16.36361111
surface_form: mohokos
instance_of: Mountain
countries: Croatia
coordinates: lat: 46.45388889
lon: 16.36361111
West of Akureyri, the Ring Road follows the valley for and then continues through Öxnadalur. Flögusel. Flögusel was the first farm in the valley; south of that point, the valley turns more to the west. A road up from there west across the heath was previously a common route to Hólar, which is in Hjaltadalur. Grjótá. The farm of Grjótá was the birthplace in 1161 of Bishop Guðmundur Arason.

Geographic entities mentioned:
surface_form: Hjaltadalur
instance_of: Valley
countries: Iceland
coordinates: lat: 65.73107
lon: -19.12997
Hörgárdalur. Hörgárdalur () is a valley in north Iceland, the valley of the river Hörgá. It is long and extends southwest from Eyjafjörður, which it meets inland. It is now part of the municipality of Hörgársveit. The valley is wide and fertile at its mouth until its intersection with Öxnadalur; the area on the east side of the river here is known as Þelamörk (Thelamörk).

Geographic entities mentioned:
surface_form: hörgárdalur
instance_of: Valley
countries: Iceland
coordinates: lat: 65.621733
lon: -18.608889
Flögusel. Flögusel was the first farm in the valley; south of that point, the valley turns more to the west. A road up from there west across the heath was previously a common route to Hólar, which is in Hjaltadalur. Grjótá. The farm of Grjótá was the birthplace in 1161 of Bishop Guðmundur Arason. Möðruvellir in Hörgárdalur.

Geographic entities mentioned:
surface_form: hörgárdalur
instance_of: Valley
countries: Iceland
coordinates: lat: 65.621733
lon: -18.608889
Snønutryggen. b3jveepzlswbh2j214mb14qa7usf" xml:space="preserve">Snønutryggen () is a broad, ice-covered ridge rising southeast of Snønutane Peaks in the Mühlig-Hofmann Mountains of Queen Maud Land. It was mapped by Norwegian cartographers from surveys and air photos by the Norwegian Antarctic Expedition (1956–60) and named &quot;Snønutryggen&quot; (&quot;the snow peak ridge&quot;).

Geographic entities mentioned:
surface_form: Snønutane Peaks
instance_of: Mountain
coordinates: lat: -72.08333333
lon: 4.8
Whilst on board the &quot;Challenger&quot;, he took part in the four-year-long &quot;Challenger&quot; expedition of 1872–76 – a scientific expedition that made many discoveries to lay the foundation of oceanography. In 1875, he transferred to the sloop to take part in the British Arctic Expedition, which was sent by the British Admiralty to attempt to reach the North Pole via Smith Sound.

Geographic entities mentioned:
surface_form: Smith Sound
instance_of: Watercourse
countries: Greenland
Canada
coordinates: lat: 78.4167
lon: -74
In 1978 a Christmas Island stamp was issued in his honour. Mount Aldrich, in Antarctica, was named after him by Robert Scott to thank him for his assistance given in preparing for Scott's expedition. Aldrich was promoted to rear-admiral on 21 December 1898, and served as admiral superintendent of Portsmouth Dockyard between 1 September 1899 and 1 September 1902, flagship HMS &quot;Asia&quot;.

Geographic entities mentioned:
surface_form: Mount Aldrich
instance_of: Mountain
coordinates: lat: -80.1167
lon: 158.217
Course. The Olmeta is long and flows through the commune of Olmeta-di-Capocorso. It rises in the center of the peninsula between the Monte Prunu to the southwest and the Monte Stello to the northeast. It flows west past the village of Olmeta-di-Capocorso to enter the sea in the village of Negru. Its mouth is between the mouths of the Fium'Albino to the south and the Guadu Grande to the north.

Geographic entities mentioned:
surface_form: Monte Stello
instance_of: Mountain
countries: France
coordinates: lat: 42.7885533
lon: 9.4185291
Purilactis Group. Purilactis Group () is a heterogeneous group of volcanic, volcano-sedimentary and formations of Cretaceous to Eocene age in Salar de Atacama basin, northern Chile. The group has a stratigraphic thickness of more than 6000 m. The group overlies basement rocks of Late Paleozoic age. The north-south El Bordo Escarpment of Cordillera Domeyko contain the main outcrops of the group.

Geographic entities mentioned:
surface_form: Salar de Atacama basin
instance_of: Lake
Body of water
countries: Chile
coordinates: lat: -23.416666666666668
lon: -68.26666666666667
War in Afghanistan. The Khost-Gardez pass was an important hot spot during the War in Afghanistan. Some notable operations took place near the area including the famous Battle of Tora Bora which occurred only 30 miles north of the pass. Likewise the pass is adjacent to the notorious Shah-i-Kot Valley, which lies south of the Paktia entrance of the pass.

Geographic entities mentioned:
surface_form: Shah-i-Kot Valley
instance_of: Valley
countries: Afghanistan
From the confluence of the L'Abbé river, the current descends the Métabetchouane River to the north on crossing Martine Falls, to the south shore of Lac Saint-Jean; from there, the current crosses the latter on towards the northeast, then borrows the course of the Saguenay River via la Petite Décharge on until Tadoussac where it merges with the Saint Lawrence estuary. Toponymy.

Geographic entities mentioned:
surface_form: Lac Saint-Jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
surface_form: saint-jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
surface_form: la petite décharge
instance_of: Watercourse
countries: Canada
coordinates: lat: 48.277777
lon: -70.980554
L'Abbé River (Métabetchouane River tributary). The L'Abbé river is a tributary of the east bank of the Métabetchouane River, flowing in the municipalities of Saint-André-du-Lac-Saint-Jean and Chambord, in the Le Domaine-du-Roy Regional County Municipality, in the administrative region of Saguenay–Lac-Saint-Jean, in the province of Quebec, in Canada.

