Sarmila/GeoWiki-Features huggingface dataset:
Beginning in 1895, local high schools held crew races on the lake. In 1952, the lake played host to the National Olympic rowing trials. The Quinsigamond Rowing Association hosted the US Rowing Masters National Championship in 2005, 2012 and 2016. Mandaean ritual use. The Mandaean-American community of Worcester regularly performs masbuta (baptism) rituals in Lake Quinsigamond.

Geographic entities mentioned:
surface_form: lake quinsigamond
instance_of: Lake
countries: United States
coordinates: lat: 42.270833333333
lon: -71.755
Cerro Otto. Cerro Otto is a mountain located from San Carlos de Bariloche, and inside the Nahuel Huapí National Park, in Patagonia, Argentina. Etymology. It took its name from German pioneer Otto Goedecke, who arrived to Bariloche in 1892 and dwelled nearby. History. The summit is and there is a cable car which takes twelve minutes to reach the top. The mountain is west of Bariloche.

Geographic entities mentioned:
surface_form: cerro otto
instance_of: Mountain
countries: Argentina
coordinates: lat: -41.1448
lon: -71.3758
The mountain is west of Bariloche. There is a gravel road which allows people to bike, hike or drive the to the top. There is a restaurant that revolves on the summit. The revolving restaurant is the Giratoria confectionery, and there is also a &quot;Refugio del cerro Otto&quot; grill which makes bondiola sandwiches. There is a zip line which is above the terrain and a climbing wall. Description.

Geographic entities mentioned:
surface_form: cerro otto
instance_of: Mountain
countries: Argentina
coordinates: lat: -41.1448
lon: -71.3758
Due to its prominence, Cerro Otto is notably a visual reference while navigating the city as it stands in between the neighbourhoods of San Joaquin, Los Cipresales, Las Vertientes, Los Maitenes, Melipal, El Faldeo, Parque Cerro Otto, Virgen Misionera, Peumayen (colloquially known as &quot;the kilometers&quot;) from the North and El Frutillar, 645 Viviendas, Lomas del Cauquen, and Arelauquen Country Club from the South.

Geographic entities mentioned:
surface_form: cerro otto
instance_of: Mountain
countries: Argentina
coordinates: lat: -41.1448
lon: -71.3758
surface_form: cerro otto
instance_of: Mountain
countries: Argentina
coordinates: lat: -41.1448
lon: -71.3758
Rów Kunowski. Rów Kunowski is a river of Poland that flows into Lake Miedwie.

Geographic entities mentioned:
surface_form: Miedwie
instance_of: Lake
countries: Poland
coordinates: lat: 53.26777777777778
lon: 14.891111111111112
Beginnings. In 1880, prospectors Joseph 'Joe' Juneau and Richard Harris discovered gold in Silver Bow Basin. This brought waves of prospectors to the region, including John Treadwell, whose first move was to purchase a lode claim on Douglas Island from Pierre Joseph Erussard (&quot;French Pete&quot;) on September 13, 1881. Treadwell formed a partnership in Sept. 1881 with Erussard de Ville, D.P.

Geographic entities mentioned:
surface_form: Silver Bow Basin
instance_of: Valley
countries: United States
coordinates: lat: 58.3111
lon: -134.343
A typical Basque mountain warrior was armed with two short spears and a knife or short sword as his main weapons, and bows or javelins for missile weapons. He would not normally wear armour. Pierre de Marca, a Béarnese author, suggests that the attackers were a reduced number of mostly local Low Navarrese, Souletines, and Baztanese, whose main motivation may have been plunder.

Geographic entities mentioned:
surface_form: Baztanese
instance_of: Valley
countries: Spain
coordinates: lat: 43.146787
lon: -1.5171681
However, the historical Roman road (also called the &quot;Route of Napoleon&quot;) followed a route different from the modern one, not crossing at Ibañeta (the traditional location) but heading up eastwards and crossing instead the Lepoeder and Bentartea passes &ndash; next to mount Astobizkar &ndash; not far from mount Urkulu, identified as the &quot;Summum Pyreneum&quot; of the classic Roman sources.

Geographic entities mentioned:
surface_form: Urkulu
instance_of: Mountain
countries: France
Spain
coordinates: lat: 43.04694444
lon: -1.24055556
Monte Astu massif. The Monte Astu massif () is a chain of mountains in the northeast of the island of Corsica, France. It takes its name from Monte Astu, the highest peak. Location. The Monte Astu massif has a main chain, the Serra di Tenda, and two secondary chains. The Serra di Tenda has all the highest peaks in the massif. It separates the Nebbio from the Ostriconi valley.

Geographic entities mentioned:
surface_form: Monte Astu
instance_of: Mountain
countries: France
coordinates: lat: 42.58122222222222
lon: 9.209888888888889
Rivière de la Savane (île d'Orléans). The Savane River flows in the municipality of Saint-François-de-l'Île-d'Orléans, in the L'Île-d'Orléans Regional County Municipality, in the administrative region of Capitale-Nationale, in the province of Quebec, in Canada. The lower part of this small valley is served by Chemin Royale (route 368) which runs along the southeast shore of Île d'Orléans.

Geographic entities mentioned:
surface_form: rivière de la savane
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.98749888888889
lon: -70.8205538888889
Background. Swahili is a Bantu language spoken by about 100 million people in Kenya, Tanzania, Uganda, Malawi, Mozambique and other areas in or near the African Great Lakes region. Most users are using Microsoft Windows and Microsoft Office, but since that is not available in Swahili, they have to use English or French. Kilinux tried to reduce the threshold by localizing Open Office.

