Sarmila/GeoWiki-Features huggingface dataset:
Lake Managua or &quot;Xolotlán&quot; is 1,052.9 km2 and is 37.8 meters above sea level and is quite contaminated. The other lake is the very large Lake Nicaragua or Cocibolca and has an area of 8,143.7 km2. Lake Colcibolca occupies the middle section of the tectonic valley shared with two other watersheds: Lake Xolotlán at upper and the San Juan River.

Geographic entities mentioned:
surface_form: Lake Nicaragua
instance_of: Lake
countries: Nicaragua
coordinates: lat: 11.5742
lon: -85.3563
The specific epithet (&quot;myrtifolium&quot;) means 'myrtle-leaved'. Distribution and habitat. This species of &quot;Hypocalymma&quot; grows amongst rocks on the middle and upper slopes of the Bluff Knoll plateau in the Stirling Range in the south-west of Western Australia. Conservation status.

Geographic entities mentioned:
surface_form: Bluff Knoll
instance_of: Mountain
countries: Australia
coordinates: lat: -34.375555555556
lon: 118.25611111111
Geography. Pahalgam is located in Anantnag district of the Indian union territory of Jammu and Kashmir. It is located at an altitude of in the Lidder Valley, which extends east of Jhelum River in the Vale of Kashmir. The two streams of Lidder River—East and West Lidder—join near Pahalgam before proceeding through the narrow valley.

Geographic entities mentioned:
surface_form: Lidder Valley
instance_of: Valley
countries: India
coordinates: lat: 33.7764
lon: 75.2133
As per Hindu mythology, Shiva is believed to have left his mount Nandi in Pahalgam, the moon he carries on his head in Chandanwari, the snakes around his neck at Sheshnag Lake, and the five natural elements at Panchtarni before entering the Amarnath cave. The yatra begins from Chandanwari, situated about from Pahalgam, and proceeds towards Amarnath via Sheshnag Lake and Panchtarni.

Geographic entities mentioned:
surface_form: Sheshnag Lake
instance_of: Lake
countries: India
coordinates: lat: 34.093697
lon: 75.496686
The yatra begins from Chandanwari, situated about from Pahalgam, and proceeds towards Amarnath via Sheshnag Lake and Panchtarni. Kolahoi Glacier is a hanging glacier situated up the Lidder Valley, just below Kolahoi Peak. It is accessible via a trail from Pahalgam via Aru. Baisaran and Betaab valleys are verdant meadows flanked by mountains and evergreen trees, located close to Pahalgam.

Geographic entities mentioned:
surface_form: Kolahoi Peak
instance_of: Mountain
countries: India
coordinates: lat: 34.16388889
lon: 75.33027778
Kolahoi Glacier is a hanging glacier situated up the Lidder Valley, just below Kolahoi Peak. It is accessible via a trail from Pahalgam via Aru. Baisaran and Betaab valleys are verdant meadows flanked by mountains and evergreen trees, located close to Pahalgam. Pahalgam Golf Course, also known as Lidder Valley Golf Course, is an 18-hole golf course inaugurated in 2011.

Geographic entities mentioned:
surface_form: Betaab
instance_of: Valley
countries: India
coordinates: lat: 34.05041
lon: 75.36381
Lakegala. Lakegala mountain is situated in Sri Lanka about away from the capital Colombo. This mountain is situated in Meemure village. Lakegala is situated near the Border between Kandy and Matale Districts. There are several access points to Lakegala rock but the safest access road is from Meemure Village. &quot;The Rock of Lanka&quot; is the meaning of &quot;Lakegala&quot; in Sinhala language.

Geographic entities mentioned:
surface_form: lakegala
instance_of: Mountain
countries: Sri Lanka
coordinates: lat: 7.4333333333333
lon: 80.833333333333
Lakegala is situated near the Border between Kandy and Matale Districts. There are several access points to Lakegala rock but the safest access road is from Meemure Village. &quot;The Rock of Lanka&quot; is the meaning of &quot;Lakegala&quot; in Sinhala language. The rock is about 1310m high and it is in the Knuckles mountain range aka &quot;Dumbara Mitiyawatha&quot;.

Geographic entities mentioned:
surface_form: lakegala
instance_of: Mountain
countries: Sri Lanka
coordinates: lat: 7.4333333333333
lon: 80.833333333333
Due to repeated Luftwaffe attacks and artillery barrage, the unit suffered heavy losses and was ordered to retreat behind the Warta river. On September 3, the division filled defensive positions behind the Warta and Widawa, near Wieluń. Due to contradictory orders of General Boncza-Uzdowski, its 15th Infantry Regiment was almost completely destroyed, and had to be replaced by the 36th Regiment.

Geographic entities mentioned:
surface_form: Widawa
instance_of: Watercourse
countries: Poland
coordinates: lat: 51.198888888889
lon: 16.918888888889
A series of tragedies occur at the end of the novella, and a hunting party kills a sacred deer with Momun and the boy as witnesses. This sends the boy into despair. Longing for love and acceptance, he dives into the waters of a stream nearby to &quot;turn into a fish&quot; and swim towards Issyk-Kul in search of his father. Reception.

Geographic entities mentioned:
surface_form: Issyk-Kul
instance_of: Lake
countries: Kyrgyzstan
coordinates: lat: 42.416666666667
lon: 77.25
Pseudotropheus interruptus. &quot;Pseudotropheus interruptus&quot; is a species of cichlid in the Cichlidae endemic to Lake Malawi where it is only known from Likoma Island. This species can reach a length of TL. It can also be found in the aquarium trade.

Geographic entities mentioned:
surface_form: Lake Malawi
instance_of: Lake
countries: Malawi
Mozambique
Tanzania
coordinates: lat: -12.183333333333
lon: 34.366666666667
Type specimen. The type specimen was collected by Otto M. Smith along White River in Southern Missouri in August 1910. Etymology. The specific epithet &quot;ozarkana&quot; references the Ozarks region. Pollination. It is pollinated by &quot;Lasioglossum nelumbonis&quot;, &quot;Lasioglossum bruneri&quot;, and &quot;Augochlora pura&quot;, which together make up 97% of all floral visitors.