Geographic entities mentioned:
surface_form: saint-jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
surface_form: saint-jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
L'Abbé River (Métabetchouane River tributary). The L'Abbé river is a tributary of the east bank of the Métabetchouane River, flowing in the municipalities of Saint-André-du-Lac-Saint-Jean and Chambord, in the Le Domaine-du-Roy Regional County Municipality, in the administrative region of Saguenay–Lac-Saint-Jean, in the province of Quebec, in Canada.

Geographic entities mentioned:
surface_form: l'abbé river (métabetchouane river tributary)
instance_of: Watercourse
countries: Canada
coordinates: lat: 48.375554
lon: -71.988055
Toponymy. The toponym Rivière L'Abbé was formalized on December 5, 1968, at the Place Names Bank of the Commission de toponymie du Québec.

Geographic entities mentioned:
surface_form: rivière l'abbé
instance_of: Watercourse
countries: Canada
coordinates: lat: 48.375554
lon: -71.988055
From its source, the course of the L'Abbé river descends on, with a drop in level of. The first segment is in length and flows north to a stream. Then, it flows over a length of towards the northwest, to its mouth, located on the east bank of the Métabetchouane River in the middle of a rapid zone, facing an island and upstream of the mouth of the Grande Désir river.

Geographic entities mentioned:
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
The mountain is situated in the Puno Region, Melgar Province, Nuñoa District. Collpacaja lies south of the mountain Yanacocha. To the west of Collpacaja is a small lake named Quellhuacocha (&quot;gull lake&quot;).

Geographic entities mentioned:
surface_form: yanacocha
instance_of: Lake
countries: Peru
coordinates: lat: -12.8997
lon: -74.1439
surface_form: collpacaja
instance_of: Mountain
countries: Peru
coordinates: lat: -14.1853
lon: -70.6408
surface_form: yanacocha
instance_of: Lake
countries: Peru
coordinates: lat: -13.4047
lon: -74.5725
surface_form: yanacocha
instance_of: Lake
countries: Peru
coordinates: lat: -12.9525
lon: -74.1194
surface_form: yanacocha
instance_of: Lake
countries: Peru
coordinates: lat: -13.285
lon: -72.0486
surface_form: yanacocha
instance_of: Mountain
countries: Peru
coordinates: lat: -13.97694444
lon: -70.90138889
surface_form: yanacocha
instance_of: Lake
countries: Peru
coordinates: lat: -9.26806
lon: -77.35
Collpacaja (Melgar). Collpacaja (possibly from Quechua &quot;qullpa&quot; salty, salpeter, &quot;qaqa&quot; rock, &quot;salpeter rock&quot;) is a mountain in the southern extension of the Vilcanota mountain range in the Andes of Peru, about high. The mountain is situated in the Puno Region, Melgar Province, Nuñoa District. Collpacaja lies south of the mountain Yanacocha.

Geographic entities mentioned:
surface_form: collpacaja
instance_of: Mountain
countries: Peru
coordinates: lat: -14.1853
lon: -70.6408
The mountain is situated in the Puno Region, Melgar Province, Nuñoa District. Collpacaja lies south of the mountain Yanacocha. To the west of Collpacaja is a small lake named Quellhuacocha (&quot;gull lake&quot;).

Geographic entities mentioned:
surface_form: quellhuacocha
instance_of: Mountain
countries: Peru
coordinates: lat: -12.473611111111
lon: -74.591944444444
Under Rennyo's leadership, Hongan-ji began to expand the teachings of Shinran's Pure Land Buddhism to areas beyond the capital. However, the rapid growth of Hongan-ji was met with hostility by the orthodox Tendai sect based at Enryaku-ji on Mount Hiei, and in 1465, Hongan-ji was destroyed by militant monks from Enryaku-ji and Rennyo was forced to flee Kyoto.

Geographic entities mentioned:
surface_form: Mount Hiei
instance_of: Mountain
countries: Japan
coordinates: lat: 35.066666666667
lon: 135.83833333333
Terrace soils typically are unsuitable for redwoods, although they do occur in ravines and on some bluffs. Point Reyes / Farallon Islands (1m). The Point Reyes/Farallon Islands ecoregion includes the Point Reyes Peninsula, Bodega Head and the sand spit at the north end of Bodega Bay, and the offshore Farallon Islands. The maritime climate is temperate and humid, with frequent fog.

Geographic entities mentioned:
surface_form: Bodega Head
instance_of: Mountain
countries: United States
coordinates: lat: 38.31111111111111
lon: -123.06583333333333
Most of the streams are small, and dry by the end of the summer. The Farallon Islands, about 20 miles southwest of Point Reyes, are a group of small granitic islands providing important habitat for seabirds, seals, and sea lions. A small outlier of the region occurs in the south in Marin County that includes the coniferous and hardwood forests of Mount Tamalpais and Bolinas Ridge.

Geographic entities mentioned:
surface_form: Mount Tamalpais
instance_of: Mountain
countries: United States
coordinates: lat: 37.9291
lon: -122.578
surface_form: Bolinas Ridge
instance_of: Mountain
countries: United States
coordinates: lat: 37.907222222222
lon: -122.62027777778
In Polling in Upper Bavaria a &quot;disaster situation&quot; was reported by the authorities, in Lower Bavaria there were more than 140 rescue operations. Initial estimates of the damage amounted to €1 billion, in Bavaria alone. The flooded area there was twice as large as lake Chiemsee. France. In France, the river Seine burst its banks and one town was evacuated. Four people died in the floods.