Geographic entities mentioned:
surface_form: African Great Lakes
instance_of: Group of lakes
countries: Burundi
Zambia
Kenya
Democratic Republic of the Congo
Malawi
Mozambique
Rwanda
Tanzania
Uganda
Ethiopia
coordinates: lat: -8
lon: 35
Lake Manly. Lake Manly was a pluvial lake in Death Valley, California. It forms occasionally in Badwater Basin after heavy rainfall, but at its maximum extent during the so-called &quot;Blackwelder stand,&quot; ending approximately 120,000 years before present, the lake covered much of Death Valley with a surface area of.

Geographic entities mentioned:
surface_form: Death Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.45693888888889
lon: -116.86528055555556
The history of Lake Manly is not as well understood as that of Lake Lahontan and Lake Bonneville, the two largest pluvial lakes recorded in the Great Basin. More recently, renewed scientific interest has stemmed from the fact that Lake Manly formerly drained the area of Yucca Mountain, a proposed nuclear waste repository.

Geographic entities mentioned:
surface_form: Yucca Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.9402
lon: -116.485
Geography. Lake Manly formed in Death Valley, a tectonic depression framed by the Cottonwood Mountains and Panamint Range to the west, Owlshead Mountains to the south and Black Mountains, Funeral Mountains and Grapevine Mountains to the east.

Geographic entities mentioned:
surface_form: Death Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.45693888888889
lon: -116.86528055555556
Before the time where it flowed into these lakes, the Mojave River drained westward. Overflow from Lake Mojave may have continued until 8,000 years ago. The Mojave River reached the Amargosa through Silurian Valley and Salt Creek; on its way it crossed Dry Lake, Silurian Lake and another pond at the foot of the Salt Spring Hills.

Geographic entities mentioned:
surface_form: Silurian Valley
instance_of: Valley
countries: United States
coordinates: lat: 35.62138889
lon: -116.26861111
At least during the Tahoe glaciation, the Owens River drained into Lake Manly after filling Owens Lake, China Lake, Searles Lake and the Panamint Valley. This river system formed 3.2 million years ago when lava flows blocked a channel that had previously drained the Owens River across the Sierra Nevada.

Geographic entities mentioned:
surface_form: Panamint Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.0592
lon: -117.244
Lake Lahontan might have drained into Lake Manly; one potential pathway would be from the Walker Lake basin over Soda Springs Valley, Fish Lake Valley and Eureka Valley where it may have been joined by overflow from Deep Springs Valley. All these valleys are at successively lower elevations.

Geographic entities mentioned:
surface_form: Fish Lake Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.6947
lon: -118.078
surface_form: Deep Springs Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.3333
lon: -118.018
A major research issue remains as to whether Lake Manly ever drained into the Colorado River. Such a drainage may have occurred through Broadwell Lake across the high pass close to Ludlow, and entered the Colorado close to present-day Parker, Arizona, after passing through Bristol Lake, Cadiz Lake and Lake Danby. Potentially such an overflow, if it existed, would have reached rates of.

Geographic entities mentioned:
surface_form: Bristol Lake
instance_of: Lake
countries: United States
coordinates: lat: 34.4622
lon: -115.6738
Further, there is no indication that Bristol Lake, the lake that water from an overflow would have entered into, was ever filled with freshwater in the last four million years; though foraminifera correlated with the Colorado River have been found, and some sedimentary and fish evolutionary data likewise support it. Water composition.

Geographic entities mentioned:
surface_form: Bristol Lake
instance_of: Lake
countries: United States
coordinates: lat: 34.4622
lon: -115.6738
Earliest highstands. According to sedimentation patterns, a southeastward flowing river occupied northern Death Valley during the late Miocene, and was gone by 3.35 million years ago. This river system started in the Cottonwood Mountains – possibly as far as Last Chance Range and Owens Valley – and passed through northern Death Valley into the Amargosa Valley, possibly into the Colorado River.

Geographic entities mentioned:
surface_form: Owens Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.8025
lon: -118.199722
Background and career. Giuliana Sgrena was born and raised in Masera, Province of Verbano-Cusio-Ossola, a town of fewer than 1,000 people that had seen intense fighting during World War II between Italian partisans and German soldiers. Her father, Franco Sgrena, was a noted partisan during the war and later became an activist in the communist railway union.

Geographic entities mentioned:
surface_form: intense fighting
instance_of: Valley
countries: Italy
coordinates: lat: 46.283333333333
lon: 8.35
This scandal soon led Sebő Vukovics, the Hungarian government's commissioner for Southern Hungary, to disband Rózsa's Free Corps. His favourite hiding places were the islets on Ludas Lake (now Ludaš Lake, Serbia). After the restoration of Habsburg power. After the fall of the revolution he was forced to flee and returned to his earlier life as a highwayman.