Geographic entities mentioned:
surface_form: Ozarks
instance_of: Plateau
countries: United States
coordinates: lat: 37.1822
lon: -92.5159
Olivia Lake (Alberta). Olivia Lake is a lake in Alberta. Due to evaporation and not enough replenishment of water, the lake is two to three times more saline than seawater.

Geographic entities mentioned:
surface_form: olivia lake (alberta)
instance_of: Lake
countries: Canada
coordinates: lat: 53.077
lon: -111.597
Olivia Lake (Alberta). Olivia Lake is a lake in Alberta. Due to evaporation and not enough replenishment of water, the lake is two to three times more saline than seawater.

Geographic entities mentioned:
surface_form: olivia lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.077
lon: -111.597
The British offered several damaged buildings and a hotel in their sector. The Americans initially offered a building on Lake Wannsee, but others objected that they would never get any work done in such a beautiful setting. Howley suggested another site not far distant from the American military headquarters, which was accepted by all on the condition that it was made serviceable. Operation.

Geographic entities mentioned:
surface_form: Lake Wannsee
instance_of: Lake
countries: Germany
coordinates: lat: 52.4275
lon: 13.173055555556
The terrain, rainforest, and climate of Central Africa, particularly in the catchments of the lower and middle Congo River and the Ubangui, Sangha, and Sanaga Rivers, present formidable obstacles to highway engineers, and paved roads there have short lifespans.

Geographic entities mentioned:
surface_form: Sangha
instance_of: Watercourse
countries: Cameroon
Central African Republic
Republic of the Congo
coordinates: lat: -1.2125
lon: 16.827777777778
surface_form: Sanaga River
instance_of: Watercourse
countries: Cameroon
coordinates: lat: 3.5593388888889
lon: 9.652175
Legacy. A shelter for homeless women and girls, Lletty Cranogwen was founded in the Rhondda valley in 1922 by the South Wales Women's Temperance Union and named to mark Rees's work to improve Welsh women's lives. There is a fisheries patrol vessel used by the Welsh Government based in Milford Haven that has been named after Cranogwen.

Geographic entities mentioned:
surface_form: Rhondda
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.615938888889
lon: -3.4175222222222
By July 1822, he was back at York Factory for the second meeting of the Northern Council, the first that he chaired. After the meeting he went by water to Lac Île-à-la-Crosse and then by dog sled to Fort Chipewyan and Fort Resolution on the Tıdeè Lake. He then went south to Fort Dunvegan on the Peace River and then Fort Edmonton and after the thaw, back to York Factory.

Geographic entities mentioned:
surface_form: Lac Île-à-la-Crosse
instance_of: Lake
countries: Canada
coordinates: lat: 55.4444
lon: -107.849
He sailed to the HBC post in Hawaii (then known as the Sandwich Islands) in February 1842, and back to Sitka, where he took a Russian ship to Okhotsk in June. He went on horseback to Yakutsk, up the Lena River by horse-drawn boat, visited Lake Baikal, went by horse and later carriage to Saint Petersburg and reached London by ship at the end of October.

Geographic entities mentioned:
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
It was later demolished to make room for Samuel Bronfman's pavilion, which was seen by Alcan CEO David Culver as an unforgivable act of vandalism. A street was named in his honor, called Simpson Street, next to Parc Percy-Walters, McGregor Street, and Maison John-Wilson-McConnell. The park was previously occupied by one of his houses, and was part of his 15 acre estate on Mount Royal.

Geographic entities mentioned:
surface_form: Mount Royal
instance_of: Mountain
countries: Canada
coordinates: lat: 45.506388888889
lon: -73.588888888889
The tall mountain is located in the Jotunheimen mountains about southeast of the village of Fossbergom and about southwest of the village of Vågåmo. The mountain is surrounded by several other notable mountains including Kvitingskjølen and Grjothovden to the west; Veslekjølen, Skarvhøi, and Ilvetjørnhøi to the northwest; Liaberget to the south; and Heranoshøi to the southwest.

Geographic entities mentioned:
surface_form: Kvitingskjølen
instance_of: Mountain
countries: Norway
coordinates: lat: 61.76666667
lon: 8.8
surface_form: Grjothovden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.77146
lon: 8.81144
surface_form: Veslekjølen
instance_of: Mountain
countries: Norway
coordinates: lat: 61.6396
lon: 8.7112
surface_form: Skarvhøi
instance_of: Mountain
countries: Norway
coordinates: lat: 61.8025
lon: 8.722777777777777
surface_form: Ilvetjørnhøi
instance_of: Mountain
countries: Norway
coordinates: lat: 61.7872
lon: 8.73776
surface_form: Liaberget
instance_of: Mountain
countries: Norway
coordinates: lat: 61.76668
lon: 8.85032
surface_form: Heranoshøi
instance_of: Mountain
countries: Norway
coordinates: lat: 61.68944444
lon: 8.80305556
Saukampen (Lom). Saukampen is a mountain in Lom Municipality in Innlandet county, Norway. The tall mountain is located in the Jotunheimen mountains about southeast of the village of Fossbergom and about southwest of the village of Vågåmo.

Geographic entities mentioned:
surface_form: saukampen
instance_of: Mountain
countries: Norway
coordinates: lat: 61.633305555556
lon: 9.4334333333333
surface_form: saukampen
instance_of: Mountain
countries: Norway
coordinates: lat: 61.62777778
lon: 9.43833333
The Herman Kluge era (1927–1955). In 1927, the Milwaukee Normal School became the Milwaukee State Teachers College and adopted its first official nickname, the &quot;Green Gulls&quot;. The name was chosen because the students were often greeted by seagulls from nearby Lake Michigan as they returned to campus in the fall.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Skogshorn. Skogshorn, also written Skogshødn, is a mountain in the municipality Hemsedal in the county Buskerud. Skogshorn is a part of Hemsedal Top 20. The summit of Skogshorn is a popular destination for day-trips both summer and winter. The east-side approach requires no climbing, and is popular for families and other mountain tourists. The south-side of the mountain can be climbed.