Geographic entities mentioned:
surface_form: Chiemsee
instance_of: Lake
countries: Germany
coordinates: lat: 47.89
lon: 12.47
Ramshead Lake. enjpc6hik9lha5j07nf4751lj08x" xml:space="preserve">#REDIRECT Lakes of Grand Teton National Park

Geographic entities mentioned:
surface_form: ramshead lake
instance_of: Lake
countries: United States
coordinates: lat: 43.7764
lon: -110.763
Byrte Hydroelectric Power Station. The Byrte Power Station is a hydroelectric power station located near the lake Byrtevatn in the municipality Tokke in Telemark, Norway. It exploits the water from Botnedalsvatn, a height difference of.

Geographic entities mentioned:
surface_form: Byrtevatn
instance_of: Lake
countries: Norway
coordinates: lat: 59.4975
lon: 7.83638889
Death. He was killed in Karp in 1938. At that time, he was building a new well in the village and had brought in two workers from Anamorava in Kosovo. At the last day of work, they killed him for unclear reasons. Personal affairs or an attack by Yugoslav agents have been put forward as possible explanations.

Geographic entities mentioned:
surface_form: Anamorava
instance_of: Valley
countries: Kosovo
coordinates: lat: 42.46666667
lon: 21.46666667
1263: Raids into Clanricarde in cooperation with Aodh na nGall Ó Conchobair (&quot;anglice&quot; &quot;Hugh O'Conor&quot;) and on his own account into County Mayo. 1272: A series of raids on the islands of Lough Erne. 1273: A series of raids on the Cenél nEógain, apparently with several Connacht chieftains serving as tributaries.

Geographic entities mentioned:
surface_form: Lough Erne
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.48262
lon: -7.80622
They arrived at Tadoussac on May 25 and Jamet went immediately with Samuel de Champlain to meet the Indians at Sault St. Louis. On June 24, 1615, at Rivière des Prairies, he celebrated the first Mass said in Quebec. He sent back to France a relation dated July 15, 1615 (addressed to Cardinal François de Joyeuse).

Geographic entities mentioned:
surface_form: Rivière des Prairies
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.708333333333
lon: -73.479166666667
Ytre Øydnavatnet. Ytre Øydnavatnet is a lake in the municipality of Lyngdal in Agder county, Norway. The lake is located along the river Audna, just south of the lake Øvre Øydnavatnet. The lake sits at an elevation of above sea level. The long lake lies about south of the village of Byremo and about north of the village of Konsmo.

Geographic entities mentioned:
surface_form: ytre øydnavatnet
instance_of: Lake
countries: Norway
coordinates: lat: 58.351388888889
lon: 7.38
Canton is located 20 minutes south of Sioux Falls in southeastern South Dakota. Canton is nestled in the rolling hills of the Sioux Valley, providing an abundance of recreational activities with the Big Sioux River bordering the eastern side, Newton Hills State Park to the south, and Lake Alvin to the north. The city was named by Norwegian settler and former legislator James M. Wahl.

Geographic entities mentioned:
surface_form: Lake Alvin
instance_of: Lake
countries: United States
coordinates: lat: 43.440833333333
lon: -96.611111111111
At around 1758, there were at least 100 people living in the general area of Pearsall's Flats, though this can't be verified by historical records. The number seems suspect unless the &quot;general area&quot; includes the South Branch River Valley eight miles south to The Trough and some 15 miles to the north at the confluence with the North Branch Potomac River.

Geographic entities mentioned:
surface_form: The Trough
instance_of: Landform
countries: United States
coordinates: lat: 39.2236
lon: -78.8575
surface_form: North Branch Potomac River
instance_of: Watercourse
countries: United States
coordinates: lat: 39.5284255
lon: -78.5875141
Boulsworth. Boulsworth is one of the 20 electoral wards that form the Parliamentary constituency of Pendle, Lancashire, England. The ward represents the area surrounding Boulsworth Hill, including the villages of Trawden, Laneshaw Bridge and Wycoller, and returns three councillors to sit on Pendle Borough Council. As of the May 2011 Council election, Boulsworth had an electorate of 4,217.

Geographic entities mentioned:
surface_form: Boulsworth Hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.816630555556
lon: -2.1093194444444
Some of the striking portraits and landscapes from her extended visits to Rhondda in 1943, 1944 and 1945 appeared as illustrations to &quot;Miner's Day&quot; by B. L. Coombes and publications on post-war social and industrial reconstruction. After this, and exploiting her extensive botanical knowledge, she consolidated her work as an illustrator.

Geographic entities mentioned:
surface_form: Rhondda
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.615938888889
lon: -3.4175222222222
Bundala, Amritsar. tf8cyif7texxejxr4khj282p9qw98" xml:space="preserve">&quot;This is about the village in India. For the valley in Pakistan, see Bandala Valley.&quot;
Bandala, also spelt as Bundala, is a large village in Amritsar district situated in Amritsar within the Indian state of Punjab. Demographics.

Geographic entities mentioned:
surface_form: Bandala Valley
instance_of: Valley
countries: Pakistan
coordinates: lat: 33.066
lon: 74.176
She founded the first girls' school in medieval Serbia. One of Helen's palaces was in the town of Brnjak (sometimes called &quot;Brnjaci&quot;) in the territory of modern Kosovo. She also possessed the town of Jeleč at Rogozna mountain. As did other members of the Nemanjić dynasty, she built monasteries and donated to churches.

Geographic entities mentioned:
surface_form: Rogozna
instance_of: Mountain
countries: Serbia
coordinates: lat: 43.01444444
lon: 20.58
Before 2017, the municipality was located in the Moesa district in the Roveredo sub-district, along both banks of the Moesa river. It consists of the village of Cama and the sections of Al Pont and Norantola. Lago di Cama is located in the municipality. Demographics. Cama has a population (as of) of., 13.6% of the population was made up of foreign nationals.