Geographic entities mentioned:
surface_form: Ludas Lake
instance_of: Lake
countries: Serbia
coordinates: lat: 46.1
lon: 19.82
Regular ferry service operated over Lake Michigan from Grand Haven to Muskegon, Milwaukee, and Chicago, including the railcar ferry originally built by the Detroit, Grand Haven and Milwaukee Railway in the 1870s. Streetcars were discontinued in 1928, although buses had replaced the rail service by 1927, and the interurban right-of-way was purchased to build highways.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Shewaki. Shewaki () is a village located in the Hindaki area of Afghanistan, in Bagrami District, Kabul Province, near the mountains Koh e Hindaki and Munar e Chakari (not related to Chakari, Afghanistan). Shewaki Stupa. Shewaki Stupa is the site of Shahbahar (King's Vihara), one of Afghanistan’s major Buddhist site.

Geographic entities mentioned:
surface_form: Koh e Hindaki
instance_of: Mountain
countries: Afghanistan
coordinates: lat: 34.4574
lon: 69.1917
Precipitation runoff from the mountain drains north into the Copland River and south to the Hooker River. Topographic relief is significant as the south face rises nearly above Hooker Lake in three kilometres. The nearest higher peak is Mount Sefton, two kilometres to the west-southwest. History.

Geographic entities mentioned:
surface_form: Hooker Lake
instance_of: Lake
countries: New Zealand
coordinates: lat: -43.67916667
lon: 170.10833333
Precipitation runoff from the mountain drains north into the Copland River and south to the Hooker River. Topographic relief is significant as the south face rises nearly above Hooker Lake in three kilometres. The nearest higher peak is Mount Sefton, two kilometres to the west-southwest. History.

Geographic entities mentioned:
surface_form: Mount Sefton
instance_of: Mountain
countries: New Zealand
coordinates: lat: -43.682
lon: 170.042
Cerro Pantoja. Cerro Pantojo is an extinct basaltic stratovolcano on the border of Argentina and Chile. It lies immediately south of Cardenal Antonio Samoré Pass and its characteristic spire-shaped summit is an eroded volcanic plug. It also has flank lava flows.

Geographic entities mentioned:
surface_form: Cardenal Antonio Samoré Pass
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -40.713175
lon: -71.944027
Cerro Pantoja. Cerro Pantojo is an extinct basaltic stratovolcano on the border of Argentina and Chile. It lies immediately south of Cardenal Antonio Samoré Pass and its characteristic spire-shaped summit is an eroded volcanic plug. It also has flank lava flows.

Geographic entities mentioned:
surface_form: cerro pantojo
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -40.766666666667
lon: -71.95
Cerro Pantoja. Cerro Pantojo is an extinct basaltic stratovolcano on the border of Argentina and Chile. It lies immediately south of Cardenal Antonio Samoré Pass and its characteristic spire-shaped summit is an eroded volcanic plug. It also has flank lava flows.

Geographic entities mentioned:
surface_form: cerro pantoja
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -40.766666666667
lon: -71.95
Parish archives from Val di Non, Val di Sole, and Rovereto contain references to Belletto households, often listed as small land holders, tradesmen, vintners, or minor functionaries. These entries consistently present the surname in its Latinized form, indicating a retention of bureaucratic nomenclature over generations.

Geographic entities mentioned:
surface_form: Val di Non
instance_of: Valley
countries: Italy
coordinates: lat: 46.366666666667
lon: 11.033333333333
surface_form: Val di Sole
instance_of: Valley
countries: Italy
coordinates: lat: 46.3
lon: 10.8
These varsity programs involve more than 550 Marist student-athletes. The crew programs are among the few in the nation that claim on-campus facilities. The red fox or reynard is indigenous to the Hudson Valley where Marist is located and is regarded as highly intelligent and cunning. It is the red fox from which Marist's school colors of red and white are derived.

Geographic entities mentioned:
surface_form: Hudson Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.9209
lon: -73.9613
Vífilsfell. Vífilsfell () is a hyaloclastite ridge in southwestern Iceland (Weichselian). It is 655 m high and located west of Jósepsdalur valley on the volcanic plateau of Hellisheiði. It forms the northernmost offset of the Bláfjöll mountain massif and is situated on top of the fissure system of Brennisteinsfjöll. Name.

Geographic entities mentioned:
surface_form: Jósepsdalur
instance_of: Valley
coordinates: lat: 64.0259
lon: -21.5527
Vífilsfell. Vífilsfell () is a hyaloclastite ridge in southwestern Iceland (Weichselian). It is 655 m high and located west of Jósepsdalur valley on the volcanic plateau of Hellisheiði. It forms the northernmost offset of the Bláfjöll mountain massif and is situated on top of the fissure system of Brennisteinsfjöll. Name.

Geographic entities mentioned:
surface_form: Brennisteinsfjöll
instance_of: Mountain
Plateau
countries: Iceland
coordinates: lat: 63.916666666667
lon: -21.833333333333
(C.W.Hamilton, 2004)
Holocene volcanism and connection to the history of Iceland. The eruption history of the region does not end in the Pleistocene. Holocene lava fields surround Vífilsfell. They are eruption products of two volcanic systems, the Hengill system to the northwest and the Brennisteinsfjöll system.

Geographic entities mentioned:
surface_form: Hengill
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.085555555556
lon: -21.313611111111
surface_form: Brennisteinsfjöll
instance_of: Mountain
Plateau
countries: Iceland
coordinates: lat: 63.916666666667
lon: -21.833333333333
surface_form: brennisteinsfjöll
instance_of: Mountain
Plateau
countries: Iceland
coordinates: lat: 63.916666666667
lon: -21.833333333333
surface_form: hengill
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.085555555556
lon: -21.313611111111
surface_form: hengill
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.085555555556
lon: -21.313611111111
The last eruptions in the Hengill system took place about 2000 years ago, but the youngest lava field, the &quot;Svínahraunsbruni&quot; (Brennisteinsfjöll volcanic system) dates from the year 1000 and was also called &quot;Kristnitökuhraun&quot;, because at the time of the eruption, the Icelandic vikings had a dispute in Þingvellir about the question, if they should become Christians, to which, in the end, they acquiesced.