Geographic entities mentioned:
surface_form: skogshorn
instance_of: Mountain
countries: Norway
coordinates: lat: 60.8815
lon: 8.695
Ribault and hundreds of other survivors washed ashore, and began to walk north along the beach. At Matanzas Inlet, a Spanish patrol encountered the remnants of the French force, and took them prisoner. Following the king of Spain's express edict, all heretics were taken behind a sand dune and put to the sword. The few confessing Catholics and the young musicians were spared their lives.

Geographic entities mentioned:
surface_form: Matanzas Inlet
instance_of: Landform
countries: United States
coordinates: lat: 29.7058
lon: -81.2283
Ysasi gave up on his dreams, and fled to Cuba. The English named two rivers and a mountain after him to commemorate his assistance in expelling the Spaniards and bringing an end to Spanish Jamaica, as well as capturing hostile Maroons. The English appointed him Colonel of the Black Militia and guaranteed his palenque land and liberties &quot;for ever&quot;. War with other Maroons and Death.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Jamaica
coordinates: lat: 18.0706
lon: -77.1268
Lake Mohawk (Ohio). Lake Mohawk is a private reservoir located about south of Malvern, Ohio, USA and east of Waynesburg, Ohio. It resides in Brown Township and Harrison Township. The lake is relatively small, being a private lake containing of water with a maximum depth of. There is only one place to put in boats, however, there are 13 community access docks that can hold boats.

Geographic entities mentioned:
surface_form: lake mohawk
instance_of: Lake
countries: United States
coordinates: lat: 40.6739
lon: -81.1914
It resides in Brown Township and Harrison Township. The lake is relatively small, being a private lake containing of water with a maximum depth of. There is only one place to put in boats, however, there are 13 community access docks that can hold boats. The lake is formed by Lake Mohawk Dam across Middle Run, a tributary of Sandy Creek. The lake is fed by a series of springs and rainwater runoff.

Geographic entities mentioned:
surface_form: lake mohawk
instance_of: Lake
countries: United States
coordinates: lat: 40.6739
lon: -81.1914
The Main Beach has a large play area with swings and a jungle-gym. There is a designated swimming area along the shoreline of the beach. The Main Beach also holds the private ski club dock that is used by the Lake Mohawk Water Ski Club. Near the main gate entrance is the golf course which is a 9-hole, par 3 course. There is a small green fee to play.

Geographic entities mentioned:
surface_form: lake mohawk
instance_of: Lake
countries: United States
coordinates: lat: 40.6739
lon: -81.1914
There is also a no-release policy on Alaskan Pike. Lake community. The community was established in 1963 by the American Realty Service Corporation on of property. The lake is inside a gated community which contains approximately 1,700 property lots that are privately owned. There are 3 beaches: Main Beach, West Beach and South Beach. The Main Beach has tennis courts nearby.

Geographic entities mentioned:
surface_form: west beach
instance_of: Landform
countries: United States
coordinates: lat: 34.4106
lon: -119.69
Mount Cain. Mount Cain is a mountain on Vancouver Island, British Columbia, Canada, located east of Woss and 2 km north of Mount Abel. The mountain is home to a local ski hill operated by the Mount Cain Alpine Park Society. The Mount Cain ski hill is run mostly by volunteers, many of whom work in the forest industry on North Vancouver Island.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mount cain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.2286
lon: -126.326
Mount Cain. Mount Cain is a mountain on Vancouver Island, British Columbia, Canada, located east of Woss and 2 km north of Mount Abel. The mountain is home to a local ski hill operated by the Mount Cain Alpine Park Society. The Mount Cain ski hill is run mostly by volunteers, many of whom work in the forest industry on North Vancouver Island.

Geographic entities mentioned:
surface_form: mount cain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.2286
lon: -126.326
The mountain is home to a local ski hill operated by the Mount Cain Alpine Park Society. The Mount Cain ski hill is run mostly by volunteers, many of whom work in the forest industry on North Vancouver Island. &quot;Cain&quot;, as it is called for short, is known mostly for its back-country. The hill itself has two t-bars and a rope tow.

Geographic entities mentioned:
surface_form: mount cain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.2286
lon: -126.326
The town of North East borders the east, Stanford to the South and Milan to the west. Three small lakes lie west of Pine Plain's hamlet: Stissing Lake which is excellent for swimming, Thompson Pond which is dedicated to conservation for wildlife, and Twin Island Lake, known locally as &quot;Mud Pond&quot;. Stissing Mountain, the town's highest point at, is immediately to the west.

Geographic entities mentioned:
surface_form: Thompson Pond
instance_of: Lake
countries: United States
coordinates: lat: 41.961119444444
lon: -73.678736111111
Age 26, on May 2, 1915, she set out with her mother Avis (age 56) in the sidecar, who noted, &quot;I do not fear breakdowns for Effie, being a most careful driver, is a good mechanic and does her own repairing with her own tools.&quot;
They rode to Albany across the Hudson Valley, then travelled to Buffalo, and on to Chicago, averaging 150 miles a day.

Geographic entities mentioned:
surface_form: Hudson Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.9209
lon: -73.9613
Mocho has its earliest certainly recorded eruption in 1759, older eruptions reported are uncertain due to the usage of different names and inexact maps. The northern foothills of Mocho-Choshuenco are surrounded by an arc of rivers and lakes formed by Fui, Enco and Llanquihue River, and Pirihueico, Panguipulli and Riñihue Lakes.