Geographic entities mentioned:
surface_form: Lago di Cama
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.254722222222
lon: 9.2288888888889
Squilax, British Columbia. Squilax is a settlement in British Columbia, located on the northeast shore of Little Shuswap Lake. Squilax, as distinguished from Chase, which is adjacent, refers to the reserve communities of the Little Shuswap Indian Band, whose head offices are on Quaaout Indian Reserve No. 1, one of the five reserves governed by that band.

Geographic entities mentioned:
surface_form: Little Shuswap Lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.84861111111111
lon: -119.6438888888889
The glacier drains the east slopes of Mount Alf and Mount Sharp, and the north slopes of the side ridge that trends 9.15 km from Mount Dalrymple on the main crest of Sentinel Range east-northeast to Robinson Pass, flows northwards and joins Newcomer Glacier northwest of Mount Lanning in Sostra Heights. The glacier is named after the Thracian god Sabazios. Location. Sabazios Glacier is centred at.

Geographic entities mentioned:
surface_form: Mount Alf
instance_of: Mountain
coordinates: lat: -77.9167
lon: -86.1167
surface_form: Mount Dalrymple
instance_of: Mountain
coordinates: lat: -77.93333333
lon: -86.05
surface_form: Mount Lanning
instance_of: Mountain
coordinates: lat: -77.783305555556
lon: -85.75
surface_form: Sostra Heights
instance_of: Plateau
coordinates: lat: -77.8833
lon: -85.4667
These migrants became known as pachucos. &quot;Pachuco&quot; could also have derived from the name of the city of Pachuca, Hidalgo, Mexico, as the majority of Mexican migration to the United States came from the Central Plateau region, of which Hidalgo is a part.

Geographic entities mentioned:
surface_form: Central Plateau
instance_of: Plateau
countries: Mexico
coordinates: lat: 24
lon: -103
War Bonnet Peak. War Bonnet Peak () is located in the southern Wind River Range in the U.S. state of Wyoming. War Bonnet Peak is on the southern side of the Cirque of the Towers, a popular climbing area, rising steeply above Jackass Pass. War Bonnet Peak sits along the Continental Divide, less than across Jackass Pass from Mitchell Peak. Hazards.

Geographic entities mentioned:
surface_form: Cirque of the Towers
instance_of: Landform
countries: United States
coordinates: lat: 42.7833
lon: -109.232
surface_form: war bonnet peak
instance_of: Mountain
countries: United States
coordinates: lat: 42.7611
lon: -109.215
War Bonnet Peak () is located in the southern Wind River Range in the U.S. state of Wyoming. War Bonnet Peak is on the southern side of the Cirque of the Towers, a popular climbing area, rising steeply above Jackass Pass. War Bonnet Peak sits along the Continental Divide, less than across Jackass Pass from Mitchell Peak. Hazards. Encountering bears is a concern in the Wind River Range.

Geographic entities mentioned:
surface_form: war bonnet peak
instance_of: Mountain
countries: United States
coordinates: lat: 42.7611
lon: -109.215
War Bonnet Peak. War Bonnet Peak () is located in the southern Wind River Range in the U.S. state of Wyoming. War Bonnet Peak is on the southern side of the Cirque of the Towers, a popular climbing area, rising steeply above Jackass Pass. War Bonnet Peak sits along the Continental Divide, less than across Jackass Pass from Mitchell Peak. Hazards.

Geographic entities mentioned:
surface_form: war bonnet peak
instance_of: Mountain
countries: United States
coordinates: lat: 42.7611
lon: -109.215
This was done for Pākānui's grandmother, Materoa, who wanted the whānau's mana restored after Ngāti Ruanuku killed her father, Poroumātā, a former resident of the area. Survivors from Ngāti Ruanuku retreated to the Waiapu Valley, where they found refuge among the Wahine-iti people while planning their attack on Pākānui.

Geographic entities mentioned:
surface_form: Waiapu Valley
instance_of: Valley
countries: New Zealand
coordinates: lat: -37.9833
lon: 178.117
Mount Inderbitzen. Mount Inderbitzen () is a mountain rising to over, located south-southeast of Mount Craddock and south of Mount Milton in Owen Ridge, the southernmost part of the Sentinel Range of the Ellsworth Mountains in Antarctica. It surmounts Wessbecher Glacier to the southeast and Sirma Glacier to the northwest. The mountain was first mapped by the U.S.

Geographic entities mentioned:
surface_form: Mount Craddock
instance_of: Mountain
coordinates: lat: -78.633333333333
lon: -85.2
surface_form: Mount Milton
instance_of: Mountain
coordinates: lat: -78.8
lon: -84.8
surface_form: owen
instance_of: Mountain
coordinates: lat: -74.41666667
lon: -62.5
surface_form: milton
instance_of: Mountain
coordinates: lat: -78.8
lon: -84.8
surface_form: craddock
instance_of: Mountain
coordinates: lat: -78.633333333333
lon: -85.2
surface_form: inderbitzen
instance_of: Mountain
coordinates: lat: -78.816666666667
lon: -84.783333333333
surface_form: mount inderbitzen
instance_of: Mountain
coordinates: lat: -78.816666666667
lon: -84.783333333333
Mount Inderbitzen. Mount Inderbitzen () is a mountain rising to over, located south-southeast of Mount Craddock and south of Mount Milton in Owen Ridge, the southernmost part of the Sentinel Range of the Ellsworth Mountains in Antarctica. It surmounts Wessbecher Glacier to the southeast and Sirma Glacier to the northwest. The mountain was first mapped by the U.S.

