Sarmila/GeoWiki-Features huggingface dataset:
The sides negotiated and Takatsugu surrendered. However, in the meantime Tokugawa Ieyasu had won the battle of Sekigahara, assuring his control of all Japan, and so the loss of Ōtsu was ultimately insignificant. Some records of the time indicate that the local inhabitants brought picnic boxes and gathered at Mii-dera on Mount Hiei to observe the battle. Historicity.

Geographic entities mentioned:
surface_form: Mount Hiei
instance_of: Mountain
countries: Japan
coordinates: lat: 35.066666666667
lon: 135.83833333333
Mons Delisle. Mons Delisle is a mountain on the Moon, located on the edge of Mare Imbrium west of the crater Delisle. It is elongated in shape and is about long. The mountain was named after the nearby crater of the same name by the IAU in 1985.

Geographic entities mentioned:
surface_form: mons delisle
instance_of: Mountain
coordinates: lat: 29.42
lon: -35.79
He also established his reputation as a monumental artist working on prestigious construction projects such as the Usher Hall and the Scotsman Building, both in Edinburgh; restoration works at Eilean Donan Castle and St. Magnus' Cathedral in Kirkwall; and also carrying out extensive work in the unusual Saint Conan's Kirk at Loch Awe.

Geographic entities mentioned:
surface_form: Loch Awe
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.291475
lon: -5.231141
This species was described by J.L.B. Smith in 1965 with the type locality given as the coastal swamps near Tamatave. It has since been found in other areas of the island, including the basin of the Nosivolo River and in the Bemarivo River.

Geographic entities mentioned:
surface_form: Bemarivo River
instance_of: Watercourse
countries: Madagascar
coordinates: lat: -14.145833333333
lon: 50.155277777778
Venture then filed on September 25 to construct a digital companion facility on channel 22 broadcasting from Overlook Mountain in Woodstock; the permit was granted on December 23. On December 18, 2014, the station was issued a license for digital operation, with its city of license moving from Kinderhook to Newburgh and its call sign changing to WEPT-CD.

Geographic entities mentioned:
surface_form: Overlook Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.0863
lon: -74.0934
Salisbury Plain () () is a broad coastal plain found with the Bay of Isles on the north coast of South Georgia. It lies between the mouths of Grace and Lucas glaciers on the southern coast of the bay, with Mount Ashley south of it. Best known as the breeding site for as many as 60,000 king penguins, its beaches are also covered with many southern elephant seals and Antarctic fur seals.

Geographic entities mentioned:
surface_form: Mount Ashley
instance_of: Mountain
countries: United Kingdom
coordinates: lat: -54.116666666667
lon: -37.35
WFAS-FM's targeted listening area was Westchester County and the lower Hudson Valley region, initially simulcasting sister station WFAS (1230 AM) before adopting a separate full-service format; it later evolved into an easy listening station, and then an adult contemporary outlet by the mid-1980s.

Geographic entities mentioned:
surface_form: Hudson Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.9209
lon: -73.9613
Topnymic variants: Bras Gariépy, Bras Nord-Ouest, Bras Nord-Ouest du Gouffre, Le Bras, Le Petit Bras, Rivière de l'Usine, Rivière du Bras, Rivière du Gouffre Bras Nord-Ouest, Rivière du Gouffre Nord-Ouest, Rivière du Nord-Ouest, Rivière Placide and Rivière Saint-Placide are variants of the official name.

Geographic entities mentioned:
surface_form: rivière du nord
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.7833
lon: -65.0833
surface_form: rivière du nord
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.53949166666666
lon: -76.389975
surface_form: le petit bras
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.20149
lon: -68.24975
surface_form: rivière du nord
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.69667
lon: -70.41917
surface_form: rivière du nord
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.071647
lon: -71.13151
Bras du Nord-Ouest. The Bras du Nord-Ouest is a tributary of the west bank of the lower part of the rivière du Gouffre, flowing entirely in the city of Baie-Saint-Paul, in the Charlevoix Regional County Municipality, in the administrative region of Capitale-Nationale, in the province of Quebec, in Canada.

Geographic entities mentioned:
surface_form: bras du nord
instance_of: Watercourse
countries: Canada
coordinates: lat: 48.562777777778
lon: -70.995555555556
surface_form: bras du nord-ouest
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.446666111111114
lon: -70.50722194444444
There is an observatory at, at 22.67 east longitude and 37.97 north latitude. From the top a large portion of northeastern Peloponnesus is visible, including the eastern part of Achaia and Chelmos, the Gulf of Corinth and most of Corinthia, the southern part of Corinthia and parts of northeastern Arcadia. The nearest mountain ranges are Oligyrtos to the south and Aroania to the west.

Geographic entities mentioned:
surface_form: Oligyrtos
instance_of: Mountain
countries: Greece
coordinates: lat: 37.807
lon: 22.387
surface_form: oligyrtos
instance_of: Mountain
countries: Greece
coordinates: lat: 37.807
lon: 22.387
Mount Kyllini. Mount Kyllini or Mount Cyllene (;,), also known as Mount Ziria (,), is a mountain on the Peloponnese in Greece famous for its association with the god Hermes. It rises to above sea level, making it the second highest point on the peninsula.

Geographic entities mentioned:
surface_form: ziria
instance_of: Mountain
countries: Greece
coordinates: lat: 37.939166666667
lon: 22.396666666667
surface_form: cyllene
instance_of: Mountain
countries: Greece
coordinates: lat: 37.939166666667
lon: 22.396666666667
surface_form: mount kyllini
instance_of: Mountain
countries: Greece
coordinates: lat: 37.939166666667
lon: 22.396666666667
surface_form: mount cyllene
instance_of: Mountain
countries: Greece
coordinates: lat: 37.939166666667
lon: 22.396666666667
surface_form: kyllini
instance_of: Mountain
countries: Greece
coordinates: lat: 37.939166666667
lon: 22.396666666667
Roads pass near the southern and western slopes, but there are not many on the mountain itself, as much of the mountain is part of a park. The municipal boundary of Stymfalia–Feneos–Evrostini and Xylokastro passes through the mountain. Mythology. Cyllene (or Kyllene) herself was a mountain nymph who had taken for her consort Pelasges in the most ancient times recounted by Greek mythographers.