Geographic entities mentioned:
surface_form: brennisteinsfjöll
instance_of: Mountain
Plateau
countries: Iceland
coordinates: lat: 63.916666666667
lon: -21.833333333333
Vífilsfell. Vífilsfell () is a hyaloclastite ridge in southwestern Iceland (Weichselian). It is 655 m high and located west of Jósepsdalur valley on the volcanic plateau of Hellisheiði. It forms the northernmost offset of the Bláfjöll mountain massif and is situated on top of the fissure system of Brennisteinsfjöll. Name.

Geographic entities mentioned:
surface_form: vífilsfell
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.0362705933
lon: -21.5566141304
The man, called &quot;Vífill&quot;, is said to have had his own farm at Vífilsstaðir, now in the vicinity of the city of Hafnarfjörður. From there – according to the Landnámabók – he went daily up to the top of Vífilsfell, some 20 km away, to look after the weather. When the weather seemed promising, he went fishing from the tip of the Seltjarnarnes peninsula near Grótta. Geography.

Geographic entities mentioned:
surface_form: vífilsfell
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.0362705933
lon: -21.5566141304
In 2010, it was planned to extract around 2-5 000 000m3 in the quarry of Bóluöldur. When scientists examined the outcrops in the quarry, they found many layers of pillow lavas. One theory about their origin is, that during the last stages of Vífilsfell's eruptions, subaerial lavas had emerged up on the mountain, degassed there and then run into a deep lake or the sea. Roads and airfield.

Geographic entities mentioned:
surface_form: vífilsfell
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.0362705933
lon: -21.5566141304
One theory about their origin is, that during the last stages of Vífilsfell's eruptions, subaerial lavas had emerged up on the mountain, degassed there and then run into a deep lake or the sea. Roads and airfield. The Hringvegur (Suðurlandsvegur) passes by at a distance of about 5 km from Vífilsfell. The mountain can be seen very well from the coffee shop &quot;Litla Kaffistofan&quot;.

Geographic entities mentioned:
surface_form: vífilsfell
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.0362705933
lon: -21.5566141304
The river is formed by the confluence of the rivers Ulvåa and Holåa on the border of Våler and Åsnes (the sources of those two rivers are located in Elverum Municipality and Sweden). The river then flows to the south and west before joining the river Glomma just south of the village of Flisa. Some of the side rivers that join the Flisa are Vermundelv (from the lake Vermunden) and Kynna.

Geographic entities mentioned:
surface_form: Vermunden
instance_of: Lake
countries: Norway
coordinates: lat: 60.695
lon: 12.386944444444
The Squam Lake Woolen Mill was established in 1840. Goods manufactured at local factories included hosiery, gloves, sporting equipment, wood products and paper. The Boston, Concord & Montreal Railroad entered in 1849, carrying freight but also tourists bound for hotels on the Squam Lakes, to which they traveled by steamer up the Squam River.

Geographic entities mentioned:
surface_form: Squam Lake
instance_of: Lake
countries: United States
coordinates: lat: 43.745277777778
lon: -71.526111111111
Geography. According to the United States Census Bureau, the town has a total area of, of which are land and are water, comprising 4.63 of the town. Bounded on the west by the Pemigewasset River, Ashland is drained by the Squam River and Owl Brook. Little Squam Lake is on the eastern boundary. The highest point in Ashland is Hicks Hill, at above sea level.

Geographic entities mentioned:
surface_form: Little Squam Lake
instance_of: Lake
countries: United States
coordinates: lat: 43.722222222222
lon: -71.599722222222
On 27 April 1972, the national park was reconstituted as the &quot;Elliot Price Conservation Park&quot; under the &quot;National Parks and Wildlife Act 1972&quot;. It occupies land on the Hunt Peninsula and on Brooks Island at the southern end of Lake Eyre as well as some adjoining land which is subject to inundation during periodic flooding.

Geographic entities mentioned:
surface_form: Lake Eyre
instance_of: Lake
countries: Australia
coordinates: lat: -28.406
lon: 137.2963
Frater. Frater is an uninhabited dispersed rural community and unincorporated place with a railway siding on the Algoma Central Railway located north of Sault Ste. Marie. It is located on Frater Lake at the boundary with Lake Superior Provincial Park, from the Ontario Highway 17 (Trans-Canada Highway) and from the shore of Lake Superior, and at geographic coordinates. Goudreau.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
Harmony Beach. Harmony Beach is a small community built around a beach on Lake Superior. Havilland Bay. Havilland Bay is a small unincorporated community built around a beach on Lake Superior. Island Lake. Island Lake (46.6711° N 84.2687°W) is a rural settlement in the Unorganized North Part of Algoma District in northeastern Ontario, Canada.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
The quality of the ore found was not sufficient to make the mine profitable. Lochalsh. Lochalsh () is a ghost town and rail siding located at the very south end of Wabatongushi Lake, along the Canadian Pacific Railway between Missanabie and Franz. A taxi ran between Lochalsh, Goudreau, and the Cline Mine. When the mine closed in 1946, both towns became ghost towns.