Geographic entities mentioned:
surface_form: Pirihueico
instance_of: Lake
countries: Chile
coordinates: lat: -39.93
lon: -71.790277777778
surface_form: mocho
instance_of: Mountain
countries: Chile
coordinates: lat: -39.909722222222
lon: -72.0375
surface_form: choshuenco
instance_of: Mountain
countries: Chile
coordinates: lat: -39.909722222222
lon: -72.0375
surface_form: llanquihue
instance_of: Lake
countries: Chile
coordinates: lat: -41.133333333333
lon: -72.783333333333
The Fui River has high degree of underground infiltration, such that in some years the Huilo-Huilo Falls may dry out completely. As consequence of this infiltration a large aquifer is situated beneath Mocho-Choshuenco. The southern and eastern slopes drain to Pillanleufú River which flows south along the Liquiñe-Ofqui Fault to Maihue Lake. Name.

Geographic entities mentioned:
surface_form: Maihue Lake
instance_of: Lake
countries: Chile
coordinates: lat: -40.283333333333
lon: -72.05
The last reported eruption, is supposed to have occurred on June 16, 1936. Little is known about this event apart from the occurrence of mudflows and lahars, this have led volcanologists to consider this eruption report as a false report just like in the case of the supposed 1906 Lanín eruption. Glaciers.

Geographic entities mentioned:
surface_form: Lanín
instance_of: Mountain
countries: Argentina
Chile
coordinates: lat: -39.632777777778
lon: -71.499722222222
Mocho-Choshuenco. Mocho-Choshuenco (Pronounced:) is a glacier covered compound stratovolcano in the Andes of Los Ríos Region, Chile. It is made of the twin volcanoes Choshuenco in the northwest and the Mocho in the southeast. The highest parts of the volcano are part of the Mocho-Choshuenco National Reserve while the eastern slopes are partly inside the Huilo-Huilo Natural Reserve.

Geographic entities mentioned:
surface_form: mocho-choshuenco
instance_of: Mountain
countries: Chile
coordinates: lat: -39.909722222222
lon: -72.0375
surface_form: choshuenco
instance_of: Mountain
countries: Chile
coordinates: lat: -39.909722222222
lon: -72.0375
Mocho-Choshuenco. Mocho-Choshuenco (Pronounced:) is a glacier covered compound stratovolcano in the Andes of Los Ríos Region, Chile. It is made of the twin volcanoes Choshuenco in the northwest and the Mocho in the southeast. The highest parts of the volcano are part of the Mocho-Choshuenco National Reserve while the eastern slopes are partly inside the Huilo-Huilo Natural Reserve.

Geographic entities mentioned:
surface_form: mocho
instance_of: Mountain
countries: Chile
coordinates: lat: -39.909722222222
lon: -72.0375
surface_form: choshuenco
instance_of: Mountain
countries: Chile
coordinates: lat: -39.909722222222
lon: -72.0375
It is made of the twin volcanoes Choshuenco in the northwest and the Mocho in the southeast. The highest parts of the volcano are part of the Mocho-Choshuenco National Reserve while the eastern slopes are partly inside the Huilo-Huilo Natural Reserve. Choshuenco, located on the northwest rim of the 4 km wide caldera, is of late glacial age. It has a heavily eroded crater and is currently dormant.

Geographic entities mentioned:
surface_form: mocho-choshuenco
instance_of: Mountain
countries: Chile
coordinates: lat: -39.909722222222
lon: -72.0375
surface_form: choshuenco
instance_of: Mountain
countries: Chile
coordinates: lat: -39.909722222222
lon: -72.0375
Choshuenco, located on the northwest rim of the 4 km wide caldera, is of late glacial age. It has a heavily eroded crater and is currently dormant. Mocho is an andesitic-dacitic volcano placed above the caldera. Some parasitic craters and cinder cones are located on the southwest and northeast flanks of the stratovolcano.

Geographic entities mentioned:
surface_form: mocho
instance_of: Mountain
countries: Chile
coordinates: lat: -39.909722222222
lon: -72.0375
It has a heavily eroded crater and is currently dormant. Mocho is an andesitic-dacitic volcano placed above the caldera. Some parasitic craters and cinder cones are located on the southwest and northeast flanks of the stratovolcano. Mocho has its earliest certainly recorded eruption in 1759, older eruptions reported are uncertain due to the usage of different names and inexact maps.

Geographic entities mentioned:
surface_form: mocho
instance_of: Mountain
countries: Chile
coordinates: lat: -39.909722222222
lon: -72.0375
The Fui River has high degree of underground infiltration, such that in some years the Huilo-Huilo Falls may dry out completely. As consequence of this infiltration a large aquifer is situated beneath Mocho-Choshuenco. The southern and eastern slopes drain to Pillanleufú River which flows south along the Liquiñe-Ofqui Fault to Maihue Lake. Name.

Geographic entities mentioned:
surface_form: mocho-choshuenco
instance_of: Mountain
countries: Chile
coordinates: lat: -39.909722222222
lon: -72.0375
surface_form: choshuenco
instance_of: Mountain
countries: Chile
coordinates: lat: -39.909722222222
lon: -72.0375
Name. The two volcanoes have had several historical names such as Valdivia, used by Juan Ignacio Molina in 1795, and Panguipulli and Lajara, which Pedro Amadeo Pissis identified in 1875, as Choshuenco and Mocho respectively because only Choshuenco is visible from Panguipulli Lake.

Geographic entities mentioned:
surface_form: mocho
instance_of: Mountain
countries: Chile
coordinates: lat: -39.909722222222
lon: -72.0375
surface_form: choshuenco
instance_of: Mountain
countries: Chile
coordinates: lat: -39.909722222222
lon: -72.0375
surface_form: choshuenco
instance_of: Mountain
countries: Chile
coordinates: lat: -39.909722222222
lon: -72.0375
Other historical spellings and names for the volcanoes include Choshuenco-Pillán, Rauco, Penguipulli, Reñihue and Riñihue. The current name for the volcano is composed of the Spanish word &quot;mocho&quot; and the native Mapudungun word &quot;choshuenco&quot; (pronounced &quot;choswenko&quot;). &quot;Mocho&quot; means short cut and refers to the headless or edgeless shape of Mocho's volcanic cone.