Geographic entities mentioned:
surface_form: kyllene
instance_of: Mountain
countries: Greece
coordinates: lat: 37.939166666667
lon: 22.396666666667
There was a port in Elis in antiquity named Cyllene near the mouth of the Alfeios, where the traveler Pausanias noted the image of Hermes, &quot;most devoutly worshiped by the inhabitants, is merely the male member upright on the pedestal.&quot;
In Greek mythology, Hermes was born in a sacred cave on the mountain, and so &quot;Cyllenius&quot; is a frequent epithet of his.

Geographic entities mentioned:
surface_form: cyllene
instance_of: Mountain
countries: Greece
coordinates: lat: 37.939166666667
lon: 22.396666666667
The Homeric Hymn &quot;Hymn to Pan&quot; recalled that &quot;Hermes... came to Arkadia... there where his sacred place is as god of Kyllene. For there, though a god, he used to tend curly-fleeced sheep.&quot;
The Pleiades were born on Mount Kyllini. Gaius Julius Hyginus records that it was on Cyllene that the seer Tiresias changed sex when he struck two copulating snakes.

Geographic entities mentioned:
surface_form: mount kyllini
instance_of: Mountain
countries: Greece
coordinates: lat: 37.939166666667
lon: 22.396666666667
surface_form: kyllini
instance_of: Mountain
countries: Greece
coordinates: lat: 37.939166666667
lon: 22.396666666667
Mount Kyllini. Mount Kyllini or Mount Cyllene (;,), also known as Mount Ziria (,), is a mountain on the Peloponnese in Greece famous for its association with the god Hermes. It rises to above sea level, making it the second highest point on the peninsula.

Geographic entities mentioned:
surface_form: mount kyllini
instance_of: Mountain
countries: Greece
coordinates: lat: 37.939166666667
lon: 22.396666666667
surface_form: kyllini
instance_of: Mountain
countries: Greece
coordinates: lat: 37.939166666667
lon: 22.396666666667
It is located near the border between the historic regions of Arcadia and Achaea—in the northeast of Arcadia, and entirely within modern Corinthia. It is located west of Corinth, northwest of Stymfalia, north of Tripoli, and south of Derveni. Several modern places are also named &quot;Kyllini&quot;. Description. Much of the mountain is barren and rocky, although the area below is largely forested.

Geographic entities mentioned:
surface_form: kyllini
instance_of: Mountain
countries: Greece
coordinates: lat: 37.939166666667
lon: 22.396666666667
The area is dominated by volcanoes that often reach over elevation and are of Miocene to Holocene age. Neighbouring volcanoes include San Pedro and San Pablo to the south, Carasilla to the northwest and the Apacheta-Aguilucho volcanic complex to the east which is sometimes grouped with Cerro del Azufre.

Geographic entities mentioned:
surface_form: Apacheta-Aguilucho volcanic complex
instance_of: Mountain
countries: Chile
coordinates: lat: -21.83333333
lon: -68.16666667
surface_form: cerro del azufre
instance_of: Mountain
countries: Chile
coordinates: lat: -21.783055555556
lon: -68.239722222222
surface_form: azufre
instance_of: Mountain
countries: Chile
coordinates: lat: -21.783055555556
lon: -68.239722222222
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -21.887777777777778
lon: -68.39138888888888
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -35.9948665
lon: -70.8863297
Geology. During the last 10 million years, caldera eruptions in the Altiplano-Puna volcanic complex (APVC) have generated ignimbrites and lavas which underlie Cerro del Azufre. The APVC is linked to the Altiplano-Puna Magma Body under the Altiplano; the latter is the highest volcanic plateau in the world.

Geographic entities mentioned:
surface_form: Altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
Cerro Pabellón is one of several geothermal fields in this part of the Andes and the only one where geothermal power is being produced. The field reaches the surface in the Apacheta-Aguilucho volcanic complex but may extend over an area of underground.

Geographic entities mentioned:
surface_form: Apacheta-Aguilucho volcanic complex
instance_of: Mountain
countries: Chile
coordinates: lat: -21.83333333
lon: -68.16666667
Cerro del Azufre. Cerro del Azufre () is a stratovolcano located in El Loa Province, Antofagasta Region, Chile. It is part of a chain of volcanoes that separate Upper Loa River basin from the endorheic Salar de Ascotán basin and is flanked to the west by a dacitic lava dome called Chanka or Pabellón. The 6000 metre volcanoes San Pedro and San Pablo are located to the southwest of Cerro del Azufre.

Geographic entities mentioned:
surface_form: cerro del azufre
instance_of: Mountain
countries: Chile
coordinates: lat: -21.783055555556
lon: -68.239722222222
surface_form: azufre
instance_of: Mountain
countries: Chile
coordinates: lat: -21.783055555556
lon: -68.239722222222
It is part of a chain of volcanoes that separate Upper Loa River basin from the endorheic Salar de Ascotán basin and is flanked to the west by a dacitic lava dome called Chanka or Pabellón. The 6000 metre volcanoes San Pedro and San Pablo are located to the southwest of Cerro del Azufre. Geography and geomorphology.

