Sarmila/GeoWiki-Features huggingface dataset:
Kakiddi Creek. Kakiddi Creek is a tributary of the Klastline River in northwest part of the province of British Columbia, Canada. It flows north about through two lakes in a broad hummocky lowland to join the Klastline River, which in turn is a tributary of the Stikine River.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: kakiddi creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.872778
lon: -130.425556
Both Kakiddi Lake and Nuttlude Lake lie behind large alluvial fans deposited by east-flowing tributaries. The glacial and landslide debris comprising these alluvial fans originated from the rapidly eroding headwalls and steep spurs on the eastern side of the Mount Edziza volcanic complex. Kakiddi Creek contains six named left tributaries.

Geographic entities mentioned:
surface_form: mount edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Both lakes also provide access to Mount Edziza Provincial Park as they are large enough to be used by float-equipped aircraft. Geology. Kakiddi Creek is the namesake of the Kakiddi Formation, a geological formation of the Mount Edziza volcanic complex. It consists of thick Pleistocene trachyte lava flows and pyroclastic rocks that extend into Kakiddi Creek valley.

Geographic entities mentioned:
surface_form: mount edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: kakiddi creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.872778
lon: -130.425556
In doing so, the lava flow temporarily blocked Kakiddi Creek to form a lava-dammed lake. Subsequent etching of this lava dam by Kakiddi Creek has exposed beds of lacustrine silt upstream from the lava. Moraine Cone and the associated lava flow are assigned to the Big Raven Formation, the youngest geological formation of the Mount Edziza volcanic complex.

Geographic entities mentioned:
surface_form: mount edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Moraine Cone and the associated lava flow are assigned to the Big Raven Formation, the youngest geological formation of the Mount Edziza volcanic complex. A Holocene lava flow from the eastern slope of the Mount Edziza volcanic complex extends almost to Nuttlude Lake and is also part of the Big Raven Formation.

Geographic entities mentioned:
surface_form: mount edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Kakiddi Creek's watershed covers and its estimated mean annual discharge is. The mouth of Kakiddi Creek is located about west of Iskut, east of Telegraph Creek and about south-southwest of Dease Lake. Kakiddi Creek's watershed's land cover is classified as 46.6% conifer forest, 17.4% barren, 15.4% shrubland, 11.2% herbaceous, 5.4% snow/glacier, and small amounts of other cover. Geography.

Geographic entities mentioned:
surface_form: dease lake
instance_of: Lake
countries: Canada
coordinates: lat: 58.63502
lon: -130.03761
surface_form: kakiddi creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.872778
lon: -130.425556
It flows north about through two lakes in a broad hummocky lowland to join the Klastline River, which in turn is a tributary of the Stikine River. Kakiddi Creek forms the northeastern boundary of Mount Edziza Provincial Park which lies within the traditional territory of the Tahltan people. Kakiddi Creek's watershed covers and its estimated mean annual discharge is.

Geographic entities mentioned:
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: kakiddi creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.872778
lon: -130.425556
The only named right tributary, Quash Creek, flows west into Kakiddi Creek. Kakiddi Lake and Nuttlude Lake are well populated with rainbow trout and provide fishing in Mount Edziza Provincial Park. Both lakes also provide access to Mount Edziza Provincial Park as they are large enough to be used by float-equipped aircraft. Geology.

Geographic entities mentioned:
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
The third named left tributary, Nido Creek, also flows northeast into Nuttlude Lake. Tenchen Creek, the fourth named left tributary, flows northeast into Kakiddi Creek. The fifth named left tributary, Pyramid Creek, flows east into Kakiddi Creek. Tsecha Creek is the sixth named left tributary which flows northeast into Kakiddi Creek.

Geographic entities mentioned:
surface_form: pyramid creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.91673
lon: -118.05237
surface_form: kakiddi creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.872778
lon: -130.425556
Kakiddi Creek. Kakiddi Creek is a tributary of the Klastline River in northwest part of the province of British Columbia, Canada. It flows north about through two lakes in a broad hummocky lowland to join the Klastline River, which in turn is a tributary of the Stikine River.

Geographic entities mentioned:
surface_form: kakiddi creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.872778
lon: -130.425556
Kakiddi Creek forms the northeastern boundary of Mount Edziza Provincial Park which lies within the traditional territory of the Tahltan people. Kakiddi Creek's watershed covers and its estimated mean annual discharge is. The mouth of Kakiddi Creek is located about west of Iskut, east of Telegraph Creek and about south-southwest of Dease Lake.

Geographic entities mentioned:
surface_form: kakiddi creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.872778
lon: -130.425556
Kakiddi Creek's watershed covers and its estimated mean annual discharge is. The mouth of Kakiddi Creek is located about west of Iskut, east of Telegraph Creek and about south-southwest of Dease Lake. Kakiddi Creek's watershed's land cover is classified as 46.6% conifer forest, 17.4% barren, 15.4% shrubland, 11.2% herbaceous, 5.4% snow/glacier, and small amounts of other cover. Geography.

Geographic entities mentioned:
surface_form: kakiddi creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.872778
lon: -130.425556
The glacial and landslide debris comprising these alluvial fans originated from the rapidly eroding headwalls and steep spurs on the eastern side of the Mount Edziza volcanic complex. Kakiddi Creek contains six named left tributaries. The first one is Sorcery Creek which flows east into Kakiddi Lake. Tennaya Creek is the second named left tributary which flows northeast into Nuttlude Lake.