Geographic entities mentioned:
surface_form: Wabatongushi Lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.4417
lon: -84.2083
His family moved to the city of Tucumán in northwestern Argentina when he was nine. In a bow to two legendary Incan kings, he adopted the stage name Atahualpa Yupanqui. In his early years, Yupanqui traveled extensively through the northwest of Argentina and the Altiplano studying the indigenous cultures. He became politically active and joined the Communist Party of Argentina.

Geographic entities mentioned:
surface_form: Altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
The strait between the peninsula and Longue Island was named &quot;Prince Albert Pass&quot; after Prince Albert I of Monaco in 1961. The highest point of the peninsula is high Mont Wyville Thomson located roughly in the middle. Another important peak is Pouce, a high volcanic plug.The small research station Port-Douzième and Phonolite are located on the peninsula.

Geographic entities mentioned:
surface_form: Mont Wyville Thomson
instance_of: Mountain
countries: France
coordinates: lat: -49.564444444444
lon: 70.160833333333
The river rises at Talakaveri in the Brahmagiri range in the Western Ghats. The source is located at an elevation of in the Kodagu district of Karnataka. The river flows for about through the Deccan plateau in Karnataka before entering Tamil Nadu. It flows further eastward in Tamil Nadu for before flowing into the Bay of Bengal near Poompuhar in Mayiladuthurai district of Tamil Nadu.

Geographic entities mentioned:
surface_form: Deccan plateau
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
The source is located at an elevation of in the Kodagu district of Karnataka. The river flows for about through the Deccan plateau in Karnataka before entering Tamil Nadu. It flows further eastward in Tamil Nadu for before flowing into the Bay of Bengal near Poompuhar in Mayiladuthurai district of Tamil Nadu. The river flows for a total length of about.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
The river flows for a total length of about. The major tributaries include Amaravati, Arkavati, Bhavani, Harangi, Hemavati, Kabini, Lakshmana Tirtha, Shimsha and Noyyal. There are a number of dams on the river which form part of an extensive irrigation system and are used for the generation of hydroelectric power.

Geographic entities mentioned:
surface_form: Shimsha
instance_of: Watercourse
countries: India
coordinates: lat: 12.3
lon: 76.233
Its follows a rough upper course consisting of rocky beds and high banks. Once it leaves the Kodagu hills, it flows eastwards and forms a series of rapids and falls. It flows through a narrow gorge onto the Deccan plateau and drops about at Chunchanakatte Falls. The river forms the island of Srirangapatna and widens to before flowing south-east.

Geographic entities mentioned:
surface_form: Deccan plateau
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
After flowing for, the two branches converge around the Srirangam island. The river further branches off into 36 different channels before emptying into the Bay of Bengal near Poompuhar in Mayiladuthurai district. The river traverses for about in Tamil Nadu for a total length of about. Tributaries. The Kaveri River has 21 major tributaries.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Kabini is another major contributor to the flow of Kaveri and joins the river in Karnataka. It meets with its second largest tributary Bhavani at Kooduthurai in Bhavani and two other tributaries Noyyal, and Amaravati join further down the stream in Tamil Nadu. Other tributaries of Kaveri include Shimsha, Arkavati, Sarabanga, and Thirumanimutharu. Geology and ecology.

Geographic entities mentioned:
surface_form: Shimsha
instance_of: Watercourse
countries: India
coordinates: lat: 12.3
lon: 76.233
It is the third largest river in the region after Godavari and Krishna. The catchment area of the Kaveri basin is estimated to be and encompasses the states of Tamil Nadu, Karnataka, Kerala, and the union territory of Puducherry. The river rises at Talakaveri in the Brahmagiri range in the Western Ghats. The source is located at an elevation of in the Kodagu district of Karnataka.

Geographic entities mentioned:
surface_form: brahmagiri
instance_of: Mountain
countries: India
The Kaveri River has 21 major tributaries. The largest tributary Hemavati, and Lakshmana Tirtha join the river at Krishna Raja Sagara. Kabini is another major contributor to the flow of Kaveri and joins the river in Karnataka. It meets with its second largest tributary Bhavani at Kooduthurai in Bhavani and two other tributaries Noyyal, and Amaravati join further down the stream in Tamil Nadu.

Geographic entities mentioned:
surface_form: kaveri
instance_of: Watercourse
countries: India
coordinates: lat: 11.370345
lon: 79.828105
Kaveri. The Kaveri (also known as Cauvery,) is a major river flowing across Southern India. It is the third largest river in the region after Godavari and Krishna. The catchment area of the Kaveri basin is estimated to be and encompasses the states of Tamil Nadu, Karnataka, Kerala, and the union territory of Puducherry. The river rises at Talakaveri in the Brahmagiri range in the Western Ghats.

Geographic entities mentioned:
surface_form: cauvery
instance_of: Watercourse
countries: India
coordinates: lat: 11.370345
lon: 79.828105
surface_form: kaveri
instance_of: Watercourse
countries: India
coordinates: lat: 11.370345
lon: 79.828105
Kaveri. The Kaveri (also known as Cauvery,) is a major river flowing across Southern India. It is the third largest river in the region after Godavari and Krishna. The catchment area of the Kaveri basin is estimated to be and encompasses the states of Tamil Nadu, Karnataka, Kerala, and the union territory of Puducherry. The river rises at Talakaveri in the Brahmagiri range in the Western Ghats.