Geographic entities mentioned:
surface_form: mocho
instance_of: Mountain
countries: Chile
coordinates: lat: -39.909722222222
lon: -72.0375
surface_form: mocho
instance_of: Mountain
countries: Chile
coordinates: lat: -39.909722222222
lon: -72.0375
surface_form: choshuenco
instance_of: Mountain
countries: Chile
coordinates: lat: -39.909722222222
lon: -72.0375
Other historical spellings and names for the volcanoes include Choshuenco-Pillán, Rauco, Penguipulli, Reñihue and Riñihue. The current name for the volcano is composed of the Spanish word &quot;mocho&quot; and the native Mapudungun word &quot;choshuenco&quot; (pronounced &quot;choswenko&quot;). &quot;Mocho&quot; means short cut and refers to the headless or edgeless shape of Mocho's volcanic cone.

Geographic entities mentioned:
surface_form: mocho
instance_of: Mountain
countries: Chile
coordinates: lat: -39.909722222222
lon: -72.0375
Glaciers of the ice sheet also reworked previously deposited layers. Some 10,300 years ago Choshuenco produced the Neltume Pumice during a plinian eruption. The earliest historical accounts of eruptions from the Mocho-Choshuenco complex may be those in Alonso de Ovalle's map &quot;Tabula Geographica Regni Chile&quot; from 1646.

Geographic entities mentioned:
surface_form: choshuenco
instance_of: Mountain
countries: Chile
coordinates: lat: -39.909722222222
lon: -72.0375
Some 10,300 years ago Choshuenco produced the Neltume Pumice during a plinian eruption. The earliest historical accounts of eruptions from the Mocho-Choshuenco complex may be those in Alonso de Ovalle's map &quot;Tabula Geographica Regni Chile&quot; from 1646. Here Mocho-Choshuenco may be one of the mountains drawn as erupting volcanoes east of Valdivia.

Geographic entities mentioned:
surface_form: mocho-choshuenco
instance_of: Mountain
countries: Chile
coordinates: lat: -39.909722222222
lon: -72.0375
surface_form: choshuenco
instance_of: Mountain
countries: Chile
coordinates: lat: -39.909722222222
lon: -72.0375
Glaciers. The uppermost part of Mocho-Choshuenco is covered by an ice cap that surrounds the volcanic cone of Mocho and some flanks of Choshuenco. By 2003 the ice cap had shrunk in area by a total of 40% of its area of 1976. The largest retreat by area occurred on Choshuenco Glacier in the northwest.

Geographic entities mentioned:
surface_form: mocho
instance_of: Mountain
countries: Chile
coordinates: lat: -39.909722222222
lon: -72.0375
surface_form: choshuenco
instance_of: Mountain
countries: Chile
coordinates: lat: -39.909722222222
lon: -72.0375
It is made of the twin volcanoes Choshuenco in the northwest and the Mocho in the southeast. The highest parts of the volcano are part of the Mocho-Choshuenco National Reserve while the eastern slopes are partly inside the Huilo-Huilo Natural Reserve. Choshuenco, located on the northwest rim of the 4 km wide caldera, is of late glacial age. It has a heavily eroded crater and is currently dormant.

Geographic entities mentioned:
surface_form: choshuenco
instance_of: Mountain
countries: Chile
coordinates: lat: -39.909722222222
lon: -72.0375
The two volcanoes have had several historical names such as Valdivia, used by Juan Ignacio Molina in 1795, and Panguipulli and Lajara, which Pedro Amadeo Pissis identified in 1875, as Choshuenco and Mocho respectively because only Choshuenco is visible from Panguipulli Lake. Other historical spellings and names for the volcanoes include Choshuenco-Pillán, Rauco, Penguipulli, Reñihue and Riñihue.

Geographic entities mentioned:
surface_form: choshuenco
instance_of: Mountain
countries: Chile
coordinates: lat: -39.909722222222
lon: -72.0375
By 2003 the ice cap had shrunk in area by a total of 40% of its area of 1976. The largest retreat by area occurred on Choshuenco Glacier in the northwest. Mocho Glacier runs from Mocho's cone to the southeast and is the largest glacier of the volcano with its 5.1 km2 followed by Choshuenco Glacier (2 km2).

Geographic entities mentioned:
surface_form: choshuenco
instance_of: Mountain
countries: Chile
coordinates: lat: -39.909722222222
lon: -72.0375
Kamilukuak Lake. Kamilukuak Lake is a large lake in the Kivalliq Region of Nunavut in Canada. Part of the lake to the west lies in the Northwest Territories. The lake is 25 km south of Dubawnt Lake.

Geographic entities mentioned:
surface_form: Dubawnt Lake
instance_of: Lake
countries: Canada
coordinates: lat: 63.1
lon: -101.53333333333
Kamilukuak Lake. Kamilukuak Lake is a large lake in the Kivalliq Region of Nunavut in Canada. Part of the lake to the west lies in the Northwest Territories. The lake is 25 km south of Dubawnt Lake.

Geographic entities mentioned:
surface_form: kamilukuak lake
instance_of: Lake
countries: Canada
coordinates: lat: 62.3193
lon: -101.802
Nisans. bravzraddcl76m601qs472nplu1w" xml:space="preserve">The Nisans (Latin: &quot;Nisane&quot;; Polish: &quot;Niżanie&quot;, &quot;Niszanie&quot;) were a Sorbian tribe that inhabited the basin of Elbe river near Dresden. They most likely were in the union with Glomatian tribe.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Guardian Nunatak. qy6j43esiopqyhw6xzxb73sidg4u" xml:space="preserve">Guardian Nunatak () is a rock exposure, high, on the ice-covered spur that descends from Mount Robert Scott east-northeastward toward the western edge of Hood Glacier, near the juncture with Ross Ice Shelf.