Geographic entities mentioned:
surface_form: kakiddi creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.872778
lon: -130.425556
The fifth named left tributary, Pyramid Creek, flows east into Kakiddi Creek. Tsecha Creek is the sixth named left tributary which flows northeast into Kakiddi Creek. The only named right tributary, Quash Creek, flows west into Kakiddi Creek. Kakiddi Lake and Nuttlude Lake are well populated with rainbow trout and provide fishing in Mount Edziza Provincial Park.

Geographic entities mentioned:
surface_form: kakiddi creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.872778
lon: -130.425556
Geology. Kakiddi Creek is the namesake of the Kakiddi Formation, a geological formation of the Mount Edziza volcanic complex. It consists of thick Pleistocene trachyte lava flows and pyroclastic rocks that extend into Kakiddi Creek valley. A Holocene lava flow from Moraine Cone on the north slope of Mount Edziza entered Kakiddi Creek near its junction with the Klastline River.

Geographic entities mentioned:
surface_form: kakiddi creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.872778
lon: -130.425556
A Holocene lava flow from Moraine Cone on the north slope of Mount Edziza entered Kakiddi Creek near its junction with the Klastline River. In doing so, the lava flow temporarily blocked Kakiddi Creek to form a lava-dammed lake. Subsequent etching of this lava dam by Kakiddi Creek has exposed beds of lacustrine silt upstream from the lava.

Geographic entities mentioned:
surface_form: kakiddi creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.872778
lon: -130.425556
In doing so, the lava flow temporarily blocked Kakiddi Creek to form a lava-dammed lake. Subsequent etching of this lava dam by Kakiddi Creek has exposed beds of lacustrine silt upstream from the lava. Moraine Cone and the associated lava flow are assigned to the Big Raven Formation, the youngest geological formation of the Mount Edziza volcanic complex.

Geographic entities mentioned:
surface_form: kakiddi creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.872778
lon: -130.425556
Local governments have frequently turned to private companies to manage these sites and operate tourism businesses. Sites may also come under many overlapping authorities, as in the case of Mount Wutai, a national park and World Heritage Site, which is managed by eight government agencies and governed by 29 international, national, and local laws.

Geographic entities mentioned:
surface_form: Mount Wutai
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 39.081388888889
lon: 113.56694444444
Briefly skirting the Haight-Ashbury and Cole Valley neighborhoods, the route ascends Parnassus Street and passes the University of California, San Francisco's main campus. Turning south onto 7th Avenue in the Inner Sunset, the route curves around Mount Sutro and the Laguna Honda Reservoir before turning east and climbing Twin Peaks.

Geographic entities mentioned:
surface_form: Mount Sutro
instance_of: Mountain
countries: United States
coordinates: lat: 37.758106
lon: -122.4571803
Like many other supernaturals, the Banded-eye God has a cleft head and a downturned mouth. Unlike others, the Banded-eye God is only known from its profile - these renditions are generally concentrated on bowls from the Valley of Mexico (as shown on left), although the Banded-eye God is one of the five supernaturals shown on Las Limas monument 1 from the Olmec heartland.

Geographic entities mentioned:
surface_form: Valley of Mexico
instance_of: Valley
countries: Mexico
coordinates: lat: 19.66666667
lon: -98.86666667
Career. Stevenson came to the Red River Valley long in advance of any of the settlements, excepting that at Pembina and Walhallalong before Bismarck, Fargo, Wahpeton or Grand Forks had any inhabitants. He was at Pembina in 1863, engaged as an army freighter in charge of a train of 300 wagons with supplies for Hatch's battalion.

Geographic entities mentioned:
surface_form: Red River Valley
instance_of: Valley
countries: Canada
United States
coordinates: lat: 49
lon: -97.5
Hirwaun. Hirwaun (,;) is a village and community at the north end of the Cynon Valley in the County Borough of Rhondda Cynon Taf, South Wales. It is NW of the town of Aberdare, and comes under the Aberdare post town. At the 2001 census, Hirwaun had a population of 4,851; increasing at the 2011 census to 4,990.

Geographic entities mentioned:
surface_form: Cynon Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.657
lon: -3.461
The tower blocks. Hirwaun made local news in May 2004 when its two 1960s-built tower blocks were demolished by dynamite detonation. Their demise marked the end of a major landmark in the Cynon Valley and was symptomatic of a broader failure in the design of British public housing. Hirwaun Common development. Currently the patch of green land known as Hirwaun Common is being strip mined again.

Geographic entities mentioned:
surface_form: Cynon Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.657
lon: -3.461
Academic sources indicate that Qendresa transitioned into a subtropical cyclone, prior to reaching peak intensity. Qendresa caused three fatalities, and at least $250 million (2014 USD) in damages in Italy. Meteorological history. A shortwave trough near the British Isles started to expand southwards to North Africa on 3 November, which caused Lake Maggiore in Italy to overflow.

Geographic entities mentioned:
surface_form: Lake Maggiore
instance_of: Lake
countries: Switzerland
Italy
coordinates: lat: 46.098055555555554
lon: 8.714722222222223
Royal geographer. In the 1680s, he prepared the first-ever map of all of New Spain, which won high praise and was widely copied. He also drew hydrologic maps of the Valley of Mexico. In 1692 King Charles II named him official geographer for the colony.