Geographic entities mentioned:
surface_form: kaveri
instance_of: Watercourse
countries: India
coordinates: lat: 11.370345
lon: 79.828105
Access to the river's waters has been a cause of dispute among the states of Karnataka and Tamil Nadu for decades. The Kaveri basin is a densely populated region, with several towns and cities located on its banks. The river is considered as sacred by the people of Southern India and is considered to be among the seven holy rivers of India.

Geographic entities mentioned:
surface_form: kaveri
instance_of: Watercourse
countries: India
coordinates: lat: 11.370345
lon: 79.828105
The river is considered as sacred by the people of Southern India and is considered to be among the seven holy rivers of India. The river is often personified and worshiped as the goddess Kaveri. The river is mentioned in various Hindu religious texts including the &quot;Mahabharata&quot; and the &quot;Puranas&quot;.

Geographic entities mentioned:
surface_form: kaveri
instance_of: Watercourse
countries: India
coordinates: lat: 11.370345
lon: 79.828105
Other tributaries of Kaveri include Shimsha, Arkavati, Sarabanga, and Thirumanimutharu. Geology and ecology. The Kaveri basin was formed in the Late Jurassic to Early Cretaceous period during Gondwana breakup and opening of the Indian Ocean. Most of the basin is made up of Precambrian rocks and the two major rock types that are found are metamorphic and igneous rocks.

Geographic entities mentioned:
surface_form: kaveri
instance_of: Watercourse
countries: India
coordinates: lat: 11.370345
lon: 79.828105
Religious significance. In Hinduism, the river is considered one of seven holy rivers in India. The river is personified and worshiped as the river goddess &quot;Kaveri Amma.&quot; Kaveri is mentioned as both a river and a goddess in various Hindu texts such as the &quot;Mahabharata&quot; and the &quot;Puranas&quot;.

Geographic entities mentioned:
surface_form: kaveri
instance_of: Watercourse
countries: India
coordinates: lat: 11.370345
lon: 79.828105
Another story narrates that during the Samudra Manthana, or churning of the Ocean of Milk, Mohini and Lopamudra retrieved the nectar of immortality for the gods. Afterwards, Brahma took care of Lopamudra as his daughter and later offered her to king Kavera, who renamed her as Kaveri. When Kaveri grew up she prayed to Brahma to transform her into a purifying river.

Geographic entities mentioned:
surface_form: kaveri
instance_of: Watercourse
countries: India
coordinates: lat: 11.370345
lon: 79.828105
In July 2021, he curated the inaugural installation for the Beatrice Trussardi Foundation by Polish sculptor Paweł Althamer. The installation, titled &quot;Franciszek&quot;, saw a sculpture of St. Francis installed within a 17th-century mountain hut in the Engadin, Switzerland, made by the artist using found materials from the local area.

Geographic entities mentioned:
surface_form: Engadin
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.5497
lon: 9.8959
La Pacana. La Pacana is a Miocene age caldera in northern Chile's Antofagasta Region. Part of the Central Volcanic Zone of the Andes, it is part of the Altiplano-Puna volcanic complex, a major caldera and silicic ignimbrite volcanic field. This volcanic field is located in remote regions at the Zapaleri tripoint between Chile, Bolivia and Argentina.

Geographic entities mentioned:
surface_form: Zapaleri
instance_of: Mountain
countries: Chile
Bolivia
Argentina
coordinates: lat: -22.813805555555554
lon: -67.1807
Geography and structure. La Pacana lies in the Antofagasta Region of Chile, in the Andes just north of the Tropic of Capricorn and close to the Paso de Jama between Chile and Argentina. The border between Chile and Bolivia crosses the northern sector of the caldera.

Geographic entities mentioned:
surface_form: Paso de Jama
instance_of: Mountain
countries: Chile
coordinates: lat: -23.2375
lon: -67.07638889
surface_form: la pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
surface_form: pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
The border between Chile and Bolivia crosses the northern sector of the caldera. The area of La Pacana is largely uninhabitated; small settlements such as Socaire, Talabre and Toconao exist close to the Salar de Atacama, where streams descend the mountain slopes to the salar. The caldera was discovered during mapping efforts in the region between 1980 and 1985.

Geographic entities mentioned:
surface_form: Salar de Atacama
instance_of: Lake
Body of water
countries: Chile
coordinates: lat: -23.416666666666668
lon: -68.26666666666667
surface_form: la pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
surface_form: pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
In addition, the Central Volcanic Zone features about 18 minor volcanic fields. The largest historical eruption of the Andes occurred in 1600 at Huaynaputina in Peru in the Central Volcanic Zone, and the most active volcano of the Central Volcanic Zone is Láscar in Chile. La Pacana has a diameter of with a north–south elongation.

Geographic entities mentioned:
surface_form: Huaynaputina
instance_of: Mountain
countries: Peru
coordinates: lat: -16.615555555555556
lon: -70.84972222222223
Volcanic activity resumed within the caldera and at the edge of the resurgent dome, forming lava domes between 4.1 and at least 1.6 million years ago. These volcanic centres include the Corral de Coquena crater and the lava domes of Morro Negro east, Cerro Bola and Purifican west and Cerros de Guayaques north of the resurgent dome.