Geographic entities mentioned:
surface_form: Mount Robert Scott
instance_of: Mountain
coordinates: lat: -83.81666667
lon: 172.8
surface_form: scott
instance_of: Mountain
coordinates: lat: -65.15158
lon: -64.04798
surface_form: guardian nunatak
instance_of: Mountain
coordinates: lat: -83.8167
lon: 173.233
Guardian Nunatak. qy6j43esiopqyhw6xzxb73sidg4u" xml:space="preserve">Guardian Nunatak () is a rock exposure, high, on the ice-covered spur that descends from Mount Robert Scott east-northeastward toward the western edge of Hood Glacier, near the juncture with Ross Ice Shelf.

Geographic entities mentioned:
surface_form: guardian nunatak
instance_of: Mountain
coordinates: lat: -83.8167
lon: 173.233
At Trevose Head in Cornwall, 600 pixies were said to have gathered dancing and laughing in a circle that had appeared upon the turf until one of them, named Omfra, lost his laugh. After searching amongst the barrows of the ancient kings of Cornwall on St Breock Downs, he wades through the bottomless Dozmary Pool on Bodmin Moor until his laugh is restored by King Arthur in the form of a Chough.

Geographic entities mentioned:
surface_form: Dozmary Pool
instance_of: Lake
countries: United Kingdom
coordinates: lat: 50.5423
lon: -4.5502
The council subsequently gained back ownership of Cessnock Airport in December 2011, which had stayed the same since. Airport usage. Cessnock Airport is a popular Flight training aerodrome servicing Newcastle and Lower Hunter based pilots and students. It is usually considered so popular due to its large training area, which it shares with Maitland Airport and other Hunter Region aerodromes.

Geographic entities mentioned:
surface_form: Lower Hunter
instance_of: Valley
countries: Australia
coordinates: lat: -32.56
lon: 151.17083333333332
Airport usage. Cessnock Airport is a popular Flight training aerodrome servicing Newcastle and Lower Hunter based pilots and students. It is usually considered so popular due to its large training area, which it shares with Maitland Airport and other Hunter Region aerodromes. It is home to flight schools, such as Phil Unicomb Aviation and Aerohunter Flight Training.

Geographic entities mentioned:
surface_form: Hunter Region
instance_of: Valley
countries: Australia
coordinates: lat: -32.56
lon: 151.17083333333332
Location. Situated at the east of the Chartreuse Mountains in Rhône-Alpes, the nature reserve stretches from Mont Granier north to the Dent de Crolles south located at about 20 km. The territory concerns 11 communes (&quot;french townships&quot;) of 2 departments.

Geographic entities mentioned:
surface_form: Mont Granier
instance_of: Mountain
countries: France
coordinates: lat: 45.46472222
lon: 5.92527778
surface_form: Dent de Crolles
instance_of: Mountain
countries: France
coordinates: lat: 45.308333
lon: 5.855278
No. 4 Troop then worked with the Vis Motor Gun Boat flotilla boarding enemy shipping. In April 1944, the commando lost No. 6 Polish Troop which was transferred to the II Polish Corps and later took part in the Polish assault on Monte Cassino. By the time of the D-Day landings the commando had lost the Yugoslav and Polish troops, and the two French troops were attached to No.

Geographic entities mentioned:
surface_form: Monte Cassino
instance_of: Mountain
countries: Italy
coordinates: lat: 41.49
lon: 13.813888888889
Hawaii Route 19 runs through the southern part of the community, leading southeast to Hilo and west to Waimea. Hawaii Route 240 branches off Route 19 and runs through the center of Honokaa, then continues west to its terminus at the Waipio Valley lookout. According to the United States Census Bureau, the CDP has a total area of, all of it land. 2000 Census data.

Geographic entities mentioned:
surface_form: Waipio Valley
instance_of: Valley
countries: United States
coordinates: lat: 20.1197
lon: -155.593
Rhondda Tunnel Society. The Rhondda Tunnel Society was formed in September 2014. Its short-term goal was to replace the tunnel's portal stone, above the entrance of the tunnel at Blaencwm. The Blaengwynfi portal stone is in the Afan Forest Park. In May 2018, the tunnel was opened up so that surveys could take place.

Geographic entities mentioned:
surface_form: Afan Forest Park
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.632802777778
lon: -3.7327583333333
His companions in this task were Gonzalo Suárez Rendón, Pedro Fernández de Valenzuela and Diego Paredes. Fonte was imprisoned but released when he informed De Quesada of the arrival of two other conquest expeditions on the Altiplano Cundiboyacense, by Nikolaus Federmann from the east and Sebastián de Belalcázar from the south. Fonte had used the skin of a deer to write his revelations.

Geographic entities mentioned:
surface_form: Altiplano Cundiboyacense
instance_of: Plateau
countries: Colombia
coordinates: lat: 5.532209
lon: -73.362877
Naranag. &quot;Naranag&quot; or &quot;(Nara Nag)&quot; is a tourist village and ancient Hindu pilgrimage site, near Ganderbal town in the Ganderbal district of the Kashmir Valley in Jammu and Kashmir. Well known for its ancient temple ruins complex, it is located around 16km from Kangan, 10km upstream from the Sind River.

Geographic entities mentioned:
surface_form: Kashmir Valley
instance_of: Valley
countries: India
coordinates: lat: 34.0333
lon: 74.6667
Well known for its ancient temple ruins complex, it is located around 16km from Kangan, 10km upstream from the Sind River. Noted for its scenic meadows, lakes and mountains, it is a base camp for trekking to the Mount Haramukh and Gangabal Lake.

Geographic entities mentioned:
surface_form: Gangabal Lake
instance_of: Lake
countries: India
coordinates: lat: 34.4325
lon: 74.925
Tourism. The Naranag valley is noted for its scenic meadows. The village is a base camp for trekkers to the Mount Haramukh, the Gangabal Lake and Satsar (the seven lakes). It is also a base for the trekkers to Gadsar Lake, the Vishansar Lake and the Krishansar Lake, though it takes 5 to 7 days of trekking. There are also many other peaks and alpine meadows around the Naranag Valley.