Geographic entities mentioned:
surface_form: Valley of Mexico
instance_of: Valley
countries: Mexico
coordinates: lat: 19.66666667
lon: -98.86666667
Roslyn made landfall on October 23 near Santa Cruz in northern Nayarit, at 11:20 UTC with winds. Inland, Roslyn weakened quickly to a tropical storm, and then dissipated over east-central Mexico on October 24. Roslyn prompted the issuance of hurricane and tropical storm watches and warnings by the Mexican government for Western Mexico.

Geographic entities mentioned:
surface_form: east-central Mexico
instance_of: Plateau
countries: Mexico
coordinates: lat: 24
lon: -103
Bridge of National Unity, in Hungary, is the longest pedestrian suspension bridge, as of 2024, and before Sky Bridge 721 was the longest which spans in the Králický Sněžník mountain in the Czech Republic, opened in May 2022. The bridge hangs above ground. The United Wholesale Mortgage Pedestrian Bridge in Pontiac, Michigan is the longest enclosed pedestrian bridge, completed on October 1, 2021.

Geographic entities mentioned:
surface_form: Králický Sněžník
instance_of: Mountain
countries: Czech Republic
Poland
coordinates: lat: 50.2075
lon: 16.846944444444
The Germans failed in their objectives. The operation, initially planned for 5 March, began after German units were moved in great secrecy to the Lake Balaton () area. Many German units were involved, including the 6th Panzer Army and its subordinate Waffen-SS divisions after being withdrawn from the failed Ardennes offensive on the Western Front.

Geographic entities mentioned:
surface_form: Lake Balaton
instance_of: Lake
countries: Hungary
coordinates: lat: 46.85
lon: 17.72
Many German units were involved, including the 6th Panzer Army and its subordinate Waffen-SS divisions after being withdrawn from the failed Ardennes offensive on the Western Front. The Germans attacked in three prongs: &quot;Frühlingserwachen&quot; in the Balaton-Lake Velence-Danube area, &quot;Eisbrecher&quot; south of Lake Balaton, and &quot;Waldteufel&quot; south of the Drava-Danube triangle.

Geographic entities mentioned:
surface_form: Lake Velence
instance_of: Lake
countries: Hungary
coordinates: lat: 47.208333333333
lon: 18.6
From 27 January through 15 February, the Soviets conducted numerous successful counter-attacks, forcing the Germans to give up the greater portion of their territorial gains, pushing the front line back to the area between Lake Velence, the village of Csősz, and Lake Balaton.

Geographic entities mentioned:
surface_form: Lake Velence
instance_of: Lake
countries: Hungary
coordinates: lat: 47.208333333333
lon: 18.6
surface_form: Lake Balaton
instance_of: Lake
countries: Hungary
coordinates: lat: 46.85
lon: 17.72
By 1291 a splendid match was arranged for Angus Mackintosh, chief of the Clan Mackintosh, when he married Eva, the only daughter of Dougal Dal, 6th chief of the Clan Chattan, which brought Angus the lands of Glen Loy and Loch Arkaig. Angus and Eva lived on the lands of Clan Chattan at Tor Castle but they later withdrew to Rothiemurchus.

Geographic entities mentioned:
surface_form: Glen Loy
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.916666666667
lon: -5.1333333333333
surface_form: Loch Arkaig
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.971989
lon: -5.158376
Water of Tanar. Water of Tanar is a river of the Grampian Mountains of Aberdeenshire, Scotland. It flows through Glen Tanar to join the River Dee at the mouth of the glen near the Tower of Ess. It is crossed in the Glen Tanar Estate by a number of listed bridges, including a Category B listed military bridge and the Bridge of Ess and the Category C listed Porphary bridge.

Geographic entities mentioned:
surface_form: Glen Tanar
instance_of: Valley
countries: United Kingdom
coordinates: lat: 57.01667
lon: -2.9
Eilean Sùbhainn. Eilean Sùbhainn is the largest of several small islands in Loch Maree, Wester Ross, Scotland. It is the second largest freshwater island in Scotland after Inchmurrin. Lying northeast of Talladale, the island is partially forested and uninhabited. It rises to and extends to. The island is a nature reserve and includes several small lochans.

Geographic entities mentioned:
surface_form: Loch Maree
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.689722222222
lon: -5.4575
It is listed as near threatened by the IUCN Red List of Threatened Species as the population trend is downwards, especially in Mongolia, where it is nearly extinct. However, several European colonies are increasing in size and the largest colony for the species, at the Small Prespa Lake in Greece, has reached about 1,400 breeding pairs following conservation measures.

Geographic entities mentioned:
surface_form: Small Prespa Lake
instance_of: Lake
countries: Albania
Greece
coordinates: lat: 40.766111111111
lon: 21.1
The 17th-century Volga Bulgar compilation &quot;Ja'far Tarikh&quot; (a work of disputed authenticity) represents Dilyarek (Telerig) as the son of the former ruler Teles (Telets). Legacy. Telerig Nunatak, on Greenwich Island, in the South Shetland Islands, in Antarctica, is named after Telerig. In fiction. Telerikh is a major character in Harry Turtledove's &quot;Islands in the Sea&quot; (1989).