Geographic entities mentioned:
surface_form: inderbitzen
instance_of: Mountain
coordinates: lat: -78.816666666667
lon: -84.783333333333
surface_form: mount inderbitzen
instance_of: Mountain
coordinates: lat: -78.816666666667
lon: -84.783333333333
It was named by the Advisory Committee on Antarctic Names in 1994 after Anton L. Inderbitzen, who was Associate Chief Scientist in the Division of Polar Programs at the National Science Foundation (NSF) between 1983–86 and was head of the Antarctic Staff at the NSF between 1986 and 1991. From 1991 he was the Deputy Assistant Director for Research at the USGS.

Geographic entities mentioned:
surface_form: inderbitzen
instance_of: Mountain
coordinates: lat: -78.816666666667
lon: -84.783333333333
From 1991 he was the Deputy Assistant Director for Research at the USGS. At the NSF, Inderbitzen was responsible for the coordination and planning of all scientific activities within the United States Antarctic Program, and for the formulation and enforcement of U.S. environmental regulations in Antarctica.

Geographic entities mentioned:
surface_form: inderbitzen
instance_of: Mountain
coordinates: lat: -78.816666666667
lon: -84.783333333333
Bass Lake (Thurston County, Washington). Bass Lake is a lake in the U.S. state of Washington. Bass Lake was named for its stock of bass fish.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: bass lake
instance_of: Lake
countries: United States
coordinates: lat: 36.1414
lon: -81.6843
surface_form: bass lake
instance_of: Lake
countries: United States
coordinates: lat: 47.22611111
lon: -95.5875
surface_form: bass lake
instance_of: Lake
countries: United States
coordinates: lat: 44.69056
lon: -85.710702
surface_form: bass lake
instance_of: Lake
countries: United States
coordinates: lat: 43.819166666667
lon: -94.079166666667
surface_form: bass lake
instance_of: Lake
countries: United States
coordinates: lat: 46.829907
lon: -122.4122768
surface_form: bass lake
instance_of: Lake
countries: United States
coordinates: lat: 37.95027778
lon: -122.77527778
Bass Lake (Thurston County, Washington). Bass Lake is a lake in the U.S. state of Washington. Bass Lake was named for its stock of bass fish.

Geographic entities mentioned:
surface_form: bass lake
instance_of: Lake
countries: United States
coordinates: lat: 36.1414
lon: -81.6843
surface_form: bass lake
instance_of: Lake
countries: United States
coordinates: lat: 47.22611111
lon: -95.5875
surface_form: bass lake
instance_of: Lake
countries: United States
coordinates: lat: 44.69056
lon: -85.710702
surface_form: bass lake
instance_of: Lake
countries: United States
coordinates: lat: 43.819166666667
lon: -94.079166666667
surface_form: bass lake
instance_of: Lake
countries: United States
coordinates: lat: 46.829907
lon: -122.4122768
surface_form: bass lake
instance_of: Lake
countries: United States
coordinates: lat: 37.95027778
lon: -122.77527778
Mountains separate the peninsula into the plains of Pedias, Mesogeia, and the Thriasian Plain. The mountains of Attica are the Hymettus, the eastern portion of the Geraneia, Parnitha (the highest mountain of Attica), Aigaleo and Penteli. Four mountains — Aigaleo, Parnitha, Penteli and Hymettus (clockwise from the southwest) — delineate the hilly plain on which the Athens urban area now spreads.

Geographic entities mentioned:
surface_form: Hymettus
instance_of: Mountain
countries: Greece
coordinates: lat: 37.9465
lon: 23.816666666666666
Mesogeia lies to the east of Mount Hymettus and is bound to the north by the foothills of Mount Penteli, to the east by the Euboean Gulf and Mount Myrrhinous, and to the south by the mountains of Lavrio (modern Lavreotiki), Paneio (Πάνειον Όρος), and Laureotic Olympus (Λαυρεωτικός Όλυμπος). The Lavrio region terminates in Cape Sounion, forming the southeastern tip of the Attic peninsula.

Geographic entities mentioned:
surface_form: Laureotic Olympus
instance_of: Mountain
countries: Greece
coordinates: lat: 37.75252
lon: 23.93272
As a result of these reforms, Attica was divided into approximately a hundred municipalities, the demes (&quot;dēmoi&quot;, δῆμοι), and also into three large sectors: the city (ἄστυ), which comprised the areas of central Athens, Ymittos, Aegaleo and the foot of Mount Parnes, the coast (παράλια), that included the area between Eleusis and Cape Sounion and the area around the city (ἐσωτερικό-μεσογαία), inhabited by people living on the north of Mount Parnitha, Penteliko and the area east of the mountain of Hymettus on the plain of Mesogeia.

Geographic entities mentioned:
surface_form: Hymettus
instance_of: Mountain
countries: Greece
coordinates: lat: 37.9465
lon: 23.816666666666666
The old province of Bari was formerly a part of the region of Terra di Bari, which once included the towns of Fasano and Cisternino, now in the province of Brindisi. The area is dominated by the Murgia hills in the inner part, a karst plateau which is the home of the Alta Murgia National Park, one of the newest national parks in Italy, established in 2004.

Geographic entities mentioned:
surface_form: Murgia
instance_of: Plateau
countries: Italy
coordinates: lat: 40.976
lon: 16.406
The south, on the contrary, does not have large population centers; its only southern municipality near 50,000 inhabitants is Monopoli. In the southern part, on the border with Taranto, is the Itria Valley, between the towns of Alberobello, Locorotondo, Cisternino and Martina Franca.