Geographic entities mentioned:
surface_form: cerro del azufre
instance_of: Mountain
countries: Chile
coordinates: lat: -21.783055555556
lon: -68.239722222222
surface_form: azufre
instance_of: Mountain
countries: Chile
coordinates: lat: -21.783055555556
lon: -68.239722222222
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -21.887777777777778
lon: -68.39138888888888
surface_form: san pedro
instance_of: Mountain
countries: Chile
coordinates: lat: -35.9948665
lon: -70.8863297
The 6000 metre volcanoes San Pedro and San Pablo are located to the southwest of Cerro del Azufre. Geography and geomorphology. Cerro del Azufre lies in northern Chile, close to the border with Bolivia and south of the Salar de Ascotan. highway, which passes northwest from the volcano, connects the city of Calama with Ollagüe town. Formerly, the Inca road system passed east of the volcano.

Geographic entities mentioned:
surface_form: cerro del azufre
instance_of: Mountain
countries: Chile
coordinates: lat: -21.783055555556
lon: -68.239722222222
surface_form: azufre
instance_of: Mountain
countries: Chile
coordinates: lat: -21.783055555556
lon: -68.239722222222
The southern edifice has moraine deposits and gorges formed by erosion; there are also traces of rock glaciers. The Chac-Inca and Cerro Chanka lava domes lie east and west, respectively, between the two edifices of Cerro del Azufre. The area is dominated by volcanoes that often reach over elevation and are of Miocene to Holocene age.

Geographic entities mentioned:
surface_form: cerro del azufre
instance_of: Mountain
countries: Chile
coordinates: lat: -21.783055555556
lon: -68.239722222222
surface_form: azufre
instance_of: Mountain
countries: Chile
coordinates: lat: -21.783055555556
lon: -68.239722222222
Cerro del Azufre and neighbouring volcanoes to the southeast form the Azufre-Inacaliri volcanic chain, which is formed mainly by lava flows with compositions ranging from basaltic andesite to rhyolite. Geology. During the last 10 million years, caldera eruptions in the Altiplano-Puna volcanic complex (APVC) have generated ignimbrites and lavas which underlie Cerro del Azufre.

Geographic entities mentioned:
surface_form: cerro del azufre
instance_of: Mountain
countries: Chile
coordinates: lat: -21.783055555556
lon: -68.239722222222
surface_form: azufre
instance_of: Mountain
countries: Chile
coordinates: lat: -21.783055555556
lon: -68.239722222222
surface_form: azufre
instance_of: Mountain
countries: Chile
coordinates: lat: -21.783055555556
lon: -68.239722222222
Geology. During the last 10 million years, caldera eruptions in the Altiplano-Puna volcanic complex (APVC) have generated ignimbrites and lavas which underlie Cerro del Azufre. The APVC is linked to the Altiplano-Puna Magma Body under the Altiplano; the latter is the highest volcanic plateau in the world.

Geographic entities mentioned:
surface_form: cerro del azufre
instance_of: Mountain
countries: Chile
coordinates: lat: -21.783055555556
lon: -68.239722222222
surface_form: azufre
instance_of: Mountain
countries: Chile
coordinates: lat: -21.783055555556
lon: -68.239722222222
Northwest-southeast trending strike-slip faults run across the volcanic arc and appear to have influenced both the volcanic activity and the formation of ore deposits; they include the Azufre-Inacaliri lineament that Cerro del Azufre is part of. The Pabelloncito graben formed in the Azufre-Inacaliri chain when the volcanoes spread under their own weight and deformed during the Pliocene-Quaternary.

Geographic entities mentioned:
surface_form: cerro del azufre
instance_of: Mountain
countries: Chile
coordinates: lat: -21.783055555556
lon: -68.239722222222
surface_form: azufre
instance_of: Mountain
countries: Chile
coordinates: lat: -21.783055555556
lon: -68.239722222222
surface_form: azufre
instance_of: Mountain
countries: Chile
coordinates: lat: -21.783055555556
lon: -68.239722222222
The Pabelloncito graben formed in the Azufre-Inacaliri chain when the volcanoes spread under their own weight and deformed during the Pliocene-Quaternary. Composition. Volcanic rocks from Cerro del Azufre define an andesite to dacite suite, with plagioclase phenocrysts. The pathways of magma formation are poorly elucidated but appear to have taken place at two different depths under the volcano.

Geographic entities mentioned:
surface_form: cerro del azufre
instance_of: Mountain
countries: Chile
coordinates: lat: -21.783055555556
lon: -68.239722222222
surface_form: azufre
instance_of: Mountain
countries: Chile
coordinates: lat: -21.783055555556
lon: -68.239722222222
The magma would be stored at two levels, and eruptions took place when magma from the lower level entered the upper level. Eruption history. Volcanic activity at Cerro del Azufre took place in four stages. The first stage crops out at isolated sites on the southern flank, and consists of eroded lava flows; one age of 1.1±0.2 million years may be attributable to this unit.

Geographic entities mentioned:
surface_form: cerro del azufre
instance_of: Mountain
countries: Chile
coordinates: lat: -21.783055555556
lon: -68.239722222222
surface_form: azufre
instance_of: Mountain
countries: Chile
coordinates: lat: -21.783055555556
lon: -68.239722222222
Eruption history. Volcanic activity at Cerro del Azufre took place in four stages. The first stage crops out at isolated sites on the southern flank, and consists of eroded lava flows; one age of 1.1±0.2 million years may be attributable to this unit. The second stage was emplaced between about 0.7-0.5 million years ago and forms parts of the western and northern parts of Cerro del Azufre.

Geographic entities mentioned:
surface_form: cerro del azufre
instance_of: Mountain
countries: Chile
coordinates: lat: -21.783055555556
lon: -68.239722222222
surface_form: azufre
instance_of: Mountain
countries: Chile
coordinates: lat: -21.783055555556
lon: -68.239722222222
Current geomorphic processes include landslides. Geothermal activity. While there are no active hydrothermal structures at Cerro del Azufre, traces of extinct fumaroles are found on the western flank of the northern edifice, and active hot springs with temperatures of about occur at the northern foot of Cerro del Azufre.