Geographic entities mentioned:
surface_form: Gangabal Lake
instance_of: Lake
countries: India
coordinates: lat: 34.4325
lon: 74.925
Tourism. The Naranag valley is noted for its scenic meadows. The village is a base camp for trekkers to the Mount Haramukh, the Gangabal Lake and Satsar (the seven lakes). It is also a base for the trekkers to Gadsar Lake, the Vishansar Lake and the Krishansar Lake, though it takes 5 to 7 days of trekking. There are also many other peaks and alpine meadows around the Naranag Valley.

Geographic entities mentioned:
surface_form: Gadsar Lake
instance_of: Lake
countries: India
coordinates: lat: 34.421669
lon: 75.057274
surface_form: Vishansar Lake
instance_of: Lake
countries: India
coordinates: lat: 34.3881
lon: 75.1188
surface_form: Krishansar Lake
instance_of: Lake
countries: India
coordinates: lat: 34.39694444444444
lon: 75.1025
Such beliefs remain popular among residents. The government has built perimeter walls around the temple ruins to protect it from encroachment. Every year on the eve of pilgrimage to Gangabal Lake by Kashmiri Pandits, prayers are offered at the temple complex to kick start the pilgrimage. Issues.

Geographic entities mentioned:
surface_form: Gangabal Lake
instance_of: Lake
countries: India
coordinates: lat: 34.4325
lon: 74.925
He is one of six known children of Thutmose and Merytre; his siblings are Pharaoh Amenhotep II, and princesses Nebetiunet, Meritamen, the second Meritamen and Iset. He is depicted together with his sisters on a statue of their maternal grandmother Hui (now in the British Museum). It is likely that some canopic jar fragments from the Valley of the Queens are his.

Geographic entities mentioned:
surface_form: Valley of the Queens
instance_of: Valley
countries: Egypt
coordinates: lat: 25.7275
lon: 32.593055555556
Mount Sir Allan MacNab. Mount Sir Allan MacNab is a mountain located in the Premier Range of British Columbia, Canada. The range is named for Sir Allan MacNab, a Canadian industrialist who was premier of the Province of Canada from 1854 to 1856.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mount sir allan macnab
instance_of: Mountain
countries: Canada
coordinates: lat: 52.52
lon: -119.203
Mount Sir Allan MacNab. Mount Sir Allan MacNab is a mountain located in the Premier Range of British Columbia, Canada. The range is named for Sir Allan MacNab, a Canadian industrialist who was premier of the Province of Canada from 1854 to 1856.

Geographic entities mentioned:
surface_form: mount sir allan macnab
instance_of: Mountain
countries: Canada
coordinates: lat: 52.52
lon: -119.203
In the same year, the Mysore-Hassan railway line of Mysore Railways was extended, linking Saligrama and Yedatur with the line at Arsikere. The first Mysore Economic Conference was inaugurated on 10 June 1910 and met once every year. In 1911/1912, construction of the Krishnaraja Sagara Dam across the Kaveri at Kannambadi village was commenced. It was Rao who invited Sir M.

Geographic entities mentioned:
surface_form: Kaveri
instance_of: Watercourse
countries: India
coordinates: lat: 11.370345
lon: 79.828105
Pardue Peak. Pardue Peak () is the northernmost peak, 1,840 m, on Smith Ridge in the Founders Peaks, Heritage Range. It was mapped by the United States Geological Survey (USGS) from surveys and U.S. Navy air photos from 1961 to 1966. It was named by the Advisory Committee on Antarctic Names (US-ACAN) for Lieutenant A. Michael Pardue, (MC) U.S.

Geographic entities mentioned:
surface_form: Founders Peaks
instance_of: Mountain
coordinates: lat: -79.1667
lon: -86.25
surface_form: smith
instance_of: Lake
coordinates: lat: -66.1167
lon: 101.283
surface_form: pardue peak
instance_of: Mountain
coordinates: lat: -79.1
lon: -86.516666666667
Pardue Peak. Pardue Peak () is the northernmost peak, 1,840 m, on Smith Ridge in the Founders Peaks, Heritage Range. It was mapped by the United States Geological Survey (USGS) from surveys and U.S. Navy air photos from 1961 to 1966. It was named by the Advisory Committee on Antarctic Names (US-ACAN) for Lieutenant A. Michael Pardue, (MC) U.S.

Geographic entities mentioned:
surface_form: pardue peak
instance_of: Mountain
coordinates: lat: -79.1
lon: -86.516666666667
Stewart married Paul Lemon, professor for plant ecology at Albany. In 1963, she obtained a Fulbright Fellowship to travel to Africa, and the two of them travelled to Malawi for a year, where she worked on the herpetofauna of the Nyika Plateau. They divorced after their return from Malawi. She later married George E. Martin, a mathematician at University at Albany.

Geographic entities mentioned:
surface_form: Nyika Plateau
instance_of: Plateau
countries: Malawi
Zambia
coordinates: lat: -10.35
lon: 33.6
It sits in the disputed border territory between Bhutan and China. The name &quot;Tongshanjiabu&quot; is indicated on a map from the Japanese Alpine News, May 2003, p. 44. The region's highpoint is sometimes given as &quot;Teri Kang&quot;, but this appears to be the name of a subsidiary top (Teri Kang). Climbing history. Tongshanjiabu has never been known to be climbed.

Geographic entities mentioned:
surface_form: Teri Kang
instance_of: Mountain
countries: Bhutan
coordinates: lat: 28.171884
lon: 89.942222
Royalton raid. The Royalton raid was a British-led Indian raid in 1780 against various towns along the White River Valley in the Vermont Republic during the American Revolutionary War. It was the last major Indian raid in New England. Raids. Lieutenant Richard Houghton of the 53rd Regiment of Foot led 300 Mohawk warriors from the Kahnawake Reserve in the British province of Quebec in October 1780.