Geographic entities mentioned:
surface_form: Itria Valley
instance_of: Valley
countries: Italy
coordinates: lat: 40.71667
lon: 17.33333
&quot;Coptodon gutturosa&quot; is a critically endangered species of fish in the cichlid family. It is endemic to Lake Bermin in Cameroon. It is threatened by pollution and sedimentation from human activities, and potentially also by large emissions of carbon dioxide (CO2) from the lake's bottom (compare Lake Nyos), although Bermin is too shallow to contain very high amounts of this gas.

Geographic entities mentioned:
surface_form: Lake Nyos
instance_of: Lake
countries: Cameroon
coordinates: lat: 6.4380555555556
lon: 10.298888888889
Patterson and other investors. Their intent in creating the rail line was to help maintain a steam-powered train line in the Pascack Valley and have future ambitions to build the system northward. Construction on the new long line began in 1866, with trains heading from New York City to the Passaic Street station in Hackensack.

Geographic entities mentioned:
surface_form: Pascack Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.022
lon: -74.053
The hill is the highest point of an Adams County dendritic ridge which Plum Run divides at Big Round Top (the drainage divide continues to the east). In addition to Little Round Top (650 ft.), nearby heights are Warfield Ridge (west), hills of and 540 ft (northwest), and Houck Ridge (north-northwest); while Carr Hill (876 ft) is the nearest higher hill.

Geographic entities mentioned:
surface_form: Warfield Ridge
instance_of: Landform
countries: United States
coordinates: lat: 39.2536
lon: -77.2536
Largely due to the military presence and resource development activities throughout Alaska, Anchorage has enjoyed significant boosts to its population and economic base from 1940 to the present. The 1964 Alaska earthquake outright destroyed or caused significant damage to most of the Anchorage neighborhoods adjacent to Knik Arm, including its downtown.

Geographic entities mentioned:
surface_form: Knik Arm
instance_of: Body of water
countries: United States
coordinates: lat: 61.2
lon: -150.217
Skalisty Golets (Stanovoy Range). Skalisty Golets () is the highest peak in the Stanovoy Range, Russia. The Skalisty Golets is a ‘’golets’’-type of mountain with a bald peak. Administratively it is located in the Sakha Republic (Yakutia) of the Russian Far East.

Geographic entities mentioned:
surface_form: skalisty golets (stanovoy range)
instance_of: Mountain
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 55.85
lon: 130.73333333333
surface_form: skalisty golets
instance_of: Mountain
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 56.400277777778
lon: 119.09583333333
Skalisty Golets (Stanovoy Range). Skalisty Golets () is the highest peak in the Stanovoy Range, Russia. The Skalisty Golets is a ‘’golets’’-type of mountain with a bald peak. Administratively it is located in the Sakha Republic (Yakutia) of the Russian Far East.

Geographic entities mentioned:
surface_form: skalisty golets
instance_of: Mountain
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 56.400277777778
lon: 119.09583333333
Lorze. The Lorze is the main river of the Canton of Zug, Switzerland. It flows from Ägerisee through Lake Zug into the Reuss.

Geographic entities mentioned:
surface_form: Ägerisee
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.12
lon: 8.6161111111111
surface_form: Lake Zug
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.116666666667
lon: 8.4833333333333
Ampato. Ampato (possibly from Quechua &quot;hamp'atu&quot; or from Aymara &quot;jamp'atu&quot;, both meaning &quot;frog&quot;) is a dormant stratovolcano in the Andes of southern Peru. It lies about northwest of Arequipa and is part of a north-south chain that includes the volcanoes Hualca Hualca and Sabancaya, the last of which has been historically active.

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
Geography and geomorphology. Ampato lies south of the Colca Canyon and at the southern end of a chain of volcanoes formed by Hualca Hualca and Sabancaya, the last of which has been historically active. Clockwise from northeast the towns of Colihuiri, Cajamarcana, Sallalli, Japo, Baylillas, Corinta and Collpa surround the volcano; the city of Arequipa lies to the southeast.

Geographic entities mentioned:
surface_form: Colca Canyon
instance_of: Valley
countries: Peru
coordinates: lat: -15.5972
lon: -72.0559
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
Clockwise from northeast the towns of Colihuiri, Cajamarcana, Sallalli, Japo, Baylillas, Corinta and Collpa surround the volcano; the city of Arequipa lies to the southeast. Ampato is part of the Central Volcanic Zone of the Andes, which in Peru manifests itself as several dozen Pleistocene volcanoes, some of which erupted in historical time including El Misti, Huaynaputina, Sabancaya and Ubinas.

Geographic entities mentioned:
surface_form: Huaynaputina
instance_of: Mountain
countries: Peru
coordinates: lat: -16.615555555555556
lon: -70.84972222222223
surface_form: Ubinas
instance_of: Mountain
countries: Peru
coordinates: lat: -16.34861111111111
lon: -70.90222222222222
surface_form: misti
instance_of: Mountain
countries: Peru
coordinates: lat: -16.296388888888888
lon: -71.41055555555556
surface_form: el misti
instance_of: Mountain
countries: Peru
coordinates: lat: -16.296388888888888
lon: -71.41055555555556
surface_form: misti
instance_of: Mountain
countries: Peru
coordinates: lat: -15.525277777778
lon: -71.690833333333
surface_form: huaynaputina
instance_of: Mountain
countries: Peru
coordinates: lat: -16.615555555555556
lon: -70.84972222222223
surface_form: ubinas
instance_of: Mountain
countries: Peru
coordinates: lat: -16.34861111111111
lon: -70.90222222222222
The largest historical eruption of the Andes took place at Huaynaputina. Other volcanoes in the Peruvian Central Volcanic Zone are Sara Sara, Solimana, Coropuna, Andagua volcanic field-Huambo volcanic field, Chachani, Ticsani, Tutupaca, Yucamane, Purupuruni and Casiri. The volcano Ampato consists of three individual steep-sided cones which rise from a gentle glacially eroded foot.