Geographic entities mentioned:
surface_form: cerro del azufre
instance_of: Mountain
countries: Chile
coordinates: lat: -21.783055555556
lon: -68.239722222222
surface_form: cerro del azufre
instance_of: Mountain
countries: Chile
coordinates: lat: -21.783055555556
lon: -68.239722222222
surface_form: azufre
instance_of: Mountain
countries: Chile
coordinates: lat: -21.783055555556
lon: -68.239722222222
surface_form: azufre
instance_of: Mountain
countries: Chile
coordinates: lat: -21.783055555556
lon: -68.239722222222
The APVC is linked to the Altiplano-Puna Magma Body under the Altiplano; the latter is the highest volcanic plateau in the world. It has a volume of about of partially molten rock and may be the source of heat for geothermal fields, of magma for lava domes that were emplaced in the area during the last 120,000 years and of the Azufre magma.

Geographic entities mentioned:
surface_form: azufre
instance_of: Mountain
countries: Chile
coordinates: lat: -21.783055555556
lon: -68.239722222222
Northwest-southeast trending strike-slip faults run across the volcanic arc and appear to have influenced both the volcanic activity and the formation of ore deposits; they include the Azufre-Inacaliri lineament that Cerro del Azufre is part of. The Pabelloncito graben formed in the Azufre-Inacaliri chain when the volcanoes spread under their own weight and deformed during the Pliocene-Quaternary.

Geographic entities mentioned:
surface_form: azufre
instance_of: Mountain
countries: Chile
coordinates: lat: -21.783055555556
lon: -68.239722222222
Morwell. Morwell is a town in the Latrobe Valley area of Gippsland, in South-Eastern Victoria, Australia approximately 152 km (94 mi) east of Melbourne. Morwell has a population of 14,389 people at the. It is both the capital and administrative centre for the City of Latrobe and the city’s second most populous town after the neighbouring Traralgon.

Geographic entities mentioned:
surface_form: Latrobe Valley
instance_of: Valley
countries: Australia
coordinates: lat: -38.1806
lon: 146.278
The first Europeans to travel through the area include party of Count Paweł Strzelecki on their journey from the Snowy Mountains in April 1840, after Strzelecki had named Australia's highest peak as Mount Kosciuszko.

Geographic entities mentioned:
surface_form: Mount Kosciuszko
instance_of: Mountain
countries: Australia
coordinates: lat: -36.4558303
lon: 148.2635105
It is composed of four villages: Mierag (&quot;Mérág&quot;), Tărcaia, Tărcăița (&quot;Tárkányka&quot;) and Totoreni (&quot;Tatárfalva&quot;). Geography. Tărcaia lies along the river bank of the Crișul Negru in the southeastern part of Bihor County,
around 65 km south-east of Oradea and 4 km south of Beiuș. Ethnic groups.

Geographic entities mentioned:
surface_form: Crișul Negru
instance_of: Watercourse
countries: Romania
Hungary
coordinates: lat: 46.700277777778
lon: 21.269166666667
Uru language. The Uru language, more specifically known as Iru-Itu, and Uchumataqu, is an extinct language formerly spoken by the Uru people. In 2004, it had 2 remaining native speakers out of an ethnic group of 140 people in the La Paz Department, Bolivia near Lake Titicaca, the rest having shifted to Aymara and Spanish.

Geographic entities mentioned:
surface_form: Lake Titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
Lake Horney. Lake Horney, named for Julius Teague Horney, is a lake that is located in Polk County, Florida. History. The lake is named after Julius Teague Horney (1888–1959), who helped develop Lakeland in the 1920s.

Geographic entities mentioned:
surface_form: lake horney
instance_of: Lake
countries: United States
coordinates: lat: 28.03316
lon: -81.93909
According to the Britannica, the Changchenmo Range and Pangong Range are sometimes considered easternmost part of the Karakoram Range. &quot;Kailash Range&quot;, runs along southern bank of the Pangong Tso, from centre of Pangong Tso at Lukung to the west to Phursook Bay and Mount Kailash. Sino-Indian border dispute. Pangong Tso is disputed territory.

Geographic entities mentioned:
surface_form: Mount Kailash
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 31.066944444444
lon: 81.312777777778
surface_form: pangong
instance_of: Lake
countries: People's Republic of China
India
coordinates: lat: 33.70472222222222
lon: 78.75
Sino-Indian border dispute. Pangong Tso is disputed territory. The Line of Actual Control (LAC) passes through the lake. A section of the lake approximately 20 km east from the LAC is controlled by China but claimed by India. To the south is the smaller Spanggur Tso lake. The eastern end of the lake is in Tibet.

Geographic entities mentioned:
surface_form: Spanggur Tso
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 33.53638889
lon: 78.90888889
On 29–30 August 2020, Indian troops occupied many heights on the south bank of Pangong Tso. The heights included Rezang La, Reqin La, Black Top, Hanan, Helmet, Gurung Hill, Gorkha Hill and Magar Hill. Some of these heights are in the grey zone of the LAC and overlook Chinese camps. India chose to pull back from these positions as leverage for larger disengagement.

Geographic entities mentioned:
surface_form: Gurung Hill
instance_of: Mountain
countries: India
People's Republic of China
coordinates: lat: 33.6116
lon: 78.7531
Pangong Tso. Pangong Tso or Pangong Lake (;;) is an endorheic lake spanning eastern Ladakh and West Tibet situated at an elevation of. It is long and divided into five sublakes, called &quot;Pangong Tso&quot;, &quot;Tso Nyak&quot;, &quot;Rum Tso&quot; (twin lakes) and &quot;Nyak Tso&quot;.