Geographic entities mentioned:
surface_form: Telerig Nunatak
instance_of: Mountain
coordinates: lat: -62.493055555556
lon: -59.925833333333
It is located in the Arica and Parinacota Region of Chile and the Oruro Department of Bolivia (in Sabaya Province, Sabaya Municipality, Julo Canton). Pukintika lies to the north of the Salar de Surire, east beside Arintika volcano which is younger than Pukintika. Pukintika also features a crater lake with a surface area of. Deposits of elemental sulfur have been found on Pukintika.

Geographic entities mentioned:
surface_form: Arintika
instance_of: Mountain
countries: Chile
coordinates: lat: -18.75
lon: -69.05
surface_form: pukintika
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -18.73333333
lon: -68.98333333
surface_form: pukintika
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -18.73333333
lon: -68.98333333
Pukintika. Pukintika (Aymara &quot;puki&quot; white soil, &quot;tika&quot; adobe, Hispanicized spellings &quot;Puguintica, Puquintica&quot;, &quot;Poquentica&quot;, &quot;Puquentica&quot;) is a volcano in the Andes, about 5,407 m (17,740 ft) high, situated in the Cordillera Occidental on the border of Bolivia and Chile.

Geographic entities mentioned:
surface_form: poquentica
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -18.73333333
lon: -68.98333333
surface_form: pukintika
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -18.73333333
lon: -68.98333333
surface_form: puquintica
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -18.73333333
lon: -68.98333333
Pukintika. Pukintika (Aymara &quot;puki&quot; white soil, &quot;tika&quot; adobe, Hispanicized spellings &quot;Puguintica, Puquintica&quot;, &quot;Poquentica&quot;, &quot;Puquentica&quot;) is a volcano in the Andes, about 5,407 m (17,740 ft) high, situated in the Cordillera Occidental on the border of Bolivia and Chile.

Geographic entities mentioned:
surface_form: pukintika
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -18.73333333
lon: -68.98333333
It is located in the Arica and Parinacota Region of Chile and the Oruro Department of Bolivia (in Sabaya Province, Sabaya Municipality, Julo Canton). Pukintika lies to the north of the Salar de Surire, east beside Arintika volcano which is younger than Pukintika. Pukintika also features a crater lake with a surface area of. Deposits of elemental sulfur have been found on Pukintika.

Geographic entities mentioned:
surface_form: pukintika
instance_of: Mountain
countries: Chile
Bolivia
coordinates: lat: -18.73333333
lon: -68.98333333
The university's science-intensive products have been exhibited at Russian and foreign exhibitions in Paris, Brussels, and Milan. KubSU possesses facilities for conducting scientific experiments; laboratories and testing grounds in the area of Gelendzhik and the Lago-Naki plateau provide students with the opportunity to carry out scientific experiments and field studies. Faculty.

Geographic entities mentioned:
surface_form: Lago-Naki plateau
instance_of: Plateau
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 44.0259
lon: 39.9044
Hohe Gaisl. Hohe Gaisl (&quot;Croda Rossa d'Ampezzo&quot; in Italian), (3,146m) is a mountain in the northern Dolomites, on the border of South Tyrol and Veneto, in northern Italy, located between the Braies Valley and the Val di Landro. It lies as an imposing and prominent mountain, dominating the valleys underneath it.

Geographic entities mentioned:
surface_form: hohe gaisl
instance_of: Mountain
countries: Italy
coordinates: lat: 46.6333
lon: 12.1333
Hohe Gaisl. Hohe Gaisl (&quot;Croda Rossa d'Ampezzo&quot; in Italian), (3,146m) is a mountain in the northern Dolomites, on the border of South Tyrol and Veneto, in northern Italy, located between the Braies Valley and the Val di Landro. It lies as an imposing and prominent mountain, dominating the valleys underneath it.

Geographic entities mentioned:
surface_form: hohe gaisl
instance_of: Mountain
countries: Italy
coordinates: lat: 46.6333
lon: 12.1333
surface_form: croda rossa
instance_of: Mountain
countries: Italy
coordinates: lat: 46.6333
lon: 12.1333
surface_form: val di landro
instance_of: Valley
countries: Italy
coordinates: lat: 46.656944444444
lon: 12.225833333333
surface_form: croda rossa
instance_of: Mountain
countries: Italy
coordinates: lat: 46.640952777778
lon: 12.375238888889
It was discovered by Charles Doolittle Walcott from the Burgess Shale in the mountains of British Columbia, Canada. Walcott reported the specimen with taxonomic description in 1911. He used the series of transverse body segments as a feature of annelid worms and classified it as a polychaete worm. He gave the name after Pika Peak, a mountain in Alberta, Canada.

Geographic entities mentioned:
surface_form: Pika Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4963889
lon: -116.1066667
The northern part of the municipality is considered to be within the rainy western mountains. Barrio Anón is home to Cerro Maravilla, a peak that at is Puerto Rico's fourth highest peak. Nineteen barrios comprise the rural areas of the municipality, and the topology of their lands varies from flatlands to hills to steep mountain slopes.

Geographic entities mentioned:
surface_form: Cerro Maravilla
instance_of: Mountain
countries: United States
coordinates: lat: 18.1531
lon: -66.5542
There is a seismic detector that the University of Puerto Rico, Mayagüez Campus, has placed in Barrio Cerrillos. Land features. Elevations include Cerro de Punta at, the highest in Puerto Rico, located in Barrio Anón in the territory of the municipality of Ponce. Mount Jayuya, at is located on the boundary between Barrio Anón and Barrio Saliente in Jayuya.