Geographic entities mentioned:
surface_form: Sara Sara
instance_of: Mountain
countries: Peru
coordinates: lat: -15.323527777778
lon: -73.449361111111
surface_form: Andagua volcanic field
instance_of: Mountain
countries: Peru
coordinates: lat: -15.257
lon: -72.483
surface_form: Chachani
instance_of: Mountain
countries: Peru
coordinates: lat: -16.194166666667
lon: -71.531666666667
surface_form: Ticsani
instance_of: Mountain
countries: Peru
coordinates: lat: -16.7675
lon: -70.5997
surface_form: Tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.02638889
lon: -70.37166667
surface_form: Yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
surface_form: Purupuruni
instance_of: Mountain
countries: Peru
coordinates: lat: -17.30916667
lon: -69.91472222
surface_form: andagua volcanic field
instance_of: Mountain
countries: Peru
coordinates: lat: -15.257
lon: -72.483
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0308
lon: -70.4483
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.02638889
lon: -70.37166667
surface_form: yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
surface_form: sara sara
instance_of: Mountain
countries: Peru
coordinates: lat: -15.323527777778
lon: -73.449361111111
surface_form: casiri
instance_of: Mountain
countries: Peru
coordinates: lat: -15.46277778
lon: -72.17138889
surface_form: casiri
instance_of: Mountain
countries: Peru
coordinates: lat: -17.46666667
lon: -69.81333333
surface_form: chachani
instance_of: Mountain
countries: Peru
coordinates: lat: -16.194166666667
lon: -71.531666666667
surface_form: purupuruni
instance_of: Mountain
countries: Peru
coordinates: lat: -17.30916667
lon: -69.91472222
surface_form: solimana
instance_of: Mountain
countries: Peru
coordinates: lat: -15.33111111
lon: -72.16222222
surface_form: solimana
instance_of: Mountain
countries: Peru
coordinates: lat: -15.41
lon: -72.893111111111
surface_form: sara sara
instance_of: Mountain
countries: Peru
coordinates: lat: -14.6381
lon: -72.7881
surface_form: ticsani
instance_of: Mountain
countries: Peru
coordinates: lat: -16.7675
lon: -70.5997
After a pause in volcanic activity and an intermediary stage (&quot;Yanajaja stage&quot;; one date obtained on this stage is 77,000 ± 4,000 years before present) that produced andesitic-dacitic lava flows which form a thick unit on top of eroded remnants of the older Ampato volcanics, the andesitic northern cone formed as the first of the three present-day cones.

Geographic entities mentioned:
surface_form: yanajaja
instance_of: Mountain
countries: Peru
coordinates: lat: -13.79194444
lon: -71.11527778
surface_form: yanajaja
instance_of: Mountain
countries: Peru
coordinates: lat: -13.7914
lon: -71.1158
surface_form: ampato
instance_of: Mountain
countries: Peru
coordinates: lat: -15.820555555555556
lon: -71.88
Ampato is part of the Central Volcanic Zone of the Andes, which in Peru manifests itself as several dozen Pleistocene volcanoes, some of which erupted in historical time including El Misti, Huaynaputina, Sabancaya and Ubinas. The largest historical eruption of the Andes took place at Huaynaputina.

Geographic entities mentioned:
surface_form: huaynaputina
instance_of: Mountain
countries: Peru
coordinates: lat: -16.615555555555556
lon: -70.84972222222223
Ampato. Ampato (possibly from Quechua &quot;hamp'atu&quot; or from Aymara &quot;jamp'atu&quot;, both meaning &quot;frog&quot;) is a dormant stratovolcano in the Andes of southern Peru. It lies about northwest of Arequipa and is part of a north-south chain that includes the volcanoes Hualca Hualca and Sabancaya, the last of which has been historically active.

Geographic entities mentioned:
surface_form: ampato
instance_of: Mountain
countries: Peru
coordinates: lat: -15.820555555555556
lon: -71.88
Ampato consists of three volcanic cones, which lie on top of an older eroded volcanic edifice. They were formed sequentially by extrusion of lava flows, but Ampato has also had explosive eruptions which have deposited ash, lapilli and pumice in the surrounding landscape.

Geographic entities mentioned:
surface_form: ampato
instance_of: Mountain
countries: Peru
coordinates: lat: -15.820555555555556
lon: -71.88
The present-day volcano is covered by an ice cap, and during the last glacial maximum glaciers advanced to low altitudes. In 1995, an Inca mummy known as Mummy Juanita was discovered on Ampato by Johan Reinhard; it had been offered as a human sacrifice more than six hundred years earlier on the mountain. Geography and geomorphology.

Geographic entities mentioned:
surface_form: ampato
instance_of: Mountain
countries: Peru
coordinates: lat: -15.820555555555556
lon: -71.88
A high plateau formed by ignimbrites and lavas of Pliocene to Miocene age rises above this basement. The terrain is cut by several different fault systems; one of these, the northeastward striking Sepina fault has been seismically active in the 20th and 21st centuries and seems to have controlled the development of the Ampato and Sabancaya volcanoes. Composition.

Geographic entities mentioned:
surface_form: ampato
instance_of: Mountain
countries: Peru
coordinates: lat: -15.820555555555556
lon: -71.88
surface_form: ampato
instance_of: Mountain
countries: Peru
coordinates: lat: -15.820555555555556
lon: -71.88
The magmas derive from mantle melts, but undergo additional differentiation processes before reaching the surface. Processes such as fractional crystallization, magma mixing and the absorption of crustal material by developing magmas have been invoked to explain the formation of the magmas of both Ampato and Sabancaya.