Geographic entities mentioned:
surface_form: pangong
instance_of: Lake
countries: People's Republic of China
India
coordinates: lat: 33.70472222222222
lon: 78.75
surface_form: pangong tso
instance_of: Lake
countries: People's Republic of China
India
coordinates: lat: 33.70472222222222
lon: 78.75
Pangong Tso. Pangong Tso or Pangong Lake (;;) is an endorheic lake spanning eastern Ladakh and West Tibet situated at an elevation of. It is long and divided into five sublakes, called &quot;Pangong Tso&quot;, &quot;Tso Nyak&quot;, &quot;Rum Tso&quot; (twin lakes) and &quot;Nyak Tso&quot;.

Geographic entities mentioned:
surface_form: pangong tso
instance_of: Lake
countries: People's Republic of China
India
coordinates: lat: 33.70472222222222
lon: 78.75
The whole lake group was and is still often referred to as Tsomo Nganglha Ringpo () in Tibetan. There are different interpretations of the meanings of both &quot;Pangong Tso&quot; and &quot;Tsomo Nganglha Ringpo&quot;. The Ladakh government website says &quot;Pangong Tso&quot; is Tibetan, meaning &quot;high grassland lake&quot;, however travel books say Pangong means &quot;hollow&quot;.

Geographic entities mentioned:
surface_form: pangong tso
instance_of: Lake
countries: People's Republic of China
India
coordinates: lat: 33.70472222222222
lon: 78.75
surface_form: pangong tso
instance_of: Lake
countries: People's Republic of China
India
coordinates: lat: 33.70472222222222
lon: 78.75
The whole lake group was and is still often referred to as Tsomo Nganglha Ringpo () in Tibetan. There are different interpretations of the meanings of both &quot;Pangong Tso&quot; and &quot;Tsomo Nganglha Ringpo&quot;. The Ladakh government website says &quot;Pangong Tso&quot; is Tibetan, meaning &quot;high grassland lake&quot;, however travel books say Pangong means &quot;hollow&quot;.

Geographic entities mentioned:
surface_form: pangong
instance_of: Lake
countries: People's Republic of China
India
coordinates: lat: 33.70472222222222
lon: 78.75
Geography. Pangong Tso is surrounded by three mountain ranges: Changchenmo Range to the north, Pangong Range to the west, and Kailash Range (Gangdise Shan range) to the south. According to the Britannica, the Changchenmo Range and Pangong Range are sometimes considered easternmost part of the Karakoram Range.

Geographic entities mentioned:
surface_form: pangong
instance_of: Lake
countries: People's Republic of China
India
coordinates: lat: 33.70472222222222
lon: 78.75
To the south is the smaller Spanggur Tso lake. The eastern end of the lake is in Tibet. After the mid-19th century, Pangong Tso was at the southern end of Johnson Line, an early attempt at demarcation between India and China in the Aksai Chin region. Khurnak Fort lies on the northern bank of the lake, about halfway up Pangong Tso.

Geographic entities mentioned:
surface_form: pangong tso
instance_of: Lake
countries: People's Republic of China
India
coordinates: lat: 33.70472222222222
lon: 78.75
In 1929, following the protests of Kashmir Durbar, they decided to drop the British claims made in behalf of Kashmir state. The Chinese established their military presence in the Khurnak Fort by 1958. On 20 October 1962, Pangong Tso saw military action during the Sino-Indian War, successful for the Chinese People's Liberation Army (PLA). The area remains a sensitive border point along the LAC.

Geographic entities mentioned:
surface_form: pangong tso
instance_of: Lake
countries: People's Republic of China
India
coordinates: lat: 33.70472222222222
lon: 78.75
Vilamacolum. Vilamacolum () is a municipality and village in the &quot;comarca&quot; of Alt Empordà, Girona, Catalonia. It is on the left side of the Fluvià river, in a flat land. The local economy is based on agriculture and tourism. The Catalan writer Maria Àngels Anglada lived and died in Vilamacolum.

Geographic entities mentioned:
surface_form: Fluvià
instance_of: Watercourse
countries: Spain
coordinates: lat: 42.0934
lon: 2.4591
Mambéré-Kadéï. Mambéré-Kadéï is one of the 20 prefectures of the Central African Republic. Its capital is Berbérati. It is named for the Mambéré River and Kadéï River. The prefecture covers an area of 13,740 km² and, according to official estimates, its population was 281,286 inhabitants in 2024.

Geographic entities mentioned:
surface_form: Kadéï River
instance_of: Watercourse
countries: Central African Republic
Cameroon
coordinates: lat: 3.51944444
lon: 16.04305556
East Valley School District (Spokane, Washington). East Valley School District encompasses approximately in the City of Spokane Valley and areas of unincorporated Spokane County. The district boundaries extend from Butler Road in Spokane Valley east to the Idaho border, and from the Spokane River north to the foothills of Mount Spokane.

Geographic entities mentioned:
surface_form: Mount Spokane
instance_of: Mountain
countries: United States
coordinates: lat: 47.9236
lon: -117.112
Between 698 and 701 the northern and western frontiers of Qapaghan's state were defined by the Tannu Ola, Altai and Tarbagatai mountain ranges. After defeating the Bayirku tribe in 706–707, the Türks occupied lands extending from the upper reaches of the Kerulen to Lake Baikal.

Geographic entities mentioned:
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
Grahovac, Montenegro. Grahovac (Montenegrin Cyrillic: Граховац) is a village in western Montenegro, in the municipality of Nikšić. The village is located on a karst plateau overlooking the Grahovo field and Lake Grahovo. According to the 2011 census, it had 117 inhabitants, vast majority of which are ethnic Montenegrins. History.

Geographic entities mentioned:
surface_form: Lake Grahovo
instance_of: Lake
countries: Montenegro
coordinates: lat: 42.67083333
lon: 18.63
The summit can be approached from the Quartz Mountain Trailhead over Chiquito pass or from one of two trailheads on the road to Glacier Point. In 1871, influential Scottish-American naturalist John Muir discovered an active alpine glacier below Merced Peak, which helped his theory that Yosemite Valley was formed by glacial action gain acceptance. Climate.