Geographic entities mentioned:
surface_form: Cerros de Guayaques
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -22.898083333333332
lon: -67.56777777777778
A few lakes such as the spring-fed Laguna de Chivato Muerto, Laguna Trinchera and Ojos del Rió Salado, as well as salt pans such as Salar de Aguas Calientes Norte, Salar de Aguas Calientes Sur, Salar de Pujsa and Salar de Quisquiro have developed within the moat. The waterbodies in the southern part of the caldera appear to be connected through groundwater, as they have similar water levels.

Geographic entities mentioned:
surface_form: Salar de Aguas Calientes
instance_of: Lake
countries: Chile
coordinates: lat: -23.5
lon: -67.6925
surface_form: aguas calientes
instance_of: Mountain
countries: Chile
coordinates: lat: -23.368333333333
lon: -67.685
surface_form: aguas calientes
instance_of: Mountain
countries: Chile
coordinates: lat: -23.368333333333
lon: -67.685
Regional. The Central Andes are the site of extensive ignimbrites that were erupted from large calderas usually located within the adjacent Altiplano, east of the principal volcanic arc. Many of these calderas are part of the Altiplano-Puna volcanic complex, a large volcanic complex covering a surface area of with about of ignimbrites.

Geographic entities mentioned:
surface_form: Altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
Two of these older ignimbrites are known as the Pampa Múcar and Antigua Chacaliri ignimbrites. La Pacana together with the Cerro Guacha and Purico Complex calderas forms the La Pacana Complex. Guacha experienced two major eruptions, of which one occurred 4.1 million years ago.

Geographic entities mentioned:
surface_form: Cerro Guacha
instance_of: Mountain
countries: Bolivia
coordinates: lat: -22.75
lon: -67.46666667
surface_form: Purico Complex
instance_of: Mountain
countries: Chile
coordinates: lat: -23
lon: -67.75
surface_form: purico
instance_of: Mountain
countries: Chile
coordinates: lat: -23
lon: -67.75
surface_form: la pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
surface_form: pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
Guacha experienced two major eruptions, of which one occurred 4.1 million years ago. The Purico complex began erupting 1.3 million years ago; it is the youngest centre of the La Pacana Complex with the youngest eruptions occurring during the Holocene. Additional volcanic centres west and southwest of La Pacana are Acamarachi, Láscar, Colachi and Cordón de Puntas Negras.

Geographic entities mentioned:
surface_form: Acamarachi
instance_of: Mountain
countries: Chile
coordinates: lat: -23.295833333333
lon: -67.617222222222
surface_form: Colachi
instance_of: Mountain
countries: Chile
coordinates: lat: -23.24192
lon: -67.64605
surface_form: Cordón de Puntas Negras
instance_of: Mountain
countries: Chile
coordinates: lat: -23.742777777778
lon: -67.534166666667
surface_form: colachi
instance_of: Mountain
countries: Chile
coordinates: lat: -23.24192
lon: -67.64605
surface_form: acamarachi
instance_of: Mountain
countries: Chile
coordinates: lat: -23.295833333333
lon: -67.617222222222
surface_form: cordón de puntas negras
instance_of: Mountain
countries: Chile
coordinates: lat: -23.742777777778
lon: -67.534166666667
surface_form: la pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
surface_form: pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
While the depth at which the Toconao ignimbrite formed is unknown, the Atana ignimbrite formed at a depth of. Such a formation depth is comparable to depths estimated for other magmatic systems such as Fish Canyon, Long Valley and Yellowstone. Climate and biota. Weather records are available for the Salar de Aguas Calientes.

Geographic entities mentioned:
surface_form: Long Valley
instance_of: Landform
countries: United States
coordinates: lat: 37.716666666667
lon: -118.88416666667
Such a formation depth is comparable to depths estimated for other magmatic systems such as Fish Canyon, Long Valley and Yellowstone. Climate and biota. Weather records are available for the Salar de Aguas Calientes. There, an average temperature of and average precipitation of have been recorded. There is little vegetation in the dry Altiplano.

Geographic entities mentioned:
surface_form: Salar de Aguas Calientes
instance_of: Lake
countries: Chile
coordinates: lat: -23.5
lon: -67.6925
surface_form: aguas calientes
instance_of: Mountain
countries: Chile
coordinates: lat: -23.368333333333
lon: -67.685
Climate and biota. Weather records are available for the Salar de Aguas Calientes. There, an average temperature of and average precipitation of have been recorded. There is little vegetation in the dry Altiplano. Nevertheless, a number of animal species are found, such as rheas, vicuñas and vizcachas. Ducks, geese and flamingos frequent waterbodies and salars. Eruption history.

Geographic entities mentioned:
surface_form: Altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
The Atana ignimbrite was once considered part of the Guaitiquina ignimbrite, which was later split off, while the Puripicar ignimbrite may be correlated with the Atana instead. Also, some of the ignimbrites erupted by La Pacana originally were attributed to Cerro Guacha.

Geographic entities mentioned:
surface_form: Cerro Guacha
instance_of: Mountain
countries: Bolivia
coordinates: lat: -22.75
lon: -67.46666667
surface_form: la pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
surface_form: pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
Its volume is about. 2.4 ± 0.4 million years ago, the Pampa Chamaca ignimbrite filled the moat between the resurgent dome and the caldera rim. The Pampa Chamaca or Talabre ignimbrite was erupted from a vent probably buried beneath the present-day Cordon de Puntas Negras or the Salar de Aguas Calientes and reached a volume of about.