Geographic entities mentioned:
surface_form: Cerro de Punta
instance_of: Mountain
countries: United States
coordinates: lat: 18.1725
lon: -66.591944444444
Mount Jayuya, at is located on the boundary between Barrio Anón and Barrio Saliente in Jayuya. Cerro Maravilla, at nearly above sea level, is located to the east of Barrio Anón. There are many other mountains at lower elevations in the municipality, such as the Montes Llanos ridge and Mount Diablo, at and Mount Marueño, at, and Pinto Peak, among others.

Geographic entities mentioned:
surface_form: Cerro Maravilla
instance_of: Mountain
countries: United States
coordinates: lat: 18.1531
lon: -66.5542
The Cerrillos State Forest is also located in the municipality of Ponce. Coastal geographic features in Ponce include Bahía de Ponce, Caleta de Cabullones (Cabullones Cove), and five cays: Jueyes, Ratones, Cardona, Gatas, and Isla del Frio. Caja de Muertos Island and Morrillito islet are located at the boundary between Ponce and Juana Díaz.

Geographic entities mentioned:
surface_form: Bahía de Ponce
instance_of: Body of water
countries: United States
coordinates: lat: 17.973888888889
lon: -66.633333333333
The tetraethers help &quot;Sulfolobus&quot; species survive extreme acid as well as high temperature. Ecology. &quot;S. solfataricus&quot; has been found in different areas including Yellowstone National Park, Mount St. Helens, Iceland, Italy, and Russia to name a few. &quot;Sulfolobus&quot; is located almost wherever there is volcanic activity.

Geographic entities mentioned:
surface_form: Mount St. Helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
Yana Urqu (Huancavelica). Yana Urqu (Quechua &quot;yana&quot; black, &quot;urqu&quot; mountain, &quot;black mountain&quot;, hispanicized spelling &quot;Yana Orjo&quot;) is a mountain in the Chunta mountain range in the Andes of Peru, about high. It is located in the Huancavelica Region, Huancavelica Province, Huacocolpa District. Yana Urqu lies northwest of Inqhana and northeast of Wayra Q'asa.

Geographic entities mentioned:
surface_form: Inqhana
instance_of: Mountain
countries: Peru
coordinates: lat: -13.09916667
lon: -74.98777778
surface_form: wayra q'asa
instance_of: Mountain
countries: Peru
coordinates: lat: -13.0894
lon: -75.0417
Yana Urqu (Huancavelica). Yana Urqu (Quechua &quot;yana&quot; black, &quot;urqu&quot; mountain, &quot;black mountain&quot;, hispanicized spelling &quot;Yana Orjo&quot;) is a mountain in the Chunta mountain range in the Andes of Peru, about high. It is located in the Huancavelica Region, Huancavelica Province, Huacocolpa District. Yana Urqu lies northwest of Inqhana and northeast of Wayra Q'asa.

Geographic entities mentioned:
surface_form: yana urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -13.64027778
lon: -70.79055556
surface_form: yana urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -13.7411
lon: -70.9597
surface_form: yana urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -13.7206
lon: -70.98
surface_form: yana urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -13.654444
lon: -70.754722
surface_form: yana urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -13.27333333
lon: -72.305
surface_form: yana urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -13.073888888889
lon: -75.011388888889
surface_form: yana urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -13.085277777778
lon: -74.978055555556
surface_form: yana urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -13.7644
lon: -71.4506
surface_form: yana urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -12.37916667
lon: -75.70944444
surface_form: yana urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -12.535555555556
lon: -74.612222222222
surface_form: yana urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -14.41388889
lon: -71.22972222
surface_form: yana urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -14.5464
lon: -72.5772
surface_form: yana urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -12.33416667
lon: -75.71861111
surface_form: yana urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -14.29861111
lon: -69.77
surface_form: yana urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -13.1161
lon: -75.0417
surface_form: yana urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -13.6828
lon: -70.9667
surface_form: yana urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -11.31777778
lon: -75.64083333
Yana Urqu (Huancavelica). Yana Urqu (Quechua &quot;yana&quot; black, &quot;urqu&quot; mountain, &quot;black mountain&quot;, hispanicized spelling &quot;Yana Orjo&quot;) is a mountain in the Chunta mountain range in the Andes of Peru, about high. It is located in the Huancavelica Region, Huancavelica Province, Huacocolpa District. Yana Urqu lies northwest of Inqhana and northeast of Wayra Q'asa.