Geographic entities mentioned:
surface_form: yosemite
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
surface_form: merced peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.6352
lon: -119.395
Merced Peak. Merced Peak, with an elevation of, is the highest point in the Clark Range, just surpassing three other peaks; Red Peak (11,704 feet), Gray Peak (11,578 feet), and Mount Clark (11,527 feet). Merced Peak is located close to southern border of Yosemite National Park, near the Ottoway Lakes.

Geographic entities mentioned:
surface_form: yosemite
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
surface_form: merced peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.6352
lon: -119.395
Merced Peak. Merced Peak, with an elevation of, is the highest point in the Clark Range, just surpassing three other peaks; Red Peak (11,704 feet), Gray Peak (11,578 feet), and Mount Clark (11,527 feet). Merced Peak is located close to southern border of Yosemite National Park, near the Ottoway Lakes.

Geographic entities mentioned:
surface_form: gray peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.1114
lon: -73.9349
surface_form: mount clark
instance_of: Mountain
countries: United States
coordinates: lat: 47.8355277
lon: -123.2317826
surface_form: merced peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.6352
lon: -119.395
Merced Peak. Merced Peak, with an elevation of, is the highest point in the Clark Range, just surpassing three other peaks; Red Peak (11,704 feet), Gray Peak (11,578 feet), and Mount Clark (11,527 feet). Merced Peak is located close to southern border of Yosemite National Park, near the Ottoway Lakes.

Geographic entities mentioned:
surface_form: merced peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.6352
lon: -119.395
Climate. According to the Köppen climate classification system, Merced Peak is located in an alpine climate zone. Most weather fronts originate in the Pacific Ocean, and travel east toward the Sierra Nevada mountains. As fronts approach, they are forced upward by the peaks (orographic lift), causing moisture in the form of rain or snowfall to drop onto the range.

Geographic entities mentioned:
surface_form: merced peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.6352
lon: -119.395
Merced Peak is located close to southern border of Yosemite National Park, near the Ottoway Lakes. The summit can be approached from the Quartz Mountain Trailhead over Chiquito pass or from one of two trailheads on the road to Glacier Point.

Geographic entities mentioned:
surface_form: quartz mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.1635
lon: -122.672
Weggis landing stage. Weggis landing stage is a ferry port in the municipality of Weggis, in the Swiss canton of Lucerne. It is located on a projection of the Rigi mountain that protrudes into the northern part of Lake Lucerne. It is served by the Lake Lucerne Navigation Company.

Geographic entities mentioned:
surface_form: Rigi
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.05
lon: 8.4666666666667
surface_form: Lake Lucerne
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.0194
lon: 8.4011
rebuilt, with a silver statue and iron doors (?)&quot;. The city of Umm el-Jimal may have also been destroyed by the Palmyrenes in connection with their efforts to subjugate the Tanukhids. After his victory, Zabdas marched south along the Jordan Valley and apparently met little opposition. There is evidence that Petra was attacked by a small contingent which penetrated the region.

Geographic entities mentioned:
surface_form: Jordan Valley
instance_of: Valley
countries: Jordan
Lebanon
Israel
Syria
State of Palestine
coordinates: lat: 32.317222222222
lon: 35.57
Shirebourne brook. The Shirebourne is a brook that rises in King George's Fields, Hadley, and eventually joins the Pymmes Brook. It may have marked the historic county boundary between Hertfordshire and Middlesex. Location. The Shirebourne rises in King George's Fields, Hadley.

Geographic entities mentioned:
surface_form: shirebourne brook
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 51.65154
lon: -0.16645
The river flows southwest to the Manicouagan Reservoir. It is about long, and has a vertical drop of. The sources of the water are in the Uapishka Biodiversity Reserve, which also feeds the Toulnustouc and Manicouagan rivers. The Hart Jaune is one of the major inlets to the Manicouagan Reservoir, along with the Mouchalagane, Seignelay, Themines and Petite Riviere Manicouagan.

Geographic entities mentioned:
surface_form: Toulnustouc
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.59361111
lon: -68.39333333
It is about long, and has a vertical drop of. The sources of the water are in the Uapishka Biodiversity Reserve, which also feeds the Toulnustouc and Manicouagan rivers. The Hart Jaune is one of the major inlets to the Manicouagan Reservoir, along with the Mouchalagane, Seignelay, Themines and Petite Riviere Manicouagan. The reservoir is drained by the Manicouagan River.

Geographic entities mentioned:
surface_form: Seignelay
instance_of: Watercourse
countries: Canada
coordinates: lat: 51.613611
lon: -69.065278
surface_form: hart jaune
instance_of: Watercourse
countries: Canada
coordinates: lat: 51.52305555555556
lon: -68.33333333333333
surface_form: petite riviere
instance_of: Watercourse
countries: Canada
coordinates: lat: 44.226597
lon: -64.434607
Hart Jaune River. The Hart Jaune River () is a river in Quebec, Canada. It flows from the Petit lac Manicouagan to the Manicouagan Reservoir. Location. The Hart Jaune River is in the unorganized territory of Rivière-Mouchalagane in the Caniapiscau Regional County Municipality.

Geographic entities mentioned:
surface_form: hart jaune river
instance_of: Watercourse
countries: Canada
coordinates: lat: 51.52305555555556
lon: -68.33333333333333
It flows from the Petit lac Manicouagan to the Manicouagan Reservoir. Location. The Hart Jaune River is in the unorganized territory of Rivière-Mouchalagane in the Caniapiscau Regional County Municipality. It forms the outlet of the Petit lac Manicouagan at the Hart-Jaune Dam, which feeds the 45.5 MW Hart-Jaune generating station. The river flows southwest to the Manicouagan Reservoir.