Geographic entities mentioned:
surface_form: ampato
instance_of: Mountain
countries: Peru
coordinates: lat: -15.820555555555556
lon: -71.88
Estimating the rate of magma production at Ampato is difficult owing to the uncertainties in determining the volume of the edifice and the duration of repose times between eruptions; on average it appears to be. This rate does not consider &quot;spurt&quot;-like behaviour; volcano growth in fits and spurts has been observed at many other volcanic arc volcanoes.

Geographic entities mentioned:
surface_form: ampato
instance_of: Mountain
countries: Peru
coordinates: lat: -15.820555555555556
lon: -71.88
Eruptive history. Growth of Ampato and Sabancaya commenced no earlier than 800,000 years ago. A thick pile of andesitic lava flows with additional scoria and which crops out on the southern, southeastern and southwestern side of the Ampato volcano is the oldest volcanic stage of this volcano, with argon-argon dating yielding ages between 400,000 - 450,000 years before present.

Geographic entities mentioned:
surface_form: ampato
instance_of: Mountain
countries: Peru
coordinates: lat: -15.820555555555556
lon: -71.88
Above this formation, another pile of dacitic lava flows constructed the first Ampato edifice, which was about the same size as the present-day volcano. This pile (&quot;Moldepampa stage&quot;) is about thick in outcrops and was emplaced between 230,000 - 200,000 years before present.

Geographic entities mentioned:
surface_form: ampato
instance_of: Mountain
countries: Peru
coordinates: lat: -15.820555555555556
lon: -71.88
More than of block-and-ash flows was erupted onto the eastern and western flanks of Ampato, and these flows consist of one andesitic and one dacitic formation; both appear to relate to a lava dome forming stage of volcanic activity.

Geographic entities mentioned:
surface_form: ampato
instance_of: Mountain
countries: Peru
coordinates: lat: -15.820555555555556
lon: -71.88
The dacitic Corinta deposits conversely were created during one large eruption which also left a crater on Ampato; it generated stratified thick tephra deposits which contain pumice embedded within ash-rich layers, and it is probably also the source of the pumice flow deposits on the south-southwestern flank.

Geographic entities mentioned:
surface_form: ampato
instance_of: Mountain
countries: Peru
coordinates: lat: -15.820555555555556
lon: -71.88
These flows are together maximally thick and one flow has been dated to 17,000 ± 6,000 years before present. A dacitic summit lava dome is not affected by glacial erosion and appears to be the youngest eruption product of Ampato. Early Holocene (11,000 - 8,000 years before present) ash layers in peat bogs around the volcano may have originated either on Ampato or on Sabancaya.

Geographic entities mentioned:
surface_form: ampato
instance_of: Mountain
countries: Peru
coordinates: lat: -15.820555555555556
lon: -71.88
Early Holocene (11,000 - 8,000 years before present) ash layers in peat bogs around the volcano may have originated either on Ampato or on Sabancaya. Late Holocene tephra layers dated to 1,790 ± 110, 2,050 ± 70 and 4,500 ± 125 likewise may have been erupted from Ampato, but Sabancaya is a more likely source for these ash layers. Hazards. Presently, Ampato is considered to be a dormant volcano.

Geographic entities mentioned:
surface_form: ampato
instance_of: Mountain
countries: Peru
coordinates: lat: -15.820555555555556
lon: -71.88
surface_form: ampato
instance_of: Mountain
countries: Peru
coordinates: lat: -15.820555555555556
lon: -71.88
Hazards. Presently, Ampato is considered to be a dormant volcano. Potential hazards from future eruptions at Ampato are lahars induced by melting of the icecap and sub-Plinian eruptions, considering the history of explosive eruptions at this volcano. The Peruvian geological service has published a hazard map that describes danger areas of both Ampato and Sabancaya.

Geographic entities mentioned:
surface_form: ampato
instance_of: Mountain
countries: Peru
coordinates: lat: -15.820555555555556
lon: -71.88
The Peruvian geological service has published a hazard map that describes danger areas of both Ampato and Sabancaya. Hazards mapped include both the fall of ash and the formation of lahars which can advance to distances of in the southerly valleys of Ampato.

Geographic entities mentioned:
surface_form: ampato
instance_of: Mountain
countries: Peru
coordinates: lat: -15.820555555555556
lon: -71.88
The subduction started during the Jurassic period after the opening of the southern Atlantic Ocean, which triggered the onset of subduction of the Nazca Plate. Volcanic arc-associated volcanism originally occurred within the Cordillera de la Costa in the Jurassic, but later it migrated resulting in the emplacement of the Tacaza and Toquepala groups and finally the Neogene Barroso group.

Geographic entities mentioned:
surface_form: barroso
instance_of: Mountain
countries: Peru
coordinates: lat: -17.556308
lon: -69.5954717
Volcanic arc-associated volcanism originally occurred within the Cordillera de la Costa in the Jurassic, but later it migrated resulting in the emplacement of the Tacaza and Toquepala groups and finally the Neogene Barroso group. The present-day volcanic arc is situated in the area of the Barroso group but has a narrower extent.

Geographic entities mentioned:
surface_form: barroso
instance_of: Mountain
countries: Peru
coordinates: lat: -17.556308
lon: -69.5954717
West Jordan, Utah. West Jordan is a city in Salt Lake County, Utah, United States. It is a suburb of Salt Lake City. According to the 2020 Census, the city had a population of 116,961, placing it as the third most populous in the state. The city occupies the southwest end of the Salt Lake Valley at an elevation of 4,330 feet (1,320 m).

Geographic entities mentioned:
surface_form: Salt Lake Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.6839
lon: -111.978