Geographic entities mentioned:
surface_form: yana urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -13.64027778
lon: -70.79055556
surface_form: yana urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -13.7411
lon: -70.9597
surface_form: yana urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -13.7206
lon: -70.98
surface_form: yana urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -13.654444
lon: -70.754722
surface_form: yana urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -13.27333333
lon: -72.305
surface_form: yana urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -13.073888888889
lon: -75.011388888889
surface_form: yana orjo
instance_of: Mountain
countries: Peru
coordinates: lat: -13.073888888889
lon: -75.011388888889
surface_form: yana urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -13.085277777778
lon: -74.978055555556
surface_form: yana urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -13.7644
lon: -71.4506
surface_form: chunta
instance_of: Mountain
countries: Peru
coordinates: lat: -11.4964
lon: -76.3772
surface_form: yana urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -12.37916667
lon: -75.70944444
surface_form: yana orjo
instance_of: Mountain
countries: Peru
coordinates: lat: -12.535555555556
lon: -74.612222222222
surface_form: yana urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -12.535555555556
lon: -74.612222222222
surface_form: yana urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -14.41388889
lon: -71.22972222
surface_form: yana urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -14.5464
lon: -72.5772
surface_form: yana urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -12.33416667
lon: -75.71861111
surface_form: chunta
instance_of: Mountain
countries: Peru
coordinates: lat: -14.7836
lon: -72.5717
surface_form: chunta
instance_of: Mountain
countries: Peru
coordinates: lat: -14.4222
lon: -73.8572
surface_form: yana urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -14.29861111
lon: -69.77
surface_form: yana orjo
instance_of: Mountain
countries: Peru
coordinates: lat: -13.1161
lon: -75.0417
surface_form: yana urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -13.1161
lon: -75.0417
surface_form: yana urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -13.6828
lon: -70.9667
surface_form: yana urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -11.31777778
lon: -75.64083333
Some of these habitats can be rather extreme; the only natural habitat of the Devils Hole pupfish (&quot;Cyprinodon diabolis&quot;) is Devils Hole: a cavern at least deep, branching out from a small opening at the surface, approximately by wide. Some specialized forms live in temporary ponds and flood plains, and typically have a much shorter lifespan.

Geographic entities mentioned:
surface_form: Devils Hole
instance_of: Lake
countries: United States
coordinates: lat: 36.425233333333
lon: -116.29087222222
Diet. Killifish feed primarily on aquatic arthropods such as insect (mosquito) larvae, aquatic crustaceans and worms. Some species of &quot;Orestias&quot; from Lake Titicaca are planktonic filter feeders. Others, such as &quot;Cynolebias&quot; and &quot;Megalebias&quot; species and &quot;Nothobranchius ocellatus&quot; are predatory and feed mainly on other fish.

Geographic entities mentioned:
surface_form: Lake Titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
Ole Bremseth. Ole Bremseth (born 2 January 1961) is a Norwegian former ski jumper. Career. At the 1982 FIS Nordic World Ski Championships in Oslo, Bremseth won a bronze medal in the individual normal hill and a gold medal in the team large hill. He has six World Cup victories (all in 1982) with the first one in Lahti and the final one in Planica.

Geographic entities mentioned:
surface_form: Planica
instance_of: Valley
countries: Slovenia
coordinates: lat: 46.476944444444
lon: 13.722222222222
Angara. The Angara (;) or Angar (мүрэн) is a major river in Siberia, which traces a course through Russia's Irkutsk Oblast and Krasnoyarsk Krai. It drains out of Lake Baikal and is the headwater tributary of the Yenisey. It is long, and has a drainage basin of. It was formerly known as the Lower or Nizhnyaya Angara (distinguishing it from the Upper Angara).

Geographic entities mentioned:
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
Unlike Buick, which was noted for its overhead valve engine, the Marquette had a flathead six-cylinder engine based on Oldsmobile's. A prominent selling point was its fine engineering and craftsmanship; its engineers remarked that one could drive it at without damaging the engine, and one was driven from Death Valley to Pikes Peak without any issues.

Geographic entities mentioned:
surface_form: Death Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.45693888888889
lon: -116.86528055555556
surface_form: Pikes Peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.840555555556
lon: -105.04416666667
Traditional origins. The name Macnab is derived from the Scottish Gaelic &quot;Mac An Aba&quot;, which means &quot;child of the abbot&quot;. According to tradition the progenitor of the clan was &quot;Abraruadh&quot; who was the Abbot of Glen Dochart and Strathearn. Abraruadh was allegedly a younger son of Kenneth MacAlpin, the first king of Scots. (See: Siol Alpin).

Geographic entities mentioned:
surface_form: Glen Dochart
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.417
lon: -4.433
surface_form: Strathearn
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.3325
lon: -3.6825
Mount Apoi. is located in the Hidaka Mountains, Hokkaidō, Japan. It is near the town of Samani. It is well known for hosting a large number of plants that are found only on Hokkaidō, such as. The mountain is made from ultramafic rock of unknown age. Mt. Apoi Geopark. Mount Apoi Geopark is a geopark covering whole territory of Samani. Mt.

Geographic entities mentioned:
surface_form: mount apoi
instance_of: Mountain
countries: Japan
coordinates: lat: 42.107777777778
lon: 143.02555555556
surface_form: apoi
instance_of: Mountain
countries: Japan
coordinates: lat: 42.107777777778
lon: 143.02555555556
The mountain is made from ultramafic rock of unknown age. Mt. Apoi Geopark. Mount Apoi Geopark is a geopark covering whole territory of Samani. Mt. Apoi Geopark is a geological area where visitors can learn about and enjoy the valuable geological heritage and the rich natural environment as well as the history and culture of Samani.

Geographic entities mentioned:
surface_form: mount apoi
instance_of: Mountain
countries: Japan
coordinates: lat: 42.107777777778
lon: 143.02555555556
surface_form: apoi
instance_of: Mountain
countries: Japan
coordinates: lat: 42.107777777778
lon: 143.02555555556
Mount Apoi. is located in the Hidaka Mountains, Hokkaidō, Japan. It is near the town of Samani. It is well known for hosting a large number of plants that are found only on Hokkaidō, such as. The mountain is made from ultramafic rock of unknown age. Mt. Apoi Geopark. Mount Apoi Geopark is a geopark covering whole territory of Samani. Mt.