Geographic entities mentioned:
surface_form: hart jaune river
instance_of: Watercourse
countries: Canada
coordinates: lat: 51.52305555555556
lon: -68.33333333333333
The name was approved in 1945 and appears on a 1962 map of Quebec. The river has also been called the Rivière La Ferté. Geology. The course of the river roughly corresponds to the Hart Jaune Shear Zone (HJSZ) as proposed by Hynes et al. (2000). Southeast extension occurred along the shear zone during the Rigolet Pulse 1010–980 Ma) of the Grenville orogeny.

Geographic entities mentioned:
surface_form: hart jaune
instance_of: Watercourse
countries: Canada
coordinates: lat: 51.52305555555556
lon: -68.33333333333333
The course of the river roughly corresponds to the Hart Jaune Shear Zone (HJSZ) as proposed by Hynes et al. (2000). Southeast extension occurred along the shear zone during the Rigolet Pulse 1010–980 Ma) of the Grenville orogeny. Hart Jaune granite and anorthosite have thrust from the northwest under the shear zone and the allochthonous Hart Jaune terrane of Pinwarian crust to the southeast.

Geographic entities mentioned:
surface_form: hart jaune
instance_of: Watercourse
countries: Canada
coordinates: lat: 51.52305555555556
lon: -68.33333333333333
The park also has marshy areas, rolling grassy hills, and wooded savannah. The Ngurdoto Crater, the Momela Lakes, and one of the sources of the Pangani River are within the park. Wild animals and birds reported in the park include elephant (uncommon), leopard, waterbuck, spotted hyena, giraffe, blue monkey, colobus monkey, turaco, trogon, African buffalo, warthog, klipspringer, and red-hot poker.

Geographic entities mentioned:
surface_form: Momela Lakes
instance_of: Lake
countries: Tanzania
Gombe Stream National Park. The second smallest of Tanzania's national parks is Gombe Stream National Park is located in Kigoma District of Kigoma Region, covering an area of only. Its natural topography consists of steep hill slopes, river valleys, and the sandy northern shores of Lake Tanganyika. It is drained by the Gombe River. Access to the park is only through marine vessels from Kigoma.

Geographic entities mentioned:
surface_form: Lake Tanganyika
instance_of: Lake
countries: Tanzania
Democratic Republic of the Congo
Burundi
Zambia
coordinates: lat: -6.1
lon: 29.5
The park’s headquarters is located at Matamba inside the park, which is from Mbeya town. Mahale Mountains National Park. Mahale Mountains National Park, next to the Gombe Stream National Park is set on the shores of the Lake Tanganyika in Uvinza District of Kigoma Region, with a watershed comprising richly forested Mahale Mountains with its peaks as high as above the lake shore.

Geographic entities mentioned:
surface_form: Lake Tanganyika
instance_of: Lake
countries: Tanzania
Democratic Republic of the Congo
Burundi
Zambia
coordinates: lat: -6.1
lon: 29.5
Lake Manyara National Park. Lake Manyara National Park, which encompasses an area of includes (at high water stage) of Lake Manyara, an alkaline lake, below the high rift valley; Ernest Hemingway called this lake “the loveliest I had seen in Africa” is located in both in Arusha Region and Manyara Region.

Geographic entities mentioned:
surface_form: Lake Manyara
instance_of: Lake
countries: Tanzania
coordinates: lat: -3.5833333333333
lon: 35.833333333333
Rubondo Island National Park is an island park with an area of. It is located in Geita Region, west of Mwanza. It includes nine smaller islands. It is in the lacustrine wetland ecosystem on the shores of the Lake Victoria. Known as a &quot;water wonderland&quot;, it is fish breeding ground; tilapia, yellow-spotted otters and Nile perch (as heavy as) are some of the special species.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
Serengeti National Park. Serengeti National Park is the oldest and most popular national park which was established in 1951, with an area of located entirely in Mara Region. The habitat, bounded by Kenya and bordered by Lake Victoria on the west, is characterized by vast plains, savannah, wooded hills, large termite mounds, rivers, and acacia woodlands.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
Tarangire National Park. Tarangire National Park is the sixth largest national park in Tanzania named after the Tarangire River which flows through the park and is a perennial river that assures water to both humans and animals even during the dry period. The park is located within Manyara Region and It has an area of to the south east of Lake Manyara.

Geographic entities mentioned:
surface_form: Lake Manyara
instance_of: Lake
countries: Tanzania
coordinates: lat: -3.5833333333333
lon: 35.833333333333
2008–2012. In 2012 Jurečka represented the Czech Republic at the European Judo Championships in Chelyabinsk, Russia. Death. Jurečka died on 25 September 2015 while scuba diving with friends in Lake Garda, Italy. Divers from Trento found Jurečka's body after searching for him in of water. The probable cause of Jurečka's death was a technical defect in his equipment.

Geographic entities mentioned:
surface_form: Lake Garda
instance_of: Lake
countries: Italy
coordinates: lat: 45.633333333333
lon: 10.666666666667
Crozzon di Lares. The Crozzon di Lares is a mountain in Trentino-Alto Adige, Italy. It is located in Val Rendena, Province of Trento. Its summit was conquered for the first time by a young Bohemian climber, Julius von Payer, along with Coronna, Gries and Hayer, on 3 September 1868; on the same day they also reached the nearby Corno di Cavento.

Geographic entities mentioned:
surface_form: Val Rendena
instance_of: Valley
countries: Italy
coordinates: lat: 46.1149
lon: 10.7536
It is located in Val Rendena, Province of Trento. Its summit was conquered for the first time by a young Bohemian climber, Julius von Payer, along with Coronna, Gries and Hayer, on 3 September 1868; on the same day they also reached the nearby Corno di Cavento. It was the theater of bitter fighting during World War I; held by Austro-Hungarian troops, it was captured by the Alpini on 29 April 1916.