Geographic entities mentioned:
surface_form: White River Valley
instance_of: Valley
coordinates: lat: 43.6484
lon: -72.3132
On October 16, they attacked and burned the towns of Royalton, Sharon, and Tunbridge along the White River in eastern Vermont. This raid was launched in conjunction with other raids led by Major Christopher Carleton of the 29th Regiment of Foot along the shores of Lake Champlain and Lake George, and Sir John Johnson of the King's Royal Regiment of New York in the Mohawk River valley.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
The Peterhof maintained special ties with Visby, although Lübeck tried to take over control only with partial success. Visby and Lübeck were in the 15th century sidelined by the Livonian towns. Ships from the Baltic accessed Novgorod over the Neva, Lake Ladoga and the Volkhov. Transport over land was in winter by sleighs, moving to Dorpat via Pskov.

Geographic entities mentioned:
surface_form: Lake Ladoga
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.842777777777776
lon: 31.459722222222222
Its source is confluence of Bijela River and Crna River, between Tarčin and Kreševo. The source of Bijela Rijeka is under the Bjelašnica mountain, while Crna Rijeka springs under the slopes of mountains of Bitovinja and Ivan. The major settlement on its course is Kiseljak, through which it passes before the confluence with the Fojnička River.

Geographic entities mentioned:
surface_form: Bitovinja
instance_of: Mountain
countries: Bosnia and Herzegovina
coordinates: lat: 43.802
lon: 17.935
surface_form: Ivan
instance_of: Mountain
countries: Bosnia and Herzegovina
coordinates: lat: 43.79198
lon: 18.0092
Lac de Pormenaz. Lac de Pormenaz is an alpine lake in the Passy National Nature Preserve (Réserve naturelle nationale de Passy) of the Haute-Savoie department of France. Its surface area of 4.4 ha is at an elevation of 1945 m. The lake can be reached by foot from the village of Plaine Joux above Servoz.

Geographic entities mentioned:
surface_form: lac de pormenaz
instance_of: Lake
countries: France
coordinates: lat: 45.962324
lon: 6.793996
By 1920, the stream was entirely diverted into the sewer system. There are many artifacts of the Creek's existence, including buried bridges along Harbord Street and Crawford Street south of Dundas Street. The unusual courses of Niagara Street (north of Fort York) and Vaughan Road (St. Clair and Bathurst area) indicate that they were once trails following the banks of the creek.

Geographic entities mentioned:
surface_form: niagara
instance_of: Mountain
countries: Canada
coordinates: lat: 43.8334
lon: -79.99966
Garrison Creek (Ontario). Garrison Creek was a short stream about long that flowed southeast into the west side of Toronto Harbour in Ontario, Canada. It has been largely covered over and filled in, but geographical traces of the creek can still be found, including the natural amphitheatre known as Christie Pits and the off-leash dog &quot;bowl&quot; of Trinity Bellwoods Park.

Geographic entities mentioned:
surface_form: garrison creek (ontario)
instance_of: Watercourse
countries: Canada
coordinates: lat: 43.641730555555554
lon: -79.406625
Garrison Creek (Ontario). Garrison Creek was a short stream about long that flowed southeast into the west side of Toronto Harbour in Ontario, Canada. It has been largely covered over and filled in, but geographical traces of the creek can still be found, including the natural amphitheatre known as Christie Pits and the off-leash dog &quot;bowl&quot; of Trinity Bellwoods Park.

Geographic entities mentioned:
surface_form: garrison creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 43.641730555555554
lon: -79.406625
It has been largely covered over and filled in, but geographical traces of the creek can still be found, including the natural amphitheatre known as Christie Pits and the off-leash dog &quot;bowl&quot; of Trinity Bellwoods Park. The name &quot;Garrison Creek&quot; was used because Fort York was built near the creek mouth. Volunteers lead popular tours of the course of the old watershed. History.

Geographic entities mentioned:
surface_form: garrison creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 43.641730555555554
lon: -79.406625
The unusual courses of Niagara Street (north of Fort York) and Vaughan Road (St. Clair and Bathurst area) indicate that they were once trails following the banks of the creek. In 2013 particularly strong rainstorms caused the storm sewers that replaced Garrison Creek to flood, at Christie Pits, Trinity Bellwoods Park, and a railway underpass at King Street and Atlantic Avenue.

Geographic entities mentioned:
surface_form: garrison creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 43.641730555555554
lon: -79.406625
Both Christie Pits and Trinity Bellwoods Park are over the original Garrison Creek Ravine, while the King and Atlantic intersection is over the course of Asylum Stream, a tributary that ran from just northwest of Fort York to Lisgar Street and Queen Street West near the former Provincial Asylum. Course. The stream had two sources, one north of St.

Geographic entities mentioned:
surface_form: garrison creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 43.641730555555554
lon: -79.406625
Topographic relief is significant as the summit rises above the Lawrence Glacier in one-half kilometre. The nearest higher peak is Red Peak, one kilometre to the west. New Zealand mountaineer Guy Mannering (1862–1947) applied the toponym on 16 May 1893 because the peak is situated at the northernmost tip of the Arrowsmith Range.

Geographic entities mentioned:
surface_form: red peak
instance_of: Mountain
coordinates: lat: -43.31444444444444
lon: 170.98944444444444
Description. North Peak is located west of Christchurch in the South Island. It is set at the eastern end of the Jollie Range of the Southern Alps. Precipitation runoff from the mountain's southwest slope drains into the headwaters of the Lawrence River, whereas all other slopes drain into Jagged Stream and Reischek Stream which are both tributaries of the Rakaia River.

Geographic entities mentioned:
surface_form: southern
instance_of: Mountain
coordinates: lat: -74.2
lon: -76.4667
It is set at the eastern end of the Jollie Range of the Southern Alps. Precipitation runoff from the mountain's southwest slope drains into the headwaters of the Lawrence River, whereas all other slopes drain into Jagged Stream and Reischek Stream which are both tributaries of the Rakaia River. Topographic relief is significant as the summit rises above the Lawrence Glacier in one-half kilometre.

Geographic entities mentioned:
surface_form: lawrence
instance_of: Mountain
coordinates: lat: -67.85
lon: 62.516666666667