Geographic entities mentioned:
surface_form: apoi
instance_of: Mountain
countries: Japan
coordinates: lat: 42.107777777778
lon: 143.02555555556
The mountain is made from ultramafic rock of unknown age. Mt. Apoi Geopark. Mount Apoi Geopark is a geopark covering whole territory of Samani. Mt. Apoi Geopark is a geological area where visitors can learn about and enjoy the valuable geological heritage and the rich natural environment as well as the history and culture of Samani.

Geographic entities mentioned:
surface_form: apoi
instance_of: Mountain
countries: Japan
coordinates: lat: 42.107777777778
lon: 143.02555555556
The town also has a long history and a rich culture based on its development as a trading hub thanks to the favorable natural harbor created by its unusual coastal terrain. The Mt. Apoi Geopark was certified as a Japanese Geopark in 2008, and a UNESCO Global Geopark in 2015.

Geographic entities mentioned:
surface_form: apoi
instance_of: Mountain
countries: Japan
coordinates: lat: 42.107777777778
lon: 143.02555555556
Pima Butte. Pima Butte () is a mountain summit in Pinal County, Arizona eight miles north of present-day Maricopa, Arizona. Pima Butte rises to above sea level. As a significant landmark in the Gila Valley it was near the site of the 1857 Battle of Pima Butte, to which it gave its name.

Geographic entities mentioned:
surface_form: gila valley
instance_of: Valley
countries: United States
coordinates: lat: 33.18339
lon: -110.21731
surface_form: battle
instance_of: Watercourse
countries: United States
coordinates: lat: 44.9266
lon: -93.0291
surface_form: pima butte
instance_of: Mountain
countries: United States
coordinates: lat: 33.1467
lon: -112.023
Pima Butte. Pima Butte () is a mountain summit in Pinal County, Arizona eight miles north of present-day Maricopa, Arizona. Pima Butte rises to above sea level. As a significant landmark in the Gila Valley it was near the site of the 1857 Battle of Pima Butte, to which it gave its name.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: pima butte
instance_of: Mountain
countries: United States
coordinates: lat: 33.1467
lon: -112.023
Pima Butte. Pima Butte () is a mountain summit in Pinal County, Arizona eight miles north of present-day Maricopa, Arizona. Pima Butte rises to above sea level. As a significant landmark in the Gila Valley it was near the site of the 1857 Battle of Pima Butte, to which it gave its name.

Geographic entities mentioned:
surface_form: pima butte
instance_of: Mountain
countries: United States
coordinates: lat: 33.1467
lon: -112.023
Most of the infrastructure present in the national park dates from public work projects enacted during the Great Depression. Alternative service camps for conscientious objectors were set up in Banff during World War II, with camps at Lake Louise, Stoney Creek, and Healy Creek. These camps were largely populated by Mennonites from Saskatchewan. Winter tourism.

Geographic entities mentioned:
surface_form: Healy Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 51.13332
lon: -115.70211
Lake Louise. Lake Louise, a hamlet northwest of the town of Banff, is home to the landmark Chateau Lake Louise at the edge of Lake Louise. Located from Lake Louise, Moraine Lake provides a scenic vista of the Valley of the Ten Peaks. This scene is on the back of the Canadian $20 bill in the 1969–1979 (&quot;Scenes of Canada&quot;) series. The Lake Louise Mountain Resort is also near the village.

Geographic entities mentioned:
surface_form: Moraine Lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
surface_form: Valley of the Ten Peaks
instance_of: Valley
countries: Canada
coordinates: lat: 51.3494444
lon: -116.1597222
Well west of the park, the Western Ranges of the Rockies pass through Yoho and Kootenay National Parks. Though the tallest peak entirely within the park is Mount Forbes at, Mount Assiniboine on the Banff-Mount Assiniboine Provincial Park border is slightly higher at. The Canadian Rockies are composed of sedimentary rock, including shale, sandstone, dolomite and limestone.

Geographic entities mentioned:
surface_form: Mount Forbes
instance_of: Mountain
countries: Canada
coordinates: lat: 51.859722222222224
lon: -116.93166666666667
surface_form: Mount Assiniboine
instance_of: Mountain
countries: Canada
coordinates: lat: 50.86972222222222
lon: -115.6511111111111
This leads to dip slope landforms, with generally steeper east and north faces, and trellis drainage, where rivers and old glacial valleys followed the weaker layers in the rocks as they were relatively easily weathered and eroded. Classic examples are found at the Banff townsite proper: Mount Rundle is a classic dip slope mountain.

Geographic entities mentioned:
surface_form: Mount Rundle
instance_of: Mountain
countries: Canada
coordinates: lat: 51.1242
lon: -115.47
Classic examples are found at the Banff townsite proper: Mount Rundle is a classic dip slope mountain. Just to the north of the Banff townsite, Castle Mountain is composed of numerous Cambrian age rock formations. The uppermost section of the peak consists of relatively harder dolomite from the Eldon Formation.

Geographic entities mentioned:
surface_form: Castle Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.29972222222222
lon: -115.9225
Below that lies the less dense shales of the Stephen Formation and the lowest exposed cliffs are limestones of the Cathedral Formation. Dogtooth mountains, such as Mount Louis, exhibit sharp, jagged slopes. The Sawback Range, which consists of nearly vertical dipping sedimentary layers, has been eroded by cross gullies.