Geographic entities mentioned:
surface_form: Corno di Cavento
instance_of: Mountain
countries: Italy
coordinates: lat: 46.1356
lon: 10.5864
Crozzon di Lares. The Crozzon di Lares is a mountain in Trentino-Alto Adige, Italy. It is located in Val Rendena, Province of Trento. Its summit was conquered for the first time by a young Bohemian climber, Julius von Payer, along with Coronna, Gries and Hayer, on 3 September 1868; on the same day they also reached the nearby Corno di Cavento.

Geographic entities mentioned:
surface_form: crozzon di lares
instance_of: Mountain
countries: Italy
coordinates: lat: 46.1486
lon: 10.5922
The Prespa minnow is endemic to the Lake Prespa drainage system which is located in Albania, Greece and North Macedonia. It is also present in the Lake Malik basin in the upper Devoll which they may have colonised through a former canal connecting the Devoll with the Prespa drainage. Within the Prespa lakes the Prespa minnow is found in the littoral zone, commonest in densely vegetated areas.

Geographic entities mentioned:
surface_form: Lake Malik
instance_of: Lake
countries: Albania
coordinates: lat: 40.733333333333334
lon: 20.766666666666666
Stephnes&quot;, left New York December 29, 1876 for San Francisco. The ship was the first to use the newly opened East River channel through Hell Gate then passing around South America through the Strait of Magellan. After voyage repairs at San Francisco the ship departed for Portland, Oregon on March 24, 1877.

Geographic entities mentioned:
surface_form: Hell Gate
instance_of: Landform
countries: United States
coordinates: lat: 40.78102
lon: -73.92452
Iskayuni. Iskayuni (Aymara &quot;iskayu&quot; headdress, &quot;-ni&quot; a suffix, &quot;the one with the headdress&quot;, also spelled &quot;Escayuni&quot;) is a mountain in the Bolivian Andes which reaches a height of approximately. It is located in the La Paz Department, Inquisivi Province, Quime Municipality. Iskayuni lies northeast of Wisk'achani.

Geographic entities mentioned:
surface_form: iskayuni
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.03388889
lon: -67.32916667
The river flows roughly southwestwards through one of the wide ravines of glacial origin that are characteristic of the plateau. As it descends to the Kulunda Plain there are many lakes in its basin, especially close to Andronovo and Nizhnechumanka. Near its mouth the river turns westwards. Finally it meets the eastern shore of Lake Kulunda about west of Shimolino. Tributaries.

Geographic entities mentioned:
surface_form: Lake Kulunda
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53
lon: 79.516666666667
To the east, west, and south of the Quadrilateral, forces of volunteers from the Italian states began to gather in order to fight against the Austrians. The Austrian forces were only able to maintain links to the motherland via a corridor to the north, running through the Adige valley on the eastern coast of Lake Garda. The Piedmontese army.

Geographic entities mentioned:
surface_form: Lake Garda
instance_of: Lake
countries: Italy
coordinates: lat: 45.633333333333
lon: 10.666666666667
The insurrection in Cadore. In Cadore, from 29 April 1848 for over a month, a small armed rebellion of around 4,000 poorly armed men clashed with hostile forces sent from Austria to Belluno, where they were meant to link up with the forces of Nugent.

Geographic entities mentioned:
surface_form: Cadore
instance_of: Valley
countries: Italy
coordinates: lat: 46.50916667
lon: 12.35722222
Mount Logan (disambiguation). pgrq791s1l8qof5vffeh1eilzwes" xml:space="preserve">Mount Logan is the highest mountain in Canada.

Geographic entities mentioned:
surface_form: Mount Logan
instance_of: Mountain
countries: Canada
coordinates: lat: 60.567222222222
lon: -140.40277777778
Telmatochromis temporalis. &quot;Telmatochromis temporalis&quot; is a species of cichlid endemic to Lake Tanganyika where they areas with rocky substrates usually at depths of from though occasionally down to. This species can reach a length of TL. It can also be found in the aquarium trade.

Geographic entities mentioned:
surface_form: Lake Tanganyika
instance_of: Lake
countries: Tanzania
Democratic Republic of the Congo
Burundi
Zambia
coordinates: lat: -6.1
lon: 29.5
It was named &quot;Østerdalens Social-Demokrat&quot; from 1915 to 1919 and &quot;Hedmark Fylkes Arbeiderblad&quot; from 1923 to 1925. Pre-history. The Labour Party for many years lacked an organ in the region Østerdalen. The region was to a certain degree covered by &quot;Hedemarkens Amts Socialdemokrat (Solungen)&quot; from 1908, and by &quot;Demokraten&quot; from September 1909.

Geographic entities mentioned:
surface_form: Østerdalen
instance_of: Valley
countries: Norway
coordinates: lat: 61.575916666666664
lon: 11.087111111111112
Dajia Lake. Dajia Lake () or Tak Kyel Tso (), is a lake in Saga County in the Shigatse Prefecture of the Tibet Autonomous Region of China. It is located about halfway between Lake Peiku and Zhari Namco, northeast of Saga.

Geographic entities mentioned:
surface_form: Zhari Namco
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 30.9167
lon: 85.6333
surface_form: namco
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 30.720833333333
lon: 90.468055555556
Dajia Lake. Dajia Lake () or Tak Kyel Tso (), is a lake in Saga County in the Shigatse Prefecture of the Tibet Autonomous Region of China. It is located about halfway between Lake Peiku and Zhari Namco, northeast of Saga.

Geographic entities mentioned:
surface_form: tak kyel tso
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 29.84277778
lon: 85.73166667
surface_form: dajia lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 29.84277778
lon: 85.73166667