Geographic entities mentioned:
surface_form: Salar de Aguas Calientes
instance_of: Lake
countries: Chile
coordinates: lat: -23.5
lon: -67.6925
surface_form: aguas calientes
instance_of: Mountain
countries: Chile
coordinates: lat: -23.368333333333
lon: -67.685
surface_form: cordon de puntas negras
instance_of: Mountain
countries: Chile
coordinates: lat: -23.742777777778
lon: -67.534166666667
The Pampa Chamaca or Talabre ignimbrite was erupted from a vent probably buried beneath the present-day Cordon de Puntas Negras or the Salar de Aguas Calientes and reached a volume of about. The 3.49 million years old Tara Ignimbrite from the Cerro Guacha caldera reached the northern margin of La Pacana.

Geographic entities mentioned:
surface_form: Cerro Guacha
instance_of: Mountain
countries: Bolivia
coordinates: lat: -22.75
lon: -67.46666667
surface_form: la pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
surface_form: pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
The collapse of the caldera cut through older volcanic centres, exposing the Ceja Alta and Quilapana porphyry deposits. Other older volcanic centres exposed in the walls of the caldera are the Cerro Aguas Calientes stratovolcano in the eastern wall and the Cerro Gigantes in the western wall.

Geographic entities mentioned:
surface_form: cerro aguas calientes
instance_of: Mountain
countries: Chile
coordinates: lat: -23.368333333333
lon: -67.685
surface_form: aguas calientes
instance_of: Mountain
countries: Chile
coordinates: lat: -23.368333333333
lon: -67.685
The Arenoso, Chamaca and Chivato Muerto lava domes in the southern wall of the caldera were originally considered to be pre-caldera; later these three domes were identified as post-caldera domes. Stratovolcanoes inside the caldera include the cones associated with the Cerros de Guayaques lava domes and the volcanoes Cerro Incaguasi, Cerros de Pili, Cerros Negros and Huailitas.

Geographic entities mentioned:
surface_form: pili
instance_of: Mountain
countries: Chile
coordinates: lat: -23.295833333333
lon: -67.617222222222
The waterbodies in the southern part of the caldera appear to be connected through groundwater, as they have similar water levels. The western caldera rim itself impedes the groundwater from draining out of the caldera. Streams such as Río de Pili and Río Salado complete the hydrology of the caldera. Gravimetric observations have been conducted on La Pacana.

Geographic entities mentioned:
surface_form: pili
instance_of: Mountain
countries: Chile
coordinates: lat: -23.295833333333
lon: -67.617222222222
La Pacana. La Pacana is a Miocene age caldera in northern Chile's Antofagasta Region. Part of the Central Volcanic Zone of the Andes, it is part of the Altiplano-Puna volcanic complex, a major caldera and silicic ignimbrite volcanic field. This volcanic field is located in remote regions at the Zapaleri tripoint between Chile, Bolivia and Argentina.

Geographic entities mentioned:
surface_form: la pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
surface_form: pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
This volcanic field is located in remote regions at the Zapaleri tripoint between Chile, Bolivia and Argentina. La Pacana along with other regional volcanoes was formed by the subduction of the Nazca Plate beneath the South American Plate in the Peru-Chile Trench. La Pacana is situated in a basement formed by various Paleozoic formations and Tertiary ignimbrites and volcanoes.

Geographic entities mentioned:
surface_form: la pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
surface_form: pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
La Pacana along with other regional volcanoes was formed by the subduction of the Nazca Plate beneath the South American Plate in the Peru-Chile Trench. La Pacana is situated in a basement formed by various Paleozoic formations and Tertiary ignimbrites and volcanoes. Several major faults cross the region at La Pacana and have influenced its volcanic activity.

Geographic entities mentioned:
surface_form: la pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
surface_form: pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
La Pacana is situated in a basement formed by various Paleozoic formations and Tertiary ignimbrites and volcanoes. Several major faults cross the region at La Pacana and have influenced its volcanic activity. La Pacana is a supervolcano and is responsible for the eruption of the giant Atana ignimbrite, which reaches a volume of and constitutes the fifth-largest explosive eruption known.

Geographic entities mentioned:
surface_form: la pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
surface_form: pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
The Atana ignimbrite was erupted 3.8 ± 0.1 and 4.2 ± 0.1 million years ago, almost simultaneously with the much smaller (volume of) Toconao ignimbrite. The Pujsa ignimbrite was erupted by La Pacana before the Atana/Toconao ignimbrites, and the Filo Delgado and Pampa Chamaca/Talabre ignimbrites afterwards. Geography and structure.

Geographic entities mentioned:
surface_form: la pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
surface_form: pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
The caldera was discovered during mapping efforts in the region between 1980 and 1985. La Pacana is part of the Central Volcanic Zone, one of the four volcanic zones that make up the Andean Volcanic Belt and which are separated from each other by gaps without ongoing volcanic activity.

Geographic entities mentioned:
surface_form: la pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
surface_form: pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
The largest historical eruption of the Andes occurred in 1600 at Huaynaputina in Peru in the Central Volcanic Zone, and the most active volcano of the Central Volcanic Zone is Láscar in Chile. La Pacana has a diameter of with a north–south elongation. This is one of the best exposed and largest calderas in the world; the largest caldera known is Toba in Sumatra with a maximum length of.

Geographic entities mentioned:
surface_form: la pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
surface_form: pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667