Geographic entities mentioned:
surface_form: Mount Louis
instance_of: Mountain
countries: Canada
coordinates: lat: 51.215
lon: -115.68
Located on the eastern side of the Continental Divide, Banff National Park receives of precipitation annually. This is considerably less than in Yoho National Park on the western side of the divide in British Columbia, where (1971-1990 normals) is received at Wapta Lake and approximately at Boulder Creek annually. Being influenced by altitude, snowfall is also greater at higher elevations.

Geographic entities mentioned:
surface_form: Wapta Lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.4392
lon: -116.35
Environment. Since the 19th century, humans have impacted Banff's environment through introduction of non-native species, controls on other species, and development in the Bow Valley, among other human activities. Bison once lived in the valleys of Banff and were hunted by indigenous people, but the last bison were killed off in 1850s.

Geographic entities mentioned:
surface_form: Bow Valley
instance_of: Valley
countries: Canada
coordinates: lat: 51.1671
lon: -115.48
Vesletind Peak. Vesletind Peak () is a small peak 3 nautical miles (6 km) east-southeast of Aurho Peak on the Ahlmann Ridge in Queen Maud Land. It was mapped by Norwegian cartographers from surveys and air photos by Norwegian-British-Swedish Antarctic Expedition (NBSAE) (1949–52) and named Vesletind, meaning &quot;little peak.&quot;

Geographic entities mentioned:
surface_form: small
instance_of: Mountain
coordinates: lat: -70.5
lon: 64.7
surface_form: vesletind peak
instance_of: Mountain
coordinates: lat: -72.1667
lon: -3.03333
Vesletind Peak. Vesletind Peak () is a small peak 3 nautical miles (6 km) east-southeast of Aurho Peak on the Ahlmann Ridge in Queen Maud Land. It was mapped by Norwegian cartographers from surveys and air photos by Norwegian-British-Swedish Antarctic Expedition (NBSAE) (1949–52) and named Vesletind, meaning &quot;little peak.&quot;

Geographic entities mentioned:
surface_form: vesletind peak
instance_of: Mountain
coordinates: lat: -72.1667
lon: -3.03333
Vesletind Peak. Vesletind Peak () is a small peak 3 nautical miles (6 km) east-southeast of Aurho Peak on the Ahlmann Ridge in Queen Maud Land. It was mapped by Norwegian cartographers from surveys and air photos by Norwegian-British-Swedish Antarctic Expedition (NBSAE) (1949–52) and named Vesletind, meaning &quot;little peak.&quot;

Geographic entities mentioned:
surface_form: vesletind
instance_of: Mountain
coordinates: lat: -72.1667
lon: -3.03333
Powder Horn Mountain. Powder Horn Mountain (PHM) is a privately owned, gated residential community on 1,250 wooded acres in Triplett, Watauga County, North Carolina, located within the Blue Ridge Mountains. In the 1970s, developer Bob Horne was inspired to build a tranquil mountain community that originally included a golf course and riding stables with trails in nearby Wilkes County.

Geographic entities mentioned:
surface_form: powder horn mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.1751
lon: -81.5265
After undergoing bankruptcy and foreclosure, the development was divided and various areas sold separately. In order to save the community's existing homes from foreclosures, a group of property owners founded a partnership called the Laurel Creek Group and purchased the at-risk homes which enabled the creation of the Powder Horn Mountain Property Owners Association (PHM POA).

Geographic entities mentioned:
surface_form: powder horn mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.1751
lon: -81.5265
Recent years have seen the PHM community resuming steady but slow growth. The PHM POA annexed more than formerly known as &quot;Brightwood IV&quot; into Powder Horn Mountain in 2005, an area now known as Powder Horn Estates. There is an unrelated Powder Horn Golf Community in Colorado. See also. Horne's

Geographic entities mentioned:
surface_form: powder horn mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.1751
lon: -81.5265
1902 eruption of Mount Pelée. The 1902 eruption of Mount Pelée was a volcanic eruption on the island of Martinique in the Lesser Antilles Volcanic Arc of the eastern Caribbean, which was one of the deadliest eruptions in recorded history. Eruptive activity began on 23 April as a series of phreatic eruptions from the summit of Mount Pelée.

Geographic entities mentioned:
surface_form: Mount Pelée
instance_of: Mountain
countries: France
coordinates: lat: 14.813055555556
lon: -61.165555555556
Svanvik, Finnmark. Svanvik (or) is a village in Sør-Varanger Municipality in Finnmark county, Norway. It is located south of the town of Kirkenes and its on the north bank of Svanevatn, a lake in the Paatsjoki river basin. The village had a population of 250 in 2019. Svanvik Church, Pasvik Folk College, and Øvre Pasvik National Park are located in Svanvik.

Geographic entities mentioned:
surface_form: Svanevatn
instance_of: Lake
countries: Norway
Russia
Russian Empire
Soviet Union
coordinates: lat: 69.433181
lon: 30.027275
surface_form: Paatsjoki
instance_of: Watercourse
countries: Russia
Finland
Norway
Russian Empire
Soviet Union
coordinates: lat: 69.68135
lon: 30.11035
Mount Goodman. we96b9ggyokgox18ter8hkdhcis" xml:space="preserve">#redirect Mount Goodman

Geographic entities mentioned:
surface_form: goodman
instance_of: Mountain
coordinates: lat: -75.2333
lon: -72.2333
surface_form: mount goodman
instance_of: Mountain
coordinates: lat: -75.2333
lon: -72.2333